text: is the normal stress on the slip plane and

text: is the normal stress on the slip plane and

answers: NDQ_003351

answers: elastic stress

answers: NDQ_003352

answers: is more likely to crack

answers: NDQ_003353

answers: voids to form

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: shrink.

answers: NDQ_003357

answers: slip is the stress on the slip plane.

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: is pushed together

answers: NDQ_003360

answers: glaciers.

answers: NDQ_003362

answers: The San Andreas Fault is a tectonic fault.

answers: NDQ_003363

answers: tectonic plates

answers: NDQ_003371

answers: the normal stress on the slip plane

answers: NDQ_003373

answers: It is subjected to a constant amount of pressure.

answers: NDQ_003376

answers: compressive forces

answers: NDQ_003378

answers: the normal stress on the slip plane

answers: NDQ_003379

answers: The normal stress on the slip plane is

answers: NDQ_003380

answers: Any force applied to rock is a stress.

answers: NDQ_003381

answers: The normal stress on the slip plane is the stress on the slip plane.

answers: NDQ_003382

answers: Compression is the normal stress on the slip plane and

answers: NDQ_003383

answers: None of the above choices .

answers: NDQ_003384

answers: A syncline is a fold that arches upward.

answers: NDQ_003385

answers: Fault zone is a zone where faults are clustered

answers: NDQ_003386

answers: the normal stress on the slip plane

answers: NDQ_003387

answers: The normal stress is on the slip plane.

answers: NDQ_003388

answers: the normal stress on the slip plane

answers: NDQ_003389

answers: The process of folding creates mountains.

answers: NDQ_003390

answers: a sloping fault

answers: NDQ_003391

answers: is a block of rock

answers: NDQ_003392

answers: a sloping fault

answers: NDQ_003393

answers: is a block of rock that is above the slip plane

answers: NDQ_003394

answers: a fault with a fault plane that is not vertical

answers: NDQ_003395

answers: is a vertical fault

answers: NDQ_003396

answers: is the normal stress on the slip plane

answer_match: lowercase, stopped, stemmed, removed trailing period, fuzz > 0.8 / true-false special handling

orig_prompt_class: QuestionPromptWithChoices

prompt_style: context: question:

answers: NDQ_003351

answers: slip plane

answers: NDQ_003352

answers: slip plane

answers: NDQ_003353

answers: normal stress on the slip plane

answers: NDQ_003354

answers: normal stress on the slip plane

answers: NDQ_003355

answers: is the normal stress on the slip plane

answers: NDQ_003356

answers: normal stress on the slip plane

answers: NDQ_003357

answers: normal stress on the slip plane

answers: NDQ_003358

answers: slip plane

answers: NDQ_003359

answers: normal stress on the slip plane

answers: NDQ_003360

answers: normal stress on the slip plane

answers: NDQ_003362

answers: is the normal stress on the slip plane

answers: NDQ_003363

answers: normal stress on the slip plane

answers: NDQ_003371

answers: normal stress on the slip plane

answers: NDQ_003373

answers: normal stress on the slip plane

answers: NDQ_003376

answers: normal stress on the slip plane

answers: NDQ_003378

answers: slip plane

answers: NDQ_003379

answers: normal stress on the slip plane

answers: NDQ_003380

answers: normal stress on the slip plane

answers: NDQ_003381

answers: normal stress on the slip plane

answers: NDQ_003382

answers: slip plane

answers: NDQ_003383

answers: normal stress on the slip plane

answers: NDQ_003384

answers: normal stress on the slip plane

answers: NDQ_003385

answers: normal stress on the slip plane

answers: NDQ_003386

answers: normal stress on the slip plane

answers: NDQ_003387

answers: slip plane

answers: NDQ_003388

answers: normal stress on the slip plane

answers: NDQ_003389

answers: normal stress on the slip plane

answers: NDQ_003390

answers: normal stress on the slip plane

answers: NDQ_003391

answers: normal stress on the slip plane

answers: NDQ_003392

answers: normal stress on the slip plane

answers: NDQ_003393

answers: normal stress on the slip plane

answers: NDQ_003394

answers: normal stress on the slip plane

answers: NDQ_003395

answers: normal stress on the slip plane

answers: NDQ_003396

answers: normal stress on the slip plane

answer_match: lowercase, stemmed, fuzz > 0.8

text: The second main terrain type—ridged terrain—comprises bands of ridges and troughs hundreds of kilometers in extent. It bounds the cratered terrain and cuts it into polygons. Within each band, which can be up to 25 to 70 km wide, are individual ridges and troughs up to 200 km long and between 10 and 35 km apart. The bands of ridged terrain often form continuations of canyons, suggesting that they may be a modified form of the graben or the result of a different reaction of the crust to the same extensional stresses, such as brittle failure.

text: The second main terrain type—ridged terrain—comprises bands of ridges and troughs hundreds of kilometers in extent. It bounds the cratered terrain and cuts it into polygons. Within each band, which can be up to 25 to 70 km wide, are individual ridges and troughs up to 200 km long and between 10 and 35 km apart. The bands of ridged terrain often form continuations of canyons, suggesting that they may be a modified form of the graben or the result of a different reaction of the crust to the same extensional stresses, such as brittle failure.

answers: NDQ_003351

answers: brittle failure

answers: NDQ_003352

answers: brittle

answers: NDQ_003353

answers: extensional stresses

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: trough

answers: NDQ_003356

answers: brittle

answers: NDQ_003357

answers: ridges and troughs can be up to

answers: NDQ_003358

answers: trough

answers: NDQ_003359

answers: extensional stresses

answers: NDQ_003360

answers: extensional stresses

answers: NDQ_003362

answers: ridged terrain often form continuations of canyons

answers: NDQ_003363

answers: ridged terrain

answers: NDQ_003371

answers: What may be the result of a different reaction of the crust to the same extensional stresses?

answers: NDQ_003373

answers: unanswerable

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What is the result of a different reaction of the crust to the same extensional stresses?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What type of fold is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: What is the cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: normal faults or extensional stresses?

answers: NDQ_003388

answers: Which of the following is not a type of terrain: ridged terrain or strike-slip faults?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: brittle failure

answers: NDQ_003391

answers: cratered terrain

answers: NDQ_003392

answers: brittle failure

answers: NDQ_003393

answers: graben

answers: NDQ_003394

answers: brittle failure

answers: NDQ_003395

answers: brittle failure

answers: NDQ_003396

answers: brittle failure

answers: NDQ_003351

answers: brittle failure.

answers: NDQ_003352

answers: brittle failure.

answers: NDQ_003353

answers: brittle failure.

answers: NDQ_003354

answers: The second main terrain type—ridged terrain—comprises

answers: NDQ_003355

answers: graben

answers: NDQ_003356

answers: brittle failure.

answers: NDQ_003357

answers: extensional stresses,

answers: NDQ_003358

answers: type—ridged terrain—comprises

answers: NDQ_003359

answers: extensional stresses,

answers: NDQ_003360

answers: extensional stresses,

answers: NDQ_003362

answers: brittle failure.

answers: NDQ_003363

answers: brittle failure.

answers: NDQ_003371

answers: brittle failure.

answers: NDQ_003373

answers: brittle failure.

answers: NDQ_003376

answers: type—ridged terrain—comprises

answers: NDQ_003378

answers: type—ridged terrain—comprises

answers: NDQ_003379

answers: type—ridged terrain—comprises

answers: NDQ_003380

answers: stresses,

answers: NDQ_003381

answers: brittle failure.

answers: NDQ_003382

answers: brittle failure.

answers: NDQ_003383

answers: extensional stresses,

answers: NDQ_003384

answers: type—ridged terrain—comprises

answers: NDQ_003385

answers: type—ridged terrain—comprises

answers: NDQ_003386

answers: brittle failure.

answers: NDQ_003387

answers: extensional stresses,

answers: NDQ_003388

answers: brittle failure.

answers: NDQ_003389

answers: type—ridged terrain—comprises

answers: NDQ_003390

answers: brittle failure.

answers: NDQ_003391

answers: graben

answers: NDQ_003392

answers: brittle failure.

answers: NDQ_003393

answers: graben

answers: NDQ_003394

answers: brittle failure.

answers: NDQ_003395

answers: brittle failure.

answers: NDQ_003396

answers: brittle failure.

text: Further complicating this is a feature of unknown structure and origin, the Olympic-Wallowa Lineament (OWL). This is a seemingly accidental alignment of topographic features that runs roughly east-southeast from the north side of the Olympic Peninsula to the Wallowa Mountains in northeastern Oregon. It aligns with the West Coast fault and Queen Charlotte Fault system of strike-slip fault zones (similar to the San Andreas Fault in California) on the west side of Vancouver Island, but does not itself show any significant or through-going strike-slip movement. It is of interest here because the various strands of the Seattle Fault change orientation where they appear to cross the OWL, and various other features, such as the Rosedale monocline and Olympia structure, and a great many local topographical features, have parallel alignments. It may also be the original location of the Darrington—Devils Mountain Fault (the dashed line "X" at the top of the following map). The OWL appears to be a deep-seated structure over which the shallower crust of the Puget Lowland is being pushed, but this remains speculative.

text: Further complicating this is a feature of unknown structure and origin, the

entity_name: Olympic-Wallowa Lineament

text: Olympic-Wallowa Lineament

text: (OWL). This is a seemingly accidental alignment of topographic features that runs roughly east-southeast from the north side of the Olympic Peninsula to the

entity_name: Wallowa Mountains

text: Wallowa Mountains

text: in northeastern Oregon. It aligns with the West Coast fault and Queen Charlotte Fault system of

entity_name: Fault (geology)

entity_section: Strike-slip faults

text: strike-slip

text: fault zones (similar to the

entity_name: San Andreas Fault

text: San Andreas Fault

text: in California) on the west side of

entity_name: Vancouver Island

text: Vancouver Island

text: , but does not itself show any significant or through-going strike-slip movement. It is of interest here because the various strands of the Seattle Fault change orientation where they appear to cross the OWL, and various other features, such as the

entity_name: Puget Sound faults

entity_section: TF

text: Rosedale monocline

text: and Olympia structure, and a great many local topographical features, have parallel alignments. It may also be the original location of the Darrington—Devils Mountain Fault (the dashed line "X" at the top of the following map). The OWL appears to be a deep-seated structure over which the shallower crust of the Puget Lowland is being pushed, but this remains speculative.

answers: NDQ_003351

answers: strike-slip

answers: NDQ_003352

answers: moves

answers: NDQ_003353

answers: fault movement

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: monocline

answers: NDQ_003356

answers: strike

answers: NDQ_003357

answers: strike-slip movement is the movement of what?

answers: NDQ_003358

answers: fault zone

answers: NDQ_003359

answers: strikes another rock

answers: NDQ_003360

answers: West Coast fault

answers: NDQ_003362

answers: shows no significant or through-going strike-slip movement

answers: NDQ_003363

answers: San Andreas Fault

answers: NDQ_003371

answers: What may be the original location of the Darrington—Devils Mountain Fault?

answers: NDQ_003373

answers: Why would a rock be deeply buried?

answers: NDQ_003376

answers: What is the basin-and-range terrain caused by?

answers: NDQ_003378

answers: strike-slip fault zones

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What type of force applied to rock is a stress?

answers: NDQ_003381

answers: What type of stress does the Olympic-Wallowa Lineament (OWL) experience?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What is the Rosedale monocline?

answers: NDQ_003385

answers: Fault zones

answers: NDQ_003386

answers: strike-slip fault zones

answers: NDQ_003387

answers: What are normal faults caused by?

answers: NDQ_003388

answers: What is the cause of strike-slip faults?

answers: NDQ_003389

answers: What is the process of folding that creates mountains?

answers: NDQ_003390

answers: strike-slip fault

answers: NDQ_003391

answers: Wallowa Mountains

answers: NDQ_003392

answers: strike-slip fault

answers: NDQ_003393

answers: Wallowa Mountains

answers: NDQ_003394

answers: strike-slip fault zones

answers: NDQ_003395

answers: strike-slip fault

answers: NDQ_003396

answers: strike-slip fault

answers: NDQ_003351

answers: strike-slip

answers: NDQ_003352

answers: strike-slip movement.

answers: NDQ_003353

answers: strike-slip fault zones

answers: NDQ_003354

answers: Olympic-Wallowa Lineament

answers: NDQ_003355

answers: monocline

answers: NDQ_003356

answers: strike-slip fault zones

answers: NDQ_003357

answers: strike-slip movement.

answers: NDQ_003358

answers: strike-slip fault zones

answers: NDQ_003359

answers: strike-slip

answers: NDQ_003360

answers: strike-slip fault zones

answers: NDQ_003362

answers: through-going strike-slip movement.

answers: NDQ_003363

answers: San Andreas Fault in California)

answers: NDQ_003371

answers: strike-slip fault zones

answers: NDQ_003373

answers: deep-seated structure

answers: NDQ_003376

answers: Olympic-Wallowa Lineament

answers: NDQ_003378

answers: strike-slip

answers: NDQ_003379

answers: strike-slip fault zones

answers: NDQ_003380

answers: strike-slip fault zones

answers: NDQ_003381

answers: strike-slip fault zones

answers: NDQ_003382

answers: strike-slip fault zones

answers: NDQ_003383

answers: strike-slip fault zones

answers: NDQ_003384

answers: monocline

answers: NDQ_003385

answers: strike-slip fault zones

answers: NDQ_003386

answers: strike-slip fault zones

answers: NDQ_003387

answers: strike-slip

answers: NDQ_003388

answers: strike-slip fault zones

answers: NDQ_003389

answers: strike-slip fault zones

answers: NDQ_003390

answers: Queen Charlotte Fault

answers: NDQ_003391

answers: shallower crust of the Puget Lowland

answers: NDQ_003392

answers: Queen Charlotte Fault

answers: NDQ_003393

answers: deep-seated structure

answers: NDQ_003394

answers: Queen Charlotte Fault

answers: NDQ_003395

answers: Queen Charlotte Fault

answers: NDQ_003396

answers: Queen Charlotte Fault

text: The second model (Protopangea-Paleopangea) is based on both palaeomagnetic and geological evidence and proposes that the continental crust comprised a single supercontinent from  until break-up during the Ediacaran Period after . The reconstruction is derived from the observation that palaeomagnetic poles converge to quasi-static positions for long intervals between ~2.7–2.2, 1.5–1.25, and  with only small peripheral modifications to the reconstruction. During the intervening periods, the poles conform to a unified apparent polar wander path. Because this model shows that exceptional demands on the paleomagnetic data are satisfied by prolonged quasi-integrity, it must be regarded as superseding the first model proposing multiple diverse continents, although the first phase (Protopangea) essentially incorporates Vaalbara and Kenorland of the first model. The explanation for the prolonged duration of the Protopangea-Paleopangea supercontinent appears to be that Lid Tectonics (comparable to the tectonics operating on Mars and Venus) prevailed during Precambrian times. Plate Tectonics as seen on the contemporary Earth became dominant only during the latter part of geological times.

text: The second model (Protopangea-Paleopangea) is based on both palaeomagnetic and geological evidence and proposes that the continental crust comprised a single supercontinent from  until break-up during the

entity_name: Ediacaran

text: Ediacaran

text: Period after . The

entity_name: Plate reconstruction

text: reconstruction

text: is derived from the observation that palaeomagnetic poles converge to quasi-static positions for long intervals between ~2.7–2.2, 1.5–1.25, and  with only small peripheral modifications to the reconstruction. During the intervening periods, the poles conform to a unified apparent polar wander path. Because this model shows that exceptional demands on the paleomagnetic data are satisfied by prolonged quasi-integrity, it must be regarded as superseding the first model proposing multiple diverse continents, although the first phase (Protopangea) essentially incorporates

entity_name: Vaalbara

text: Vaalbara

text: and

entity_name: Kenorland

text: Kenorland

text: of the first model. The explanation for the prolonged duration of the Protopangea-Paleopangea supercontinent appears to be that Lid Tectonics (comparable to the tectonics operating on Mars and Venus) prevailed during

entity_name: Precambrian

text: Precambrian

text: times. Plate Tectonics as seen on the contemporary Earth became dominant only during the latter part of geological times.

method: UNH-qee

method: Bert-DRMMTKS

answers: NDQ_003351

answers: Plate Tectonics

answers: NDQ_003352

answers: converge to quasi-static

answers: NDQ_003353

answers: plates to break apart

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: tectonics

answers: NDQ_003356

answers: break-up

answers: NDQ_003357

answers: 2.7–2.2, 1.5–1.25 and with only small peripheral modifications to the reconstruction

answers: NDQ_003358

answers: quasi-static

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's surface

answers: NDQ_003362

answers: multiple diverse continents

answers: NDQ_003363

answers: Precambrian times

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: Why is this model superseding the first model?

answers: NDQ_003376

answers: Plate Tectonics

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: How does this model show exceptional demands on the paleomagnetic data

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: plate tectonics

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is the area where faults are clustered called?

answers: NDQ_003386

answers: Plate Tectonics

answers: NDQ_003387

answers: What are normal faults caused by?

answers: NDQ_003388

answers: What type of stress is shear stress?

answers: NDQ_003389

answers: Plate Tectonics

answers: NDQ_003390

answers: Plate Tectonics

answers: NDQ_003391

answers: Tectonics

answers: NDQ_003392

answers: Lid Tectonics

answers: NDQ_003393

answers: Plate Tectonics

answers: NDQ_003394

answers: plate tectonics

answers: NDQ_003395

answers: plate tectonics

answers: NDQ_003396

answers: Tectonics

answers: NDQ_003351

answers: Lid Tectonics

answers: NDQ_003352

answers: Plate Tectonics

answers: NDQ_003353

answers: palaeomagnetic poles converge to quasi-static positions

answers: NDQ_003354

answers: Lid Tectonics

answers: NDQ_003355

answers: Lid Tectonics

answers: NDQ_003356

answers: quasi-static positions

answers: NDQ_003357

answers: Plate Tectonics

answers: NDQ_003358

answers: quasi-static

answers: NDQ_003359

answers: Lid Tectonics

answers: NDQ_003360

answers: Lid Tectonics

answers: NDQ_003362

answers: multiple diverse continents,

answers: NDQ_003363

answers: Precambrian

answers: NDQ_003371

answers: Lid Tectonics

answers: NDQ_003373

answers: Lid Tectonics

answers: NDQ_003376

answers: Lid Tectonics

answers: NDQ_003378

answers: polar wander path.

answers: NDQ_003379

answers: Lid Tectonics

answers: NDQ_003380

answers: Lid Tectonics

answers: NDQ_003381

answers: palaeomagnetic poles converge to quasi-static

answers: NDQ_003382

answers: palaeomagnetic poles converge to quasi-static

answers: NDQ_003383

answers: Lid Tectonics

answers: NDQ_003384

answers: Lid Tectonics

answers: NDQ_003385

answers: break-up during the Ediacaran Period

answers: NDQ_003386

answers: Plate Tectonics

answers: NDQ_003387

answers: Lid Tectonics

answers: NDQ_003388

answers: Lid Tectonics

answers: NDQ_003389

answers: Plate Tectonics

answers: NDQ_003390

answers: break-up during the Ediacaran Period

answers: NDQ_003391

answers: Plate Tectonics

answers: NDQ_003392

answers: Lid Tectonics

answers: NDQ_003393

answers: Plate Tectonics

answers: NDQ_003394

answers: Lid Tectonics

answers: NDQ_003395

answers: Plate Tectonics

answers: NDQ_003396

answers: Lid Tectonics

text: This theory views volcanism as the resultant of lithospheric processes rather than heat from the mantle rising up. Instead of heat coming up from deep in the mantle, volcanic anomalies come from a shallow source. Volcanism thus occurs where the crust is easier to break up because it has been stretched by lithospheric extension, allowing melt to reach the surface. Volcanic anomalies are created by plate tectonics such as spreading plate boundaries or subduction zones. The location of the volcanism is governed by the stress field in the plate and the amount of melt is governed by the fusibility of the mantle beneath. Plate tectonics can explain most of the volcanism on Earth.

text: This theory views volcanism as the resultant of lithospheric processes rather than heat from the mantle rising up. Instead of heat coming up from deep in the mantle, volcanic anomalies come from a shallow source. Volcanism thus occurs where the crust is easier to break up because it has been stretched by lithospheric extension, allowing

entity_name: Magma

text: melt

text: to reach the surface. Volcanic anomalies are created by plate tectonics such as spreading plate boundaries or

entity_name: Subduction

text: subduction zones

text: . The location of the volcanism is governed by the stress field in the plate and the amount of melt is governed by the fusibility of the mantle beneath. Plate tectonics can explain most of the volcanism on Earth.

answers: NDQ_003351

answers: subduction zones

answers: NDQ_003352

answers: is more likely to crack

answers: NDQ_003353

answers: volcanism

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: subduction zone

answers: NDQ_003356

answers: break up

answers: NDQ_003357

answers: heat from the mantle rises up

answers: NDQ_003358

answers: subduction zone

answers: NDQ_003359

answers: has been stretched

answers: NDQ_003360

answers: plate boundaries

answers: NDQ_003362

answers: heat from the mantle rising up

answers: NDQ_003363

answers: subduction zones

answers: NDQ_003371

answers: Which of the following is not a type of plate tectonics?

answers: NDQ_003373

answers: why is it easier to break up because it has been stretched by lithospheric extension

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What is the location of the volcanism governed by?

answers: NDQ_003381

answers: Which of the following is not a resultant of lithospheric processes?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not a type of fold that arches upward?

answers: NDQ_003385

answers: What is the term for an area where faults are clustered?

answers: NDQ_003386

answers: plate tectonics

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: normal faults or plate tectonics?

answers: NDQ_003388

answers: Which of the following is not a resultant of lithospheric processes?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: subduction zone

answers: NDQ_003391

answers: subduction zone

answers: NDQ_003392

answers: subduction zone

answers: NDQ_003393

answers: subduction zone

answers: NDQ_003394

answers: subduction zones

answers: NDQ_003395

answers: subduction zones

answers: NDQ_003396

answers: subduction zones

answers: NDQ_003351

answers: spreading plate boundaries or subduction zones.

answers: NDQ_003352

answers: stretched by lithospheric extension,

answers: NDQ_003353

answers: stretched by lithospheric extension,

answers: NDQ_003354

answers: Plate tectonics

answers: NDQ_003355

answers: subduction zones.

answers: NDQ_003356

answers: melt to reach the surface.

answers: NDQ_003357

answers: melt to reach the surface.

answers: NDQ_003358

answers: Volcanism

answers: NDQ_003359

answers: stretched by lithospheric extension,

answers: NDQ_003360

answers: plate tectonics

answers: NDQ_003362

answers: heat from the mantle rising up.

answers: NDQ_003363

answers: Plate tectonics

answers: NDQ_003371

answers: spreading plate boundaries or subduction zones.

answers: NDQ_003373

answers: stretched by lithospheric extension,

answers: NDQ_003376

answers: lithospheric extension,

answers: NDQ_003378

answers: stretched by lithospheric extension,

answers: NDQ_003379

answers: stretched by lithospheric extension,

answers: NDQ_003380

answers: stretched by lithospheric extension,

answers: NDQ_003381

answers: stretched by lithospheric extension,

answers: NDQ_003382

answers: stretched by lithospheric extension,

answers: NDQ_003383

answers: stress field in the plate

answers: NDQ_003384

answers: lithospheric extension,

answers: NDQ_003385

answers: spreading plate boundaries or subduction zones.

answers: NDQ_003386

answers: plate tectonics

answers: NDQ_003387

answers: lithospheric extension,

answers: NDQ_003388

answers: lithospheric extension,

answers: NDQ_003389

answers: plate tectonics

answers: NDQ_003390

answers: subduction zones.

answers: NDQ_003391

answers: subduction zones.

answers: NDQ_003392

answers: stretched by lithospheric extension,

answers: NDQ_003393

answers: subduction zones.

answers: NDQ_003394

answers: spreading plate boundaries or subduction zones.

answers: NDQ_003395

answers: spreading plate boundaries or subduction zones.

answers: NDQ_003396

answers: subduction zones.

text: There are several different types of stress balls that originate from many different countries. The most common type of stress ball (in America) is the “bean bag” type (commonly known as a “Hacky Sack” in Australia). The stress ball that is most common in Australia is the foam type, this type prevents stress through resistance from squeezing the ball. The third type of stress ball is the Chinese form. These are not like the others as these are not squeezable, they are solid, they usually come in pairs so you can roll them together to make a soothing a sound and a smooth sensation feeling in your hands.

text: There are several different types of stress balls that originate from many different countries. The most common type of stress ball (in America) is the “bean bag” type (commonly known as a “Hacky Sack” in Australia). The stress ball that is most common in Australia is the foam type, this type prevents stress through resistance from squeezing the ball. The third type of stress ball is the Chinese form. These are not like the others as these are not squeezable, they are solid, they usually come in pairs so you can roll them together to make a soothing a sound and a smooth sensation feeling in your hands.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: is likely to crack

answers: NDQ_003353

answers: rocks to break apart

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fold that bends downward

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: if a stress ball is squeezable, it is

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: stress balls are not squeezable

answers: NDQ_003363

answers: the same time

answers: NDQ_003371

answers: Which of the following is not a type of stress ball?

answers: NDQ_003373

answers: How would you describe compressive stresses?

answers: NDQ_003376

answers: basin-and-range

answers: NDQ_003378

answers: What type of stress ball is the Chinese form?

answers: NDQ_003379

answers: The dip of the fault plane is vertical

answers: NDQ_003380

answers: What is the most common type of stress ball?

answers: NDQ_003381

answers: What is the most common type of stress ball?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What type of stress ball is the Chinese form?

answers: NDQ_003386

answers: What is the most common type of stress ball in America?

answers: NDQ_003387

answers: Which of the following is not a type of stress ball?

answers: NDQ_003388

answers: What type of stress ball is the Chinese form?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: a fault

answers: NDQ_003391

answers: dip-slip fault

answers: NDQ_003392

answers: sloping

answers: NDQ_003393

answers: dip-slip fault

answers: NDQ_003394

answers: vertical fault

answers: NDQ_003395

answers: vertical fault plane

answers: NDQ_003396

answers: NDQ_003351

answers: “bean bag”

answers: NDQ_003352

answers: ball.

answers: NDQ_003353

answers: squeezing the ball.

answers: NDQ_003354

answers: Chinese

answers: NDQ_003355

answers: “Hacky Sack”

answers: NDQ_003356

answers: squeezable,

answers: NDQ_003357

answers: stress through resistance from squeezing the ball.

answers: NDQ_003358

answers: “Hacky Sack”

answers: NDQ_003359

answers: resistance from squeezing the ball.

answers: NDQ_003360

answers: Chinese

answers: NDQ_003362

answers: There are several different types of stress balls

answers: NDQ_003363

answers: Chinese form.

answers: NDQ_003371

answers: There are several different types of stress balls

answers: NDQ_003373

answers: There are several different types of stress balls

answers: NDQ_003376

answers: Chinese

answers: NDQ_003378

answers: Chinese

answers: NDQ_003379

answers: Chinese

answers: NDQ_003380

answers: stress balls

answers: NDQ_003381

answers: foam

answers: NDQ_003382

answers: “bean bag”

answers: NDQ_003383

answers: stress balls

answers: NDQ_003384

answers: Chinese

answers: NDQ_003385

answers: “Hacky Sack”

answers: NDQ_003386

answers: Chinese

answers: NDQ_003387

answers: Chinese

answers: NDQ_003388

answers: Chinese

answers: NDQ_003389

answers: squeezable,

answers: NDQ_003390

answers: “Hacky Sack”

answers: NDQ_003391

answers: “bean bag”

answers: NDQ_003392

answers: “Hacky Sack” in Australia).

answers: NDQ_003393

answers: “bean bag”

answers: NDQ_003394

answers: squeezable,

answers: NDQ_003395

answers: “Hacky Sack”

answers: NDQ_003396

answers: “Hacky Sack”

text: However, nearly all metal prices have been declining over time in inflation adjusted terms, because of a number of false assumptions in the above. Firstly, metal resources are non-renewable, but on a world scale, largely inexhaustible.  This is because they are present throughout the earth's crust on a vast scale, far exceeding human demand on all time scales. Metal ores however, are only extracted in those areas where nature has concentrated the metal in the crust to a level whereby it is locally economic to extract. This also depends on the available technology for both finding the metal ores as well as extracting them, which is constantly changing. If the technology or demand changes, vast amounts of metal previously ignored can become economically extractable. This is why Ricardo's simplistic notion that the price of a mineral resource should increase over time has in fact turned out to be the opposite, nearly all metal ores have decreased in inflation adjusted prices since well before the early 20th century. The main reason he was wrong is that he assumed that metals are exhaustible on a world scale, and he also misunderstood the effect of globally competing markets; in human terms the amount of metal in the earth's crust is essentially limitless. It is only in localized areas that metal ores can become depleted, as these local areas compete with extraction costs of resources elsewhere, which does have ramifications for the sustainability of local economies.

answers: NDQ_003351

answers: non-renewable

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: igneous rocks to form

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: increase in price

answers: NDQ_003357

answers: metal ores are only extracted in those areas where nature has concentrated the metal in the crust

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: metal resources are non-renewable

answers: NDQ_003363

answers: Earth's crust

answers: NDQ_003371

answers: Which of the following is not an example of a thrust fault?

answers: NDQ_003373

answers: yes

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: What is the term for the amount the ground moves in an earthquake?

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What is the main reason Ricardo was wrong?

answers: NDQ_003381

answers: What happens to rock when confining stress occurs?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: yes

answers: NDQ_003387

answers: Which of the following is not the cause of normal faults?

answers: NDQ_003388

answers: Which of the following is not a type of strike-slip fault?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: dip-slip fault

answers: NDQ_003392

answers: unanswerable

answers: NDQ_003393

answers: dip-slip fault plane

answers: NDQ_003394

answers: vertical fault

answers: NDQ_003395

answers: a vertical fault plane

answers: NDQ_003396

answers: NDQ_003351

answers: globally competing markets;

answers: NDQ_003352

answers: metal ores can become depleted,

answers: NDQ_003353

answers: largely inexhaustible.

answers: NDQ_003354

answers: largely inexhaustible.

answers: NDQ_003355

answers: nearly all metal prices have been declining over time in inflation adjusted terms,

answers: NDQ_003356

answers: localized areas that metal ores can become depleted,

answers: NDQ_003357

answers: he assumed that metals are exhaustible on a world scale,

answers: NDQ_003358

answers: localized areas

answers: NDQ_003359

answers: localized areas that metal ores can become depleted,

answers: NDQ_003360

answers: nature has concentrated the metal in the crust

answers: NDQ_003362

answers: largely inexhaustible.

answers: NDQ_003363

answers: early 20th century.

answers: NDQ_003371

answers: largely inexhaustible.

answers: NDQ_003373

answers: largely inexhaustible.

answers: NDQ_003376

answers: largely inexhaustible.

answers: NDQ_003378

answers: largely inexhaustible.

answers: NDQ_003379

answers: largely inexhaustible.

answers: NDQ_003380

answers: largely inexhaustible.

answers: NDQ_003381

answers: localized areas

answers: NDQ_003382

answers: largely inexhaustible.

answers: NDQ_003383

answers: largely inexhaustible.

answers: NDQ_003384

answers: largely inexhaustible.

answers: NDQ_003385

answers: largely inexhaustible.

answers: NDQ_003386

answers: largely inexhaustible.

answers: NDQ_003387

answers: largely inexhaustible.

answers: NDQ_003388

answers: largely inexhaustible.

answers: NDQ_003389

answers: localized areas

answers: NDQ_003390

answers: nearly all metal prices have been declining over time in inflation adjusted terms,

answers: NDQ_003391

answers: Metal ores

answers: NDQ_003392

answers: nearly all metal prices have been declining over time in inflation adjusted terms,

answers: NDQ_003393

answers: Metal ores

answers: NDQ_003394

answers: nearly all metal prices have been declining over time in inflation adjusted terms,

answers: NDQ_003395

answers: largely inexhaustible.

answers: NDQ_003396

answers: largely inexhaustible.

text: The orogeny is commonly attributed to events off the west coast of North America, where the Kula and Farallon Plates were sliding under the North American plate. Most hypotheses propose that oceanic crust was undergoing flat-slab subduction, i.e., with a shallow subduction angle, and as a consequence, no magmatism occurred in the central west of the continent, and the underlying oceanic lithosphere actually caused drag on the root of the overlying continental lithosphere. One cause for shallow subduction may have been an increased rate of plate convergence. Another proposed cause was subduction of thickened oceanic crust.

text: The orogeny is commonly attributed to events off the west coast of North America, where the

entity_name: Kula Plate

text: Kula

text: and

entity_name: Farallon Plate

text: Farallon Plate

text: s were sliding under the

entity_name: North American Plate

text: North American plate

text: . Most hypotheses propose that oceanic crust was undergoing

entity_section: Subduction angle

text: flat-slab subduction

text: , i.e., with a shallow

text: subduction

text: angle, and as a consequence, no

entity_name: Magmatism

text: magmatism

text: occurred in the central west of the continent, and the underlying oceanic

entity_name: Lithosphere

text: lithosphere

text: actually caused drag on the root of the overlying continental lithosphere. One cause for shallow subduction may have been an increased rate of plate convergence. Another proposed cause was subduction of thickened oceanic crust.

answers: NDQ_003351

answers: flat-slab subduction

answers: NDQ_003352

answers: subducts

answers: NDQ_003353

answers: subduction

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: subduction angle

answers: NDQ_003356

answers: subduct

answers: NDQ_003357

answers: subduction of thickened oceanic crust occurs

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: subducts

answers: NDQ_003360

answers: North American plate

answers: NDQ_003362

answers: flat-slab subduction

answers: NDQ_003363

answers: the west coast of North America

answers: NDQ_003371

answers: What may have been an increased rate of plate convergence?

answers: NDQ_003373

answers: What is the main idea of this passage?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What type of rock deforms?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What is the opposite of flat-slab subduction?

answers: NDQ_003385

answers: What is the name of the area where faults are clustered?

answers: NDQ_003386

answers: what is the cause of earthquakes

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: normal faults, flat-slab subduction, or thickened oceanic crust?

answers: NDQ_003388

answers: What is the cause of shallow subduction?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: subduction angle

answers: NDQ_003391

answers: continental lithosphere

answers: NDQ_003392

answers: subduction angle

answers: NDQ_003393

answers: continental lithosphere

answers: NDQ_003394

answers: flat-slab subduction

answers: NDQ_003395

answers: flat-slab subduction

answers: NDQ_003396

answers: flat-slab

answers: NDQ_003351

answers: flat-slab subduction,

answers: NDQ_003352

answers: drag

answers: NDQ_003353

answers: magmatism

answers: NDQ_003354

answers: Kula and Farallon Plates were sliding under the North American plate.

answers: NDQ_003355

answers: flat-slab subduction,

answers: NDQ_003356

answers: drag

answers: NDQ_003357

answers: shallow subduction angle,

answers: NDQ_003358

answers: no magmatism

answers: NDQ_003359

answers: flat-slab subduction,

answers: NDQ_003360

answers: Kula and Farallon Plates were sliding under the North American plate.

answers: NDQ_003362

answers: no magmatism occurred in the central west of the continent,

answers: NDQ_003363

answers: off the west coast of North America,

answers: NDQ_003371

answers: flat-slab subduction,

answers: NDQ_003373

answers: flat-slab subduction,

answers: NDQ_003376

answers: flat-slab subduction,

answers: NDQ_003378

answers: sliding under the North American plate.

answers: NDQ_003379

answers: shallow subduction angle,

answers: NDQ_003380

answers: drag

answers: NDQ_003381

answers: flat-slab subduction,

answers: NDQ_003382

answers: flat-slab subduction,

answers: NDQ_003383

answers: flat-slab subduction,

answers: NDQ_003384

answers: flat-slab subduction,

answers: NDQ_003385

answers: flat-slab subduction,

answers: NDQ_003386

answers: flat-slab subduction,

answers: NDQ_003387

answers: flat-slab subduction,

answers: NDQ_003388

answers: flat-slab subduction,

answers: NDQ_003389

answers: no magmatism

answers: NDQ_003390

answers: flat-slab subduction,

answers: NDQ_003391

answers: flat-slab subduction,

answers: NDQ_003392

answers: flat-slab subduction,

answers: NDQ_003393

answers: flat-slab subduction,

answers: NDQ_003394

answers: flat-slab subduction,

answers: NDQ_003395

answers: flat-slab subduction,

answers: NDQ_003396

answers: flat-slab subduction,

text: Arequipa-Antofalla is a basement unit underlying the central Andes in northwestern Argentina, western Bolivia, northern Chile and southern Peru. Geologically it corresponds to a craton, terrane or block of continental crust. Arequipa-Antofalla collided and amalgamated with the Amazonian craton about 1000 Ma ago during the Sunsás orogeny. As a terrane Arequipa-Antofalla was ribbon-shaped during the Paleozoic, a time when it was bounded by the west by the Iapetus Ocean and by the east by the Puncoviscana Ocean.

text: Arequipa-Antofalla is a

entity_name: Basement (geology)

text: basement

text: unit underlying the central

entity_name: Andes

text: Andes

text: in

entity_name: Argentine Northwest

text: northwestern Argentina

text: , western

entity_name: Bolivia

text: Bolivia

entity_name: Norte Grande

text: northern Chile

text: and southern

entity_name: Peru

text: Peru

text: . Geologically it corresponds to a

entity_name: Craton

text: craton

entity_name: Terrane

text: terrane

text: or block of

entity_name: Continental crust

text: continental crust

text: . Arequipa-Antofalla

entity_name: Continental collision

text: collided

text: and

entity_name: Accretion (geology)

text: amalgamated

text: with the

entity_name: Amazonian Craton

text: Amazonian craton

text: about 1000 Ma ago during the

entity_name: Sunsás orogeny

text: Sunsás orogeny

text: . As a terrane Arequipa-Antofalla was ribbon-shaped during the

entity_name: Paleozoic

text: Paleozoic

text: , a time when it was bounded by the west by the

entity_name: Iapetus Ocean

text: Iapetus Ocean

text: and by the east by the

entity_name: Puncoviscana Formation

text: Puncoviscana Ocean

method: UNH-ecn

answers: NDQ_003351

answers: Iapetus Ocean

answers: NDQ_003352

answers: collides with other rocks

answers: NDQ_003353

answers: igneous rocks to form

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: ribbon-shaped

answers: NDQ_003356

answers: ribbon-shaped

answers: NDQ_003357

answers: Arequipa-Antofalla collided with what?

answers: NDQ_003358

answers: craton

answers: NDQ_003359

answers: collides

answers: NDQ_003360

answers: Sunsás orogeny

answers: NDQ_003362

answers: arequipa-antofalla was ribbon-shaped during the Paleozoic

answers: NDQ_003363

answers: Sunsás orogeny

answers: NDQ_003371

answers: What may happen if very old rocks are above much younger rocks?

answers: NDQ_003373

answers: What is the main idea of this passage?

answers: NDQ_003376

answers: What type of forces caused the terrain known as basin-and-range?

answers: NDQ_003378

answers: How long ago did the Sunsás orogeny occur?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What type of force applied to rock is stress?

answers: NDQ_003381

answers: Arequipa-Antofalla was ribbon-shaped during the Paleozoic

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Arequipa-Antofalla was ribbon-shaped during the Paleozoic

answers: NDQ_003384

answers: What type of fold was Arequipa-Antofalla?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: Arequipa-Antofalla collided and amalgamated

answers: NDQ_003387

answers: Arequipa-Antofalla collided and amalgamated with the Amazonian craton

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip faults, craton or block of continental crust?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: arequipa-antofalla

answers: NDQ_003391

answers: craton

answers: NDQ_003392

answers: arequipa-antofalla

answers: NDQ_003393

answers: craton

answers: NDQ_003394

answers: ribbon-shaped

answers: NDQ_003395

answers: Arequipa-Antofalla

answers: NDQ_003396

answers: ribbon-shaped

answers: NDQ_003351

answers: Sunsás orogeny.

answers: NDQ_003352

answers: ribbon-shaped

answers: NDQ_003353

answers: ribbon-shaped

answers: NDQ_003354

answers: Arequipa-Antofalla

answers: NDQ_003355

answers: ribbon-shaped

answers: NDQ_003356

answers: ribbon-shaped

answers: NDQ_003357

answers: Sunsás orogeny.

answers: NDQ_003358

answers: craton,

answers: NDQ_003359

answers: Sunsás orogeny.

answers: NDQ_003360

answers: Arequipa-Antofalla

answers: NDQ_003362

answers: ribbon-shaped

answers: NDQ_003363

answers: Sunsás orogeny.

answers: NDQ_003371

answers: Arequipa-Antofalla

answers: NDQ_003373

answers: Arequipa-Antofalla

answers: NDQ_003376

answers: ribbon-shaped during the Paleozoic,

answers: NDQ_003378

answers: Arequipa-Antofalla

answers: NDQ_003379

answers: Sunsás orogeny.

answers: NDQ_003380

answers: Sunsás orogeny.

answers: NDQ_003381

answers: ribbon-shaped during the Paleozoic,

answers: NDQ_003382

answers: Sunsás orogeny.

answers: NDQ_003383

answers: ribbon-shaped

answers: NDQ_003384

answers: ribbon-shaped during the Paleozoic,

answers: NDQ_003385

answers: Arequipa-Antofalla

answers: NDQ_003386

answers: Sunsás orogeny.

answers: NDQ_003387

answers: Sunsás orogeny.

answers: NDQ_003388

answers: Sunsás orogeny.

answers: NDQ_003389

answers: Sunsás orogeny.

answers: NDQ_003390

answers: ribbon-shaped

answers: NDQ_003391

answers: craton,

answers: NDQ_003392

answers: ribbon-shaped

answers: NDQ_003393

answers: craton,

answers: NDQ_003394

answers: ribbon-shaped

answers: NDQ_003395

answers: Sunsás orogeny.

answers: NDQ_003396

answers: Sunsás orogeny.

text: Much of Venus' surface appears to have been shaped by volcanic activity. Overall, Venus has several times as many volcanoes as Earth, and it possesses some 167 giant volcanoes that are over  across. The only volcanic complex of this size on Earth is the Big Island of Hawaii. However, this is not because Venus is more volcanically active than Earth, but because its crust is older. Earth's crust is continually recycled by subduction at the boundaries of tectonic plates, and has an average age of about 100 million years, while Venus' surface is estimated to be about 500 million years old.Venusian craters range from  to  in diameter. There are no craters smaller than 3 km, because of the effects of the dense atmosphere on incoming objects. Objects with less than a certain kinetic energy are slowed down so much by the atmosphere that they do not create an impact crater.

text: Much of Venus' surface appears to have been shaped by volcanic activity. Overall, Venus has several times as many volcanoes as Earth, and it possesses some 167 giant volcanoes that are over  across. The only volcanic complex of this size on Earth is the

entity_name: Hawaii (island)

text: Big Island

text: of

entity_name: Hawaii

text: Hawaii

text: . However, this is not because Venus is more volcanically active than Earth, but because its crust is older. Earth's crust is continually recycled by

text: subduction

text: at the boundaries of

entity_name: Plate tectonics

text: tectonic plate

text: s, and has an average age of about 100 million years, while Venus' surface is estimated to be about 500 million years old.Venusian craters range from  to  in diameter. There are no craters smaller than 3 km, because of the effects of the dense atmosphere on incoming objects. Objects with less than a certain

entity_name: Kinetic energy

text: kinetic energy

text: are slowed down so much by the atmosphere that they do not create an impact crater.

method: Bert-ConvKNRM

answers: NDQ_003351

answers: subduction

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: subduction

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: subduction

answers: NDQ_003356

answers: crater

answers: NDQ_003357

answers: Earth's crust is continually recycled by subduction

answers: NDQ_003358

answers: impact crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: Earth's crust is continually recycled by subduction

answers: NDQ_003363

answers: Venus

answers: NDQ_003371

answers: What is the only volcanic complex of this size on Earth?

answers: NDQ_003373

answers: Why is the Big Island of Hawaii shaped by volcanic activity?

answers: NDQ_003376

answers: What is the only volcanic complex of this size on Earth?

answers: NDQ_003378

answers: What is the only volcanic complex of this size on Earth?

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What is the only volcanic complex of this size on Earth?

answers: NDQ_003381

answers: What is the only volcanic complex of this size on Earth?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the only volcanic complex of this size on Earth?

answers: NDQ_003384

answers: What is the only volcanic complex of this size on Earth?

answers: NDQ_003385

answers: What is the only volcanic complex of this size on Earth?

answers: NDQ_003386

answers: Earth's crust is continually recycled by subduction

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: subduction at the boundaries of tectonic plates, or normal faults?

answers: NDQ_003388

answers: What is the only volcanic complex of this size on Earth?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: subduction

answers: NDQ_003391

answers: subduction

answers: NDQ_003392

answers: subduction

answers: NDQ_003393

answers: subduction

answers: NDQ_003394

answers: tectonic plates

answers: NDQ_003395

answers: tectonic plates

answers: NDQ_003396

answers: subduction

answers: NDQ_003351

answers: subduction

answers: NDQ_003352

answers: impact crater.

answers: NDQ_003353

answers: subduction

answers: NDQ_003354

answers: Venus has several times as many volcanoes

answers: NDQ_003355

answers: subduction

answers: NDQ_003356

answers: craters

answers: NDQ_003357

answers: subduction

answers: NDQ_003358

answers: impact crater.

answers: NDQ_003359

answers: tectonic plates,

answers: NDQ_003360

answers: Venus' surface appears to have been shaped by volcanic activity.

answers: NDQ_003362

answers: Venus is more volcanically active than Earth,

answers: NDQ_003363

answers: Venus' surface appears to have been shaped by volcanic activity.

answers: NDQ_003371

answers: Earth's crust is continually recycled by subduction

answers: NDQ_003373

answers: subduction at the boundaries of tectonic plates,

answers: NDQ_003376

answers: 167 giant volcanoes

answers: NDQ_003378

answers: subduction

answers: NDQ_003379

answers: 167 giant volcanoes

answers: NDQ_003380

answers: craters

answers: NDQ_003381

answers: subduction at the boundaries of tectonic plates,

answers: NDQ_003382

answers: subduction

answers: NDQ_003383

answers: tectonic plates,

answers: NDQ_003384

answers: Venus has several times as many volcanoes

answers: NDQ_003385

answers: tectonic plates,

answers: NDQ_003386

answers: tectonic plates,

answers: NDQ_003387

answers: tectonic plates,

answers: NDQ_003388

answers: subduction at the boundaries of tectonic plates,

answers: NDQ_003389

answers: subduction at the boundaries of tectonic plates,

answers: NDQ_003390

answers: subduction

answers: NDQ_003391

answers: subduction

answers: NDQ_003392

answers: subduction

answers: NDQ_003393

answers: impact crater.

answers: NDQ_003394

answers: subduction

answers: NDQ_003395

answers: subduction

answers: NDQ_003396

answers: subduction

text: Zones of thickened crust, such as those formed during continent-continent collision tend to spread laterally; this spreading occurs even when the collisional event is still in progress. After the collision has finished the zone of thickened crust generally undergoes gravitational collapse, often with the formation of very large extensional faults. Large-scale Devonian extension, for example, followed immediately after the end of the Caledonian orogeny particularly in East Greenland and western Norway.

text: Zones of thickened crust, such as those formed during

text: continent-continent collision

text: tend to spread laterally; this spreading occurs even when the collisional event is still in progress. After the collision has finished the zone of thickened crust generally undergoes

entity_name: Post-orogenic collapse

text: gravitational collapse

text: , often with the formation of very large extensional faults. Large-scale

entity_name: Devonian

text: Devonian

text: extension, for example, followed immediately after the end of the

entity_name: Caledonian orogeny

text: Caledonian orogeny

text: particularly in East

entity_name: Greenland

text: Greenland

text: and western

entity_name: Norway

text: Norway

answers: NDQ_003351

answers: gravitational collapse

answers: NDQ_003352

answers: tends to thicken

answers: NDQ_003353

answers: Gravitational collapse

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fault

answers: NDQ_003356

answers: spread laterally

answers: NDQ_003357

answers: the zone of thickened crust generally undergoes gravity

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: collapses

answers: NDQ_003360

answers: continent-continent collision

answers: NDQ_003362

answers: After the collision has finished the zone of thickened crust generally undergoes gravitational collapse

answers: NDQ_003363

answers: Devonian

answers: NDQ_003371

answers: Which of the following is not a type of fault: extensional faults, thrust faults or Devonian extension?

answers: NDQ_003373

answers: unanswerable

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What type of stress does the zone of thickened crust generally undergo?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: yes

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: no

answers: NDQ_003388

answers: unanswerable

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: extensional faults

answers: NDQ_003391

answers: zone of thickened crust

answers: NDQ_003392

answers: extensional faults

answers: NDQ_003393

answers: thickened crust

answers: NDQ_003394

answers: extensional

answers: NDQ_003395

answers: large extensional faults

answers: NDQ_003396

answers: extensional

answers: NDQ_003351

answers: gravitational collapse,

answers: NDQ_003352

answers: spread laterally;

answers: NDQ_003353

answers: extensional faults.

answers: NDQ_003354

answers: Zones of thickened crust,

answers: NDQ_003355

answers: extensional faults.

answers: NDQ_003356

answers: spread laterally;

answers: NDQ_003357

answers: laterally;

answers: NDQ_003358

answers: extensional faults.

answers: NDQ_003359

answers: gravitational collapse,

answers: NDQ_003360

answers: continent-continent collision

answers: NDQ_003362

answers: the collisional event is still in progress.

answers: NDQ_003363

answers: continent-continent collision

answers: NDQ_003371

answers: extensional faults.

answers: NDQ_003373

answers: Zones of thickened crust,

answers: NDQ_003376

answers: Zones of thickened crust,

answers: NDQ_003378

answers: Zones of thickened crust,

answers: NDQ_003379

answers: laterally;

answers: NDQ_003380

answers: Zones of thickened crust,

answers: NDQ_003381

answers: gravitational collapse,

answers: NDQ_003382

answers: gravitational collapse,

answers: NDQ_003383

answers: extensional faults.

answers: NDQ_003384

answers: extensional faults.

answers: NDQ_003385

answers: extensional faults.

answers: NDQ_003386

answers: extensional faults.

answers: NDQ_003387

answers: extensional faults.

answers: NDQ_003388

answers: extensional faults.

answers: NDQ_003389

answers: extensional faults.

answers: NDQ_003390

answers: extensional faults.

answers: NDQ_003391

answers: extensional faults.

answers: NDQ_003392

answers: extensional faults.

answers: NDQ_003393

answers: thickened crust,

answers: NDQ_003394

answers: extensional faults.

answers: NDQ_003395

answers: extensional faults.

answers: NDQ_003396

answers: extensional faults.

text: In the Directa, the Pope dealt with the fact that clerics (deacons, priests, and bishops) were still living with their wives and having children, thus contravening the Council of Elvira and the First Ecumenical Council. Priests were justifying this by referring to the traditions of the Levitical priesthood of the Old Testament. Siricius was emphatic that clerical continence belonged to immemorial, even apostolic, tradition. He declared that priests had been under a duty to observe temporary continence when serving in the Temple, but that the coming of Christ had brought the old priesthood to completion, and by this fact the duty of temporary continence had become an obligation to perpetual continence. Fifteen points are studied in the decretal, but the key passage is that

text: In the Directa, the Pope dealt with the fact that clerics (deacons, priests, and bishops) were still living with their wives and having children, thus contravening the

text: Council of Elvira

text: and the

text: First Ecumenical Council

text: . Priests were justifying this by referring to the traditions of the

text: Levitical priesthood

text: of the

text: Old Testament

text: . Siricius was emphatic that clerical continence belonged to immemorial, even apostolic, tradition. He declared that priests had been under a duty to observe temporary continence when serving in

text: the Temple

text: , but that the

text: coming of Christ

text: had brought the old priesthood to completion, and by this fact the duty of temporary continence had become an obligation to perpetual continence. Fifteen points are studied in the decretal, but the key passage is that

answers: NDQ_003351

answers: discontinuous

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: Directa

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: living with their wives and having children

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: continental plates

answers: NDQ_003362

answers: the duty of temporary continence had become an obligation to perpetual continence

answers: NDQ_003363

answers: the same time

answers: NDQ_003371

answers: The coming of Christ had brought the old priesthood to completion,

answers: NDQ_003373

answers: compressive stresses

answers: NDQ_003376

answers: basin-and-range

answers: NDQ_003378

answers: The amount the ground moves in an earthquake is called slip.

answers: NDQ_003379

answers: the dip of the fault plane is vertical

answers: NDQ_003380

answers: any force applied to rock is a stress

answers: NDQ_003381

answers: constricting stress occurs, rock deforms

answers: NDQ_003382

answers: Convergent plates

answers: NDQ_003383

answers: stress is the cause of joints in rock

answers: NDQ_003384

answers: syncline

answers: NDQ_003385

answers: fault zone

answers: NDQ_003386

answers: movement of rock at faults

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: shear stress

answers: NDQ_003389

answers: the process of folding

answers: NDQ_003390

answers: clerics

answers: NDQ_003391

answers: a dip-slip fault plane

answers: NDQ_003392

answers: Fault in which the hanging wall pushes up relative to the footwall

answers: NDQ_003393

answers: a dip-slip fault plane

answers: NDQ_003394

answers: Fault with a fault plane that is not vertical

answers: NDQ_003395

answers: Fault with a vertical fault plane

answers: NDQ_003396

answers: a reverse fault in which the fault plane is nearly horizontal

answers: NDQ_003351

answers: perpetual continence.

answers: NDQ_003352

answers: temporary continence had become an obligation to perpetual continence.

answers: NDQ_003353

answers: duty of temporary continence had become an obligation to perpetual continence.

answers: NDQ_003354

answers: duty of temporary continence had become an obligation to perpetual continence.

answers: NDQ_003355

answers: Directa,

answers: NDQ_003356

answers: perpetual continence.

answers: NDQ_003357

answers: living with their wives and having children,

answers: NDQ_003358

answers: immemorial,

answers: NDQ_003359

answers: First Ecumenical Council.

answers: NDQ_003360

answers: Christ

answers: NDQ_003362

answers: the duty of temporary continence had become an obligation to perpetual continence.

answers: NDQ_003363

answers: Christ

answers: NDQ_003371

answers: Directa,

answers: NDQ_003373

answers: clerical continence

answers: NDQ_003376

answers: the duty of temporary continence had become an obligation to perpetual continence.

answers: NDQ_003378

answers: duty of temporary continence had become an obligation to perpetual continence.

answers: NDQ_003379

answers: the duty of temporary continence had become an obligation to perpetual continence.

answers: NDQ_003380

answers: Directa,

answers: NDQ_003381

answers: the duty of temporary continence had become an obligation to perpetual continence.

answers: NDQ_003382

answers: First Ecumenical Council.

answers: NDQ_003383

answers: First Ecumenical Council.

answers: NDQ_003384

answers: perpetual continence.

answers: NDQ_003385

answers: First Ecumenical Council.

answers: NDQ_003386

answers: the duty of temporary continence had become an obligation to perpetual continence.

answers: NDQ_003387

answers: the duty of temporary continence had become an obligation to perpetual continence.

answers: NDQ_003388

answers: the duty of temporary continence had become an obligation to perpetual continence.

answers: NDQ_003389

answers: duty of temporary continence had become an obligation to perpetual continence.

answers: NDQ_003390

answers: First Ecumenical Council.

answers: NDQ_003391

answers: clerical continence

answers: NDQ_003392

answers: Council of Elvira and the First Ecumenical Council.

answers: NDQ_003393

answers: temporary continence had become an obligation to perpetual continence.

answers: NDQ_003394

answers: Council of Elvira and the First Ecumenical Council.

answers: NDQ_003395

answers: First Ecumenical Council.

answers: NDQ_003396

answers: First Ecumenical Council.

text: Stress can also result from an apparent lack of direction of the investigation or not knowing when it will end.  The amount of elaborate planning, risk, and expenditure can pressure an agent to succeed, which can cause considerable stress.  The stress that an undercover agent faces is considerably different from his counterparts on regular duties, whose main source of stress is the administration and the bureaucracy.  As the undercover agents are removed from the bureaucracy, it may result in another problem.  The lack of the usual controls of a uniform, badge, constant supervision, a fixed place of work, or (often) a set assignment could, combined with their continual contact with the organized crime, increase the likelihood for corruption.

text: Stress

text: can also result from an apparent lack of direction of the investigation or not knowing when it will end.  The amount of elaborate planning, risk, and expenditure can pressure an agent to succeed, which can cause considerable stress.  The stress that an undercover agent faces is considerably different from his counterparts on regular duties, whose main source of stress is the administration and the bureaucracy.  As the undercover agents are removed from the bureaucracy, it may result in another problem.  The lack of the usual controls of a uniform, badge, constant supervision, a fixed place of work, or (often) a set assignment could, combined with their continual contact with the

text: organized crime

text: , increase the likelihood for

text: corruption

answers: NDQ_003351

answers: not knowing when it will end

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: unanswerable

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: unanswerable

answers: NDQ_003356

answers: cause stress

answers: NDQ_003357

answers: whose main source of stress is the administration and the bureaucracy

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's surface

answers: NDQ_003362

answers: undercover agents are removed from the bureaucracy

answers: NDQ_003363

answers: unanswerable

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: What can pressure an agent to succeed?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: unanswerable

answers: NDQ_003381

answers: unanswerable

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: no

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: unanswerable

answers: NDQ_003386

answers: movement of rock

answers: NDQ_003387

answers: What can pressure an agent to succeed, which can cause considerable stress?

answers: NDQ_003388

answers: unanswerable

answers: NDQ_003389

answers: unknown

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: dip-slip fault plane

answers: NDQ_003392

answers: unanswerable

answers: NDQ_003393

answers: dip-slip fault plane

answers: NDQ_003394

answers: can cause considerable stress

answers: NDQ_003395

answers: a vertical fault plane

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: lack of direction of the investigation or not knowing when it will end.

answers: NDQ_003352

answers: stress.

answers: NDQ_003353

answers: stress.

answers: NDQ_003354

answers: lack of direction of the investigation or not knowing when it will end.

answers: NDQ_003355

answers: Stress

answers: NDQ_003356

answers: corruption.

answers: NDQ_003357

answers: lack of direction of the investigation or not knowing when it will end.

answers: NDQ_003358

answers: fixed place of work,

answers: NDQ_003359

answers: lack of direction of the investigation or not knowing when it will end.

answers: NDQ_003360

answers: stress.

answers: NDQ_003362

answers: lack of direction of the investigation or not knowing when it will end.

answers: NDQ_003363

answers: lack of direction of the investigation or not knowing when it will end.

answers: NDQ_003371

answers: Stress

answers: NDQ_003373

answers: stress.

answers: NDQ_003376

answers: stress.

answers: NDQ_003378

answers: stress.

answers: NDQ_003379

answers: stress.

answers: NDQ_003380

answers: stress.

answers: NDQ_003381

answers: undercover agents are removed from the bureaucracy,

answers: NDQ_003382

answers: administration and the bureaucracy.

answers: NDQ_003383

answers: stress.

answers: NDQ_003384

answers: whose main source of stress is the administration and the bureaucracy.

answers: NDQ_003385

answers: Stress

answers: NDQ_003386

answers: Stress

answers: NDQ_003387

answers: administration and the bureaucracy.

answers: NDQ_003388

answers: whose main source of stress is the administration and the bureaucracy.

answers: NDQ_003389

answers: whose main source of stress is the administration and the bureaucracy.

answers: NDQ_003390

answers: lack of direction of the investigation or not knowing when it will end.

answers: NDQ_003391

answers: Stress

answers: NDQ_003392

answers: lack of direction of the investigation or not knowing when it will end.

answers: NDQ_003393

answers: Stress

answers: NDQ_003394

answers: Stress can also result from an apparent lack of direction of the investigation

answers: NDQ_003395

answers: lack of direction of the investigation or not knowing when it will end.

answers: NDQ_003396

answers: apparent lack of direction of the investigation or not knowing when it will end.

text: Mountain chains are typically formed by the process of plate tectonics. Tectonic plates slide very slowly over the Earth's mantle, a lower place of rock that is heated from the Earth's interior. Several huge sections of the earth’s crust are impelled by heat currents in the mantle, producing tremendous forces that can buckle the material at the edges of the plates to form mountains. Usually one plate is forced underneath the other, and the lower plate is slowly absorbed by the mantle. Where the two plates pass one another, heated rock from the mantle can burst through the crust to form volcanoes. The movement of the plates against one another can also cause earthquakes.

text: Mountain chains are typically formed by the process of

text: plate tectonics

text: Tectonic plate

text: s slide very slowly over the

text: Earth

text: 's

text: mantle

text: , a lower place of rock that is heated from the Earth's interior. Several huge sections of the earth’s crust are impelled by heat currents in the mantle, producing tremendous forces that can buckle the material at the edges of the plates to form

text: mountain

text: s. Usually one plate is forced underneath the other, and the lower plate is slowly absorbed by the mantle. Where the two plates pass one another, heated

text: rock

text: from the mantle can burst through the

text: crust

text: to form

text: volcano

text: es. The movement of the plates against one another can also cause

text: earthquake

text: s.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: is more likely to crack

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: mountain

answers: NDQ_003356

answers: form mountains

answers: NDQ_003357

answers: tectonic plates slide very slowly over the Earth's mantle

answers: NDQ_003358

answers: volcano

answers: NDQ_003359

answers: passes through the crust

answers: NDQ_003360

answers: plate tectonics

answers: NDQ_003362

answers: volcanoes can burst through the crust to form volcanoes

answers: NDQ_003363

answers: plate tectonics

answers: NDQ_003371

answers: Which of the following is not a type of plate tectonics?

answers: NDQ_003373

answers: what is the second to last word in the passage?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: Which of the following is not an example of confining stress: plate tectonics, volcanoes, or earthquakes?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not a type of fold that arches upward?

answers: NDQ_003385

answers: Which of the following is not an example of a fault zone?

answers: NDQ_003386

answers: yes

answers: NDQ_003387

answers: Which of the following is not caused by compression stress?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip faults or earthquakes?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: plate tectonics

answers: NDQ_003391

answers: mantle

answers: NDQ_003392

answers: plate tectonics

answers: NDQ_003393

answers: mantle

answers: NDQ_003394

answers: Tectonic

answers: NDQ_003395

answers: unanswerable

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: earthquakes.

answers: NDQ_003352

answers: buckle the material

answers: NDQ_003353

answers: buckle the material at the edges of the plates to form mountains.

answers: NDQ_003354

answers: Mountain chains are typically formed by the process of plate tectonics.

answers: NDQ_003355

answers: mountains.

answers: NDQ_003356

answers: volcanoes.

answers: NDQ_003357

answers: the lower plate is slowly absorbed by the mantle.

answers: NDQ_003358

answers: volcanoes.

answers: NDQ_003359

answers: heated rock

answers: NDQ_003360

answers: plate tectonics.

answers: NDQ_003362

answers: volcanoes.

answers: NDQ_003363

answers: plate tectonics.

answers: NDQ_003371

answers: volcanoes.

answers: NDQ_003373

answers: the lower plate is slowly absorbed by the mantle.

answers: NDQ_003376

answers: mountains.

answers: NDQ_003378

answers: The movement of the plates against one another

answers: NDQ_003379

answers: Tectonic plates slide very slowly over the Earth's mantle,

answers: NDQ_003380

answers: forces

answers: NDQ_003381

answers: buckle the material at the edges of the plates to form mountains.

answers: NDQ_003382

answers: one plate is forced underneath the other, and the lower plate

answers: NDQ_003383

answers: buckle the material at the edges of the plates to form mountains.

answers: NDQ_003384

answers: Mountain chains are typically formed by the process of plate tectonics.

answers: NDQ_003385

answers: Mountain chains are typically formed by the process of plate tectonics.

answers: NDQ_003386

answers: The movement of the plates against one another

answers: NDQ_003387

answers: earthquakes.

answers: NDQ_003388

answers: Tectonic plates slide very slowly over the Earth's mantle,

answers: NDQ_003389

answers: plate tectonics.

answers: NDQ_003390

answers: earthquakes.

answers: NDQ_003391

answers: mantle,

answers: NDQ_003392

answers: earthquakes.

answers: NDQ_003393

answers: Tectonic plates slide very slowly over the Earth's mantle,

answers: NDQ_003394

answers: earthquakes.

answers: NDQ_003395

answers: earthquakes.

answers: NDQ_003396

answers: earthquakes.

text: In 1961 the United States began Project Mohole, an ambitious attempt to drill through the Earth's crust into the Mohorovičić discontinuity. The project was discontinued due to high cost.

text: In 1961 the United States began

text: Project Mohole

text: , an ambitious attempt to drill through the Earth's

text: crust

text: into the

text: Mohorovičić discontinuity

text: . The project was discontinued due to high cost.

answers: NDQ_003351

answers: high cost

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: discontinuity

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: Mohorovi i discontinuity

answers: NDQ_003358

answers: discontinuity

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: The United States began Project Mohole

answers: NDQ_003363

answers: Mohole

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: yes

answers: NDQ_003376

answers: unknown

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: no

answers: NDQ_003380

answers: None of the above choices.

answers: NDQ_003381

answers: what is the last word in the passage?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: None of the above choices.

answers: NDQ_003384

answers: None of the above choices are available

answers: NDQ_003385

answers: unanswerable

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: unanswerable

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: discontinuity

answers: NDQ_003391

answers: Mohole

answers: NDQ_003392

answers: discontinuity

answers: NDQ_003393

answers: i discontinuity

answers: NDQ_003394

answers: discontinuity

answers: NDQ_003395

answers: Mohorovi

answers: NDQ_003396

answers: discontinuity

answers: NDQ_003351

answers: Mohorovi<unk>i<unk> discontinuity.

answers: NDQ_003352

answers: discontinued due to high cost.

answers: NDQ_003353

answers: Mohorovi<unk>i<unk> discontinuity.

answers: NDQ_003354

answers: Project Mohole,

answers: NDQ_003355

answers: discontinuity.

answers: NDQ_003356

answers: drill through the Earth's crust

answers: NDQ_003357

answers: Mohorovi<unk>i<unk> discontinuity.

answers: NDQ_003358

answers: discontinuity.

answers: NDQ_003359

answers: Mohorovi<unk>i<unk> discontinuity.

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: The project was discontinued due to high cost.

answers: NDQ_003363

answers: Mohorovi<unk>i<unk> discontinuity.

answers: NDQ_003371

answers: Mohorovi<unk>i<unk> discontinuity.

answers: NDQ_003373

answers: Project Mohole,

answers: NDQ_003376

answers: Project Mohole,

answers: NDQ_003378

answers: Project Mohole,

answers: NDQ_003379

answers: Mohorovi<unk>i<unk> discontinuity.

answers: NDQ_003380

answers: Project Mohole,

answers: NDQ_003381

answers: Project Mohole,

answers: NDQ_003382

answers: Mohorovi<unk>i<unk> discontinuity.

answers: NDQ_003383

answers: Mohorovi<unk>i<unk> discontinuity.

answers: NDQ_003384

answers: Mohorovi<unk>i<unk> discontinuity.

answers: NDQ_003385

answers: Mohorovi<unk>i<unk> discontinuity.

answers: NDQ_003386

answers: Mohorovi<unk>i<unk> discontinuity.

answers: NDQ_003387

answers: Mohorovi<unk>i<unk> discontinuity.

answers: NDQ_003388

answers: Mohorovi<unk>i<unk> discontinuity.

answers: NDQ_003389

answers: Project Mohole, an ambitious attempt to drill through the Earth's crust

answers: NDQ_003390

answers: Mohorovi<unk>i<unk> discontinuity.

answers: NDQ_003391

answers: Mohorovi<unk>i<unk> discontinuity.

answers: NDQ_003392

answers: Mohorovi<unk>i<unk> discontinuity.

answers: NDQ_003393

answers: Mohorovi<unk>i<unk> discontinuity.

answers: NDQ_003394

answers: Mohorovi<unk>i<unk> discontinuity.

answers: NDQ_003395

answers: Mohorovi<unk>i<unk> discontinuity.

answers: NDQ_003396

answers: Mohorovi<unk>i<unk> discontinuity.

text: Oceanic detachment faults occur at spreading ridges where magmatic activity is not enough to account for the entire plate spreading rate. They are characterized by long domes parallel to the spreading direction (oceanic core complexes of the footwall). Slip on these faults can range from 10s to 100s of km. They cannot be structurally restored, as slip on the fault exceeds the thickness of oceanic crust (~30 km compared to ~6 km, for example).

text: Oceanic detachment faults occur at spreading ridges where magmatic activity is not enough to account for the entire plate spreading rate. They are characterized by long domes parallel to the spreading direction (oceanic core complexes of the footwall). Slip on these faults can range from 10s to 100s of km. They cannot be structurally restored, as slip on the fault exceeds the thickness of oceanic crust (~30 km compared to ~6 km, for example).

answers: NDQ_003351

answers: Oceanic detachment faults

answers: NDQ_003352

answers: increases in thickness

answers: NDQ_003353

answers: faults

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: footwall

answers: NDQ_003356

answers: detach

answers: NDQ_003357

answers: slip on the fault exceeds the thickness of oceanic crust

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: detachment

answers: NDQ_003360

answers: detachment faults

answers: NDQ_003362

answers: can be structurally restored

answers: NDQ_003363

answers: oceanic detachment faults

answers: NDQ_003371

answers: Which of the following is not a type of fault: oceanic detachment faults or thrust faults?

answers: NDQ_003373

answers: How would you describe a deep buried rock?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What can be structurally restored?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: What type of fold is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: What is the cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: Oceanic detachment faults or normal faults?

answers: NDQ_003388

answers: Which of the following is not a type of fault: oceanic detachment faults or strike-slip faults?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: detachment faults

answers: NDQ_003391

answers: footwall

answers: NDQ_003392

answers: detachment faults

answers: NDQ_003393

answers: footwall

answers: NDQ_003394

answers: parallel to the spreading direction

answers: NDQ_003395

answers: They are characterized by long domes parallel to the spreading direction

answers: NDQ_003396

answers: detachment faults

answers: NDQ_003351

answers: Oceanic detachment faults

answers: NDQ_003352

answers: slip on the fault exceeds the thickness of oceanic crust

answers: NDQ_003353

answers: slip on the fault exceeds the thickness of oceanic crust

answers: NDQ_003354

answers: Oceanic detachment faults

answers: NDQ_003355

answers: Oceanic detachment faults

answers: NDQ_003356

answers: slip on the fault exceeds the thickness of oceanic crust

answers: NDQ_003357

answers: 6 km,

answers: NDQ_003358

answers: Oceanic detachment faults

answers: NDQ_003359

answers: magmatic activity is not enough to account for the entire plate spreading rate.

answers: NDQ_003360

answers: Oceanic detachment faults

answers: NDQ_003362

answers: structurally restored,

answers: NDQ_003363

answers: spreading ridges

answers: NDQ_003371

answers: Oceanic detachment faults

answers: NDQ_003373

answers: Oceanic detachment faults

answers: NDQ_003376

answers: long domes parallel to the spreading direction

answers: NDQ_003378

answers: slip

answers: NDQ_003379

answers: parallel to the spreading direction

answers: NDQ_003380

answers: slip on the fault exceeds the thickness of oceanic crust

answers: NDQ_003381

answers: slip on the fault exceeds the thickness of oceanic crust

answers: NDQ_003382

answers: Oceanic detachment faults

answers: NDQ_003383

answers: slip on the fault exceeds the thickness of oceanic crust

answers: NDQ_003384

answers: Oceanic detachment faults occur at spreading ridges

answers: NDQ_003385

answers: long domes parallel to the spreading direction

answers: NDQ_003386

answers: magmatic activity is not enough to account for the entire plate spreading rate.

answers: NDQ_003387

answers: Oceanic detachment faults

answers: NDQ_003388

answers: Oceanic detachment faults

answers: NDQ_003389

answers: magmatic activity is not enough to account for the entire plate spreading rate.

answers: NDQ_003390

answers: Oceanic detachment faults

answers: NDQ_003391

answers: oceanic crust

answers: NDQ_003392

answers: Oceanic detachment faults

answers: NDQ_003393

answers: thickness of oceanic crust

answers: NDQ_003394

answers: Oceanic detachment faults

answers: NDQ_003395

answers: long domes parallel to the spreading direction

answers: NDQ_003396

answers: Oceanic detachment faults

text: Pat Abbott, a professor emeritus of geology at San Diego State University, said, "Any quake of this size seems to pass some kind of threshold where it’s large enough to disturb or trigger other faults. In cases like this, that often means increasing stress on other faults, which makes them more prone to movement. The energy seems to be moving northward toward the San Andreas Fault. I don’t want to anthropomorphize, but it’s like this quake was goading the San Andreas." It remains to be seen how the  San Andreas Fault was affected by these temblors. The southern section of the San Andreas Fault worries scientists, because it has not ruptured in more than 300 years. The region also includes other faults, including the Imperial Fault Zone.

text: Pat Abbott, a professor emeritus of geology at

text: San Diego State University

text: , said, "Any quake of this size seems to pass some kind of threshold where it’s large enough to disturb or trigger other faults. In cases like this, that often means increasing stress on other faults, which makes them more prone to movement. The energy seems to be moving northward toward the San Andreas Fault. I don’t want to anthropomorphize, but it’s like this quake was goading the San Andreas." It remains to be seen how the  San Andreas Fault was affected by these temblors. The southern section of the

text: San Andreas Fault

text: worries scientists, because it has not ruptured in more than 300 years. The region also includes other faults, including the

text: Imperial Fault Zone

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: makes it more prone to movement

answers: NDQ_003353

answers: movement

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fault

answers: NDQ_003356

answers: increase stress

answers: NDQ_003357

answers: increasing stress on other faults makes them more prone to movement

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: passes some kind of threshold

answers: NDQ_003360

answers: San Andreas fault

answers: NDQ_003362

answers: it has not ruptured in more than 300 years

answers: NDQ_003363

answers: San Andreas fault

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: unanswerable

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: what is the last word in the passage?

answers: NDQ_003379

answers: no

answers: NDQ_003380

answers: What kind of force is applied to rock?

answers: NDQ_003381

answers: what is the last word in the passage?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What kind of fold does Pat Abbott refer to?

answers: NDQ_003385

answers: yes

answers: NDQ_003386

answers: yes

answers: NDQ_003387

answers: What does increasing stress on other faults mean?

answers: NDQ_003388

answers: unanswerable

answers: NDQ_003389

answers: Fault

answers: NDQ_003390

answers: San Andreas Fault

answers: NDQ_003391

answers: Imperial Fault Zone

answers: NDQ_003392

answers: San Andreas Fault

answers: NDQ_003393

answers: Imperial Fault Zone

answers: NDQ_003394

answers: San Andreas Fault

answers: NDQ_003395

answers: San Andreas Fault

answers: NDQ_003396

answers: San Andreas Fault

answers: NDQ_003351

answers: other faults, which makes them more prone to movement.

answers: NDQ_003352

answers: makes them more prone to movement.

answers: NDQ_003353

answers: movement.

answers: NDQ_003354

answers: San Andreas Fault.

answers: NDQ_003355

answers: faults.

answers: NDQ_003356

answers: movement.

answers: NDQ_003357

answers: increasing stress on other faults, which makes them more prone to movement.

answers: NDQ_003358

answers: faults.

answers: NDQ_003359

answers: stress

answers: NDQ_003360

answers: San Andreas Fault.

answers: NDQ_003362

answers: it has not ruptured in more than 300 years.

answers: NDQ_003363

answers: San Andreas Fault.

answers: NDQ_003371

answers: faults.

answers: NDQ_003373

answers: San Andreas Fault.

answers: NDQ_003376

answers: San Andreas Fault.

answers: NDQ_003378

answers: stress on other faults, which makes them more prone to movement.

answers: NDQ_003379

answers: San Andreas Fault.

answers: NDQ_003380

answers: stress on other faults, which makes them more prone to movement.

answers: NDQ_003381

answers: increasing stress on other faults,

answers: NDQ_003382

answers: increasing stress on other faults, which makes them more prone to movement.

answers: NDQ_003383

answers: stress on other faults, which makes them more prone to movement.

answers: NDQ_003384

answers: San Andreas Fault.

answers: NDQ_003385

answers: Imperial Fault Zone.

answers: NDQ_003386

answers: increasing stress

answers: NDQ_003387

answers: increasing stress on other faults, which makes them more prone to movement.

answers: NDQ_003388

answers: increasing stress on other faults, which makes them more prone to movement.

answers: NDQ_003389

answers: faults.

answers: NDQ_003390

answers: San Andreas Fault.

answers: NDQ_003391

answers: Imperial Fault Zone.

answers: NDQ_003392

answers: San Andreas Fault.

answers: NDQ_003393

answers: Imperial Fault Zone.

answers: NDQ_003394

answers: San Andreas Fault.

answers: NDQ_003395

answers: San Andreas Fault.

answers: NDQ_003396

answers: San Andreas Fault.

text: Folding usually occurs in areas with a very slow strain rate or when the rock being deformed is relatively weak and ductile. As folding occurs the units of rock bend forming anticlines, ridges, and synclines, valleys. While the true thickness of the underlying crust may not be equal to the elevation changes of the resulting mountains and hills, the average crustal thickness is greater than before the deformation occurred. One way in which folding can occur in such a formation is by a small amount of subduction of one plate. One continent may be partially overridden by the other but since the plate is far too light to sink it will uplift the overriding plate creating very large folds that deform the entire crust.

text: Folding usually occurs in areas with a very slow strain rate or when the rock being deformed is relatively weak and ductile. As folding occurs the units of rock bend forming anticlines, ridges, and synclines, valleys. While the true thickness of the underlying crust may not be equal to the elevation changes of the resulting mountains and hills, the average crustal thickness is greater than before the deformation occurred. One way in which folding can occur in such a formation is by a small amount of subduction of one plate. One continent may be partially overridden by the other but since the plate is far too light to sink it will uplift the overriding plate creating very large folds that deform the entire crust.

answers: NDQ_003351

answers: subduction

answers: NDQ_003352

answers: is more likely to be

answers: NDQ_003353

answers: anticlines

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: anticlines

answers: NDQ_003356

answers: bend

answers: NDQ_003357

answers: the rock being deformed is relatively weak and ductile

answers: NDQ_003358

answers: synclines

answers: NDQ_003359

answers: weak and ductile

answers: NDQ_003360

answers: continents

answers: NDQ_003362

answers: one continent may be partially overridden by the other

answers: NDQ_003363

answers: subduction of one plate

answers: NDQ_003371

answers: Which of the following is not a formation: anticlines, ridges, and synclines, valleys?

answers: NDQ_003373

answers: unanswerable

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What type of force applied to rock is a stress?

answers: NDQ_003381

answers: What type of stress occurs when rock deforms?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: normal faults or subduction of one plate?

answers: NDQ_003388

answers: Which of the following is not a type of fault: anticlines, ridges, or synclines?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: anticlines

answers: NDQ_003391

answers: subduction

answers: NDQ_003392

answers: anticlines

answers: NDQ_003393

answers: unanswerable

answers: NDQ_003394

answers: anticlines

answers: NDQ_003395

answers: anticlines

answers: NDQ_003396

answers: synclines

answers: NDQ_003351

answers: Folding

answers: NDQ_003352

answers: units of rock bend

answers: NDQ_003353

answers: Folding

answers: NDQ_003354

answers: Folding usually occurs in areas with a very slow strain rate

answers: NDQ_003355

answers: anticlines,

answers: NDQ_003356

answers: Folding

answers: NDQ_003357

answers: subduction of one plate.

answers: NDQ_003358

answers: Folding usually occurs in areas with a very slow strain rate

answers: NDQ_003359

answers: weak and ductile.

answers: NDQ_003360

answers: subduction of one plate.

answers: NDQ_003362

answers: the plate is far too light to sink

answers: NDQ_003363

answers: subduction of one plate.

answers: NDQ_003371

answers: a small amount of subduction of one plate.

answers: NDQ_003373

answers: weak and ductile.

answers: NDQ_003376

answers: anticlines, ridges, and synclines, valleys.

answers: NDQ_003378

answers: Folding

answers: NDQ_003379

answers: anticlines, ridges, and synclines, valleys.

answers: NDQ_003380

answers: Folding usually occurs in areas with a very slow strain rate

answers: NDQ_003381

answers: weak and ductile.

answers: NDQ_003382

answers: Folding usually occurs in areas with a very slow strain rate

answers: NDQ_003383

answers: anticlines, ridges, and synclines, valleys.

answers: NDQ_003384

answers: synclines,

answers: NDQ_003385

answers: Folding usually occurs in areas with a very slow strain rate

answers: NDQ_003386

answers: Folding

answers: NDQ_003387

answers: Folding usually occurs in areas with a very slow strain rate

answers: NDQ_003388

answers: Folding usually occurs in areas with a very slow strain rate

answers: NDQ_003389

answers: anticlines, ridges, and synclines, valleys.

answers: NDQ_003390

answers: subduction

answers: NDQ_003391

answers: subduction

answers: NDQ_003392

answers: anticlines,

answers: NDQ_003393

answers: Folding

answers: NDQ_003394

answers: Folding usually occurs in areas with a very slow strain rate

answers: NDQ_003395

answers: Folding usually occurs in areas with a very slow strain rate

answers: NDQ_003396

answers: Folding usually occurs in areas with a very slow strain rate

text: The northernmost coastal area is one of California's most seismically active regions and, in a 50-year period, the area including the Mendocino Fracture Zone at the southern flank of the Gorda Plate generated about 25 percent of all seismic energy unleashed in the state. The Mendocino Triple Junction (strike-slip/strike-slip/trench) formed 29–30 mya at 31° N (west of present-day Baja California) when the Pacific-Farallon spreading center initially approached the subduction zone off the coast of western North America. Simultaneously, the Rivera Triple Junction shifted to the southeast to its current position at 23° N. Once the Pacific Plate and North American Plate connected the boundary became that of a transform fault (San Andreas) due to the northwestward motion of the Pacific Plate relative to the North American Plate. The San Andreas Fault continues to lengthen to the northwest and the southeast as the two triple junctions continue their transient motion.

text: The northernmost coastal area is one of California's most seismically active regions and, in a 50-year period, the area including the

text: Mendocino Fracture Zone

text: at the southern flank of the

text: Gorda Plate

text: generated about 25 percent of all seismic energy unleashed in the state. The

text: Mendocino Triple Junction

text: (strike-slip/strike-slip/

text: trench

text: ) formed 29–30

text: mya

text: at 31° N (west of present-day

text: Baja California

text: ) when the Pacific-Farallon spreading center initially approached the subduction zone off the coast of western North America. Simultaneously, the

text: Rivera Triple Junction

text: shifted to the southeast to its current position at 23° N. Once the

text: Pacific Plate

text: and

text: North American Plate

text: connected the boundary became that of a

text: transform fault

text: (San Andreas) due to the northwestward motion of the Pacific Plate relative to the North American Plate. The

text: San Andreas Fault

text: continues to lengthen to the northwest and the southeast as the two

text: triple junction

text: s continue their transient motion.

answers: NDQ_003351

answers: strike-slip

answers: NDQ_003352

answers: lengthens

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: transform fault

answers: NDQ_003356

answers: lengthen

answers: NDQ_003357

answers: Strike-slip/strike-slip/trench

answers: NDQ_003358

answers: unanswerable

answers: NDQ_003359

answers: The San Andreas Fault

answers: NDQ_003360

answers: Pacific Plate

answers: NDQ_003362

answers: The San Andreas Fault continues to lengthen to the northwest

answers: NDQ_003363

answers: San Andreas Fault

answers: NDQ_003371

answers: What type of fault is the San Andreas Fault?

answers: NDQ_003373

answers: Why is the Mendocino Triple Junction at the southern flank of the Gorda Plate?

answers: NDQ_003376

answers: What type of forces caused the terrain known as basin-and-range?

answers: NDQ_003378

answers: what is the last word in the passage?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What is the San Andreas Fault?

answers: NDQ_003381

answers: How does the San Andreas Fault deform?

answers: NDQ_003382

answers: What is the most common stress at convergent plates

answers: NDQ_003383

answers: What is the San Andreas Fault?

answers: NDQ_003384

answers: What type of fold is the Mendocino Triple Junction?

answers: NDQ_003385

answers: What is the San Andreas Fault?

answers: NDQ_003386

answers: What is the San Andreas Fault?

answers: NDQ_003387

answers: Which of the following is not a normal fault: Mendocino Fracture Zone or San Andreas Fault?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip, transform, or trench?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: San Andreas Fault

answers: NDQ_003391

answers: subduction zone

answers: NDQ_003392

answers: San Andreas Fault

answers: NDQ_003393

answers: subduction zone

answers: NDQ_003394

answers: transform fault

answers: NDQ_003395

answers: San Andreas Fault

answers: NDQ_003396

answers: transform fault

answers: NDQ_003351

answers: transform fault

answers: NDQ_003352

answers: (strike-slip/strike-slip/trench)

answers: NDQ_003353

answers: transform fault

answers: NDQ_003354

answers: Mendocino Fracture Zone

answers: NDQ_003355

answers: (strike-slip/strike-slip/trench)

answers: NDQ_003356

answers: (strike-slip/strike-slip/trench)

answers: NDQ_003357

answers: northwestward motion of the Pacific Plate relative to the North American Plate.

answers: NDQ_003358

answers: (strike-slip/strike-slip/trench)

answers: NDQ_003359

answers: northwestward motion of the Pacific Plate relative to the North American Plate.

answers: NDQ_003360

answers: northwestward motion of the Pacific Plate

answers: NDQ_003362

answers: continues to lengthen to the northwest and the southeast

answers: NDQ_003363

answers: 31° N

answers: NDQ_003371

answers: transform fault

answers: NDQ_003373

answers: Mendocino Fracture Zone

answers: NDQ_003376

answers: Mendocino Fracture Zone

answers: NDQ_003378

answers: (strike-slip/strike-slip/trench)

answers: NDQ_003379

answers: The Mendocino Triple Junction

answers: NDQ_003380

answers: seismic energy

answers: NDQ_003381

answers: The Mendocino Triple Junction

answers: NDQ_003382

answers: subduction zone

answers: NDQ_003383

answers: (strike-slip/strike-slip/trench)

answers: NDQ_003384

answers: transform fault

answers: NDQ_003385

answers: Fracture Zone

answers: NDQ_003386

answers: northwestward motion of the Pacific Plate relative to the North American Plate.

answers: NDQ_003387

answers: transform fault

answers: NDQ_003388

answers: Mendocino Triple Junction

answers: NDQ_003389

answers: The Mendocino Triple Junction

answers: NDQ_003390

answers: San Andreas Fault

answers: NDQ_003391

answers: (strike-slip/strike-slip/trench)

answers: NDQ_003392

answers: San Andreas Fault

answers: NDQ_003393

answers: (strike-slip/strike-slip/trench)

answers: NDQ_003394

answers: transform fault

answers: NDQ_003395

answers: transform fault

answers: NDQ_003396

answers: transform fault

text: Motorways of the Sea are a concept in the transport policy of the European Union, stressing the importance of sea transport. The main aim of these Motorways of the Sea is to improve port communications with peripheral regions of the European continent and thus strengthen the networks between the EU candidate countries and those countries already part of the European Union.

text: Motorways of the Sea are a concept in the

text: transport

text: policy of the

text: European Union

text: , stressing the importance of sea transport. The main aim of these Motorways of the Sea is to improve port communications with peripheral regions of the European continent and thus strengthen the networks between the

entity_name: Future enlargement of the European Union

text: EU candidate countries

text: and those countries already part of the European Union.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: voids to form

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: weaken

answers: NDQ_003357

answers: peripheral regions of the European continent and those countries already part of the European Union

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: continental plates

answers: NDQ_003362

answers: Motorways of the Sea are a concept in the transport policy of the European Union

answers: NDQ_003363

answers: the same time

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: None of the above choices.

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: strike-slip fault

answers: NDQ_003380

answers: What is the main purpose of these Motorways of the Sea?

answers: NDQ_003381

answers: What is the main purpose of these Motorways of the Sea?

answers: NDQ_003382

answers: None of the above choices.

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: unanswerable

answers: NDQ_003386

answers: no

answers: NDQ_003387

answers: What is the main aim of these Motorways of the Sea?

answers: NDQ_003388

answers: The main aim of these Motorways of the Sea is to improve port communications with peripheral regions

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: dip-slip fault

answers: NDQ_003392

answers: unanswerable

answers: NDQ_003393

answers: a dip-slip fault plane

answers: NDQ_003394

answers: is a fault

answers: NDQ_003395

answers: a vertical fault plane

answers: NDQ_003396

answers: fault in which the fault plane is nearly horizontal

answers: NDQ_003351

answers: Motorways of the Sea

answers: NDQ_003352

answers: Motorways of the Sea

answers: NDQ_003353

answers: Motorways of the Sea

answers: NDQ_003354

answers: Motorways of the Sea

answers: NDQ_003355

answers: peripheral regions

answers: NDQ_003356

answers: Motorways of the Sea

answers: NDQ_003357

answers: EU candidate countries and those countries already part of the European Union.

answers: NDQ_003358

answers: Motorways

answers: NDQ_003359

answers: Motorways of the Sea

answers: NDQ_003360

answers: sea transport.

answers: NDQ_003362

answers: Motorways of the Sea

answers: NDQ_003363

answers: sea transport.

answers: NDQ_003371

answers: Motorways of the Sea

answers: NDQ_003373

answers: Motorways of the Sea

answers: NDQ_003376

answers: Motorways of the Sea

answers: NDQ_003378

answers: Motorways of the Sea

answers: NDQ_003379

answers: Motorways of the Sea is to improve port communications with peripheral regions

answers: NDQ_003380

answers: Motorways of the Sea

answers: NDQ_003381

answers: Motorways of the Sea

answers: NDQ_003382

answers: Motorways of the Sea

answers: NDQ_003383

answers: Motorways of the Sea

answers: NDQ_003384

answers: Motorways of the Sea

answers: NDQ_003385

answers: Motorways of the Sea is to improve port communications with peripheral regions

answers: NDQ_003386

answers: Motorways of the Sea

answers: NDQ_003387

answers: Motorways of the Sea

answers: NDQ_003388

answers: Motorways of the Sea

answers: NDQ_003389

answers: Motorways of the Sea

answers: NDQ_003390

answers: Motorways of the Sea

answers: NDQ_003391

answers: Motorways of the Sea

answers: NDQ_003392

answers: Motorways of the Sea

answers: NDQ_003393

answers: Motorways of the Sea

answers: NDQ_003394

answers: Motorways of the Sea

answers: NDQ_003395

answers: Motorways of the Sea is to improve port communications with peripheral regions

answers: NDQ_003396

answers: Motorways of the Sea

text: Most languages have at most one degree of stress on the phonemic level. That is, each syllable has stress or it does not. Many languages have rhythmic stress; location of the stress may not be predictable, but when the location of one stressed syllable (which may be the primary stress) is known, certain syllables before or after can be predicted to also be stressed; these may have secondary stress. An example is Dutch, where the rule is that initial and final syllables (word boundaries) take secondary stress, then every alternate syllable before and after the primary stress, as long as two stressed syllables are not adjacent and stress does not fall on  (there are, however, some exceptions to this rule). See . A similar rule applies in Romanian: secondary stress falls on every alternate syllable, starting with the first, as long as it does not fall adjacent to the primary stress. In other languages (including Egyptian Radio Arabic, Bhojpuri, Cayuga, Estonian, Hawaiian, Kaure, Malayalam, and Warrgamay), secondary stress can be predicted to fall on heavy syllables.

text: Most languages have at most one degree of stress on the

text: phonemic

text: level. That is, each

text: syllable

text: has stress or it does not. Many languages have rhythmic stress; location of the stress may not be predictable, but when the location of one stressed syllable (which may be the primary stress) is known, certain syllables before or after can be predicted to also be stressed; these may have secondary stress. An example is

text: Dutch

text: , where the rule is that initial and final syllables (word boundaries) take secondary stress, then every alternate syllable before and after the primary stress, as long as two stressed syllables are not adjacent and stress does not fall on  (there are, however, some exceptions to this rule). See . A similar rule applies in

text: Romanian

text: : secondary stress falls on every alternate syllable, starting with the first, as long as it does not fall adjacent to the primary stress. In other languages (including Egyptian Radio Arabic,

text: Bhojpuri

text: Cayuga

text: Estonian

text: Hawaiian

text: Kaure

text: Malayalam

text: , and

text: Warrgamay

text: ), secondary stress can be predicted to fall on

text: heavy syllable

text: s.

answers: NDQ_003351

answers: secondary stress

answers: NDQ_003352

answers: is more likely to crack

answers: NDQ_003353

answers: secondary stress

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: secondary stress

answers: NDQ_003357

answers: secondary stress can be predicted to fall on heavy syllables

answers: NDQ_003358

answers: stress

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: secondary stress

answers: NDQ_003362

answers: secondary stress can be predicted to fall on heavy syllables

answers: NDQ_003363

answers: secondary stress

answers: NDQ_003371

answers: context: Many languages have at most one degree of stress on the phonemic level. That is, each syllable has stress or it does not. Many languages have rhythmic stress; location of the stress may not be predictable

answers: NDQ_003373

answers: secondary stress

answers: NDQ_003376

answers: compressive forces

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: strike-slip fault

answers: NDQ_003380

answers: unanswerable

answers: NDQ_003381

answers: unanswerable

answers: NDQ_003382

answers: secondary stress

answers: NDQ_003383

answers: no

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: Fault zone

answers: NDQ_003386

answers: cause of earthquakes

answers: NDQ_003387

answers: secondary stress

answers: NDQ_003388

answers: secondary stress

answers: NDQ_003389

answers: fold

answers: NDQ_003390

answers: secondary stress

answers: NDQ_003391

answers: dip-slip fault plane

answers: NDQ_003392

answers: secondary stress

answers: NDQ_003393

answers: dip-slip fault plane

answers: NDQ_003394

answers: a fault plane that is not vertical

answers: NDQ_003395

answers: a vertical fault plane

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: rhythmic stress;

answers: NDQ_003352

answers: heavy syllables.

answers: NDQ_003353

answers: stress on the phonemic level.

answers: NDQ_003354

answers: Most languages have at most one degree of stress on the phonemic level.

answers: NDQ_003355

answers: heavy syllables.

answers: NDQ_003356

answers: heavy syllables.

answers: NDQ_003357

answers: stress does not fall on

answers: NDQ_003358

answers: heavy syllables.

answers: NDQ_003359

answers: two stressed syllables are not adjacent

answers: NDQ_003360

answers: stress on the phonemic level.

answers: NDQ_003362

answers: Most languages have at most one degree of stress on the phonemic level.

answers: NDQ_003363

answers: one degree of stress on the phonemic level.

answers: NDQ_003371

answers: Most languages have at most one degree of stress on the phonemic level.

answers: NDQ_003373

answers: Most languages have at most one degree of stress on the phonemic level.

answers: NDQ_003376

answers: rhythmic stress;

answers: NDQ_003378

answers: secondary stress.

answers: NDQ_003379

answers: heavy syllables.

answers: NDQ_003380

answers: stress

answers: NDQ_003381

answers: Most languages have at most one degree of stress on the phonemic level.

answers: NDQ_003382

answers: rhythmic stress;

answers: NDQ_003383

answers: stress

answers: NDQ_003384

answers: Most languages have at most one degree of stress on the phonemic level.

answers: NDQ_003385

answers: Most languages have at most one degree of stress on the phonemic level.

answers: NDQ_003386

answers: Most languages have at most one degree of stress on the phonemic level.

answers: NDQ_003387

answers: rhythmic stress;

answers: NDQ_003388

answers: heavy syllables.

answers: NDQ_003389

answers: Most languages have at most one degree of stress on the phonemic level.

answers: NDQ_003390

answers: Most languages have at most one degree of stress on the phonemic level.

answers: NDQ_003391

answers: heavy syllables.

answers: NDQ_003392

answers: Most languages have at most one degree of stress on the phonemic level.

answers: NDQ_003393

answers: heavy syllables.

answers: NDQ_003394

answers: two stressed syllables

answers: NDQ_003395

answers: two stressed syllables

answers: NDQ_003396

answers: heavy syllables.

text: Modeling and simulation is used to evaluate the theoretical reliability for large systems. The outcome of this kind of model is used to evaluate different design options. A model of the entire system is created, and the model is stressed by removing components. Redundancy simulation involves the N-x criteria. N represents the total number of components in the system. x is the number of components used to stress the system. N-1 means the model is stressed by evaluating performance with all possible combinations where one component is faulted. N-2 means the model is stressed by evaluating performance with all possible combinations where two component are faulted simultaneously.

text: Modeling and simulation

text: is used to evaluate the theoretical reliability for large systems. The outcome of this kind of model is used to evaluate different design options. A model of the entire system is created, and the model is stressed by removing components. Redundancy simulation involves the N-x criteria. N represents the total number of components in the system. x is the number of components used to stress the system. N-1 means the model is stressed by evaluating performance with all possible combinations where one component is faulted. N-2 means the model is stressed by evaluating performance with all possible combinations where two component are faulted simultaneously.

answers: NDQ_003351

answers: N-2

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone.

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: N-1 means the model is stressed by evaluating performance with all possible combinations where one component is faulted.

answers: NDQ_003358

answers: rock pocket

answers: NDQ_003359

answers: N-2

answers: NDQ_003360

answers: continental plates

answers: NDQ_003362

answers: two component are faulted simultaneously.

answers: NDQ_003363

answers: N-2

answers: NDQ_003371

answers: N-2

answers: NDQ_003373

answers: How would you describe compressive stresses?

answers: NDQ_003376

answers: compressive forces

answers: NDQ_003378

answers: What is the amount of slip in an earthquake?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What is the most common type of stress?

answers: NDQ_003381

answers: What is the result of confining stress?

answers: NDQ_003382

answers: N-2

answers: NDQ_003383

answers: How does stress cause joints in rock?

answers: NDQ_003384

answers: What type of fold is a syncline?

answers: NDQ_003385

answers: What is the term for an area where faults are clustered?

answers: NDQ_003386

answers: N-2

answers: NDQ_003387

answers: Which of the following is not a normal fault?

answers: NDQ_003388

answers: N-2

answers: NDQ_003389

answers: N-2

answers: NDQ_003390

answers: N-2

answers: NDQ_003391

answers: N-2

answers: NDQ_003392

answers: N-2

answers: NDQ_003393

answers: N-2

answers: NDQ_003394

answers: N-2

answers: NDQ_003395

answers: N-2

answers: NDQ_003396

answers: N-2

answers: NDQ_003351

answers: N-2

answers: NDQ_003352

answers: N-2

answers: NDQ_003353

answers: removing components.

answers: NDQ_003354

answers: N-2

answers: NDQ_003355

answers: N-2

answers: NDQ_003356

answers: N-2

answers: NDQ_003357

answers: one component

answers: NDQ_003358

answers: N-2

answers: NDQ_003359

answers: two component are faulted simultaneously.

answers: NDQ_003360

answers: Modeling and simulation

answers: NDQ_003362

answers: one component is faulted.

answers: NDQ_003363

answers: N-2

answers: NDQ_003371

answers: N-2

answers: NDQ_003373

answers: N-2

answers: NDQ_003376

answers: N-2

answers: NDQ_003378

answers: N-2

answers: NDQ_003379

answers: N-2

answers: NDQ_003380

answers: stressed by removing components.

answers: NDQ_003381

answers: N-2

answers: NDQ_003382

answers: N-2

answers: NDQ_003383

answers: stressed by removing components.

answers: NDQ_003384

answers: N-2

answers: NDQ_003385

answers: N-2

answers: NDQ_003386

answers: N-2

answers: NDQ_003387

answers: N-2

answers: NDQ_003388

answers: N-2

answers: NDQ_003389

answers: Modeling and simulation is used to evaluate the theoretical reliability for large systems.

answers: NDQ_003390

answers: N-2

answers: NDQ_003391

answers: N-2

answers: NDQ_003392

answers: N-2

answers: NDQ_003393

answers: N-2

answers: NDQ_003394

answers: N-2

answers: NDQ_003395

answers: N-2

answers: NDQ_003396

answers: N-2

text: Reconstruction of seismic reflections in the deep interior indicate some major discontinuities in seismic velocities that demarcate the major zones of the Earth: inner core, outer core, mantle, lithosphere and crust. The mantle itself is divided into the upper mantle, transition zone, lower mantle and D′′ layer. Between the crust and the mantle is the Mohorovičić discontinuity.

text: Reconstruction of seismic reflections in the deep interior indicate some major discontinuities in seismic velocities that demarcate the major zones of the Earth:

text: inner core

text: outer core

text: mantle

text: lithosphere

text: and

text: crust

text: . The

text: mantle

text: itself is divided into the upper mantle, transition zone, lower mantle and D′′ layer. Between the crust and the mantle is the

text: Mohorovičić discontinuity

answers: NDQ_003351

answers: lower mantle

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: D′′ layer

answers: NDQ_003356

answers: discontinuity

answers: NDQ_003357

answers: Mohorovi i discontinuity is between the crust and the mantle

answers: NDQ_003358

answers: discontinuity

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: mantle

answers: NDQ_003362

answers: the San Andreas fault is between the crust and the mantle

answers: NDQ_003363

answers: deep interior

answers: NDQ_003371

answers: What is the Mohorovi i discontinuity?

answers: NDQ_003373

answers: What is the Mohorovi i discontinuity?

answers: NDQ_003376

answers: The Mohorovi i discontinuity

answers: NDQ_003378

answers: what is the last word in the passage?

answers: NDQ_003379

answers: The Mohorovi i discontinuity

answers: NDQ_003380

answers: Which of the following is not a major zone of the Earth?

answers: NDQ_003381

answers: Which of the following is not a zone of the Earth: inner core, outer core, mantle, lithosphere and crust?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the Mohorovi i discontinuity?

answers: NDQ_003384

answers: What type of fold is the Mohorovi i discontinuity?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: What is the Mohorovi i discontinuity

answers: NDQ_003387

answers: What is the Mohorovi i discontinuity?

answers: NDQ_003388

answers: Which of the following is not a zone of the Earth: inner core, outer core, mantle, lithosphere and crust?

answers: NDQ_003389

answers: D′′ layer

answers: NDQ_003390

answers: Mohorovi i

answers: NDQ_003391

answers: lithosphere

answers: NDQ_003392

answers: Mohorovi

answers: NDQ_003393

answers: lithosphere

answers: NDQ_003394

answers: non-vertical

answers: NDQ_003395

answers: between the crust and the mantle

answers: NDQ_003396

answers: Mohorovi

answers: NDQ_003351

answers: seismic velocities

answers: NDQ_003352

answers: discontinuities

answers: NDQ_003353

answers: discontinuities

answers: NDQ_003354

answers: Reconstruction of seismic reflections in the deep interior indicate some major discontinuities

answers: NDQ_003355

answers: lithosphere and crust.

answers: NDQ_003356

answers: discontinuities in seismic velocities

answers: NDQ_003357

answers: Mohorovi<unk>i<unk> discontinuity.

answers: NDQ_003358

answers: lithosphere

answers: NDQ_003359

answers: discontinuities in seismic velocities

answers: NDQ_003360

answers: seismic reflections

answers: NDQ_003362

answers: Reconstruction of seismic reflections in the deep interior indicate some major discontinuities

answers: NDQ_003363

answers: deep interior

answers: NDQ_003371

answers: Mohorovi<unk>i<unk> discontinuity.

answers: NDQ_003373

answers: Reconstruction of seismic reflections in the deep interior

answers: NDQ_003376

answers: Reconstruction of seismic reflections in the deep interior

answers: NDQ_003378

answers: seismic velocities

answers: NDQ_003379

answers: Mohorovi<unk>i<unk> discontinuity.

answers: NDQ_003380

answers: Reconstruction of seismic reflections in the deep interior

answers: NDQ_003381

answers: Reconstruction of seismic reflections in the deep interior indicate some major discontinuities

answers: NDQ_003382

answers: Reconstruction of seismic reflections in the deep interior indicate some major discontinuities

answers: NDQ_003383

answers: Reconstruction of seismic reflections in the deep interior indicate some major discontinuities

answers: NDQ_003384

answers: Mohorovi<unk>i<unk> discontinuity.

answers: NDQ_003385

answers: major discontinuities

answers: NDQ_003386

answers: discontinuities

answers: NDQ_003387

answers: Mohorovi<unk>i<unk> discontinuity.

answers: NDQ_003388

answers: Reconstruction of seismic reflections in the deep interior

answers: NDQ_003389

answers: Reconstruction of seismic reflections in the deep interior indicate some major discontinuities

answers: NDQ_003390

answers: Mohorovi<unk>i<unk> discontinuity.

answers: NDQ_003391

answers: lithosphere and crust.

answers: NDQ_003392

answers: Mohorovi<unk>i<unk> discontinuity.

answers: NDQ_003393

answers: lithosphere and crust.

answers: NDQ_003394

answers: Mohorovi<unk>i<unk> discontinuity.

answers: NDQ_003395

answers: Mohorovi<unk>i<unk> discontinuity.

answers: NDQ_003396

answers: Mohorovi<unk>i<unk> discontinuity.

text: In November 1983, the office of the Connecticut state medical examiner issued a report stating that Slee's death may have been related to stress. The report stated: "This 26-year-old male reportedly collapsed during a group meeting described as a self-improvement seminar. A complete autopsy determined no anatomic cause of death. ... Available history indicates that Mr. Slee collapsed in a situation in which high emotional stress could be expected. Such emotional stress may have neural and hormonal effects that are deleterious to cardiac rhythm." The New Haven Register reported that Chief Medical Examiner Catherine Galvin said that "arrhythmia, an electrical malfunction of the heart, is believed to have been the cause of Slee's death, but it couldn't be verified".  Galvin said that stressful situations can cause such an arrhythmia: "In a stress situation you've got adrenalin pumping into the circulation. That can trigger it." According to the Boston Phoenix, the pathologist that had examined Slee's body stated: "I don’t like the word 'fright', but there are recognized entities of sudden death", though it may not be possible to determine the cause, "where emotions come into play" such as an instance where an individual believes that a curse will harm them. On November 19, 1983, the New Haven Register reported that police were "no longer actively investigating the case", and went on to note that therefore "any connection between Slee's death and his experiences at the seminar" were not likely to be confirmed.

text: In November 1983, the office of the Connecticut state

text: medical examiner

text: issued a report stating that Slee's death may have been related to stress. The report stated: "This 26-year-old male reportedly collapsed during a group meeting described as a self-improvement seminar. A complete autopsy determined no anatomic cause of death. ... Available history indicates that Mr. Slee collapsed in a situation in which high emotional stress could be expected. Such emotional stress may have neural and hormonal effects that are deleterious to cardiac rhythm." The

text: New Haven Register

text: reported that Chief Medical Examiner Catherine Galvin said that "arrhythmia, an electrical malfunction of the heart, is believed to have been the cause of Slee's death, but it couldn't be verified".  Galvin said that stressful situations can cause such an arrhythmia: "In a stress situation you've got adrenalin pumping into the circulation. That can trigger it." According to the Boston Phoenix, the

text: pathologist

text: that had examined Slee's body stated: "I don’t like the word 'fright', but there are recognized entities of sudden death", though it may not be possible to determine the cause, "where emotions come into play" such as an instance where an individual believes that a

text: curse

text: will harm them. On November 19, 1983, the New Haven Register reported that police were "no longer actively investigating the case", and went on to note that therefore "any connection between Slee's death and his experiences at the seminar" were not likely to be confirmed.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: can cause arrhythmia

answers: NDQ_003353

answers: Arrhythmia

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: unanswerable

answers: NDQ_003356

answers: unbalance

answers: NDQ_003357

answers: adrenalin pumping into the circulation can trigger what?

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: unanswerable

answers: NDQ_003363

answers: unanswerable

answers: NDQ_003371

answers: What may have been the cause of Slee's death?

answers: NDQ_003373

answers: How would you describe Slee's death?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: unanswerable

answers: NDQ_003381

answers: unanswerable

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: Which of the following is not a form of stress: adrenalin pumping into the circulation. That can trigger it.

answers: NDQ_003385

answers: what is the first word in the passage?

answers: NDQ_003386

answers: What is the cause of Slee's death?

answers: NDQ_003387

answers: Which of the following is not a cause of Slee's death: arrhythmia, an electrical malfunction of the heart, or stress?

answers: NDQ_003388

answers: Which of the following is not a cause of Slee's death: arrhythmia, an electrical malfunction of the heart, or stress?

answers: NDQ_003389

answers: unknown

answers: NDQ_003390

answers: a curse

answers: NDQ_003391

answers: unanswerable

answers: NDQ_003392

answers: a curse

answers: NDQ_003393

answers: unanswerable

answers: NDQ_003394

answers: NDQ_003395

answers: unanswerable

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: emotional stress

answers: NDQ_003352

answers: neural and hormonal effects that are deleterious to cardiac rhythm."

answers: NDQ_003353

answers: neural and hormonal effects that are deleterious to cardiac rhythm."

answers: NDQ_003354

answers: high emotional stress could be expected.

answers: NDQ_003355

answers: "arrhythmia,

answers: NDQ_003356

answers: rhythm."

answers: NDQ_003357

answers: adrenalin pumping into the circulation.

answers: NDQ_003358

answers: curse

answers: NDQ_003359

answers: high emotional stress

answers: NDQ_003360

answers: stress.

answers: NDQ_003362

answers: "arrhythmia,

answers: NDQ_003363

answers: high emotional stress

answers: NDQ_003371

answers: In November 1983,

answers: NDQ_003373

answers: high emotional stress

answers: NDQ_003376

answers: stress.

answers: NDQ_003378

answers: stress.

answers: NDQ_003379

answers: "arrhythmia,

answers: NDQ_003380

answers: high emotional stress

answers: NDQ_003381

answers: emotional stress

answers: NDQ_003382

answers: emotional stress

answers: NDQ_003383

answers: high emotional stress

answers: NDQ_003384

answers: "arrhythmia,

answers: NDQ_003385

answers: 1983,

answers: NDQ_003386

answers: "arrhythmia,

answers: NDQ_003387

answers: emotional stress

answers: NDQ_003388

answers: high emotional stress

answers: NDQ_003389

answers: high emotional stress

answers: NDQ_003390

answers: 1983,

answers: NDQ_003391

answers: "arrhythmia,

answers: NDQ_003392

answers: 1983,

answers: NDQ_003393

answers: "arrhythmia,

answers: NDQ_003394

answers: "arrhythmia,

answers: NDQ_003395

answers: electrical malfunction of the heart,

answers: NDQ_003396

answers: "arrhythmia,

text: The thickness of the crust beneath the rift is disputed, as the structures of the rift deep beneath the surface are unknown. The difference in thickness of the crust, between the crust under the rift and that under the surrounding areas, has been bounded to be less than . Although some seismic data is evidence for a rise in the Lithosphere-Asthenosphere boundary, other researchers have claimed that there are deep structures which influence seismic activity, and that the lower crusts is intruded by mafic sills. They interpret the extension as a pure shear process.

text: The thickness of the crust beneath the rift is disputed, as the structures of the rift deep beneath the surface are unknown. The difference in thickness of the crust, between the

text: crust

text: under the rift and that under the surrounding areas, has been bounded to be less than . Although some seismic data is evidence for a rise in the

text: Lithosphere

text: Asthenosphere

text: boundary, other researchers have claimed that there are deep structures which influence seismic activity, and that the lower crusts is intruded by

text: mafic

text: sills

text: . They interpret the extension as a

text: pure shear

text: process.

answers: NDQ_003351

answers: shear

answers: NDQ_003352

answers: increases in thickness

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: rift

answers: NDQ_003356

answers: shrink

answers: NDQ_003357

answers: The difference in thickness of the crust between the crust under the rift and that under the surrounding areas has been bounded to be less than

answers: NDQ_003358

answers: rift

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: seismic waves

answers: NDQ_003362

answers: the thickness of the crust beneath the rift is disputed

answers: NDQ_003363

answers: a pure shear process

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: yes

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: no

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What would happen if the thickness of the crust under the rift is disputed?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: What is the cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: normal faults, extension, or shear?

answers: NDQ_003388

answers: What is the difference in thickness of the crust, between the crust under the rift and that under the surrounding areas?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: rift

answers: NDQ_003391

answers: rift

answers: NDQ_003392

answers: rift

answers: NDQ_003393

answers: surface

answers: NDQ_003394

answers: rift

answers: NDQ_003395

answers: rift with a vertical fault plane

answers: NDQ_003396

answers: rift fault

answers: NDQ_003351

answers: shear

answers: NDQ_003352

answers: shear process.

answers: NDQ_003353

answers: shear

answers: NDQ_003354

answers: The thickness of the crust beneath the rift is disputed,

answers: NDQ_003355

answers: mafic sills.

answers: NDQ_003356

answers: shear process.

answers: NDQ_003357

answers: less than.

answers: NDQ_003358

answers: rift

answers: NDQ_003359

answers: shear process.

answers: NDQ_003360

answers: shear process.

answers: NDQ_003362

answers: The thickness of the crust beneath the rift is disputed,

answers: NDQ_003363

answers: shear process.

answers: NDQ_003371

answers: The thickness of the crust beneath the rift is disputed,

answers: NDQ_003373

answers: mafic sills.

answers: NDQ_003376

answers: shear process.

answers: NDQ_003378

answers: shear

answers: NDQ_003379

answers: The thickness of the crust beneath the rift is disputed,

answers: NDQ_003380

answers: shear process.

answers: NDQ_003381

answers: shear process.

answers: NDQ_003382

answers: shear process.

answers: NDQ_003383

answers: shear

answers: NDQ_003384

answers: mafic sills.

answers: NDQ_003385

answers: The thickness of the crust beneath the rift

answers: NDQ_003386

answers: shear process.

answers: NDQ_003387

answers: shear process.

answers: NDQ_003388

answers: They interpret the extension as a pure shear process.

answers: NDQ_003389

answers: shear process.

answers: NDQ_003390

answers: rift

answers: NDQ_003391

answers: mafic sills.

answers: NDQ_003392

answers: rift

answers: NDQ_003393

answers: mafic sills.

answers: NDQ_003394

answers: The thickness of the crust beneath the rift

answers: NDQ_003395

answers: The thickness of the crust beneath the rift is disputed,

answers: NDQ_003396

answers: shear process.

text: Metamorphic core complexes are exposures of deep crust exhumed in association with largely amagmatic extension.  They form, and are exhumed, through relatively fast transport of middle and lower continental crust to the Earth's surface. During this process, high-grade  metamorphic rocks (eclogite-, granulite- to amphibolite- facies) are exposed below  low-angle detachment faults (mylonite shear zones) that show ductile deformation on the lower side  (footwall) with amphibolite- to greenschist-facies  syndeformational metamorphism, and  ductile-brittle to brittle deformation on the upper-side (hanging-wall) with tilted geometries.

text: Metamorphic core complexes are exposures of deep

text: crust

text: exhumed in association with largely amagmatic extension.  They form, and are exhumed, through relatively fast transport of middle and lower

text: continental crust

text: to the

text: Earth

text: 's surface. During this process, high-grade

text: metamorphic rock

text: s (

text: eclogite

text: granulite

text: - to

text: amphibolite

text: facies

text: ) are exposed below  low-angle

text: detachment fault

text: s (

text: mylonite

text: shear zones) that show

text: ductile

text: deformation on the lower side  (footwall) with

text: amphibolite

text: - to

text: greenschist

text: -facies  syndeformational

text: metamorphism

text: , and  ductile-brittle to

text: brittle

text: deformation on the upper-side (hanging-wall) with

text: tilted

text: geometries.

answers: NDQ_003351

answers: ductile-brittle

answers: NDQ_003352

answers: brittle

answers: NDQ_003353

answers: ductile deformation

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: footwall

answers: NDQ_003356

answers: brittle

answers: NDQ_003357

answers: low-angle detachment faults

answers: NDQ_003358

answers: shear zone

answers: NDQ_003359

answers: deformation on the lower side

answers: NDQ_003360

answers: Earth's surface

answers: NDQ_003362

answers: ductile deformation on the lower side (footwall)

answers: NDQ_003363

answers: metamorphic core complexes

answers: NDQ_003371

answers: Which of the following is not a type of fault: low-angle detachment faults (mylonite shear zones)

answers: NDQ_003373

answers: What type of stresses is a deeply buried rock under?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: What is the amount the ground moves in an earthquake?

answers: NDQ_003379

answers: no

answers: NDQ_003380

answers: What type of force applied to rock is a stress?

answers: NDQ_003381

answers: What does ductile deformation on the lower side (footwall) show

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: What is the cause of earthquakes?

answers: NDQ_003387

answers: no

answers: NDQ_003388

answers: Which of the following is not a type of strike-slip fault: strike-slip faults, detachment faults, or strike-slip faults?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: detachment faults

answers: NDQ_003392

answers: detachment faults

answers: NDQ_003393

answers: granulite

answers: NDQ_003394

answers: low-angle

answers: NDQ_003395

answers: low-angle detachment

answers: NDQ_003396

answers: low-angle detachment

answers: NDQ_003351

answers: ductile

answers: NDQ_003352

answers: ductile-brittle to brittle

answers: NDQ_003353

answers: ductile deformation

answers: NDQ_003354

answers: below low-angle detachment faults

answers: NDQ_003355

answers: (footwall)

answers: NDQ_003356

answers: ductile-brittle to brittle

answers: NDQ_003357

answers: ductile deformation

answers: NDQ_003358

answers: (mylonite shear zones)

answers: NDQ_003359

answers: faults

answers: NDQ_003360

answers: largely amagmatic extension.

answers: NDQ_003362

answers: largely amagmatic extension.

answers: NDQ_003363

answers: amagmatic extension.

answers: NDQ_003371

answers: low-angle detachment faults

answers: NDQ_003373

answers: ductile deformation

answers: NDQ_003376

answers: largely amagmatic extension.

answers: NDQ_003378

answers: ductile deformation

answers: NDQ_003379

answers: low-angle detachment faults

answers: NDQ_003380

answers: ductile deformation

answers: NDQ_003381

answers: ductile

answers: NDQ_003382

answers: largely amagmatic extension.

answers: NDQ_003383

answers: ductile deformation

answers: NDQ_003384

answers: syndeformational metamorphism,

answers: NDQ_003385

answers: (mylonite shear zones)

answers: NDQ_003386

answers: ductile deformation

answers: NDQ_003387

answers: low-angle detachment faults

answers: NDQ_003388

answers: low-angle detachment faults

answers: NDQ_003389

answers: Metamorphic core complexes

answers: NDQ_003390

answers: low-angle detachment faults

answers: NDQ_003391

answers: (mylonite shear zones)

answers: NDQ_003392

answers: low-angle detachment faults

answers: NDQ_003393

answers: (mylonite shear zones)

answers: NDQ_003394

answers: low-angle detachment faults

answers: NDQ_003395

answers: low-angle detachment faults

answers: NDQ_003396

answers: low-angle detachment faults

text: It is a member of the Paediatric Continence Forum, which presses for improvements in paediatric continence care.

text: It is a member of the Paediatric Continence Forum, which presses for improvements in paediatric continence care.

answers: NDQ_003351

answers: helical

answers: NDQ_003352

answers: is likely to crack

answers: NDQ_003353

answers: igneous rocks to form

answers: NDQ_003354

answers: Toroweap Formation is a geologic formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: swell

answers: NDQ_003357

answers: Paediatric Continence Forum presses for improvements in what?

answers: NDQ_003358

answers: rockfall

answers: NDQ_003359

answers: is in contact with it.

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: The San Andreas fault is located in the Pacific Ocean.

answers: NDQ_003363

answers: the same time.

answers: NDQ_003371

answers: What is the reason for the thrust fault?

answers: NDQ_003373

answers: What will happen to the rock?

answers: NDQ_003376

answers: None of the above choices.

answers: NDQ_003378

answers: It is not possible to tell

answers: NDQ_003379

answers: It's impossible to say

answers: NDQ_003380

answers: None of the above choices .

answers: NDQ_003381

answers: What will happen to the rock?

answers: NDQ_003382

answers: no

answers: NDQ_003383

answers: None of the above choices are true

answers: NDQ_003384

answers: None of the above choices.

answers: NDQ_003385

answers: None of the above choices.

answers: NDQ_003386

answers: no

answers: NDQ_003387

answers: None of the above choices.

answers: NDQ_003388

answers: None of the above choices.

answers: NDQ_003389

answers: None of the above choices.

answers: NDQ_003390

answers: can not be used to describe

answers: NDQ_003391

answers: dip-slip fault

answers: NDQ_003392

answers: can't be used

answers: NDQ_003393

answers: dip-slip fault

answers: NDQ_003394

answers: can not be vertical

answers: NDQ_003395

answers: can not be used to describe

answers: NDQ_003396

answers: can be used to describe

answers: NDQ_003351

answers: Paediatric Continence Forum,

answers: NDQ_003352

answers: Paediatric Continence Forum,

answers: NDQ_003353

answers: Paediatric Continence Forum,

answers: NDQ_003354

answers: Paediatric Continence Forum,

answers: NDQ_003355

answers: Paediatric Continence Forum,

answers: NDQ_003356

answers: Paediatric Continence Forum,

answers: NDQ_003357

answers: Paediatric Continence Forum,

answers: NDQ_003358

answers: Paediatric Continence Forum,

answers: NDQ_003359

answers: Paediatric Continence Forum,

answers: NDQ_003360

answers: Paediatric Continence Forum,

answers: NDQ_003362

answers: Paediatric Continence Forum,

answers: NDQ_003363

answers: Paediatric Continence Forum,

answers: NDQ_003371

answers: Paediatric Continence Forum,

answers: NDQ_003373

answers: Paediatric Continence Forum,

answers: NDQ_003376

answers: Paediatric Continence Forum,

answers: NDQ_003378

answers: Paediatric Continence Forum,

answers: NDQ_003379

answers: Paediatric Continence Forum,

answers: NDQ_003380

answers: Paediatric Continence Forum,

answers: NDQ_003381

answers: Paediatric Continence Forum,

answers: NDQ_003382

answers: Paediatric Continence Forum,

answers: NDQ_003383

answers: Paediatric Continence Forum,

answers: NDQ_003384

answers: Paediatric Continence Forum,

answers: NDQ_003385

answers: Paediatric Continence Forum,

answers: NDQ_003386

answers: Paediatric Continence Forum,

answers: NDQ_003387

answers: Paediatric Continence Forum,

answers: NDQ_003388

answers: Paediatric Continence Forum,

answers: NDQ_003389

answers: Paediatric Continence Forum,

answers: NDQ_003390

answers: Paediatric Continence Forum,

answers: NDQ_003391

answers: Paediatric Continence Forum,

answers: NDQ_003392

answers: Paediatric Continence Forum,

answers: NDQ_003393

answers: Paediatric Continence Forum,

answers: NDQ_003394

answers: Paediatric Continence Forum,

answers: NDQ_003395

answers: Paediatric Continence Forum,

answers: NDQ_003396

answers: Paediatric Continence Forum,

text: The researchers in the Seismology, Geology and Tectonophysics Division (SGT) study theoretical and observational seismology, solid Earth dynamics, rock mechanics, structural geology and tectonics, and sedimentary geology. They also contribute to understanding of earthquakes; the structure of Earth’s crust, mantle, and core; and the large-scale motions and deformation of the tectonic plates. In addition, the division operates several facilities for the scientific community. In partnership with the U.S. Geological Survey, SGT operates a network of seismographs throughout the northeastern U.S., supports National Science Foundation (NSF) efforts to conduct ocean-bottom seismology research, and provides accurate earthquake source mechanisms to government and academic researchers around the world.

text: The researchers in the Seismology, Geology and Tectonophysics Division (SGT) study theoretical and observational

text: seismology

text: , solid Earth dynamics, rock mechanics, structural geology and tectonics, and sedimentary geology. They also contribute to understanding of

text: earthquakes

text: ; the structure of Earth’s

text: crust

text: , mantle, and core; and the large-scale motions and deformation of the tectonic plates. In addition, the division operates several facilities for the scientific community. In partnership with the

text: U.S. Geological Survey

text: , SGT operates a network of seismographs throughout the northeastern U.S., supports

text: National Science Foundation

text: (NSF) efforts to conduct ocean-bottom seismology research, and provides accurate earthquake source mechanisms to government and academic researchers around the world.

answers: NDQ_003351

answers: deformation

answers: NDQ_003352

answers: deforms

answers: NDQ_003353

answers: deformation

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: tectonic

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: large-scale motions and deformation of the plates

answers: NDQ_003358

answers: seismograph

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: tectonic plates

answers: NDQ_003362

answers: ocean-bottom seismology research

answers: NDQ_003363

answers: tectonic plates

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: What type of stresses does a deeply buried rock have?

answers: NDQ_003376

answers: What type of terrain is caused by compressive forces?

answers: NDQ_003378

answers: What does SGT contribute to understanding of earthquakes

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What type of force applied to rock is a stress?

answers: NDQ_003381

answers: What type of stress does the Seismology, Geology and Tectonophysics Division study?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: What type of fold is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: What is the structure of Earth’s crust, mantle, and core

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: normal faults, mantle, or core?

answers: NDQ_003388

answers: Which of the following is not a result of shear stress: strike-slip faults, earthquakes, or solid Earth dynamics?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: Tectonic

answers: NDQ_003391

answers: sedimentary

answers: NDQ_003392

answers: Tectonic

answers: NDQ_003393

answers: mantle

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: tectonic plates

answers: NDQ_003396

answers: earthquake source mechanisms

answers: NDQ_003351

answers: tectonic plates.

answers: NDQ_003352

answers: rock mechanics,

answers: NDQ_003353

answers: deformation

answers: NDQ_003354

answers: (SGT) study theoretical and observational seismology,

answers: NDQ_003355

answers: tectonic plates.

answers: NDQ_003356

answers: tectonic plates.

answers: NDQ_003357

answers: tectonic plates.

answers: NDQ_003358

answers: earthquakes;

answers: NDQ_003359

answers: tectonic plates.

answers: NDQ_003360

answers: tectonic plates.

answers: NDQ_003362

answers: ocean-bottom seismology research, and provides accurate earthquake source mechanisms

answers: NDQ_003363

answers: tectonic plates.

answers: NDQ_003371

answers: Seismology, Geology and Tectonophysics Division

answers: NDQ_003373

answers: rock mechanics,

answers: NDQ_003376

answers: tectonic plates.

answers: NDQ_003378

answers: earthquakes;

answers: NDQ_003379

answers: Seismology, Geology and Tectonophysics Division

answers: NDQ_003380

answers: rock mechanics,

answers: NDQ_003381

answers: tectonic plates.

answers: NDQ_003382

answers: tectonic plates.

answers: NDQ_003383

answers: rock mechanics,

answers: NDQ_003384

answers: tectonic plates.

answers: NDQ_003385

answers: earthquakes;

answers: NDQ_003386

answers: tectonic plates.

answers: NDQ_003387

answers: tectonic plates.

answers: NDQ_003388

answers: earthquake source mechanisms

answers: NDQ_003389

answers: tectonic plates.

answers: NDQ_003390

answers: tectonic plates.

answers: NDQ_003391

answers: sedimentary geology.

answers: NDQ_003392

answers: earthquake source mechanisms

answers: NDQ_003393

answers: sedimentary geology.

answers: NDQ_003394

answers: tectonic plates.

answers: NDQ_003395

answers: tectonic plates.

answers: NDQ_003396

answers: tectonic plates.

text: A subduction zone is formed at a convergent plate boundary when one or both of the tectonic plates is composed of oceanic crust.  The denser plate, made of oceanic crust, is subducted underneath the less dense plate, which can be either continental or oceanic crust. When both of the plates are made of oceanic crust, convergence is associated with island arcs such as the Solomon Islands.

text: A subduction zone is formed at a convergent plate boundary when one or both of the tectonic plates is composed of

text: oceanic crust

text: .  The denser plate, made of oceanic crust, is subducted underneath the less dense plate, which can be either continental or oceanic crust. When both of the plates are made of oceanic crust, convergence is associated with

text: island arcs

text: such as the

text: Solomon Islands

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: denser

answers: NDQ_003353

answers: subduction

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: arc

answers: NDQ_003356

answers: subduct

answers: NDQ_003357

answers: The denser plate is subducted underneath the less dense plate

answers: NDQ_003358

answers: unanswerable

answers: NDQ_003359

answers: subducted underneath the less dense plate

answers: NDQ_003360

answers: oceanic crust

answers: NDQ_003362

answers: When both of the plates are made of oceanic crust, convergence is associated with island arcs

answers: NDQ_003363

answers: subduction zone

answers: NDQ_003371

answers: What is a subduction zone?

answers: NDQ_003373

answers: subducted underneath the less dense plate

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What is the result of confining stress?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: unanswerable

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: Which of the following is not a result of shear stress?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: subduction zone

answers: NDQ_003391

answers: subducted

answers: NDQ_003392

answers: subduction zone

answers: NDQ_003393

answers: subducted

answers: NDQ_003394

answers: convergent

answers: NDQ_003395

answers: is associated with island arcs

answers: NDQ_003396

answers: subduction zone

answers: NDQ_003351

answers: oceanic crust.

answers: NDQ_003352

answers: subducted underneath the less dense

answers: NDQ_003353

answers: subduction zone

answers: NDQ_003354

answers: A subduction zone

answers: NDQ_003355

answers: arcs

answers: NDQ_003356

answers: subduction zone

answers: NDQ_003357

answers: subducted underneath the less dense plate,

answers: NDQ_003358

answers: subduction zone

answers: NDQ_003359

answers: subduction zone

answers: NDQ_003360

answers: tectonic plates is composed of oceanic crust.

answers: NDQ_003362

answers: convergence is associated with island arcs

answers: NDQ_003363

answers: subduction zone

answers: NDQ_003371

answers: A subduction zone

answers: NDQ_003373

answers: A subduction zone

answers: NDQ_003376

answers: A subduction zone

answers: NDQ_003378

answers: A subduction zone

answers: NDQ_003379

answers: oceanic crust.

answers: NDQ_003380

answers: A subduction zone

answers: NDQ_003381

answers: A subduction zone

answers: NDQ_003382

answers: oceanic crust.

answers: NDQ_003383

answers: A subduction zone

answers: NDQ_003384

answers: island arcs

answers: NDQ_003385

answers: subduction zone

answers: NDQ_003386

answers: subduction zone

answers: NDQ_003387

answers: A subduction zone

answers: NDQ_003388

answers: oceanic crust.

answers: NDQ_003389

answers: island arcs

answers: NDQ_003390

answers: subduction zone

answers: NDQ_003391

answers: subduction zone

answers: NDQ_003392

answers: subduction zone

answers: NDQ_003393

answers: subduction zone

answers: NDQ_003394

answers: A subduction zone

answers: NDQ_003395

answers: subduction zone

answers: NDQ_003396

answers: subduction zone

text: Human activities have a major effect on the global sulfur cycle.  The burning of coal, natural gas, and other fossil fuels has greatly increased the amount of S in the atmosphere and ocean and depleted the sedimentary rock sink.  Without human impact sulfur would stay tied up in rocks for millions of years until it was uplifted through tectonic events and then released through erosion and weathering processes.  Instead it is being drilled, pumped and burned at a steadily increasing rate.  Over the most polluted areas there has been a 30-fold increase in sulfate deposition.   	Although the sulfur curve shows shifts between net sulfur oxidation and net sulfur reduction in the geologic past, the magnitude of the current human impact is probably unprecedented in the geologic record.  Human activities greatly increase the flux of sulfur to the atmosphere, some of which is transported globally.  Humans are mining coal and extracting petroleum from the Earth's crust at a rate that mobilizes 150 x 10 gS/yr, which is more than double the rate of 100 years ago.  The result of human impact on these processes is to increase the pool of oxidized sulfur (SO) in the global cycle, at the expense of the storage of reduced sulfur in the Earth's crust.  Therefore, human activities do not cause a major change in the global pools of S, but they do produce massive changes in the annual flux of S through the atmosphere.	When SO is emitted as an air pollutant, it forms sulfuric acid through reactions with water in the atmosphere.  Once the acid is completely dissociated in water the pH can drop to 4.3 or lower causing damage to both man-made and natural systems.  According to the EPA, acid rain is a broad term referring to a mixture of wet and dry deposition (deposited material) from the atmosphere containing higher than normal amounts of nitric and sulfuric acids.  Distilled water (water without any dissolved constituents), which contains no carbon dioxide, has a neutral pH of 7.  Rain naturally has a slightly acidic pH of 5.6, because carbon dioxide and water in the air react together to form carbonic acid, a very weak acid. Around Washington, D.C., however, the average rain pH is between 4.2 and 4.4.  Since pH is on a log scale dropping by 1 (the difference between normal rain water and acid rain) has a dramatic effect on the strength of the acid.  In the United States, roughly 2/3 of all SO and 1/4 of all NO come from electric power generation that relies on burning fossil fuels, like coal.

text: Human activities have a major effect on the global sulfur cycle.  The burning of

text: coal

text: natural gas

text: , and other

text: fossil fuel

text: s has greatly increased the amount of S in the atmosphere and ocean and depleted the sedimentary rock sink.  Without human impact sulfur would stay tied up in rocks for millions of years until it was uplifted through

text: tectonic

text: events and then released through

text: erosion

text: and

text: weathering

text: processes.  Instead it is being drilled, pumped and burned at a steadily increasing rate.  Over the most polluted areas there has been a 30-fold increase in sulfate deposition.   	Although the sulfur curve shows shifts between net sulfur oxidation and net sulfur reduction in the geologic past, the magnitude of the current human impact is probably unprecedented in the geologic record.  Human activities greatly increase the flux of sulfur to the

text: atmosphere

text: , some of which is transported globally.  Humans are mining coal and extracting petroleum from the

text: Earth's crust

text: at a rate that mobilizes 150 x 10 gS/yr, which is more than double the rate of 100 years ago.  The result of human impact on these processes is to increase the pool of oxidized sulfur (SO) in the global cycle, at the expense of the storage of reduced sulfur in the Earth's crust.  Therefore, human activities do not cause a major change in the global pools of S, but they do produce massive changes in the annual flux of S through the atmosphere.	When SO is emitted as an air pollutant, it forms

text: sulfuric acid

text: through reactions with water in the atmosphere.  Once the acid is completely dissociated in water the

text: pH

text: can drop to 4.3 or lower causing damage to both man-made and natural systems.  According to the EPA,

text: acid rain

text: is a broad term referring to a mixture of wet and dry deposition (deposited material) from the atmosphere containing higher than normal amounts of nitric and sulfuric acids.  Distilled water (water without any dissolved constituents), which contains no

text: carbon dioxide

text: , has a neutral pH of 7.  Rain naturally has a slightly acidic pH of 5.6, because carbon dioxide and water in the air react together to form carbonic acid, a very weak acid. Around Washington, D.C., however, the average rain pH is between 4.2 and 4.4.  Since pH is on a log scale dropping by 1 (the difference between normal rain water and acid rain) has a dramatic effect on the strength of the acid.  In the United States, roughly 2/3 of all SO and 1/4 of all NO come from electric power generation that relies on burning fossil fuels, like coal.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: has a higher pH

answers: NDQ_003353

answers: erosion and weathering

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: erode

answers: NDQ_003357

answers: sulfur would stay tied up in rocks for millions of years

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: is pushed together

answers: NDQ_003360

answers: tectonic events

answers: NDQ_003362

answers: Human activities greatly increase the flux of sulfur to the atmosphere

answers: NDQ_003363

answers: tectonic events

answers: NDQ_003371

answers: unanswerable

answers: NDQ_003373

answers: It is subjected to tectonic forces.

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: vertical

answers: NDQ_003380

answers: Which of the following is not a stress?

answers: NDQ_003381

answers: Which of the following is not a type of constraining stress?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: Which of the following is not a type of fold?

answers: NDQ_003385

answers: What is the term for an area where faults are clustered?

answers: NDQ_003386

answers: Which of the following is not a cause of earthquakes?

answers: NDQ_003387

answers: without human impact

answers: NDQ_003388

answers: Which of the following is not a result of shear stress?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: tectonic

answers: NDQ_003391

answers: sedimentary rock sink

answers: NDQ_003392

answers: tectonic

answers: NDQ_003393

answers: sedimentary rock sink

answers: NDQ_003394

answers: lateral fault

answers: NDQ_003395

answers: tectonic

answers: NDQ_003396

answers: horizontal fault

answers: NDQ_003351

answers: 5.6,

answers: NDQ_003352

answers: uplifted

answers: NDQ_003353

answers: 5.6,

answers: NDQ_003354

answers: 4.3

answers: NDQ_003355

answers: 5.6,

answers: NDQ_003356

answers: 5.6,

answers: NDQ_003357

answers: tectonic events

answers: NDQ_003358

answers: sedimentary rock sink.

answers: NDQ_003359

answers: 5.6,

answers: NDQ_003360

answers: tectonic events

answers: NDQ_003362

answers: 5.6,

answers: NDQ_003363

answers: tectonic events

answers: NDQ_003371

answers: tectonic events

answers: NDQ_003373

answers: 5.6,

answers: NDQ_003376

answers: acid rain

answers: NDQ_003378

answers: 5.6,

answers: NDQ_003379

answers: 5.6,

answers: NDQ_003380

answers: 5.6,

answers: NDQ_003381

answers: 5.6,

answers: NDQ_003382

answers: 5.6,

answers: NDQ_003383

answers: human activities

answers: NDQ_003384

answers: 5.6,

answers: NDQ_003385

answers: 5.6,

answers: NDQ_003386

answers: 5.6,

answers: NDQ_003387

answers: human activities

answers: NDQ_003388

answers: 5.6,

answers: NDQ_003389

answers: 5.6,

answers: NDQ_003390

answers: 5.6,

answers: NDQ_003391

answers: 5.6,

answers: NDQ_003392

answers: 5.6,

answers: NDQ_003393

answers: 5.6,

answers: NDQ_003394

answers: 5.6,

answers: NDQ_003395

answers: 5.6,

answers: NDQ_003396

answers: 5.6,

text: In the quoted section, the stressed syllables have been underlined. (Normally, the stressed syllable must be long if followed by another syllable in a word.  However, by a rule known as syllable resolution, two short syllables in a single word are considered equal to a single long syllable.  Hence, sometimes two syllables have been underlined, as in hige and mægen.) The first three half-lines have the type A pattern "DUM-da-(da-)DUM-da", while the last one has the type C pattern "da-(da-da-)DUM-DUM-da", with parentheses indicating optional unstressed syllables that have been inserted.  Note also the pervasive pattern of alliteration, where the first and/or second stress alliterate with the third, but not with the fourth.

text: In the quoted section, the stressed syllables have been underlined. (Normally, the stressed syllable must be long if followed by another syllable in a word.  However, by a rule known as syllable resolution, two short syllables in a single word are considered equal to a single long syllable.  Hence, sometimes two syllables have been underlined, as in hige and mægen.) The first three half-lines have the

text: type A

text: pattern "DUM-da-(da-)DUM-da", while the last one has the type C pattern "da-(da-da-)DUM-DUM-da", with parentheses indicating optional unstressed syllables that have been inserted.  Note also the pervasive pattern of alliteration, where the first and/or second stress alliterate with the third, but not with the fourth.

answers: NDQ_003351

answers: DUM-da-(da-)DUM

answers: NDQ_003352

answers: As a rock experiences more stress it

answers: NDQ_003353

answers: Stresses change rock

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation.

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: When rocks deform plastically, they tend to

answers: NDQ_003357

answers: DUM-da-(da-)DUM-da

answers: NDQ_003358

answers: A place where rock breaks but doesnt move it is called a

answers: NDQ_003359

answers: A fracture becomes a fault only if rock

answers: NDQ_003360

answers: Grand Tetons in Wyoming, are uplifted on

answers: NDQ_003362

answers: underlined, as in hige and m gen

answers: NDQ_003363

answers: Most of the worlds largest mountains formed

answers: NDQ_003371

answers: If very old rocks are above much younger rocks there may be a thrust fault in between.

answers: NDQ_003373

answers: A deeply buried rock is under compressive stresses.

answers: NDQ_003376

answers: The terrain known as basin-and-range is caused by compressive forces.

answers: NDQ_003378

answers: The amount the ground moves in an earthquake is called slip.

answers: NDQ_003379

answers: In a strike-slip fault, the dip of the fault plane is vertical

answers: NDQ_003380

answers: Any force applied to rock is a stress.

answers: NDQ_003381

answers: When confining stress occurs, rock deforms.

answers: NDQ_003382

answers: Compression is the most common stress at convergent plates

answers: NDQ_003383

answers: Stress is the cause of joints in rock.

answers: NDQ_003384

answers: syncline

answers: NDQ_003385

answers: Fault zone

answers: NDQ_003386

answers: Movement of rock at faults is the cause of earthquakes.

answers: NDQ_003387

answers: DUM-da-(da-)DUM-da

answers: NDQ_003388

answers: Strike-slip faults result from shear stress.

answers: NDQ_003389

answers: Only the process of folding creates mountain ranges.

answers: NDQ_003390

answers: fault in which the hanging wall drops down relative to the footwall

answers: NDQ_003391

answers: block of rock that is beneath a dip-slip fault plane

answers: NDQ_003392

answers: fault in which the hanging wall pushes up relative to the footwall

answers: NDQ_003393

answers: block of rock that is above a dip-slip fault plane

answers: NDQ_003394

answers: fault with a fault plane that is not vertical

answers: NDQ_003395

answers: fault with a vertical fault plane

answers: NDQ_003396

answers: reverse fault in which the fault plane is nearly horizontal

answers: NDQ_003351

answers: alliteration,

answers: NDQ_003352

answers: alliteration,

answers: NDQ_003353

answers: alliteration,

answers: NDQ_003354

answers: alliteration,

answers: NDQ_003355

answers: half-lines

answers: NDQ_003356

answers: "da-(da-da-)DUM-DUM-da",

answers: NDQ_003357

answers: the stressed syllable must be long

answers: NDQ_003358

answers: hige and m<unk>gen.)

answers: NDQ_003359

answers: long if followed by another syllable in a word.

answers: NDQ_003360

answers: alliteration,

answers: NDQ_003362

answers: two short syllables

answers: NDQ_003363

answers: hige and m<unk>gen.)

answers: NDQ_003371

answers: "da-(da-da-)DUM-DUM-da",

answers: NDQ_003373

answers: "da-(da-da-)DUM-DUM-da",

answers: NDQ_003376

answers: "da-(da-da-)DUM-DUM-da",

answers: NDQ_003378

answers: "da-(da-da-)DUM-DUM-da",

answers: NDQ_003379

answers: "da-(da-da-)DUM-DUM-da",

answers: NDQ_003380

answers: stress

answers: NDQ_003381

answers: "da-(da-da-)DUM-DUM-da",

answers: NDQ_003382

answers: alliteration,

answers: NDQ_003383

answers: stress alliterate with the third, but not with the fourth.

answers: NDQ_003384

answers: half-lines

answers: NDQ_003385

answers: syllable resolution,

answers: NDQ_003386

answers: "da-(da-da-)DUM-DUM-da",

answers: NDQ_003387

answers: syllable resolution,

answers: NDQ_003388

answers: "da-(da-da-)DUM-DUM-da",

answers: NDQ_003389

answers: "da-(da-da-)DUM-DUM-da",

answers: NDQ_003390

answers: hige and m<unk>gen.)

answers: NDQ_003391

answers: "da-(da-da-)DUM-DUM-da",

answers: NDQ_003392

answers: hige and m<unk>gen.)

answers: NDQ_003393

answers: "da-(da-da-)DUM-DUM-da",

answers: NDQ_003394

answers: fourth.

answers: NDQ_003395

answers: "da-(da-da-)DUM-DUM-da",

answers: NDQ_003396

answers: "da-(da-da-)DUM-DUM-da",

text: The formation of the Intermontane Belt is complex. It began forming during the early Jurassic period when an island arc  called the Intermontane Islands collided against a pre-existing continental margin. This island arc is believed to have formed on a pre-existing tectonic plate called the Intermontane Plate about 245 million years ago by subduction of the former Insular Plate during the Triassic period. This subduction zone records another subduction zone called the Intermontane Trench under an ancient ocean between the Intermontane Islands and the former continental margin of North America called the Slide Mountain Ocean. This arrangement of two parallel subduction zones is unusual because very few twin subduction zones exist on Earth; the Philippine Mobile Belt off the eastern coast of Asia is an example of a modern twin subduction zone. As the Intermontane Plate drew closer to the pre-existing continental margin by ongoing subduction under the Slide Mountain Ocean, the Intermontane Islands drew closer to the former continental margin and coastline of western North America, supporting a pre-existing volcanic arc on the former continental margin of North America. As the North American Plate drifted west and the Intermontane Plate drifted east to the ancient continental margin of western North America, the Slide Mountain Ocean eventually closed by ongoing subduction under the Slide Mountain Ocean. The subduction zone eventually jammed and shut down completely about 180 million years ago, ending the volcanic arc on the ancient continental margin of western North America and the Intermontane Islands collided, forming the Intermontane Belt. This collision crushed and folded sedimentary and igneous rocks, creating a mountain range called the Kootenay Fold Belt which existed in far eastern Washington State and British Columbia.

text: The formation of the Intermontane Belt is complex. It began forming during the early

text: Jurassic

text: period when an

text: island arc

text: called the

text: Intermontane Islands

text: collided against a pre-existing

text: continental margin

text: . This island arc is believed to have formed on a pre-existing

text: tectonic plate

text: called the

text: Intermontane Plate

text: about 245 million years ago by

text: subduction

text: of the former

text: Insular Plate

text: during the

text: Triassic

text: period. This subduction zone records another subduction zone called the

text: Intermontane Trench

text: under an ancient ocean between the Intermontane Islands and the former continental margin of North America called the

text: Slide Mountain Ocean

text: . This arrangement of two parallel subduction zones is unusual because very few twin subduction zones exist on Earth; the

text: Philippine Mobile Belt

text: off the eastern coast of

text: Asia

text: is an example of a modern twin subduction zone. As the Intermontane Plate drew closer to the pre-existing continental margin by ongoing

text: subduction

text: under the Slide Mountain Ocean, the Intermontane Islands drew closer to the former continental margin and coastline of western North America, supporting a pre-existing volcanic arc on the former continental margin of North America. As the

text: North American Plate

text: drifted west and the Intermontane Plate drifted east to the ancient continental margin of western North America, the Slide Mountain Ocean eventually closed by ongoing subduction under the Slide Mountain Ocean. The subduction zone eventually jammed and shut down completely about 180 million years ago, ending the volcanic arc on the ancient continental margin of western North America and the Intermontane Islands collided, forming the Intermontane Belt. This collision crushed and

text: fold

text: ed

text: sedimentary

text: and

text: igneous rock

text: s, creating a

text: mountain range

text: called the

text: Kootenay Fold Belt

text: which existed in far eastern

text: Washington

text: State and British Columbia.

answers: NDQ_003351

answers: subduction

answers: NDQ_003352

answers: folds

answers: NDQ_003353

answers: subduction

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: mountain range

answers: NDQ_003356

answers: fold

answers: NDQ_003357

answers: subduction of the former Insular Plate occurs when

answers: NDQ_003358

answers: subduction zone

answers: NDQ_003359

answers: collides

answers: NDQ_003360

answers: tectonic plates

answers: NDQ_003362

answers: very few twin subduction zones exist on Earth

answers: NDQ_003363

answers: Kootenay Fold Belt

answers: NDQ_003371

answers: What is an example of a thrust fault in between?

answers: NDQ_003373

answers: What is the Intermontane Trench?

answers: NDQ_003376

answers: Which of the following is not a type of terrain: basin-and-range or mountain range?

answers: NDQ_003378

answers: How many parallel subduction zones exist on Earth

answers: NDQ_003379

answers: Which of the following is not a type of strike-slip fault?

answers: NDQ_003380

answers: Which of the following is not an example of twin subduction zones?

answers: NDQ_003381

answers: What is the main idea of this passage?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the main idea of this passage?

answers: NDQ_003384

answers: What type of fold is the Kootenay Fold Belt?

answers: NDQ_003385

answers: What is the name of the intermontane plate?

answers: NDQ_003386

answers: Which of the following is not an example of a modern twin subduction zone?

answers: NDQ_003387

answers: Which of the following is not an example of a modern twin subduction zone?

answers: NDQ_003388

answers: Which of the following is not an example of a modern twin subduction zone?

answers: NDQ_003389

answers: It is not possible to tell

answers: NDQ_003390

answers: Kootenay Fold Belt

answers: NDQ_003391

answers: intermontane plate

answers: NDQ_003392

answers: tectonic plate

answers: NDQ_003393

answers: tectonic plate

answers: NDQ_003394

answers: tectonic plate

answers: NDQ_003395

answers: tectonic plate

answers: NDQ_003396

answers: intermontane trench

answers: NDQ_003351

answers: subduction

answers: NDQ_003352

answers: crushed and folded

answers: NDQ_003353

answers: crushed and folded

answers: NDQ_003354

answers: Kootenay Fold Belt

answers: NDQ_003355

answers: Kootenay Fold Belt

answers: NDQ_003356

answers: crushed and folded sedimentary and igneous rocks,

answers: NDQ_003357

answers: subduction

answers: NDQ_003358

answers: Kootenay Fold Belt

answers: NDQ_003359

answers: crushed and folded sedimentary and igneous rocks,

answers: NDQ_003360

answers: coastline of western North America,

answers: NDQ_003362

answers: pre-existing volcanic arc

answers: NDQ_003363

answers: volcanic arc on the former continental margin of North America.

answers: NDQ_003371

answers: Kootenay Fold Belt

answers: NDQ_003373

answers: sedimentary and igneous rocks,

answers: NDQ_003376

answers: sedimentary

answers: NDQ_003378

answers: subduction

answers: NDQ_003379

answers: North American Plate

answers: NDQ_003380

answers: crushed and folded sedimentary and igneous rocks,

answers: NDQ_003381

answers: folded sedimentary and igneous rocks,

answers: NDQ_003382

answers: subduction

answers: NDQ_003383

answers: crushed and folded

answers: NDQ_003384

answers: Kootenay Fold Belt

answers: NDQ_003385

answers: North American Plate

answers: NDQ_003386

answers: subduction

answers: NDQ_003387

answers: subduction

answers: NDQ_003388

answers: North American Plate

answers: NDQ_003389

answers: Kootenay Fold Belt

answers: NDQ_003390

answers: subduction

answers: NDQ_003391

answers: Slide Mountain Ocean.

answers: NDQ_003392

answers: Kootenay Fold Belt

answers: NDQ_003393

answers: Intermontane Plate

answers: NDQ_003394

answers: subduction

answers: NDQ_003395

answers: subduction

answers: NDQ_003396

answers: subduction

text: Earth's crust is composed of 90% silicate minerals and their abundance in the Earth is as follows: plagioclase feldspar (39%), alkali feldspar (12%), quartz (12%), pyroxene (11%), amphiboles (5%), micas (5%), clay minerals (5%); the remaining silicate minerals make up another 3% of Earth's crust.  Only 8% of the Earth is composed of non-silicate minerals such as carbonates, oxides, and sulfides.

text: Earth's crust is composed of 90% silicate minerals and their abundance in the Earth is as follows:

text: plagioclase feldspar

text: alkali feldspar

text: (12%), quartz (12%),

text: pyroxene

text: amphiboles

text: micas

text: clay minerals

text: (5%); the remaining silicate minerals make up another 3% of Earth's crust.  Only 8% of the Earth is composed of non-silicate minerals such as

text: carbonates

text: oxides

text: , and

text: sulfides

answers: NDQ_003351

answers: alkali feldspar

answers: NDQ_003352

answers: is likely to be made of silicate minerals

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: pyroxene

answers: NDQ_003357

answers: plagioclase feldspar and alkali feldspar are the same

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: only 8% of the Earth is composed of non-silicate minerals

answers: NDQ_003363

answers: alkali feldspar

answers: NDQ_003371

answers: How many percent of the Earth's crust is composed of non-silicate minerals?

answers: NDQ_003373

answers: how many percent of earth's crust is composed of silicate minerals

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: 5%

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: How many percent of the Earth's crust is composed of non-silicate minerals?

answers: NDQ_003381

answers: How many percent of the Earth is composed of non-silicate minerals?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: How many percent of the Earth's crust is composed of non-silicate minerals?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: faults are clustered

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: How many percent of Earth's crust is composed of non-silicate minerals?

answers: NDQ_003388

answers: how many percent of earth's crust is composed of non-silicate minerals

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: unanswerable

answers: NDQ_003392

answers: a fault

answers: NDQ_003393

answers: Earth's crust

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: pyroxene

answers: NDQ_003396

answers: amphiboles

answers: NDQ_003351

answers: silicate minerals

answers: NDQ_003352

answers: 8% of the Earth is composed of non-silicate minerals

answers: NDQ_003353

answers: 90% silicate minerals

answers: NDQ_003354

answers: Earth's crust is composed of 90% silicate minerals

answers: NDQ_003355

answers: Earth's

answers: NDQ_003356

answers: pyroxene (11%), amphiboles

answers: NDQ_003357

answers: 8%

answers: NDQ_003358

answers: Earth's crust

answers: NDQ_003359

answers: Earth's crust is composed of 90% silicate minerals

answers: NDQ_003360

answers: silicate minerals

answers: NDQ_003362

answers: Earth's crust is composed of 90% silicate minerals

answers: NDQ_003363

answers: Earth's crust is composed of 90% silicate minerals

answers: NDQ_003371

answers: Earth's crust is composed of 90% silicate minerals

answers: NDQ_003373

answers: Earth's crust is composed of 90% silicate minerals

answers: NDQ_003376

answers: 8%

answers: NDQ_003378

answers: 3%

answers: NDQ_003379

answers: 3%

answers: NDQ_003380

answers: 8%

answers: NDQ_003381

answers: 3%

answers: NDQ_003382

answers: 3%

answers: NDQ_003383

answers: 90% silicate minerals

answers: NDQ_003384

answers: 8%

answers: NDQ_003385

answers: 3%

answers: NDQ_003386

answers: Earth's crust is composed of 90% silicate minerals

answers: NDQ_003387

answers: 3%

answers: NDQ_003388

answers: 90% silicate minerals

answers: NDQ_003389

answers: 8%

answers: NDQ_003390

answers: 3%

answers: NDQ_003391

answers: quartz (12%), pyroxene

answers: NDQ_003392

answers: 3%

answers: NDQ_003393

answers: quartz (12%), pyroxene

answers: NDQ_003394

answers: Earth's

answers: NDQ_003395

answers: 3%

answers: NDQ_003396

answers: pyroxene

text: The main reason for the slowing down of the Earth's rotation is tidal friction, which alone would lengthen the day by 2.3 ms/century. Other contributing factors are the movement of the Earth's crust relative to its core, changes in mantle convection, and any other events or processes that cause a significant redistribution of mass. These processes change the Earth's moment of inertia, affecting the rate of rotation due to conservation of angular momentum, sometimes increasing earth's rotational speed (decreasing the solar day and opposing tidal friction). For example, glacial rebound shortens the solar day by 0.6 ms/century and the 2004 Indian Ocean earthquake is thought to have shortened it by 2.68 microseconds.  It is evident from the figure that the Earth has actually sped up since the initiation of the current system in 1971, and the rate of leap second insertions has therefore been decreasing.

text: The main reason for the slowing down of the Earth's rotation is

text: tidal friction

text: , which alone would lengthen the day by 2.3 ms/century. Other contributing factors are the movement of the Earth's

text: crust

text: relative to its

text: core

text: , changes in

text: mantle convection

text: , and any other events or processes that cause a significant redistribution of mass. These processes change the Earth's

text: moment of inertia

text: , affecting the rate of rotation due to conservation of

text: angular momentum

text: , sometimes increasing earth's rotational speed (decreasing the solar day and opposing tidal friction). For example,

text: glacial rebound

text: shortens the solar day by 0.6 ms/century and the

entity_name: 2004 Indian Ocean earthquake and tsunami

text: 2004 Indian Ocean earthquake

text: is thought to have shortened it by 2.68 microseconds.  It is evident from the figure that the Earth has actually sped up since the initiation of the current system in 1971, and the rate of leap second insertions has therefore been decreasing.

answers: NDQ_003351

answers: glacial rebound

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: significant redistribution of mass

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: glacial rebound

answers: NDQ_003356

answers: change the Earth's moment of inertia

answers: NDQ_003357

answers: glacial rebound shortens the solar day by

answers: NDQ_003358

answers: glacial rebound

answers: NDQ_003359

answers: movement

answers: NDQ_003360

answers: mantle convection

answers: NDQ_003362

answers: Earth has actually sped up since the initiation of the current system in 1971

answers: NDQ_003363

answers: tidal friction

answers: NDQ_003371

answers: What is the main reason for the slowing down of the Earth's rotation?

answers: NDQ_003373

answers: unanswerable

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: vertical

answers: NDQ_003380

answers: What does glacial rebound shorten the solar day by?

answers: NDQ_003381

answers: What does glacial rebound shorten the solar day by?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: unanswerable

answers: NDQ_003386

answers: movement of the Earth's crust relative to its core

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: unanswerable

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: glacial rebound

answers: NDQ_003391

answers: mantle

answers: NDQ_003392

answers: glacial rebound

answers: NDQ_003393

answers: mantle

answers: NDQ_003394

answers: non-vertical

answers: NDQ_003395

answers: unanswerable

answers: NDQ_003396

answers: glacial rebound

answers: NDQ_003351

answers: tidal friction,

answers: NDQ_003352

answers: a significant redistribution of mass.

answers: NDQ_003353

answers: the Earth's moment of inertia,

answers: NDQ_003354

answers: the Earth has actually sped up

answers: NDQ_003355

answers: glacial rebound

answers: NDQ_003356

answers: glacial rebound shortens the solar day

answers: NDQ_003357

answers: 0.6 ms/century

answers: NDQ_003358

answers: glacial rebound

answers: NDQ_003359

answers: movement of the Earth's crust relative to its core,

answers: NDQ_003360

answers: changes in mantle convection,

answers: NDQ_003362

answers: the Earth has actually sped up

answers: NDQ_003363

answers: 2004 Indian Ocean

answers: NDQ_003371

answers: tidal friction,

answers: NDQ_003373

answers: tidal friction,

answers: NDQ_003376

answers: movement of the Earth's crust relative to its core,

answers: NDQ_003378

answers: movement of the Earth's crust relative to its core,

answers: NDQ_003379

answers: 2.3 ms/century.

answers: NDQ_003380

answers: movement of the Earth's crust relative to its core,

answers: NDQ_003381

answers: change the Earth's moment of inertia,

answers: NDQ_003382

answers: tidal friction,

answers: NDQ_003383

answers: movement of the Earth's crust relative to its core,

answers: NDQ_003384

answers: tidal friction,

answers: NDQ_003385

answers: tidal friction,

answers: NDQ_003386

answers: movement of the Earth's crust relative to its core,

answers: NDQ_003387

answers: tidal friction,

answers: NDQ_003388

answers: tidal friction,

answers: NDQ_003389

answers: tidal friction,

answers: NDQ_003390

answers: earthquake

answers: NDQ_003391

answers: glacial rebound

answers: NDQ_003392

answers: glacial rebound

answers: NDQ_003393

answers: glacial rebound

answers: NDQ_003394

answers: 2.3 ms/century.

answers: NDQ_003395

answers: 2.3 ms/century.

answers: NDQ_003396

answers: glacial rebound

text: The Wyoming province can be subdivided into three subprovinces, namely, from oldest to youngest, the Montana metasedimentary province, the Beartooth-Bighorn magmatic zone, and the Southern accreted terranes. Archean rocks of the Montana metasedimentary province and the Beartooth-Bighorn magmatic zone are characterized by (1) their antiquity (rock ages to 3.5 Ga, detrital zircon ages up to 4.0 Ga, and Nd model ages exceeding 4.0 Ga); (2) a distinctly enriched 207Pb/204Pb isotopic signature, which suggests that this part of the province was not produced by the amalgamation of already-formed exotic terranes; and (3) a distinctively thick (15–20 km), mafic lower crust. The Montana metasedimentary province and Beartooth-Bighorn magmatic zone were established as cratons by about 3.0–2.8 Ga. Crustal growth occurred through a combination of continental-arc magmatism resulting from oceanic crust subducted beneath continental crust on an adjacent plate, creating an arc-shaped mountain belt, together with terrane accretion in the Southern accreted terranes along the southern margin of the province at 2.68–2.50 Ga. By the end of the Archean, the three subprovinces were joined as part of what is now the Wyoming craton. Subsequent to amalgamation of the Wyoming crust to Laurentia at ca. 1.8–1.9 Ga, Paleoproterozoic crust (1.7–2.4 Ga) was juxtaposed along the southern and western boundaries of the province. Subsequent tectonism and magmatism in the Wyoming region are concentrated in the areas underlain by these Proterozoic mobile belts.

text: The Wyoming

text: province

text: can be subdivided into three subprovinces, namely, from oldest to youngest, the Montana metasedimentary province, the Beartooth-Bighorn magmatic zone, and the Southern accreted terranes. Archean rocks of the Montana metasedimentary province and the Beartooth-Bighorn magmatic zone are characterized by (1) their antiquity (rock ages to 3.5 Ga,

text: detrital

text: zircon

text: ages up to 4.0 Ga, and

text: Nd model

text: ages exceeding 4.0 Ga); (2) a distinctly enriched 207

text: Pb

text: isotopic

text: signature, which suggests that this part of the province was not produced by the amalgamation of already-formed exotic terranes; and (3) a distinctively thick (15–20 km),

text: mafic

text: lower crust. The Montana metasedimentary province and Beartooth-Bighorn magmatic zone were established as cratons by about 3.0–2.8 Ga. Crustal growth occurred through a combination of

text: continental-arc

text: magmatism resulting from oceanic crust subducted beneath continental crust on an adjacent plate, creating an arc-shaped mountain belt, together with

text: terrane accretion

text: in the Southern accreted terranes along the southern margin of the province at 2.68–2.50 Ga. By the end of the Archean, the three subprovinces were joined as part of what is now the Wyoming craton. Subsequent to amalgamation of the Wyoming crust to Laurentia at ca. 1.8–1.9 Ga, Paleoproterozoic crust (1.7–2.4 Ga) was juxtaposed along the southern and western boundaries of the province. Subsequent tectonism and magmatism in the Wyoming region are concentrated in the areas underlain by these Proterozoic mobile belts.

answers: NDQ_003351

answers: tectonism

answers: NDQ_003352

answers: ages

answers: NDQ_003353

answers: tectonic movement

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: mountain belt

answers: NDQ_003356

answers: age to 3.5 Ga

answers: NDQ_003357

answers: The Wyoming province can be subdivided into three subprovinces

answers: NDQ_003358

answers: craton

answers: NDQ_003359

answers: subducted beneath continental crust

answers: NDQ_003360

answers: plate boundaries

answers: NDQ_003362

answers: a distinctively thick (15–20 km), mafic lower crust

answers: NDQ_003363

answers: Wyoming

answers: NDQ_003371

answers: What may be a thrust fault in between

answers: NDQ_003373

answers: Why is the Wyoming province subdivided into three subprovinces

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What type of rock deforms?

answers: NDQ_003382

answers: What is the most common stress at convergent plates

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: tectonism

answers: NDQ_003387

answers: What are normal faults caused by?

answers: NDQ_003388

answers: Which of the following is not a type of strike-slip fault?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: tectonism

answers: NDQ_003391

answers: craton

answers: NDQ_003392

answers: tectonism

answers: NDQ_003393

answers: craton

answers: NDQ_003394

answers: tectonism

answers: NDQ_003395

answers: Wyoming craton

answers: NDQ_003396

answers: tectonism

answers: NDQ_003351

answers: tectonism

answers: NDQ_003352

answers: arc-shaped mountain belt,

answers: NDQ_003353

answers: arc-shaped mountain belt,

answers: NDQ_003354

answers: continental-arc magmatism

answers: NDQ_003355

answers: arc-shaped mountain belt,

answers: NDQ_003356

answers: arc-shaped mountain belt,

answers: NDQ_003357

answers: adjacent plate, creating an arc-shaped mountain belt,

answers: NDQ_003358

answers: mountain belt,

answers: NDQ_003359

answers: adjacent plate,

answers: NDQ_003360

answers: oceanic crust subducted beneath continental crust on an adjacent plate,

answers: NDQ_003362

answers: beneath continental crust on an adjacent plate,

answers: NDQ_003363

answers: Wyoming craton.

answers: NDQ_003371

answers: arc-shaped mountain belt,

answers: NDQ_003373

answers: beneath continental crust

answers: NDQ_003376

answers: arc-shaped mountain belt,

answers: NDQ_003378

answers: Wyoming crust to Laurentia

answers: NDQ_003379

answers: arc-shaped mountain belt,

answers: NDQ_003380

answers: Wyoming craton.

answers: NDQ_003381

answers: arc-shaped mountain belt,

answers: NDQ_003382

answers: Wyoming craton.

answers: NDQ_003383

answers: Wyoming craton.

answers: NDQ_003384

answers: arc-shaped mountain belt,

answers: NDQ_003385

answers: arc-shaped mountain belt,

answers: NDQ_003386

answers: tectonism

answers: NDQ_003387

answers: Wyoming craton.

answers: NDQ_003388

answers: Wyoming craton.

answers: NDQ_003389

answers: arc-shaped mountain belt,

answers: NDQ_003390

answers: arc-shaped mountain belt,

answers: NDQ_003391

answers: arc-shaped mountain belt,

answers: NDQ_003392

answers: arc-shaped mountain belt,

answers: NDQ_003393

answers: mountain belt,

answers: NDQ_003394

answers: arc-shaped mountain belt,

answers: NDQ_003395

answers: arc-shaped mountain belt,

answers: NDQ_003396

answers: arc-shaped mountain belt,

text: McClelland also recorded the widespread fear and sense of doom that pervaded the area for months, as the earth’s crust continued to heave and settle. The effect was not merely structural, but psychological and religious. Seeded by decades of backcountry revivals and "awakenings," fear of the earthquakes was heightened by apocalyptic foretellings of the coming end of time.

text: McClelland also recorded the widespread fear and sense of doom that pervaded the area for months, as the earth’s crust continued to heave and settle. The effect was not merely structural, but psychological and religious. Seeded by decades of backcountry revivals and "awakenings," fear of the earthquakes was heightened by apocalyptic foretellings of the coming end of time.

answers: NDQ_003351

answers: heave

answers: NDQ_003352

answers: heave

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: earthquake

answers: NDQ_003356

answers: settle

answers: NDQ_003357

answers: heave and settle

answers: NDQ_003358

answers: heave

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth’s crust

answers: NDQ_003362

answers: apocalyptic foretellings of the coming end of time

answers: NDQ_003363

answers: the end of time

answers: NDQ_003371

answers: What may be the reason for the fear of the earthquakes?

answers: NDQ_003373

answers: Why did the fear of the earthquakes pervade the area for months?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: heave

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What type of force applied to rock is stress?

answers: NDQ_003381

answers: heave and settle

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: fault zone

answers: NDQ_003386

answers: the earth’s crust

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip, apocalyptic, or apocalyptic?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: earthquakes

answers: NDQ_003392

answers: heave

answers: NDQ_003393

answers: earthquakes

answers: NDQ_003394

answers: isobath

answers: NDQ_003395

answers: fault with a vertical fault plane

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: earthquakes

answers: NDQ_003352

answers: heave and settle.

answers: NDQ_003353

answers: heave and settle.

answers: NDQ_003354

answers: McClelland also recorded the widespread fear and sense of doom

answers: NDQ_003355

answers: earthquakes

answers: NDQ_003356

answers: heave and settle.

answers: NDQ_003357

answers: heave and settle.

answers: NDQ_003358

answers: earthquakes

answers: NDQ_003359

answers: earth’s crust continued to heave and settle.

answers: NDQ_003360

answers: earth’s crust

answers: NDQ_003362

answers: coming end of time.

answers: NDQ_003363

answers: earth’s crust continued to heave and settle.

answers: NDQ_003371

answers: McClelland also recorded the widespread fear and sense of doom

answers: NDQ_003373

answers: earth’s crust

answers: NDQ_003376

answers: earth’s crust continued to heave and settle.

answers: NDQ_003378

answers: heave and settle.

answers: NDQ_003379

answers: McClelland also recorded the widespread fear and sense of doom

answers: NDQ_003380

answers: earth’s crust continued to heave and settle.

answers: NDQ_003381

answers: heave and settle.

answers: NDQ_003382

answers: heave and settle.

answers: NDQ_003383

answers: heave and settle.

answers: NDQ_003384

answers: McClelland also recorded the widespread fear and sense of doom

answers: NDQ_003385

answers: earth’s crust

answers: NDQ_003386

answers: the earth’s crust continued to heave and settle.

answers: NDQ_003387

answers: earth’s crust continued to heave

answers: NDQ_003388

answers: the earth’s crust continued to heave

answers: NDQ_003389

answers: earth’s crust

answers: NDQ_003390

answers: earth’s crust continued to heave

answers: NDQ_003391

answers: earth’s crust

answers: NDQ_003392

answers: earth’s crust continued to heave

answers: NDQ_003393

answers: earth’s crust

answers: NDQ_003394

answers: earth’s crust

answers: NDQ_003395

answers: earth’s crust

answers: NDQ_003396

answers: McClelland also recorded the widespread fear and sense of doom

text: The OFZ (also called the Trans-Idaho Discontinuity) is a local segment of a larger structure that has only recently been recognized, the Great Divide Megashear. East of the WISZ this turns to the southeast (much as the OWL may be doing past the Wallula Gap) to follow the Clearwater fault zone down the continental divide near the Idaho—Montana border to the northwestern corner of Wyoming.  From there it seems to connect with the Snake River—Wichita fault zone, which passes through Colorado, and Oklahoma., and possibly further. There is a significant age discrepancy here.  Whereas the OFZ is a mere 90 to 70 Ma old, this megashear is ancient, having been dated to the Mesoproterozoic – about a billion years ago.  The Snake River—Wichita fault zone is of a similar age.  What appears to be happening is exploitation of ancient weaknesses in the crust.  This could explain the Newberry "hotspot track": parallel weaknesses in the crust open as the Brothers, Eugene—Denio, and Mendocino Fault Zones in response to development of the Basin and Range Province; magma from the event that initiated the Yellowstone hotspot (and possibly the Columbia River and other basalt flows) simply exploits the faults of the Brothers Fault Zone.  The other faults do not develop as "hotspot tracks" simply because there is no magma source nearby.  Similarly, it may be that the OWL reflects a similar zone of weakness, but does not develop as a major fault zone because it is too far from the stresses of the Basin and Range Province.

text: The OFZ (also called the Trans-Idaho Discontinuity) is a local segment of a larger structure that has only recently been recognized, the Great Divide Megashear. East of the WISZ this turns to the southeast (much as the OWL may be doing past the Wallula Gap) to follow the Clearwater fault zone down the continental divide near the Idaho—Montana border to the northwestern corner of Wyoming.  From there it seems to connect with the Snake River—Wichita fault zone, which passes through Colorado, and Oklahoma., and possibly further. There is a significant age discrepancy here.  Whereas the OFZ is a mere 90 to 70 Ma old, this megashear is ancient, having been dated to the

text: Mesoproterozoic

text: – about a billion years ago.  The Snake River—Wichita fault zone is of a similar age.  What appears to be happening is exploitation of ancient weaknesses in the crust.  This could explain the Newberry "hotspot track": parallel weaknesses in the crust open as the Brothers, Eugene—Denio, and Mendocino Fault Zones in response to development of the

text: Basin and Range Province

text: ; magma from the event that initiated the Yellowstone hotspot (and possibly the Columbia River and other basalt flows) simply exploits the faults of the Brothers Fault Zone.  The other faults do not develop as "hotspot tracks" simply because there is no magma source nearby.  Similarly, it may be that the OWL reflects a similar zone of weakness, but does not develop as a major fault zone because it is too far from the stresses of the Basin and Range Province.

answers: NDQ_003351

answers: basalt flows

answers: NDQ_003352

answers: develops cracks

answers: NDQ_003353

answers: faults

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: wallula gap

answers: NDQ_003356

answers: develop as faults

answers: NDQ_003357

answers: parallel weaknesses in the crust open as what?

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: weakens

answers: NDQ_003360

answers: faults

answers: NDQ_003362

answers: it is too far from the stresses of the Basin and Range Province.

answers: NDQ_003363

answers: Basin and Range Province

answers: NDQ_003371

answers: What could explain the Newberry "hotspot track"?

answers: NDQ_003373

answers: Why is the OWL too far from the stresses of the Basin and Range Province?

answers: NDQ_003376

answers: What appears to be happening is exploitation of ancient weaknesses in the crust

answers: NDQ_003378

answers: What is the amount the ground moves in an earthquake?

answers: NDQ_003379

answers: What appears to be happening is exploitation of ancient weaknesses in the crust

answers: NDQ_003380

answers: What type of force applied to rock is a stress?

answers: NDQ_003381

answers: What type of stress does the OFZ experience?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What could explain the Newberry "hotspot track"?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: fault zone

answers: NDQ_003386

answers: What is the cause of earthquakes?

answers: NDQ_003387

answers: What type of faults are caused by compression stress?

answers: NDQ_003388

answers: What could explain the Newberry "hotspot track"?

answers: NDQ_003389

answers: What appears to be happening is exploitation of ancient weaknesses in the crust

answers: NDQ_003390

answers: Clearwater fault zone

answers: NDQ_003391

answers: wallula gap

answers: NDQ_003392

answers: the OWL

answers: NDQ_003393

answers: wallula gap

answers: NDQ_003394

answers: Fault Zone

answers: NDQ_003395

answers: Clearwater fault zone

answers: NDQ_003396

answers: Snake River–Wichita fault zone

answers: NDQ_003351

answers: Basin and Range Province;

answers: NDQ_003352

answers: weakness,

answers: NDQ_003353

answers: Fault Zones

answers: NDQ_003354

answers: too far from the stresses of the Basin and Range Province.

answers: NDQ_003355

answers: "hotspot tracks"

answers: NDQ_003356

answers: Fault Zones

answers: NDQ_003357

answers: magma source nearby.

answers: NDQ_003358

answers: fault zone

answers: NDQ_003359

answers: exploitation of ancient weaknesses in the crust.

answers: NDQ_003360

answers: exploitation of ancient weaknesses in the crust.

answers: NDQ_003362

answers: "hotspot tracks"

answers: NDQ_003363

answers: Fault Zones

answers: NDQ_003371

answers: "hotspot tracks"

answers: NDQ_003373

answers: there is no magma source nearby.

answers: NDQ_003376

answers: Basin and Range Province;

answers: NDQ_003378

answers: Great Divide Megashear.

answers: NDQ_003379

answers: "hotspot tracks"

answers: NDQ_003380

answers: stresses

answers: NDQ_003381

answers: exploitation of ancient weaknesses in the crust.

answers: NDQ_003382

answers: Fault Zones

answers: NDQ_003383

answers: Fault Zones

answers: NDQ_003384

answers: OWL

answers: NDQ_003385

answers: "hotspot tracks"

answers: NDQ_003386

answers: exploitation of ancient weaknesses in the crust.

answers: NDQ_003387

answers: there is no magma source nearby.

answers: NDQ_003388

answers: exploitation of ancient weaknesses in the crust.

answers: NDQ_003389

answers: there is no magma source nearby.

answers: NDQ_003390

answers: OWL

answers: NDQ_003391

answers: "hotspot tracks"

answers: NDQ_003392

answers: OWL

answers: NDQ_003393

answers: "hotspot tracks"

answers: NDQ_003394

answers: Fault Zones

answers: NDQ_003395

answers: Brothers Fault Zone.

answers: NDQ_003396

answers: Fault Zones

text: Capitol Reef encompasses the Waterpocket Fold, a warp in the earth's crust that is 65 million years old. It is the largest exposed monocline in North America. In this fold, newer and older layers of earth folded over each other in an S-shape. This warp, probably caused by the same colliding continental plates that created the Rocky Mountains, has weathered and eroded over millennia to expose layers of rock and fossils.  The park is filled with brilliantly colored sandstone cliffs, gleaming white domes, and  contrasting layers of stone and earth.

text: Capitol Reef encompasses the

text: Waterpocket Fold

text: , a warp in the

text: earth's crust

text: that is 65 million years old. It is the largest exposed

text: monocline

text: in North America. In this fold, newer and older layers of earth folded over each other in an S-shape. This warp, probably caused by the same colliding

text: continental plates

text: that created the

text: Rocky Mountains

text: , has weathered and

text: eroded

text: over millennia to expose layers of rock and

text: fossil

text: s.  The park is filled with brilliantly colored

text: sandstone

text: cliffs, gleaming white domes, and  contrasting layers of stone and earth.

answers: NDQ_003351

answers: colliding continental plates

answers: NDQ_003352

answers: weathers

answers: NDQ_003353

answers: weathering

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: monocline

answers: NDQ_003356

answers: erode

answers: NDQ_003357

answers: newer and older layers of earth folded over each other

answers: NDQ_003358

answers: monocline

answers: NDQ_003359

answers: collides with another rock

answers: NDQ_003360

answers: continental plates

answers: NDQ_003362

answers: It is the largest exposed monocline in North America

answers: NDQ_003363

answers: colliding continental plates

answers: NDQ_003371

answers: Which of the following is not a type of fold?

answers: NDQ_003373

answers: None of the above choices.

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: What is the largest exposed monocline in North America?

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What type of stress does the Waterpocket Fold experience?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: What type of fold is the Waterpocket Fold?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: colliding continental plates

answers: NDQ_003387

answers: Which of the following is not caused by colliding continental plates that created the Rocky Mountains?

answers: NDQ_003388

answers: Which of the following is not caused by the same colliding continental plates that created the Rocky Mountains?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: Waterpocket Fold

answers: NDQ_003391

answers: monocline

answers: NDQ_003392

answers: Waterpocket Fold

answers: NDQ_003393

answers: monocline

answers: NDQ_003394

answers: monocline

answers: NDQ_003395

answers: monocline

answers: NDQ_003396

answers: monocline

answers: NDQ_003351

answers: colliding continental plates

answers: NDQ_003352

answers: eroded

answers: NDQ_003353

answers: weathered and eroded

answers: NDQ_003354

answers: Capitol Reef encompasses the Waterpocket Fold,

answers: NDQ_003355

answers: monocline

answers: NDQ_003356

answers: eroded

answers: NDQ_003357

answers: S-shape.

answers: NDQ_003358

answers: monocline

answers: NDQ_003359

answers: colliding continental plates

answers: NDQ_003360

answers: colliding continental plates

answers: NDQ_003362

answers: the Rocky Mountains,

answers: NDQ_003363

answers: colliding continental plates

answers: NDQ_003371

answers: S-shape.

answers: NDQ_003373

answers: S-shape.

answers: NDQ_003376

answers: colliding continental plates

answers: NDQ_003378

answers: S-shape.

answers: NDQ_003379

answers: S-shape.

answers: NDQ_003380

answers: S-shape.

answers: NDQ_003381

answers: S-shape.

answers: NDQ_003382

answers: plates that created the Rocky Mountains,

answers: NDQ_003383

answers: S-shape.

answers: NDQ_003384

answers: monocline

answers: NDQ_003385

answers: S-shape.

answers: NDQ_003386

answers: colliding continental plates

answers: NDQ_003387

answers: colliding continental plates

answers: NDQ_003388

answers: plates

answers: NDQ_003389

answers: Rocky Mountains,

answers: NDQ_003390

answers: Waterpocket Fold,

answers: NDQ_003391

answers: Waterpocket Fold,

answers: NDQ_003392

answers: Waterpocket Fold,

answers: NDQ_003393

answers: Waterpocket Fold,

answers: NDQ_003394

answers: monocline

answers: NDQ_003395

answers: S-shape.

answers: NDQ_003396

answers: monocline

text: Beginning about 20 million years ago, during the Miocene Epoch, both the Basin and Range and Colorado Plateau regions were uplifted as much as 3 kilometers. Great tension developed in the crust, probably related to changing plate motions far to the west. As the crust stretched, the Basin and Range Province broke up into a multitude of down-dropped valleys and elongate mountains. Yet for some reason not fully understood, the neighboring Colorado Plateau was able to preserve its structural integrity and remained a single tectonic block. Eventually, the great block of Colorado Plateau crust rose a kilometer higher than the Basin and Range.

text: Beginning about 20 million years ago, during the

text: Miocene

text: Epoch, both the Basin and Range and Colorado Plateau regions were uplifted as much as 3 kilometers. Great tension developed in the crust, probably related to changing plate motions far to the west. As the crust stretched, the Basin and Range Province broke up into a multitude of down-dropped valleys and elongate mountains. Yet for some reason not fully understood, the neighboring Colorado Plateau was able to preserve its structural integrity and remained a single tectonic block. Eventually, the great block of Colorado Plateau crust rose a kilometer higher than the Basin and Range.

answers: NDQ_003351

answers: down-dropped valleys

answers: NDQ_003352

answers: breaks up

answers: NDQ_003353

answers: the crust to stretch

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: valley

answers: NDQ_003356

answers: elongate

answers: NDQ_003357

answers: Basin and Range Province breaks up into a multitude of down-dropped valleys

answers: NDQ_003358

answers: valley

answers: NDQ_003359

answers: cracks

answers: NDQ_003360

answers: plates

answers: NDQ_003362

answers: Basin and Range Province broke up into a multitude of down-dropped valleys and elongate mountains

answers: NDQ_003363

answers: Basin and Range Province

answers: NDQ_003371

answers: What may have caused the Basin and Range Province to break up into a multitude of down-dropped valleys?

answers: NDQ_003373

answers: Why is the Basin and Range Province able to preserve its structural integrity?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: uplifted as much as 3 kilometers

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: Which of the following is not a type of stress?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Why did the Basin and Range Province break up?

answers: NDQ_003384

answers: Which of the following is not a type of fold: down-dropped valleys or elongate mountains?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: Which of the following is not a type of fault?

answers: NDQ_003388

answers: Which of the following is not a reason not fully understood, the neighboring Colorado Plateau was able to preserve its structural integrity?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: down-dropped valley

answers: NDQ_003391

answers: Colorado Plateau

answers: NDQ_003392

answers: tectonic

answers: NDQ_003393

answers: Colorado Plateau

answers: NDQ_003394

answers: down-dropped

answers: NDQ_003395

answers: unanswerable

answers: NDQ_003396

answers: down-dropped

answers: NDQ_003351

answers: changing plate motions

answers: NDQ_003352

answers: stretched,

answers: NDQ_003353

answers: the crust stretched,

answers: NDQ_003354

answers: Colorado Plateau crust rose a kilometer higher

answers: NDQ_003355

answers: down-dropped valleys

answers: NDQ_003356

answers: down-dropped valleys and elongate mountains.

answers: NDQ_003357

answers: changing plate motions

answers: NDQ_003358

answers: valleys

answers: NDQ_003359

answers: tension

answers: NDQ_003360

answers: changing plate motions

answers: NDQ_003362

answers: remained a single tectonic block.

answers: NDQ_003363

answers: Miocene Epoch,

answers: NDQ_003371

answers: Great tension developed in the crust, probably related to changing plate motions

answers: NDQ_003373

answers: Great tension developed in the crust, probably related to changing plate motions

answers: NDQ_003376

answers: down-dropped valleys and elongate mountains.

answers: NDQ_003378

answers: uplifted

answers: NDQ_003379

answers: west.

answers: NDQ_003380

answers: tension

answers: NDQ_003381

answers: stretched,

answers: NDQ_003382

answers: stretched,

answers: NDQ_003383

answers: tension developed in the crust, probably related to changing plate motions

answers: NDQ_003384

answers: mountains.

answers: NDQ_003385

answers: Miocene Epoch,

answers: NDQ_003386

answers: changing plate motions

answers: NDQ_003387

answers: Great tension developed in the crust, probably related to changing plate motions

answers: NDQ_003388

answers: changing plate motions

answers: NDQ_003389

answers: stretched,

answers: NDQ_003390

answers: down-dropped valleys

answers: NDQ_003391

answers: Colorado Plateau

answers: NDQ_003392

answers: Great tension developed in the crust, probably related to changing plate motions

answers: NDQ_003393

answers: Colorado Plateau

answers: NDQ_003394

answers: west.

answers: NDQ_003395

answers: changing plate motions

answers: NDQ_003396

answers: down-dropped valleys and elongate mountains.

text: There are three major psychological types of conflicts that can cause stress.

text: There are three major psychological types of conflicts that can cause stress.

answers: NDQ_003351

answers: psychological

answers: NDQ_003352

answers: is more likely to crack

answers: NDQ_003353

answers: lava to form.

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: swell.

answers: NDQ_003357

answers: stress is caused by

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: falls on it.

answers: NDQ_003360

answers: Earth's surface.

answers: NDQ_003362

answers: The San Andreas fault is a fault in the ocean.

answers: NDQ_003363

answers: volcanoes

answers: NDQ_003371

answers: Which of the following is an example of a thrust fault?

answers: NDQ_003373

answers: What is the best way to describe the stress of a rock?

answers: NDQ_003376

answers: The terrain known as basin-and-range is caused by compressive forces

answers: NDQ_003378

answers: (iv)

answers: NDQ_003379

answers: The dip of the fault plane is horizontal.

answers: NDQ_003380

answers: How would you describe a stress?

answers: NDQ_003381

answers: Which of the following is not a type of stress?

answers: NDQ_003382

answers: None of the above choices.

answers: NDQ_003383

answers: It is caused by a lack of energy.

answers: NDQ_003384

answers: Which of the following is not a type of fold?

answers: NDQ_003385

answers: A fault zone is a type of

answers: NDQ_003386

answers: (4).

answers: NDQ_003387

answers: Which of the following is not a type of stress?

answers: NDQ_003388

answers: What is shear stress?

answers: NDQ_003389

answers: None of the above choices.

answers: NDQ_003390

answers: can cause stress

answers: NDQ_003391

answers: is called a crater

answers: NDQ_003392

answers: is a type of

answers: NDQ_003393

answers: is a crater

answers: NDQ_003394

answers: can cause stress

answers: NDQ_003395

answers: is a type of fault

answers: NDQ_003396

answers: can cause stress

answers: NDQ_003351

answers: psychological types of conflicts

answers: NDQ_003352

answers: three major psychological types of conflicts

answers: NDQ_003353

answers: There are three major psychological types of conflicts

answers: NDQ_003354

answers: three major psychological types of conflicts that can cause stress.

answers: NDQ_003355

answers: There are three major psychological types of conflicts that can cause stress.

answers: NDQ_003356

answers: stress.

answers: NDQ_003357

answers: stress.

answers: NDQ_003358

answers: There are three major psychological types of conflicts that can cause stress.

answers: NDQ_003359

answers: three major psychological types of conflicts that can cause stress.

answers: NDQ_003360

answers: three major psychological types of conflicts

answers: NDQ_003362

answers: There are three major psychological types of conflicts that can cause stress.

answers: NDQ_003363

answers: three major psychological types of conflicts

answers: NDQ_003371

answers: three major psychological types of conflicts that can cause stress.

answers: NDQ_003373

answers: There are three major psychological types of conflicts

answers: NDQ_003376

answers: There are three major psychological types of conflicts that can cause stress.

answers: NDQ_003378

answers: three major psychological types of conflicts that can cause stress.

answers: NDQ_003379

answers: three major psychological types of conflicts that can cause stress.

answers: NDQ_003380

answers: There are three major psychological types of conflicts

answers: NDQ_003381

answers: There are three major psychological types of conflicts

answers: NDQ_003382

answers: three major psychological types of conflicts

answers: NDQ_003383

answers: There are three major psychological types of conflicts

answers: NDQ_003384

answers: There are three major psychological types of conflicts that can cause stress.

answers: NDQ_003385

answers: three major psychological types of conflicts that can cause stress.

answers: NDQ_003386

answers: There are three major psychological types of conflicts that can cause stress.

answers: NDQ_003387

answers: There are three major psychological types of conflicts

answers: NDQ_003388

answers: There are three major psychological types of conflicts

answers: NDQ_003389

answers: There are three major psychological types of conflicts

answers: NDQ_003390

answers: three major psychological types of conflicts that can cause stress.

answers: NDQ_003391

answers: three major psychological types of conflicts that can cause stress.

answers: NDQ_003392

answers: three major psychological types of conflicts that can cause stress.

answers: NDQ_003393

answers: three major psychological types of conflicts that can cause stress.

answers: NDQ_003394

answers: three major psychological types of conflicts that can cause stress.

answers: NDQ_003395

answers: three major psychological types of conflicts that can cause stress.

answers: NDQ_003396

answers: There are three major psychological types of conflicts that can cause stress.

text: Tension, however, accounts for most of the "opposite directions" pull on the plates.  As the separating oceanic crust cools over time, it becomes more dense and sinks farther and farther away from the ridge axis.  The cooling and sinking ocean crust causes a tensile stress that also helps drive the pulling apart of the plates at the ridge axis.

text: Tension, however, accounts for most of the "opposite directions" pull on the plates.  As the separating oceanic crust cools over time, it becomes more dense and sinks farther and farther away from the

text: ridge

text: axis.  The cooling and sinking ocean crust causes a tensile stress that also helps drive the pulling apart of the plates at the ridge axis.

answers: NDQ_003351

answers: Tension

answers: NDQ_003352

answers: sinks

answers: NDQ_003353

answers: cooling and sinking

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: ridge

answers: NDQ_003356

answers: sink

answers: NDQ_003357

answers: Tension accounts for most of the what?

answers: NDQ_003358

answers: ridge

answers: NDQ_003359

answers: is pushed apart

answers: NDQ_003360

answers: plates

answers: NDQ_003362

answers: cooling and sinking ocean crust causes a tensile stress

answers: NDQ_003363

answers: ridge axis

answers: NDQ_003371

answers: What is a thrust fault?

answers: NDQ_003373

answers: What is the main idea of the passage?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: no

answers: NDQ_003380

answers: It's impossible to say

answers: NDQ_003381

answers: What happens to the oceanic crust as it sinks?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: no

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: Which of the following is not a type of fault: Strike-slip faults or shear stress?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: ridge axis

answers: NDQ_003391

answers: ridge axis

answers: NDQ_003392

answers: ridge axis

answers: NDQ_003393

answers: ridge axis

answers: NDQ_003394

answers: "opposite directions"

answers: NDQ_003395

answers: NDQ_003396

answers: ridge axis

answers: NDQ_003351

answers: Tension,

answers: NDQ_003352

answers: sinks farther and farther away from the ridge axis.

answers: NDQ_003353

answers: sinks farther and farther away from the ridge axis.

answers: NDQ_003354

answers: The cooling and sinking ocean crust causes a tensile stress

answers: NDQ_003355

answers: "opposite directions"

answers: NDQ_003356

answers: Tension,

answers: NDQ_003357

answers: pulling apart of the plates at the ridge axis.

answers: NDQ_003358

answers: ridge axis.

answers: NDQ_003359

answers: tensile stress

answers: NDQ_003360

answers: Tension,

answers: NDQ_003362

answers: "opposite directions"

answers: NDQ_003363

answers: ridge axis.

answers: NDQ_003371

answers: The cooling and sinking ocean crust causes a tensile stress

answers: NDQ_003373

answers: tensile stress

answers: NDQ_003376

answers: Tension,

answers: NDQ_003378

answers: Tension,

answers: NDQ_003379

answers: ridge axis.

answers: NDQ_003380

answers: Tension,

answers: NDQ_003381

answers: tensile stress

answers: NDQ_003382

answers: Tension,

answers: NDQ_003383

answers: Tension,

answers: NDQ_003384

answers: ridge axis.

answers: NDQ_003385

answers: "opposite directions" pull on the plates.

answers: NDQ_003386

answers: Tension,

answers: NDQ_003387

answers: tensile

answers: NDQ_003388

answers: tensile stress

answers: NDQ_003389

answers: Tension,

answers: NDQ_003390

answers: ridge axis.

answers: NDQ_003391

answers: oceanic crust

answers: NDQ_003392

answers: "opposite directions"

answers: NDQ_003393

answers: ridge axis.

answers: NDQ_003394

answers: "opposite directions"

answers: NDQ_003395

answers: ridge axis.

answers: NDQ_003396

answers: "opposite directions"

text: The coefficient of lateral earth pressure, K, is defined as the ratio of the horizontal effective stress, σ’, to the vertical effective stress, σ’. The effective stress is the intergranular stress calculated by subtracting the pore pressure from the total stress as described in soil mechanics. K for a particular soil deposit is a function of the soil properties and the stress history. The minimum stable value of K is called the active earth pressure coefficient, K; the active earth pressure is obtained, for example,when a retaining wall moves away from the soil.  The maximum stable value of K is called the passive earth pressure coefficient, K; the passive earth pressure would develop, for example against a vertical plow that is pushing soil horizontally. For a level ground deposit with zero lateral strain in the soil, the "at-rest" coefficient of lateral earth pressure, K is obtained.

text: The coefficient of lateral earth pressure, K, is defined as the ratio of the horizontal

text: effective stress

text: , σ’, to the vertical effective stress, σ’. The

text: effective stress

text: is the intergranular stress calculated by subtracting the pore pressure from the total stress as described in

text: soil mechanics

text: . K for a particular soil deposit is a function of the

text: soil properties

text: and the stress history. The minimum stable value of K is called the active earth pressure coefficient, K; the active earth pressure is obtained, for example,when a retaining wall moves away from the soil.  The maximum stable value of K is called the passive earth pressure coefficient, K; the passive earth pressure would develop, for example against a vertical plow that is pushing soil horizontally. For a level ground deposit with zero lateral strain in the soil, the "at-rest" coefficient of lateral earth pressure, K is obtained.

answers: NDQ_003351

answers: active earth pressure

answers: NDQ_003352

answers: is more likely to crack

answers: NDQ_003353

answers: intergranular stress

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: at-rest

answers: NDQ_003357

answers: active earth pressure would develop against a vertical plow

answers: NDQ_003358

answers: passive earth pressure

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: lateral earth pressure

answers: NDQ_003362

answers: active earth pressure is obtained, for example,when a retaining wall moves away from the soil

answers: NDQ_003363

answers: active earth pressure

answers: NDQ_003371

answers: What is the minimum stable value of K?

answers: NDQ_003373

answers: lateral strain in the soil

answers: NDQ_003376

answers: lateral strain in the soil

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: vertical effective stress,

answers: NDQ_003380

answers: What is the minimum stable value of K?

answers: NDQ_003381

answers: What is the minimum stable value of K?

answers: NDQ_003382

answers: What is the minimum stable value of K?

answers: NDQ_003383

answers: What is the minimum stable value of K?

answers: NDQ_003384

answers: What is the minimum stable value of K?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: What is the minimum stable value of K?

answers: NDQ_003387

answers: Which of the following is not caused by compression stress?

answers: NDQ_003388

answers: What is the minimum stable value of K?

answers: NDQ_003389

answers: fold

answers: NDQ_003390

answers: active earth pressure

answers: NDQ_003391

answers: retaining wall

answers: NDQ_003392

answers: active earth pressure

answers: NDQ_003393

answers: retaining wall

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: a vertical fault plane

answers: NDQ_003396

answers: horizontal effective stress

answers: NDQ_003351

answers: intergranular stress

answers: NDQ_003352

answers: retaining wall moves away from the soil.

answers: NDQ_003353

answers: retaining wall moves away from the soil.

answers: NDQ_003354

answers: The coefficient of lateral earth pressure,

answers: NDQ_003355

answers: retaining wall

answers: NDQ_003356

answers: retaining wall moves away from the soil.

answers: NDQ_003357

answers: passive earth pressure

answers: NDQ_003358

answers: passive

answers: NDQ_003359

answers: vertical plow that is pushing soil

answers: NDQ_003360

answers: earth pressure,

answers: NDQ_003362

answers: retaining wall moves away from the soil.

answers: NDQ_003363

answers: earth pressure,

answers: NDQ_003371

answers: The coefficient of lateral earth pressure,

answers: NDQ_003373

answers: The coefficient of lateral earth pressure,

answers: NDQ_003376

answers: The coefficient of lateral earth pressure,

answers: NDQ_003378

answers: vertical plow

answers: NDQ_003379

answers: vertical

answers: NDQ_003380

answers: intergranular stress

answers: NDQ_003381

answers: retaining wall moves away from the soil.

answers: NDQ_003382

answers: The coefficient of lateral earth pressure,

answers: NDQ_003383

answers: intergranular stress

answers: NDQ_003384

answers: The coefficient of lateral earth pressure,

answers: NDQ_003385

answers: The coefficient of lateral earth pressure,

answers: NDQ_003386

answers: The coefficient of lateral earth pressure,

answers: NDQ_003387

answers: The coefficient of lateral earth pressure,

answers: NDQ_003388

answers: The coefficient of lateral earth pressure,

answers: NDQ_003389

answers: The coefficient of lateral earth pressure,

answers: NDQ_003390

answers: retaining wall

answers: NDQ_003391

answers: retaining wall

answers: NDQ_003392

answers: retaining wall

answers: NDQ_003393

answers: retaining wall

answers: NDQ_003394

answers: vertical plow that is pushing soil horizontally.

answers: NDQ_003395

answers: vertical plow

answers: NDQ_003396

answers: vertical

text: Subsequently, this definition has been broadened to mean the emplacement of continental lithosphere by oceanic lithosphere at a convergent plate boundary, such as closing of an ocean or a mountain building episode. This process is uncommon because the denser oceanic lithosphere usually subducts underneath the less dense continental plate.Obduction occurs where a fragment of continental crust is caught in a subduction zone with resulting overthrusting of oceanic mafic and ultramafic rocks from the mantle onto the continental crust. Obduction may occur where a small tectonic plate is caught between two larger plates, with the lithosphere (both island arc and oceanic) welding onto an adjacent continent as a new terrane. When two continental plates collide, obduction of the oceanic lithosphere between them is often a part of the resulting orogeny.

text: Subsequently, this definition has been broadened to mean the emplacement of

text: continental lithosphere

text: by

text: oceanic lithosphere

text: at a

text: convergent plate boundary

text: , such as closing of an ocean or a

text: mountain building

text: episode. This process is uncommon because the denser oceanic lithosphere usually subducts underneath the less dense continental plate.Obduction occurs where a fragment of continental

text: crust

text: is caught in a

text: subduction zone

text: with resulting overthrusting of oceanic

text: mafic

text: and ultramafic rocks from the mantle onto the continental crust. Obduction may occur where a small

text: tectonic plate

text: is caught between two larger plates, with the lithosphere (both

text: island arc

text: and oceanic) welding onto an adjacent

text: continent

text: as a new

text: terrane

text: . When two

text: continental plates

text: collide, obduction of the oceanic lithosphere between them is often a part of the resulting orogeny.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: overthrusts

answers: NDQ_003353

answers: overthrust

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: subduction zone

answers: NDQ_003356

answers: overthrust

answers: NDQ_003357

answers: oceanic mafic and ultramafic rocks from the mantle onto the continental crust

answers: NDQ_003358

answers: subduction zone

answers: NDQ_003359

answers: is caught in a subduction zone

answers: NDQ_003360

answers: continental plates

answers: NDQ_003362

answers: the denser oceanic lithosphere usually subducts underneath the less dense continental plate

answers: NDQ_003363

answers: convergent plate boundary

answers: NDQ_003371

answers: subduction zone with resulting overthrusting of oceanic mafic and ultramafic rocks from the mantle onto the continental crust

answers: NDQ_003373

answers: subduction zone

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: overthrusting

answers: NDQ_003379

answers: vertical

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What happens when a fragment of continental crust is caught in a subduction zone?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: overthrusting

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: subduction zone

answers: NDQ_003386

answers: overthrusting

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: unanswerable

answers: NDQ_003389

answers: subducts

answers: NDQ_003390

answers: subduction zone

answers: NDQ_003391

answers: subduction zone

answers: NDQ_003392

answers: subduction zone

answers: NDQ_003393

answers: subduction zone

answers: NDQ_003394

answers: subduction zone

answers: NDQ_003395

answers: subduction zone with resulting overthrusting

answers: NDQ_003396

answers: Obduction

answers: NDQ_003351

answers: subduction zone

answers: NDQ_003352

answers: overthrusting

answers: NDQ_003353

answers: overthrusting

answers: NDQ_003354

answers: subducts underneath the less dense continental plate.Obduction

answers: NDQ_003355

answers: island arc

answers: NDQ_003356

answers: overthrusting

answers: NDQ_003357

answers: subducts underneath the less dense continental plate.Obduction

answers: NDQ_003358

answers: subduction zone

answers: NDQ_003359

answers: overthrusting

answers: NDQ_003360

answers: convergent plate boundary,

answers: NDQ_003362

answers: closing of an ocean or a mountain building episode.

answers: NDQ_003363

answers: convergent plate boundary,

answers: NDQ_003371

answers: plate.Obduction

answers: NDQ_003373

answers: overthrusting

answers: NDQ_003376

answers: plate.Obduction

answers: NDQ_003378

answers: plate.Obduction

answers: NDQ_003379

answers: subduction zone

answers: NDQ_003380

answers: overthrusting

answers: NDQ_003381

answers: plate.Obduction

answers: NDQ_003382

answers: plate.Obduction

answers: NDQ_003383

answers: overthrusting

answers: NDQ_003384

answers: convergent plate boundary,

answers: NDQ_003385

answers: convergent plate boundary,

answers: NDQ_003386

answers: overthrusting

answers: NDQ_003387

answers: plate.Obduction

answers: NDQ_003388

answers: plate.Obduction

answers: NDQ_003389

answers: uncommon

answers: NDQ_003390

answers: subduction zone

answers: NDQ_003391

answers: plate.Obduction

answers: NDQ_003392

answers: mountain building episode.

answers: NDQ_003393

answers: plate.Obduction

answers: NDQ_003394

answers: convergent plate boundary,

answers: NDQ_003395

answers: subduction zone

answers: NDQ_003396

answers: plate.Obduction

text: Savai'i is the largest shield volcano in the South Pacific  and only 3% is above water.It is an active volcano, which last erupted in 1905-1911 with lava flows that destroyed villages on the central north coast. The island is formed by a massive basaltic shield volcano which rises from the seafloor of the western Pacific Ocean. A possible model for the formation of the volcanic Samoa island chain is explained by the Samoa hotspot situated at the east end of the Samoa Islands. In theory, the Samoa hotspot is a result of the Pacific Tectonic Plate moving over a 'fixed' deep and narrow mantle plume spewing up through the Earth's crust. The Samoa islands generally lie in a straight line, east to west, in the same direction the Plate is moving. In the classic hotspot model, primarily based on studies of the Hawaii hotspot, the volcanic islands and seamounts further away from the Samoa hotspot should be progressively older. However, Savai'i, the most western of the Samoa island chain, and Ta'u Island, the most eastern of the Samoa islands, both erupted in the last century, data which is an enigma for scientists. Ta'u last erupted in 1866. Another discrepancy in the data from the Samoa islands is that subaerial rock samples from Savai'i were too young by several million years to fit the classic hotspot model of age progression in an island chain, raising arguments among scientists that the Samoa islands does not have a plume origin. The nearness of Savai'i and the Samoa island chain to the Tonga Trench at the south became a possible explanation for these discrepancies as well as the possibility that the islands were formed by magma seeping through cracks in stressed fracture zones. However, in 2005, an international team gathered further submarine samples from the deep flanks and rifts of Savai'i. Tests on these later samples showed much older ages, about five million years old, that fit the hotspot model. The discovery in 1975 of Vailulu'u Seamount 45 km east of Ta'u in

text: Savai'i is the largest

text: shield volcano

text: in the South Pacific  and only 3% is above water.It is an

text: active volcano

text: , which last erupted in 1905-1911 with

text: lava flow

text: s that destroyed villages on the central north coast. The island is formed by a massive

text: basalt

text: ic shield volcano which rises from the seafloor of the western

text: Pacific Ocean

text: . A possible model for the formation of the volcanic Samoa island chain is explained by the

text: Samoa hotspot

text: situated at the east end of the

text: Samoa Islands

text: . In theory, the Samoa hotspot is a result of the

text: Pacific Tectonic Plate

text: moving over a 'fixed' deep and narrow

text: mantle plume

text: spewing up through the Earth's crust. The Samoa islands generally lie in a straight line, east to west, in the same direction the Plate is moving. In the classic hotspot model, primarily based on studies of the

text: Hawaii hotspot

text: , the volcanic islands and

text: seamount

text: s further away from the Samoa hotspot should be progressively older. However, Savai'i, the most western of the Samoa island chain, and

text: Ta'u Island

text: , the most eastern of the Samoa islands, both erupted in the last century, data which is an enigma for scientists. Ta'u last erupted in 1866. Another discrepancy in the data from the Samoa islands is that

text: subaerial

text: rock samples from Savai'i were too young by several million years to fit the classic hotspot model of age progression in an island chain, raising arguments among scientists that the Samoa islands does not have a plume origin. The nearness of Savai'i and the Samoa island chain to the

text: Tonga Trench

text: at the south became a possible explanation for these discrepancies as well as the possibility that the islands were formed by

text: magma

text: seeping through cracks in stressed

text: fracture zones.

text: However, in 2005, an international team gathered further submarine samples from the deep flanks and

text: rift

text: s of Savai'i. Tests on these later samples showed much older ages, about five million years old, that fit the hotspot model. The discovery in 1975 of

text: Vailulu'u Seamount

text: 45 km east of Ta'u in

answers: NDQ_003351

answers: fracture zones

answers: NDQ_003352

answers: fractures

answers: NDQ_003353

answers: fracture zones

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: rift

answers: NDQ_003356

answers: crack

answers: NDQ_003357

answers: The Samoa islands generally lie in a straight line, east to west

answers: NDQ_003358

answers: rift

answers: NDQ_003359

answers: stressed

answers: NDQ_003360

answers: Pacific Tectonic Plate

answers: NDQ_003362

answers: the Samoa islands does not have a plume origin

answers: NDQ_003363

answers: Hawaii hotspot

answers: NDQ_003371

answers: The Samoa islands

answers: NDQ_003373

answers: no

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: Savai'i

answers: NDQ_003380

answers: Which of the following is not a stress?

answers: NDQ_003381

answers: fracture zones

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: fracture zones

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: Savai'i

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: not enough information

answers: NDQ_003388

answers: unanswerable

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: rift

answers: NDQ_003391

answers: Stress fracture zones

answers: NDQ_003392

answers: rift

answers: NDQ_003393

answers: rift

answers: NDQ_003394

answers: Pacific Tectonic Plate

answers: NDQ_003395

answers: Tectonic plate moving over a 'fixed' deep and narrow mantle plume

answers: NDQ_003396

answers: Tonga Trench

answers: NDQ_003351

answers: fracture zones.

answers: NDQ_003352

answers: fracture zones.

answers: NDQ_003353

answers: fracture zones.

answers: NDQ_003354

answers: Savai'i were too young by several million years

answers: NDQ_003355

answers: rifts

answers: NDQ_003356

answers: Va

answers: NDQ_003357

answers: Ta'u Island,

answers: NDQ_003358

answers: fracture zones.

answers: NDQ_003359

answers: stressed fracture zones.

answers: NDQ_003360

answers: Pacific Tectonic Plate

answers: NDQ_003362

answers: progressively older.

answers: NDQ_003363

answers: Tonga Trench

answers: NDQ_003371

answers: hotspot model

answers: NDQ_003373

answers: Tonga Trench

answers: NDQ_003376

answers: magma seeping through cracks in stressed fracture zones.

answers: NDQ_003378

answers: progressively older.

answers: NDQ_003379

answers: hotspot model

answers: NDQ_003380

answers: stressed fracture zones.

answers: NDQ_003381

answers: progressively older.

answers: NDQ_003382

answers: progressively older.

answers: NDQ_003383

answers: Vail

answers: NDQ_003384

answers: Savai'i.

answers: NDQ_003385

answers: stressed fracture zones.

answers: NDQ_003386

answers: Savai'i.

answers: NDQ_003387

answers: Vail

answers: NDQ_003388

answers: Savai'i.

answers: NDQ_003389

answers: Tonga Trench

answers: NDQ_003390

answers: Savai'i.

answers: NDQ_003391

answers: Tonga Trench

answers: NDQ_003392

answers: fracture zones.

answers: NDQ_003393

answers: Tonga Trench

answers: NDQ_003394

answers: Va

answers: NDQ_003395

answers: Ta'u Island,

answers: NDQ_003396

answers: Va

text: Transtension is the state in which a rock mass or area of the Earth's crust experiences both extensive and transtensive shear. As such, transtensional regions are characterised by both extensional structures (normal faults, grabens) and wrench structures (strike-slip faults). In general, many tectonic regimes that were previously defined as simple strike-slip shear zones are actually transtensional. It is unlikely that a deforming body will experience 'pure' extension or 'pure' strike-slip.

text: Transtension is the state in which a rock mass or area of the Earth's

text: crust

text: experiences both extensive and transtensive

text: shear

text: . As such, transtensional regions are characterised by both extensional structures (

text: normal faults

text: graben

text: s) and wrench structures (

text: strike-slip fault

text: s). In general, many tectonic regimes that were previously defined as simple strike-slip shear zones are actually transtensional. It is unlikely that a deforming body will experience 'pure' extension or 'pure' strike-slip.

answers: NDQ_003351

answers: strike-slip

answers: NDQ_003352

answers: extends

answers: NDQ_003353

answers: shear

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: graben

answers: NDQ_003356

answers: transtensive shear

answers: NDQ_003357

answers: extensional structures

answers: NDQ_003358

answers: extensional structures

answers: NDQ_003359

answers: shear

answers: NDQ_003360

answers: tectonic plates

answers: NDQ_003362

answers: pure strike-slip faults

answers: NDQ_003363

answers: transtensional regions

answers: NDQ_003371

answers: What is the state in which a rock mass or area of the Earth's crust experiences both extensive and transtensive shear?

answers: NDQ_003373

answers: not enough information

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: no

answers: NDQ_003380

answers: What is a stress?

answers: NDQ_003381

answers: Extensive and transtensive

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: transtensional regions

answers: NDQ_003386

answers: normal faults

answers: NDQ_003387

answers: no

answers: NDQ_003388

answers: unanswerable

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: grabens

answers: NDQ_003391

answers: a rock mass

answers: NDQ_003392

answers: grabens

answers: NDQ_003393

answers: a rock mass

answers: NDQ_003394

answers: strike-slip faults

answers: NDQ_003395

answers: normal faults

answers: NDQ_003396

answers: grabens

answers: NDQ_003351

answers: Transtension

answers: NDQ_003352

answers: Transtension

answers: NDQ_003353

answers: shear.

answers: NDQ_003354

answers: Transtension

answers: NDQ_003355

answers: grabens)

answers: NDQ_003356

answers: 'pure' extension or 'pure' strike-slip.

answers: NDQ_003357

answers: extensional structures

answers: NDQ_003358

answers: 'pure' extension

answers: NDQ_003359

answers: Transtension

answers: NDQ_003360

answers: Transtension

answers: NDQ_003362

answers: 'pure' extension or 'pure' strike-slip.

answers: NDQ_003363

answers: Transtension

answers: NDQ_003371

answers: Transtension

answers: NDQ_003373

answers: Transtension

answers: NDQ_003376

answers: Transtension

answers: NDQ_003378

answers: strike-slip.

answers: NDQ_003379

answers: wrench structures

answers: NDQ_003380

answers: Transtension

answers: NDQ_003381

answers: Transtension

answers: NDQ_003382

answers: Transtension

answers: NDQ_003383

answers: extensional structures (normal faults, grabens) and wrench structures

answers: NDQ_003384

answers: Transtension

answers: NDQ_003385

answers: extensional structures (normal faults, grabens) and wrench structures

answers: NDQ_003386

answers: Transtension

answers: NDQ_003387

answers: extensional

answers: NDQ_003388

answers: wrench structures

answers: NDQ_003389

answers: Transtension

answers: NDQ_003390

answers: (strike-slip faults).

answers: NDQ_003391

answers: wrench structures

answers: NDQ_003392

answers: (strike-slip faults).

answers: NDQ_003393

answers: extensional structures (normal faults, grabens)

answers: NDQ_003394

answers: (strike-slip faults).

answers: NDQ_003395

answers: (normal faults,

answers: NDQ_003396

answers: (strike-slip faults).

text: The rift is presently nearly tectonically quiescent, but significant deformation and faulting with offsets of many kilometers were responsible for its formation starting about 35 Ma.  The largest-scale manifestation of rifting involves a pure-shear rifting mechanism, in which both sides of the rift pull apart evenly and slowly, with the lower crust and upper mantle (the lithosphere) stretching like taffy.  This extension is associated with very low seismic velocities in the upper mantle above approximately 400 km depth associated with relatively hot mantle and low degrees of partial melting. This intrusion of the asthenosphere into the lithosphere and continental crust is thought to be responsible for nearly all of the volcanism associated with the Rio Grande rift.

text: The rift is presently nearly tectonically quiescent, but significant deformation and faulting with offsets of many kilometers were responsible for its formation starting about 35 Ma.  The largest-scale manifestation of rifting involves a pure-shear rifting mechanism, in which both sides of the rift pull apart evenly and slowly, with the lower crust and upper mantle (the

text: lithosphere

text: ) stretching like

text: taffy

text: .  This extension is associated with very low seismic velocities in the upper mantle above approximately 400 km depth associated with relatively hot mantle and low degrees of partial melting. This intrusion of the

text: asthenosphere

text: into the

text: lithosphere

text: and

text: continental crust

text: is thought to be responsible for nearly all of the volcanism associated with the Rio Grande rift.

answers: NDQ_003351

answers: pure-shear

answers: NDQ_003352

answers: pulls apart

answers: NDQ_003353

answers: deformation

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: rift

answers: NDQ_003356

answers: stretch like taffy

answers: NDQ_003357

answers: both sides of the rift pull apart evenly and slowly

answers: NDQ_003358

answers: quiescent

answers: NDQ_003359

answers: deforms

answers: NDQ_003360

answers: tectonic plates

answers: NDQ_003362

answers: tectonically quiescent

answers: NDQ_003363

answers: 35 Ma

answers: NDQ_003371

answers: What may be the reason for the Rio Grande rift?

answers: NDQ_003373

answers: How would you describe taffy?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: what is the largest-scale manifestation of rifting

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What is the lowest-scale manifestation of rifting

answers: NDQ_003382

answers: What is the largest-scale manifestation of rifting?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What is the largest-scale manifestation of rifting?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: significant deformation and faulting

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: normal faults, deformation, or rifting?

answers: NDQ_003388

answers: Which of the following is not an example of a pure-shear rifting mechanism?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: pure-shear rifting

answers: NDQ_003391

answers: Rio Grande rift

answers: NDQ_003392

answers: pure-shear

answers: NDQ_003393

answers: lithosphere

answers: NDQ_003394

answers: offsets

answers: NDQ_003395

answers: offsets of many kilometers

answers: NDQ_003396

answers: pure-shear

answers: NDQ_003351

answers: pure-shear

answers: NDQ_003352

answers: stretching like taffy.

answers: NDQ_003353

answers: faulting

answers: NDQ_003354

answers: Rio Grande rift.

answers: NDQ_003355

answers: rifting involves a pure-shear

answers: NDQ_003356

answers: stretching like taffy.

answers: NDQ_003357

answers: both sides of the rift pull apart evenly and slowly,

answers: NDQ_003358

answers: tectonically quiescent,

answers: NDQ_003359

answers: deformation

answers: NDQ_003360

answers: rifting

answers: NDQ_003362

answers: nearly tectonically quiescent,

answers: NDQ_003363

answers: Rio Grande rift.

answers: NDQ_003371

answers: significant deformation and faulting

answers: NDQ_003373

answers: stretching like taffy.

answers: NDQ_003376

answers: taffy.

answers: NDQ_003378

answers: rifting

answers: NDQ_003379

answers: pure-shear

answers: NDQ_003380

answers: deformation

answers: NDQ_003381

answers: stretching like taffy.

answers: NDQ_003382

answers: pure-shear

answers: NDQ_003383

answers: stretching like taffy.

answers: NDQ_003384

answers: taffy.

answers: NDQ_003385

answers: faulting

answers: NDQ_003386

answers: volcanism

answers: NDQ_003387

answers: pure-shear

answers: NDQ_003388

answers: pure-shear

answers: NDQ_003389

answers: faulting

answers: NDQ_003390

answers: pure-shear

answers: NDQ_003391

answers: lithosphere)

answers: NDQ_003392

answers: pure-shear

answers: NDQ_003393

answers: lithosphere)

answers: NDQ_003394

answers: faulting with offsets of many kilometers

answers: NDQ_003395

answers: offsets of many kilometers

answers: NDQ_003396

answers: pure-shear

text: Mid-Ocean ridges are active volcanic mountain ranges snaking through the depths of the Earth’s oceans. They occur where the edges of the Earth’s tectonic plates are separating, allowing mantle rock to rise to the seafloor and harden, creating new crust. The addition of this crust can cause ocean basins to widen perpendicular to the ridge. This seafloor spreading is the engine of continental drift. At intervals along the mid-ocean ridges super-heated mineral-rich fluids are vented from the seabed. These hydrothermal vents are populated by animal and bacterial species not found elsewhere on Earth.

text: Mid-Ocean ridges are active volcanic mountain ranges snaking through the depths of the Earth’s oceans. They occur where the edges of the Earth’s

text: tectonic plates

text: are separating, allowing

text: mantle

text: rock to rise to the seafloor and harden, creating new

text: crust

text: . The addition of this crust can cause ocean basins to widen perpendicular to the ridge. This

text: seafloor spreading

text: is the engine of

text: continental drift

text: . At intervals along the mid-ocean ridges super-heated mineral-rich fluids are vented from the seabed. These

text: hydrothermal vent

text: s are populated by animal and bacterial species not found elsewhere on Earth.

answers: NDQ_003351

answers: seafloor spreading

answers: NDQ_003352

answers: hardens

answers: NDQ_003353

answers: mantle rock to rise

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: tectonic plate

answers: NDQ_003356

answers: harden

answers: NDQ_003357

answers: mantle rock rises to the seafloor and hardens

answers: NDQ_003358

answers: unanswerable

answers: NDQ_003359

answers: hardens

answers: NDQ_003360

answers: tectonic plates

answers: NDQ_003362

answers: seafloor spreading is the engine of continental drift

answers: NDQ_003363

answers: Mid-Ocean ridges

answers: NDQ_003371

answers: Which of the following is not a type of seafloor spreading?

answers: NDQ_003373

answers: Which of the following is not a type of rock?

answers: NDQ_003376

answers: Which of the following is not caused by compressive forces?

answers: NDQ_003378

answers: What is the engine of continental drift?

answers: NDQ_003379

answers: Which of the following is not a type of strike-slip fault?

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What happens to mantle rock when it rises to the seafloor?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What can cause ocean basins to widen perpendicular to the ridge

answers: NDQ_003384

answers: Which of the following is not a type of fold that arches upward?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: Which of the following is not a cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: Mid-Ocean ridges or normal faults?

answers: NDQ_003388

answers: What can cause ocean basins to widen perpendicular to the ridge?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: tectonic plate

answers: NDQ_003391

answers: seafloor

answers: NDQ_003392

answers: tectonic plate

answers: NDQ_003393

answers: mantle

answers: NDQ_003394

answers: perpendicular

answers: NDQ_003395

answers: tectonic plates are separating

answers: NDQ_003396

answers: perpendicular

answers: NDQ_003351

answers: seafloor spreading

answers: NDQ_003352

answers: harden,

answers: NDQ_003353

answers: harden,

answers: NDQ_003354

answers: Mid-Ocean ridges

answers: NDQ_003355

answers: Mid-Ocean ridges

answers: NDQ_003356

answers: harden,

answers: NDQ_003357

answers: separating,

answers: NDQ_003358

answers: Mid-Ocean ridges

answers: NDQ_003359

answers: harden,

answers: NDQ_003360

answers: tectonic plates

answers: NDQ_003362

answers: mantle rock to rise to the seafloor

answers: NDQ_003363

answers: Mid-Ocean ridges

answers: NDQ_003371

answers: Mid-Ocean ridges

answers: NDQ_003373

answers: mantle rock to rise to the seafloor

answers: NDQ_003376

answers: ocean basins to widen perpendicular to the ridge.

answers: NDQ_003378

answers: separating,

answers: NDQ_003379

answers: perpendicular

answers: NDQ_003380

answers: mantle rock

answers: NDQ_003381

answers: mantle rock

answers: NDQ_003382

answers: separating,

answers: NDQ_003383

answers: mantle rock

answers: NDQ_003384

answers: Mid-Ocean ridges

answers: NDQ_003385

answers: the edges of the Earth’s tectonic plates are separating,

answers: NDQ_003386

answers: tectonic plates are separating,

answers: NDQ_003387

answers: separating,

answers: NDQ_003388

answers: the edges of the Earth’s tectonic plates are separating,

answers: NDQ_003389

answers: separating,

answers: NDQ_003390

answers: Mid-Ocean ridges

answers: NDQ_003391

answers: mantle

answers: NDQ_003392

answers: Mid-Ocean ridges

answers: NDQ_003393

answers: mantle

answers: NDQ_003394

answers: perpendicular

answers: NDQ_003395

answers: tectonic plates are separating,

answers: NDQ_003396

answers: tectonic plates are separating,

text: San Jose lies near several active faults, including the Monte Vista Fault, Hayward Fault Zone, Calaveras Fault, Silver Creek Fault, and the San Andreas Fault. Significant events occurred in 1856, 1858, 1864, 1865, 1868, 1881, 1891, 1897, 1898, 1906, 1957, 1989, and 2007.  The 1906 San Francisco earthquake, with its epicenter slightly off the coast of San Francisco near Golden Gate Park, devastated many buildings in San Jose. The city was still primarily rural and the population was much smaller than San Francisco. Houses and businesses were not built as close as they were on the peninsula, and this provided less opportunity for major fires. The all-brick Agnews Asylum (later Agnews State Hospital) was destroyed, killing over 100 people as the walls and roof collapsed. The 8-year-old San Jose High School's three-story stone and brick structure also collapsed, and many other buildings were severely damaged.  There have been many other moderate earthquakes that have been felt in San Jose that caused little or no damage. Most damage from earthquakes are quickly repaired, but some effects may still be seen in the form of cracked sidewalks and raised curbs.

text: San Jose lies near several active

text: faults

text: , including the

text: Monte Vista Fault

text: Hayward Fault Zone

text: Calaveras Fault

text: Silver Creek Fault

text: , and the

text: San Andreas Fault

text: . Significant events occurred in 1856, 1858, 1864, 1865,

text: , 1881, 1891, 1897, 1898,

text: , and

text: .  The 1906 San Francisco earthquake, with its epicenter slightly off the coast of

text: San Francisco

text: near

text: Golden Gate Park

text: , devastated many buildings in San Jose. The city was still primarily rural and the population was much smaller than San Francisco. Houses and businesses were not built as close as they were on the peninsula, and this provided less opportunity for major fires. The all-brick Agnews Asylum (later

text: Agnews State Hospital

text: ) was destroyed, killing over 100 people as the walls and roof collapsed. The 8-year-old

text: San Jose High School

text: 's three-story stone and brick structure also collapsed, and many other buildings were severely damaged.  There have been many other moderate earthquakes that have been felt in San Jose that caused little or no damage. Most damage from earthquakes are quickly repaired, but some effects may still be seen in the form of cracked sidewalks and raised curbs.

answers: NDQ_003351

answers: San Andreas Fault

answers: NDQ_003352

answers: cracks

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: Fault

answers: NDQ_003356

answers: collapse in what way?

answers: NDQ_003357

answers: San Jose High School's three-story stone and brick structure also collapsed

answers: NDQ_003358

answers: active fault

answers: NDQ_003359

answers: cracks

answers: NDQ_003360

answers: San Andreas Fault

answers: NDQ_003362

answers: The city was still primarily rural and the population was much smaller than San Francisco

answers: NDQ_003363

answers: San Francisco

answers: NDQ_003371

answers: Which of the following is not an active fault: Monte Vista Fault, Hayward Fault Zone, Calaveras Fault, Silver Creek Fault, or the San Andreas Fault?

answers: NDQ_003373

answers: How would you describe San Jose High School?

answers: NDQ_003376

answers: Which of the following is not caused by compressive forces: basin-and-range or earthquakes?

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: Which of the following is not a strike-slip fault?

answers: NDQ_003380

answers: Which happened first, the San Francisco earthquake or the 1906 San Francisco earthquake?

answers: NDQ_003381

answers: What type of stress does the San Andreas Fault cause?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which happened first, the 1906 San Francisco earthquake or the 1906 San Francisco earthquake?

answers: NDQ_003384

answers: Which of the following is not a type of fold: Monte Vista Fault, Hayward Fault Zone, Calaveras Fault, Silver Creek Fault, or San Andreas Fault?

answers: NDQ_003385

answers: Hayward Fault Zone

answers: NDQ_003386

answers: active faults

answers: NDQ_003387

answers: Which of the following is not a normal fault: Monte Vista Fault, Hayward Fault Zone, Silver Creek Fault, or San Andreas Fault?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip faults, earthquakes, or earthquakes?

answers: NDQ_003389

answers: active faults

answers: NDQ_003390

answers: San Andreas Fault

answers: NDQ_003391

answers: San Andreas Fault

answers: NDQ_003392

answers: San Andreas Fault

answers: NDQ_003393

answers: San Andreas Fault

answers: NDQ_003394

answers: San Andreas Fault

answers: NDQ_003395

answers: San Andreas Fault

answers: NDQ_003396

answers: Hayward Fault Zone

answers: NDQ_003351

answers: San Andreas Fault.

answers: NDQ_003352

answers: cracked sidewalks and raised curbs.

answers: NDQ_003353

answers: faults,

answers: NDQ_003354

answers: San Jose lies near several active faults, including the Monte Vista Fault,

answers: NDQ_003355

answers: faults,

answers: NDQ_003356

answers: cracked sidewalks and raised curbs.

answers: NDQ_003357

answers: cracked sidewalks and raised curbs.

answers: NDQ_003358

answers: active faults,

answers: NDQ_003359

answers: faults,

answers: NDQ_003360

answers: faults,

answers: NDQ_003362

answers: little or no damage.

answers: NDQ_003363

answers: San Andreas Fault.

answers: NDQ_003371

answers: San Andreas Fault.

answers: NDQ_003373

answers: cracked sidewalks and raised curbs.

answers: NDQ_003376

answers: San Jose lies near several active faults,

answers: NDQ_003378

answers: cracked sidewalks and raised curbs.

answers: NDQ_003379

answers: 1897, 1898,

answers: NDQ_003380

answers: earthquakes

answers: NDQ_003381

answers: cracked sidewalks and raised curbs.

answers: NDQ_003382

answers: San Andreas Fault.

answers: NDQ_003383

answers: active faults,

answers: NDQ_003384

answers: cracked sidewalks and raised curbs.

answers: NDQ_003385

answers: Hayward Fault Zone,

answers: NDQ_003386

answers: active faults,

answers: NDQ_003387

answers: San Andreas Fault.

answers: NDQ_003388

answers: San Andreas Fault.

answers: NDQ_003389

answers: faults,

answers: NDQ_003390

answers: Calaveras Fault, Silver Creek Fault,

answers: NDQ_003391

answers: Hayward Fault Zone,

answers: NDQ_003392

answers: Calaveras Fault, Silver Creek Fault,

answers: NDQ_003393

answers: raised curbs.

answers: NDQ_003394

answers: San Andreas Fault.

answers: NDQ_003395

answers: San Andreas Fault.

answers: NDQ_003396

answers: Calaveras Fault, Silver Creek Fault,

text: Mount Ararat lies within a complex, sinistral pull-apart basin that originally was a single, continuous depression. The growth of Mount Ararat partitioned this depression into two smaller basins, the Iğdir and Doğubeyazıt basins. This pull-apart basin is the result of strike-slip movement along two en-echelon fault segments, the Doğubeyazıt–Gürbulak and Iğdir faults, of a sinistral strike–slip fault system. Tension between these faults, not only formed the original pull-apart basin, but created a system of faults, exhibiting a horsetail splay pattern, that control the position of the principal volcanic eruption centers of Mount Ararat and associated linear belt of parasitic volcanic cones. The strike-slip fault system within which Mount Ararat located is the result of north–south convergence and tectonic compression between the Arabian Platform and Laurasia that continued after the Tethys Ocean closed during the Eocene epoch along the Bitlis–Zagros suture.

text: Mount Ararat lies within a complex, sinistral

text: pull-apart basin

text: that originally was a single, continuous depression. The growth of Mount Ararat partitioned this depression into two smaller basins, the Iğdir and Doğubeyazıt basins. This pull-apart basin is the result of

text: strike-slip

text: movement along two en-echelon fault segments, the Doğubeyazıt–Gürbulak and Iğdir faults, of a sinistral strike–slip fault system. Tension between these faults, not only formed the original pull-apart basin, but created a system of faults, exhibiting a horsetail splay pattern, that control the position of the principal volcanic eruption centers of Mount Ararat and associated linear belt of parasitic volcanic cones. The strike-slip fault system within which Mount Ararat located is the result of north–south convergence and

text: tectonic

text: compression between the Arabian Platform and

text: Laurasia

text: that continued after the

text: Tethys Ocean

text: closed during the

text: Eocene

text: epoch

text: along the Bitlis–Zagros

text: suture

answers: NDQ_003351

answers: strike-slip

answers: NDQ_003352

answers: is more likely to crack

answers: NDQ_003353

answers: Faults

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: pull-apart basin

answers: NDQ_003356

answers: splay

answers: NDQ_003357

answers: Strike-slip movement is the result of what?

answers: NDQ_003358

answers: unanswerable

answers: NDQ_003359

answers: tension between these faults

answers: NDQ_003360

answers: tectonic plates

answers: NDQ_003362

answers: the San Andreas fault is the result of north–south convergence and tectonic compression

answers: NDQ_003363

answers: Tethys Ocean

answers: NDQ_003371

answers: What is the result of north–south convergence?

answers: NDQ_003373

answers: What is the result of north–south convergence

answers: NDQ_003376

answers: What is the result of north–south convergence and tectonic compression?

answers: NDQ_003378

answers: What is the result of north–south convergence and tectonic compression

answers: NDQ_003379

answers: no

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What is the result of north–south convergence?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What type of fold is the I dir fault?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: What is the cause of earthquakes?

answers: NDQ_003387

answers: What is the result of north–south convergence?

answers: NDQ_003388

answers: What is the cause of the pull-apart basin?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: en-echelon

answers: NDQ_003391

answers: Mount Ararat

answers: NDQ_003392

answers: en-echelon

answers: NDQ_003393

answers: Mount Ararat

answers: NDQ_003394

answers: sinistral

answers: NDQ_003395

answers: en-echelon fault segments

answers: NDQ_003396

answers: horsetail splay

answers: NDQ_003351

answers: strike-slip

answers: NDQ_003352

answers: a horsetail splay pattern,

answers: NDQ_003353

answers: faults,

answers: NDQ_003354

answers: Mount Ararat

answers: NDQ_003355

answers: depression.

answers: NDQ_003356

answers: strike-slip

answers: NDQ_003357

answers: strike-slip

answers: NDQ_003358

answers: depression.

answers: NDQ_003359

answers: Tension between these faults,

answers: NDQ_003360

answers: tectonic compression

answers: NDQ_003362

answers: continuous depression.

answers: NDQ_003363

answers: tectonic compression between the Arabian Platform and Laurasia

answers: NDQ_003371

answers: strike–slip fault system.

answers: NDQ_003373

answers: tectonic compression

answers: NDQ_003376

answers: tectonic compression

answers: NDQ_003378

answers: strike-slip

answers: NDQ_003379

answers: horsetail splay pattern,

answers: NDQ_003380

answers: Tension

answers: NDQ_003381

answers: strike-slip movement along two en-echelon fault segments,

answers: NDQ_003382

answers: tectonic compression

answers: NDQ_003383

answers: horsetail splay pattern,

answers: NDQ_003384

answers: sinistral

answers: NDQ_003385

answers: horsetail splay pattern,

answers: NDQ_003386

answers: strike-slip

answers: NDQ_003387

answers: tectonic compression

answers: NDQ_003388

answers: north–south convergence and tectonic compression

answers: NDQ_003389

answers: strike-slip

answers: NDQ_003390

answers: I<unk>dir faults,

answers: NDQ_003391

answers: strike–slip fault system.

answers: NDQ_003392

answers: sinistral strike–slip fault system.

answers: NDQ_003393

answers: strike-slip movement along two en-echelon fault segments,

answers: NDQ_003394

answers: horsetail splay pattern,

answers: NDQ_003395

answers: horsetail splay pattern,

answers: NDQ_003396

answers: horsetail splay pattern,

text: Other important examples of radiogenic elements are radon and helium, both of which form during the decay of heavier elements in bedrock. Radon is entirely radiogenic, since it has too short a half-life to occur primordially. Helium, however, occurs in the crust of the Earth primordially, since both helium-3 and helium-4 are stable, and small amounts were trapped in the crust of the Earth as it formed. Helium-3 is almost entirely primordial (a small amount is formed by natural nuclear reactions in the crust). The global supply of helium (which occurs in gas wells and well as the atmosphere) is almost entirely (about 90-99%) radiogenic, as shown by its factor of 10 to 100 times enrichment in radiogenic helium-4 relative to the primordial ratio of helium-4 to helium-3. This latter ratio is known from extraterrestrial sources, such as some moon rocks and meteorites, which are relatively free of parental sources for helium-3 and helium-4.

text: Other important examples of radiogenic elements are

text: radon

text: and

text: helium

text: , both of which form during the decay of heavier elements in bedrock. Radon is entirely radiogenic, since it has too short a half-life to occur primordially. Helium, however, occurs in the crust of the Earth primordially, since both helium-3 and helium-4 are stable, and small amounts were trapped in the crust of the Earth as it formed. Helium-3 is almost entirely primordial (a small amount is formed by natural nuclear reactions in the crust). The global supply of helium (which occurs in gas wells and well as the atmosphere) is almost entirely (about 90-99%) radiogenic, as shown by its factor of 10 to 100 times enrichment in radiogenic helium-4 relative to the primordial ratio of helium-4 to helium-3. This latter ratio is known from extraterrestrial sources, such as some moon rocks and meteorites, which are relatively free of parental sources for helium-3 and helium-4.

answers: NDQ_003351

answers: radon

answers: NDQ_003352

answers: oxidizes

answers: NDQ_003353

answers: radiogenic elements to form

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: radon

answers: NDQ_003357

answers: Helium-3 is almost entirely primordial

answers: NDQ_003358

answers: bedrock

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: it has too short a half-life to occur primordially

answers: NDQ_003363

answers: radiogenic

answers: NDQ_003371

answers: What may be the reason for a thrust fault?

answers: NDQ_003373

answers: unanswerable

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: vertical

answers: NDQ_003380

answers: What is a stress?

answers: NDQ_003381

answers: How does rock deform?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: Fault zone

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: Which of the following is not caused by compression stress?

answers: NDQ_003388

answers: Which of the following is not a radiogenic element: radon or helium?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: bedrock

answers: NDQ_003392

answers: a fault

answers: NDQ_003393

answers: bedrock

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: is almost entirely primordial

answers: NDQ_003396

answers: radon

answers: NDQ_003351

answers: radon

answers: NDQ_003352

answers: radiogenic elements are radon

answers: NDQ_003353

answers: decay of heavier elements

answers: NDQ_003354

answers: Other important examples of radiogenic elements are radon

answers: NDQ_003355

answers: radon

answers: NDQ_003356

answers: radiogenic elements are radon and helium,

answers: NDQ_003357

answers: heavier elements in bedrock.

answers: NDQ_003358

answers: bedrock.

answers: NDQ_003359

answers: decay of heavier elements in bedrock.

answers: NDQ_003360

answers: heavier elements in bedrock.

answers: NDQ_003362

answers: Radon is entirely radiogenic,

answers: NDQ_003363

answers: decay of heavier elements in bedrock.

answers: NDQ_003371

answers: Other important examples of radiogenic elements are radon and helium,

answers: NDQ_003373

answers: heavier elements in bedrock.

answers: NDQ_003376

answers: decay of heavier elements in bedrock.

answers: NDQ_003378

answers: heavier elements in bedrock.

answers: NDQ_003379

answers: Radon is entirely radiogenic,

answers: NDQ_003380

answers: heavier elements in bedrock.

answers: NDQ_003381

answers: decay of heavier elements in bedrock.

answers: NDQ_003382

answers: decay of heavier elements in bedrock.

answers: NDQ_003383

answers: decay of heavier elements in bedrock.

answers: NDQ_003384

answers: bedrock.

answers: NDQ_003385

answers: heavier elements in bedrock.

answers: NDQ_003386

answers: decay of heavier elements in bedrock.

answers: NDQ_003387

answers: decay of heavier elements in bedrock.

answers: NDQ_003388

answers: decay of heavier elements in bedrock.

answers: NDQ_003389

answers: decay of heavier elements in bedrock.

answers: NDQ_003390

answers: decay of heavier elements in bedrock.

answers: NDQ_003391

answers: bedrock.

answers: NDQ_003392

answers: heavier elements in bedrock.

answers: NDQ_003393

answers: bedrock.

answers: NDQ_003394

answers: heavier elements in bedrock.

answers: NDQ_003395

answers: heavier elements in bedrock.

answers: NDQ_003396

answers: heavier elements in bedrock.

text: As extension continued in the mid to late Jurassic, multiple pull-apart basins and oblique right-lateral strike-slip faulting in the eastern margin of the Exmouth Plateau continued to dominate. The simple shear stress of the Exmouth detachment fault between the base of the upper crust, and the lower crust had been reduced in the east plateau. This reduction in simple shear was in part caused by the deformation that developed series negative flower structures and half-graben systems in the west plateau. By this time, the lithospheric thinning that had been initiated in during the early Jurassic was now considerably thinner. At this period, a magmatic intrusion between the lower crystalline crest and the lithosphere been introduce, underplating this region.

text: As extension continued in the mid to late Jurassic, multiple

text: pull-apart basin

text: s and oblique right-lateral strike-slip faulting in the eastern margin of the Exmouth Plateau continued to dominate. The simple shear stress of the Exmouth detachment fault between the base of the upper crust, and the lower crust had been reduced in the east plateau. This reduction in simple shear was in part caused by the deformation that developed series negative flower structures and half-graben systems in the west plateau. By this time, the lithospheric thinning that had been initiated in during the early Jurassic was now considerably thinner. At this period, a magmatic intrusion between the lower crystalline crest and the lithosphere been introduce, underplating this region.

answers: NDQ_003351

answers: simple shear

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: simple shear

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: half-graben

answers: NDQ_003356

answers: develop series negative flower structures

answers: NDQ_003357

answers: oblique right-lateral strike-slip faulting

answers: NDQ_003358

answers: simple shear

answers: NDQ_003359

answers: deforms

answers: NDQ_003360

answers: Exmouth Plateau

answers: NDQ_003362

answers: a magmatic intrusion between the lower crystalline crest and the lithosphere

answers: NDQ_003363

answers: Jurassic

answers: NDQ_003371

answers: What may be the reason for the magmatic intrusion?

answers: NDQ_003373

answers: no

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: no

answers: NDQ_003380

answers: What is shear stress?

answers: NDQ_003381

answers: What type of stress does the Exmouth detachment fault cause?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: yes

answers: NDQ_003386

answers: yes

answers: NDQ_003387

answers: no

answers: NDQ_003388

answers: yes

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: Exmouth detachment fault

answers: NDQ_003391

answers: Exmouth Plateau

answers: NDQ_003392

answers: Exmouth detachment fault

answers: NDQ_003393

answers: Exmouth Plateau

answers: NDQ_003394

answers: oblique

answers: NDQ_003395

answers: Exmouth detachment fault

answers: NDQ_003396

answers: right-lateral strike-slip faulting

answers: NDQ_003351

answers: simple shear

answers: NDQ_003352

answers: reduced

answers: NDQ_003353

answers: series negative flower structures and half-graben systems

answers: NDQ_003354

answers: As extension continued in the mid to late Jurassic,

answers: NDQ_003355

answers: pull-apart basins

answers: NDQ_003356

answers: series negative flower structures and half-graben systems

answers: NDQ_003357

answers: simple shear stress

answers: NDQ_003358

answers: simple shear stress

answers: NDQ_003359

answers: deformation

answers: NDQ_003360

answers: oblique right-lateral strike-slip faulting

answers: NDQ_003362

answers: reduced

answers: NDQ_003363

answers: mid to late Jurassic,

answers: NDQ_003371

answers: oblique right-lateral strike-slip faulting

answers: NDQ_003373

answers: The simple shear stress

answers: NDQ_003376

answers: pull-apart basins

answers: NDQ_003378

answers: strike-slip

answers: NDQ_003379

answers: oblique right-lateral

answers: NDQ_003380

answers: stress

answers: NDQ_003381

answers: negative flower structures and half-graben systems

answers: NDQ_003382

answers: simple shear stress

answers: NDQ_003383

answers: The simple shear stress

answers: NDQ_003384

answers: oblique right-lateral strike-slip faulting

answers: NDQ_003385

answers: oblique right-lateral strike-slip faulting

answers: NDQ_003386

answers: oblique right-lateral strike-slip faulting

answers: NDQ_003387

answers: shear

answers: NDQ_003388

answers: The simple shear stress

answers: NDQ_003389

answers: extension

answers: NDQ_003390

answers: Exmouth detachment fault

answers: NDQ_003391

answers: crystalline crest

answers: NDQ_003392

answers: Exmouth detachment fault

answers: NDQ_003393

answers: crystalline crest

answers: NDQ_003394

answers: oblique right-lateral strike-slip faulting

answers: NDQ_003395

answers: oblique right-lateral strike-slip faulting

answers: NDQ_003396

answers: oblique right-lateral strike-slip faulting

text: Oceanic core complex structures form at slow spreading oceanic plate boundaries which have a limited supply of upwelling magma. These zones have low upper mantle temperatures and long transform faults develop. Rift valleys do not develop along the expansion axes of slow spreading boundaries.  Expansion takes place along low-angle detachment faults. The core complex builds on the uplifted side of the fault where most of the gabbroic (or crustal) material is stripped away to expose mantle peridotite.  They comprise peridotites ultramafic rocks of mantle and to a lesser extent gabbroic rocks from the Earth's crust.

text: Oceanic core complex structures form at slow spreading oceanic

text: plate boundaries

text: which have a limited supply of upwelling

text: magma

text: . These zones have low upper

text: mantle

text: temperatures and long

text: transform faults

text: develop.

text: Rift valley

text: s do not develop along the expansion axes of slow spreading boundaries.  Expansion takes place along low-angle

text: detachment fault

text: s. The core complex builds on the uplifted side of the fault where most of the

text: gabbro

text: ic (or crustal) material is stripped away to expose mantle

text: peridotite

text: .  They comprise peridotites

text: ultramafic rock

text: s of

text: mantle

text: and to a lesser extent gabbroic rocks from the Earth's crust.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: Faults

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: Rift

answers: NDQ_003356

answers: expand

answers: NDQ_003357

answers: low-angle detachment faults do not develop

answers: NDQ_003358

answers: valley

answers: NDQ_003359

answers: is uplifted

answers: NDQ_003360

answers: slow spreading oceanic plate boundaries

answers: NDQ_003362

answers: The core complex builds on the uplifted side

answers: NDQ_003363

answers: slow spreading oceanic plate boundaries

answers: NDQ_003371

answers: Which of the following is not a type of fault: low-angle detachment faults or thrust faults?

answers: NDQ_003373

answers: What is the main idea of this passage?

answers: NDQ_003376

answers: Which of the following is not a type of terrain: basin-and-range or compressive forces?

answers: NDQ_003378

answers: What is the amount of the gabbroic (or crustal) material is stripped away to expose mantle peridotite

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: Which of the following is not a stress?

answers: NDQ_003381

answers: Which of the following is not a type of fault: low-angle detachment faults or transform faults?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not a type of fold that arches upward?

answers: NDQ_003385

answers: what is the first word in the passage?

answers: NDQ_003386

answers: Which of the following is not the cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: low-angle detachment faults or normal faults?

answers: NDQ_003388

answers: Which of the following is not a type of fault: long transform faults, low-angle detachment faults, or strike-slip faults?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: low-angle detachment

answers: NDQ_003391

answers: detachment

answers: NDQ_003392

answers: detachment

answers: NDQ_003393

answers: detachment fault

answers: NDQ_003394

answers: low-angle

answers: NDQ_003395

answers: low-angle

answers: NDQ_003396

answers: detachment faults

answers: NDQ_003351

answers: long transform faults

answers: NDQ_003352

answers: stripped away

answers: NDQ_003353

answers: long transform faults

answers: NDQ_003354

answers: Oceanic core complex structures form at slow spreading oceanic plate boundaries

answers: NDQ_003355

answers: Rift valleys

answers: NDQ_003356

answers: long transform faults

answers: NDQ_003357

answers: uplifted side

answers: NDQ_003358

answers: Rift valleys

answers: NDQ_003359

answers: uplifted

answers: NDQ_003360

answers: low-angle detachment faults.

answers: NDQ_003362

answers: Rift valleys do not develop along the expansion axes

answers: NDQ_003363

answers: slow spreading oceanic plate boundaries

answers: NDQ_003371

answers: long transform faults

answers: NDQ_003373

answers: long transform faults

answers: NDQ_003376

answers: Rift valleys

answers: NDQ_003378

answers: uplifted

answers: NDQ_003379

answers: low-angle detachment faults.

answers: NDQ_003380

answers: Expansion

answers: NDQ_003381

answers: long transform faults

answers: NDQ_003382

answers: long transform faults

answers: NDQ_003383

answers: long transform faults

answers: NDQ_003384

answers: uplifted

answers: NDQ_003385

answers: long transform faults

answers: NDQ_003386

answers: Expansion

answers: NDQ_003387

answers: long transform faults

answers: NDQ_003388

answers: long transform faults

answers: NDQ_003389

answers: Expansion

answers: NDQ_003390

answers: low-angle detachment faults.

answers: NDQ_003391

answers: gabbroic

answers: NDQ_003392

answers: low-angle detachment faults.

answers: NDQ_003393

answers: uplifted

answers: NDQ_003394

answers: low-angle detachment faults.

answers: NDQ_003395

answers: low-angle detachment faults.

answers: NDQ_003396

answers: low-angle detachment faults.

text: If the body is constrained so that it cannot expand, then internal stress will be caused (or changed) by a change in temperature. This stress can be calculated by considering the strain that would occur if the body were free to expand and the stress required to reduce that strain to zero, through the stress/strain relationship characterised by the elastic or Young's modulus. In the special case of solid materials, external ambient pressure does not usually appreciably affect the size of an object and so it is not usually necessary to consider the effect of pressure changes.

text: If the body is constrained so that it cannot expand, then internal stress will be caused (or changed) by a change in temperature. This stress can be calculated by considering the strain that would occur if the body were free to expand and the stress required to reduce that strain to zero, through the stress/strain relationship characterised by the elastic or

text: Young's modulus

text: . In the special case of

text: solid

text: materials, external ambient pressure does not usually appreciably affect the size of an object and so it is not usually necessary to consider the effect of pressure changes.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: change in temperature

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: strain

answers: NDQ_003356

answers: expand

answers: NDQ_003357

answers: internal stress will be caused (or changed) by a change in temperature

answers: NDQ_003358

answers: stress

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: external ambient pressure

answers: NDQ_003362

answers: it is not usually necessary to consider the effect of pressure changes.

answers: NDQ_003363

answers: external ambient pressure

answers: NDQ_003371

answers: What would occur if the body were free to expand?

answers: NDQ_003373

answers: it is not usually necessary to consider the effect of pressure changes

answers: NDQ_003376

answers: compressive forces

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: strike-slip fault

answers: NDQ_003380

answers: what is the special case of solid materials

answers: NDQ_003381

answers: unanswerable

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: Fault zone

answers: NDQ_003386

answers: movement of rock at faults

answers: NDQ_003387

answers: What can be calculated by considering the strain that would occur if the body were free to expand?

answers: NDQ_003388

answers: What can be calculated by considering the strain that would occur if the body were free to expand?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: a dip-slip fault

answers: NDQ_003392

answers: unanswerable

answers: NDQ_003393

answers: a dip-slip fault

answers: NDQ_003394

answers: isosceles

answers: NDQ_003395

answers: is not usually necessary to consider the effect of pressure changes

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: internal stress

answers: NDQ_003352

answers: external ambient pressure does not usually appreciably affect the size of an object

answers: NDQ_003353

answers: change in temperature.

answers: NDQ_003354

answers: external ambient pressure

answers: NDQ_003355

answers: elastic

answers: NDQ_003356

answers: external ambient pressure

answers: NDQ_003357

answers: internal stress will be caused (or changed) by a change in temperature.

answers: NDQ_003358

answers: solid materials, external ambient pressure

answers: NDQ_003359

answers: external ambient pressure

answers: NDQ_003360

answers: external ambient pressure

answers: NDQ_003362

answers: internal stress will be caused (or changed) by a change in temperature.

answers: NDQ_003363

answers: temperature.

answers: NDQ_003371

answers: internal stress will be caused (or changed) by a change in temperature.

answers: NDQ_003373

answers: external ambient pressure

answers: NDQ_003376

answers: external ambient pressure

answers: NDQ_003378

answers: external ambient pressure

answers: NDQ_003379

answers: Young's modulus.

answers: NDQ_003380

answers: external ambient pressure

answers: NDQ_003381

answers: solid materials,

answers: NDQ_003382

answers: internal stress

answers: NDQ_003383

answers: external ambient pressure

answers: NDQ_003384

answers: Young's modulus.

answers: NDQ_003385

answers: Young's modulus.

answers: NDQ_003386

answers: internal stress will be caused (or changed) by a change in temperature.

answers: NDQ_003387

answers: internal stress will be caused (or changed) by a change in temperature.

answers: NDQ_003388

answers: external ambient pressure

answers: NDQ_003389

answers: solid materials,

answers: NDQ_003390

answers: Young's modulus.

answers: NDQ_003391

answers: solid materials,

answers: NDQ_003392

answers: If the body is constrained so that it cannot expand, then internal stress

answers: NDQ_003393

answers: solid materials,

answers: NDQ_003394

answers: internal stress will be caused (or changed) by a change in temperature.

answers: NDQ_003395

answers: Young's modulus.

answers: NDQ_003396

answers: Young's modulus.

text: An abyssal plain is an underwater plain on the deep ocean floor, usually found at depths between  and . Lying generally between the foot of a continental rise and a mid-ocean ridge, abyssal plains are among the flattest, smoothest and least explored regions on Earth. Abyssal plains are key geologic elements of oceanic basins (the other elements being an elevated mid-ocean ridge and flanking abyssal hills). In addition to these elements, active oceanic basins (those that are associated with a moving plate tectonic boundary) also typically include an oceanic trench and a subduction zone. Abyssal plains cover more than 33% of the ocean floor (about 23% of Earth’s surface), but they are poorly preserved in the sedimentary record because they tend to be consumed by the subduction process.

text: An

text: abyssal plain

text: is an underwater

text: plain

text: on the deep

text: ocean floor

text: , usually found at depths between  and . Lying generally between the foot of a

text: continental rise

text: and a

text: mid-ocean ridge

text: , abyssal plains are among the flattest, smoothest and least explored regions on Earth. Abyssal plains are key geologic elements of

text: oceanic basin

text: s (the other elements being an elevated mid-ocean ridge and flanking

text: abyssal hill

text: s). In addition to these elements, active oceanic basins (those that are associated with a moving

text: plate tectonic

text: boundary) also typically include an

text: oceanic trench

text: and a

text: subduction zone

text: . Abyssal plains cover more than 33% of the ocean floor (about 23% of Earth’s surface), but they are poorly preserved in the

text: sedimentary record

text: because they tend to be consumed by the subduction process.

answers: NDQ_003351

answers: subduction zone

answers: NDQ_003352

answers: is more likely to crack

answers: NDQ_003353

answers: subduction

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: ridge

answers: NDQ_003356

answers: consume

answers: NDQ_003357

answers: oceanic trench and a subduction zone

answers: NDQ_003358

answers: oceanic trench

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: continental rise

answers: NDQ_003362

answers: Abyssal plains cover more than 33% of the ocean floor

answers: NDQ_003363

answers: Abyssal plains

answers: NDQ_003371

answers: Which of the following is not an element of active oceanic basins?

answers: NDQ_003373

answers: abyssal plains

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a stress?

answers: NDQ_003381

answers: Which of the following is not an element of oceanic basins: oceanic trench, abyssal plains, or subduction zone?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: active oceanic basins

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: normal faults or subduction zone?

answers: NDQ_003388

answers: Which of the following is not a result of shear stress: strike-slip faults, abyssal plains, or subduction zone?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: subduction zone

answers: NDQ_003391

answers: subduction zone

answers: NDQ_003392

answers: subduction zone

answers: NDQ_003393

answers: elevated mid-ocean ridge

answers: NDQ_003394

answers: oceanic trench

answers: NDQ_003395

answers: oceanic trench

answers: NDQ_003396

answers: oceanic trench

answers: NDQ_003351

answers: subduction zone.

answers: NDQ_003352

answers: consumed by the subduction process.

answers: NDQ_003353

answers: subduction process.

answers: NDQ_003354

answers: An abyssal plain

answers: NDQ_003355

answers: oceanic trench

answers: NDQ_003356

answers: consumed by the subduction process.

answers: NDQ_003357

answers: oceanic trench and a subduction zone.

answers: NDQ_003358

answers: abyssal plain

answers: NDQ_003359

answers: moving plate tectonic boundary)

answers: NDQ_003360

answers: tectonic boundary)

answers: NDQ_003362

answers: An abyssal plain

answers: NDQ_003363

answers: abyssal hills).

answers: NDQ_003371

answers: oceanic trench and a subduction zone.

answers: NDQ_003373

answers: abyssal plain

answers: NDQ_003376

answers: oceanic basins

answers: NDQ_003378

answers: oceanic trench and a subduction zone.

answers: NDQ_003379

answers: oceanic trench and a subduction zone.

answers: NDQ_003380

answers: oceanic trench and a subduction zone.

answers: NDQ_003381

answers: oceanic trench and a subduction zone.

answers: NDQ_003382

answers: oceanic trench and a subduction zone.

answers: NDQ_003383

answers: oceanic trench and a subduction zone.

answers: NDQ_003384

answers: elevated mid-ocean ridge

answers: NDQ_003385

answers: subduction zone.

answers: NDQ_003386

answers: moving plate tectonic boundary)

answers: NDQ_003387

answers: oceanic trench and a subduction zone.

answers: NDQ_003388

answers: oceanic trench and a subduction zone.

answers: NDQ_003389

answers: abyssal hills).

answers: NDQ_003390

answers: oceanic trench and a subduction zone.

answers: NDQ_003391

answers: subduction zone.

answers: NDQ_003392

answers: oceanic trench and a subduction zone.

answers: NDQ_003393

answers: mid-ocean ridge

answers: NDQ_003394

answers: oceanic trench and a subduction zone.

answers: NDQ_003395

answers: oceanic trench and a subduction zone.

answers: NDQ_003396

answers: oceanic trench and a subduction zone.

text: The Hikurangi Trench (also called the Hikurangi Trough) is a linear feature in the bed of the Pacific Ocean off the east coast of the North Island of New Zealand, lying between the southern end of the Cook Strait and the Chatham Rise.  Though much shallower, it is the southward continuation of the Kermadec Trench and forms part of the Kermadec-Tonga subduction zone. It represents the part of the subduction zone where the thick oceanic Hikurangi Plateau is subducting beneath continental crust of the Indo-Australian Plate. By contrast, the Kermadec and Tonga Trenches represent the parts of the subduction zone where oceanic crust of the Pacific Plate is subducting beneath oceanic crust of the Indo-Australian Plate.

text: The Hikurangi Trench (also called the Hikurangi Trough) is a linear feature in the bed of the

text: Pacific Ocean

text: off the east coast of the

text: North Island

text: of New Zealand, lying between the southern end of the

text: Cook Strait

text: and the

text: Chatham Rise

text: .  Though much shallower, it is the southward continuation of the

text: Kermadec Trench

text: and forms part of the

text: Kermadec-Tonga subduction zone

text: . It represents the part of the

text: subduction

text: zone where the thick oceanic

text: Hikurangi Plateau

text: is subducting beneath

text: continental crust

text: of the

text: Indo-Australian Plate

text: . By contrast, the Kermadec and

text: Tonga Trench

text: es represent the parts of the subduction zone where

text: oceanic crust

text: of the

text: Pacific Plate

text: is subducting beneath oceanic crust of the Indo-Australian Plate.

answers: NDQ_003351

answers: subduction

answers: NDQ_003352

answers: subducts

answers: NDQ_003353

answers: subduction

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: subduction zone

answers: NDQ_003356

answers: subduct

answers: NDQ_003357

answers: Hikurangi Plateau is subducting beneath continental crust

answers: NDQ_003358

answers: trough

answers: NDQ_003359

answers: subducts beneath continental crust

answers: NDQ_003360

answers: continental crust

answers: NDQ_003362

answers: the Kermadec and Tonga Trenches represent the parts of the subduction zone

answers: NDQ_003363

answers: Hikurangi Trench

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: Why is the Hikurangi Trench shallower?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: what is the part of the subduction zone where oceanic crust of the Pacific Plate is subducting beneath oceanic crust of the Indo-Australian Plate?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What type of stress does the Hikurangi Trench experience?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What type of fold is Hikurangi Trench?

answers: NDQ_003385

answers: What is the Kermadec-Tonga subduction zone?

answers: NDQ_003386

answers: What is the cause of earthquakes?

answers: NDQ_003387

answers: What type of stress is caused by normal faults?

answers: NDQ_003388

answers: What is the cause of strike-slip faults?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: subduction zone

answers: NDQ_003391

answers: Hikurangi Plateau

answers: NDQ_003392

answers: subduction zone

answers: NDQ_003393

answers: continental crust

answers: NDQ_003394

answers: subduction zone

answers: NDQ_003395

answers: The Hikurangi Trench

answers: NDQ_003396

answers: Hikurangi Trough

answers: NDQ_003351

answers: Indo-Australian Plate.

answers: NDQ_003352

answers: subducting

answers: NDQ_003353

answers: subducting

answers: NDQ_003354

answers: The Hikurangi Trench

answers: NDQ_003355

answers: Plateau

answers: NDQ_003356

answers: subducting

answers: NDQ_003357

answers: subducting beneath continental crust of the Indo-Australian Plate.

answers: NDQ_003358

answers: The Hikurangi Trench

answers: NDQ_003359

answers: subducting

answers: NDQ_003360

answers: subducting beneath continental crust of the Indo-Australian Plate.

answers: NDQ_003362

answers: The Hikurangi Trench

answers: NDQ_003363

answers: Kermadec-Tonga subduction zone.

answers: NDQ_003371

answers: The Hikurangi Trench

answers: NDQ_003373

answers: continental crust of the Indo-Australian Plate.

answers: NDQ_003376

answers: Kermadec-Tonga subduction zone.

answers: NDQ_003378

answers: Kermadec-Tonga subduction zone.

answers: NDQ_003379

answers: Kermadec-Tonga subduction zone.

answers: NDQ_003380

answers: Kermadec-Tonga subduction zone.

answers: NDQ_003381

answers: Kermadec-Tonga subduction zone.

answers: NDQ_003382

answers: Indo-Australian Plate.

answers: NDQ_003383

answers: The Hikurangi Trench

answers: NDQ_003384

answers: The Hikurangi Trench

answers: NDQ_003385

answers: Kermadec-Tonga subduction zone.

answers: NDQ_003386

answers: subduction zone.

answers: NDQ_003387

answers: Kermadec-Tonga subduction zone.

answers: NDQ_003388

answers: Kermadec-Tonga subduction zone.

answers: NDQ_003389

answers: subducting beneath continental crust

answers: NDQ_003390

answers: The Hikurangi Trench

answers: NDQ_003391

answers: oceanic Hikurangi Plateau

answers: NDQ_003392

answers: The Hikurangi Trench

answers: NDQ_003393

answers: Hikurangi Plateau

answers: NDQ_003394

answers: Kermadec-Tonga subduction zone.

answers: NDQ_003395

answers: Indo-Australian Plate.

answers: NDQ_003396

answers: Kermadec-Tonga subduction zone.

text: The collision between terranes folded the Earth's crust, and produced enough heat and pressure to metamorphose then-existing rock. Repeated continental collisions, compression along a north-south axis, and subduction resulted in the uprising of the Algoman Mountains. This was followed by intrusions of granite plutons and batholithic domes within the gneisses about ; two examples are the Sacred Heart granite of southwestern Minnesota and the Watersmeet Domes metagabbros (metamorphosed gabbros) that straddle the border of Wisconsin and Michigan's Upper Peninsula. After the intrusions solidified, new stresses on the greenstone belt caused movement horizontally along several faults and moved huge blocks of the crust vertically relative to adjacent blocks. This combination of folding, intrusion and faulting built mountain ranges throughout northern Minnesota, northern Wisconsin, Michigan's Upper Peninsula and southernmost Ontario. Igneous and high-grade metamorphic rocks are associated with the orogeny.

text: The collision between terranes folded the Earth's crust, and produced enough heat and pressure to

text: metamorphose

text: then-existing rock. Repeated continental collisions, compression along a north-south axis, and

text: subduction

text: resulted in the uprising of the Algoman Mountains. This was followed by intrusions of

text: granite

text: pluton

text: s and

text: batholithic domes

text: within the gneisses about ; two examples are the

text: Sacred Heart granite

text: of southwestern Minnesota and the Watersmeet Domes metagabbros (metamorphosed

text: gabbro

text: s) that straddle the border of Wisconsin and Michigan's

text: Upper Peninsula

text: . After the intrusions solidified, new stresses on the greenstone belt caused movement horizontally along several faults and moved huge blocks of the crust vertically relative to adjacent blocks. This combination of folding, intrusion and faulting built mountain ranges throughout northern Minnesota, northern Wisconsin, Michigan's Upper Peninsula and southernmost Ontario. Igneous and high-grade metamorphic rocks are associated with the orogeny.

answers: NDQ_003351

answers: subduction

answers: NDQ_003352

answers: moves vertically

answers: NDQ_003353

answers: movement

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: vertical fold

answers: NDQ_003356

answers: solidify

answers: NDQ_003357

answers: vertically relative to adjacent blocks

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: faulting

answers: NDQ_003362

answers: The collision between terranes folded the Earth's crust

answers: NDQ_003363

answers: northern Minnesota, northern Wisconsin

answers: NDQ_003371

answers: Which of the following is not a type of fault: folding, intrusion and faulting

answers: NDQ_003373

answers: yes

answers: NDQ_003376

answers: Which of the following is not caused by compressive forces: folding, intrusion and faulting

answers: NDQ_003378

answers: vertically relative to adjacent blocks

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What type of force applied to rock is a stress?

answers: NDQ_003381

answers: What type of stress does the collision between terranes cause?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Faulting

answers: NDQ_003384

answers: What was followed by intrusions of granite plutons and batholithic domes

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: horizontally

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: Which of the following is not an example of a strike-slip fault?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: subduction

answers: NDQ_003391

answers: huge blocks of the crust

answers: NDQ_003392

answers: vertically

answers: NDQ_003393

answers: vertically

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: huge blocks of the crust

answers: NDQ_003396

answers: vertically

answers: NDQ_003351

answers: subduction

answers: NDQ_003352

answers: movement horizontally along several faults

answers: NDQ_003353

answers: movement horizontally along several faults

answers: NDQ_003354

answers: Sacred Heart granite

answers: NDQ_003355

answers: subduction

answers: NDQ_003356

answers: metamorphose

answers: NDQ_003357

answers: moved huge blocks of the crust vertically relative to adjacent blocks.

answers: NDQ_003358

answers: faults

answers: NDQ_003359

answers: stresses

answers: NDQ_003360

answers: folding, intrusion and faulting

answers: NDQ_003362

answers: huge blocks of the crust vertically relative to adjacent blocks.

answers: NDQ_003363

answers: northern Minnesota, northern Wisconsin, Michigan's Upper Peninsula and southernmost Ontario.

answers: NDQ_003371

answers: faults

answers: NDQ_003373

answers: compression along a north-south axis,

answers: NDQ_003376

answers: mountain ranges

answers: NDQ_003378

answers: vertically relative to adjacent blocks.

answers: NDQ_003379

answers: vertically relative to adjacent blocks.

answers: NDQ_003380

answers: stresses

answers: NDQ_003381

answers: moved huge blocks of the crust vertically relative to adjacent blocks.

answers: NDQ_003382

answers: compression along a north-south axis,

answers: NDQ_003383

answers: faults

answers: NDQ_003384

answers: vertically relative to adjacent blocks.

answers: NDQ_003385

answers: faults

answers: NDQ_003386

answers: moved huge blocks of the crust vertically relative to adjacent blocks.

answers: NDQ_003387

answers: compression along a north-south axis,

answers: NDQ_003388

answers: new stresses

answers: NDQ_003389

answers: folding, intrusion and faulting

answers: NDQ_003390

answers: faults

answers: NDQ_003391

answers: huge blocks of the crust vertically relative to adjacent blocks.

answers: NDQ_003392

answers: faults and moved huge blocks of the crust vertically relative to adjacent blocks.

answers: NDQ_003393

answers: vertically relative to adjacent blocks.

answers: NDQ_003394

answers: horizontally

answers: NDQ_003395

answers: faults and moved huge blocks of the crust vertically relative to adjacent blocks.

answers: NDQ_003396

answers: faults

text: At the occasion of his 80th birthday the Swiss Geological Society honoured Ziegler with a symposium on the theme “Deep Earth - from Crust to Core”, held in Lugano, November 23, 2008.

text: At the occasion of his 80th birthday the Swiss Geological Society honoured Ziegler with a symposium on the theme “Deep Earth - from Crust to Core”, held in Lugano, November 23, 2008.

answers: NDQ_003351

answers: Deep Earth

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: trough

answers: NDQ_003356

answers: shrink

answers: NDQ_003357

answers: Deep Earth - from Crust to Core

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: Deep Earth - from Crust to Core

answers: NDQ_003363

answers: Deep Earth

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: How would you describe Ziegler?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: Ziegler

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What is Ziegler's profession?

answers: NDQ_003381

answers: What does Ziegler mean?

answers: NDQ_003382

answers: Ziegler

answers: NDQ_003383

answers: what is the reason for joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: Ziegler

answers: NDQ_003387

answers: Ziegler

answers: NDQ_003388

answers: Ziegler

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: can be used to describe

answers: NDQ_003391

answers: dip-slip fault

answers: NDQ_003392

answers: can be used to describe

answers: NDQ_003393

answers: dip-slip fault

answers: NDQ_003394

answers: is a fault

answers: NDQ_003395

answers: Ziegler

answers: NDQ_003396

answers: Ziegler

answers: NDQ_003351

answers: “Deep Earth - from Crust to Core”,

answers: NDQ_003352

answers: “Deep Earth - from Crust to Core”,

answers: NDQ_003353

answers: Crust to Core”,

answers: NDQ_003354

answers: At the occasion of his 80th birthday the Swiss Geological Society

answers: NDQ_003355

answers: “Deep Earth

answers: NDQ_003356

answers: Crust to Core”,

answers: NDQ_003357

answers: “Deep Earth - from Crust to Core”,

answers: NDQ_003358

answers: “Deep Earth

answers: NDQ_003359

answers: “Deep Earth - from Crust to Core”,

answers: NDQ_003360

answers: “Deep Earth

answers: NDQ_003362

answers: “Deep Earth - from Crust to Core”,

answers: NDQ_003363

answers: “Deep Earth

answers: NDQ_003371

answers: “Deep Earth - from Crust to Core”,

answers: NDQ_003373

answers: “Deep Earth - from Crust to Core”,

answers: NDQ_003376

answers: “Deep Earth - from Crust to Core”,

answers: NDQ_003378

answers: “Deep Earth - from Crust to Core”,

answers: NDQ_003379

answers: 2008.

answers: NDQ_003380

answers: “Deep Earth - from Crust to Core”,

answers: NDQ_003381

answers: “Deep Earth - from Crust to Core”,

answers: NDQ_003382

answers: “Deep Earth - from Crust to Core”,

answers: NDQ_003383

answers: “Deep Earth - from Crust to Core”,

answers: NDQ_003384

answers: “Deep Earth - from Crust to Core”,

answers: NDQ_003385

answers: “Deep Earth - from Crust to Core”,

answers: NDQ_003386

answers: “Deep Earth - from Crust to Core”,

answers: NDQ_003387

answers: “Deep Earth - from Crust to Core”,

answers: NDQ_003388

answers: “Deep Earth - from Crust to Core”,

answers: NDQ_003389

answers: “Deep Earth

answers: NDQ_003390

answers: “Deep Earth

answers: NDQ_003391

answers: “Deep Earth - from Crust to Core”,

answers: NDQ_003392

answers: “Deep Earth - from Crust to Core”,

answers: NDQ_003393

answers: “Deep Earth - from Crust to Core”,

answers: NDQ_003394

answers: “Deep Earth

answers: NDQ_003395

answers: “Deep Earth

answers: NDQ_003396

answers: “Deep Earth - from Crust to Core”,

text: Tectonics explains the large-scale structure of the Earth's crust and its constituent rocks in terms of blocks moving along faults, uplifted into horsts or downthrown into grabens.The ACT is positioned on the Australian continent, which was once a part of the supercontinent Gondwana. The ACT is in the Tasmanides, the deformed rocks of the orogen that make up the core of the old mountain range that makes up the Australian continent east of the Tasman Line. These rocks are an addition onto the Proterozoic core of the continent. The Tasmanides are the result of compression, horizontal shortening, and vertical thickening of various "terranes" such as small continental fragments and volcanic island arcs that were plastered against the original continental margin as a result of plate tectonic movements.

text: Tectonics

text: explains the large-scale structure of the Earth's crust and its constituent rocks in terms of blocks moving along

text: fault

text: s, uplifted into

text: horst

text: s or downthrown into

text: graben

text: s.The ACT is positioned on the

text: Australian continent

text: , which was once a part of the supercontinent

text: Gondwana

text: . The ACT is in the

text: Tasmanides

text: , the deformed rocks of the

text: orogen

text: that make up the core of the old mountain range that makes up the Australian continent east of the

text: Tasman Line

text: . These rocks are an addition onto the

text: Proterozoic

text: core of the continent. The Tasmanides are the result of compression, horizontal shortening, and vertical thickening of various "terranes" such as small continental fragments and volcanic island arcs that were plastered against the original continental margin as a result of

text: plate tectonic

text: movements.

answers: NDQ_003351

answers: horizontal shortening

answers: NDQ_003352

answers: compresses

answers: NDQ_003353

answers: compression

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: graben

answers: NDQ_003356

answers: vertical thickening

answers: NDQ_003357

answers: blocks move along faults

answers: NDQ_003358

answers: graben

answers: NDQ_003359

answers: blocks moving along faults

answers: NDQ_003360

answers: plate tectonic movements

answers: NDQ_003362

answers: Tectonics explains the large-scale structure of the Earth's crust

answers: NDQ_003363

answers: Gondwana

answers: NDQ_003371

answers: Which of the following is not a result of plate tectonic movements?

answers: NDQ_003373

answers: How would you describe the Tasmanides?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: what is the last word in the passage?

answers: NDQ_003379

answers: vertical thickening of various "terranes

answers: NDQ_003380

answers: What is a stress?

answers: NDQ_003381

answers: What is the Tasmanides the result of?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: What is the cause of plate tectonic movements?

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: compression, horizontal shortening, or vertical thickening?

answers: NDQ_003388

answers: Which of the following is not a result of shear stress: compression, horizontal shortening, or vertical thickening?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: grabens

answers: NDQ_003391

answers: grabens

answers: NDQ_003392

answers: graben

answers: NDQ_003393

answers: grabens

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: vertical thickening

answers: NDQ_003396

answers: vertical thickening

answers: NDQ_003351

answers: uplifted into horsts

answers: NDQ_003352

answers: uplifted into horsts

answers: NDQ_003353

answers: compression, horizontal shortening, and vertical thickening

answers: NDQ_003354

answers: The ACT is in the Tasmanides,

answers: NDQ_003355

answers: grabens.The

answers: NDQ_003356

answers: compression, horizontal shortening, and vertical thickening

answers: NDQ_003357

answers: blocks

answers: NDQ_003358

answers: horsts or downthrown into grabens.The

answers: NDQ_003359

answers: blocks moving along faults,

answers: NDQ_003360

answers: faults,

answers: NDQ_003362

answers: once a part of the supercontinent Gondwana.

answers: NDQ_003363

answers: plate tectonic movements.

answers: NDQ_003371

answers: Tectonics

answers: NDQ_003373

answers: The Tasmanides

answers: NDQ_003376

answers: The Tasmanides

answers: NDQ_003378

answers: blocks moving along faults,

answers: NDQ_003379

answers: vertical thickening

answers: NDQ_003380

answers: compression,

answers: NDQ_003381

answers: compression, horizontal shortening, and vertical thickening

answers: NDQ_003382

answers: compression,

answers: NDQ_003383

answers: compression,

answers: NDQ_003384

answers: horsts or downthrown into grabens.The

answers: NDQ_003385

answers: faults,

answers: NDQ_003386

answers: blocks moving along faults,

answers: NDQ_003387

answers: compression, horizontal shortening, and vertical thickening

answers: NDQ_003388

answers: Tectonics

answers: NDQ_003389

answers: compression, horizontal shortening, and vertical thickening

answers: NDQ_003390

answers: grabens.The

answers: NDQ_003391

answers: grabens.The

answers: NDQ_003392

answers: horsts or downthrown into grabens.The

answers: NDQ_003393

answers: horsts

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: vertical thickening

answers: NDQ_003396

answers: grabens.The

text: The structure of Earth can be defined in two ways: by mechanical properties such as rheology, or chemically. Mechanically, it can be divided into lithosphere, asthenosphere, mesospheric mantle, outer core, and the inner core. Chemically, Earth can be divided into the crust, upper mantle, lower mantle, outer core, and inner core. The geologic component layers of Earth are at the following depths below the surface:

text: The structure of Earth can be defined in two ways: by mechanical properties such as

text: rheology

text: , or chemically. Mechanically, it can be divided into

text: lithosphere

text: asthenosphere

text: mesospheric mantle

text: outer core

text: , and the

text: inner core

text: . Chemically, Earth can be divided into the crust, upper mantle, lower mantle, outer core, and inner core. The geologic component layers of Earth are at the following depths below the surface:

answers: NDQ_003351

answers: rheology

answers: NDQ_003352

answers: is more likely to crack

answers: NDQ_003353

answers: chemical changes

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: asthenosphere

answers: NDQ_003356

answers: swell

answers: NDQ_003357

answers: Earth can be divided into the crust, upper mantle, lower mantle, outer core, and inner core

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: tectonic plates

answers: NDQ_003362

answers: The San Andreas fault is located in the Pacific Ocean.

answers: NDQ_003363

answers: lithosphere

answers: NDQ_003371

answers: What is a thrust fault?

answers: NDQ_003373

answers: mechanically

answers: NDQ_003376

answers: mechanically

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: vertical

answers: NDQ_003380

answers: Which of the following is not a type of stress: mechanical, chemical, or rheological?

answers: NDQ_003381

answers: What can be defined mechanically?

answers: NDQ_003382

answers: what is the most common stress at convergent plates

answers: NDQ_003383

answers: mechanically

answers: NDQ_003384

answers: what is the first type of fold mentioned?

answers: NDQ_003385

answers: fault zone

answers: NDQ_003386

answers: mechanically

answers: NDQ_003387

answers: What can be defined by mechanical properties such as rheology?

answers: NDQ_003388

answers: What type of stress is shear stress?

answers: NDQ_003389

answers: chemically

answers: NDQ_003390

answers: a fault

answers: NDQ_003391

answers: lithosphere

answers: NDQ_003392

answers: rheology

answers: NDQ_003393

answers: lithosphere

answers: NDQ_003394

answers: lateral

answers: NDQ_003395

answers: isospheric

answers: NDQ_003396

answers: rheology

answers: NDQ_003351

answers: rheology,

answers: NDQ_003352

answers: following depths below the surface:

answers: NDQ_003353

answers: rheology,

answers: NDQ_003354

answers: following depths below the surface:

answers: NDQ_003355

answers: lithosphere, asthenosphere,

answers: NDQ_003356

answers: rheology,

answers: NDQ_003357

answers: following depths below the surface:

answers: NDQ_003358

answers: lithosphere, asthenosphere,

answers: NDQ_003359

answers: following depths below the surface:

answers: NDQ_003360

answers: following depths below the surface:

answers: NDQ_003362

answers: the following depths below the surface:

answers: NDQ_003363

answers: following depths below the surface:

answers: NDQ_003371

answers: following depths below the surface:

answers: NDQ_003373

answers: geologic component layers of Earth are at the following depths below the surface:

answers: NDQ_003376

answers: following depths below the surface:

answers: NDQ_003378

answers: following depths below the surface:

answers: NDQ_003379

answers: following depths below the surface:

answers: NDQ_003380

answers: following depths below the surface:

answers: NDQ_003381

answers: following depths below the surface:

answers: NDQ_003382

answers: mesospheric mantle,

answers: NDQ_003383

answers: rheology,

answers: NDQ_003384

answers: lithosphere, asthenosphere,

answers: NDQ_003385

answers: lithosphere,

answers: NDQ_003386

answers: following depths below the surface:

answers: NDQ_003387

answers: The structure of Earth

answers: NDQ_003388

answers: rheology,

answers: NDQ_003389

answers: following depths below the surface:

answers: NDQ_003390

answers: rheology,

answers: NDQ_003391

answers: lithosphere,

answers: NDQ_003392

answers: rheology,

answers: NDQ_003393

answers: lithosphere,

answers: NDQ_003394

answers: The structure of Earth

answers: NDQ_003395

answers: The structure of Earth

answers: NDQ_003396

answers: mesospheric mantle,

text: and the stress drop. Therefore, the longer the length and the wider the width of the faulted area, the larger the resulting magnitude. The topmost, brittle part of the Earth's crust, and the cool slabs of the tectonic plates that are descending down into the hot mantle, are the only parts of our planet which can store elastic energy and release it in fault ruptures. Rocks hotter than about 300 degrees Celsius flow in response to stress; they do not rupture in earthquakes. The maximum observed lengths of ruptures and mapped faults (which may break in a single rupture) are approximately 1000 km. Examples are the earthquakes in Chile, 1960; Alaska, 1957; Sumatra, 2004, all in subduction zones. The longest earthquake ruptures on strike-slip faults, like the San Andreas Fault (1857, 1906), the North Anatolian Fault in Turkey (1939) and the Denali Fault in Alaska (2002), are about half to one third as long as the lengths along subducting plate margins, and those along normal faults are even shorter.

text: and the stress drop. Therefore, the longer the length and the wider the width of the faulted area, the larger the resulting magnitude. The topmost, brittle part of the Earth's crust, and the cool slabs of the tectonic plates that are descending down into the hot mantle, are the only parts of our planet which can store elastic energy and release it in fault ruptures. Rocks hotter than about 300 degrees Celsius flow in response to stress; they do not rupture in earthquakes. The maximum observed lengths of ruptures and mapped faults (which may break in a single rupture) are approximately 1000 km. Examples are the earthquakes in

text: Chile, 1960

text: Alaska, 1957

text: Sumatra, 2004

text: , all in subduction zones. The longest earthquake ruptures on strike-slip faults, like the

text: San Andreas Fault

text: (1857, 1906), the

text: North Anatolian Fault

text: in Turkey (1939) and the

text: Denali Fault

text: in Alaska (2002), are about half to one third as long as the lengths along subducting plate margins, and those along normal faults are even shorter.

answers: NDQ_003351

answers: subducting

answers: NDQ_003352

answers: ruptures

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: subduction zone

answers: NDQ_003356

answers: rupture

answers: NDQ_003357

answers: the longest earthquake ruptures on strike-slip faults are even shorter

answers: NDQ_003358

answers: normal fault

answers: NDQ_003359

answers: ruptures in response to stress

answers: NDQ_003360

answers: strike-slip faults

answers: NDQ_003362

answers: rocks hotter than about 300 degrees Celsius flow in response to stress

answers: NDQ_003363

answers: subduction zones

answers: NDQ_003371

answers: What is the maximum observed lengths of ruptures and mapped faults?

answers: NDQ_003373

answers: What is the main idea of this passage?

answers: NDQ_003376

answers: What is the maximum observed lengths of ruptures and mapped faults?

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: no

answers: NDQ_003380

answers: Which of the following is not a stress?

answers: NDQ_003381

answers: What happens to rocks hotter than about 300 degrees Celsius?

answers: NDQ_003382

answers: what is the most common stress at convergent plates

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not a type of fold?

answers: NDQ_003385

answers: Fault zone

answers: NDQ_003386

answers: yes

answers: NDQ_003387

answers: Which of the following is not a type of normal fault?

answers: NDQ_003388

answers: What type of stress is shear stress?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: strike-slip fault

answers: NDQ_003391

answers: subduction zones

answers: NDQ_003392

answers: strike-slip fault

answers: NDQ_003393

answers: subducting plate margins

answers: NDQ_003394

answers: strike-slip faults

answers: NDQ_003395

answers: strike-slip

answers: NDQ_003396

answers: strike-slip

answers: NDQ_003351

answers: subduction zones.

answers: NDQ_003352

answers: Rocks hotter than about 300 degrees Celsius

answers: NDQ_003353

answers: Rocks hotter than about 300 degrees Celsius

answers: NDQ_003354

answers: hotter than about 300 degrees Celsius

answers: NDQ_003355

answers: subduction zones.

answers: NDQ_003356

answers: rupture in earthquakes.

answers: NDQ_003357

answers: shorter.

answers: NDQ_003358

answers: earthquakes.

answers: NDQ_003359

answers: Rocks hotter than about 300 degrees Celsius

answers: NDQ_003360

answers: strike-slip faults,

answers: NDQ_003362

answers: normal faults are even shorter.

answers: NDQ_003363

answers: subduction zones.

answers: NDQ_003371

answers: hotter than about 300 degrees Celsius

answers: NDQ_003373

answers: hotter than about 300 degrees Celsius

answers: NDQ_003376

answers: the longer the length and the wider the width of the faulted area,

answers: NDQ_003378

answers: rupture

answers: NDQ_003379

answers: strike-slip faults,

answers: NDQ_003380

answers: Rocks hotter than about 300 degrees Celsius flow in response to stress;

answers: NDQ_003381

answers: Rocks hotter than about 300 degrees Celsius

answers: NDQ_003382

answers: subduction zones.

answers: NDQ_003383

answers: Rocks hotter than about 300 degrees Celsius

answers: NDQ_003384

answers: fault ruptures.

answers: NDQ_003385

answers: the longer the length and the wider the width of the faulted area,

answers: NDQ_003386

answers: Rocks hotter than about 300 degrees Celsius

answers: NDQ_003387

answers: those along normal faults are even shorter.

answers: NDQ_003388

answers: strike-slip faults,

answers: NDQ_003389

answers: fault ruptures.

answers: NDQ_003390

answers: strike-slip faults,

answers: NDQ_003391

answers: hotter than about 300 degrees Celsius

answers: NDQ_003392

answers: strike-slip faults,

answers: NDQ_003393

answers: hotter than about 300 degrees Celsius

answers: NDQ_003394

answers: strike-slip faults,

answers: NDQ_003395

answers: strike-slip faults,

answers: NDQ_003396

answers: strike-slip faults,

text: This is a list of pastries, which are small cakes or confections made using pastry — a stiff dough enriched with fat. Some dishes, such as pies, are made of a pastry casing that covers or completely contains a filling of various sweet or savory ingredients. There are five basic types of pastry (a food that combines flour and fat) - these are shortcrust pastry, filo pastry, choux pastry, flaky pastry and puff pastry. Two main types of pastry are nonlaminated, when fat is cut or rubbed into the flour, and laminated, when fat is repeatedly folded into the dough using a technique called lamination. An example of a nonlaminated pastry would be a pie or tart crust and brioche. An example of a laminated pastry would be a croissant, danish, or puff pastry. Many pastries are prepared using shortening, a fat food product that is solid at room temperature, the composition of which lends to creating crumbly, shortcrust-style pastries and pastry crusts.

text: This is a list of pastries, which are small cakes or confections made using

text: pastry

text: — a stiff dough enriched with fat. Some dishes, such as pies, are made of a pastry casing that covers or completely contains a filling of various

text: sweet

text: or

text: savory

text: ingredients. There are five basic types of pastry (a food that combines

text: flour

text: and

text: fat

text: ) - these are

text: shortcrust pastry

text: filo pastry

text: choux pastry

text: flaky pastry

text: and

text: puff pastry

text: . Two main types of pastry are

text: nonlaminated

text: , when fat is cut or rubbed into the flour, and

text: laminated

text: , when fat is repeatedly folded into the dough using a technique called lamination. An example of a nonlaminated pastry would be a

text: pie

text: or

text: tart crust

text: and

text: brioche

text: . An example of a laminated pastry would be a

text: croissant

text: danish

text: , or

text: puff pastry

text: . Many pastries are prepared using

text: shortening

text: , a

text: fat

text: food product that is solid at room temperature, the composition of which lends to creating crumbly,

text: shortcrust

text: -style pastries and

text: pastry crust

text: s.

answers: NDQ_003351

answers: nonlaminated

answers: NDQ_003352

answers: is more likely to crack

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: choux

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: lamination is when fat is repeatedly folded into the dough

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: continental plates

answers: NDQ_003362

answers: pies are made of a pastry casing

answers: NDQ_003363

answers: the same time

answers: NDQ_003371

answers: What is a thrust fault?

answers: NDQ_003373

answers: compressive stresses

answers: NDQ_003376

answers: basin-and-range

answers: NDQ_003378

answers: slip

answers: NDQ_003379

answers: strike-slip fault

answers: NDQ_003380

answers: What is a stress?

answers: NDQ_003381

answers: What is a nonlaminated pastry?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: Fault zone

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: Which of the following is not a type of pastry?

answers: NDQ_003388

answers: unanswerable

answers: NDQ_003389

answers: lamination

answers: NDQ_003390

answers: Fracture

answers: NDQ_003391

answers: igneous rock

answers: NDQ_003392

answers: Fracture

answers: NDQ_003393

answers: igneous rock

answers: NDQ_003394

answers: horizontal fault

answers: NDQ_003395

answers: vertical fault plane

answers: NDQ_003396

answers: Flaky pastry

answers: NDQ_003351

answers: choux pastry, flaky pastry and puff pastry.

answers: NDQ_003352

answers: crumbly,

answers: NDQ_003353

answers: crumbly, shortcrust-style pastries and pastry crusts.

answers: NDQ_003354

answers: shortening,

answers: NDQ_003355

answers: croissant,

answers: NDQ_003356

answers: crumbly, shortcrust-style pastries

answers: NDQ_003357

answers: shortening, a fat food product that is solid at room temperature,

answers: NDQ_003358

answers: pastries,

answers: NDQ_003359

answers: pastry — a stiff dough enriched with fat.

answers: NDQ_003360

answers: five basic types of pastry

answers: NDQ_003362

answers: This is a list of pastries,

answers: NDQ_003363

answers: shortening, a fat food product that is solid at room temperature,

answers: NDQ_003371

answers: five basic types of pastry

answers: NDQ_003373

answers: five basic types of pastry

answers: NDQ_003376

answers: five basic types of pastry

answers: NDQ_003378

answers: five basic types of pastry

answers: NDQ_003379

answers: five basic types of pastry

answers: NDQ_003380

answers: five basic types of pastry

answers: NDQ_003381

answers: five basic types of pastry

answers: NDQ_003382

answers: choux pastry, flaky pastry and puff pastry.

answers: NDQ_003383

answers: five basic types of pastry

answers: NDQ_003384

answers: choux pastry, flaky pastry and puff pastry.

answers: NDQ_003385

answers: shortcrust pastry,

answers: NDQ_003386

answers: five basic types of pastry

answers: NDQ_003387

answers: choux pastry, flaky pastry and puff pastry.

answers: NDQ_003388

answers: choux pastry, flaky pastry and puff pastry.

answers: NDQ_003389

answers: laminated,

answers: NDQ_003390

answers: choux pastry, flaky pastry and puff pastry.

answers: NDQ_003391

answers: five

answers: NDQ_003392

answers: choux pastry, flaky pastry and puff pastry.

answers: NDQ_003393

answers: five

answers: NDQ_003394

answers: choux pastry, flaky pastry and puff pastry.

answers: NDQ_003395

answers: choux pastry, flaky pastry and puff pastry.

answers: NDQ_003396

answers: choux pastry, flaky pastry and puff pastry.

text: At well-studied plate boundaries like the San Andreas fault system in California, scientists can often make observations that allow them to identify the specific fault on which an earthquake took place. In contrast, east of the Rocky Mountains this is rarely the case. The NYC area  is far from the boundaries of the North American plate, which are in the center of the Atlantic Ocean, in the Caribbean Sea, and along the west coast of North America. The seismicity of the northeastern U.S. is generally considered to be due to ancient zones of weakness that are being reactivated in the present-day stress field. In this model, pre-existing faults that were formed during ancient geological episodes, persist in the intraplate crust, and the earthquakes occur when the present-day stress is released along these zones of weakness. The stress that causes the earthquakes is generally considered to be derived from present-day rifting at the Mid-Atlantic ridge.

text: At well-studied plate boundaries like the

text: San Andreas fault

text: system in California, scientists can often make observations that allow them to identify the specific fault on which an earthquake took place. In contrast, east of the Rocky Mountains this is rarely the case. The NYC area  is far from the boundaries of the North American plate, which are in the center of the Atlantic Ocean, in the Caribbean Sea, and along the west coast of North America. The seismicity of the northeastern U.S. is generally considered to be due to ancient zones of weakness that are being reactivated in the present-day stress field. In this model, pre-existing faults that were formed during ancient geological episodes, persist in the intraplate crust, and the earthquakes occur when the present-day stress is released along these zones of weakness. The stress that causes the earthquakes is generally considered to be derived from present-day rifting at the

text: Mid-Atlantic ridge

answers: NDQ_003351

answers: present-day

answers: NDQ_003352

answers: more likely to crack

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: Rocky Mountains

answers: NDQ_003356

answers: cause earthquakes

answers: NDQ_003357

answers: present-day stress is released along these zones of weakness

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: weakens

answers: NDQ_003360

answers: plate boundaries

answers: NDQ_003362

answers: east of the Rocky Mountains this is rarely the case

answers: NDQ_003363

answers: San Andreas fault system

answers: NDQ_003371

answers: Which of the following is not a type of fault?

answers: NDQ_003373

answers: what is the last word in the passage?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: what is the stress that causes the earthquakes

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: what is the last word in the passage?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: faults that are clustered

answers: NDQ_003386

answers: yes

answers: NDQ_003387

answers: What type of stress is released along these zones of weakness?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip faults or strike-slip faults?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: San Andreas fault

answers: NDQ_003391

answers: zone of weakness

answers: NDQ_003392

answers: San Andreas fault

answers: NDQ_003393

answers: Rocky Mountains

answers: NDQ_003394

answers: San Andreas fault

answers: NDQ_003395

answers: San Andreas fault system

answers: NDQ_003396

answers: San Andreas fault system

answers: NDQ_003351

answers: present-day rifting

answers: NDQ_003352

answers: released along these zones of weakness.

answers: NDQ_003353

answers: the earthquakes

answers: NDQ_003354

answers: east of the Rocky Mountains

answers: NDQ_003355

answers: fault

answers: NDQ_003356

answers: earthquakes

answers: NDQ_003357

answers: the present-day stress is released along these zones of weakness.

answers: NDQ_003358

answers: faults

answers: NDQ_003359

answers: stress is released

answers: NDQ_003360

answers: plate boundaries

answers: NDQ_003362

answers: east of the Rocky Mountains

answers: NDQ_003363

answers: ancient geological episodes,

answers: NDQ_003371

answers: pre-existing faults

answers: NDQ_003373

answers: pre-existing faults that were formed during ancient geological episodes,

answers: NDQ_003376

answers: ancient zones of weakness

answers: NDQ_003378

answers: present-day stress

answers: NDQ_003379

answers: east of the Rocky Mountains

answers: NDQ_003380

answers: stress

answers: NDQ_003381

answers: the present-day stress is released

answers: NDQ_003382

answers: rifting at the Mid-Atlantic ridge.

answers: NDQ_003383

answers: Mid-Atlantic ridge.

answers: NDQ_003384

answers: east of the Rocky Mountains

answers: NDQ_003385

answers: zones of weakness.

answers: NDQ_003386

answers: the present-day stress is released along these zones of weakness.

answers: NDQ_003387

answers: present-day stress is released along these zones of weakness.

answers: NDQ_003388

answers: the present-day stress is released along these zones of weakness.

answers: NDQ_003389

answers: Rocky Mountains

answers: NDQ_003390

answers: San Andreas fault

answers: NDQ_003391

answers: intraplate crust,

answers: NDQ_003392

answers: San Andreas fault

answers: NDQ_003393

answers: Rocky Mountains

answers: NDQ_003394

answers: San Andreas fault system

answers: NDQ_003395

answers: San Andreas

answers: NDQ_003396

answers: San Andreas

text: Mountain formation refers to the geological processes that underlie the formation of mountains. These processes are associated with large-scale movements of the Earth's  crust (plate tectonics).  Folding, faulting, volcanic activity, igneous intrusion and metamorphism can all be parts of the orogenic process of mountain building. The understanding of specific landscape features in terms of the underlying tectonic processes is called tectonic geomorphology, and the study of geologically young or ongoing processes is called neotectonics.

text: Mountain formation refers to the geological processes that underlie the formation of

text: mountain

text: s. These processes are associated with large-scale movements of the Earth's  crust (

text: plate tectonics

text: Folding

text: faulting

text: volcanic activity

text: igneous intrusion

text: and

text: metamorphism

text: can all be parts of the

text: orogenic process

text: of mountain building. The understanding of specific landscape features in terms of the underlying tectonic processes is called

text: tectonic geomorphology

text: , and the study of geologically young or ongoing processes is called

text: neotectonics

answers: NDQ_003351

answers: faulting

answers: NDQ_003352

answers: folds

answers: NDQ_003353

answers: metamorphism

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: faulting

answers: NDQ_003356

answers: metamorphize

answers: NDQ_003357

answers: large-scale movements of the Earth's crust

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: plate tectonics

answers: NDQ_003362

answers: volcanic activity can all be parts of the orogenic process of mountain building

answers: NDQ_003363

answers: plate tectonics

answers: NDQ_003371

answers: What can all be parts of the orogenic process of mountain building?

answers: NDQ_003373

answers: How would you describe a rock that is under compressive stresses?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: large-scale movements of the Earth's crust

answers: NDQ_003379

answers: What is the name of the process that underlie the formation of mountains?

answers: NDQ_003380

answers: What type of movement of the Earth's crust is associated with large-scale movements of the Earth's crust?

answers: NDQ_003381

answers: What is the term for tectonic geomorphology?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: What is the name of the process that underlies the formation of mountains?

answers: NDQ_003385

answers: What is the term for an area where faults are clustered?

answers: NDQ_003386

answers: plate tectonics

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: folding, faulting, volcanic activity, igneous intrusion or metamorphism?

answers: NDQ_003388

answers: Which of the following is not a geological process: folding, faulting, volcanic activity, igneous intrusion and metamorphism

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: faulting

answers: NDQ_003391

answers: mountain

answers: NDQ_003392

answers: faulting

answers: NDQ_003393

answers: mountain

answers: NDQ_003394

answers: faulting

answers: NDQ_003395

answers: NDQ_003396

answers: faulting

answers: NDQ_003351

answers: faulting,

answers: NDQ_003352

answers: metamorphism

answers: NDQ_003353

answers: metamorphism

answers: NDQ_003354

answers: Mountain formation

answers: NDQ_003355

answers: faulting,

answers: NDQ_003356

answers: metamorphism

answers: NDQ_003357

answers: faulting,

answers: NDQ_003358

answers: igneous intrusion and metamorphism

answers: NDQ_003359

answers: faulting,

answers: NDQ_003360

answers: (plate tectonics).

answers: NDQ_003362

answers: Mountain formation

answers: NDQ_003363

answers: large-scale movements of the Earth's crust

answers: NDQ_003371

answers: neotectonics.

answers: NDQ_003373

answers: tectonic geomorphology,

answers: NDQ_003376

answers: tectonic geomorphology,

answers: NDQ_003378

answers: tectonic geomorphology,

answers: NDQ_003379

answers: tectonic geomorphology,

answers: NDQ_003380

answers: Folding, faulting,

answers: NDQ_003381

answers: tectonic geomorphology,

answers: NDQ_003382

answers: tectonic geomorphology,

answers: NDQ_003383

answers: igneous intrusion and metamorphism

answers: NDQ_003384

answers: tectonic geomorphology,

answers: NDQ_003385

answers: tectonic geomorphology,

answers: NDQ_003386

answers: large-scale movements of the Earth's crust

answers: NDQ_003387

answers: tectonic geomorphology,

answers: NDQ_003388

answers: tectonic geomorphology,

answers: NDQ_003389

answers: Folding,

answers: NDQ_003390

answers: faulting,

answers: NDQ_003391

answers: igneous intrusion

answers: NDQ_003392

answers: faulting,

answers: NDQ_003393

answers: igneous intrusion

answers: NDQ_003394

answers: faulting,

answers: NDQ_003395

answers: faulting,

answers: NDQ_003396

answers: faulting,

text: Early Earth's mantle was hotter and it has been proposed that flat slab subduction was the dominant style. Computer modeling has shown that an increase in oceanic plate buoyancy associated with enhanced oceanic crust production would have the been counteracted by decreased mantle viscosity, so flat slab subduction would not have been dominant or non-existent.

text: Early Earth's mantle was hotter and it has been proposed that flat slab subduction was the dominant style. Computer modeling has shown that an increase in oceanic plate buoyancy associated with enhanced oceanic crust production would have the been counteracted by decreased mantle viscosity, so flat slab subduction would not have been dominant or non-existent.

answers: NDQ_003351

answers: flat slab subduction

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: subduction

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: subduction

answers: NDQ_003356

answers: subduct

answers: NDQ_003357

answers: flat slab subduction would not have been dominant

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: oceanic plate

answers: NDQ_003362

answers: flat slab subduction would not have been dominant or non-existent

answers: NDQ_003363

answers: Early Earth

answers: NDQ_003371

answers: Which of the following is not a type of subduction?

answers: NDQ_003373

answers: How would you describe a rock that is deeply buried?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: Which of the following is not a type of stress?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not a type of fold?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: Which of the following is not a type of normal fault?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip, flat slab, or non-existent?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: flat slab subduction

answers: NDQ_003391

answers: oceanic crust

answers: NDQ_003392

answers: subduction

answers: NDQ_003393

answers: oceanic crust

answers: NDQ_003394

answers: flat slab subduction

answers: NDQ_003395

answers: flat slab subduction

answers: NDQ_003396

answers: subduction

answers: NDQ_003351

answers: flat slab subduction

answers: NDQ_003352

answers: decreased mantle viscosity,

answers: NDQ_003353

answers: decreased mantle viscosity,

answers: NDQ_003354

answers: flat slab subduction would not have been dominant or non-existent.

answers: NDQ_003355

answers: flat slab subduction

answers: NDQ_003356

answers: buoyancy

answers: NDQ_003357

answers: decreased mantle viscosity,

answers: NDQ_003358

answers: flat slab subduction

answers: NDQ_003359

answers: decreased mantle viscosity,

answers: NDQ_003360

answers: oceanic plate buoyancy

answers: NDQ_003362

answers: flat slab subduction was the dominant style.

answers: NDQ_003363

answers: flat slab subduction

answers: NDQ_003371

answers: flat slab subduction

answers: NDQ_003373

answers: flat slab subduction

answers: NDQ_003376

answers: flat slab subduction

answers: NDQ_003378

answers: flat slab subduction

answers: NDQ_003379

answers: flat slab subduction

answers: NDQ_003380

answers: increase in oceanic plate buoyancy

answers: NDQ_003381

answers: decreased mantle viscosity,

answers: NDQ_003382

answers: flat slab subduction

answers: NDQ_003383

answers: decreased mantle viscosity,

answers: NDQ_003384

answers: flat slab subduction

answers: NDQ_003385

answers: flat slab subduction

answers: NDQ_003386

answers: flat slab subduction

answers: NDQ_003387

answers: decreased mantle viscosity,

answers: NDQ_003388

answers: flat slab subduction

answers: NDQ_003389

answers: flat slab subduction

answers: NDQ_003390

answers: subduction

answers: NDQ_003391

answers: flat slab subduction

answers: NDQ_003392

answers: flat slab subduction

answers: NDQ_003393

answers: flat slab subduction

answers: NDQ_003394

answers: flat slab subduction

answers: NDQ_003395

answers: flat slab subduction

answers: NDQ_003396

answers: flat slab subduction

text: The 6.4 and 6.3 intraplate earthquakes occurred as a result of oblique strike-slip faulting in the shallow crust about 300 km east of the Eurasia-Arabian Plate boundary. The two earthquakes are separated by 10 km in an east-west direction.

text: The 6.4 and 6.3

text: intraplate earthquake

text: s occurred as a result of oblique strike-slip faulting in the shallow crust about 300 km east of the Eurasia-Arabian Plate boundary. The two earthquakes are separated by 10 km in an east-west direction.

answers: NDQ_003351

answers: strike-slip

answers: NDQ_003352

answers: is likely to crack

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: oblique fold

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: oblique strike-slip faulting is a type of

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: continental plates

answers: NDQ_003362

answers: The San Andreas fault is located in the Pacific Ocean.

answers: NDQ_003363

answers: 6.3 intraplate earthquakes

answers: NDQ_003371

answers: Which of the following is not a type of fault: strike-slip faulting or thrust faulting?

answers: NDQ_003373

answers: Which of the following is not a type of stress?

answers: NDQ_003376

answers: Which of the following is not a type of terrain: basin-and-range or strike-slip faulting?

answers: NDQ_003378

answers: what is the first type of movement mentioned?

answers: NDQ_003379

answers: no

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: Which of the following is not a result of oblique strike-slip faulting in the shallow crust?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not a type of fold?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: yes

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: strike-slip faulting or normal faults?

answers: NDQ_003388

answers: It's impossible to say

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: strike-slip faulting

answers: NDQ_003391

answers: the shallow crust

answers: NDQ_003392

answers: strike-slip faulting

answers: NDQ_003393

answers: strike-slip fault

answers: NDQ_003394

answers: oblique

answers: NDQ_003395

answers: oblique

answers: NDQ_003396

answers: oblique

answers: NDQ_003351

answers: oblique strike-slip faulting

answers: NDQ_003352

answers: oblique strike-slip faulting

answers: NDQ_003353

answers: oblique strike-slip faulting

answers: NDQ_003354

answers: The two earthquakes are separated by 10 km in an east-west direction.

answers: NDQ_003355

answers: oblique strike-slip faulting

answers: NDQ_003356

answers: oblique strike-slip faulting

answers: NDQ_003357

answers: east-west direction.

answers: NDQ_003358

answers: intraplate earthquakes

answers: NDQ_003359

answers: oblique strike-slip faulting

answers: NDQ_003360

answers: oblique strike-slip faulting

answers: NDQ_003362

answers: The two earthquakes are separated by 10 km in an east-west direction.

answers: NDQ_003363

answers: oblique strike-slip faulting

answers: NDQ_003371

answers: oblique strike-slip faulting

answers: NDQ_003373

answers: shallow crust

answers: NDQ_003376

answers: oblique strike-slip faulting

answers: NDQ_003378

answers: strike-slip

answers: NDQ_003379

answers: oblique

answers: NDQ_003380

answers: oblique strike-slip faulting

answers: NDQ_003381

answers: oblique strike-slip faulting

answers: NDQ_003382

answers: oblique strike-slip faulting

answers: NDQ_003383

answers: oblique strike-slip faulting

answers: NDQ_003384

answers: oblique strike-slip faulting

answers: NDQ_003385

answers: oblique strike-slip faulting

answers: NDQ_003386

answers: oblique strike-slip faulting

answers: NDQ_003387

answers: oblique strike-slip faulting

answers: NDQ_003388

answers: oblique strike-slip faulting

answers: NDQ_003389

answers: oblique strike-slip faulting

answers: NDQ_003390

answers: oblique strike-slip

answers: NDQ_003391

answers: shallow crust

answers: NDQ_003392

answers: oblique strike-slip faulting

answers: NDQ_003393

answers: strike-slip faulting in the shallow crust

answers: NDQ_003394

answers: oblique

answers: NDQ_003395

answers: oblique strike-slip faulting

answers: NDQ_003396

answers: oblique strike-slip faulting

text: Palaeo means past, thus paleostress (or palaeostress) means stresses that acted in the geological past (i.e. thousands to millions of years ago). In Geology paleostress analysis is concerned with deriving the directions along which the stress acted and gave rise to present structural feature in the rocks on earth.

text: Palaeo means past, thus paleostress (or palaeostress) means stresses that acted in the geological past (i.e. thousands to millions of years ago). In Geology paleostress analysis is concerned with deriving the directions along which the stress acted and gave rise to present structural feature in the rocks on earth.

answers: NDQ_003351

answers: paleostress

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: Paleostress

answers: NDQ_003356

answers: elongate

answers: NDQ_003357

answers: Paleostress analysis is concerned with deriving the directions along which the stress acted

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: Paleostress analysis is concerned with deriving the directions along which the stress acted

answers: NDQ_003363

answers: millions of years ago

answers: NDQ_003371

answers: What is a thrust fault?

answers: NDQ_003373

answers: How would you describe paleostress?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: It's impossible to say

answers: NDQ_003381

answers: What does palaeostress mean?

answers: NDQ_003382

answers: What does paleostress mean?

answers: NDQ_003383

answers: What does paleostress mean?

answers: NDQ_003384

answers: What does paleostress analysis mean?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: what does paleostress analysis mean?

answers: NDQ_003387

answers: Which of the following is not a cause of normal faults?

answers: NDQ_003388

answers: What type of stress does strike-slip faults result from?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: Paleostress

answers: NDQ_003391

answers: a dip-slip fault

answers: NDQ_003392

answers: Paleostress

answers: NDQ_003393

answers: Paleostress

answers: NDQ_003394

answers: isobath

answers: NDQ_003395

answers: is a vertical fault

answers: NDQ_003396

answers: paleostress

answers: NDQ_003351

answers: paleostress

answers: NDQ_003352

answers: structural feature

answers: NDQ_003353

answers: structural feature

answers: NDQ_003354

answers: Palaeo

answers: NDQ_003355

answers: Palaeo means past, thus paleostress

answers: NDQ_003356

answers: present structural feature

answers: NDQ_003357

answers: stresses that acted in the geological past

answers: NDQ_003358

answers: paleostress

answers: NDQ_003359

answers: stresses that acted in the geological past

answers: NDQ_003360

answers: stresses

answers: NDQ_003362

answers: thousands to millions of years ago).

answers: NDQ_003363

answers: thousands to millions of years ago).

answers: NDQ_003371

answers: paleostress

answers: NDQ_003373

answers: paleostress

answers: NDQ_003376

answers: paleostress

answers: NDQ_003378

answers: paleostress

answers: NDQ_003379

answers: Palaeo

answers: NDQ_003380

answers: paleostress

answers: NDQ_003381

answers: paleostress

answers: NDQ_003382

answers: Palaeo means past, thus paleostress

answers: NDQ_003383

answers: present structural feature

answers: NDQ_003384

answers: Palaeo

answers: NDQ_003385

answers: paleostress

answers: NDQ_003386

answers: paleostress

answers: NDQ_003387

answers: paleostress

answers: NDQ_003388

answers: paleostress

answers: NDQ_003389

answers: Palaeo means past, thus paleostress

answers: NDQ_003390

answers: paleostress

answers: NDQ_003391

answers: paleostress

answers: NDQ_003392

answers: paleostress

answers: NDQ_003393

answers: paleostress

answers: NDQ_003394

answers: Palaeo

answers: NDQ_003395

answers: Palaeo

answers: NDQ_003396

answers: Palaeo means past, thus paleostress

text: Lazarus Pits are composed of a unique unknown green chemical blend that bubbles up somewhere within the Earth's crust to the surface at key points on Earth, typically at the junction of ley lines. The substance possesses the ability to rejuvenate the sick and injured, and even resurrect the dead. The pits also decrease the age of the user depending on how long they stay submerged in the pit. If a healthy person goes into the pits, they will be killed in most instances.

text: Lazarus Pits are composed of a unique unknown green chemical blend that bubbles up somewhere within the Earth's crust to the surface at key points on Earth, typically at the junction of

text: ley line

text: s. The substance possesses the ability to rejuvenate the sick and injured, and even resurrect the dead. The pits also decrease the age of the user depending on how long they stay submerged in the pit. If a healthy person goes into the pits, they will be killed in most instances.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: resurrect

answers: NDQ_003357

answers: Lazarus Pits are composed of what?

answers: NDQ_003358

answers: pit

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: a healthy person goes into the pits, they will be killed in most instances

answers: NDQ_003363

answers: Lazarus Pits

answers: NDQ_003371

answers: Which of the following is not a type of rock: Lazarus Pits, ley lines, or young rocks?

answers: NDQ_003373

answers: Why would a healthy person go into the pits?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: How does the substance affect the age of the user?

answers: NDQ_003381

answers: What is the reason for the Lazarus Pits?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: normal faults, Lazarus Pits or normal faults?

answers: NDQ_003388

answers: unanswerable

answers: NDQ_003389

answers: not enough information

answers: NDQ_003390

answers: ley fault

answers: NDQ_003391

answers: unanswerable

answers: NDQ_003392

answers: ley fault

answers: NDQ_003393

answers: unanswerable

answers: NDQ_003394

answers: ley lines

answers: NDQ_003395

answers: unanswerable

answers: NDQ_003396

answers: NDQ_003351

answers: ley lines.

answers: NDQ_003352

answers: Lazarus Pits

answers: NDQ_003353

answers: ley lines.

answers: NDQ_003354

answers: Lazarus Pits

answers: NDQ_003355

answers: ley lines.

answers: NDQ_003356

answers: killed

answers: NDQ_003357

answers: ley lines.

answers: NDQ_003358

answers: Lazarus Pits

answers: NDQ_003359

answers: ley lines.

answers: NDQ_003360

answers: ley lines.

answers: NDQ_003362

answers: resurrect the dead.

answers: NDQ_003363

answers: ley lines.

answers: NDQ_003371

answers: ley lines.

answers: NDQ_003373

answers: Lazarus Pits

answers: NDQ_003376

answers: ley lines.

answers: NDQ_003378

answers: ley lines.

answers: NDQ_003379

answers: ley lines.

answers: NDQ_003380

answers: Earth's crust

answers: NDQ_003381

answers: ley lines.

answers: NDQ_003382

answers: ley lines.

answers: NDQ_003383

answers: ley lines.

answers: NDQ_003384

answers: ley lines.

answers: NDQ_003385

answers: ley lines.

answers: NDQ_003386

answers: ley lines.

answers: NDQ_003387

answers: ley lines.

answers: NDQ_003388

answers: ley lines.

answers: NDQ_003389

answers: ley lines.

answers: NDQ_003390

answers: ley lines.

answers: NDQ_003391

answers: ley lines.

answers: NDQ_003392

answers: ley lines.

answers: NDQ_003393

answers: ley lines.

answers: NDQ_003394

answers: ley lines.

answers: NDQ_003395

answers: ley lines.

answers: NDQ_003396

answers: ley lines.

text: The Andes are a Mesozoic–Tertiary orogenic belt of mountains along the Pacific Ring of Fire, a zone of volcanic activity that encompasses the Pacific rim of the Americas as well as the Asia-Pacific region. The Andes are the result of plate tectonics processes, caused by the subduction of oceanic crust beneath the South American plate. The main cause of the rise of the Andes is the compression of the western rim of the South American Plate due to the subduction of the Nazca Plate and the Antarctic Plate. To the east, the Andes range is bounded by several sedimentary basins, such as Orinoco, Amazon Basin, Madre de Dios and Gran Chaco, that separate the Andes from the ancient cratons in eastern South America. In the south, the Andes share a long boundary with the former Patagonia Terrane. To the west, the Andes end at the Pacific Ocean, although the Peru-Chile trench can be considered their ultimate western limit. From a geographical approach, the Andes are considered to have their western boundaries marked by the appearance of coastal lowlands and a less rugged topography. The Andes Mountains also contain large quantities of iron ore located in many mountains within the range.

text: The Andes are a

text: Mesozoic

text: Tertiary

text: orogenic

text: belt of mountains along the

text: Pacific Ring of Fire

text: , a zone of

text: volcanic activity

text: that encompasses the Pacific rim of the Americas as well as the

text: Asia-Pacific

text: region. The Andes are the result of

text: plate tectonics

text: processes, caused by the

text: subduction

text: of

text: oceanic crust

text: beneath the

text: South American plate

text: . The main cause of the rise of the Andes is the compression of the western rim of the

text: South American Plate

text: due to the subduction of the

text: Nazca Plate

text: and the

text: Antarctic Plate

text: . To the east, the Andes range is bounded by several

text: sedimentary basin

text: s, such as

text: Orinoco

text: Amazon Basin

text: Madre de Dios

text: and

text: Gran Chaco

text: , that separate the Andes from the ancient

text: craton

text: s in eastern South America. In the south, the Andes share a long boundary with the former

text: Patagonia Terrane

text: . To the west, the Andes end at the

text: Pacific Ocean

text: , although the

text: Peru-Chile trench

text: can be considered their ultimate western limit. From a geographical approach, the Andes are considered to have their western boundaries marked by the appearance of coastal lowlands and a less rugged topography. The Andes Mountains also contain large quantities of iron ore located in many mountains within the range.

answers: NDQ_003351

answers: subduction

answers: NDQ_003352

answers: compresses

answers: NDQ_003353

answers: compression

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: subduction

answers: NDQ_003356

answers: subduct

answers: NDQ_003357

answers: subduction of oceanic crust beneath the South American plate

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: subducts

answers: NDQ_003360

answers: plate tectonics

answers: NDQ_003362

answers: The Andes are the result of plate tectonics processes

answers: NDQ_003363

answers: Pacific Ring of Fire

answers: NDQ_003371

answers: What is the main cause of the rise of the Andes?

answers: NDQ_003373

answers: subduction of the Nazca Plate and the Antarctic Plate

answers: NDQ_003376

answers: What is the main cause of the rise of the Andes?

answers: NDQ_003378

answers: What is the main cause of the rise of the Andes?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What is the main cause of the rise of the Andes

answers: NDQ_003381

answers: What is the result of plate tectonics processes?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the main cause of the rise of the Andes?

answers: NDQ_003384

answers: What is the main cause of the rise of the Andes?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: plate tectonics processes

answers: NDQ_003387

answers: What is the main cause of the rise of the Andes?

answers: NDQ_003388

answers: What is the main cause of the rise of the Andes is the compression of the western rim of the South American Plate?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: subduction

answers: NDQ_003391

answers: South American plate

answers: NDQ_003392

answers: plate tectonics processes

answers: NDQ_003393

answers: the South American Plate

answers: NDQ_003394

answers: subduction

answers: NDQ_003395

answers: subduction of the Nazca Plate

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: compression of the western rim of the South American Plate

answers: NDQ_003352

answers: compression of the western rim of the South American Plate

answers: NDQ_003353

answers: subduction of oceanic crust

answers: NDQ_003354

answers: bounded by several sedimentary basins,

answers: NDQ_003355

answers: lowlands

answers: NDQ_003356

answers: rugged topography.

answers: NDQ_003357

answers: subduction of oceanic crust

answers: NDQ_003358

answers: cratons

answers: NDQ_003359

answers: subduction of oceanic crust

answers: NDQ_003360

answers: plate tectonics

answers: NDQ_003362

answers: coastal lowlands

answers: NDQ_003363

answers: subduction of oceanic crust beneath the South American plate.

answers: NDQ_003371

answers: iron ore

answers: NDQ_003373

answers: subduction of oceanic crust beneath the South American plate.

answers: NDQ_003376

answers: sedimentary basins,

answers: NDQ_003378

answers: iron ore

answers: NDQ_003379

answers: iron ore

answers: NDQ_003380

answers: compression

answers: NDQ_003381

answers: subduction of oceanic crust beneath the South American plate.

answers: NDQ_003382

answers: compression of the western rim of the South American Plate

answers: NDQ_003383

answers: the compression of the western rim of the South American Plate

answers: NDQ_003384

answers: Nazca Plate and the Antarctic Plate.

answers: NDQ_003385

answers: Pacific Ring of Fire,

answers: NDQ_003386

answers: plate tectonics

answers: NDQ_003387

answers: compression of the western rim of the South American Plate

answers: NDQ_003388

answers: subduction of oceanic crust

answers: NDQ_003389

answers: plate tectonics

answers: NDQ_003390

answers: subduction of oceanic crust beneath the South American plate.

answers: NDQ_003391

answers: South American plate.

answers: NDQ_003392

answers: compression of the western rim of the South American Plate

answers: NDQ_003393

answers: South American plate.

answers: NDQ_003394

answers: Nazca Plate and the Antarctic Plate.

answers: NDQ_003395

answers: subduction of oceanic crust beneath the South American plate.

answers: NDQ_003396

answers: subduction of oceanic crust beneath the South American plate.

text: Transform faults within continental plates include some of the best known examples of strike-slip structures, such as the San Andreas Fault, the Dead Sea Transform, the North Anatolian Fault and the Alpine Fault.

text: Transform faults within continental plates include some of the best known examples of strike-slip structures, such as the

text: San Andreas Fault

text: , the

text: Dead Sea Transform

text: , the

text: North Anatolian Fault

text: and the

text: Alpine Fault

answers: NDQ_003351

answers: strike-slip

answers: NDQ_003352

answers: is likely to crack

answers: NDQ_003353

answers: strike-slip structures

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: transform

answers: NDQ_003356

answers: change shape

answers: NDQ_003357

answers: strike-slip structures

answers: NDQ_003358

answers: Transform fault

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: continental plates

answers: NDQ_003362

answers: The Dead Sea Transform is not a transform fault.

answers: NDQ_003363

answers: Transform faults

answers: NDQ_003371

answers: Which of the following is not an example of a strike-slip structure?

answers: NDQ_003373

answers: Why would a rock be deeply buried?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: no

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What is the opposite of strike-slip structures?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is the opposite of strike-slip structures?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: no

answers: NDQ_003387

answers: no

answers: NDQ_003388

answers: It's impossible to say

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: strike-slip

answers: NDQ_003391

answers: strike-slip

answers: NDQ_003392

answers: strike-slip

answers: NDQ_003393

answers: strike-slip

answers: NDQ_003394

answers: strike-slip

answers: NDQ_003395

answers: strike-slip

answers: NDQ_003396

answers: Alpine Fault

answers: NDQ_003351

answers: strike-slip

answers: NDQ_003352

answers: strike-slip structures,

answers: NDQ_003353

answers: Transform faults

answers: NDQ_003354

answers: Transform faults within continental plates

answers: NDQ_003355

answers: strike-slip

answers: NDQ_003356

answers: strike-slip

answers: NDQ_003357

answers: strike-slip

answers: NDQ_003358

answers: strike-slip structures,

answers: NDQ_003359

answers: Transform faults within continental plates

answers: NDQ_003360

answers: Transform faults

answers: NDQ_003362

answers: San Andreas Fault, the Dead Sea Transform,

answers: NDQ_003363

answers: Transform faults

answers: NDQ_003371

answers: Transform faults

answers: NDQ_003373

answers: Transform faults

answers: NDQ_003376

answers: Transform faults within continental plates

answers: NDQ_003378

answers: strike-slip

answers: NDQ_003379

answers: strike-slip structures,

answers: NDQ_003380

answers: strike-slip structures,

answers: NDQ_003381

answers: strike-slip structures,

answers: NDQ_003382

answers: Transform faults within continental plates

answers: NDQ_003383

answers: strike-slip structures,

answers: NDQ_003384

answers: Transform faults within continental plates

answers: NDQ_003385

answers: Transform faults

answers: NDQ_003386

answers: strike-slip structures,

answers: NDQ_003387

answers: Transform faults

answers: NDQ_003388

answers: Transform faults

answers: NDQ_003389

answers: Transform faults within continental plates

answers: NDQ_003390

answers: strike-slip

answers: NDQ_003391

answers: strike-slip

answers: NDQ_003392

answers: strike-slip

answers: NDQ_003393

answers: strike-slip

answers: NDQ_003394

answers: strike-slip

answers: NDQ_003395

answers: Alpine Fault.

answers: NDQ_003396

answers: Alpine Fault.

text: On September 14, 2016 a doctor in Uruguay stated that Abu Wa'el Dhiab "was unconscious" and had slipped into a coma due to a prolonged hunger strike and that it was hard to tell if "it was reversible".He was given medical treatment, came out of the coma, then continued his hunger strike.

text: On September 14, 2016 a doctor in Uruguay stated that Abu Wa'el Dhiab "was unconscious" and had slipped into a coma due to a prolonged hunger strike and that it was hard to tell if "it was reversible".He was given medical treatment, came out of the coma, then continued his hunger strike.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: Abu Wa'el Dhiab would be in what state?

answers: NDQ_003358

answers: coma

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's surface

answers: NDQ_003362

answers: it was reversible

answers: NDQ_003363

answers: the same time

answers: NDQ_003371

answers: What may be the reason for Abu Wa'el Dhiab's coma?

answers: NDQ_003373

answers: How would you describe Abu Wa'el Dhiab?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: what is the second to last word in the passage?

answers: NDQ_003381

answers: What does Abu Wa'el Dhiab need to do before this?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: what is the second to last word in the passage?

answers: NDQ_003385

answers: what is the first word in the passage?

answers: NDQ_003386

answers: None of the above choices.

answers: NDQ_003387

answers: Which of the following is not a reason for Abu Wa'el Dhiab to continue his hunger strike?

answers: NDQ_003388

answers: What type of fault is Abu Wa'el Dhiab?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: dip-slip fault plane

answers: NDQ_003392

answers: unanswerable

answers: NDQ_003393

answers: a dip-slip fault plane

answers: NDQ_003394

answers: NDQ_003395

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: hunger strike

answers: NDQ_003352

answers: coma

answers: NDQ_003353

answers: coma

answers: NDQ_003354

answers: unconscious" and had slipped into a coma

answers: NDQ_003355

answers: coma

answers: NDQ_003356

answers: coma

answers: NDQ_003357

answers: continued his hunger strike.

answers: NDQ_003358

answers: coma

answers: NDQ_003359

answers: reversible".He

answers: NDQ_003360

answers: hunger strike

answers: NDQ_003362

answers: "it was reversible".He

answers: NDQ_003363

answers: Uruguay

answers: NDQ_003371

answers: coma due to a prolonged hunger strike

answers: NDQ_003373

answers: unconscious" and had slipped into a coma

answers: NDQ_003376

answers: On September 14, 2016

answers: NDQ_003378

answers: slipped

answers: NDQ_003379

answers: reversible".He

answers: NDQ_003380

answers: hunger strike

answers: NDQ_003381

answers: coma

answers: NDQ_003382

answers: reversible".He

answers: NDQ_003383

answers: a prolonged hunger strike

answers: NDQ_003384

answers: coma

answers: NDQ_003385

answers: coma

answers: NDQ_003386

answers: On September 14, 2016

answers: NDQ_003387

answers: a prolonged hunger strike

answers: NDQ_003388

answers: Abu Wa'el Dhiab

answers: NDQ_003389

answers: reversible".He

answers: NDQ_003390

answers: hunger strike

answers: NDQ_003391

answers: coma

answers: NDQ_003392

answers: Abu Wa'el Dhiab

answers: NDQ_003393

answers: Abu Wa'el Dhiab

answers: NDQ_003394

answers: reversible".He

answers: NDQ_003395

answers: reversible".He

answers: NDQ_003396

answers: reversible".He

text: Stress can be external and related to the environment, but may also be created by internal perceptions that cause an individual to experience anxiety or other negative emotions surrounding a situation, such as pressure, discomfort, etc., which they then deem stressful.

text: Stress can be external and related to the environment, but may also be created by internal perceptions that cause an individual to experience

text: anxiety

text: or other negative emotions surrounding a situation, such as pressure, discomfort, etc., which they then deem stressful.

answers: NDQ_003351

answers: internal perceptions

answers: NDQ_003352

answers: is likely to crack

answers: NDQ_003353

answers: negative emotions

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: stress

answers: NDQ_003356

answers: stress

answers: NDQ_003357

answers: stress can be created by internal perceptions

answers: NDQ_003358

answers: stress

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: tectonic plates

answers: NDQ_003362

answers: stress can be external and related to the environment

answers: NDQ_003363

answers: volcanoes

answers: NDQ_003371

answers: stress

answers: NDQ_003373

answers: external perceptions

answers: NDQ_003376

answers: compressive forces

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: external

answers: NDQ_003381

answers: pressure

answers: NDQ_003382

answers: external and related to the environment

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: unanswerable

answers: NDQ_003386

answers: not enough information

answers: NDQ_003387

answers: internal perceptions

answers: NDQ_003388

answers: external and related to the environment

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: stress

answers: NDQ_003391

answers: can cause stress

answers: NDQ_003392

answers: stress

answers: NDQ_003393

answers: is a block

answers: NDQ_003394

answers: can cause stress

answers: NDQ_003395

answers: is a type of

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: pressure, discomfort,

answers: NDQ_003352

answers: pressure, discomfort,

answers: NDQ_003353

answers: anxiety or other negative emotions

answers: NDQ_003354

answers: Stress can be external and related to the environment,

answers: NDQ_003355

answers: Stress

answers: NDQ_003356

answers: pressure, discomfort,

answers: NDQ_003357

answers: internal perceptions

answers: NDQ_003358

answers: Stress

answers: NDQ_003359

answers: Stress can be external and related to the environment,

answers: NDQ_003360

answers: Stress

answers: NDQ_003362

answers: Stress can be external

answers: NDQ_003363

answers: Stress can be external and related to the environment,

answers: NDQ_003371

answers: Stress

answers: NDQ_003373

answers: Stress

answers: NDQ_003376

answers: Stress

answers: NDQ_003378

answers: Stress

answers: NDQ_003379

answers: Stress can be external and related to the environment,

answers: NDQ_003380

answers: pressure,

answers: NDQ_003381

answers: Stress can be external

answers: NDQ_003382

answers: pressure,

answers: NDQ_003383

answers: Stress

answers: NDQ_003384

answers: Stress can be external and related to the environment,

answers: NDQ_003385

answers: Stress

answers: NDQ_003386

answers: Stress

answers: NDQ_003387

answers: Stress

answers: NDQ_003388

answers: Stress

answers: NDQ_003389

answers: Stress

answers: NDQ_003390

answers: Stress

answers: NDQ_003391

answers: Stress

answers: NDQ_003392

answers: Stress

answers: NDQ_003393

answers: Stress

answers: NDQ_003394

answers: Stress

answers: NDQ_003395

answers: Stress

answers: NDQ_003396

answers: Stress

text: The Seattle Fault is believed to date from about 40 million years ago (late Eocene).  This is about the time that the strike-slip movement on the north-striking Straight Creek Fault to the east ceased, due to the intrusions of plutons.  It appears that when the Straight Creek Fault became stuck the north–south compressive force that it had accommodated by strike-slip motion was transferred to the crust of the Puget Lowland, which subsequently folded and faulted, and the various blocks jammed over one another.

text: The Seattle Fault is believed to date from about 40 million years ago (late

text: Eocene

text: ).  This is about the time that the strike-slip movement on the north-striking

text: Straight Creek Fault

text: to the east ceased, due to the intrusions of

text: pluton

text: s.  It appears that when the Straight Creek Fault became stuck the north–south compressive force that it had accommodated by strike-slip motion was transferred to the crust of the Puget Lowland, which subsequently folded and faulted, and the various blocks jammed over one another.

answers: NDQ_003351

answers: compressive

answers: NDQ_003352

answers: compresses

answers: NDQ_003353

answers: compressive force

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: Straight Creek Fault

answers: NDQ_003356

answers: fold and fault

answers: NDQ_003357

answers: north–south compressive force

answers: NDQ_003358

answers: Fault

answers: NDQ_003359

answers: folded

answers: NDQ_003360

answers: faults

answers: NDQ_003362

answers: the various blocks jammed over one another.

answers: NDQ_003363

answers: Puget Lowland

answers: NDQ_003371

answers: What is the Seattle Fault?

answers: NDQ_003373

answers: yes

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: strike-slip

answers: NDQ_003379

answers: no

answers: NDQ_003380

answers: What is a stress?

answers: NDQ_003381

answers: What happens to the Puget Lowland?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: yes

answers: NDQ_003387

answers: What is the Seattle Fault?

answers: NDQ_003388

answers: What is the cause of the Seattle Fault?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: Seattle Fault

answers: NDQ_003391

answers: Puget Lowland

answers: NDQ_003392

answers: Seattle Fault

answers: NDQ_003393

answers: Puget Lowland

answers: NDQ_003394

answers: Straight Creek Fault

answers: NDQ_003395

answers: Straight Creek Fault

answers: NDQ_003396

answers: Straight Creek Fault

answers: NDQ_003351

answers: north–south compressive force

answers: NDQ_003352

answers: folded and faulted, and the various blocks jammed over one another.

answers: NDQ_003353

answers: folded and faulted,

answers: NDQ_003354

answers: Straight Creek Fault

answers: NDQ_003355

answers: faulted,

answers: NDQ_003356

answers: jammed over one another.

answers: NDQ_003357

answers: strike-slip movement

answers: NDQ_003358

answers: Seattle Fault

answers: NDQ_003359

answers: folded and faulted,

answers: NDQ_003360

answers: Seattle Fault

answers: NDQ_003362

answers: 40 million years ago

answers: NDQ_003363

answers: Seattle Fault

answers: NDQ_003371

answers: The Seattle Fault

answers: NDQ_003373

answers: north–south compressive force

answers: NDQ_003376

answers: north–south compressive force

answers: NDQ_003378

answers: strike-slip

answers: NDQ_003379

answers: north-striking Straight Creek Fault

answers: NDQ_003380

answers: compressive force

answers: NDQ_003381

answers: folded and faulted,

answers: NDQ_003382

answers: compressive force

answers: NDQ_003383

answers: the various blocks jammed over one another.

answers: NDQ_003384

answers: folded and faulted,

answers: NDQ_003385

answers: The Seattle Fault

answers: NDQ_003386

answers: folded and faulted,

answers: NDQ_003387

answers: north–south compressive force

answers: NDQ_003388

answers: north–south compressive force

answers: NDQ_003389

answers: folded and faulted,

answers: NDQ_003390

answers: Seattle Fault

answers: NDQ_003391

answers: Puget Lowland,

answers: NDQ_003392

answers: Seattle Fault

answers: NDQ_003393

answers: Puget Lowland,

answers: NDQ_003394

answers: Straight Creek Fault

answers: NDQ_003395

answers: Straight Creek Fault

answers: NDQ_003396

answers: Straight Creek Fault

text: The fault surface is usually near vertical and the footwall moves either left or right or laterally with very little vertical motion. Strike-slip faults with left-lateral motion are also known as sinistral faults. Those with right-lateral motion are also known as dextral faults. Each is defined by the direction of movement of the ground on the opposite side of the fault from an observer.

text: The fault surface is usually near vertical and the footwall moves either left or right or laterally with very little vertical motion. Strike-slip faults with left-lateral motion are also known as sinistral faults. Those with right-lateral motion are also known as dextral faults. Each is defined by the direction of movement of the ground on the opposite side of the fault from an observer.

answers: NDQ_003351

answers: strike-slip

answers: NDQ_003352

answers: causes it to move

answers: NDQ_003353

answers: movement

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: sinistral fault

answers: NDQ_003356

answers: move in the same direction

answers: NDQ_003357

answers: the footwall moves either left or right

answers: NDQ_003358

answers: dextral

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: faults

answers: NDQ_003362

answers: the footwall moves either left or right or laterally

answers: NDQ_003363

answers: strike-slip faults

answers: NDQ_003371

answers: Which of the following is not a type of strike-slip fault?

answers: NDQ_003373

answers: How would you describe a rock that is deeply buried?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: Which of the following is not a type of fault: Strike-slip faults with left-lateral motion or dextral faults?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a type of fault: Strike-slip faults with left-lateral motion or dextral faults?

answers: NDQ_003384

answers: Which of the following is not a type of fault: strike-slip faults with left-lateral motion or dextral faults?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: yes

answers: NDQ_003387

answers: Which of the following is not a type of normal fault?

answers: NDQ_003388

answers: Which of the following is not a cause of strike-slip faults?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: dextral faults

answers: NDQ_003391

answers: footwall

answers: NDQ_003392

answers: dextral faults

answers: NDQ_003393

answers: footwall

answers: NDQ_003394

answers: dextral faults

answers: NDQ_003395

answers: dextral faults

answers: NDQ_003396

answers: dextral faults

answers: NDQ_003351

answers: Strike-slip

answers: NDQ_003352

answers: vertical motion.

answers: NDQ_003353

answers: Strike-slip faults

answers: NDQ_003354

answers: The fault surface is usually near vertical

answers: NDQ_003355

answers: sinistral faults.

answers: NDQ_003356

answers: Strike-slip

answers: NDQ_003357

answers: footwall moves either left or right or laterally with very little vertical motion.

answers: NDQ_003358

answers: sinistral faults.

answers: NDQ_003359

answers: vertical motion.

answers: NDQ_003360

answers: Strike-slip faults

answers: NDQ_003362

answers: very little vertical motion.

answers: NDQ_003363

answers: Strike-slip faults

answers: NDQ_003371

answers: sinistral faults.

answers: NDQ_003373

answers: The fault surface is usually near vertical

answers: NDQ_003376

answers: sinistral faults.

answers: NDQ_003378

answers: Strike-slip

answers: NDQ_003379

answers: The fault surface is usually near vertical

answers: NDQ_003380

answers: The fault surface is usually near vertical

answers: NDQ_003381

answers: The fault surface is usually near vertical

answers: NDQ_003382

answers: vertical

answers: NDQ_003383

answers: vertical motion.

answers: NDQ_003384

answers: sinistral faults.

answers: NDQ_003385

answers: The fault surface

answers: NDQ_003386

answers: footwall moves either left or right or laterally with very little vertical motion.

answers: NDQ_003387

answers: The fault surface is usually near vertical

answers: NDQ_003388

answers: Strike-slip faults

answers: NDQ_003389

answers: Strike-slip faults

answers: NDQ_003390

answers: sinistral faults.

answers: NDQ_003391

answers: footwall

answers: NDQ_003392

answers: sinistral faults.

answers: NDQ_003393

answers: footwall

answers: NDQ_003394

answers: sinistral faults.

answers: NDQ_003395

answers: The fault surface is usually near vertical

answers: NDQ_003396

answers: sinistral faults.

text: Active rifting, such as is formed by the Iceland plume, is driven by hotspot or mantle plume activity. From deep within the Earth, hot mantle rises to force doming of the crust.This causes thinning of the crust and lithosphere, then melting and underplating occur.  Finally, there is rifting at the crest of the domed crust and volcanism occurs.  In passive rifting, driven by plate tectonics, the crust and lithosphere extend as a result of plate boundary forces such as slab pull.  Far field stresses thin the crust and lithospheric mantle, and hot asthenospheric mantle passively enters the thinned area.  The upwelling of asthenosphere is not involved in the actual rifting process. The upward flow of the asthenosphere results in decompression melting, magmatic underplating and some volcanism that may occur in the rift area.

text: Active rifting, such as is formed by the

text: Iceland plume

text: , is driven by hotspot or mantle plume activity. From deep within the Earth, hot mantle rises to force doming of the crust.This causes thinning of the crust and lithosphere, then melting and

text: underplating

text: occur.  Finally, there is rifting at the crest of the domed crust and volcanism occurs.  In passive rifting, driven by plate tectonics, the crust and lithosphere extend as a result of plate boundary forces such as

text: slab pull

text: .  Far field stresses thin the crust and lithospheric mantle, and hot asthenospheric mantle passively enters the thinned area.  The upwelling of

text: asthenosphere

text: is not involved in the actual rifting process. The upward flow of the asthenosphere results in decompression melting, magmatic underplating and some volcanism that may occur in the rift area.

answers: NDQ_003351

answers: slab pull

answers: NDQ_003352

answers: thinning

answers: NDQ_003353

answers: thinning

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: rift

answers: NDQ_003356

answers: deform

answers: NDQ_003357

answers: the crust and lithosphere extend as a result of plate boundary forces

answers: NDQ_003358

answers: passive rifting

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: plate boundary forces

answers: NDQ_003362

answers: active rifting, such as is formed by the Iceland plume

answers: NDQ_003363

answers: Active rifting

answers: NDQ_003371

answers: What may occur in the rift area?

answers: NDQ_003373

answers: What is the opposite of decompression?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What is a result of plate boundary forces such as slab pull?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not a result of plate boundary forces such as slab pull?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: plate tectonics

answers: NDQ_003387

answers: Which of the following is not a cause of normal faults?

answers: NDQ_003388

answers: Which of the following is not a type of strike-slip fault?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: active rifting

answers: NDQ_003391

answers: underplating

answers: NDQ_003392

answers: active rifting

answers: NDQ_003393

answers: lithosphere

answers: NDQ_003394

answers: active rifting

answers: NDQ_003395

answers: active rifting

answers: NDQ_003396

answers: active rifting

answers: NDQ_003351

answers: slab pull.

answers: NDQ_003352

answers: thinning

answers: NDQ_003353

answers: thin the crust and lithospheric mantle,

answers: NDQ_003354

answers: Active rifting,

answers: NDQ_003355

answers: Active rifting, such as is formed by the Iceland plume,

answers: NDQ_003356

answers: melting and underplating

answers: NDQ_003357

answers: passive rifting,

answers: NDQ_003358

answers: passive rifting,

answers: NDQ_003359

answers: Active rifting,

answers: NDQ_003360

answers: Active rifting,

answers: NDQ_003362

answers: The upwelling of asthenosphere

answers: NDQ_003363

answers: Active rifting,

answers: NDQ_003371

answers: Active rifting,

answers: NDQ_003373

answers: hot mantle rises to force doming of the crust.This

answers: NDQ_003376

answers: passive rifting, driven by plate tectonics,

answers: NDQ_003378

answers: Active rifting,

answers: NDQ_003379

answers: Active rifting, such as is formed by the Iceland plume,

answers: NDQ_003380

answers: stresses

answers: NDQ_003381

answers: Far field stresses

answers: NDQ_003382

answers: decompression

answers: NDQ_003383

answers: Far field stresses

answers: NDQ_003384

answers: Active rifting, such as is formed by the Iceland plume,

answers: NDQ_003385

answers: rift area.

answers: NDQ_003386

answers: Active rifting,

answers: NDQ_003387

answers: decompression melting,

answers: NDQ_003388

answers: Active rifting,

answers: NDQ_003389

answers: Active rifting,

answers: NDQ_003390

answers: Iceland plume,

answers: NDQ_003391

answers: lithosphere,

answers: NDQ_003392

answers: Iceland plume,

answers: NDQ_003393

answers: crest of the domed crust

answers: NDQ_003394

answers: Active rifting, such as is formed by the Iceland plume,

answers: NDQ_003395

answers: Active rifting, such as is formed by the Iceland plume,

answers: NDQ_003396

answers: Active rifting,

text: There are about  of convergent plate margins, mostly around the Pacific Ocean—the reason for the reference “Pacific-type” margin—but they are also in the eastern Indian Ocean, with relatively short convergent margin segments in the Atlantic Ocean and in the Mediterranean Sea. Globally, there are over 50 major ocean trenches covering an area of 1.9 million km2 or about 0.5% of the oceans. Trenches that are partially infilled are known as "troughs" and sometimes they are completely buried and lack bathymetric expression, but the fundamental structures that these represent mean that the great name should also be applied here. This applies to Cascadia, Makran, southern Lesser Antilles, and Calabrian trenches.  Trenches along with volcanic arcs and zones of earthquakes that dip under the volcanic arc as deeply as  are diagnostic of convergent plate boundaries and their deeper manifestations, subduction zones. Trenches are related to but distinguished from continental collision zones (like that between India and Asia to form the Himalaya), where continental crust enters the subduction zone. When buoyant continental crust enters a trench, subduction eventually stops and the convergent plate margin becomes a collision zone.  Features analogous to trenches are associated with collisions zones; these are sediment-filled foredeeps referred to as peripheral foreland basins, such as that which the Ganges River and Tigris-Euphrates rivers flow along.

text: There are about  of

text: convergent plate margins

text: , mostly around the

text: Pacific Ocean

text: —the reason for the reference “Pacific-type” margin—but they are also in the eastern

text: Indian Ocean

text: , with relatively short convergent margin segments in the

text: Atlantic Ocean

text: and in the

text: Mediterranean Sea

text: . Globally, there are over 50 major ocean trenches covering an area of 1.9 million km2 or about 0.5% of the oceans. Trenches that are partially infilled are known as "troughs" and sometimes they are completely buried and lack bathymetric expression, but the fundamental structures that these represent mean that the great name should also be applied here. This applies to

text: Cascadia

text: Makran

text: , southern

text: Lesser Antilles

text: , and

text: Calabrian trenches

text: .  Trenches along with

text: volcanic arc

text: s and zones of

text: earthquake

text: s that dip under the volcanic arc as deeply as  are diagnostic of convergent plate boundaries and their deeper manifestations,

text: subduction zones

text: . Trenches are related to but distinguished from continental collision zones (like that between India and Asia to form the

text: Himalaya

text: ), where

text: continental crust

text: enters the subduction zone. When buoyant continental crust enters a trench, subduction eventually stops and the convergent plate margin becomes a collision zone.  Features analogous to trenches are associated with collisions zones; these are sediment-filled foredeeps referred to as peripheral foreland basins, such as that which the

text: Ganges River

text: and Tigris-Euphrates rivers flow along.

answers: NDQ_003351

answers: subduction

answers: NDQ_003352

answers: subduction eventually stops

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: trench

answers: NDQ_003356

answers: subduct

answers: NDQ_003357

answers: subduction eventually stops and the convergent plate margin becomes a collision zone

answers: NDQ_003358

answers: subduction zone

answers: NDQ_003359

answers: subduction eventually stops

answers: NDQ_003360

answers: continental collision zones

answers: NDQ_003362

answers: troughs" and sometimes they are completely buried

answers: NDQ_003363

answers: Pacific Ocean

answers: NDQ_003371

answers: What is a thrust fault?

answers: NDQ_003373

answers: unanswerable

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: no

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What type of stress occurs when rock deforms?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: What is the reason for the reference “Pacific-type” margin

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: subduction zones

answers: NDQ_003386

answers: subduction zones

answers: NDQ_003387

answers: What are normal faults caused by?

answers: NDQ_003388

answers: What type of stress results from strike-slip faults?

answers: NDQ_003389

answers: continental collision zones

answers: NDQ_003390

answers: subduction zone

answers: NDQ_003391

answers: subduction zone

answers: NDQ_003392

answers: subduction zone

answers: NDQ_003393

answers: subduction zone

answers: NDQ_003394

answers: subduction zones

answers: NDQ_003395

answers: subduction zones

answers: NDQ_003396

answers: subduction zones

answers: NDQ_003351

answers: subduction zones.

answers: NDQ_003352

answers: subduction zones.

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: over 50 major ocean trenches

answers: NDQ_003355

answers: "troughs"

answers: NDQ_003356

answers: subduction eventually stops

answers: NDQ_003357

answers: subduction

answers: NDQ_003358

answers: "troughs"

answers: NDQ_003359

answers: continental crust enters the subduction zone.

answers: NDQ_003360

answers: convergent plate margins,

answers: NDQ_003362

answers: “Pacific-type” margin—but

answers: NDQ_003363

answers: between India and Asia

answers: NDQ_003371

answers: Trenches along with volcanic arcs

answers: NDQ_003373

answers: completely buried and lack bathymetric expression,

answers: NDQ_003376

answers: peripheral foreland basins,

answers: NDQ_003378

answers: earthquakes that dip under the volcanic arc

answers: NDQ_003379

answers: volcanic arc

answers: NDQ_003380

answers: earthquakes

answers: NDQ_003381

answers: Trenches are related to but distinguished from continental collision zones

answers: NDQ_003382

answers: volcanic arcs and zones of earthquakes

answers: NDQ_003383

answers: earthquakes

answers: NDQ_003384

answers: volcanic arcs

answers: NDQ_003385

answers: Trenches are related to but distinguished from continental collision zones

answers: NDQ_003386

answers: subduction zones.

answers: NDQ_003387

answers: subduction zones.

answers: NDQ_003388

answers: subduction zones.

answers: NDQ_003389

answers: continental collision zones

answers: NDQ_003390

answers: subduction zones.

answers: NDQ_003391

answers: subduction zones.

answers: NDQ_003392

answers: subduction zones. Trenches

answers: NDQ_003393

answers: volcanic arc

answers: NDQ_003394

answers: convergent plate boundaries and their deeper manifestations, subduction zones.

answers: NDQ_003395

answers: convergent plate boundaries and their deeper manifestations, subduction zones.

answers: NDQ_003396

answers: subduction zones.

text: Boyko G. E., 1968. The Transformation of Abyssal Petroleum under the Conditions of the Earth's Crust. – Kiev, Naukova Dumka Publ.

text: Boyko G. E., 1968. The Transformation of Abyssal Petroleum under the Conditions of the Earth's Crust. – Kiev, Naukova Dumka Publ.

answers: NDQ_003351

answers: divergent plate boundary

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: igneous rocks to form

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: fold that bends downward

answers: NDQ_003356

answers: swell

answers: NDQ_003357

answers: Abyssal Petroleum under the Conditions of the Earth's Crust

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: Abyssal petroleum under the conditions of the Earth's crust

answers: NDQ_003363

answers: Abyssal Petroleum

answers: NDQ_003371

answers: Boyko G. E.

answers: NDQ_003373

answers: Boyko G. E.

answers: NDQ_003376

answers: compressive forces

answers: NDQ_003378

answers: the amount the ground moves

answers: NDQ_003379

answers: The dip of the fault plane is vertical

answers: NDQ_003380

answers: Any force applied to rock is a stress.

answers: NDQ_003381

answers: Boyko G. E.

answers: NDQ_003382

answers: Compression is the most common stress at convergent plates

answers: NDQ_003383

answers: Boyko G. E.

answers: NDQ_003384

answers: Syncline

answers: NDQ_003385

answers: Fault zone

answers: NDQ_003386

answers: Boyko G. E.

answers: NDQ_003387

answers: Boyko G. E.

answers: NDQ_003388

answers: Boyko G. E.

answers: NDQ_003389

answers: Boyko G. E

answers: NDQ_003390

answers: the hanging wall drops down relative to the footwall

answers: NDQ_003391

answers: Abyssal Petroleum

answers: NDQ_003392

answers: the hanging wall pushes up relative to the footwall

answers: NDQ_003393

answers: Abyssal Petroleum

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: a fault with a vertical fault plane

answers: NDQ_003396

answers: reverse fault in which the fault plane is nearly horizontal

answers: NDQ_003351

answers: The Transformation of Abyssal Petroleum

answers: NDQ_003352

answers: Naukova Dumka Publ.

answers: NDQ_003353

answers: The Transformation of Abyssal Petroleum

answers: NDQ_003354

answers: Naukova Dumka Publ.

answers: NDQ_003355

answers: Earth's Crust.

answers: NDQ_003356

answers: The Transformation of Abyssal Petroleum

answers: NDQ_003357

answers: Earth's Crust.

answers: NDQ_003358

answers: Abyssal

answers: NDQ_003359

answers: Conditions of the Earth's Crust.

answers: NDQ_003360

answers: Earth's Crust.

answers: NDQ_003362

answers: The Transformation of Abyssal Petroleum

answers: NDQ_003363

answers: Earth's Crust.

answers: NDQ_003371

answers: Boyko G. E.,

answers: NDQ_003373

answers: The Transformation of Abyssal Petroleum

answers: NDQ_003376

answers: Conditions of the Earth's Crust.

answers: NDQ_003378

answers: Naukova Dumka Publ.

answers: NDQ_003379

answers: Naukova Dumka Publ.

answers: NDQ_003380

answers: Naukova Dumka Publ.

answers: NDQ_003381

answers: Naukova Dumka Publ.

answers: NDQ_003382

answers: Naukova Dumka Publ.

answers: NDQ_003383

answers: Naukova Dumka Publ.

answers: NDQ_003384

answers: Naukova Dumka Publ.

answers: NDQ_003385

answers: Naukova Dumka Publ.

answers: NDQ_003386

answers: Boyko G. E.,

answers: NDQ_003387

answers: Boyko G. E.,

answers: NDQ_003388

answers: Boyko G. E.,

answers: NDQ_003389

answers: Earth's Crust.

answers: NDQ_003390

answers: Boyko G. E.,

answers: NDQ_003391

answers: Abyssal Petroleum

answers: NDQ_003392

answers: Boyko G. E.,

answers: NDQ_003393

answers: Petroleum

answers: NDQ_003394

answers: Boyko G. E.,

answers: NDQ_003395

answers: Boyko G. E.,

answers: NDQ_003396

answers: Boyko G. E.,

text: The difference between singular and plural in these languages is easily explained: the PIE root is *hes-. In the singular, the stem is stressed, so it remains in the e-grade, and it takes the inflection -ti. In the plural, however, the inflection -énti was stressed, causing the stem to reduce to the zero grade: *hes-énti → *hs-énti. See main article: Indo-European copula.

text: The difference between singular and plural in these languages is easily explained: the PIE root is *hes-. In the singular, the stem is stressed, so it remains in the e-grade, and it takes the inflection -ti. In the plural, however, the inflection -énti was stressed, causing the stem to reduce to the zero grade: *hes-énti → *hs-énti. See main article:

text: Indo-European copula

answers: NDQ_003351

answers: -ti

answers: NDQ_003352

answers: is likely to crack

answers: NDQ_003353

answers: earthquakes.

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone.

answers: NDQ_003355

answers: fold.

answers: NDQ_003356

answers: deform

answers: NDQ_003357

answers: normal faults do not have a zero grade.

answers: NDQ_003358

answers: place

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: glaciers.

answers: NDQ_003362

answers: The difference between singular and plural in these languages is easily explained

answers: NDQ_003363

answers: the end of the Cretaceous

answers: NDQ_003371

answers: If very old rocks are above much younger rocks there may be a thrust fault in between.

answers: NDQ_003373

answers: A deeply buried rock is under compressive stresses.

answers: NDQ_003376

answers: basin-and-range

answers: NDQ_003378

answers: the ground moves in an earthquake

answers: NDQ_003379

answers: strike-slip fault

answers: NDQ_003380

answers: Any force applied to rock is a stress.

answers: NDQ_003381

answers: When confining stress occurs, rock deforms.

answers: NDQ_003382

answers: is the most common stress at convergent plates

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: Fault zone

answers: NDQ_003386

answers: movement of rock at faults

answers: NDQ_003387

answers: Normal faults are caused by what?

answers: NDQ_003388

answers: Strike-slip faults result from what?

answers: NDQ_003389

answers: only the process of folding creates mountain ranges

answers: NDQ_003390

answers: -ti

answers: NDQ_003391

answers: dip-slip fault

answers: NDQ_003392

answers: ti

answers: NDQ_003393

answers: block of rock that is above

answers: NDQ_003394

answers: fault with a fault plane that is vertical

answers: NDQ_003395

answers: vertical fault plane

answers: NDQ_003396

answers: horizontal fault

answers: NDQ_003351

answers: e-grade,

answers: NDQ_003352

answers: e-grade,

answers: NDQ_003353

answers: causing the stem to reduce to the zero grade:

answers: NDQ_003354

answers: The difference between singular and plural in these languages is easily explained:

answers: NDQ_003355

answers: Indo-European copula.

answers: NDQ_003356

answers: zero grade:

answers: NDQ_003357

answers: e-grade,

answers: NDQ_003358

answers: Indo-European copula.

answers: NDQ_003359

answers: stressed,

answers: NDQ_003360

answers: Indo-European copula.

answers: NDQ_003362

answers: The difference between singular and plural in these languages is easily explained:

answers: NDQ_003363

answers: Indo-European

answers: NDQ_003371

answers: The difference between singular and plural in these languages is easily explained:

answers: NDQ_003373

answers: The difference between singular and plural in these languages is easily explained:

answers: NDQ_003376

answers: Indo-European copula.

answers: NDQ_003378

answers: Indo-European copula.

answers: NDQ_003379

answers: e-grade,

answers: NDQ_003380

answers: stressed,

answers: NDQ_003381

answers: causing the stem to reduce to the zero grade:

answers: NDQ_003382

answers: e-grade,

answers: NDQ_003383

answers: stressed,

answers: NDQ_003384

answers: Indo-European copula.

answers: NDQ_003385

answers: e-grade,

answers: NDQ_003386

answers: The difference between singular and plural in these languages is easily explained:

answers: NDQ_003387

answers: e-grade,

answers: NDQ_003388

answers: *hes-énti

answers: NDQ_003389

answers: Indo-European copula.

answers: NDQ_003390

answers: Indo-European copula.

answers: NDQ_003391

answers: Indo-European copula.

answers: NDQ_003392

answers: Indo-European copula.

answers: NDQ_003393

answers: Indo-European copula.

answers: NDQ_003394

answers: e-grade,

answers: NDQ_003395

answers: Indo-European copula.

answers: NDQ_003396

answers: e-grade,

text: Subduction usually occurs at convergent fault lines. The underlying tectonic plate descends, or subducts, into the Earth's mantle. Earthquakes occurring at these faults are very large in magnitude and scale. In this case the disappearing Arabian plate is part of the oceanic crust while the Eurasia plate is part of the continental crust.

text: Subduction usually occurs at convergent fault lines. The underlying tectonic plate descends, or subducts, into the

text: Earth's mantle

text: . Earthquakes occurring at these faults are very large in magnitude and scale. In this case the disappearing Arabian plate is part of the oceanic crust while the Eurasia plate is part of the continental crust.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: subducts

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation is part of the continental crust

answers: NDQ_003355

answers: fault

answers: NDQ_003356

answers: subduct

answers: NDQ_003357

answers: tectonic plate descends

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: falls on top of it

answers: NDQ_003360

answers: fault lines

answers: NDQ_003362

answers: Arabian plate is part of the oceanic crust while the Eurasia plate is part of the continental crust.

answers: NDQ_003363

answers: Subduction

answers: NDQ_003371

answers: Which of the following is not a type of fault: convergent fault lines or thrust faults?

answers: NDQ_003373

answers: What is the underlying tectonic plate?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: What is the underlying tectonic plate?

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: Which of the following is not part of the continental crust: Arabian plate, continental crust, or tectonic plate?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not a type of fold: syncline, fold, or fold?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: What is the cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not a type of normal fault?

answers: NDQ_003388

answers: Which of the following is not a type of fault: convergent fault lines, strike-slip faults or strike-slip faults?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: Subduction

answers: NDQ_003391

answers: tectonic plate

answers: NDQ_003392

answers: convergent

answers: NDQ_003393

answers: tectonic plate

answers: NDQ_003394

answers: convergent

answers: NDQ_003395

answers: convergent

answers: NDQ_003396

answers: convergent

answers: NDQ_003351

answers: Subduction usually occurs at convergent fault lines.

answers: NDQ_003352

answers: Subduction

answers: NDQ_003353

answers: Earthquakes

answers: NDQ_003354

answers: Subduction usually occurs at convergent fault lines.

answers: NDQ_003355

answers: Subduction

answers: NDQ_003356

answers: Earthquakes

answers: NDQ_003357

answers: underlying tectonic plate descends, or subducts,

answers: NDQ_003358

answers: convergent fault lines.

answers: NDQ_003359

answers: convergent fault lines.

answers: NDQ_003360

answers: Subduction usually occurs at convergent fault lines.

answers: NDQ_003362

answers: disappearing Arabian plate is part of the oceanic crust

answers: NDQ_003363

answers: Subduction usually occurs at convergent fault lines.

answers: NDQ_003371

answers: Subduction usually occurs at convergent fault lines.

answers: NDQ_003373

answers: Subduction

answers: NDQ_003376

answers: Subduction usually occurs at convergent fault lines.

answers: NDQ_003378

answers: Subduction

answers: NDQ_003379

answers: Subduction usually occurs at convergent fault lines.

answers: NDQ_003380

answers: Earthquakes

answers: NDQ_003381

answers: Subduction usually occurs at convergent fault lines.

answers: NDQ_003382

answers: Subduction

answers: NDQ_003383

answers: Subduction usually occurs at convergent fault lines.

answers: NDQ_003384

answers: Subduction usually occurs at convergent fault lines.

answers: NDQ_003385

answers: convergent fault lines.

answers: NDQ_003386

answers: Subduction

answers: NDQ_003387

answers: Subduction usually occurs at convergent fault lines.

answers: NDQ_003388

answers: Subduction usually occurs at convergent fault lines.

answers: NDQ_003389

answers: Subduction

answers: NDQ_003390

answers: Subduction usually occurs at convergent fault lines.

answers: NDQ_003391

answers: tectonic plate

answers: NDQ_003392

answers: convergent fault lines.

answers: NDQ_003393

answers: tectonic plate

answers: NDQ_003394

answers: convergent fault lines.

answers: NDQ_003395

answers: convergent fault lines.

answers: NDQ_003396

answers: convergent fault lines.

text: In addition, there exists a hierarchy of stress level in the three fault types. Thrust faults are generated by the highest, strike slip by intermediate, and normal faults by the lowest stress levels. This can easily be understood by considering the direction of the greatest principal stress, the direction of the force that 'pushes' the rock mass during the faulting. In the case of normal faults, the rock mass is pushed down in a vertical direction, thus the pushing force (greatest principal stress) equals the weight of the rock mass itself. In the case of thrusting, the rock mass 'escapes' in the direction of the least principal stress, namely upward, lifting the rock mass up, thus the overburden equals the least principal stress. Strike-slip faulting is intermediate between the other two types described above. This difference in stress regime in the three faulting environments can contribute to differences in stress drop during faulting, which contributes to differences in the radiated energy, regardless of fault dimensions.

text: In addition, there exists a hierarchy of stress level in the three fault types. Thrust faults are generated by the highest, strike slip by intermediate, and normal faults by the lowest stress levels. This can easily be understood by considering the direction of the greatest principal stress, the direction of the force that 'pushes' the rock mass during the faulting. In the case of normal faults, the rock mass is pushed down in a vertical direction, thus the pushing force (greatest principal stress) equals the weight of the rock mass itself. In the case of thrusting, the rock mass 'escapes' in the direction of the least principal stress, namely upward, lifting the rock mass up, thus the overburden equals the least principal stress. Strike-slip faulting is intermediate between the other two types described above. This difference in stress regime in the three faulting environments can contribute to differences in stress drop during faulting, which contributes to differences in the radiated energy, regardless of fault dimensions.

answers: NDQ_003351

answers: normal faults

answers: NDQ_003352

answers: 'escapes'

answers: NDQ_003353

answers: radiated energy

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: normal fault

answers: NDQ_003356

answers: 'escape'

answers: NDQ_003357

answers: rock mass is pushed down in a vertical direction

answers: NDQ_003358

answers: normal faults

answers: NDQ_003359

answers: Strike-slip faulting

answers: NDQ_003360

answers: Thrust faults

answers: NDQ_003362

answers: normal faults are generated by the lowest stress levels

answers: NDQ_003363

answers: Thrust faults

answers: NDQ_003371

answers: What type of fault is generated by the highest stress levels?

answers: NDQ_003373

answers: The rock mass is pushed down in a vertical direction

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: Strike-slip

answers: NDQ_003379

answers: no

answers: NDQ_003380

answers: What is the direction of the greatest principal stress

answers: NDQ_003381

answers: What happens to the rock mass when a fault occurs?

answers: NDQ_003382

answers: Thrust faults

answers: NDQ_003383

answers: Thrust faults are generated by the highest

answers: NDQ_003384

answers: What type of fold is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: Thrust faults

answers: NDQ_003387

answers: Which type of faults are caused by compression stress?

answers: NDQ_003388

answers: unanswerable

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: normal faults

answers: NDQ_003391

answers: strike slip faulting

answers: NDQ_003392

answers: thrusting

answers: NDQ_003393

answers: overburden

answers: NDQ_003394

answers: thrusting

answers: NDQ_003395

answers: normal faults

answers: NDQ_003396

answers: normal faults

answers: NDQ_003351

answers: Thrust faults

answers: NDQ_003352

answers: weight of the rock mass itself.

answers: NDQ_003353

answers: overburden

answers: NDQ_003354

answers: there exists a hierarchy of stress level in the three fault types.

answers: NDQ_003355

answers: normal faults,

answers: NDQ_003356

answers: pushed down in a vertical direction,

answers: NDQ_003357

answers: the rock mass is pushed down in a vertical direction,

answers: NDQ_003358

answers: normal faults

answers: NDQ_003359

answers: faulting.

answers: NDQ_003360

answers: faulting.

answers: NDQ_003362

answers: (greatest principal stress) equals the weight of the rock mass itself.

answers: NDQ_003363

answers: Thrust faults

answers: NDQ_003371

answers: Thrust faults

answers: NDQ_003373

answers: pushed down

answers: NDQ_003376

answers: Thrust faults

answers: NDQ_003378

answers: Strike-slip

answers: NDQ_003379

answers: Strike-slip faulting is intermediate

answers: NDQ_003380

answers: 'pushes' the rock mass during the faulting.

answers: NDQ_003381

answers: differences in the radiated energy,

answers: NDQ_003382

answers: Thrust faults

answers: NDQ_003383

answers: faulting.

answers: NDQ_003384

answers: thrusting,

answers: NDQ_003385

answers: fault types.

answers: NDQ_003386

answers: faulting.

answers: NDQ_003387

answers: lowest stress levels.

answers: NDQ_003388

answers: Strike-slip faulting

answers: NDQ_003389

answers: Thrust faults

answers: NDQ_003390

answers: Strike-slip

answers: NDQ_003391

answers: overburden

answers: NDQ_003392

answers: thrusting,

answers: NDQ_003393

answers: overburden

answers: NDQ_003394

answers: Strike-slip faulting

answers: NDQ_003395

answers: normal faults,

answers: NDQ_003396

answers: Thrust faults

text: It is well known that perceptions of social support availability predict better adjustment to stressful life events. It has been found that the perception of support availability is inherently comforting, and can serve as a psychological safety-net that motivates self-reliant coping efforts in the face of stress. Although the perception of support availability is associated with better adjustment, the knowledge that one has been the recipient of specific supportive acts has often been unhelpful to effectively reduce stress. The knowledge of receiving help may come at a cost with decreased feelings of self-esteem and self-efficacy, because it increases recipients' awareness towards their personal difficulties to manage stressors. People's well-intentioned support attempts may also be miscarried, and their efforts could either fail or even worsen the situation for a person under stress.  Since supportive acts benefit recipients but their actual knowledge of receiving support is sometimes harmful, it has been theorized that the most effective support exchange would involve one in which the provider reports giving support but the recipient does not notice that support has occurred. From a cost-benefit point of view, invisible support would be optimal for the recipient because the benefits of provision are accrued while the costs of receipt are avoided. Using the same idea, it also implies that the least effective type of support would be one in which the provider does not report providing support but the recipient reports receiving it. The first investigation of invisible support involved a couples study in which one member was preparing for the New York State Bar Exam. Support receipt and provision were measured by having both couple members complete daily diary entries. Over the course of one month, stressed individuals who reported low frequency of received support (but whose partner ranked his or her own actions as highly supportive) rated themselves low on anxiety and depression compared to other individuals who reported high frequency of received support.

text: It is well known that perceptions of social support availability predict better adjustment to stressful life events. It has been found that the perception of support availability is inherently comforting, and can serve as a psychological safety-net that motivates self-reliant

text: coping

text: efforts in the face of

text: stress

text: . Although the perception of support availability is associated with better adjustment, the knowledge that one has been the recipient of specific supportive acts has often been unhelpful to effectively reduce stress. The knowledge of receiving help may come at a cost with decreased feelings of

text: self-esteem

text: and

text: self-efficacy

answers: NDQ_003351

answers: invisible support

answers: NDQ_003352

answers: does not know that it is receiving support

answers: NDQ_003353

answers: perceptions of social support availability

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: unanswerable

answers: NDQ_003356

answers: splinter

answers: NDQ_003357

answers: the recipient does not notice that support has occurred

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's surface

answers: NDQ_003362

answers: the perception of support availability is inherently comforting

answers: NDQ_003363

answers: unanswerable

answers: NDQ_003371

answers: What would be the least effective type of support?

answers: NDQ_003373

answers: It has been found that the perception of support availability is inherently comforting

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What is the least effective type of support?

answers: NDQ_003381

answers: What is the least effective type of support?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What would be optimal for the recipient?

answers: NDQ_003386

answers: Which of the following is not a cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not a type of support?

answers: NDQ_003388

answers: Which of the following is not a type of support?

answers: NDQ_003389

answers: not enough information

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: unanswerable

answers: NDQ_003392

answers: unanswerable

answers: NDQ_003393

answers: unanswerable

answers: NDQ_003394

answers: invisible support

answers: NDQ_003395

answers: It has been found that the perception of support availability is inherently comforting

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: anxiety and depression

answers: NDQ_003352

answers: low frequency of received support

answers: NDQ_003353

answers: anxiety and depression

answers: NDQ_003354

answers: invisible support

answers: NDQ_003355

answers: invisible support

answers: NDQ_003356

answers: invisible support

answers: NDQ_003357

answers: decreased feelings of self-esteem and self-efficacy,

answers: NDQ_003358

answers: invisible support

answers: NDQ_003359

answers: the benefits of provision are accrued while the costs of receipt are avoided.

answers: NDQ_003360

answers: invisible support

answers: NDQ_003362

answers: the benefits of provision are accrued while the costs of receipt are avoided.

answers: NDQ_003363

answers: recipient

answers: NDQ_003371

answers: invisible support

answers: NDQ_003373

answers: invisible support

answers: NDQ_003376

answers: low frequency of received support

answers: NDQ_003378

answers: low frequency of received support

answers: NDQ_003379

answers: invisible support

answers: NDQ_003380

answers: invisible support

answers: NDQ_003381

answers: low frequency of received support

answers: NDQ_003382

answers: invisible support

answers: NDQ_003383

answers: the provider does not report providing support

answers: NDQ_003384

answers: invisible support

answers: NDQ_003385

answers: low frequency of received support

answers: NDQ_003386

answers: invisible support

answers: NDQ_003387

answers: the provider does not report providing support

answers: NDQ_003388

answers: invisible support

answers: NDQ_003389

answers: invisible support

answers: NDQ_003390

answers: the least effective type of support

answers: NDQ_003391

answers: support

answers: NDQ_003392

answers: low frequency of received support

answers: NDQ_003393

answers: support

answers: NDQ_003394

answers: the least effective type of support

answers: NDQ_003395

answers: invisible support

answers: NDQ_003396

answers: the least effective type of support

text: Based on calculations of Earth's cooling rate, which assumed constant conductivity in the Earth's interior, in 1862 Lord Kelvin (William Thomson) estimated the age of the Earth at 98 million years, in contrast to the age of 4.5 billion years obtained by radiometric dating. As pointed out by John Perry in 1895 a variable conductivity in the Earth's interior could expand the computed age of the Earth to billions of years, as later confirmed by radiometric dating. Contrary to the usual representation of Kelvin's argument, the observed thermal gradient of the Earth's crust would not be explained by the addition of radioactivity as a heat source. More significantly, mantle convection alters how heat is transported within the Earth, invalidating Kelvin's assumption of purely conductive cooling.

text: Based on calculations of Earth's cooling rate, which assumed constant conductivity in the Earth's interior, in 1862

text: Lord Kelvin

text: (William Thomson) estimated the age of the Earth at 98 million years, in contrast to the age of 4.5 billion years obtained by

text: radiometric dating

text: . As pointed out by John Perry in 1895 a variable conductivity in the Earth's interior could expand the computed age of the Earth to billions of years, as later confirmed by radiometric dating. Contrary to the usual representation of Kelvin's argument, the observed thermal gradient of the Earth's crust would not be explained by the addition of radioactivity as a heat source. More significantly,

text: mantle convection

text: alters how heat is transported within the Earth, invalidating Kelvin's assumption of purely conductive cooling.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: heats up

answers: NDQ_003353

answers: thermal gradient

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: thermal gradient

answers: NDQ_003356

answers: heat up

answers: NDQ_003357

answers: mantle convection alters how heat is transported within the Earth

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: mantle

answers: NDQ_003362

answers: radioactivity as a heat source

answers: NDQ_003363

answers: 4.5 billion years

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: unanswerable

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What is a stress?

answers: NDQ_003381

answers: How does rock deform?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: Fault zone

answers: NDQ_003386

answers: movement of rock at faults

answers: NDQ_003387

answers: Which of the following is not a cause of normal faults?

answers: NDQ_003388

answers: how heat is transported within the Earth

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: thermal gradient

answers: NDQ_003391

answers: mantle

answers: NDQ_003392

answers: thermal gradient

answers: NDQ_003393

answers: mantle

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: mantle convection

answers: NDQ_003396

answers: thermal gradient

answers: NDQ_003351

answers: mantle convection

answers: NDQ_003352

answers: mantle convection

answers: NDQ_003353

answers: mantle convection

answers: NDQ_003354

answers: 98 million years,

answers: NDQ_003355

answers: thermal gradient

answers: NDQ_003356

answers: mantle convection

answers: NDQ_003357

answers: mantle convection

answers: NDQ_003358

answers: mantle convection

answers: NDQ_003359

answers: mantle convection

answers: NDQ_003360

answers: mantle convection

answers: NDQ_003362

answers: purely conductive cooling.

answers: NDQ_003363

answers: mantle convection

answers: NDQ_003371

answers: 98 million years,

answers: NDQ_003373

answers: mantle convection

answers: NDQ_003376

answers: mantle convection

answers: NDQ_003378

answers: 1895

answers: NDQ_003379

answers: a variable conductivity

answers: NDQ_003380

answers: 4.5 billion years obtained by radiometric dating.

answers: NDQ_003381

answers: mantle convection

answers: NDQ_003382

answers: mantle convection

answers: NDQ_003383

answers: mantle convection

answers: NDQ_003384

answers: mantle convection

answers: NDQ_003385

answers: 4.5 billion years obtained by radiometric dating.

answers: NDQ_003386

answers: mantle convection

answers: NDQ_003387

answers: mantle convection

answers: NDQ_003388

answers: mantle convection

answers: NDQ_003389

answers: mantle convection

answers: NDQ_003390

answers: 98 million years,

answers: NDQ_003391

answers: mantle convection

answers: NDQ_003392

answers: 98 million years,

answers: NDQ_003393

answers: mantle convection

answers: NDQ_003394

answers: a variable conductivity

answers: NDQ_003395

answers: Earth's cooling rate,

answers: NDQ_003396

answers: mantle convection

text: Following total subduction of an oceanic tract, continuing convergence may lead to a further sequence of intra-continental mechanisms of crustal shortening. This mechanism is thought to be responsible for the various ocean basins of the Mediterranean region. The Alpine belt is believed to register a complex history of plate interactions during the general convergence of the Eurasian plate and African plates.

text: Following total subduction of an oceanic tract, continuing convergence may lead to a further sequence of intra-continental mechanisms of crustal shortening. This mechanism is thought to be responsible for the various ocean basins of the Mediterranean region. The Alpine belt is believed to register a complex history of plate interactions during the general convergence of the Eurasian plate and African plates.

answers: NDQ_003351

answers: crustal shortening

answers: NDQ_003352

answers: shortens

answers: NDQ_003353

answers: crustal shortening

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: Alpine belt

answers: NDQ_003356

answers: shorten

answers: NDQ_003357

answers: crustal shortening

answers: NDQ_003358

answers: Alpine belt

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: plate interactions

answers: NDQ_003362

answers: The Alpine belt is believed to register a complex history of plate interactions

answers: NDQ_003363

answers: subduction of an oceanic tract

answers: NDQ_003371

answers: What is the Alpine belt believed to register?

answers: NDQ_003373

answers: What is the Alpine belt believed to register?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What is the Alpine belt believed to register?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is the Alpine belt?

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: What is the Alpine belt believed to register?

answers: NDQ_003388

answers: What type of stress is shear stress?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: subduction

answers: NDQ_003391

answers: subduction

answers: NDQ_003392

answers: subduction

answers: NDQ_003393

answers: subduction

answers: NDQ_003394

answers: Alpine belt

answers: NDQ_003395

answers: a fault with a vertical fault plane

answers: NDQ_003396

answers: Alpine belt

answers: NDQ_003351

answers: crustal shortening.

answers: NDQ_003352

answers: shortening.

answers: NDQ_003353

answers: crustal shortening.

answers: NDQ_003354

answers: Following total subduction

answers: NDQ_003355

answers: subduction

answers: NDQ_003356

answers: shortening.

answers: NDQ_003357

answers: crustal shortening.

answers: NDQ_003358

answers: ocean basins of the Mediterranean region. The Alpine belt

answers: NDQ_003359

answers: crustal shortening.

answers: NDQ_003360

answers: subduction of an oceanic tract,

answers: NDQ_003362

answers: total subduction

answers: NDQ_003363

answers: subduction of an oceanic tract,

answers: NDQ_003371

answers: crustal shortening.

answers: NDQ_003373

answers: crustal shortening.

answers: NDQ_003376

answers: crustal shortening.

answers: NDQ_003378

answers: crustal shortening.

answers: NDQ_003379

answers: Following total subduction of an oceanic tract,

answers: NDQ_003380

answers: crustal shortening.

answers: NDQ_003381

answers: crustal shortening.

answers: NDQ_003382

answers: crustal shortening.

answers: NDQ_003383

answers: crustal shortening.

answers: NDQ_003384

answers: Following total subduction of an oceanic tract,

answers: NDQ_003385

answers: Following total subduction of an oceanic tract,

answers: NDQ_003386

answers: crustal shortening.

answers: NDQ_003387

answers: crustal shortening.

answers: NDQ_003388

answers: crustal shortening.

answers: NDQ_003389

answers: crustal shortening.

answers: NDQ_003390

answers: subduction

answers: NDQ_003391

answers: subduction

answers: NDQ_003392

answers: subduction

answers: NDQ_003393

answers: crustal shortening.

answers: NDQ_003394

answers: intra-continental mechanisms of crustal shortening.

answers: NDQ_003395

answers: Following total subduction of an oceanic tract,

answers: NDQ_003396

answers: total subduction

text: The analysis of structures is often accomplished by plotting the orientations of various features onto stereonets. A stereonet is a stereographic projection of a sphere onto a plane, in which planes are projected as lines and lines are projected as points. These can be used to find the locations of fold axes, relationships between faults, and relationships between other geologic structures.

text: The analysis of structures is often accomplished by plotting the orientations of various features onto

text: stereonets

text: . A stereonet is a stereographic projection of a sphere onto a plane, in which planes are projected as lines and lines are projected as points. These can be used to find the locations of fold axes, relationships between faults, and relationships between other geologic structures.

answers: NDQ_003351

answers: lateral

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: fold axis

answers: NDQ_003356

answers: fold

answers: NDQ_003357

answers: fold axes are projected as lines

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: faults

answers: NDQ_003362

answers: a stereonet is a stereographic projection

answers: NDQ_003363

answers: faults

answers: NDQ_003371

answers: The thrust fault may be in between

answers: NDQ_003373

answers: how would you describe compressive stresses?

answers: NDQ_003376

answers: basin-and-range

answers: NDQ_003378

answers: the amount the ground moves in an earthquake

answers: NDQ_003379

answers: vertical

answers: NDQ_003380

answers: What is a stress?

answers: NDQ_003381

answers: What can be used to find the locations of fold axes?

answers: NDQ_003382

answers: compression is the most common stress

answers: NDQ_003383

answers: What is the main reason for joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: movement of rock at faults

answers: NDQ_003387

answers: What type of stress causes normal faults?

answers: NDQ_003388

answers: How do strike-slip faults result from shear stress?

answers: NDQ_003389

answers: stereonets

answers: NDQ_003390

answers: the hanging wall drops down relative to the footwall

answers: NDQ_003391

answers: dip-slip fault

answers: NDQ_003392

answers: is a fault

answers: NDQ_003393

answers: is a block of rock

answers: NDQ_003394

answers: isobath

answers: NDQ_003395

answers: can be found

answers: NDQ_003396

answers: stereonet

answers: NDQ_003351

answers: faults,

answers: NDQ_003352

answers: faults,

answers: NDQ_003353

answers: fold axes, relationships between faults,

answers: NDQ_003354

answers: stereonets.

answers: NDQ_003355

answers: fold axes,

answers: NDQ_003356

answers: fold axes,

answers: NDQ_003357

answers: fold axes,

answers: NDQ_003358

answers: faults,

answers: NDQ_003359

answers: faults,

answers: NDQ_003360

answers: stereonets.

answers: NDQ_003362

answers: planes are projected as lines and lines are projected as points.

answers: NDQ_003363

answers: faults,

answers: NDQ_003371

answers: stereonets.

answers: NDQ_003373

answers: stereonets.

answers: NDQ_003376

answers: stereonets.

answers: NDQ_003378

answers: stereonets.

answers: NDQ_003379

answers: stereonets.

answers: NDQ_003380

answers: stereonets.

answers: NDQ_003381

answers: stereonets.

answers: NDQ_003382

answers: stereonets.

answers: NDQ_003383

answers: stereonets.

answers: NDQ_003384

answers: fold axes,

answers: NDQ_003385

answers: stereonet

answers: NDQ_003386

answers: stereonets.

answers: NDQ_003387

answers: stereonet

answers: NDQ_003388

answers: stereonets.

answers: NDQ_003389

answers: fold axes,

answers: NDQ_003390

answers: faults,

answers: NDQ_003391

answers: fold axes,

answers: NDQ_003392

answers: faults,

answers: NDQ_003393

answers: fold axes,

answers: NDQ_003394

answers: faults,

answers: NDQ_003395

answers: faults,

answers: NDQ_003396

answers: faults,

text: At a 'typical' subduction zone, an oceanic plate typically sinks at a fairly high angle (see above). A volcanic arc grows above the subducting plate. During the growth of the Rocky Mountains, the angle of the subducting plate may have been significantly flattened, moving the focus of melting and mountain building much farther inland than is normally expected.

text: At a 'typical' subduction zone, an oceanic plate typically sinks at a fairly high angle (see above). A volcanic arc grows above the subducting plate. During the growth of the Rocky Mountains, the angle of the subducting plate may have been significantly flattened, moving the focus of melting and mountain building much farther inland than is normally expected.

answers: NDQ_003351

answers: subduction zone

answers: NDQ_003352

answers: sinks

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: subduction zone

answers: NDQ_003356

answers: sink at a fairly high angle

answers: NDQ_003357

answers: an oceanic plate typically sinks at a fairly high angle

answers: NDQ_003358

answers: subduction zone

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: subducting plates

answers: NDQ_003362

answers: the Rocky Mountains moved the focus of melting and mountain building much farther inland than is normally expected

answers: NDQ_003363

answers: subduction zone

answers: NDQ_003371

answers: Which of the following is not a type of fault: subduction zone, volcanic arc, or thrust fault?

answers: NDQ_003373

answers: How would you describe a rock that is deeply buried?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a stress?

answers: NDQ_003381

answers: What would happen if an oceanic plate sinks at a fairly high angle?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: unanswerable

answers: NDQ_003386

answers: Which of the following is not a type of fault?

answers: NDQ_003387

answers: Which of the following is not a type of fault: subduction zone, volcanic arc, or mountain building?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip, strike-slip, or strike-slip?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: subduction zone

answers: NDQ_003391

answers: subducting plate

answers: NDQ_003392

answers: subduction zone

answers: NDQ_003393

answers: volcanic arc

answers: NDQ_003394

answers: flattened

answers: NDQ_003395

answers: unanswerable

answers: NDQ_003396

answers: flattened

answers: NDQ_003351

answers: subduction zone,

answers: NDQ_003352

answers: sinks at a fairly high angle

answers: NDQ_003353

answers: melting

answers: NDQ_003354

answers: volcanic arc grows above the subducting plate.

answers: NDQ_003355

answers: arc

answers: NDQ_003356

answers: melting

answers: NDQ_003357

answers: an oceanic plate typically sinks at a fairly high angle

answers: NDQ_003358

answers: subduction zone,

answers: NDQ_003359

answers: high angle

answers: NDQ_003360

answers: subduction zone,

answers: NDQ_003362

answers: significantly flattened,

answers: NDQ_003363

answers: subduction zone,

answers: NDQ_003371

answers: volcanic arc grows above the subducting plate.

answers: NDQ_003373

answers: At a 'typical' subduction zone,

answers: NDQ_003376

answers: Rocky Mountains,

answers: NDQ_003378

answers: At a 'typical' subduction zone,

answers: NDQ_003379

answers: high angle

answers: NDQ_003380

answers: oceanic plate typically sinks at a fairly high angle

answers: NDQ_003381

answers: At a 'typical' subduction zone,

answers: NDQ_003382

answers: 'typical' subduction zone,

answers: NDQ_003383

answers: At a 'typical' subduction zone,

answers: NDQ_003384

answers: volcanic arc

answers: NDQ_003385

answers: subduction zone,

answers: NDQ_003386

answers: subduction zone,

answers: NDQ_003387

answers: subduction zone,

answers: NDQ_003388

answers: At a 'typical' subduction zone,

answers: NDQ_003389

answers: melting

answers: NDQ_003390

answers: subduction zone,

answers: NDQ_003391

answers: volcanic arc grows above the subducting plate.

answers: NDQ_003392

answers: subduction zone,

answers: NDQ_003393

answers: volcanic arc

answers: NDQ_003394

answers: high angle

answers: NDQ_003395

answers: oceanic plate typically sinks at a fairly high angle

answers: NDQ_003396

answers: flattened,

text: Both the continental and oceanic crust "float" on the mantle. Because the continental crust is thicker, it extends both to greater elevations and greater depth than the oceanic crust. The slightly lower density of felsic continental rock compared to basaltic oceanic rock contributes to the higher relative elevation of the top of the continental crust. As the top of the continental crust reaches elevations higher than that of the oceanic, water runs off the continents and collects above the oceanic crust. Because of the change in velocity of seismic waves it is believed that beneath continents at a certain depth continental crust (sial) becomes close in its physical properties to oceanic crust (sima), and the transition zone is referred to as the Conrad discontinuity.

text: Both the continental and oceanic crust

text: "float" on the mantle

text: . Because the continental crust is thicker, it extends both to greater elevations and greater depth than the oceanic crust. The slightly lower density of felsic continental rock compared to basaltic oceanic rock contributes to the higher relative elevation of the top of the continental crust. As the top of the continental crust reaches elevations higher than that of the oceanic, water runs off the continents and collects above the oceanic crust. Because of the change in velocity of

text: seismic wave

text: s it is believed that beneath continents at a certain depth continental crust (

text: sial

text: ) becomes close in its physical properties to oceanic crust (

text: sima

text: ), and the transition zone is referred to as the

text: Conrad discontinuity

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: is likely to be more

answers: NDQ_003353

answers: seismic waves

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: continental crust

answers: NDQ_003356

answers: greater elevations and greater depth

answers: NDQ_003357

answers: water runs off the continents and collects above the oceanic crust

answers: NDQ_003358

answers: unanswerable

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: the mantle

answers: NDQ_003362

answers: water runs off the continents

answers: NDQ_003363

answers: oceanic crust

answers: NDQ_003371

answers: Which of the following is not a type of crust: continental, oceanic or basaltic?

answers: NDQ_003373

answers: because of the change in velocity of seismic waves

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: Which of the following is not a type of rock: felsic, basaltic, or oceanic?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a type of rock: felsic, basaltic, or oceanic?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: movement of rock at faults is the cause of earthquakes

answers: NDQ_003387

answers: Which of the following is not a type of normal fault?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip faults, basaltic faults, or strike-slip faults?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: Conrad discontinuity

answers: NDQ_003391

answers: Conrad discontinuity

answers: NDQ_003392

answers: Conrad discontinuity

answers: NDQ_003393

answers: oceanic crust

answers: NDQ_003394

answers: Conrad discontinuity

answers: NDQ_003395

answers: Conrad discontinuity

answers: NDQ_003396

answers: Conrad discontinuity

answers: NDQ_003351

answers: seismic waves

answers: NDQ_003352

answers: Conrad discontinuity.

answers: NDQ_003353

answers: seismic waves

answers: NDQ_003354

answers: Both the continental and oceanic crust "float" on the mantle.

answers: NDQ_003355

answers: Conrad discontinuity.

answers: NDQ_003356

answers: greater elevations

answers: NDQ_003357

answers: Conrad discontinuity.

answers: NDQ_003358

answers: Conrad discontinuity.

answers: NDQ_003359

answers: Both the continental and oceanic crust "float" on the mantle.

answers: NDQ_003360

answers: mantle.

answers: NDQ_003362

answers: Both the continental and oceanic crust "float" on the mantle.

answers: NDQ_003363

answers: continental and oceanic crust "float" on the mantle.

answers: NDQ_003371

answers: Conrad discontinuity.

answers: NDQ_003373

answers: The slightly lower density

answers: NDQ_003376

answers: water runs off the continents and collects above the oceanic crust.

answers: NDQ_003378

answers: seismic waves

answers: NDQ_003379

answers: Conrad discontinuity.

answers: NDQ_003380

answers: Both the continental and oceanic crust "float" on the mantle.

answers: NDQ_003381

answers: Both the continental and oceanic crust "float" on the mantle.

answers: NDQ_003382

answers: Conrad discontinuity.

answers: NDQ_003383

answers: seismic waves

answers: NDQ_003384

answers: Conrad discontinuity.

answers: NDQ_003385

answers: Conrad discontinuity.

answers: NDQ_003386

answers: seismic waves

answers: NDQ_003387

answers: Conrad discontinuity.

answers: NDQ_003388

answers: Conrad discontinuity.

answers: NDQ_003389

answers: Both the continental and oceanic crust "float" on the mantle.

answers: NDQ_003390

answers: Conrad discontinuity.

answers: NDQ_003391

answers: Conrad discontinuity.

answers: NDQ_003392

answers: Conrad discontinuity.

answers: NDQ_003393

answers: Conrad discontinuity.

answers: NDQ_003394

answers: Conrad discontinuity.

answers: NDQ_003395

answers: Conrad discontinuity.

answers: NDQ_003396

answers: Conrad discontinuity.

text: Radioactive primordial nuclides found in the Earth are residues from ancient supernova explosions which occurred before the formation of the solar system. They are the fraction of radionuclides that survived from that time, through the formation of the primordial solar nebula,  through planet accretion, and up to the present time. The naturally occurring short-lived radiogenic radionuclides found in today's rocks, are the daughters of those radioactive primordial nuclides. Another minor source of naturally occurring radioactive nuclides are cosmogenic nuclides, that are formed by cosmic ray bombardment of material in the Earth's atmosphere or crust. The decay of the radionuclides in rocks of the Earth's mantle and crust contribute significantly to Earth's internal heat budget.

text: Radioactive

text: primordial nuclide

text: s found in the

text: Earth

text: are residues from ancient

text: supernova

text: explosions which occurred before the formation of the

text: solar system

text: . They are the fraction of radionuclides that survived from that time, through the formation of the primordial solar

text: nebula

text: ,  through planet

text: accretion

text: , and up to the present time. The naturally occurring short-lived

text: radiogenic

text: radionuclide

text: s found in today's

text: rocks

text: , are the daughters of those radioactive

text: primordial nuclide

text: s. Another minor source of naturally occurring radioactive nuclides are

text: cosmogenic nuclide

text: s, that are formed by cosmic ray bombardment of material in the Earth's

text: atmosphere

text: or

text: crust

text: . The decay of the radionuclides in rocks of the Earth's

text: mantle

text: and

text: crust

text: contribute significantly to

text: Earth's internal heat budget

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: radioactive nuclides

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: decay

answers: NDQ_003357

answers: radioactive primordial nuclides found in the Earth are residues from ancient supernova explosions

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: accretion

answers: NDQ_003362

answers: radioactive primordial nuclides found in the Earth are residues from ancient supernova explosions

answers: NDQ_003363

answers: supernova explosions

answers: NDQ_003371

answers: Which of the following is not a source of naturally occurring radioactive nuclides?

answers: NDQ_003373

answers: How would you describe compressive stresses?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: Which of the following is not a source of naturally occurring radioactive nuclides?

answers: NDQ_003381

answers: What does the decay of the radionuclides in rocks of the Earth's mantle and crust contribute to?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: What is the cause of Earth's internal heat budget?

answers: NDQ_003387

answers: Which of the following is not a source of naturally occurring radioactive nuclides?

answers: NDQ_003388

answers: Which of the following is not a type of strike-slip fault?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: mantle

answers: NDQ_003392

answers: accretion

answers: NDQ_003393

answers: mantle

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: unanswerable

answers: NDQ_003396

answers: horizontal

answers: NDQ_003351

answers: cosmic ray bombardment

answers: NDQ_003352

answers: The decay of the radionuclides

answers: NDQ_003353

answers: The decay of the radionuclides

answers: NDQ_003354

answers: Radioactive primordial nuclides

answers: NDQ_003355

answers: Radioactive primordial nuclides

answers: NDQ_003356

answers: heat budget.

answers: NDQ_003357

answers: cosmic ray bombardment

answers: NDQ_003358

answers: rocks,

answers: NDQ_003359

answers: accretion,

answers: NDQ_003360

answers: planet accretion,

answers: NDQ_003362

answers: Radioactive primordial nuclides

answers: NDQ_003363

answers: ancient supernova explosions

answers: NDQ_003371

answers: Radioactive primordial nuclides

answers: NDQ_003373

answers: Radioactive primordial nuclides

answers: NDQ_003376

answers: Radioactive primordial nuclides

answers: NDQ_003378

answers: Radioactive primordial nuclides

answers: NDQ_003379

answers: Radioactive primordial nuclides

answers: NDQ_003380

answers: cosmic ray bombardment

answers: NDQ_003381

answers: radiogenic radionuclides

answers: NDQ_003382

answers: accretion,

answers: NDQ_003383

answers: radiogenic radionuclides

answers: NDQ_003384

answers: Radioactive primordial nuclides

answers: NDQ_003385

answers: Radioactive primordial nuclides

answers: NDQ_003386

answers: Radioactive primordial nuclides

answers: NDQ_003387

answers: cosmogenic nuclides,

answers: NDQ_003388

answers: Radioactive primordial nuclides

answers: NDQ_003389

answers: planet accretion,

answers: NDQ_003390

answers: Radioactive primordial nuclides

answers: NDQ_003391

answers: Radioactive primordial nuclides

answers: NDQ_003392

answers: Radioactive primordial nuclides

answers: NDQ_003393

answers: Radioactive primordial nuclides

answers: NDQ_003394

answers: Radioactive primordial nuclides

answers: NDQ_003395

answers: Radioactive primordial nuclides

answers: NDQ_003396

answers: Radioactive primordial nuclides

text: Areas of the crust where new crust is created are called divergent boundaries, those where it is brought back into the Earth are convergent boundaries and those where plates slide past each other, but no new lithospheric material is created or destroyed, are referred to as transform (or conservative) boundaries Earthquakes result from the movement of the lithospheric plates, and they often occur near convergent boundaries where parts of the crust are forced into the Earth as part of subduction.

text: Areas of the crust where new crust is created are called divergent boundaries, those where it is brought back into the Earth are convergent boundaries and those where plates slide past each other, but no new lithospheric material is created or destroyed, are referred to as

text: transform

text: (or conservative) boundaries

text: Earthquakes

text: result from the movement of the lithospheric plates, and they often occur near convergent boundaries where parts of the crust are forced into the Earth as part of subduction.

answers: NDQ_003351

answers: subduction

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: divergent boundary

answers: NDQ_003356

answers: subduct

answers: NDQ_003357

answers: transform (or conservative) boundaries

answers: NDQ_003358

answers: conservative boundary

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: plates

answers: NDQ_003362

answers: no new lithospheric material is created or destroyed

answers: NDQ_003363

answers: divergent boundaries

answers: NDQ_003371

answers: Which of the following is not an example of a transform (or conservative) boundary?

answers: NDQ_003373

answers: subduction

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: transform (or conservative) boundaries

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: Fault zone

answers: NDQ_003386

answers: no

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: unanswerable

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: subduction

answers: NDQ_003391

answers: subduction

answers: NDQ_003392

answers: subduction

answers: NDQ_003393

answers: subduction

answers: NDQ_003394

answers: divergent boundary

answers: NDQ_003395

answers: divergent boundaries

answers: NDQ_003396

answers: divergent boundary

answers: NDQ_003351

answers: Earthquakes

answers: NDQ_003352

answers: Earthquakes

answers: NDQ_003353

answers: Earthquakes

answers: NDQ_003354

answers: Areas of the crust where new crust is created are called divergent boundaries,

answers: NDQ_003355

answers: divergent boundaries,

answers: NDQ_003356

answers: Earthquakes

answers: NDQ_003357

answers: no new lithospheric material is created or destroyed,

answers: NDQ_003358

answers: transform (or conservative) boundaries

answers: NDQ_003359

answers: no new lithospheric material is created or destroyed,

answers: NDQ_003360

answers: Earthquakes

answers: NDQ_003362

answers: no new lithospheric material is created or destroyed,

answers: NDQ_003363

answers: subduction.

answers: NDQ_003371

answers: Earthquakes

answers: NDQ_003373

answers: Earthquakes

answers: NDQ_003376

answers: convergent boundaries

answers: NDQ_003378

answers: slide past each other,

answers: NDQ_003379

answers: convergent boundaries

answers: NDQ_003380

answers: Earthquakes

answers: NDQ_003381

answers: transform (or conservative) boundaries Earthquakes

answers: NDQ_003382

answers: Earthquakes

answers: NDQ_003383

answers: movement of the lithospheric plates,

answers: NDQ_003384

answers: divergent boundaries,

answers: NDQ_003385

answers: divergent boundaries,

answers: NDQ_003386

answers: lithospheric plates,

answers: NDQ_003387

answers: convergent boundaries

answers: NDQ_003388

answers: the movement of the lithospheric plates,

answers: NDQ_003389

answers: no new lithospheric material

answers: NDQ_003390

answers: subduction.

answers: NDQ_003391

answers: subduction.

answers: NDQ_003392

answers: divergent boundaries,

answers: NDQ_003393

answers: transform (or conservative) boundaries

answers: NDQ_003394

answers: divergent boundaries,

answers: NDQ_003395

answers: convergent boundaries

answers: NDQ_003396

answers: convergent boundaries

text: An extensional fault is a fault that vertically thins and horizontally extends portions of the Earth's crust and/or lithosphere. In most cases such a fault is also a normal fault, but may be rotated to have a shallower geometry normally associated with a thrust fault. Extensional faults are generally planar and, so long as the stress field is oriented with the maximum stress direction orthogonal to the Earth's surface initiate with a dip of 60° typically continuing down to the base of the seismogenic layer.

text: An extensional fault is a fault that vertically thins and horizontally extends portions of the

text: Earth's crust

text: and/or

text: lithosphere

text: . In most cases such a fault is also a

text: normal fault

text: , but may be rotated to have a shallower geometry normally associated with a

text: thrust fault

text: . Extensional faults are generally planar and, so long as the

text: stress field

text: is oriented with the maximum stress direction orthogonal to the Earth's surface initiate with a dip of 60° typically continuing down to the base of the

text: seismogenic layer

answers: NDQ_003351

answers: orthogonal

answers: NDQ_003352

answers: is more likely to break apart

answers: NDQ_003353

answers: a dip

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: thrust fault

answers: NDQ_003356

answers: extend

answers: NDQ_003357

answers: horizontally extends portions of the Earth's crust and/or lithosphere

answers: NDQ_003358

answers: normal fault

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: extensional faults

answers: NDQ_003362

answers: horizontally extends portions of the Earth's crust

answers: NDQ_003363

answers: extensional faults

answers: NDQ_003371

answers: Which of the following is not an example of an extensional fault?

answers: NDQ_003373

answers: What is the maximum stress direction orthogonal to the Earth's surface

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: no

answers: NDQ_003380

answers: What is an example of a stress field?

answers: NDQ_003381

answers: What type of fault is an extensional fault?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: What is the cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not a cause of normal faults?

answers: NDQ_003388

answers: Which of the following is not a cause of strike-slip faults?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: extensional fault

answers: NDQ_003391

answers: seismogenic layer

answers: NDQ_003392

answers: thrust fault

answers: NDQ_003393

answers: seismogenic layer

answers: NDQ_003394

answers: extensional fault

answers: NDQ_003395

answers: extensional fault

answers: NDQ_003396

answers: thrust fault

answers: NDQ_003351

answers: extensional fault

answers: NDQ_003352

answers: seismogenic layer.

answers: NDQ_003353

answers: thins and horizontally extends

answers: NDQ_003354

answers: An extensional fault

answers: NDQ_003355

answers: thrust fault.

answers: NDQ_003356

answers: extensional fault

answers: NDQ_003357

answers: a dip of 60°

answers: NDQ_003358

answers: extensional fault

answers: NDQ_003359

answers: stress field is oriented with the maximum stress direction

answers: NDQ_003360

answers: extensional fault

answers: NDQ_003362

answers: thrust fault.

answers: NDQ_003363

answers: extensional fault

answers: NDQ_003371

answers: extensional fault

answers: NDQ_003373

answers: extensional fault

answers: NDQ_003376

answers: extensional fault

answers: NDQ_003378

answers: extensional fault

answers: NDQ_003379

answers: 60°

answers: NDQ_003380

answers: stress

answers: NDQ_003381

answers: extensional fault

answers: NDQ_003382

answers: extensional fault

answers: NDQ_003383

answers: stress direction orthogonal to the Earth's surface

answers: NDQ_003384

answers: extensional fault

answers: NDQ_003385

answers: extensional fault

answers: NDQ_003386

answers: seismogenic layer.

answers: NDQ_003387

answers: extensional fault

answers: NDQ_003388

answers: extensional fault

answers: NDQ_003389

answers: extensional fault

answers: NDQ_003390

answers: extensional fault

answers: NDQ_003391

answers: seismogenic layer.

answers: NDQ_003392

answers: extensional fault

answers: NDQ_003393

answers: seismogenic layer.

answers: NDQ_003394

answers: thrust fault.

answers: NDQ_003395

answers: Extensional faults are generally planar

answers: NDQ_003396

answers: thrust fault.

text: In Superman and Superman II: The Richard Donner Cut, Superman's speed was shown as fast enough to reverse the timestream. In Superman II and Superman IV: The Quest for Peace, he possessed the ability to erase Lois Lane's (Margot Kidder) memory of the knowledge that he is Clark Kent by passionately kissing her. The kiss put her in a trance-like state and when she awoke, she remembered nothing but felt disoriented. Nevertheless, she remained undaunted and was in a sexually invigorated state. Because the three Kryptonian villains of the movie had the ability to shoot beams from their hands, Superman presumably would have the same power. In Superman III, he was able to create a diamond from coal using super strength and raising his heat temperature with a glowing yellow flash from his hand. In Superman IV: The Quest for Peace, he demonstrates the ability to repair damaged structures with a telekinetic beam from his eyes, and to levitate several falling people; he also shows a greater extension of his superhuman strength to draw the moon out of orbit and then return it to normal. In Superman Returns, Superman is shown to possess enough invulnerability to stare unblinkingly as a gun is fired point blank at his eye and receive no damage at all. Kryptonite only visibly exhausts him and makes him more physically vulnerable. By flying above the clouds and into the rays of the sun, he gained enough amplified strength to lift Lex Luthor's kryptonite-based sub-continent beyond the Earth's atmosphere and into space, despite the Kryptonite shard in his body and the Kryptonite pillars coming from the continent, though this severely weakens him and he falls back down to Earth in a coma. (However, the sub-continent was only poisoned with Kryptonite, not actually fully formed from it - the gigantic island was made from the crystal of Superman's homeworld.)

text: In

text: Superman

text: and

text: Superman II: The Richard Donner Cut

text: , Superman's speed was shown as fast enough to reverse the

text: timestream

text: . In

text: Superman II

text: and

text: Superman IV: The Quest for Peace

text: , he possessed the ability to erase

text: Lois Lane

text: 's (

text: Margot Kidder

text: ) memory of the knowledge that he is Clark Kent by passionately kissing her. The kiss put her in a trance-like state and when she awoke, she remembered nothing but felt disoriented. Nevertheless, she remained undaunted and was in a sexually invigorated state. Because the three Kryptonian villains of the movie had the ability to shoot beams from their hands, Superman presumably would have the same power. In

text: Superman III

text: , he was able to create a diamond from coal using super strength and raising his heat temperature with a glowing yellow flash from his hand. In Superman IV: The Quest for Peace, he demonstrates the ability to repair damaged structures with a telekinetic beam from his eyes, and to levitate several falling people; he also shows a greater extension of his superhuman strength to draw the moon out of orbit and then return it to normal. In

text: Superman Returns

text: , Superman is shown to possess enough invulnerability to stare unblinkingly as a gun is fired point blank at his eye and receive no damage at all. Kryptonite only visibly exhausts him and makes him more physically vulnerable. By flying above the clouds and into the rays of the sun, he gained enough amplified strength to lift Lex Luthor's kryptonite-based sub-continent beyond the Earth's atmosphere and into space, despite the Kryptonite shard in his body and the Kryptonite pillars coming from the continent, though this severely weakens him and he falls back down to Earth in a coma. (However, the sub-continent was only poisoned with Kryptonite, not actually fully formed from it - the gigantic island was made from the crystal of Superman's homeworld.)

answers: NDQ_003351

answers: Kryptonite

answers: NDQ_003352

answers: more likely to crack

answers: NDQ_003353

answers: Kryptonite pillars

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: Kryptonite only makes him more physically vulnerable.

answers: NDQ_003358

answers: shard

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's surface

answers: NDQ_003362

answers: the gigantic island was made from the crystal of Superman's homeworld.

answers: NDQ_003363

answers: Kryptonite

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: How does the sub-continent get poisoned with Kryptonite

answers: NDQ_003376

answers: What is caused by compressive forces?

answers: NDQ_003378

answers: What is the amount the ground moves in an earthquake?

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What was the sub-continent made from the crystal of Superman's homeworld?

answers: NDQ_003381

answers: How does the sub-continent deform?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: movement of rock at faults

answers: NDQ_003387

answers: What does Superman presumably have the same power as?

answers: NDQ_003388

answers: What does shear stress result from?

answers: NDQ_003389

answers: Kryptonite

answers: NDQ_003390

answers: Kryptonite

answers: NDQ_003391

answers: Kryptonite

answers: NDQ_003392

answers: The Richard Donner Cut

answers: NDQ_003393

answers: Kryptonite

answers: NDQ_003394

answers: Kryptonite

answers: NDQ_003395

answers: In Superman IV: The Quest for Peace, he demonstrates the ability to repair damaged structures

answers: NDQ_003396

answers: Kryptonite

answers: NDQ_003351

answers: falling people;

answers: NDQ_003352

answers: Kryptonite

answers: NDQ_003353

answers: crystal

answers: NDQ_003354

answers: Superman Returns, Superman

answers: NDQ_003355

answers: falling people;

answers: NDQ_003356

answers: falling people;

answers: NDQ_003357

answers: Superman

answers: NDQ_003358

answers: Kryptonite

answers: NDQ_003359

answers: Superman

answers: NDQ_003360

answers: Kryptonite

answers: NDQ_003362

answers: several falling people;

answers: NDQ_003363

answers: Kryptonite

answers: NDQ_003371

answers: Superman

answers: NDQ_003373

answers: Superman

answers: NDQ_003376

answers: to levitate several falling people;

answers: NDQ_003378

answers: Superman Returns, Superman

answers: NDQ_003379

answers: Superman

answers: NDQ_003380

answers: Superman

answers: NDQ_003381

answers: Superman

answers: NDQ_003382

answers: Superman

answers: NDQ_003383

answers: Superman Returns, Superman

answers: NDQ_003384

answers: Superman Returns, Superman

answers: NDQ_003385

answers: Superman

answers: NDQ_003386

answers: Superman

answers: NDQ_003387

answers: Superman

answers: NDQ_003388

answers: Superman

answers: NDQ_003389

answers: Superman Returns, Superman

answers: NDQ_003390

answers: Superman

answers: NDQ_003391

answers: Kryptonite

answers: NDQ_003392

answers: superhuman strength

answers: NDQ_003393

answers: Kryptonite

answers: NDQ_003394

answers: people;

answers: NDQ_003395

answers: Superman Returns,

answers: NDQ_003396

answers: falling people;

text: Pangaea has tremendously affected the setup of the world now. We live in a post Pangaea time period where the reconfiguration of continents and oceans has changed the climate of many areas. There is scientific evidence that proves that climate was drastically altered. When the continents separated and reformed themselves, it changed the flow of the oceanic currents and winds. The scientific reasoning behind all of the changes is Continental Drift. The theory of Continental Drift, created by Alfred Wegener, explained how the continents shifted Earth’s surface and how that affected many aspects such as climate, rock formations found on different continents and plant and animal fossils. Wegener studied plant fossils from the frigid Arctic of Svalbard, Norway. He determined that such plants were not meant to adapt to a glacial climate. The fossils he found were from tropical plants that were meant to adapt and thrive in warmer and tropical climate. Because we would not assume that the plant fossils were capable of traveling to a different place we suspect that Svalbard possibly had a warmer, less frigid climate in the past.

text: Pangaea has tremendously affected the setup of the world now. We live in a post Pangaea time period where the reconfiguration of continents and oceans has changed the climate of many areas. There is scientific evidence that proves that climate was drastically altered. When the continents separated and reformed themselves, it changed the flow of the oceanic currents and winds. The scientific reasoning behind all of the changes is

text: Continental Drift

text: . The theory of Continental Drift, created by

text: Alfred Wegener

text: , explained how the continents shifted Earth’s surface and how that affected many aspects such as climate, rock formations found on different continents and plant and animal fossils. Wegener studied plant fossils from the frigid Arctic of

text: Svalbard

text: Norway

text: . He determined that such plants were not meant to adapt to a glacial climate. The fossils he found were from tropical plants that were meant to adapt and thrive in warmer and tropical climate. Because we would not assume that the plant fossils were capable of traveling to a different place we suspect that Svalbard possibly had a warmer, less frigid climate in the past.

answers: NDQ_003351

answers: continental drift

answers: NDQ_003352

answers: is likely to crack

answers: NDQ_003353

answers: igneous rocks to form

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: glacial

answers: NDQ_003356

answers: change their shape

answers: NDQ_003357

answers: the flow of the oceanic currents and winds would be

answers: NDQ_003358

answers: rock formation

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: continents

answers: NDQ_003362

answers: the San Andreas fault is caused by tectonic plates

answers: NDQ_003363

answers: Pangaea

answers: NDQ_003371

answers: Which of the following is an example of a thrust fault?

answers: NDQ_003373

answers: Which of the following is not a type of stress?

answers: NDQ_003376

answers: Which of the following is not a type of terrain: basin-and-range or continental drift?

answers: NDQ_003378

answers: Which of the following is not a type of fossil found in Svalbard, Norway?

answers: NDQ_003379

answers: Which of the following is not a type of fault?

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: Which of the following is not an example of confining stress?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not a type of fold?

answers: NDQ_003385

answers: Which of the following is not an area where faults are clustered?

answers: NDQ_003386

answers: Which of the following is not a cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not a cause of normal faults?

answers: NDQ_003388

answers: Which of the following is not an example of a strike-slip fault?

answers: NDQ_003389

answers: Which of the following is not a type of mountain range?

answers: NDQ_003390

answers: Continental Drift

answers: NDQ_003391

answers: continental drift

answers: NDQ_003392

answers: Continental Drift

answers: NDQ_003393

answers: continental drift

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: is a

answers: NDQ_003396

answers: continental drift

answers: NDQ_003351

answers: Continental Drift.

answers: NDQ_003352

answers: Continental Drift.

answers: NDQ_003353

answers: Continental Drift.

answers: NDQ_003354

answers: Pangaea

answers: NDQ_003355

answers: Continental Drift.

answers: NDQ_003356

answers: Continental Drift.

answers: NDQ_003357

answers: oceanic currents and winds.

answers: NDQ_003358

answers: rock formations

answers: NDQ_003359

answers: Continental Drift.

answers: NDQ_003360

answers: Pangaea

answers: NDQ_003362

answers: Pangaea

answers: NDQ_003363

answers: Pangaea

answers: NDQ_003371

answers: Continental Drift.

answers: NDQ_003373

answers: Continental Drift.

answers: NDQ_003376

answers: Continental Drift.

answers: NDQ_003378

answers: Continental Drift.

answers: NDQ_003379

answers: Continental Drift.

answers: NDQ_003380

answers: Continental Drift.

answers: NDQ_003381

answers: Continental Drift.

answers: NDQ_003382

answers: Continental Drift.

answers: NDQ_003383

answers: Continental Drift.

answers: NDQ_003384

answers: Continental Drift.

answers: NDQ_003385

answers: Pangaea

answers: NDQ_003386

answers: Continental Drift.

answers: NDQ_003387

answers: Continental Drift.

answers: NDQ_003388

answers: Continental Drift.

answers: NDQ_003389

answers: Continental Drift.

answers: NDQ_003390

answers: Pangaea

answers: NDQ_003391

answers: Continental Drift.

answers: NDQ_003392

answers: Pangaea

answers: NDQ_003393

answers: Continental Drift.

answers: NDQ_003394

answers: Pangaea

answers: NDQ_003395

answers: Pangaea

answers: NDQ_003396

answers: Continental Drift.

text: The Trans-Hudson orogen sutured together the Hearne-Rae, Superior, and Wyoming cratons to form the cratonic core of North America in a network of Paleoproterozoic orogenic belts. These orogenic belts include the margins of at least nine independent microcontinents that were themselves sections of at least three former major supercontinents, including Laurasia, Pangaea and Kenorland (ca. 2.7 Ga), and contain parts of some of the oldest cratonic continental crust on Earth.  These old cratonic blocks, along with accreted island arc terranes and intraoceanic deposits from earlier Proterozoic and Mesozoic oceans and seaways, were sutured together in the Trans-Hudson Orogen (THO) and resulted in extensive folding and thrust faulting along with metamorphism and hundreds of huge granitic intrusions.

text: The Trans-Hudson orogen sutured together the

text: Hearne

text: Rae

text: Superior

text: , and

text: Wyoming

text: cratons

text: to form the cratonic core of North America in a network of Paleoproterozoic orogenic belts. These orogenic belts include the margins of at least nine independent

text: microcontinents

text: that were themselves sections of at least three former major supercontinents, including

text: Laurasia

text: Pangaea

text: and

text: Kenorland

text: (ca. 2.7

text: Ga

text: ), and contain parts of some of the oldest cratonic

text: continental crust

text: on

text: Earth

text: .  These old cratonic blocks, along with accreted

text: island arc

text: terrane

text: s and

text: intraoceanic

text: deposits from earlier Proterozoic and

text: Mesozoic

text: oceans and seaways, were sutured together in the Trans-Hudson Orogen (THO) and resulted in extensive folding and

text: thrust fault

text: ing along with metamorphism and hundreds of huge

text: granitic

text: intrusion

text: s.

answers: NDQ_003351

answers: thrust faulting

answers: NDQ_003352

answers: folds

answers: NDQ_003353

answers: metamorphism

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: orogenic belt

answers: NDQ_003356

answers: fold

answers: NDQ_003357

answers: thrust faulting is a type of

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: folds

answers: NDQ_003360

answers: Trans-Hudson orogen

answers: NDQ_003362

answers: extensive folding and thrust faulting along with metamorphism

answers: NDQ_003363

answers: Trans-Hudson orogen

answers: NDQ_003371

answers: What is the result of folding and thrust faulting?

answers: NDQ_003373

answers: What type of stresses does the Trans-Hudson Orogen cause?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: what is the last word in the passage?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What type of force applied to rock is a stress?

answers: NDQ_003381

answers: What is the result of extensive folding and thrust faulting?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What was the result of extensive folding and thrust faulting along with metamorphism?

answers: NDQ_003384

answers: What type of folds resulted in extensive folding and thrust faulting along with metamorphism?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: Which of the following is not a cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: thrust faulting, folding, or metamorphism?

answers: NDQ_003388

answers: Which of the following is not a type of fault: thrust faulting, folding, or thrust faulting?

answers: NDQ_003389

answers: None of the above choices

answers: NDQ_003390

answers: thrust faulting

answers: NDQ_003391

answers: cratonic blocks

answers: NDQ_003392

answers: thrust faulting

answers: NDQ_003393

answers: cratonic blocks

answers: NDQ_003394

answers: thrust faulting

answers: NDQ_003395

answers: thrust faulting

answers: NDQ_003396

answers: thrust faulting

answers: NDQ_003351

answers: thrust faulting

answers: NDQ_003352

answers: folding and thrust faulting

answers: NDQ_003353

answers: metamorphism

answers: NDQ_003354

answers: Trans-Hudson Orogen

answers: NDQ_003355

answers: thrust faulting

answers: NDQ_003356

answers: folding and thrust faulting

answers: NDQ_003357

answers: thrust faulting

answers: NDQ_003358

answers: thrust faulting

answers: NDQ_003359

answers: thrust faulting

answers: NDQ_003360

answers: The Trans-Hudson orogen

answers: NDQ_003362

answers: folding and thrust faulting

answers: NDQ_003363

answers: Trans-Hudson orogen

answers: NDQ_003371

answers: thrust faulting

answers: NDQ_003373

answers: thrust faulting

answers: NDQ_003376

answers: folding and thrust faulting

answers: NDQ_003378

answers: thrust faulting

answers: NDQ_003379

answers: thrust faulting

answers: NDQ_003380

answers: thrust faulting

answers: NDQ_003381

answers: folding and thrust faulting

answers: NDQ_003382

answers: thrust faulting

answers: NDQ_003383

answers: folding and thrust faulting

answers: NDQ_003384

answers: thrust faulting

answers: NDQ_003385

answers: thrust faulting

answers: NDQ_003386

answers: thrust faulting

answers: NDQ_003387

answers: thrust faulting

answers: NDQ_003388

answers: thrust faulting

answers: NDQ_003389

answers: folding

answers: NDQ_003390

answers: thrust

answers: NDQ_003391

answers: granitic

answers: NDQ_003392

answers: thrust

answers: NDQ_003393

answers: granitic

answers: NDQ_003394

answers: thrust faulting

answers: NDQ_003395

answers: thrust faulting

answers: NDQ_003396

answers: thrust

text: The San Andreas Fault System has been the subject of a flood of studies. In particular, scientific research performed during the last 23 years has given rise to about 3,400 publications.

text: The San Andreas Fault System has been the subject of a flood of studies. In particular, scientific research performed during the last 23 years has given rise to about 3,400 publications.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: more likely to crack

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: fold that bends downward

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: San Andreas Fault System has been the subject of a flood

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: San Andreas faults

answers: NDQ_003362

answers: The San Andreas Fault System has been the subject of a flood of studies

answers: NDQ_003363

answers: San Andreas Fault

answers: NDQ_003371

answers: What is the San Andreas Fault System?

answers: NDQ_003373

answers: None of the above choices.

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What is the San Andreas Fault System?

answers: NDQ_003382

answers: None of the above choices.

answers: NDQ_003383

answers: None of the above choices.

answers: NDQ_003384

answers: None of the above choices.

answers: NDQ_003385

answers: What is the San Andreas Fault System?

answers: NDQ_003386

answers: no

answers: NDQ_003387

answers: None of the above choices.

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip, strike-slip or strike-slip?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: San Andreas Fault System

answers: NDQ_003391

answers: dip-slip fault

answers: NDQ_003392

answers: San Andreas Fault System

answers: NDQ_003393

answers: dip-slip fault

answers: NDQ_003394

answers: San Andreas

answers: NDQ_003395

answers: San Andreas Fault

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: The San Andreas Fault System

answers: NDQ_003352

answers: 3,400 publications.

answers: NDQ_003353

answers: The San Andreas Fault System

answers: NDQ_003354

answers: The San Andreas Fault System

answers: NDQ_003355

answers: The San Andreas Fault System

answers: NDQ_003356

answers: The San Andreas Fault System

answers: NDQ_003357

answers: 3,400 publications.

answers: NDQ_003358

answers: Fault System

answers: NDQ_003359

answers: The San Andreas Fault System

answers: NDQ_003360

answers: The San Andreas Fault System

answers: NDQ_003362

answers: a flood of studies.

answers: NDQ_003363

answers: San Andreas Fault System

answers: NDQ_003371

answers: The San Andreas Fault System

answers: NDQ_003373

answers: The San Andreas Fault System

answers: NDQ_003376

answers: The San Andreas Fault System

answers: NDQ_003378

answers: 3,400 publications.

answers: NDQ_003379

answers: 3,400 publications.

answers: NDQ_003380

answers: The San Andreas Fault System

answers: NDQ_003381

answers: The San Andreas Fault System

answers: NDQ_003382

answers: 3,400 publications.

answers: NDQ_003383

answers: The San Andreas Fault System

answers: NDQ_003384

answers: The San Andreas Fault System

answers: NDQ_003385

answers: The San Andreas Fault System

answers: NDQ_003386

answers: The San Andreas Fault System

answers: NDQ_003387

answers: The San Andreas Fault System

answers: NDQ_003388

answers: The San Andreas Fault System

answers: NDQ_003389

answers: The San Andreas Fault System

answers: NDQ_003390

answers: San Andreas Fault System

answers: NDQ_003391

answers: The San Andreas Fault System

answers: NDQ_003392

answers: San Andreas Fault System

answers: NDQ_003393

answers: The San Andreas Fault System

answers: NDQ_003394

answers: San Andreas Fault System

answers: NDQ_003395

answers: San Andreas Fault System

answers: NDQ_003396

answers: San Andreas Fault System

text: Within Earth's crust, iridium is found at highest concentrations in three types of geologic structure: igneous deposits (crustal intrusions from below), impact craters, and deposits reworked from one of the former structures. The largest known primary reserves are in the Bushveld igneous complex in South Africa, though the large copper–nickel deposits near Norilsk in Russia, and the Sudbury Basin in Canada are also significant sources of iridium. Smaller reserves are found in the United States. Iridium is also found in secondary deposits, combined with platinum and other platinum group metals in alluvial deposits. The alluvial deposits used by pre-Columbian people in the Chocó Department of Colombia are still a source for platinum-group metals.  As of 2003, the world reserves had not been estimated.

text: Within Earth's crust, iridium is found at highest concentrations in three types of geologic structure: igneous deposits (crustal intrusions from below), impact craters, and deposits reworked from one of the former structures. The largest known primary reserves are in the

text: Bushveld igneous complex

text: in

text: South Africa

text: , though the large copper–nickel deposits near

text: Norilsk

text: in

text: Russia

text: , and the

text: Sudbury Basin

text: in

text: Canada

text: are also significant sources of iridium. Smaller reserves are found in the United States. Iridium is also found in secondary deposits, combined with platinum and other platinum group metals in

text: alluvial

text: deposits. The alluvial deposits used by

text: pre-Columbian

text: people in the

text: Chocó Department

text: of

text: Colombia

text: are still a source for platinum-group metals.  As of 2003, the world reserves had not been estimated.

answers: NDQ_003351

answers: impact craters

answers: NDQ_003352

answers: deposits more iridium

answers: NDQ_003353

answers: impact craters

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: igneous deposit

answers: NDQ_003356

answers: impact craters

answers: NDQ_003357

answers: igneous deposits (crustal intrusions from below)

answers: NDQ_003358

answers: impact craters

answers: NDQ_003359

answers: fractures from below

answers: NDQ_003360

answers: Earth's

answers: NDQ_003362

answers: the world reserves had not been estimated.

answers: NDQ_003363

answers: Earth's crust

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: igneous deposits

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: what is the first type of geologic structure mentioned?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: fault zone

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: unanswerable

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: impact craters

answers: NDQ_003391

answers: igneous deposits

answers: NDQ_003392

answers: impact craters

answers: NDQ_003393

answers: igneous deposits

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: impact craters

answers: NDQ_003396

answers: impact craters

answers: NDQ_003351

answers: (crustal intrusions from below), impact craters,

answers: NDQ_003352

answers: impact craters,

answers: NDQ_003353

answers: (crustal intrusions from below), impact craters,

answers: NDQ_003354

answers: Smaller reserves are found in the United States.

answers: NDQ_003355

answers: impact craters,

answers: NDQ_003356

answers: impact craters,

answers: NDQ_003357

answers: impact craters,

answers: NDQ_003358

answers: impact craters,

answers: NDQ_003359

answers: below),

answers: NDQ_003360

answers: (crustal intrusions from below),

answers: NDQ_003362

answers: Within Earth's crust, iridium

answers: NDQ_003363

answers: below),

answers: NDQ_003371

answers: impact craters,

answers: NDQ_003373

answers: igneous deposits

answers: NDQ_003376

answers: igneous deposits (crustal intrusions from below),

answers: NDQ_003378

answers: (crustal intrusions from below), impact craters,

answers: NDQ_003379

answers: Bushveld igneous complex in South Africa,

answers: NDQ_003380

answers: impact craters,

answers: NDQ_003381

answers: (crustal intrusions from below), impact craters,

answers: NDQ_003382

answers: Bushveld igneous complex in South Africa,

answers: NDQ_003383

answers: impact craters,

answers: NDQ_003384

answers: igneous deposits (crustal intrusions from below),

answers: NDQ_003385

answers: Within Earth's crust,

answers: NDQ_003386

answers: (crustal intrusions from below), impact craters,

answers: NDQ_003387

answers: impact craters,

answers: NDQ_003388

answers: Bushveld igneous complex in South Africa,

answers: NDQ_003389

answers: igneous deposits

answers: NDQ_003390

answers: impact craters,

answers: NDQ_003391

answers: igneous deposits

answers: NDQ_003392

answers: impact craters,

answers: NDQ_003393

answers: impact craters,

answers: NDQ_003394

answers: impact craters,

answers: NDQ_003395

answers: impact craters,

answers: NDQ_003396

answers: impact craters,

text: Columnar jointing is a geological structure where sets of intersecting closely spaced fractures, referred to as joints, result in the formation of a regular array of polygonal prisms, or columns. Columnar jointing occurs in many types of volcanic rocks and forms as the rock cools and contracts. Columnar jointing can occur in cooling lava flows and ashflow tuffs (ignimbrites), as well as in some shallow intrusions.

text: Columnar jointing is a geological structure where sets of intersecting closely spaced fractures, referred to as

text: joints

text: , result in the formation of a regular array of polygonal

text: prisms

text: , or columns. Columnar jointing occurs in many types of

text: volcanic rock

text: s and forms as the rock cools and contracts. Columnar jointing can occur in cooling

text: lava flows

text: and ashflow

text: tuff

text: s (

text: ignimbrite

text: s), as well as in some shallow

text: intrusion

text: s.

answers: NDQ_003351

answers: Columnar jointing

answers: NDQ_003352

answers: cools

answers: NDQ_003353

answers: fractures

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: columnar jointing

answers: NDQ_003356

answers: contract

answers: NDQ_003357

answers: columns of intersecting closely spaced fractures

answers: NDQ_003358

answers: joints

answers: NDQ_003359

answers: cools

answers: NDQ_003360

answers: volcanoes

answers: NDQ_003362

answers: Columnar jointing occurs in many types of volcanic rocks

answers: NDQ_003363

answers: Columnar jointing

answers: NDQ_003371

answers: What is a geological structure where sets of intersecting closely spaced fractures, referred to as joints

answers: NDQ_003373

answers: Why would a rock be under compressive stresses?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What happens when the rock cools and contracts?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: What is the term for a geological structure where sets of intersecting closely spaced fractures

answers: NDQ_003386

answers: Which of the following is not a cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: normal faults, lava flows, or ashflow tuffs?

answers: NDQ_003388

answers: Which of the following is not a geological structure: Columnar jointing, strike-slip faults, or ignimbrites?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: Columnar jointing

answers: NDQ_003391

answers: tuffs

answers: NDQ_003392

answers: Columnar jointing

answers: NDQ_003393

answers: tuffs

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: columnar jointing

answers: NDQ_003396

answers: Columnar jointing

answers: NDQ_003351

answers: Columnar jointing

answers: NDQ_003352

answers: Columnar jointing

answers: NDQ_003353

answers: fractures,

answers: NDQ_003354

answers: Columnar jointing

answers: NDQ_003355

answers: Columnar jointing

answers: NDQ_003356

answers: cools and contracts.

answers: NDQ_003357

answers: intersecting closely spaced fractures,

answers: NDQ_003358

answers: joints,

answers: NDQ_003359

answers: cools and contracts.

answers: NDQ_003360

answers: Columnar jointing

answers: NDQ_003362

answers: formation of a regular array of polygonal prisms,

answers: NDQ_003363

answers: volcanic rocks

answers: NDQ_003371

answers: Columnar jointing

answers: NDQ_003373

answers: Columnar jointing occurs in many types of volcanic rocks

answers: NDQ_003376

answers: Columnar jointing

answers: NDQ_003378

answers: Columnar jointing

answers: NDQ_003379

answers: Columnar jointing can occur in cooling lava flows

answers: NDQ_003380

answers: Columnar jointing occurs in many types of volcanic rocks

answers: NDQ_003381

answers: Columnar jointing occurs in many types of volcanic rocks

answers: NDQ_003382

answers: Columnar jointing occurs in many types of volcanic rocks

answers: NDQ_003383

answers: fractures,

answers: NDQ_003384

answers: Columnar jointing

answers: NDQ_003385

answers: sets of intersecting closely spaced fractures,

answers: NDQ_003386

answers: Columnar jointing

answers: NDQ_003387

answers: Columnar jointing

answers: NDQ_003388

answers: Columnar jointing

answers: NDQ_003389

answers: Columnar jointing

answers: NDQ_003390

answers: Columnar jointing

answers: NDQ_003391

answers: Columnar jointing

answers: NDQ_003392

answers: Columnar jointing

answers: NDQ_003393

answers: Columnar jointing

answers: NDQ_003394

answers: Columnar jointing

answers: NDQ_003395

answers: Columnar jointing

answers: NDQ_003396

answers: Columnar jointing

text: The Angoumian forms part of two very open synclines striking NW-SE (the Combiers-Saint-Crépin-de-Richemont syncline in the NE) and WNW-ESE (the Gout-Rossignol-Léguillac synline in the SW) respectively. The group is therefore mainly flat-lying, yet in some places (like near Champeaux it dips 5° to the SW. Only near Beaussac a greater dip (of about 30°) can be found caused by local faulting. Nearby in the Aucors quarry, a  slump overlies the rudist reef, followed by a grain flow. These synsedimentary structures point to a tectonically disturbed setting possibly related to the rising Mareuil Anticline. Small strike-slip faults can be observed near Brantôme which mostly show a horizontal movement direction pointing to the SSE, rarely to the SE. There is also a fairly common occurrence of slickolites (a special kind of stylolite), which indicate the direction of pressure solution in the rock. This direction is mostly vertical, i.e. merely representing the overburden of the overlying strata. Yet significant aberrations from this direction can be observed as well, proving that the group was also under the influence of directional stresses.

text: The Angoumian forms part of two very open

text: syncline

text: s striking NW-SE (the Combiers-Saint-Crépin-de-Richemont syncline in the NE) and WNW-ESE (the Gout-Rossignol-Léguillac synline in the SW) respectively. The group is therefore mainly flat-lying, yet in some places (like near

text: Champeaux

text: it dips 5° to the SW. Only near

text: Beaussac

text: a greater dip (of about 30°) can be found caused by local faulting. Nearby in the Aucors quarry, a

text: slump

text: overlies the rudist reef, followed by a

text: grain flow

text: . These synsedimentary structures point to a tectonically disturbed setting possibly related to the rising

text: Mareuil Anticline

text: . Small

text: strike-slip

text: faults can be observed near Brantôme which mostly show a horizontal movement direction pointing to the SSE, rarely to the SE. There is also a fairly common occurrence of

text: slickolite

text: s (a special kind of

text: stylolite

text: ), which indicate the direction of

text: pressure solution

text: in the rock. This direction is mostly vertical, i.e. merely representing the overburden of the overlying strata. Yet significant aberrations from this direction can be observed as well, proving that the group was also under the influence of directional stresses.

answers: NDQ_003351

answers: directional stresses

answers: NDQ_003352

answers: dips

answers: NDQ_003353

answers: direction of pressure solution

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: WNW-ES

answers: NDQ_003356

answers: slickolites

answers: NDQ_003357

answers: direction of pressure solution in the rock

answers: NDQ_003358

answers: strike-slip

answers: NDQ_003359

answers: strikes another rock

answers: NDQ_003360

answers: tectonic plates

answers: NDQ_003362

answers: the group was also under the influence of directional stresses.

answers: NDQ_003363

answers: Angoumian

answers: NDQ_003371

answers: What can be observed near Brantôme?

answers: NDQ_003373

answers: no

answers: NDQ_003376

answers: Why is the group mainly flat-lying?

answers: NDQ_003378

answers: strike-slip faults

answers: NDQ_003379

answers: no

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What can be observed in the Aucors quarry?

answers: NDQ_003382

answers: What direction is the group mainly flat-lying?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What type of fold does the Angoumian form part of?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: What is the cause of directional stresses?

answers: NDQ_003387

answers: What is the direction of pressure solution in the rock?

answers: NDQ_003388

answers: What is the direction of pressure solution in the rock?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: strike-slip faults

answers: NDQ_003391

answers: rudist reef

answers: NDQ_003392

answers: strike-slip faults

answers: NDQ_003393

answers: the overlying strata

answers: NDQ_003394

answers: strike-slip faults

answers: NDQ_003395

answers: strike-slip faults can be observed near Brantôme

answers: NDQ_003396

answers: strike-slip faults

answers: NDQ_003351

answers: directional

answers: NDQ_003352

answers: directional stresses.

answers: NDQ_003353

answers: aberrations

answers: NDQ_003354

answers: The Angoumian

answers: NDQ_003355

answers: strike-slip faults

answers: NDQ_003356

answers: directional stresses.

answers: NDQ_003357

answers: horizontal movement direction

answers: NDQ_003358

answers: strike-slip faults

answers: NDQ_003359

answers: directional stresses.

answers: NDQ_003360

answers: directional stresses.

answers: NDQ_003362

answers: rising Mareuil Anticline.

answers: NDQ_003363

answers: The Angoumian

answers: NDQ_003371

answers: strike-slip faults

answers: NDQ_003373

answers: directional stresses.

answers: NDQ_003376

answers: directional stresses.

answers: NDQ_003378

answers: strike-slip

answers: NDQ_003379

answers: direction of pressure solution

answers: NDQ_003380

answers: directional stresses.

answers: NDQ_003381

answers: directional stresses.

answers: NDQ_003382

answers: directional stresses.

answers: NDQ_003383

answers: directional stresses.

answers: NDQ_003384

answers: synclines

answers: NDQ_003385

answers: synclines

answers: NDQ_003386

answers: directional stresses.

answers: NDQ_003387

answers: directional stresses.

answers: NDQ_003388

answers: directional stresses.

answers: NDQ_003389

answers: faulting.

answers: NDQ_003390

answers: strike-slip

answers: NDQ_003391

answers: rudist reef,

answers: NDQ_003392

answers: strike-slip

answers: NDQ_003393

answers: rudist reef,

answers: NDQ_003394

answers: strike-slip faults

answers: NDQ_003395

answers: slickolites

answers: NDQ_003396

answers: strike-slip faults

text: The sedimentary rock cover of the continents of the Earth's crust is extensive (73% of the Earth's current land surface), but the total contribution of sedimentary rocks is estimated to be only 8% of the total volume of the crust. Sedimentary rocks are only a thin veneer over a crust consisting mainly of igneous and metamorphic rocks. Sedimentary rocks are deposited in layers as strata, forming a structure called bedding. The study of sedimentary rocks and rock strata provides information about the subsurface that is useful for civil engineering, for example in the construction of roads, houses, tunnels, canals or other structures. Sedimentary rocks are also important sources of natural resources like coal, fossil fuels, drinking water or ores.

text: The sedimentary rock cover of the continents of the

text: Earth's crust

text: is extensive (73% of the Earth's current land surface), but the total contribution of sedimentary rocks is estimated to be only 8% of the total volume of the crust. Sedimentary rocks are only a thin veneer over a crust consisting mainly of

text: igneous

text: and

text: metamorphic rock

text: s. Sedimentary rocks are deposited in layers as

text: strata

text: , forming a structure called

text: bedding

text: . The study of sedimentary rocks and rock strata provides information about the subsurface that is useful for

text: civil engineering

text: , for example in the construction of

text: road

text: s,

text: house

text: s,

text: tunnel

text: s,

text: canal

text: s or other structures. Sedimentary rocks are also important sources of

text: natural resource

text: s like

text: coal

text: fossil fuel

text: s,

text: drinking water

text: or

text: ore

text: s.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: metamorphism

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: strata

answers: NDQ_003356

answers: erode

answers: NDQ_003357

answers: sedimentary rocks are deposited in layers as strata, forming a structure called bedding

answers: NDQ_003358

answers: igneous

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: only 8% of the total volume of the crust

answers: NDQ_003363

answers: sedimentary rocks

answers: NDQ_003371

answers: Which of the following is not a type of rock: igneous or metamorphic?

answers: NDQ_003373

answers: what is the last word in the passage?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: what is the last word in the passage?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a type of rock: igneous or metamorphic?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: movement of rock at faults is the cause of earthquakes

answers: NDQ_003387

answers: Which of the following is not a type of rock: igneous or metamorphic?

answers: NDQ_003388

answers: Which of the following is not a source of natural resources like coal, fossil fuels, drinking water or ores?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: a structure called bedding

answers: NDQ_003391

answers: strata

answers: NDQ_003392

answers: igneous

answers: NDQ_003393

answers: strata

answers: NDQ_003394

answers: igneous

answers: NDQ_003395

answers: igneous

answers: NDQ_003396

answers: igneous

answers: NDQ_003351

answers: igneous and metamorphic rocks.

answers: NDQ_003352

answers: bedding.

answers: NDQ_003353

answers: bedding.

answers: NDQ_003354

answers: The sedimentary rock

answers: NDQ_003355

answers: bedding.

answers: NDQ_003356

answers: bedding.

answers: NDQ_003357

answers: bedding.

answers: NDQ_003358

answers: bedding.

answers: NDQ_003359

answers: The sedimentary rock

answers: NDQ_003360

answers: sedimentary rock

answers: NDQ_003362

answers: 8%

answers: NDQ_003363

answers: igneous and metamorphic rocks.

answers: NDQ_003371

answers: 8% of the total volume of the crust. Sedimentary rocks

answers: NDQ_003373

answers: bedding.

answers: NDQ_003376

answers: bedding.

answers: NDQ_003378

answers: bedding. The study of sedimentary rocks

answers: NDQ_003379

answers: 8%

answers: NDQ_003380

answers: bedding.

answers: NDQ_003381

answers: bedding. The study of sedimentary rocks

answers: NDQ_003382

answers: 8% of the total volume of the crust. Sedimentary rocks

answers: NDQ_003383

answers: bedding.

answers: NDQ_003384

answers: 8% of the total volume of the crust. Sedimentary rocks

answers: NDQ_003385

answers: 8% of the total volume of the crust. Sedimentary rocks

answers: NDQ_003386

answers: The sedimentary rock

answers: NDQ_003387

answers: igneous and metamorphic rocks.

answers: NDQ_003388

answers: 8% of the total volume of the crust. Sedimentary rocks

answers: NDQ_003389

answers: Sedimentary rocks

answers: NDQ_003390

answers: The sedimentary rock

answers: NDQ_003391

answers: bedding.

answers: NDQ_003392

answers: The sedimentary rock

answers: NDQ_003393

answers: Sedimentary rocks

answers: NDQ_003394

answers: The sedimentary rock

answers: NDQ_003395

answers: igneous and metamorphic rocks.

answers: NDQ_003396

answers: igneous and metamorphic rocks.

text: The collision of India with Asia is the latest major tectonic event to affect deformation in the Tian Shan. Thrust faulting is the predominant style of Cenozoic deformation in the Tian Shan, which propagated outward and rose progressively as a wedge-shaped block. Dextral NW-SE trending strike slip faults either merge with or crosscut east-west trending thrust systems. The Talas-Fergana Fault is the longest of these structures. Active deformation in the Tian Shan is the result of compressional stresses generated at the Indo-Asia collisional zone, where the Himalayas formed and continue to grow. Active deformation is observed in the Tian Shan, which is within Asia’s continental interior, because Asia is not as internally rigid as the continental crust is expected to be.

text: The collision of

text: India

text: with

text: Asia

text: is the latest major tectonic event to affect deformation in the Tian Shan.

text: Thrust faulting

text: is the predominant style of

text: Cenozoic

text: deformation in the Tian Shan, which propagated outward and rose progressively as a wedge-shaped block.

text: Dextral

text: NW-SE trending

text: strike slip faults

text: either merge with or crosscut east-west trending

text: thrust systems

text: . The

text: Talas-Fergana Fault

text: is the longest of these structures. Active deformation in the Tian Shan is the result of compressional stresses generated at the Indo-Asia collisional zone, where the Himalayas formed and continue to grow. Active deformation is observed in the Tian Shan, which is within Asia’s continental interior, because Asia is not as internally rigid as the continental crust is expected to be.

answers: NDQ_003351

answers: compressional

answers: NDQ_003352

answers: compresses

answers: NDQ_003353

answers: compressional stresses

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: Thrust fault

answers: NDQ_003356

answers: grow

answers: NDQ_003357

answers: Thrust faulting is the predominant style of what?

answers: NDQ_003358

answers: Fault

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: major tectonic event

answers: NDQ_003362

answers: the San Andreas fault is the longest of these structures

answers: NDQ_003363

answers: Indo-Asia collision

answers: NDQ_003371

answers: What type of faulting is the predominant style of Cenozoic deformation in the Tian Shan?

answers: NDQ_003373

answers: Why is Asia not as internally rigid as the continental crust is expected to be

answers: NDQ_003376

answers: Which of the following is not a type of terrain: basin-and-range or active deformation?

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What type of stress is generated at the Indo-Asia collisional zone?

answers: NDQ_003382

answers: Which of the following is not a type of plate: Indo-Asia collisional zone, Himalayas, or convergent plates?

answers: NDQ_003383

answers: Which of the following is not a type of deformation: Thrust faulting, strike slip faults, or thrust systems?

answers: NDQ_003384

answers: What is the longest of these structures?

answers: NDQ_003385

answers: what is the longest of these structures

answers: NDQ_003386

answers: Which of the following is not a cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not caused by compressional stresses?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike slip faults, thrust faults, or compressional stresses?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: strike slip faults

answers: NDQ_003391

answers: wedge-shaped block

answers: NDQ_003392

answers: Thrust faulting

answers: NDQ_003393

answers: wedge-shaped block

answers: NDQ_003394

answers: crosscut

answers: NDQ_003395

answers: Dextral NW-SE trending strike slip faults

answers: NDQ_003396

answers: Strike slip faults

answers: NDQ_003351

answers: Thrust faulting

answers: NDQ_003352

answers: grow.

answers: NDQ_003353

answers: deformation

answers: NDQ_003354

answers: Active deformation is observed in the Tian Shan,

answers: NDQ_003355

answers: Thrust faulting

answers: NDQ_003356

answers: Thrust faulting

answers: NDQ_003357

answers: strike slip faults

answers: NDQ_003358

answers: Thrust faulting

answers: NDQ_003359

answers: Thrust faulting

answers: NDQ_003360

answers: Thrust faulting

answers: NDQ_003362

answers: The collision of India with Asia is the latest major tectonic event

answers: NDQ_003363

answers: Indo-Asia collisional zone,

answers: NDQ_003371

answers: Thrust faulting

answers: NDQ_003373

answers: Indo-Asia collisional zone,

answers: NDQ_003376

answers: compressional stresses generated at the Indo-Asia collisional zone,

answers: NDQ_003378

answers: slip faults

answers: NDQ_003379

answers: NW-SE trending strike slip faults

answers: NDQ_003380

answers: compressional stresses

answers: NDQ_003381

answers: compressional stresses

answers: NDQ_003382

answers: compressional stresses generated at the Indo-Asia collisional zone,

answers: NDQ_003383

answers: compressional stresses

answers: NDQ_003384

answers: Thrust faulting

answers: NDQ_003385

answers: Thrust faulting

answers: NDQ_003386

answers: Thrust faulting

answers: NDQ_003387

answers: compressional stresses

answers: NDQ_003388

answers: Dextral NW-SE trending strike slip faults

answers: NDQ_003389

answers: compressional stresses

answers: NDQ_003390

answers: Talas-Fergana Fault

answers: NDQ_003391

answers: Thrust faulting

answers: NDQ_003392

answers: Thrust faulting

answers: NDQ_003393

answers: Thrust faulting

answers: NDQ_003394

answers: Dextral NW-SE trending strike slip faults

answers: NDQ_003395

answers: Dextral NW-SE trending strike slip faults

answers: NDQ_003396

answers: strike slip faults

text: Sites such as the Wopmay Orogen provide evidence for early and ongoing plate tectonics. Traces of old oceanic crust, island arcs, and colliding continents indicate that the same forces at work today have been at work in the early Proterozoic and probably earlier. Alignments of magnetic particles in rocks demonstrate that continents were drifting across the surface of the Earth relative to the magnetic poles then as now, and that the ocean floor was rifting and subducting, all at least 1.5 billion years ago. This crust cycling is referred to as the supercontinent cycle.

text: Sites such as the Wopmay Orogen provide evidence for early and ongoing

text: plate tectonics

text: . Traces of old

text: oceanic crust

text: island arcs

text: , and

text: colliding continents

text: indicate that the same forces at work today have been at work in the early Proterozoic and probably earlier. Alignments of magnetic particles in rocks demonstrate that continents were drifting across the surface of the Earth relative to the magnetic poles then as now, and that the ocean floor was rifting and subducting, all at least 1.5 billion years ago. This crust cycling is referred to as the

text: supercontinent cycle

answers: NDQ_003351

answers: subducting

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: magnetic particles to align

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: arc

answers: NDQ_003356

answers: subduct

answers: NDQ_003357

answers: the ocean floor was rifting and subducting

answers: NDQ_003358

answers: arc

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: plates

answers: NDQ_003362

answers: continents were drifting across the surface of the Earth

answers: NDQ_003363

answers: Wopmay Orogen

answers: NDQ_003371

answers: What is a thrust fault?

answers: NDQ_003373

answers: what is the first group of forces mentioned?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What type of force applied to rock is a stress?

answers: NDQ_003381

answers: What type of rock deforms?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What type of fold is the Wopmay Orogen?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: plate tectonics

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: normal faults, island arcs, or colliding continents?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip faults, island arcs, or colliding continents?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: subducting

answers: NDQ_003391

answers: oceanic crust

answers: NDQ_003392

answers: rifting

answers: NDQ_003393

answers: island arcs

answers: NDQ_003394

answers: plate tectonics

answers: NDQ_003395

answers: rifting and subducting

answers: NDQ_003396

answers: rifting

answers: NDQ_003351

answers: oceanic crust,

answers: NDQ_003352

answers: magnetic particles

answers: NDQ_003353

answers: magnetic particles

answers: NDQ_003354

answers: Wopmay Orogen

answers: NDQ_003355

answers: arcs,

answers: NDQ_003356

answers: magnetic particles

answers: NDQ_003357

answers: magnetic poles

answers: NDQ_003358

answers: island arcs,

answers: NDQ_003359

answers: magnetic poles

answers: NDQ_003360

answers: plate tectonics.

answers: NDQ_003362

answers: early and ongoing plate tectonics.

answers: NDQ_003363

answers: Wopmay Orogen

answers: NDQ_003371

answers: Wopmay Orogen

answers: NDQ_003373

answers: Alignments of magnetic particles

answers: NDQ_003376

answers: island arcs, and colliding continents

answers: NDQ_003378

answers: plate tectonics.

answers: NDQ_003379

answers: magnetic poles

answers: NDQ_003380

answers: forces

answers: NDQ_003381

answers: oceanic crust,

answers: NDQ_003382

answers: oceanic crust,

answers: NDQ_003383

answers: magnetic particles

answers: NDQ_003384

answers: island arcs,

answers: NDQ_003385

answers: Wopmay Orogen

answers: NDQ_003386

answers: plate tectonics.

answers: NDQ_003387

answers: oceanic crust,

answers: NDQ_003388

answers: Wopmay Orogen

answers: NDQ_003389

answers: oceanic crust,

answers: NDQ_003390

answers: Wopmay Orogen

answers: NDQ_003391

answers: oceanic crust,

answers: NDQ_003392

answers: Wopmay Orogen

answers: NDQ_003393

answers: island arcs,

answers: NDQ_003394

answers: plate tectonics.

answers: NDQ_003395

answers: Wopmay Orogen

answers: NDQ_003396

answers: Wopmay Orogen

text: North of U.S. Route 250 west of Durbin, the same structural fold of the Earth's crust that forms Back Allegheny Mountain continues north as Shavers Mountain for an additional .

text: North of

text: U.S. Route 250

text: west of

text: Durbin

text: , the same structural fold of the Earth's crust that forms Back Allegheny Mountain continues north as

text: Shavers Mountain

text: for an additional .

answers: NDQ_003351

answers: lateral

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: a structural fold

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: structural fold

answers: NDQ_003356

answers: swell

answers: NDQ_003357

answers: back allegheny mountain is formed by

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: is pushed together

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: The San Andreas fault is located in the Pacific Ocean.

answers: NDQ_003363

answers: Earth's crust

answers: NDQ_003371

answers: What may be the reason for Shavers Mountain?

answers: NDQ_003373

answers: How would you describe the rock?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: no

answers: NDQ_003380

answers: How would you describe Shavers Mountain?

answers: NDQ_003381

answers: What will happen to Shavers Mountain?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: None of the above choices.

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: None of the above choices.

answers: NDQ_003388

answers: What type of faults do strike-slip faults result from?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: Shavers Mountain

answers: NDQ_003391

answers: NDQ_003392

answers: structural fold

answers: NDQ_003393

answers: NDQ_003394

answers: NDQ_003395

answers: NDQ_003396

answers: NDQ_003351

answers: Earth's crust

answers: NDQ_003352

answers: Back Allegheny Mountain

answers: NDQ_003353

answers: structural fold

answers: NDQ_003354

answers: Back Allegheny Mountain continues north as Shavers Mountain

answers: NDQ_003355

answers: structural fold

answers: NDQ_003356

answers: Back Allegheny Mountain

answers: NDQ_003357

answers: structural fold

answers: NDQ_003358

answers: structural fold

answers: NDQ_003359

answers: Earth's crust

answers: NDQ_003360

answers: structural fold of the Earth's crust

answers: NDQ_003362

answers: Back Allegheny Mountain continues north as Shavers Mountain for an additional.

answers: NDQ_003363

answers: Earth's crust

answers: NDQ_003371

answers: Back Allegheny Mountain

answers: NDQ_003373

answers: Back Allegheny Mountain

answers: NDQ_003376

answers: structural fold

answers: NDQ_003378

answers: North of U.S. Route 250

answers: NDQ_003379

answers: North of U.S. Route 250

answers: NDQ_003380

answers: Back Allegheny Mountain

answers: NDQ_003381

answers: Back Allegheny Mountain

answers: NDQ_003382

answers: North of U.S. Route 250

answers: NDQ_003383

answers: Earth's crust

answers: NDQ_003384

answers: fold

answers: NDQ_003385

answers: North of U.S. Route 250

answers: NDQ_003386

answers: structural fold

answers: NDQ_003387

answers: North of U.S. Route 250

answers: NDQ_003388

answers: North of U.S. Route 250

answers: NDQ_003389

answers: structural fold of the Earth's crust

answers: NDQ_003390

answers: Back Allegheny Mountain

answers: NDQ_003391

answers: Back Allegheny Mountain

answers: NDQ_003392

answers: Back Allegheny Mountain

answers: NDQ_003393

answers: Back Allegheny Mountain

answers: NDQ_003394

answers: North of U.S. Route 250

answers: NDQ_003395

answers: Back Allegheny Mountain

answers: NDQ_003396

answers: Back Allegheny Mountain

text: Flat slab subduction is characterized by a low subduction angle (<30 degrees to horizontal) beyond the seismogenic zone and a resumption of normal subduction far from the trench. A slab is slang for the subducting lower plate. Although, some would characterize flat slab subduction as any shallowly dipping lower plate as in western Mexico. Flat slab subduction is associated with the pinching out of the asthenosphere, an inland migration of arc magmatism (magmatic sweep), and an eventual cessation of arc magmatism. The coupling of the flat slab to the upper plate is thought to change the style of deformation occurring on the upper plate's surface and form basement-cored uplifts like the Rocky Mountains. The flat slab also may hydrate the lower continental lithosphere and be involved in the formation of economically important ore deposits. The failure of a flat slab is associated with ignimbritic volcanism and the reverse migration of arc volcanism. Multiple working hypotheses about the cause of flat slabs are subduction of thick, buoyant oceanic crust (15–20 km) and  trench rollback accompanying a rapidly overriding upper plate  and enhanced trench suction. The west coast of South America has two of the largest flat slab subduction zones. Flat slab subduction is occurring at 10% of subduction zones.

text: Flat slab

text: subduction

text: is characterized by a low

text: subduction

text: angle (<30 degrees to horizontal) beyond the

text: seismogenic zone

text: and a resumption of normal subduction far from the

text: trench

text: . A slab is slang for the subducting lower

text: plate

text: . Although, some would characterize flat slab

text: subduction

text: as any shallowly dipping lower

text: plate

text: as in western

text: Mexico

text: . Flat slab

text: subduction

text: is associated with the pinching out of the

text: asthenosphere

text: , an inland migration of arc

text: magmatism

text: (magmatic sweep), and an eventual cessation of arc

text: magmatism

text: . The coupling of the flat slab to the upper plate is thought to change the style of

text: deformation

text: occurring on the upper plate's surface and form basement-cored uplifts like the

text: Rocky Mountains

text: . The flat slab also may hydrate the lower continental lithosphere and be involved in the formation of economically important

text: ore

text: deposits. The failure of a flat slab is associated with

text: ignimbritic

text: volcanism and the reverse migration of arc volcanism. Multiple working hypotheses about the cause of flat slabs are subduction of thick, buoyant

text: oceanic crust

text: (15–20 km) and  trench rollback accompanying a rapidly overriding upper plate  and enhanced trench suction. The west coast of South America has two of the largest flat slab subduction zones. Flat slab subduction is occurring at 10% of subduction zones.

answers: NDQ_003351

answers: ignimbritic

answers: NDQ_003352

answers: deforms

answers: NDQ_003353

answers: deformation

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: trench

answers: NDQ_003356

answers: change the style of deformation

answers: NDQ_003357

answers: flat slab subduction is characterized by a low subduction angle

answers: NDQ_003358

answers: flat slab

answers: NDQ_003359

answers: subducts

answers: NDQ_003360

answers: flat slab subduction

answers: NDQ_003362

answers: Flat slab subduction is occurring at 10% of subduction zones.

answers: NDQ_003363

answers: Flat slab subduction

answers: NDQ_003371

answers: Which of the following is not a type of subduction zone: flat slab subduction or thrust fault?

answers: NDQ_003373

answers: What type of stresses is a deeply buried rock under?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What type of force applied to rock is a stress?

answers: NDQ_003381

answers: What type of rock deforms?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: What is the cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: normal faults or normal faults?

answers: NDQ_003388

answers: Which of the following is not a type of strike-slip fault: strike-slip, strike-slip, or strike-slip?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: trench rollback

answers: NDQ_003391

answers: slab

answers: NDQ_003392

answers: trench rollback

answers: NDQ_003393

answers: lithosphere

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: flat slab

answers: NDQ_003396

answers: Flat slab subduction

answers: NDQ_003351

answers: ignimbritic volcanism

answers: NDQ_003352

answers: basement-cored uplifts

answers: NDQ_003353

answers: deformation

answers: NDQ_003354

answers: Flat slab subduction

answers: NDQ_003355

answers: slab

answers: NDQ_003356

answers: basement-cored uplifts

answers: NDQ_003357

answers: subduction far from the trench.

answers: NDQ_003358

answers: slab

answers: NDQ_003359

answers: rapidly overriding upper plate and enhanced trench suction.

answers: NDQ_003360

answers: basement-cored

answers: NDQ_003362

answers: Flat slab subduction

answers: NDQ_003363

answers: basement-cored uplifts

answers: NDQ_003371

answers: Flat slab subduction

answers: NDQ_003373

answers: basement-cored uplifts like the Rocky Mountains.

answers: NDQ_003376

answers: Flat slab subduction

answers: NDQ_003378

answers: Flat slab subduction

answers: NDQ_003379

answers: horizontal)

answers: NDQ_003380

answers: deformation

answers: NDQ_003381

answers: basement-cored uplifts

answers: NDQ_003382

answers: arc magmatism

answers: NDQ_003383

answers: basement-cored uplifts like the Rocky Mountains.

answers: NDQ_003384

answers: arc magmatism

answers: NDQ_003385

answers: subduction zones.

answers: NDQ_003386

answers: Flat slab subduction

answers: NDQ_003387

answers: Flat slab subduction

answers: NDQ_003388

answers: Flat slab subduction

answers: NDQ_003389

answers: basement-cored uplifts

answers: NDQ_003390

answers: Flat slab subduction

answers: NDQ_003391

answers: Flat slab subduction

answers: NDQ_003392

answers: Flat slab subduction

answers: NDQ_003393

answers: Flat slab subduction

answers: NDQ_003394

answers: Flat slab subduction

answers: NDQ_003395

answers: Flat slab subduction

answers: NDQ_003396

answers: Flat slab subduction

text: In breed standards, the term fault does not imply that a dog with a fault cannot be a good companion; it is merely an indication that dogs with faults should not be chosen for breeding unless the dog has desirable qualities that outweigh the fault. Faults may be minor, such as a color the breed club has decided is undesirable, or the fault may be major, such as structural problems that would prevent the dog from doing the work for which it was bred. Fault is used to describe an aspect of appearance or temperament that is considered by the breed club to be detrimental to the breed type of the breed, and dogs with major faults will not finish a kennel club conformation championship.

text: In breed standards, the term fault does not imply that a dog with a fault cannot be a good companion; it is merely an indication that dogs with faults should not be chosen for breeding unless the dog has desirable qualities that outweigh the fault. Faults may be minor, such as a color the breed club has decided is undesirable, or the fault may be major, such as structural problems that would prevent the dog from doing the work for which it was bred. Fault is used to describe an aspect of appearance or temperament that is considered by the breed club to be detrimental to the

text: breed type

text: of the breed, and dogs with major faults will not finish a kennel club conformation

text: championship

answers: NDQ_003351

answers: structural problems

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: faults

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: crack

answers: NDQ_003357

answers: the breed club has decided is undesirable

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: faults

answers: NDQ_003362

answers: that a dog with a fault cannot be a good companion

answers: NDQ_003363

answers: faults

answers: NDQ_003371

answers: unanswerable

answers: NDQ_003373

answers: compressive stresses

answers: NDQ_003376

answers: basin-and-range

answers: NDQ_003378

answers: Faults

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: unanswerable

answers: NDQ_003381

answers: how does rock deform?

answers: NDQ_003382

answers: Fault

answers: NDQ_003383

answers: structural problems

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: Fault zone

answers: NDQ_003386

answers: faults

answers: NDQ_003387

answers: structural problems

answers: NDQ_003388

answers: structural problems

answers: NDQ_003389

answers: Fault

answers: NDQ_003390

answers: structural problems

answers: NDQ_003391

answers: dip-slip fault

answers: NDQ_003392

answers: structural problems

answers: NDQ_003393

answers: Fault

answers: NDQ_003394

answers: structural problems

answers: NDQ_003395

answers: structural problems

answers: NDQ_003396

answers: a color the breed club has decided is undesirable

answers: NDQ_003351

answers: structural problems

answers: NDQ_003352

answers: structural problems

answers: NDQ_003353

answers: structural problems

answers: NDQ_003354

answers: In breed standards,

answers: NDQ_003355

answers: structural problems

answers: NDQ_003356

answers: structural problems

answers: NDQ_003357

answers: a color the breed club has decided is undesirable,

answers: NDQ_003358

answers: structural problems

answers: NDQ_003359

answers: structural problems

answers: NDQ_003360

answers: structural problems

answers: NDQ_003362

answers: a dog with a fault cannot be a good companion;

answers: NDQ_003363

answers: structural problems

answers: NDQ_003371

answers: In breed standards,

answers: NDQ_003373

answers: structural problems

answers: NDQ_003376

answers: structural problems

answers: NDQ_003378

answers: fault

answers: NDQ_003379

answers: major, such as structural problems

answers: NDQ_003380

answers: fault

answers: NDQ_003381

answers: structural problems

answers: NDQ_003382

answers: structural problems

answers: NDQ_003383

answers: structural problems

answers: NDQ_003384

answers: In breed standards,

answers: NDQ_003385

answers: Fault

answers: NDQ_003386

answers: Faults

answers: NDQ_003387

answers: structural problems

answers: NDQ_003388

answers: structural problems

answers: NDQ_003389

answers: In breed standards,

answers: NDQ_003390

answers: structural problems

answers: NDQ_003391

answers: structural problems

answers: NDQ_003392

answers: structural problems

answers: NDQ_003393

answers: structural problems

answers: NDQ_003394

answers: structural problems

answers: NDQ_003395

answers: structural problems

answers: NDQ_003396

answers: structural problems

text: The shape of the flat slab is constrained through earthquakes within the subducting slab and the interface between the upper plate and the subducting slab. Flat slab zones along the Andean margin release 3-5 times more energy through upper plate earthquakes than adjacent, more steeply dipping subduction zones. Upper plate earthquake focal mechanisms indicate that stress is aligned parallel with motion of the plate, and that stress is transmitted high into the upper plate from the lower. The reason for this enhanced seismicity is more effective coupling of the upper and lower plates. In normal subduction zones the coupling interface, the area in which the two plates are in close proximity, between the two plates is ~100–200 km long, but in flat slab subduction zones the coupling interface is much longer, 400–500 km. Although the lower lithosphere of the upper deforms plastically, numerical modeling has shown stress can be transmitted to crustal regions which behave in a brittle fashion. Along the subducting plate seismicity is more variable, especially intermediate-depth earthquakes. The variability may be controlled by the thickness of the crust and how efficiently it can release water. Thick crust that is not as deeply fractured by trench rise normal faulting may not dehydrate rapidly enough to induce intermediate-depth earthquakes. The Peruvian flat slab lacks significant intermediate-depth earthquakes and is associated with the subduction of the ~17 km thick Nazca Ridge.

text: The shape of the flat slab is constrained through

text: earthquake

text: s within the subducting slab and the interface between the upper plate and the subducting slab. Flat slab zones along the Andean margin release 3-5 times more energy through upper plate earthquakes than adjacent, more steeply dipping subduction zones. Upper plate earthquake focal mechanisms indicate that stress is aligned parallel with motion of the plate, and that stress is transmitted high into the upper plate from the lower. The reason for this enhanced seismicity is more effective coupling of the upper and lower plates. In normal subduction zones the coupling interface, the area in which the two plates are in close proximity, between the two plates is ~100–200 km long, but in flat slab subduction zones the coupling interface is much longer, 400–500 km. Although the lower lithosphere of the upper deforms plastically, numerical modeling has shown stress can be transmitted to crustal regions which behave in a brittle fashion. Along the subducting plate seismicity is more variable, especially intermediate-depth earthquakes. The variability may be controlled by the thickness of the crust and how efficiently it can release water. Thick crust that is not as deeply fractured by trench rise

text: normal fault

text: ing may not dehydrate rapidly enough to induce intermediate-depth earthquakes. The Peruvian flat slab lacks significant intermediate-depth earthquakes and is associated with the subduction of the ~17 km thick Nazca Ridge.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: is more likely to deform

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: slope

answers: NDQ_003356

answers: brittle

answers: NDQ_003357

answers: the area in which the two plates are in close proximity, between the two plates is  100–200 km long

answers: NDQ_003358

answers: flat slab

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: subduction plates

answers: NDQ_003362

answers: Thick crust that is not as deeply fractured by trench rise normal faulting may not dehydrate rapidly enough to induce intermediate-depth earthquakes

answers: NDQ_003363

answers: Andean margin

answers: NDQ_003371

answers: What type of faulting may not dehydrate rapidly enough to induce intermediate-depth earthquakes

answers: NDQ_003373

answers: What is the reason for this enhanced seismicity?

answers: NDQ_003376

answers: What type of terrain is caused by compressive forces?

answers: NDQ_003378

answers: What is the area in which the two plates are in close proximity?

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What is the reason for this enhanced seismicity?

answers: NDQ_003381

answers: What type of rock does the flat slab deform?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the reason for this enhanced seismicity?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is the term for an area where faults are clustered?

answers: NDQ_003386

answers: What is the cause of earthquakes?

answers: NDQ_003387

answers: What type of stress is transmitted high into the upper plate from the lower?

answers: NDQ_003388

answers: What is the reason for this enhanced seismicity is more effective coupling of the upper and lower plates

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: trench rise

answers: NDQ_003391

answers: flat slab

answers: NDQ_003392

answers: trench rise

answers: NDQ_003393

answers: flat slab

answers: NDQ_003394

answers: steeply dipping

answers: NDQ_003395

answers: normal faulting

answers: NDQ_003396

answers: trench rise

answers: NDQ_003351

answers: intermediate-depth earthquakes.

answers: NDQ_003352

answers: brittle

answers: NDQ_003353

answers: brittle fashion.

answers: NDQ_003354

answers: <unk>17 km thick Nazca Ridge.

answers: NDQ_003355

answers: steeply dipping subduction zones.

answers: NDQ_003356

answers: brittle fashion.

answers: NDQ_003357

answers: <unk>100–200 km long,

answers: NDQ_003358

answers: trench rise normal faulting

answers: NDQ_003359

answers: trench rise

answers: NDQ_003360

answers: upper plate earthquakes than adjacent, more steeply dipping subduction zones.

answers: NDQ_003362

answers: intermediate-depth earthquakes.

answers: NDQ_003363

answers: subduction zones.

answers: NDQ_003371

answers: Thick crust

answers: NDQ_003373

answers: crustal regions which behave in a brittle fashion.

answers: NDQ_003376

answers: The shape of the flat slab is constrained through earthquakes

answers: NDQ_003378

answers: stress

answers: NDQ_003379

answers: steeply

answers: NDQ_003380

answers: stress

answers: NDQ_003381

answers: plastically,

answers: NDQ_003382

answers: stress is transmitted high into the upper plate from the lower.

answers: NDQ_003383

answers: stress is transmitted high into the upper plate from the lower.

answers: NDQ_003384

answers: <unk>17 km thick Nazca Ridge.

answers: NDQ_003385

answers: coupling interface, the area in which the two plates are in close proximity,

answers: NDQ_003386

answers: stress is aligned parallel with motion of the plate,

answers: NDQ_003387

answers: Thick crust

answers: NDQ_003388

answers: stress is transmitted high into the upper plate from the lower.

answers: NDQ_003389

answers: earthquakes

answers: NDQ_003390

answers: trench rise normal faulting

answers: NDQ_003391

answers: flat slab

answers: NDQ_003392

answers: trench rise

answers: NDQ_003393

answers: flat slab

answers: NDQ_003394

answers: steeply dipping subduction zones.

answers: NDQ_003395

answers: trench rise normal faulting

answers: NDQ_003396

answers: steeply dipping subduction zones.

text: The typing speed can be increased gradually and speeds of 60 WPM or higher can be achieved. The rate of speed increase varies between individuals. Many websites and software products are available to learn touch typing and many of these are free. Learning touch typing can be stressful both to the fingers as well as the mind in the beginning, but once it is learned to a decent level, it exerts minimal stress on the fingers. For individuals with past typing experience, learning to touch type is particularly difficult due to motivational reasons: the initial performance level in touch typing is far lower than in visually guided typing; therefore it does not initially seem worthwhile to study touch typing.

text: The typing speed can be increased gradually and speeds of 60 WPM or higher can be achieved. The rate of speed increase varies between individuals. Many websites and software products are available to learn touch typing and many of these are free. Learning touch typing can be stressful both to the fingers as well as the mind in the beginning, but once it is learned to a decent level, it exerts minimal stress on the fingers. For individuals with past typing experience, learning to touch type is particularly difficult due to motivational reasons: the initial performance level in touch typing is far lower than in visually guided typing; therefore it does not initially seem worthwhile to study touch typing.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: tends to crack

answers: NDQ_003353

answers: voids to form

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: if a person has a normal fault, what would happen to them?

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: it exerts minimal stress on the fingers

answers: NDQ_003363

answers: the same time

answers: NDQ_003371

answers: Which of the following is not an example of a thrust fault?

answers: NDQ_003373

answers: How would you describe the stress?

answers: NDQ_003376

answers: basin-and-range

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: vertical

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: Which of the following is not an example of confining stress?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: Which of the following is not a type of fold?

answers: NDQ_003385

answers: what is the first word in the passage?

answers: NDQ_003386

answers: movement of rock at faults

answers: NDQ_003387

answers: Which of the following is true of normal faults?

answers: NDQ_003388

answers: Which of the following is not a type of stress?

answers: NDQ_003389

answers: mountain ranges

answers: NDQ_003390

answers: The hanging wall drops down relative to the footwall

answers: NDQ_003391

answers: dip-slip fault

answers: NDQ_003392

answers: The hanging wall pushes up relative to the footwall

answers: NDQ_003393

answers: dip-slip fault

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: a vertical fault plane

answers: NDQ_003396

answers: NDQ_003351

answers: Learning touch typing

answers: NDQ_003352

answers: Learning touch typing

answers: NDQ_003353

answers: Learning touch typing

answers: NDQ_003354

answers: The typing speed can be increased gradually and speeds of 60 WPM

answers: NDQ_003355

answers: The typing speed can be increased gradually

answers: NDQ_003356

answers: Many websites and software products are available to learn touch typing

answers: NDQ_003357

answers: visually guided typing;

answers: NDQ_003358

answers: The typing speed can be increased gradually and speeds of 60 WPM

answers: NDQ_003359

answers: The typing speed can be increased gradually and speeds of 60 WPM

answers: NDQ_003360

answers: The typing speed

answers: NDQ_003362

answers: The typing speed can be increased gradually and speeds of 60 WPM

answers: NDQ_003363

answers: The typing speed can be increased gradually and speeds of 60 WPM

answers: NDQ_003371

answers: The typing speed can be increased gradually and speeds of 60 WPM

answers: NDQ_003373

answers: Learning touch typing

answers: NDQ_003376

answers: Many websites and software products are available to learn touch typing

answers: NDQ_003378

answers: The typing speed can be increased gradually and speeds of 60 WPM

answers: NDQ_003379

answers: free.

answers: NDQ_003380

answers: stress

answers: NDQ_003381

answers: Learning touch typing

answers: NDQ_003382

answers: Learning touch typing

answers: NDQ_003383

answers: Learning touch typing

answers: NDQ_003384

answers: The typing speed can be increased gradually and speeds of 60 WPM

answers: NDQ_003385

answers: speeds of 60 WPM

answers: NDQ_003386

answers: The typing speed can be increased gradually and speeds of 60 WPM

answers: NDQ_003387

answers: Learning touch typing

answers: NDQ_003388

answers: learning to touch type is particularly difficult due to motivational reasons:

answers: NDQ_003389

answers: The typing speed can be increased gradually and speeds of 60 WPM

answers: NDQ_003390

answers: The typing speed can be increased gradually and speeds of 60 WPM

answers: NDQ_003391

answers: The typing speed can be increased gradually and speeds of 60 WPM

answers: NDQ_003392

answers: The typing speed can be increased gradually

answers: NDQ_003393

answers: The typing speed can be increased gradually and speeds of 60 WPM

answers: NDQ_003394

answers: The typing speed can be increased gradually and speeds of 60 WPM

answers: NDQ_003395

answers: The typing speed can be increased gradually and speeds of 60 WPM

answers: NDQ_003396

answers: The typing speed can be increased gradually and speeds of 60 WPM

text: The Southern Uplands Fault (or occasionally Southern Upland Fault) is a fault in Scotland that runs from Girvan (or more specifically from the Rhins of Galloway) to Dunbar on the East coast. It marks the southern boundary of the Scottish Midland Valley and the northern margin of the Southern Uplands; indeed it is recognised as a boundary between these two terranes. Both sinistral and dextral strike-slip movement is recorded from parts of the fault as are down-north and down-south normal movements suggestive of a complex history.

text: The Southern Uplands Fault (or occasionally Southern Upland Fault) is a

text: fault

text: in

text: Scotland

text: that runs from

text: Girvan

text: (or more specifically from the

text: Rhins of Galloway

text: ) to

text: Dunbar

text: on the East coast. It marks the southern boundary of the Scottish

text: Midland Valley

text: and the northern margin of the

text: Southern Uplands

text: ; indeed it is recognised as a boundary between these two

text: terrane

text: s. Both

text: sinistral

text: and

text: dextral

text: strike-slip

text: movement is recorded from parts of the fault as are down-north and down-south

text: normal movements

text: suggestive of a complex history.

answers: NDQ_003351

answers: strike-slip

answers: NDQ_003352

answers: is likely to move

answers: NDQ_003353

answers: strike-slip movement

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: down-south

answers: NDQ_003356

answers: dextral

answers: NDQ_003357

answers: down-south normal movements suggestive of a complex history

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: strike-slip

answers: NDQ_003360

answers: Southern Uplands Fault

answers: NDQ_003362

answers: The Southern Uplands Fault (or occasionally Southern Upland Fault) is a fault in Scotland

answers: NDQ_003363

answers: Southern Uplands Fault

answers: NDQ_003371

answers: What type of movement is recorded from parts of the fault?

answers: NDQ_003373

answers: What is the Southern Uplands Fault?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: dextral

answers: NDQ_003380

answers: What is the Southern Uplands Fault?

answers: NDQ_003381

answers: What type of movement is recorded from parts of the fault?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the Southern Uplands Fault?

answers: NDQ_003384

answers: What type of fold is the Southern Uplands Fault?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: yes

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: strike-slip movement or normal faults?

answers: NDQ_003388

answers: What type of movement is recorded from parts of the fault?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: sinistral

answers: NDQ_003391

answers: Southern Uplands Fault

answers: NDQ_003392

answers: sinistral

answers: NDQ_003393

answers: terranes

answers: NDQ_003394

answers: sinistral

answers: NDQ_003395

answers: sinistral and dextral strike-slip movement

answers: NDQ_003396

answers: sinistral

answers: NDQ_003351

answers: sinistral and dextral strike-slip

answers: NDQ_003352

answers: strike-slip

answers: NDQ_003353

answers: strike-slip movement

answers: NDQ_003354

answers: The Southern Uplands Fault

answers: NDQ_003355

answers: sinistral

answers: NDQ_003356

answers: strike-slip

answers: NDQ_003357

answers: down-north and down-south

answers: NDQ_003358

answers: dextral

answers: NDQ_003359

answers: fault

answers: NDQ_003360

answers: The Southern Uplands Fault

answers: NDQ_003362

answers: The Southern Uplands Fault

answers: NDQ_003363

answers: Southern Uplands Fault

answers: NDQ_003371

answers: The Southern Uplands Fault

answers: NDQ_003373

answers: The Southern Uplands Fault

answers: NDQ_003376

answers: The Southern Uplands Fault

answers: NDQ_003378

answers: strike-slip

answers: NDQ_003379

answers: sinistral and dextral

answers: NDQ_003380

answers: strike-slip

answers: NDQ_003381

answers: sinistral and dextral strike-slip movement

answers: NDQ_003382

answers: sinistral and dextral strike-slip

answers: NDQ_003383

answers: sinistral and dextral strike-slip

answers: NDQ_003384

answers: sinistral

answers: NDQ_003385

answers: The Southern Uplands Fault

answers: NDQ_003386

answers: strike-slip

answers: NDQ_003387

answers: down-north and down-south

answers: NDQ_003388

answers: sinistral and dextral

answers: NDQ_003389

answers: The Southern Uplands Fault

answers: NDQ_003390

answers: Southern Uplands Fault

answers: NDQ_003391

answers: sinistral and dextral

answers: NDQ_003392

answers: Southern Uplands Fault

answers: NDQ_003393

answers: sinistral and dextral

answers: NDQ_003394

answers: sinistral and dextral

answers: NDQ_003395

answers: sinistral

answers: NDQ_003396

answers: sinistral and dextral

text: Partly by analogy to what is known about the Moon, Earth is considered to have differentiated from an aggregate of planetesimals into its core, mantle and crust within about 100 million years of the formation of the planet, 4.6 billion years ago. The primordial crust was very thin and was probably recycled by much more vigorous plate tectonics and destroyed by significant asteroid impacts, which were much more common in the early stages of the solar system.

text: Partly by analogy to what is known about the Moon, Earth is considered to have differentiated from an aggregate of

text: planetesimals

text: into its core, mantle and crust within about 100 million years of the formation of the planet, 4.6 billion years ago. The

text: primordial

text: crust was very thin and was probably recycled by much more vigorous

text: plate tectonics

text: and destroyed by significant

text: asteroid

text: impacts, which were much more common in the early stages of the solar system.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: increases in thickness

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: plate

answers: NDQ_003356

answers: recycle

answers: NDQ_003357

answers: plate tectonics

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: plate tectonics

answers: NDQ_003362

answers: Earth is considered to have differentiated from an aggregate of planetesimals

answers: NDQ_003363

answers: 4.6 billion years ago

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: What is the best title for this passage?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What type of force applied to rock is a stress?

answers: NDQ_003381

answers: What is the primary cause of rock deforms?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: what is the primordial crust

answers: NDQ_003386

answers: plate tectonics

answers: NDQ_003387

answers: Which of the following is not a type of plate tectonics?

answers: NDQ_003388

answers: unanswerable

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: tectonics

answers: NDQ_003391

answers: mantle

answers: NDQ_003392

answers: plate tectonics

answers: NDQ_003393

answers: mantle

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: tectonics

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: asteroid impacts,

answers: NDQ_003352

answers: destroyed by significant asteroid impacts,

answers: NDQ_003353

answers: plate tectonics

answers: NDQ_003354

answers: asteroid impacts,

answers: NDQ_003355

answers: plate tectonics

answers: NDQ_003356

answers: destroyed by significant asteroid impacts,

answers: NDQ_003357

answers: asteroid impacts,

answers: NDQ_003358

answers: plate tectonics

answers: NDQ_003359

answers: asteroid impacts,

answers: NDQ_003360

answers: plate tectonics

answers: NDQ_003362

answers: destroyed by significant asteroid impacts,

answers: NDQ_003363

answers: 4.6 billion years ago.

answers: NDQ_003371

answers: plate tectonics

answers: NDQ_003373

answers: plate tectonics

answers: NDQ_003376

answers: plate tectonics

answers: NDQ_003378

answers: plate tectonics

answers: NDQ_003379

answers: 4.6 billion years ago.

answers: NDQ_003380

answers: asteroid impacts,

answers: NDQ_003381

answers: plate tectonics

answers: NDQ_003382

answers: asteroid impacts,

answers: NDQ_003383

answers: plate tectonics

answers: NDQ_003384

answers: plate tectonics

answers: NDQ_003385

answers: 4.6

answers: NDQ_003386

answers: plate tectonics

answers: NDQ_003387

answers: plate tectonics

answers: NDQ_003388

answers: plate tectonics

answers: NDQ_003389

answers: plate tectonics

answers: NDQ_003390

answers: plate tectonics

answers: NDQ_003391

answers: core, mantle and crust

answers: NDQ_003392

answers: plate tectonics

answers: NDQ_003393

answers: core, mantle and crust

answers: NDQ_003394

answers: plate tectonics

answers: NDQ_003395

answers: plate tectonics

answers: NDQ_003396

answers: plate tectonics

text: The inhomogeneity and structural complexity of continental crust causes faults to deviate from a straight course and frequently causes bends or step-overs in fault paths.  Bends and step-overs of adjacent faults become favorable locations for extensional and compressional stress or transtension and transpression stress, if the shear motion is oblique.  Pull-apart basins form in extensional to transtensional environments along fault bends or between two adjacent left-lateral faults or two right-lateral faults.  The step-over or bend in the fault must be the same direction as sense of motion on the fault otherwise the area will be subject to transpression.

text: The inhomogeneity and structural complexity of

text: continental crust

text: causes faults to deviate from a straight course and frequently causes bends or step-overs in fault paths.  Bends and step-overs of adjacent faults become favorable locations for extensional and compressional stress or

text: transtension

text: and

text: transpression

text: stress, if the

text: shear

text: motion is oblique.  Pull-apart basins form in extensional to transtensional environments along fault bends or between two adjacent left-lateral faults or two right-lateral faults.  The step-over or bend in the fault must be the same direction as sense of motion on the fault otherwise the area will be subject to transpression.

answers: NDQ_003351

answers: transtension

answers: NDQ_003352

answers: bends

answers: NDQ_003353

answers: pull-apart

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: step-over

answers: NDQ_003356

answers: bend

answers: NDQ_003357

answers: Bends and step-overs of adjacent faults become favorable locations for

answers: NDQ_003358

answers: unanswerable

answers: NDQ_003359

answers: bends or step-overs in fault paths

answers: NDQ_003360

answers: faults

answers: NDQ_003362

answers: The step-over or bend in the fault must be the same direction as sense of motion on the fault

answers: NDQ_003363

answers: fault bends

answers: NDQ_003371

answers: Which of the following is not a type of stress: extensional and compressional or transtension and transpression?

answers: NDQ_003373

answers: Why would a rock be deeply buried?

answers: NDQ_003376

answers: pull-apart basins

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: Which of the following is not a type of stress: compressional, transtension or transpression?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: Bends and step-overs of adjacent faults become favorable locations

answers: NDQ_003384

answers: What is the opposite of oblique?

answers: NDQ_003385

answers: what is the first word in the passage?

answers: NDQ_003386

answers: What is the cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not caused by compression stress?

answers: NDQ_003388

answers: Which of the following is not a type of strike-slip fault?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: oblique

answers: NDQ_003391

answers: oblique

answers: NDQ_003392

answers: transtensional

answers: NDQ_003393

answers: pull-apart

answers: NDQ_003394

answers: oblique

answers: NDQ_003395

answers: left-lateral faults

answers: NDQ_003396

answers: oblique

answers: NDQ_003351

answers: extensional and compressional

answers: NDQ_003352

answers: bends or step-overs

answers: NDQ_003353

answers: bends or step-overs in fault paths.

answers: NDQ_003354

answers: The inhomogeneity

answers: NDQ_003355

answers: step-overs

answers: NDQ_003356

answers: bends or step-overs

answers: NDQ_003357

answers: the same direction as sense of motion on the fault

answers: NDQ_003358

answers: Pull-apart basins

answers: NDQ_003359

answers: same direction as sense of motion

answers: NDQ_003360

answers: faults

answers: NDQ_003362

answers: straight course

answers: NDQ_003363

answers: faults to deviate from a straight course

answers: NDQ_003371

answers: bends or step-overs in fault paths.

answers: NDQ_003373

answers: Bends and step-overs of adjacent faults

answers: NDQ_003376

answers: Pull-apart basins

answers: NDQ_003378

answers: shear motion

answers: NDQ_003379

answers: transpression.

answers: NDQ_003380

answers: extensional and compressional stress

answers: NDQ_003381

answers: transpression.

answers: NDQ_003382

answers: transpression.

answers: NDQ_003383

answers: extensional and compressional stress

answers: NDQ_003384

answers: oblique.

answers: NDQ_003385

answers: Bends and step-overs of adjacent faults

answers: NDQ_003386

answers: The inhomogeneity and structural complexity of continental crust

answers: NDQ_003387

answers: transpression.

answers: NDQ_003388

answers: oblique.

answers: NDQ_003389

answers: The inhomogeneity and structural complexity of continental crust

answers: NDQ_003390

answers: Pull-apart basins

answers: NDQ_003391

answers: Pull-apart basins

answers: NDQ_003392

answers: Pull-apart basins

answers: NDQ_003393

answers: Pull-apart basins

answers: NDQ_003394

answers: oblique.

answers: NDQ_003395

answers: left-lateral faults or two right-lateral faults.

answers: NDQ_003396

answers: left-lateral faults or two right-lateral faults.

text: Hardware stress testing and stability are subjective and may vary according to how the system will be used. A stress test for a system running 24/7 or that will perform error sensitive tasks such as distributed computing or 'folding' projects may differ from one that needs to be able to run a single game with reasonably reliability. For example, a comprehensive guide on overclocking Sandy Bridge found that:

text: Hardware stress testing and stability are subjective and may vary according to how the system will be used. A stress test for a system running 24/7 or that will perform error sensitive tasks such as

text: distributed computing

text: or

text: 'folding' projects

text: may differ from one that needs to be able to run a single game with reasonably reliability. For example, a comprehensive guide on overclocking

text: Sandy Bridge

text: found that:

answers: NDQ_003351

answers: earthquakes

answers: NDQ_003352

answers: cracks

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation is a geologic formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: Sandy Bridge would be able to run a game with reasonably reliability

answers: NDQ_003358

answers: rockfall

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: a comprehensive guide on overclocking Sandy Bridge found that:

answers: NDQ_003363

answers: the same time

answers: NDQ_003371

answers: context:

answers: NDQ_003373

answers: a rock that is deeply buried is under compressive stresses

answers: NDQ_003376

answers: basin-and-range

answers: NDQ_003378

answers: The amount the ground moves in an earthquake is called slip

answers: NDQ_003379

answers: The dip of the fault plane is horizontal.

answers: NDQ_003380

answers: context: What is a stress?

answers: NDQ_003381

answers: constricting stress

answers: NDQ_003382

answers: convernent plates

answers: NDQ_003383

answers: no

answers: NDQ_003384

answers: description

answers: NDQ_003385

answers: fault zone

answers: NDQ_003386

answers: context:

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: The answer: shear stress.

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: a hanging wall

answers: NDQ_003391

answers: crater

answers: NDQ_003392

answers: 'folding'

answers: NDQ_003393

answers: igneous rock

answers: NDQ_003394

answers: NDQ_003395

answers: a vertical fault plane

answers: NDQ_003396

answers: NDQ_003351

answers: overclocking

answers: NDQ_003352

answers: overclocking Sandy Bridge

answers: NDQ_003353

answers: overclocking Sandy Bridge

answers: NDQ_003354

answers: overclocking Sandy Bridge

answers: NDQ_003355

answers: 'folding'

answers: NDQ_003356

answers: overclocking Sandy Bridge

answers: NDQ_003357

answers: 24/7

answers: NDQ_003358

answers: stress test

answers: NDQ_003359

answers: subjective and may vary according to how the system will be used.

answers: NDQ_003360

answers: Hardware stress testing

answers: NDQ_003362

answers: overclocking Sandy Bridge

answers: NDQ_003363

answers: overclocking Sandy Bridge

answers: NDQ_003371

answers: overclocking Sandy Bridge

answers: NDQ_003373

answers: overclocking Sandy Bridge

answers: NDQ_003376

answers: overclocking Sandy Bridge

answers: NDQ_003378

answers: overclocking Sandy Bridge

answers: NDQ_003379

answers: 24/7

answers: NDQ_003380

answers: stress test

answers: NDQ_003381

answers: overclocking Sandy Bridge

answers: NDQ_003382

answers: overclocking Sandy Bridge

answers: NDQ_003383

answers: overclocking Sandy Bridge

answers: NDQ_003384

answers: 'folding' projects

answers: NDQ_003385

answers: 24/7 or that will perform error sensitive tasks

answers: NDQ_003386

answers: overclocking Sandy Bridge

answers: NDQ_003387

answers: 'folding' projects

answers: NDQ_003388

answers: overclocking Sandy Bridge

answers: NDQ_003389

answers: stress test for a system running 24/7 or that will perform error sensitive tasks

answers: NDQ_003390

answers: overclocking Sandy Bridge

answers: NDQ_003391

answers: Sandy Bridge

answers: NDQ_003392

answers: overclocking Sandy Bridge

answers: NDQ_003393

answers: Sandy Bridge

answers: NDQ_003394

answers: overclocking Sandy Bridge

answers: NDQ_003395

answers: Sandy Bridge

answers: NDQ_003396

answers: Sandy Bridge

text: North of the DDMFZ (and west of the SCF) is the Chuckanut Formation (part of the "Northwest Cascade System" of rocks shown in green on the map), an Eocene sedimentary formation which formed adjacent to the Swauk, Roslyn and other formations (also in green) south of Mount Stuart; their wide separation is attributed to right-lateral strike-slip movement along the SCF. That the northern part of the DDMFZ shows left-lateral strike-slip movement is not the inconsistency it may initially seem – think of the motion on either side of an arrowhead.

text: North of the DDMFZ (and west of the SCF) is the

text: Chuckanut Formation

text: (part of the "Northwest Cascade System" of rocks shown in green on the map), an

text: Eocene

text: sedimentary formation which formed adjacent to the Swauk, Roslyn and other formations (also in green) south of

text: Mount Stuart

text: ; their wide separation is attributed to right-lateral strike-slip movement along the SCF. That the northern part of the DDMFZ shows left-lateral strike-slip movement is not the inconsistency it may initially seem – think of the motion on either side of an arrowhead.

answers: NDQ_003351

answers: strike-slip

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: strike-slip movement

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: arrowhead

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: left-lateral strike-slip movement is the opposite of what?

answers: NDQ_003358

answers: arrowhead

answers: NDQ_003359

answers: slips away

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: left-lateral strike-slip movement

answers: NDQ_003363

answers: Eocene

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: What type of stresses is the Chuckanut Formation under?

answers: NDQ_003376

answers: What type of forces is the terrain known as basin-and-range?

answers: NDQ_003378

answers: what is the first formation mentioned?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What type of stress does the Chuckanut Formation experience?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: what is the first formation mentioned?

answers: NDQ_003386

answers: What type of movement is the cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: strike-slip movement or normal faults?

answers: NDQ_003388

answers: What type of movement is attributed to the wide separation?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: strike-slip

answers: NDQ_003391

answers: DDMFZ

answers: NDQ_003392

answers: strike-slip

answers: NDQ_003393

answers: DDMFZ

answers: NDQ_003394

answers: left-lateral

answers: NDQ_003395

answers: strike-slip movement

answers: NDQ_003396

answers: strike-slip

answers: NDQ_003351

answers: right-lateral strike-slip

answers: NDQ_003352

answers: arrowhead.

answers: NDQ_003353

answers: strike-slip movement

answers: NDQ_003354

answers: Chuckanut Formation

answers: NDQ_003355

answers: arrowhead.

answers: NDQ_003356

answers: arrowhead.

answers: NDQ_003357

answers: right-lateral strike-slip movement

answers: NDQ_003358

answers: arrowhead.

answers: NDQ_003359

answers: strike-slip

answers: NDQ_003360

answers: strike-slip movement

answers: NDQ_003362

answers: arrowhead.

answers: NDQ_003363

answers: strike-slip movement along the SCF.

answers: NDQ_003371

answers: right-lateral strike-slip movement

answers: NDQ_003373

answers: arrowhead.

answers: NDQ_003376

answers: right-lateral strike-slip movement

answers: NDQ_003378

answers: strike-slip

answers: NDQ_003379

answers: left-lateral strike-slip movement

answers: NDQ_003380

answers: motion on either side of an arrowhead.

answers: NDQ_003381

answers: strike-slip movement

answers: NDQ_003382

answers: strike-slip

answers: NDQ_003383

answers: strike-slip movement

answers: NDQ_003384

answers: arrowhead.

answers: NDQ_003385

answers: DDMFZ

answers: NDQ_003386

answers: strike-slip

answers: NDQ_003387

answers: strike-slip movement

answers: NDQ_003388

answers: think of the motion on either side of an arrowhead.

answers: NDQ_003389

answers: strike-slip movement

answers: NDQ_003390

answers: strike-slip

answers: NDQ_003391

answers: arrowhead.

answers: NDQ_003392

answers: strike-slip

answers: NDQ_003393

answers: arrowhead.

answers: NDQ_003394

answers: left-lateral strike-slip movement

answers: NDQ_003395

answers: right-lateral strike-slip

answers: NDQ_003396

answers: left-lateral strike-slip

text: Iran suffers from frequent earthquakes, with minor quakes occurring almost daily. This earthquake occurred as a result of stresses generated by the Arabian plate moving northward against the Eurasian plate at approximately  per year. The Earth's crust deforms in response to the plate motion in a broad zone that spans the width of Iran and extends into Turkmenistan. Earthquakes occur as the result of reverse faulting and strike-slip faulting in the zone of deformation.

text: Iran

text: suffers from frequent earthquakes, with minor quakes occurring almost daily. This earthquake occurred as a result of stresses generated by the

text: Arabian plate

text: moving northward against the

text: Eurasian plate

text: at approximately  per year. The

text: Earth

text: 's crust deforms in response to the plate motion in a broad zone that spans the width of Iran and extends into

text: Turkmenistan

text: . Earthquakes occur as the result of

text: reverse

text: faulting and

text: strike-slip

text: faulting in the zone of deformation.

answers: NDQ_003351

answers: strike-slip

answers: NDQ_003352

answers: deforms

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: plate

answers: NDQ_003356

answers: quake

answers: NDQ_003357

answers: strike-slip faulting occurs in the zone of deformation.

answers: NDQ_003358

answers: quake

answers: NDQ_003359

answers: deforms

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: the Arabian plate moving northward against the Eurasian plate

answers: NDQ_003363

answers: Eurasian plate

answers: NDQ_003371

answers: Which of the following is not a type of fault: strike-slip faulting or strike-slip faulting?

answers: NDQ_003373

answers: How would you describe a rock that is deeply buried?

answers: NDQ_003376

answers: Which of the following is not caused by compressive forces: strike-slip faulting or reverse faulting?

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: How does the Earth's crust deform in response to the plate motion?

answers: NDQ_003381

answers: How does the Earth's crust deform in response to the plate motion?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock: strike-slip faulting or earthquakes?

answers: NDQ_003384

answers: Which of the following is not a type of fault: reverse faulting or strike-slip faulting?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: What is the cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: strike-slip faulting or normal faults?

answers: NDQ_003388

answers: Which of the following is not a type of fault: reverse faulting, strike-slip faulting, or shear stress?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: strike-slip

answers: NDQ_003391

answers: strike-slip

answers: NDQ_003392

answers: strike-slip

answers: NDQ_003393

answers: strike-slip

answers: NDQ_003394

answers: strike-slip

answers: NDQ_003395

answers: strike-slip

answers: NDQ_003396

answers: strike-slip faulting

answers: NDQ_003351

answers: reverse faulting and strike-slip faulting

answers: NDQ_003352

answers: deforms

answers: NDQ_003353

answers: The Earth's crust deforms

answers: NDQ_003354

answers: Iran suffers from frequent earthquakes,

answers: NDQ_003355

answers: reverse faulting

answers: NDQ_003356

answers: Earthquakes

answers: NDQ_003357

answers: strike-slip faulting

answers: NDQ_003358

answers: Earthquakes

answers: NDQ_003359

answers: reverse faulting and strike-slip faulting

answers: NDQ_003360

answers: Arabian plate moving northward against the Eurasian plate

answers: NDQ_003362

answers: Iran suffers from frequent earthquakes,

answers: NDQ_003363

answers: Arabian plate moving northward against the Eurasian plate

answers: NDQ_003371

answers: strike-slip faulting

answers: NDQ_003373

answers: Iran suffers from frequent earthquakes,

answers: NDQ_003376

answers: Arabian plate moving northward against the Eurasian plate

answers: NDQ_003378

answers: strike-slip faulting

answers: NDQ_003379

answers: strike-slip faulting

answers: NDQ_003380

answers: stresses

answers: NDQ_003381

answers: The Earth's crust deforms in response to the plate motion

answers: NDQ_003382

answers: Arabian plate moving northward against the Eurasian plate

answers: NDQ_003383

answers: stresses

answers: NDQ_003384

answers: Arabian plate moving northward against the Eurasian plate

answers: NDQ_003385

answers: zone of deformation.

answers: NDQ_003386

answers: reverse faulting and strike-slip faulting

answers: NDQ_003387

answers: reverse faulting and strike-slip faulting

answers: NDQ_003388

answers: reverse faulting and strike-slip faulting

answers: NDQ_003389

answers: reverse faulting and strike-slip faulting

answers: NDQ_003390

answers: strike-slip faulting

answers: NDQ_003391

answers: strike-slip faulting

answers: NDQ_003392

answers: strike-slip faulting

answers: NDQ_003393

answers: strike-slip faulting

answers: NDQ_003394

answers: strike-slip faulting

answers: NDQ_003395

answers: strike-slip faulting

answers: NDQ_003396

answers: strike-slip faulting

text: When the San Andreas Fault originally formed, tension on the North American Plate grew. The plate buckled and began uplifting similar to swelling in nearly all portions of the west. Numerous faults were created as a result; geologic blocks that rose and fell over and over again in patterns and in sequences. The extension of surface led to cracks which formed many independent faults. This is the creation of the Basin and Range Province. Sometimes these faults created a pathway, which molten rock could flow up to the surface creating cinder cone volcanoes. The Los Angeles Area has a few volcanoes that formed. Along Route 66 in Amboy, California is the extinct volcano Amboy Crater called that is estimated to be aged at 80,000 years. It's a relatively new speaking in geologic terms, but heavily eroded by wind. While driving along Interstate 40, lava fields are seen that can stretch for miles. Within Death Valley National Park another, much larger cinder cone volcano called Ubehebe Crater. It is extremely young, although many geologist dispute the numbers with some estimates as old as 10,000 years with recent ages such as 800 years. One thing is for sure, that this volcano is still very active and can erupt. Luckily, because of its location, will likely not effect many people. Within Orange County, lava flows and dikes can be seen in El Modena, California although no actual crater can be seen. Likely because either it has been totally eroded or it was formed in a small fissure, which would explain why it's so localized.

text: When the San Andreas Fault originally formed, tension on the North American Plate grew. The plate buckled and began uplifting similar to swelling in nearly all portions of the west. Numerous faults were created as a result; geologic blocks that rose and fell over and over again in patterns and in sequences. The extension of surface led to cracks which formed many independent faults. This is the creation of the

text: Basin and Range Province

text: . Sometimes these faults created a pathway, which molten rock could flow up to the surface creating

text: cinder cone

text: volcanoes. The Los Angeles Area has a few volcanoes that formed. Along

text: Route 66

text: in

text: Amboy, California

text: is the extinct volcano

text: Amboy Crater

text: called that is estimated to be aged at 80,000 years. It's a relatively new speaking in geologic terms, but heavily eroded by wind. While driving along

text: Interstate 40

text: , lava fields are seen that can stretch for miles. Within

text: Death Valley National Park

text: another, much larger cinder cone volcano called

text: Ubehebe Crater

text: . It is extremely young, although many geologist dispute the numbers with some estimates as old as 10,000 years with recent ages such as 800 years. One thing is for sure, that this volcano is still very active and can erupt. Luckily, because of its location, will likely not effect many people. Within Orange County,

text: lava flows

text: and

text: dikes

text: can be seen in

text: El Modena, California

text: although no actual crater can be seen. Likely because either it has been totally eroded or it was formed in a small fissure, which would explain why it's so localized.

answers: NDQ_003351

answers: independent faults

answers: NDQ_003352

answers: cracks

answers: NDQ_003353

answers: cracks

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fault

answers: NDQ_003356

answers: erupt

answers: NDQ_003357

answers: molten rock could flow up to the surface creating what?

answers: NDQ_003358

answers: unanswerable

answers: NDQ_003359

answers: cracks

answers: NDQ_003360

answers: San Andreas Fault?

answers: NDQ_003362

answers: lava flows and dikes can be seen

answers: NDQ_003363

answers: San Andreas Fault

answers: NDQ_003371

answers: Which of the following is not a volcano: Amboy Crater, Ubehebe Crater or Death Valley National Park?

answers: NDQ_003373

answers: Which of the following is not a type of stress?

answers: NDQ_003376

answers: Which of the following is not a type of fault: faults, faults, or faults?

answers: NDQ_003378

answers: Which of the following is not a type of volcano: cinder cone volcanoes or Ubehebe Crater?

answers: NDQ_003379

answers: What is the dip of the fault plane in a strike-slip fault?

answers: NDQ_003380

answers: What type of force applied to rock is a stress?

answers: NDQ_003381

answers: What is the result of the San Andreas Fault?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not a fault: Basin and Range Province, Amboy Crater, or Ubehebe Crater?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: Which of the following is not the cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not a type of fault: San Andreas Fault, Basin and Range Province, or normal faults?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip faults, basin and range faults, or independent faults?

answers: NDQ_003389

answers: What is the San Andreas Fault?

answers: NDQ_003390

answers: San Andreas Fault

answers: NDQ_003391

answers: Basin and Range Province

answers: NDQ_003392

answers: San Andreas Fault

answers: NDQ_003393

answers: Basin and Range Province

answers: NDQ_003394

answers: independent faults

answers: NDQ_003395

answers: San Andreas Fault

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: cinder cone volcanoes.

answers: NDQ_003352

answers: cracks

answers: NDQ_003353

answers: cracks

answers: NDQ_003354

answers: be Crater.

answers: NDQ_003355

answers: dikes

answers: NDQ_003356

answers: cinder cone volcanoes.

answers: NDQ_003357

answers: molten rock could flow up to the surface

answers: NDQ_003358

answers: cinder cone volcanoes.

answers: NDQ_003359

answers: cracks

answers: NDQ_003360

answers: San Andreas Fault

answers: NDQ_003362

answers: 80,000 years.

answers: NDQ_003363

answers: San Andreas Fault

answers: NDQ_003371

answers: cinder cone volcanoes.

answers: NDQ_003373

answers: cinder cone volcanoes.

answers: NDQ_003376

answers: cracks which formed many independent faults.

answers: NDQ_003378

answers: cinder cone volcanoes.

answers: NDQ_003379

answers: cinder cone volcanoes.

answers: NDQ_003380

answers: tension

answers: NDQ_003381

answers: cracks which formed many independent faults.

answers: NDQ_003382

answers: cinder cone volcanoes.

answers: NDQ_003383

answers: cracks

answers: NDQ_003384

answers: cinder cone volcanoes.

answers: NDQ_003385

answers: cinder cone volcanoes.

answers: NDQ_003386

answers: molten rock could flow up to the surface

answers: NDQ_003387

answers: cinder cone volcanoes.

answers: NDQ_003388

answers: cinder cone volcanoes.

answers: NDQ_003389

answers: cinder cone volcanoes.

answers: NDQ_003390

answers: San Andreas Fault

answers: NDQ_003391

answers: cinder cone volcanoes.

answers: NDQ_003392

answers: San Andreas Fault

answers: NDQ_003393

answers: cinder cone volcanoes.

answers: NDQ_003394

answers: San Andreas Fault

answers: NDQ_003395

answers: San Andreas Fault

answers: NDQ_003396

answers: San Andreas Fault

text: Many thousand years of dormancy are expected between large explosive eruptions of volcanoes in the Garibaldi Belt. A possible explanation for the lower rates of volcanism in the Garibaldi chain is that the associated terrain is being compressed in contrast to the more southern portions of the Cascade Arc. In continental rift zones, magma is able to push its way up through the Earth's crust rapidly along faults, providing less chance for differentiation. This is likely the case south of Mount Hood to the California border and east-southeast of the massive Newberry shield volcano adjacent to the Cascade Range in central Oregon because the Brothers Fault Zone lies in this region. This rift zone might explain the massive amounts of basaltic lava in this part of the central Cascade Arc. A low convergence rate in a compressional setting with massive stationary bodies of magma under the surface could explain the low volume and differentiated magmas throughout the Garibaldi Volcanic Belt. In 1958, Canadian volcanologist Bill Mathews proposed there could be a connection between regional glaciation of the North American continent during glacial periods and higher rates of volcanic activity during regional glacial unload of the continent. However, this is hard to predict due to the infrequent geological record in this region. But there is specific data, including the temporal grouping of eruptions synglacially or just postglacial within the Garibaldi Belt, that suggests this could be probable.

text: Many thousand years of dormancy are expected between large

text: explosive eruption

text: s of volcanoes in the Garibaldi Belt. A possible explanation for the lower rates of volcanism in the Garibaldi chain is that the associated

text: terrain

text: is being compressed in contrast to the more southern portions of the Cascade Arc. In continental

text: rift

text: zones, magma is able to push its way up through the Earth's crust rapidly along faults, providing less chance for differentiation. This is likely the case south of

text: Mount Hood

text: to the

text: California

text: border and east-southeast of the massive

text: Newberry shield volcano

text: adjacent to the

text: Cascade Range

text: in central

text: Oregon

text: because the

text: Brothers Fault Zone

text: lies in this region. This rift zone might explain the massive amounts of basaltic lava in this part of the central Cascade Arc. A low convergence rate in a compressional setting with massive stationary bodies of magma under the surface could explain the low volume and differentiated magmas throughout the Garibaldi Volcanic Belt. In 1958, Canadian volcanologist

text: Bill Mathews

text: proposed there could be a connection between regional glaciation of the North American continent during

text: glacial period

text: s and higher rates of volcanic activity during regional glacial unload of the continent. However, this is hard to predict due to the infrequent geological record in this region. But there is specific data, including the temporal grouping of eruptions synglacially or just postglacial within the Garibaldi Belt, that suggests this could be probable.

answers: NDQ_003351

answers: magma

answers: NDQ_003352

answers: compresses

answers: NDQ_003353

answers: Faults

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fault

answers: NDQ_003356

answers: erupt

answers: NDQ_003357

answers: magma is able to push its way up through the Earth's crust

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: fault lines

answers: NDQ_003362

answers: the San Andreas fault lies in this region

answers: NDQ_003363

answers: Garibaldi Belt

answers: NDQ_003371

answers: What may be the reason for the lower rates of volcanism in the Garibaldi chain

answers: NDQ_003373

answers: Why is the associated terrain being compressed?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What is the main idea of this passage?

answers: NDQ_003381

answers: What is the main idea of the passage?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: What is the main idea of this passage?

answers: NDQ_003384

answers: Which of the following is not a fault zone: continental rift zones, faults, or Cascade Arc?

answers: NDQ_003385

answers: Fault zone

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: Which of the following is not an example of a strike-slip fault?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: Brothers Fault

answers: NDQ_003391

answers: Brothers Fault Zone

answers: NDQ_003392

answers: Brothers Fault

answers: NDQ_003393

answers: shield volcano

answers: NDQ_003394

answers: Brothers Fault

answers: NDQ_003395

answers: Brothers Fault

answers: NDQ_003396

answers: Brothers Fault Zone

answers: NDQ_003351

answers: differentiation.

answers: NDQ_003352

answers: differentiation.

answers: NDQ_003353

answers: differentiation.

answers: NDQ_003354

answers: compressed in contrast to the more southern portions of the Cascade Arc.

answers: NDQ_003355

answers: rift zones,

answers: NDQ_003356

answers: differentiation.

answers: NDQ_003357

answers: less chance for differentiation.

answers: NDQ_003358

answers: rift zones,

answers: NDQ_003359

answers: faults,

answers: NDQ_003360

answers: rift zones,

answers: NDQ_003362

answers: Many thousand years of dormancy

answers: NDQ_003363

answers: continental rift zones,

answers: NDQ_003371

answers: Brothers Fault Zone

answers: NDQ_003373

answers: massive stationary bodies of magma

answers: NDQ_003376

answers: compressed in contrast to the more southern portions of the Cascade Arc.

answers: NDQ_003378

answers: compressed in contrast to the more southern portions of the Cascade Arc.

answers: NDQ_003379

answers: continental rift zones,

answers: NDQ_003380

answers: compressed

answers: NDQ_003381

answers: compressed

answers: NDQ_003382

answers: compressional setting with massive stationary bodies of magma

answers: NDQ_003383

answers: faults,

answers: NDQ_003384

answers: synglacially

answers: NDQ_003385

answers: rift zones,

answers: NDQ_003386

answers: magma

answers: NDQ_003387

answers: rift zones,

answers: NDQ_003388

answers: magma

answers: NDQ_003389

answers: compressed in contrast to the more southern portions of the Cascade Arc.

answers: NDQ_003390

answers: Brothers Fault Zone

answers: NDQ_003391

answers: massive stationary bodies of magma

answers: NDQ_003392

answers: Brothers Fault Zone

answers: NDQ_003393

answers: Newberry shield volcano

answers: NDQ_003394

answers: Brothers Fault Zone

answers: NDQ_003395

answers: Brothers Fault Zone

answers: NDQ_003396

answers: Brothers Fault Zone

text: When rock units are placed under horizontal compression, they shorten and become thicker. Because rock units, other than muds, do not significantly change in volume, this is accomplished in two primary ways: through faulting and folding. In the shallow crust, where brittle deformation can occur, thrust faults form, which cause deeper rock to move on top of shallower rock. Because deeper rock is often older, as noted by the principle of superposition, this can result in older rocks moving on top of younger ones. Movement along faults can result in folding, either because the faults are not planar or because rock layers are dragged along, forming drag folds as slip occurs along the fault. Deeper in the Earth, rocks behave plastically, and fold instead of faulting. These folds can either be those where the material in the center of the fold buckles upwards, creating "antiforms", or where it buckles downwards, creating "synforms". If the tops of the rock units within the folds remain pointing upwards, they are called anticlines and synclines, respectively. If some of the units in the fold are facing downward, the structure is called an overturned anticline or syncline, and if all of the rock units are overturned or the correct up-direction is unknown, they are simply called by the most general terms, antiforms and synforms.

text: When rock units are placed under horizontal

text: compression

text: , they shorten and become thicker. Because rock units, other than muds,

text: do not significantly change in volume

text: , this is accomplished in two primary ways: through

text: faulting

text: and

text: folding

text: . In the shallow crust, where

text: brittle deformation

text: can occur, thrust faults form, which cause deeper rock to move on top of shallower rock. Because deeper rock is often older, as noted by the

text: principle of superposition

text: , this can result in older rocks moving on top of younger ones. Movement along faults can result in folding, either because the faults are not planar or because rock layers are dragged along, forming drag folds as slip occurs along the fault. Deeper in the Earth, rocks behave plastically, and fold instead of faulting. These folds can either be those where the material in the center of the fold buckles upwards, creating "

text: antiform

text: s", or where it buckles downwards, creating "

text: synform

text: s". If the tops of the rock units within the folds remain pointing upwards, they are called

text: anticline

text: s and

text: syncline

text: s, respectively. If some of the units in the fold are facing downward, the structure is called an overturned anticline or syncline, and if all of the rock units are overturned or the correct up-direction is unknown, they are simply called by the most general terms, antiforms and synforms.

answers: NDQ_003351

answers: thrust faults

answers: NDQ_003352

answers: becomes thicker

answers: NDQ_003353

answers: horizontal compression

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: synforms

answers: NDQ_003356

answers: fold

answers: NDQ_003357

answers: thrust faults cause deeper rock to move on top of shallower rock

answers: NDQ_003358

answers: antiforms

answers: NDQ_003359

answers: thrust faults form

answers: NDQ_003360

answers: faults

answers: NDQ_003362

answers: deeper rock is often older

answers: NDQ_003363

answers: thrust faults

answers: NDQ_003371

answers: Why might older rocks move on top of younger ones?

answers: NDQ_003373

answers: because deeper rock is often older

answers: NDQ_003376

answers: horizontal compression, they shorten and become thicker

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: no

answers: NDQ_003380

answers: What is the term for horizontal compression?

answers: NDQ_003381

answers: horizontal compression

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: horizontal compression

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: no

answers: NDQ_003387

answers: What are thrust faults caused by?

answers: NDQ_003388

answers: unanswerable

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: thrust faults

answers: NDQ_003391

answers: shallower rock

answers: NDQ_003392

answers: thrust faults

answers: NDQ_003393

answers: shallower rock

answers: NDQ_003394

answers: thrust faults

answers: NDQ_003395

answers: thrust faults

answers: NDQ_003396

answers: thrust faults

answers: NDQ_003351

answers: thrust faults

answers: NDQ_003352

answers: they shorten and become thicker.

answers: NDQ_003353

answers: they shorten and become thicker.

answers: NDQ_003354

answers: older rocks moving on top of younger ones.

answers: NDQ_003355

answers: overturned anticline or syncline,

answers: NDQ_003356

answers: fold instead of faulting.

answers: NDQ_003357

answers: drag folds

answers: NDQ_003358

answers: "antiforms",

answers: NDQ_003359

answers: horizontal compression,

answers: NDQ_003360

answers: thrust faults

answers: NDQ_003362

answers: faulting.

answers: NDQ_003363

answers: thrust faults

answers: NDQ_003371

answers: thrust faults

answers: NDQ_003373

answers: fold instead of faulting.

answers: NDQ_003376

answers: thrust faults

answers: NDQ_003378

answers: slip

answers: NDQ_003379

answers: thrust faults

answers: NDQ_003380

answers: horizontal compression,

answers: NDQ_003381

answers: horizontal compression,

answers: NDQ_003382

answers: horizontal compression,

answers: NDQ_003383

answers: horizontal compression,

answers: NDQ_003384

answers: anticlines

answers: NDQ_003385

answers: thrust faults

answers: NDQ_003386

answers: folding,

answers: NDQ_003387

answers: thrust faults

answers: NDQ_003388

answers: thrust faults

answers: NDQ_003389

answers: faulting and folding.

answers: NDQ_003390

answers: thrust faults

answers: NDQ_003391

answers: drag folds

answers: NDQ_003392

answers: thrust faults

answers: NDQ_003393

answers: anticlines

answers: NDQ_003394

answers: folding,

answers: NDQ_003395

answers: thrust faults

answers: NDQ_003396

answers: thrust faults

text: The Azores Plateau began to form around 10 Ma, and is characterized by isotopic and elemental variations indicative of large heterogeneities in the mantle beneath it.  There is also evidence of only one magmatic source, and no interaction with other volcanic systems.  Additionally, the presence of thick crust and complex volcano-tectonic fabric implies the plateau developed through the migration of the Terceira Rift towards the NE, causing a constant position over a fixed hotspot. As previously mentioned, the Azores hotspot is thought to be the primary source for the excess magmatism along the Terceira Rift, resulting in the anomalously high relief of along-strike topography, and is considered to be sampling a relatively undegassed, primitive reservoir.  Lines of evidence for the plume-shaped structure in this area include mantle seismic anomalies, bathymetry and gravity anomalies, and plume noble gas signatures associated with the hotspot.  However, there is also a possibility the increased magmatic activity on the Terceira Rift is a partial result of the involvement with the rift-rift-rift triple junction between the Eurasian, African, and North American plates.

text: The Azores Plateau began to form around 10 Ma, and is characterized by isotopic and elemental variations indicative of large heterogeneities in the mantle beneath it.  There is also evidence of only one magmatic source, and no interaction with other volcanic systems.  Additionally, the presence of thick crust and complex volcano-tectonic fabric implies the plateau developed through the migration of the Terceira Rift towards the NE, causing a constant position over a fixed hotspot. As previously mentioned, the Azores hotspot is thought to be the primary source for the excess magmatism along the Terceira Rift, resulting in the anomalously high relief of along-strike topography, and is considered to be sampling a relatively undegassed, primitive reservoir.  Lines of evidence for the plume-shaped structure in this area include mantle seismic anomalies, bathymetry and gravity anomalies, and plume noble gas signatures associated with the hotspot.  However, there is also a possibility the increased magmatic activity on the Terceira Rift is a partial result of the involvement with the rift-rift-rift

text: triple junction

text: between the Eurasian, African, and North American plates.

answers: NDQ_003351

answers: gravity

answers: NDQ_003352

answers: more likely to crack

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: Rift

answers: NDQ_003356

answers: deform plastically

answers: NDQ_003357

answers: The Azores Plateau began to form around how many years ago?

answers: NDQ_003358

answers: hotspot

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: North American plates

answers: NDQ_003362

answers: the San Andreas fault is a partial result of the involvement with the rift-rift-rift triple junction between the Eurasian, African, and North American plates.

answers: NDQ_003363

answers: Terceira Rift

answers: NDQ_003371

answers: What is the Azores Plateau characterized by?

answers: NDQ_003373

answers: What is the Azores Plateau characterized by?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What is the Azores Plateau characterized by?

answers: NDQ_003382

answers: what is the most common stress at convergent plates

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: fault zone

answers: NDQ_003386

answers: the Terceira Rift

answers: NDQ_003387

answers: What type of stress is caused by normal faults?

answers: NDQ_003388

answers: What is the primary source for the excess magmatism along the Terceira Rift?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: Terceira Rift

answers: NDQ_003391

answers: The Azores Plateau

answers: NDQ_003392

answers: The Azores Plateau

answers: NDQ_003393

answers: The Azores Plateau

answers: NDQ_003394

answers: Terceira Rift

answers: NDQ_003395

answers: Terceira Rift

answers: NDQ_003396

answers: Terceira Rift

answers: NDQ_003351

answers: gravity

answers: NDQ_003352

answers: relief

answers: NDQ_003353

answers: constant position over a fixed hotspot.

answers: NDQ_003354

answers: Terceira Rift

answers: NDQ_003355

answers: rift-rift-rift

answers: NDQ_003356

answers: high relief

answers: NDQ_003357

answers: constant position over a fixed hotspot.

answers: NDQ_003358

answers: fixed hotspot.

answers: NDQ_003359

answers: migration of the Terceira Rift

answers: NDQ_003360

answers: North American plates.

answers: NDQ_003362

answers: rift-rift-rift triple junction

answers: NDQ_003363

answers: 10 Ma,

answers: NDQ_003371

answers: rift-rift-rift triple junction

answers: NDQ_003373

answers: large heterogeneities in the mantle

answers: NDQ_003376

answers: along-strike topography,

answers: NDQ_003378

answers: along-strike

answers: NDQ_003379

answers: NE,

answers: NDQ_003380

answers: gravity

answers: NDQ_003381

answers: constant position over a fixed hotspot.

answers: NDQ_003382

answers: rift-rift-rift triple junction

answers: NDQ_003383

answers: seismic anomalies,

answers: NDQ_003384

answers: Terceira Rift

answers: NDQ_003385

answers: rift-rift-rift triple junction

answers: NDQ_003386

answers: seismic anomalies,

answers: NDQ_003387

answers: mantle seismic anomalies,

answers: NDQ_003388

answers: along-strike topography,

answers: NDQ_003389

answers: one magmatic source, and no interaction with other volcanic systems.

answers: NDQ_003390

answers: Terceira Rift

answers: NDQ_003391

answers: The Azores Plateau

answers: NDQ_003392

answers: rift-rift-rift triple junction

answers: NDQ_003393

answers: hotspot.

answers: NDQ_003394

answers: rift-rift-rift triple junction

answers: NDQ_003395

answers: rift-rift-rift triple junction

answers: NDQ_003396

answers: Terceira Rift

text: West of South America, the Nazca Plate subducts beneath the South America Plate. This process has formed the Andean Volcanic Belt, which is subdivided into the Northern Volcanic Zone, the Central Volcanic Zone and the Southern Volcanic Zone. These belts have different underlying crusts and have thus different typical magma compositions. These volcanic zones are separated from each other by zones where there is no volcanism, associated with a shallow dip of the seismic zone of the subducting plate.

text: West of

text: South America

text: , the

text: Nazca Plate

text: subduct

text: s beneath the

text: South America Plate

text: . This process has formed the

text: Andean Volcanic Belt

text: , which is subdivided into the

text: Northern Volcanic Zone

text: , the Central Volcanic Zone and the

text: Southern Volcanic Zone

text: . These belts have different underlying crusts and have thus different typical magma compositions. These volcanic zones are separated from each other by zones where there is no volcanism, associated with a shallow dip of the seismic zone of the subducting plate.

answers: NDQ_003351

answers: shallow dip

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: seismic waves

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: Andean

answers: NDQ_003356

answers: subduct

answers: NDQ_003357

answers: seismic zone of the subducting plate

answers: NDQ_003358

answers: seismic zone

answers: NDQ_003359

answers: subducts

answers: NDQ_003360

answers: Andean Volcanic Belt

answers: NDQ_003362

answers: the Andean Volcanic Belt is subdivided into the Northern Volcanic Zone

answers: NDQ_003363

answers: Andean Volcanic Belt

answers: NDQ_003371

answers: Which of the following is not a type of volcano: Andean Volcanic Belt, Central Volcanic Zone or Southern Volcanic Zone?

answers: NDQ_003373

answers: What type of stresses does a deeply buried rock have?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: no

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What type of stress does the Andean Volcanic Belt experience?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What type of fold is the Andean Volcanic Belt?

answers: NDQ_003385

answers: What is the name of the Andean Volcanic Belt?

answers: NDQ_003386

answers: The Andean Volcanic Belt

answers: NDQ_003387

answers: Which of the following is not a type of normal fault?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip, strike-slip, or strike-slip?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: seismic zone

answers: NDQ_003391

answers: subducting plate

answers: NDQ_003392

answers: seismic zone

answers: NDQ_003393

answers: subducting plate

answers: NDQ_003394

answers: dip

answers: NDQ_003395

answers: shallow dip of the seismic zone

answers: NDQ_003396

answers: shallow dip

answers: NDQ_003351

answers: seismic zone

answers: NDQ_003352

answers: shallow dip of the seismic zone

answers: NDQ_003353

answers: different typical magma compositions.

answers: NDQ_003354

answers: the Nazca Plate subducts beneath the South America Plate.

answers: NDQ_003355

answers: dip

answers: NDQ_003356

answers: volcanism,

answers: NDQ_003357

answers: a shallow dip of the seismic zone of the subducting plate.

answers: NDQ_003358

answers: no volcanism,

answers: NDQ_003359

answers: Nazca Plate subducts beneath the South America Plate.

answers: NDQ_003360

answers: the Nazca Plate subducts beneath the South America Plate.

answers: NDQ_003362

answers: no volcanism,

answers: NDQ_003363

answers: Andean Volcanic Belt,

answers: NDQ_003371

answers: Andean Volcanic Belt,

answers: NDQ_003373

answers: shallow dip of the seismic zone

answers: NDQ_003376

answers: Andean Volcanic Belt,

answers: NDQ_003378

answers: shallow dip of the seismic zone

answers: NDQ_003379

answers: shallow

answers: NDQ_003380

answers: volcanism,

answers: NDQ_003381

answers: Andean Volcanic Belt,

answers: NDQ_003382

answers: South America Plate.

answers: NDQ_003383

answers: a shallow dip of the seismic zone

answers: NDQ_003384

answers: Andean Volcanic Belt,

answers: NDQ_003385

answers: Northern Volcanic Zone,

answers: NDQ_003386

answers: Andean Volcanic Belt,

answers: NDQ_003387

answers: shallow dip of the seismic zone

answers: NDQ_003388

answers: Andean Volcanic Belt,

answers: NDQ_003389

answers: Andean Volcanic Belt,

answers: NDQ_003390

answers: shallow dip of the seismic zone

answers: NDQ_003391

answers: seismic zone of the subducting plate.

answers: NDQ_003392

answers: Andean Volcanic Belt,

answers: NDQ_003393

answers: seismic zone

answers: NDQ_003394

answers: shallow dip of the seismic zone

answers: NDQ_003395

answers: shallow dip of the seismic zone

answers: NDQ_003396

answers: shallow dip

text: Underplating is the accumulation of partial melts at the base of the crust where an ocean plate is subducting under continental crust. Underplating is the result of partial melts being produced in the mantle wedge above a subducting plate. The partial melting is induced by a lowering of the melting temperature, the solidus, by the input of water and other volatiles supplied by phase transitions in the subducting slab. When the buoyant partial melt rises upwards through the mantle, it will usually stall at the base of the crust and pond there. This is because the crust is usually less dense than the underplating magma, and this is the point at which the ascending magma reaches a level of neutral buoyancy.

text: Underplating is the accumulation of partial melts at the base of the

text: crust

text: where an ocean

text: plate

text: is

text: subducting

text: under continental

text: crust

text: . Underplating is the result of partial melts being produced in the

text: mantle wedge

text: above a

text: subducting

text: plate

text: . The partial melting is induced by a lowering of the melting temperature, the

text: solidus

text: , by the input of water and other volatiles supplied by

text: phase transition

text: s in the subducting

text: slab

text: . When the buoyant partial melt rises upwards through the

text: mantle

text: , it will usually stall at the base of the

text: crust

text: and pond there. This is because the crust is usually less dense than the underplating

text: magma

text: , and this is the point at which the ascending magma reaches a level of neutral buoyancy.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: is likely to crack

answers: NDQ_003353

answers: partial melts

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: mantle wedge

answers: NDQ_003356

answers: subduct

answers: NDQ_003357

answers: Underplating is the result of partial melts being produced in the mantle

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: ocean plates

answers: NDQ_003362

answers: underplating magma reaches a level of neutral buoyancy.

answers: NDQ_003363

answers: Underplating

answers: NDQ_003371

answers: What is the result of partial melts being produced in the mantle wedge above a subducting plate

answers: NDQ_003373

answers: unanswerable

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a stress?

answers: NDQ_003381

answers: What is the result of partial melts being produced in the mantle wedge

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: unanswerable

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: What is the result of partial melts being produced in the mantle wedge above a subducting plate?

answers: NDQ_003389

answers: underplating

answers: NDQ_003390

answers: subducting

answers: NDQ_003391

answers: subducting slab

answers: NDQ_003392

answers: subducting plate

answers: NDQ_003393

answers: mantle wedge

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: subducting plate

answers: NDQ_003396

answers: Underplating

answers: NDQ_003351

answers: Underplating

answers: NDQ_003352

answers: lowering of the melting temperature,

answers: NDQ_003353

answers: lowering of the melting temperature,

answers: NDQ_003354

answers: Underplating

answers: NDQ_003355

answers: Underplating

answers: NDQ_003356

answers: pond there.

answers: NDQ_003357

answers: neutral buoyancy.

answers: NDQ_003358

answers: Underplating

answers: NDQ_003359

answers: less dense than the underplating magma,

answers: NDQ_003360

answers: Underplating

answers: NDQ_003362

answers: Underplating

answers: NDQ_003363

answers: Underplating

answers: NDQ_003371

answers: Underplating

answers: NDQ_003373

answers: Underplating

answers: NDQ_003376

answers: Underplating

answers: NDQ_003378

answers: Underplating

answers: NDQ_003379

answers: crust.

answers: NDQ_003380

answers: Underplating

answers: NDQ_003381

answers: less dense

answers: NDQ_003382

answers: Underplating

answers: NDQ_003383

answers: Underplating

answers: NDQ_003384

answers: Underplating

answers: NDQ_003385

answers: Underplating

answers: NDQ_003386

answers: Underplating

answers: NDQ_003387

answers: Underplating

answers: NDQ_003388

answers: Underplating

answers: NDQ_003389

answers: Underplating

answers: NDQ_003390

answers: Underplating

answers: NDQ_003391

answers: Underplating

answers: NDQ_003392

answers: Underplating

answers: NDQ_003393

answers: mantle wedge above a subducting plate.

answers: NDQ_003394

answers: Underplating

answers: NDQ_003395

answers: Underplating

answers: NDQ_003396

answers: Underplating

text: Inversion tectonics is recognised to form as a result of: <br>1 Regional temporal variations in stress patterns within plates, resulting from forces caused by changes in plate boundary configuration, the blocking of subduction zones by buoyant crust (collision) and changes in relative motion at nearby plate boundaries.

text: Inversion tectonics is recognised to form as a result of: <br>1 Regional temporal variations in stress patterns within plates, resulting from forces caused by changes in plate boundary configuration, the blocking of subduction zones by buoyant crust (collision) and changes in relative motion at nearby plate boundaries.

answers: NDQ_003351

answers: relative motion

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: changes in plate boundaries

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: change in shape

answers: NDQ_003357

answers: subduction zones are blocked by buoyant crust

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: plates

answers: NDQ_003362

answers: the blocking of subduction zones by buoyant crust

answers: NDQ_003363

answers: subduction zones

answers: NDQ_003371

answers: What is a result of changes in plate boundary configuration?

answers: NDQ_003373

answers: How would you describe compressive stresses?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What causes rock to deform?

answers: NDQ_003382

answers: what is the most common stress at convergent plates

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What type of fold is a syncline?

answers: NDQ_003385

answers: What is the term for an area where faults are clustered?

answers: NDQ_003386

answers: None of the above choices.

answers: NDQ_003387

answers: Which of the following is not a cause of normal faults?

answers: NDQ_003388

answers: What type of stress does shear stress cause?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: subduction zone

answers: NDQ_003391

answers: subduction zone

answers: NDQ_003392

answers: subduction zone

answers: NDQ_003393

answers: subduction zone

answers: NDQ_003394

answers: isobath

answers: NDQ_003395

answers: is recognised to form as a result of:

answers: NDQ_003396

answers: horizontal

answers: NDQ_003351

answers: (collision) and changes in relative motion

answers: NDQ_003352

answers: buoyant crust

answers: NDQ_003353

answers: changes in relative motion

answers: NDQ_003354

answers: Inversion tectonics

answers: NDQ_003355

answers: subduction zones

answers: NDQ_003356

answers: buoyant crust

answers: NDQ_003357

answers: subduction zones by buoyant crust

answers: NDQ_003358

answers: subduction zones

answers: NDQ_003359

answers: buoyant crust

answers: NDQ_003360

answers: Inversion tectonics

answers: NDQ_003362

answers: buoyant crust

answers: NDQ_003363

answers: Inversion tectonics

answers: NDQ_003371

answers: Inversion tectonics

answers: NDQ_003373

answers: Inversion tectonics

answers: NDQ_003376

answers: changes in plate boundary configuration,

answers: NDQ_003378

answers: relative motion

answers: NDQ_003379

answers: blocking of subduction zones by buoyant crust

answers: NDQ_003380

answers: stress

answers: NDQ_003381

answers: buoyant crust

answers: NDQ_003382

answers: blocking of subduction zones by buoyant crust

answers: NDQ_003383

answers: stress patterns within plates,

answers: NDQ_003384

answers: Inversion tectonics

answers: NDQ_003385

answers: changes in plate boundary configuration, the blocking of subduction zones

answers: NDQ_003386

answers: changes in relative motion at nearby plate boundaries.

answers: NDQ_003387

answers: Inversion tectonics

answers: NDQ_003388

answers: Inversion tectonics

answers: NDQ_003389

answers: Inversion tectonics

answers: NDQ_003390

answers: Inversion tectonics

answers: NDQ_003391

answers: buoyant crust

answers: NDQ_003392

answers: Inversion tectonics

answers: NDQ_003393

answers: buoyant crust

answers: NDQ_003394

answers: Inversion tectonics

answers: NDQ_003395

answers: Inversion tectonics

answers: NDQ_003396

answers: Inversion tectonics

text: Siletzia corresponds geographically to the Coast Range Volcanic Province (or Coast Range basalts), but is distinguished from slightly younger basalts that erupted after Siletzia accreted to the continent and differ in chemical composition.  The Siletzia basalts are tholeiitic, a characteristic of mantle-derived magma erupted from a spreading ridge between plates of oceanic crust. The younger basalts are alkalic or calc-alkaline, characteristic of magmas derived from a subduction zone. This change of composition reflects a change from marine to continental volcanism that becomes evident around 48 to 42 Ma (millions of years ago), and is attributed to the accretion of Siletzia against the North American continent.

text: Siletzia corresponds geographically to the Coast Range Volcanic Province (or Coast Range basalts), but is distinguished from slightly younger basalts that erupted after Siletzia accreted to the continent and differ in chemical composition.  The Siletzia basalts are

text: tholeiitic

text: , a characteristic of

text: mantle

text: -derived magma erupted from a

text: spreading ridge

text: between plates of oceanic crust. The younger basalts are alkalic or

text: calc-alkaline

text: , characteristic of magmas derived from a

text: subduction zone

text: . This change of composition reflects a change from marine to continental volcanism that becomes evident around 48 to 42

text: Ma

text: (millions of years ago), and is attributed to the accretion of Siletzia against the

text: North America

text: n continent.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: is more likely to crack

answers: NDQ_003353

answers: a change in composition

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: subduction zone

answers: NDQ_003356

answers: change in chemical composition

answers: NDQ_003357

answers: magma derived from a subduction zone

answers: NDQ_003358

answers: unanswerable

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: plates of oceanic crust

answers: NDQ_003362

answers: Siletzia corresponds geographically to the Coast Range Volcanic Province

answers: NDQ_003363

answers: Siletzia

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: How would you describe tholeiitic?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What type of rock is Siletzia?

answers: NDQ_003381

answers: What type of rock does Siletzia correspond to geographically?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: unanswerable

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: What type of faults result from shear stress?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: subduction zone

answers: NDQ_003391

answers: subduction zone

answers: NDQ_003392

answers: subduction zone

answers: NDQ_003393

answers: subduction zone

answers: NDQ_003394

answers: spreading ridge

answers: NDQ_003395

answers: spreading ridge

answers: NDQ_003396

answers: spreading ridge

answers: NDQ_003351

answers: subduction zone.

answers: NDQ_003352

answers: alkalic or calc-alkaline,

answers: NDQ_003353

answers: chemical composition.

answers: NDQ_003354

answers: Siletzia

answers: NDQ_003355

answers: subduction zone.

answers: NDQ_003356

answers: tholeiitic,

answers: NDQ_003357

answers: subduction zone.

answers: NDQ_003358

answers: subduction zone.

answers: NDQ_003359

answers: accretion

answers: NDQ_003360

answers: a spreading ridge between plates of oceanic crust.

answers: NDQ_003362

answers: Siletzia

answers: NDQ_003363

answers: Siletzia against the North American continent.

answers: NDQ_003371

answers: subduction zone.

answers: NDQ_003373

answers: tholeiitic,

answers: NDQ_003376

answers: spreading ridge between plates of oceanic crust.

answers: NDQ_003378

answers: tholeiitic,

answers: NDQ_003379

answers: tholeiitic,

answers: NDQ_003380

answers: tholeiitic,

answers: NDQ_003381

answers: tholeiitic,

answers: NDQ_003382

answers: ridge between plates of oceanic crust.

answers: NDQ_003383

answers: ridge

answers: NDQ_003384

answers: ridge

answers: NDQ_003385

answers: subduction zone.

answers: NDQ_003386

answers: spreading ridge between plates of oceanic crust.

answers: NDQ_003387

answers: subduction zone.

answers: NDQ_003388

answers: tholeiitic,

answers: NDQ_003389

answers: spreading ridge between plates of oceanic crust.

answers: NDQ_003390

answers: ridge

answers: NDQ_003391

answers: subduction zone.

answers: NDQ_003392

answers: ridge

answers: NDQ_003393

answers: subduction zone.

answers: NDQ_003394

answers: ridge

answers: NDQ_003395

answers: spreading ridge

answers: NDQ_003396

answers: subduction zone.

text: Epigenetics may play a role in a wide array of vascular complications and in diabetes. The epigenetic variations involved with diabetes can change chromatin structure as well as gene expression. Regardless of whether glycemic control has been achieved through treatment these epigenetic mechanisms are lasting and do not change with the alteration of diet. The most common vascular complication in patients with Type 2 Diabetes is retinopathy which causes many patients to go blind. Studies showed that retinal damage persisted even after the reversal of hyperglycemia in dogs. Studies with streptozotocin injected Type 1 diabetes rats showed that the re-institution of glycemic control after a short period of hyperglycemia had protective effects in the eyes, including reduction in parameters of oxidant stress and inflammation. However, specimens with prolonged diabetes failed to show similar protection. It was then seen with endothelial cells (which line blood vessels) cultured in high glucose that there was a sustained increase in the expression of key extracellular and pro-fibrotic genes and persistently increased oxidant stress, after subsequent glucose normalization. These studies show that the deleterious effects of prior hyperglycemic exposure have long-lasting effects on target organs even after subsequent glycaemic control underscoring the beneficial effects of intensive glycemic control in diabetes. The persistence of these symptoms points to epigenesis as an underlying cause.

text: Epigenetics may play a role in a wide array of

text: vascular complication

text: s and in diabetes. The epigenetic variations involved with diabetes can change

text: chromatin structure

text: as well as gene expression. Regardless of whether glycemic control has been achieved through treatment these epigenetic mechanisms are lasting and do not change with the alteration of diet. The most common vascular complication in patients with Type 2 Diabetes is

text: retinopathy

text: which causes many patients to go blind. Studies showed that retinal damage persisted even after the reversal of

text: hyperglycemia

text: in dogs. Studies with

text: streptozotocin

text: injected

text: Type 1 diabetes

text: rats showed that the re-institution of glycemic control after a short period of hyperglycemia had protective effects in the eyes, including reduction in parameters of

text: oxidant stress

text: and inflammation. However, specimens with prolonged diabetes failed to show similar protection. It was then seen with

text: endothelial cells

text: (which line blood vessels) cultured in high glucose that there was a sustained increase in the expression of key extracellular and

text: pro-fibrotic

text: genes and persistently increased oxidant stress, after subsequent glucose normalization. These studies show that the deleterious effects of prior hyperglycemic exposure have long-lasting effects on target organs even after subsequent glycaemic control underscoring the beneficial effects of intensive glycemic control in diabetes. The persistence of these symptoms points to epigenesis as an underlying cause.

answers: NDQ_003351

answers: oxidant stress

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: a chemical reaction

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: endothelial cells

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: Regardless of whether glycemic control has been achieved through treatment

answers: NDQ_003363

answers: the same time

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: What is the main idea of this passage?

answers: NDQ_003376

answers: What is the most common vascular complication in patients with Type 2 Diabetes

answers: NDQ_003378

answers: What is the most common vascular complication in patients with Type 2 Diabetes

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: Which of the following is not a stress?

answers: NDQ_003381

answers: What is the main idea of this passage?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the main idea of this passage?

answers: NDQ_003384

answers: What is the most common vascular complication in patients with Type 2 Diabetes?

answers: NDQ_003385

answers: What is the term for an area where faults are clustered?

answers: NDQ_003386

answers: What is the main cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not a cause of normal faults?

answers: NDQ_003388

answers: What is the most common vascular complication in patients with Type 2 Diabetes?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: Type 2 Diabetes

answers: NDQ_003391

answers: dip-slip

answers: NDQ_003392

answers: Type 2 Diabetes

answers: NDQ_003393

answers: igneous rock

answers: NDQ_003394

answers: type 1

answers: NDQ_003395

answers: type 1 diabetes rats

answers: NDQ_003396

answers: Type 1

answers: NDQ_003351

answers: oxidant

answers: NDQ_003352

answers: oxidant stress

answers: NDQ_003353

answers: chromatin structure

answers: NDQ_003354

answers: Epigenetics

answers: NDQ_003355

answers: Epigenetics

answers: NDQ_003356

answers: retinopathy

answers: NDQ_003357

answers: do not change with the alteration of diet.

answers: NDQ_003358

answers: retinopathy

answers: NDQ_003359

answers: Epigenetics

answers: NDQ_003360

answers: Epigenetics

answers: NDQ_003362

answers: Epigenetics

answers: NDQ_003363

answers: Epigenetics

answers: NDQ_003371

answers: Epigenetics

answers: NDQ_003373

answers: Epigenetics

answers: NDQ_003376

answers: Epigenetics

answers: NDQ_003378

answers: Epigenetics

answers: NDQ_003379

answers: diabetes.

answers: NDQ_003380

answers: oxidant stress

answers: NDQ_003381

answers: Epigenetics

answers: NDQ_003382

answers: oxidant stress

answers: NDQ_003383

answers: Epigenetics

answers: NDQ_003384

answers: endothelial cells

answers: NDQ_003385

answers: Epigenetics

answers: NDQ_003386

answers: Epigenetics

answers: NDQ_003387

answers: Epigenetics

answers: NDQ_003388

answers: Epigenetics

answers: NDQ_003389

answers: Epigenetics

answers: NDQ_003390

answers: Epigenetics

answers: NDQ_003391

answers: Epigenetics

answers: NDQ_003392

answers: Epigenetics

answers: NDQ_003393

answers: Epigenetics

answers: NDQ_003394

answers: Epigenetics

answers: NDQ_003395

answers: Epigenetics

answers: NDQ_003396

answers: Epigenetics

text: New Zealand lies along the boundary between the Indo-Australian and Pacific Plates. In the North Island the displacement is mainly taken up along the Hikurangi Subduction Zone, although the remaining dextral strike-slip component of the relative plate motion is accommodated by the North Island Fault System (NIFS). Both earthquakes are believed to have occurred along the Hikurangi Subduction Zone, in close proximity to each other. Both earthquakes generated tsunami, caused by the sudden release of energy from the Earth's crust.

text: New Zealand

text: lies along the boundary between the

text: Indo-Australian

text: and

text: Pacific Plate

text: s. In the

text: North Island

text: the displacement is mainly taken up along the Hikurangi Subduction Zone, although the remaining dextral strike-slip component of the relative plate motion is accommodated by the North Island Fault System (NIFS). Both earthquakes are believed to have occurred along the Hikurangi Subduction Zone, in close proximity to each other. Both earthquakes generated tsunami, caused by the sudden release of energy from the

text: Earth's crust

answers: NDQ_003351

answers: strike-slip

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: Subduction Zone

answers: NDQ_003356

answers: generate tsunami

answers: NDQ_003357

answers: dextral strike-slip component of the relative plate motion is

answers: NDQ_003358

answers: earthquake

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Plates

answers: NDQ_003362

answers: New Zealand lies along the boundary between the Indo-Australian and Pacific Plates

answers: NDQ_003363

answers: Pacific Plates

answers: NDQ_003371

answers: What may be the reason for the sudden release of energy from the Earth's crust?

answers: NDQ_003373

answers: what is the last word in the passage?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What type of stress does the Hikurangi Subduction Zone experience?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: what is the last word in the passage?

answers: NDQ_003386

answers: What is the cause of earthquakes?

answers: NDQ_003387

answers: What is the cause of the sudden release of energy from the Earth's crust?

answers: NDQ_003388

answers: What is the cause of the sudden release of energy from the Earth's crust?

answers: NDQ_003389

answers: subduction zone

answers: NDQ_003390

answers: North Island Fault System

answers: NDQ_003391

answers: Subduction Zone

answers: NDQ_003392

answers: North Island Fault System

answers: NDQ_003393

answers: Subduction Zone

answers: NDQ_003394

answers: dextral

answers: NDQ_003395

answers: North Island Fault System

answers: NDQ_003396

answers: North Island Fault System

answers: NDQ_003351

answers: strike-slip

answers: NDQ_003352

answers: tsunami,

answers: NDQ_003353

answers: sudden release of energy from the Earth's crust.

answers: NDQ_003354

answers: Hikurangi Subduction Zone,

answers: NDQ_003355

answers: tsunami,

answers: NDQ_003356

answers: tsunami,

answers: NDQ_003357

answers: dextral strike-slip

answers: NDQ_003358

answers: tsunami,

answers: NDQ_003359

answers: Fault System

answers: NDQ_003360

answers: Hikurangi Subduction Zone,

answers: NDQ_003362

answers: Both earthquakes

answers: NDQ_003363

answers: Hikurangi Subduction Zone,

answers: NDQ_003371

answers: Hikurangi Subduction Zone,

answers: NDQ_003373

answers: tsunami, caused by the sudden release of energy from the Earth's crust.

answers: NDQ_003376

answers: sudden release of energy from the Earth's crust.

answers: NDQ_003378

answers: strike-slip

answers: NDQ_003379

answers: dextral

answers: NDQ_003380

answers: Both earthquakes

answers: NDQ_003381

answers: Hikurangi Subduction Zone,

answers: NDQ_003382

answers: Hikurangi Subduction Zone,

answers: NDQ_003383

answers: North Island Fault System

answers: NDQ_003384

answers: Hikurangi Subduction Zone,

answers: NDQ_003385

answers: Hikurangi Subduction Zone,

answers: NDQ_003386

answers: sudden release of energy from the Earth's crust.

answers: NDQ_003387

answers: sudden release of energy from the Earth's crust.

answers: NDQ_003388

answers: strike-slip

answers: NDQ_003389

answers: Hikurangi Subduction Zone,

answers: NDQ_003390

answers: North Island Fault System

answers: NDQ_003391

answers: Hikurangi Subduction Zone,

answers: NDQ_003392

answers: North Island Fault System

answers: NDQ_003393

answers: Hikurangi Subduction Zone,

answers: NDQ_003394

answers: dextral

answers: NDQ_003395

answers: North Island Fault System

answers: NDQ_003396

answers: North Island Fault System

text: The current mantle plume theory is that material and energy from Earth's interior are exchanged with the surface crust in two distinct modes: the predominant, steady state plate tectonic regime driven by upper mantle convection, and a punctuated, intermittently dominant, mantle overturn regime driven by plume convection. This second regime, while often discontinuous, is periodically significant in mountain building and continental breakup.

text: The current mantle plume theory is that material and energy from Earth's interior are exchanged with the surface crust in two distinct modes: the predominant, steady state plate tectonic regime driven by upper mantle convection, and a punctuated, intermittently dominant, mantle overturn regime driven by plume convection. This second regime, while often discontinuous, is periodically significant in mountain building and continental breakup.

answers: NDQ_003351

answers: mantle overturn

answers: NDQ_003352

answers: is likely to crack

answers: NDQ_003353

answers: plume convection

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: mountain

answers: NDQ_003356

answers: break up

answers: NDQ_003357

answers: upper mantle convection

answers: NDQ_003358

answers: discontinuous

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: plume convection

answers: NDQ_003362

answers: periodic significant in mountain building and continental breakup

answers: NDQ_003363

answers: mantle overturn regime

answers: NDQ_003371

answers: What is the second regime?

answers: NDQ_003373

answers: How would you describe compressive stresses?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What is the second regime?

answers: NDQ_003381

answers: What type of rock deforms?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is the first regime?

answers: NDQ_003385

answers: plate tectonic regime

answers: NDQ_003386

answers: not enough information

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: unanswerable

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: mantle overturn

answers: NDQ_003391

answers: mountain

answers: NDQ_003392

answers: mantle overturn

answers: NDQ_003393

answers: mountain

answers: NDQ_003394

answers: discontinuous

answers: NDQ_003395

answers: plate tectonic

answers: NDQ_003396

answers: mantle overturn

answers: NDQ_003351

answers: upper mantle convection,

answers: NDQ_003352

answers: mountain building and continental breakup.

answers: NDQ_003353

answers: mountain building and continental breakup.

answers: NDQ_003354

answers: The current mantle plume theory

answers: NDQ_003355

answers: mountain

answers: NDQ_003356

answers: mountain building and continental breakup.

answers: NDQ_003357

answers: mountain building and continental breakup.

answers: NDQ_003358

answers: mountain

answers: NDQ_003359

answers: upper mantle convection,

answers: NDQ_003360

answers: upper mantle convection,

answers: NDQ_003362

answers: discontinuous, is periodically significant in mountain building and continental breakup.

answers: NDQ_003363

answers: mantle overturn regime driven by plume convection.

answers: NDQ_003371

answers: mantle overturn regime driven by plume convection.

answers: NDQ_003373

answers: The current mantle plume theory

answers: NDQ_003376

answers: mountain building

answers: NDQ_003378

answers: upper mantle convection,

answers: NDQ_003379

answers: upper mantle convection,

answers: NDQ_003380

answers: mountain building and continental breakup.

answers: NDQ_003381

answers: plume convection.

answers: NDQ_003382

answers: upper mantle convection,

answers: NDQ_003383

answers: upper mantle convection,

answers: NDQ_003384

answers: upper mantle convection,

answers: NDQ_003385

answers: upper mantle convection,

answers: NDQ_003386

answers: mantle plume theory

answers: NDQ_003387

answers: plume convection.

answers: NDQ_003388

answers: upper mantle convection,

answers: NDQ_003389

answers: mantle overturn regime driven by plume convection.

answers: NDQ_003390

answers: mantle overturn

answers: NDQ_003391

answers: mountain

answers: NDQ_003392

answers: mountain building and continental breakup.

answers: NDQ_003393

answers: mountain

answers: NDQ_003394

answers: mountain building and continental breakup.

answers: NDQ_003395

answers: upper mantle convection,

answers: NDQ_003396

answers: mantle overturn

text: The Earth's interior radiates heat at a rate of about 47 TW (terawatts), which is less than 0.1% of the incoming solar energy. Part of this heat loss is accounted for by the heat generated upon decay of radioactive isotopes in the Earth interior. The remaining heat loss is due to the secular cooling of the Earth, growth of the Earth’s inner core (gravitational energy and latent heat contributions), and other processes. The most important heat-producing elements are uranium (U), thorium (Th), and potassium (K). The debate about their abundances in the Earth has not concluded. Various compositional estimates exist where the total Earth’s internal radiogenic heating rate ranges from as low at ~10 TW to as high as ~30 TW. About 7 TW worth of heat-producing elements reside in the Earth's crust,  the remaining power is distributed in the Earth mantle; the amount of U, Th, and K in the Earth core is probably negligible. Radioactivity in the Earth mantle provides internal heating to power mantle convection, which is the driver of plate tectonics. The amount of mantle radioactivity and its spatial distribution—is the mantle compositionally uniform at large scale or composed of distinct reservoirs?—is of importance to geophysics.

text: The

text: Earth

text: 's interior radiates heat at a rate of about 47 TW (

text: terawatts

text: ), which is less than 0.1% of the incoming solar energy. Part of this heat loss is accounted for by the heat generated upon decay of radioactive isotopes in the Earth interior. The remaining heat loss is due to the secular cooling of the Earth, growth of the Earth’s

text: inner core

text: (gravitational energy and latent heat contributions), and other processes. The most important heat-producing elements are

text: uranium

text: (U),

text: thorium

text: (Th), and

text: potassium

text: (K). The debate about their abundances in the Earth has not concluded. Various compositional estimates exist where the total Earth’s internal radiogenic heating rate ranges from as low at ~10 TW to as high as ~30 TW. About 7 TW worth of heat-producing elements reside in the

text: Earth's crust

text: ,  the remaining power is distributed in the

text: Earth mantle

text: ; the amount of U, Th, and K in the

text: Earth core

text: is probably negligible. Radioactivity in the Earth mantle provides internal heating to power

text: mantle convection

text: , which is the driver of

text: plate tectonics

text: . The amount of mantle radioactivity and its spatial distribution—is the mantle compositionally uniform at large scale or composed of distinct reservoirs?—is of importance to geophysics.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: convection

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: heat up

answers: NDQ_003357

answers: about 7 TW worth of heat-producing elements reside in the Earth's crust

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: plate tectonics

answers: NDQ_003362

answers: The debate about their abundances in the Earth has not concluded

answers: NDQ_003363

answers: plate tectonics

answers: NDQ_003371

answers: What is the driver of plate tectonics?

answers: NDQ_003373

answers: What is the most important heat-producing element in the Earth?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: The debate about their abundances in the Earth has not concluded

answers: NDQ_003380

answers: What is the most important heat-producing element?

answers: NDQ_003381

answers: What is the most important heat-producing element?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is the debate about their abundances in the Earth?

answers: NDQ_003385

answers: What is the driver of plate tectonics?

answers: NDQ_003386

answers: plate tectonics

answers: NDQ_003387

answers: What is the driver of plate tectonics?

answers: NDQ_003388

answers: What is the most important heat-producing element?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: tectonics

answers: NDQ_003391

answers: mantle

answers: NDQ_003392

answers: plate tectonics

answers: NDQ_003393

answers: mantle

answers: NDQ_003394

answers: tectonics

answers: NDQ_003395

answers: plate tectonics

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: mantle convection,

answers: NDQ_003352

answers: mantle convection,

answers: NDQ_003353

answers: mantle convection,

answers: NDQ_003354

answers: 10 TW to as high as <unk>30 TW.

answers: NDQ_003355

answers: mantle convection,

answers: NDQ_003356

answers: radioactive isotopes

answers: NDQ_003357

answers: mantle convection,

answers: NDQ_003358

answers: plate tectonics.

answers: NDQ_003359

answers: 0.1% of the incoming solar energy.

answers: NDQ_003360

answers: plate tectonics.

answers: NDQ_003362

answers: less than 0.1% of the incoming solar energy.

answers: NDQ_003363

answers: Earth mantle;

answers: NDQ_003371

answers: 47 TW

answers: NDQ_003373

answers: 7 TW worth of heat-producing elements

answers: NDQ_003376

answers: mantle convection,

answers: NDQ_003378

answers: mantle convection,

answers: NDQ_003379

answers: 10 TW to as high as <unk>30 TW.

answers: NDQ_003380

answers: The Earth's interior radiates heat

answers: NDQ_003381

answers: mantle convection,

answers: NDQ_003382

answers: mantle convection,

answers: NDQ_003383

answers: 47 TW

answers: NDQ_003384

answers: mantle convection,

answers: NDQ_003385

answers: 47 TW

answers: NDQ_003386

answers: plate tectonics.

answers: NDQ_003387

answers: mantle convection,

answers: NDQ_003388

answers: mantle convection,

answers: NDQ_003389

answers: mantle convection,

answers: NDQ_003390

answers: 47 TW

answers: NDQ_003391

answers: mantle convection,

answers: NDQ_003392

answers: 47 TW

answers: NDQ_003393

answers: crust,

answers: NDQ_003394

answers: plate tectonics.

answers: NDQ_003395

answers: 0.1% of the incoming solar energy.

answers: NDQ_003396

answers: plate tectonics.

text: Some good examples of shear zones of the strike-slip type are the South Armorican Shear Zone and the North Armorican Shear Zone in Brittany, the North Anatolian Fault Zone in Turkey, and the Dead Sea Fault in Israel. Shear zones of the transform type are the San Andreas Fault in California, and the Alpine Fault in New Zealand. A shear zone of the thrust type is the Moine Thrust in northwestern Scotland. An example for the subduction zone setting is the Japan Median Tectonic Line. Detachment fault related shear zones can be found in southeastern California, e.g. the Whipple Mountain Detachment Fault. An example of a huge anastomosing shear-zone is the Borborema Shear Zone in Brazil.

text: Some good examples of shear zones of the strike-slip type are the

text: South Armorican Shear Zone

text: and the

text: North Armorican Shear Zone

text: in

text: Brittany

text: , the

text: North Anatolian Fault Zone

text: in

text: Turkey

text: , and the

text: Dead Sea Fault

text: in

text: Israel

text: . Shear zones of the transform type are the

text: San Andreas Fault

text: in

text: California

text: , and the

text: Alpine Fault

text: in

text: New Zealand

text: . A shear zone of the thrust type is the

text: Moine Thrust

text: in northwestern

text: Scotland

text: . An example for the subduction zone setting is the

text: Japan Median Tectonic Line

text: . Detachment fault related shear zones can be found in southeastern California, e.g. the

text: Whipple Mountain Detachment Fault

text: . An example of a huge anastomosing shear-zone is the

text: Borborema Shear Zone

text: in

text: Brazil

answers: NDQ_003351

answers: strike-slip

answers: NDQ_003352

answers: is more likely to crack

answers: NDQ_003353

answers: shear zones

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: strike-slip

answers: NDQ_003356

answers: change shape

answers: NDQ_003357

answers: Strike-slip type shear zones are

answers: NDQ_003358

answers: subduction zone

answers: NDQ_003359

answers: deforms

answers: NDQ_003360

answers: faults

answers: NDQ_003362

answers: Moine Thrust in northwestern Scotland

answers: NDQ_003363

answers: subduction zone

answers: NDQ_003371

answers: What type of fault is the Moine Thrust?

answers: NDQ_003373

answers: What type of stresses is a deeply buried rock under?

answers: NDQ_003376

answers: What type of terrain is caused by compressive forces?

answers: NDQ_003378

answers: What type of zone is the Moine Thrust in northwestern Scotland?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What type of zone is the Moine Thrust?

answers: NDQ_003381

answers: What type of stress does the Moine Thrust exhibit?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What type of fold is the Moine Thrust?

answers: NDQ_003385

answers: anastomosing

answers: NDQ_003386

answers: What is the cause of earthquakes?

answers: NDQ_003387

answers: Which type of faults are caused by compression stress?

answers: NDQ_003388

answers: What type of faults result from shear stress?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: Detachment fault

answers: NDQ_003391

answers: subduction zone

answers: NDQ_003392

answers: Detachment fault

answers: NDQ_003393

answers: subduction zone

answers: NDQ_003394

answers: Alpine Fault

answers: NDQ_003395

answers: Detachment fault

answers: NDQ_003396

answers: Transform

answers: NDQ_003351

answers: strike-slip

answers: NDQ_003352

answers: shear zones of the strike-slip

answers: NDQ_003353

answers: shear zones

answers: NDQ_003354

answers: San Andreas Fault

answers: NDQ_003355

answers: thrust type is the Moine Thrust

answers: NDQ_003356

answers: shear zones of the strike-slip

answers: NDQ_003357

answers: strike-slip

answers: NDQ_003358

answers: subduction zone

answers: NDQ_003359

answers: shear zones of the strike-slip

answers: NDQ_003360

answers: shear zones

answers: NDQ_003362

answers: thrust type is the Moine Thrust

answers: NDQ_003363

answers: subduction zone setting is the Japan Median Tectonic Line.

answers: NDQ_003371

answers: Moine Thrust

answers: NDQ_003373

answers: shear zones

answers: NDQ_003376

answers: shear zones

answers: NDQ_003378

answers: strike-slip

answers: NDQ_003379

answers: strike-slip

answers: NDQ_003380

answers: shear zones

answers: NDQ_003381

answers: shear zones of the strike-slip

answers: NDQ_003382

answers: strike-slip

answers: NDQ_003383

answers: shear zones

answers: NDQ_003384

answers: thrust type is the Moine Thrust

answers: NDQ_003385

answers: North Anatolian Fault Zone

answers: NDQ_003386

answers: shear zones

answers: NDQ_003387

answers: strike-slip

answers: NDQ_003388

answers: strike-slip

answers: NDQ_003389

answers: shear zones

answers: NDQ_003390

answers: Detachment fault

answers: NDQ_003391

answers: subduction zone

answers: NDQ_003392

answers: Detachment fault

answers: NDQ_003393

answers: thrust type is the Moine Thrust

answers: NDQ_003394

answers: transform type

answers: NDQ_003395

answers: thrust type is the Moine Thrust

answers: NDQ_003396

answers: thrust type is the Moine Thrust

text: The Management Area includes much of the Tuolumne ultramafic complex, one of the largest exposures of serpentine rocks in the Sierra Nevada metamorphic belt. Nearly the entire area is underlain by dunite, a variety of peridotite consisting of dark green olivine and minor chromite, which has been partly or entirely serpentinized to antigorite magnesite-magnetite. The dunite intruded into andesite pillow breccias and flows of the Peñon Blanco volcanic formation, which crops out near the northeast and southern boundaries of the Management Area. The intrusion of ultramafic material occurred along crustal weaknesses associated with the Bear Mountain fault, a northwestward trending thrust fault that dips steeply to the northeast, and has over 10,000 feet of vertical displacement. The fault zone is on the southwestern boundary of the Management Area, and is believed to have once penetrated the earth's crust down to the mantle, a probable source of the peridotite.

text: The Management Area includes much of the Tuolumne ultramafic complex, one of the largest exposures of

text: serpentine

text: rocks in the Sierra Nevada metamorphic belt. Nearly the entire area is underlain by

text: dunite

text: , a variety of

text: peridotite

text: consisting of dark green

text: olivine

text: and minor

text: chromite

text: , which has been partly or entirely serpentinized to

text: antigorite

text: magnesite

text: magnetite

text: . The dunite intruded into andesite pillow

text: breccia

text: s and flows of the Peñon Blanco volcanic formation, which crops out near the northeast and southern boundaries of the Management Area. The intrusion of

text: ultramafic

text: material occurred along crustal weaknesses associated with the Bear Mountain fault, a northwestward trending

text: thrust fault

text: that dips steeply to the northeast, and has over 10,000 feet of vertical displacement. The fault zone is on the southwestern boundary of the Management Area, and is believed to have once penetrated the earth's crust down to the mantle, a probable source of the peridotite.

answers: NDQ_003351

answers: thrust

answers: NDQ_003352

answers: displacement increases

answers: NDQ_003353

answers: displacement

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: thrust fault

answers: NDQ_003356

answers: dip steeply

answers: NDQ_003357

answers: over 10,000 feet of vertical displacement

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Sierra Nevada metamorphic belt

answers: NDQ_003362

answers: the San Andreas fault is on the southwestern boundary of the Management Area

answers: NDQ_003363

answers: Sierra Nevada

answers: NDQ_003371

answers: What is a probable source of the peridotite?

answers: NDQ_003373

answers: Why is it believed to have once penetrated the earth's crust down to the mantle

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: vertical displacement

answers: NDQ_003379

answers: no

answers: NDQ_003380

answers: What type of force applied to rock is a stress?

answers: NDQ_003381

answers: What type of stress does the Bear Mountain fault cause?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What type of fold is the Bear Mountain fault?

answers: NDQ_003385

answers: yes

answers: NDQ_003386

answers: What is the cause of earthquakes?

answers: NDQ_003387

answers: What type of fault is the Bear Mountain fault?

answers: NDQ_003388

answers: What type of fault is the Bear Mountain fault?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: thrust fault

answers: NDQ_003391

answers: peridotite

answers: NDQ_003392

answers: thrust fault

answers: NDQ_003393

answers: dunite

answers: NDQ_003394

answers: thrust fault

answers: NDQ_003395

answers: thrust fault that dips steeply to the northeast

answers: NDQ_003396

answers: thrust fault

answers: NDQ_003351

answers: thrust fault

answers: NDQ_003352

answers: displacement.

answers: NDQ_003353

answers: crustal weaknesses

answers: NDQ_003354

answers: Pe<unk>on Blanco volcanic formation,

answers: NDQ_003355

answers: thrust fault

answers: NDQ_003356

answers: serpentinized

answers: NDQ_003357

answers: thrust fault that dips steeply to the northeast,

answers: NDQ_003358

answers: fault zone

answers: NDQ_003359

answers: crustal weaknesses

answers: NDQ_003360

answers: Bear Mountain fault,

answers: NDQ_003362

answers: once penetrated the earth's crust down to the mantle,

answers: NDQ_003363

answers: Sierra Nevada metamorphic belt.

answers: NDQ_003371

answers: Bear Mountain fault,

answers: NDQ_003373

answers: crustal weaknesses

answers: NDQ_003376

answers: Bear Mountain fault,

answers: NDQ_003378

answers: vertical displacement.

answers: NDQ_003379

answers: thrust fault that dips steeply to the northeast,

answers: NDQ_003380

answers: vertical displacement.

answers: NDQ_003381

answers: Bear Mountain fault,

answers: NDQ_003382

answers: thrust fault

answers: NDQ_003383

answers: crustal weaknesses

answers: NDQ_003384

answers: northwestward trending thrust fault

answers: NDQ_003385

answers: The fault zone

answers: NDQ_003386

answers: crustal weaknesses

answers: NDQ_003387

answers: thrust fault

answers: NDQ_003388

answers: thrust fault

answers: NDQ_003389

answers: Bear Mountain fault,

answers: NDQ_003390

answers: Bear Mountain fault,

answers: NDQ_003391

answers: Bear Mountain fault,

answers: NDQ_003392

answers: Bear Mountain fault,

answers: NDQ_003393

answers: Bear Mountain fault,

answers: NDQ_003394

answers: Bear Mountain fault,

answers: NDQ_003395

answers: Bear Mountain fault,

answers: NDQ_003396

answers: thrust fault

text: As tectonic plates converge, the closing of an ocean will result in the convergence of two landmasses, each of which is either an island arc or continental margin. When these two bodies collide, the result is orogenesis, at which time the underthrusting oceanic crust slows down.<ref name="Brown and Spadea 1999">{{cite journal |last=Brown|first=D. |last2=Spadea|first2=P |title = Processes of forearc and accretionary complex formation during arc-continent collision in the southern Ural Mountains |journal = Geology |pages= 649–652|year=2013 |volume=27 |doi=10.1130/0091-7613(1999)027

text: As tectonic plates converge, the closing of an ocean will result in the convergence of two landmasses, each of which is either an

text: island arc

text: or continental margin. When these two bodies collide, the result is

text: orogenesis

text: , at which time the underthrusting oceanic crust slows down.<ref name="Brown and Spadea 1999">{{cite journal |last=Brown|first=D. |last2=Spadea|first2=P |title = Processes of forearc and accretionary complex formation during arc-continent collision in the southern Ural Mountains |journal = Geology |pages= 649–652|year=2013 |volume=27 |doi=10.1130/0091-7613(1999)027

answers: NDQ_003351

answers: oceanic crust

answers: NDQ_003352

answers: slows down

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: continental margin

answers: NDQ_003356

answers: Converge

answers: NDQ_003357

answers: underthrusting oceanic crust slows down

answers: NDQ_003358

answers: island arc

answers: NDQ_003359

answers: collides with another

answers: NDQ_003360

answers: oceanic crust

answers: NDQ_003362

answers: underthrusting oceanic crust slows down

answers: NDQ_003363

answers: Ural Mountains

answers: NDQ_003371

answers: What is a thrust fault?

answers: NDQ_003373

answers: What is the result of a deep buried rock?

answers: NDQ_003376

answers: The terrain known as basin-and-range is caused by compressive forces.

answers: NDQ_003378

answers: What is the term for the amount the ground moves in an earthquake?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What is a stress?

answers: NDQ_003381

answers: What is the result of confining stress?

answers: NDQ_003382

answers: It's impossible to say

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What type of fold is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: tectonic plates collide

answers: NDQ_003387

answers: What is the cause of normal faults?

answers: NDQ_003388

answers: ref name="Brown and Spadea 1999">

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: tectonic plate

answers: NDQ_003391

answers: dip-slip fault

answers: NDQ_003392

answers: tectonic plate

answers: NDQ_003393

answers: tectonic plate

answers: NDQ_003394

answers: tectonic plate

answers: NDQ_003395

answers: tectonic plate

answers: NDQ_003396

answers: is a type of fault

answers: NDQ_003351

answers: orogenesis,

answers: NDQ_003352

answers: slows down.

answers: NDQ_003353

answers: the underthrusting oceanic crust slows down.

answers: NDQ_003354

answers: arc-continent collision in the southern Ural Mountains

answers: NDQ_003355

answers: continental margin.

answers: NDQ_003356

answers: the underthrusting oceanic crust slows down.

answers: NDQ_003357

answers: the underthrusting oceanic crust slows down.

answers: NDQ_003358

answers: orogenesis,

answers: NDQ_003359

answers: arc-continent collision

answers: NDQ_003360

answers: tectonic plates

answers: NDQ_003362

answers: convergence of two landmasses,

answers: NDQ_003363

answers: tectonic plates converge,

answers: NDQ_003371

answers: arc-continent collision in the southern Ural Mountains

answers: NDQ_003373

answers: underthrusting oceanic crust

answers: NDQ_003376

answers: arc-continent collision in the southern Ural Mountains

answers: NDQ_003378

answers: orogenesis,

answers: NDQ_003379

answers: arc-continent collision in the southern Ural Mountains

answers: NDQ_003380

answers: arc-continent collision in the southern Ural Mountains

answers: NDQ_003381

answers: the underthrusting oceanic crust slows down.

answers: NDQ_003382

answers: orogenesis,

answers: NDQ_003383

answers: arc-continent collision in the southern Ural Mountains

answers: NDQ_003384

answers: island arc

answers: NDQ_003385

answers: island arc or continental margin.

answers: NDQ_003386

answers: tectonic plates

answers: NDQ_003387

answers: orogenesis,

answers: NDQ_003388

answers: arc-continent collision in the southern Ural Mountains

answers: NDQ_003389

answers: arc-continent collision in the southern Ural Mountains

answers: NDQ_003390

answers: arc-continent collision in the southern Ural Mountains

answers: NDQ_003391

answers: oceanic crust

answers: NDQ_003392

answers: arc-continent collision in the southern Ural Mountains

answers: NDQ_003393

answers: orogenesis,

answers: NDQ_003394

answers: arc-continent collision in the southern Ural Mountains

answers: NDQ_003395

answers: arc-continent collision in the southern Ural Mountains

answers: NDQ_003396

answers: arc-continent collision in the southern Ural Mountains

text: To fold is to discard one's hand and forfeit interest in the current pot. No further bets are required by the folding player, but the player cannot win.  Folding may be indicated verbally or by discarding one's hand face down into the pile of other discards called the muck, or into the pot (uncommon). For this reason it is also called mucking.  In stud poker played in the United States, it is customary to signal folding by turning all of one's cards face down. Once a person indicates a fold or states  I fold, that person cannot re-enter the hand. In casinos in the United Kingdom, a player folds by giving their hand as is to the "house" dealer, who spreads the cards face up for the other players to see before mucking them.

text: To fold is to discard one's hand and forfeit interest in the current pot. No further bets are required by the folding player, but the player cannot win.  Folding may be indicated verbally or by discarding one's hand face down into the pile of other discards called the muck, or into the pot (uncommon). For this reason it is also called mucking.  In

text: stud poker

text: played in the

text: United States

text: , it is customary to signal folding by turning all of one's cards face down. Once a person indicates a fold or states  I fold, that person cannot re-enter the hand. In

text: casino

text: s in the

text: United Kingdom

text: , a player folds by giving their hand as is to the "house" dealer, who spreads the cards face up for the other players to see before mucking them.

answers: NDQ_003351

answers: uncommon

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: igneous rocks to form

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: muck

answers: NDQ_003356

answers: fold

answers: NDQ_003357

answers: How many cards does the "house" dealer spread before mucking?

answers: NDQ_003358

answers: muck

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's surface

answers: NDQ_003362

answers: unanswerable

answers: NDQ_003363

answers: unanswerable

answers: NDQ_003371

answers: What may be the reason for a thrust fault?

answers: NDQ_003373

answers: How would you describe the stress?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: How does rock deform?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: unanswerable

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: Which of the following is not a cause of normal faults?

answers: NDQ_003388

answers: What type of stress is shear stress?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: uncommon

answers: NDQ_003391

answers: dip-slip fault plane

answers: NDQ_003392

answers: stud poker

answers: NDQ_003393

answers: muck

answers: NDQ_003394

answers: uncommon

answers: NDQ_003395

answers: unanswerable

answers: NDQ_003396

answers: uncommon

answers: NDQ_003351

answers: pot

answers: NDQ_003352

answers: mucking. In stud poker

answers: NDQ_003353

answers: To fold

answers: NDQ_003354

answers: stud poker played in the United States,

answers: NDQ_003355

answers: mucking.

answers: NDQ_003356

answers: mucking. In stud poker

answers: NDQ_003357

answers: the player cannot win.

answers: NDQ_003358

answers: muck,

answers: NDQ_003359

answers: To fold

answers: NDQ_003360

answers: To fold

answers: NDQ_003362

answers: the player cannot win.

answers: NDQ_003363

answers: To fold

answers: NDQ_003371

answers: To fold

answers: NDQ_003373

answers: To fold

answers: NDQ_003376

answers: muck,

answers: NDQ_003378

answers: muck,

answers: NDQ_003379

answers: spreads the cards face up

answers: NDQ_003380

answers: To fold

answers: NDQ_003381

answers: To fold

answers: NDQ_003382

answers: muck, or into the pot

answers: NDQ_003383

answers: To fold

answers: NDQ_003384

answers: stud poker

answers: NDQ_003385

answers: muck,

answers: NDQ_003386

answers: To fold

answers: NDQ_003387

answers: To fold

answers: NDQ_003388

answers: To fold

answers: NDQ_003389

answers: muck,

answers: NDQ_003390

answers: To fold

answers: NDQ_003391

answers: muck,

answers: NDQ_003392

answers: To fold

answers: NDQ_003393

answers: mucking. In stud poker played in the United States,

answers: NDQ_003394

answers: To fold

answers: NDQ_003395

answers: To fold

answers: NDQ_003396

answers: To fold

text: The Tibetan Plateau is an area of thickened continental crust, a result of the ongoing collision of the Indo-Australian Plate with the Eurasian Plate. The way in which this zone accommodates the collision remains unclear with two end-member models being proposed. The first regards the crust as being made up of a mosaic of strong blocks separated by weak fault zones, the 'microplate' model. The second regards the deformation as being continuous within the mid to lower crust, the 'continuum' model. The change in width of the deformed zone along the collisional belt, with the narrow zone of western Tibet compared to the main part of the Tibetan Plateau, is explained as either lateral escape to the east along the Altyn Tagh and Karakorum faults in the microplate model or as the effect of the rigid Tarim Basin block causing heterogeneous deformation within a generally weaker lithosphere in the continuum model. The rate of displacement along the major fault zones such as the Altyn Tagh and Kunlun faults compared to the degree of distributed deformation of the intervening crust is critical to discriminating between these two models.

text: The Tibetan Plateau is an area of thickened

text: continental crust

text: , a result of the ongoing collision of the

text: Indo-Australian Plate

text: with the

text: Eurasian Plate

text: . The way in which this zone accommodates the collision remains unclear with two end-member models being proposed. The first regards the crust as being made up of a mosaic of strong blocks separated by weak fault zones, the 'microplate' model. The second regards the deformation as being continuous within the mid to lower crust, the 'continuum' model. The change in width of the deformed zone along the collisional belt, with the narrow zone of western Tibet compared to the main part of the Tibetan Plateau, is explained as either lateral escape to the east along the Altyn Tagh and Karakorum faults in the microplate model or as the effect of the rigid Tarim Basin block causing heterogeneous deformation within a generally weaker lithosphere in the continuum model. The rate of displacement along the major fault zones such as the Altyn Tagh and

text: Kunlun fault

text: s compared to the degree of distributed deformation of the intervening crust is critical to discriminating between these two models.

answers: NDQ_003351

answers: weak fault zones

answers: NDQ_003352

answers: deforms

answers: NDQ_003353

answers: deformation

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fault

answers: NDQ_003356

answers: lateral escape

answers: NDQ_003357

answers: The rate of displacement along the major fault zones is critical to discriminating between which two models?

answers: NDQ_003358

answers: weak fault zones

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: continental crust

answers: NDQ_003362

answers: unanswerable

answers: NDQ_003363

answers: the Indo-Australian Plate

answers: NDQ_003371

answers: What type of model is the Tibetan Plateau?

answers: NDQ_003373

answers: What is the 'continuum' model?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: What is the dip of the fault plane

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What happens to rock when confining stress occurs?

answers: NDQ_003382

answers: What is the most common stress at convergent plates

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: faults are the cause of earthquakes

answers: NDQ_003387

answers: What are normal faults caused by?

answers: NDQ_003388

answers: What type of faults do strike-slip faults result from?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: Karakorum faults

answers: NDQ_003391

answers: Tarim Basin

answers: NDQ_003392

answers: Karakorum

answers: NDQ_003393

answers: Tarim Basin

answers: NDQ_003394

answers: Karakorum faults

answers: NDQ_003395

answers: Karakorum faults

answers: NDQ_003396

answers: Karakorum faults

answers: NDQ_003351

answers: weak fault zones,

answers: NDQ_003352

answers: displacement

answers: NDQ_003353

answers: heterogeneous deformation

answers: NDQ_003354

answers: The Tibetan Plateau

answers: NDQ_003355

answers: faults

answers: NDQ_003356

answers: lateral escape to the east

answers: NDQ_003357

answers: weak fault zones,

answers: NDQ_003358

answers: the'microplate'

answers: NDQ_003359

answers: distributed deformation

answers: NDQ_003360

answers: collision of the Indo-Australian Plate with the Eurasian Plate.

answers: NDQ_003362

answers: weak fault zones,

answers: NDQ_003363

answers: collision of the Indo-Australian Plate with the Eurasian Plate.

answers: NDQ_003371

answers: weak fault zones,

answers: NDQ_003373

answers: continuous within the mid to lower crust,

answers: NDQ_003376

answers: collision of the Indo-Australian Plate with the Eurasian Plate.

answers: NDQ_003378

answers: displacement

answers: NDQ_003379

answers: the'microplate' model.

answers: NDQ_003380

answers: deformation

answers: NDQ_003381

answers: heterogeneous deformation

answers: NDQ_003382

answers: collision of the Indo-Australian Plate with the Eurasian Plate.

answers: NDQ_003383

answers: weak fault zones,

answers: NDQ_003384

answers: collision of the Indo-Australian Plate with the Eurasian Plate.

answers: NDQ_003385

answers: fault zones

answers: NDQ_003386

answers: weak fault zones,

answers: NDQ_003387

answers: weak fault zones,

answers: NDQ_003388

answers: collision of the Indo-Australian Plate with the Eurasian Plate.

answers: NDQ_003389

answers: collision of the Indo-Australian Plate with the Eurasian Plate.

answers: NDQ_003390

answers: Altyn Tagh and Karakorum faults

answers: NDQ_003391

answers: Tarim Basin

answers: NDQ_003392

answers: Altyn Tagh and Karakorum faults

answers: NDQ_003393

answers: Tarim Basin

answers: NDQ_003394

answers: Altyn Tagh and Karakorum faults

answers: NDQ_003395

answers: Altyn Tagh and Karakorum faults

answers: NDQ_003396

answers: Karakorum faults

text: Block mountains are caused by faults in the crust: a seam where rocks can move past each other. When rocks on one side of a fault rise relative to the other, it can form a mountain. The uplifted blocks are block mountains or horsts. The intervening dropped blocks are termed graben: these can be small or form extensive rift valley systems. This form of landscape can be seen in East Africa, the Vosges, the Basin and Range Province of Western North America and the Rhine valley. These areas often occur when the regional stress is extensional and the crust is thinned.

text: Block mountains are caused by

text: faults

text: in the crust: a seam where rocks can move past each other. When rocks on one side of a fault rise relative to the other, it can form a mountain. The uplifted blocks are block mountains or

text: horsts

text: . The intervening dropped blocks are termed

text: graben

text: : these can be small or form extensive

text: rift valley

text: systems. This form of

text: landscape

text: can be seen in

text: East Africa

text: , the

text: Vosges

text: , the

text: Basin and Range Province

text: of Western

text: North America

text: and the

text: Rhine

text: valley. These areas often occur when the regional stress is extensional and the

text: crust

text: is thinned.

answers: NDQ_003351

answers: extensional

answers: NDQ_003352

answers: rises

answers: NDQ_003353

answers: faults

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: graben

answers: NDQ_003356

answers: move past each other

answers: NDQ_003357

answers: rocks can move past each other

answers: NDQ_003358

answers: unanswerable

answers: NDQ_003359

answers: move past each other

answers: NDQ_003360

answers: faults

answers: NDQ_003362

answers: Block mountains are caused by faults in the crust

answers: NDQ_003363

answers: faults

answers: NDQ_003371

answers: Which of the following is not a type of block mountain?

answers: NDQ_003373

answers: Which of the following is not a type of rock: block mountains or horsts?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: What can be seen in East Africa?

answers: NDQ_003379

answers: What is the dip of the fault plane in a strike-slip fault

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: Which of the following is not a type of block mountain: block mountains or horsts?

answers: NDQ_003382

answers: Which of the following is not a type of mountain: block mountains or horsts?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not a type of mountain: block mountains or horsts?

answers: NDQ_003385

answers: Which of the following is not a type of mountain?

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: Which of the following is not a type of block mountain?

answers: NDQ_003388

answers: Which of the following is not a type of fault: block mountains or horsts?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: graben

answers: NDQ_003391

answers: graben

answers: NDQ_003392

answers: graben

answers: NDQ_003393

answers: block mountains

answers: NDQ_003394

answers: extensional

answers: NDQ_003395

answers: block mountains

answers: NDQ_003396

answers: graben

answers: NDQ_003351

answers: extensional

answers: NDQ_003352

answers: rise relative to the other,

answers: NDQ_003353

answers: faults

answers: NDQ_003354

answers: Block mountains

answers: NDQ_003355

answers: graben:

answers: NDQ_003356

answers: rise relative to the other, it can form a mountain.

answers: NDQ_003357

answers: rocks on one side of a fault rise relative to the other,

answers: NDQ_003358

answers: graben:

answers: NDQ_003359

answers: move past each other.

answers: NDQ_003360

answers: faults

answers: NDQ_003362

answers: Block mountains

answers: NDQ_003363

answers: faults

answers: NDQ_003371

answers: Block mountains

answers: NDQ_003373

answers: Block mountains

answers: NDQ_003376

answers: extensional

answers: NDQ_003378

answers: Block mountains

answers: NDQ_003379

answers: extensional

answers: NDQ_003380

answers: stress is extensional

answers: NDQ_003381

answers: extensional

answers: NDQ_003382

answers: extensional

answers: NDQ_003383

answers: extensional

answers: NDQ_003384

answers: graben:

answers: NDQ_003385

answers: Block mountains are caused by faults

answers: NDQ_003386

answers: Block mountains

answers: NDQ_003387

answers: extensional

answers: NDQ_003388

answers: extensional

answers: NDQ_003389

answers: faults

answers: NDQ_003390

answers: graben:

answers: NDQ_003391

answers: graben:

answers: NDQ_003392

answers: horsts.

answers: NDQ_003393

answers: horsts.

answers: NDQ_003394

answers: faults

answers: NDQ_003395

answers: Block mountains are caused by faults

answers: NDQ_003396

answers: graben:

text: Even the stiffest of rock is not perfectly rigid.  Given a large force (such as between two immense tectonic plates moving past each other) the earth's crust will bend or deform. According to the elastic rebound theory of , eventually the deformation (strain) becomes great enough that something breaks, usually at an existing fault.  Slippage along the break (an earthquake) allows the rock on each side to rebound to a less deformed state. In the process energy is released in various forms, including seismic waves. The cycle of tectonic force being accumulated in elastic deformation and released in a sudden rebound is then repeated. As the displacement from a single earthquake ranges from less than a meter to around 10 meters (for an M 8 quake), the demonstrated existence of large strike-slip displacements of hundreds of miles shows the existence of a long running earthquake cycle.

text: Even the stiffest of rock is not perfectly rigid.  Given a large force (such as between two immense tectonic plates moving past each other) the earth's crust will bend or deform. According to the

text: elastic rebound

text: theory of , eventually the deformation (strain) becomes great enough that something breaks, usually at an existing fault.  Slippage along the break (an earthquake) allows the rock on each side to rebound to a less deformed state. In the process energy is released in various forms, including seismic waves. The cycle of tectonic force being accumulated in elastic deformation and released in a sudden rebound is then repeated. As the displacement from a single earthquake ranges from less than a meter to around 10 meters (for an M 8 quake), the demonstrated existence of large

text: strike-slip

text: displacements of hundreds of miles shows the existence of a long running earthquake cycle.

answers: NDQ_003351

answers: elastic deformation

answers: NDQ_003352

answers: breaks

answers: NDQ_003353

answers: deformation

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: earthquake

answers: NDQ_003356

answers: break

answers: NDQ_003357

answers: tectonic plates moving past each other

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: deforms

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: tectonic plates moving past each other

answers: NDQ_003363

answers: given a large force

answers: NDQ_003371

answers: What is the cycle of tectonic force being accumulated in elastic deformation?

answers: NDQ_003373

answers: given a large force

answers: NDQ_003376

answers: given a large force (such as between two immense tectonic plates moving past each other

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What does the earth's crust do when confining stress occurs?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: what does elastic rebound theory mean?

answers: NDQ_003384

answers: What type of fold is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: given a large force

answers: NDQ_003387

answers: Which of the following is not caused by compression stress?

answers: NDQ_003388

answers: Which of the following is not a result of shear stress?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: strike-slip

answers: NDQ_003391

answers: tectonic plate

answers: NDQ_003392

answers: strike-slip

answers: NDQ_003393

answers: Earth's crust

answers: NDQ_003394

answers: strike-slip

answers: NDQ_003395

answers: tectonic plate

answers: NDQ_003396

answers: strike-slip

answers: NDQ_003351

answers: elastic rebound theory

answers: NDQ_003352

answers: bend or deform.

answers: NDQ_003353

answers: bend or deform.

answers: NDQ_003354

answers: Even the stiffest of rock is not perfectly rigid.

answers: NDQ_003355

answers: earthquake)

answers: NDQ_003356

answers: something breaks,

answers: NDQ_003357

answers: allows the rock on each side to rebound to a less deformed state.

answers: NDQ_003358

answers: earthquake)

answers: NDQ_003359

answers: existing fault.

answers: NDQ_003360

answers: tectonic plates moving past each other)

answers: NDQ_003362

answers: long running earthquake cycle.

answers: NDQ_003363

answers: tectonic plates

answers: NDQ_003371

answers: two immense tectonic plates

answers: NDQ_003373

answers: Even the stiffest of rock is not perfectly rigid.

answers: NDQ_003376

answers: tectonic plates

answers: NDQ_003378

answers: Slippage

answers: NDQ_003379

answers: elastic rebound theory

answers: NDQ_003380

answers: deformation

answers: NDQ_003381

answers: a large force

answers: NDQ_003382

answers: elastic rebound theory

answers: NDQ_003383

answers: something breaks,

answers: NDQ_003384

answers: tectonic plates

answers: NDQ_003385

answers: fault.

answers: NDQ_003386

answers: Slippage along the break

answers: NDQ_003387

answers: elastic rebound theory

answers: NDQ_003388

answers: elastic rebound theory

answers: NDQ_003389

answers: bend

answers: NDQ_003390

answers: fault.

answers: NDQ_003391

answers: rock on each side to rebound to a less deformed state.

answers: NDQ_003392

answers: fault.

answers: NDQ_003393

answers: rock on each side to rebound to a less deformed state.

answers: NDQ_003394

answers: fault.

answers: NDQ_003395

answers: fault.

answers: NDQ_003396

answers: fault.

text: Zealandia is largely made up of two nearly parallel ridges, separated by a failed rift, where the rift breakup of the continent stops and becomes a filled graben. The ridges rise above the sea floor to heights of , with infrequent rocky islands rising above sea level. The ridges are continental rock, but are lower in elevation than normal continents because their crust is thinner than usual, approximately  thick, and consequently they do not float as high above the Earth's mantle.

text: Zealandia is largely made up of two nearly parallel ridges, separated by a

text: failed

text: rift

text: , where the rift breakup of the continent stops and becomes a filled

text: graben

text: . The ridges rise above the

text: sea floor

text: to heights of , with infrequent rocky

text: island

text: s rising above

text: sea level

text: . The ridges are continental rock, but are lower in elevation than normal continents because their crust is thinner than usual, approximately  thick, and consequently they do not float as high above the Earth's

text: mantle

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: graben

answers: NDQ_003356

answers: float

answers: NDQ_003357

answers: the rift breakup of the continent stops

answers: NDQ_003358

answers: rift

answers: NDQ_003359

answers: fails

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: the rift breakup of the continent stops and becomes a filled graben

answers: NDQ_003363

answers: a failed rift

answers: NDQ_003371

answers: Which of the following is not a type of ridge: parallel ridges, separated by a failed rift, or filled graben?

answers: NDQ_003373

answers: Why are the ridges lower in elevation?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What would happen if the rift breakup of the continent stops?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: rift breakup of the continent stops and becomes a filled graben

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip, rift, or graben?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: rift

answers: NDQ_003391

answers: fill graben

answers: NDQ_003392

answers: rift

answers: NDQ_003393

answers: ridges

answers: NDQ_003394

answers: rift

answers: NDQ_003395

answers: fill graben

answers: NDQ_003396

answers: a filled graben

answers: NDQ_003351

answers: rift breakup of the continent stops and becomes a filled graben.

answers: NDQ_003352

answers: float as high above the Earth's mantle.

answers: NDQ_003353

answers: crust is thinner than usual,

answers: NDQ_003354

answers: rocky islands rising above sea level.

answers: NDQ_003355

answers: graben.

answers: NDQ_003356

answers: float as high above the Earth's mantle.

answers: NDQ_003357

answers: rift breakup of the continent stops and becomes a filled graben.

answers: NDQ_003358

answers: failed rift,

answers: NDQ_003359

answers: failed rift,

answers: NDQ_003360

answers: a failed rift,

answers: NDQ_003362

answers: rift breakup of the continent stops and becomes a filled graben.

answers: NDQ_003363

answers: a failed rift,

answers: NDQ_003371

answers: failed rift,

answers: NDQ_003373

answers: float as high above the Earth's mantle.

answers: NDQ_003376

answers: filled graben.

answers: NDQ_003378

answers: rift,

answers: NDQ_003379

answers: of, with infrequent rocky islands rising above sea level.

answers: NDQ_003380

answers: continental rock,

answers: NDQ_003381

answers: float as high above the Earth's mantle.

answers: NDQ_003382

answers: rift,

answers: NDQ_003383

answers: rift breakup of the continent stops and becomes a filled graben.

answers: NDQ_003384

answers: filled graben.

answers: NDQ_003385

answers: rift,

answers: NDQ_003386

answers: rift breakup

answers: NDQ_003387

answers: rift breakup of the continent stops and becomes a filled graben.

answers: NDQ_003388

answers: rift breakup of the continent stops and becomes a filled graben.

answers: NDQ_003389

answers: rift,

answers: NDQ_003390

answers: failed rift,

answers: NDQ_003391

answers: filled graben.

answers: NDQ_003392

answers: failed rift,

answers: NDQ_003393

answers: continental rock,

answers: NDQ_003394

answers: rift,

answers: NDQ_003395

answers: rift,

answers: NDQ_003396

answers: rift,

text: In 2004, work began just north of Parkfield on the San Andreas Fault Observatory at Depth (SAFOD). The goal of SAFOD is to drill a hole nearly 3 km (2 mi) into the Earth's crust and into the San Andreas Fault. An array of sensors will be installed to record earthquakes that happen near this area.

text: In 2004, work began just north of Parkfield on the

text: San Andreas Fault Observatory at Depth

text: (SAFOD). The goal of SAFOD is to drill a hole nearly 3 km (2 mi) into the Earth's crust and into the San Andreas Fault. An array of sensors will be installed to record earthquakes that happen near this area.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: fold that bends downward

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: San Andreas Fault is a type of

answers: NDQ_003358

answers: Fault

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: San Andreas fault

answers: NDQ_003362

answers: The goal of SAFOD is to drill a hole nearly 3 km

answers: NDQ_003363

answers: San Andreas Fault

answers: NDQ_003371

answers: Which of the following is not a type of fault: San Andreas Fault Observatory at Depth or San Andreas Fault?

answers: NDQ_003373

answers: Why is the San Andreas Fault Observatory at Depth (SAFOD) being built?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: what is the first word in the first paragraph?

answers: NDQ_003379

answers: Which of the following is not a type of strike-slip fault?

answers: NDQ_003380

answers: What is the purpose of the San Andreas Fault Observatory at Depth?

answers: NDQ_003381

answers: What is the purpose of drilling a hole into the Earth's crust?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: What is the purpose of the San Andreas Fault Observatory at Depth?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: What is the San Andreas Fault?

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: San Andreas Fault or normal faults?

answers: NDQ_003388

answers: What type of fault does the San Andreas Fault Observatory at Depth (SAFOD) study?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: San Andreas Fault

answers: NDQ_003391

answers: San Andreas Fault

answers: NDQ_003392

answers: a hanging wall

answers: NDQ_003393

answers: San Andreas fault

answers: NDQ_003394

answers: San Andreas Fault

answers: NDQ_003395

answers: San Andreas Fault

answers: NDQ_003396

answers: San Andreas Fault

answers: NDQ_003351

answers: earthquakes

answers: NDQ_003352

answers: earthquakes

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: San Andreas Fault Observatory at Depth

answers: NDQ_003355

answers: Fault Observatory at Depth

answers: NDQ_003356

answers: earthquakes

answers: NDQ_003357

answers: earthquakes

answers: NDQ_003358

answers: earthquakes

answers: NDQ_003359

answers: San Andreas Fault.

answers: NDQ_003360

answers: San Andreas Fault

answers: NDQ_003362

answers: 3 km (2 mi) into the Earth's crust

answers: NDQ_003363

answers: San Andreas Fault.

answers: NDQ_003371

answers: San Andreas Fault.

answers: NDQ_003373

answers: 3 km (2 mi) into the Earth's crust

answers: NDQ_003376

answers: San Andreas Fault Observatory at Depth

answers: NDQ_003378

answers: earthquakes

answers: NDQ_003379

answers: San Andreas Fault Observatory at Depth

answers: NDQ_003380

answers: earthquakes

answers: NDQ_003381

answers: San Andreas Fault Observatory at Depth

answers: NDQ_003382

answers: San Andreas Fault Observatory at Depth

answers: NDQ_003383

answers: San Andreas Fault Observatory at Depth

answers: NDQ_003384

answers: San Andreas Fault Observatory at Depth

answers: NDQ_003385

answers: San Andreas Fault.

answers: NDQ_003386

answers: earthquakes

answers: NDQ_003387

answers: San Andreas Fault.

answers: NDQ_003388

answers: San Andreas Fault.

answers: NDQ_003389

answers: San Andreas Fault.

answers: NDQ_003390

answers: San Andreas Fault

answers: NDQ_003391

answers: San Andreas Fault.

answers: NDQ_003392

answers: San Andreas Fault.

answers: NDQ_003393

answers: San Andreas Fault.

answers: NDQ_003394

answers: San Andreas Fault

answers: NDQ_003395

answers: San Andreas Fault.

answers: NDQ_003396

answers: San Andreas Fault

text: The type of dominating deformation process also has a great impact on the types of rocks and structures found at certain depths within the Earth's crust. As evident from Fig. 1.1, different geological formations and rocks are found in accordance to the dominant deformation process. Gouge and Breccia form in the uppermost, brittle regime while Cataclasite and Pseudotachylite form in the lower parts of the brittle regime, edging upon the transition zone. Mylonite forms in the more ductile regime at greater depths while Blastomylonite forms well past the transition zone and well into the ductile regime, even deeper into the crust.

text: The type of dominating deformation process also has a great impact on the types of rocks and structures found at certain depths within the Earth's crust. As evident from Fig. 1.1, different geological formations and rocks are found in accordance to the dominant deformation process. Gouge and

text: Breccia

text: form in the uppermost, brittle regime while

text: Cataclasite

text: and

text: Pseudotachylite

text: form in the lower parts of the brittle regime, edging upon the transition zone.

text: Mylonite

text: forms in the more ductile regime at greater depths while Blastomylonite forms well past the transition zone and well into the ductile regime, even deeper into the crust.

answers: NDQ_003351

answers: brittle regime

answers: NDQ_003352

answers: brittle

answers: NDQ_003353

answers: brittle regime

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: Gouge

answers: NDQ_003356

answers: brittle

answers: NDQ_003357

answers: Cataclasite and Pseudotachylite form in the lower parts of the brittle regime

answers: NDQ_003358

answers: Gouge

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: dominant deformation process

answers: NDQ_003362

answers: ductile regime at greater depths

answers: NDQ_003363

answers: ductile regime

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: ductile regime

answers: NDQ_003376

answers: basin-and-range

answers: NDQ_003378

answers: what is the amount the ground moves in an earthquake

answers: NDQ_003379

answers: strike-slip fault

answers: NDQ_003380

answers: What type of force applied to rock is a stress?

answers: NDQ_003381

answers: What type of deformation process occurs when confining stress occurs?

answers: NDQ_003382

answers: ductile regime at greater depths

answers: NDQ_003383

answers: Gouge and Breccia

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: Fault zone

answers: NDQ_003386

answers: What is the cause of earthquakes?

answers: NDQ_003387

answers: Gouge and Breccia form in the uppermost, brittle regime

answers: NDQ_003388

answers: Gouge and Breccia form in the uppermost, brittle regime

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: Gouge

answers: NDQ_003391

answers: Cataclasite

answers: NDQ_003392

answers: Gouge

answers: NDQ_003393

answers: Gouge and Breccia

answers: NDQ_003394

answers: Blastomylonite

answers: NDQ_003395

answers: Fig. 1.1

answers: NDQ_003396

answers: Breccia

answers: NDQ_003351

answers: brittle regime

answers: NDQ_003352

answers: brittle

answers: NDQ_003353

answers: brittle regime

answers: NDQ_003354

answers: Cataclasite and Pseudotachylite

answers: NDQ_003355

answers: Gouge and Breccia

answers: NDQ_003356

answers: ductile

answers: NDQ_003357

answers: brittle regime, edging upon the transition zone.

answers: NDQ_003358

answers: brittle regime

answers: NDQ_003359

answers: dominating deformation

answers: NDQ_003360

answers: dominating deformation process

answers: NDQ_003362

answers: brittle regime

answers: NDQ_003363

answers: brittle regime

answers: NDQ_003371

answers: The type of dominating deformation process

answers: NDQ_003373

answers: ductile

answers: NDQ_003376

answers: brittle regime

answers: NDQ_003378

answers: rocks and structures found at certain depths within the Earth's crust.

answers: NDQ_003379

answers: Fig. 1.1,

answers: NDQ_003380

answers: deformation

answers: NDQ_003381

answers: brittle regime

answers: NDQ_003382

answers: brittle regime

answers: NDQ_003383

answers: brittle regime

answers: NDQ_003384

answers: Cataclasite and Pseudotachylite

answers: NDQ_003385

answers: transition zone.

answers: NDQ_003386

answers: The type of dominating deformation

answers: NDQ_003387

answers: brittle regime

answers: NDQ_003388

answers: Cataclasite and Pseudotachylite

answers: NDQ_003389

answers: The type of dominating deformation

answers: NDQ_003390

answers: The type of dominating deformation

answers: NDQ_003391

answers: Blastomylonite

answers: NDQ_003392

answers: dominating deformation

answers: NDQ_003393

answers: Gouge and Breccia

answers: NDQ_003394

answers: Fig. 1.1,

answers: NDQ_003395

answers: Fig. 1.1,

answers: NDQ_003396

answers: Cataclasite and Pseudotachylite

text: The Pernambuco-Alagoas domain, part of the Borborema Province, is primarily made of rocks aged between 1,600 and 1,000 million years, significantly younger than the areas to the north and south.The Pernambuco fault in this domain is a continuation of the Foumban Shear Zone in Cameroon, itself the western end of the Central African Shear Zone.To the west, the fault splays into numerous faults along a distance of about 50 km, suggesting that the crust was weak at this point, which is on the line where South America separated from Africa around 115 million years ago.

text: The Pernambuco-Alagoas domain, part of the

text: Borborema Province

text: , is primarily made of rocks aged between 1,600 and 1,000 million years, significantly younger than the areas to the north and south.The Pernambuco fault in this domain is a continuation of the

text: Foumban Shear Zone

text: in

text: Cameroon

text: , itself the western end of the

text: Central African Shear Zone

text: .To the west, the fault splays into numerous faults along a distance of about 50 km, suggesting that the crust was weak at this point, which is on the line where

text: South America

text: separated from

text: Africa

text: around 115 million years ago.

answers: NDQ_003351

answers: Shear

answers: NDQ_003352

answers: more likely to crack

answers: NDQ_003353

answers: Shear

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: Shear

answers: NDQ_003356

answers: Shear

answers: NDQ_003357

answers: splays into numerous faults along a distance of about 50 km

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: weakens

answers: NDQ_003360

answers: faults

answers: NDQ_003362

answers: South America separated from Africa around 115 million years ago.

answers: NDQ_003363

answers: 115 million years ago

answers: NDQ_003371

answers: What is the Pernambuco fault in this domain?

answers: NDQ_003373

answers: How would you describe the Pernambuco fault?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: How old is the Pernambuco fault?

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What type of force applied to rock is a stress?

answers: NDQ_003381

answers: How does the Pernambuco fault in this domain deform?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: How would you describe the Pernambuco fault?

answers: NDQ_003384

answers: What type of fold is the Foumban Shear Zone?

answers: NDQ_003385

answers: yes

answers: NDQ_003386

answers: What is the Pernambuco fault?

answers: NDQ_003387

answers: What type of stress does the Pernambuco fault cause?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip faults or strike-slip faults?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: Pernambuco fault

answers: NDQ_003391

answers: Shear zone

answers: NDQ_003392

answers: Foumban

answers: NDQ_003393

answers: splays

answers: NDQ_003394

answers: Pernambuco fault

answers: NDQ_003395

answers: Foumban Shear Zone

answers: NDQ_003396

answers: Central African Shear Zone

answers: NDQ_003351

answers: Foumban Shear Zone

answers: NDQ_003352

answers: weak

answers: NDQ_003353

answers: faults

answers: NDQ_003354

answers: Foumban Shear Zone

answers: NDQ_003355

answers: fault

answers: NDQ_003356

answers: faults

answers: NDQ_003357

answers: 50 km,

answers: NDQ_003358

answers: south.The Pernambuco fault

answers: NDQ_003359

answers: weak

answers: NDQ_003360

answers: Foumban Shear Zone

answers: NDQ_003362

answers: weak

answers: NDQ_003363

answers: South America separated from Africa around 115 million years ago.

answers: NDQ_003371

answers: south.The Pernambuco fault

answers: NDQ_003373

answers: Foumban Shear Zone

answers: NDQ_003376

answers: Foumban Shear Zone

answers: NDQ_003378

answers: Foumban Shear Zone

answers: NDQ_003379

answers: Foumban Shear Zone

answers: NDQ_003380

answers: faults

answers: NDQ_003381

answers: Foumban Shear Zone

answers: NDQ_003382

answers: Foumban Shear Zone

answers: NDQ_003383

answers: faults

answers: NDQ_003384

answers: Foumban Shear Zone

answers: NDQ_003385

answers: Foumban Shear Zone

answers: NDQ_003386

answers: the crust was weak

answers: NDQ_003387

answers: Foumban Shear Zone

answers: NDQ_003388

answers: Foumban Shear Zone

answers: NDQ_003389

answers: Foumban Shear Zone

answers: NDQ_003390

answers: Pernambuco fault

answers: NDQ_003391

answers: Foumban Shear Zone

answers: NDQ_003392

answers: Pernambuco fault

answers: NDQ_003393

answers: Foumban Shear Zone

answers: NDQ_003394

answers: south.The Pernambuco fault

answers: NDQ_003395

answers: south.The Pernambuco fault

answers: NDQ_003396

answers: Foumban Shear Zone

text: A special class of strike-slip faults is the transform fault, where such faults form a plate boundary. These are found related to offsets in spreading centers, such as mid-ocean ridges, and less commonly within continental lithosphere, such as the Dead Sea Transform in the Middle East, or the Alpine Fault, New Zealand. Transform faults are also referred to as conservative plate boundaries, as lithosphere is neither created nor destroyed.

text: A special class of strike-slip faults is the

text: transform fault

text: , where such faults form a

text: plate

text: boundary. These are found related to offsets in

text: spreading center

text: s, such as

text: mid-ocean ridge

text: s, and less commonly within continental

text: lithosphere

text: , such as the

text: Dead Sea Transform

text: in the

text: Middle East

text: , or the

text: Alpine Fault

text: New Zealand

text: . Transform faults are also referred to as conservative plate boundaries, as lithosphere is neither created nor destroyed.

answers: NDQ_003351

answers: strike-slip

answers: NDQ_003352

answers: is likely to crack

answers: NDQ_003353

answers: Transform faults

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: Alpine Fault

answers: NDQ_003356

answers: form plate boundaries

answers: NDQ_003357

answers: plate boundaries are neither created nor destroyed

answers: NDQ_003358

answers: conservative plate boundary

answers: NDQ_003359

answers: strike-slip

answers: NDQ_003360

answers: plate boundaries

answers: NDQ_003362

answers: lithosphere is neither created nor destroyed

answers: NDQ_003363

answers: Alpine Fault, New Zealand

answers: NDQ_003371

answers: Which of the following is not a plate boundary: mid-ocean ridges, or the Alpine Fault, New Zealand?

answers: NDQ_003373

answers: What is a special class of strike-slip faults

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: no

answers: NDQ_003380

answers: Which of the following is not an example of a stress?

answers: NDQ_003381

answers: What is the opposite of deforms?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: What is the cause of joints in rock

answers: NDQ_003384

answers: What class of strike-slip faults is the transform fault

answers: NDQ_003385

answers: Fault zone

answers: NDQ_003386

answers: What is the cause of earthquakes?

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: unanswerable

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: strike-slip fault

answers: NDQ_003391

answers: lithosphere

answers: NDQ_003392

answers: strike-slip fault

answers: NDQ_003393

answers: lithosphere

answers: NDQ_003394

answers: Alpine Fault

answers: NDQ_003395

answers: Alpine Fault

answers: NDQ_003396

answers: Alpine Fault

answers: NDQ_003351

answers: strike-slip faults is the transform fault,

answers: NDQ_003352

answers: lithosphere is neither created nor destroyed.

answers: NDQ_003353

answers: strike-slip faults

answers: NDQ_003354

answers: A special class of strike-slip faults is the transform fault,

answers: NDQ_003355

answers: ridges,

answers: NDQ_003356

answers: lithosphere is neither created nor destroyed.

answers: NDQ_003357

answers: offsets

answers: NDQ_003358

answers: conservative plate boundaries,

answers: NDQ_003359

answers: offsets

answers: NDQ_003360

answers: strike-slip faults

answers: NDQ_003362

answers: lithosphere is neither created nor destroyed.

answers: NDQ_003363

answers: mid-ocean ridges,

answers: NDQ_003371

answers: transform fault,

answers: NDQ_003373

answers: strike-slip faults is the transform fault,

answers: NDQ_003376

answers: mid-ocean ridges,

answers: NDQ_003378

answers: strike-slip

answers: NDQ_003379

answers: transform fault,

answers: NDQ_003380

answers: strike-slip faults is the transform fault,

answers: NDQ_003381

answers: lithosphere is neither created nor destroyed.

answers: NDQ_003382

answers: transform fault,

answers: NDQ_003383

answers: offsets

answers: NDQ_003384

answers: mid-ocean ridges,

answers: NDQ_003385

answers: transform fault, where such faults form a plate boundary.

answers: NDQ_003386

answers: strike-slip faults

answers: NDQ_003387

answers: strike-slip faults is the transform fault,

answers: NDQ_003388

answers: offsets in spreading centers,

answers: NDQ_003389

answers: lithosphere is neither created nor destroyed.

answers: NDQ_003390

answers: strike-slip faults is the transform fault,

answers: NDQ_003391

answers: lithosphere

answers: NDQ_003392

answers: strike-slip faults is the transform fault,

answers: NDQ_003393

answers: strike-slip faults is the transform fault,

answers: NDQ_003394

answers: transform fault,

answers: NDQ_003395

answers: transform fault,

answers: NDQ_003396

answers: transform fault,

text: Farther south, the growth of the Rocky Mountains in the United States is a geological puzzle. Mountain building is normally focused between  inland from a subduction zone boundary.  Geologists continue to gather evidence to explain the rise of the Rockies so much farther inland; the answer most likely lies with the unusual subduction of the Farallon plate, or possibly due to the subduction of an oceanic plateau.

text: Farther south, the growth of the Rocky Mountains in the United States is a geological puzzle. Mountain building is normally focused between  inland from a

text: subduction zone

text: boundary.  Geologists continue to gather evidence to explain the rise of the Rockies so much farther inland; the answer most likely lies with the unusual subduction of the

text: Farallon plate

text: , or possibly due to the subduction of an

text: oceanic plateau

answers: NDQ_003351

answers: subduction

answers: NDQ_003352

answers: subducts

answers: NDQ_003353

answers: subduction

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: Rocky Mountains

answers: NDQ_003356

answers: subduct

answers: NDQ_003357

answers: mountain building is normally focused between inland from a subduction zone boundary

answers: NDQ_003358

answers: plateau

answers: NDQ_003359

answers: subducts

answers: NDQ_003360

answers: subduction zone boundary

answers: NDQ_003362

answers: the Rocky Mountains in the United States is a geological puzzle

answers: NDQ_003363

answers: subduction zone boundary

answers: NDQ_003371

answers: Which of the following is not a type of fault?

answers: NDQ_003373

answers: subduction of an oceanic plateau

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: what is the last word in the passage?

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What is the most likely reason for the growth of the Rockies?

answers: NDQ_003381

answers: what is the last word in the passage?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: None of the above choices.

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: subduction zone boundary

answers: NDQ_003386

answers: subduction

answers: NDQ_003387

answers: Which of the following is not a type of normal fault?

answers: NDQ_003388

answers: Which of the following is not an example of a strike-slip fault?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: subduction zone

answers: NDQ_003391

answers: subduction zone

answers: NDQ_003392

answers: subduction zone

answers: NDQ_003393

answers: subduction zone

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: subduction zone boundary

answers: NDQ_003396

answers: subduction

answers: NDQ_003351

answers: subduction zone

answers: NDQ_003352

answers: Mountain building

answers: NDQ_003353

answers: subduction zone

answers: NDQ_003354

answers: subduction zone boundary.

answers: NDQ_003355

answers: subduction zone

answers: NDQ_003356

answers: Mountain building

answers: NDQ_003357

answers: Mountain building is normally focused between inland from a subduction zone boundary.

answers: NDQ_003358

answers: subduction zone

answers: NDQ_003359

answers: subduction zone boundary.

answers: NDQ_003360

answers: subduction zone boundary.

answers: NDQ_003362

answers: Mountain building is normally focused between inland from a subduction zone boundary.

answers: NDQ_003363

answers: subduction zone boundary.

answers: NDQ_003371

answers: Mountain building is normally focused between inland from a subduction zone boundary.

answers: NDQ_003373

answers: subduction zone

answers: NDQ_003376

answers: Mountain building is normally focused between inland from a subduction zone boundary.

answers: NDQ_003378

answers: subduction zone

answers: NDQ_003379

answers: subduction zone boundary.

answers: NDQ_003380

answers: Mountain building

answers: NDQ_003381

answers: subduction zone boundary.

answers: NDQ_003382

answers: subduction zone boundary.

answers: NDQ_003383

answers: Mountain building is normally focused between inland from a subduction zone boundary.

answers: NDQ_003384

answers: subduction zone boundary.

answers: NDQ_003385

answers: subduction zone

answers: NDQ_003386

answers: subduction zone

answers: NDQ_003387

answers: subduction zone

answers: NDQ_003388

answers: subduction zone boundary.

answers: NDQ_003389

answers: subduction zone

answers: NDQ_003390

answers: subduction

answers: NDQ_003391

answers: subduction zone

answers: NDQ_003392

answers: subduction zone boundary.

answers: NDQ_003393

answers: subduction zone

answers: NDQ_003394

answers: subduction zone

answers: NDQ_003395

answers: subduction

answers: NDQ_003396

answers: subduction zone

text: Self-blame is a cognitive process in which an individual attributes the occurrence of a stressful event to oneself. The direction of blame often has implications for individuals’ emotions and behaviors during and following stressful situations. Self-blame is a common reaction to stressful events  and has certain effects on how individuals adapt.  Types of self-blame are hypothesized to contribute to depression, and self-blame is a component of self-directed emotions like guilt and self-disgust. Because of self-blame’s commonality in response to stress and its role in emotion, self-blame should be examined using psychology’s perspectives on stress and coping. This article will attempt to give an overview of the contemporary study on self-blame in psychology.

text: Self-blame is a

text: cognitive process

text: in which an individual attributes the occurrence of a

text: stressful

text: event to oneself. The direction of

text: blame

text: often has implications for individuals’

text: emotion

text: s and

text: behavior

text: s during and following stressful situations. Self-blame is a common reaction to stressful events  and has certain effects on how individuals adapt.  Types of self-blame are hypothesized to contribute to

text: depression

text: , and self-blame is a component of self-directed emotions like guilt and self-disgust. Because of self-blame’s commonality in response to

text: stress

text: and its role in emotion, self-blame should be examined using psychology’s perspectives on stress and

text: coping

text: . This article will attempt to give an overview of the contemporary study on self-blame in

text: psychology

answers: NDQ_003351

answers: divergent plate boundary stress

answers: NDQ_003352

answers: is more likely to break

answers: NDQ_003353

answers: rocks to break apart.

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone.

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: break apart.

answers: NDQ_003357

answers: self-blame is a component of self-directed emotions like guilt

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures.

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: self-blame is a common reaction to stressful events

answers: NDQ_003363

answers: the same time

answers: NDQ_003371

answers: Context: A thrust fault is a type of fault in geology. A thrust fault is a type of fault in geology. If very old rocks are above much younger rocks there may be a thrust fault in between.

answers: NDQ_003373

answers: Context: A rock that is deeply buried is under compressive stresses. A rock that is deeply buried is under compressive stresses.

answers: NDQ_003376

answers: Context: The terrain known as basin-and-range is caused by compressive forces.

answers: NDQ_003378

answers: Context: Slip is the amount the ground moves in an earthquake. The amount the ground moves in an earthquake is called slip.

answers: NDQ_003379

answers: Context: In a strike-slip fault, the dip of the fault plane is horizontal.

answers: NDQ_003380

answers: Context: Self-blame is a cognitive process in which an individual attributes the occurrence of a stressful event to oneself. Types of self-blame are hypothesized to contribute to depression, and self-blame is a component of self-directed emotions like guilt and self-disgust. Because of self-blame’s commonality in response to stressful events and its role in emotion, self-blame should be examined using psychology’s perspectives on stress and coping.

answers: NDQ_003381

answers: Context: Conceiving stress occurs when a rock is subjected to a certain amount of pressure.

answers: NDQ_003382

answers: Convergent plates are formed by convergent plates collapsing at the same time.

answers: NDQ_003383

answers: Context: Self-blame is a cognitive process in which an individual attributes the occurrence of a stressful event to oneself

answers: NDQ_003384

answers: Context: A syncline is a fold that arches upward.

answers: NDQ_003385

answers: Context: A fault zone is an area where faults are clustered.

answers: NDQ_003386

answers: Context: Earthquakes are caused by movement of rock at faults. The movement of rock at faults is the cause of earthquakes.

answers: NDQ_003387

answers: Context: Normal faults are caused by compression stress.

answers: NDQ_003388

answers: Context: Strike-slip faults result from shear stress.

answers: NDQ_003389

answers: Context: The process of folding creates mountain ranges.

answers: NDQ_003390

answers: a fault

answers: NDQ_003391

answers: dip-slip

answers: NDQ_003392

answers: sloping

answers: NDQ_003393

answers: dip-slip

answers: NDQ_003394

answers: fault with a fault plane that is not vertical

answers: NDQ_003395

answers: a fault with a vertical fault plane

answers: NDQ_003396

answers: horizontal fault

answers: NDQ_003351

answers: Self-blame

answers: NDQ_003352

answers: Self-blame

answers: NDQ_003353

answers: Self-blame

answers: NDQ_003354

answers: Self-blame

answers: NDQ_003355

answers: Self-blame

answers: NDQ_003356

answers: Self-blame

answers: NDQ_003357

answers: guilt and self-disgust.

answers: NDQ_003358

answers: Self-blame

answers: NDQ_003359

answers: Self-blame

answers: NDQ_003360

answers: Self-blame

answers: NDQ_003362

answers: Self-blame

answers: NDQ_003363

answers: Self-blame

answers: NDQ_003371

answers: Self-blame

answers: NDQ_003373

answers: Self-blame

answers: NDQ_003376

answers: Self-blame

answers: NDQ_003378

answers: Self-blame

answers: NDQ_003379

answers: Self-blame

answers: NDQ_003380

answers: Self-blame

answers: NDQ_003381

answers: Self-blame

answers: NDQ_003382

answers: Self-blame

answers: NDQ_003383

answers: Self-blame

answers: NDQ_003384

answers: Self-blame

answers: NDQ_003385

answers: Self-blame

answers: NDQ_003386

answers: Self-blame

answers: NDQ_003387

answers: Self-blame

answers: NDQ_003388

answers: Self-blame

answers: NDQ_003389

answers: Self-blame

answers: NDQ_003390

answers: Self-blame

answers: NDQ_003391

answers: Self-blame

answers: NDQ_003392

answers: Self-blame

answers: NDQ_003393

answers: Self-blame

answers: NDQ_003394

answers: Self-blame

answers: NDQ_003395

answers: Self-blame

answers: NDQ_003396

answers: Self-blame

text: As the Jeanne d'Arc rift basin subsided, it was gradually in-filled with sediments eroded from adjacent areas of crustal uplift. Characteristics of the sedimentary basin fill and their relationships to the extensional history of the Jeanne d'Arc Basin have been variably described by numerous authors with general agreement on the applicability of rift concepts to the basin. There are, however, divergent conclusions regarding the number of Mesozoic rift episodes which affected the Jeanne d'Arc Basin (i.e. two or three), their ages of initiation and duration, and the orientations of extensional stresses that created different fault sets active during the rift episodes. Rift episodes were followed by initiation of sea-floor spreading first to the south, then to the east, and finally to the northeast of the Grand Banks area. Widely faulted and moderately rotated Upper Triassic to Lower Cretaceous beds within the rift basin were subsequently buried beneath a relatively unstructured cover of Upper Cretaceous and Tertiary strata.  These latter minimally deformed strata were deposited on the newly established passive margin. The current passive margin conditions were established when the last rifted border to the three-sided promontory of continental crust underlying the Grand Banks bathymetric feature formed along its northeast margin near the start of Late Cretaceous times.

text: As the Jeanne d'Arc rift basin subsided, it was gradually in-filled with

text: sediment

text: s eroded from adjacent areas of crustal uplift. Characteristics of the sedimentary basin fill and their relationships to the extensional history of the Jeanne d'Arc Basin have been variably described by numerous authors with general agreement on the applicability of rift concepts to the basin. There are, however, divergent conclusions regarding the number of Mesozoic rift episodes which affected the Jeanne d'Arc Basin (i.e. two or three), their ages of initiation and duration, and the orientations of extensional stresses that created different fault sets active during the rift episodes. Rift episodes were followed by initiation of sea-floor spreading first to the south, then to the east, and finally to the northeast of the Grand Banks area. Widely faulted and moderately rotated Upper

text: Triassic

text: to Lower

text: Cretaceous

text: beds within the rift basin were subsequently buried beneath a relatively unstructured cover of Upper Cretaceous and

text: Tertiary

text: strata.  These latter minimally deformed strata were deposited on the newly established

text: passive margin

text: . The current passive margin conditions were established when the last rifted border to the three-sided promontory of continental crust underlying the Grand Banks bathymetric feature formed along its northeast margin near the start of Late Cretaceous times.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: deforms

answers: NDQ_003353

answers: faults

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: passive margin

answers: NDQ_003356

answers: deform minimally

answers: NDQ_003357

answers: Upper Cretaceous and Tertiary strata were deposited on the newly established passive margin

answers: NDQ_003358

answers: passive margin

answers: NDQ_003359

answers: extensional stresses

answers: NDQ_003360

answers: continental crust

answers: NDQ_003362

answers: unstructured cover of Upper Cretaceous and Tertiary strata

answers: NDQ_003363

answers: Late Cretaceous times

answers: NDQ_003371

answers: What is a thrust fault?

answers: NDQ_003373

answers: no

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: no

answers: NDQ_003380

answers: What is a stress?

answers: NDQ_003381

answers: What type of stress does the Jeanne d'Arc Basin experience?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: Rift episodes

answers: NDQ_003387

answers: Which is not the type of stresses that created different fault sets active during the rift episodes

answers: NDQ_003388

answers: What type of faults are strike-slip faults?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: rift basin subsided

answers: NDQ_003391

answers: rift basin

answers: NDQ_003392

answers: rift basin

answers: NDQ_003393

answers: passive margin

answers: NDQ_003394

answers: the orientations of extensional stresses

answers: NDQ_003395

answers: different fault sets active during the rift episodes

answers: NDQ_003396

answers: Widely faulted

answers: NDQ_003351

answers: extensional stresses

answers: NDQ_003352

answers: fault sets

answers: NDQ_003353

answers: fault sets

answers: NDQ_003354

answers: Upper Triassic to Lower Cretaceous

answers: NDQ_003355

answers: passive margin.

answers: NDQ_003356

answers: deposited on the newly established passive margin.

answers: NDQ_003357

answers: moderately rotated

answers: NDQ_003358

answers: passive margin.

answers: NDQ_003359

answers: extensional stresses

answers: NDQ_003360

answers: crustal uplift.

answers: NDQ_003362

answers: two or three),

answers: NDQ_003363

answers: Grand Banks

answers: NDQ_003371

answers: Widely faulted

answers: NDQ_003373

answers: Widely faulted

answers: NDQ_003376

answers: crustal uplift.

answers: NDQ_003378

answers: uplift.

answers: NDQ_003379

answers: Widely faulted

answers: NDQ_003380

answers: stresses

answers: NDQ_003381

answers: minimally deformed strata were deposited on the newly established passive margin.

answers: NDQ_003382

answers: extensional stresses

answers: NDQ_003383

answers: fault sets

answers: NDQ_003384

answers: crustal uplift.

answers: NDQ_003385

answers: fault sets

answers: NDQ_003386

answers: extensional stresses

answers: NDQ_003387

answers: extensional stresses

answers: NDQ_003388

answers: extensional stresses

answers: NDQ_003389

answers: sea-floor spreading

answers: NDQ_003390

answers: fault sets

answers: NDQ_003391

answers: Upper Triassic to Lower Cretaceous beds

answers: NDQ_003392

answers: fault sets

answers: NDQ_003393

answers: passive margin.

answers: NDQ_003394

answers: fault sets

answers: NDQ_003395

answers: fault sets

answers: NDQ_003396

answers: Widely faulted

text: In addition, there is a large (but unknown) amount of methane in methane clathrates in the ocean floors as well as the Earth's crust.

text: In addition, there is a large (but unknown) amount of methane in

text: methane clathrates

text: in the ocean floors as well as the Earth's

text: crust

answers: NDQ_003351

answers: methane

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: methane to form

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: swell

answers: NDQ_003357

answers: methane clathrates are found where?

answers: NDQ_003358

answers: fault line

answers: NDQ_003359

answers: is pushed together

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: there is no methane in the ocean floors

answers: NDQ_003363

answers: ocean floors

answers: NDQ_003371

answers: Which of the following is not a type of fault?

answers: NDQ_003373

answers: how would you describe it?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What is the result of confining stress?

answers: NDQ_003382

answers: None of the above choices.

answers: NDQ_003383

answers: None of the above choices.

answers: NDQ_003384

answers: None of the above choices.

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: no

answers: NDQ_003387

answers: None of the above choices.

answers: NDQ_003388

answers: Which of the following is not an example of a strike-slip fault?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: can be used to describe

answers: NDQ_003391

answers: can be described as a

answers: NDQ_003392

answers: can be used to describe

answers: NDQ_003393

answers: is a clathrate

answers: NDQ_003394

answers: isobath

answers: NDQ_003395

answers: is a fault

answers: NDQ_003396

answers: can be used to describe

answers: NDQ_003351

answers: methane in methane clathrates

answers: NDQ_003352

answers: methane in methane clathrates

answers: NDQ_003353

answers: methane in methane clathrates

answers: NDQ_003354

answers: methane in methane clathrates

answers: NDQ_003355

answers: clathrates

answers: NDQ_003356

answers: methane in methane clathrates

answers: NDQ_003357

answers: methane in methane clathrates

answers: NDQ_003358

answers: clathrates

answers: NDQ_003359

answers: Earth's crust.

answers: NDQ_003360

answers: methane

answers: NDQ_003362

answers: unknown) amount of methane

answers: NDQ_003363

answers: methane in methane clathrates

answers: NDQ_003371

answers: methane in methane clathrates

answers: NDQ_003373

answers: methane in methane clathrates

answers: NDQ_003376

answers: methane in methane clathrates

answers: NDQ_003378

answers: methane in methane clathrates

answers: NDQ_003379

answers: methane clathrates

answers: NDQ_003380

answers: Earth's crust.

answers: NDQ_003381

answers: methane in methane clathrates

answers: NDQ_003382

answers: methane clathrates

answers: NDQ_003383

answers: methane in methane clathrates

answers: NDQ_003384

answers: methane clathrates

answers: NDQ_003385

answers: methane clathrates

answers: NDQ_003386

answers: methane in methane clathrates

answers: NDQ_003387

answers: methane in methane clathrates

answers: NDQ_003388

answers: methane clathrates

answers: NDQ_003389

answers: methane in methane clathrates

answers: NDQ_003390

answers: methane clathrates

answers: NDQ_003391

answers: methane clathrates

answers: NDQ_003392

answers: methane clathrates

answers: NDQ_003393

answers: methane clathrates

answers: NDQ_003394

answers: Earth's crust.

answers: NDQ_003395

answers: Earth's crust.

answers: NDQ_003396

answers: methane clathrates

text: In the 1960s, it was discovered that the Earth's lithosphere, including the crust and rigid uppermost portion of the upper mantle, is separated into a number of tectonic plates that move across the plastically deforming, solid, upper mantle, which is called the asthenosphere. This theory is supported by a number of observations, including seafloor spreading, and the global distribution of mountain terrain and seismicity.

text: In the 1960s, it was discovered that the Earth's

text: lithosphere

text: , including the

text: crust

text: and rigid uppermost portion of the

text: upper mantle

text: , is separated into a number of

text: tectonic plate

text: s that move across the

text: plastically

text: deforming, solid, upper mantle, which is called the

text: asthenosphere

text: . This theory is supported by a number of observations, including seafloor spreading, and the global distribution of mountain terrain and seismicity.

answers: NDQ_003351

answers: plastically deforming

answers: NDQ_003352

answers: deforms

answers: NDQ_003353

answers: plastically deforming

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: plate

answers: NDQ_003356

answers: solidify

answers: NDQ_003357

answers: tectonic plates that move across the plastically deforming, solid, upper mantle

answers: NDQ_003358

answers: solid

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: tectonic plates

answers: NDQ_003362

answers: seafloor spreading

answers: NDQ_003363

answers: tectonic plates

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: What is the reason for this?

answers: NDQ_003376

answers: mountain terrain

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: vertical

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What does plastically deforming mean?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: tectonic plates

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip, asthenosphere, or seismicity?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: seafloor spreading

answers: NDQ_003391

answers: seafloor

answers: NDQ_003392

answers: tectonic plates

answers: NDQ_003393

answers: lithosphere

answers: NDQ_003394

answers: tectonic

answers: NDQ_003395

answers: tectonic plates

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: seismicity.

answers: NDQ_003352

answers: deforming,

answers: NDQ_003353

answers: plastically deforming,

answers: NDQ_003354

answers: In the 1960s,

answers: NDQ_003355

answers: mountain terrain

answers: NDQ_003356

answers: solid,

answers: NDQ_003357

answers: plastically deforming, solid, upper mantle,

answers: NDQ_003358

answers: mountain terrain

answers: NDQ_003359

answers: tectonic plates that move across the plastically deforming,

answers: NDQ_003360

answers: tectonic plates

answers: NDQ_003362

answers: seafloor spreading,

answers: NDQ_003363

answers: tectonic plates

answers: NDQ_003371

answers: tectonic plates

answers: NDQ_003373

answers: In the 1960s,

answers: NDQ_003376

answers: mountain terrain

answers: NDQ_003378

answers: seismicity.

answers: NDQ_003379

answers: tectonic plates

answers: NDQ_003380

answers: tectonic plates that move across the plastically deforming,

answers: NDQ_003381

answers: plastically deforming,

answers: NDQ_003382

answers: tectonic plates

answers: NDQ_003383

answers: tectonic plates that move across the plastically deforming,

answers: NDQ_003384

answers: tectonic plates

answers: NDQ_003385

answers: tectonic plates

answers: NDQ_003386

answers: tectonic plates

answers: NDQ_003387

answers: tectonic plates

answers: NDQ_003388

answers: tectonic plates

answers: NDQ_003389

answers: tectonic plates that move across the plastically deforming,

answers: NDQ_003390

answers: seismicity.

answers: NDQ_003391

answers: seafloor

answers: NDQ_003392

answers: tectonic plates

answers: NDQ_003393

answers: crust and rigid uppermost portion of the upper mantle,

answers: NDQ_003394

answers: tectonic plates

answers: NDQ_003395

answers: tectonic plates

answers: NDQ_003396

answers: tectonic plates

text: In geology the term compression refers to a set of stress directed toward the center of a rock mass. Compressive strength refers to the maximum compressive stress that can be applied to a material before failure occurs. When the maximum compressive stress is in a horizontal orientation, thrust faulting can occur, resulting in the shortening and thickening of that portion of the crust. When the maximum compressive stress is vertical, a section of rock will often fail in normal faults, horizontally extending and vertically thinning a given layer of rock. Compressive stresses can also result in folding of rocks. Because of the large magnitudes of lithostatic stress in tectonic plates, tectonic-scale deformation is always subjected to net compressive stress.

text: In

text: geology

text: the term compression refers to a set of stress directed toward the center of a rock mass.

text: Compressive strength

text: refers to the maximum

text: compressive stress

text: that can be applied to a material before failure occurs. When the maximum compressive stress is in a horizontal orientation,

text: thrust fault

text: ing can occur, resulting in the shortening and thickening of that portion of the

text: crust

text: . When the maximum compressive stress is vertical, a section of rock will often fail in

text: normal fault

text: s, horizontally extending and vertically thinning a given layer of rock. Compressive stresses can also result in

text: folding

text: of rocks. Because of the large magnitudes of

text: lithostatic stress

text: in

text: tectonic plate

text: s, tectonic-scale

text: deformation

text: is always subjected to net compressive stress.

answers: NDQ_003351

answers: compressive stress

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: thrust faulting

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: horizontal

answers: NDQ_003356

answers: fold

answers: NDQ_003357

answers: vertically thinning a given layer of rock

answers: NDQ_003358

answers: normal fault

answers: NDQ_003359

answers: horizontally

answers: NDQ_003360

answers: plates

answers: NDQ_003362

answers: horizontally extending and vertically thinning a given layer of rock

answers: NDQ_003363

answers: the same time

answers: NDQ_003371

answers: When the maximum compressive stress is horizontal

answers: NDQ_003373

answers: vertical

answers: NDQ_003376

answers: horizontally extending

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: vertical

answers: NDQ_003380

answers: Yes

answers: NDQ_003381

answers: When the maximum compressive stress is in a horizontal orientation

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: horizontally extending and vertically thinning

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is the term for an area where faults are clustered?

answers: NDQ_003386

answers: What is the cause of earthquakes?

answers: NDQ_003387

answers: yes

answers: NDQ_003388

answers: unanswerable

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: thrust faulting

answers: NDQ_003391

answers: a section of rock will often fail in normal faults

answers: NDQ_003392

answers: thrust faulting

answers: NDQ_003393

answers: a given layer of rock

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: vertically thinning a given layer of rock

answers: NDQ_003396

answers: thrust faulting

answers: NDQ_003351

answers: lithostatic

answers: NDQ_003352

answers: failure

answers: NDQ_003353

answers: folding of rocks.

answers: NDQ_003354

answers: In geology

answers: NDQ_003355

answers: vertically thinning a given layer of rock. Compressive stresses

answers: NDQ_003356

answers: folding

answers: NDQ_003357

answers: a section of rock will often fail

answers: NDQ_003358

answers: normal faults,

answers: NDQ_003359

answers: horizontal orientation,

answers: NDQ_003360

answers: tectonic plates,

answers: NDQ_003362

answers: shortening and thickening

answers: NDQ_003363

answers: tectonic plates,

answers: NDQ_003371

answers: When the maximum compressive stress is in a horizontal orientation,

answers: NDQ_003373

answers: folding of rocks.

answers: NDQ_003376

answers: folding of rocks.

answers: NDQ_003378

answers: thrust faulting

answers: NDQ_003379

answers: a section of rock will often fail in normal faults,

answers: NDQ_003380

answers: Compressive strength refers to the maximum compressive stress

answers: NDQ_003381

answers: Compressive stresses can also result in folding of rocks.

answers: NDQ_003382

answers: compressive stress.

answers: NDQ_003383

answers: Compressive stresses

answers: NDQ_003384

answers: Compressive stresses can also result in folding of rocks.

answers: NDQ_003385

answers: normal faults,

answers: NDQ_003386

answers: thrust faulting

answers: NDQ_003387

answers: When the maximum compressive stress is vertical,

answers: NDQ_003388

answers: thrust faulting

answers: NDQ_003389

answers: Compressive stresses

answers: NDQ_003390

answers: thrust faulting

answers: NDQ_003391

answers: normal faults,

answers: NDQ_003392

answers: thrust faulting

answers: NDQ_003393

answers: normal faults,

answers: NDQ_003394

answers: normal faults,

answers: NDQ_003395

answers: normal faults,

answers: NDQ_003396

answers: thrust faulting

text: Nummer twaalf, variations on a theme40’00”, 4k video. Marshall Chess Club, Mt St Helens & San Andreas Fault USA, 2009

text: Nummer twaalf, variations on a theme40’00”, 4k video. Marshall Chess Club, Mt St Helens & San Andreas Fault USA, 2009

answers: NDQ_003351

answers: tensile

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation is a formation

answers: NDQ_003355

answers: fold that bends downward

answers: NDQ_003356

answers: shrink

answers: NDQ_003357

answers: Mt St Helens and San Andreas Fault are two examples of what?

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: cracks

answers: NDQ_003360

answers: San Andreas fault

answers: NDQ_003362

answers: The San Andreas Fault is located in the Pacific Ocean.

answers: NDQ_003363

answers: San Andreas Fault

answers: NDQ_003371

answers: What is the San Andreas Fault?

answers: NDQ_003373

answers: What would happen if a rock is buried for a long time?

answers: NDQ_003376

answers: Which of the following is not a type of terrain: basin-and-range or range?

answers: NDQ_003378

answers: What is the amount of the ground moving in an earthquake?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What is a stress?

answers: NDQ_003381

answers: What is the purpose of the video?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is the name of the video?

answers: NDQ_003386

answers: What is the San Andreas Fault?

answers: NDQ_003387

answers: Which of the following is not a normal fault: Mt St Helens & San Andreas Fault?

answers: NDQ_003388

answers: What is the name of the chess club?

answers: NDQ_003389

answers: What is the process of folding?

answers: NDQ_003390

answers: San Andreas Fault

answers: NDQ_003391

answers: sandstone

answers: NDQ_003392

answers: San Andreas Fault

answers: NDQ_003393

answers: sandstone

answers: NDQ_003394

answers: San Andreas Fault

answers: NDQ_003395

answers: San Andreas Fault

answers: NDQ_003396

answers: San Andreas Fault

answers: NDQ_003351

answers: San Andreas Fault

answers: NDQ_003352

answers: San Andreas Fault

answers: NDQ_003353

answers: San Andreas Fault

answers: NDQ_003354

answers: Mt St Helens & San Andreas Fault USA, 2009

answers: NDQ_003355

answers: Nummer twaalf,

answers: NDQ_003356

answers: San Andreas Fault

answers: NDQ_003357

answers: Mt St Helens

answers: NDQ_003358

answers: Fault

answers: NDQ_003359

answers: San Andreas Fault

answers: NDQ_003360

answers: San Andreas Fault

answers: NDQ_003362

answers: Nummer twaalf,

answers: NDQ_003363

answers: San Andreas Fault

answers: NDQ_003371

answers: Mt St Helens & San Andreas Fault

answers: NDQ_003373

answers: Mt St Helens & San Andreas Fault USA,

answers: NDQ_003376

answers: Mt St Helens & San Andreas Fault USA,

answers: NDQ_003378

answers: Mt St Helens & San Andreas Fault

answers: NDQ_003379

answers: Mt St Helens & San Andreas Fault USA, 2009

answers: NDQ_003380

answers: Mt St Helens & San Andreas Fault

answers: NDQ_003381

answers: Mt St Helens & San Andreas Fault USA,

answers: NDQ_003382

answers: 2009

answers: NDQ_003383

answers: Mt St Helens & San Andreas Fault

answers: NDQ_003384

answers: Nummer twaalf,

answers: NDQ_003385

answers: Mt St Helens & San Andreas Fault USA,

answers: NDQ_003386

answers: Mt St Helens & San Andreas Fault USA,

answers: NDQ_003387

answers: Mt St Helens & San Andreas Fault

answers: NDQ_003388

answers: Mt St Helens & San Andreas Fault USA, 2009

answers: NDQ_003389

answers: Mt St Helens & San Andreas Fault

answers: NDQ_003390

answers: San Andreas Fault

answers: NDQ_003391

answers: Mt St Helens & San Andreas Fault

answers: NDQ_003392

answers: San Andreas Fault

answers: NDQ_003393

answers: Mt St Helens

answers: NDQ_003394

answers: San Andreas Fault

answers: NDQ_003395

answers: San Andreas Fault

answers: NDQ_003396

answers: Mt St Helens & San Andreas Fault

text: A lesion caused by recurrence of a latent herpes simplex infection can occur in the corner of the mouth. Really this is herpes labialis (a cold sore), and is sometimes termed "angular herpes simplex". A cold sore at the corner of the mouth behaves similarly to elsewhere on the lips, and follows a pattern of vesicle (blister) formation followed by rupture leaving a crusted sore which resolves in about 7–10 days, and recurs in the same spot periodically, especially during periods of stress. Rather than utilizing antifungal creams, angular herpes simplex is treated in the same way as a cold sore, with topical antiviral drugs such as aciclovir.

text: A lesion caused by recurrence of a latent

text: herpes simplex

text: infection can occur in the corner of the mouth. Really this is

text: herpes labialis

text: (a cold sore), and is sometimes termed "angular herpes simplex". A cold sore at the corner of the mouth behaves similarly to elsewhere on the lips, and follows a pattern of

text: vesicle

text: (blister) formation followed by rupture leaving a crusted sore which resolves in about 7–10 days, and recurs in the same spot periodically, especially during periods of stress. Rather than utilizing antifungal creams, angular herpes simplex is treated in the same way as a cold sore, with topical

text: antiviral drug

text: s such as

text: aciclovir

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: cracks

answers: NDQ_003353

answers: unanswerable

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: angular

answers: NDQ_003356

answers: crack

answers: NDQ_003357

answers: vesicle formation followed by rupture leaving a crusted sore which resolves in about 7–10 days

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: continental plates

answers: NDQ_003362

answers: unanswerable

answers: NDQ_003363

answers: unanswerable

answers: NDQ_003371

answers: Which of the following is not an example of a thrust fault?

answers: NDQ_003373

answers: how would you describe compressive stresses?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: what is the dip of the fault plane

answers: NDQ_003380

answers: What is the last word in the passage?

answers: NDQ_003381

answers: unanswerable

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: no

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: Which of the following is not a type of shear stress: strike-slip faults, shear stress or shear stress?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: angular herpes simplex

answers: NDQ_003391

answers: dip-slip fault plane

answers: NDQ_003392

answers: unanswerable

answers: NDQ_003393

answers: dip-slip fault plane

answers: NDQ_003394

answers: angular

answers: NDQ_003395

answers: unanswerable

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: aciclovir.

answers: NDQ_003352

answers: cold sore

answers: NDQ_003353

answers: vesicle

answers: NDQ_003354

answers: A lesion

answers: NDQ_003355

answers: corner of the mouth. Really this is herpes labialis

answers: NDQ_003356

answers: rupture

answers: NDQ_003357

answers: 7–10 days,

answers: NDQ_003358

answers: herpes labialis

answers: NDQ_003359

answers: rupture

answers: NDQ_003360

answers: stress.

answers: NDQ_003362

answers: A lesion caused by recurrence

answers: NDQ_003363

answers: periods of stress.

answers: NDQ_003371

answers: A lesion

answers: NDQ_003373

answers: stress.

answers: NDQ_003376

answers: stress.

answers: NDQ_003378

answers: rupture

answers: NDQ_003379

answers: aciclovir.

answers: NDQ_003380

answers: stress.

answers: NDQ_003381

answers: cold sore at the corner of the mouth

answers: NDQ_003382

answers: stress.

answers: NDQ_003383

answers: stress.

answers: NDQ_003384

answers: vesicle

answers: NDQ_003385

answers: "angular herpes simplex".

answers: NDQ_003386

answers: vesicle

answers: NDQ_003387

answers: stress.

answers: NDQ_003388

answers: aciclovir.

answers: NDQ_003389

answers: vesicle

answers: NDQ_003390

answers: "angular herpes simplex".

answers: NDQ_003391

answers: "angular herpes simplex".

answers: NDQ_003392

answers: "angular herpes simplex".

answers: NDQ_003393

answers: "angular herpes simplex".

answers: NDQ_003394

answers: "angular herpes simplex".

answers: NDQ_003395

answers: rupture

answers: NDQ_003396

answers: "angular herpes simplex".

text: A number of architecture firms have been experimenting with using the Rift for visualisation and design. With the right software, the Rift allows architects to see exactly what their building will look like, and get an understanding of the scale that is impossible on a traditional monitor.

text: A number of architecture firms have been experimenting with using the Rift for visualisation and design. With the right software, the Rift allows architects to see exactly what their building will look like, and get an understanding of the scale that is impossible on a traditional monitor.

answers: NDQ_003351

answers: Rift

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation is higher

answers: NDQ_003355

answers: Rift

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: Rift allows architects to see exactly what their building will look like

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: the San Andreas fault is located in the Pacific Ocean

answers: NDQ_003363

answers: the same time

answers: NDQ_003371

answers: Which of the following is not an example of a thrust fault?

answers: NDQ_003373

answers: What will happen to the rock?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: What does the Rift allow architects to see?

answers: NDQ_003379

answers: The dip of the fault plane is horizontal

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: Which of the following is not a type of stress?

answers: NDQ_003382

answers: None of the above choices.

answers: NDQ_003383

answers: None of the above choices.

answers: NDQ_003384

answers: What does the Rift allow architects to do?

answers: NDQ_003385

answers: what is the first word in the passage?

answers: NDQ_003386

answers: None of the above choices.

answers: NDQ_003387

answers: Which of the following is not a type of normal fault?

answers: NDQ_003388

answers: Which of the following is not a result of shear stress?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: dip-slip fault

answers: NDQ_003392

answers: unanswerable

answers: NDQ_003393

answers: dip-slip fault

answers: NDQ_003394

answers: is a fault

answers: NDQ_003395

answers: NDQ_003396

answers: NDQ_003351

answers: Rift

answers: NDQ_003352

answers: Rift

answers: NDQ_003353

answers: Rift

answers: NDQ_003354

answers: Rift

answers: NDQ_003355

answers: Rift

answers: NDQ_003356

answers: scale that is impossible on a traditional monitor.

answers: NDQ_003357

answers: scale that is impossible on a traditional monitor.

answers: NDQ_003358

answers: Rift

answers: NDQ_003359

answers: Rift

answers: NDQ_003360

answers: Rift

answers: NDQ_003362

answers: impossible on a traditional monitor.

answers: NDQ_003363

answers: Rift

answers: NDQ_003371

answers: Rift

answers: NDQ_003373

answers: A number of architecture firms have been experimenting with using the Rift

answers: NDQ_003376

answers: monitor.

answers: NDQ_003378

answers: Rift

answers: NDQ_003379

answers: impossible on a traditional monitor.

answers: NDQ_003380

answers: monitor.

answers: NDQ_003381

answers: Rift

answers: NDQ_003382

answers: Rift

answers: NDQ_003383

answers: Rift

answers: NDQ_003384

answers: monitor.

answers: NDQ_003385

answers: Rift

answers: NDQ_003386

answers: Rift

answers: NDQ_003387

answers: Rift

answers: NDQ_003388

answers: A number of architecture firms have been experimenting with using the Rift

answers: NDQ_003389

answers: Rift

answers: NDQ_003390

answers: Rift

answers: NDQ_003391

answers: Rift

answers: NDQ_003392

answers: Rift

answers: NDQ_003393

answers: Rift

answers: NDQ_003394

answers: impossible on a traditional monitor.

answers: NDQ_003395

answers: a traditional monitor.

answers: NDQ_003396

answers: impossible on a traditional monitor.

text: Most rifts consist of a series of separate segments that together form the linear zone characteristic of rifts. The individual rift segments have a dominantly half-graben geometry, controlled by a single basin-bounding fault. Segment lengths vary between rifts, depending on the elastic thickness of the lithosphere. Areas of thick colder lithosphere, such as the Baikal Rift have segment lengths in excess of 80 km, while in areas of warmer thin lithosphere, segment lengths may be less than 30 km. Along the axis of the rift the position, and in some cases the polarity (the dip direction), of the main rift bounding fault changes from segment to segment. Segment boundaries often have a more complex structure and generally cross the rift axis at a high angle. These segment boundary zones accommodate the differences in fault displacement between the segments and are therefore known as accommodation zones.

text: Most rifts consist of a series of separate segments that together form the linear zone characteristic of rifts. The individual rift segments have a dominantly half-graben geometry, controlled by a single basin-bounding fault. Segment lengths vary between rifts, depending on the elastic thickness of the lithosphere. Areas of thick colder lithosphere, such as the Baikal Rift have segment lengths in excess of 80 km, while in areas of warmer thin lithosphere, segment lengths may be less than 30 km. Along the axis of the rift the position, and in some cases the polarity (the dip direction), of the main rift bounding fault changes from segment to segment. Segment boundaries often have a more complex structure and generally cross the rift axis at a high angle. These segment boundary zones accommodate the differences in fault displacement between the segments and are therefore known as accommodation zones.

answers: NDQ_003351

answers: fault displacement

answers: NDQ_003352

answers: is more likely to crack

answers: NDQ_003353

answers: fault displacement

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: dip

answers: NDQ_003356

answers: stretch

answers: NDQ_003357

answers: segment lengths may be less than 30 km

answers: NDQ_003358

answers: accommodation zone

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: faults

answers: NDQ_003362

answers: The individual rift segments have a dominantly half-graben geometry

answers: NDQ_003363

answers: Baikal Rift

answers: NDQ_003371

answers: Segment boundaries often have a more complex structure

answers: NDQ_003373

answers: Segment boundaries often have a more complex structure

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: no

answers: NDQ_003380

answers: What is the elastic thickness of the lithosphere?

answers: NDQ_003381

answers: Segment boundaries often have a more complex structure

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: segment boundaries often have a more complex structure

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: yes

answers: NDQ_003386

answers: fault displacement between the segments

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: What is the dip direction of the main rift bounding fault?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: basin-bounding fault

answers: NDQ_003391

answers: lithosphere

answers: NDQ_003392

answers: basin-bounding fault

answers: NDQ_003393

answers: lithosphere

answers: NDQ_003394

answers: basin-bounding fault

answers: NDQ_003395

answers: basin-bounding fault

answers: NDQ_003396

answers: basin-bounding fault

answers: NDQ_003351

answers: fault displacement

answers: NDQ_003352

answers: accommodation zones.

answers: NDQ_003353

answers: fault displacement

answers: NDQ_003354

answers: Baikal Rift

answers: NDQ_003355

answers: dip

answers: NDQ_003356

answers: elastic thickness

answers: NDQ_003357

answers: rift bounding fault changes from segment to segment.

answers: NDQ_003358

answers: accommodation zones.

answers: NDQ_003359

answers: fault.

answers: NDQ_003360

answers: rifts

answers: NDQ_003362

answers: half-graben geometry,

answers: NDQ_003363

answers: rifts

answers: NDQ_003371

answers: accommodation zones.

answers: NDQ_003373

answers: elastic thickness

answers: NDQ_003376

answers: basin-bounding fault.

answers: NDQ_003378

answers: fault displacement

answers: NDQ_003379

answers: polarity (the dip direction),

answers: NDQ_003380

answers: accommodation zones.

answers: NDQ_003381

answers: accommodation zones.

answers: NDQ_003382

answers: accommodation zones.

answers: NDQ_003383

answers: segment boundary zones accommodate the differences in fault displacement

answers: NDQ_003384

answers: accommodation zones.

answers: NDQ_003385

answers: accommodation zones.

answers: NDQ_003386

answers: fault displacement

answers: NDQ_003387

answers: accommodation zones.

answers: NDQ_003388

answers: accommodation zones.

answers: NDQ_003389

answers: rifts.

answers: NDQ_003390

answers: rift bounding fault

answers: NDQ_003391

answers: accommodation zones.

answers: NDQ_003392

answers: basin-bounding fault.

answers: NDQ_003393

answers: accommodation zones.

answers: NDQ_003394

answers: basin-bounding fault.

answers: NDQ_003395

answers: basin-bounding fault.

answers: NDQ_003396

answers: basin-bounding fault.

text: Stress interviews are still in common use. One type of stress interview is where the employer uses a succession of interviewers (one at a time or en masse) whose mission is to intimidate the candidate and keep him/her off-balance. The ostensible purpose of this interview: to find out how the candidate handles stress. Stress interviews might involve testing an applicant's behavior in a busy environment. Questions about handling work overload, dealing with multiple projects, and handling conflict are typical.

text: Stress interviews are still in common use. One type of stress interview is where the employer uses a succession of interviewers (one at a time or en masse) whose mission is to intimidate the candidate and keep him/her off-balance. The ostensible purpose of this interview: to find out how the candidate handles stress. Stress interviews might involve testing an applicant's behavior in a busy environment. Questions about handling work overload, dealing with multiple projects, and handling conflict are typical.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: is likely to crack

answers: NDQ_003353

answers: a chemical reaction

answers: NDQ_003354

answers: Toroweap Formation is a formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: stress interviews might involve testing an applicant's behavior in a busy environment

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures.

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: stress interviews are still in common use

answers: NDQ_003363

answers: the same time

answers: NDQ_003371

answers: Which of the following is not a type of stress interview?

answers: NDQ_003373

answers: What is the best way to describe this situation?

answers: NDQ_003376

answers: basin-and-range

answers: NDQ_003378

answers: The amount of the ground moving in an earthquake is called slip

answers: NDQ_003379

answers: The dip of the fault plane is horizontal

answers: NDQ_003380

answers: How would you describe a stress interview?

answers: NDQ_003381

answers: Which of the following is not an example of confining stress?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: no

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: Faults are clustered in an area called a fault zone.

answers: NDQ_003386

answers: earthquakes are caused by movement of rock at faults.

answers: NDQ_003387

answers: Which of the following is not a type of stress interview?

answers: NDQ_003388

answers: Which of the following is not a type of stress interview?

answers: NDQ_003389

answers: None of the above choices.

answers: NDQ_003390

answers: stress interview

answers: NDQ_003391

answers: dip-slip fault plane

answers: NDQ_003392

answers: stress interview

answers: NDQ_003393

answers: dip-slip fault plane

answers: NDQ_003394

answers: is not vertical

answers: NDQ_003395

answers: a vertical fault

answers: NDQ_003396

answers: NDQ_003351

answers: conflict

answers: NDQ_003352

answers: off-balance.

answers: NDQ_003353

answers: off-balance.

answers: NDQ_003354

answers: Stress interviews

answers: NDQ_003355

answers: Stress interviews

answers: NDQ_003356

answers: Stress interviews

answers: NDQ_003357

answers: intimidate the candidate and keep him/her off-balance.

answers: NDQ_003358

answers: Stress interviews

answers: NDQ_003359

answers: off-balance.

answers: NDQ_003360

answers: Stress interviews

answers: NDQ_003362

answers: Stress interviews

answers: NDQ_003363

answers: Stress interviews

answers: NDQ_003371

answers: Stress interviews

answers: NDQ_003373

answers: Stress interviews

answers: NDQ_003376

answers: Stress interviews

answers: NDQ_003378

answers: Stress interviews

answers: NDQ_003379

answers: Stress interviews

answers: NDQ_003380

answers: Stress interviews

answers: NDQ_003381

answers: Stress interviews

answers: NDQ_003382

answers: Stress interviews

answers: NDQ_003383

answers: Stress interviews

answers: NDQ_003384

answers: Stress interviews

answers: NDQ_003385

answers: Stress interviews

answers: NDQ_003386

answers: Stress interviews

answers: NDQ_003387

answers: Stress interviews

answers: NDQ_003388

answers: Stress interviews

answers: NDQ_003389

answers: Stress interviews

answers: NDQ_003390

answers: Stress interviews

answers: NDQ_003391

answers: Stress interviews

answers: NDQ_003392

answers: off-balance.

answers: NDQ_003393

answers: Stress interviews

answers: NDQ_003394

answers: Stress interviews

answers: NDQ_003395

answers: Stress interviews

answers: NDQ_003396

answers: Stress interviews

text: Before the concept of plate tectonics, global cooling was a geophysical theory by James Dwight Dana, also referred to as the contracting earth theory.  It suggested that the Earth had been in a molten state, and features such as mountains formed as it cooled and shrank.  As the interior of the Earth cooled and shrank, the rigid crust would have to shrink and crumple.  The crumpling could produce features such as mountain ranges.

text: Before the concept of

text: plate tectonics

text: , global cooling was a

text: geophysical

text: theory by

text: James Dwight Dana

text: , also referred to as the contracting earth theory.  It suggested that the

text: Earth

text: had been in a molten state, and features such as mountains formed as it cooled and shrank.  As the interior of the Earth cooled and shrank, the rigid crust would have to shrink and crumple.  The crumpling could produce features such as mountain ranges.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: shrinks

answers: NDQ_003353

answers: crumpling

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: crumple

answers: NDQ_003356

answers: shrink

answers: NDQ_003357

answers: rigid crust would have to shrink and crumple

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: crumples

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: the Earth had been in a molten state

answers: NDQ_003363

answers: global cooling

answers: NDQ_003371

answers: Which of the following is not a theory: plate tectonics, global cooling or contracting earth theory?

answers: NDQ_003373

answers: How would you describe Dana's theory?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What would happen if the crust shrinks and crumples?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not a type of fold that arches upward?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: What is the cause of plate tectonics?

answers: NDQ_003387

answers: Which of the following is not a type of normal fault?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip faults, shear stress or crumpling?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: tectonics

answers: NDQ_003391

answers: mountain ranges

answers: NDQ_003392

answers: tectonics

answers: NDQ_003393

answers: rigid crust

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: tectonics

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: The crumpling

answers: NDQ_003352

answers: The crumpling

answers: NDQ_003353

answers: The crumpling

answers: NDQ_003354

answers: Before the concept of plate tectonics,

answers: NDQ_003355

answers: mountain ranges.

answers: NDQ_003356

answers: crumple.

answers: NDQ_003357

answers: The crumpling

answers: NDQ_003358

answers: mountain ranges.

answers: NDQ_003359

answers: The crumpling

answers: NDQ_003360

answers: The crumpling

answers: NDQ_003362

answers: molten state,

answers: NDQ_003363

answers: as it cooled and shrank.

answers: NDQ_003371

answers: The crumpling could produce features such as mountain ranges.

answers: NDQ_003373

answers: The crumpling could produce features such as mountain ranges.

answers: NDQ_003376

answers: mountain ranges.

answers: NDQ_003378

answers: Before the concept of plate tectonics,

answers: NDQ_003379

answers: Before the concept of plate tectonics,

answers: NDQ_003380

answers: the rigid crust would have to shrink and crumple.

answers: NDQ_003381

answers: the rigid crust would have to shrink and crumple.

answers: NDQ_003382

answers: crumple.

answers: NDQ_003383

answers: The crumpling

answers: NDQ_003384

answers: Before the concept of plate tectonics,

answers: NDQ_003385

answers: plate tectonics,

answers: NDQ_003386

answers: plate tectonics,

answers: NDQ_003387

answers: The crumpling

answers: NDQ_003388

answers: Before the concept of plate tectonics,

answers: NDQ_003389

answers: The crumpling

answers: NDQ_003390

answers: plate tectonics,

answers: NDQ_003391

answers: mountain ranges.

answers: NDQ_003392

answers: plate tectonics,

answers: NDQ_003393

answers: mountain ranges.

answers: NDQ_003394

answers: plate tectonics,

answers: NDQ_003395

answers: plate tectonics,

answers: NDQ_003396

answers: plate tectonics,

text: What also needs to be taken into account when looking for benefits of abiotic stress, is that one phenomenon may not affect an entire ecosystem in the same way.  While a flood will kill most plants living low on the ground in a certain area, if there is rice there, it will thrive in the wet conditions.Another example of this is in phytoplankton and zooplankton.  The same types of conditions are usually considered stressful for these two types of organisms.  They act very similarly when exposed to ultraviolet light and most toxins, but at elevated temperatures the phytoplankton reacts negatively, while the thermophilic zooplankton reacts positively to the increase in temperature. The two may be living in the same environment, but an increase in temperature of the area would prove stressful only for one of the organisms.

text: What also needs to be taken into account when looking for benefits of abiotic stress, is that one phenomenon may not affect an entire ecosystem in the same way.  While a flood will kill most plants living low on the ground in a certain area, if there is rice there, it will thrive in the wet conditions.Another example of this is in

text: phytoplankton

text: and

text: zooplankton

text: .  The same types of conditions are usually considered stressful for these two types of organisms.  They act very similarly when exposed to ultraviolet light and most toxins, but at elevated temperatures the phytoplankton reacts negatively, while the

text: thermophilic

text: zooplankton reacts positively to the increase in temperature. The two may be living in the same environment, but an increase in temperature of the area would prove stressful only for one of the organisms.

answers: NDQ_003351

answers: abiotic stress

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: abiotic stress

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: rice will thrive in the wet conditions

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: abiotic stress

answers: NDQ_003362

answers: rice there, it will thrive in the wet conditions

answers: NDQ_003363

answers: abiotic stress

answers: NDQ_003371

answers: Which of the following is an example of a thrust fault?

answers: NDQ_003373

answers: how would you describe compressive stresses?

answers: NDQ_003376

answers: basin-and-range

answers: NDQ_003378

answers: what is the second to last word in the passage?

answers: NDQ_003379

answers: what is the dip of the fault plane

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What type of stress does abiotic stress cause?

answers: NDQ_003382

answers: what is the most common stress at convergent plates

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: what is the cause of earthquakes

answers: NDQ_003387

answers: Which of the following is not an example of abiotic stress?

answers: NDQ_003388

answers: Which of the following is not an example of abiotic stress?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: a structural fault

answers: NDQ_003391

answers: dip-slip fault

answers: NDQ_003392

answers: Fracture

answers: NDQ_003393

answers: dip-slip fault

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: a vertical fault plane

answers: NDQ_003396

answers: horizontal fault

answers: NDQ_003351

answers: abiotic stress,

answers: NDQ_003352

answers: phytoplankton

answers: NDQ_003353

answers: toxins, but at elevated temperatures the phytoplankton reacts negatively,

answers: NDQ_003354

answers: one phenomenon may not affect an entire ecosystem in the same way.

answers: NDQ_003355

answers: low on the ground

answers: NDQ_003356

answers: one phenomenon may not affect an entire ecosystem in the same way.

answers: NDQ_003357

answers: flood will kill most plants living low on the ground in a certain area,

answers: NDQ_003358

answers: abiotic stress,

answers: NDQ_003359

answers: abiotic stress,

answers: NDQ_003360

answers: abiotic stress,

answers: NDQ_003362

answers: rice there, it will thrive in the wet conditions.Another

answers: NDQ_003363

answers: abiotic stress,

answers: NDQ_003371

answers: one phenomenon may not affect an entire ecosystem in the same way.

answers: NDQ_003373

answers: abiotic stress,

answers: NDQ_003376

answers: one phenomenon may not affect an entire ecosystem in the same way.

answers: NDQ_003378

answers: abiotic stress,

answers: NDQ_003379

answers: one phenomenon may not affect an entire ecosystem in the same way.

answers: NDQ_003380

answers: abiotic stress,

answers: NDQ_003381

answers: abiotic stress,

answers: NDQ_003382

answers: abiotic stress,

answers: NDQ_003383

answers: abiotic stress,

answers: NDQ_003384

answers: phytoplankton and zooplankton.

answers: NDQ_003385

answers: one phenomenon may not affect an entire ecosystem in the same way.

answers: NDQ_003386

answers: one phenomenon may not affect an entire ecosystem in the same way.

answers: NDQ_003387

answers: abiotic stress,

answers: NDQ_003388

answers: one phenomenon may not affect an entire ecosystem in the same way.

answers: NDQ_003389

answers: one phenomenon may not affect an entire ecosystem in the same way.

answers: NDQ_003390

answers: abiotic stress,

answers: NDQ_003391

answers: abiotic stress,

answers: NDQ_003392

answers: abiotic stress,

answers: NDQ_003393

answers: phytoplankton and zooplankton.

answers: NDQ_003394

answers: one phenomenon may not affect an entire ecosystem in the same way.

answers: NDQ_003395

answers: phytoplankton and zooplankton.

answers: NDQ_003396

answers: phytoplankton and zooplankton.

text: As it was observed early that although granite existed on continents, seafloor seemed to be composed of denser basalt, the prevailing concept during the first half of the twentieth century was that there were two types of crust, named "sial" (continental type crust) and "sima" (oceanic type crust). Furthermore, it was supposed that a static shell of strata was present under the continents. It therefore looked apparent that a layer of basalt (sial) underlies the continental rocks.

text: As it was observed early that although granite existed on continents, seafloor seemed to be composed of denser basalt, the prevailing concept during the first half of the twentieth century was that there were two types of crust, named "sial" (continental type crust) and "sima" (oceanic type crust). Furthermore, it was supposed that a static shell of strata was present under the continents. It therefore looked apparent that a layer of basalt (sial) underlies the continental rocks.

answers: NDQ_003351

answers: sial

answers: NDQ_003352

answers: denser

answers: NDQ_003353

answers: basalt to form

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: sial

answers: NDQ_003356

answers: swell

answers: NDQ_003357

answers: strata is present under the continents

answers: NDQ_003358

answers: static shell

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: continents

answers: NDQ_003362

answers: a static shell of strata was present under the continents

answers: NDQ_003363

answers: sial

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: what is the first type of crust?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a type of crust?

answers: NDQ_003381

answers: What would happen if a layer of basalt underlies the continental rocks?

answers: NDQ_003382

answers: what is the most common stress at convergent plates

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: What is the cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not a type of crust: continental, sial, or oceanic?

answers: NDQ_003388

answers: Which of the following is not an example of a strike-slip fault?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: silt

answers: NDQ_003391

answers: seafloor

answers: NDQ_003392

answers: silt

answers: NDQ_003393

answers: strata

answers: NDQ_003394

answers: lateral fault

answers: NDQ_003395

answers: a vertical fault plane

answers: NDQ_003396

answers: Sima

answers: NDQ_003351

answers: granite

answers: NDQ_003352

answers: denser

answers: NDQ_003353

answers: denser basalt,

answers: NDQ_003354

answers: a layer of basalt (sial) underlies the continental rocks.

answers: NDQ_003355

answers: "sial"

answers: NDQ_003356

answers: granite

answers: NDQ_003357

answers: a layer of basalt (sial) underlies the continental rocks.

answers: NDQ_003358

answers: static

answers: NDQ_003359

answers: a static shell of strata

answers: NDQ_003360

answers: continents,

answers: NDQ_003362

answers: a static shell of strata was present under the continents.

answers: NDQ_003363

answers: continents,

answers: NDQ_003371

answers: a layer of basalt (sial) underlies the continental rocks.

answers: NDQ_003373

answers: a layer of basalt (sial) underlies the continental rocks.

answers: NDQ_003376

answers: granite existed on continents,

answers: NDQ_003378

answers: two types of crust,

answers: NDQ_003379

answers: two types of crust,

answers: NDQ_003380

answers: two types of crust,

answers: NDQ_003381

answers: a layer of basalt (sial) underlies the continental rocks.

answers: NDQ_003382

answers: granite

answers: NDQ_003383

answers: granite

answers: NDQ_003384

answers: "sial"

answers: NDQ_003385

answers: "sial" (continental type crust)

answers: NDQ_003386

answers: two types of crust,

answers: NDQ_003387

answers: granite

answers: NDQ_003388

answers: granite

answers: NDQ_003389

answers: granite

answers: NDQ_003390

answers: granite

answers: NDQ_003391

answers: basalt

answers: NDQ_003392

answers: first half of the twentieth century

answers: NDQ_003393

answers: basalt (sial) underlies the continental rocks.

answers: NDQ_003394

answers: two types of crust,

answers: NDQ_003395

answers: two types of crust,

answers: NDQ_003396

answers: granite

text: Carrán-Los Venados () is a volcanic group of scoria cones, maars and small stratovolcanoes in southern Chile, southeast of Ranco Lake. The highest cone is Los Guindos (Spanish for "The Cherry Trees), which is a small stratovolcano with an elevation of .  The volcanic group has recorded eruptions from 1955 and 1979. Located south of Maihue Lake and north Puyehue Volcano Carrán-Los Venados group is placed at the intersection of several faults on the thin crust (~30 km) of southern Chile, among them Liquiñe-Ofqui and Futrono Fault.

text: Carrán-Los Venados () is a

text: volcanic group

text: of

text: scoria cone

text: s,

text: maars

text: and small

text: stratovolcano

text: es in

text: southern Chile

text: , southeast of

text: Ranco Lake

text: . The highest cone is Los Guindos (Spanish for "The Cherry Trees), which is a small stratovolcano with an elevation of .  The volcanic group has recorded eruptions from 1955 and 1979. Located south of

text: Maihue Lake

text: and north

text: Puyehue Volcano

text: Carrán-Los Venados group is placed at the intersection of several

text: fault

text: s on the thin

text: crust

text: (~30 km) of southern Chile, among them

text: Liquiñe-Ofqui

text: and

text: Futrono Fault

answers: NDQ_003351

answers: Fracture

answers: NDQ_003352

answers: more likely to crack

answers: NDQ_003353

answers: faults

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: maar

answers: NDQ_003356

answers: erupt

answers: NDQ_003357

answers: e-Ofqui and Futrono Fault are types of what?

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: faults

answers: NDQ_003362

answers: Futrono Fault is located on the thin crust

answers: NDQ_003363

answers: Futrono Fault

answers: NDQ_003371

answers: Which of the following is not a fault: Liqui e-Ofqui or Futrono Fault?

answers: NDQ_003373

answers: What is the main idea of this passage?

answers: NDQ_003376

answers: What type of forces are responsible for the formation of this terrain?

answers: NDQ_003378

answers: What is the highest cone?

answers: NDQ_003379

answers: What is the dip of the fault plane in a strike-slip fault?

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What type of stress does Carrán-Los Venados group experience?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is the name of the group placed at the intersection of several faults on the thin crust?

answers: NDQ_003386

answers: How would you describe Carrán-Los Venados group?

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: Liqui e-Ofqui or Futrono Fault?

answers: NDQ_003388

answers: What type of faults are Futrono Fault and Liqui e-Ofqui Fault?

answers: NDQ_003389

answers: It's impossible to say

answers: NDQ_003390

answers: Futrono

answers: NDQ_003391

answers: Futrono Fault

answers: NDQ_003392

answers: Futrono

answers: NDQ_003393

answers: stratovolcano

answers: NDQ_003394

answers: Futrono

answers: NDQ_003395

answers: futrono fault

answers: NDQ_003396

answers: Futrono

answers: NDQ_003351

answers: Futrono Fault.

answers: NDQ_003352

answers: faults

answers: NDQ_003353

answers: faults

answers: NDQ_003354

answers: Carrán-Los Venados

answers: NDQ_003355

answers: faults

answers: NDQ_003356

answers: faults

answers: NDQ_003357

answers: Futrono Fault.

answers: NDQ_003358

answers: faults

answers: NDQ_003359

answers: faults

answers: NDQ_003360

answers: faults

answers: NDQ_003362

answers: Futrono Fault.

answers: NDQ_003363

answers: faults

answers: NDQ_003371

answers: Futrono Fault.

answers: NDQ_003373

answers: faults

answers: NDQ_003376

answers: faults

answers: NDQ_003378

answers: faults

answers: NDQ_003379

answers: Futrono Fault.

answers: NDQ_003380

answers: faults

answers: NDQ_003381

answers: faults

answers: NDQ_003382

answers: faults

answers: NDQ_003383

answers: faults

answers: NDQ_003384

answers: faults

answers: NDQ_003385

answers: faults

answers: NDQ_003386

answers: faults

answers: NDQ_003387

answers: Futrono Fault.

answers: NDQ_003388

answers: Futrono Fault.

answers: NDQ_003389

answers: faults

answers: NDQ_003390

answers: Futrono Fault.

answers: NDQ_003391

answers: Futrono Fault.

answers: NDQ_003392

answers: Futrono Fault.

answers: NDQ_003393

answers: Futrono Fault.

answers: NDQ_003394

answers: Futrono Fault.

answers: NDQ_003395

answers: Futrono Fault.

answers: NDQ_003396

answers: Futrono Fault.

text: The Pan-African orogeny is equivalent to Asynitic in other parts of the earth. This event was associated with metamorphism, magmatism, folding, and faulting during Late Precambrian–Early Cambrian in Iran (e.g., south of Zanjan–Mahabad in Azerbaijan, Bafq in Central Iran. This tectonic phase started with tension or extension leading to the formation of rifts and generation of oceanic crust (e.g., in Takab and Anarak) and ended with folding, closure, metamorphism, growth of the continental crust, and development of regional faults.

text: The

text: Pan-African orogeny

text: is equivalent to Asynitic in other parts of the earth. This event was associated with

text: metamorphism

text: magmatism

text: , folding, and faulting during Late Precambrian–Early Cambrian in Iran (e.g., south of

text: Zanjan

text: Mahabad

text: in

text: Azerbaijan

text: Bafq

text: in Central Iran. This tectonic phase started with tension or extension leading to the formation of rifts and generation of oceanic crust (e.g., in Takab and Anarak) and ended with folding, closure, metamorphism, growth of the continental crust, and development of regional faults.

answers: NDQ_003351

answers: extension

answers: NDQ_003352

answers: folds

answers: NDQ_003353

answers: metamorphism

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: rift

answers: NDQ_003356

answers: fold

answers: NDQ_003357

answers: rifts and generation of oceanic crust

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: folds

answers: NDQ_003360

answers: continental crust

answers: NDQ_003362

answers: The Pan-African orogeny is equivalent to Asynitic in other parts of the earth.

answers: NDQ_003363

answers: Pan-African orogeny

answers: NDQ_003371

answers: What event was associated with magmatism, folding, and faulting during Late Precambrian–Early Cambrian in Iran?

answers: NDQ_003373

answers: What event was associated with magmatism, folding, and faulting during Late Precambrian–Early Cambrian in Iran

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: What event was associated with magmatism, folding, and faulting during Late Precambrian–Early Cambrian in Iran

answers: NDQ_003379

answers: What is the dip of the fault plane in a strike-slip fault?

answers: NDQ_003380

answers: What event was associated with magmatism?

answers: NDQ_003381

answers: What event was associated with magmatism?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What event was associated with metamorphism, magmatism, folding, and faulting?

answers: NDQ_003384

answers: What is the Pan-African orogeny equivalent to in other parts of the earth?

answers: NDQ_003385

answers: What is the name of the area where faults are clustered?

answers: NDQ_003386

answers: What is the cause of earthquakes?

answers: NDQ_003387

answers: What event was associated with metamorphism, magmatism, folding, and faulting?

answers: NDQ_003388

answers: What is the cause of strike-slip faults?

answers: NDQ_003389

answers: It's impossible to say

answers: NDQ_003390

answers: regional faulting

answers: NDQ_003391

answers: continental crust

answers: NDQ_003392

answers: faulting

answers: NDQ_003393

answers: continental crust

answers: NDQ_003394

answers: regional faults

answers: NDQ_003395

answers: regional faults

answers: NDQ_003396

answers: faulting

answers: NDQ_003351

answers: tension or extension

answers: NDQ_003352

answers: formation of rifts

answers: NDQ_003353

answers: rifts

answers: NDQ_003354

answers: The Pan-African orogeny

answers: NDQ_003355

answers: rifts

answers: NDQ_003356

answers: folding, and faulting

answers: NDQ_003357

answers: tension or extension

answers: NDQ_003358

answers: rifts

answers: NDQ_003359

answers: faults.

answers: NDQ_003360

answers: Pan-African orogeny

answers: NDQ_003362

answers: growth of the continental crust, and development of regional faults.

answers: NDQ_003363

answers: Pan-African orogeny

answers: NDQ_003371

answers: faulting

answers: NDQ_003373

answers: tension

answers: NDQ_003376

answers: metamorphism, magmatism, folding, and faulting

answers: NDQ_003378

answers: tension or extension

answers: NDQ_003379

answers: Late Precambrian–Early Cambrian

answers: NDQ_003380

answers: tension or extension

answers: NDQ_003381

answers: folding, and faulting

answers: NDQ_003382

answers: tension or extension

answers: NDQ_003383

answers: tension or extension

answers: NDQ_003384

answers: Asynitic

answers: NDQ_003385

answers: regional faults.

answers: NDQ_003386

answers: regional faults.

answers: NDQ_003387

answers: tension

answers: NDQ_003388

answers: regional faults.

answers: NDQ_003389

answers: folding,

answers: NDQ_003390

answers: regional faults.

answers: NDQ_003391

answers: rifts and generation of oceanic crust

answers: NDQ_003392

answers: regional faults.

answers: NDQ_003393

answers: rifts and generation of oceanic crust

answers: NDQ_003394

answers: regional faults.

answers: NDQ_003395

answers: regional faults.

answers: NDQ_003396

answers: regional faults.

text: During rifting, as the crust is thinned, the Earth's surface subsides and the Moho becomes correspondingly raised. At the same time, the mantle lithosphere becomes thinned, causing a rise of the top of the asthenosphere. Once rifting ceases, the mantle beneath the rift cools and this is accompanied by a broad area of post-rift subsidence. The amount of subsidence is directly related to the amount of thinning during the rifting phase calculated as the beta factor (initial crustal thickness divided by final crustal thickness), but is also affected by the degree to which the rift basin is filled at each stage, due to the greater density of sediments in contrast to water. The simple 'McKenzie model' of rifting, which considers the rifting stage to be instantaneous, provides a good first order estimate of the amount of crustal thinning from observations of the amount of post-rift subsidence. This has generally been replaced by the 'flexural cantilever model', which takes into account the geometry of the rift faults and the flexural isostasy of the upper part of the crust.

text: During rifting, as the crust is thinned, the Earth's surface subsides and the

text: Moho

text: becomes correspondingly raised. At the same time, the mantle lithosphere becomes thinned, causing a rise of the top of the

text: asthenosphere

text: . Once rifting ceases, the mantle beneath the rift cools and this is accompanied by a broad area of post-rift subsidence. The amount of subsidence is directly related to the amount of thinning during the rifting phase calculated as the beta factor (initial crustal thickness divided by final crustal thickness), but is also affected by the degree to which the rift basin is filled at each stage, due to the greater density of sediments in contrast to water. The simple 'McKenzie model' of rifting, which considers the rifting stage to be instantaneous, provides a good first order estimate of the amount of crustal thinning from observations of the amount of post-rift subsidence. This has generally been replaced by the 'flexural cantilever model', which takes into account the geometry of the rift faults and the

text: flexural

text: isostasy

text: of the upper part of the crust.

answers: NDQ_003351

answers: Moho

answers: NDQ_003352

answers: cantilever model

answers: NDQ_003353

answers: Moho

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: rift fault

answers: NDQ_003356

answers: subside

answers: NDQ_003357

answers: initial crustal thickness divided by final crustal thickness

answers: NDQ_003358

answers: rift

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: rift faults

answers: NDQ_003362

answers: the Earth's surface subsides and the Moho becomes correspondingly raised

answers: NDQ_003363

answers: rifting

answers: NDQ_003371

answers: What has generally been replaced by the 'flexural cantilever model'

answers: NDQ_003373

answers: What is the beta factor?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: vertical

answers: NDQ_003380

answers: What is a stress?

answers: NDQ_003381

answers: What is the Moho?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: What is the Moho?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: What is the cause of earthquakes?

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: unanswerable

answers: NDQ_003389

answers: rifting

answers: NDQ_003390

answers: rift faults

answers: NDQ_003391

answers: rift basin

answers: NDQ_003392

answers: rift faults

answers: NDQ_003393

answers: asthenosphere

answers: NDQ_003394

answers: rift faults

answers: NDQ_003395

answers: rift faults

answers: NDQ_003396

answers: rift faults

answers: NDQ_003351

answers: Moho becomes correspondingly raised.

answers: NDQ_003352

answers: raised.

answers: NDQ_003353

answers: Moho becomes correspondingly raised.

answers: NDQ_003354

answers: During rifting,

answers: NDQ_003355

answers: 'flexural cantilever

answers: NDQ_003356

answers: flexural isostasy

answers: NDQ_003357

answers: Moho becomes correspondingly raised.

answers: NDQ_003358

answers: rift faults

answers: NDQ_003359

answers: rift faults

answers: NDQ_003360

answers: rifting,

answers: NDQ_003362

answers: instantaneous,

answers: NDQ_003363

answers: rifting,

answers: NDQ_003371

answers: During rifting,

answers: NDQ_003373

answers: post-rift subsidence.

answers: NDQ_003376

answers: rift basin is filled at each stage,

answers: NDQ_003378

answers: post-rift subsidence.

answers: NDQ_003379

answers: raised.

answers: NDQ_003380

answers: post-rift subsidence.

answers: NDQ_003381

answers: During rifting,

answers: NDQ_003382

answers: rifting,

answers: NDQ_003383

answers: rift faults and the flexural isostasy

answers: NDQ_003384

answers: During rifting,

answers: NDQ_003385

answers: rift faults

answers: NDQ_003386

answers: During rifting,

answers: NDQ_003387

answers: rift faults

answers: NDQ_003388

answers: rift

answers: NDQ_003389

answers: rifting,

answers: NDQ_003390

answers: rift faults

answers: NDQ_003391

answers: mantle

answers: NDQ_003392

answers: rift faults

answers: NDQ_003393

answers: flexural isostasy

answers: NDQ_003394

answers: rift faults

answers: NDQ_003395

answers: rift faults

answers: NDQ_003396

answers: rift faults

text: The stress field in the crust has not yet been measured.

text: The stress field in the crust has not yet been measured.

answers: NDQ_003351

answers: unmeasured

answers: NDQ_003352

answers: is likely to crack

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: the stress field in the crust has not yet been measured

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: swell

answers: NDQ_003357

answers: if the stress field is not measured, what will happen to the crust?

answers: NDQ_003358

answers: stress zone

answers: NDQ_003359

answers: is pushed together

answers: NDQ_003360

answers: tectonic plates

answers: NDQ_003362

answers: The San Andreas fault is a tectonic fault.

answers: NDQ_003363

answers: the same time as the Earth.

answers: NDQ_003371

answers: Which of the following is an example of a thrust fault?

answers: NDQ_003373

answers: How would you describe the stress field in the crust?

answers: NDQ_003376

answers: None of the above choices.

answers: NDQ_003378

answers: The answer is no.

answers: NDQ_003379

answers: The dip of the fault plane is horizontal.

answers: NDQ_003380

answers: How would you describe the stress field in the crust?

answers: NDQ_003381

answers: Which of the following is an example of confining stress?

answers: NDQ_003382

answers: None of the above choices.

answers: NDQ_003383

answers: None of the above choices.

answers: NDQ_003384

answers: How would you describe a syncline?

answers: NDQ_003385

answers: None of the above choices.

answers: NDQ_003386

answers: None of the above choices.

answers: NDQ_003387

answers: Which of the following is not a cause of normal faults?

answers: NDQ_003388

answers: Which of the following is not a type of stress?

answers: NDQ_003389

answers: None of the above choices.

answers: NDQ_003390

answers: can not be determined

answers: NDQ_003391

answers: can not be mapped

answers: NDQ_003392

answers: can not be determined

answers: NDQ_003393

answers: does not have a stress field

answers: NDQ_003394

answers: is not vertical

answers: NDQ_003395

answers: is a fault

answers: NDQ_003396

answers: can be used to describe

answers: NDQ_003351

answers: The stress field in the crust has not yet been measured.

answers: NDQ_003352

answers: The stress field in the crust has not yet been measured.

answers: NDQ_003353

answers: The stress field in the crust has not yet been measured.

answers: NDQ_003354

answers: The stress field in the crust has not yet been measured.

answers: NDQ_003355

answers: The stress field

answers: NDQ_003356

answers: The stress field

answers: NDQ_003357

answers: The stress field

answers: NDQ_003358

answers: stress field

answers: NDQ_003359

answers: stress field in the crust has not yet been measured.

answers: NDQ_003360

answers: stress field in the crust

answers: NDQ_003362

answers: The stress field in the crust has not yet been measured.

answers: NDQ_003363

answers: The stress field in the crust has not yet been measured.

answers: NDQ_003371

answers: The stress field in the crust has not yet been measured.

answers: NDQ_003373

answers: The stress field in the crust has not yet been measured.

answers: NDQ_003376

answers: The stress field in the crust has not yet been measured.

answers: NDQ_003378

answers: The stress field in the crust has not yet been measured.

answers: NDQ_003379

answers: The stress field in the crust has not yet been measured.

answers: NDQ_003380

answers: The stress field in the crust has not yet been measured.

answers: NDQ_003381

answers: The stress field in the crust has not yet been measured.

answers: NDQ_003382

answers: The stress field in the crust has not yet been measured.

answers: NDQ_003383

answers: The stress field in the crust has not yet been measured.

answers: NDQ_003384

answers: The stress field in the crust has not yet been measured.

answers: NDQ_003385

answers: The stress field in the crust has not yet been measured.

answers: NDQ_003386

answers: The stress field in the crust has not yet been measured.

answers: NDQ_003387

answers: The stress field in the crust has not yet been measured.

answers: NDQ_003388

answers: The stress field in the crust has not yet been measured.

answers: NDQ_003389

answers: The stress field in the crust has not yet been measured.

answers: NDQ_003390

answers: The stress field in the crust has not yet been measured.

answers: NDQ_003391

answers: The stress field in the crust has not yet been measured.

answers: NDQ_003392

answers: The stress field in the crust has not yet been measured.

answers: NDQ_003393

answers: The stress field in the crust has not yet been measured.

answers: NDQ_003394

answers: The stress field in the crust has not yet been measured.

answers: NDQ_003395

answers: The stress field in the crust has not yet been measured.

answers: NDQ_003396

answers: The stress field in the crust has not yet been measured.

text: Stressful life experiences may be a cause of memory loss as a person ages. Glucocorticoids that are released during stress damage neurons that are located in the hippocampal region of the brain. Therefore, the more stressful situations that someone encounters, the more susceptible they are to memory loss later on. The CA1 neurons found in the hippocampus are destroyed due to glucocorticoids decreasing the release of glucose and the reuptake of glutamate. This high level of extracellular glutamate allow calcium to enter NMDA receptors which in return kills neurons. Stressful life experiences can also cause repression of memories where a person moves an unbearable memory to the unconscious mind. This directly relates to traumatic events in one's past such as kidnappings, being prisoners of war or sexual abuse as a child.

text: Stressful life experiences may be a cause of memory loss as a person ages. Glucocorticoids that are released during stress damage neurons that are located in the hippocampal region of the brain. Therefore, the more stressful situations that someone encounters, the more susceptible they are to memory loss later on. The CA1 neurons found in the hippocampus are destroyed due to glucocorticoids decreasing the release of glucose and the reuptake of glutamate. This high level of extracellular glutamate allow calcium to enter NMDA receptors which in return kills neurons. Stressful life experiences can also cause repression of memories where a person moves an unbearable memory to the unconscious mind. This directly relates to traumatic events in one's past such as kidnappings, being prisoners of war or sexual abuse as a child.

answers: NDQ_003351

answers: Glucocorticoids

answers: NDQ_003352

answers: is more likely to break

answers: NDQ_003353

answers: calcium to enter NMDA receptors

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: lose their shape

answers: NDQ_003357

answers: Glucocorticoids decrease the release of what?

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: kidnappings, being prisoners of war

answers: NDQ_003363

answers: stressful life experiences

answers: NDQ_003371

answers: What may be a cause of memory loss as a person ages?

answers: NDQ_003373

answers: What is the main idea of this passage?

answers: NDQ_003376

answers: Which of the following is not caused by compressive forces?

answers: NDQ_003378

answers: Which of the following is not a type of memory loss?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: Which of the following is not a cause of memory loss as a person ages?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: Which of the following is not a type of syncline?

answers: NDQ_003385

answers: Which of the following is not an example of a fault zone?

answers: NDQ_003386

answers: Which of the following is not a cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not a cause of memory loss as a person ages

answers: NDQ_003388

answers: Which of the following is not a result of shear stress?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: repression

answers: NDQ_003391

answers: dip-slip fault plane

answers: NDQ_003392

answers: repression

answers: NDQ_003393

answers: dip-slip fault plane

answers: NDQ_003394

answers: is a

answers: NDQ_003395

answers: a vertical fault plane

answers: NDQ_003396

answers: NDQ_003351

answers: kidnappings, being prisoners of war

answers: NDQ_003352

answers: Glucocorticoids

answers: NDQ_003353

answers: Glucocorticoids

answers: NDQ_003354

answers: Stressful life experiences

answers: NDQ_003355

answers: Stressful life experiences may be a cause of memory loss

answers: NDQ_003356

answers: memory loss

answers: NDQ_003357

answers: a person moves an unbearable memory to the unconscious mind.

answers: NDQ_003358

answers: Stressful life experiences

answers: NDQ_003359

answers: calcium

answers: NDQ_003360

answers: Stressful life experiences

answers: NDQ_003362

answers: Glucocorticoids

answers: NDQ_003363

answers: prisoners of war

answers: NDQ_003371

answers: Stressful life experiences may be a cause of memory loss

answers: NDQ_003373

answers: Stressful life experiences

answers: NDQ_003376

answers: Glucocorticoids

answers: NDQ_003378

answers: Glucocorticoids

answers: NDQ_003379

answers: Glucocorticoids

answers: NDQ_003380

answers: stress

answers: NDQ_003381

answers: Glucocorticoids

answers: NDQ_003382

answers: Glucocorticoids

answers: NDQ_003383

answers: Glucocorticoids

answers: NDQ_003384

answers: Glucocorticoids

answers: NDQ_003385

answers: Glucocorticoids

answers: NDQ_003386

answers: Stressful life experiences

answers: NDQ_003387

answers: traumatic events

answers: NDQ_003388

answers: Glucocorticoids

answers: NDQ_003389

answers: Glucocorticoids

answers: NDQ_003390

answers: Stressful life experiences may be a cause of memory loss

answers: NDQ_003391

answers: Glucocorticoids

answers: NDQ_003392

answers: Stressful life experiences

answers: NDQ_003393

answers: Glucocorticoids

answers: NDQ_003394

answers: NMDA receptors

answers: NDQ_003395

answers: NMDA receptors

answers: NDQ_003396

answers: reuptake of glutamate.

text: The Deep Energy Community is dedicated to quantifying the environmental conditions and processes from the molecular to the global scale that control the origins, forms, quantities and movements of reduced carbon compounds derived from deep carbon through deep geologic time.  The Deep Energy Community uses field-based investigations of approximately 25 globally representative terrestrial and marine environments to determine processes controlling the origin, form, quantities and movements of abiotic gases and organic species in Earth’s crust and uppermost mantle. Deep Energy also uses DCO-sponsored instrumentation, especially revolutionary isotopologue measurements, to discriminate between the abiotic and biotic methane gas and organic species sampled from global terrestrial and marine field sites. Another research activity of Deep Energy is to quantify the mechanisms and rates of fluid-rock interactions that produce abiotic hydrogen and organic compounds as a function of temperature, pressure, fluid and solid compositions.

text: The Deep Energy Community is dedicated to quantifying the environmental conditions and processes from the molecular to the global scale that control the origins, forms, quantities and movements of reduced carbon compounds derived from deep carbon through deep geologic time.  The Deep Energy Community uses field-based investigations of approximately 25 globally representative terrestrial and marine environments to determine processes controlling the origin, form, quantities and movements of abiotic gases and organic species in Earth’s crust and uppermost mantle. Deep Energy also uses DCO-sponsored instrumentation, especially revolutionary isotopologue measurements, to discriminate between the abiotic and biotic methane gas and organic species sampled from global terrestrial and marine field sites. Another research activity of Deep Energy is to quantify the mechanisms and rates of fluid-rock interactions that produce abiotic hydrogen and organic compounds as a function of temperature, pressure, fluid and solid compositions.

answers: NDQ_003351

answers: pressure

answers: NDQ_003352

answers: produces more organic compounds

answers: NDQ_003353

answers: fluid-rock interactions

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: mantle

answers: NDQ_003356

answers: produce organic compounds

answers: NDQ_003357

answers: temperature, pressure, fluid and solid compositions

answers: NDQ_003358

answers: solid

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth’s crust

answers: NDQ_003362

answers: Deep Energy also uses DCO-sponsored instrumentation

answers: NDQ_003363

answers: Deep Energy Community

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: pressure

answers: NDQ_003376

answers: basin-and-range

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What is a function of temperature, pressure, fluid and solid compositions

answers: NDQ_003381

answers: What is a function of temperature?

answers: NDQ_003382

answers: What is the most common stress at convergent plates

answers: NDQ_003383

answers: temperature, pressure

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: movement of rock at faults

answers: NDQ_003387

answers: temperature, pressure, fluid and solid compositions

answers: NDQ_003388

answers: The Deep Energy Community uses field-based investigations

answers: NDQ_003389

answers: geologic time

answers: NDQ_003390

answers: isotopologue measurements

answers: NDQ_003391

answers: mantle

answers: NDQ_003392

answers: isotopologue

answers: NDQ_003393

answers: uppermost mantle

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: Earth’s crust and uppermost mantle

answers: NDQ_003396

answers: abiotic

answers: NDQ_003351

answers: pressure,

answers: NDQ_003352

answers: temperature, pressure, fluid and solid compositions.

answers: NDQ_003353

answers: abiotic hydrogen and organic compounds

answers: NDQ_003354

answers: 25 globally representative terrestrial and marine environments

answers: NDQ_003355

answers: uppermost mantle.

answers: NDQ_003356

answers: solid

answers: NDQ_003357

answers: temperature, pressure,

answers: NDQ_003358

answers: biotic

answers: NDQ_003359

answers: fluid-rock interactions

answers: NDQ_003360

answers: deep geologic time.

answers: NDQ_003362

answers: time.

answers: NDQ_003363

answers: deep carbon through deep geologic time.

answers: NDQ_003371

answers: deep geologic time.

answers: NDQ_003373

answers: temperature, pressure,

answers: NDQ_003376

answers: temperature, pressure,

answers: NDQ_003378

answers: movements of reduced carbon compounds derived from deep carbon through deep geologic time.

answers: NDQ_003379

answers: 25 globally representative terrestrial and marine environments

answers: NDQ_003380

answers: temperature, pressure,

answers: NDQ_003381

answers: temperature, pressure,

answers: NDQ_003382

answers: pressure,

answers: NDQ_003383

answers: temperature, pressure,

answers: NDQ_003384

answers: uppermost mantle.

answers: NDQ_003385

answers: deep geologic time.

answers: NDQ_003386

answers: fluid-rock interactions

answers: NDQ_003387

answers: temperature, pressure,

answers: NDQ_003388

answers: time.

answers: NDQ_003389

answers: fluid-rock interactions

answers: NDQ_003390

answers: deep geologic time.

answers: NDQ_003391

answers: uppermost mantle.

answers: NDQ_003392

answers: time.

answers: NDQ_003393

answers: uppermost mantle.

answers: NDQ_003394

answers: Earth’s crust and uppermost mantle.

answers: NDQ_003395

answers: Earth’s crust and uppermost mantle.

answers: NDQ_003396

answers: uppermost mantle.

text: An overturned anticline is an asymmetrical anticline with a limb that has been tilted beyond perpendicular so that the beds in that limb have basically flipped over and may dip in the same direction on both sides of the axial plane. If the angle between the limbs is large (70-120 degrees), then the fold is an open fold, but if the angle between the limbs is small (30 degrees or less), then the fold is a tight fold. If an anticline plunges (i.e., the anticline crest is inclined to the Earth's surface), it will form Vs on a geologic map view that point in the direction of plunge. A plunging anticline has a hinge that is not parallel to the earth's surface.  All anticlines and synclines have some degree of plunge. Periclinal folds are a type of anticlines that have a well-defined, but curved hinge line and are doubly plunging and thus elongate domes.

text: An overturned anticline is an asymmetrical anticline with a limb that has been tilted beyond

text: perpendicular

text: so that the beds in that limb have basically flipped over and may dip in the same direction on both sides of the axial plane. If the angle between the limbs is large (70-120 degrees), then the fold is an open fold, but if the angle between the limbs is small (30 degrees or less), then the fold is a tight fold. If an anticline plunges (i.e., the anticline crest is inclined to the Earth's surface), it will form Vs on a

text: geologic map

text: view that point in the direction of

text: plunge

text: . A plunging anticline has a hinge that is not parallel to the earth's surface.  All anticlines and synclines have some degree of plunge. Periclinal folds are a type of anticlines that have a well-defined, but curved hinge line and are doubly plunging and thus elongate

text: domes

answers: NDQ_003351

answers: open fold

answers: NDQ_003352

answers: is more likely to crack

answers: NDQ_003353

answers: Anticlines and synclines to form Vs

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: unanswerable

answers: NDQ_003356

answers: overturn

answers: NDQ_003357

answers: anticline crest is inclined to the Earth's surface

answers: NDQ_003358

answers: syncline

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's surface

answers: NDQ_003362

answers: anticline crest is inclined to the Earth's surface

answers: NDQ_003363

answers: overturned anticlines

answers: NDQ_003371

answers: What type of fold is an overturned anticline with a limb that has been tilted beyond perpendicular

answers: NDQ_003373

answers: If the angle between the limbs is large (70-120 degrees), then the fold is an open fold

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: What is the amount the ground moves in an earthquake?

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a stress?

answers: NDQ_003381

answers: What type of rock deforms?

answers: NDQ_003382

answers: What is the most common stress at convergent plates

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not a type of anticlines: Periclinal folds?

answers: NDQ_003385

answers: What is the term for an area where faults are clustered?

answers: NDQ_003386

answers: What is the cause of earthquakes?

answers: NDQ_003387

answers: Which is not a type of anticlines that have a well-defined, but curved hinge line?

answers: NDQ_003388

answers: Which of the following is not a type of anticline that have a well-defined, but curved hinge line?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: a plunging anticline

answers: NDQ_003391

answers: anticline

answers: NDQ_003392

answers: overturned anticline

answers: NDQ_003393

answers: anticline crest

answers: NDQ_003394

answers: A plunging anticline

answers: NDQ_003395

answers: An overturned anticline

answers: NDQ_003396

answers: synclines

answers: NDQ_003351

answers: overturned anticline

answers: NDQ_003352

answers: Vs

answers: NDQ_003353

answers: Vs

answers: NDQ_003354

answers: An overturned anticline

answers: NDQ_003355

answers: plunging anticline

answers: NDQ_003356

answers: Vs

answers: NDQ_003357

answers: All anticlines and synclines have some degree of plunge.

answers: NDQ_003358

answers: tight fold.

answers: NDQ_003359

answers: plunge.

answers: NDQ_003360

answers: overturned anticline

answers: NDQ_003362

answers: An overturned anticline

answers: NDQ_003363

answers: overturned anticline

answers: NDQ_003371

answers: overturned anticline

answers: NDQ_003373

answers: overturned anticline

answers: NDQ_003376

answers: overturned anticline

answers: NDQ_003378

answers: plunge.

answers: NDQ_003379

answers: same direction on both sides of the axial plane.

answers: NDQ_003380

answers: All anticlines and synclines have some degree of plunge.

answers: NDQ_003381

answers: Vs

answers: NDQ_003382

answers: plunge.

answers: NDQ_003383

answers: Vs

answers: NDQ_003384

answers: synclines have some degree of plunge.

answers: NDQ_003385

answers: overturned anticline

answers: NDQ_003386

answers: overturned anticline

answers: NDQ_003387

answers: All anticlines and synclines have some degree of plunge.

answers: NDQ_003388

answers: An overturned anticline

answers: NDQ_003389

answers: Periclinal folds

answers: NDQ_003390

answers: overturned anticline

answers: NDQ_003391

answers: overturned anticline

answers: NDQ_003392

answers: overturned anticline

answers: NDQ_003393

answers: overturned anticline

answers: NDQ_003394

answers: A plunging anticline

answers: NDQ_003395

answers: axial plane.

answers: NDQ_003396

answers: overturned anticline

text: As the earth's crust was stretched above the mantle hotspot under stress from plate rifting, fissures opened up along a line from Ireland to the Hebrides and plutonic complexes were formed. Hot magma over 1000 °C surfaced as multiple, successive and extensive lava flows covered over the original landscape, burning forests, filling river valleys, burying hills, to eventually form the Thulean Plateau, which contained various volcanic landforms such as lava fields and volcanoes. There was more than one period of volcanic activity during the NAIP, in between which sea levels rose and fell and erosion took place.

text: As the earth's crust was stretched above the

text: mantle

text: hotspot under stress from plate rifting, fissures opened up along a line from Ireland to the

text: Hebrides

text: and

text: plutonic

text: complexes were formed. Hot

text: magma

text: over 1000 °C surfaced as multiple, successive and extensive

text: lava

text: flows covered over the original landscape, burning forests, filling river valleys, burying hills, to eventually form the Thulean Plateau, which contained various volcanic landforms such as

text: lava fields

text: and

text: volcanoes

text: . There was more than one period of volcanic activity during the NAIP, in between which sea levels rose and fell and

text: erosion

text: took place.

answers: NDQ_003351

answers: plate rifting

answers: NDQ_003352

answers: is more likely to crack

answers: NDQ_003353

answers: fissures

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fissure

answers: NDQ_003356

answers: erode

answers: NDQ_003357

answers: landforms such as lava fields and volcanoes are formed

answers: NDQ_003358

answers: fissure

answers: NDQ_003359

answers: plate rifting

answers: NDQ_003360

answers: plate faulting

answers: NDQ_003362

answers: sea levels rose and fell and erosion took place.

answers: NDQ_003363

answers: Thulean Plateau

answers: NDQ_003371

answers: Which of the following is not a landform: lava fields and volcanoes?

answers: NDQ_003373

answers: not enough information

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What type of force applied to rock is stress?

answers: NDQ_003381

answers: unanswerable

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What type of fold does the text describe?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: plate rifting

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: Which of the following is not a type of strike-slip fault?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: plate rifting

answers: NDQ_003391

answers: mantle hotspot

answers: NDQ_003392

answers: plate rifting

answers: NDQ_003393

answers: mantle hotspot

answers: NDQ_003394

answers: fissures opened up along a line

answers: NDQ_003395

answers: plate rifting

answers: NDQ_003396

answers: plate rifting

answers: NDQ_003351

answers: plate rifting,

answers: NDQ_003352

answers: fissures opened up

answers: NDQ_003353

answers: fissures

answers: NDQ_003354

answers: Thulean Plateau,

answers: NDQ_003355

answers: fissures

answers: NDQ_003356

answers: erosion

answers: NDQ_003357

answers: fissures

answers: NDQ_003358

answers: fissures

answers: NDQ_003359

answers: stress

answers: NDQ_003360

answers: plate rifting,

answers: NDQ_003362

answers: Ireland to the Hebrides

answers: NDQ_003363

answers: Thulean Plateau,

answers: NDQ_003371

answers: plate rifting,

answers: NDQ_003373

answers: hills,

answers: NDQ_003376

answers: Thulean Plateau,

answers: NDQ_003378

answers: stress from plate rifting,

answers: NDQ_003379

answers: Thulean Plateau,

answers: NDQ_003380

answers: stress

answers: NDQ_003381

answers: plate rifting,

answers: NDQ_003382

answers: plate rifting,

answers: NDQ_003383

answers: fissures

answers: NDQ_003384

answers: Thulean Plateau,

answers: NDQ_003385

answers: fissures

answers: NDQ_003386

answers: fissures

answers: NDQ_003387

answers: plate rifting,

answers: NDQ_003388

answers: plate rifting,

answers: NDQ_003389

answers: plate rifting,

answers: NDQ_003390

answers: fissures

answers: NDQ_003391

answers: hills,

answers: NDQ_003392

answers: fissures

answers: NDQ_003393

answers: mantle hotspot

answers: NDQ_003394

answers: fissures

answers: NDQ_003395

answers: fissures

answers: NDQ_003396

answers: plate rifting,

text: Most geological samples from Earth are unable to give a direct date of the formation of Earth from the solar nebula because Earth has undergone differentiation into the core, mantle, and crust, and this has then undergone a long history of mixing and unmixing of these sample reservoirs by plate tectonics, weathering and hydrothermal circulation.

text: Most geological samples from Earth are unable to give a direct date of the formation of Earth from the solar nebula because Earth has undergone differentiation into the core, mantle, and crust, and this has then undergone a long history of mixing and unmixing of these sample reservoirs by

text: plate tectonics

text: weathering

text: and

text: hydrothermal circulation

answers: NDQ_003351

answers: hydrothermal circulation

answers: NDQ_003352

answers: increases in hardness

answers: NDQ_003353

answers: weathering

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: weather

answers: NDQ_003357

answers: plate tectonics is the movement of

answers: NDQ_003358

answers: weathering

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: plate tectonics

answers: NDQ_003362

answers: most geological samples from Earth are unable to give a direct date

answers: NDQ_003363

answers: plate tectonics

answers: NDQ_003371

answers: Which of the following is not a type of fault?

answers: NDQ_003373

answers: what is the last word in the passage?

answers: NDQ_003376

answers: not enough information

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a stress?

answers: NDQ_003381

answers: What is the main idea of this passage?

answers: NDQ_003382

answers: what is the most common stress at convergent plates

answers: NDQ_003383

answers: None of the above choices.

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: plate tectonics

answers: NDQ_003386

answers: plate tectonics

answers: NDQ_003387

answers: Which of the following is not a type of plate tectonics?

answers: NDQ_003388

answers: Which of the following is not an example of plate tectonics?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: plate tectonics

answers: NDQ_003391

answers: mantle

answers: NDQ_003392

answers: plate tectonics

answers: NDQ_003393

answers: mantle

answers: NDQ_003394

answers: isobath

answers: NDQ_003395

answers: is a type

answers: NDQ_003396

answers: unmixed

answers: NDQ_003351

answers: plate tectonics,

answers: NDQ_003352

answers: weathering

answers: NDQ_003353

answers: weathering

answers: NDQ_003354

answers: Most geological samples

answers: NDQ_003355

answers: plate tectonics,

answers: NDQ_003356

answers: weathering

answers: NDQ_003357

answers: mixing and unmixing

answers: NDQ_003358

answers: weathering

answers: NDQ_003359

answers: mixing and unmixing

answers: NDQ_003360

answers: plate tectonics,

answers: NDQ_003362

answers: direct date of the formation of Earth from the solar nebula

answers: NDQ_003363

answers: solar nebula

answers: NDQ_003371

answers: Most geological samples

answers: NDQ_003373

answers: Most geological samples

answers: NDQ_003376

answers: plate tectonics, weathering and hydrothermal circulation.

answers: NDQ_003378

answers: Most geological samples

answers: NDQ_003379

answers: solar nebula

answers: NDQ_003380

answers: Earth has undergone differentiation into the core, mantle, and crust,

answers: NDQ_003381

answers: Most geological samples

answers: NDQ_003382

answers: plate tectonics,

answers: NDQ_003383

answers: Most geological samples

answers: NDQ_003384

answers: solar nebula

answers: NDQ_003385

answers: plate tectonics,

answers: NDQ_003386

answers: plate tectonics,

answers: NDQ_003387

answers: Most geological samples

answers: NDQ_003388

answers: Most geological samples

answers: NDQ_003389

answers: plate tectonics,

answers: NDQ_003390

answers: plate tectonics,

answers: NDQ_003391

answers: core, mantle, and crust,

answers: NDQ_003392

answers: plate tectonics,

answers: NDQ_003393

answers: crust,

answers: NDQ_003394

answers: plate tectonics,

answers: NDQ_003395

answers: plate tectonics,

answers: NDQ_003396

answers: plate tectonics,

text: Strike slip dulexes are passive structures; they form as a response to displacement of the bounding fault rather than by the stresses from plate motion. Each horse has a length that varies from half to twice the spacing between the bounding fault planes. Depending on the properties of the rocks and the fault, the duplexes will have different length ratios and will develop on either major or subtle offsets, although it is possible to observe duplex structures that develop on nearly straight fault segments.Because the motion of the duplexes may be heterogeneous, the individual horses can experience a rotation with a horizontal axis, which results in the formation of scissor faults. Scissor faults exhibit normal motion at one end of the horse and a thrust motion ant the other end. Because strike slip duplexes structures have more horizontal motion than vertical motion, they are best observed on a map rather than a vertical projection, and are a good indication that the main fault has a strike slip motion.

text: Strike slip dulexes are passive structures; they form as a response to displacement of the bounding fault rather than by the stresses from plate motion. Each horse has a length that varies from half to twice the spacing between the bounding fault planes. Depending on the properties of the rocks and the fault, the duplexes will have different length ratios and will develop on either major or subtle offsets, although it is possible to observe duplex structures that develop on nearly straight fault segments.Because the motion of the duplexes may be heterogeneous, the individual horses can experience a rotation with a horizontal axis, which results in the formation of scissor faults. Scissor faults exhibit normal motion at one end of the horse and a thrust motion ant the other end. Because strike slip duplexes structures have more horizontal motion than vertical motion, they are best observed on a map rather than a vertical projection, and are a good indication that the main fault has a strike slip motion.

answers: NDQ_003351

answers: plate motion

answers: NDQ_003352

answers: is more likely to form

answers: NDQ_003353

answers: strike slip duplexes

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: scissor fault

answers: NDQ_003356

answers: Strike slip dulexes

answers: NDQ_003357

answers: normal motion at one end of the horse and a thrust motion at the other end

answers: NDQ_003358

answers: unanswerable

answers: NDQ_003359

answers: displacement

answers: NDQ_003360

answers: plate motion

answers: NDQ_003362

answers: Strike slip dulexes are passive structures

answers: NDQ_003363

answers: strike slip duplexes

answers: NDQ_003371

answers: What is a good indication that the main fault has a strike slip motion?

answers: NDQ_003373

answers: unanswerable

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: no

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: Which of the following is not a result of plate motion: Strike slip dulexes

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: What is the name of the area where faults are clustered?

answers: NDQ_003386

answers: plate motion

answers: NDQ_003387

answers: Which of the following is not a type of strike slip duplex?

answers: NDQ_003388

answers: unanswerable

answers: NDQ_003389

answers: plate motion

answers: NDQ_003390

answers: scissor faults

answers: NDQ_003391

answers: duplexes

answers: NDQ_003392

answers: scissor faults

answers: NDQ_003393

answers: strike slip dulexes

answers: NDQ_003394

answers: scissor faults

answers: NDQ_003395

answers: strike slip duplexes structures have more horizontal motion than vertical motion

answers: NDQ_003396

answers: scissor fault

answers: NDQ_003351

answers: plate motion.

answers: NDQ_003352

answers: scissor faults.

answers: NDQ_003353

answers: scissor faults.

answers: NDQ_003354

answers: Strike slip dulexes

answers: NDQ_003355

answers: scissor faults.

answers: NDQ_003356

answers: scissor faults.

answers: NDQ_003357

answers: normal motion

answers: NDQ_003358

answers: Strike slip dulexes

answers: NDQ_003359

answers: displacement of the bounding fault

answers: NDQ_003360

answers: plate motion.

answers: NDQ_003362

answers: stresses from plate motion.

answers: NDQ_003363

answers: bounding fault

answers: NDQ_003371

answers: Scissor faults

answers: NDQ_003373

answers: Strike slip dulexes

answers: NDQ_003376

answers: scissor faults.

answers: NDQ_003378

answers: Strike slip

answers: NDQ_003379

answers: strike slip duplexes structures have more horizontal motion than vertical

answers: NDQ_003380

answers: stresses

answers: NDQ_003381

answers: scissor faults.

answers: NDQ_003382

answers: plate motion.

answers: NDQ_003383

answers: stresses from plate motion.

answers: NDQ_003384

answers: scissor faults.

answers: NDQ_003385

answers: Strike slip dulexes

answers: NDQ_003386

answers: displacement of the bounding fault rather than by the stresses from plate motion.

answers: NDQ_003387

answers: plate motion.

answers: NDQ_003388

answers: plate motion.

answers: NDQ_003389

answers: Strike slip dulexes

answers: NDQ_003390

answers: scissor faults.

answers: NDQ_003391

answers: Strike slip dulexes

answers: NDQ_003392

answers: scissor faults.

answers: NDQ_003393

answers: Strike slip dulexes

answers: NDQ_003394

answers: scissor faults.

answers: NDQ_003395

answers: scissor faults.

answers: NDQ_003396

answers: scissor faults.

text: The region is also traversed by six major slip-strike fault systems with hundreds of related faults, many of which are "sister faults" of the infamous San Andreas Fault, all of which are stressed by the relative motion between the Pacific Plate and the North American Plate or by compressive stresses between these plates. The fault systems include the Hayward Fault Zone, Concord-Green Valley Fault, Calaveras Fault, Clayton-Marsh Creek-Greenville Fault, and the San Gregorio Fault. Significant blind thrust faults (faults with near vertical motion and no surface ruptures) are associated with portions of the Santa Cruz Mountains and the northern reaches of the Diablo Range and Mount Diablo.

text: The region is also traversed by six major slip-strike fault systems with hundreds of related faults, many of which are "sister faults" of the infamous

text: San Andreas Fault

text: , all of which are stressed by the relative motion between the

text: Pacific Plate

text: and the

text: North American Plate

text: or by compressive stresses between these plates. The fault systems include the

text: Hayward Fault Zone

text: Concord-Green Valley Fault

text: Calaveras Fault

text: Clayton-Marsh Creek-Greenville Fault

text: , and the

text: San Gregorio Fault

text: . Significant blind

text: thrust fault

text: s (faults with near vertical motion and no surface ruptures) are associated with portions of the

text: Santa Cruz Mountains

text: and the northern reaches of the

text: Diablo Range

text: and

text: Mount Diablo

answers: NDQ_003351

answers: compressive stresses

answers: NDQ_003352

answers: compresses

answers: NDQ_003353

answers: compressive stresses

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: blind thrust faults

answers: NDQ_003356

answers: compress

answers: NDQ_003357

answers: surface ruptures

answers: NDQ_003358

answers: blind thrust fault

answers: NDQ_003359

answers: compressive stresses

answers: NDQ_003360

answers: Pacific Plate

answers: NDQ_003362

answers: many of which are "sister faults" of the infamous San Andreas Fault

answers: NDQ_003363

answers: San Andreas Fault

answers: NDQ_003371

answers: What type of faults are associated with portions of the Santa Cruz Mountains?

answers: NDQ_003373

answers: not enough information

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: relative motion

answers: NDQ_003379

answers: not enough information

answers: NDQ_003380

answers: compressive stresses between these plates

answers: NDQ_003381

answers: compressive stresses

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: compressive stresses between these plates

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: Fault Zone

answers: NDQ_003386

answers: What is the cause of earthquakes?

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: Which of the following is not a type of fault: slip-strike fault or blind thrust fault?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: blind thrust faults

answers: NDQ_003391

answers: Santa Cruz Mountains

answers: NDQ_003392

answers: blind thrust

answers: NDQ_003393

answers: surface ruptures

answers: NDQ_003394

answers: blind thrust faults

answers: NDQ_003395

answers: blind thrust faults

answers: NDQ_003396

answers: blind thrust faults

answers: NDQ_003351

answers: compressive stresses

answers: NDQ_003352

answers: surface ruptures)

answers: NDQ_003353

answers: surface ruptures)

answers: NDQ_003354

answers: six major slip-strike fault systems with hundreds of related faults,

answers: NDQ_003355

answers: blind thrust faults

answers: NDQ_003356

answers: surface ruptures)

answers: NDQ_003357

answers: surface ruptures)

answers: NDQ_003358

answers: blind thrust faults

answers: NDQ_003359

answers: compressive stresses

answers: NDQ_003360

answers: relative motion between the Pacific Plate and the North American Plate

answers: NDQ_003362

answers: "sister faults"

answers: NDQ_003363

answers: San Andreas Fault,

answers: NDQ_003371

answers: Significant blind thrust faults

answers: NDQ_003373

answers: compressive stresses

answers: NDQ_003376

answers: compressive stresses

answers: NDQ_003378

answers: slip-strike

answers: NDQ_003379

answers: blind thrust faults

answers: NDQ_003380

answers: compressive stresses

answers: NDQ_003381

answers: compressive stresses

answers: NDQ_003382

answers: compressive stresses

answers: NDQ_003383

answers: compressive stresses

answers: NDQ_003384

answers: blind thrust faults

answers: NDQ_003385

answers: The fault systems

answers: NDQ_003386

answers: compressive stresses between these plates.

answers: NDQ_003387

answers: compressive stresses between these plates.

answers: NDQ_003388

answers: compressive stresses between these plates.

answers: NDQ_003389

answers: six major slip-strike fault systems

answers: NDQ_003390

answers: blind thrust faults

answers: NDQ_003391

answers: blind thrust faults

answers: NDQ_003392

answers: blind thrust faults

answers: NDQ_003393

answers: blind thrust faults

answers: NDQ_003394

answers: blind thrust faults

answers: NDQ_003395

answers: blind thrust faults

answers: NDQ_003396

answers: blind thrust faults

text: Earth movements after the Carboniferous period resulted in the up-doming of the area and, particularly in the west, the folding of the rock strata along north–south axes. The region was raised in a north–south line which resulted in this dome-like shape and the shale and sandstone were worn away until limestone was exposed. At the end of this period, the Earth's crust sank here which led to the area being covered by sea, depositing a variety of new rocks.

text: Earth movements after the Carboniferous period resulted in the up-doming of the area and, particularly in the west, the folding of the rock strata along north–south axes. The region was raised in a north–south line which resulted in this dome-like shape and the shale and sandstone were worn away until limestone was exposed. At the end of this period, the Earth's crust sank here which led to the area being covered by sea, depositing a variety of new rocks.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: wears away

answers: NDQ_003353

answers: the rock to fold

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: up-doming

answers: NDQ_003356

answers: up-dome

answers: NDQ_003357

answers: rock strata along north–south axes

answers: NDQ_003358

answers: unanswerable

answers: NDQ_003359

answers: folds

answers: NDQ_003360

answers: North–South axes

answers: NDQ_003362

answers: the Earth's crust sank here

answers: NDQ_003363

answers: Carboniferous

answers: NDQ_003371

answers: Which of the following is not a result of Earth movements after the Carboniferous period?

answers: NDQ_003373

answers: How would you describe a rock that is deeply buried?

answers: NDQ_003376

answers: What caused the region to be raised in a north–south line?

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What was the result of the up-doming of the area?

answers: NDQ_003381

answers: Which of the following is not a type of rock: shale and sandstone?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: What type of fold is raised in a north–south line?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: Which of the following is not the cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: up-doming of the area or normal faults?

answers: NDQ_003388

answers: Which of the following is not a result of shear stress: up-doming of the area and, particularly in the west, the folding of the rock strata

answers: NDQ_003389

answers: It is impossible to say

answers: NDQ_003390

answers: up-doming

answers: NDQ_003391

answers: Dome

answers: NDQ_003392

answers: up-doming

answers: NDQ_003393

answers: dome

answers: NDQ_003394

answers: south axes

answers: NDQ_003395

answers: north–south

answers: NDQ_003396

answers: north–south

answers: NDQ_003351

answers: north–south axes.

answers: NDQ_003352

answers: worn away

answers: NDQ_003353

answers: folding

answers: NDQ_003354

answers: Earth movements after the Carboniferous

answers: NDQ_003355

answers: up-doming

answers: NDQ_003356

answers: folding of the rock strata along north–south axes.

answers: NDQ_003357

answers: north–south axes.

answers: NDQ_003358

answers: up-doming

answers: NDQ_003359

answers: folding of the rock strata along north–south axes.

answers: NDQ_003360

answers: north–south axes.

answers: NDQ_003362

answers: the Earth's crust sank here

answers: NDQ_003363

answers: Carboniferous period

answers: NDQ_003371

answers: north–south axes.

answers: NDQ_003373

answers: rock strata along north–south axes.

answers: NDQ_003376

answers: folding of the rock strata along north–south axes.

answers: NDQ_003378

answers: folding of the rock strata along north–south axes.

answers: NDQ_003379

answers: north–south axes.

answers: NDQ_003380

answers: folding of the rock strata along north–south axes.

answers: NDQ_003381

answers: folding of the rock strata along north–south axes.

answers: NDQ_003382

answers: north–south axes.

answers: NDQ_003383

answers: folding of the rock strata along north–south axes.

answers: NDQ_003384

answers: north–south line

answers: NDQ_003385

answers: north–south axes.

answers: NDQ_003386

answers: Earth movements

answers: NDQ_003387

answers: north–south axes.

answers: NDQ_003388

answers: north–south axes.

answers: NDQ_003389

answers: folding of the rock strata

answers: NDQ_003390

answers: north–south axes.

answers: NDQ_003391

answers: limestone

answers: NDQ_003392

answers: up-doming

answers: NDQ_003393

answers: limestone

answers: NDQ_003394

answers: north–south axes.

answers: NDQ_003395

answers: north–south axes.

answers: NDQ_003396

answers: north–south axes.

text: Secondary stress occurs when a word contains two or more primary stressed syllables, in which case all but one primary stress is reduced to secondary. There are exceptions in certain syllables that are always secondarily stressed, regardless of the alternating pattern of lightly and heavily stressed syllables following the primarily stressed syllable. This type of secondary stress is included as part of the morpheme. Suffixes that have this type of stress include  'plural habitual', and  'sentence connective'.

text: Secondary stress occurs when a word contains two or more primary stressed syllables, in which case all but one primary stress is reduced to secondary. There are exceptions in certain syllables that are always secondarily stressed, regardless of the alternating pattern of lightly and heavily stressed syllables following the primarily stressed syllable. This type of secondary stress is included as part of the morpheme. Suffixes that have this type of stress include  'plural habitual', and  'sentence connective'.

answers: NDQ_003351

answers: secondary

answers: NDQ_003352

answers: swells

answers: NDQ_003353

answers: secondary stress

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone.

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: deform

answers: NDQ_003357

answers: primary stress is reduced to secondary

answers: NDQ_003358

answers: place

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Wyoming

answers: NDQ_003362

answers: secondary stress is included as part of the morpheme

answers: NDQ_003363

answers: most

answers: NDQ_003371

answers: very old

answers: NDQ_003373

answers: compressive

answers: NDQ_003376

answers: compressive forces

answers: NDQ_003378

answers: slip

answers: NDQ_003379

answers: vertical

answers: NDQ_003380

answers: Any

answers: NDQ_003381

answers: secondary

answers: NDQ_003382

answers: secondary

answers: NDQ_003383

answers: secondary stress

answers: NDQ_003384

answers: syncline

answers: NDQ_003385

answers: fault zone

answers: NDQ_003386

answers: Secondary stress

answers: NDQ_003387

answers: secondary stress

answers: NDQ_003388

answers: shear stress

answers: NDQ_003389

answers: secondary

answers: NDQ_003390

answers: secondary

answers: NDQ_003391

answers: block of rock

answers: NDQ_003392

answers: secondary

answers: NDQ_003393

answers: block of rock

answers: NDQ_003394

answers: vertical

answers: NDQ_003395

answers: fault

answers: NDQ_003396

answers: horizontal

answers: NDQ_003351

answers: Secondary stress

answers: NDQ_003352

answers: Secondary stress

answers: NDQ_003353

answers: Secondary stress

answers: NDQ_003354

answers: Secondary stress

answers: NDQ_003355

answers: Secondary stress

answers: NDQ_003356

answers: Secondary stress

answers: NDQ_003357

answers: lightly and heavily stressed syllables

answers: NDQ_003358

answers: Secondary stress

answers: NDQ_003359

answers: two or more primary stressed syllables,

answers: NDQ_003360

answers: Secondary stress

answers: NDQ_003362

answers: Secondary stress

answers: NDQ_003363

answers: Secondary stress

answers: NDQ_003371

answers: Secondary stress

answers: NDQ_003373

answers: Secondary stress

answers: NDQ_003376

answers: Secondary stress

answers: NDQ_003378

answers: Secondary stress

answers: NDQ_003379

answers: Secondary stress

answers: NDQ_003380

answers: Secondary stress

answers: NDQ_003381

answers: Secondary stress

answers: NDQ_003382

answers: Secondary stress

answers: NDQ_003383

answers: Secondary stress

answers: NDQ_003384

answers: Secondary stress

answers: NDQ_003385

answers: Secondary stress

answers: NDQ_003386

answers: Secondary stress

answers: NDQ_003387

answers: Secondary stress

answers: NDQ_003388

answers: Secondary stress

answers: NDQ_003389

answers: Secondary stress

answers: NDQ_003390

answers: Secondary stress

answers: NDQ_003391

answers: Secondary stress

answers: NDQ_003392

answers: Secondary stress

answers: NDQ_003393

answers: Secondary stress

answers: NDQ_003394

answers: Secondary stress

answers: NDQ_003395

answers: Secondary stress

answers: NDQ_003396

answers: Secondary stress

text: The continental crust consists of various layers, with a bulk composition that is intermediate to felsic. The average density of continental crust is about 2.7 g/cm, less dense than the ultramafic material that makes up the mantle, which has a density of around 3.3 g/cm. Continental crust is also less dense than oceanic crust, whose density is about 2.9 g/cm. At 25 to 70 km, continental crust is considerably thicker than oceanic crust, which has an average thickness of around 7–10 km. About 40% of Earth's surface is currently occupied by continental crust.It makes up about 70% of the volume of Earth's crust.

text: The continental crust consists of various layers, with a bulk composition that is

text: intermediate

text: to felsic. The average density of continental crust is about 2.7 g/cm, less

text: dense

text: than the ultramafic material that makes up the

text: mantle

text: , which has a density of around 3.3 g/cm. Continental crust is also less dense than oceanic crust, whose density is about 2.9 g/cm. At 25 to 70 km, continental crust is considerably thicker than oceanic crust, which has an average thickness of around 7–10 km. About 40% of Earth's surface is currently occupied by continental crust.It makes up about 70% of the volume of

text: Earth's crust

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: has a higher density

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: continental crust

answers: NDQ_003356

answers: be less dense than oceanic crust

answers: NDQ_003357

answers: continental crust is considerably thicker than oceanic crust

answers: NDQ_003358

answers: mantle

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: continental crust

answers: NDQ_003362

answers: about 70% of the volume of Earth's crust.

answers: NDQ_003363

answers: oceanic crust

answers: NDQ_003371

answers: What is the bulk composition of continental crust?

answers: NDQ_003373

answers: about 70% of the volume of Earth's crust

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a stress?

answers: NDQ_003381

answers: How does rock deform?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: fault zone

answers: NDQ_003386

answers: movement of rock at faults

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: normal faults, mantle or oceanic crust?

answers: NDQ_003388

answers: What is the average density of continental crust?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: a hanging wall

answers: NDQ_003391

answers: continental crust

answers: NDQ_003392

answers: a hanging wall

answers: NDQ_003393

answers: continental crust

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: fault with a vertical fault plane

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: The continental crust

answers: NDQ_003352

answers: thicker

answers: NDQ_003353

answers: thicker than oceanic crust,

answers: NDQ_003354

answers: 40% of Earth's surface is currently occupied by continental crust.It

answers: NDQ_003355

answers: The continental crust

answers: NDQ_003356

answers: felsic.

answers: NDQ_003357

answers: 25 to 70 km, continental crust is considerably thicker than oceanic crust,

answers: NDQ_003358

answers: The continental crust

answers: NDQ_003359

answers: The continental crust

answers: NDQ_003360

answers: continental crust

answers: NDQ_003362

answers: The continental crust

answers: NDQ_003363

answers: 25 to 70 km, continental crust is considerably thicker than oceanic crust,

answers: NDQ_003371

answers: The continental crust

answers: NDQ_003373

answers: The continental crust

answers: NDQ_003376

answers: 40% of Earth's surface is currently occupied by continental crust.It

answers: NDQ_003378

answers: 40% of Earth's surface is currently occupied by continental crust.It

answers: NDQ_003379

answers: 70%

answers: NDQ_003380

answers: 40% of Earth's surface is currently occupied by continental crust.It

answers: NDQ_003381

answers: The continental crust

answers: NDQ_003382

answers: 40% of Earth's surface is currently occupied by continental crust.It

answers: NDQ_003383

answers: The continental crust

answers: NDQ_003384

answers: 40% of Earth's surface is currently occupied by continental crust.It

answers: NDQ_003385

answers: The continental crust

answers: NDQ_003386

answers: The continental crust

answers: NDQ_003387

answers: The continental crust

answers: NDQ_003388

answers: 2.7 g/cm,

answers: NDQ_003389

answers: The continental crust

answers: NDQ_003390

answers: The continental crust

answers: NDQ_003391

answers: continental crust

answers: NDQ_003392

answers: The continental crust

answers: NDQ_003393

answers: continental crust

answers: NDQ_003394

answers: The continental crust

answers: NDQ_003395

answers: The continental crust

answers: NDQ_003396

answers: continental crust is considerably thicker than oceanic crust,

text: Stress ulcers, as defined by overt bleeding and hemodynamic instability, decreased hemoglobin, and/or need for transfusion, were seen in 1.5% of patients in the 2252 patients in the Canadian Critical Care Trials group study. People with stress ulcers have a longer ICU length of stay (up to 8 days) and a higher mortality (up to 4 fold) than compared to patients who do not have stress ulceration and bleeding. While the bleeding and transfusions associated with the stress ulcerations contribute to the increased mortality, the contribution of factors like hypotension, sepsis, and respiratory failure to the mortality independently of the stress ulceration cannot be ignored.

text: Stress ulcers, as defined by overt bleeding and hemodynamic instability, decreased hemoglobin, and/or need for transfusion, were seen in 1.5% of patients in the 2252 patients in the Canadian Critical Care Trials group study. People with stress ulcers have a longer ICU length of stay (up to 8 days) and a higher mortality (up to 4 fold) than compared to patients who do not have stress ulceration and bleeding. While the bleeding and transfusions associated with the stress ulcerations contribute to the increased mortality, the contribution of factors like hypotension, sepsis, and respiratory failure to the mortality independently of the stress ulceration cannot be ignored.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: is more likely to crack

answers: NDQ_003353

answers: stress ulcers

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: stress ulcer

answers: NDQ_003356

answers: bleed

answers: NDQ_003357

answers: hemodynamic instability is defined by

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: a higher mortality (up to 4 folds)

answers: NDQ_003363

answers: the same time

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: What is the main idea of this passage?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: stress ulcers

answers: NDQ_003379

answers: strike-slip fault

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: Which of the following is not an example of confining stress?

answers: NDQ_003382

answers: what is the most common stress at convergent plates

answers: NDQ_003383

answers: no

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: Fault zone

answers: NDQ_003386

answers: None of the above choices.

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: hemodynamic instability, decreased hemoglobin, or need for transfusion?

answers: NDQ_003388

answers: Which of the following is not a result of shear stress?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: stress ulcers

answers: NDQ_003391

answers: dip-slip fault

answers: NDQ_003392

answers: stress ulcers

answers: NDQ_003393

answers: a dip-slip fault plane

answers: NDQ_003394

answers: can be ignored

answers: NDQ_003395

answers: NDQ_003396

answers: NDQ_003351

answers: Stress ulcers,

answers: NDQ_003352

answers: Stress ulcers,

answers: NDQ_003353

answers: bleeding and hemodynamic instability, decreased hemoglobin,

answers: NDQ_003354

answers: Stress ulcers,

answers: NDQ_003355

answers: Stress ulcers,

answers: NDQ_003356

answers: Stress ulcers,

answers: NDQ_003357

answers: hypotension, sepsis, and respiratory failure

answers: NDQ_003358

answers: Stress ulcers,

answers: NDQ_003359

answers: Stress ulcers,

answers: NDQ_003360

answers: Stress ulcers,

answers: NDQ_003362

answers: Stress ulcers,

answers: NDQ_003363

answers: Stress ulcers,

answers: NDQ_003371

answers: Stress ulcers,

answers: NDQ_003373

answers: Stress ulcers,

answers: NDQ_003376

answers: Stress ulcers,

answers: NDQ_003378

answers: Stress ulcers,

answers: NDQ_003379

answers: Stress ulcers,

answers: NDQ_003380

answers: Stress ulcers,

answers: NDQ_003381

answers: Stress ulcers,

answers: NDQ_003382

answers: Stress ulcers,

answers: NDQ_003383

answers: Stress ulcers,

answers: NDQ_003384

answers: Stress ulcers,

answers: NDQ_003385

answers: Stress ulcers,

answers: NDQ_003386

answers: Stress ulcers,

answers: NDQ_003387

answers: Stress ulcers,

answers: NDQ_003388

answers: Stress ulcers,

answers: NDQ_003389

answers: Stress ulcers,

answers: NDQ_003390

answers: Stress ulcers,

answers: NDQ_003391

answers: Stress ulcers,

answers: NDQ_003392

answers: Stress ulcers,

answers: NDQ_003393

answers: Stress ulcers,

answers: NDQ_003394

answers: Stress ulcers,

answers: NDQ_003395

answers: Stress ulcers,

answers: NDQ_003396

answers: Stress ulcers,

text: Most of these "faults" are actually zones of complex faulting at the boundaries between sedimentary basins (synclines) and crustal uplifts (anticlines). There is a general pattern where most of these faults partition a series of basins and uplifts, each about 20 km wide. From the north these are (see the map at right):

text: Most of these "faults" are actually zones of complex faulting at the boundaries between sedimentary basins (

text: synclines

text: ) and crustal uplifts (

text: anticlines

text: ). There is a general pattern where most of these faults partition a series of basins and uplifts, each about 20 km wide. From the north these are (see the map at right):

answers: NDQ_003351

answers: anticlines

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: syncline

answers: NDQ_003356

answers: swell

answers: NDQ_003357

answers: a series of basins and uplifts, each about 20 km wide

answers: NDQ_003358

answers: anticlinal

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: crustal uplifts

answers: NDQ_003362

answers: a series of basins and uplifts, each about 20 km wide

answers: NDQ_003363

answers: the boundaries between sedimentary basins

answers: NDQ_003371

answers: Which of the following is not a type of fault?

answers: NDQ_003373

answers: What is the term for this type of stress?

answers: NDQ_003376

answers: Which of the following is not a cause of basin-and-range terrain?

answers: NDQ_003378

answers: Which of the following is not a type of fault?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What is the result of confining stress?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the main cause of joints in rock?

answers: NDQ_003384

answers: What type of fold is a syncline?

answers: NDQ_003385

answers: what is the correct answer?

answers: NDQ_003386

answers: What is the main cause of earthquakes?

answers: NDQ_003387

answers: What type of stress is caused by normal faults?

answers: NDQ_003388

answers: Which of the following is not a type of fault?

answers: NDQ_003389

answers: What is the process of folding?

answers: NDQ_003390

answers: Anticline

answers: NDQ_003391

answers: Anticline

answers: NDQ_003392

answers: Anticline

answers: NDQ_003393

answers: Anticline

answers: NDQ_003394

answers: anticlinal

answers: NDQ_003395

answers: Anticline

answers: NDQ_003396

answers: Anticline

answers: NDQ_003351

answers: (anticlines).

answers: NDQ_003352

answers: "faults"

answers: NDQ_003353

answers: faulting

answers: NDQ_003354

answers: Most of these "faults"

answers: NDQ_003355

answers: (anticlines).

answers: NDQ_003356

answers: "faults"

answers: NDQ_003357

answers: a series of basins and uplifts, each about 20 km wide.

answers: NDQ_003358

answers: (anticlines).

answers: NDQ_003359

answers: faulting

answers: NDQ_003360

answers: "faults"

answers: NDQ_003362

answers: Most of these "faults"

answers: NDQ_003363

answers: "faults"

answers: NDQ_003371

answers: "faults"

answers: NDQ_003373

answers: "faults"

answers: NDQ_003376

answers: "faults" are actually zones of complex faulting

answers: NDQ_003378

answers: "faults" are actually zones of complex faulting

answers: NDQ_003379

answers: (synclines) and crustal uplifts

answers: NDQ_003380

answers: "faults" are actually zones of complex faulting

answers: NDQ_003381

answers: "faults" are actually zones of complex faulting

answers: NDQ_003382

answers: (synclines) and crustal uplifts

answers: NDQ_003383

answers: "faults" are actually zones of complex faulting

answers: NDQ_003384

answers: sedimentary basins

answers: NDQ_003385

answers: "faults"

answers: NDQ_003386

answers: faulting

answers: NDQ_003387

answers: complex faulting

answers: NDQ_003388

answers: complex faulting

answers: NDQ_003389

answers: "faults" are actually zones of complex faulting

answers: NDQ_003390

answers: "faults"

answers: NDQ_003391

answers: (anticlines).

answers: NDQ_003392

answers: (anticlines).

answers: NDQ_003393

answers: (anticlines).

answers: NDQ_003394

answers: (anticlines).

answers: NDQ_003395

answers: (anticlines).

answers: NDQ_003396

answers: (anticlines).

text: The Sea of Marmara is a pull-apart basin formed at a releasing bend in the North Anatolian Fault, a right-lateral strike-slip fault. This local zone of extension occurs where this transform boundary between the Anatolian Plate and the Eurasian Plate steps northwards to the west of Izmit from the Izmit Fault to the Ganos Fault. The pattern of faults within the Sea of Marmara basin is complex but near Istanbul there is a single main fault segment with a sharp bend. To the west, the fault trends west-east and is pure strike-slip in type. To the east, the fault is NW-SE trending and shows evidence of both normal and strike-slip motion. Movement on this fault, which bounds the Çınarcık Basin, was the most likely cause of the 1509 event.

text: The

text: Sea of Marmara

text: is a

text: pull-apart basin

text: formed at a

entity_section: Releasing bends along strike-slip faults

text: releasing bend

text: in the

text: North Anatolian Fault

text: , a right-lateral

text: strike-slip fault

text: . This local zone of extension occurs where this

text: transform

text: boundary between the

text: Anatolian Plate

text: and the

text: Eurasian Plate

text: steps northwards to the west of

text: Izmit

text: from the Izmit Fault to the Ganos Fault. The pattern of faults within the Sea of Marmara basin is complex but near

text: Istanbul

text: there is a single main fault segment with a sharp bend. To the west, the fault trends west-east and is pure strike-slip in type. To the east, the fault is NW-SE trending and shows evidence of

text: both normal and strike-slip

text: motion. Movement on this fault, which bounds the Çınarcık Basin, was the most likely cause of the 1509 event.

answers: NDQ_003351

answers: strike-slip

answers: NDQ_003352

answers: is more likely to crack

answers: NDQ_003353

answers: Strike-slip

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: strike-slip

answers: NDQ_003356

answers: pull apart

answers: NDQ_003357

answers: west-east and pure strike-slip in type

answers: NDQ_003358

answers: normal

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: faults

answers: NDQ_003362

answers: The pattern of faults within the Sea of Marmara basin is complex

answers: NDQ_003363

answers: North Anatolian Fault

answers: NDQ_003371

answers: What is the most likely cause of the 1509 event?

answers: NDQ_003373

answers: What is the most likely cause of the 1509 event?

answers: NDQ_003376

answers: What is the most likely cause of the 1509 event?

answers: NDQ_003378

answers: strike-slip

answers: NDQ_003379

answers: What is the dip of the fault plane

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What is the most likely cause of the 1509 event?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the most likely cause of the 1509 event?

answers: NDQ_003384

answers: What type of fold is the Sea of Marmara?

answers: NDQ_003385

answers: The pattern of faults within the Sea of Marmara basin

answers: NDQ_003386

answers: What is the most likely cause of the 1509 event?

answers: NDQ_003387

answers: Which of the following is not a type of fault: strike-slip or normal?

answers: NDQ_003388

answers: What type of fault is the North Anatolian Fault?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: strike-slip fault

answers: NDQ_003391

answers: Anatolian Plate

answers: NDQ_003392

answers: strike-slip fault

answers: NDQ_003393

answers: plate

answers: NDQ_003394

answers: North Anatolian Fault

answers: NDQ_003395

answers: North Anatolian Fault

answers: NDQ_003396

answers: strike-slip fault

answers: NDQ_003351

answers: strike-slip

answers: NDQ_003352

answers: normal and strike-slip motion.

answers: NDQ_003353

answers: strike-slip fault.

answers: NDQ_003354

answers: North Anatolian Fault,

answers: NDQ_003355

answers: strike-slip fault.

answers: NDQ_003356

answers: strike-slip

answers: NDQ_003357

answers: strike-slip

answers: NDQ_003358

answers: normal

answers: NDQ_003359

answers: normal and strike-slip motion.

answers: NDQ_003360

answers: North Anatolian Fault,

answers: NDQ_003362

answers: pure strike-slip

answers: NDQ_003363

answers: North Anatolian Fault,

answers: NDQ_003371

answers: strike-slip fault.

answers: NDQ_003373

answers: North Anatolian Fault,

answers: NDQ_003376

answers: North Anatolian Fault,

answers: NDQ_003378

answers: strike-slip

answers: NDQ_003379

answers: right-lateral

answers: NDQ_003380

answers: strike-slip fault.

answers: NDQ_003381

answers: North Anatolian Fault,

answers: NDQ_003382

answers: strike-slip

answers: NDQ_003383

answers: bend.

answers: NDQ_003384

answers: North Anatolian Fault,

answers: NDQ_003385

answers: complex but near Istanbul there is a single main fault segment

answers: NDQ_003386

answers: 1509

answers: NDQ_003387

answers: strike-slip

answers: NDQ_003388

answers: strike-slip

answers: NDQ_003389

answers: North Anatolian Fault,

answers: NDQ_003390

answers: North Anatolian Fault,

answers: NDQ_003391

answers: strike-slip

answers: NDQ_003392

answers: North Anatolian Fault,

answers: NDQ_003393

answers: strike-slip

answers: NDQ_003394

answers: right-lateral

answers: NDQ_003395

answers: North Anatolian Fault,

answers: NDQ_003396

answers: right-lateral strike-slip

text: All of the fragments that make up the Armorican terrane are thought to have originally formed part of the northern margin of Gondwana. Rifting initiated in the Cambrian to Ordovician although the terrane was still close enough to Gondwana to be affected by the Andean-Saharan glaciation during the late Ordovician. Complete separation from Gondwana, across the developing Paleotethys Ocean, is thought to have occurred towards the end of the Silurian. At this time Armorica was separated from Laurussia by the Rheic Ocean. One possible model includes Armorica as part of the Hun superterrane, while other show it moving separately. The Rheic Ocean closed during the Devonian and early Carboniferous, as the oceanic crust was subducted. The Variscan orogeny marks the final closure of the Rheic Ocean as the various continental fragments, including Armorica, collided with Laurussia towards the end of the Carboniferous.

text: All of the fragments that make up the Armorican terrane are thought to have originally formed part of the northern margin of Gondwana. Rifting initiated in the

text: Cambrian

text: to

text: Ordovician

text: although the terrane was still close enough to Gondwana to be affected by the

text: Andean-Saharan glaciation

text: during the late Ordovician. Complete separation from Gondwana, across the developing

text: Paleotethys Ocean

text: , is thought to have occurred towards the end of the Silurian. At this time Armorica was separated from Laurussia by the

text: Rheic Ocean

text: . One possible model includes Armorica as part of the Hun superterrane, while other show it moving separately. The Rheic Ocean closed during the Devonian and early Carboniferous, as the

text: oceanic crust

text: was

text: subducted

text: . The Variscan orogeny marks the final closure of the Rheic Ocean as the various continental fragments, including Armorica, collided with Laurussia towards the end of the Carboniferous.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: collides with other rocks

answers: NDQ_003353

answers: Rifting

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: Rifting

answers: NDQ_003356

answers: collide

answers: NDQ_003357

answers: The Rheic Ocean closed during what time period?

answers: NDQ_003358

answers: glaciation

answers: NDQ_003359

answers: collides

answers: NDQ_003360

answers: Variscan orogeny

answers: NDQ_003362

answers: Armorica as part of the Hun superterrane

answers: NDQ_003363

answers: Variscan orogeny

answers: NDQ_003371

answers: What is the name of the oceanic crust?

answers: NDQ_003373

answers: How would you describe the Rheic Ocean?

answers: NDQ_003376

answers: What type of terrain is caused by compressive forces?

answers: NDQ_003378

answers: what is the first time period mentioned?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What happened to the Rheic Ocean during the Devonian?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Rifting initiated in the Cambrian to Ordovician

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: Rifting initiated in the Cambrian to Ordovician

answers: NDQ_003387

answers: Which happened first, the Cambrian to Ordovician or the end of the Silurian?

answers: NDQ_003388

answers: What type of fault is Armorica?

answers: NDQ_003389

answers: Rifting

answers: NDQ_003390

answers: Variscan

answers: NDQ_003391

answers: Armorica

answers: NDQ_003392

answers: Variscan

answers: NDQ_003393

answers: terrane

answers: NDQ_003394

answers: Variscan

answers: NDQ_003395

answers: Variscan

answers: NDQ_003396

answers: Variscan orogeny

answers: NDQ_003351

answers: Andean-Saharan glaciation

answers: NDQ_003352

answers: Rifting

answers: NDQ_003353

answers: Rifting

answers: NDQ_003354

answers: Cambrian to Ordovician

answers: NDQ_003355

answers: Rifting

answers: NDQ_003356

answers: Rifting

answers: NDQ_003357

answers: subducted.

answers: NDQ_003358

answers: terrane

answers: NDQ_003359

answers: subducted.

answers: NDQ_003360

answers: Rifting

answers: NDQ_003362

answers: Andean-Saharan glaciation

answers: NDQ_003363

answers: Gondwana.

answers: NDQ_003371

answers: Rifting initiated in the Cambrian to Ordovician

answers: NDQ_003373

answers: oceanic crust was subducted.

answers: NDQ_003376

answers: Rifting

answers: NDQ_003378

answers: Rifting initiated in the Cambrian to Ordovician

answers: NDQ_003379

answers: Cambrian to Ordovician

answers: NDQ_003380

answers: Rifting

answers: NDQ_003381

answers: Rifting initiated in the Cambrian to Ordovician

answers: NDQ_003382

answers: Andean-Saharan glaciation

answers: NDQ_003383

answers: Rifting

answers: NDQ_003384

answers: Cambrian to Ordovician

answers: NDQ_003385

answers: Rifting initiated in the Cambrian to Ordovician

answers: NDQ_003386

answers: Rifting

answers: NDQ_003387

answers: Rifting initiated in the Cambrian to Ordovician

answers: NDQ_003388

answers: Cambrian to Ordovician

answers: NDQ_003389

answers: Rifting

answers: NDQ_003390

answers: Rifting initiated in the Cambrian to Ordovician

answers: NDQ_003391

answers: oceanic crust was subducted.

answers: NDQ_003392

answers: Rifting initiated in the Cambrian to Ordovician

answers: NDQ_003393

answers: Armorican terrane

answers: NDQ_003394

answers: Rifting initiated in the Cambrian to Ordovician

answers: NDQ_003395

answers: Rifting initiated in the Cambrian to Ordovician

answers: NDQ_003396

answers: Cambrian to Ordovician

text: Tin is the 49th most abundant element in Earth's crust, representing 2 ppm compared with 75 ppm for zinc, 50 ppm for copper, and 14 ppm for lead.

text: Tin is the 49th most abundant element in

text: Earth

text: 's

text: crust

text: , representing 2

text: ppm

text: compared with 75 ppm for zinc, 50 ppm for copper, and 14 ppm for lead.

answers: NDQ_003351

answers: lead

answers: NDQ_003352

answers: is exposed to more heat

answers: NDQ_003353

answers: voids to form.

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: lead

answers: NDQ_003357

answers: zinc is more abundant than lead.

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: Tin is the 49th most abundant element in Earth's crust

answers: NDQ_003363

answers: Earth's crust

answers: NDQ_003371

answers: What is the most abundant element in Earth's crust?

answers: NDQ_003373

answers: How would you describe the stress?

answers: NDQ_003376

answers: ppm

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What is the most abundant element in Earth's crust?

answers: NDQ_003381

answers: What is the most abundant element in Earth's crust?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: None of the above choices.

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: unanswerable

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: what is the second most abundant element in Earth's crust?

answers: NDQ_003388

answers: what is the second most abundant element in Earth's crust?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: NDQ_003392

answers: fault in which the hanging wall pushes

answers: NDQ_003393

answers: dip-slip fault plane

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: is a fault

answers: NDQ_003396

answers: NDQ_003351

answers: lead.

answers: NDQ_003352

answers: 75 ppm for zinc,

answers: NDQ_003353

answers: Tin is the 49th most abundant element in Earth's crust,

answers: NDQ_003354

answers: 75 ppm for zinc,

answers: NDQ_003355

answers: Tin is the 49th most abundant element in Earth's crust,

answers: NDQ_003356

answers: 75 ppm for zinc,

answers: NDQ_003357

answers: lead.

answers: NDQ_003358

answers: Tin is the 49th most abundant element in Earth's crust,

answers: NDQ_003359

answers: Tin is the 49th most abundant element in Earth's crust,

answers: NDQ_003360

answers: Tin is the 49th most abundant element in Earth's crust,

answers: NDQ_003362

answers: Tin is the 49th most abundant element in Earth's crust,

answers: NDQ_003363

answers: Tin is the 49th most abundant element in Earth's crust,

answers: NDQ_003371

answers: 75 ppm

answers: NDQ_003373

answers: 75 ppm for zinc,

answers: NDQ_003376

answers: 75 ppm for zinc,

answers: NDQ_003378

answers: 2 ppm

answers: NDQ_003379

answers: 75 ppm for zinc,

answers: NDQ_003380

answers: 75 ppm for zinc,

answers: NDQ_003381

answers: 75 ppm for zinc,

answers: NDQ_003382

answers: 75 ppm for zinc,

answers: NDQ_003383

answers: 75 ppm for zinc,

answers: NDQ_003384

answers: 75 ppm for zinc,

answers: NDQ_003385

answers: 75 ppm for zinc,

answers: NDQ_003386

answers: 75 ppm for zinc,

answers: NDQ_003387

answers: 75 ppm for zinc,

answers: NDQ_003388

answers: 75 ppm for zinc,

answers: NDQ_003389

answers: Tin

answers: NDQ_003390

answers: Tin is the 49th most abundant element in Earth's crust,

answers: NDQ_003391

answers: Tin is the 49th most abundant element in Earth's crust,

answers: NDQ_003392

answers: 75 ppm

answers: NDQ_003393

answers: 75 ppm for zinc,

answers: NDQ_003394

answers: Tin is the 49th most abundant element in Earth's crust,

answers: NDQ_003395

answers: 75 ppm for zinc,

answers: NDQ_003396

answers: 75 ppm for zinc,

text: Some fielding positions are used offensively. That is, players are put there with the main aim being to catch out the batsman rather than to stop or slow down the scoring of runs. These positions include Slip (often there are multiple slips next to each other, designated First slip, Second slip, Third slip, etc., numbered outwards from the wicket-keeper—collectively known as the slips cordon) meant to catch balls that just edge off the bat; Gully; Fly slip; Leg slip; Leg gully; the short and silly positions. Short leg, also known as bat pad, is a position specifically intended to catch balls that unintentionally strike the bat and leg pad, and thus end up only a metre or two to the leg side.

text: Some fielding positions are used offensively. That is, players are put there with the main aim being to

text: catch out

text: the batsman rather than to stop or slow down the scoring of runs. These positions include

text: Slip

text: (often there are multiple slips next to each other, designated First slip, Second slip, Third slip, etc., numbered outwards from the wicket-keeper—collectively known as the slips cordon) meant to catch balls that just

text: edge

text: off the bat; Gully; Fly slip; Leg slip; Leg gully; the short and silly positions. Short leg, also known as bat pad, is a position specifically intended to catch balls that unintentionally strike the bat and leg pad, and thus end up only a metre or two to the leg side.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: changes in its structure

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: gully

answers: NDQ_003356

answers: unbalance themselves

answers: NDQ_003357

answers: short leg is a position specifically intended to catch balls that unintentionally strike the bat and leg pad, and thus end up only a metre or two to the leg side

answers: NDQ_003358

answers: gully

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: continental plates

answers: NDQ_003362

answers: unanswerable

answers: NDQ_003363

answers: unanswerable

answers: NDQ_003371

answers: What is a thrust fault?

answers: NDQ_003373

answers: None of the above choices.

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What is the main aim of some fielding positions?

answers: NDQ_003381

answers: What is the purpose of slips cordon?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: unanswerable

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: unanswerable

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: Gully

answers: NDQ_003391

answers: dip-slip fault

answers: NDQ_003392

answers: Gully

answers: NDQ_003393

answers: gully

answers: NDQ_003394

answers: is a fault with a fault plane that is not vertical

answers: NDQ_003395

answers: unanswerable

answers: NDQ_003396

answers: Gully

answers: NDQ_003351

answers: slips cordon) meant to catch balls that just edge off the bat;

answers: NDQ_003352

answers: slips cordon)

answers: NDQ_003353

answers: slips cordon)

answers: NDQ_003354

answers: Some fielding positions are used offensively.

answers: NDQ_003355

answers: Gully;

answers: NDQ_003356

answers: slips cordon)

answers: NDQ_003357

answers: Short leg,

answers: NDQ_003358

answers: Gully;

answers: NDQ_003359

answers: slips cordon)

answers: NDQ_003360

answers: Some fielding positions

answers: NDQ_003362

answers: Some fielding positions

answers: NDQ_003363

answers: slips cordon)

answers: NDQ_003371

answers: Some fielding positions are used offensively.

answers: NDQ_003373

answers: Some fielding positions

answers: NDQ_003376

answers: slips cordon)

answers: NDQ_003378

answers: Slip

answers: NDQ_003379

answers: Slip

answers: NDQ_003380

answers: slips cordon)

answers: NDQ_003381

answers: slips cordon)

answers: NDQ_003382

answers: slips cordon) meant to catch balls that just edge off the bat;

answers: NDQ_003383

answers: slips cordon)

answers: NDQ_003384

answers: slips cordon)

answers: NDQ_003385

answers: slips cordon)

answers: NDQ_003386

answers: slips cordon)

answers: NDQ_003387

answers: slips cordon) meant to catch balls that just edge off the bat;

answers: NDQ_003388

answers: slips cordon) meant to catch balls that just edge off the bat;

answers: NDQ_003389

answers: slips cordon)

answers: NDQ_003390

answers: slips cordon)

answers: NDQ_003391

answers: slips cordon)

answers: NDQ_003392

answers: slips cordon)

answers: NDQ_003393

answers: slips cordon)

answers: NDQ_003394

answers: Fly slip; Leg slip; Leg gully;

answers: NDQ_003395

answers: slips cordon) meant to catch balls that just edge off the bat;

answers: NDQ_003396

answers: slips cordon)

text: Stresses are indicated by a slash "/" and Stress Maxima by "M". A single underline indicates a violation of (ii)-1; a double underline indicates a violation of (ii)-1 & 2. In addition, the Stress Maximum "lap", since it occurs on a W position, violating (ii)-3, should get a third underline, rendering the line unmetrical. (Because of display limitations, this is here indicated by striking out the "M".)

text: Stresses are indicated by a slash "/" and Stress Maxima by "M". A single underline indicates a violation of (ii)-1; a double underline indicates a violation of (ii)-1 & 2. In addition, the Stress Maximum "lap", since it occurs on a W position, violating (ii)-3, should get a third underline, rendering the line unmetrical. (Because of display limitations, this is here indicated by striking out the "M".)

answers: NDQ_003351

answers: Stress Maxima

answers: NDQ_003352

answers: is more likely to crack

answers: NDQ_003353

answers: stress maxima

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: (ii)-1 & 2

answers: NDQ_003358

answers: stress

answers: NDQ_003359

answers: (ii)-1

answers: NDQ_003360

answers: continental plates

answers: NDQ_003362

answers: Stress Maximum "lap", since it occurs on a W position, violating (ii)-3

answers: NDQ_003363

answers: (ii)-1

answers: NDQ_003371

answers: (ii)-1

answers: NDQ_003373

answers: NDQ_003376

answers: compressive forces

answers: NDQ_003378

answers: the amount the ground moves in an earthquake

answers: NDQ_003379

answers: (ii)-1

answers: NDQ_003380

answers: None of the above choices.

answers: NDQ_003381

answers: (ii)-1

answers: NDQ_003382

answers: Stress Maxima

answers: NDQ_003383

answers: (ii)-1

answers: NDQ_003384

answers: description

answers: NDQ_003385

answers: Fault zone

answers: NDQ_003386

answers: movement of rock

answers: NDQ_003387

answers: stress maxima

answers: NDQ_003388

answers: (ii)-1

answers: NDQ_003389

answers: process of folding

answers: NDQ_003390

answers: (ii)-3

answers: NDQ_003391

answers: dip-slip fault plane

answers: NDQ_003392

answers: NDQ_003393

answers: dip-slip fault plane

answers: NDQ_003394

answers: lateral

answers: NDQ_003395

answers: vertical fault plane

answers: NDQ_003396

answers: NDQ_003351

answers: Stress Maxima

answers: NDQ_003352

answers: W position, violating (ii)-3,

answers: NDQ_003353

answers: Stresses

answers: NDQ_003354

answers: Stresses

answers: NDQ_003355

answers: "lap",

answers: NDQ_003356

answers: Stresses

answers: NDQ_003357

answers: Stress Maximum "lap", since it occurs on a W position,

answers: NDQ_003358

answers: Stresses

answers: NDQ_003359

answers: violation of (ii)-1;

answers: NDQ_003360

answers: Stresses

answers: NDQ_003362

answers: Stresses

answers: NDQ_003363

answers: W position,

answers: NDQ_003371

answers: Stresses

answers: NDQ_003373

answers: Stresses

answers: NDQ_003376

answers: Stresses

answers: NDQ_003378

answers: Stresses

answers: NDQ_003379

answers: W position, violating (ii)-3,

answers: NDQ_003380

answers: Stresses

answers: NDQ_003381

answers: Stress Maximum

answers: NDQ_003382

answers: Stress Maximum

answers: NDQ_003383

answers: Stresses

answers: NDQ_003384

answers: unmetrical.

answers: NDQ_003385

answers: Stresses

answers: NDQ_003386

answers: Stresses

answers: NDQ_003387

answers: Stress Maximum

answers: NDQ_003388

answers: Stress Maximum

answers: NDQ_003389

answers: Stresses

answers: NDQ_003390

answers: Stresses

answers: NDQ_003391

answers: Stresses

answers: NDQ_003392

answers: Stresses

answers: NDQ_003393

answers: Stresses

answers: NDQ_003394

answers: W position,

answers: NDQ_003395

answers: W position,

answers: NDQ_003396

answers: W position, violating (ii)-3,

text: Compressive stresses are produced by offset and converging slip-strike motions between the Calaveras Fault and the Clayton-Marsh Creek-Greenville Fault which manifest in the Mount Diablo Thrust Fault.

text: Compressive stresses are produced by offset and converging slip-strike motions between the

text: Calaveras Fault

text: and the

text: Clayton-Marsh Creek-Greenville Fault

text: which manifest in the Mount Diablo Thrust Fault.

answers: NDQ_003351

answers: Compressive stresses

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: fracturing

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: fold that bends downward

answers: NDQ_003356

answers: swell

answers: NDQ_003357

answers: Compressive stresses are produced by

answers: NDQ_003358

answers: Fault

answers: NDQ_003359

answers: is pushed together

answers: NDQ_003360

answers: faults

answers: NDQ_003362

answers: the Calaveras Fault and the Clayton-Marsh Creek-Greenville Fault are the same

answers: NDQ_003363

answers: Calaveras Fault

answers: NDQ_003371

answers: What is the Calaveras Fault?

answers: NDQ_003373

answers: yes

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: no

answers: NDQ_003380

answers: It's impossible to say

answers: NDQ_003381

answers: What is the result of compressive stresses?

answers: NDQ_003382

answers: no

answers: NDQ_003383

answers: no

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: NDQ_003386

answers: yes

answers: NDQ_003387

answers: no

answers: NDQ_003388

answers: no

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: Mount Diablo Thrust

answers: NDQ_003391

answers: cantilever fault

answers: NDQ_003392

answers: Mount Diablo Thrust

answers: NDQ_003393

answers: cantilever

answers: NDQ_003394

answers: Clayton-Marsh Creek

answers: NDQ_003395

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: Compressive

answers: NDQ_003352

answers: Compressive stresses

answers: NDQ_003353

answers: Mount Diablo Thrust Fault.

answers: NDQ_003354

answers: Clayton-Marsh Creek-Greenville Fault

answers: NDQ_003355

answers: Compressive stresses

answers: NDQ_003356

answers: Compressive stresses

answers: NDQ_003357

answers: Compressive stresses

answers: NDQ_003358

answers: Compressive stresses

answers: NDQ_003359

answers: converging slip-strike motions

answers: NDQ_003360

answers: Compressive stresses

answers: NDQ_003362

answers: Mount Diablo Thrust Fault.

answers: NDQ_003363

answers: Calaveras Fault

answers: NDQ_003371

answers: Mount Diablo Thrust Fault.

answers: NDQ_003373

answers: Compressive stresses

answers: NDQ_003376

answers: Compressive stresses

answers: NDQ_003378

answers: slip-strike motions

answers: NDQ_003379

answers: Clayton-Marsh Creek-Greenville Fault

answers: NDQ_003380

answers: Compressive stresses

answers: NDQ_003381

answers: Compressive stresses

answers: NDQ_003382

answers: slip-strike motions

answers: NDQ_003383

answers: Compressive stresses

answers: NDQ_003384

answers: Clayton-Marsh Creek-Greenville Fault

answers: NDQ_003385

answers: Clayton-Marsh Creek-Greenville Fault

answers: NDQ_003386

answers: Compressive stresses

answers: NDQ_003387

answers: Mount Diablo Thrust Fault.

answers: NDQ_003388

answers: Compressive stresses

answers: NDQ_003389

answers: Compressive stresses

answers: NDQ_003390

answers: Mount Diablo Thrust Fault.

answers: NDQ_003391

answers: Thrust Fault.

answers: NDQ_003392

answers: Mount Diablo Thrust Fault.

answers: NDQ_003393

answers: Thrust Fault.

answers: NDQ_003394

answers: Clayton-Marsh Creek-Greenville Fault

answers: NDQ_003395

answers: Mount Diablo Thrust Fault.

answers: NDQ_003396

answers: Mount Diablo Thrust Fault.

text: Rift valleys, such as the Albertine Rift, are formed by the expansion of the Earth's crust due to tectonic activity beneath the Earth's surface.

text: Rift valleys, such as the

text: Albertine Rift

text: , are formed by the expansion of the

text: Earth

text: 's crust due to

text: tectonic

text: activity beneath the Earth's surface.

answers: NDQ_003351

answers: tectonic

answers: NDQ_003352

answers: expands

answers: NDQ_003353

answers: lava to form

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: rift valley

answers: NDQ_003356

answers: expand

answers: NDQ_003357

answers: tectonic activity beneath the Earth's surface

answers: NDQ_003358

answers: valley

answers: NDQ_003359

answers: is pushed together

answers: NDQ_003360

answers: tectonic activity

answers: NDQ_003362

answers: The San Andreas Fault was formed by tectonic activity.

answers: NDQ_003363

answers: tectonic activity

answers: NDQ_003371

answers: Which of the following is not a type of tectonic activity?

answers: NDQ_003373

answers: How would you describe compressive stresses?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: what is the last word in the passage?

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What would happen if there was no tectonic activity?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not the cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not a type of fold that arches upward?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: (iv)

answers: NDQ_003387

answers: Which of the following is not caused by expansion of the Earth's crust?

answers: NDQ_003388

answers: Which of the following is not a type of fault: Albertine Rift, Strike-slip fault or Albertine Rift?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: rift valley

answers: NDQ_003391

answers: rift valley

answers: NDQ_003392

answers: rift valley

answers: NDQ_003393

answers: rift valley

answers: NDQ_003394

answers: tectonic

answers: NDQ_003395

answers: is not the same as

answers: NDQ_003396

answers: Albertine

answers: NDQ_003351

answers: tectonic activity

answers: NDQ_003352

answers: expansion of the Earth's crust due to tectonic activity

answers: NDQ_003353

answers: expansion of the Earth's crust

answers: NDQ_003354

answers: Rift valleys,

answers: NDQ_003355

answers: Rift valleys,

answers: NDQ_003356

answers: Rift valleys,

answers: NDQ_003357

answers: expansion of the Earth's crust

answers: NDQ_003358

answers: Rift valleys,

answers: NDQ_003359

answers: expansion of the Earth's crust due to tectonic activity

answers: NDQ_003360

answers: tectonic activity beneath the Earth's surface.

answers: NDQ_003362

answers: expansion of the Earth's crust due to tectonic activity

answers: NDQ_003363

answers: tectonic activity beneath the Earth's surface.

answers: NDQ_003371

answers: Rift valleys,

answers: NDQ_003373

answers: Rift valleys,

answers: NDQ_003376

answers: expansion of the Earth's crust due to tectonic activity

answers: NDQ_003378

answers: expansion of the Earth's crust due to tectonic activity

answers: NDQ_003379

answers: Rift valleys, such as the Albertine Rift,

answers: NDQ_003380

answers: tectonic activity

answers: NDQ_003381

answers: expansion of the Earth's crust due to tectonic activity

answers: NDQ_003382

answers: expansion of the Earth's crust due to tectonic activity

answers: NDQ_003383

answers: tectonic activity

answers: NDQ_003384

answers: Rift valleys,

answers: NDQ_003385

answers: Rift valleys,

answers: NDQ_003386

answers: tectonic activity

answers: NDQ_003387

answers: expansion of the Earth's crust due to tectonic activity

answers: NDQ_003388

answers: tectonic activity

answers: NDQ_003389

answers: expansion of the Earth's crust

answers: NDQ_003390

answers: Rift valleys, such as the Albertine Rift,

answers: NDQ_003391

answers: Rift valleys,

answers: NDQ_003392

answers: Rift valleys, such as the Albertine Rift,

answers: NDQ_003393

answers: Rift valleys,

answers: NDQ_003394

answers: Rift valleys, such as the Albertine Rift,

answers: NDQ_003395

answers: Rift valleys, such as the Albertine Rift,

answers: NDQ_003396

answers: Albertine Rift,

text: Recent research indicates prolonged chronic stress can contribute to metabolic syndrome by disrupting the hormonal balance of the hypothalamic-pituitary-adrenal axis (HPA-axis).A dysfunctional HPA-axis causes high cortisol levels to circulate, which results in raising glucose and insulin levels, which in turn cause insulin-mediated effects on adipose tissue, ultimately promoting visceral adiposity, insulin resistance, dyslipidemia and hypertension, with direct effects on the bone, causing "low turnover" osteoporosis. HPA-axis dysfunction may explain the reported risk indication of abdominal obesity to cardiovascular disease (CVD), type 2 diabetes and stroke. Psychosocial stress is also linked to heart disease.

text: Recent research indicates prolonged chronic

text: stress

text: can contribute to metabolic syndrome by disrupting the hormonal balance of the

text: hypothalamic-pituitary-adrenal axis

text: (HPA-axis).A dysfunctional HPA-axis causes high

text: cortisol

text: levels to circulate, which results in raising

text: glucose

text: and

text: insulin

text: levels, which in turn cause insulin-mediated effects on adipose tissue, ultimately promoting

text: visceral adiposity

text: , insulin resistance, dyslipidemia and hypertension, with direct effects on the bone, causing "low turnover"

text: osteoporosis

text: . HPA-axis dysfunction may explain the reported risk indication of

text: abdominal obesity

text: to

text: cardiovascular disease

text: (CVD), type 2 diabetes and

text: stroke

text: Psychosocial

text: stress is also linked to

text: heart disease

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: osteoporosis

answers: NDQ_003353

answers: low turnover osteoporosis

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: unanswerable

answers: NDQ_003356

answers: increase in size

answers: NDQ_003357

answers: high cortisol levels to circulate

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's surface

answers: NDQ_003362

answers: low turnover" osteoporosis

answers: NDQ_003363

answers: unanswerable

answers: NDQ_003371

answers: Which of the following is not a result of a thrust fault?

answers: NDQ_003373

answers: What is the main idea of this passage?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: Which of the following is not a cause of osteoporosis?

answers: NDQ_003382

answers: what is the most common stress at convergent plates

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: unanswerable

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: Which of the following is not a result of shear stress?

answers: NDQ_003389

answers: non-existent

answers: NDQ_003390

answers: osteoporosis

answers: NDQ_003391

answers: osteoporosis

answers: NDQ_003392

answers: unanswerable

answers: NDQ_003393

answers: osteoporosis

answers: NDQ_003394

answers: type 2 diabetes and stroke

answers: NDQ_003395

answers: NDQ_003396

answers: type 2 diabetes

answers: NDQ_003351

answers: prolonged chronic stress

answers: NDQ_003352

answers: osteoporosis.

answers: NDQ_003353

answers: osteoporosis.

answers: NDQ_003354

answers: Recent research indicates prolonged chronic stress can contribute to metabolic syndrome

answers: NDQ_003355

answers: visceral adiposity,

answers: NDQ_003356

answers: "low turnover" osteoporosis.

answers: NDQ_003357

answers: "low turnover" osteoporosis.

answers: NDQ_003358

answers: osteoporosis.

answers: NDQ_003359

answers: prolonged chronic stress

answers: NDQ_003360

answers: prolonged chronic stress

answers: NDQ_003362

answers: "low turnover" osteoporosis.

answers: NDQ_003363

answers: prolonged chronic stress

answers: NDQ_003371

answers: prolonged chronic stress can contribute to metabolic syndrome

answers: NDQ_003373

answers: prolonged chronic stress can contribute to metabolic syndrome

answers: NDQ_003376

answers: (HPA-axis).A

answers: NDQ_003378

answers: (HPA-axis).A

answers: NDQ_003379

answers: (HPA-axis).A

answers: NDQ_003380

answers: "low turnover" osteoporosis.

answers: NDQ_003381

answers: "low turnover" osteoporosis.

answers: NDQ_003382

answers: prolonged chronic stress can contribute to metabolic syndrome

answers: NDQ_003383

answers: "low turnover" osteoporosis.

answers: NDQ_003384

answers: hypothalamic-pituitary-adrenal axis

answers: NDQ_003385

answers: (HPA-axis).A

answers: NDQ_003386

answers: (HPA-axis).A

answers: NDQ_003387

answers: "low turnover" osteoporosis.

answers: NDQ_003388

answers: prolonged chronic stress can contribute to metabolic syndrome

answers: NDQ_003389

answers: Recent research indicates prolonged chronic stress can contribute to metabolic syndrome

answers: NDQ_003390

answers: "low turnover" osteoporosis.

answers: NDQ_003391

answers: "low turnover" osteoporosis.

answers: NDQ_003392

answers: "low turnover" osteoporosis.

answers: NDQ_003393

answers: osteoporosis.

answers: NDQ_003394

answers: "low turnover" osteoporosis.

answers: NDQ_003395

answers: prolonged chronic stress can contribute to metabolic syndrome

answers: NDQ_003396

answers: "low turnover" osteoporosis.

text: Andreas (his name and the name of the episode, "Andreas' Fault", are a play on the San Andreas Fault) is a large, bulky, yellow, armored alien with jackhammers and drills in his arms and is Armodrillo's genetic donor. He is reckless, as well as oblivious, proven when he repeatedly attempted to wreck a spaceship while still inside it. His intelligence is quite low, and doesn't even know what an asteroid is. However, being dimwitted, he often uses these powers at the inconvenience of allies and enemies alike. His personality and actions are very similar to Rath. On the other hand, Andreas is a little more gullible than hardheaded as he tends to make attachments to pretty much anyone who he thinks is nice or is the strongest (this was proven when he blindly followed P'andor, who had over-powered Bivalvan and taken charge). Andreas has shown him to be a gentle giant, getting easily scared, and thinks most people are his friends.

text: Andreas (his name and the name of the episode, "Andreas' Fault", are a play on the

text: San Andreas Fault

text: ) is a large, bulky, yellow, armored alien with jackhammers and drills in his arms and is Armodrillo's genetic donor. He is reckless, as well as oblivious, proven when he repeatedly attempted to wreck a spaceship while still inside it. His intelligence is quite low, and doesn't even know what an

text: asteroid

text: is. However, being dimwitted, he often uses these powers at the inconvenience of allies and enemies alike. His personality and actions are very similar to Rath. On the other hand, Andreas is a little more gullible than hardheaded as he tends to make attachments to pretty much anyone who he thinks is nice or is the strongest (this was proven when he blindly followed P'andor, who had over-powered Bivalvan and taken charge). Andreas has shown him to be a gentle giant, getting easily scared, and thinks most people are his friends.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: is likely to crack

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: make attachments

answers: NDQ_003357

answers: Andreas doesn't even know what an asteroid is

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: San Andreas fault

answers: NDQ_003362

answers: doesn't even know what an asteroid is

answers: NDQ_003363

answers: San Andreas Fault

answers: NDQ_003371

answers: What is the San Andreas Fault?

answers: NDQ_003373

answers: How would you describe Andreas?

answers: NDQ_003376

answers: What is the name of the episode?

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What is Andreas' Fault?

answers: NDQ_003381

answers: What is the name of the episode?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is the name of the episode that Andreas is a play on?

answers: NDQ_003385

answers: what is the San Andreas Fault

answers: NDQ_003386

answers: San Andreas Fault

answers: NDQ_003387

answers: What is the San Andreas Fault?

answers: NDQ_003388

answers: What does Andreas' Fault result from?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: San Andreas Fault

answers: NDQ_003391

answers: San Andreas Fault

answers: NDQ_003392

answers: San Andreas Fault

answers: NDQ_003393

answers: San Andreas Fault

answers: NDQ_003394

answers: San Andreas Fault

answers: NDQ_003395

answers: San Andreas Fault

answers: NDQ_003396

answers: San Andreas Fault

answers: NDQ_003351

answers: San Andreas Fault)

answers: NDQ_003352

answers: "Andreas' Fault",

answers: NDQ_003353

answers: San Andreas Fault)

answers: NDQ_003354

answers: Andreas is a little more gullible than hardheaded

answers: NDQ_003355

answers: "Andreas' Fault",

answers: NDQ_003356

answers: wreck a spaceship

answers: NDQ_003357

answers: San Andreas

answers: NDQ_003358

answers: Fault",

answers: NDQ_003359

answers: San Andreas Fault)

answers: NDQ_003360

answers: San Andreas Fault)

answers: NDQ_003362

answers: gentle giant, getting easily scared, and thinks most people are his friends.

answers: NDQ_003363

answers: San Andreas Fault)

answers: NDQ_003371

answers: San Andreas Fault)

answers: NDQ_003373

answers: San Andreas Fault)

answers: NDQ_003376

answers: San Andreas Fault)

answers: NDQ_003378

answers: San Andreas Fault)

answers: NDQ_003379

answers: San Andreas Fault)

answers: NDQ_003380

answers: jackhammers

answers: NDQ_003381

answers: San Andreas Fault)

answers: NDQ_003382

answers: San Andreas Fault)

answers: NDQ_003383

answers: San Andreas Fault)

answers: NDQ_003384

answers: Andreas

answers: NDQ_003385

answers: San Andreas Fault)

answers: NDQ_003386

answers: San Andreas Fault)

answers: NDQ_003387

answers: San Andreas Fault)

answers: NDQ_003388

answers: San Andreas Fault)

answers: NDQ_003389

answers: "Andreas' Fault",

answers: NDQ_003390

answers: San Andreas Fault)

answers: NDQ_003391

answers: asteroid

answers: NDQ_003392

answers: San Andreas Fault)

answers: NDQ_003393

answers: asteroid

answers: NDQ_003394

answers: San Andreas Fault)

answers: NDQ_003395

answers: San Andreas Fault)

answers: NDQ_003396

answers: San Andreas Fault)

text: The Lesser Antilles subduction zone is a convergent plate boundary on the seafloor along the eastern margin of the Lesser Antilles island arc.  In this subduction zone, oceanic crust of the South American Plate is being subducted under the Caribbean Plate.

text: The Lesser Antilles subduction zone is a

text: convergent plate boundary

text: on the seafloor along the eastern margin of the

text: Lesser Antilles

text: island arc.  In this

text: subduction zone

text: oceanic crust

text: of the

text: South American Plate

text: is being subducted under the

text: Caribbean Plate

answers: NDQ_003351

answers: convergent

answers: NDQ_003352

answers: subducts

answers: NDQ_003353

answers: subduction

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: subduction zone

answers: NDQ_003356

answers: subduct

answers: NDQ_003357

answers: the South American Plate is being subducted under the Caribbean Plate

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: subducts

answers: NDQ_003360

answers: plate boundaries

answers: NDQ_003362

answers: The Lesser Antilles subduction zone is a convergent plate boundary

answers: NDQ_003363

answers: Lesser Antilles

answers: NDQ_003371

answers: What is a convergent plate boundary?

answers: NDQ_003373

answers: Why is the Lesser Antilles subduction zone important?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: what is the last word in the passage?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: Which of the following is not a stress?

answers: NDQ_003381

answers: What type of stress does the Lesser Antilles subduction zone experience?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: What is a convergent plate boundary?

answers: NDQ_003385

answers: What is the Lesser Antilles subduction zone?

answers: NDQ_003386

answers: What is the Lesser Antilles subduction zone?

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: Lesser Antilles subduction zone, oceanic crust or normal faults?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip, strike-slip or strike-slip?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: subduction zone

answers: NDQ_003391

answers: subduction zone

answers: NDQ_003392

answers: subduction zone

answers: NDQ_003393

answers: subduction zone

answers: NDQ_003394

answers: subduction zone

answers: NDQ_003395

answers: convergent plate boundary

answers: NDQ_003396

answers: subduction zone

answers: NDQ_003351

answers: South American Plate

answers: NDQ_003352

answers: subducted

answers: NDQ_003353

answers: subducted

answers: NDQ_003354

answers: The Lesser Antilles subduction zone

answers: NDQ_003355

answers: The Lesser Antilles subduction zone

answers: NDQ_003356

answers: subducted

answers: NDQ_003357

answers: South American Plate is being subducted under the Caribbean Plate.

answers: NDQ_003358

answers: The Lesser Antilles subduction zone

answers: NDQ_003359

answers: subducted

answers: NDQ_003360

answers: The Lesser Antilles subduction zone

answers: NDQ_003362

answers: subducted under the Caribbean Plate.

answers: NDQ_003363

answers: The Lesser Antilles subduction zone

answers: NDQ_003371

answers: The Lesser Antilles subduction zone

answers: NDQ_003373

answers: The Lesser Antilles subduction zone

answers: NDQ_003376

answers: The Lesser Antilles subduction zone

answers: NDQ_003378

answers: The Lesser Antilles subduction zone

answers: NDQ_003379

answers: South American Plate is being subducted under the Caribbean Plate.

answers: NDQ_003380

answers: The Lesser Antilles subduction zone

answers: NDQ_003381

answers: South American Plate is being subducted under the Caribbean Plate.

answers: NDQ_003382

answers: South American Plate is being subducted under the Caribbean Plate.

answers: NDQ_003383

answers: The Lesser Antilles subduction zone

answers: NDQ_003384

answers: The Lesser Antilles subduction zone

answers: NDQ_003385

answers: The Lesser Antilles subduction zone

answers: NDQ_003386

answers: The Lesser Antilles subduction zone

answers: NDQ_003387

answers: The Lesser Antilles subduction zone

answers: NDQ_003388

answers: The Lesser Antilles subduction zone

answers: NDQ_003389

answers: The Lesser Antilles subduction zone

answers: NDQ_003390

answers: The Lesser Antilles subduction zone

answers: NDQ_003391

answers: South American Plate is being subducted under the Caribbean Plate.

answers: NDQ_003392

answers: The Lesser Antilles subduction zone

answers: NDQ_003393

answers: South American Plate is being subducted under the Caribbean Plate.

answers: NDQ_003394

answers: convergent plate boundary

answers: NDQ_003395

answers: convergent plate boundary on the seafloor

answers: NDQ_003396

answers: convergent plate boundary

text: Yusifzadeh is the honorary geologist of the former USSR and the honored engineer of the Republic of Azerbaijan. He was awarded with the Honorary Explorationist of the Earth Crust.

text: Yusifzadeh is the honorary geologist of the former USSR and the honored engineer of the

text: Republic of Azerbaijan

text: . He was awarded with the Honorary Explorationist of the Earth Crust.

answers: NDQ_003351

answers: deformation

answers: NDQ_003352

answers: is likely to crack

answers: NDQ_003353

answers: voids to form

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: swell

answers: NDQ_003357

answers: Yusifzadeh is the engineer of which country?

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: is pushed together

answers: NDQ_003360

answers: Earth faults

answers: NDQ_003362

answers: Yusifzadeh is the engineer of the Republic of Azerbaijan

answers: NDQ_003363

answers: Azerbaijan

answers: NDQ_003371

answers: Which of the following is not a type of fault?

answers: NDQ_003373

answers: How would you describe Yusifzadeh?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: How would you describe Yusifzadeh?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: How would you describe Yusifzadeh?

answers: NDQ_003381

answers: How would you describe Yusifzadeh?

answers: NDQ_003382

answers: None of the above choices.

answers: NDQ_003383

answers: How would you describe Yusifzadeh?

answers: NDQ_003384

answers: What kind of fold does Yusifzadeh have?

answers: NDQ_003385

answers: What is Yusifzadeh?

answers: NDQ_003386

answers: None of the above choices.

answers: NDQ_003387

answers: How would you describe Yusifzadeh?

answers: NDQ_003388

answers: How would you describe Yusifzadeh?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: a fault

answers: NDQ_003391

answers: craton

answers: NDQ_003392

answers: a fault

answers: NDQ_003393

answers: igneous rock

answers: NDQ_003394

answers: isosceles

answers: NDQ_003395

answers: is a type of

answers: NDQ_003396

answers: lateral fault

answers: NDQ_003351

answers: Earth Crust.

answers: NDQ_003352

answers: Honorary Explorationist of the Earth Crust.

answers: NDQ_003353

answers: Earth Crust.

answers: NDQ_003354

answers: Yusifzadeh

answers: NDQ_003355

answers: Earth Crust.

answers: NDQ_003356

answers: Honorary Explorationist of the Earth Crust.

answers: NDQ_003357

answers: Earth Crust.

answers: NDQ_003358

answers: Earth Crust.

answers: NDQ_003359

answers: Earth Crust.

answers: NDQ_003360

answers: Earth Crust.

answers: NDQ_003362

answers: Yusifzadeh

answers: NDQ_003363

answers: Earth Crust.

answers: NDQ_003371

answers: Honorary Explorationist of the Earth Crust.

answers: NDQ_003373

answers: Honorary Explorationist of the Earth Crust.

answers: NDQ_003376

answers: Honorary Explorationist of the Earth Crust.

answers: NDQ_003378

answers: Honorary Explorationist of the Earth Crust.

answers: NDQ_003379

answers: Honorary Explorationist of the Earth Crust.

answers: NDQ_003380

answers: Honorary Explorationist of the Earth Crust.

answers: NDQ_003381

answers: Honorary Explorationist of the Earth Crust.

answers: NDQ_003382

answers: Honorary Explorationist of the Earth Crust.

answers: NDQ_003383

answers: Honorary Explorationist of the Earth Crust.

answers: NDQ_003384

answers: Honorary Explorationist of the Earth Crust.

answers: NDQ_003385

answers: Honorary Explorationist of the Earth Crust.

answers: NDQ_003386

answers: Honorary Explorationist of the Earth Crust.

answers: NDQ_003387

answers: Honorary Explorationist of the Earth Crust.

answers: NDQ_003388

answers: Honorary Explorationist of the Earth Crust.

answers: NDQ_003389

answers: Earth Crust.

answers: NDQ_003390

answers: Honorary Explorationist of the Earth Crust.

answers: NDQ_003391

answers: Earth Crust.

answers: NDQ_003392

answers: Honorary Explorationist of the Earth Crust.

answers: NDQ_003393

answers: Earth Crust.

answers: NDQ_003394

answers: Earth Crust.

answers: NDQ_003395

answers: Earth Crust.

answers: NDQ_003396

answers: Honorary Explorationist of the Earth Crust.

text: A future sculptural design for which the artist acquired land and started a non-profit organization to raise funds is his San Andreas Fault Sculpture Project: a proposed  monolith of concrete () meant to straddle both sides of the San Andreas Fault so that over time the Earth's own plate-tectonic forces will crack the block into two golden rectangles that will continue to move past each other in opposite directions. The artist's intent would be to use "the Earth itself, as a tool to make the movement of massive continents visible on a scale that can be understood in human terms".

text: A future sculptural design for which the artist acquired land and started a non-profit organization to raise funds is his San Andreas Fault Sculpture Project: a proposed  monolith of

text: concrete

text: () meant to straddle both sides of the

text: San Andreas Fault

text: so that over time the Earth's own

text: plate-tectonic forces

text: will crack the block into two

text: golden rectangle

text: s that will continue to move past each other in opposite directions. The artist's intent would be to use "the Earth itself, as a tool to make the movement of massive continents visible on a scale that can be understood in human terms".

answers: NDQ_003351

answers: plate-tectonic forces

answers: NDQ_003352

answers: cracks

answers: NDQ_003353

answers: plates to break apart

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fold that bends downward

answers: NDQ_003356

answers: crack

answers: NDQ_003357

answers: plate-tectonic forces will crack the block into two golden rectangles that will continue to move past each other in opposite directions.

answers: NDQ_003358

answers: Fault

answers: NDQ_003359

answers: plate-tectonic forces

answers: NDQ_003360

answers: plate-tectonic forces

answers: NDQ_003362

answers: the Earth itself, as a tool to make the movement of massive continents visible on a scale that can be understood in human terms

answers: NDQ_003363

answers: San Andreas Fault

answers: NDQ_003371

answers: What may be the reason for the San Andreas Fault Sculpture Project?

answers: NDQ_003373

answers: How would you describe the artist's intent?

answers: NDQ_003376

answers: Which of the following is not a type of terrain: basin-and-range or plate-tectonic forces?

answers: NDQ_003378

answers: what is the last word in the passage?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What type of force is the San Andreas Fault?

answers: NDQ_003381

answers: What will happen to the block?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: How would you describe the San Andreas Fault?

answers: NDQ_003384

answers: What type of fold is the San Andreas Fault Sculpture Project?

answers: NDQ_003385

answers: What is the San Andreas Fault?

answers: NDQ_003386

answers: What is the San Andreas Fault?

answers: NDQ_003387

answers: What is the purpose of the San Andreas Fault?

answers: NDQ_003388

answers: What type of fault is the San Andreas Fault?

answers: NDQ_003389

answers: plate-tectonic forces

answers: NDQ_003390

answers: San Andreas Fault

answers: NDQ_003391

answers: San Andreas Fault

answers: NDQ_003392

answers: San Andreas Fault

answers: NDQ_003393

answers: monolith

answers: NDQ_003394

answers: San Andreas Fault

answers: NDQ_003395

answers: San Andreas Fault

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: plate-tectonic

answers: NDQ_003352

answers: crack the block into two golden rectangles

answers: NDQ_003353

answers: crack the block into two golden rectangles

answers: NDQ_003354

answers: San Andreas Fault Sculpture Project:

answers: NDQ_003355

answers: rectangles that will continue to move past each other in opposite directions.

answers: NDQ_003356

answers: crack the block into two golden rectangles

answers: NDQ_003357

answers: opposite directions.

answers: NDQ_003358

answers: San Andreas Fault

answers: NDQ_003359

answers: plate-tectonic forces

answers: NDQ_003360

answers: plate-tectonic forces

answers: NDQ_003362

answers: the Earth's own plate-tectonic forces

answers: NDQ_003363

answers: San Andreas Fault

answers: NDQ_003371

answers: San Andreas Fault

answers: NDQ_003373

answers: plate-tectonic forces

answers: NDQ_003376

answers: plate-tectonic

answers: NDQ_003378

answers: the Earth's own plate-tectonic forces

answers: NDQ_003379

answers: San Andreas Fault

answers: NDQ_003380

answers: plate-tectonic forces

answers: NDQ_003381

answers: plate-tectonic forces

answers: NDQ_003382

answers: the Earth's own plate-tectonic forces

answers: NDQ_003383

answers: plate-tectonic forces

answers: NDQ_003384

answers: Earth's own plate-tectonic forces

answers: NDQ_003385

answers: Fault

answers: NDQ_003386

answers: plate-tectonic forces

answers: NDQ_003387

answers: plate-tectonic forces

answers: NDQ_003388

answers: plate-tectonic forces

answers: NDQ_003389

answers: continents

answers: NDQ_003390

answers: San Andreas Fault

answers: NDQ_003391

answers: concrete

answers: NDQ_003392

answers: San Andreas Fault

answers: NDQ_003393

answers: concrete

answers: NDQ_003394

answers: San Andreas Fault

answers: NDQ_003395

answers: San Andreas Fault

answers: NDQ_003396

answers: San Andreas Fault

text: Most photos of the Golden Gate Bridge and San Francisco are taken with the photographer standing in Marin County.  In the Pacific Ocean, just beyond the Golden Gate Bridge, is the San Andreas Fault, separating the Pacific and North American Plates of the earth’s crust, creating the Coastal Range of mountains and Mount Tamalpais (Mt. Tam,) rising 2,574 feet a stone’s throw north of the Golden Gate Bridge.  Marin County, just north of San Francisco, is split by the San Andreas Fault and has unique history that gave birth to the sport of mountain biking.  WTB has been mountain biking from the beginning of the mountain bike.

text: Most photos of the Golden Gate Bridge and San Francisco are taken with the photographer standing in Marin County.  In the Pacific Ocean, just beyond the Golden Gate Bridge, is the San Andreas Fault, separating the Pacific and North American Plates of the earth’s crust, creating the Coastal Range of mountains and Mount Tamalpais (Mt. Tam,) rising 2,574 feet a stone’s throw north of the Golden Gate Bridge.  Marin County, just north of San Francisco, is split by the San Andreas Fault and has unique history that gave birth to the sport of mountain biking.  WTB has been mountain biking from the beginning of the mountain bike.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: Coastal Range

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: separating the Pacific and North American Plates

answers: NDQ_003358

answers: Fault

answers: NDQ_003359

answers: separates

answers: NDQ_003360

answers: San Andreas Fault

answers: NDQ_003362

answers: Marin County, just north of San Francisco, is split by the San Andreas Fault

answers: NDQ_003363

answers: San Andreas Fault

answers: NDQ_003371

answers: Which of the following is not a type of fault: San Andreas Fault, Pacific and North American Plates

answers: NDQ_003373

answers: what is the last word in the passage?

answers: NDQ_003376

answers: what is the last word in the passage?

answers: NDQ_003378

answers: what is the last word in the passage?

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What does the San Andreas Fault cause?

answers: NDQ_003382

answers: What is the most common stress at convergent plates

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not a type of fold that arches upward?

answers: NDQ_003385

answers: what is the last word in the passage?

answers: NDQ_003386

answers: what is the last word in the passage?

answers: NDQ_003387

answers: Which of the following is not a normal fault: Pacific or North American Plates?

answers: NDQ_003388

answers: Which of the following is not an example of a strike-slip fault?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: San Andreas Fault

answers: NDQ_003391

answers: Mount Tamalpais

answers: NDQ_003392

answers: San Andreas Fault

answers: NDQ_003393

answers: Coastal Range

answers: NDQ_003394

answers: San Andreas Fault

answers: NDQ_003395

answers: San Andreas Fault

answers: NDQ_003396

answers: San Andreas Fault

answers: NDQ_003351

answers: San Andreas Fault,

answers: NDQ_003352

answers: 2,574 feet

answers: NDQ_003353

answers: San Andreas Fault,

answers: NDQ_003354

answers: San Andreas Fault,

answers: NDQ_003355

answers: San Andreas Fault,

answers: NDQ_003356

answers: mountains

answers: NDQ_003357

answers: separating the Pacific and North American Plates

answers: NDQ_003358

answers: San Andreas Fault,

answers: NDQ_003359

answers: separating the Pacific and North American Plates

answers: NDQ_003360

answers: San Andreas Fault,

answers: NDQ_003362

answers: photographer standing in Marin County.

answers: NDQ_003363

answers: San Andreas Fault,

answers: NDQ_003371

answers: San Andreas Fault,

answers: NDQ_003373

answers: San Andreas Fault,

answers: NDQ_003376

answers: Coastal Range of mountains

answers: NDQ_003378

answers: San Andreas Fault,

answers: NDQ_003379

answers: San Andreas Fault,

answers: NDQ_003380

answers: San Andreas Fault,

answers: NDQ_003381

answers: San Andreas Fault,

answers: NDQ_003382

answers: San Andreas Fault,

answers: NDQ_003383

answers: San Andreas Fault,

answers: NDQ_003384

answers: San Andreas Fault,

answers: NDQ_003385

answers: San Andreas Fault,

answers: NDQ_003386

answers: separating the Pacific and North American Plates

answers: NDQ_003387

answers: San Andreas Fault,

answers: NDQ_003388

answers: San Andreas Fault,

answers: NDQ_003389

answers: San Andreas Fault,

answers: NDQ_003390

answers: San Andreas Fault,

answers: NDQ_003391

answers: Pacific and North American Plates

answers: NDQ_003392

answers: San Andreas Fault,

answers: NDQ_003393

answers: Mount Tamalpais

answers: NDQ_003394

answers: San Andreas Fault,

answers: NDQ_003395

answers: San Andreas Fault,

answers: NDQ_003396

answers: San Andreas Fault,

text: Franciscan rocks are thought to have formed prior to creation of the San Andreas Fault when an ancient deep-sea trench existed along the California continental margin. This trench, most of which is no longer evident, resulted from subduction of oceanic crust of the Farallon tectonic plate beneath continental crust of the North American Plate. As oceanic crust descended beneath the continent, volcanic rocks, mainly basalt, making up the lower plate, and marine sediments deposited on top of it were scraped off and accreted (i.e., added) to the leading edge of the overriding plate. This resulted in widespread deformation with development of thrust faults and folding. Ophiolite (which weathers to serpentine), and rocks altered by high-pressure metamorphism (such as blueschist) were emplaced during this episode. Deformation and emplacement continued during subsequent creation of the San Andreas fault to result in a complex chaotic assemblage of diverse rock types that some refer to as a mélange.

text: Franciscan rocks are thought to have formed prior to creation of the

text: San Andreas Fault

text: when an ancient

text: deep-sea trench

text: existed along the

text: California

text: continental margin

text: . This trench, most of which is no longer evident, resulted from

text: subduction

text: of

text: oceanic crust

text: of the

text: Farallon tectonic plate

text: beneath

text: continental crust

text: of the

text: North American Plate

text: . As oceanic crust descended beneath the continent,

text: volcanic

text: rocks, mainly

text: basalt

text: , making up the lower plate, and marine sediments deposited on top of it were scraped off and accreted (i.e., added) to the leading edge of the overriding plate. This resulted in widespread deformation with development of

text: thrust faults

text: and

text: folding

text: Ophiolite

text: (which weathers to

text: serpentine

text: ), and rocks altered by high-pressure

text: metamorphism

text: (such as

text: blueschist

text: ) were emplaced during this episode. Deformation and emplacement continued during subsequent creation of the

text: San Andreas fault

text: to result in a complex chaotic assemblage of diverse rock types that some refer to as a

text: mélange

answers: NDQ_003351

answers: thrust faults

answers: NDQ_003352

answers: deforms

answers: NDQ_003353

answers: metamorphism

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: fold

answers: NDQ_003357

answers: thrust faults and folding are types of

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: widespread deformation

answers: NDQ_003360

answers: San Andreas Fault

answers: NDQ_003362

answers: an ancient deep-sea trench existed along the California continental margin

answers: NDQ_003363

answers: San Andreas Fault

answers: NDQ_003371

answers: What is the San Andreas Fault?

answers: NDQ_003373

answers: subduction of oceanic crust

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What is the result of subduction of oceanic crust?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of thrust faults and folding?

answers: NDQ_003384

answers: What type of fold is the San Andreas Fault?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: What is the cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: thrust faults or folding?

answers: NDQ_003388

answers: Which of the following is not a type of fault: thrust faults or folding?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: thrust faults

answers: NDQ_003391

answers: San Andreas Fault

answers: NDQ_003392

answers: thrust faults

answers: NDQ_003393

answers: San Andreas Fault

answers: NDQ_003394

answers: thrust faults

answers: NDQ_003395

answers: San Andreas Fault

answers: NDQ_003396

answers: thrust faults

answers: NDQ_003351

answers: thrust faults and folding.

answers: NDQ_003352

answers: folding.

answers: NDQ_003353

answers: high-pressure metamorphism

answers: NDQ_003354

answers: Franciscan rocks

answers: NDQ_003355

answers: thrust faults

answers: NDQ_003356

answers: thrust faults and folding.

answers: NDQ_003357

answers: thrust faults and folding.

answers: NDQ_003358

answers: thrust faults

answers: NDQ_003359

answers: deformation

answers: NDQ_003360

answers: San Andreas Fault

answers: NDQ_003362

answers: ancient deep-sea trench

answers: NDQ_003363

answers: San Andreas Fault

answers: NDQ_003371

answers: thrust faults

answers: NDQ_003373

answers: deformation

answers: NDQ_003376

answers: mélange.

answers: NDQ_003378

answers: deformation

answers: NDQ_003379

answers: thrust faults

answers: NDQ_003380

answers: deformation

answers: NDQ_003381

answers: thrust faults and folding.

answers: NDQ_003382

answers: thrust faults and folding.

answers: NDQ_003383

answers: thrust faults

answers: NDQ_003384

answers: thrust faults

answers: NDQ_003385

answers: thrust faults

answers: NDQ_003386

answers: deformation

answers: NDQ_003387

answers: thrust faults

answers: NDQ_003388

answers: thrust faults

answers: NDQ_003389

answers: folding.

answers: NDQ_003390

answers: San Andreas Fault

answers: NDQ_003391

answers: mélange.

answers: NDQ_003392

answers: thrust faults

answers: NDQ_003393

answers: thrust faults

answers: NDQ_003394

answers: San Andreas Fault

answers: NDQ_003395

answers: thrust faults

answers: NDQ_003396

answers: thrust faults

text: It consists of a series of faults and folds which have the effect of bringing old Malvernian rocks to the surface. Being largely hard igneous rocks, the Malverns Complex rocks have resisted erosion better than those of the surrounding countryside and result in a striking line of hills of which the Malvern Hills are the most impressive. The Abberley Hills to their north also form a part of this lineament. This line is considered to mark the edge of two terranes - two once separate fragments of the Earth's crust now joined as one - the Wrekin Terrane to the west and the Charnwood Terrane to the east.

text: It consists of a series of

text: faults

text: and

text: folds

text: which have the effect of bringing old

text: Malvernian

text: rocks to the surface. Being largely hard

text: igneous

text: rocks, the

text: Malverns Complex

text: rocks have resisted

text: erosion

text: better than those of the surrounding countryside and result in a striking line of hills of which the Malvern Hills are the most impressive. The

text: Abberley Hills

text: to their north also form a part of this lineament. This line is considered to mark the edge of two

text: terrane

text: s - two once separate fragments of the Earth's crust now joined as one - the

text: Wrekin Terrane

text: to the west and the

text: Charnwood Terrane

text: to the east.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: more likely to fold

answers: NDQ_003353

answers: faults and folds

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: resist erosion

answers: NDQ_003357

answers: bringing old Malvernian rocks to the surface

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: faults and folds

answers: NDQ_003362

answers: two once separate fragments of the Earth's crust now joined as one

answers: NDQ_003363

answers: Wrekin Terrane

answers: NDQ_003371

answers: Which of the following is not a series of faults and folds?

answers: NDQ_003373

answers: None of the above choices.

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What type of force applied to rock is a stress?

answers: NDQ_003381

answers: What type of rocks are the Malverns Complex?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What type of rocks are the Malverns Complex?

answers: NDQ_003384

answers: Which of the following is not a type of fold?

answers: NDQ_003385

answers: what is the most impressive

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip faults, folds or folds?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: Malvern Hills

answers: NDQ_003391

answers: Malvernian rocks

answers: NDQ_003392

answers: Malvern Hills

answers: NDQ_003393

answers: Malvernian rocks

answers: NDQ_003394

answers: Malvern Hills

answers: NDQ_003395

answers: unanswerable

answers: NDQ_003396

answers: Malvern Hills

answers: NDQ_003351

answers: faults and folds

answers: NDQ_003352

answers: erosion

answers: NDQ_003353

answers: bringing old Malvernian rocks to the surface.

answers: NDQ_003354

answers: Malverns Complex

answers: NDQ_003355

answers: folds

answers: NDQ_003356

answers: erosion

answers: NDQ_003357

answers: bringing old Malvernian rocks

answers: NDQ_003358

answers: erosion

answers: NDQ_003359

answers: bringing old Malvernian rocks to the surface.

answers: NDQ_003360

answers: faults and folds

answers: NDQ_003362

answers: bringing old Malvernian rocks

answers: NDQ_003363

answers: Malvernian

answers: NDQ_003371

answers: faults and folds

answers: NDQ_003373

answers: erosion

answers: NDQ_003376

answers: faults and folds

answers: NDQ_003378

answers: faults and folds

answers: NDQ_003379

answers: Wrekin Terrane

answers: NDQ_003380

answers: erosion

answers: NDQ_003381

answers: faults and folds

answers: NDQ_003382

answers: faults and folds

answers: NDQ_003383

answers: faults and folds

answers: NDQ_003384

answers: two once separate fragments of the Earth's crust now joined as one

answers: NDQ_003385

answers: faults

answers: NDQ_003386

answers: bringing old Malvernian rocks to the surface.

answers: NDQ_003387

answers: bringing old Malvernian rocks

answers: NDQ_003388

answers: bringing old Malvernian rocks

answers: NDQ_003389

answers: faults and folds

answers: NDQ_003390

answers: faults and folds

answers: NDQ_003391

answers: old Malvernian rocks

answers: NDQ_003392

answers: faults and folds

answers: NDQ_003393

answers: Malvernian rocks

answers: NDQ_003394

answers: faults

answers: NDQ_003395

answers: faults and folds

answers: NDQ_003396

answers: folds

text: Deformation of the lithosphere in the plane of the earth (i.e. such that faults are vertical) occurs as a result of near horizontal maximum and minimum principal stresses.  The resulting zones of subsidence are known as strike-slip or pull-apart basins.Basins formed through strike-slip action occur where a vertical fault plane curves.  When the curve in the fault plane moves apart, a region of transtension results, creating a basin.  Another term for a transtensional basin is a rhombochasm.  A classic rhombochasm is illustrated by the Dead Sea rift, where northward movement of the Arabian Plate relative to the Anatolian Plate has caused a rhombochasm.

text: Deformation of the lithosphere in the plane of the earth (i.e. such that faults are vertical) occurs as a result of near horizontal maximum and minimum

entity_section: Principal stresses and stress invariants

text: principal stresses

text: .  The resulting zones of subsidence are known as strike-slip or

text: pull-apart basin

text: s.Basins formed through strike-slip action occur where a vertical fault plane curves.  When the curve in the fault plane moves apart, a region of transtension results, creating a basin.  Another term for a transtensional basin is a rhombochasm.  A classic rhombochasm is illustrated by the

text: Dead Sea

text: rift, where northward movement of the

text: Arabian Plate

text: relative to the

text: Anatolian Plate

text: has caused a rhombochasm.

answers: NDQ_003351

answers: principal stresses

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: Subdistribution

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: vertical fault plane

answers: NDQ_003356

answers: subsidence

answers: NDQ_003357

answers: horizontal maximum and minimum principal stresses

answers: NDQ_003358

answers: unanswerable

answers: NDQ_003359

answers: horizontal maximum and minimum principal stresses

answers: NDQ_003360

answers: faults

answers: NDQ_003362

answers: horizontal maximum and minimum principal stresses

answers: NDQ_003363

answers: strike-slip action

answers: NDQ_003371

answers: Which of the following is not a result of near horizontal maximum and minimum principal stresses?

answers: NDQ_003373

answers: What is a rhombochasm?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: no

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What is the result of near horizontal maximum and minimum principal stresses?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What type of fold is illustrated by the Dead Sea rift?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: Deformation of the lithosphere

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: unanswerable

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: strike-slip

answers: NDQ_003391

answers: basin

answers: NDQ_003392

answers: rhombochasm

answers: NDQ_003393

answers: lithosphere

answers: NDQ_003394

answers: unanswerable

answers: NDQ_003395

answers: Basins formed through strike-slip action

answers: NDQ_003396

answers: strike-slip

answers: NDQ_003351

answers: horizontal maximum and minimum principal stresses.

answers: NDQ_003352

answers: subsidence

answers: NDQ_003353

answers: subsidence

answers: NDQ_003354

answers: Deformation of the lithosphere

answers: NDQ_003355

answers: rhombochasm.

answers: NDQ_003356

answers: subsidence

answers: NDQ_003357

answers: horizontal maximum and minimum principal stresses.

answers: NDQ_003358

answers: rhombochasm.

answers: NDQ_003359

answers: horizontal maximum and minimum principal stresses.

answers: NDQ_003360

answers: Deformation of the lithosphere

answers: NDQ_003362

answers: vertical)

answers: NDQ_003363

answers: Deformation of the lithosphere

answers: NDQ_003371

answers: strike-slip or pull-apart basins.Basins

answers: NDQ_003373

answers: horizontal maximum and minimum principal stresses.

answers: NDQ_003376

answers: strike-slip or pull-apart basins.Basins

answers: NDQ_003378

answers: strike-slip

answers: NDQ_003379

answers: vertical fault plane curves.

answers: NDQ_003380

answers: stresses.

answers: NDQ_003381

answers: horizontal maximum and minimum principal stresses.

answers: NDQ_003382

answers: horizontal maximum and minimum principal stresses.

answers: NDQ_003383

answers: horizontal maximum and minimum principal stresses.

answers: NDQ_003384

answers: rhombochasm.

answers: NDQ_003385

answers: strike-slip or pull-apart basins.Basins

answers: NDQ_003386

answers: Deformation of the lithosphere

answers: NDQ_003387

answers: horizontal maximum and minimum principal stresses.

answers: NDQ_003388

answers: near horizontal maximum and minimum principal stresses.

answers: NDQ_003389

answers: Deformation of the lithosphere

answers: NDQ_003390

answers: strike-slip

answers: NDQ_003391

answers: strike-slip or pull-apart basins.Basins

answers: NDQ_003392

answers: strike-slip or pull-apart basins.Basins

answers: NDQ_003393

answers: strike-slip or pull-apart basins.Basins

answers: NDQ_003394

answers: rhombochasm.

answers: NDQ_003395

answers: curves.

answers: NDQ_003396

answers: rhombochasm.

text: The Coastal Batholith of Peru () is a group of hundred if not thousands of individual plutons that crop out near or at the coast of Peru. The batholith runs a length of ca. 1600 km. Most of the plutons of the batholith were intruded in an elongated coast-parallel extensional basin. The magma that formed the batholith's plutons is thought to have originated from the partial melting of hydrated basaltic rocks at the base of the crust during rifting (extension). Subsequently, the rift basin was inverted. During the ascent the magma followed vertical pathways but emplacement was mostly in the form of tabular bodies.

text: The Coastal Batholith of Peru () is a group of hundred if not thousands of individual

text: pluton

text: s that crop out near or at the coast of

text: Peru

text: . The batholith runs a length of ca. 1600 km. Most of the plutons of the batholith were intruded in an elongated coast-parallel

text: extensional

text: basin

text: . The

text: magma

text: that formed the batholith's plutons is thought to have originated from the

text: partial melting

text: of

text: hydrated

text: basaltic rocks

text: at the base of the

text: crust

text: during

text: rift

text: ing (extension). Subsequently, the rift basin was

text: inverted

text: . During the ascent the magma followed vertical pathways but

text: emplacement

text: was mostly in the form of

text: tabular bodies

answers: NDQ_003351

answers: extension

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: magma

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: extensional basin

answers: NDQ_003356

answers: invert

answers: NDQ_003357

answers: The magma that formed the batholith's plutons is thought to have originated from the partial melting of hydrated basaltic rocks

answers: NDQ_003358

answers: rift basin

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: magma

answers: NDQ_003362

answers: During the ascent the magma followed vertical pathways but emplacement was mostly in the form of tabular bodies

answers: NDQ_003363

answers: rifting

answers: NDQ_003371

answers: Which of the following is not a type of magma: basaltic rocks at the base of the crust during rifting (extension)?

answers: NDQ_003373

answers: What is the main idea of this passage?

answers: NDQ_003376

answers: Which of the following is not a cause of the terrain known as basin-and-range?

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What type of stress does the Coastal Batholith of Peru experience?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: What type of fold is the Coastal Batholith of Peru?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: Which of the following is not a cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: normal faults, rifting, or extension?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip faults, extensional faults, or strike-slip?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: extensional basin

answers: NDQ_003391

answers: rift basin

answers: NDQ_003392

answers: extensional basin

answers: NDQ_003393

answers: rift basin

answers: NDQ_003394

answers: inverted

answers: NDQ_003395

answers: During the ascent the magma followed vertical pathways but emplacement was mostly in the form of tabular bodies

answers: NDQ_003396

answers: extensional basin

answers: NDQ_003351

answers: (extension).

answers: NDQ_003352

answers: emplacement was mostly in the form of tabular bodies.

answers: NDQ_003353

answers: rifting

answers: NDQ_003354

answers: The Coastal Batholith of Peru

answers: NDQ_003355

answers: tabular bodies.

answers: NDQ_003356

answers: inverted.

answers: NDQ_003357

answers: rift basin was inverted.

answers: NDQ_003358

answers: tabular bodies.

answers: NDQ_003359

answers: inverted.

answers: NDQ_003360

answers: rifting

answers: NDQ_003362

answers: inverted.

answers: NDQ_003363

answers: coast-parallel extensional basin.

answers: NDQ_003371

answers: rifting

answers: NDQ_003373

answers: elongated coast-parallel extensional basin.

answers: NDQ_003376

answers: elongated coast-parallel extensional basin.

answers: NDQ_003378

answers: rifting

answers: NDQ_003379

answers: vertical

answers: NDQ_003380

answers: (extension).

answers: NDQ_003381

answers: rifting

answers: NDQ_003382

answers: rifting (extension).

answers: NDQ_003383

answers: rifting (extension).

answers: NDQ_003384

answers: vertical

answers: NDQ_003385

answers: elongated coast-parallel extensional basin.

answers: NDQ_003386

answers: rifting

answers: NDQ_003387

answers: rifting (extension).

answers: NDQ_003388

answers: rifting

answers: NDQ_003389

answers: rifting

answers: NDQ_003390

answers: elongated coast-parallel extensional basin.

answers: NDQ_003391

answers: coast-parallel extensional basin.

answers: NDQ_003392

answers: elongated coast-parallel extensional basin.

answers: NDQ_003393

answers: plutons

answers: NDQ_003394

answers: inverted.

answers: NDQ_003395

answers: During the ascent the magma followed vertical pathways

answers: NDQ_003396

answers: extensional basin.

text: In this region, the geology is dominated by the transition of the tectonic plate boundary from rift to fault. The southernmost strands of the San Andreas Fault connect the northern-most extensions of the East Pacific Rise. Consequently, the region is subject to earthquakes, and the crust is being stretched, resulting in a sinking of the terrain over time.  Related to the active geology are some interesting hydrothermal features.

text: In this region, the

text: geology

text: is dominated by the transition of the

text: tectonic plate

text: boundary from

text: rift

text: to

text: fault

text: . The southernmost strands of the

text: San Andreas Fault

text: connect the northern-most extensions of the

text: East Pacific Rise

text: . Consequently, the region is subject to

text: earthquakes

text: , and the crust is being stretched, resulting in a sinking of the terrain over time.  Related to the active geology are some interesting hydrothermal features.

answers: NDQ_003351

answers: earthquakes

answers: NDQ_003352

answers: sinks

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: rift

answers: NDQ_003356

answers: sink

answers: NDQ_003357

answers: the crust is stretched, resulting in a sinking of the terrain over time

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: is stretched

answers: NDQ_003360

answers: San Andreas Fault

answers: NDQ_003362

answers: the San Andreas Fault connects the northern-most extensions of the East Pacific Rise

answers: NDQ_003363

answers: San Andreas Fault

answers: NDQ_003371

answers: Which of the following is not a tectonic plate boundary: San Andreas Fault, East Pacific Rise, or rift?

answers: NDQ_003373

answers: Which of the following is not a tectonic plate boundary?

answers: NDQ_003376

answers: Which of the following is not caused by compressive forces: basin-and-range or earthquakes?

answers: NDQ_003378

answers: Which of the following is not a tectonic plate boundary: rift, rift, or fault?

answers: NDQ_003379

answers: What is the dip of the fault plane in a strike-slip fault?

answers: NDQ_003380

answers: How is the crust being stretched?

answers: NDQ_003381

answers: Which of the following is not a result of earthquakes: sinking of the terrain over time?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not a type of fold: syncline, rift, or fault?

answers: NDQ_003385

answers: What is the southernmost strands of the San Andreas Fault called?

answers: NDQ_003386

answers: what is the southernmost strands of the San Andreas Fault

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: San Andreas Fault, East Pacific Rise, or normal faults?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip or rift?

answers: NDQ_003389

answers: Which of the following is not a type of folding?

answers: NDQ_003390

answers: San Andreas Fault

answers: NDQ_003391

answers: rift

answers: NDQ_003392

answers: rift

answers: NDQ_003393

answers: East Pacific Rise

answers: NDQ_003394

answers: San Andreas Fault

answers: NDQ_003395

answers: San Andreas Fault

answers: NDQ_003396

answers: San Andreas

answers: NDQ_003351

answers: earthquakes,

answers: NDQ_003352

answers: sinking

answers: NDQ_003353

answers: the crust is being stretched, resulting in a sinking

answers: NDQ_003354

answers: earthquakes,

answers: NDQ_003355

answers: fault.

answers: NDQ_003356

answers: sinking

answers: NDQ_003357

answers: the crust is being stretched,

answers: NDQ_003358

answers: fault.

answers: NDQ_003359

answers: stretched,

answers: NDQ_003360

answers: tectonic plate boundary

answers: NDQ_003362

answers: a sinking of the terrain over time.

answers: NDQ_003363

answers: East Pacific Rise.

answers: NDQ_003371

answers: San Andreas Fault

answers: NDQ_003373

answers: stretched,

answers: NDQ_003376

answers: the crust is being stretched, resulting in a sinking

answers: NDQ_003378

answers: the crust is being stretched,

answers: NDQ_003379

answers: East Pacific Rise.

answers: NDQ_003380

answers: stretched,

answers: NDQ_003381

answers: stretched,

answers: NDQ_003382

answers: stretched,

answers: NDQ_003383

answers: stretched,

answers: NDQ_003384

answers: East Pacific Rise.

answers: NDQ_003385

answers: Fault connect the northern-most extensions of the East Pacific Rise.

answers: NDQ_003386

answers: the crust is being stretched,

answers: NDQ_003387

answers: stretched,

answers: NDQ_003388

answers: stretched,

answers: NDQ_003389

answers: stretched,

answers: NDQ_003390

answers: San Andreas Fault

answers: NDQ_003391

answers: East Pacific Rise.

answers: NDQ_003392

answers: San Andreas Fault

answers: NDQ_003393

answers: East Pacific Rise.

answers: NDQ_003394

answers: San Andreas Fault

answers: NDQ_003395

answers: San Andreas Fault

answers: NDQ_003396

answers: San Andreas Fault

text: The Juan de Fuca plate system has its origins with Panthalassa's oceanic basin and crust. This oceanic crust has primarily been subducted under the North American plate, and the Eurasian Plate. Panthalassa's oceanic plate remnants are understood to be the Juan de Fuca, Gorda, Cocos and the Nazca plates, all four of which were part of the Farallon Plate.

text: The Juan de Fuca plate system has its origins with

text: Panthalassa

text: 's

text: oceanic basin

text: and

text: crust

text: . This oceanic crust has primarily been

text: subducted

text: under the

text: North American plate

text: , and the

text: Eurasian Plate

text: . Panthalassa's oceanic plate remnants are understood to be the Juan de Fuca,

text: Gorda

text: Cocos

text: and the

text: Nazca

text: plates, all four of which were part of the

text: Farallon Plate

answers: NDQ_003351

answers: subduction

answers: NDQ_003352

answers: subducts

answers: NDQ_003353

answers: subduction

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: subduct

answers: NDQ_003357

answers: The Juan de Fuca plate system has its origins with what?

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: subducted

answers: NDQ_003360

answers: North American plate

answers: NDQ_003362

answers: the Juan de Fuca plate system has its origins with Panthalassa's oceanic basin and crust

answers: NDQ_003363

answers: North American plate

answers: NDQ_003371

answers: What is a thrust fault?

answers: NDQ_003373

answers: Why is the Juan de Fuca plate system thought to be the Nazca plates?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: what is the last word in the passage?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: How many plates were part of the Farallon Plate?

answers: NDQ_003381

answers: What does the Juan de Fuca plate system have its origins with?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is the Juan de Fuca plate system?

answers: NDQ_003386

answers: What is the Juan de Fuca plate system?

answers: NDQ_003387

answers: How many plates are part of the Farallon Plate?

answers: NDQ_003388

answers: What does shear stress result from?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: unanswerable

answers: NDQ_003392

answers: Juan de Fuca plate system

answers: NDQ_003393

answers: unanswerable

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: North American plate, and the Eurasian Plate.

answers: NDQ_003352

answers: subducted

answers: NDQ_003353

answers: subducted

answers: NDQ_003354

answers: North American plate, and the Eurasian Plate.

answers: NDQ_003355

answers: The Juan de Fuca

answers: NDQ_003356

answers: subducted

answers: NDQ_003357

answers: subducted under the North American plate, and the Eurasian Plate.

answers: NDQ_003358

answers: oceanic basin

answers: NDQ_003359

answers: subducted under the North American plate,

answers: NDQ_003360

answers: North American plate,

answers: NDQ_003362

answers: subducted under the North American plate,

answers: NDQ_003363

answers: Panthalassa's

answers: NDQ_003371

answers: The Juan de Fuca

answers: NDQ_003373

answers: North American plate, and the Eurasian Plate.

answers: NDQ_003376

answers: oceanic basin and crust.

answers: NDQ_003378

answers: The Juan de Fuca

answers: NDQ_003379

answers: North American plate, and the Eurasian Plate.

answers: NDQ_003380

answers: North American plate, and the Eurasian Plate.

answers: NDQ_003381

answers: subducted under the North American plate, and the Eurasian Plate.

answers: NDQ_003382

answers: North American plate, and the Eurasian Plate.

answers: NDQ_003383

answers: North American plate, and the Eurasian Plate.

answers: NDQ_003384

answers: North American plate, and the Eurasian Plate.

answers: NDQ_003385

answers: North American plate, and the Eurasian Plate.

answers: NDQ_003386

answers: The Juan de Fuca

answers: NDQ_003387

answers: North American plate, and the Eurasian Plate.

answers: NDQ_003388

answers: The Juan de Fuca

answers: NDQ_003389

answers: subducted under the North American plate,

answers: NDQ_003390

answers: The Juan de Fuca

answers: NDQ_003391

answers: North American plate, and the Eurasian Plate.

answers: NDQ_003392

answers: The Juan de Fuca

answers: NDQ_003393

answers: North American plate, and the Eurasian Plate.

answers: NDQ_003394

answers: The Juan de Fuca

answers: NDQ_003395

answers: The Juan de Fuca

answers: NDQ_003396

answers: The Juan de Fuca

text: As the aircraft flies, the magnetometer measures and records the total intensity of the magnetic field at the sensor, which is a combination of the desired magnetic field generated in the Earth as well as tiny variations due to the temporal effects of the constantly varying solar wind and the magnetic field of the survey aircraft. By subtracting the solar, regional, and aircraft effects, the resulting aeromagnetic map shows the spatial distribution and relative abundance of magnetic minerals (most commonly the iron oxide mineral magnetite) in the upper levels of the Earth's crust. Because different rock types differ in their content of magnetic minerals, the magnetic map allows a visualization of the geological structure of the upper crust in the subsurface, particularly the spatial geometry of bodies of rock and the presence of faults and folds. This is particularly useful where bedrock is obscured by surface sand, soil or water. Aeromagnetic data was once presented as contour plots, but now is more commonly expressed as thematic (colored) and shaded computer generated pseudo-topography images. The apparent hills, ridges and valleys are referred to as aeromagnetic anomalies. A geophysicist can use mathematical modeling to infer the shape, depth and properties of the rock bodies responsible for the anomalies.

text: As the aircraft flies, the magnetometer measures and records the total intensity of the

text: magnetic field

text: at the sensor, which is a combination of the desired magnetic field generated in the

text: Earth

text: as well as tiny variations due to the temporal effects of the constantly varying

text: solar wind

text: and the magnetic field of the survey aircraft. By subtracting the solar, regional, and aircraft effects, the resulting aeromagnetic map shows the spatial distribution and relative abundance of magnetic minerals (most commonly the

text: iron oxide

text: mineral

text: magnetite

text: ) in the upper levels of the

text: Earth's crust

text: . Because different rock types differ in their content of magnetic minerals, the magnetic map allows a visualization of the

text: geological structure

text: of the upper crust in the subsurface, particularly the spatial geometry of bodies of rock and the presence of faults and folds. This is particularly useful where bedrock is obscured by surface sand, soil or water. Aeromagnetic data was once presented as contour plots, but now is more commonly expressed as

text: thematic

text: (colored) and shaded computer generated pseudo-topography images. The apparent hills, ridges and valleys are referred to as

text: aeromagnetic anomalies

text: . A

text: geophysicist

text: can use mathematical modeling to infer the shape, depth and properties of the rock bodies responsible for the anomalies.

answers: NDQ_003351

answers: magnetic minerals

answers: NDQ_003352

answers: folds

answers: NDQ_003353

answers: faults

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: ridge

answers: NDQ_003356

answers: fold

answers: NDQ_003357

answers: the magnetic map allows a visualization of what?

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: aeromagnetic anomalies

answers: NDQ_003363

answers: Earth's crust

answers: NDQ_003371

answers: the magnetic map allows a visualization of the geological structure

answers: NDQ_003373

answers: the presence of faults and folds

answers: NDQ_003376

answers: faults and folds

answers: NDQ_003378

answers: the presence of faults and folds

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What type of force applied to rock is a stress?

answers: NDQ_003381

answers: What does the magnetic map allow a visualization of?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Faults and folds

answers: NDQ_003384

answers: Which of the following is not a type of fold: faults and folds?

answers: NDQ_003385

answers: What is the term for an area where faults are clustered?

answers: NDQ_003386

answers: the presence of faults and folds

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: normal faults or folds?

answers: NDQ_003388

answers: What does the magnetic map allow a visualization of the geological structure of the upper crust in the subsurface

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: ridges

answers: NDQ_003391

answers: body of rock

answers: NDQ_003392

answers: ridges

answers: NDQ_003393

answers: body of rock

answers: NDQ_003394

answers: vertical

answers: NDQ_003395

answers: a magnetic map allows a visualization

answers: NDQ_003396

answers: folds

answers: NDQ_003351

answers: faults and folds.

answers: NDQ_003352

answers: faults and folds.

answers: NDQ_003353

answers: faults and folds.

answers: NDQ_003354

answers: faults and folds.

answers: NDQ_003355

answers: faults and folds.

answers: NDQ_003356

answers: faults and folds.

answers: NDQ_003357

answers: faults and folds.

answers: NDQ_003358

answers: faults

answers: NDQ_003359

answers: faults

answers: NDQ_003360

answers: solar wind

answers: NDQ_003362

answers: aeromagnetic anomalies.

answers: NDQ_003363

answers: upper levels of the Earth's crust.

answers: NDQ_003371

answers: faults and folds.

answers: NDQ_003373

answers: faults and folds.

answers: NDQ_003376

answers: aeromagnetic anomalies.

answers: NDQ_003378

answers: aeromagnetic anomalies.

answers: NDQ_003379

answers: faults and folds.

answers: NDQ_003380

answers: faults and folds.

answers: NDQ_003381

answers: faults and folds.

answers: NDQ_003382

answers: faults and folds.

answers: NDQ_003383

answers: faults and folds.

answers: NDQ_003384

answers: faults and folds.

answers: NDQ_003385

answers: faults

answers: NDQ_003386

answers: faults and folds.

answers: NDQ_003387

answers: faults and folds.

answers: NDQ_003388

answers: faults and folds.

answers: NDQ_003389

answers: faults and folds.

answers: NDQ_003390

answers: faults and folds.

answers: NDQ_003391

answers: faults and folds.

answers: NDQ_003392

answers: faults and folds.

answers: NDQ_003393

answers: faults and folds.

answers: NDQ_003394

answers: faults

answers: NDQ_003395

answers: faults and folds.

answers: NDQ_003396

answers: faults and folds.

text: Because the solubility of aluminium in orthopyroxene increases with increasing pressure, many researchers, have suggested that the HAOM crystallized at depth, near the base of the Earth's crust. The maximum amounts of aluminium correspond to a  depth.

text: Because the solubility of aluminium in orthopyroxene increases with increasing pressure, many researchers, have suggested that the HAOM crystallized at depth, near the base of the Earth's crust. The maximum amounts of aluminium correspond to a  depth.

answers: NDQ_003351

answers: depth

answers: NDQ_003352

answers: increases the solubility of aluminium

answers: NDQ_003353

answers: pressure to increase

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: increase in size

answers: NDQ_003357

answers: the maximum amounts of aluminium correspond to a depth

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: the HAOM crystallized at depth

answers: NDQ_003363

answers: depth

answers: NDQ_003371

answers: Which of the following is not an example of a thrust fault?

answers: NDQ_003373

answers: yes

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: Which of the following is not an example of confining stress?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a reason for joints in rock?

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: unanswerable

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: Which of the following is not a type of normal fault?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip faults or shear stress?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: unanswerable

answers: NDQ_003392

answers: a hanging wall

answers: NDQ_003393

answers: dip-slip fault plane

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: is a

answers: NDQ_003396

answers: NDQ_003351

answers: pressure,

answers: NDQ_003352

answers: crystallized at depth,

answers: NDQ_003353

answers: pressure,

answers: NDQ_003354

answers: depth,

answers: NDQ_003355

answers: depth,

answers: NDQ_003356

answers: crystallized at depth,

answers: NDQ_003357

answers: depth,

answers: NDQ_003358

answers: depth,

answers: NDQ_003359

answers: increasing pressure,

answers: NDQ_003360

answers: pressure,

answers: NDQ_003362

answers: HAOM crystallized at depth,

answers: NDQ_003363

answers: depth,

answers: NDQ_003371

answers: Because the solubility of aluminium in orthopyroxene

answers: NDQ_003373

answers: pressure,

answers: NDQ_003376

answers: pressure,

answers: NDQ_003378

answers: depth,

answers: NDQ_003379

answers: depth,

answers: NDQ_003380

answers: pressure,

answers: NDQ_003381

answers: increasing pressure,

answers: NDQ_003382

answers: pressure,

answers: NDQ_003383

answers: pressure,

answers: NDQ_003384

answers: Because the solubility of aluminium in orthopyroxene

answers: NDQ_003385

answers: depth, near the base of the Earth's crust.

answers: NDQ_003386

answers: depth, near the base of the Earth's crust.

answers: NDQ_003387

answers: pressure,

answers: NDQ_003388

answers: pressure,

answers: NDQ_003389

answers: Because the solubility of aluminium in orthopyroxene

answers: NDQ_003390

answers: pressure,

answers: NDQ_003391

answers: depth, near the base of the Earth's crust.

answers: NDQ_003392

answers: HAOM

answers: NDQ_003393

answers: depth,

answers: NDQ_003394

answers: depth,

answers: NDQ_003395

answers: Because the solubility of aluminium in orthopyroxene

answers: NDQ_003396

answers: HAOM

text: Near Cape Mendocino, the Mendocino Triple Junction is an area of active seismicity where three tectonic plates come together. The Mendocino Fracture Zone (also known as the Mendocino Fault east of the Gorda Ridge) is a transform fault that separates the Pacific and Gorda Plates. To the south, the relative motion between the Pacific Plate and North American Plate is accommodated by the San Andreas Fault, and to the north, the Gorda Plate is converging with the North American Plate at the Cascadia Subduction Zone.

text: Near

text: Cape Mendocino

text: , the

text: Mendocino Triple Junction

text: is an area of active seismicity where three tectonic plates come together. The

text: Mendocino Fracture Zone

text: (also known as the Mendocino Fault east of the

text: Gorda Ridge

text: ) is a

text: transform fault

text: that separates the

text: Pacific

text: and

text: Gorda Plate

text: s. To the south, the relative motion between the Pacific Plate and

text: North American Plate

text: is accommodated by the

text: San Andreas Fault

text: , and to the north, the Gorda Plate is converging with the North American Plate at the

text: Cascadia Subduction Zone

answers: NDQ_003351

answers: the San Andreas Fault

answers: NDQ_003352

answers: causes cracks

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: Gorda Ridge

answers: NDQ_003356

answers: change shape

answers: NDQ_003357

answers: separates the Pacific and Gorda plates

answers: NDQ_003358

answers: Fracture Zone

answers: NDQ_003359

answers: separates

answers: NDQ_003360

answers: San Andreas fault

answers: NDQ_003362

answers: The Gorda Plate is converging with the North American Plate at the Cascadia Subduction Zone.

answers: NDQ_003363

answers: San Andreas Fault

answers: NDQ_003371

answers: What type of fault is the Gorda Ridge?

answers: NDQ_003373

answers: How would you describe the Mendocino Fracture Zone?

answers: NDQ_003376

answers: How many tectonic plates come together?

answers: NDQ_003378

answers: What is the area of active seismicity where three tectonic plates come together?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What is the name of the fault that separates the Pacific and Gorda Plates

answers: NDQ_003381

answers: What type of stress does the Mendocino Fracture Zone experience?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What type of fold is the Gorda Ridge?

answers: NDQ_003385

answers: yes

answers: NDQ_003386

answers: What is the Mendocino Fracture Zone?

answers: NDQ_003387

answers: Which of the following is not a normal fault: transform fault, Gorda Ridge, or San Andreas Fault?

answers: NDQ_003388

answers: What type of fault is the Mendocino Fracture Zone?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: transform fault

answers: NDQ_003391

answers: Gorda Ridge

answers: NDQ_003392

answers: transform fault

answers: NDQ_003393

answers: Gorda Ridge

answers: NDQ_003394

answers: transform fault

answers: NDQ_003395

answers: transform fault

answers: NDQ_003396

answers: transform fault

answers: NDQ_003351

answers: San Andreas Fault,

answers: NDQ_003352

answers: The Mendocino Fracture Zone

answers: NDQ_003353

answers: seismicity

answers: NDQ_003354

answers: Near Cape Mendocino,

answers: NDQ_003355

answers: transform fault

answers: NDQ_003356

answers: seismicity

answers: NDQ_003357

answers: separates the Pacific and Gorda Plates.

answers: NDQ_003358

answers: transform fault

answers: NDQ_003359

answers: transform fault

answers: NDQ_003360

answers: tectonic plates

answers: NDQ_003362

answers: Cascadia Subduction Zone.

answers: NDQ_003363

answers: tectonic plates

answers: NDQ_003371

answers: The Mendocino Fracture Zone

answers: NDQ_003373

answers: Near Cape Mendocino,

answers: NDQ_003376

answers: The Mendocino Fracture Zone

answers: NDQ_003378

answers: motion

answers: NDQ_003379

answers: transform fault

answers: NDQ_003380

answers: seismicity

answers: NDQ_003381

answers: The Mendocino Fracture Zone

answers: NDQ_003382

answers: Cascadia Subduction Zone.

answers: NDQ_003383

answers: The Mendocino Fracture Zone

answers: NDQ_003384

answers: Mendocino Fracture Zone

answers: NDQ_003385

answers: The Mendocino Fracture Zone

answers: NDQ_003386

answers: tectonic plates

answers: NDQ_003387

answers: transform fault

answers: NDQ_003388

answers: transform fault

answers: NDQ_003389

answers: three tectonic plates

answers: NDQ_003390

answers: Mendocino Fracture Zone

answers: NDQ_003391

answers: Gorda Ridge)

answers: NDQ_003392

answers: San Andreas Fault,

answers: NDQ_003393

answers: Gorda Ridge)

answers: NDQ_003394

answers: transform fault

answers: NDQ_003395

answers: transform fault

answers: NDQ_003396

answers: transform fault

text: Real life failures in naturally deposited mixed soils are not necessarily circular, but prior to computers, it was far easier to analyse such a simplified geometry.  Nevertheless, failures in 'pure' clay can be quite close to circular.  Such slips often occur after a period of heavy rain, when the pore water pressure at the slip surface increases, reducing the effective normal stress and thus diminishing the restraining friction along the slip line.  This is combined with increased soil weight due to the added groundwater.  A 'shrinkage' crack (formed during prior dry weather) at the top of the slip may also fill with rain water, pushing the slip forward.  At the other extreme, slab-shaped slips on hillsides can remove a layer of soil from the top of the underlying bedrock.  Again, this is usually initiated by heavy rain, sometimes combined with increased loading from new buildings or removal of support at the toe (resulting from road widening or other construction work).  Stability can thus be significantly improved by installing drainage paths to reduce the destabilising forces.  Once the slip has occurred, however, a weakness along the slip circle remains, which may then recur at the next monsoon.

text: Real life failures in naturally deposited mixed soils are not necessarily circular, but prior to computers, it was far easier to analyse such a simplified geometry.  Nevertheless, failures in 'pure' clay can be quite close to circular.  Such slips often occur after a period of heavy rain, when the pore water pressure at the slip surface increases, reducing the effective

text: normal stress

text: and thus diminishing the restraining

text: friction

text: along the slip line.  This is combined with increased soil weight due to the added groundwater.  A 'shrinkage' crack (formed during prior dry weather) at the top of the slip may also fill with rain water, pushing the slip forward.  At the other extreme, slab-shaped slips on hillsides can remove a layer of soil from the top of the underlying bedrock.  Again, this is usually initiated by heavy rain, sometimes combined with increased loading from new buildings or removal of support at the toe (resulting from road widening or other construction work).  Stability can thus be significantly improved by installing drainage paths to reduce the destabilising forces.  Once the slip has occurred, however, a weakness along the slip circle remains, which may then recur at the next monsoon.

answers: NDQ_003351

answers: effective normal stress

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: friction

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: shrinkage

answers: NDQ_003356

answers: shrink

answers: NDQ_003357

answers: pore water pressure at the slip surface increases

answers: NDQ_003358

answers: slip

answers: NDQ_003359

answers: weakens

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: prior to computers, it was far easier to analyse such a simplified geometry

answers: NDQ_003363

answers: heavy rain

answers: NDQ_003371

answers: Which of the following is not a weakness along the slip circle remains:

answers: NDQ_003373

answers: unanswerable

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: not necessarily circular

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What can be done to reduce the destabilising forces?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: faults are clustered

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: unanswerable

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: A 'shrinkage' crack

answers: NDQ_003391

answers: bedrock

answers: NDQ_003392

answers: 'shrinkage' crack

answers: NDQ_003393

answers: bedrock

answers: NDQ_003394

answers: slab-shaped slips

answers: NDQ_003395

answers: can be quite close to circular

answers: NDQ_003396

answers: slab-shaped slips

answers: NDQ_003351

answers: reducing the effective normal stress

answers: NDQ_003352

answers: restraining friction along the slip line.

answers: NDQ_003353

answers: restraining friction

answers: NDQ_003354

answers: Real life failures in naturally deposited mixed soils

answers: NDQ_003355

answers: A'shrinkage'

answers: NDQ_003356

answers: circular,

answers: NDQ_003357

answers: restraining friction along the slip line.

answers: NDQ_003358

answers: A'shrinkage' crack

answers: NDQ_003359

answers: heavy rain,

answers: NDQ_003360

answers: heavy rain,

answers: NDQ_003362

answers: circular,

answers: NDQ_003363

answers: heavy rain,

answers: NDQ_003371

answers: A'shrinkage' crack

answers: NDQ_003373

answers: underlying bedrock.

answers: NDQ_003376

answers: heavy rain,

answers: NDQ_003378

answers: slips

answers: NDQ_003379

answers: circular,

answers: NDQ_003380

answers: stress

answers: NDQ_003381

answers: restraining friction along the slip line.

answers: NDQ_003382

answers: reducing the effective normal stress

answers: NDQ_003383

answers: crack

answers: NDQ_003384

answers: slip line.

answers: NDQ_003385

answers: circular,

answers: NDQ_003386

answers: slips often occur after a period of heavy rain,

answers: NDQ_003387

answers: pore water pressure at the slip surface increases, reducing the effective normal stress

answers: NDQ_003388

answers: heavy rain,

answers: NDQ_003389

answers: computers,

answers: NDQ_003390

answers: circular,

answers: NDQ_003391

answers: bedrock.

answers: NDQ_003392

answers: A'shrinkage' crack

answers: NDQ_003393

answers: underlying bedrock.

answers: NDQ_003394

answers: circular,

answers: NDQ_003395

answers: circular,

answers: NDQ_003396

answers: failures in 'pure' clay can be quite close to circular.

text: Deeper in the Earth's crust, where temperatures and pressures are higher, the rocks in the fault zone can still brecciate, but they keep their internal cohesion. The resulting type of rock is called a cataclasite.

text: Deeper in the Earth's

text: crust

text: , where temperatures and pressures are higher, the rocks in the fault zone can still brecciate, but they keep their internal cohesion. The resulting type of rock is called a

text: cataclasite

answers: NDQ_003351

answers: brecciate

answers: NDQ_003352

answers: brecciates

answers: NDQ_003353

answers: brecciation

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fault

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: the rocks in the fault zone can still brecciate

answers: NDQ_003358

answers: fault zone

answers: NDQ_003359

answers: brecciate

answers: NDQ_003360

answers: fault lines

answers: NDQ_003362

answers: Deeper in the Earth's crust, where temperatures and pressures are lower, the rocks in the fault zone can still brecciate

answers: NDQ_003363

answers: deeper in the Earth's crust

answers: NDQ_003371

answers: Which of the following is not a type of rock: cataclasite or thrust fault?

answers: NDQ_003373

answers: yes

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What does brecciate mean?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not a type of fold?

answers: NDQ_003385

answers: yes

answers: NDQ_003386

answers: no

answers: NDQ_003387

answers: Which of the following is not a cause of normal faults: compression stress, temperature, or pressure?

answers: NDQ_003388

answers: Which of the following is not a result of shear stress: strike-slip faults, cataclasites or shear stress?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: Cataclasite

answers: NDQ_003391

answers: cataclasite

answers: NDQ_003392

answers: Cataclasite

answers: NDQ_003393

answers: cataclasite

answers: NDQ_003394

answers: cataclasite

answers: NDQ_003395

answers: a cataclasite

answers: NDQ_003396

answers: Cataclasite

answers: NDQ_003351

answers: brecciate,

answers: NDQ_003352

answers: brecciate,

answers: NDQ_003353

answers: brecciate,

answers: NDQ_003354

answers: cataclasite.

answers: NDQ_003355

answers: cataclasite.

answers: NDQ_003356

answers: brecciate,

answers: NDQ_003357

answers: brecciate, but they keep their internal cohesion.

answers: NDQ_003358

answers: cataclasite.

answers: NDQ_003359

answers: temperatures and pressures are higher,

answers: NDQ_003360

answers: fault zone

answers: NDQ_003362

answers: they keep their internal cohesion.

answers: NDQ_003363

answers: fault zone

answers: NDQ_003371

answers: cataclasite.

answers: NDQ_003373

answers: temperatures and pressures

answers: NDQ_003376

answers: cataclasite.

answers: NDQ_003378

answers: brecciate,

answers: NDQ_003379

answers: cataclasite.

answers: NDQ_003380

answers: pressures

answers: NDQ_003381

answers: brecciate,

answers: NDQ_003382

answers: brecciate,

answers: NDQ_003383

answers: brecciate,

answers: NDQ_003384

answers: cataclasite.

answers: NDQ_003385

answers: fault zone

answers: NDQ_003386

answers: brecciate,

answers: NDQ_003387

answers: Deeper in the Earth's crust,

answers: NDQ_003388

answers: cataclasite.

answers: NDQ_003389

answers: cataclasite.

answers: NDQ_003390

answers: cataclasite.

answers: NDQ_003391

answers: cataclasite.

answers: NDQ_003392

answers: cataclasite.

answers: NDQ_003393

answers: cataclasite.

answers: NDQ_003394

answers: cataclasite.

answers: NDQ_003395

answers: cataclasite.

answers: NDQ_003396

answers: cataclasite.

text: The mantle differs substantially from the crust in its mechanical properties which is the direct consequence of chemical composition change (expressed as different mineralogy). The distinction between crust and mantle is based on chemistry, rock types, rheology and seismic characteristics. The crust is a solidification product of mantle derived melts, expressed as various degrees of partial melting products during geologic time. Partial melting of mantle material is believed to cause incompatible elements to separate from the mantle, with less dense material floating upward through pore spaces, cracks, or fissures, that would subsequently cool and solidify at the surface. Typical mantle rocks have a higher magnesium to iron ratio and a smaller proportion of silicon and aluminium than the crust. This behavior is also predicted by experiments that partly melt rocks thought to be representative of Earth's mantle.

text: The mantle differs substantially from the crust in its mechanical properties which is the direct consequence of chemical composition change (expressed as different mineralogy). The distinction between crust and mantle is based on chemistry, rock types,

text: rheology

text: and

text: seismic

text: characteristics. The crust is a solidification product of mantle derived melts, expressed as various degrees of partial melting products during geologic time. Partial melting of mantle material is believed to cause incompatible elements to separate from the mantle, with less dense material floating upward through pore spaces, cracks, or fissures, that would subsequently cool and solidify at the surface. Typical mantle rocks have a higher magnesium to iron ratio and a smaller proportion of

text: silicon

text: and

text: aluminium

text: than the crust. This behavior is also predicted by experiments that partly melt rocks thought to be representative of Earth's mantle.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: cracks

answers: NDQ_003353

answers: chemical composition change

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fissure

answers: NDQ_003356

answers: solidify at the surface

answers: NDQ_003357

answers: Partial melting of mantle material is believed to cause incompatible elements to separate from the mantle

answers: NDQ_003358

answers: crack

answers: NDQ_003359

answers: Partial melting

answers: NDQ_003360

answers: mantle

answers: NDQ_003362

answers: Partial melting of mantle material is believed to cause incompatible elements to separate from the mantle

answers: NDQ_003363

answers: mantle

answers: NDQ_003371

answers: What is the difference between crust and mantle?

answers: NDQ_003373

answers: What is the difference between crust and mantle?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What is the direct consequence of chemical composition change?

answers: NDQ_003381

answers: What is the direct consequence of chemical composition change?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Partial melting of mantle material

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: What is the distinction between crust and mantle based on?

answers: NDQ_003387

answers: What is the distinction between crust and mantle based on?

answers: NDQ_003388

answers: What is the difference between crust and mantle?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: seismic characteristics

answers: NDQ_003391

answers: mantle

answers: NDQ_003392

answers: fissures

answers: NDQ_003393

answers: The crust

answers: NDQ_003394

answers: pore spaces

answers: NDQ_003395

answers: cracks

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: seismic characteristics.

answers: NDQ_003352

answers: pore spaces, cracks, or fissures,

answers: NDQ_003353

answers: pore spaces, cracks, or fissures,

answers: NDQ_003354

answers: The mantle

answers: NDQ_003355

answers: pore spaces, cracks, or fissures,

answers: NDQ_003356

answers: pore spaces, cracks, or fissures,

answers: NDQ_003357

answers: pore spaces, cracks, or fissures,

answers: NDQ_003358

answers: cracks, or fissures,

answers: NDQ_003359

answers: Partial melting

answers: NDQ_003360

answers: The mantle

answers: NDQ_003362

answers: The mantle

answers: NDQ_003363

answers: mantle derived melts,

answers: NDQ_003371

answers: pore spaces, cracks, or fissures,

answers: NDQ_003373

answers: The mantle

answers: NDQ_003376

answers: The mantle

answers: NDQ_003378

answers: seismic characteristics.

answers: NDQ_003379

answers: chemistry, rock types, rheology and seismic characteristics.

answers: NDQ_003380

answers: seismic characteristics.

answers: NDQ_003381

answers: Partial melting

answers: NDQ_003382

answers: The mantle

answers: NDQ_003383

answers: pore spaces, cracks, or fissures,

answers: NDQ_003384

answers: pore spaces, cracks, or fissures,

answers: NDQ_003385

answers: The mantle

answers: NDQ_003386

answers: seismic characteristics.

answers: NDQ_003387

answers: chemical composition change

answers: NDQ_003388

answers: The mantle

answers: NDQ_003389

answers: The mantle

answers: NDQ_003390

answers: seismic characteristics.

answers: NDQ_003391

answers: The mantle

answers: NDQ_003392

answers: seismic characteristics.

answers: NDQ_003393

answers: The mantle

answers: NDQ_003394

answers: seismic characteristics.

answers: NDQ_003395

answers: The mantle

answers: NDQ_003396

answers: The mantle

text: An RRR junction is always stable using these definitions and therefore very common on earth, though in a geological sense ridge spreading is usually discontinued in one direction leaving failed rift zone. There are many examples of these present both now and in the geological past such as the South Atlantic opening with ridges spreading North and South to form the Mid-Atlantic Ridge, and an associated aulacogen in the Niger Delta region of Africa. RRR junctions are also common as rifting along three fractures at 120° is the best way to relieve stresses from uplift at the surface of a sphere; on earth stresses similar to these are believed to be caused by the mantle hotspots thought to initiate rifting in continents.

text: An RRR junction is always stable using these definitions and therefore very common on earth, though in a geological sense ridge spreading is usually discontinued in one direction leaving failed

text: rift

text: zone. There are many examples of these present both now and in the geological past such as the South Atlantic opening with ridges spreading North and South to form the

text: Mid-Atlantic Ridge

text: , and an associated

text: aulacogen

text: in the

text: Niger Delta

text: region of Africa. RRR junctions are also common as rifting along three fractures at 120° is the best way to relieve stresses from uplift at the surface of a sphere; on earth stresses similar to these are believed to be caused by the mantle

text: hotspots

text: thought to initiate rifting in continents.

answers: NDQ_003351

answers: uplift

answers: NDQ_003352

answers: uplifts

answers: NDQ_003353

answers: fractures

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: rift zone

answers: NDQ_003356

answers: relieve stresses

answers: NDQ_003357

answers: ridges spreading North and South to form the Mid-Atlantic Ridge

answers: NDQ_003358

answers: rift zone

answers: NDQ_003359

answers: uplifts

answers: NDQ_003360

answers: Earth

answers: NDQ_003362

answers: An RRR junction is always stable using these definitions

answers: NDQ_003363

answers: RRR junctions

answers: NDQ_003371

answers: What is the best way to relieve stresses from uplift?

answers: NDQ_003373

answers: no

answers: NDQ_003376

answers: no

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: no

answers: NDQ_003380

answers: unanswerable

answers: NDQ_003381

answers: unanswerable

answers: NDQ_003382

answers: no

answers: NDQ_003383

answers: no

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: Fault zone

answers: NDQ_003386

answers: uplift

answers: NDQ_003387

answers: no

answers: NDQ_003388

answers: unanswerable

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: aulacogen

answers: NDQ_003391

answers: rift zone

answers: NDQ_003392

answers: aulacogen

answers: NDQ_003393

answers: rift zone

answers: NDQ_003394

answers: RRR

answers: NDQ_003395

answers: RRR junctions

answers: NDQ_003396

answers: RRR

answers: NDQ_003351

answers: uplift

answers: NDQ_003352

answers: uplift

answers: NDQ_003353

answers: rifting

answers: NDQ_003354

answers: Mid-Atlantic Ridge,

answers: NDQ_003355

answers: aulacogen

answers: NDQ_003356

answers: ridge spreading is usually discontinued in one direction leaving failed rift zone.

answers: NDQ_003357

answers: ridge spreading is usually discontinued in one direction

answers: NDQ_003358

answers: failed rift zone.

answers: NDQ_003359

answers: fractures at 120° is the best way to relieve stresses from uplift

answers: NDQ_003360

answers: earth,

answers: NDQ_003362

answers: ridge spreading is usually discontinued in one direction leaving failed rift zone.

answers: NDQ_003363

answers: rifting along three fractures at 120°

answers: NDQ_003371

answers: RRR junction

answers: NDQ_003373

answers: mantle hotspots

answers: NDQ_003376

answers: uplift

answers: NDQ_003378

answers: uplift

answers: NDQ_003379

answers: 120°

answers: NDQ_003380

answers: stresses from uplift

answers: NDQ_003381

answers: uplift

answers: NDQ_003382

answers: uplift

answers: NDQ_003383

answers: stresses from uplift

answers: NDQ_003384

answers: Mid-Atlantic Ridge, and an associated aulacogen

answers: NDQ_003385

answers: rift zone.

answers: NDQ_003386

answers: uplift

answers: NDQ_003387

answers: uplift

answers: NDQ_003388

answers: mantle hotspots

answers: NDQ_003389

answers: uplift

answers: NDQ_003390

answers: RRR junction

answers: NDQ_003391

answers: aulacogen

answers: NDQ_003392

answers: RRR junction

answers: NDQ_003393

answers: aulacogen

answers: NDQ_003394

answers: 120°

answers: NDQ_003395

answers: three fractures at 120°

answers: NDQ_003396

answers: RRR

text: Author of the book: The Evolution of weathering crusts in the history of the Earth.

text: Author of the book: The Evolution of weathering crusts in the history of the Earth.

answers: NDQ_003351

answers: deformation

answers: NDQ_003352

answers: increases in size.

answers: NDQ_003353

answers: weathering

answers: NDQ_003354

answers: Toroweap Formation is a formation

answers: NDQ_003355

answers: elongation

answers: NDQ_003356

answers: change shape

answers: NDQ_003357

answers: weathering crusts are exposed to heat.

answers: NDQ_003358

answers: crack

answers: NDQ_003359

answers: is broken apart

answers: NDQ_003360

answers: crustal plates

answers: NDQ_003362

answers: The San Andreas fault is not a fault.

answers: NDQ_003363

answers: tectonic plates

answers: NDQ_003371

answers: What is a thrust fault?

answers: NDQ_003373

answers: The author of The Evolution of weathering crusts in the history of the Earth.

answers: NDQ_003376

answers: The Evolution of weathering crusts in the history of the Earth.

answers: NDQ_003378

answers: The amount of the ground moves in an earthquake is called

answers: NDQ_003379

answers: The dip of the fault plane is horizontal.

answers: NDQ_003380

answers: What is a stress?

answers: NDQ_003381

answers: The author is a geologist

answers: NDQ_003382

answers: The Evolution of weathering crusts in the history of the Earth.

answers: NDQ_003383

answers: The author of The Evolution of weathering crusts in the history of the Earth

answers: NDQ_003384

answers: A syncline is a fold that arches upward.

answers: NDQ_003385

answers: Isotopes

answers: NDQ_003386

answers: The author is a geologist

answers: NDQ_003387

answers: The author of The Evolution of weathering crusts in the history of the Earth

answers: NDQ_003388

answers: The Evolution of weathering crusts

answers: NDQ_003389

answers: The process of folding does not create mountains

answers: NDQ_003390

answers: a fault in which the hanging wall drops

answers: NDQ_003391

answers: is a block of rock

answers: NDQ_003392

answers: is a type of fault

answers: NDQ_003393

answers: is a block of rock

answers: NDQ_003394

answers: is not vertical

answers: NDQ_003395

answers: is a type of

answers: NDQ_003396

answers: Faults in the Earth's crust

answers: NDQ_003351

answers: weathering crusts

answers: NDQ_003352

answers: weathering crusts

answers: NDQ_003353

answers: weathering crusts

answers: NDQ_003354

answers: The Evolution of weathering crusts in the history of the Earth.

answers: NDQ_003355

answers: crusts

answers: NDQ_003356

answers: weathering crusts

answers: NDQ_003357

answers: weathering crusts

answers: NDQ_003358

answers: crusts

answers: NDQ_003359

answers: weathering crusts

answers: NDQ_003360

answers: The Evolution of weathering crusts

answers: NDQ_003362

answers: The Evolution of weathering crusts

answers: NDQ_003363

answers: weathering crusts

answers: NDQ_003371

answers: The Evolution of weathering crusts in the history of the Earth.

answers: NDQ_003373

answers: The Evolution of weathering crusts

answers: NDQ_003376

answers: The Evolution of weathering crusts

answers: NDQ_003378

answers: The Evolution of weathering crusts

answers: NDQ_003379

answers: The Evolution of weathering crusts in the history of the Earth.

answers: NDQ_003380

answers: The Evolution of weathering crusts in the history of the Earth.

answers: NDQ_003381

answers: The Evolution of weathering crusts

answers: NDQ_003382

answers: The Evolution of weathering crusts in the history of the Earth.

answers: NDQ_003383

answers: The Evolution of weathering crusts

answers: NDQ_003384

answers: Author of the book: The Evolution of weathering crusts

answers: NDQ_003385

answers: The Evolution of weathering crusts

answers: NDQ_003386

answers: The Evolution of weathering crusts

answers: NDQ_003387

answers: The Evolution of weathering crusts

answers: NDQ_003388

answers: The Evolution of weathering crusts

answers: NDQ_003389

answers: The Evolution of weathering crusts

answers: NDQ_003390

answers: The Evolution of weathering crusts

answers: NDQ_003391

answers: crusts

answers: NDQ_003392

answers: The Evolution of weathering crusts

answers: NDQ_003393

answers: crusts

answers: NDQ_003394

answers: The Evolution of weathering crusts

answers: NDQ_003395

answers: The Evolution of weathering crusts

answers: NDQ_003396

answers: The Evolution of weathering crusts in the history of the Earth.

text: For circuits operating at or above 2,000 volts between conductors, a conductive shield may surround each insulated conductor. This equalizes electrical stress on the cable insulation. This technique was patented by Martin Hochstadter in 1916; the shield is sometimes called a Hochstadter shield. The individual conductor shields of a cable are connected to earth ground at the ends of the cable, and at locations along the length if voltage rise during faults would be dangerous.

text: For circuits operating at or above 2,000 volts between conductors, a conductive shield may surround each insulated conductor. This equalizes electrical stress on the cable insulation. This technique was patented by Martin Hochstadter in 1916; the shield is sometimes called a Hochstadter shield. The individual conductor shields of a cable are connected to earth ground at the ends of the cable, and at locations along the length if voltage rise during

text: faults

text: would be dangerous.

answers: NDQ_003351

answers: electrical stress

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: earth ground is connected to the ends of the cable

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: a conductive shield may surround each insulated conductor

answers: NDQ_003363

answers: Earth's core

answers: NDQ_003371

answers: What technique was patented by Martin Hochstadter in 1916?

answers: NDQ_003373

answers: what is the first word in the first paragraph?

answers: NDQ_003376

answers: basin-and-range

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What is the opposite of equalizes electrical stress?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: The individual conductor shields of a cable are connected to earth ground

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: normal faults or Hochstadter shields?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip faults or Hochstadter shields?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: Hochstadter shield

answers: NDQ_003391

answers: earth

answers: NDQ_003392

answers: Hochstadter shield

answers: NDQ_003393

answers: earth ground

answers: NDQ_003394

answers: a Hochstadter shield

answers: NDQ_003395

answers: a Hochstadter shield

answers: NDQ_003396

answers: NDQ_003351

answers: 2,000 volts

answers: NDQ_003352

answers: faults would be dangerous.

answers: NDQ_003353

answers: voltage rise during faults

answers: NDQ_003354

answers: For circuits operating at or above 2,000 volts

answers: NDQ_003355

answers: Hochstadter shield.

answers: NDQ_003356

answers: voltage rise

answers: NDQ_003357

answers: voltage rise

answers: NDQ_003358

answers: faults

answers: NDQ_003359

answers: voltage rise

answers: NDQ_003360

answers: 2,000 volts

answers: NDQ_003362

answers: voltage rise during faults would be dangerous.

answers: NDQ_003363

answers: 2,000 volts

answers: NDQ_003371

answers: 2,000 volts

answers: NDQ_003373

answers: For circuits operating at or above 2,000 volts

answers: NDQ_003376

answers: 2,000 volts

answers: NDQ_003378

answers: earth ground

answers: NDQ_003379

answers: The individual conductor shields of a cable are connected to earth ground

answers: NDQ_003380

answers: stress

answers: NDQ_003381

answers: electrical stress

answers: NDQ_003382

answers: 2,000 volts

answers: NDQ_003383

answers: stress

answers: NDQ_003384

answers: 2,000 volts

answers: NDQ_003385

answers: Hochstadter shield.

answers: NDQ_003386

answers: voltage rise during faults

answers: NDQ_003387

answers: voltage rise during faults

answers: NDQ_003388

answers: voltage rise during faults

answers: NDQ_003389

answers: For circuits operating at or above 2,000 volts

answers: NDQ_003390

answers: voltage rise during faults

answers: NDQ_003391

answers: earth ground

answers: NDQ_003392

answers: faults

answers: NDQ_003393

answers: earth ground

answers: NDQ_003394

answers: faults

answers: NDQ_003395

answers: faults

answers: NDQ_003396

answers: Hochstadter shield.

text: All processes that move, elevate or build up portions of the earth’s crust come under diastrophism. They include: (i) orogenic processes involving mountain building through severe folding and affecting long and narrow belts of the earth’s crust; (ii) epeirogenic processes involving uplift or warping of large parts of the earth’s crust; (iii) earthquakes involving local relatively minor movements; (iv) plate tectonics involving horizontal movements of crustal plates.

text: All processes that move, elevate or build up portions of the earth’s crust come under diastrophism. They include: (i) orogenic processes involving mountain building through severe folding and affecting long and narrow belts of the earth’s crust; (ii) epeirogenic processes involving uplift or warping of large parts of the earth’s crust; (iii) earthquakes involving local relatively minor movements; (iv) plate tectonics involving horizontal movements of crustal plates.

answers: NDQ_003351

answers: (iv)

answers: NDQ_003352

answers: (iv)

answers: NDQ_003353

answers: (iv)

answers: NDQ_003354

answers: (iv)

answers: NDQ_003355

answers: orogenic process

answers: NDQ_003356

answers: (iv)

answers: NDQ_003357

answers: (iii)

answers: NDQ_003358

answers: earthquake

answers: NDQ_003359

answers: (iv)

answers: NDQ_003360

answers: (ii)

answers: NDQ_003362

answers: earthquakes involving local relatively minor movements

answers: NDQ_003363

answers: (iv)

answers: NDQ_003371

answers: (iv)

answers: NDQ_003373

answers: (iv)

answers: NDQ_003376

answers: (iv)

answers: NDQ_003378

answers: (iii)

answers: NDQ_003379

answers: (iv)

answers: NDQ_003380

answers: (iii)

answers: NDQ_003381

answers: (iv)

answers: NDQ_003382

answers: (iv)

answers: NDQ_003383

answers: (iv)

answers: NDQ_003384

answers: (iv)

answers: NDQ_003385

answers: (iv)

answers: NDQ_003386

answers: (iii)

answers: NDQ_003387

answers: (iv)

answers: NDQ_003388

answers: (iv)

answers: NDQ_003389

answers: (i)

answers: NDQ_003390

answers: (iv)

answers: NDQ_003391

answers: (iv)

answers: NDQ_003392

answers: (iv)

answers: NDQ_003393

answers: (iv)

answers: NDQ_003394

answers: (iv)

answers: NDQ_003395

answers: (iv)

answers: NDQ_003396

answers: (iv)

answers: NDQ_003351

answers: epeirogenic processes

answers: NDQ_003352

answers: warping

answers: NDQ_003353

answers: warping

answers: NDQ_003354

answers: diastrophism.

answers: NDQ_003355

answers: orogenic processes

answers: NDQ_003356

answers: warping

answers: NDQ_003357

answers: local relatively minor movements;

answers: NDQ_003358

answers: earthquakes

answers: NDQ_003359

answers: movements;

answers: NDQ_003360

answers: epeirogenic processes

answers: NDQ_003362

answers: local relatively minor movements;

answers: NDQ_003363

answers: orogenic processes involving mountain building through severe folding

answers: NDQ_003371

answers: diastrophism.

answers: NDQ_003373

answers: diastrophism.

answers: NDQ_003376

answers: orogenic processes

answers: NDQ_003378

answers: local relatively minor movements;

answers: NDQ_003379

answers: horizontal movements of crustal plates.

answers: NDQ_003380

answers: uplift or warping

answers: NDQ_003381

answers: epeirogenic processes involving uplift or warping

answers: NDQ_003382

answers: horizontal movements of crustal plates.

answers: NDQ_003383

answers: uplift or warping

answers: NDQ_003384

answers: orogenic processes involving mountain building through severe folding

answers: NDQ_003385

answers: diastrophism.

answers: NDQ_003386

answers: local relatively minor movements;

answers: NDQ_003387

answers: folding

answers: NDQ_003388

answers: (i) orogenic processes involving mountain building through severe folding

answers: NDQ_003389

answers: orogenic processes

answers: NDQ_003390

answers: diastrophism.

answers: NDQ_003391

answers: mountain building

answers: NDQ_003392

answers: diastrophism.

answers: NDQ_003393

answers: mountain building

answers: NDQ_003394

answers: plate tectonics

answers: NDQ_003395

answers: horizontal movements of crustal plates.

answers: NDQ_003396

answers: plate tectonics

text: The Northern Cordilleran Volcanic Province has been a zone of active volcanism since it began to form 20 million years ago. Unlike other parts of the Pacific Ring of Fire, the Northern Cordilleran Volcanic Province has its origins in continental rifting—an area where the Earth's crust and lithosphere is being pulled apart. This differs from other portions of the Pacific Ring of Fire as it consists largely of volcanic arcs formed by subducting oceanic crust at oceanic trenches along continental margins circling the Pacific Ocean. The continental crust at the Northern Cordilleran Volcanic Province is being stretched at a rate of about  per year. This incipient rifting formed as a result of the Pacific Plate sliding northward along the Queen Charlotte Fault, on its way to the Aleutian Trench, which extends along the southern coastline of Alaska and the adjacent waters off the southern coast of the Kamchatka Peninsula. As a result, volcanism in the Northern Cordilleran Volcanic Province is also not related to back-arc basin volcanism. When the stored energy is suddenly released by slippage across the fault at irregular intervals, it can create very large earthquakes, such as the magnitude 8.1 Queen Charlotte Islands earthquake of 1949. As these far-field forces stretch the North American crust, the near surface rocks fracture along steeply dipping faults parallel to the rift zone. Hot magma rises between these fractures to create passive or effusive eruptions. Volcanoes within the Northern Cordilleran Volcanic Province are located along short northerly trending segments which in the northern part of the volcanic province are unmistakenably involved with north-trending rift structures, including synvolcanic grabens and grabens with one major fault line along only one of the boundaries (half-grabens). Grabens are indicative of tensional forces and crustal stretching.

text: The Northern Cordilleran Volcanic Province has been a zone of active

text: volcanism

text: since it began to form 20 million years ago. Unlike other parts of the Pacific Ring of Fire, the Northern Cordilleran Volcanic Province has its origins in continental

text: rift

text: ing—an area where the Earth's

text: crust

text: and

text: lithosphere

text: is being pulled apart. This differs from other portions of the Pacific Ring of Fire as it consists largely of

text: volcanic arc

text: s formed by

text: subducting

text: oceanic crust

text: at

text: oceanic trench

text: es along

text: continental margin

text: s circling the

text: Pacific Ocean

text: . The

text: continental crust

text: at the Northern Cordilleran Volcanic Province is being stretched at a rate of about  per year. This incipient rifting formed as a result of the

text: Pacific Plate

text: sliding northward along the

text: Queen Charlotte Fault

text: , on its way to the

text: Aleutian Trench

text: , which extends along the southern coastline of Alaska and the adjacent waters off the southern coast of the

text: Kamchatka Peninsula

text: . As a result, volcanism in the Northern Cordilleran Volcanic Province is also not related to

text: back-arc basin

text: volcanism. When the stored energy is suddenly released by slippage across the

text: fault

text: at irregular intervals, it can create very large

text: earthquake

text: s, such as the

text: magnitude

text: Queen Charlotte Islands earthquake of 1949

text: . As these far-field forces stretch the North American crust, the near surface rocks fracture along steeply dipping faults parallel to the rift zone. Hot magma rises between these fractures to create passive or

text: effusive eruption

text: s. Volcanoes within the Northern Cordilleran Volcanic Province are located along short northerly trending segments which in the northern part of the volcanic province are unmistakenably involved with north-trending rift structures, including synvolcanic

text: graben

text: s and grabens with one major fault line along only one of the boundaries (

text: half-graben

text: s). Grabens are indicative of tensional forces and crustal stretching.

answers: NDQ_003351

answers: tensional

answers: NDQ_003352

answers: fractures

answers: NDQ_003353

answers: Fracture

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: Fault

answers: NDQ_003356

answers: create what type of eruption?

answers: NDQ_003357

answers: steeply dipping faults parallel to the rift zone

answers: NDQ_003358

answers: passive

answers: NDQ_003359

answers: as far-field forces stretch

answers: NDQ_003360

answers: far-field forces

answers: NDQ_003362

answers: not related to back-arc basin volcanism

answers: NDQ_003363

answers: Pacific Ring of Fire

answers: NDQ_003371

answers: Which of the following is not an indication of tensional forces and crustal stretching: grabens?

answers: NDQ_003373

answers: Which of the following is not an indication of tensional forces and crustal stretching?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: no

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What is the opposite of rifting?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not an indication of tensional forces and crustal stretching?

answers: NDQ_003385

answers: what is the area where the Earth's crust and lithosphere is being pulled apart

answers: NDQ_003386

answers: What is the cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not a type of normal fault: tensional forces or crustal stretching?

answers: NDQ_003388

answers: Which of the following is not indicative of tensional forces and crustal stretching: grabens?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: Queen Charlotte Fault

answers: NDQ_003391

answers: grabens

answers: NDQ_003392

answers: Queen Charlotte Fault

answers: NDQ_003393

answers: surface rocks

answers: NDQ_003394

answers: steeply dipping faults

answers: NDQ_003395

answers: Queen Charlotte Fault

answers: NDQ_003396

answers: Queen Charlotte Fault

answers: NDQ_003351

answers: canism.

answers: NDQ_003352

answers: fracture

answers: NDQ_003353

answers: fracture

answers: NDQ_003354

answers: Northern Cordilleran Volcanic Province

answers: NDQ_003355

answers: steeply dipping faults

answers: NDQ_003356

answers: fracture along steeply dipping faults parallel to the rift zone.

answers: NDQ_003357

answers: stored energy is suddenly released by slippage

answers: NDQ_003358

answers: passive

answers: NDQ_003359

answers: near surface rocks fracture along steeply dipping faults

answers: NDQ_003360

answers: back-arc basin volcanism.

answers: NDQ_003362

answers: volcanism.

answers: NDQ_003363

answers: continental rifting—an

answers: NDQ_003371

answers: steeply dipping faults

answers: NDQ_003373

answers: oceanic trenches

answers: NDQ_003376

answers: back-arc basin volcanism.

answers: NDQ_003378

answers: slippage

answers: NDQ_003379

answers: steeply dipping faults parallel to the rift zone.

answers: NDQ_003380

answers: tensional forces

answers: NDQ_003381

answers: the near surface rocks fracture along steeply dipping faults

answers: NDQ_003382

answers: tensional forces and crustal stretching.

answers: NDQ_003383

answers: fracture along steeply dipping faults

answers: NDQ_003384

answers: synvolcanic grabens

answers: NDQ_003385

answers: rift zone.

answers: NDQ_003386

answers: the stored energy is suddenly released by slippage

answers: NDQ_003387

answers: steeply dipping faults

answers: NDQ_003388

answers: steeply dipping faults parallel to the rift zone.

answers: NDQ_003389

answers: subducting oceanic crust at oceanic trenches

answers: NDQ_003390

answers: Queen Charlotte Fault,

answers: NDQ_003391

answers: near surface rocks

answers: NDQ_003392

answers: Queen Charlotte Fault,

answers: NDQ_003393

answers: near surface rocks

answers: NDQ_003394

answers: Queen Charlotte Fault,

answers: NDQ_003395

answers: Queen Charlotte Fault,

answers: NDQ_003396

answers: steeply dipping faults

text: Earth minerals and metal ores are examples of non-renewable resources. The metals themselves are present in vast amounts in Earth's crust, and their extraction by humans only occurs where they are concentrated by natural geological processes (such as heat, pressure, organic activity, weathering and other processes) enough to become economically viable to extract. These processes generally take from tens of thousands to millions of years, through plate tectonics, tectonic subsidence and crustal recycling.

text: Earth

text: minerals and

text: metal

text: ores are examples of non-renewable resources. The metals themselves are present in vast amounts in Earth's

text: crust

text: , and their extraction by humans only occurs where they are concentrated by

text: natural geological processes

text: (such as heat, pressure, organic activity, weathering and other processes) enough to become economically viable to extract. These processes generally take from tens of thousands to millions of years, through

text: plate tectonics

text: tectonic subsidence

text: and

text: crustal recycling

answers: NDQ_003351

answers: pressure

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: pressure

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: plate

answers: NDQ_003356

answers: subsidence

answers: NDQ_003357

answers: plate tectonics, tectonic subsidence and crustal recycling

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: plate tectonic

answers: NDQ_003362

answers: humans only occur where they are concentrated by natural geological processes

answers: NDQ_003363

answers: plate tectonics

answers: NDQ_003371

answers: What is a non-renewable resource?

answers: NDQ_003373

answers: How would you describe compressive stresses?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What is a non-renewable resource

answers: NDQ_003381

answers: what is the first type of stress mentioned?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: plate tectonics

answers: NDQ_003386

answers: plate tectonics

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: What kind of stress does shear stress cause?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: tectonic subsidence

answers: NDQ_003391

answers: Subsidy

answers: NDQ_003392

answers: tectonic subsidence

answers: NDQ_003393

answers: subduction

answers: NDQ_003394

answers: plate tectonics

answers: NDQ_003395

answers: plate tectonics

answers: NDQ_003396

answers: plate tectonics

answers: NDQ_003351

answers: tectonic subsidence

answers: NDQ_003352

answers: weathering

answers: NDQ_003353

answers: weathering

answers: NDQ_003354

answers: Earth minerals and metal ores are examples of non-renewable resources.

answers: NDQ_003355

answers: tectonic subsidence

answers: NDQ_003356

answers: weathering

answers: NDQ_003357

answers: tectonic subsidence

answers: NDQ_003358

answers: tectonic subsidence

answers: NDQ_003359

answers: concentrated by natural geological processes

answers: NDQ_003360

answers: plate tectonics,

answers: NDQ_003362

answers: non-renewable resources.

answers: NDQ_003363

answers: plate tectonics,

answers: NDQ_003371

answers: tectonic subsidence

answers: NDQ_003373

answers: heat, pressure,

answers: NDQ_003376

answers: natural geological processes

answers: NDQ_003378

answers: tectonic subsidence

answers: NDQ_003379

answers: Earth minerals and metal ores are examples of non-renewable resources.

answers: NDQ_003380

answers: pressure,

answers: NDQ_003381

answers: Earth minerals and metal ores are examples of non-renewable resources.

answers: NDQ_003382

answers: pressure,

answers: NDQ_003383

answers: pressure,

answers: NDQ_003384

answers: Earth minerals and metal ores are examples of non-renewable resources.

answers: NDQ_003385

answers: Earth minerals and metal ores are examples of non-renewable resources.

answers: NDQ_003386

answers: plate tectonics,

answers: NDQ_003387

answers: tectonic subsidence

answers: NDQ_003388

answers: Earth minerals and metal ores are examples of non-renewable resources.

answers: NDQ_003389

answers: plate tectonics,

answers: NDQ_003390

answers: tectonic subsidence

answers: NDQ_003391

answers: tectonic subsidence

answers: NDQ_003392

answers: tectonic subsidence

answers: NDQ_003393

answers: tectonic subsidence

answers: NDQ_003394

answers: Earth minerals and metal ores are examples of non-renewable resources.

answers: NDQ_003395

answers: tectonic subsidence

answers: NDQ_003396

answers: tectonic subsidence

text: Molecules as components of matter are common in organic substances (and therefore biochemistry). They also make up most of the oceans and atmosphere. However, the majority of familiar solid substances on Earth, including most of the minerals that make up the crust, mantle, and core of the Earth, contain many chemical bonds, but are not made of identifiable molecules. Also, no typical molecule can be defined for ionic crystals (salts) and covalent crystals (network solids), although these are often composed of repeating unit cells that extend either in a plane (such as in graphene) or three-dimensionally (such as in diamond, quartz, or sodium chloride). The theme of repeated unit-cellular-structure also holds for most condensed phases with metallic bonding, which means that solid metals are also not made of molecules. In glasses (solids that exist in a vitreous disordered state), atoms may also be held together by chemical bonds with no presence of any definable molecule, nor any of the regularity of repeating units that characterizes crystals.

text: Molecules as components of matter are common in organic substances (and therefore biochemistry). They also make up most of the oceans and atmosphere. However, the majority of familiar solid substances on Earth, including most of the minerals that make up the

text: crust

text: mantle

text: , and

text: core of the Earth

text: , contain many chemical bonds, but are not made of identifiable molecules. Also, no typical molecule can be defined for

text: ionic crystal

text: s (

text: salts

text: ) and covalent crystals (

text: network solid

text: s), although these are often composed of repeating

text: unit cell

text: s that extend either in a

text: plane

text: (such as in

text: graphene

text: ) or three-dimensionally (such as in

text: diamond

text: quartz

text: , or

text: sodium chloride

text: ). The theme of repeated unit-cellular-structure also holds for most condensed phases with

text: metallic bond

text: ing, which means that solid metals are also not made of molecules. In

text: glass

text: es (solids that exist in a vitreous disordered state), atoms may also be held together by chemical bonds with no presence of any definable molecule, nor any of the regularity of repeating units that characterizes crystals.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: chemical bonds

answers: NDQ_003353

answers: chemical bonds

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: make up most of the oceans

answers: NDQ_003357

answers: atoms may also be held together by chemical bonds

answers: NDQ_003358

answers: mantle

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: Molecules as components of matter are common in organic substances

answers: NDQ_003363

answers: the core of the Earth

answers: NDQ_003371

answers: What is a thrust fault?

answers: NDQ_003373

answers: None of the above choices.

answers: NDQ_003376

answers: basin-and-range

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What is a stress?

answers: NDQ_003381

answers: What type of rock deforms?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: chemical bonds

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: fault zone

answers: NDQ_003386

answers: movement of rock at faults

answers: NDQ_003387

answers: None of the above choices.

answers: NDQ_003388

answers: What type of stress is shear stress?

answers: NDQ_003389

answers: minerals

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: mantle

answers: NDQ_003392

answers: a vitreous disordered state

answers: NDQ_003393

answers: mantle

answers: NDQ_003394

answers: 3D

answers: NDQ_003395

answers: graphene

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: chemical bonds

answers: NDQ_003352

answers: molecules.

answers: NDQ_003353

answers: chemical bonds,

answers: NDQ_003354

answers: Molecules

answers: NDQ_003355

answers: Molecules

answers: NDQ_003356

answers: molecules.

answers: NDQ_003357

answers: atoms may also be held together by chemical bonds

answers: NDQ_003358

answers: glasses

answers: NDQ_003359

answers: molecules.

answers: NDQ_003360

answers: Molecules

answers: NDQ_003362

answers: Molecules

answers: NDQ_003363

answers: Molecules

answers: NDQ_003371

answers: molecules.

answers: NDQ_003373

answers: Molecules

answers: NDQ_003376

answers: molecules.

answers: NDQ_003378

answers: molecules.

answers: NDQ_003379

answers: molecules.

answers: NDQ_003380

answers: molecules.

answers: NDQ_003381

answers: molecules.

answers: NDQ_003382

answers: Molecules

answers: NDQ_003383

answers: chemical bonds, but are not made of identifiable molecules.

answers: NDQ_003384

answers: graphene) or three-dimensionally

answers: NDQ_003385

answers: molecules.

answers: NDQ_003386

answers: Molecules

answers: NDQ_003387

answers: molecules.

answers: NDQ_003388

answers: molecules.

answers: NDQ_003389

answers: Molecules

answers: NDQ_003390

answers: Molecules

answers: NDQ_003391

answers: diamond, quartz, or sodium chloride).

answers: NDQ_003392

answers: Molecules

answers: NDQ_003393

answers: diamond, quartz, or sodium chloride).

answers: NDQ_003394

answers: three-dimensionally

answers: NDQ_003395

answers: graphene)

answers: NDQ_003396

answers: molecules.

text: Crustal strain and deformation is the change in shape and volume of continental and oceanic crust caused by stress applied to rock through tectonic forces. An array of variables including composition, temperature, pressure, etc., determines how the crust will deform.

text: Crustal

text: strain

text: and

text: deformation

text: is the change in shape and volume of continental and oceanic crust caused by stress applied to rock through tectonic forces. An array of variables including composition, temperature, pressure, etc., determines how the crust will deform.

answers: NDQ_003351

answers: pressure

answers: NDQ_003352

answers: deforms

answers: NDQ_003353

answers: tectonic forces

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: deformation

answers: NDQ_003356

answers: change in shape

answers: NDQ_003357

answers: change in shape and volume of continental and oceanic crust

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: deforms

answers: NDQ_003360

answers: tectonic forces

answers: NDQ_003362

answers: The San Andreas fault is not a fault.

answers: NDQ_003363

answers: tectonic forces

answers: NDQ_003371

answers: Which of the following is not a variable that determines how the crust will deform?

answers: NDQ_003373

answers: How would you describe tectonic forces?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: Yes

answers: NDQ_003381

answers: What is the change in shape and volume of continental and oceanic crust caused by?

answers: NDQ_003382

answers: what is the most common stress at convergent plates

answers: NDQ_003383

answers: None of the above choices.

answers: NDQ_003384

answers: What is a fold that arches upward?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: Which of the following is not a cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not a cause of normal faults?

answers: NDQ_003388

answers: Which of the following is not a cause of strike-slip faults?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: tectonic

answers: NDQ_003391

answers: can not be deformed

answers: NDQ_003392

answers: tectonic

answers: NDQ_003393

answers: tectonic forces

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: is a type of

answers: NDQ_003396

answers: isobath

answers: NDQ_003351

answers: tectonic forces.

answers: NDQ_003352

answers: change in shape and volume

answers: NDQ_003353

answers: Crustal strain and deformation

answers: NDQ_003354

answers: Crustal strain and deformation

answers: NDQ_003355

answers: Crustal strain

answers: NDQ_003356

answers: composition,

answers: NDQ_003357

answers: stress applied to rock through tectonic forces.

answers: NDQ_003358

answers: Crustal strain

answers: NDQ_003359

answers: stress applied to rock through tectonic forces.

answers: NDQ_003360

answers: tectonic forces.

answers: NDQ_003362

answers: Crustal strain and deformation

answers: NDQ_003363

answers: tectonic forces.

answers: NDQ_003371

answers: Crustal strain and deformation

answers: NDQ_003373

answers: tectonic forces.

answers: NDQ_003376

answers: tectonic forces.

answers: NDQ_003378

answers: Crustal strain

answers: NDQ_003379

answers: tectonic forces.

answers: NDQ_003380

answers: tectonic forces.

answers: NDQ_003381

answers: tectonic forces.

answers: NDQ_003382

answers: pressure,

answers: NDQ_003383

answers: stress applied to rock through tectonic forces.

answers: NDQ_003384

answers: tectonic forces.

answers: NDQ_003385

answers: tectonic forces.

answers: NDQ_003386

answers: tectonic forces.

answers: NDQ_003387

answers: tectonic forces.

answers: NDQ_003388

answers: tectonic forces.

answers: NDQ_003389

answers: tectonic forces.

answers: NDQ_003390

answers: Crustal strain and deformation

answers: NDQ_003391

answers: Crustal strain

answers: NDQ_003392

answers: Crustal strain and deformation

answers: NDQ_003393

answers: Crustal strain

answers: NDQ_003394

answers: Crustal strain and deformation

answers: NDQ_003395

answers: tectonic forces.

answers: NDQ_003396

answers: Crustal strain and deformation

text: Thus there is reason to believe that ophiolites are indeed oceanic mantle and crust; however, certain problems arise when looking closer. Compositional differences regarding silica (SiO) and titania (TiO) contents, for example, place ophiolite basalts in the domain of subduction zones (~55% silica, <1% TiO), whereas mid-ocean ridge basalts typically have ~50% silica and 1.5-2.5% TiO. These chemical differences extend to a range of trace elements as well (that is, chemical elements occurring in amounts of 1000 ppm or less). In particular, trace elements associated with subduction zone (island arc) volcanics tend to be high in ophiolites, whereas trace elements that are high in ocean ridge basalts but low in subduction zone volcanics are also low in ophiolites.

text: Thus there is reason to believe that ophiolites are indeed oceanic mantle and crust; however, certain problems arise when looking closer. Compositional differences regarding

text: silica

text: (SiO) and titania (TiO) contents, for example, place ophiolite basalts in the domain of subduction zones (~55% silica, <1% TiO), whereas mid-ocean ridge basalts typically have ~50% silica and 1.5-2.5% TiO. These chemical differences extend to a range of

text: trace element

text: s as well (that is, chemical elements occurring in amounts of 1000 ppm or less). In particular, trace elements associated with subduction zone (island arc) volcanics tend to be high in ophiolites, whereas trace elements that are high in ocean ridge basalts but low in subduction zone volcanics are also low in ophiolites.

answers: NDQ_003351

answers: subduction zone

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: chemical differences

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: subduction zone

answers: NDQ_003356

answers: ophiolites

answers: NDQ_003357

answers: 55% silica,  1% TiO

answers: NDQ_003358

answers: subduction zone

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: subduction zones

answers: NDQ_003362

answers: ophiolites are indeed oceanic mantle and crust

answers: NDQ_003363

answers: subduction zones

answers: NDQ_003371

answers: Which of the following is not a type of rock: ophiolites, mid-ocean ridge basalts, or subduction zones?

answers: NDQ_003373

answers: What is the reason for this?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What type of force applied to rock is a stress?

answers: NDQ_003381

answers: What type of rock deforms?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: What is the cause of joints in rock

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: subduction zones

answers: NDQ_003386

answers: subduction zones

answers: NDQ_003387

answers: What type of faults are caused by compression stress?

answers: NDQ_003388

answers: What type of stress results from strike-slip faults?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: subduction zone

answers: NDQ_003391

answers: ophiolites

answers: NDQ_003392

answers: subduction zone

answers: NDQ_003393

answers: ophiolites

answers: NDQ_003394

answers: subduction zone

answers: NDQ_003395

answers: subduction zone (island arc)

answers: NDQ_003396

answers: ophiolites

answers: NDQ_003351

answers: subduction zones

answers: NDQ_003352

answers: subduction zones

answers: NDQ_003353

answers: chemical differences

answers: NDQ_003354

answers: ophiolite basalts in the domain of subduction zones

answers: NDQ_003355

answers: subduction zones

answers: NDQ_003356

answers: subduction zones

answers: NDQ_003357

answers: subduction zones

answers: NDQ_003358

answers: subduction zones

answers: NDQ_003359

answers: subduction zones

answers: NDQ_003360

answers: subduction zones

answers: NDQ_003362

answers: ophiolites

answers: NDQ_003363

answers: subduction zones

answers: NDQ_003371

answers: subduction zones

answers: NDQ_003373

answers: subduction zones

answers: NDQ_003376

answers: subduction zones

answers: NDQ_003378

answers: subduction zones

answers: NDQ_003379

answers: subduction zones

answers: NDQ_003380

answers: subduction zones

answers: NDQ_003381

answers: subduction zones

answers: NDQ_003382

answers: subduction zones

answers: NDQ_003383

answers: subduction zones

answers: NDQ_003384

answers: subduction zones

answers: NDQ_003385

answers: subduction zones

answers: NDQ_003386

answers: subduction zones

answers: NDQ_003387

answers: subduction zones

answers: NDQ_003388

answers: subduction zones

answers: NDQ_003389

answers: subduction zones

answers: NDQ_003390

answers: subduction zones

answers: NDQ_003391

answers: ophiolites

answers: NDQ_003392

answers: subduction zones

answers: NDQ_003393

answers: ophiolites

answers: NDQ_003394

answers: subduction zones

answers: NDQ_003395

answers: subduction zones

answers: NDQ_003396

answers: subduction zones

text: According to the Fellowship, the Lemurian Philosophy was revealed to Stelle by highly advanced men and women, called Masters or Elder Brothers. The Philosophy is said to have formed the foundation of the so-called Mukulian civilization on the legendary continent of Mu (also known as Lemuria) now covered by the Pacific Ocean. This lost continent is considered incompatible with the theory of plate tectonics, the standard theory describing movement of the earth's lithosphere accepted by most, but not all, earth scientists. Nonetheless, the Lemurian Philosophy points to various megalithic structures and other features on various Pacific Islands, and in South America and Asia, as indications that the continent and an advanced civilization did at one time exist.

text: According to the Fellowship, the Lemurian Philosophy was revealed to Stelle by highly advanced men and women, called Masters or Elder Brothers. The Philosophy is said to have formed the foundation of the so-called Mukulian

text: civilization

text: on the legendary

text: continent

text: of Mu (also known as

text: Lemuria

text: ) now covered by the Pacific Ocean. This

text: lost continent

text: is considered incompatible with the

text: theory

text: of

text: plate tectonics

text: , the standard theory describing movement of the

text: earth

text: 's

text: lithosphere

text: accepted by most, but not all,

text: earth scientists

text: . Nonetheless, the Lemurian Philosophy points to various

text: megalith

text: ic structures and other features on various

text: Pacific Islands

text: , and in South America and Asia, as indications that the continent and an advanced civilization did at one time exist.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: movement

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: unanswerable

answers: NDQ_003356

answers: move

answers: NDQ_003357

answers: movement of the earth's lithosphere

answers: NDQ_003358

answers: lithosphere

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: plate tectonics

answers: NDQ_003362

answers: This lost continent is considered incompatible with the theory of plate tectonics

answers: NDQ_003363

answers: plate tectonics

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: not enough information

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: vertical

answers: NDQ_003380

answers: unanswerable

answers: NDQ_003381

answers: unanswerable

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: unanswerable

answers: NDQ_003386

answers: plate tectonics

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: unanswerable

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: lithosphere

answers: NDQ_003392

answers: tectonics

answers: NDQ_003393

answers: lithosphere

answers: NDQ_003394

answers: tectonics

answers: NDQ_003395

answers: unanswerable

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: lithosphere

answers: NDQ_003352

answers: lithosphere

answers: NDQ_003353

answers: movement of the earth's lithosphere

answers: NDQ_003354

answers: the Lemurian Philosophy

answers: NDQ_003355

answers: plate tectonics,

answers: NDQ_003356

answers: megalithic structures

answers: NDQ_003357

answers: movement of the earth's lithosphere

answers: NDQ_003358

answers: megalithic structures

answers: NDQ_003359

answers: movement of the earth's lithosphere

answers: NDQ_003360

answers: plate tectonics,

answers: NDQ_003362

answers: This lost continent

answers: NDQ_003363

answers: plate tectonics,

answers: NDQ_003371

answers: plate tectonics,

answers: NDQ_003373

answers: plate tectonics,

answers: NDQ_003376

answers: plate tectonics,

answers: NDQ_003378

answers: plate tectonics,

answers: NDQ_003379

answers: Masters or Elder Brothers.

answers: NDQ_003380

answers: megalithic structures

answers: NDQ_003381

answers: plate tectonics,

answers: NDQ_003382

answers: plate tectonics,

answers: NDQ_003383

answers: plate tectonics,

answers: NDQ_003384

answers: plate tectonics,

answers: NDQ_003385

answers: plate tectonics,

answers: NDQ_003386

answers: plate tectonics,

answers: NDQ_003387

answers: plate tectonics,

answers: NDQ_003388

answers: plate tectonics,

answers: NDQ_003389

answers: plate tectonics,

answers: NDQ_003390

answers: plate tectonics,

answers: NDQ_003391

answers: megalithic structures

answers: NDQ_003392

answers: plate tectonics,

answers: NDQ_003393

answers: megalithic structures

answers: NDQ_003394

answers: plate tectonics,

answers: NDQ_003395

answers: plate tectonics,

answers: NDQ_003396

answers: plate tectonics,

text: Saliva testing also has specific uses in clinical and experimental psychological settings. Due to its ability to provide insight into human behavior, emotions, and development, it has been used to investigate psychological phenomenon such as anxiety, depression, PTSD, and other behavioral disorders. Its primary purpose is to test cortisol and alpha amylase levels, which are indicative of stress levels. Salivary cortisol is a good stress index, with increased levels of cortisol correlating positively with increased levels of stress. Cortisol levels rise slowly over time and take a while to return to base level, indicating that cortisol is more associated with chronic stress levels. Alpha amylase, on the other hand, spikes quickly when confronted with a stressor and returns to baseline soon after the stress has passed, making salivary amylase measurement a powerful tool for psychological research studying acute stress responses. Samples are usually collected from participants by having them drool through a straw into a collection tube while experiencing a stimulus, with samples taken every few minutes to record the gradual change in stress hormone levels. Because the collection of saliva samples is non-invasive, it has the advantage of not introducing further stress on the participant that may otherwise distort results.

text: Saliva testing also has specific uses in clinical and

text: experimental psychological

text: settings. Due to its ability to provide insight into human behavior, emotions, and development, it has been used to investigate psychological phenomenon such as

text: anxiety

text: depression

text: PTSD

text: , and other behavioral disorders. Its primary purpose is to test

text: cortisol

text: and

text: alpha amylase

text: levels, which are indicative of stress levels. Salivary cortisol is a good stress index, with increased levels of cortisol correlating positively with increased levels of stress. Cortisol levels rise slowly over time and take a while to return to base level, indicating that cortisol is more associated with

text: chronic stress

text: levels. Alpha amylase, on the other hand, spikes quickly when confronted with a stressor and returns to baseline soon after the stress has passed, making salivary amylase measurement a powerful tool for psychological research studying acute stress responses. Samples are usually collected from participants by having them drool through a straw into a collection tube while experiencing a stimulus, with samples taken every few minutes to record the gradual change in stress hormone levels. Because the collection of saliva samples is non-invasive, it has the advantage of not introducing further stress on the participant that may otherwise distort results.

answers: NDQ_003351

answers: acute stress

answers: NDQ_003352

answers: cortisol levels increase

answers: NDQ_003353

answers: alpha amylase to spike

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: swell

answers: NDQ_003357

answers: alpha amylase spikes quickly when confronted with a stressor

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: cortisol is more associated with chronic stress levels

answers: NDQ_003363

answers: the same time

answers: NDQ_003371

answers: context: Saliva testing also has specific uses in clinical and experimental psychological settings

answers: NDQ_003373

answers: it has the advantage of not introducing further stress on the participant

answers: NDQ_003376

answers: basin-and-range

answers: NDQ_003378

answers: the amount the ground moves in an earthquake

answers: NDQ_003379

answers: strike-slip fault

answers: NDQ_003380

answers: What is the primary purpose of saliva testing?

answers: NDQ_003381

answers: cortisol levels rise slowly over time

answers: NDQ_003382

answers: Salivary cortisol

answers: NDQ_003383

answers: None of the above choices

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: Fault zone

answers: NDQ_003386

answers: movement of rock at faults

answers: NDQ_003387

answers: What is the primary purpose of saliva testing?

answers: NDQ_003388

answers: context: Strike-slip faults result from shear stress.

answers: NDQ_003389

answers: process of folding

answers: NDQ_003390

answers: a fault

answers: NDQ_003391

answers: dip-slip fault plane

answers: NDQ_003392

answers: Fracture

answers: NDQ_003393

answers: a dip-slip fault plane

answers: NDQ_003394

answers: is a fault

answers: NDQ_003395

answers: a vertical fault plane

answers: NDQ_003396

answers: NDQ_003351

answers: chronic stress levels.

answers: NDQ_003352

answers: Alpha amylase,

answers: NDQ_003353

answers: Alpha amylase,

answers: NDQ_003354

answers: Saliva testing also has specific uses in clinical and experimental psychological settings.

answers: NDQ_003355

answers: Saliva testing

answers: NDQ_003356

answers: Alpha amylase,

answers: NDQ_003357

answers: Alpha amylase,

answers: NDQ_003358

answers: Saliva testing

answers: NDQ_003359

answers: Saliva testing also has specific uses in clinical and experimental psychological settings.

answers: NDQ_003360

answers: stressor

answers: NDQ_003362

answers: cortisol is more associated with chronic stress levels.

answers: NDQ_003363

answers: Saliva testing

answers: NDQ_003371

answers: Saliva testing also has specific uses in clinical and experimental psychological settings.

answers: NDQ_003373

answers: Saliva testing also has specific uses in clinical and experimental psychological settings.

answers: NDQ_003376

answers: Saliva testing also has specific uses in clinical and experimental psychological settings.

answers: NDQ_003378

answers: stimulus,

answers: NDQ_003379

answers: Alpha amylase,

answers: NDQ_003380

answers: stress levels.

answers: NDQ_003381

answers: Alpha amylase,

answers: NDQ_003382

answers: Alpha amylase,

answers: NDQ_003383

answers: increased levels of cortisol correlating positively with increased levels of stress.

answers: NDQ_003384

answers: Saliva testing also has specific uses in clinical and experimental psychological settings.

answers: NDQ_003385

answers: Saliva testing also has specific uses in clinical and experimental psychological settings.

answers: NDQ_003386

answers: Saliva testing

answers: NDQ_003387

answers: chronic stress levels. Alpha amylase,

answers: NDQ_003388

answers: Saliva testing also has specific uses in clinical and experimental psychological settings.

answers: NDQ_003389

answers: Saliva testing

answers: NDQ_003390

answers: Saliva testing also has specific uses in clinical and experimental psychological settings.

answers: NDQ_003391

answers: Saliva testing

answers: NDQ_003392

answers: Saliva testing also has specific uses in clinical and experimental psychological settings.

answers: NDQ_003393

answers: Saliva testing

answers: NDQ_003394

answers: Saliva testing also has specific uses in clinical and experimental psychological settings.

answers: NDQ_003395

answers: Saliva testing also has specific uses in clinical and experimental psychological settings.

answers: NDQ_003396

answers: Saliva testing also has specific uses in clinical and experimental psychological settings.

text: The Pliocene-Pleistocene changes in Tyrrhenian back-arc extension may have also been influenced by the adjacent Adriatic and Sicilian forelands. These sectors were not thinned by rifting and are characterized by normal continental lithosphere. During its southeastward migration, the passively retreating oceanic slab had to adjust and deform in relation the large and buoyant continental sectors. Post-Pliocene migration was eventually driven through the narrow corridor (250 km) represented by the present Ionian Sea and thus separated the Adriatic and Sicilian sectors. Changes in lithospheric composition may have also contributed to differences in subduction geometry. For instance, during the first episode of subduction, thinned continental lithosphere underlying the Apenninic margin subducted beneath the Eurasian plate. However, in the second episode of subduction, it was instead Ionian oceanic lithosphere that was involved in subduction. A transition from continental to oceanic lithosphere subduction could explain the late onset of arc volcanism (2-1.5 Ma) as well as the lack of arc volcanism in the central Tyrrhenian basin.

text: The Pliocene-Pleistocene changes in Tyrrhenian back-arc extension may have also been influenced by the adjacent Adriatic and Sicilian forelands. These sectors were not thinned by rifting and are characterized by normal continental lithosphere. During its southeastward migration, the passively retreating oceanic slab had to adjust and deform in relation the large and buoyant continental sectors. Post-Pliocene migration was eventually driven through the narrow corridor (250 km) represented by the present Ionian Sea and thus separated the Adriatic and Sicilian sectors. Changes in lithospheric composition may have also contributed to differences in subduction geometry. For instance, during the first episode of subduction, thinned continental lithosphere underlying the Apenninic margin subducted beneath the Eurasian plate. However, in the second episode of subduction, it was instead Ionian oceanic lithosphere that was involved in subduction. A transition from continental to oceanic lithosphere subduction could explain the late onset of arc volcanism (2-1.5 Ma) as well as the lack of arc volcanism in the central Tyrrhenian basin.

answers: NDQ_003351

answers: subduction

answers: NDQ_003352

answers: deforms

answers: NDQ_003353

answers: deformation

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: back-arc extension

answers: NDQ_003356

answers: subduct beneath the Eurasian plate

answers: NDQ_003357

answers: continental lithosphere is involved in subduction

answers: NDQ_003358

answers: rifting

answers: NDQ_003359

answers: subducts

answers: NDQ_003360

answers: continental plates

answers: NDQ_003362

answers: These sectors were not thinned by rifting

answers: NDQ_003363

answers: Subduction

answers: NDQ_003371

answers: What may have contributed to differences in subduction geometry?

answers: NDQ_003373

answers: What type of stresses is a deeply buried rock under?

answers: NDQ_003376

answers: What type of terrain is the central Tyrrhenian basin?

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What is the passively retreating oceanic slab?

answers: NDQ_003381

answers: What happened to the Adriatic and Sicilian sectors?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: subduction

answers: NDQ_003387

answers: Which of the following is not a cause of normal faults: compression stress, rifting or rifting?

answers: NDQ_003388

answers: Which of the following is not a type of strike-slip fault?

answers: NDQ_003389

answers: subduction

answers: NDQ_003390

answers: rifting

answers: NDQ_003391

answers: lithosphere

answers: NDQ_003392

answers: rifting

answers: NDQ_003393

answers: rifting

answers: NDQ_003394

answers: rifting

answers: NDQ_003395

answers: Subduction geometry

answers: NDQ_003396

answers: rifting

answers: NDQ_003351

answers: arc volcanism

answers: NDQ_003352

answers: deform

answers: NDQ_003353

answers: deform

answers: NDQ_003354

answers: The Pliocene-Pleistocene

answers: NDQ_003355

answers: arc volcanism

answers: NDQ_003356

answers: buoyant

answers: NDQ_003357

answers: continental lithosphere.

answers: NDQ_003358

answers: arc volcanism

answers: NDQ_003359

answers: thinned by rifting

answers: NDQ_003360

answers: rifting

answers: NDQ_003362

answers: These sectors were not thinned by rifting

answers: NDQ_003363

answers: Tyrrhenian

answers: NDQ_003371

answers: rifting

answers: NDQ_003373

answers: continental lithosphere.

answers: NDQ_003376

answers: rifting

answers: NDQ_003378

answers: rifting

answers: NDQ_003379

answers: normal continental lithosphere.

answers: NDQ_003380

answers: deform

answers: NDQ_003381

answers: oceanic slab had to adjust and deform

answers: NDQ_003382

answers: rifting

answers: NDQ_003383

answers: deform

answers: NDQ_003384

answers: arc volcanism

answers: NDQ_003385

answers: Adriatic and Sicilian forelands.

answers: NDQ_003386

answers: arc volcanism

answers: NDQ_003387

answers: rifting

answers: NDQ_003388

answers: Changes in lithospheric composition

answers: NDQ_003389

answers: rifting

answers: NDQ_003390

answers: rifting

answers: NDQ_003391

answers: Eurasian plate.

answers: NDQ_003392

answers: rifting

answers: NDQ_003393

answers: Apenninic margin

answers: NDQ_003394

answers: rifting

answers: NDQ_003395

answers: Eurasian plate.

answers: NDQ_003396

answers: back-arc extension

text: The last part of the curve, perhaps the most important part, can be filled in by inference. This would come from studying similar geology throughout the world (using analogs to extend time), or by a study of fault mechanics. For example, large-scale studies have been conducted for Stable Continental Regions (SCR's), which are defined "as regions of continental crust that have not experienced any major tectonism, magmatism, basement metamorphism or anorogenic intrusion since the early Cretaceous, and no rifting or major extension or transtension since the Paleogene."

text: The last part of the curve, perhaps the most important part, can be filled in by inference. This would come from studying similar geology throughout the world (using analogs to extend time), or by a study of

text: fault mechanics

text: . For example, large-scale studies have been conducted for Stable Continental Regions (SCR's), which are defined "as regions of continental crust that have not experienced any major tectonism, magmatism, basement metamorphism or anorogenic intrusion since the early Cretaceous, and no rifting or major extension or transtension since the Paleogene."

answers: NDQ_003351

answers: transtension

answers: NDQ_003352

answers: liquefies

answers: NDQ_003353

answers: metamorphism

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: transtension

answers: NDQ_003356

answers: change shape

answers: NDQ_003357

answers: tectonism, magmatism, basement metamorphism or anorogenic intrusion

answers: NDQ_003358

answers: Stable Continental Region

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: fault mechanics

answers: NDQ_003362

answers: the last part of the curve, perhaps the most important part, can be filled in by inference

answers: NDQ_003363

answers: Stable Continental Regions

answers: NDQ_003371

answers: Stable Continental Regions

answers: NDQ_003373

answers: basement metamorphism

answers: NDQ_003376

answers: basin-and-range

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: strike-slip fault

answers: NDQ_003380

answers: What is the most important part of the curve?

answers: NDQ_003381

answers: Stable Continental Regions

answers: NDQ_003382

answers: the Paleogene

answers: NDQ_003383

answers: fault mechanics

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: fault mechanics

answers: NDQ_003386

answers: tectonism

answers: NDQ_003387

answers: a study of fault mechanics

answers: NDQ_003388

answers: study of fault mechanics

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: transtension

answers: NDQ_003391

answers: basement

answers: NDQ_003392

answers: rifting

answers: NDQ_003393

answers: basement

answers: NDQ_003394

answers: tectonism

answers: NDQ_003395

answers: tectonism

answers: NDQ_003396

answers: Stable Continental Regions

answers: NDQ_003351

answers: transtension

answers: NDQ_003352

answers: rifting or major extension or transtension

answers: NDQ_003353

answers: magmatism, basement metamorphism

answers: NDQ_003354

answers: Stable Continental Regions

answers: NDQ_003355

answers: transtension

answers: NDQ_003356

answers: basement metamorphism

answers: NDQ_003357

answers: rifting or major extension or transtension

answers: NDQ_003358

answers: Stable Continental Regions

answers: NDQ_003359

answers: fault mechanics.

answers: NDQ_003360

answers: fault mechanics.

answers: NDQ_003362

answers: major tectonism,

answers: NDQ_003363

answers: early Cretaceous,

answers: NDQ_003371

answers: fault mechanics.

answers: NDQ_003373

answers: fault mechanics.

answers: NDQ_003376

answers: fault mechanics.

answers: NDQ_003378

answers: fault mechanics.

answers: NDQ_003379

answers: fault mechanics.

answers: NDQ_003380

answers: fault mechanics.

answers: NDQ_003381

answers: fault mechanics.

answers: NDQ_003382

answers: fault mechanics.

answers: NDQ_003383

answers: fault mechanics.

answers: NDQ_003384

answers: fault mechanics.

answers: NDQ_003385

answers: fault mechanics.

answers: NDQ_003386

answers: fault mechanics.

answers: NDQ_003387

answers: fault mechanics.

answers: NDQ_003388

answers: fault mechanics.

answers: NDQ_003389

answers: tectonism,

answers: NDQ_003390

answers: transtension

answers: NDQ_003391

answers: basement

answers: NDQ_003392

answers: transtension

answers: NDQ_003393

answers: basement metamorphism or anorogenic intrusion

answers: NDQ_003394

answers: fault mechanics.

answers: NDQ_003395

answers: fault mechanics.

answers: NDQ_003396

answers: fault mechanics.

text: As an ocean is progressively trapped in between two colliding continental lithospheres, the rising wedges of oceanic crust and mantle rise are caught in the jaws of the continent/continent vise and detach and begin to move up the advancing continental rise. Continued convergence may lead to the overthrusting of the arc-trench gap and eventually overthrusting of the metamorphic plutonic and volcanic rocks of the volcanic arc.

text: As an ocean is progressively trapped in between two colliding continental lithospheres, the rising wedges of oceanic crust and mantle rise are caught in the jaws of the continent/continent vise and detach and begin to move up the advancing continental rise. Continued convergence may lead to the overthrusting of the arc-trench gap and eventually overthrusting of the metamorphic plutonic and volcanic rocks of the volcanic arc.

answers: NDQ_003351

answers: overthrusting

answers: NDQ_003352

answers: overthrusts

answers: NDQ_003353

answers: overthrusting

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: arc

answers: NDQ_003356

answers: overthrust

answers: NDQ_003357

answers: overthrusting of the arc-trench gap

answers: NDQ_003358

answers: arc

answers: NDQ_003359

answers: overturns

answers: NDQ_003360

answers: continents

answers: NDQ_003362

answers: The San Andreas fault is not a volcano.

answers: NDQ_003363

answers: a volcanic arc

answers: NDQ_003371

answers: Which of the following is not a type of thrust fault?

answers: NDQ_003373

answers: None of the above choices.

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: what is the first type of rock mentioned?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: None of the above choices.

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: overthrusting

answers: NDQ_003387

answers: Which of the following is not a type of normal fault?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip faults, arc-trench faults, or volcanic arcs?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: overthrusting

answers: NDQ_003391

answers: lithosphere

answers: NDQ_003392

answers: overthrusting

answers: NDQ_003393

answers: volcanic arc

answers: NDQ_003394

answers: overthrusting

answers: NDQ_003395

answers: is a

answers: NDQ_003396

answers: isobath

answers: NDQ_003351

answers: overthrusting

answers: NDQ_003352

answers: overthrusting

answers: NDQ_003353

answers: metamorphic plutonic and volcanic rocks

answers: NDQ_003354

answers: progressively trapped in between two colliding continental lithospheres,

answers: NDQ_003355

answers: arc-trench gap

answers: NDQ_003356

answers: overthrusting

answers: NDQ_003357

answers: overthrusting of the arc-trench gap

answers: NDQ_003358

answers: arc-trench gap

answers: NDQ_003359

answers: overthrusting

answers: NDQ_003360

answers: colliding continental lithospheres,

answers: NDQ_003362

answers: detach and begin to move up the advancing continental rise.

answers: NDQ_003363

answers: volcanic arc.

answers: NDQ_003371

answers: overthrusting of the arc-trench gap

answers: NDQ_003373

answers: overthrusting

answers: NDQ_003376

answers: the rising wedges of oceanic crust and mantle rise

answers: NDQ_003378

answers: rising wedges of oceanic crust

answers: NDQ_003379

answers: progressively trapped in between two colliding continental lithospheres,

answers: NDQ_003380

answers: overthrusting

answers: NDQ_003381

answers: overthrusting

answers: NDQ_003382

answers: overthrusting of the arc-trench gap

answers: NDQ_003383

answers: overthrusting

answers: NDQ_003384

answers: arc-trench gap

answers: NDQ_003385

answers: two colliding continental lithospheres,

answers: NDQ_003386

answers: overthrusting

answers: NDQ_003387

answers: arc-trench gap

answers: NDQ_003388

answers: progressively trapped in between two colliding continental lithospheres,

answers: NDQ_003389

answers: continental rise.

answers: NDQ_003390

answers: arc-trench gap

answers: NDQ_003391

answers: arc-trench gap

answers: NDQ_003392

answers: arc-trench gap

answers: NDQ_003393

answers: volcanic arc.

answers: NDQ_003394

answers: arc-trench gap

answers: NDQ_003395

answers: arc-trench gap

answers: NDQ_003396

answers: volcanic arc.

text: Volcanoes that occur above subduction zones, such as Mount St. Helens, Mount Etna and Mount Fuji, lie at approximately one hundred kilometres from the trench in arcuate chains, hence the term volcanic arc. Two kinds of arcs are generally observed on Earth: island arcs that form on oceanic lithosphere (for example, the Mariana and the Tonga island arcs), and continental arcs such as the Cascade Volcanic Arc, that form along the coast of continents. Island arcs are produced by the subduction of oceanic lithosphere beneath another oceanic lithosphere (ocean-ocean subduction) while continental arcs formed during subduction of oceanic lithosphere beneath a continental lithosphere (ocean-continent subduction).  An example of a volcanic arc having both island and continental arc sections is found behind the Aleutian Trench subduction zone in Alaska.

text: Volcano

text: es that occur above subduction zones, such as

text: Mount St. Helens

text: Mount Etna

text: and

text: Mount Fuji

text: , lie at approximately one hundred kilometres from the trench in arcuate chains, hence the term

text: volcanic arc

text: . Two kinds of arcs are generally observed on Earth:

text: island arcs

text: that form on oceanic lithosphere (for example, the

text: Mariana

text: and the

text: Tonga

text: island arcs), and

text: continental arc

text: s such as the

text: Cascade Volcanic Arc

text: , that form along the coast of continents. Island arcs are produced by the subduction of oceanic lithosphere beneath another oceanic lithosphere (ocean-ocean subduction) while continental arcs formed during subduction of oceanic lithosphere beneath a continental lithosphere (ocean-continent subduction).  An example of a volcanic arc having both island and continental arc sections is found behind the

text: Aleutian Trench

text: subduction zone in Alaska.

answers: NDQ_003351

answers: ocean-ocean subduction

answers: NDQ_003352

answers: subducts

answers: NDQ_003353

answers: subduction

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: Arc

answers: NDQ_003356

answers: subduct

answers: NDQ_003357

answers: subduction of oceanic lithosphere beneath another oceanic lithosphere

answers: NDQ_003358

answers: arc

answers: NDQ_003359

answers: subduction

answers: NDQ_003360

answers: continental arcs

answers: NDQ_003362

answers: Mount Fuji lie at approximately one hundred kilometres from the trench in arcuate chains

answers: NDQ_003363

answers: subduction zones

answers: NDQ_003371

answers: What kind of arcs are generally observed on Earth

answers: NDQ_003373

answers: subduction

answers: NDQ_003376

answers: not enough information

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What kind of force applied to rock is a stress?

answers: NDQ_003381

answers: What kind of arcs are generally observed on Earth?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: subduction zones

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: unanswerable

answers: NDQ_003389

answers: subduction

answers: NDQ_003390

answers: subduction zone

answers: NDQ_003391

answers: subduction zone

answers: NDQ_003392

answers: subduction zone

answers: NDQ_003393

answers: subduction zone

answers: NDQ_003394

answers: Arcuate

answers: NDQ_003395

answers: subduction zone

answers: NDQ_003396

answers: subduction zone

answers: NDQ_003351

answers: (ocean-ocean subduction)

answers: NDQ_003352

answers: continental arcs

answers: NDQ_003353

answers: subduction

answers: NDQ_003354

answers: Volcanoes that occur above subduction zones,

answers: NDQ_003355

answers: volcanic arc.

answers: NDQ_003356

answers: volcanic arc.

answers: NDQ_003357

answers: subduction

answers: NDQ_003358

answers: volcanic arc.

answers: NDQ_003359

answers: subduction

answers: NDQ_003360

answers: subduction zones,

answers: NDQ_003362

answers: one hundred kilometres

answers: NDQ_003363

answers: subduction zones,

answers: NDQ_003371

answers: Volcanoes that occur above subduction zones,

answers: NDQ_003373

answers: Volcanoes

answers: NDQ_003376

answers: subduction of oceanic lithosphere

answers: NDQ_003378

answers: volcanic arc.

answers: NDQ_003379

answers: continental arcs

answers: NDQ_003380

answers: volcanic arc.

answers: NDQ_003381

answers: continental arcs

answers: NDQ_003382

answers: Volcanoes that occur above subduction zones,

answers: NDQ_003383

answers: arcuate chains,

answers: NDQ_003384

answers: arcuate chains,

answers: NDQ_003385

answers: volcanic arc.

answers: NDQ_003386

answers: Volcanoes that occur above subduction zones,

answers: NDQ_003387

answers: continental arcs

answers: NDQ_003388

answers: continental arcs

answers: NDQ_003389

answers: subduction

answers: NDQ_003390

answers: subduction zones,

answers: NDQ_003391

answers: volcanic arc.

answers: NDQ_003392

answers: volcanic arc.

answers: NDQ_003393

answers: volcanic arc.

answers: NDQ_003394

answers: volcanic arc.

answers: NDQ_003395

answers: arcuate chains,

answers: NDQ_003396

answers: (ocean-ocean subduction)

text: Tallulah Dome is a rock formation caused by the double folding of the Earth's crust during the formation of Pangaea, about 500 to 250 million years ago. The dome is made up of mostly quartzite along with schist.

text: Tallulah Dome is a rock formation caused by the double

text: folding

text: of the Earth's

text: crust

text: during the formation of

text: Pangaea

text: , about 500 to 250 million years ago. The dome is made up of mostly

text: quartzite

text: along with

text: schist

answers: NDQ_003351

answers: double folding

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: folding

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fold that bends downward

answers: NDQ_003356

answers: fold

answers: NDQ_003357

answers: quartzite and schist are types of

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: folds

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: The San Andreas fault is a fault in the Earth's crust.

answers: NDQ_003363

answers: Pangaea

answers: NDQ_003371

answers: Which of the following is not a type of rock formation: Pangaea?

answers: NDQ_003373

answers: Why is the dome made up of mostly quartzite along with schist?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: what is the last word in the passage?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What is the result of the double folding of Earth's crust?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not a type of fold: syncline, dome or schist?

answers: NDQ_003385

answers: what is the last word in the passage?

answers: NDQ_003386

answers: It's impossible to say

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: normal faults, Pangaea, or schist?

answers: NDQ_003388

answers: Which of the following is not a result of shear stress: strike-slip faults, quartzite, or schist?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: schist

answers: NDQ_003391

answers: schist

answers: NDQ_003392

answers: a fault

answers: NDQ_003393

answers: schist

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: unanswerable

answers: NDQ_003396

answers: vertical fault

answers: NDQ_003351

answers: double folding

answers: NDQ_003352

answers: double folding

answers: NDQ_003353

answers: double folding of the Earth's crust

answers: NDQ_003354

answers: Tallulah Dome

answers: NDQ_003355

answers: double folding

answers: NDQ_003356

answers: double folding

answers: NDQ_003357

answers: double folding

answers: NDQ_003358

answers: Tallulah Dome

answers: NDQ_003359

answers: double folding

answers: NDQ_003360

answers: double folding of the Earth's crust

answers: NDQ_003362

answers: double folding of the Earth's crust

answers: NDQ_003363

answers: Pangaea,

answers: NDQ_003371

answers: Tallulah Dome

answers: NDQ_003373

answers: double folding of the Earth's crust

answers: NDQ_003376

answers: double folding of the Earth's crust

answers: NDQ_003378

answers: double folding of the Earth's crust

answers: NDQ_003379

answers: double folding of the Earth's crust

answers: NDQ_003380

answers: double folding

answers: NDQ_003381

answers: double folding

answers: NDQ_003382

answers: double folding

answers: NDQ_003383

answers: double folding

answers: NDQ_003384

answers: double folding

answers: NDQ_003385

answers: double folding of the Earth's crust

answers: NDQ_003386

answers: double folding of the Earth's crust

answers: NDQ_003387

answers: double folding of the Earth's crust

answers: NDQ_003388

answers: double folding of the Earth's crust

answers: NDQ_003389

answers: double folding

answers: NDQ_003390

answers: double folding

answers: NDQ_003391

answers: Tallulah Dome

answers: NDQ_003392

answers: double folding

answers: NDQ_003393

answers: Tallulah Dome

answers: NDQ_003394

answers: double folding of the Earth's crust

answers: NDQ_003395

answers: double folding of the Earth's crust

answers: NDQ_003396

answers: double folding of the Earth's crust

text: In 1953, geologist Thomas Dibblee astounded the scientific establishment with his conclusion that hundreds of miles of lateral movement could occur along the fault. A project called the San Andreas Fault Observatory at Depth (SAFOD) near Parkfield, Monterey County, is drilling into the fault to improve prediction and recording of future earthquakes.

text: In 1953, geologist

text: Thomas Dibblee

text: astounded the scientific establishment with his conclusion that hundreds of miles of lateral movement could occur along the fault. A project called the

text: San Andreas Fault Observatory at Depth (SAFOD)

text: near

text: Parkfield

text: Monterey County

text: , is drilling into the fault to improve prediction and recording of future earthquakes.

answers: NDQ_003351

answers: lateral movement

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: lateral movement

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: lateral movement

answers: NDQ_003356

answers: lateral movement

answers: NDQ_003357

answers: lateral movement could occur along the fault

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: lateral movement

answers: NDQ_003360

answers: faults

answers: NDQ_003362

answers: hundreds of miles of lateral movement could occur along the fault

answers: NDQ_003363

answers: San Andreas Fault

answers: NDQ_003371

answers: What is the San Andreas Fault Observatory at Depth?

answers: NDQ_003373

answers: How would you describe Thomas Dibblee?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: what is the last word in the passage?

answers: NDQ_003379

answers: Which of the following is not a type of strike-slip fault?

answers: NDQ_003380

answers: Which of the following is not an example of lateral movement?

answers: NDQ_003381

answers: What is the purpose of drilling into the fault?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not a type of fold that arches upward?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: yes

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: San Andreas Fault Observatory at Depth (SAFOD) near Parkfield, Monterey County, or earthquakes?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip, strike-slip, or strike-slip?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: lateral movement

answers: NDQ_003391

answers: lateral movement

answers: NDQ_003392

answers: lateral movement

answers: NDQ_003393

answers: lateral movement

answers: NDQ_003394

answers: lateral movement

answers: NDQ_003395

answers: unanswerable

answers: NDQ_003396

answers: lateral movement

answers: NDQ_003351

answers: lateral movement

answers: NDQ_003352

answers: lateral movement

answers: NDQ_003353

answers: lateral movement

answers: NDQ_003354

answers: San Andreas Fault Observatory at Depth

answers: NDQ_003355

answers: lateral movement

answers: NDQ_003356

answers: lateral movement

answers: NDQ_003357

answers: lateral movement

answers: NDQ_003358

answers: lateral movement could occur along the fault.

answers: NDQ_003359

answers: lateral movement

answers: NDQ_003360

answers: San Andreas Fault

answers: NDQ_003362

answers: hundreds of miles of lateral movement

answers: NDQ_003363

answers: San Andreas

answers: NDQ_003371

answers: hundreds of miles of lateral movement

answers: NDQ_003373

answers: San Andreas Fault Observatory at Depth

answers: NDQ_003376

answers: lateral movement

answers: NDQ_003378

answers: lateral movement

answers: NDQ_003379

answers: San Andreas Fault Observatory at Depth

answers: NDQ_003380

answers: lateral movement

answers: NDQ_003381

answers: lateral movement

answers: NDQ_003382

answers: lateral movement

answers: NDQ_003383

answers: lateral movement

answers: NDQ_003384

answers: San Andreas Fault Observatory at Depth

answers: NDQ_003385

answers: Fault Observatory at Depth

answers: NDQ_003386

answers: lateral movement

answers: NDQ_003387

answers: lateral movement

answers: NDQ_003388

answers: San Andreas Fault Observatory at Depth

answers: NDQ_003389

answers: lateral movement

answers: NDQ_003390

answers: San Andreas Fault

answers: NDQ_003391

answers: Depth

answers: NDQ_003392

answers: San Andreas Fault

answers: NDQ_003393

answers: San Andreas Fault Observatory at Depth

answers: NDQ_003394

answers: San Andreas Fault

answers: NDQ_003395

answers: San Andreas Fault

answers: NDQ_003396

answers: San Andreas Fault

text: Fionavar has many similarities to Tolkien's Middle-earth, and seems to be directly influenced by it (perhaps not surprising, since Kay worked with Christopher Tolkien to edit The Silmarillion and prepare it for publication). The map of Fionavar shows the northwestern part of the continent and its western coasts, bordered by an ocean, like most of the Middle-earth maps drawn by Tolkien, especially of Beleriand. Beyond the western sea lies a place where the Lios Alfar (Elves) go when they want to abandon the world, similar to Tolkien's Valinor.

text: Fionavar has many similarities to Tolkien's

text: Middle-earth

text: , and seems to be directly influenced by it (perhaps not surprising, since Kay worked with

text: Christopher Tolkien

text: to edit

text: The Silmarillion

text: and prepare it for publication). The map of Fionavar shows the northwestern part of the continent and its western coasts, bordered by an ocean, like most of the Middle-earth maps drawn by Tolkien, especially of

text: Beleriand

text: . Beyond the western sea lies a place where the Lios Alfar (Elves) go when they want to abandon the world, similar to Tolkien's

text: Valinor

answers: NDQ_003351

answers: oceanic

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: unanswerable

answers: NDQ_003356

answers: swell

answers: NDQ_003357

answers: Lios Alfar (Elves) go when they want to abandon the world

answers: NDQ_003358

answers: coast

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: continental plates

answers: NDQ_003362

answers: Tolkien's Middle-earth

answers: NDQ_003363

answers: Middle-earth

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: How would you describe Tolkien?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: What is the amount the ground moves in an earthquake?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: Which of the following is not a type of stress: applied force, rock, or stress?

answers: NDQ_003381

answers: What kind of stress does the map of Fionavar show?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: movement of rock at faults

answers: NDQ_003387

answers: What does Kay work with Christopher Tolkien to edit The Silmarillion?

answers: NDQ_003388

answers: What type of stress is shear stress?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: Fionavar

answers: NDQ_003391

answers: unanswerable

answers: NDQ_003392

answers: Tolkien's Middle-earth

answers: NDQ_003393

answers: dip-slip fault plane

answers: NDQ_003394

answers: NDQ_003395

answers: a fault with a vertical fault plane

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: ocean,

answers: NDQ_003352

answers: ocean,

answers: NDQ_003353

answers: ocean,

answers: NDQ_003354

answers: Fionavar has many similarities to Tolkien's

answers: NDQ_003355

answers: western coasts,

answers: NDQ_003356

answers: ocean,

answers: NDQ_003357

answers: Kay worked with Christopher Tolkien

answers: NDQ_003358

answers: sea

answers: NDQ_003359

answers: ocean,

answers: NDQ_003360

answers: Fionavar

answers: NDQ_003362

answers: (Elves) go when they want to abandon the world,

answers: NDQ_003363

answers: Fionavar

answers: NDQ_003371

answers: Fionavar

answers: NDQ_003373

answers: Fionavar has many similarities to Tolkien's

answers: NDQ_003376

answers: ocean,

answers: NDQ_003378

answers: ocean,

answers: NDQ_003379

answers: ocean,

answers: NDQ_003380

answers: ocean,

answers: NDQ_003381

answers: ocean,

answers: NDQ_003382

answers: ocean,

answers: NDQ_003383

answers: Fionavar has many similarities to Tolkien's

answers: NDQ_003384

answers: ocean,

answers: NDQ_003385

answers: Fionavar

answers: NDQ_003386

answers: Fionavar

answers: NDQ_003387

answers: ocean,

answers: NDQ_003388

answers: Fionavar has many similarities to Tolkien's

answers: NDQ_003389

answers: ocean,

answers: NDQ_003390

answers: Fionavar

answers: NDQ_003391

answers: ocean,

answers: NDQ_003392

answers: Fionavar

answers: NDQ_003393

answers: ocean,

answers: NDQ_003394

answers: ocean,

answers: NDQ_003395

answers: Fionavar

answers: NDQ_003396

answers: ocean,

text: Areas of strike-slip tectonics are associated with:

text: Areas of strike-slip tectonics are associated with:

answers: NDQ_003351

answers: lateral

answers: NDQ_003352

answers: is likely to crack

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: the Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: strike-slip

answers: NDQ_003356

answers: change shape

answers: NDQ_003357

answers: strike-slip tectonics is associated with

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: erodes away.

answers: NDQ_003360

answers: fault lines

answers: NDQ_003362

answers: the San Andreas fault is not a fault.

answers: NDQ_003363

answers: tectonic plate boundaries

answers: NDQ_003371

answers: tectonic plates

answers: NDQ_003373

answers: tectonics

answers: NDQ_003376

answers: tectonics

answers: NDQ_003378

answers: earthquakes

answers: NDQ_003379

answers: tectonic plate movement

answers: NDQ_003380

answers: tectonic plate movement

answers: NDQ_003381

answers: constricting stress

answers: NDQ_003382

answers: convergent plates

answers: NDQ_003383

answers: tectonics

answers: NDQ_003384

answers: tectonic plate movement

answers: NDQ_003385

answers: faults are clustered

answers: NDQ_003386

answers: earthquakes

answers: NDQ_003387

answers: tectonics

answers: NDQ_003388

answers: earthquakes

answers: NDQ_003389

answers: earthquakes

answers: NDQ_003390

answers: landslides

answers: NDQ_003391

answers: block of rock

answers: NDQ_003392

answers: tectonic plate movement

answers: NDQ_003393

answers: block of rock

answers: NDQ_003394

answers: lateral faults

answers: NDQ_003395

answers: tectonic plates

answers: NDQ_003396

answers: tectonic plates

answers: NDQ_003351

answers: strike-slip

answers: NDQ_003352

answers: strike-slip tectonics

answers: NDQ_003353

answers: strike-slip tectonics

answers: NDQ_003354

answers: Areas of strike-slip tectonics

answers: NDQ_003355

answers: strike-slip tectonics

answers: NDQ_003356

answers: strike-slip tectonics

answers: NDQ_003357

answers: strike-slip tectonics

answers: NDQ_003358

answers: strike-slip tectonics

answers: NDQ_003359

answers: strike-slip tectonics

answers: NDQ_003360

answers: strike-slip tectonics

answers: NDQ_003362

answers: strike-slip tectonics

answers: NDQ_003363

answers: strike-slip tectonics

answers: NDQ_003371

answers: strike-slip tectonics

answers: NDQ_003373

answers: strike-slip tectonics

answers: NDQ_003376

answers: strike-slip tectonics

answers: NDQ_003378

answers: strike-slip tectonics

answers: NDQ_003379

answers: Areas of strike-slip tectonics

answers: NDQ_003380

answers: strike-slip tectonics

answers: NDQ_003381

answers: strike-slip tectonics

answers: NDQ_003382

answers: strike-slip tectonics

answers: NDQ_003383

answers: strike-slip tectonics

answers: NDQ_003384

answers: strike-slip tectonics

answers: NDQ_003385

answers: strike-slip tectonics

answers: NDQ_003386

answers: strike-slip tectonics

answers: NDQ_003387

answers: strike-slip tectonics

answers: NDQ_003388

answers: strike-slip tectonics

answers: NDQ_003389

answers: strike-slip tectonics

answers: NDQ_003390

answers: strike-slip tectonics

answers: NDQ_003391

answers: strike-slip tectonics

answers: NDQ_003392

answers: strike-slip tectonics

answers: NDQ_003393

answers: strike-slip tectonics

answers: NDQ_003394

answers: strike-slip tectonics

answers: NDQ_003395

answers: strike-slip tectonics

answers: NDQ_003396

answers: strike-slip tectonics

text: About 50 million years ago the Siletzia terrane, being borne to the northeast by the subducting plate, refused to be subducted. It ran it into the edge of the continent and embayed the overlying crust, bending the section of the Wrangellia—Pacific Rim contact now known as the San Juan fault to its current easterly orientation.  This also initiated the oblique left-lateral Devils Mountain fault, including the section now known as the Leech River fault, and its right-lateral extension, the Darrington fault, that strikes southward from the town of Darrington to converge with the right-lateral strike-slip Straight Creek Fault at the OWL (see map). About 42 million years ago this northeastward force rotated to a northerly direction which, striking the SWIF more obliquely, caused the strike-slip movement that offset the LRF past Victoria.

text: About 50 million years ago the

text: Siletzia

text: terrane, being borne to the northeast by the subducting plate, refused to be subducted. It ran it into the edge of the continent and embayed the overlying crust, bending the section of the Wrangellia—Pacific Rim contact now known as the San Juan fault to its current easterly orientation.  This also initiated the oblique left-lateral Devils Mountain fault, including the section now known as the Leech River fault, and its right-lateral extension, the Darrington fault, that strikes southward from the town of

text: Darrington

text: to converge with the right-lateral strike-slip

text: Straight Creek Fault

text: at the OWL (see map). About 42 million years ago this northeastward force rotated to a northerly direction which, striking the SWIF more obliquely, caused the strike-slip movement that offset the LRF past Victoria.

answers: NDQ_003351

answers: strike-slip

answers: NDQ_003352

answers: is more likely to crack

answers: NDQ_003353

answers: strike-slip

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: San Juan fault

answers: NDQ_003356

answers: strike southward

answers: NDQ_003357

answers: strike-slip movement that offset the LRF past Victoria

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: strike-slip

answers: NDQ_003360

answers: subducting plates

answers: NDQ_003362

answers: the San Juan fault to its current easterly orientation

answers: NDQ_003363

answers: About 42 million years ago this northeastward force rotated to a northerly direction

answers: NDQ_003371

answers: Which of the following is not a fault: Leech River fault, Devils Mountain fault, or the Darrington fault?

answers: NDQ_003373

answers: How would you describe the Siletzia terrane?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: strike-slip

answers: NDQ_003379

answers: no

answers: NDQ_003380

answers: What type of force applied to rock is a stress?

answers: NDQ_003381

answers: What is the San Juan fault?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the San Juan fault?

answers: NDQ_003384

answers: What type of fold is the San Juan fault?

answers: NDQ_003385

answers: Fault zone

answers: NDQ_003386

answers: What is the San Juan fault?

answers: NDQ_003387

answers: What type of stress is the San Juan fault caused by?

answers: NDQ_003388

answers: What type of stress is shear stress?

answers: NDQ_003389

answers: What is the San Juan fault?

answers: NDQ_003390

answers: Straight Creek Fault

answers: NDQ_003391

answers: terrane

answers: NDQ_003392

answers: right-lateral strike-slip

answers: NDQ_003393

answers: Siletzia terrane

answers: NDQ_003394

answers: oblique left-lateral

answers: NDQ_003395

answers: Straight Creek Fault

answers: NDQ_003396

answers: oblique left-lateral

answers: NDQ_003351

answers: strike-slip

answers: NDQ_003352

answers: bending

answers: NDQ_003353

answers: bending

answers: NDQ_003354

answers: About 50 million years ago the Siletzia terrane,

answers: NDQ_003355

answers: San Juan fault

answers: NDQ_003356

answers: strike-slip

answers: NDQ_003357

answers: right-lateral strike-slip

answers: NDQ_003358

answers: strike-slip Straight Creek Fault

answers: NDQ_003359

answers: right-lateral strike-slip Straight Creek Fault

answers: NDQ_003360

answers: subducting plate,

answers: NDQ_003362

answers: San Juan fault

answers: NDQ_003363

answers: Wrangellia—Pacific Rim

answers: NDQ_003371

answers: San Juan fault

answers: NDQ_003373

answers: About 50 million years ago the Siletzia terrane,

answers: NDQ_003376

answers: subducting plate, refused to be subducted.

answers: NDQ_003378

answers: strike-slip

answers: NDQ_003379

answers: right-lateral strike-slip Straight Creek Fault

answers: NDQ_003380

answers: strike-slip

answers: NDQ_003381

answers: bending

answers: NDQ_003382

answers: right-lateral strike-slip Straight Creek Fault

answers: NDQ_003383

answers: San Juan fault

answers: NDQ_003384

answers: oblique left-lateral Devils Mountain fault,

answers: NDQ_003385

answers: San Juan fault

answers: NDQ_003386

answers: strike-slip

answers: NDQ_003387

answers: right-lateral strike-slip Straight Creek Fault

answers: NDQ_003388

answers: strike-slip

answers: NDQ_003389

answers: bending

answers: NDQ_003390

answers: Straight Creek Fault

answers: NDQ_003391

answers: Siletzia terrane,

answers: NDQ_003392

answers: Straight Creek Fault

answers: NDQ_003393

answers: strike-slip Straight Creek Fault

answers: NDQ_003394

answers: oblique left-lateral

answers: NDQ_003395

answers: Straight Creek Fault

answers: NDQ_003396

answers: oblique left-lateral Devils Mountain fault,

text: The structure of the Earth is a rigid outer crust that is composed of thicker continental crust and thinner oceanic crust, solid but plastically flowing mantle, a liquid outer core, and a solid inner core. The fluidity of a material is proportional to temperature; thus, the solid mantle can still flow on long time scales, as a function of its temperature and therefore as a function of the flow of Earth's internal heat. The mantle convects in response to heat escaping from Earth's interior, with hotter and more buoyant mantle rising and cooler, and therefore denser, mantle sinking. This convective flow of the mantle drives the movement of Earth's lithospheric plates; thus, an additional reservoir of heat in the lower mantle is critical for the operation of plate tectonics and one possible source is an enrichment of radioactive elements in the lower mantle.

text: The

text: structure of the Earth

text: is a rigid outer

text: crust

text: that is composed of thicker

text: continental crust

text: and thinner

text: oceanic crust

text: , solid but plastically flowing

text: mantle

text: , a liquid

text: outer core

text: , and a solid

text: inner core

text: . The

text: fluidity

text: of a material is proportional to temperature; thus, the solid mantle can still flow on long time scales, as a function of its temperature and therefore as a function of the flow of Earth's internal heat. The

text: mantle convects

text: in response to heat escaping from Earth's interior, with hotter and more buoyant mantle rising and cooler, and therefore denser, mantle sinking. This convective flow of the mantle drives the movement of Earth's

text: lithospheric plates

text: ; thus, an additional reservoir of heat in the lower mantle is critical for the operation of plate tectonics and one possible source is an enrichment of radioactive elements in the lower mantle.

answers: NDQ_003351

answers: convective

answers: NDQ_003352

answers: denser

answers: NDQ_003353

answers: heat to escape

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: continental fold

answers: NDQ_003356

answers: sink

answers: NDQ_003357

answers: convective flow of the mantle drives the movement of Earth's lithospheric plates

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: continental plates

answers: NDQ_003362

answers: the solid mantle can still flow on long time scales

answers: NDQ_003363

answers: continental crust

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: what is the second to last word in the passage?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What is the fluidity of a material?

answers: NDQ_003381

answers: What does the solid mantle can still flow on long time scales?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What type of fold is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: plate tectonics

answers: NDQ_003387

answers: What is the fluidity of a material proportional to?

answers: NDQ_003388

answers: What does the solid mantle convect?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: tectonics

answers: NDQ_003391

answers: continental crust

answers: NDQ_003392

answers: tectonics

answers: NDQ_003393

answers: continental crust

answers: NDQ_003394

answers: isosceles

answers: NDQ_003395

answers: plate tectonics

answers: NDQ_003396

answers: horizontal

answers: NDQ_003351

answers: heat escaping from Earth's interior,

answers: NDQ_003352

answers: denser, mantle sinking.

answers: NDQ_003353

answers: denser, mantle sinking.

answers: NDQ_003354

answers: the solid mantle can still flow on long time scales,

answers: NDQ_003355

answers: plates;

answers: NDQ_003356

answers: flowing mantle,

answers: NDQ_003357

answers: hotter and more buoyant mantle rising and cooler,

answers: NDQ_003358

answers: lithospheric plates;

answers: NDQ_003359

answers: temperature;

answers: NDQ_003360

answers: heat

answers: NDQ_003362

answers: the solid mantle can still flow on long time scales,

answers: NDQ_003363

answers: heat escaping from Earth's interior,

answers: NDQ_003371

answers: thicker continental crust and thinner oceanic crust,

answers: NDQ_003373

answers: denser, mantle sinking.

answers: NDQ_003376

answers: heat escaping from Earth's interior,

answers: NDQ_003378

answers: The mantle convects

answers: NDQ_003379

answers: Earth's internal heat.

answers: NDQ_003380

answers: The fluidity of a material is proportional to temperature;

answers: NDQ_003381

answers: heat escaping from Earth's interior,

answers: NDQ_003382

answers: lithospheric plates;

answers: NDQ_003383

answers: heat escaping from Earth's interior,

answers: NDQ_003384

answers: hotter and more buoyant mantle

answers: NDQ_003385

answers: The structure of the Earth

answers: NDQ_003386

answers: Earth's lithospheric plates;

answers: NDQ_003387

answers: heat escaping from Earth's interior,

answers: NDQ_003388

answers: heat escaping from Earth's interior,

answers: NDQ_003389

answers: lithospheric plates;

answers: NDQ_003390

answers: plate tectonics

answers: NDQ_003391

answers: mantle,

answers: NDQ_003392

answers: thicker continental crust and thinner oceanic crust,

answers: NDQ_003393

answers: thicker continental crust and thinner oceanic crust,

answers: NDQ_003394

answers: Earth

answers: NDQ_003395

answers: Earth

answers: NDQ_003396

answers: oceanic crust,

text: The Mountain States Telephone Building, also known as Telephone Building is a building in Denver, Colorado, United States that served as the headquarters of the Mountain States Telephone & Telegraph Company, later known as Mountain Bell.  Constructed in a variant of the Gothic Revival style named "Modern American Perpendicular Gothic," the building was designed by local architect William N. Bowman.  The new building, completed in 1929, was built to provide dial telephone service for the first time in Denver.

text: The Mountain States Telephone Building, also known as Telephone Building is a building in

text: Denver

text: Colorado

text: United States

text: that served as the headquarters of the Mountain States Telephone & Telegraph Company, later known as

text: Mountain Bell

text: .  Constructed in a variant of the

text: Gothic Revival

text: style named "Modern American Perpendicular Gothic," the building was designed by local architect

text: William N. Bowman

text: .  The new building, completed in 1929, was built to provide

text: dial telephone service

text: for the first time in Denver.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation is a formation

answers: NDQ_003355

answers: fold that bends downward

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: Mountain States Telephone & Telegraph Company was known as what?

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: continental plates

answers: NDQ_003362

answers: The Mountain States Telephone Building, also known as Telephone Building is a building in Denver, Colorado

answers: NDQ_003363

answers: the same time

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: How would you describe the Mountain States Telephone Building?

answers: NDQ_003376

answers: What is caused by compressive forces?

answers: NDQ_003378

answers: What is the amount the ground moves in an earthquake?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: How would you describe the Mountain States Telephone Building?

answers: NDQ_003381

answers: How does the Mountain States Telephone Building deform?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the Mountain States Telephone Building?

answers: NDQ_003384

answers: What type of fold is the Mountain States Telephone Building?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: What is the cause of earthquakes?

answers: NDQ_003387

answers: What type of stress is caused by normal faults?

answers: NDQ_003388

answers: What is the cause of strike-slip faults?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: mountain

answers: NDQ_003392

answers: unanswerable

answers: NDQ_003393

answers: mountain

answers: NDQ_003394

answers: NDQ_003395

answers: fault with a vertical fault plane

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: "Modern American Perpendicular Gothic,"

answers: NDQ_003352

answers: "Modern American Perpendicular Gothic,"

answers: NDQ_003353

answers: "Modern American Perpendicular Gothic,"

answers: NDQ_003354

answers: The Mountain States Telephone Building,

answers: NDQ_003355

answers: Perpendicular

answers: NDQ_003356

answers: Gothic Revival

answers: NDQ_003357

answers: The new building, completed in 1929,

answers: NDQ_003358

answers: Mountain Bell.

answers: NDQ_003359

answers: The Mountain States Telephone Building,

answers: NDQ_003360

answers: Colorado, United States

answers: NDQ_003362

answers: The Mountain States Telephone Building,

answers: NDQ_003363

answers: Colorado, United States

answers: NDQ_003371

answers: The Mountain States Telephone Building,

answers: NDQ_003373

answers: The Mountain States Telephone Building,

answers: NDQ_003376

answers: "Modern American Perpendicular Gothic,"

answers: NDQ_003378

answers: "Modern American Perpendicular Gothic,"

answers: NDQ_003379

answers: "Modern American Perpendicular Gothic,"

answers: NDQ_003380

answers: The Mountain States Telephone Building,

answers: NDQ_003381

answers: "Modern American Perpendicular Gothic,"

answers: NDQ_003382

answers: "Modern American Perpendicular Gothic,"

answers: NDQ_003383

answers: "Modern American Perpendicular Gothic,"

answers: NDQ_003384

answers: "Modern American Perpendicular Gothic,"

answers: NDQ_003385

answers: The Mountain States Telephone Building,

answers: NDQ_003386

answers: The Mountain States Telephone Building,

answers: NDQ_003387

answers: "Modern American Perpendicular Gothic,"

answers: NDQ_003388

answers: "Modern American Perpendicular Gothic,"

answers: NDQ_003389

answers: "Modern American Perpendicular Gothic,"

answers: NDQ_003390

answers: Gothic Revival style named "Modern American Perpendicular

answers: NDQ_003391

answers: Perpendicular Gothic,"

answers: NDQ_003392

answers: Perpendicular

answers: NDQ_003393

answers: Perpendicular Gothic,"

answers: NDQ_003394

answers: Perpendicular Gothic,"

answers: NDQ_003395

answers: Perpendicular Gothic,"

answers: NDQ_003396

answers: Perpendicular Gothic,"

text: The physical stress of beating egg whites can create a foam.  Two types of physical stress are caused by beating them with a whisk, the first of which occurs as the whisk drags the liquid through itself, creating a force that unfolds the protein molecules. This process is called denaturation. The second stress comes from the mixing of air into the whites, which causes the proteins to come out of their natural state.  These denatured proteins gather together where the air and water meet and create multiple bonds with the other unraveled proteins, and thus become a foam, holding the incorporated air in place. This is because the proteins consist of amino acids; some are hydrophilic (attracted to water) and some are hydrophobic (repelled by water). This process is called coagulation.

text: The physical stress of beating egg whites can create a foam.  Two types of physical stress are caused by beating them with a whisk, the first of which occurs as the whisk drags the liquid through itself, creating a force that unfolds the protein molecules. This process is called

text: denaturation

text: . The second stress comes from the mixing of air into the whites, which causes the proteins to come out of their natural state.  These denatured proteins gather together where the air and water meet and create multiple bonds with the other unraveled proteins, and thus become a foam, holding the incorporated air in place. This is because the proteins consist of amino acids; some are hydrophilic (attracted to water) and some are hydrophobic (repelled by water). This process is called

text: coagulation

answers: NDQ_003351

answers: denaturation

answers: NDQ_003352

answers: denaturation

answers: NDQ_003353

answers: denaturation

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: swell

answers: NDQ_003357

answers: denaturation occurs as the whisk drags the liquid

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: the San Andreas fault is caused by a volcano

answers: NDQ_003363

answers: the same time

answers: NDQ_003371

answers: Which of the following is not a type of physical stress?

answers: NDQ_003373

answers: How would you describe compressive stresses?

answers: NDQ_003376

answers: basin-and-range

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: The dip of the fault plane is vertical

answers: NDQ_003380

answers: How would you describe a force applied to rock?

answers: NDQ_003381

answers: What is the result of confining stress?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: what is the first of which occurs as the whisk drags the liquid through itself

answers: NDQ_003385

answers: Fault zones are areas where faults are clustered.

answers: NDQ_003386

answers: Which of the following is not an example of movement of rock at faults?

answers: NDQ_003387

answers: Which of the following is not a type of physical stress?

answers: NDQ_003388

answers: Which of the following is not a type of stress: shear stress, denaturation, or coagulation?

answers: NDQ_003389

answers: denaturation

answers: NDQ_003390

answers: footwall

answers: NDQ_003391

answers: dip-slip fault plane

answers: NDQ_003392

answers: a hanging wall

answers: NDQ_003393

answers: dip-slip fault plane

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: a vertical fault plane

answers: NDQ_003396

answers: horizontal

answers: NDQ_003351

answers: coagulation.

answers: NDQ_003352

answers: coagulation.

answers: NDQ_003353

answers: coagulation.

answers: NDQ_003354

answers: coagulation.

answers: NDQ_003355

answers: coagulation.

answers: NDQ_003356

answers: foam.

answers: NDQ_003357

answers: coagulation.

answers: NDQ_003358

answers: coagulation.

answers: NDQ_003359

answers: The physical stress of beating egg whites can create a foam.

answers: NDQ_003360

answers: physical stress

answers: NDQ_003362

answers: The physical stress of beating egg whites can create a foam.

answers: NDQ_003363

answers: coagulation.

answers: NDQ_003371

answers: coagulation.

answers: NDQ_003373

answers: coagulation.

answers: NDQ_003376

answers: coagulation.

answers: NDQ_003378

answers: coagulation.

answers: NDQ_003379

answers: coagulation.

answers: NDQ_003380

answers: The physical stress of beating egg whites

answers: NDQ_003381

answers: coagulation.

answers: NDQ_003382

answers: coagulation.

answers: NDQ_003383

answers: coagulation.

answers: NDQ_003384

answers: coagulation.

answers: NDQ_003385

answers: denaturation.

answers: NDQ_003386

answers: denaturation.

answers: NDQ_003387

answers: coagulation.

answers: NDQ_003388

answers: coagulation.

answers: NDQ_003389

answers: coagulation.

answers: NDQ_003390

answers: coagulation.

answers: NDQ_003391

answers: coagulation.

answers: NDQ_003392

answers: coagulation.

answers: NDQ_003393

answers: coagulation.

answers: NDQ_003394

answers: coagulation.

answers: NDQ_003395

answers: denaturation.

answers: NDQ_003396

answers: coagulation.

text: A mountain hut (also known as alpine hut, mountain shelter, mountain refuge, mountain lodge, and mountain hostel) is a building located high in the mountains, generally accessible only by foot, intended to provide food and shelter to mountaineers, climbers and hikers. Mountain huts are usually operated by an Alpine Club or some organisation dedicated to hiking or mountain recreation.

text: A mountain hut (also known as alpine hut, mountain shelter, mountain refuge, mountain lodge, and mountain hostel) is a building located high in the mountains, generally accessible only by foot, intended to provide food and shelter to

text: mountaineers

text: climbers

text: and

text: hiker

text: s. Mountain huts are usually operated by an

text: Alpine Club

text: or some organisation dedicated to hiking or mountain recreation.

answers: NDQ_003351

answers: mountain hut

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: mountain

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: mountain huts are usually operated by some organisation dedicated to hiking or mountain recreation

answers: NDQ_003358

answers: refuge

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: The San Andreas fault is not a mountain hut

answers: NDQ_003363

answers: the same time

answers: NDQ_003371

answers: What is an example of a thrust fault?

answers: NDQ_003373

answers: What is a mountain hut?

answers: NDQ_003376

answers: basin-and-range

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: The dip of the fault plane is vertical

answers: NDQ_003380

answers: What is a stress?

answers: NDQ_003381

answers: What is the purpose of mountain huts?

answers: NDQ_003382

answers: None of the above choices.

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: movement of rock at faults

answers: NDQ_003387

answers: Which of the following is not a cause of normal faults?

answers: NDQ_003388

answers: What kind of stress does shear stress cause?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: mountain hut

answers: NDQ_003391

answers: dip-slip fault

answers: NDQ_003392

answers: mountain hut

answers: NDQ_003393

answers: mountain hut

answers: NDQ_003394

answers: isobath

answers: NDQ_003395

answers: is a vertical fault plane

answers: NDQ_003396

answers: mountain hut

answers: NDQ_003351

answers: A mountain hut

answers: NDQ_003352

answers: A mountain hut

answers: NDQ_003353

answers: A mountain hut

answers: NDQ_003354

answers: A mountain hut

answers: NDQ_003355

answers: mountain hut

answers: NDQ_003356

answers: A mountain hut

answers: NDQ_003357

answers: A mountain hut

answers: NDQ_003358

answers: mountain hut

answers: NDQ_003359

answers: foot,

answers: NDQ_003360

answers: mountain hut

answers: NDQ_003362

answers: A mountain hut

answers: NDQ_003363

answers: mountain hut

answers: NDQ_003371

answers: mountain hut

answers: NDQ_003373

answers: mountain hut

answers: NDQ_003376

answers: A mountain hut

answers: NDQ_003378

answers: A mountain hut

answers: NDQ_003379

answers: Alpine Club or some organisation dedicated to hiking or mountain recreation.

answers: NDQ_003380

answers: A mountain hut

answers: NDQ_003381

answers: A mountain hut

answers: NDQ_003382

answers: A mountain hut

answers: NDQ_003383

answers: A mountain hut

answers: NDQ_003384

answers: mountain hut

answers: NDQ_003385

answers: mountain hut

answers: NDQ_003386

answers: A mountain hut

answers: NDQ_003387

answers: A mountain hut

answers: NDQ_003388

answers: A mountain hut

answers: NDQ_003389

answers: A mountain hut

answers: NDQ_003390

answers: mountain hut

answers: NDQ_003391

answers: mountain hut

answers: NDQ_003392

answers: mountain hut

answers: NDQ_003393

answers: mountain hut

answers: NDQ_003394

answers: A mountain hut

answers: NDQ_003395

answers: A mountain hut

answers: NDQ_003396

answers: A mountain hut (also known as alpine hut,

text: Strike-slip tectonics is concerned with the structures formed by, and the tectonic processes associated with, zones of lateral displacement within the crust or lithosphere.

text: Strike-slip tectonics is concerned with the structures formed by, and the

text: tectonic

text: processes associated with, zones of lateral displacement within the

text: crust

text: or

text: lithosphere

answers: NDQ_003351

answers: lateral displacement

answers: NDQ_003352

answers: erodes

answers: NDQ_003353

answers: lateral displacement

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: strike-slip

answers: NDQ_003356

answers: lateral displacement

answers: NDQ_003357

answers: zones of lateral displacement

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: tectonic plates

answers: NDQ_003362

answers: The San Andreas fault is not a tectonic fault.

answers: NDQ_003363

answers: zones of lateral displacement

answers: NDQ_003371

answers: What type of tectonics is strike-slip tectonics?

answers: NDQ_003373

answers: How would you describe a rock under compressive stresses?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: Which of the following is not an example of tectonic processes associated with zones of lateral displacement within the crust?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: what is the first word in the passage?

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: strike-slip tectonics or normal faults?

answers: NDQ_003388

answers: Which of the following is not a tectonic process associated with strike-slip faults?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: strike-slip

answers: NDQ_003391

answers: lithosphere

answers: NDQ_003392

answers: strike-slip

answers: NDQ_003393

answers: lithosphere

answers: NDQ_003394

answers: lateral displacement

answers: NDQ_003395

answers: lateral displacement

answers: NDQ_003396

answers: strike-slip

answers: NDQ_003351

answers: Strike-slip

answers: NDQ_003352

answers: lateral displacement

answers: NDQ_003353

answers: lateral displacement

answers: NDQ_003354

answers: Strike-slip tectonics

answers: NDQ_003355

answers: Strike-slip

answers: NDQ_003356

answers: lateral displacement

answers: NDQ_003357

answers: lateral displacement

answers: NDQ_003358

answers: Strike-slip tectonics

answers: NDQ_003359

answers: lateral displacement

answers: NDQ_003360

answers: Strike-slip tectonics

answers: NDQ_003362

answers: Strike-slip tectonics

answers: NDQ_003363

answers: Strike-slip tectonics

answers: NDQ_003371

answers: Strike-slip tectonics

answers: NDQ_003373

answers: Strike-slip tectonics

answers: NDQ_003376

answers: Strike-slip tectonics

answers: NDQ_003378

answers: lateral displacement

answers: NDQ_003379

answers: lateral displacement

answers: NDQ_003380

answers: lateral displacement

answers: NDQ_003381

answers: lateral displacement

answers: NDQ_003382

answers: Strike-slip tectonics

answers: NDQ_003383

answers: lateral displacement

answers: NDQ_003384

answers: Strike-slip tectonics

answers: NDQ_003385

answers: zones of lateral displacement

answers: NDQ_003386

answers: Strike-slip tectonics

answers: NDQ_003387

answers: Strike-slip tectonics

answers: NDQ_003388

answers: zones of lateral displacement

answers: NDQ_003389

answers: Strike-slip tectonics

answers: NDQ_003390

answers: Strike-slip tectonics

answers: NDQ_003391

answers: lithosphere.

answers: NDQ_003392

answers: Strike-slip tectonics

answers: NDQ_003393

answers: lithosphere.

answers: NDQ_003394

answers: lateral displacement

answers: NDQ_003395

answers: Strike-slip tectonics

answers: NDQ_003396

answers: Strike-slip tectonics

text: In the middle of the 20th century some geologists formed an idea about existing fault-fold systems in the earth's crust, in sediment cover, and this gave creekology a "scientific base".  Linear forms in earth landscape connect with fault tectonics, and some folds near faults can be reservoirs of hydrocarbons. The non-fold types of traps mark by lineation too (paleo-rivers formed on faults). Now some geologists mark probable gas-oil areas with the help of space image lineation interpreting. This activity can be defined as "new creekology".

text: In the middle of the 20th century some

text: geologist

text: s formed an idea about existing

text: fault-fold

text: systems in the

text: earth's crust

text: , in sediment cover, and this gave creekology a "scientific base".  Linear forms in earth landscape connect with fault

text: tectonics

text: , and some folds near faults can be reservoirs of

text: hydrocarbon

text: s. The non-fold types of traps mark by

text: lineation

text: too (paleo-rivers formed on faults). Now some geologists mark probable gas-oil areas with the help of space image lineation interpreting. This activity can be defined as "new creekology".

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: folds

answers: NDQ_003353

answers: faults

answers: NDQ_003354

answers: Toroweap Formation is a formation

answers: NDQ_003355

answers: fault

answers: NDQ_003356

answers: fold

answers: NDQ_003357

answers: folds near faults can be reservoirs of hydrocarbons

answers: NDQ_003358

answers: trap

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: faults

answers: NDQ_003362

answers: Paleo-rivers formed on faults

answers: NDQ_003363

answers: faults

answers: NDQ_003371

answers: Which of the following is not a type of trap: paleo-rivers formed on faults

answers: NDQ_003373

answers: How would you describe a rock that is deeply buried?

answers: NDQ_003376

answers: What is the non-fold types of traps mark by lineation too (paleo-rivers formed on faults)?

answers: NDQ_003378

answers: What can be defined as new creekology?

answers: NDQ_003379

answers: What is the dip of the fault plane in a strike-slip fault?

answers: NDQ_003380

answers: How would you describe the non-fold types of traps?

answers: NDQ_003381

answers: Which of the following is not a type of trap: Paleo-rivers, faults, or folds?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not a type of fold: fault-fold systems or synclines?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: Which of the following is not a cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not a cause of normal faults?

answers: NDQ_003388

answers: Which of the following is not a type of trap: Paleo-rivers, strike-slip, or non-fold?

answers: NDQ_003389

answers: It's impossible to say

answers: NDQ_003390

answers: Fault tectonics

answers: NDQ_003391

answers: traps

answers: NDQ_003392

answers: Fault tectonics

answers: NDQ_003393

answers: sediment cover

answers: NDQ_003394

answers: non-fold

answers: NDQ_003395

answers: fault tectonics

answers: NDQ_003396

answers: non-fold

answers: NDQ_003351

answers: fault-fold systems

answers: NDQ_003352

answers: folds

answers: NDQ_003353

answers: fault-fold systems

answers: NDQ_003354

answers: In the middle of the 20th century

answers: NDQ_003355

answers: traps

answers: NDQ_003356

answers: fault-fold systems

answers: NDQ_003357

answers: folds near faults can be reservoirs of hydrocarbons.

answers: NDQ_003358

answers: traps

answers: NDQ_003359

answers: fault-fold systems in the earth's crust,

answers: NDQ_003360

answers: fault tectonics,

answers: NDQ_003362

answers: some folds near faults can be reservoirs of hydrocarbons.

answers: NDQ_003363

answers: fault tectonics,

answers: NDQ_003371

answers: fault-fold systems

answers: NDQ_003373

answers: fault-fold systems

answers: NDQ_003376

answers: fault-fold systems

answers: NDQ_003378

answers: fault-fold systems

answers: NDQ_003379

answers: Linear forms in earth landscape connect with fault tectonics,

answers: NDQ_003380

answers: fault tectonics,

answers: NDQ_003381

answers: fault-fold systems

answers: NDQ_003382

answers: fault tectonics,

answers: NDQ_003383

answers: fault tectonics,

answers: NDQ_003384

answers: fault tectonics,

answers: NDQ_003385

answers: fault-fold systems

answers: NDQ_003386

answers: fault tectonics,

answers: NDQ_003387

answers: fault tectonics,

answers: NDQ_003388

answers: fault tectonics,

answers: NDQ_003389

answers: fault-fold systems

answers: NDQ_003390

answers: fault tectonics,

answers: NDQ_003391

answers: folds

answers: NDQ_003392

answers: fault tectonics,

answers: NDQ_003393

answers: folds

answers: NDQ_003394

answers: non-fold

answers: NDQ_003395

answers: fault tectonics,

answers: NDQ_003396

answers: fault tectonics,

text: When two tectonic plates collide, relatively denser oceanic crust will be subducted under relatively lighter continental crust. Because of the subduction process, the relatively cooler oceanic crust, along with water, is subducted to the asthenosphere, where pressures and temperatures are much higher than the surface of earth. Under such conditions, the downgoing plate releases volatiles such as HO and CO, which cause partial melting of the above asthenosphere. This process can create relatively buoyant magma, which subsequently forms a series of volcanoes at the surface along the subduction zone. There are some researchers who argue that refertilization of arc lithospheric mantle may also be an important process associated with arc magmatism. Because the subduction zone (which is also the plate boundary) is generally an arc-shape, geologists named those volcanoes volcanic arcs. A volcanic arc built on continental crust is called a continental arc; when built on oceanic crust the volcanoes form an island arc.

text: When two

text: tectonic plate

text: s collide, relatively denser

text: oceanic crust

text: will be subducted under relatively lighter

text: continental crust

text: . Because of the subduction process, the relatively cooler oceanic crust, along with water, is subducted to the

text: asthenosphere

text: , where pressures and temperatures are much higher than the surface of earth. Under such conditions, the downgoing plate releases

text: volatiles

text: such as HO and CO, which cause

text: partial melting

text: of the above asthenosphere. This process can create relatively buoyant

text: magma

text: , which subsequently forms a series of

text: volcano

text: es at the surface along the

text: subduction zone

text: . There are some researchers who argue that refertilization of arc lithospheric mantle may also be an important process associated with arc magmatism. Because the subduction zone (which is also the plate boundary) is generally an arc-shape, geologists named those volcanoes

text: volcanic arc

text: s. A volcanic arc built on continental crust is called a continental arc; when built on oceanic crust the volcanoes form an

text: island arc

answers: NDQ_003351

answers: subduction

answers: NDQ_003352

answers: subducts

answers: NDQ_003353

answers: pressures and temperatures

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: downgoing plate

answers: NDQ_003356

answers: subduct

answers: NDQ_003357

answers: lighter continental crust will be subducted under

answers: NDQ_003358

answers: arc

answers: NDQ_003359

answers: collides

answers: NDQ_003360

answers: continental crust

answers: NDQ_003362

answers: volcanoes at the surface along the subduction zone

answers: NDQ_003363

answers: subduction zone

answers: NDQ_003371

answers: What is the process called when two tectonic plates collide?

answers: NDQ_003373

answers: What is a subduction zone?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What type of rock deforms?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: unanswerable

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip faults, continental arcs, or subduction zones?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: subduction zone

answers: NDQ_003391

answers: continental crust

answers: NDQ_003392

answers: subduction zone

answers: NDQ_003393

answers: continental crust

answers: NDQ_003394

answers: continental arc

answers: NDQ_003395

answers: subduction zone

answers: NDQ_003396

answers: island arc

answers: NDQ_003351

answers: subducted

answers: NDQ_003352

answers: melting

answers: NDQ_003353

answers: partial melting

answers: NDQ_003354

answers: When two tectonic plates

answers: NDQ_003355

answers: island arc.

answers: NDQ_003356

answers: volcanoes

answers: NDQ_003357

answers: denser oceanic crust will be subducted under relatively lighter continental crust.

answers: NDQ_003358

answers: island arc.

answers: NDQ_003359

answers: When two tectonic plates collide,

answers: NDQ_003360

answers: tectonic plates

answers: NDQ_003362

answers: island arc.

answers: NDQ_003363

answers: When two tectonic plates collide,

answers: NDQ_003371

answers: When two tectonic plates

answers: NDQ_003373

answers: pressures and temperatures are much higher than the surface of earth.

answers: NDQ_003376

answers: When two tectonic plates

answers: NDQ_003378

answers: When two tectonic plates

answers: NDQ_003379

answers: continental arc;

answers: NDQ_003380

answers: pressures and temperatures are much higher than the surface of earth.

answers: NDQ_003381

answers: When two tectonic plates

answers: NDQ_003382

answers: relatively denser oceanic crust will be subducted

answers: NDQ_003383

answers: pressures and temperatures are much higher than the surface of earth.

answers: NDQ_003384

answers: continental arc;

answers: NDQ_003385

answers: volcanic arcs.

answers: NDQ_003386

answers: When two tectonic plates

answers: NDQ_003387

answers: When two tectonic plates

answers: NDQ_003388

answers: When two tectonic plates

answers: NDQ_003389

answers: volcanoes

answers: NDQ_003390

answers: When two tectonic plates

answers: NDQ_003391

answers: island arc.

answers: NDQ_003392

answers: When two tectonic plates

answers: NDQ_003393

answers: island arc.

answers: NDQ_003394

answers: two tectonic plates

answers: NDQ_003395

answers: two tectonic plates

answers: NDQ_003396

answers: island arc.

text: The canyon lies between the San Andreas Fault on the north and the San Jacinto Fault to the south.

text: The canyon lies between the

text: San Andreas Fault

text: on the north and the

text: San Jacinto Fault

text: to the south.

answers: NDQ_003351

answers: unbalanced

answers: NDQ_003352

answers: is likely to crack

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: change shape

answers: NDQ_003357

answers: San Jacinto Fault would be

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: is pushed together

answers: NDQ_003360

answers: faults

answers: NDQ_003362

answers: The San Jacinto Fault is on the south.

answers: NDQ_003363

answers: San Andreas Fault

answers: NDQ_003371

answers: Which of the following is not a type of fault?

answers: NDQ_003373

answers: How would you describe the rock?

answers: NDQ_003376

answers: It is not possible to tell

answers: NDQ_003378

answers: The San Jacinto Fault

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a stress?

answers: NDQ_003381

answers: Which of the following is not a type of stress?

answers: NDQ_003382

answers: None of the above choices.

answers: NDQ_003383

answers: None of the above choices .

answers: NDQ_003384

answers: Which of the following is not a type of fold: San Andreas Fault, San Jacinto Fault, or a canyon?

answers: NDQ_003385

answers: The San Jacinto Fault

answers: NDQ_003386

answers: It's impossible to say

answers: NDQ_003387

answers: It's impossible to say

answers: NDQ_003388

answers: Which of the following is not a type of fault?

answers: NDQ_003389

answers: It's impossible to say

answers: NDQ_003390

answers: San Andreas Fault

answers: NDQ_003391

answers: is a fault

answers: NDQ_003392

answers: San Andreas Fault

answers: NDQ_003393

answers: a fault

answers: NDQ_003394

answers: San Andreas Fault

answers: NDQ_003395

answers: San Andreas Fault

answers: NDQ_003396

answers: San Andreas Fault

answers: NDQ_003351

answers: San Andreas Fault

answers: NDQ_003352

answers: San Andreas Fault

answers: NDQ_003353

answers: San Andreas Fault

answers: NDQ_003354

answers: The canyon lies between the San Andreas Fault

answers: NDQ_003355

answers: canyon

answers: NDQ_003356

answers: The canyon lies between the San Andreas Fault

answers: NDQ_003357

answers: San Jacinto Fault to the south.

answers: NDQ_003358

answers: canyon

answers: NDQ_003359

answers: San Andreas Fault

answers: NDQ_003360

answers: San Andreas Fault

answers: NDQ_003362

answers: The canyon lies between the San Andreas Fault on the north

answers: NDQ_003363

answers: San Andreas Fault

answers: NDQ_003371

answers: San Andreas Fault

answers: NDQ_003373

answers: The canyon lies between the San Andreas Fault

answers: NDQ_003376

answers: The canyon lies between the San Andreas Fault

answers: NDQ_003378

answers: San Andreas Fault

answers: NDQ_003379

answers: San Jacinto Fault

answers: NDQ_003380

answers: San Andreas Fault

answers: NDQ_003381

answers: San Andreas Fault

answers: NDQ_003382

answers: San Jacinto Fault

answers: NDQ_003383

answers: San Andreas Fault

answers: NDQ_003384

answers: The canyon lies between the San Andreas Fault

answers: NDQ_003385

answers: The canyon lies between the San Andreas Fault

answers: NDQ_003386

answers: San Andreas Fault

answers: NDQ_003387

answers: San Andreas Fault

answers: NDQ_003388

answers: San Andreas Fault

answers: NDQ_003389

answers: The canyon lies between the San Andreas Fault

answers: NDQ_003390

answers: San Jacinto Fault

answers: NDQ_003391

answers: The canyon

answers: NDQ_003392

answers: San Jacinto Fault

answers: NDQ_003393

answers: The canyon

answers: NDQ_003394

answers: San Jacinto Fault

answers: NDQ_003395

answers: San Andreas Fault

answers: NDQ_003396

answers: San Jacinto Fault

text: From 1920 onward Dr. Bucher was noted for his studies in cryptovolcanic structures, significant deformations of the crust of the Earth, and structural geology.

text: From 1920 onward Dr. Bucher was noted for his studies in cryptovolcanic structures, significant deformations of the crust of the Earth, and structural geology.

answers: NDQ_003351

answers: significant deformation

answers: NDQ_003352

answers: deforms

answers: NDQ_003353

answers: deformation

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: swell

answers: NDQ_003357

answers: significant deformations of the crust

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: deforms

answers: NDQ_003360

answers: volcanoes

answers: NDQ_003362

answers: the San Andreas fault is not a volcano

answers: NDQ_003363

answers: volcanoes

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: How would you describe Bucher?

answers: NDQ_003376

answers: What type of terrain is caused by compressive forces

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What is Bucher known for?

answers: NDQ_003381

answers: What does Bucher study?

answers: NDQ_003382

answers: None of the above choices.

answers: NDQ_003383

answers: What is Bucher's profession?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: deformations of the crust

answers: NDQ_003387

answers: Which of the following is not a cause of normal faults?

answers: NDQ_003388

answers: Which of the following is not a result of shear stress?

answers: NDQ_003389

answers: deformations

answers: NDQ_003390

answers: a fault in which the hanging wall drops down relative to the footwall

answers: NDQ_003391

answers: igneous rock

answers: NDQ_003392

answers: a fault in which the hanging wall pushes

answers: NDQ_003393

answers: igneous rock

answers: NDQ_003394

answers: isobath

answers: NDQ_003395

answers: NDQ_003396

answers: elongated fault

answers: NDQ_003351

answers: cryptovolcanic structures,

answers: NDQ_003352

answers: deformations

answers: NDQ_003353

answers: deformations

answers: NDQ_003354

answers: From 1920 onward Dr. Bucher

answers: NDQ_003355

answers: cryptovolcanic structures,

answers: NDQ_003356

answers: significant deformations of the crust of the Earth,

answers: NDQ_003357

answers: significant deformations of the crust of the Earth,

answers: NDQ_003358

answers: cryptovolcanic structures,

answers: NDQ_003359

answers: significant deformations

answers: NDQ_003360

answers: crust of the Earth,

answers: NDQ_003362

answers: cryptovolcanic structures,

answers: NDQ_003363

answers: cryptovolcanic

answers: NDQ_003371

answers: structural geology.

answers: NDQ_003373

answers: significant deformations of the crust of the Earth, and structural geology.

answers: NDQ_003376

answers: structural geology.

answers: NDQ_003378

answers: significant deformations of the crust of the Earth,

answers: NDQ_003379

answers: cryptovolcanic structures,

answers: NDQ_003380

answers: significant deformations

answers: NDQ_003381

answers: significant deformations of the crust of the Earth, and structural geology.

answers: NDQ_003382

answers: cryptovolcanic structures,

answers: NDQ_003383

answers: structural geology.

answers: NDQ_003384

answers: cryptovolcanic structures,

answers: NDQ_003385

answers: significant deformations of the crust of the Earth, and structural geology.

answers: NDQ_003386

answers: significant deformations of the crust of the Earth,

answers: NDQ_003387

answers: cryptovolcanic structures,

answers: NDQ_003388

answers: cryptovolcanic structures,

answers: NDQ_003389

answers: cryptovolcanic structures,

answers: NDQ_003390

answers: cryptovolcanic structures,

answers: NDQ_003391

answers: cryptovolcanic structures,

answers: NDQ_003392

answers: cryptovolcanic structures,

answers: NDQ_003393

answers: cryptovolcanic structures,

answers: NDQ_003394

answers: cryptovolcanic structures,

answers: NDQ_003395

answers: cryptovolcanic structures,

answers: NDQ_003396

answers: cryptovolcanic

text: The first offshore drillship was the CUSS 1 developed for the Mohole project to drill into the Earth's crust.

text: The first offshore

text: drillship

text: was the CUSS 1 developed for the

text: Mohole

text: project to drill into the Earth's crust.

answers: NDQ_003351

answers: lateral

answers: NDQ_003352

answers: increases in size.

answers: NDQ_003353

answers: voids to form

answers: NDQ_003354

answers: Toroweap Formation is a geologic formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: Mohole is a type of

answers: NDQ_003358

answers: Mohole

answers: NDQ_003359

answers: is pushed together

answers: NDQ_003360

answers: Earth's crust.

answers: NDQ_003362

answers: The San Andreas fault is located in the Pacific Ocean.

answers: NDQ_003363

answers: the same time as the Earth

answers: NDQ_003371

answers: Which of the following is not an example of a thrust fault?

answers: NDQ_003373

answers: How would you describe CUSS 1?

answers: NDQ_003376

answers: None of the above choices.

answers: NDQ_003378

answers: The answer: slip.

answers: NDQ_003379

answers: The dip of the fault plane is horizontal.

answers: NDQ_003380

answers: Which of the following is not a stress?

answers: NDQ_003381

answers: What would happen if the drillship drilled into the Earth's crust?

answers: NDQ_003382

answers: None of the above choices.

answers: NDQ_003383

answers: None of the above choices.

answers: NDQ_003384

answers: What is the opposite of a fold that arches upward?

answers: NDQ_003385

answers: what is the first offshore drillship?

answers: NDQ_003386

answers: The answer: faults.

answers: NDQ_003387

answers: Which of the following is not a cause of normal faults?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip or shear stress?

answers: NDQ_003389

answers: None of the above choices.

answers: NDQ_003390

answers: Mohole

answers: NDQ_003391

answers: is a crater

answers: NDQ_003392

answers: Mohole

answers: NDQ_003393

answers: is a crater

answers: NDQ_003394

answers: is a fault

answers: NDQ_003395

answers: is a

answers: NDQ_003396

answers: is a type

answers: NDQ_003351

answers: Earth's crust.

answers: NDQ_003352

answers: Earth's crust.

answers: NDQ_003353

answers: Earth's crust.

answers: NDQ_003354

answers: The first offshore drillship was the CUSS 1

answers: NDQ_003355

answers: Mohole project to drill into the Earth's crust.

answers: NDQ_003356

answers: Mohole project to drill into the Earth's crust.

answers: NDQ_003357

answers: Mohole

answers: NDQ_003358

answers: Mohole

answers: NDQ_003359

answers: Earth's crust.

answers: NDQ_003360

answers: Earth's crust.

answers: NDQ_003362

answers: drill into the Earth's crust.

answers: NDQ_003363

answers: Mohole project to drill into the Earth's crust.

answers: NDQ_003371

answers: CUSS 1

answers: NDQ_003373

answers: Mohole project to drill into the Earth's crust.

answers: NDQ_003376

answers: The first offshore drillship was the CUSS 1

answers: NDQ_003378

answers: CUSS 1

answers: NDQ_003379

answers: The first offshore drillship was the CUSS 1

answers: NDQ_003380

answers: Earth's crust.

answers: NDQ_003381

answers: CUSS 1

answers: NDQ_003382

answers: CUSS 1

answers: NDQ_003383

answers: Earth's crust.

answers: NDQ_003384

answers: The first offshore drillship was the CUSS 1

answers: NDQ_003385

answers: Earth's crust.

answers: NDQ_003386

answers: Earth's crust.

answers: NDQ_003387

answers: The first offshore drillship was the CUSS 1

answers: NDQ_003388

answers: The first offshore drillship was the CUSS 1

answers: NDQ_003389

answers: Earth's crust.

answers: NDQ_003390

answers: Mohole

answers: NDQ_003391

answers: Mohole

answers: NDQ_003392

answers: Mohole

answers: NDQ_003393

answers: Mohole project to drill into the Earth's crust.

answers: NDQ_003394

answers: Mohole project to drill into the Earth's crust.

answers: NDQ_003395

answers: Mohole project to drill into the Earth's crust.

answers: NDQ_003396

answers: Mohole project to drill into the Earth's crust.

text: Volcanism in the Chilean Andes is caused by subduction of the Nazca and Antarctic tectonic plates under the South American Plate. Volcanoes in Chile occur in the Central (CVZ), South (SVZ), and Austral Volcanic Zones (AVZ). The gap that separates the Central and South Volcanic Zones is caused by shallow-angle subduction in the Pampean flat-slab segment where the more buoyant Juan Fernández Ridge subducts under the South American continent. This buoyant region prevents the  slab (subducting tectonic plate) from diving deep into the mantle, where the heat and pressure would destabilize the mineral chlorite, releasing water that would in turn cause melting and volcanism. The Patagonian Volcanic Gap, which separates the South and Austral Volcanic Zones, is caused by the subduction of the Chile Ridge, though it is less clear whether this gap also is due to flat-slab subduction; it may instead arise because melting of the subducting slab there produced felsic igneous rocks instead of volcanoes.

text: Volcanism in the Chilean Andes

text: is caused by

text: subduction

text: of the

text: Nazca

text: and

text: Antarctic

text: tectonic plate

text: s under the

text: South American Plate

text: . Volcanoes in Chile occur in the

text: Central

text: (CVZ),

text: South

text: (SVZ), and

text: Austral

text: Volcanic Zones (AVZ). The gap that separates the Central and South Volcanic Zones is caused by shallow-angle subduction in the

text: Pampean flat-slab segment

text: where the more buoyant

text: Juan Fernández Ridge

text: subducts under the South American continent. This buoyant region prevents the

text: slab

text: (subducting tectonic plate) from diving deep into the

text: mantle

text: , where the heat and pressure would destabilize the mineral

text: chlorite

text: , releasing water that would in turn cause

text: melting

text: and

text: volcanism

text: . The

text: Patagonian Volcanic Gap

text: , which separates the South and Austral Volcanic Zones, is caused by the subduction of the

text: Chile Ridge

text: , though it is less clear whether this gap also is due to

text: flat-slab subduction

text: ; it may instead arise because melting of the subducting slab there produced

text: felsic

text: igneous rock

text: s instead of volcanoes.

answers: NDQ_003351

answers: subduction

answers: NDQ_003352

answers: destabilizes

answers: NDQ_003353

answers: subduction

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: ridge

answers: NDQ_003356

answers: volcanism

answers: NDQ_003357

answers: subduction of tectonic plates causes what?

answers: NDQ_003358

answers: unanswerable

answers: NDQ_003359

answers: destabilizes

answers: NDQ_003360

answers: tectonic plates

answers: NDQ_003362

answers: melting of the subducting slab there produced felsic igneous rocks instead of volcanoes.

answers: NDQ_003363

answers: subduction

answers: NDQ_003371

answers: Which of the following is not caused by shallow-angle subduction in the Pampean flat-slab segment

answers: NDQ_003373

answers: What is the difference between subduction and subduction?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What would destabilize the mineral chlorite?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What type of fold is Juan Fernández Ridge?

answers: NDQ_003385

answers: What is the Central (CVZ)?

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: Which is not caused by subduction of the Nazca and Antarctic tectonic plates?

answers: NDQ_003388

answers: Which of the following is not caused by subduction of the Nazca and Antarctic tectonic plates?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: Juan Fernández Ridge

answers: NDQ_003391

answers: Juan Fernández Ridge

answers: NDQ_003392

answers: Patagonian

answers: NDQ_003393

answers: Juan Fernández Ridge

answers: NDQ_003394

answers: shallow-angle

answers: NDQ_003395

answers: subduction

answers: NDQ_003396

answers: shallow-angle

answers: NDQ_003351

answers: subduction

answers: NDQ_003352

answers: destabilize the mineral chlorite,

answers: NDQ_003353

answers: melting and volcanism.

answers: NDQ_003354

answers: shallow-angle subduction in the Pampean flat-slab segment

answers: NDQ_003355

answers: flat-slab segment

answers: NDQ_003356

answers: melting and volcanism.

answers: NDQ_003357

answers: diving deep into the mantle,

answers: NDQ_003358

answers: The Patagonian Volcanic Gap,

answers: NDQ_003359

answers: heat and pressure

answers: NDQ_003360

answers: subduction of the Nazca and Antarctic tectonic plates

answers: NDQ_003362

answers: deep into the mantle,

answers: NDQ_003363

answers: South American Plate.

answers: NDQ_003371

answers: shallow-angle subduction

answers: NDQ_003373

answers: the heat and pressure would destabilize the mineral chlorite,

answers: NDQ_003376

answers: subduction of the Nazca and Antarctic tectonic plates

answers: NDQ_003378

answers: Volcanism

answers: NDQ_003379

answers: shallow-angle subduction

answers: NDQ_003380

answers: pressure

answers: NDQ_003381

answers: destabilize the mineral chlorite,

answers: NDQ_003382

answers: pressure

answers: NDQ_003383

answers: pressure

answers: NDQ_003384

answers: Juan Fernández Ridge

answers: NDQ_003385

answers: Austral Volcanic Zones (AVZ).

answers: NDQ_003386

answers: Volcanism in the Chilean Andes is caused by subduction

answers: NDQ_003387

answers: subduction of the Nazca and Antarctic tectonic plates

answers: NDQ_003388

answers: subduction of the Nazca and Antarctic tectonic plates

answers: NDQ_003389

answers: subduction

answers: NDQ_003390

answers: Juan Fernández Ridge

answers: NDQ_003391

answers: flat-slab

answers: NDQ_003392

answers: shallow-angle subduction in the Pampean flat-slab segment

answers: NDQ_003393

answers: flat-slab

answers: NDQ_003394

answers: shallow-angle subduction

answers: NDQ_003395

answers: shallow-angle subduction

answers: NDQ_003396

answers: shallow-angle subduction

text: Williamson and Adams first developed the theory in 1923. They concluded that "It is therefore impossible to explain the high density of the Earth on the basis of compression alone. The dense interior cannot consist of ordinary rocks compressed to a small volume; we must therefore fall back on the only reasonable alternative, namely, the presence of a heavier material, presumably some metal, which, to judge from its abundance in the Earth's crust, in meteorites and in the Sun, is probably iron."

text: Williamson and Adams first developed the theory in 1923. They concluded that "It is therefore impossible to explain the high density of the Earth on the basis of compression alone. The dense interior cannot consist of ordinary rocks compressed to a small volume; we must therefore fall back on the only reasonable alternative, namely, the presence of a heavier material, presumably some metal, which, to judge from its abundance in the Earth's crust, in meteorites and in the Sun, is probably iron."

answers: NDQ_003351

answers: compression

answers: NDQ_003352

answers: compresses

answers: NDQ_003353

answers: compression

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: compress

answers: NDQ_003357

answers: rocks compressed to a small volume

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: compresses

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: density of the Earth on the basis of compression alone

answers: NDQ_003363

answers: the Sun

answers: NDQ_003371

answers: unanswerable

answers: NDQ_003373

answers: unanswerable

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: no

answers: NDQ_003380

answers: unanswerable

answers: NDQ_003381

answers: compresses to a small volume

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: no

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: fault zone

answers: NDQ_003386

answers: no

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: unanswerable

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: unanswerable

answers: NDQ_003392

answers: a fault

answers: NDQ_003393

answers: unanswerable

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: NDQ_003396

answers: NDQ_003351

answers: iron."

answers: NDQ_003352

answers: compressed to a small volume;

answers: NDQ_003353

answers: compressed to a small volume;

answers: NDQ_003354

answers: Williamson and Adams first developed the theory in 1923.

answers: NDQ_003355

answers: compression

answers: NDQ_003356

answers: compressed to a small volume;

answers: NDQ_003357

answers: iron."

answers: NDQ_003358

answers: meteorites

answers: NDQ_003359

answers: a heavier material,

answers: NDQ_003360

answers: iron."

answers: NDQ_003362

answers: compression alone.

answers: NDQ_003363

answers: iron."

answers: NDQ_003371

answers: Williamson and Adams first developed the theory in 1923.

answers: NDQ_003373

answers: rocks compressed to a small volume;

answers: NDQ_003376

answers: Williamson and Adams first developed the theory in 1923.

answers: NDQ_003378

answers: compression

answers: NDQ_003379

answers: Williamson and Adams first developed the theory in 1923.

answers: NDQ_003380

answers: compression

answers: NDQ_003381

answers: compression alone. The dense interior cannot consist of ordinary rocks

answers: NDQ_003382

answers: compression

answers: NDQ_003383

answers: compression

answers: NDQ_003384

answers: Williamson and Adams first developed the theory in 1923.

answers: NDQ_003385

answers: Williamson and Adams first developed the theory in 1923.

answers: NDQ_003386

answers: the presence of a heavier material,

answers: NDQ_003387

answers: iron."

answers: NDQ_003388

answers: Williamson and Adams first developed the theory in 1923.

answers: NDQ_003389

answers: compression

answers: NDQ_003390

answers: Williamson and Adams first developed the theory in 1923.

answers: NDQ_003391

answers: iron."

answers: NDQ_003392

answers: Williamson and Adams first developed the theory in 1923.

answers: NDQ_003393

answers: iron."

answers: NDQ_003394

answers: Williamson and Adams first developed the theory in 1923.

answers: NDQ_003395

answers: Williamson and Adams first developed the theory in 1923.

answers: NDQ_003396

answers: Williamson and Adams first developed the theory in 1923.

text: Uranium is a fairly common element in the Earth's crust. Uranium is approximately as common as tin or germanium in the Earth's crust, and is about 40 times more common than silver. Uranium is present in trace concentrations in most rocks, dirt, and ocean water, but can be economically extracted currently only where it is present in high concentrations. Still, the world's present measured resources of uranium, economically recoverable at the arbitrary price ceiling of 130 USD/kg, are enough to last for between 70 and 100 years.

text: Uranium

text: is a fairly common

text: element

text: in the Earth's crust. Uranium is approximately as common as

text: tin

text: or

text: germanium

text: in the Earth's crust, and is about 40 times more common than silver. Uranium is present in trace concentrations in most rocks, dirt, and ocean water, but can be economically extracted currently only where it is present in high concentrations. Still, the world's present measured resources of uranium, economically recoverable at the arbitrary price ceiling of 130 USD/kg, are enough to last for between 70 and 100 years.

answers: NDQ_003351

answers: Uranium

answers: NDQ_003352

answers: more likely to contain uranium

answers: NDQ_003353

answers: voids to form

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: oxidize

answers: NDQ_003357

answers: Uranium is present in trace concentrations

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: can be economically extracted currently only where it is present in high concentrations

answers: NDQ_003363

answers: Uranium

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: unanswerable

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: vertical

answers: NDQ_003380

answers: How is uranium present in most rocks?

answers: NDQ_003381

answers: Uranium is about 40 times more common than silver

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: fault zone

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: unanswerable

answers: NDQ_003389

answers: mountains

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: unanswerable

answers: NDQ_003392

answers: unanswerable

answers: NDQ_003393

answers: unanswerable

answers: NDQ_003394

answers: isosceles

answers: NDQ_003395

answers: unanswerable

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: Uranium

answers: NDQ_003352

answers: Uranium

answers: NDQ_003353

answers: Uranium

answers: NDQ_003354

answers: Uranium

answers: NDQ_003355

answers: Uranium

answers: NDQ_003356

answers: Uranium

answers: NDQ_003357

answers: high concentrations.

answers: NDQ_003358

answers: rocks,

answers: NDQ_003359

answers: Uranium

answers: NDQ_003360

answers: Uranium

answers: NDQ_003362

answers: Uranium

answers: NDQ_003363

answers: Uranium

answers: NDQ_003371

answers: Uranium

answers: NDQ_003373

answers: can be economically extracted currently only where it is present in high concentrations.

answers: NDQ_003376

answers: Uranium is a fairly common element in the Earth's crust.

answers: NDQ_003378

answers: Uranium

answers: NDQ_003379

answers: 40 times more common than silver.

answers: NDQ_003380

answers: Uranium

answers: NDQ_003381

answers: can be economically extracted currently only where it is present in high concentrations.

answers: NDQ_003382

answers: 40 times more common than silver.

answers: NDQ_003383

answers: Uranium

answers: NDQ_003384

answers: 40 times more common than silver.

answers: NDQ_003385

answers: Uranium

answers: NDQ_003386

answers: Uranium

answers: NDQ_003387

answers: Uranium

answers: NDQ_003388

answers: Uranium

answers: NDQ_003389

answers: Uranium

answers: NDQ_003390

answers: Uranium is a fairly common element in the Earth's crust.

answers: NDQ_003391

answers: Uranium

answers: NDQ_003392

answers: Uranium is a fairly common element in the Earth's crust.

answers: NDQ_003393

answers: Uranium

answers: NDQ_003394

answers: Uranium is a fairly common element in the Earth's crust.

answers: NDQ_003395

answers: Uranium

answers: NDQ_003396

answers: Uranium

text: is the height of the mountain and c the thickness of the crust.

text: is the height of the mountain and c the thickness of the crust.

answers: NDQ_003351

answers: c

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: earthquakes.

answers: NDQ_003354

answers: c

answers: NDQ_003355

answers: glacier

answers: NDQ_003356

answers: swell

answers: NDQ_003357

answers: c is the height of the mountain and d is the thickness of the crust

answers: NDQ_003358

answers: glacier

answers: NDQ_003359

answers: is too thin.

answers: NDQ_003360

answers: c .

answers: NDQ_003362

answers: the San Andreas fault is a fault in the Earth's crust

answers: NDQ_003363

answers: the same time as the Earth.

answers: NDQ_003371

answers: c

answers: NDQ_003373

answers: c

answers: NDQ_003376

answers: c

answers: NDQ_003378

answers: c

answers: NDQ_003379

answers: c

answers: NDQ_003380

answers: c

answers: NDQ_003381

answers: c

answers: NDQ_003382

answers: c

answers: NDQ_003383

answers: c

answers: NDQ_003384

answers: c

answers: NDQ_003385

answers: c

answers: NDQ_003386

answers: c

answers: NDQ_003387

answers: c

answers: NDQ_003388

answers: c

answers: NDQ_003389

answers: c

answers: NDQ_003390

answers: is the height of the mountain

answers: NDQ_003391

answers: is the thickness of the crust

answers: NDQ_003392

answers: is the height of the mountain

answers: NDQ_003393

answers: is a mountain

answers: NDQ_003394

answers: lateral fault

answers: NDQ_003395

answers: a fault with a vertical fault plane

answers: NDQ_003396

answers: is the height of the mountain

answers: NDQ_003351

answers: height of the mountain and c the thickness of the crust.

answers: NDQ_003352

answers: the thickness of the crust.

answers: NDQ_003353

answers: c the thickness of the crust.

answers: NDQ_003354

answers: c the thickness of the crust.

answers: NDQ_003355

answers: height of the mountain

answers: NDQ_003356

answers: c the thickness of the crust.

answers: NDQ_003357

answers: c the thickness of the crust.

answers: NDQ_003358

answers: mountain

answers: NDQ_003359

answers: c the thickness of the crust.

answers: NDQ_003360

answers: c the thickness of the crust.

answers: NDQ_003362

answers: the height of the mountain

answers: NDQ_003363

answers: height of the mountain and c the thickness of the crust.

answers: NDQ_003371

answers: c the thickness of the crust.

answers: NDQ_003373

answers: c the thickness of the crust.

answers: NDQ_003376

answers: c the thickness of the crust.

answers: NDQ_003378

answers: c the thickness of the crust.

answers: NDQ_003379

answers: height of the mountain and c the thickness of the crust.

answers: NDQ_003380

answers: height of the mountain and c the thickness of the crust.

answers: NDQ_003381

answers: c the thickness of the crust.

answers: NDQ_003382

answers: c the thickness of the crust.

answers: NDQ_003383

answers: c the thickness of the crust.

answers: NDQ_003384

answers: height of the mountain and c the thickness of the crust.

answers: NDQ_003385

answers: height of the mountain and c the thickness of the crust.

answers: NDQ_003386

answers: height of the mountain and c the thickness of the crust.

answers: NDQ_003387

answers: c the thickness of the crust.

answers: NDQ_003388

answers: c the thickness of the crust.

answers: NDQ_003389

answers: c the thickness of the crust.

answers: NDQ_003390

answers: height of the mountain

answers: NDQ_003391

answers: the thickness of the crust.

answers: NDQ_003392

answers: height of the mountain and c the thickness of the crust.

answers: NDQ_003393

answers: height of the mountain and c the thickness of the crust.

answers: NDQ_003394

answers: height of the mountain and c the thickness of the crust.

answers: NDQ_003395

answers: c the thickness of the crust.

answers: NDQ_003396

answers: height of the mountain and c the thickness of the crust.

text: The theory of plate tectonics states that the Earth's crust is made up of rigid plates that "float" on top of the mantle and move relative to one another. As the plates move, the crust deforms dominantly along the plate margins. Intraplate deformation differs from that respect by the observation that deformation can occur anywhere the crust is weak and not just at plate margins.

text: The theory of plate tectonics states that the Earth's crust is made up of rigid plates that "float" on top of the mantle and move relative to one another. As the plates move, the crust deforms dominantly along the plate margins. Intraplate deformation differs from that respect by the observation that deformation can occur anywhere the crust is weak and not just at plate margins.

answers: NDQ_003351

answers: deformation

answers: NDQ_003352

answers: deforms

answers: NDQ_003353

answers: deformation

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: plate margin

answers: NDQ_003356

answers: weaken

answers: NDQ_003357

answers: deformation can occur anywhere the crust is weak

answers: NDQ_003358

answers: plate margin

answers: NDQ_003359

answers: deforms

answers: NDQ_003360

answers: plates

answers: NDQ_003362

answers: deformation can occur anywhere the crust is weak

answers: NDQ_003363

answers: plate margins

answers: NDQ_003371

answers: What is the theory of plate tectonics?

answers: NDQ_003373

answers: how would you describe compressive stresses?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What is the theory of plate tectonics?

answers: NDQ_003382

answers: what is the most common stress at convergent plates

answers: NDQ_003383

answers: what is the last word in the passage?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: plate tectonics

answers: NDQ_003387

answers: Which of the following is not a type of plate tectonics?

answers: NDQ_003388

answers: what is the name of the theory of plate tectonics?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: Intraplate deformation

answers: NDQ_003391

answers: Intraplate deformation

answers: NDQ_003392

answers: Intraplate deformation

answers: NDQ_003393

answers: plate margins

answers: NDQ_003394

answers: intraplate deformation

answers: NDQ_003395

answers: plate tectonics

answers: NDQ_003396

answers: Intraplate deformation

answers: NDQ_003351

answers: Intraplate deformation

answers: NDQ_003352

answers: deformation can occur anywhere the crust is weak

answers: NDQ_003353

answers: the crust deforms

answers: NDQ_003354

answers: deformation can occur anywhere the crust is weak

answers: NDQ_003355

answers: Intraplate deformation

answers: NDQ_003356

answers: deformation can occur anywhere the crust is weak

answers: NDQ_003357

answers: deformation can occur anywhere the crust is weak

answers: NDQ_003358

answers: Intraplate deformation

answers: NDQ_003359

answers: weak

answers: NDQ_003360

answers: plate tectonics

answers: NDQ_003362

answers: the crust deforms dominantly along the plate margins.

answers: NDQ_003363

answers: plate tectonics

answers: NDQ_003371

answers: The theory of plate tectonics

answers: NDQ_003373

answers: The theory of plate tectonics

answers: NDQ_003376

answers: deformation can occur anywhere the crust is weak

answers: NDQ_003378

answers: Intraplate deformation

answers: NDQ_003379

answers: The theory of plate tectonics

answers: NDQ_003380

answers: deformation can occur anywhere the crust is weak

answers: NDQ_003381

answers: Intraplate deformation

answers: NDQ_003382

answers: the crust deforms dominantly along the plate margins.

answers: NDQ_003383

answers: deformation

answers: NDQ_003384

answers: The theory of plate tectonics

answers: NDQ_003385

answers: the crust deforms dominantly along the plate margins.

answers: NDQ_003386

answers: plate tectonics

answers: NDQ_003387

answers: Intraplate deformation

answers: NDQ_003388

answers: Intraplate deformation

answers: NDQ_003389

answers: deformation can occur anywhere the crust is weak

answers: NDQ_003390

answers: Intraplate deformation

answers: NDQ_003391

answers: Intraplate deformation

answers: NDQ_003392

answers: Intraplate deformation

answers: NDQ_003393

answers: plates that "float" on top of the mantle

answers: NDQ_003394

answers: Intraplate deformation

answers: NDQ_003395

answers: The theory of plate tectonics

answers: NDQ_003396

answers: Intraplate deformation

text: New oceanic crust, closest to the mid-oceanic ridges, is mostly basalt at shallow levels and has a rugged topography. The roughness of this topography is a function of the rate at which the mid-ocean ridge is spreading (the spreading rate). Magnitudes of spreading rates vary quite significantly. Typical values for fast-spreading ridges are greater than 100 mm/yr, while slow-spreading ridges are typically less than 20 mm/yr. Studies have shown that the slower the spreading rate, the rougher the new oceanic crust will be, and vice versa. It is thought this phenomenon is due to faulting at the mid-ocean ridge when the new oceanic crust was formed. These faults pervading the oceanic crust, along with their bounding abyssal hills, are the most common tectonic and topographic features on the surface of the Earth. The process of seafloor spreading helps to explain the concept of continental drift in the theory of plate tectonics.

text: New oceanic crust, closest to the mid-oceanic ridges, is mostly basalt at shallow levels and has a rugged

text: topography

text: . The roughness of this topography is a function of the rate at which the mid-ocean ridge is spreading (the spreading rate). Magnitudes of spreading rates vary quite significantly. Typical values for fast-spreading ridges are greater than 100 mm/yr, while slow-spreading ridges are typically less than 20 mm/yr. Studies have shown that the slower the spreading rate, the rougher the new oceanic crust will be, and vice versa. It is thought this phenomenon is due to

text: faulting

text: at the mid-ocean ridge when the new oceanic crust was formed. These faults pervading the oceanic crust, along with their bounding abyssal hills, are the most common tectonic and topographic features on the surface of the Earth. The process of seafloor spreading helps to explain the concept of

text: continental drift

text: in the theory of plate tectonics.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: is more likely to crack

answers: NDQ_003353

answers: faulting

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: ridge

answers: NDQ_003356

answers: smooth out

answers: NDQ_003357

answers: slow-spreading ridges are typically less than 20 mm/yr

answers: NDQ_003358

answers: ridge

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: plate boundaries

answers: NDQ_003362

answers: slow-spreading ridges are typically less than 20 mm/yr

answers: NDQ_003363

answers: mid-ocean ridge

answers: NDQ_003371

answers: What is the most common tectonic and topographic features on the surface of the Earth?

answers: NDQ_003373

answers: What is the main idea of this passage?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What is the most common tectonic feature on the surface of the Earth?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: What is a fast-spreading ridge?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: What is the most common tectonic and topographic features on the surface of the Earth?

answers: NDQ_003388

answers: What is the most common tectonic and topographic features on the surface of the Earth?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: abyssal

answers: NDQ_003391

answers: abyssal hills

answers: NDQ_003392

answers: abyssal

answers: NDQ_003393

answers: Mid-ocean Ridge

answers: NDQ_003394

answers: non-vertical

answers: NDQ_003395

answers: unanswerable

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: faulting

answers: NDQ_003352

answers: rougher

answers: NDQ_003353

answers: faulting

answers: NDQ_003354

answers: New oceanic crust,

answers: NDQ_003355

answers: faulting

answers: NDQ_003356

answers: rougher

answers: NDQ_003357

answers: 20 mm/yr.

answers: NDQ_003358

answers: abyssal hills,

answers: NDQ_003359

answers: faulting

answers: NDQ_003360

answers: faulting

answers: NDQ_003362

answers: 100 mm/yr,

answers: NDQ_003363

answers: faulting at the mid-ocean ridge

answers: NDQ_003371

answers: faulting at the mid-ocean ridge

answers: NDQ_003373

answers: faulting

answers: NDQ_003376

answers: faulting at the mid-ocean ridge

answers: NDQ_003378

answers: faulting

answers: NDQ_003379

answers: 100 mm/yr,

answers: NDQ_003380

answers: faulting

answers: NDQ_003381

answers: faulting

answers: NDQ_003382

answers: faulting

answers: NDQ_003383

answers: faulting

answers: NDQ_003384

answers: faulting at the mid-ocean ridge

answers: NDQ_003385

answers: faults

answers: NDQ_003386

answers: faulting at the mid-ocean ridge

answers: NDQ_003387

answers: faulting at the mid-ocean ridge

answers: NDQ_003388

answers: faulting at the mid-ocean ridge

answers: NDQ_003389

answers: faulting

answers: NDQ_003390

answers: faulting at the mid-ocean ridge

answers: NDQ_003391

answers: abyssal hills,

answers: NDQ_003392

answers: faulting at the mid-ocean ridge

answers: NDQ_003393

answers: abyssal hills,

answers: NDQ_003394

answers: faulting at the mid-ocean ridge

answers: NDQ_003395

answers: faulting at the mid-ocean ridge

answers: NDQ_003396

answers: faulting at the mid-ocean ridge

text: It was erected on Mount Washington in 1853 to compete with The Summit House, a nearby hotel established in 1852. Built by Samuel F. Spaulding at a cost of $7000, The Tip-Top House was made of rock blasted from the mountain. On clear days, a telescope was placed on its flat roof to create an observatory, although in the early 1860s, the flat roof was replaced with a pitched roof. Beginning in 1877, the building functioned for seven years as a printing office for Among the Clouds, the mountain's newspaper.

text: It was erected on Mount Washington in 1853 to compete with The Summit House, a nearby hotel established in 1852. Built by Samuel F. Spaulding at a cost of $7000, The Tip-Top House was made of rock blasted from the mountain. On clear days, a telescope was placed on its flat roof to create an

text: observatory

text: , although in the early 1860s, the flat roof was replaced with a pitched roof. Beginning in 1877, the building functioned for seven years as a printing office for Among the Clouds, the mountain's newspaper.

answers: NDQ_003351

answers: flat roof

answers: NDQ_003352

answers: is likely to crack

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: pitched roof

answers: NDQ_003356

answers: flat roof

answers: NDQ_003357

answers: The Tip-Top House was made of rock blasted from

answers: NDQ_003358

answers: rock blasted

answers: NDQ_003359

answers: blasted

answers: NDQ_003360

answers: continental plates

answers: NDQ_003362

answers: The Summit House, a nearby hotel established in 1852.

answers: NDQ_003363

answers: the same time

answers: NDQ_003371

answers: What was the Tip-Top House made of?

answers: NDQ_003373

answers: How would you describe the Tip-Top House?

answers: NDQ_003376

answers: what is the last word in the passage?

answers: NDQ_003378

answers: what is the first time period mentioned?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What was the Tip-Top House made of?

answers: NDQ_003381

answers: What was the Tip-Top House made of?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Why was the flat roof replaced with a pitched roof?

answers: NDQ_003384

answers: What was the Tip-Top House made of?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: What is the Tip-Top House made of?

answers: NDQ_003387

answers: Which happened first, The Summit House was established or The Tip-Top House was made of rock blasted from the mountain?

answers: NDQ_003388

answers: What was the Tip-Top House made of?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: Mount Washington

answers: NDQ_003392

answers: Mount Washington

answers: NDQ_003393

answers: Mount Washington

answers: NDQ_003394

answers: NDQ_003395

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: rock blasted from the mountain.

answers: NDQ_003352

answers: blasted

answers: NDQ_003353

answers: blasted

answers: NDQ_003354

answers: The Tip-Top House

answers: NDQ_003355

answers: Tip-Top House

answers: NDQ_003356

answers: rock blasted

answers: NDQ_003357

answers: rock blasted from the mountain.

answers: NDQ_003358

answers: blasted from the mountain.

answers: NDQ_003359

answers: blasted

answers: NDQ_003360

answers: rock blasted from the mountain.

answers: NDQ_003362

answers: rock blasted from the mountain.

answers: NDQ_003363

answers: rock blasted from the mountain.

answers: NDQ_003371

answers: 1852.

answers: NDQ_003373

answers: rock blasted from the mountain.

answers: NDQ_003376

answers: rock blasted from the mountain.

answers: NDQ_003378

answers: The Tip-Top House

answers: NDQ_003379

answers: The Tip-Top House

answers: NDQ_003380

answers: rock blasted from the mountain.

answers: NDQ_003381

answers: rock blasted from the mountain.

answers: NDQ_003382

answers: The Tip-Top House

answers: NDQ_003383

answers: blasted

answers: NDQ_003384

answers: 1852.

answers: NDQ_003385

answers: Mount Washington in 1853

answers: NDQ_003386

answers: rock blasted from the mountain.

answers: NDQ_003387

answers: The Tip-Top House

answers: NDQ_003388

answers: rock blasted from the mountain.

answers: NDQ_003389

answers: rock

answers: NDQ_003390

answers: rock blasted from the mountain.

answers: NDQ_003391

answers: Mount Washington

answers: NDQ_003392

answers: The Tip-Top

answers: NDQ_003393

answers: Mount Washington

answers: NDQ_003394

answers: Mount Washington in 1853

answers: NDQ_003395

answers: Mount Washington in 1853

answers: NDQ_003396

answers: Mount Washington

text: The D'Entrecasteaux Islands are volcanically active, with a number of areas of historic/geologic volcanism and active geothermal fields. Fergusson island has three volcanic masses over 1,828 m high. There are geothermal areas in the south east area of Goodenough Island and the Bwabwadana and Iamalele on Fergusson Island.  A particularly active hot springs is located at Deidei on Fergusson. Between Fergusson and Normanby Islands the Dawson Straights Group has several volcanic centres that may define a partly submerged caldera; one of the cones on southwestern Fergusson Island may have erupted in 1350.  Geologically the islands are largely made up of rock that probably once belonged to the northern edge of the Australian plate that was thrust deep into the Earth's crust by plate collision. The burial of these rocks to great depths (where they also encountered correspondingly high temperatures) metamorphosed the rocks to eclogite facies: >2GPa and >700˚C. Specifically, these islands play host to the youngest known coesite-eclogite sample; CA-TIMS dating of zircons within this sample dates its formation to ~5Ma, meaning it has been exhumed from a depth of ~100 km at the remarkable rate of ~20mm/yr. The rock at the centre of the tall domes in these islands was thus recently very deep in the Earth. Over a very short time, geologically speaking, these packets of rocks have ascended through the Earth's shallow mantle and pushed through the crust to form the gneiss domes we find today - the vestiges of the crust these massifs have thrust through are still draped as carapaces over the edges of the domes. These islands are thought to be geophysically significant because they lie immediately ahead of the west-most rift tip of the Woodlark spreading centre, which has been propagating westwards into the continent. The D'Entrecasteaux thus represent a stage of continental breakup just preceding fully-fledged volcanic spreading.

text: The D'Entrecasteaux Islands are volcanically active, with a number of areas of historic/geologic volcanism and active

text: geothermal

text: fields. Fergusson island has three volcanic masses over 1,828 m high. There are geothermal areas in the south east area of Goodenough Island and the Bwabwadana and Iamalele on Fergusson Island.  A particularly active hot springs is located at Deidei on Fergusson. Between Fergusson and Normanby Islands the Dawson Straights Group has several volcanic centres that may define a partly submerged

text: caldera

text: ; one of the cones on southwestern Fergusson Island may have erupted in 1350.  Geologically the islands are largely made up of rock that probably once belonged to the northern edge of the Australian

text: plate

text: that was thrust deep into the Earth's crust by plate collision. The burial of these rocks to great depths (where they also encountered correspondingly high temperatures) metamorphosed the rocks to

text: eclogite facies

text: : >2GPa and >700˚C. Specifically, these islands play host to the youngest known coesite-eclogite sample; CA-

text: TIMS

text: dating of zircons within this sample dates its formation to ~5Ma, meaning it has been exhumed from a depth of ~100 km at the remarkable rate of ~20mm/yr. The rock at the centre of the tall domes in these islands was thus recently very deep in the Earth. Over a very short time, geologically speaking, these packets of rocks have ascended through the Earth's shallow mantle and pushed through the crust to form the gneiss domes we find today - the vestiges of the crust these massifs have thrust through are still draped as carapaces over the edges of the domes. These islands are thought to be geophysically significant because they lie immediately ahead of the west-most rift tip of the Woodlark spreading centre, which has been propagating westwards into the continent. The D'Entrecasteaux thus represent a stage of continental breakup just preceding fully-fledged volcanic spreading.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: metamorphosed

answers: NDQ_003353

answers: high temperatures

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: carapaces

answers: NDQ_003356

answers: eclogite

answers: NDQ_003357

answers: What type of fault is the Woodlark spreading centre?

answers: NDQ_003358

answers: caldera

answers: NDQ_003359

answers: plate collision

answers: NDQ_003360

answers: plate collision

answers: NDQ_003362

answers: fully-fledged volcanic spreading.

answers: NDQ_003363

answers: plate collision

answers: NDQ_003371

answers: The D'Entrecasteaux Islands are volcanically active

answers: NDQ_003373

answers: What type of stresses does a deeply buried rock experience?

answers: NDQ_003376

answers: What type of forces caused the terrain known as basin-and-range?

answers: NDQ_003378

answers: What is the rate of  20mm/yr?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What type of force applied to rock is a stress?

answers: NDQ_003381

answers: How does the rock at the centre of the tall domes in these islands was thus recently very deep in the Earth?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is the name of the area where faults are clustered?

answers: NDQ_003386

answers: What is the cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: plate collision, geothermal fields, or plate collision?

answers: NDQ_003388

answers: Which of the following is not a type of strike-slip fault: strike-slip faults, strike-slip faults or shear stress?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: The Dawson Straights Group

answers: NDQ_003391

answers: The Dawson Straights Group

answers: NDQ_003392

answers: rift tip of the Woodlark spreading centre

answers: NDQ_003393

answers: gneiss domes

answers: NDQ_003394

answers: west-most rift tip

answers: NDQ_003395

answers: Woodlark spreading centre

answers: NDQ_003396

answers: Woodlark spreading centre

answers: NDQ_003351

answers: plate collision.

answers: NDQ_003352

answers: metamorphosed the rocks to eclogite facies:

answers: NDQ_003353

answers: metamorphosed the rocks to eclogite facies:

answers: NDQ_003354

answers: eclogite facies:

answers: NDQ_003355

answers: rift

answers: NDQ_003356

answers: gneiss domes

answers: NDQ_003357

answers: plate collision.

answers: NDQ_003358

answers: gneiss domes

answers: NDQ_003359

answers: pushed through the crust

answers: NDQ_003360

answers: plate collision.

answers: NDQ_003362

answers: >700 <unk>C.

answers: NDQ_003363

answers: 700 <unk>C.

answers: NDQ_003371

answers: thrust deep into the Earth's crust by plate collision.

answers: NDQ_003373

answers: high temperatures)

answers: NDQ_003376

answers: gneiss domes

answers: NDQ_003378

answers: 20mm/yr.

answers: NDQ_003379

answers: fully-f

answers: NDQ_003380

answers: plate collision.

answers: NDQ_003381

answers: plate collision.

answers: NDQ_003382

answers: plate collision.

answers: NDQ_003383

answers: plate collision.

answers: NDQ_003384

answers: >700 <unk>C.

answers: NDQ_003385

answers: Woodlark spreading centre,

answers: NDQ_003386

answers: plate collision.

answers: NDQ_003387

answers: D'Entrecasteaux

answers: NDQ_003388

answers: >700 <unk>C.

answers: NDQ_003389

answers: gneiss domes

answers: NDQ_003390

answers: The D'Entrecasteaux

answers: NDQ_003391

answers: gneiss domes

answers: NDQ_003392

answers: The D'Entrecasteaux

answers: NDQ_003393

answers: gneiss domes

answers: NDQ_003394

answers: The D'Entrecasteaux

answers: NDQ_003395

answers: Woodlark spreading centre,

answers: NDQ_003396

answers: The D'Entrecasteaux

text: The Earth was compared to a cooling ball of iron, or a steam boiler with shifting boiler plates.  By the early 1900s, it was known that temperature increased with increasing depth.  With the thickness of the crust, the "boiler plates", being estimated at ten to fifty miles, the downward pressure would be hundreds of thousands of pounds per square inch.  Although groundwater was expected to turn to steam at a great depth, usually the downward pressure would contain any steam.  Steam's effect upon molten rock was suspected of being a cause of volcanoes and earthquakes, as it had been noticed that most volcanoes are near water.  It was not clear whether the molten rock from volcanoes had its origin in the molten rock under the crust, or if increased heat due to pressure under mountains caused the rock to melt.  One of the reasons for volcanoes was as a way in which "the contracting earth disposes of the matter it can no longer contain."  A relationship between earthquakes and volcanoes had been noted, although the causes were not known.  Fault lines and earthquakes tended to happen along the boundaries of the shifting "boiler plates", but the folding of mountains indicated that sometimes the plates buckled.

text: The Earth was compared to a cooling ball of iron, or a steam boiler with shifting boiler plates.  By the early 1900s, it was known that temperature increased with increasing depth.  With the thickness of the crust, the "boiler plates", being estimated at ten to fifty miles, the downward pressure would be hundreds of thousands of pounds per square inch.  Although groundwater was expected to turn to steam at a great depth, usually the downward pressure would contain any steam.  Steam's effect upon molten rock was suspected of being a cause of volcanoes and earthquakes, as it had been noticed that most volcanoes are near water.  It was not clear whether the molten rock from volcanoes had its origin in the molten rock under the crust, or if increased heat due to pressure under mountains caused the rock to melt.  One of the reasons for volcanoes was as a way in which "the contracting earth disposes of the matter it can no longer contain."  A relationship between earthquakes and volcanoes had been noted, although the causes were not known.  Fault lines and earthquakes tended to happen along the boundaries of the shifting "boiler plates", but the folding of mountains indicated that sometimes the plates buckled.

answers: NDQ_003351

answers: earthquakes

answers: NDQ_003352

answers: melts

answers: NDQ_003353

answers: downward pressure

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: mountains

answers: NDQ_003356

answers: melt

answers: NDQ_003357

answers: downward pressure would contain any steam

answers: NDQ_003358

answers: Fault lines

answers: NDQ_003359

answers: molten

answers: NDQ_003360

answers: fault lines

answers: NDQ_003362

answers: the folding of mountains indicated that sometimes the plates buckled

answers: NDQ_003363

answers: ten to fifty miles

answers: NDQ_003371

answers: Which of the following is not a cause of volcanoes and earthquakes?

answers: NDQ_003373

answers: It was known that temperature increased with increasing depth.

answers: NDQ_003376

answers: Which of the following is not a reason for volcanoes?

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a cause of volcanoes and earthquakes?

answers: NDQ_003381

answers: What is the reason for volcanoes?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Fault lines and earthquakes tended to happen along the boundaries

answers: NDQ_003384

answers: Which of the following is not a type of fold: Fault lines or earthquakes?

answers: NDQ_003385

answers: what is the last word in the passage?

answers: NDQ_003386

answers: yes

answers: NDQ_003387

answers: Which of the following is not a reason for volcanoes: the contracting earth disposes of the matter it can no longer contain?

answers: NDQ_003388

answers: Which of the following is not a reason for volcanoes: the contracting earth disposes of the matter it can no longer contain

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: Fault lines

answers: NDQ_003391

answers: a cooling ball of iron

answers: NDQ_003392

answers: Fault lines

answers: NDQ_003393

answers: a cooling ball of iron

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: unanswerable

answers: NDQ_003396

answers: Fault lines

answers: NDQ_003351

answers: earthquakes

answers: NDQ_003352

answers: melt.

answers: NDQ_003353

answers: molten rock

answers: NDQ_003354

answers: Fault lines and earthquakes

answers: NDQ_003355

answers: mountains

answers: NDQ_003356

answers: volcanoes and earthquakes,

answers: NDQ_003357

answers: along the boundaries of the shifting "boiler plates",

answers: NDQ_003358

answers: Fault lines

answers: NDQ_003359

answers: Fault lines

answers: NDQ_003360

answers: "boiler plates",

answers: NDQ_003362

answers: water.

answers: NDQ_003363

answers: near water.

answers: NDQ_003371

answers: Fault lines

answers: NDQ_003373

answers: temperature increased with increasing depth.

answers: NDQ_003376

answers: Steam's effect upon molten rock

answers: NDQ_003378

answers: Fault lines

answers: NDQ_003379

answers: shifting "boiler plates",

answers: NDQ_003380

answers: Steam's effect upon molten rock

answers: NDQ_003381

answers: shifting "boiler plates",

answers: NDQ_003382

answers: hundreds of thousands of pounds per square inch.

answers: NDQ_003383

answers: Fault lines

answers: NDQ_003384

answers: Fault lines

answers: NDQ_003385

answers: Fault lines

answers: NDQ_003386

answers: "boiler plates",

answers: NDQ_003387

answers: shifting "boiler plates",

answers: NDQ_003388

answers: shifting "boiler plates",

answers: NDQ_003389

answers: the folding of mountains

answers: NDQ_003390

answers: Fault lines

answers: NDQ_003391

answers: "boiler plates",

answers: NDQ_003392

answers: Fault lines

answers: NDQ_003393

answers: "boiler plates",

answers: NDQ_003394

answers: Fault lines

answers: NDQ_003395

answers: Fault lines

answers: NDQ_003396

answers: Fault lines

text: This is a list of the named geological faults affecting the rocks of Wales. See the main article on faults for a fuller treatment of fault types and nomenclature but in brief, the main types are normal faults, reverse faults, thrusts or thrust faults and strike-slip faults. Many faults may have acted as both normal faults at one time and as reverse or thrust faults at another and may or may not have also incorporated some degree of strike-slip movement too. Fault zones, fault belts and fault complexes typically describe assemblages of faults which have a common origin and history and whose alignments tend to be sub-parallel to one another.

text: This is a list of the named geological faults affecting the rocks of

text: Wales

text: . See the

text: main article on faults

text: for a fuller treatment of fault types and nomenclature but in brief, the main types are normal faults, reverse faults, thrusts or thrust faults and strike-slip faults. Many faults may have acted as both normal faults at one time and as reverse or thrust faults at another and may or may not have also incorporated some degree of strike-slip movement too. Fault zones, fault belts and fault complexes typically describe assemblages of faults which have a common origin and history and whose alignments tend to be sub-parallel to one another.

answers: NDQ_003351

answers: strike-slip

answers: NDQ_003352

answers: is subjected to more movement.

answers: NDQ_003353

answers: Faults

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: normal fault

answers: NDQ_003356

answers: strike-slip

answers: NDQ_003357

answers: Fault zones, fault belts and fault complexes typically describe assemblages of faults which have a common origin

answers: NDQ_003358

answers: normal fault

answers: NDQ_003359

answers: Strike-slip

answers: NDQ_003360

answers: faults.

answers: NDQ_003362

answers: normal faults at one time and as reverse or thrust faults at another

answers: NDQ_003363

answers: Fault Zones

answers: NDQ_003371

answers: Strike-slip faults

answers: NDQ_003373

answers: What is the term for a rock that is deeply buried?

answers: NDQ_003376

answers: List of faults affecting the rocks of Wales

answers: NDQ_003378

answers: What is the term for the movement of the ground in an earthquake?

answers: NDQ_003379

answers: Strike-slip faults

answers: NDQ_003380

answers: What is the term for a force applied to rock?

answers: NDQ_003381

answers: What is the term for a rock that deforms due to confining stress?

answers: NDQ_003382

answers: Compression is the most common stress at convergent plates.

answers: NDQ_003383

answers: What causes joints in rocks?

answers: NDQ_003384

answers: Syncline

answers: NDQ_003385

answers: Fault zones, fault belts and fault complexes

answers: NDQ_003386

answers: What is the main cause of earthquakes?

answers: NDQ_003387

answers: What are normal faults caused by?

answers: NDQ_003388

answers: Strike-slip faults result from what?

answers: NDQ_003389

answers: Fault zones, fault belts and fault complexes

answers: NDQ_003390

answers: Strike-slip

answers: NDQ_003391

answers: strike-slip

answers: NDQ_003392

answers: Strike-slip

answers: NDQ_003393

answers: strike-slip

answers: NDQ_003394

answers: normal faults

answers: NDQ_003395

answers: normal faults

answers: NDQ_003396

answers: strike-slip fault

answers: NDQ_003351

answers: strike-slip faults.

answers: NDQ_003352

answers: strike-slip faults.

answers: NDQ_003353

answers: geological faults

answers: NDQ_003354

answers: Fault zones, fault belts and fault complexes

answers: NDQ_003355

answers: thrusts

answers: NDQ_003356

answers: strike-slip faults.

answers: NDQ_003357

answers: alignments tend to be sub-parallel to one another.

answers: NDQ_003358

answers: normal faults,

answers: NDQ_003359

answers: strike-slip movement

answers: NDQ_003360

answers: geological faults

answers: NDQ_003362

answers: sub-parallel to one another.

answers: NDQ_003363

answers: geological faults

answers: NDQ_003371

answers: thrusts or thrust faults

answers: NDQ_003373

answers: faults

answers: NDQ_003376

answers: strike-slip faults.

answers: NDQ_003378

answers: strike-slip faults.

answers: NDQ_003379

answers: strike-slip faults.

answers: NDQ_003380

answers: faults

answers: NDQ_003381

answers: strike-slip faults.

answers: NDQ_003382

answers: strike-slip faults.

answers: NDQ_003383

answers: faults

answers: NDQ_003384

answers: strike-slip faults.

answers: NDQ_003385

answers: Fault zones, fault belts and fault complexes

answers: NDQ_003386

answers: faults

answers: NDQ_003387

answers: normal faults,

answers: NDQ_003388

answers: strike-slip faults.

answers: NDQ_003389

answers: geological faults

answers: NDQ_003390

answers: strike-slip faults.

answers: NDQ_003391

answers: strike-slip faults.

answers: NDQ_003392

answers: strike-slip faults.

answers: NDQ_003393

answers: strike-slip faults.

answers: NDQ_003394

answers: strike-slip faults.

answers: NDQ_003395

answers: strike-slip faults.

answers: NDQ_003396

answers: reverse faults,

text: If the Earth's crust was expanding along the oceanic ridges, Hess and Dietz reasoned like Holmes and others before them, it must be shrinking elsewhere. Hess followed Heezen, suggesting that new oceanic crust continuously spreads away from the ridges in a conveyor belt–like motion. And, using the mobilistic concepts developed before, he correctly concluded that many millions of years later, the oceanic crust eventually descends along the continental margins where oceanic trenches – very deep, narrow canyons – are formed, e.g. along the rim of the Pacific Ocean basin. The important step Hess made was that convection currents would be the driving force in this process, arriving at the same conclusions as Holmes had decades before with the only difference that the thinning of the ocean crust was performed using Heezen's mechanism of spreading along the ridges. Hess therefore concluded that the Atlantic Ocean was expanding while the Pacific Ocean was shrinking. As old oceanic crust is "consumed" in the trenches (like Holmes and others, he thought this was done by thickening of the continental lithosphere, not, as now understood, by underthrusting at a larger scale of the oceanic crust itself into the mantle), new magma rises and erupts along the spreading ridges to form new crust. In effect, the ocean basins are perpetually being "recycled," with the creation of new crust and the destruction of old oceanic lithosphere occurring simultaneously. Thus, the new mobilistic concepts neatly explained why the Earth does not get bigger with sea floor spreading, why there is so little sediment accumulation on the ocean floor, and why oceanic rocks are much younger than continental rocks.

text: If the Earth's crust was expanding along the oceanic ridges, Hess and Dietz reasoned like Holmes and others before them, it must be shrinking elsewhere. Hess followed Heezen, suggesting that new oceanic crust continuously spreads away from the ridges in a conveyor belt–like motion. And, using the mobilistic concepts developed before, he correctly concluded that many millions of years later, the oceanic crust eventually descends along the continental margins where oceanic trenches – very deep, narrow canyons – are formed, e.g. along

text: the rim of the Pacific Ocean basin

text: . The important step Hess made was that convection currents would be the driving force in this process, arriving at the same conclusions as Holmes had decades before with the only difference that the thinning of the ocean crust was performed using Heezen's mechanism of spreading along the ridges. Hess therefore concluded that the Atlantic Ocean was expanding while the

text: Pacific Ocean

text: was shrinking. As old oceanic crust is "consumed" in the trenches (like Holmes and others, he thought this was done by thickening of the continental lithosphere, not, as now understood, by underthrusting at a larger scale of the oceanic crust itself into the mantle), new magma rises and erupts along the spreading ridges to form new crust. In effect, the ocean basins are perpetually being "recycled," with the creation of new crust and the destruction of old oceanic lithosphere occurring simultaneously. Thus, the new mobilistic concepts neatly explained why the Earth does not get bigger with sea floor spreading, why there is so little sediment accumulation on the ocean floor, and why oceanic rocks are much younger than continental rocks.

answers: NDQ_003351

answers: convection currents

answers: NDQ_003352

answers: shrinks

answers: NDQ_003353

answers: magma to rise

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: oceanic trench

answers: NDQ_003356

answers: shrink

answers: NDQ_003357

answers: new magma rises and erupts along the spreading ridges to form new crust

answers: NDQ_003358

answers: oceanic trench

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: oceanic ridges

answers: NDQ_003362

answers: the Atlantic Ocean was expanding while the Pacific Ocean was shrinking

answers: NDQ_003363

answers: oceanic trenches

answers: NDQ_003371

answers: Why oceanic rocks are much younger than continental rocks

answers: NDQ_003373

answers: why oceanic rocks are much younger than continental rocks

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not an example of a stress?

answers: NDQ_003381

answers: What is the result of confining stress?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Why oceanic rocks are much younger than continental rocks?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: underthrusting at a larger scale

answers: NDQ_003387

answers: Which of the following is not a type of fault: normal faults are caused by compression stress?

answers: NDQ_003388

answers: Which of the following is not an example of a strike-slip fault?

answers: NDQ_003389

answers: oceanic trenches

answers: NDQ_003390

answers: oceanic trenches

answers: NDQ_003391

answers: oceanic trenches

answers: NDQ_003392

answers: oceanic trenches

answers: NDQ_003393

answers: oceanic trenches

answers: NDQ_003394

answers: subduction fault

answers: NDQ_003395

answers: oceanic trenches

answers: NDQ_003396

answers: oceanic trenches

answers: NDQ_003351

answers: convection currents

answers: NDQ_003352

answers: new magma

answers: NDQ_003353

answers: new magma

answers: NDQ_003354

answers: oceanic rocks are much younger than continental rocks.

answers: NDQ_003355

answers: oceanic trenches

answers: NDQ_003356

answers: new magma

answers: NDQ_003357

answers: new magma

answers: NDQ_003358

answers: oceanic trenches

answers: NDQ_003359

answers: underthrusting

answers: NDQ_003360

answers: spreading ridges

answers: NDQ_003362

answers: thickening of the continental lithosphere,

answers: NDQ_003363

answers: spreading ridges

answers: NDQ_003371

answers: oceanic rocks are much younger than continental rocks.

answers: NDQ_003373

answers: underthrusting

answers: NDQ_003376

answers: the ocean basins are perpetually being "recycled,"

answers: NDQ_003378

answers: new magma

answers: NDQ_003379

answers: new magma

answers: NDQ_003380

answers: underthrusting at a larger scale of the oceanic crust

answers: NDQ_003381

answers: underthrusting

answers: NDQ_003382

answers: new magma

answers: NDQ_003383

answers: underthrusting

answers: NDQ_003384

answers: spreading ridges

answers: NDQ_003385

answers: new magma

answers: NDQ_003386

answers: new magma

answers: NDQ_003387

answers: underthrusting

answers: NDQ_003388

answers: new magma

answers: NDQ_003389

answers: underthrusting

answers: NDQ_003390

answers: spreading ridges

answers: NDQ_003391

answers: oceanic trenches

answers: NDQ_003392

answers: trenches

answers: NDQ_003393

answers: oceanic trenches

answers: NDQ_003394

answers: underthrusting

answers: NDQ_003395

answers: the Earth does not get bigger

answers: NDQ_003396

answers: underthrusting

text: Pangea started to break up during the Triassic ~225Ma.  Rifting affected regions which became the central Atlantic (between North America and Africa) and the Gulf of Mexico at about the same time.  This rifting created a divergent plate margin that would play an integral role of the future geologic processes to follow.  Rifting which involves the stretching of pre-existing crust and mantle lithosphere was initiated by the existence of sufficient horizontal deviatoric tensional stress that broke the lithosphere. Eventually rifting gave way to sea floor spreading in the Atlantic and Gulf of Mexico in the mid Jurassic, around ~165 Ma.  Sea floor spreading is where new oceanic lithosphere is being created by upwelling of material, unlike rifting where it only involved the stretching of the crust.  Convection currents in the sub-lithospheric mantle are the driving mechanisms that caused sea floor spreading to occur.  New lithosphere is made when hot material beneath ocean ridges is brought to the surface by these cells.  As the new lithosphere moves horizontally away from the ridges, the new crust added to the Gulf of Mexico and the Atlantic caused the continents of North America and South America to be moved apart.  Seafloor spreading in the Gulf of Mexico ceased by the beginning of the Cretaceous and spreading shifted to the proto-Caribbean.

text: Pangea started to break up during the

text: Triassic

text: Rifting

text: affected regions which became the central Atlantic (between North America and Africa) and the Gulf of Mexico at about the same time.  This rifting created a

text: divergent plate

text: margin that would play an integral role of the future geologic processes to follow.

text: Rifting

text: which involves the stretching of pre-existing crust and mantle lithosphere was initiated by the existence of sufficient horizontal deviatoric tensional stress that broke the lithosphere. Eventually rifting gave way to

text: sea floor spreading

text: in the Atlantic and Gulf of Mexico in the mid

text: Jurassic

text: , around ~165 Ma.  Sea floor spreading is where new oceanic lithosphere is being created by

text: upwelling

text: of material, unlike rifting where it only involved the stretching of the crust.

text: Convection

text: currents in the sub-lithospheric mantle are the driving mechanisms that caused sea floor spreading to occur.  New lithosphere is made when hot material beneath ocean ridges is brought to the surface by these cells.  As the new

text: lithosphere

text: moves horizontally away from the ridges, the new crust added to the Gulf of Mexico and the Atlantic caused the continents of North America and South America to be moved apart.

text: Seafloor spreading

text: in the Gulf of Mexico ceased by the beginning of the Cretaceous and spreading shifted to the proto-Caribbean.

answers: NDQ_003351

answers: horizontal deviatoric

answers: NDQ_003352

answers: breaks apart

answers: NDQ_003353

answers: Rifting

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: ridge

answers: NDQ_003356

answers: stretch

answers: NDQ_003357

answers: Rifting involves the stretching of what?

answers: NDQ_003358

answers: rifting

answers: NDQ_003359

answers: deviatoric

answers: NDQ_003360

answers: Rifting

answers: NDQ_003362

answers: Seafloor spreading in the Gulf of Mexico ceased by the beginning of the Cretaceous

answers: NDQ_003363

answers: Pangea

answers: NDQ_003371

answers: Which happened first, rifting gave way to sea floor spreading in the Atlantic and Gulf of Mexico or spreading shifted to the proto-Caribbean?

answers: NDQ_003373

answers: Which of the following is not a type of stress: horizontal deviatoric tensional stress or compressive stresses?

answers: NDQ_003376

answers: Which happened first, rifting gave way to sea floor spreading in the Atlantic and Gulf of Mexico in the mid Jurassic, around  165 Ma.

answers: NDQ_003378

answers: What was created by upwelling of material?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: Which of the following is not an example of a stress?

answers: NDQ_003381

answers: Which of the following is not a type of stress: horizontal deviatoric tensional stress or convection currents?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Rifting which involves the stretching of pre-existing crust and mantle lithosphere

answers: NDQ_003384

answers: Which of the following is not a type of fold: syncline, ridge, or fold?

answers: NDQ_003385

answers: What is the name of the area where faults are clustered?

answers: NDQ_003386

answers: Rifting which involves the stretching of pre-existing crust

answers: NDQ_003387

answers: Which of the following is not a cause of normal faults: deviatoric tensional stress or compression stress?

answers: NDQ_003388

answers: Which of the following is not a result of shear stress: strike-slip faults, rifting, or upwelling?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: deviatoric

answers: NDQ_003391

answers: sea floor

answers: NDQ_003392

answers: deviatoric

answers: NDQ_003393

answers: sea floor

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: deviatoric

answers: NDQ_003396

answers: deviatoric

answers: NDQ_003351

answers: horizontal deviatoric tensional stress

answers: NDQ_003352

answers: broke the lithosphere.

answers: NDQ_003353

answers: stretching

answers: NDQ_003354

answers: Pangea started to break up during the Triassic

answers: NDQ_003355

answers: ridges

answers: NDQ_003356

answers: stretching

answers: NDQ_003357

answers: horizontal deviatoric tensional stress

answers: NDQ_003358

answers: rifting

answers: NDQ_003359

answers: horizontal deviatoric tensional stress

answers: NDQ_003360

answers: hot material beneath ocean ridges

answers: NDQ_003362

answers: North America and South America to be moved apart.

answers: NDQ_003363

answers: Pangea started to break up during the Triassic

answers: NDQ_003371

answers: Rifting

answers: NDQ_003373

answers: Rifting

answers: NDQ_003376

answers: Sea floor spreading

answers: NDQ_003378

answers: Rifting

answers: NDQ_003379

answers: horizontal

answers: NDQ_003380

answers: stretching

answers: NDQ_003381

answers: Rifting

answers: NDQ_003382

answers: horizontal deviatoric tensional stress

answers: NDQ_003383

answers: horizontal deviatoric tensional stress

answers: NDQ_003384

answers: ocean ridges

answers: NDQ_003385

answers: Rifting

answers: NDQ_003386

answers: Rifting

answers: NDQ_003387

answers: horizontal deviatoric tensional stress

answers: NDQ_003388

answers: horizontal deviatoric tensional stress

answers: NDQ_003389

answers: Sea floor spreading

answers: NDQ_003390

answers: Rifting

answers: NDQ_003391

answers: ocean ridges

answers: NDQ_003392

answers: Rifting

answers: NDQ_003393

answers: sea floor

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: horizontal deviatoric tensional stress

answers: NDQ_003396

answers: Rifting

text: The Marlborough Fault System consists of four main dominantly strike-slip fault strands, which together carry almost all of the displacement associated with the plate boundary. Other smaller faults form as splays of these main faults or accommodate deformation of the crust between them, such as the Newton and Hura Faults at the western end of the Hope Fault and the Jordan Thrust that formed the Seaward Kaikoura Range. The dextral strike-slip across this zone has also involved clockwise rotation of the intervening fault blocks of about 20° since the early Pliocene.

text: The Marlborough Fault System consists of four main dominantly strike-slip fault strands, which together carry almost all of the displacement associated with the plate boundary. Other smaller faults form as splays of these main faults or accommodate deformation of the crust between them, such as the Newton and Hura Faults at the western end of the Hope Fault and the Jordan Thrust that formed the

text: Seaward Kaikoura Range

text: . The dextral strike-slip across this zone has also involved clockwise rotation of the intervening fault blocks of about 20° since the early

text: Pliocene

answers: NDQ_003351

answers: strike-slip

answers: NDQ_003352

answers: deforms

answers: NDQ_003353

answers: displacement

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: splay

answers: NDQ_003356

answers: Rotate

answers: NDQ_003357

answers: deformation of the crust between them

answers: NDQ_003358

answers: dextral

answers: NDQ_003359

answers: deforms

answers: NDQ_003360

answers: plate boundary

answers: NDQ_003362

answers: clockwise rotation of the intervening fault blocks of about 20°

answers: NDQ_003363

answers: Marlborough Fault System

answers: NDQ_003371

answers: What type of fault is the Jordan Thrust?

answers: NDQ_003373

answers: What type of stresses does the Marlborough Fault System experience?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: displacement

answers: NDQ_003379

answers: no

answers: NDQ_003380

answers: What does the Marlborough Fault System consist of?

answers: NDQ_003381

answers: What type of stress does the Marlborough Fault System experience?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What type of fold does the Marlborough Fault System consist of?

answers: NDQ_003385

answers: Fault zone

answers: NDQ_003386

answers: What is the cause of earthquakes?

answers: NDQ_003387

answers: What type of stress is the Marlborough Fault System caused by?

answers: NDQ_003388

answers: What does the Marlborough Fault System consist of?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: strike-slip

answers: NDQ_003391

answers: fault blocks

answers: NDQ_003392

answers: strike-slip

answers: NDQ_003393

answers: strike-slip fault

answers: NDQ_003394

answers: dextral strike-slip

answers: NDQ_003395

answers: dextral strike-slip

answers: NDQ_003396

answers: dextral strike-slip

answers: NDQ_003351

answers: strike-slip

answers: NDQ_003352

answers: deformation

answers: NDQ_003353

answers: deformation

answers: NDQ_003354

answers: The Marlborough Fault System

answers: NDQ_003355

answers: Thrust

answers: NDQ_003356

answers: clockwise rotation

answers: NDQ_003357

answers: clockwise rotation of the intervening fault blocks of about 20°

answers: NDQ_003358

answers: dextral

answers: NDQ_003359

answers: deformation

answers: NDQ_003360

answers: plate boundary.

answers: NDQ_003362

answers: four main dominantly strike-slip fault strands,

answers: NDQ_003363

answers: Marlborough Fault System

answers: NDQ_003371

answers: Jordan Thrust

answers: NDQ_003373

answers: The Marlborough Fault System

answers: NDQ_003376

answers: Seaward Kaikoura Range.

answers: NDQ_003378

answers: displacement

answers: NDQ_003379

answers: 20°

answers: NDQ_003380

answers: deformation

answers: NDQ_003381

answers: deformation

answers: NDQ_003382

answers: strike-slip

answers: NDQ_003383

answers: deformation

answers: NDQ_003384

answers: 20° since the early Pliocene.

answers: NDQ_003385

answers: fault strands,

answers: NDQ_003386

answers: deformation

answers: NDQ_003387

answers: strike-slip

answers: NDQ_003388

answers: displacement associated with the plate boundary.

answers: NDQ_003389

answers: deformation

answers: NDQ_003390

answers: strike-slip

answers: NDQ_003391

answers: fault blocks

answers: NDQ_003392

answers: dextral strike-slip

answers: NDQ_003393

answers: fault blocks

answers: NDQ_003394

answers: dextral

answers: NDQ_003395

answers: dextral strike-slip

answers: NDQ_003396

answers: dextral

text: Aviation is a high-stress industry, given that it requires a high level of precision at all times.  Chronically high stress levels can ultimately decrease performance and compromise safety.  To be effective, stress measurement tools must be specific to the aviation industry, given its unique working environment and other stressors. Stress measurement in aviation seeks to quantify the psychological stress experienced by aviators, with the goal of making needed improvements to aviators' coping and stress management skills.

text: Aviation is a

text: high-stress industry

text: , given that it requires a high level of precision at all times.  Chronically high stress levels can ultimately decrease performance and compromise safety.  To be effective, stress measurement tools must be specific to the aviation industry, given its unique working environment and other

text: stressor

text: s. Stress measurement in aviation seeks to quantify the

text: psychological stress

text: experienced by

text: aviator

text: s, with the goal of making needed improvements to aviators'

text: coping

text: and stress management skills.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: stress to increase

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: decrease in size

answers: NDQ_003357

answers: stress levels can ultimately decrease performance

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's surface

answers: NDQ_003362

answers: it requires a high level of precision at all times

answers: NDQ_003363

answers: unanswerable

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: how would you describe compressive stresses?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What is the purpose of stress measurement?

answers: NDQ_003381

answers: Which of the following is not a result of confining stress: decrease performance and compromise safety

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: movement of rock at faults

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: normal faults or stress management skills?

answers: NDQ_003388

answers: Which of the following is not a stressor: Strike-slip faults or shear stress?

answers: NDQ_003389

answers: mountains ranges

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: dip-slip fault plane

answers: NDQ_003392

answers: a hanging wall

answers: NDQ_003393

answers: can ultimately decrease performance and compromise safety

answers: NDQ_003394

answers: can ultimately decrease performance and compromise safety

answers: NDQ_003395

answers: a vertical fault plane

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: psychological stress

answers: NDQ_003352

answers: Chronically high stress levels can ultimately decrease performance and compromise safety.

answers: NDQ_003353

answers: Chronically high stress levels

answers: NDQ_003354

answers: Aviation is a high-stress industry,

answers: NDQ_003355

answers: Aviation is a high-stress industry,

answers: NDQ_003356

answers: decrease performance and compromise safety.

answers: NDQ_003357

answers: safety.

answers: NDQ_003358

answers: Aviation is a high-stress industry,

answers: NDQ_003359

answers: Aviation is a high-stress industry,

answers: NDQ_003360

answers: Aviation is a high-stress

answers: NDQ_003362

answers: Aviation is a high-stress industry,

answers: NDQ_003363

answers: Aviation is a high-stress industry,

answers: NDQ_003371

answers: Aviation is a high-stress industry,

answers: NDQ_003373

answers: Aviation is a high-stress industry,

answers: NDQ_003376

answers: Aviation is a high-stress industry,

answers: NDQ_003378

answers: Aviation is a high-stress industry,

answers: NDQ_003379

answers: stress measurement tools must be specific to the aviation industry,

answers: NDQ_003380

answers: Aviation is a high-stress industry,

answers: NDQ_003381

answers: Chronically high stress levels can ultimately decrease performance and compromise safety.

answers: NDQ_003382

answers: Aviation is a high-stress industry,

answers: NDQ_003383

answers: Aviation

answers: NDQ_003384

answers: Aviation is a high-stress industry,

answers: NDQ_003385

answers: Aviation is a high-stress industry,

answers: NDQ_003386

answers: Aviation

answers: NDQ_003387

answers: Aviation is a high-stress industry,

answers: NDQ_003388

answers: Aviation is a high-stress industry,

answers: NDQ_003389

answers: Aviation is a high-stress industry,

answers: NDQ_003390

answers: precision at all times.

answers: NDQ_003391

answers: Aviation is a high-stress industry,

answers: NDQ_003392

answers: Aviation is a high-stress industry,

answers: NDQ_003393

answers: Aviation is a high-stress industry,

answers: NDQ_003394

answers: Aviation is a high-stress industry,

answers: NDQ_003395

answers: Aviation is a high-stress industry,

answers: NDQ_003396

answers: Aviation is a high-stress industry,

text: About  a fourth tectonic event occurred in the Lake Superior region. A hotspot of magma from the earth’s mantle beneath present-day Lake Superior rose, causing the crust to dome and break apart. This zone of crustal thinning and fracturing is the Midcontinent Rift System; it extends in a boomerang shape for over  from northeastern Kansas northward through Iowa, under the Twin Cities of Minnesota, beneath Lake Superior, and then south through the eastern Upper Peninsula of Michigan and beneath the central Lower Peninsula of Michigan. As the crust was being stretched thin and more magma flowed out from below, the center of the rift was continuously subsiding. The vast quantities of rising magma created a vacuum under the crust, the weight of the solidified magma on the surface caused the crust to subside into that vacuum so the edges of the rift tilted toward the center. The rifting stopped after a few million years; one reason could be that the Grenville orogeny stopped the rift process when that collision occurred. Subsidence continued for several million years after the lava flows had ceased; immense volumes of sediments – sand, gravel and mud – were eroded off the barren landscape into the still-sinking basin along the rift axis. As much as  of sedimentary rocks accumulated in the center before the sinking stopped and the region stabilized. A north-northeast trending branch of the Midcontinent Rift System separated the Animikie Basin into two distinct segments; the present-day Animikie Group and the Marquette Range Supergroup; the historical name for the Marquette Range Supergroup is the Animikie Series.

text: About  a fourth tectonic event occurred in the Lake Superior region. A

text: hotspot

text: of magma from the earth’s mantle beneath present-day Lake Superior rose, causing the crust to dome and break apart. This zone of crustal thinning and fracturing is the

text: Midcontinent Rift System

text: ; it extends in a boomerang shape for over  from northeastern Kansas northward through Iowa, under the Twin Cities of Minnesota, beneath Lake Superior, and then south through the eastern Upper Peninsula of Michigan and beneath the central Lower Peninsula of Michigan. As the crust was being stretched thin and more magma flowed out from below, the center of the rift was continuously

text: subsiding

text: . The vast quantities of rising magma created a vacuum under the crust, the weight of the solidified magma on the surface caused the crust to subside into that vacuum so the edges of the rift tilted toward the center. The rifting stopped after a few million years; one reason could be that the

text: Grenville orogeny

text: stopped the rift process when that collision occurred. Subsidence continued for several million years after the lava flows had ceased; immense volumes of sediments – sand, gravel and mud – were eroded off the barren landscape into the still-sinking basin along the rift axis. As much as  of sedimentary rocks accumulated in the center before the sinking stopped and the region stabilized. A north-northeast trending branch of the Midcontinent Rift System separated the Animikie Basin into two distinct segments; the present-day Animikie Group and the Marquette Range Supergroup; the historical name for the Marquette Range Supergroup is the Animikie Series.

answers: NDQ_003351

answers: weight of the solidified magma

answers: NDQ_003352

answers: sinks

answers: NDQ_003353

answers: Subsidence

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: rift

answers: NDQ_003356

answers: sink

answers: NDQ_003357

answers: a hotspot of magma from the earth’s mantle beneath present-day Lake Superior rose

answers: NDQ_003358

answers: rift

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: tectonic plates

answers: NDQ_003362

answers: Grenville orogeny stopped the rift process

answers: NDQ_003363

answers: Grenville orogeny

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: what is the last word in the passage?

answers: NDQ_003376

answers: Which of the following is not a type of terrain: basin-and-range or rifting?

answers: NDQ_003378

answers: What caused the crust to subside into that vacuum?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What caused the crust to subside?

answers: NDQ_003381

answers: What caused the crust to subside into that vacuum?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What caused the crust to dome and break apart?

answers: NDQ_003384

answers: What is the historical name for the Marquette Range Supergroup?

answers: NDQ_003385

answers: What is the Midcontinent Rift System?

answers: NDQ_003386

answers: Which of the following is not a cause of earthquakes?

answers: NDQ_003387

answers: What caused the crust to dome and break apart?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip faults, rift faults, or Animikie Series?

answers: NDQ_003389

answers: What is the Marquette Range Supergroup?

answers: NDQ_003390

answers: rifting

answers: NDQ_003391

answers: Animikie Group

answers: NDQ_003392

answers: rifting

answers: NDQ_003393

answers: Animikie Basin

answers: NDQ_003394

answers: north-northeast trending branch

answers: NDQ_003395

answers: A north-northeast trending branch

answers: NDQ_003396

answers: Grenville orogeny

answers: NDQ_003351

answers: the weight of the solidified magma

answers: NDQ_003352

answers: subsiding.

answers: NDQ_003353

answers: fracturing

answers: NDQ_003354

answers: enville orogeny

answers: NDQ_003355

answers: Animikie Group

answers: NDQ_003356

answers: subsiding.

answers: NDQ_003357

answers: Animikie Group and the Marquette Range Supergroup;

answers: NDQ_003358

answers: Animikie Group

answers: NDQ_003359

answers: magma

answers: NDQ_003360

answers: the rift process

answers: NDQ_003362

answers: Subsidence continued for several million years

answers: NDQ_003363

answers: Midcontinent Rift System

answers: NDQ_003371

answers: Animikie

answers: NDQ_003373

answers: the weight of the solidified magma

answers: NDQ_003376

answers: Subsidence

answers: NDQ_003378

answers: Subsidence

answers: NDQ_003379

answers: Animikie

answers: NDQ_003380

answers: the weight

answers: NDQ_003381

answers: Subsidence

answers: NDQ_003382

answers: Animikie Group

answers: NDQ_003383

answers: the weight of the solidified magma

answers: NDQ_003384

answers: Animikie Group

answers: NDQ_003385

answers: Midcontinent Rift System;

answers: NDQ_003386

answers: Midcontinent Rift System;

answers: NDQ_003387

answers: the weight of the solidified magma

answers: NDQ_003388

answers: Animikie Group

answers: NDQ_003389

answers: Midcontinent Rift

answers: NDQ_003390

answers: collision occurred.

answers: NDQ_003391

answers: Animikie Group

answers: NDQ_003392

answers: Animikie Group

answers: NDQ_003393

answers: Animikie Group

answers: NDQ_003394

answers: Midcontinent Rift System

answers: NDQ_003395

answers: Animikie Group and the Marquette Range Supergroup;

answers: NDQ_003396

answers: Midcontinent Rift System

text: The first event began 130 million years ago when a group of active volcanic islands approached a pre-existing continental margin and coastline of North America. These volcanic islands, known as the Insular Islands by geoscientists, were formed on a pre-existing tectonic plate called the Insular Plate by subduction of the former Farallon Plate to the west during the early Paleozoic era. This subduction zone records another subduction zone to the east under an ancient ocean basin between the Insular Islands and the former continental margin of North America called the Bridge River Ocean. This arrangement of two parallel subduction zones is unusual in that very few twin subduction zones exist on Earth; the Philippine Mobile Belt off the southeastern coast of Asia is an example of a modern twin subduction zone. As the Insular Plate drew closer to the pre-existing continental margin by ongoing subduction under the Bridge River Ocean, the Insular Islands drew closer to the former continental margin and coastline of western North America, supporting a pre-existing volcanic arc on the former continental margin of North America called the Omineca Arc. As the North American Plate drifted west and the Insular Plate drifted east to the old continental margin of western North America, the Bridge River Ocean eventually closed by ongoing subduction under the Bridge River Ocean. This subduction zone eventually jammed and shut down completely 115 million years ago, ending the Omineca Arc and the Insular Islands collided, forming the Insular Belt. Compression resulting from this collision crushed, fractured and folded rocks along the old continental margin. The Insular Belt then welded onto the pre-existing continental margin by magma that eventually cooled to create a large mass of igneous rock, creating a new continental margin. This large mass of igneous rock is the largest granite outcropping in North America.

text: The first event began 130 million years ago when a group of active volcanic islands approached a pre-existing

text: continental margin

text: and coastline of North America. These volcanic islands, known as the

text: Insular Islands

text: by geoscientists, were formed on a pre-existing

text: tectonic plate

text: called the

text: Insular Plate

text: by

text: subduction

text: of the former

text: Farallon Plate

text: to the west during the early

text: Paleozoic

text: era. This subduction zone records another subduction zone to the east under an ancient

text: ocean basin

text: between the Insular Islands and the former continental margin of North America called the

text: Bridge River Ocean

text: . This arrangement of two parallel subduction zones is unusual in that very few twin subduction zones exist on Earth; the

text: Philippine Mobile Belt

text: off the southeastern coast of

text: Asia

text: is an example of a modern twin subduction zone. As the Insular Plate drew closer to the pre-existing continental margin by ongoing subduction under the Bridge River Ocean, the Insular Islands drew closer to the former continental margin and coastline of western North America, supporting a pre-existing volcanic arc on the former continental margin of North America called the

text: Omineca Arc

text: . As the

text: North American Plate

text: drifted west and the Insular Plate drifted east to the old continental margin of western North America, the Bridge River Ocean eventually closed by ongoing subduction under the Bridge River Ocean. This subduction zone eventually jammed and shut down completely 115 million years ago, ending the Omineca Arc and the Insular Islands collided, forming the

text: Insular Belt

text: . Compression resulting from this collision crushed, fractured and

text: folded

text: rocks along the old continental margin. The Insular Belt then welded onto the pre-existing continental margin by magma that eventually cooled to create a large mass of

text: igneous rock

text: , creating a new continental margin. This large mass of igneous rock is the largest

text: granite

text: outcropping in North America.

answers: NDQ_003351

answers: subduction

answers: NDQ_003352

answers: compresses

answers: NDQ_003353

answers: crushed, fractured and folded rocks

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: Insular Belt

answers: NDQ_003356

answers: fold

answers: NDQ_003357

answers: The Insular Islands drew closer to the pre-existing continental margin and coastline of western North America

answers: NDQ_003358

answers: What is the largest granite outcropping in North America?

answers: NDQ_003359

answers: Compression results from this collision

answers: NDQ_003360

answers: tectonic plates

answers: NDQ_003362

answers: The Insular Islands drew closer to the pre-existing continental margin and coastline of western North America

answers: NDQ_003363

answers: 115 million years ago

answers: NDQ_003371

answers: What is the largest granite outcropping in North America?

answers: NDQ_003373

answers: What is the largest granite outcropping in North America?

answers: NDQ_003376

answers: What is the largest granite outcropping in North America?

answers: NDQ_003378

answers: How long ago did the first event begin?

answers: NDQ_003379

answers: Which of the following is not an example of a modern twin subduction zone?

answers: NDQ_003380

answers: What is the main idea of this passage?

answers: NDQ_003381

answers: How does the Insular Belt deform?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the main idea of this passage?

answers: NDQ_003384

answers: What is the largest granite outcropping in North America?

answers: NDQ_003385

answers: What is the name of the area where faults are clustered?

answers: NDQ_003386

answers: Which of the following is not a cause of earthquakes?

answers: NDQ_003387

answers: Which happened first, the Insular Islands collided or the Insular Islands collided?

answers: NDQ_003388

answers: Which of the following is not an example of a modern twin subduction zone?

answers: NDQ_003389

answers: What is the largest granite outcropping in North America?

answers: NDQ_003390

answers: subduction zone

answers: NDQ_003391

answers: the Insular Plate

answers: NDQ_003392

answers: subduction zone

answers: NDQ_003393

answers: the Insular Plate

answers: NDQ_003394

answers: parallel subduction zones

answers: NDQ_003395

answers: subduction zone

answers: NDQ_003396

answers: Twin subduction zone

answers: NDQ_003351

answers: subduction

answers: NDQ_003352

answers: crushed, fractured and folded

answers: NDQ_003353

answers: crushed, fractured and folded rocks

answers: NDQ_003354

answers: Omineca Arc.

answers: NDQ_003355

answers: Omineca Arc.

answers: NDQ_003356

answers: crushed, fractured and folded

answers: NDQ_003357

answers: Omineca Arc

answers: NDQ_003358

answers: Omineca Arc.

answers: NDQ_003359

answers: Compression

answers: NDQ_003360

answers: Omineca Arc.

answers: NDQ_003362

answers: Omineca Arc.

answers: NDQ_003363

answers: Omineca Arc.

answers: NDQ_003371

answers: Omineca Arc.

answers: NDQ_003373

answers: crushed, fractured and folded rocks

answers: NDQ_003376

answers: crushed, fractured and folded rocks

answers: NDQ_003378

answers: Omineca Arc.

answers: NDQ_003379

answers: Insular Islands

answers: NDQ_003380

answers: Compression

answers: NDQ_003381

answers: Compression resulting from this collision crushed, fractured and folded rocks

answers: NDQ_003382

answers: Insular Belt.

answers: NDQ_003383

answers: Compression

answers: NDQ_003384

answers: Omineca Arc.

answers: NDQ_003385

answers: Omineca Arc.

answers: NDQ_003386

answers: Compression

answers: NDQ_003387

answers: crushed, fractured and folded rocks

answers: NDQ_003388

answers: Omineca Arc.

answers: NDQ_003389

answers: Compression resulting from this collision crushed, fractured and folded rocks

answers: NDQ_003390

answers: Omineca Arc.

answers: NDQ_003391

answers: Insular Belt.

answers: NDQ_003392

answers: Omineca Arc.

answers: NDQ_003393

answers: granite outcropping

answers: NDQ_003394

answers: Omineca Arc.

answers: NDQ_003395

answers: Omineca Arc

answers: NDQ_003396

answers: Omineca Arc.

text: The Chuya Steppe in the Siberian Altai Mountains is a depression formed by tectonic movement of major faults in the Earths crust. The name Chuya Steppe comes from the large river which runs through the steppe, the Chuya River.

text: The Chuya Steppe in the

text: Siberian

text: Altai Mountains

text: is a depression formed by

text: tectonic

text: movement of major faults in the Earths crust. The name Chuya Steppe comes from the large river which runs through the

text: steppe

text: , the

text: Chuya River

answers: NDQ_003351

answers: tectonic

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: tectonic movement

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: steppe

answers: NDQ_003356

answers: change shape

answers: NDQ_003357

answers: tectonic movement of major faults occurs

answers: NDQ_003358

answers: steppe

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: The Chuya Steppe in the Siberian Altai Mountains is a depression formed by tectonic movement

answers: NDQ_003363

answers: tectonic movement

answers: NDQ_003371

answers: Which of the following is not a type of fault?

answers: NDQ_003373

answers: Why is the Chuya Steppe a depression?

answers: NDQ_003376

answers: what is the name of the large river which runs through the steppe?

answers: NDQ_003378

answers: What is the name of the large river which runs through the steppe?

answers: NDQ_003379

answers: What is the dip of the fault plane in a strike-slip fault?

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What is the name of the river that runs through the Chuya Steppe?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: What is the name of the large river which runs through the steppe?

answers: NDQ_003385

answers: what is the first word in the passage?

answers: NDQ_003386

answers: It's impossible to say

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: tectonic movement of major faults in the Earths crust?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip, strike-slip, or strike-slip?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: major faults

answers: NDQ_003391

answers: a depression

answers: NDQ_003392

answers: major faults

answers: NDQ_003393

answers: steppe

answers: NDQ_003394

answers: major faults

answers: NDQ_003395

answers: major faults

answers: NDQ_003396

answers: NDQ_003351

answers: tectonic movement of major faults

answers: NDQ_003352

answers: depression formed by tectonic movement of major faults

answers: NDQ_003353

answers: tectonic movement of major faults

answers: NDQ_003354

answers: The Chuya Steppe

answers: NDQ_003355

answers: depression

answers: NDQ_003356

answers: tectonic movement

answers: NDQ_003357

answers: tectonic movement of major faults in the Earths crust.

answers: NDQ_003358

answers: depression

answers: NDQ_003359

answers: tectonic movement

answers: NDQ_003360

answers: tectonic movement of major faults in the Earths crust.

answers: NDQ_003362

answers: The Chuya Steppe

answers: NDQ_003363

answers: tectonic movement of major faults in the Earths crust.

answers: NDQ_003371

answers: major faults

answers: NDQ_003373

answers: major faults in the Earths crust.

answers: NDQ_003376

answers: tectonic movement of major faults

answers: NDQ_003378

answers: tectonic movement

answers: NDQ_003379

answers: The Chuya Steppe

answers: NDQ_003380

answers: tectonic movement

answers: NDQ_003381

answers: tectonic movement of major faults

answers: NDQ_003382

answers: tectonic movement

answers: NDQ_003383

answers: tectonic movement

answers: NDQ_003384

answers: The Chuya Steppe

answers: NDQ_003385

answers: major faults

answers: NDQ_003386

answers: tectonic

answers: NDQ_003387

answers: tectonic movement of major faults in the Earths crust.

answers: NDQ_003388

answers: tectonic movement of major faults in the Earths crust.

answers: NDQ_003389

answers: tectonic movement of major faults

answers: NDQ_003390

answers: faults

answers: NDQ_003391

answers: depression

answers: NDQ_003392

answers: faults

answers: NDQ_003393

answers: The Chuya Steppe

answers: NDQ_003394

answers: faults

answers: NDQ_003395

answers: major faults

answers: NDQ_003396

answers: faults

text: The northern segment of the fault runs from Hollister, through the Santa Cruz Mountains, epicenter of the 1989 Loma Prieta earthquake, then up the San Francisco Peninsula, where it was first identified by Professor Lawson in 1895, then offshore at Daly City near Mussel Rock. This is the approximate location of the epicenter of the 1906 San Francisco earthquake. The fault returns onshore at Bolinas Lagoon just north of Stinson Beach in Marin County. It returns underwater through the linear trough of Tomales Bay which separates the Point Reyes Peninsula from the mainland, runs just east of the Bodega Heads through Bodega Bay and back underwater, returning onshore at Fort Ross. (In this region around the San Francisco Bay Area several significant "sister faults" run more-or-less parallel, and each of these can create significantly destructive earthquakes.)From Fort Ross the northern segment continues overland, forming in part a linear valley through which the Gualala River flows. It goes back offshore at Point Arena. After that, it runs underwater along the coast until it nears Cape Mendocino, where it begins to bend to the west, terminating at the Mendocino Triple Junction.

text: The northern segment of the fault runs from

text: Hollister

text: , through the

text: Santa Cruz Mountains

text: , epicenter of the

text: 1989 Loma Prieta earthquake

text: , then up the

text: San Francisco Peninsula

text: , where it was first identified by

text: Professor Lawson

text: in 1895, then offshore at

text: Daly City

text: near

text: Mussel Rock

text: . This is the approximate location of the epicenter of the

text: 1906 San Francisco earthquake

text: . The fault returns onshore at

text: Bolinas Lagoon

text: just north of

text: Stinson Beach

text: in

text: Marin County

text: . It returns underwater through the linear trough of

text: Tomales Bay

text: which separates the

text: Point Reyes Peninsula

text: from the mainland, runs just east of the Bodega Heads through Bodega Bay and back underwater, returning onshore at

text: Fort Ross

text: . (In this region around the

text: San Francisco Bay Area

text: several significant "sister faults" run more-or-less parallel, and each of these can create significantly destructive earthquakes.)From Fort Ross the northern segment continues overland, forming in part a linear valley through which the

text: Gualala River

text: flows. It goes back offshore at

text: Point Arena

text: . After that, it runs underwater along the coast until it nears

text: Cape Mendocino

text: , where it begins to bend to the west, terminating at the

text: Mendocino Triple Junction

answers: NDQ_003351

answers: underwater

answers: NDQ_003352

answers: bends

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: trough

answers: NDQ_003356

answers: bend to the west

answers: NDQ_003357

answers: The fault returns onshore at Bolinas Lagoon

answers: NDQ_003358

answers: epicenter

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: faults

answers: NDQ_003362

answers: The fault returns onshore at Bolinas Lagoon just north of Stinson Beach in Marin County

answers: NDQ_003363

answers: unanswerable

answers: NDQ_003371

answers: What is a thrust fault?

answers: NDQ_003373

answers: How would you describe a rock that is deeply buried?

answers: NDQ_003376

answers: Which of the following is not a type of terrain: basin-and-range or fault?

answers: NDQ_003378

answers: What is the approximate location of the epicenter of the 1906 San Francisco earthquake

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What can cause rock to deform?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: What is the cause of earthquakes?

answers: NDQ_003387

answers: What type of stress is caused by normal faults?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip faults, sister faults, or faults?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: the Mendocino Triple Junction

answers: NDQ_003391

answers: Mussel Rock

answers: NDQ_003392

answers: the Mendocino Triple Junction

answers: NDQ_003393

answers: Mussel Rock

answers: NDQ_003394

answers: trough

answers: NDQ_003395

answers: fault with a vertical fault plane

answers: NDQ_003396

answers: parallel fault

answers: NDQ_003351

answers: destructive earthquakes.)From

answers: NDQ_003352

answers: bend to the west,

answers: NDQ_003353

answers: a linear valley

answers: NDQ_003354

answers: Bolinas Lagoon

answers: NDQ_003355

answers: "sister faults"

answers: NDQ_003356

answers: destructive earthquakes.)From

answers: NDQ_003357

answers: Mendocino Triple Junction.

answers: NDQ_003358

answers: linear valley

answers: NDQ_003359

answers: faults"

answers: NDQ_003360

answers: faults"

answers: NDQ_003362

answers: 1989 Loma Prieta earthquake,

answers: NDQ_003363

answers: Santa Cruz Mountains,

answers: NDQ_003371

answers: Santa Cruz Mountains,

answers: NDQ_003373

answers: Mendocino Triple Junction.

answers: NDQ_003376

answers: linear valley

answers: NDQ_003378

answers: 1895,

answers: NDQ_003379

answers: Mendocino Triple Junction.

answers: NDQ_003380

answers: earthquakes.)From

answers: NDQ_003381

answers: Mendocino Triple Junction.

answers: NDQ_003382

answers: Mendocino Triple Junction.

answers: NDQ_003383

answers: Mendocino Triple Junction.

answers: NDQ_003384

answers: Mendocino Triple Junction.

answers: NDQ_003385

answers: parallel,

answers: NDQ_003386

answers: "sister faults"

answers: NDQ_003387

answers: Mendocino Triple Junction.

answers: NDQ_003388

answers: 1895,

answers: NDQ_003389

answers: Santa Cruz Mountains,

answers: NDQ_003390

answers: Mendocino Triple Junction.

answers: NDQ_003391

answers: Mussel Rock.

answers: NDQ_003392

answers: fault runs from Hollister, through the Santa Cruz Mountains,

answers: NDQ_003393

answers: Mussel Rock.

answers: NDQ_003394

answers: parallel,

answers: NDQ_003395

answers: Mendocino Triple Junction.

answers: NDQ_003396

answers: parallel,

text: All faults have a measurable thickness, made up of deformed rock characteristic of the level in the crust where the faulting happened, of the rock types affected by the fault and of the presence and nature of any mineralising fluids. Fault rocks are classified by their textures and the implied mechanism of deformation. A fault that passes through different levels of the lithosphere will have many different types of fault rock developed along its surface. Continued dip-slip displacement tends to juxtapose fault rocks characteristic of different crustal levels, with varying degrees of overprinting. This effect is particularly clear in the case of detachment faults and major thrust faults.

text: All faults have a measurable thickness, made up of deformed rock characteristic of the level in the crust where the faulting happened, of the rock types affected by the fault and of the presence and nature of any

text: mineralising fluids

text: . Fault rocks are classified by their

text: textures

text: and the implied mechanism of deformation. A fault that passes through different levels of the

text: lithosphere

text: will have many different types of fault rock developed along its surface. Continued dip-slip displacement tends to juxtapose fault rocks characteristic of different crustal levels, with varying degrees of overprinting. This effect is particularly clear in the case of

text: detachment fault

text: s and major

text: thrust fault

text: s.

answers: NDQ_003351

answers: dip-slip

answers: NDQ_003352

answers: deforms

answers: NDQ_003353

answers: deformation

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: dip-slip

answers: NDQ_003356

answers: varying degrees of overprinting

answers: NDQ_003357

answers: deformed rock characteristic of the level in the crust

answers: NDQ_003358

answers: detachment

answers: NDQ_003359

answers: deformed

answers: NDQ_003360

answers: faults

answers: NDQ_003362

answers: detachment faults and major thrust faults

answers: NDQ_003363

answers: faults

answers: NDQ_003371

answers: This effect is particularly clear in the case of detachment faults and major thrust faults

answers: NDQ_003373

answers: What type of rock is under compressive stresses?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: displacement

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What is the implied mechanism of deformation?

answers: NDQ_003381

answers: What is the implied mechanism of deformation?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the implied mechanism of deformation?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: Fault rocks are classified by their textures and the implied mechanism of deformation

answers: NDQ_003386

answers: Faulting

answers: NDQ_003387

answers: What is the implied mechanism of deformation?

answers: NDQ_003388

answers: What is the implied mechanism of deformation?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: detachment

answers: NDQ_003391

answers: deformed rock

answers: NDQ_003392

answers: major thrust faults

answers: NDQ_003393

answers: deformed rock

answers: NDQ_003394

answers: dip-slip

answers: NDQ_003395

answers: detachment faults

answers: NDQ_003396

answers: major thrust faults

answers: NDQ_003351

answers: dip-slip displacement

answers: NDQ_003352

answers: overprinting.

answers: NDQ_003353

answers: deformation.

answers: NDQ_003354

answers: detachment faults and major thrust faults.

answers: NDQ_003355

answers: detachment faults

answers: NDQ_003356

answers: juxtapose fault rocks characteristic of different crustal levels,

answers: NDQ_003357

answers: measurable thickness,

answers: NDQ_003358

answers: detachment faults

answers: NDQ_003359

answers: deformed rock characteristic of the level in the crust where the faulting happened,

answers: NDQ_003360

answers: faults

answers: NDQ_003362

answers: All faults have a measurable thickness,

answers: NDQ_003363

answers: thrust faults.

answers: NDQ_003371

answers: thrust faults.

answers: NDQ_003373

answers: detachment faults and major thrust faults.

answers: NDQ_003376

answers: detachment faults and major thrust faults.

answers: NDQ_003378

answers: dip-slip

answers: NDQ_003379

answers: dip-slip

answers: NDQ_003380

answers: deformation.

answers: NDQ_003381

answers: Fault rocks are classified by their textures and the implied mechanism of deformation.

answers: NDQ_003382

answers: detachment faults and major thrust faults.

answers: NDQ_003383

answers: deformation.

answers: NDQ_003384

answers: detachment faults and major thrust faults.

answers: NDQ_003385

answers: Continued dip-slip displacement tends to juxtapose fault rocks

answers: NDQ_003386

answers: dip-slip displacement

answers: NDQ_003387

answers: All faults have a measurable thickness,

answers: NDQ_003388

answers: dip-slip

answers: NDQ_003389

answers: faults

answers: NDQ_003390

answers: detachment faults

answers: NDQ_003391

answers: fault rocks characteristic of different crustal levels,

answers: NDQ_003392

answers: detachment faults

answers: NDQ_003393

answers: fault rocks characteristic of different crustal levels,

answers: NDQ_003394

answers: detachment faults and major thrust faults.

answers: NDQ_003395

answers: detachment faults and major thrust faults.

answers: NDQ_003396

answers: detachment faults and major thrust faults.

text: An essential feature of many cells is their ability to migrate towards certain mechanical (Durotaxis) or chemical (Chemotaxis) stimuli. Cell migration takes place through the concerted action of three Rho family GTPases: Rho, Rac, and Cdc42. When GTP-bound, Rac will cause the formation of lamellipodia, and Cdc42 will cause the formation of filopodia, thus promoting cell migration. In the migrating cell, there are three main types of stress fibers: ventral stress fibers, transverse arcs, and dorsal stress fibers.  Ventral stress fibers are associated with focal adhesions at both ends, are located on the ventral surface of the cell, and function in adhesion and contraction. Transverse arcs are not directly linked to focal adhesions, and typically flow from the leading edge of the cell, back towards the cell centre. Dorsal stress fibers are located at the trailing edge of the cell. They attach to focal adhesions on the ventral surface of the trailing edge, and extend dorsally, towards the cell centre to attach to transverse arcs. During cell migration, actin filaments within stress fibers will be recycled by a process of retrograde actin flow. The mechanism of dissolution of the focal adhesion itself is poorly understood.

text: An essential feature of many cells is their ability to migrate towards certain mechanical (

text: Durotaxis

text: ) or chemical (

text: Chemotaxis

text: ) stimuli. Cell migration takes place through the concerted action of three Rho family GTPases: Rho, Rac, and Cdc42. When GTP-bound, Rac will cause the formation of

text: lamellipodia

text: , and Cdc42 will cause the formation of

text: filopodia

text: , thus promoting cell migration. In the migrating cell, there are three main types of stress fibers: ventral stress fibers, transverse arcs, and dorsal stress fibers.  Ventral stress fibers are associated with focal adhesions at both ends, are located on the ventral surface of the cell, and function in adhesion and contraction. Transverse arcs are not directly linked to focal adhesions, and typically flow from the leading edge of the cell, back towards the cell centre. Dorsal stress fibers are located at the trailing edge of the cell. They attach to focal adhesions on the ventral surface of the trailing edge, and extend dorsally, towards the cell centre to attach to transverse arcs. During cell migration, actin filaments within stress fibers will be recycled by a process of

text: retrograde actin flow

text: . The mechanism of dissolution of the focal adhesion itself is poorly understood.

answers: NDQ_003351

answers: transverse arcs

answers: NDQ_003352

answers: does not migrate

answers: NDQ_003353

answers: contraction

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: lamellipodia

answers: NDQ_003356

answers: migrate towards certain mechanical

answers: NDQ_003357

answers: actin filaments within stress fibers will be recycled by a process of retrograde actin flow

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: fault lines

answers: NDQ_003362

answers: The mechanism of dissolution of the focal adhesion itself is poorly understood

answers: NDQ_003363

answers: the same time

answers: NDQ_003371

answers: What is a thrust fault?

answers: NDQ_003373

answers: None of the above choices.

answers: NDQ_003376

answers: basin-and-range

answers: NDQ_003378

answers: Dorsal stress fibers

answers: NDQ_003379

answers: vertical

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: How does rock deform?

answers: NDQ_003382

answers: Ventral stress fibers

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: Fault zone

answers: NDQ_003386

answers: transverse arcs

answers: NDQ_003387

answers: Which of the following is not a type of stress fiber?

answers: NDQ_003388

answers: What are the three main types of stress fibers?

answers: NDQ_003389

answers: poorly understood

answers: NDQ_003390

answers: Dorsal stress fibers

answers: NDQ_003391

answers: dip-slip fault

answers: NDQ_003392

answers: Dorsal stress fibers

answers: NDQ_003393

answers: dip-slip fault

answers: NDQ_003394

answers: transverse

answers: NDQ_003395

answers: transverse arcs

answers: NDQ_003396

answers: transverse

answers: NDQ_003351

answers: (Durotaxis)

answers: NDQ_003352

answers: poorly understood.

answers: NDQ_003353

answers: contraction.

answers: NDQ_003354

answers: Dorsal stress fibers

answers: NDQ_003355

answers: (Durotaxis)

answers: NDQ_003356

answers: cells

answers: NDQ_003357

answers: Rac will cause the formation of lamellipodia,

answers: NDQ_003358

answers: (Durotaxis)

answers: NDQ_003359

answers: cells

answers: NDQ_003360

answers: stress fibers:

answers: NDQ_003362

answers: Transverse arcs are not directly linked to focal adhesions,

answers: NDQ_003363

answers: cells is their ability to migrate towards certain mechanical (Durotaxis)

answers: NDQ_003371

answers: Dorsal stress fibers

answers: NDQ_003373

answers: Dorsal stress fibers

answers: NDQ_003376

answers: stress fibers:

answers: NDQ_003378

answers: Dorsal stress fibers

answers: NDQ_003379

answers: Dorsal stress fibers

answers: NDQ_003380

answers: stress fibers:

answers: NDQ_003381

answers: cells

answers: NDQ_003382

answers: contraction.

answers: NDQ_003383

answers: adhesion and contraction.

answers: NDQ_003384

answers: Transverse arcs

answers: NDQ_003385

answers: three main types of stress fibers: ventral stress fibers,

answers: NDQ_003386

answers: three main types of stress fibers:

answers: NDQ_003387

answers: contraction.

answers: NDQ_003388

answers: Dorsal stress fibers

answers: NDQ_003389

answers: retrograde actin flow.

answers: NDQ_003390

answers: (Durotaxis)

answers: NDQ_003391

answers: Dorsal stress fibers

answers: NDQ_003392

answers: (Durotaxis)

answers: NDQ_003393

answers: Dorsal stress fibers

answers: NDQ_003394

answers: Transverse arcs

answers: NDQ_003395

answers: Transverse arcs

answers: NDQ_003396

answers: (Durotaxis)

text: The orogeny affected adjacent regions of northern Minnesota and Ontario in the Superior province as well as the Slave and the eastern part of the Nain province, a far wider region of influence than in subsequent orogenies. It is the earliest datable orogeny in North America and brought the Archean Eon to a close. The end of the Archean Eon marks a major change in the development of the Earth’s crust: the crust was essentially formed and achieved thicknesses of about  under the continents.

text: The orogeny affected adjacent regions of northern Minnesota and Ontario in the

text: Superior province

text: as well as the

text: Slave

text: and the eastern part of the

text: Nain province

text: , a far wider region of influence than in subsequent orogenies. It is the earliest datable orogeny in North America and brought the Archean Eon to a close. The end of the Archean Eon marks a major change in the development of the

text: Earth’s crust

text: : the crust was essentially formed and achieved thicknesses of about  under the continents.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: thickens

answers: NDQ_003353

answers: thicknesses to increase

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: orogeny

answers: NDQ_003356

answers: thicken

answers: NDQ_003357

answers: a far wider region of influence than in subsequent orogenies

answers: NDQ_003358

answers: orogeny

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Archean Eon

answers: NDQ_003362

answers: It is the earliest datable orogeny in North America

answers: NDQ_003363

answers: Archean Eon

answers: NDQ_003371

answers: What is the first orogeny in North America?

answers: NDQ_003373

answers: What is the earliest datable orogeny in North America

answers: NDQ_003376

answers: what is the earliest datable orogeny in North America

answers: NDQ_003378

answers: what is the first orogeny mentioned?

answers: NDQ_003379

answers: What is the earliest datable orogeny in North America?

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What is the first orogeny in North America?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the earliest datable orogeny in North America?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: what is the earliest datable orogeny in North America

answers: NDQ_003386

answers: Which of the following is not a cause of earthquakes?

answers: NDQ_003387

answers: What is the earliest datable orogeny in North America and brought the Archean Eon to a close

answers: NDQ_003388

answers: What is the earliest datable orogeny in North America?

answers: NDQ_003389

answers: What is the earliest datable orogeny?

answers: NDQ_003390

answers: Superior province

answers: NDQ_003391

answers: Superior province

answers: NDQ_003392

answers: orogeny

answers: NDQ_003393

answers: Superior province

answers: NDQ_003394

answers: lateral

answers: NDQ_003395

answers: a vertical fault plane

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: Archean Eon

answers: NDQ_003352

answers: thicknesses

answers: NDQ_003353

answers: thicknesses

answers: NDQ_003354

answers: earliest datable orogeny in North America

answers: NDQ_003355

answers: orogenies.

answers: NDQ_003356

answers: under the continents.

answers: NDQ_003357

answers: under the continents.

answers: NDQ_003358

answers: orogenies.

answers: NDQ_003359

answers: The orogeny

answers: NDQ_003360

answers: The orogeny

answers: NDQ_003362

answers: under the continents.

answers: NDQ_003363

answers: Archean Eon

answers: NDQ_003371

answers: The orogeny

answers: NDQ_003373

answers: under the continents.

answers: NDQ_003376

answers: The orogeny

answers: NDQ_003378

answers: The orogeny affected adjacent regions of northern Minnesota

answers: NDQ_003379

answers: Archean Eon

answers: NDQ_003380

answers: Archean Eon

answers: NDQ_003381

answers: under the continents.

answers: NDQ_003382

answers: Archean Eon

answers: NDQ_003383

answers: The orogeny

answers: NDQ_003384

answers: Archean Eon

answers: NDQ_003385

answers: orogenies.

answers: NDQ_003386

answers: The orogeny

answers: NDQ_003387

answers: The orogeny

answers: NDQ_003388

answers: The orogeny affected adjacent regions of northern Minnesota

answers: NDQ_003389

answers: the crust was essentially formed

answers: NDQ_003390

answers: The orogeny

answers: NDQ_003391

answers: under the continents.

answers: NDQ_003392

answers: The orogeny

answers: NDQ_003393

answers: under the continents.

answers: NDQ_003394

answers: Slave and the eastern part of the Nain province,

answers: NDQ_003395

answers: The orogeny

answers: NDQ_003396

answers: subsequent orogenies.

text: In 2004, work began just north of Parkfield on the San Andreas Fault Observatory at Depth (SAFOD).  The goal of SAFOD is to drill a hole nearly 2.5 miles (4 kilometers) into the Earth's crust, across the San Andreas Fault. The specific target of the probe was a patch of fault known to generate sequences of repeating microearthquakes of around magnitude 1.0. The drilling was completed in the midyear of 2005, and an array of sensors was installed to capture and record earthquakes that happen near this area. It is hoped that SAFOD observations will provide insight into the source mechanisms of these small earthquakes, which can be scaled up in an effort to understand larger events. The drilling discovered a mineral called serpentinite at the site of origin of 2004 earthquake. Serpentinite can transform into talc, a very soft mineral, thus facilitating easy slippage of plates. It has been hypothesized that aseismic creep at Hollister is also due to the presence of serpentinite. No drilling has been done at Hollister to confirm this.

text: In 2004, work began just north of Parkfield on the

text: San Andreas Fault Observatory at Depth

text: (SAFOD).  The goal of SAFOD is to drill a hole nearly 2.5 miles (4 kilometers) into the Earth's crust, across the San Andreas Fault. The specific target of the probe was a patch of fault known to generate sequences of repeating microearthquakes of around magnitude 1.0. The drilling was completed in the midyear of 2005, and an array of sensors was installed to capture and record earthquakes that happen near this area. It is hoped that SAFOD observations will provide insight into the source mechanisms of these small earthquakes, which can be scaled up in an effort to understand larger events. The drilling discovered a mineral called

text: serpentinite

text: at the site of origin of 2004 earthquake.

text: Serpentinite

text: can transform into

text: talc

text: , a very soft mineral, thus facilitating easy slippage of plates. It has been hypothesized that aseismic creep at

text: Hollister

text: is also due to the presence of

text: serpentinite

text: . No drilling has been done at

text: Hollister

text: to confirm this.

answers: NDQ_003351

answers: talc

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: slippage of plates

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: slip

answers: NDQ_003357

answers: Serpentinite can transform into what?

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: slippage of plates

answers: NDQ_003360

answers: San Andreas fault

answers: NDQ_003362

answers: No drilling has been done at Hollister to confirm this.

answers: NDQ_003363

answers: San Andreas Fault

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: What is the purpose of drilling a hole nearly 2.5 miles

answers: NDQ_003376

answers: What type of terrain is caused by compressive forces?

answers: NDQ_003378

answers: Creep

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What can transform into talc?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: slippage of plates

answers: NDQ_003387

answers: What type of stress does the San Andreas Fault cause?

answers: NDQ_003388

answers: What type of faults result from shear stress?

answers: NDQ_003389

answers: folds

answers: NDQ_003390

answers: San Andreas Fault

answers: NDQ_003391

answers: San Andreas Fault

answers: NDQ_003392

answers: San Andreas Fault

answers: NDQ_003393

answers: San Andreas Fault

answers: NDQ_003394

answers: San Andreas Fault

answers: NDQ_003395

answers: San Andreas Fault

answers: NDQ_003396

answers: San Andreas Fault

answers: NDQ_003351

answers: slippage

answers: NDQ_003352

answers: talc, a very soft mineral,

answers: NDQ_003353

answers: slippage of plates.

answers: NDQ_003354

answers: serpentinite

answers: NDQ_003355

answers: creep

answers: NDQ_003356

answers: easy slippage of plates.

answers: NDQ_003357

answers: slippage of plates.

answers: NDQ_003358

answers: aseismic creep

answers: NDQ_003359

answers: slippage of plates.

answers: NDQ_003360

answers: San Andreas Fault.

answers: NDQ_003362

answers: No drilling has been done at Hollister to confirm this.

answers: NDQ_003363

answers: San Andreas Fault.

answers: NDQ_003371

answers: serpentinite

answers: NDQ_003373

answers: easy slippage of plates.

answers: NDQ_003376

answers: serpentinite

answers: NDQ_003378

answers: creep

answers: NDQ_003379

answers: serpentinite

answers: NDQ_003380

answers: slippage of plates.

answers: NDQ_003381

answers: slippage of plates.

answers: NDQ_003382

answers: slippage

answers: NDQ_003383

answers: slippage of plates.

answers: NDQ_003384

answers: serpentinite

answers: NDQ_003385

answers: San Andreas Fault.

answers: NDQ_003386

answers: slippage of plates.

answers: NDQ_003387

answers: serpentinite

answers: NDQ_003388

answers: serpentinite

answers: NDQ_003389

answers: slippage of plates.

answers: NDQ_003390

answers: San Andreas Fault

answers: NDQ_003391

answers: serpentinite

answers: NDQ_003392

answers: San Andreas Fault

answers: NDQ_003393

answers: serpentinite

answers: NDQ_003394

answers: San Andreas Fault

answers: NDQ_003395

answers: San Andreas Fault.

answers: NDQ_003396

answers: San Andreas Fault

text: The fault cut the basin into two pieces and moved the pieces apart. It is found on the east side of the fault in western San Francisco and northern San Mateo County. On the west side of the fault it was carried  north to the Bolinas headlands of western Marin County.

text: The fault cut the basin into two pieces and moved the pieces apart. It is found on the east side of the fault in western

text: San Francisco

text: and northern

text: San Mateo County

text: . On the west side of the fault it was carried  north to the

text: Bolinas

text: headlands of western

text: Marin County

answers: NDQ_003351

answers: lateral

answers: NDQ_003352

answers: moves faster

answers: NDQ_003353

answers: movement

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: fault

answers: NDQ_003356

answers: move apart

answers: NDQ_003357

answers: San Francisco is on the west side of the fault.

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: breaks apart

answers: NDQ_003360

answers: faults

answers: NDQ_003362

answers: It cut the basin into two pieces and moved the pieces apart.

answers: NDQ_003363

answers: San Francisco

answers: NDQ_003371

answers: Which of the following is not a type of fault?

answers: NDQ_003373

answers: How would you describe the rock?

answers: NDQ_003376

answers: Which of the following is not a type of terrain?

answers: NDQ_003378

answers: Which of the following is not a type of earthquake?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: Which of the following is not a type of stress?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not a type of fold?

answers: NDQ_003385

answers: what is the first word in the passage?

answers: NDQ_003386

answers: It's impossible to say

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: San Francisco or Marin County?

answers: NDQ_003388

answers: Which of the following is not an example of a strike-slip fault?

answers: NDQ_003389

answers: It is not possible to tell

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: a basin

answers: NDQ_003392

answers: unanswerable

answers: NDQ_003393

answers: a basin

answers: NDQ_003394

answers: San Francisco

answers: NDQ_003395

answers: San Francisco and northern San Mateo

answers: NDQ_003396

answers: southwestern San Francisco

answers: NDQ_003351

answers: The fault cut the basin into two pieces

answers: NDQ_003352

answers: moved the pieces apart.

answers: NDQ_003353

answers: moved the pieces apart.

answers: NDQ_003354

answers: Bolinas headlands of western Marin County.

answers: NDQ_003355

answers: The fault

answers: NDQ_003356

answers: The fault cut the basin into two pieces and moved the pieces apart.

answers: NDQ_003357

answers: cut the basin into two pieces and moved the pieces apart.

answers: NDQ_003358

answers: headlands

answers: NDQ_003359

answers: The fault cut the basin into two pieces and moved the pieces apart.

answers: NDQ_003360

answers: The fault

answers: NDQ_003362

answers: The fault cut the basin into two pieces

answers: NDQ_003363

answers: The fault cut the basin into two pieces

answers: NDQ_003371

answers: The fault

answers: NDQ_003373

answers: The fault

answers: NDQ_003376

answers: The fault cut the basin into two pieces and moved the pieces apart.

answers: NDQ_003378

answers: moved the pieces apart.

answers: NDQ_003379

answers: San Mateo County.

answers: NDQ_003380

answers: The fault cut the basin into two pieces

answers: NDQ_003381

answers: The fault cut the basin into two pieces and moved the pieces apart.

answers: NDQ_003382

answers: Bolinas headlands of western Marin County.

answers: NDQ_003383

answers: moved the pieces apart.

answers: NDQ_003384

answers: Bolinas headlands of western Marin County.

answers: NDQ_003385

answers: fault in western San Francisco and northern San Mateo County.

answers: NDQ_003386

answers: The fault cut the basin into two pieces and moved the pieces apart.

answers: NDQ_003387

answers: The fault cut the basin into two pieces

answers: NDQ_003388

answers: The fault cut the basin into two pieces and moved the pieces apart.

answers: NDQ_003389

answers: The fault cut the basin into two pieces

answers: NDQ_003390

answers: The fault cut the basin into two pieces

answers: NDQ_003391

answers: basin

answers: NDQ_003392

answers: The fault cut the basin into two pieces

answers: NDQ_003393

answers: Bolinas headlands

answers: NDQ_003394

answers: San Mateo County.

answers: NDQ_003395

answers: San Mateo County.

answers: NDQ_003396

answers: San Mateo County.

text: The Tsetserleg earthquake is believed to be a strike-slip rupture of a branch of the Bolnai Fault, extending about 190 km. The fault displacement during the earthquake was greater than 5 m, and the duration is estimated at about one minute. However, this interpretation is contested; field surveys after the earthquake show a complex rupture not necessarily characteristic of a strike-slip mechanism.

text: The Tsetserleg earthquake is believed to be a strike-slip rupture of a branch of the Bolnai Fault, extending about 190 km. The fault displacement during the earthquake was greater than 5 m, and the duration is estimated at about one minute. However, this interpretation is contested; field surveys after the earthquake show a complex rupture not necessarily characteristic of a strike-slip mechanism.

answers: NDQ_003351

answers: strike-slip

answers: NDQ_003352

answers: more likely to crack

answers: NDQ_003353

answers: displacement

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: strike-slip

answers: NDQ_003356

answers: strike

answers: NDQ_003357

answers: a strike-slip mechanism is a type of

answers: NDQ_003358

answers: strike-slip

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: faults

answers: NDQ_003362

answers: a complex rupture not necessarily characteristic of a strike-slip mechanism

answers: NDQ_003363

answers: Bolnai Fault

answers: NDQ_003371

answers: Which of the following is not a type of strike-slip mechanism: strike-slip, strike-slip rupture, or thrust fault?

answers: NDQ_003373

answers: How would you describe the Tsetserleg earthquake?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: no

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What type of stress does the Bolnai Fault experience?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What type of fold is the Bolnai Fault?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: yes

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: strike-slip rupture or normal faults?

answers: NDQ_003388

answers: What is the cause of the Tsetserleg earthquake?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: Bolnai Fault

answers: NDQ_003391

answers: strike-slip rupture

answers: NDQ_003392

answers: Bolnai Fault

answers: NDQ_003393

answers: strike-slip rupture

answers: NDQ_003394

answers: Bolnai Fault

answers: NDQ_003395

answers: Bolnai Fault

answers: NDQ_003396

answers: Bolnai Fault

answers: NDQ_003351

answers: strike-slip

answers: NDQ_003352

answers: displacement

answers: NDQ_003353

answers: fault displacement

answers: NDQ_003354

answers: Bolnai Fault,

answers: NDQ_003355

answers: Bolnai Fault,

answers: NDQ_003356

answers: strike-slip

answers: NDQ_003357

answers: displacement during the earthquake was greater than 5 m,

answers: NDQ_003358

answers: strike-slip

answers: NDQ_003359

answers: strike-slip

answers: NDQ_003360

answers: Bolnai Fault,

answers: NDQ_003362

answers: a complex rupture not necessarily characteristic of a strike-slip mechanism.

answers: NDQ_003363

answers: Bolnai Fault,

answers: NDQ_003371

answers: Bolnai Fault,

answers: NDQ_003373

answers: Bolnai Fault,

answers: NDQ_003376

answers: 190 km.

answers: NDQ_003378

answers: displacement

answers: NDQ_003379

answers: strike-slip mechanism.

answers: NDQ_003380

answers: strike-slip

answers: NDQ_003381

answers: strike-slip mechanism.

answers: NDQ_003382

answers: strike-slip

answers: NDQ_003383

answers: strike-slip

answers: NDQ_003384

answers: Bolnai Fault,

answers: NDQ_003385

answers: Bolnai Fault,

answers: NDQ_003386

answers: strike-slip

answers: NDQ_003387

answers: strike-slip

answers: NDQ_003388

answers: strike-slip mechanism.

answers: NDQ_003389

answers: Bolnai Fault,

answers: NDQ_003390

answers: Bolnai Fault,

answers: NDQ_003391

answers: Bolnai Fault,

answers: NDQ_003392

answers: Bolnai Fault,

answers: NDQ_003393

answers: strike-slip

answers: NDQ_003394

answers: Bolnai Fault,

answers: NDQ_003395

answers: Bolnai Fault,

answers: NDQ_003396

answers: Bolnai Fault,

text: Final Fantasy IX takes place primarily on the four continents of a world named Gaia. Most of Gaia's population reside on the Mist Continent, named so because the entire continent is blanketed in thick Mist. Lands outside the Mist Continent—the Outer, Lost and Forgotten continents—are uncharted territories not explored until midway through the game. Several locations on the parallel world of Terra and the dream land of Memoria round out the game's areas. The Mist Continent features four nations: Alexandria, Lindblum, Burmecia, and Cleyra. Alexandria is a kingdom to the northeast of the Mist Continent ruled by a monarchy located in Alexandria Castle. The technologically advanced Lindblum, ruled by a regent, is nestled on a plateau to the southwest where airships regularly fly by. The Kingdom of Burmecia, whose capital is showered by eternal rain is to the northwest and nearby to the isolated Cleyran civilisation, which is nestled in a giant tree in the desert, protected by a powerful sandstorm. Treno, a large, perpetually dark city, heavily populated by both aristocrats and paupers, is located on the southeast part of the continent. The Mist Continent is extremely mountainous resulting in a natural barrier between many of the ruling nations.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: more likely to crack

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: vertical fold

answers: NDQ_003356

answers: swell

answers: NDQ_003357

answers: The Kingdom of Burmecia is showered by eternal rain

answers: NDQ_003358

answers: plateau

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: The Mist Continent

answers: NDQ_003362

answers: uncharted territories not explored until midway through the game

answers: NDQ_003363

answers: The Mist Continent

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: Why is the Mist Continent blanketed in thick Mist

answers: NDQ_003376

answers: What is the Mist Continent?

answers: NDQ_003378

answers: How many nations does the Mist Continent feature?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What is a natural barrier between many of the ruling nations?

answers: NDQ_003381

answers: What is the natural barrier between many of the ruling nations?

answers: NDQ_003382

answers: What is the name of the Kingdom of Burmecia?

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is the name of the mountainous resulting in a natural barrier between many of the ruling nations?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: What is the cause of earthquakes?

answers: NDQ_003387

answers: What are normal faults caused by?

answers: NDQ_003388

answers: What does the Mist Continent consist of?

answers: NDQ_003389

answers: The Mist Continent

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: natural barrier between many of the ruling nations

answers: NDQ_003392

answers: a natural barrier

answers: NDQ_003393

answers: a plateau

answers: NDQ_003394

answers: The Mist Continent is extremely mountainous

answers: NDQ_003395

answers: natural barrier between many of the ruling nations.

answers: NDQ_003396

answers: The Mist Continent

answers: NDQ_003351

answers: sandstorm.

answers: NDQ_003352

answers: The Mist Continent is extremely mountainous

answers: NDQ_003353

answers: mountainous

answers: NDQ_003354

answers: The Mist Continent is extremely mountainous

answers: NDQ_003355

answers: plateau

answers: NDQ_003356

answers: Mist.

answers: NDQ_003357

answers: The Mist Continent is extremely mountainous

answers: NDQ_003358

answers: desert,

answers: NDQ_003359

answers: a powerful sandstorm.

answers: NDQ_003360

answers: The Mist Continent

answers: NDQ_003362

answers: eternal rain

answers: NDQ_003363

answers: The Mist Continent

answers: NDQ_003371

answers: The Mist Continent is extremely mountainous

answers: NDQ_003373

answers: giant tree in the desert, protected by a powerful sandstorm.

answers: NDQ_003376

answers: mountainous

answers: NDQ_003378

answers: Mist.

answers: NDQ_003379

answers: southwest

answers: NDQ_003380

answers: sandstorm.

answers: NDQ_003381

answers: The Mist Continent is extremely mountainous

answers: NDQ_003382

answers: sandstorm.

answers: NDQ_003383

answers: The Mist Continent is extremely mountainous

answers: NDQ_003384

answers: plateau to the southwest

answers: NDQ_003385

answers: Mist Continent,

answers: NDQ_003386

answers: The Mist Continent is extremely mountainous

answers: NDQ_003387

answers: sandstorm.

answers: NDQ_003388

answers: The Mist Continent is extremely mountainous

answers: NDQ_003389

answers: The Mist Continent is extremely mountainous

answers: NDQ_003390

answers: mountainous

answers: NDQ_003391

answers: giant tree

answers: NDQ_003392

answers: Final Fantasy IX

answers: NDQ_003393

answers: giant tree

answers: NDQ_003394

answers: The Mist Continent is extremely mountainous

answers: NDQ_003395

answers: The Mist Continent is extremely mountainous

answers: NDQ_003396

answers: The Mist Continent is extremely mountainous

text: In the past several decades, the most popular fault model used in practice is the single stuck-at fault model. In this model, one of the signal lines in a circuit is assumed to be stuck at a fixed logic value, regardless of what inputs are supplied to the circuit. Hence, if a circuit has n signal lines, there are potentially 2n stuck-at faults defined on the circuit, of which some can be viewed as being equivalent to others. The stuck-at fault model is a logical fault model because no delay information is associated with the fault definition. It is also called a permanent fault model because the faulty effect is assumed to be permanent, in contrast to intermittent faults which occur (seemingly) at random and transient faults which occur sporadically, perhaps depending on operating conditions (e.g. temperature, power supply voltage) or on the data values (high or low voltage states) on surrounding signal lines. The single stuck-at fault model is structural because it is defined based on a structural gate-level circuit model.

text: In the past several decades, the most popular fault model used in practice is the single

text: stuck-at fault

text: model. In this model, one of the signal lines in a circuit is assumed to be stuck at a fixed logic value, regardless of what inputs are supplied to the circuit. Hence, if a circuit has n signal lines, there are potentially 2n stuck-at faults defined on the circuit, of which some can be viewed as being equivalent to others. The stuck-at fault model is a logical fault model because no delay information is associated with the fault definition. It is also called a permanent fault model because the faulty effect is assumed to be permanent, in contrast to intermittent faults which occur (seemingly) at random and transient faults which occur sporadically, perhaps depending on operating conditions (e.g. temperature, power supply voltage) or on the data values (high or low voltage states) on surrounding signal lines. The single stuck-at fault model is structural because it is defined based on a structural gate-level circuit model.

answers: NDQ_003351

answers: permanent

answers: NDQ_003352

answers: is more likely to crack

answers: NDQ_003353

answers: permanent faults

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: stick

answers: NDQ_003357

answers: one of the signal lines in a circuit is assumed to be stuck at a fixed logic value

answers: NDQ_003358

answers: permanent fault

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: continental plates

answers: NDQ_003362

answers: the faulty effect is assumed to be permanent

answers: NDQ_003363

answers: unanswerable

answers: NDQ_003371

answers: What is the most popular fault model used in practice

answers: NDQ_003373

answers: the stuck-at fault model

answers: NDQ_003376

answers: basin-and-range

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What is the most popular fault model used in practice

answers: NDQ_003381

answers: What is the most popular fault model used in practice

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: what is the most popular fault model used in practice

answers: NDQ_003386

answers: Faults are the cause of earthquakes

answers: NDQ_003387

answers: What is the most popular fault model used in practice?

answers: NDQ_003388

answers: What is the most popular fault model used in practice?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: transient faults

answers: NDQ_003391

answers: a permanent fault model

answers: NDQ_003392

answers: stuck-at fault

answers: NDQ_003393

answers: a permanent fault model

answers: NDQ_003394

answers: transient faults

answers: NDQ_003395

answers: stuck-at fault model

answers: NDQ_003396

answers: transient faults which occur sporadically

answers: NDQ_003351

answers: intermittent faults

answers: NDQ_003352

answers: single stuck-at fault model.

answers: NDQ_003353

answers: permanent, in contrast to intermittent faults

answers: NDQ_003354

answers: single stuck-at fault model.

answers: NDQ_003355

answers: n

answers: NDQ_003356

answers: permanent, in contrast to intermittent faults

answers: NDQ_003357

answers: permanent,

answers: NDQ_003358

answers: intermittent faults

answers: NDQ_003359

answers: single stuck-at fault model.

answers: NDQ_003360

answers: single stuck-at fault model.

answers: NDQ_003362

answers: intermittent faults which occur (seemingly) at random

answers: NDQ_003363

answers: single stuck-at fault model.

answers: NDQ_003371

answers: single stuck-at fault model.

answers: NDQ_003373

answers: single stuck-at fault model.

answers: NDQ_003376

answers: single stuck-at fault model.

answers: NDQ_003378

answers: single stuck-at fault model.

answers: NDQ_003379

answers: single stuck-at fault model.

answers: NDQ_003380

answers: single stuck-at fault model.

answers: NDQ_003381

answers: single stuck-at fault model.

answers: NDQ_003382

answers: single stuck-at fault model.

answers: NDQ_003383

answers: single stuck-at fault model.

answers: NDQ_003384

answers: single stuck-at fault model.

answers: NDQ_003385

answers: 2n stuck-at faults

answers: NDQ_003386

answers: intermittent faults

answers: NDQ_003387

answers: permanent,

answers: NDQ_003388

answers: single stuck-at fault model.

answers: NDQ_003389

answers: single stuck-at fault model.

answers: NDQ_003390

answers: single stuck-at fault model.

answers: NDQ_003391

answers: single stuck-at fault model.

answers: NDQ_003392

answers: single stuck-at fault model.

answers: NDQ_003393

answers: single stuck-at fault model.

answers: NDQ_003394

answers: intermittent faults

answers: NDQ_003395

answers: single stuck-at fault model.

answers: NDQ_003396

answers: intermittent faults

text: The oldest rocks in New Zealand date from mid Cambrian times (510 Ma), although there are older rocks in the Auckland Islands.  The lower (basement) rocks are divided into the "Western Province", consisting mainly of granite and gneiss, and an "Eastern Province", consisting mainly of greywacke and schist.  The provinces are further divided into terranes – large slices of crust with different geological histories that have been brought together by tectonic activity (subduction and strike-slip faulting) to form New Zealand.

text: The oldest rocks in New Zealand date from mid

text: Cambrian

text: times (510 Ma), although there are older rocks in the

text: Auckland Islands

text: .  The lower (basement) rocks are divided into the "Western Province", consisting mainly of

text: granite

text: and

text: gneiss

text: , and an "Eastern Province", consisting mainly of

text: greywacke

text: and

text: schist

text: .  The provinces are further divided into

text: terranes

text: – large slices of crust with different geological histories that have been brought together by tectonic activity (

text: subduction

text: and

text: strike-slip faulting

text: ) to form New Zealand.

answers: NDQ_003351

answers: subduction

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: strike-slip faulting

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: terranes

answers: NDQ_003356

answers: subduct

answers: NDQ_003357

answers: large slices of crust with different geological histories have been brought together

answers: NDQ_003358

answers: strike-slip

answers: NDQ_003359

answers: subducts

answers: NDQ_003360

answers: tectonic activity

answers: NDQ_003362

answers: unanswerable

answers: NDQ_003363

answers: subduction

answers: NDQ_003371

answers: Which of the following is not a type of fault: strike-slip faulting, strike-slip faulting or strike-slip faulting?

answers: NDQ_003373

answers: How would you describe the lower (basement) rocks?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What type of force applied to rock is a stress?

answers: NDQ_003381

answers: What type of stress do the oldest rocks in New Zealand have?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a type of stress: subduction and strike-slip faulting

answers: NDQ_003384

answers: Which of the following is not a type of fold that arches upward?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: Which of the following is not a cause of earthquakes: strike-slip faulting

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: subduction and strike-slip faulting?

answers: NDQ_003388

answers: Which of the following is not a type of tectonic activity: subduction and strike-slip faulting?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: strike-slip

answers: NDQ_003391

answers: terranes

answers: NDQ_003392

answers: strike-slip faulting

answers: NDQ_003393

answers: terranes

answers: NDQ_003394

answers: strike-slip

answers: NDQ_003395

answers: strike-slip faulting

answers: NDQ_003396

answers: strike-slip

answers: NDQ_003351

answers: strike-slip faulting)

answers: NDQ_003352

answers: strike-slip faulting)

answers: NDQ_003353

answers: strike-slip faulting)

answers: NDQ_003354

answers: (510 Ma), although there are older rocks in the Auckland Islands.

answers: NDQ_003355

answers: strike-slip faulting)

answers: NDQ_003356

answers: (subduction and strike-slip faulting) to form New Zealand.

answers: NDQ_003357

answers: strike-slip

answers: NDQ_003358

answers: terranes

answers: NDQ_003359

answers: tectonic activity (subduction and strike-slip faulting)

answers: NDQ_003360

answers: tectonic activity

answers: NDQ_003362

answers: (subduction and strike-slip faulting) to form New Zealand.

answers: NDQ_003363

answers: (subduction and strike-slip faulting)

answers: NDQ_003371

answers: strike-slip faulting)

answers: NDQ_003373

answers: (subduction and strike-slip faulting)

answers: NDQ_003376

answers: tectonic activity

answers: NDQ_003378

answers: strike-slip

answers: NDQ_003379

answers: strike-slip faulting) to form New Zealand.

answers: NDQ_003380

answers: tectonic activity

answers: NDQ_003381

answers: (subduction and strike-slip faulting) to form New Zealand.

answers: NDQ_003382

answers: (subduction and strike-slip faulting)

answers: NDQ_003383

answers: tectonic activity

answers: NDQ_003384

answers: terranes

answers: NDQ_003385

answers: strike-slip faulting)

answers: NDQ_003386

answers: tectonic activity (subduction and strike-slip faulting)

answers: NDQ_003387

answers: strike-slip faulting)

answers: NDQ_003388

answers: strike-slip faulting) to form New Zealand.

answers: NDQ_003389

answers: tectonic activity

answers: NDQ_003390

answers: strike-slip

answers: NDQ_003391

answers: terranes

answers: NDQ_003392

answers: strike-slip

answers: NDQ_003393

answers: terranes

answers: NDQ_003394

answers: strike-slip

answers: NDQ_003395

answers: strike-slip

answers: NDQ_003396

answers: strike-slip

text: Current genetic research has demonstrated that humans on the African continent are the most genetically diverse. There is more human genetic diversity in Africa than anywhere else on Earth. The genetic structure of Africans was traced to 14 ancestral population clusters. Human genetic diversity decreases in native populations with migratory distance from Africa and this is thought to be the result of bottlenecks during human migration. Humans have lived in Africa for the longest time, which has allowed accumulation of a higher diversity of genetic mutations in these populations. Only part of Africa's population migrated out of the continent, bringing just part of the original African genetic variety with them. African populations harbor genetic alleles that are not found in other places of the world. All the common alleles found in populations outside of Africa are found on the African continent.

text: Current genetic research has demonstrated that humans on the

text: African continent

text: are the most genetically diverse. There is more human genetic diversity in Africa than anywhere else on Earth. The genetic structure of Africans was traced to 14 ancestral population clusters. Human genetic diversity decreases in native populations with migratory distance from Africa and this is thought to be the result of

text: bottleneck

text: s during human migration. Humans have lived in Africa for the longest time, which has allowed accumulation of a higher diversity of genetic mutations in these populations. Only part of Africa's population migrated out of the continent, bringing just part of the original African genetic variety with them. African populations harbor genetic alleles that are not found in other places of the world. All the common alleles found in populations outside of Africa are found on the African continent.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: mutations

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: human genetic diversity decreases in native populations with migratory

answers: NDQ_003358

answers: rockfall

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: continents

answers: NDQ_003362

answers: humans on the African continent are the most genetically diverse

answers: NDQ_003363

answers: Africa

answers: NDQ_003371

answers: Which of the following is not the result of bottlenecks during human migration?

answers: NDQ_003373

answers: How would you describe a rock under compressive stresses?

answers: NDQ_003376

answers: what is the last word in the passage?

answers: NDQ_003378

answers: The amount the ground moves in an earthquake is called slip.

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What is the result of bottlenecks during human migration?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not the cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not the result of bottlenecks during human migration?

answers: NDQ_003385

answers: Which of the following is not a type of population cluster?

answers: NDQ_003386

answers: Which of the following is not a cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not the result of bottlenecks during human migration?

answers: NDQ_003388

answers: What is the most common alleles found in populations outside of Africa?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: The hanging wall drops down relative to the footwall

answers: NDQ_003391

answers: dip-slip fault plane

answers: NDQ_003392

answers: a fault

answers: NDQ_003393

answers: dip-slip fault plane

answers: NDQ_003394

answers: is a

answers: NDQ_003395

answers: is a

answers: NDQ_003396

answers: NDQ_003351

answers: bottlenecks

answers: NDQ_003352

answers: migratory distance from Africa

answers: NDQ_003353

answers: genetic mutations

answers: NDQ_003354

answers: There is more human genetic diversity in Africa than anywhere else on Earth.

answers: NDQ_003355

answers: migratory distance from Africa

answers: NDQ_003356

answers: migratory distance from Africa

answers: NDQ_003357

answers: migratory distance from Africa

answers: NDQ_003358

answers: bottlenecks

answers: NDQ_003359

answers: bottlenecks during human migration.

answers: NDQ_003360

answers: African continent

answers: NDQ_003362

answers: humans on the African continent are the most genetically diverse.

answers: NDQ_003363

answers: Africa

answers: NDQ_003371

answers: bottlenecks

answers: NDQ_003373

answers: migratory distance from Africa

answers: NDQ_003376

answers: bottlenecks

answers: NDQ_003378

answers: migratory distance from Africa

answers: NDQ_003379

answers: Africa

answers: NDQ_003380

answers: migratory distance from Africa

answers: NDQ_003381

answers: bottlenecks

answers: NDQ_003382

answers: bottlenecks

answers: NDQ_003383

answers: migratory distance from Africa

answers: NDQ_003384

answers: migratory distance from Africa

answers: NDQ_003385

answers: 14 ancestral population clusters.

answers: NDQ_003386

answers: migratory distance from Africa

answers: NDQ_003387

answers: migratory distance from Africa

answers: NDQ_003388

answers: migratory distance from Africa

answers: NDQ_003389

answers: migrated out of the continent,

answers: NDQ_003390

answers: migratory distance from Africa

answers: NDQ_003391

answers: migratory distance from Africa

answers: NDQ_003392

answers: migratory distance from Africa

answers: NDQ_003393

answers: migratory distance from Africa

answers: NDQ_003394

answers: migratory distance from Africa

answers: NDQ_003395

answers: migratory distance from Africa

answers: NDQ_003396

answers: Africa

text: Where rock units slide past one another, strike-slip faults develop in shallow regions, and become shear zones at deeper depths where the rocks deform ductilely.

text: Where rock units slide past one another,

text: strike-slip fault

text: s develop in shallow regions, and become

text: shear zone

text: s at deeper depths where the rocks deform ductilely.

answers: NDQ_003351

answers: shear

answers: NDQ_003352

answers: deforms

answers: NDQ_003353

answers: shear zones

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: shear zone

answers: NDQ_003356

answers: slide past one another

answers: NDQ_003357

answers: rock units slide past one another

answers: NDQ_003358

answers: shear zone

answers: NDQ_003359

answers: deforms

answers: NDQ_003360

answers: tectonic plates

answers: NDQ_003362

answers: The San Andreas fault is not a shear zone.

answers: NDQ_003363

answers: shear zones

answers: NDQ_003371

answers: Which of the following is not a type of fault?

answers: NDQ_003373

answers: Yes

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: no

answers: NDQ_003380

answers: Which of the following is not a stress?

answers: NDQ_003381

answers: Which of the following is not a type of stress: strike-slip faults, shear zones or ductilely?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not the cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not a type of fold?

answers: NDQ_003385

answers: yes

answers: NDQ_003386

answers: yes

answers: NDQ_003387

answers: Which of the following is not a type of normal fault?

answers: NDQ_003388

answers: no

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: strike-slip fault

answers: NDQ_003391

answers: is a shear zone

answers: NDQ_003392

answers: strike-slip fault

answers: NDQ_003393

answers: is a shear zone

answers: NDQ_003394

answers: lateral fault

answers: NDQ_003395

answers: strike-slip fault

answers: NDQ_003396

answers: strike-slip

answers: NDQ_003351

answers: strike-slip faults

answers: NDQ_003352

answers: deform ductilely.

answers: NDQ_003353

answers: deform ductilely.

answers: NDQ_003354

answers: Where rock units slide past one another, strike-slip faults

answers: NDQ_003355

answers: strike-slip faults

answers: NDQ_003356

answers: shear zones

answers: NDQ_003357

answers: rock units slide past one another,

answers: NDQ_003358

answers: shear zones

answers: NDQ_003359

answers: rock units slide past one another,

answers: NDQ_003360

answers: strike-slip faults

answers: NDQ_003362

answers: strike-slip faults develop in shallow regions,

answers: NDQ_003363

answers: strike-slip faults

answers: NDQ_003371

answers: strike-slip faults

answers: NDQ_003373

answers: shear zones

answers: NDQ_003376

answers: strike-slip faults

answers: NDQ_003378

answers: strike-slip faults

answers: NDQ_003379

answers: strike-slip faults

answers: NDQ_003380

answers: ductilely.

answers: NDQ_003381

answers: ductilely.

answers: NDQ_003382

answers: shear zones

answers: NDQ_003383

answers: the rocks deform ductilely.

answers: NDQ_003384

answers: shear zones

answers: NDQ_003385

answers: shear zones

answers: NDQ_003386

answers: strike-slip faults

answers: NDQ_003387

answers: strike-slip faults

answers: NDQ_003388

answers: Where rock units slide past one another, strike-slip faults

answers: NDQ_003389

answers: rock units slide past one another, strike-slip faults

answers: NDQ_003390

answers: strike-slip faults

answers: NDQ_003391

answers: shear zones

answers: NDQ_003392

answers: strike-slip faults

answers: NDQ_003393

answers: shear zones

answers: NDQ_003394

answers: strike-slip faults

answers: NDQ_003395

answers: strike-slip faults

answers: NDQ_003396

answers: strike-slip faults

text: The subducting basalt and sediment are normally rich in hydrous minerals and clays.  Additionally, large quantities of water are introduced into cracks and fractures created as the subducting slab bends downward. During the transition from basalt to eclogite, these hydrous materials break down, producing copious quantities of water, which at such great pressure and temperature exists as a supercritical fluid. The supercritical water, which is hot and more buoyant than the surrounding rock, rises into the overlying mantle where it lowers the pressure in (and thus the melting temperature of) the mantle rock to the point of actual melting, generating magma. The magmas, in turn, rise because they are less dense than the rocks of the mantle. The mantle-derived magmas (which are basaltic in composition) can continue to rise, ultimately to Earth's surface, resulting in a volcanic eruption. The chemical composition of the erupting lava depends upon the degree to which the mantle-derived basalt interacts with (melts) Earth's crust and/or undergoes fractional crystallization.

text: The subducting basalt and sediment are normally rich in

text: hydrous

text: minerals and clays.  Additionally, large quantities of water are introduced into cracks and fractures created as the subducting slab bends downward. During the transition from basalt to eclogite, these hydrous materials break down, producing copious quantities of water, which at such great pressure and temperature exists as a

text: supercritical fluid

text: . The supercritical water, which is hot and more buoyant than the surrounding rock, rises into the overlying mantle where it lowers the pressure in (and thus the melting temperature of) the mantle rock to the point of actual melting, generating

text: magma

text: . The magmas, in turn, rise because they are less dense than the rocks of the mantle. The mantle-derived magmas (which are basaltic in composition) can continue to rise, ultimately to Earth's surface, resulting in a volcanic eruption. The chemical composition of the erupting lava depends upon the degree to which the mantle-derived basalt interacts with (melts) Earth's crust and/or undergoes

text: fractional crystallization

answers: NDQ_003351

answers: subducting

answers: NDQ_003352

answers: melts

answers: NDQ_003353

answers: cracks and fractures

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: subducting slab

answers: NDQ_003356

answers: produce magma

answers: NDQ_003357

answers: large quantities of water are introduced into cracks and fractures

answers: NDQ_003358

answers: crack

answers: NDQ_003359

answers: subducting

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: mantle-derived magmas can continue to rise, ultimately to Earth's surface

answers: NDQ_003363

answers: subducting basalt

answers: NDQ_003371

answers: Which of the following is not a type of rock: basalt, magma, or sediment?

answers: NDQ_003373

answers: Why is the rock under compressive stresses?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What does the subducting slab bend downward?

answers: NDQ_003381

answers: What does the subducting slab bend downward?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the subducting slab bends downward?

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: subducting slab bends downward

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: normal faults or magma?

answers: NDQ_003388

answers: Which of the following is not a type of strike-slip fault: strike-slip, strike-slip, or strike-slip?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: subducting slab

answers: NDQ_003391

answers: slab

answers: NDQ_003392

answers: subducting slab

answers: NDQ_003393

answers: slab

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: subducting slab

answers: NDQ_003396

answers: horizontal

answers: NDQ_003351

answers: subducting slab bends downward.

answers: NDQ_003352

answers: melting, generating magma.

answers: NDQ_003353

answers: cracks and fractures

answers: NDQ_003354

answers: The subducting basalt

answers: NDQ_003355

answers: subducting slab

answers: NDQ_003356

answers: cracks and fractures

answers: NDQ_003357

answers: large quantities of water are introduced into cracks and fractures

answers: NDQ_003358

answers: cracks and fractures

answers: NDQ_003359

answers: cracks and fractures created as the subducting slab bends downward.

answers: NDQ_003360

answers: subducting basalt

answers: NDQ_003362

answers: melting,

answers: NDQ_003363

answers: subducting basalt

answers: NDQ_003371

answers: large quantities of water are introduced into cracks and fractures

answers: NDQ_003373

answers: large quantities of water are introduced into cracks and fractures

answers: NDQ_003376

answers: cracks and fractures

answers: NDQ_003378

answers: downward.

answers: NDQ_003379

answers: downward.

answers: NDQ_003380

answers: cracks and fractures

answers: NDQ_003381

answers: cracks and fractures

answers: NDQ_003382

answers: supercritical fluid.

answers: NDQ_003383

answers: cracks and fractures

answers: NDQ_003384

answers: volcanic eruption.

answers: NDQ_003385

answers: supercritical fluid.

answers: NDQ_003386

answers: subducting slab bends downward.

answers: NDQ_003387

answers: large quantities of water are introduced into cracks and fractures

answers: NDQ_003388

answers: water are introduced into cracks and fractures

answers: NDQ_003389

answers: subducting slab bends downward.

answers: NDQ_003390

answers: cracks and fractures

answers: NDQ_003391

answers: basalt

answers: NDQ_003392

answers: cracks and fractures

answers: NDQ_003393

answers: basalt

answers: NDQ_003394

answers: downward.

answers: NDQ_003395

answers: subducting slab bends downward.

answers: NDQ_003396

answers: downward.

text: The geology of Armenia was shaped by geological upheaval pushed up the Earth's crust to form the Armenian Plateau 25 million years ago. This created the complex topography of Armenia.

text: The geology of Armenia was shaped by geological upheaval pushed up the

text: Earth's crust

text: to form the

text: Armenian Plateau

text: 25 million years ago. This created the complex

text: topography

text: of Armenia.

answers: NDQ_003351

answers: uniaxial

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: upheaval

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: Plateau

answers: NDQ_003356

answers: change shape

answers: NDQ_003357

answers: geological upheaval pushes up the Earth's crust

answers: NDQ_003358

answers: Plateau

answers: NDQ_003359

answers: is pushed up

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: The San Andreas fault is a fault in the Earth's crust

answers: NDQ_003363

answers: 25 million years ago

answers: NDQ_003371

answers: Which of the following is not a type of geological upheaval?

answers: NDQ_003373

answers: How would you describe Armenian Plateau?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: what is the last word in the passage?

answers: NDQ_003379

answers: Which of the following is not a type of fault?

answers: NDQ_003380

answers: Which of the following is not a stress?

answers: NDQ_003381

answers: What would happen if the Armenian Plateau was pushed up?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not an example of a fold that arches upward?

answers: NDQ_003385

answers: Which of the following is not a type of fault?

answers: NDQ_003386

answers: Which of the following is not a cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not a cause of normal faults?

answers: NDQ_003388

answers: Which of the following is not a result of shear stress: strike-slip faults or Armenian Plateau?

answers: NDQ_003389

answers: It's impossible to say

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: Armenian Plateau

answers: NDQ_003392

answers: unanswerable

answers: NDQ_003393

answers: Armenian Plateau

answers: NDQ_003394

answers: isobath

answers: NDQ_003395

answers: unanswerable

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: geological upheaval

answers: NDQ_003352

answers: pushed up the Earth's crust

answers: NDQ_003353

answers: geological upheaval

answers: NDQ_003354

answers: Armenian Plateau

answers: NDQ_003355

answers: Armenian Plateau

answers: NDQ_003356

answers: Armenian Plateau

answers: NDQ_003357

answers: pushed up the Earth's crust

answers: NDQ_003358

answers: Armenian Plateau

answers: NDQ_003359

answers: geological upheaval

answers: NDQ_003360

answers: geological upheaval pushed up the Earth's crust

answers: NDQ_003362

answers: 25 million years ago.

answers: NDQ_003363

answers: Armenian Plateau

answers: NDQ_003371

answers: geological upheaval

answers: NDQ_003373

answers: The geology of Armenia was shaped by geological upheaval

answers: NDQ_003376

answers: Armenian Plateau

answers: NDQ_003378

answers: geological upheaval

answers: NDQ_003379

answers: Armenian Plateau

answers: NDQ_003380

answers: geological upheaval

answers: NDQ_003381

answers: geological upheaval

answers: NDQ_003382

answers: geological upheaval

answers: NDQ_003383

answers: geological upheaval

answers: NDQ_003384

answers: Armenian Plateau

answers: NDQ_003385

answers: geological upheaval

answers: NDQ_003386

answers: geological upheaval

answers: NDQ_003387

answers: geological upheaval

answers: NDQ_003388

answers: geological upheaval

answers: NDQ_003389

answers: geological upheaval

answers: NDQ_003390

answers: geological upheaval

answers: NDQ_003391

answers: Armenian Plateau

answers: NDQ_003392

answers: geological upheaval

answers: NDQ_003393

answers: Armenian Plateau

answers: NDQ_003394

answers: geological upheaval

answers: NDQ_003395

answers: geological upheaval

answers: NDQ_003396

answers: geological upheaval

text: The process by which cratons are formed from early rock is called cratonization. The first large cratonic landmasses formed during the Archean eon. During the early Archean, Earth's heat flow was nearly three times higher than it is today because of the greater concentration of radioactive isotopes and the residual heat from the Earth's accretion. There was considerably greater tectonic and volcanic activity; the mantle was less viscous and the crust thinner. This resulted in rapid formation of oceanic crust at ridges and hot spots, and rapid recycling of oceanic crust at subduction zones. There are at least three hypotheses of how cratons have been formed:  1) surface crust was thickened by a rising plume of deep molten material, 2) successive subducting plates of oceanic lithosphere became lodged beneath a proto-craton in an under-plating process, 3) accretion from island arcs or continental fragments rafting together to thicken into a craton.

text: The process by which cratons are formed from early rock is called cratonization. The first large cratonic landmasses formed during the

text: Archean

text: eon. During the early Archean, Earth's heat flow was nearly three times higher than it is today because of the greater concentration of radioactive isotopes and the residual heat from the Earth's

text: accretion

text: . There was considerably greater

text: tectonic

text: and

text: volcanic

text: activity; the

text: mantle

text: was less viscous and the crust thinner. This resulted in rapid formation of

text: oceanic crust

text: at ridges and

text: hot spots

text: , and rapid

text: recycling of oceanic crust

text: at

text: subduction

text: zones. There are at least three hypotheses of how cratons have been formed:  1) surface crust was thickened by a rising plume of deep molten material, 2) successive subducting plates of oceanic lithosphere became lodged beneath a proto-craton in an under-plating process, 3) accretion from island arcs or continental fragments rafting together to thicken into a craton.

answers: NDQ_003351

answers: subduction

answers: NDQ_003352

answers: is more likely to crack

answers: NDQ_003353

answers: subduction zones

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: ridge

answers: NDQ_003356

answers: accretion

answers: NDQ_003357

answers: Subduction zones are formed by the movement of

answers: NDQ_003358

answers: unanswerable

answers: NDQ_003359

answers: subducting plates

answers: NDQ_003360

answers: continental plates

answers: NDQ_003362

answers: surface crust was thickened by a rising plume of deep molten material

answers: NDQ_003363

answers: Archean

answers: NDQ_003371

answers: accretion from island arcs or continental fragments

answers: NDQ_003373

answers: successive subducting plates

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: vertical

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: Which of the following is not a type of stress: subducting plates of oceanic lithosphere became lodged beneath a proto-craton in an under-plating process?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: Which of the following is not a type of fold?

answers: NDQ_003385

answers: what is the first large cratonic landmasses formed

answers: NDQ_003386

answers: tectonic

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: normal faults, subduction zones, or volcanic activity?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip, subduction, or accretion?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: subduction zones

answers: NDQ_003391

answers: subduction zones

answers: NDQ_003392

answers: subduction zones

answers: NDQ_003393

answers: subduction zones

answers: NDQ_003394

answers: subduction zones

answers: NDQ_003395

answers: subduction zones

answers: NDQ_003396

answers: subduction zones

answers: NDQ_003351

answers: subduction zones.

answers: NDQ_003352

answers: thickened by a rising plume of deep molten material,

answers: NDQ_003353

answers: thickened by a rising plume of deep molten material,

answers: NDQ_003354

answers: successive subducting plates

answers: NDQ_003355

answers: ridges

answers: NDQ_003356

answers: thickened by a rising plume of deep molten material,

answers: NDQ_003357

answers: successive subducting plates

answers: NDQ_003358

answers: subduction zones.

answers: NDQ_003359

answers: cratonization.

answers: NDQ_003360

answers: successive subducting plates

answers: NDQ_003362

answers: a rising plume of deep molten material,

answers: NDQ_003363

answers: during the Archean eon.

answers: NDQ_003371

answers: successive subducting plates

answers: NDQ_003373

answers: successive subducting plates

answers: NDQ_003376

answers: successive subducting plates

answers: NDQ_003378

answers: cratonization.

answers: NDQ_003379

answers: successive subducting plates

answers: NDQ_003380

answers: cratonization.

answers: NDQ_003381

answers: successive subducting plates

answers: NDQ_003382

answers: successive subducting plates

answers: NDQ_003383

answers: cratonization.

answers: NDQ_003384

answers: rising plume of deep molten material,

answers: NDQ_003385

answers: subduction zones.

answers: NDQ_003386

answers: successive subducting plates

answers: NDQ_003387

answers: under-plating process,

answers: NDQ_003388

answers: successive subducting plates

answers: NDQ_003389

answers: cratonization.

answers: NDQ_003390

answers: subduction zones.

answers: NDQ_003391

answers: proto-craton

answers: NDQ_003392

answers: cratonization.

answers: NDQ_003393

answers: proto-craton

answers: NDQ_003394

answers: successive subducting plates

answers: NDQ_003395

answers: successive subducting plates

answers: NDQ_003396

answers: under-plating process,

text: Silicon is the eighth most common element in the universe by mass, but very rarely occurs as the pure element in the Earth's crust. It is most widely distributed in dusts, sands, planetoids, and planets as various forms of silicon dioxide (silica) or silicates. Over 90% of the Earth's crust is composed of silicate minerals, making silicon the second most abundant element in the Earth's crust (about 28% by mass) after oxygen.

text: Silicon is the eighth most

text: common element

text: in the universe by mass, but very rarely occurs as the pure element in the Earth's crust. It is most widely distributed in

text: dust

text: s,

text: sand

text: s,

text: planetoids

text: , and

text: planet

text: s as various forms of

text: silicon dioxide

text: (silica) or

text: silicate

text: s. Over 90% of the Earth's crust is composed of

text: silicate minerals

text: , making silicon the

text: second most abundant element

text: in the Earth's crust (about 28% by mass) after

text: oxygen

answers: NDQ_003351

answers: silicates

answers: NDQ_003352

answers: more likely has silicate minerals in it

answers: NDQ_003353

answers: silicate minerals to form

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: oxidize

answers: NDQ_003357

answers: over 90% of the Earth's crust is composed of silicate minerals

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: Silicon is the eighth most common element in the universe by mass

answers: NDQ_003363

answers: silicate minerals

answers: NDQ_003371

answers: What is the second most abundant element in the Earth's crust?

answers: NDQ_003373

answers: None of the above choices.

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: vertical

answers: NDQ_003380

answers: What is the second most abundant element in the Earth's crust?

answers: NDQ_003381

answers: What is the most common element in the universe by mass?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is the second most abundant element in the Earth's crust?

answers: NDQ_003385

answers: faults are clustered

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: what is the second most abundant element in the Earth's crust?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: unanswerable

answers: NDQ_003392

answers: unanswerable

answers: NDQ_003393

answers: Earth's crust

answers: NDQ_003394

answers: sands

answers: NDQ_003395

answers: unanswerable

answers: NDQ_003396

answers: horizontal

answers: NDQ_003351

answers: oxygen.

answers: NDQ_003352

answers: silicate minerals,

answers: NDQ_003353

answers: Over 90% of the Earth's crust is composed of silicate minerals,

answers: NDQ_003354

answers: Silicon

answers: NDQ_003355

answers: Silicon

answers: NDQ_003356

answers: Silicon

answers: NDQ_003357

answers: oxygen.

answers: NDQ_003358

answers: Silicon

answers: NDQ_003359

answers: Silicon is the eighth most common element in the universe by mass,

answers: NDQ_003360

answers: Silicon

answers: NDQ_003362

answers: Silicon

answers: NDQ_003363

answers: Over 90% of the Earth's crust is composed of silicate minerals,

answers: NDQ_003371

answers: Silicon is the eighth most common element in the universe by mass,

answers: NDQ_003373

answers: Silicon

answers: NDQ_003376

answers: Silicon

answers: NDQ_003378

answers: Silicon is the eighth most common element in the universe by mass,

answers: NDQ_003379

answers: Silicon is the eighth most common element in the universe by mass,

answers: NDQ_003380

answers: Silicon

answers: NDQ_003381

answers: Silicon

answers: NDQ_003382

answers: oxygen.

answers: NDQ_003383

answers: Silicon

answers: NDQ_003384

answers: oxygen.

answers: NDQ_003385

answers: Silicon

answers: NDQ_003386

answers: Silicon

answers: NDQ_003387

answers: Silicon

answers: NDQ_003388

answers: Silicon

answers: NDQ_003389

answers: Silicon

answers: NDQ_003390

answers: Silicon is the eighth most common element in the universe by mass,

answers: NDQ_003391

answers: silicate minerals,

answers: NDQ_003392

answers: Silicon is the eighth most common element in the universe by mass,

answers: NDQ_003393

answers: Silicon

answers: NDQ_003394

answers: Silicon

answers: NDQ_003395

answers: Silicon is the eighth most common element in the universe by mass,

answers: NDQ_003396

answers: Silicon is the eighth most common element in the universe by mass,

text: This was immediately followed by a symposium in Tasmania in March 1956. In this symposium, the evidence was used in the theory of an expansion of the global crust. In this hypothesis the shifting of the continents can be simply explained by a large increase in size of the Earth since its formation. However, this was unsatisfactory because its supporters could offer no convincing mechanism to produce a significant expansion of the Earth. Certainly there is no evidence that the moon has expanded in the past 3 billion years; other work would soon show that the evidence was equally in support of continental drift on a globe with a stable radius.

text: This was immediately followed by a symposium in

text: Tasmania

text: in March 1956. In this symposium, the evidence was used in the theory of an

text: expansion of the global crust

text: . In this hypothesis the shifting of the continents can be simply explained by a large increase in size of the Earth since its formation. However, this was unsatisfactory because its supporters could offer no convincing mechanism to produce a significant expansion of the Earth. Certainly there is no evidence that the moon has expanded in the past 3 billion years; other work would soon show that the evidence was equally in support of continental drift on a globe with a stable radius.

answers: NDQ_003351

answers: a large increase in size

answers: NDQ_003352

answers: expands

answers: NDQ_003353

answers: a large increase in size

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: continental drift

answers: NDQ_003356

answers: expand

answers: NDQ_003357

answers: continental drift on a globe with a stable radius

answers: NDQ_003358

answers: stable radius

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: there is no evidence that the moon has expanded in the past 3 billion years

answers: NDQ_003363

answers: an expansion of the global crust

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: What is the reason for this?

answers: NDQ_003376

answers: the theory of an expansion of the global crust

answers: NDQ_003378

answers: what is the amount the ground moves in an earthquake

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What was unsatisfactory?

answers: NDQ_003381

answers: What is the theory of an expansion of the global crust?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: Fault zones are areas where faults are clustered

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: What is the theory of an expansion of the global crust?

answers: NDQ_003388

answers: What was unsatisfactory?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: unsatisfactory

answers: NDQ_003391

answers: continental drift

answers: NDQ_003392

answers: continental drift on a globe with a stable radius

answers: NDQ_003393

answers: continental drift

answers: NDQ_003394

answers: continental drift

answers: NDQ_003395

answers: fault with a vertical fault plane

answers: NDQ_003396

answers: continental drift

answers: NDQ_003351

answers: continental drift

answers: NDQ_003352

answers: expansion of the global crust.

answers: NDQ_003353

answers: expansion of the global crust.

answers: NDQ_003354

answers: 1956.

answers: NDQ_003355

answers: continental drift

answers: NDQ_003356

answers: expansion of the global crust.

answers: NDQ_003357

answers: stable radius.

answers: NDQ_003358

answers: expansion of the global crust.

answers: NDQ_003359

answers: expansion of the global crust.

answers: NDQ_003360

answers: a large increase in size of the Earth

answers: NDQ_003362

answers: the moon has expanded in the past 3 billion years;

answers: NDQ_003363

answers: Tasmania in March 1956.

answers: NDQ_003371

answers: expansion of the global crust.

answers: NDQ_003373

answers: expansion of the global crust.

answers: NDQ_003376

answers: expansion of the global crust.

answers: NDQ_003378

answers: continental drift

answers: NDQ_003379

answers: 1956.

answers: NDQ_003380

answers: expansion of the global crust.

answers: NDQ_003381

answers: expansion of the global crust.

answers: NDQ_003382

answers: expansion of the global crust.

answers: NDQ_003383

answers: expansion of the global crust.

answers: NDQ_003384

answers: 1956.

answers: NDQ_003385

answers: 1956.

answers: NDQ_003386

answers: continental drift

answers: NDQ_003387

answers: expansion of the global crust.

answers: NDQ_003388

answers: 1956.

answers: NDQ_003389

answers: continental drift

answers: NDQ_003390

answers: 1956.

answers: NDQ_003391

answers: expansion of the global crust.

answers: NDQ_003392

answers: 1956.

answers: NDQ_003393

answers: crust.

answers: NDQ_003394

answers: 1956.

answers: NDQ_003395

answers: 1956.

answers: NDQ_003396

answers: expansion of the global crust.

text: The fault was first identified in 1895 by Professor Andrew Lawson of UC Berkeley, who discovered the northern zone. It is often described as having been named after San Andreas Lake, a small body of water that was formed in a valley between the two plates. However, according to some of his reports from 1895 and 1908, Lawson actually named it after the surrounding San Andreas Valley. Following the 1906 San Francisco earthquake, Lawson concluded that the fault extended all the way into southern California.

text: The fault was first identified in 1895 by Professor

text: Andrew Lawson

text: of

text: UC Berkeley

text: , who discovered the northern zone. It is often described as having been named after

text: San Andreas Lake

text: , a small body of water that was formed in a valley between the two plates. However, according to some of his reports from 1895 and 1908, Lawson actually named it after the surrounding San Andreas Valley. Following the

text: 1906 San Francisco earthquake

text: , Lawson concluded that the fault extended all the way into southern California.

answers: NDQ_003351

answers: San Francisco earthquake

answers: NDQ_003352

answers: more likely to crack

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fault

answers: NDQ_003356

answers: swell

answers: NDQ_003357

answers: San Andreas Lake is formed in a valley between the two plates

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: plates

answers: NDQ_003362

answers: the fault extended all the way into southern California

answers: NDQ_003363

answers: San Andreas

answers: NDQ_003371

answers: Which of the following is not a fault: San Andreas Lake, San Andreas Lake, or San Andreas Valley?

answers: NDQ_003373

answers: what is the last word in the passage?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: How would you describe San Andreas Lake?

answers: NDQ_003381

answers: What does Lawson's conclusion mean?

answers: NDQ_003382

answers: what is the most common stress at convergent plates

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: yes

answers: NDQ_003386

answers: no

answers: NDQ_003387

answers: Which of the following is not a normal fault: San Andreas Lake, San Andreas Lake, or San Andreas Valley?

answers: NDQ_003388

answers: Which of the following is not a type of strike-slip fault?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: San Andreas

answers: NDQ_003391

answers: San Andreas Valley

answers: NDQ_003392

answers: San Andreas fault

answers: NDQ_003393

answers: San Andreas Valley

answers: NDQ_003394

answers: San Andreas

answers: NDQ_003395

answers: San Andreas Lake

answers: NDQ_003396

answers: San Andreas Valley

answers: NDQ_003351

answers: 1906 San Francisco earthquake,

answers: NDQ_003352

answers: earthquake, Lawson concluded that the fault extended all the way into southern California.

answers: NDQ_003353

answers: earthquake,

answers: NDQ_003354

answers: California.

answers: NDQ_003355

answers: The fault

answers: NDQ_003356

answers: 1906 San Francisco earthquake,

answers: NDQ_003357

answers: between the two plates.

answers: NDQ_003358

answers: The fault

answers: NDQ_003359

answers: between the two plates.

answers: NDQ_003360

answers: San Andreas Lake,

answers: NDQ_003362

answers: Lawson actually named it after the surrounding San Andreas Valley.

answers: NDQ_003363

answers: San Andreas Lake,

answers: NDQ_003371

answers: The fault was first identified in 1895

answers: NDQ_003373

answers: The fault was first identified in 1895

answers: NDQ_003376

answers: San Andreas Lake,

answers: NDQ_003378

answers: The fault was first identified in 1895

answers: NDQ_003379

answers: San Andreas Lake,

answers: NDQ_003380

answers: 1906 San Francisco earthquake,

answers: NDQ_003381

answers: The fault was first identified in 1895

answers: NDQ_003382

answers: San Andreas Lake,

answers: NDQ_003383

answers: named after San Andreas Lake,

answers: NDQ_003384

answers: San Andreas Lake,

answers: NDQ_003385

answers: San Andreas Valley.

answers: NDQ_003386

answers: The fault was first identified in 1895

answers: NDQ_003387

answers: San Andreas Lake,

answers: NDQ_003388

answers: San Andreas Lake,

answers: NDQ_003389

answers: plates.

answers: NDQ_003390

answers: San Andreas Lake,

answers: NDQ_003391

answers: San Andreas Lake,

answers: NDQ_003392

answers: San Andreas Lake,

answers: NDQ_003393

answers: San Andreas Lake,

answers: NDQ_003394

answers: San Andreas Lake,

answers: NDQ_003395

answers: San Andreas Lake,

answers: NDQ_003396

answers: San Andreas Lake,

text: This involves field-based projects in Africa, aimed at structural and tectonic understanding, and assessing hydrocarbon potential. Part of the Afar rift consortium, this is an inter-disciplinary study of how the Earth’s crust grows at divergent plate boundaries. It is within this field that she, in collaboration with Derek Keir, published her highest cited paper during the 2008-2013 time window relevant for inclusion in the Research Excellence Framework.

text: This involves field-based projects in

text: Africa

text: , aimed at structural and

text: tectonic

text: understanding, and assessing hydrocarbon potential. Part of the Afar rift consortium, this is an inter-disciplinary study of how the

text: Earth’s crust

text: grows at divergent plate boundaries. It is within this field that she, in collaboration with

text: Derek Keir

text: , published her highest cited paper during the 2008-2013 time window relevant for inclusion in the

text: Research Excellence Framework

answers: NDQ_003351

answers: tectonic

answers: NDQ_003352

answers: more likely to crack

answers: NDQ_003353

answers: igneous rocks to form

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: divergent plate boundary

answers: NDQ_003356

answers: grow

answers: NDQ_003357

answers: divergent plate boundaries

answers: NDQ_003358

answers: rift

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: plate boundaries

answers: NDQ_003362

answers: divergent plate boundaries

answers: NDQ_003363

answers: Afar rift

answers: NDQ_003371

answers: What is a thrust fault?

answers: NDQ_003373

answers: how does the Earth’s crust grow at divergent plate boundaries

answers: NDQ_003376

answers: how the Earth’s crust grows at divergent plate boundaries

answers: NDQ_003378

answers: What is the amount the ground moves in an earthquake?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What is an example of a stress?

answers: NDQ_003381

answers: What is the result of confining stress?

answers: NDQ_003382

answers: What is the most common stress at divergent plate boundaries?

answers: NDQ_003383

answers: what is the cause of joints in rock

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: Fault zones are areas where faults are clustered.

answers: NDQ_003386

answers: tectonic

answers: NDQ_003387

answers: What are normal faults caused by?

answers: NDQ_003388

answers: What is shear stress?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: Afar rift

answers: NDQ_003391

answers: rift zone

answers: NDQ_003392

answers: Afar rift

answers: NDQ_003393

answers: rift zone

answers: NDQ_003394

answers: divergent plate boundaries

answers: NDQ_003395

answers: Afar rift

answers: NDQ_003396

answers: Afar rift

answers: NDQ_003351

answers: hydrocarbon potential. Part of the Afar rift consortium,

answers: NDQ_003352

answers: grows at divergent plate boundaries.

answers: NDQ_003353

answers: grows at divergent plate boundaries.

answers: NDQ_003354

answers: Afar rift consortium,

answers: NDQ_003355

answers: rift

answers: NDQ_003356

answers: grows at divergent plate boundaries.

answers: NDQ_003357

answers: divergent plate boundaries.

answers: NDQ_003358

answers: rift

answers: NDQ_003359

answers: divergent plate boundaries.

answers: NDQ_003360

answers: tectonic

answers: NDQ_003362

answers: hydrocarbon potential.

answers: NDQ_003363

answers: divergent plate boundaries.

answers: NDQ_003371

answers: Afar rift consortium,

answers: NDQ_003373

answers: Afar rift consortium,

answers: NDQ_003376

answers: Afar rift consortium,

answers: NDQ_003378

answers: Afar rift consortium,

answers: NDQ_003379

answers: Afar rift consortium,

answers: NDQ_003380

answers: Afar rift consortium,

answers: NDQ_003381

answers: Afar rift consortium,

answers: NDQ_003382

answers: Afar rift consortium,

answers: NDQ_003383

answers: Afar rift consortium,

answers: NDQ_003384

answers: Afar rift consortium,

answers: NDQ_003385

answers: Afar rift consortium,

answers: NDQ_003386

answers: the Earth’s crust grows at divergent plate boundaries.

answers: NDQ_003387

answers: Afar rift consortium,

answers: NDQ_003388

answers: Afar rift consortium,

answers: NDQ_003389

answers: the Earth’s crust grows at divergent plate boundaries.

answers: NDQ_003390

answers: Afar rift consortium,

answers: NDQ_003391

answers: Afar rift consortium,

answers: NDQ_003392

answers: Afar rift consortium,

answers: NDQ_003393

answers: crust grows at divergent plate boundaries.

answers: NDQ_003394

answers: divergent plate boundaries.

answers: NDQ_003395

answers: divergent plate boundaries.

answers: NDQ_003396

answers: Afar rift

text: The current Rocky Mountains were raised in the Laramide orogeny from between 80 and 55 Ma. For the Canadian Rockies, the mountain building is analogous to a rug being pushed on a hardwood floor: the rug bunches up and forms wrinkles (mountains). In Canada, the terranes and subduction are the foot pushing the rug, the ancestral rocks are the rug, and the Canadian Shield in the middle of the continent is the hardwood floor.

text: The current Rocky Mountains were raised in the

text: Laramide orogeny

text: from between 80 and 55 Ma. For the Canadian Rockies, the mountain building is analogous to a rug being pushed on a hardwood floor: the rug bunches up and forms wrinkles (mountains). In Canada, the terranes and subduction are the foot pushing the rug, the ancestral rocks are the rug, and the

text: Canadian Shield

text: in the middle of the continent is the hardwood floor.

answers: NDQ_003351

answers: subduction

answers: NDQ_003352

answers: forms wrinkles

answers: NDQ_003353

answers: subduction

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: wrinkle

answers: NDQ_003356

answers: wrinkle

answers: NDQ_003357

answers: Rocky Mountains were raised from between 80 and 55 Ma

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: subducts

answers: NDQ_003360

answers: Laramide orogeny

answers: NDQ_003362

answers: Rocky Mountains were raised in the Laramide orogeny from between 80 and 55 Ma

answers: NDQ_003363

answers: Laramide orogeny

answers: NDQ_003371

answers: Which of the following is not a type of orogeny: Laramide orogeny, subduction, or hardwood floor?

answers: NDQ_003373

answers: what is the second to last word in the passage?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: How would you describe the Rocky Mountains?

answers: NDQ_003381

answers: What kind of rock is the Rocky Mountains?

answers: NDQ_003382

answers: what is the most common stress at convergent plates

answers: NDQ_003383

answers: what is the last word in the passage?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: Which of the following is not a cause of earthquakes: movement of rock at faults

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: normal faults, subduction, or erosion?

answers: NDQ_003388

answers: What kind of stress is shear stress?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: subduction

answers: NDQ_003391

answers: subduction

answers: NDQ_003392

answers: subduction

answers: NDQ_003393

answers: subduction

answers: NDQ_003394

answers: subduction

answers: NDQ_003395

answers: a fault with a vertical fault plane

answers: NDQ_003396

answers: subduction

answers: NDQ_003351

answers: subduction

answers: NDQ_003352

answers: bunches up and forms wrinkles

answers: NDQ_003353

answers: wrinkles

answers: NDQ_003354

answers: The current Rocky Mountains were raised in the Laramide orogeny

answers: NDQ_003355

answers: wrinkles

answers: NDQ_003356

answers: wrinkles

answers: NDQ_003357

answers: subduction

answers: NDQ_003358

answers: Canadian Shield

answers: NDQ_003359

answers: subduction

answers: NDQ_003360

answers: Laramide orogeny

answers: NDQ_003362

answers: The current Rocky Mountains were raised in the Laramide orogeny

answers: NDQ_003363

answers: Laramide orogeny

answers: NDQ_003371

answers: The current Rocky Mountains were raised in the Laramide orogeny

answers: NDQ_003373

answers: a rug being pushed on a hardwood floor:

answers: NDQ_003376

answers: a rug being pushed on a hardwood floor:

answers: NDQ_003378

answers: a rug being pushed on a hardwood floor:

answers: NDQ_003379

answers: 80 and 55 Ma.

answers: NDQ_003380

answers: a rug being pushed

answers: NDQ_003381

answers: the rug bunches up and forms wrinkles

answers: NDQ_003382

answers: a rug being pushed on a hardwood floor:

answers: NDQ_003383

answers: a rug being pushed on a hardwood floor:

answers: NDQ_003384

answers: a rug being pushed on a hardwood floor:

answers: NDQ_003385

answers: Laramide orogeny

answers: NDQ_003386

answers: subduction

answers: NDQ_003387

answers: a rug being pushed on a hardwood floor:

answers: NDQ_003388

answers: a rug being pushed on a hardwood floor:

answers: NDQ_003389

answers: the rug bunches up and forms wrinkles

answers: NDQ_003390

answers: subduction

answers: NDQ_003391

answers: ancestral rocks

answers: NDQ_003392

answers: subduction

answers: NDQ_003393

answers: ancestral rocks

answers: NDQ_003394

answers: subduction

answers: NDQ_003395

answers: subduction

answers: NDQ_003396

answers: subduction

text: The main quake occurred as a result of strike-slip faulting within the crust of the Pacific plate, near the eastern foothills of the Southern Alps at the western edge of the Canterbury Plains. The earthquake epicentre is located about  to the south and east of the current surface expression of the Australia–Pacific plate boundary through the island (the Alpine and Hope Faults). Though removed from the plate boundary itself, the earthquake likely reflects right-lateral motion on one of a number of regional faults related to the overall relative motion of these plates and may be related to the overall southern propagation of the Marlborough Fault System in recent geologic time. The peak ground acceleration measured near Darfield was 1.26g (12.36 m/s), recorded near Darfield. This was considered by GNS scientists as an "extremely rare seismic recording made near a fault rupture". However, the February 2011 Christchurch earthquake experienced PGA of 2.2 g.

text: The main quake occurred as a result of

text: strike-slip fault

text: ing within the crust of the

text: Pacific plate

text: , near the eastern foothills of the

text: Southern Alps

text: at the western edge of the

text: Canterbury Plains

text: . The earthquake epicentre is located about  to the south and east of the current surface expression of the

text: Australia

text: Pacific plate

text: boundary through the island (the

text: Alpine

text: and

text: Hope Fault

text: s). Though removed from the plate boundary itself, the earthquake likely reflects right-lateral motion on one of a number of regional faults related to the overall relative motion of these plates and may be related to the overall southern propagation of the

text: Marlborough Fault System

text: in recent geologic time. The

text: peak ground acceleration

text: measured near Darfield was 1.26g (12.36 m/s), recorded near Darfield. This was considered by GNS scientists as an "extremely rare seismic recording made near a fault rupture". However, the

text: February 2011 Christchurch earthquake

text: experienced PGA of 2.2 g.

answers: NDQ_003351

answers: strike-slip

answers: NDQ_003352

answers: more likely to crack

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: foothills

answers: NDQ_003356

answers: strike

answers: NDQ_003357

answers: Strike-slip faulting occurs when plates move in opposite directions

answers: NDQ_003358

answers: earthquake epicentre

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: plate boundaries

answers: NDQ_003362

answers: the earthquake epicentre is located about to the south and east of the current surface expression of the Australia–Pacific plate boundary

answers: NDQ_003363

answers: Pacific plate

answers: NDQ_003371

answers: What type of fault is the Marlborough Fault System?

answers: NDQ_003373

answers: What type of stresses does a deeply buried rock experience?

answers: NDQ_003376

answers: What type of terrain is caused by compressive forces?

answers: NDQ_003378

answers: strike-slip

answers: NDQ_003379

answers: no

answers: NDQ_003380

answers: What was the peak ground acceleration measured near Darfield?

answers: NDQ_003381

answers: What is the main quake a result of?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What was considered by GNS scientists as an "extremely rare seismic recording made near a fault rupture?"

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: Fault zone

answers: NDQ_003386

answers: yes

answers: NDQ_003387

answers: Which of the following is not a normal fault?

answers: NDQ_003388

answers: What type of stress is shear stress?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: strike-slip faulting

answers: NDQ_003391

answers: the Pacific plate

answers: NDQ_003392

answers: strike-slip faulting

answers: NDQ_003393

answers: Southern Alps

answers: NDQ_003394

answers: right-lateral

answers: NDQ_003395

answers: Alpine and Hope Faults

answers: NDQ_003396

answers: strike-slip faulting

answers: NDQ_003351

answers: relative motion

answers: NDQ_003352

answers: acceleration

answers: NDQ_003353

answers: ground acceleration

answers: NDQ_003354

answers: 1.26g (12.36 m/s), recorded near Darfield.

answers: NDQ_003355

answers: eastern foothills of the Southern Alps

answers: NDQ_003356

answers: right-lateral motion

answers: NDQ_003357

answers: 2.2 g.

answers: NDQ_003358

answers: strike-slip faulting

answers: NDQ_003359

answers: strike-slip faulting

answers: NDQ_003360

answers: Pacific plate,

answers: NDQ_003362

answers: "extremely rare seismic recording made near a fault rupture".

answers: NDQ_003363

answers: Pacific plate,

answers: NDQ_003371

answers: strike-slip faulting

answers: NDQ_003373

answers: strike-slip faulting

answers: NDQ_003376

answers: Canterbury Plains.

answers: NDQ_003378

answers: strike-slip

answers: NDQ_003379

answers: strike-slip faulting within the crust of the Pacific plate,

answers: NDQ_003380

answers: acceleration

answers: NDQ_003381

answers: strike-slip faulting

answers: NDQ_003382

answers: strike-slip faulting within the crust of the Pacific plate,

answers: NDQ_003383

answers: strike-slip faulting

answers: NDQ_003384

answers: Southern Alps

answers: NDQ_003385

answers: Marlborough Fault System

answers: NDQ_003386

answers: strike-slip faulting

answers: NDQ_003387

answers: strike-slip

answers: NDQ_003388

answers: strike-slip faulting within the crust of the Pacific plate,

answers: NDQ_003389

answers: Southern Alps

answers: NDQ_003390

answers: strike-slip

answers: NDQ_003391

answers: strike-slip faulting within the crust of the Pacific plate,

answers: NDQ_003392

answers: strike-slip

answers: NDQ_003393

answers: Southern Alps

answers: NDQ_003394

answers: right-lateral

answers: NDQ_003395

answers: Marlborough Fault System

answers: NDQ_003396

answers: Marlborough Fault System

text: In 2004 it was suggested by a team of Penn State geoscientists that a blind thrust fault, like the one that caused the infamous Northridge earthquake, lies beneath Mount Tamalpais. This idea was partly based on the steepness of Mount Tamalpais and of nearby Bolinas Ridge, such steepness on the visible surface often being the result of blind thrust faults. Another reason for the suggestion was that the San Andreas Fault creeps more slowly south of Mount Tamalpais than it does in its sections north of Mount Tamalpais and in the Olema Valley, and that the existence of a blind thrust fault may explain the different creeping velocities. If a blind thrust fault does exist under Mount Tamalpais, and if it ruptures, it could be potentially devastating to the North Bay, San Francisco, and any other nearby locale resting on unstable earth and loose fill.

text: In 2004 it was suggested by a team of Penn State geoscientists that a

text: blind thrust fault

text: , like the one that caused the infamous

text: Northridge earthquake

text: , lies beneath Mount Tamalpais. This idea was partly based on the steepness of Mount Tamalpais and of nearby

text: Bolinas Ridge

text: , such steepness on the visible surface often being the result of blind thrust faults. Another reason for the suggestion was that the San Andreas Fault creeps more slowly south of Mount Tamalpais than it does in its sections north of Mount Tamalpais and in the

text: Olema Valley

text: , and that the existence of a blind thrust fault may explain the different creeping velocities. If a blind thrust fault does exist under Mount Tamalpais, and if it ruptures, it could be potentially devastating to the North Bay, San Francisco, and any other nearby locale resting on unstable earth and loose fill.

answers: NDQ_003351

answers: blind thrust fault

answers: NDQ_003352

answers: more likely to crack

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: thrust fault

answers: NDQ_003356

answers: steepness

answers: NDQ_003357

answers: the San Andreas Fault creeps more slowly south of Mount Tamalpais than it does in its sections north of Mount Tamalpais

answers: NDQ_003358

answers: blind thrust fault

answers: NDQ_003359

answers: loose fill

answers: NDQ_003360

answers: San Andreas fault

answers: NDQ_003362

answers: it could be potentially devastating to the North Bay, San Francisco, and any other nearby locale resting on unstable earth and loose fill.

answers: NDQ_003363

answers: San Andreas fault

answers: NDQ_003371

answers: unanswerable

answers: NDQ_003373

answers: unanswerable

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: not enough information

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What is the result of a blind thrust fault?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: yes

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: unanswerable

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: blind thrust fault

answers: NDQ_003391

answers: unanswerable

answers: NDQ_003392

answers: blind thrust fault

answers: NDQ_003393

answers: Bolinas Ridge

answers: NDQ_003394

answers: blind thrust fault

answers: NDQ_003395

answers: San Andreas Fault

answers: NDQ_003396

answers: blind thrust fault

answers: NDQ_003351

answers: blind thrust faults.

answers: NDQ_003352

answers: steepness

answers: NDQ_003353

answers: blind thrust fault,

answers: NDQ_003354

answers: Mount Tamalpais.

answers: NDQ_003355

answers: blind thrust fault,

answers: NDQ_003356

answers: steepness

answers: NDQ_003357

answers: creeps more slowly

answers: NDQ_003358

answers: blind thrust fault,

answers: NDQ_003359

answers: unstable earth

answers: NDQ_003360

answers: blind thrust fault,

answers: NDQ_003362

answers: north of Mount Tamalpais and in the Olema Valley,

answers: NDQ_003363

answers: blind thrust faults.

answers: NDQ_003371

answers: blind thrust faults.

answers: NDQ_003373

answers: unstable earth

answers: NDQ_003376

answers: blind thrust faults.

answers: NDQ_003378

answers: creeps more slowly

answers: NDQ_003379

answers: blind thrust fault,

answers: NDQ_003380

answers: earthquake,

answers: NDQ_003381

answers: blind thrust faults.

answers: NDQ_003382

answers: blind thrust faults.

answers: NDQ_003383

answers: blind thrust faults.

answers: NDQ_003384

answers: Bolinas Ridge,

answers: NDQ_003385

answers: blind thrust fault,

answers: NDQ_003386

answers: steepness on the visible surface often being the result of blind thrust faults.

answers: NDQ_003387

answers: thrust fault,

answers: NDQ_003388

answers: blind thrust faults.

answers: NDQ_003389

answers: blind thrust fault,

answers: NDQ_003390

answers: blind thrust fault,

answers: NDQ_003391

answers: blind thrust fault,

answers: NDQ_003392

answers: blind thrust fault,

answers: NDQ_003393

answers: Bolinas Ridge,

answers: NDQ_003394

answers: blind thrust fault,

answers: NDQ_003395

answers: blind thrust fault,

answers: NDQ_003396

answers: blind thrust fault,

text: The active rift model sees rupture driven by hotspot or mantle plume activity.  Upwellings of hot mantle, known as mantle plumes, originate deep in Earth  and rise to heat and thin the lithosphere.  Heated lithosphere thins, weakens, rises, and  finally rifts, Enhanced melting following continental breakup is very important in VPMs, creating thicker than normal oceanic crust of 20 to 40 km thick.  Other melts caused by convection related upwelling form reservoirs of magma from which dike swarms and sills eventually radiate to the surface, creating the characteristic seaward dipping lava flows.  This model is controversial.

text: The active rift model sees rupture driven by hotspot or mantle plume activity.  Upwellings of hot mantle, known as mantle plumes, originate deep in Earth  and rise to heat and thin the lithosphere.  Heated lithosphere thins, weakens, rises, and  finally rifts, Enhanced melting following continental breakup is very important in VPMs, creating thicker than normal oceanic crust of 20 to 40 km thick.  Other melts caused by

text: convection

text: related upwelling form reservoirs of

text: magma

text: from which

text: dike swarm

text: s and

text: sill

text: s eventually radiate to the surface, creating the characteristic seaward dipping lava flows.  This model is controversial.

answers: NDQ_003351

answers: mantle plume

answers: NDQ_003352

answers: weakens

answers: NDQ_003353

answers: upwellings

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: dike

answers: NDQ_003356

answers: shrink

answers: NDQ_003357

answers: oceanic crust of 20 to 40 km thick

answers: NDQ_003358

answers: unanswerable

answers: NDQ_003359

answers: upwells

answers: NDQ_003360

answers: mantle plumes

answers: NDQ_003362

answers: Enhanced melting following continental breakup is very important in VPMs

answers: NDQ_003363

answers: VPMs

answers: NDQ_003371

answers: Which of the following is not a type of rift fault: active rift model or mantle plume

answers: NDQ_003373

answers: Why is this model controversial?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What type of stress does the active rift model see?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What does the active rift model see?

answers: NDQ_003384

answers: What type of fold is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: What is the active rift model?

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: Which of the following is not a type of strike-slip fault?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: seaward dipping

answers: NDQ_003391

answers: lithosphere

answers: NDQ_003392

answers: rift

answers: NDQ_003393

answers: lithosphere

answers: NDQ_003394

answers: seaward dipping

answers: NDQ_003395

answers: Enhanced melting following continental breakup

answers: NDQ_003396

answers: VPMs

answers: NDQ_003351

answers: hotspot or mantle plume activity.

answers: NDQ_003352

answers: thins, weakens, rises, and finally rifts,

answers: NDQ_003353

answers: thin the lithosphere.

answers: NDQ_003354

answers: The active rift model

answers: NDQ_003355

answers: seaward dipping lava flows.

answers: NDQ_003356

answers: Enhanced melting

answers: NDQ_003357

answers: 20 to 40 km thick.

answers: NDQ_003358

answers: hotspot

answers: NDQ_003359

answers: rupture driven by hotspot or mantle plume activity.

answers: NDQ_003360

answers: Upwellings of hot mantle,

answers: NDQ_003362

answers: The active rift model

answers: NDQ_003363

answers: Enhanced melting following continental breakup

answers: NDQ_003371

answers: The active rift model

answers: NDQ_003373

answers: Upwellings of hot mantle,

answers: NDQ_003376

answers: The active rift model

answers: NDQ_003378

answers: The active rift model

answers: NDQ_003379

answers: seaward

answers: NDQ_003380

answers: The active rift model

answers: NDQ_003381

answers: The active rift model

answers: NDQ_003382

answers: Enhanced melting

answers: NDQ_003383

answers: The active rift model

answers: NDQ_003384

answers: mantle plumes,

answers: NDQ_003385

answers: The active rift model

answers: NDQ_003386

answers: The active rift model

answers: NDQ_003387

answers: hotspot or mantle plume activity.

answers: NDQ_003388

answers: hotspot or mantle plume activity.

answers: NDQ_003389

answers: lava flows.

answers: NDQ_003390

answers: The active rift model

answers: NDQ_003391

answers: lava flows.

answers: NDQ_003392

answers: The active rift model

answers: NDQ_003393

answers: lava flows.

answers: NDQ_003394

answers: The active rift model

answers: NDQ_003395

answers: The active rift model

answers: NDQ_003396

answers: active rift model

text: During this era the earliest global-scale continent-continent collisional belts developed.

text: During this era the earliest global-scale continent-continent collisional belts developed.

answers: NDQ_003351

answers: gravitational

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: continents collide with each other

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: is pushed together

answers: NDQ_003360

answers: collisional belts

answers: NDQ_003362

answers: The San Andreas fault is not a fault.

answers: NDQ_003363

answers: the end of the last ice age

answers: NDQ_003371

answers: Which of the following is not an example of a thrust fault?

answers: NDQ_003373

answers: how would you describe compressive stresses?

answers: NDQ_003376

answers: what is the last time period mentioned?

answers: NDQ_003378

answers: what is the last word in the passage?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What is a result of confining stress?

answers: NDQ_003382

answers: Which of the following is not a type of plate?

answers: NDQ_003383

answers: None of the above choices.

answers: NDQ_003384

answers: what is the first time period mentioned?

answers: NDQ_003385

answers: what is the first time period mentioned?

answers: NDQ_003386

answers: the Cretaceous Period

answers: NDQ_003387

answers: Which of the following is not a cause of normal faults?

answers: NDQ_003388

answers: Which of the following is not an example of a strike-slip fault?

answers: NDQ_003389

answers: None of the above choices.

answers: NDQ_003390

answers: collapsing fault

answers: NDQ_003391

answers: is a block of rock

answers: NDQ_003392

answers: collapsing fault

answers: NDQ_003393

answers: is a block of rock

answers: NDQ_003394

answers: isobath

answers: NDQ_003395

answers: NDQ_003396

answers: NDQ_003351

answers: continent-continent collisional belts

answers: NDQ_003352

answers: earliest global-scale continent-continent collisional belts

answers: NDQ_003353

answers: continent-continent collisional belts

answers: NDQ_003354

answers: During this era

answers: NDQ_003355

answers: continent-continent collisional belts

answers: NDQ_003356

answers: earliest global-scale continent-continent collisional belts

answers: NDQ_003357

answers: continent-continent collisional belts

answers: NDQ_003358

answers: continent-continent collisional belts

answers: NDQ_003359

answers: earliest global-scale continent-continent collisional belts

answers: NDQ_003360

answers: continent-continent collisional belts

answers: NDQ_003362

answers: earliest global-scale continent-continent collisional belts

answers: NDQ_003363

answers: continent-continent collisional belts

answers: NDQ_003371

answers: earliest global-scale continent-continent collisional belts

answers: NDQ_003373

answers: During

answers: NDQ_003376

answers: earliest global-scale continent-continent collisional belts

answers: NDQ_003378

answers: earliest global-scale continent-continent collisional belts

answers: NDQ_003379

answers: During this era

answers: NDQ_003380

answers: earliest global-scale continent-continent collisional belts

answers: NDQ_003381

answers: earliest global-scale continent-continent collisional belts

answers: NDQ_003382

answers: During this era

answers: NDQ_003383

answers: During

answers: NDQ_003384

answers: During

answers: NDQ_003385

answers: earliest global-scale continent-continent collisional belts

answers: NDQ_003386

answers: earliest global-scale continent-continent collisional belts

answers: NDQ_003387

answers: earliest global-scale continent-continent collisional belts

answers: NDQ_003388

answers: During this era

answers: NDQ_003389

answers: During this era

answers: NDQ_003390

answers: earliest global-scale continent-continent collisional belts

answers: NDQ_003391

answers: continent-continent collisional belts

answers: NDQ_003392

answers: earliest global-scale continent-continent collisional belts

answers: NDQ_003393

answers: continent-continent collisional belts

answers: NDQ_003394

answers: continent-continent collisional belts

answers: NDQ_003395

answers: continent-continent collisional belts

answers: NDQ_003396

answers: continent-continent collisional belts

text: The mainshock was followed by a series of aftershocks that continued for at least 3.75 years, although the total number of large aftershocks was less than would be expected for an earthquake of this size. The four largest aftershocks all had magnitudes greater than 6, although there are large uncertainties in both location and magnitude due to the limited number of data points available. On the night of 9 January there was a large aftershock with an estimated magnitude of about 6.25, with a possible epicenter near the Garlock Fault. The largest aftershock occurred on the afternoon of 16 January with an estimated magnitude of about 6.7, with a possible offshore location, and high felt intensities in Southern California communities. Santa Barbara and San Bernardino reported an MM intensity of V and Los Angeles reported V and VI. Two significant events occurred in the San Bernardino area on 15–16 December 1858, with the latter having an estimated magnitude of about 6. The last recorded major aftershock occurred on 16 April 1860, with an estimated magnitude of about 6.3, with an epicenter close to the Parkfield section of the San Andreas Fault.

text: The mainshock was followed by a series of

text: aftershocks

text: that continued for at least 3.75 years, although the total number of large aftershocks was less than would be expected for an earthquake of this size. The four largest aftershocks all had magnitudes greater than 6, although there are large uncertainties in both location and magnitude due to the limited number of data points available. On the night of 9 January there was a large aftershock with an estimated magnitude of about 6.25, with a possible epicenter near the

text: Garlock Fault

text: . The largest aftershock occurred on the afternoon of 16 January with an estimated magnitude of about 6.7, with a possible offshore location, and high felt intensities in Southern California communities.

text: Santa Barbara

text: and

text: San Bernardino

text: reported an MM intensity of V and Los Angeles reported V and VI. Two significant events occurred in the San Bernardino area on 15–16 December 1858, with the latter having an estimated magnitude of about 6. The last recorded major aftershock occurred on 16 April 1860, with an estimated magnitude of about 6.3, with an epicenter close to the Parkfield section of the San Andreas Fault.

answers: NDQ_003351

answers: magnitude of about 6.7

answers: NDQ_003352

answers: increases in magnitude

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: Fault

answers: NDQ_003356

answers: aftershocks

answers: NDQ_003357

answers: How many aftershocks had magnitudes greater than 6?

answers: NDQ_003358

answers: aftershock

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: aftershocks

answers: NDQ_003362

answers: Garlock Fault

answers: NDQ_003363

answers: San Andreas Fault

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: What type of stresses does a deeply buried rock experience?

answers: NDQ_003376

answers: What type of terrain is caused by compressive forces?

answers: NDQ_003378

answers: What was the magnitude of the largest aftershock?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What type of stress does the San Andreas Fault cause?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What type of fold is the Garlock Fault?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: What is the San Andreas Fault

answers: NDQ_003387

answers: What type of fault is the San Andreas Fault?

answers: NDQ_003388

answers: What type of fault is the San Andreas Fault?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: San Andreas Fault

answers: NDQ_003391

answers: San Andreas Fault

answers: NDQ_003392

answers: San Andreas Fault

answers: NDQ_003393

answers: San Andreas Fault

answers: NDQ_003394

answers: San Andreas Fault

answers: NDQ_003395

answers: San Andreas Fault

answers: NDQ_003396

answers: Garlock Fault

answers: NDQ_003351

answers: San Andreas Fault.

answers: NDQ_003352

answers: 6.7,

answers: NDQ_003353

answers: aftershocks

answers: NDQ_003354

answers: 6.7,

answers: NDQ_003355

answers: Garlock Fault.

answers: NDQ_003356

answers: 6.7,

answers: NDQ_003357

answers: San Andreas Fault.

answers: NDQ_003358

answers: epicenter

answers: NDQ_003359

answers: San Andreas Fault.

answers: NDQ_003360

answers: earthquake

answers: NDQ_003362

answers: Garlock Fault.

answers: NDQ_003363

answers: San Andreas Fault.

answers: NDQ_003371

answers: Garlock Fault.

answers: NDQ_003373

answers: 6.7,

answers: NDQ_003376

answers: 6.7,

answers: NDQ_003378

answers: aftershocks

answers: NDQ_003379

answers: 6.7,

answers: NDQ_003380

answers: earthquake

answers: NDQ_003381

answers: 6.7,

answers: NDQ_003382

answers: 6.7,

answers: NDQ_003383

answers: 6.7,

answers: NDQ_003384

answers: Garlock Fault.

answers: NDQ_003385

answers: San Andreas Fault.

answers: NDQ_003386

answers: San Andreas Fault.

answers: NDQ_003387

answers: San Andreas Fault.

answers: NDQ_003388

answers: San Andreas Fault.

answers: NDQ_003389

answers: San Andreas Fault.

answers: NDQ_003390

answers: Garlock Fault.

answers: NDQ_003391

answers: Garlock Fault.

answers: NDQ_003392

answers: Garlock Fault.

answers: NDQ_003393

answers: Garlock Fault.

answers: NDQ_003394

answers: Garlock Fault.

answers: NDQ_003395

answers: San Andreas Fault.

answers: NDQ_003396

answers: Garlock Fault.

text: In the Palaeozoic (Paleozoic) walked the continental drift a southern continent to continent on a north. This collided intervening dwarf-continent and in the Devonian and Carboniferous period (about 380-320 million years ago), the Variscan Mountains to the Odw counts delayed. was already in the history of Böllsteiner gneiss. He emerged from granitic rocks, which have penetrated about 410 million years ago as molten rock from below into older sedimentary rocks. These were common - sunk into deeper areas of the earth's crust and converted there, at a high temperature pressure to schists and gneisses - a result of the co-thrusts. At the Otzberg column is welded these rocks - in the course of plate collision - with those of the Bergstrasse Odws.

text: In the Palaeozoic (Paleozoic) walked the continental drift a southern continent to continent on a north. This collided intervening dwarf-continent and in the Devonian and Carboniferous period (about 380-320 million years ago), the Variscan Mountains to the Odw counts delayed. was already in the history of Böllsteiner gneiss. He emerged from granitic rocks, which have penetrated about 410 million years ago as molten rock from below into older sedimentary rocks. These were common - sunk into deeper areas of the earth's crust and converted there, at a high temperature pressure to schists and gneisses - a result of the co-thrusts. At the Otzberg column is welded these rocks - in the course of plate collision - with those of the Bergstrasse Odws.

answers: NDQ_003351

answers: high temperature

answers: NDQ_003352

answers: increases in temperature and pressure

answers: NDQ_003353

answers: high temperature and pressure

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: swell

answers: NDQ_003357

answers: sunk into deeper areas of the earth's crust

answers: NDQ_003358

answers: co-thrust

answers: NDQ_003359

answers: collides with another

answers: NDQ_003360

answers: plate collision

answers: NDQ_003362

answers: the Variscan Mountains to the Odw counts delayed

answers: NDQ_003363

answers: Devonian and Carboniferous

answers: NDQ_003371

answers: Which of the following is not a result of the co-thrusts?

answers: NDQ_003373

answers: What is the main idea of this passage?

answers: NDQ_003376

answers: Which of the following is not a cause of the terrain known as basin-and-range?

answers: NDQ_003378

answers: what is the first time period mentioned?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What type of force applied to rock is a stress?

answers: NDQ_003381

answers: What is a result of the co-thrusts

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: Which of the following is not a cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not a cause of normal faults: compression stress, schists, or gneisses?

answers: NDQ_003388

answers: Which of the following is not a result of shear stress: strike-slip faults, schists, or gneisses?

answers: NDQ_003389

answers: It is not possible to tell

answers: NDQ_003390

answers: co-thrust

answers: NDQ_003391

answers: gneiss

answers: NDQ_003392

answers: co-thrusts

answers: NDQ_003393

answers: Otzberg column

answers: NDQ_003394

answers: co-thrusts

answers: NDQ_003395

answers: fault with a vertical fault plane

answers: NDQ_003396

answers: co-thrusts

answers: NDQ_003351

answers: co-thrusts.

answers: NDQ_003352

answers: schists and gneisses

answers: NDQ_003353

answers: high temperature pressure to schists and gneisses

answers: NDQ_003354

answers: In the Palaeozoic

answers: NDQ_003355

answers: co-thrusts.

answers: NDQ_003356

answers: welded

answers: NDQ_003357

answers: co-thrusts.

answers: NDQ_003358

answers: co-thrusts.

answers: NDQ_003359

answers: plate collision

answers: NDQ_003360

answers: plate collision

answers: NDQ_003362

answers: a southern continent to continent on a north.

answers: NDQ_003363

answers: plate collision

answers: NDQ_003371

answers: co-thrusts.

answers: NDQ_003373

answers: high temperature pressure

answers: NDQ_003376

answers: co-thrusts.

answers: NDQ_003378

answers: co-thrusts.

answers: NDQ_003379

answers: north.

answers: NDQ_003380

answers: pressure

answers: NDQ_003381

answers: plate collision

answers: NDQ_003382

answers: co-thrusts.

answers: NDQ_003383

answers: co-thrusts.

answers: NDQ_003384

answers: north.

answers: NDQ_003385

answers: In the Palaeozoic

answers: NDQ_003386

answers: plate collision

answers: NDQ_003387

answers: co-thrusts.

answers: NDQ_003388

answers: co-thrusts.

answers: NDQ_003389

answers: plate collision

answers: NDQ_003390

answers: co-thrusts.

answers: NDQ_003391

answers: Böllsteiner gneiss.

answers: NDQ_003392

answers: co-thrusts.

answers: NDQ_003393

answers: Böllsteiner gneiss.

answers: NDQ_003394

answers: north.

answers: NDQ_003395

answers: co-thrusts.

answers: NDQ_003396

answers: co-thrusts.

text: Buckling strength is less than elastic buckling strength of a structure, due to non-linear (plastic) behavior of the material. When the compression load is near the buckling load, the structure will bend significantly and the material of the column will diverge from a linear stress-strain behavior. The stress-strain behavior of materials is not strictly linear even below the yield point, and the modulus of elasticity decreases as stress increases, and significantly so as the stresses approach the yield strength. This lower rigidity reduces the buckling strength of the structure and results in a bucking load less than that predicted by the assumption of lineal elastic behavior.

text: Buckling strength is less than elastic buckling strength of a structure, due to non-linear (plastic) behavior of the material. When the compression load is near the buckling load, the structure will bend significantly and the material of the column will diverge from a linear stress-strain behavior. The stress-strain behavior of materials is not strictly linear even below the yield point, and the modulus of elasticity decreases as stress increases, and significantly so as the stresses approach the yield strength. This lower rigidity reduces the buckling strength of the structure and results in a bucking load less than that predicted by the assumption of lineal elastic behavior.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: modulus of elasticity decreases

answers: NDQ_003353

answers: modulus of elasticity

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: buckling load

answers: NDQ_003356

answers: bend

answers: NDQ_003357

answers: The modulus of elasticity decreases as stress increases, and significantly so as the stresses approach the yield strength

answers: NDQ_003358

answers: buckling

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: Buckling strength is less than elastic buckling strength

answers: NDQ_003363

answers: unanswerable

answers: NDQ_003371

answers: Which of the following is not an example of non-linear (plastic) behavior?

answers: NDQ_003373

answers: When the compression load is near the buckling load

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What is the modulus of elasticity of materials?

answers: NDQ_003381

answers: When the compression load is near the buckling load

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: Which of the following is not a cause of normal faults?

answers: NDQ_003388

answers: What is the modulus of elasticity of materials?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: buckling load

answers: NDQ_003391

answers: dip-slip fault plane

answers: NDQ_003392

answers: buckling load

answers: NDQ_003393

answers: dip-slip fault plane

answers: NDQ_003394

answers: buckling

answers: NDQ_003395

answers: a vertical fault plane

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: compression load

answers: NDQ_003352

answers: modulus of elasticity decreases

answers: NDQ_003353

answers: bend significantly

answers: NDQ_003354

answers: Buckling strength is less than elastic buckling strength

answers: NDQ_003355

answers: Buckling strength is less than elastic buckling strength

answers: NDQ_003356

answers: bend significantly

answers: NDQ_003357

answers: compression load is near the buckling load,

answers: NDQ_003358

answers: yield point,

answers: NDQ_003359

answers: compression load is near the buckling load,

answers: NDQ_003360

answers: compression load

answers: NDQ_003362

answers: Buckling strength is less than elastic buckling strength

answers: NDQ_003363

answers: yield point,

answers: NDQ_003371

answers: Buckling strength is less than elastic buckling strength

answers: NDQ_003373

answers: the compression load is near the buckling load,

answers: NDQ_003376

answers: compression load is near the buckling load,

answers: NDQ_003378

answers: bend significantly

answers: NDQ_003379

answers: linear stress-strain behavior.

answers: NDQ_003380

answers: compression load

answers: NDQ_003381

answers: When the compression load is near the buckling load,

answers: NDQ_003382

answers: compression load is near the buckling load,

answers: NDQ_003383

answers: bend

answers: NDQ_003384

answers: Buckling strength is less than elastic buckling strength of a structure,

answers: NDQ_003385

answers: Buckling strength is less than elastic buckling strength of a structure,

answers: NDQ_003386

answers: stress-strain behavior.

answers: NDQ_003387

answers: When the compression load is near the buckling load,

answers: NDQ_003388

answers: Buckling strength is less than elastic buckling strength of a structure,

answers: NDQ_003389

answers: bend

answers: NDQ_003390

answers: column will diverge from a linear stress-strain behavior.

answers: NDQ_003391

answers: yield point,

answers: NDQ_003392

answers: column will diverge from a linear stress-strain behavior.

answers: NDQ_003393

answers: yield point,

answers: NDQ_003394

answers: linear stress-strain behavior.

answers: NDQ_003395

answers: linear stress-strain behavior.

answers: NDQ_003396

answers: Buckling strength is less than elastic buckling strength

text: Fold is a Unix command used for making a file with long lines more readable on a limited width terminal. Most Unix terminals have a default screen width of 80, and therefore reading files with long lines could get annoying. The fold command puts a line feed every X characters if it does not reach a new line before that point. If the -w argument is set, the fold command allows the user to set the maximum length of a line.

text: Fold is a

text: Unix

text: command used for making a

text: file

text: with long lines more readable on a limited width terminal. Most

text: Unix

text: terminals have a default screen width of 80, and therefore reading files with long lines could get annoying. The fold command puts a

text: line feed

text: every X characters if it does not reach a new line before that point. If the -w argument is set, the fold command allows the user to set the maximum length of a line.

answers: NDQ_003351

answers: tensile

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: a chemical reaction

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone.

answers: NDQ_003355

answers: fold that bends downward

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: if x == 0 and y == 0 and z == 0:

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures.

answers: NDQ_003360

answers: glaciers.

answers: NDQ_003362

answers: unix terminals have a default screen width of 80

answers: NDQ_003363

answers: the same time.

answers: NDQ_003371

answers: context: If very old rocks are above much younger rocks there may be a thrust fault in between.

answers: NDQ_003373

answers: context: A deeply buried rock is under compressive stresses.

answers: NDQ_003376

answers: fold

answers: NDQ_003378

answers: context: The amount the ground moves in an earthquake is called slip

answers: NDQ_003379

answers: context: The dip of the fault plane is vertical.

answers: NDQ_003380

answers: any force applied to rock is a stress

answers: NDQ_003381

answers: context: When confining stress occurs, rock deforms.

answers: NDQ_003382

answers: context: Compression is the most common stress at convergent plates

answers: NDQ_003383

answers: context: Stress is the cause of joints in rock.

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: Faults are clustered in a fault zone.

answers: NDQ_003386

answers: context: earthquakes are caused by movement of rock at faults

answers: NDQ_003387

answers: Condensation

answers: NDQ_003388

answers: context: Strike-slip faults result from shear stress.

answers: NDQ_003389

answers: fold

answers: NDQ_003390

answers: -w

answers: NDQ_003391

answers: -w

answers: NDQ_003392

answers: -w

answers: NDQ_003393

answers: is above a dip-slip fault

answers: NDQ_003394

answers: -w

answers: NDQ_003395

answers: a fault with a vertical fault plane

answers: NDQ_003396

answers: -w

answers: NDQ_003351

answers: X characters

answers: NDQ_003352

answers: X

answers: NDQ_003353

answers: Fold

answers: NDQ_003354

answers: X characters

answers: NDQ_003355

answers: Fold

answers: NDQ_003356

answers: Fold

answers: NDQ_003357

answers: The fold command puts a line feed every X characters

answers: NDQ_003358

answers: Fold

answers: NDQ_003359

answers: X characters if it does not reach a new line before that point.

answers: NDQ_003360

answers: Fold

answers: NDQ_003362

answers: Fold

answers: NDQ_003363

answers: X characters

answers: NDQ_003371

answers: Fold

answers: NDQ_003373

answers: Fold

answers: NDQ_003376

answers: X characters

answers: NDQ_003378

answers: X

answers: NDQ_003379

answers: 80,

answers: NDQ_003380

answers: Fold

answers: NDQ_003381

answers: X

answers: NDQ_003382

answers: X characters

answers: NDQ_003383

answers: Fold

answers: NDQ_003384

answers: X characters

answers: NDQ_003385

answers: Fold

answers: NDQ_003386

answers: Fold

answers: NDQ_003387

answers: X

answers: NDQ_003388

answers: Fold

answers: NDQ_003389

answers: Fold

answers: NDQ_003390

answers: Fold

answers: NDQ_003391

answers: X characters

answers: NDQ_003392

answers: Fold

answers: NDQ_003393

answers: X characters

answers: NDQ_003394

answers: X characters

answers: NDQ_003395

answers: X

answers: NDQ_003396

answers: Fold

text: A hypothesis based on research conducted on the Bay of Islands complex in Newfoundland suggests that an irregular continental margin colliding with an island arc complex causes ophiolite generation in a back-arc basin and obduction due to compression.  The continental margin, promontories and reentrants along its length, is attached to the subducting oceanic crust, which dips away from it underneath the island arc complex. As subduction takes place, the buoyant continent and island arc complex converge, initially colliding with the promontories. However, oceanic crust is still at the surface between the promontories, not having been subducted beneath the island arc yet. The subducting oceanic crust is thought to split from the continental margin to aid subduction. In the event that the rate of trench retreat is greater than that of the island arc complex’s progression, trench rollback will take place, and by consequence, extension of the overriding plate will occur to allow the island arc complex to match the trench retreat’s speed. The extension, a back-arc basin, generates oceanic crust: ophiolites. Finally, when the oceanic lithosphere is entirely subducted, the island arc complex’s extensional regime becomes compressional. The hot, positively buoyant ocean crust from the extension won’t subduct, instead obducting onto the island arc as an ophiolite. As compression persists, the ophiolite is emplaced onto the continental margin.

text: A hypothesis based on research conducted on the Bay of Islands complex in Newfoundland suggests that an irregular continental margin colliding with an

text: island arc complex

text: causes ophiolite generation in a

text: back-arc basin

text: and

text: obduction

text: due to compression.  The continental margin,

text: promontories

text: and

text: reentrants

text: along its length, is attached to the subducting oceanic crust, which dips away from it underneath the island arc complex. As subduction takes place, the buoyant continent and island arc complex converge, initially colliding with the promontories. However, oceanic crust is still at the surface between the promontories, not having been subducted beneath the island arc yet. The subducting oceanic crust is thought to split from the continental margin to aid subduction. In the event that the rate of trench retreat is greater than that of the island arc complex’s progression,

text: trench rollback

text: will take place, and by consequence, extension of the overriding plate will occur to allow the island arc complex to match the trench retreat’s speed. The extension, a back-arc basin, generates oceanic crust: ophiolites. Finally, when the oceanic lithosphere is entirely subducted, the island arc complex’s extensional regime becomes compressional. The hot, positively buoyant ocean crust from the extension won’t subduct, instead obducting onto the island arc as an ophiolite. As compression persists, the ophiolite is emplaced onto the continental margin.

answers: NDQ_003351

answers: trench rollback

answers: NDQ_003352

answers: compresses

answers: NDQ_003353

answers: compression

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: trench

answers: NDQ_003356

answers: subduct

answers: NDQ_003357

answers: oceanic crust is still at the surface between the promontories

answers: NDQ_003358

answers: trench

answers: NDQ_003359

answers: collapses

answers: NDQ_003360

answers: continental plates

answers: NDQ_003362

answers: oceanic crust is still at the surface between the promontories

answers: NDQ_003363

answers: Bay of Islands complex

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: yes

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a stress?

answers: NDQ_003381

answers: What happens when the oceanic crust from the extension won’t subduct?

answers: NDQ_003382

answers: What is the most common stress at convergent plates

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: What type of fold is the Bay of Islands complex in Newfoundland?

answers: NDQ_003385

answers: What is the area where faults are clustered called?

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: Which of the following is not caused by compression stress?

answers: NDQ_003388

answers: Which of the following is not a type of strike-slip fault?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: trench rollback

answers: NDQ_003391

answers: trench

answers: NDQ_003392

answers: trench rollback

answers: NDQ_003393

answers: ophiolite

answers: NDQ_003394

answers: trench rollback

answers: NDQ_003395

answers: trench rollback will take place

answers: NDQ_003396

answers: trench rollback

answers: NDQ_003351

answers: compression.

answers: NDQ_003352

answers: the ophiolite is emplaced onto the continental margin.

answers: NDQ_003353

answers: compression.

answers: NDQ_003354

answers: oceanic crust is still at the surface

answers: NDQ_003355

answers: trench rollback

answers: NDQ_003356

answers: compression.

answers: NDQ_003357

answers: oceanic crust

answers: NDQ_003358

answers: trench

answers: NDQ_003359

answers: compression.

answers: NDQ_003360

answers: subduction

answers: NDQ_003362

answers: not having been subducted beneath the island arc yet.

answers: NDQ_003363

answers: Bay of Islands complex in Newfoundland

answers: NDQ_003371

answers: trench rollback

answers: NDQ_003373

answers: compression.

answers: NDQ_003376

answers: back-arc basin

answers: NDQ_003378

answers: trench rollback

answers: NDQ_003379

answers: dips away from it underneath the island arc complex.

answers: NDQ_003380

answers: compression.

answers: NDQ_003381

answers: compression.

answers: NDQ_003382

answers: compression.

answers: NDQ_003383

answers: compression.

answers: NDQ_003384

answers: island arc complex

answers: NDQ_003385

answers: back-arc basin

answers: NDQ_003386

answers: an irregular continental margin colliding with an island arc complex

answers: NDQ_003387

answers: compression.

answers: NDQ_003388

answers: compression.

answers: NDQ_003389

answers: subduction

answers: NDQ_003390

answers: trench rollback

answers: NDQ_003391

answers: subducting oceanic crust,

answers: NDQ_003392

answers: trench rollback

answers: NDQ_003393

answers: ophiolite

answers: NDQ_003394

answers: irregular continental margin colliding with an island arc complex

answers: NDQ_003395

answers: trench rollback

answers: NDQ_003396

answers: trench rollback

text: Because most stresses relate to the tectonic activity of moving plates, most motion between blocks is horizontal, that is parallel to the Earth's crust by strike-slip faults.  However vertical movement of blocks produces much more dramatic results.  Landforms (mountains, hills, ridges, lakes, valleys, etc.) are sometimes formed when the faults have a large vertical displacement.  Adjacent raised blocks (horsts) and down-dropped blocks (grabens) can form high escarpments.  Often the movement of these blocks is accompanied by tilting, due to compaction or stretching of the crust at that point.

text: Because most stresses relate to the tectonic activity of moving

text: plates

text: , most motion between blocks is horizontal, that is parallel to the Earth's crust by

text: strike-slip faults

text: .  However vertical movement of blocks produces much more dramatic results.  Landforms (

text: mountain

text: s, hills, ridges, lakes, valleys, etc.) are sometimes formed when the faults have a large vertical displacement.  Adjacent raised blocks (

text: horst

text: s) and down-dropped blocks (

text: graben

text: s) can form high

text: escarpment

text: s.  Often the movement of these blocks is accompanied by tilting, due to compaction or stretching of the crust at that point.

answers: NDQ_003351

answers: horizontal

answers: NDQ_003352

answers: tilts more

answers: NDQ_003353

answers: vertical displacement

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: grabens

answers: NDQ_003356

answers: tilt

answers: NDQ_003357

answers: horizontal movement of blocks produces much more dramatic results

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: faults

answers: NDQ_003362

answers: vertical movement of blocks produces much more dramatic results

answers: NDQ_003363

answers: vertical movement of blocks

answers: NDQ_003371

answers: Which of the following is not a type of landform?

answers: NDQ_003373

answers: what is the last word in the passage?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: vertical displacement

answers: NDQ_003379

answers: horizontal

answers: NDQ_003380

answers: Which of the following is not a stress?

answers: NDQ_003381

answers: What is a result of compaction?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: horizontal movement of blocks

answers: NDQ_003384

answers: Which of the following is not a landform?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: horizontal

answers: NDQ_003387

answers: Which of the following is not a type of strike-slip fault?

answers: NDQ_003388

answers: Which of the following is not a result of shear stress: compaction or stretching of the crust at that point?

answers: NDQ_003389

answers: vertical movement

answers: NDQ_003390

answers: down-dropped blocks

answers: NDQ_003391

answers: block

answers: NDQ_003392

answers: down-dropped blocks

answers: NDQ_003393

answers: raised blocks

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: landforms

answers: NDQ_003396

answers: slip faults

answers: NDQ_003351

answers: strike-slip faults.

answers: NDQ_003352

answers: tilting,

answers: NDQ_003353

answers: compaction or stretching of the crust

answers: NDQ_003354

answers: vertical movement of blocks produces much more dramatic results. Landforms

answers: NDQ_003355

answers: (grabens)

answers: NDQ_003356

answers: tilting,

answers: NDQ_003357

answers: most motion between blocks is horizontal,

answers: NDQ_003358

answers: (horsts)

answers: NDQ_003359

answers: vertical displacement.

answers: NDQ_003360

answers: strike-slip faults.

answers: NDQ_003362

answers: vertical movement of blocks produces much more dramatic results.

answers: NDQ_003363

answers: when the faults have a large vertical displacement.

answers: NDQ_003371

answers: strike-slip faults.

answers: NDQ_003373

answers: compaction or stretching of the crust

answers: NDQ_003376

answers: (mountains, hills, ridges, lakes, valleys,

answers: NDQ_003378

answers: strike-slip faults.

answers: NDQ_003379

answers: vertical

answers: NDQ_003380

answers: stretching

answers: NDQ_003381

answers: compaction or stretching of the crust

answers: NDQ_003382

answers: compaction or stretching

answers: NDQ_003383

answers: stresses relate to the tectonic activity of moving plates,

answers: NDQ_003384

answers: (horsts)

answers: NDQ_003385

answers: strike-slip faults.

answers: NDQ_003386

answers: vertical movement of blocks

answers: NDQ_003387

answers: strike-slip faults.

answers: NDQ_003388

answers: horizontal, that is parallel to the Earth's crust

answers: NDQ_003389

answers: vertical displacement.

answers: NDQ_003390

answers: (grabens)

answers: NDQ_003391

answers: (grabens)

answers: NDQ_003392

answers: (horsts)

answers: NDQ_003393

answers: (horsts)

answers: NDQ_003394

answers: strike-slip faults.

answers: NDQ_003395

answers: large vertical displacement.

answers: NDQ_003396

answers: strike-slip faults.

text: The Timor Plate is a microplate in southeast Asia carrying the island of Timor and surrounding islands. The Australian Plate is subducting under the southern edge of the plate, while a small divergent boundary is located on the eastern edge. Another convergent boundary exists with the Banda Sea Plate to the north, and to the west is a transform boundary.

text: The Timor Plate is a microplate in southeast

text: Asia

text: carrying the island of

text: Timor

text: and surrounding islands. The

text: Australian Plate

text: is

text: subducting

text: under the southern edge of the plate, while a small

text: divergent boundary

text: is located on the eastern edge. Another

text: convergent boundary

text: exists with the

text: Banda Sea Plate

text: to the north, and to the west is a

text: transform boundary

answers: NDQ_003351

answers: subducting

answers: NDQ_003352

answers: subducts

answers: NDQ_003353

answers: subduction

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: plate fold

answers: NDQ_003356

answers: subduct

answers: NDQ_003357

answers: The Australian Plate is subducting under the southern edge of the plate

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: subducts

answers: NDQ_003360

answers: The Timor Plate

answers: NDQ_003362

answers: The Australian Plate is subducting under the southern edge

answers: NDQ_003363

answers: Timor Plate

answers: NDQ_003371

answers: Which of the following is not a type of boundary: convergent, divergent, or transform?

answers: NDQ_003373

answers: How would you describe a rock that is deeply buried?

answers: NDQ_003376

answers: Which of the following is not a type of terrain: basin-and-range or transform boundary?

answers: NDQ_003378

answers: what is the last word in the passage?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What would happen if the Australian Plate was subducting under the southern edge of the plate?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not a type of fold that arches upward?

answers: NDQ_003385

answers: Which of the following is not a type of fault?

answers: NDQ_003386

answers: Which of the following is not a cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not a normal fault?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip or transform?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: subducting

answers: NDQ_003391

answers: The Australian Plate

answers: NDQ_003392

answers: subducting

answers: NDQ_003393

answers: The Australian Plate

answers: NDQ_003394

answers: divergent boundary

answers: NDQ_003395

answers: convergent boundary

answers: NDQ_003396

answers: divergent boundary

answers: NDQ_003351

answers: subducting

answers: NDQ_003352

answers: subducting

answers: NDQ_003353

answers: subducting

answers: NDQ_003354

answers: Banda Sea Plate

answers: NDQ_003355

answers: divergent boundary

answers: NDQ_003356

answers: subducting

answers: NDQ_003357

answers: subducting

answers: NDQ_003358

answers: convergent boundary

answers: NDQ_003359

answers: subducting

answers: NDQ_003360

answers: The Timor Plate

answers: NDQ_003362

answers: The Timor Plate is a microplate

answers: NDQ_003363

answers: The Timor Plate is a microplate in southeast Asia

answers: NDQ_003371

answers: The Timor Plate

answers: NDQ_003373

answers: The Australian Plate is subducting

answers: NDQ_003376

answers: The Timor Plate

answers: NDQ_003378

answers: The Timor Plate

answers: NDQ_003379

answers: convergent boundary exists with the Banda Sea Plate

answers: NDQ_003380

answers: The Timor Plate

answers: NDQ_003381

answers: The Timor Plate

answers: NDQ_003382

answers: convergent boundary exists with the Banda Sea Plate

answers: NDQ_003383

answers: subducting

answers: NDQ_003384

answers: transform boundary.

answers: NDQ_003385

answers: The Timor Plate

answers: NDQ_003386

answers: subducting

answers: NDQ_003387

answers: The Timor Plate

answers: NDQ_003388

answers: The Timor Plate

answers: NDQ_003389

answers: subducting

answers: NDQ_003390

answers: subducting

answers: NDQ_003391

answers: The Australian Plate

answers: NDQ_003392

answers: The Timor Plate

answers: NDQ_003393

answers: Australian Plate

answers: NDQ_003394

answers: divergent boundary

answers: NDQ_003395

answers: transform boundary.

answers: NDQ_003396

answers: divergent boundary

text: Mountain ranges are formed by the folding and buckling of a planet's crust. The mountain ranges of Venus, like those of the Earth, are characterized by many parallel folds and faults.

text: Mountain ranges are formed by the folding and buckling of a planet's crust. The mountain ranges of Venus, like those of the Earth, are characterized by many parallel folds and faults.

answers: NDQ_003351

answers: buckling

answers: NDQ_003352

answers: folds

answers: NDQ_003353

answers: buckling

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: fault

answers: NDQ_003356

answers: fold

answers: NDQ_003357

answers: parallel folds are formed

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: folds

answers: NDQ_003360

answers: Earth

answers: NDQ_003362

answers: The San Andreas fault is not a fault.

answers: NDQ_003363

answers: Venus

answers: NDQ_003371

answers: Which of the following is not a type of fault?

answers: NDQ_003373

answers: what is the reason for this?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: The amount the ground moves in an earthquake is called slip

answers: NDQ_003379

answers: no

answers: NDQ_003380

answers: None of the above choices.

answers: NDQ_003381

answers: Which of the following is not a type of stress: folding and buckling or faults?

answers: NDQ_003382

answers: what is the most common stress at convergent plates

answers: NDQ_003383

answers: None of the above choices.

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: (iv)

answers: NDQ_003387

answers: Which of the following is not caused by compression stress?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip faults, parallel folds or faults?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: parallel fold

answers: NDQ_003391

answers: unanswerable

answers: NDQ_003392

answers: parallel folds

answers: NDQ_003393

answers: is a fault

answers: NDQ_003394

answers: parallel

answers: NDQ_003395

answers: parallel folds

answers: NDQ_003396

answers: parallel fault

answers: NDQ_003351

answers: buckling

answers: NDQ_003352

answers: buckling

answers: NDQ_003353

answers: folding and buckling

answers: NDQ_003354

answers: Mountain ranges

answers: NDQ_003355

answers: buckling

answers: NDQ_003356

answers: buckling

answers: NDQ_003357

answers: folding and buckling

answers: NDQ_003358

answers: Mountain ranges

answers: NDQ_003359

answers: folding and buckling

answers: NDQ_003360

answers: folding and buckling of a planet's crust.

answers: NDQ_003362

answers: Venus,

answers: NDQ_003363

answers: Venus,

answers: NDQ_003371

answers: parallel folds and faults.

answers: NDQ_003373

answers: Mountain ranges

answers: NDQ_003376

answers: folding and buckling of a planet's crust.

answers: NDQ_003378

answers: folding and buckling

answers: NDQ_003379

answers: parallel folds

answers: NDQ_003380

answers: folding and buckling

answers: NDQ_003381

answers: buckling

answers: NDQ_003382

answers: buckling

answers: NDQ_003383

answers: folding and buckling

answers: NDQ_003384

answers: parallel folds

answers: NDQ_003385

answers: parallel folds and faults.

answers: NDQ_003386

answers: folding and buckling

answers: NDQ_003387

answers: folding and buckling of a planet's crust.

answers: NDQ_003388

answers: folding and buckling of a planet's crust.

answers: NDQ_003389

answers: the folding and buckling of a planet's crust.

answers: NDQ_003390

answers: faults.

answers: NDQ_003391

answers: Mountain ranges

answers: NDQ_003392

answers: parallel folds and faults.

answers: NDQ_003393

answers: Mountain ranges

answers: NDQ_003394

answers: parallel folds and faults.

answers: NDQ_003395

answers: parallel folds and faults.

answers: NDQ_003396

answers: parallel folds and faults.

text: The basement rocks of the continental crust tend to be much older than the oceanic crust. The oceanic crust can be from 0-250 million years in age, and is usually thinner (10 miles or so) and composed of basaltic rocks. Continental crust is older because continental crust is light and thick enough so it is not subducted, while oceanic crust is periodically subducted and replaced at subduction and oceanic rifting areas.

text: The basement rocks of the continental crust tend to be much older than the oceanic crust. The oceanic crust can be from 0-250 million years in age, and is usually thinner (10 miles or so) and composed of

text: basalt

text: ic rocks. Continental crust is older because continental crust is light and thick enough so it is not subducted, while oceanic crust is periodically subducted and replaced at

text: subduction

text: and

text: oceanic rifting

text: areas.

answers: NDQ_003351

answers: subduction

answers: NDQ_003352

answers: subducts

answers: NDQ_003353

answers: subduction

answers: NDQ_003354

answers: Toroweap Formation is older

answers: NDQ_003355

answers: subduction

answers: NDQ_003356

answers: subduct

answers: NDQ_003357

answers: continental crust is light and thick enough so it is not subducted

answers: NDQ_003358

answers: basaltic

answers: NDQ_003359

answers: subducts

answers: NDQ_003360

answers: continental crust

answers: NDQ_003362

answers: oceanic crust can be from 0-250 million years in age

answers: NDQ_003363

answers: oceanic crust

answers: NDQ_003371

answers: What may be the reason for the thicker crust?

answers: NDQ_003373

answers: Why is the continental crust lighter than the oceanic crust?

answers: NDQ_003376

answers: basin-and-range

answers: NDQ_003378

answers: The amount the ground moves in an earthquake is called slip.

answers: NDQ_003379

answers: vertical

answers: NDQ_003380

answers: Which of the following is not a stress?

answers: NDQ_003381

answers: What type of rock does the oceanic crust contain?

answers: NDQ_003382

answers: None of the above choices.

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: What type of fold is a syncline?

answers: NDQ_003385

answers: faults are clustered

answers: NDQ_003386

answers: subduction and oceanic rifting areas

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: basaltic rocks or oceanic crust?

answers: NDQ_003388

answers: Which of the following is not a type of strike-slip fault?

answers: NDQ_003389

answers: subduction

answers: NDQ_003390

answers: subduction

answers: NDQ_003391

answers: basement

answers: NDQ_003392

answers: subduction

answers: NDQ_003393

answers: basement

answers: NDQ_003394

answers: isobath

answers: NDQ_003395

answers: is a fault

answers: NDQ_003396

answers: The oceanic crust

answers: NDQ_003351

answers: subducted and replaced at subduction

answers: NDQ_003352

answers: subducted,

answers: NDQ_003353

answers: subducted,

answers: NDQ_003354

answers: Continental crust

answers: NDQ_003355

answers: subduction

answers: NDQ_003356

answers: subducted,

answers: NDQ_003357

answers: oceanic crust is periodically subducted and replaced at subduction

answers: NDQ_003358

answers: basement rocks

answers: NDQ_003359

answers: subducted,

answers: NDQ_003360

answers: continental crust tend to be much older than the oceanic crust.

answers: NDQ_003362

answers: continental crust is light and thick enough so it is not subducted,

answers: NDQ_003363

answers: subduction and oceanic rifting areas.

answers: NDQ_003371

answers: continental crust tend to be much older than the oceanic crust.

answers: NDQ_003373

answers: The basement rocks

answers: NDQ_003376

answers: continental crust is light and thick enough so it is not subducted,

answers: NDQ_003378

answers: The oceanic crust

answers: NDQ_003379

answers: The oceanic crust

answers: NDQ_003380

answers: The oceanic crust

answers: NDQ_003381

answers: subducted,

answers: NDQ_003382

answers: subducted,

answers: NDQ_003383

answers: oceanic crust is periodically subducted

answers: NDQ_003384

answers: Continental crust

answers: NDQ_003385

answers: The basement rocks of the continental crust

answers: NDQ_003386

answers: oceanic crust is periodically subducted and replaced at subduction

answers: NDQ_003387

answers: The oceanic crust

answers: NDQ_003388

answers: The oceanic crust

answers: NDQ_003389

answers: continental crust is light and thick enough so it is not subducted,

answers: NDQ_003390

answers: subduction

answers: NDQ_003391

answers: basement rocks

answers: NDQ_003392

answers: subduction

answers: NDQ_003393

answers: basement rocks

answers: NDQ_003394

answers: subducted,

answers: NDQ_003395

answers: subduction

answers: NDQ_003396

answers: oceanic crust.

text: Finally, in the Paleogene and Neogene Periods (~66 million to ~1.8 million years ago), the mountain chains that today constitute the Atlas were uplifted, as the land masses of Europe and Africa collided at the southern end of the Iberian Peninsula. Such convergent tectonic boundaries occur where two plates slide towards each other forming a subduction zone (if one plate moves underneath the other), and/or a continental collision (when the two plates contain continental crust). In the case of the Africa-Europe collision, it is clear that tectonic convergence is partially responsible for the formation of the High Atlas, as well as for the closure of the Strait of Gibraltar and the formation of the Alps and the Pyrenees. However, there is a lack of evidence for the nature of the subduction in the Atlas region, or for the thickening of the Earth's crust generally associated with continental collisions. In fact, one of the most striking features of the Atlas to geologists is the relative small amount of crustal thickening and tectonic shortening despite the important altitude of the mountain range. Recent studies suggest that deep processes rooted in the Earth's mantle may have contributed to the uplift of the High and Middle Atlas.

text: Finally, in the

text: Paleogene

text: and

text: Neogene

text: Periods (~66 million to ~1.8 million years ago), the mountain chains that today constitute the Atlas were uplifted, as the land masses of Europe and Africa collided at the southern end of the

text: Iberian Peninsula

text: . Such

text: convergent tectonic boundaries

text: occur where two plates slide towards each other forming a

text: subduction

text: zone (if one plate moves underneath the other), and/or a

text: continental collision

text: (when the two plates contain

text: continental crust

text: ). In the case of the Africa-Europe collision, it is clear that tectonic convergence is partially responsible for the formation of the

text: High Atlas

text: , as well as for the closure of the

text: Strait of Gibraltar

text: and the formation of the

text: Alps

text: and the

text: Pyrenees

text: . However, there is a lack of evidence for the nature of the subduction in the Atlas region, or for the thickening of the Earth's crust generally associated with continental collisions. In fact, one of the most striking features of the Atlas to geologists is the relative small amount of crustal thickening and tectonic shortening despite the important altitude of the mountain range. Recent studies suggest that deep processes rooted in the Earth's mantle may have contributed to the uplift of the High and Middle Atlas.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: thickens

answers: NDQ_003353

answers: subduction

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: subduction zone

answers: NDQ_003356

answers: thicken

answers: NDQ_003357

answers: one plate moves underneath the other

answers: NDQ_003358

answers: unanswerable

answers: NDQ_003359

answers: one plate moves underneath the other

answers: NDQ_003360

answers: tectonic boundaries

answers: NDQ_003362

answers: there is a lack of evidence for the nature of the subduction

answers: NDQ_003363

answers: Paleogene and Neogene Periods

answers: NDQ_003371

answers: subduction zone (if one plate moves underneath the other)

answers: NDQ_003373

answers: if one plate moves underneath the other

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What happens when one plate moves underneath the other?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: unanswerable

answers: NDQ_003386

answers: two plates slide towards each other

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: unanswerable

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: subduction zone

answers: NDQ_003391

answers: subduction zone

answers: NDQ_003392

answers: subduction zone

answers: NDQ_003393

answers: subduction zone

answers: NDQ_003394

answers: subduction zone

answers: NDQ_003395

answers: convergent tectonic boundaries occur where two plates slide towards each other

answers: NDQ_003396

answers: subduction zone

answers: NDQ_003351

answers: subduction zone

answers: NDQ_003352

answers: thickening

answers: NDQ_003353

answers: thickening

answers: NDQ_003354

answers: subduction zone

answers: NDQ_003355

answers: subduction zone

answers: NDQ_003356

answers: subduction zone

answers: NDQ_003357

answers: one plate moves underneath the other),

answers: NDQ_003358

answers: subduction zone

answers: NDQ_003359

answers: one plate moves underneath the other),

answers: NDQ_003360

answers: the land masses of Europe and Africa collided

answers: NDQ_003362

answers: thickening of the Earth's crust generally associated with continental collisions.

answers: NDQ_003363

answers: southern end of the Iberian Peninsula.

answers: NDQ_003371

answers: subduction zone

answers: NDQ_003373

answers: deep processes rooted in the Earth's mantle

answers: NDQ_003376

answers: subduction zone

answers: NDQ_003378

answers: subduction zone

answers: NDQ_003379

answers: subduction zone

answers: NDQ_003380

answers: subduction zone

answers: NDQ_003381

answers: subduction zone

answers: NDQ_003382

answers: subduction zone

answers: NDQ_003383

answers: subduction zone

answers: NDQ_003384

answers: subduction zone

answers: NDQ_003385

answers: subduction zone

answers: NDQ_003386

answers: subduction zone

answers: NDQ_003387

answers: subduction zone

answers: NDQ_003388

answers: two plates slide towards each other forming a subduction zone

answers: NDQ_003389

answers: uplifted,

answers: NDQ_003390

answers: subduction zone

answers: NDQ_003391

answers: subduction zone

answers: NDQ_003392

answers: subduction zone

answers: NDQ_003393

answers: subduction zone

answers: NDQ_003394

answers: two plates slide towards each other forming a subduction zone

answers: NDQ_003395

answers: subduction zone

answers: NDQ_003396

answers: subduction zone

text: Heat flows constantly from its sources within the Earth to the surface. Total heat loss from the Earth is estimated at 44.2 TW (). Mean heat flow is 65 mW/m over continental crust and 101 mW/m over oceanic crust. This is 0.087 watt/square meter on average (0.03 percent of solar power absorbed by the Earth ), but is much more concentrated in areas where thermal energy is transported toward the crust by convection such as along mid-ocean ridges and mantle plumes.The Earth's crust effectively acts as a thick insulating blanket which must be pierced by fluid conduits (of magma, water or other) in order to release the heat underneath. More of the heat in the Earth is lost through plate tectonics, by mantle upwelling associated with mid-ocean ridges. The final major mode of heat loss is by conduction through the lithosphere, the majority of which occurs in the oceans due to the crust there being much thinner and younger than under the continents.

text: Heat flows constantly from its sources within the Earth to the surface. Total heat loss from the Earth is estimated at 44.2 TW (). Mean heat flow is 65 mW/m over

text: continental crust

text: and 101 mW/m over

text: oceanic crust

text: . This is 0.087 watt/square meter on average (0.03 percent of solar power absorbed by the Earth ), but is much more concentrated in areas where thermal energy is transported toward the crust by convection such as along

text: mid-ocean ridge

text: s and

text: mantle plume

text: s.The

text: Earth's crust

text: effectively acts as a thick insulating blanket which must be pierced by fluid conduits (of magma, water or other) in order to release the heat underneath. More of the heat in the Earth is lost through plate tectonics, by mantle upwelling associated with mid-ocean ridges. The final major mode of heat loss is by

text: conduction

text: through the

text: lithosphere

text: , the majority of which occurs in the oceans due to the crust there being much thinner and younger than under the continents.

answers: NDQ_003351

answers: convection

answers: NDQ_003352

answers: heats up

answers: NDQ_003353

answers: heat to flow

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: ridge

answers: NDQ_003356

answers: heat up

answers: NDQ_003357

answers: heat flow is 65 mW/m

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: continental crust

answers: NDQ_003362

answers: heat flows constantly from its sources within the Earth to the surface

answers: NDQ_003363

answers: tectonics

answers: NDQ_003371

answers: What is the last major mode of heat loss?

answers: NDQ_003373

answers: What is the last major mode of heat loss?

answers: NDQ_003376

answers: What is the last major mode of heat loss?

answers: NDQ_003378

answers: What is the last major mode of heat loss?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: How does the Earth's crust effectively act as a thick insulating blanket

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the final major mode of heat loss?

answers: NDQ_003384

answers: What type of fold is a syncline?

answers: NDQ_003385

answers: What is the last major mode of heat loss?

answers: NDQ_003386

answers: plate tectonics

answers: NDQ_003387

answers: What causes plate tectonics?

answers: NDQ_003388

answers: What is the primary mode of heat loss from the Earth?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: plate tectonics

answers: NDQ_003391

answers: continental crust

answers: NDQ_003392

answers: tectonics

answers: NDQ_003393

answers: continental crust

answers: NDQ_003394

answers: continental crust

answers: NDQ_003395

answers: plate tectonics

answers: NDQ_003396

answers: tectonics

answers: NDQ_003351

answers: mantle upwelling

answers: NDQ_003352

answers: mantle upwelling

answers: NDQ_003353

answers: mantle upwelling

answers: NDQ_003354

answers: 101 mW/m over oceanic crust.

answers: NDQ_003355

answers: ridges

answers: NDQ_003356

answers: insulating blanket

answers: NDQ_003357

answers: mantle upwelling

answers: NDQ_003358

answers: lithosphere,

answers: NDQ_003359

answers: pierced by fluid conduits

answers: NDQ_003360

answers: plate tectonics,

answers: NDQ_003362

answers: Heat

answers: NDQ_003363

answers: plate tectonics,

answers: NDQ_003371

answers: mid-ocean ridges.

answers: NDQ_003373

answers: plumes.The Earth's crust effectively acts as a thick insulating blanket

answers: NDQ_003376

answers: mid-ocean ridges

answers: NDQ_003378

answers: Heat

answers: NDQ_003379

answers: 44.2 TW

answers: NDQ_003380

answers: pierced by fluid conduits

answers: NDQ_003381

answers: plumes.The Earth's crust effectively acts as a thick insulating blanket

answers: NDQ_003382

answers: mantle upwelling

answers: NDQ_003383

answers: pierced by fluid conduits

answers: NDQ_003384

answers: mid-ocean ridges

answers: NDQ_003385

answers: Heat

answers: NDQ_003386

answers: plate tectonics,

answers: NDQ_003387

answers: plate tectonics,

answers: NDQ_003388

answers: Heat

answers: NDQ_003389

answers: plate tectonics,

answers: NDQ_003390

answers: plate tectonics,

answers: NDQ_003391

answers: lithosphere,

answers: NDQ_003392

answers: Heat

answers: NDQ_003393

answers: lithosphere,

answers: NDQ_003394

answers: plate tectonics,

answers: NDQ_003395

answers: plate tectonics,

answers: NDQ_003396

answers: plate tectonics,

text: Taixinan Basin is located on the continental shelf, on the margin of the continental crust. Its tectonic evolution can be divided in three periods. The first peiod was from Paleocene to Oligocene. Starting in the Paleocene, Taixinan Basin had been experiencing the effect of rifting, which eventually caused the formation of the basin. The tensile stress field was in the NE-SW direction. Many normal faults developed at this period. The second period was the end of Oligocene. During this period, the Taixinan Basin experienced the effect of compression. Part of the early normal faults underwent tectonic inversion, and a lot of reverse faults and related folds developed. The third period was the thermal subsidence beginning from Miocene. Since the late Miocene, the South China Sea basin stopped its expansion. During this period, the sediment layers are horizontal and basically not controlled by the effects of faulting.

text: Taixinan Basin is located on the continental shelf, on the margin of the continental crust. Its tectonic evolution can be divided in three periods. The first peiod was from Paleocene to Oligocene. Starting in the Paleocene, Taixinan Basin had been experiencing the effect of rifting, which eventually caused the formation of the basin. The tensile stress field was in the NE-SW direction. Many normal faults developed at this period. The second period was the end of Oligocene. During this period, the Taixinan Basin experienced the effect of compression. Part of the early normal faults underwent tectonic inversion, and a lot of reverse faults and related folds developed. The third period was the thermal subsidence beginning from Miocene. Since the late Miocene, the South China Sea basin stopped its expansion. During this period, the

text: sediment

text: layers are horizontal and basically not controlled by the effects of faulting.

answers: NDQ_003351

answers: normal faults

answers: NDQ_003352

answers: compresses

answers: NDQ_003353

answers: normal faults to develop

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: reverse fault

answers: NDQ_003356

answers: compress

answers: NDQ_003357

answers: The tensile stress field was in the NE-SW direction.

answers: NDQ_003358

answers: normal fault

answers: NDQ_003359

answers: normal faults

answers: NDQ_003360

answers: continental crust

answers: NDQ_003362

answers: Its tectonic evolution can be divided in three periods

answers: NDQ_003363

answers: Paleocene

answers: NDQ_003371

answers: Which of the following is not a type of fault: normal faults, compression, or thermal subsidence?

answers: NDQ_003373

answers: Which of the following is not a type of stress?

answers: NDQ_003376

answers: Which of the following is not a type of terrain: basin-and-range or rifting?

answers: NDQ_003378

answers: what is the last period mentioned?

answers: NDQ_003379

answers: What is the dip of the fault plane in a strike-slip fault?

answers: NDQ_003380

answers: What caused the formation of the basin?

answers: NDQ_003381

answers: Which of the following is not a type of stress: compression, rifting, or thermal subsidence?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock: normal faults or compression?

answers: NDQ_003384

answers: Which of the following is not a type of fold: reverse faults or synclines?

answers: NDQ_003385

answers: Which of the following is not a type of fault?

answers: NDQ_003386

answers: Which of the following is not the cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: normal faults or reverse faults?

answers: NDQ_003388

answers: Which of the following is not a type of fault: normal faults, strike-slip faults or reverse faults?

answers: NDQ_003389

answers: Which of the following is not a type of fold: normal faults, folding or thermal subsidence?

answers: NDQ_003390

answers: normal faults

answers: NDQ_003391

answers: rifting

answers: NDQ_003392

answers: rifting

answers: NDQ_003393

answers: rifting

answers: NDQ_003394

answers: normal faults

answers: NDQ_003395

answers: normal faults

answers: NDQ_003396

answers: thermal subsidence

answers: NDQ_003351

answers: tensile

answers: NDQ_003352

answers: normal faults

answers: NDQ_003353

answers: normal faults

answers: NDQ_003354

answers: Taixinan Basin

answers: NDQ_003355

answers: reverse faults

answers: NDQ_003356

answers: compression.

answers: NDQ_003357

answers: NE-SW direction.

answers: NDQ_003358

answers: thermal subsidence

answers: NDQ_003359

answers: tectonic inversion,

answers: NDQ_003360

answers: continental shelf, on the margin of the continental crust.

answers: NDQ_003362

answers: not controlled by the effects of faulting.

answers: NDQ_003363

answers: Paleocene to Oligocene.

answers: NDQ_003371

answers: normal faults

answers: NDQ_003373

answers: Oligocene.

answers: NDQ_003376

answers: The second period was the end of Oligocene.

answers: NDQ_003378

answers: compression.

answers: NDQ_003379

answers: thermal subsidence

answers: NDQ_003380

answers: tensile stress

answers: NDQ_003381

answers: compression.

answers: NDQ_003382

answers: compression.

answers: NDQ_003383

answers: faults

answers: NDQ_003384

answers: reverse faults and related folds

answers: NDQ_003385

answers: normal faults

answers: NDQ_003386

answers: normal faults

answers: NDQ_003387

answers: compression.

answers: NDQ_003388

answers: reverse faults

answers: NDQ_003389

answers: thermal subsidence

answers: NDQ_003390

answers: reverse faults

answers: NDQ_003391

answers: folds

answers: NDQ_003392

answers: reverse faults

answers: NDQ_003393

answers: folds

answers: NDQ_003394

answers: reverse faults

answers: NDQ_003395

answers: normal faults

answers: NDQ_003396

answers: thermal subsidence

text: The most important parameter controlling the maximum earthquake magnitude on a fault is however not the maximum available length, but the available width because the latter varies by a factor of 20. Along converging plate margins, the dip angle of the rupture plane is very shallow, typically about 10 degrees. Thus the width of the plane within the top brittle crust of the Earth can become 50 to 100 km (Japan, 2011; Alaska, 1964), making the most powerful earthquakes possible.

text: The most important parameter controlling the maximum earthquake magnitude on a fault is however not the maximum available length, but the available width because the latter varies by a factor of 20. Along converging plate margins, the dip angle of the rupture plane is very shallow, typically about 10 degrees. Thus the width of the plane within the top brittle crust of the Earth can become 50 to 100 km (

text: Japan, 2011

text: Alaska, 1964

text: ), making the most powerful earthquakes possible.

answers: NDQ_003351

answers: about 10 degrees

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: dip angle

answers: NDQ_003356

answers: crack

answers: NDQ_003357

answers: the dip angle of the rupture plane is very shallow

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: ruptures

answers: NDQ_003360

answers: plate margins

answers: NDQ_003362

answers: the maximum available length

answers: NDQ_003363

answers: unanswerable

answers: NDQ_003371

answers: What is the maximum earthquake magnitude on a fault?

answers: NDQ_003373

answers: Why is the dip angle of the rupture plane very shallow

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: no

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What does the dip angle of the rupture plane typically mean?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: Fault zone

answers: NDQ_003386

answers: yes

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: What is the maximum earthquake magnitude on a fault?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: dip angle of the rupture plane

answers: NDQ_003391

answers: brittle crust

answers: NDQ_003392

answers: converging plate margins

answers: NDQ_003393

answers: brittle crust

answers: NDQ_003394

answers: converging plate margins

answers: NDQ_003395

answers: converging plate margins

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: the dip angle of the rupture plane is very shallow, typically about 10 degrees.

answers: NDQ_003352

answers: brittle

answers: NDQ_003353

answers: brittle

answers: NDQ_003354

answers: The most important parameter controlling the maximum earthquake magnitude

answers: NDQ_003355

answers: fault

answers: NDQ_003356

answers: brittle

answers: NDQ_003357

answers: width

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: brittle crust

answers: NDQ_003360

answers: converging plate margins,

answers: NDQ_003362

answers: maximum available length,

answers: NDQ_003363

answers: converging plate margins,

answers: NDQ_003371

answers: The most important parameter controlling the maximum earthquake magnitude on a fault

answers: NDQ_003373

answers: 50 to 100 km

answers: NDQ_003376

answers: width

answers: NDQ_003378

answers: width

answers: NDQ_003379

answers: 10 degrees.

answers: NDQ_003380

answers: earthquake magnitude on a fault is however not the maximum available length,

answers: NDQ_003381

answers: width

answers: NDQ_003382

answers: the dip angle of the rupture plane is very shallow, typically about 10 degrees.

answers: NDQ_003383

answers: length,

answers: NDQ_003384

answers: fault is however not the maximum available length,

answers: NDQ_003385

answers: fault

answers: NDQ_003386

answers: width

answers: NDQ_003387

answers: width

answers: NDQ_003388

answers: width because the latter varies by a factor of 20.

answers: NDQ_003389

answers: width

answers: NDQ_003390

answers: the dip angle of the rupture plane is very shallow, typically about 10 degrees.

answers: NDQ_003391

answers: brittle crust

answers: NDQ_003392

answers: fault

answers: NDQ_003393

answers: brittle crust

answers: NDQ_003394

answers: Along converging plate margins,

answers: NDQ_003395

answers: the dip angle of the rupture plane is very shallow, typically about 10 degrees.

answers: NDQ_003396

answers: Along converging plate margins,

text: Scientifically the archipelago is defined as a volcanic arc. The origin of the Aeolian Islands is due to movement of the Earth's crust as a result of plate tectonics. The African continental shelf is in constant movement towards Europe. The resulting collision has created a volcanic area with ruptures in the Earth's crust with consequent eruptions of magma. The "Aeolian Arc" extends for more than , but the area of geological instability caused by the collision of Africa and Europe is much larger. It includes Sicily, Calabria, and Campania together with Greece and the Aegean islands.

text: Scientifically the archipelago is defined as a

text: volcanic arc

text: . The origin of the Aeolian Islands is due to movement of the

text: Earth's crust

text: as a result of

text: plate tectonics

text: . The

text: Africa

text: n

text: continental shelf

text: is in constant movement towards Europe. The resulting collision has created a volcanic area with ruptures in the Earth's crust with consequent eruptions of

text: magma

text: . The "Aeolian Arc" extends for more than , but the area of geological instability caused by the collision of Africa and Europe is much larger. It includes Sicily, Calabria, and Campania together with Greece and the Aegean islands.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: ruptures

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: erupt

answers: NDQ_003357

answers: ruptures in the Earth's crust with consequent eruptions of magma

answers: NDQ_003358

answers: volcanic area

answers: NDQ_003359

answers: ruptures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: the area of geological instability caused by the collision of Africa and Europe is much larger

answers: NDQ_003363

answers: plate tectonics

answers: NDQ_003371

answers: Which of the following is not a result of plate tectonics: movement of the Earth's crust as a result of plate tectonics?

answers: NDQ_003373

answers: what is the last word in the passage?

answers: NDQ_003376

answers: Which of the following is not a type of terrain: basin-and-range or plate tectonics?

answers: NDQ_003378

answers: what is the last word in the passage?

answers: NDQ_003379

answers: Which of the following is not true of strike-slip faults:

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: Which of the following is not a result of plate tectonics: movement of the Earth's crust?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock: plate tectonics?

answers: NDQ_003384

answers: Which of the following is not a type of fold: syncline, fold, or fold?

answers: NDQ_003385

answers: What is the area of geological instability caused by the collision of Africa and Europe

answers: NDQ_003386

answers: plate tectonics

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: plate tectonics, plate tectonics, or magma?

answers: NDQ_003388

answers: Which of the following is not a result of plate tectonics: movement of the Earth's crust as a result of plate tectonics?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: plate tectonics

answers: NDQ_003391

answers: continental shelf

answers: NDQ_003392

answers: ruptures in the Earth's crust

answers: NDQ_003393

answers: continental shelf

answers: NDQ_003394

answers: ruptures

answers: NDQ_003395

answers: plate tectonics

answers: NDQ_003396

answers: plate tectonics

answers: NDQ_003351

answers: eruptions of magma.

answers: NDQ_003352

answers: ruptures

answers: NDQ_003353

answers: ruptures

answers: NDQ_003354

answers: "Aeolian Arc"

answers: NDQ_003355

answers: volcanic arc.

answers: NDQ_003356

answers: eruptions of magma.

answers: NDQ_003357

answers: ruptures in the Earth's crust

answers: NDQ_003358

answers: volcanic arc.

answers: NDQ_003359

answers: plate tectonics.

answers: NDQ_003360

answers: plate tectonics.

answers: NDQ_003362

answers: eruptions of magma.

answers: NDQ_003363

answers: collision of Africa and Europe

answers: NDQ_003371

answers: plate tectonics.

answers: NDQ_003373

answers: plate tectonics.

answers: NDQ_003376

answers: plate tectonics.

answers: NDQ_003378

answers: Earth's crust as a result of plate tectonics.

answers: NDQ_003379

answers: Europe.

answers: NDQ_003380

answers: geological instability

answers: NDQ_003381

answers: geological instability

answers: NDQ_003382

answers: Europe.

answers: NDQ_003383

answers: ruptures

answers: NDQ_003384

answers: volcanic arc.

answers: NDQ_003385

answers: volcanic arc.

answers: NDQ_003386

answers: plate tectonics.

answers: NDQ_003387

answers: plate tectonics.

answers: NDQ_003388

answers: plate tectonics.

answers: NDQ_003389

answers: plate tectonics.

answers: NDQ_003390

answers: plate tectonics.

answers: NDQ_003391

answers: volcanic arc.

answers: NDQ_003392

answers: "Aeolian Arc"

answers: NDQ_003393

answers: volcanic arc.

answers: NDQ_003394

answers: ruptures

answers: NDQ_003395

answers: ruptures in the Earth's crust

answers: NDQ_003396

answers: plate tectonics.

text: While the San Andreas Fault is the principal transform boundary between the Pacific Plate and the North American Plate, the Hayward Fault takes up a share of the overall motion between the plates.

text: While the San Andreas Fault is the principal

text: transform boundary

text: between the

text: Pacific Plate

text: and the

text: North American Plate

text: , the Hayward Fault takes up a share of the overall motion between the plates.

answers: NDQ_003351

answers: Hayward Fault

answers: NDQ_003352

answers: moves faster

answers: NDQ_003353

answers: movement

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: change shape

answers: NDQ_003357

answers: the San Andreas Fault is where?

answers: NDQ_003358

answers: Fault

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Hayward Fault

answers: NDQ_003362

answers: The Hayward Fault takes up a share of the overall motion between the plates.

answers: NDQ_003363

answers: San Andreas Fault

answers: NDQ_003371

answers: Which of the following is not a type of fault?

answers: NDQ_003373

answers: How would you describe compressive stresses?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What is the main idea of this passage?

answers: NDQ_003381

answers: What is the principal transform boundary between the Pacific Plate and the North American Plate

answers: NDQ_003382

answers: what is the most common stress at convergent plates?

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What type of fold is the San Andreas Fault?

answers: NDQ_003385

answers: NDQ_003386

answers: (d).

answers: NDQ_003387

answers: What is the cause of the San Andreas Fault?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip, Hayward, or transform?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: Hayward Fault

answers: NDQ_003391

answers: sandstone

answers: NDQ_003392

answers: Hayward Fault

answers: NDQ_003393

answers: isotope

answers: NDQ_003394

answers: Hayward Fault

answers: NDQ_003395

answers: Hayward Fault

answers: NDQ_003396

answers: Hayward Fault

answers: NDQ_003351

answers: Hayward Fault

answers: NDQ_003352

answers: Hayward Fault

answers: NDQ_003353

answers: motion

answers: NDQ_003354

answers: the Hayward Fault

answers: NDQ_003355

answers: San Andreas Fault

answers: NDQ_003356

answers: Hayward Fault

answers: NDQ_003357

answers: motion between the plates.

answers: NDQ_003358

answers: Hayward Fault

answers: NDQ_003359

answers: San Andreas Fault

answers: NDQ_003360

answers: San Andreas Fault

answers: NDQ_003362

answers: the Hayward Fault

answers: NDQ_003363

answers: San Andreas Fault

answers: NDQ_003371

answers: Hayward Fault

answers: NDQ_003373

answers: While the San Andreas Fault

answers: NDQ_003376

answers: the Hayward Fault

answers: NDQ_003378

answers: the Hayward Fault takes up a share of the overall motion

answers: NDQ_003379

answers: Hayward Fault

answers: NDQ_003380

answers: motion

answers: NDQ_003381

answers: Hayward Fault

answers: NDQ_003382

answers: the Hayward Fault

answers: NDQ_003383

answers: motion

answers: NDQ_003384

answers: Hayward Fault

answers: NDQ_003385

answers: San Andreas Fault

answers: NDQ_003386

answers: the Hayward Fault

answers: NDQ_003387

answers: Hayward Fault

answers: NDQ_003388

answers: Hayward Fault

answers: NDQ_003389

answers: the San Andreas Fault

answers: NDQ_003390

answers: Hayward Fault

answers: NDQ_003391

answers: Pacific Plate and the North American Plate,

answers: NDQ_003392

answers: Hayward Fault

answers: NDQ_003393

answers: Hayward Fault

answers: NDQ_003394

answers: Hayward Fault

answers: NDQ_003395

answers: Hayward Fault

answers: NDQ_003396

answers: Hayward Fault

text: Contact with India began along the Yarlung-Zangbo suture around 50 Ma during the Eocene, and the two continents continue to converge. Magmatism continued in the Gangdese arc until as late as 40 Ma.There are competing hypotheses about the details of the tectonic processes during the collision between the Indian and Eurasian plates.At one extreme, some consider that during the collision the Indian crust was underthrust beneath the southern Asian crust, or injected into this crust. At the other extreme, some consider that the convergence was mostly accommodated by shortening of the Asian crust.

text: Contact with India began along the Yarlung-Zangbo suture around 50 Ma during the

text: Eocene

text: , and the two continents continue to converge. Magmatism continued in the Gangdese arc until as late as 40 Ma.There are competing hypotheses about the details of the

text: tectonic

text: processes during the collision between the Indian and Eurasian plates.At one extreme, some consider that during the collision the Indian crust was underthrust beneath the southern Asian crust, or injected into this crust. At the other extreme, some consider that the convergence was mostly accommodated by shortening of the Asian crust.

answers: NDQ_003351

answers: underthrust

answers: NDQ_003352

answers: underthrusts

answers: NDQ_003353

answers: magma

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: suture

answers: NDQ_003356

answers: underthrust

answers: NDQ_003357

answers: underthrust is a term used to describe

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: underthrust

answers: NDQ_003360

answers: plates

answers: NDQ_003362

answers: Indian crust was underthrust beneath the southern Asian crust

answers: NDQ_003363

answers: Eocene

answers: NDQ_003371

answers: Which of the following is not a tectonic process: collision between the Indian and Eurasian plates?

answers: NDQ_003373

answers: How would you describe a rock that is deeply buried?

answers: NDQ_003376

answers: What type of terrain is caused by compressive forces?

answers: NDQ_003378

answers: what is the last time period mentioned?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What would happen if the Indian crust was underthrust beneath the southern Asian crust?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: What type of fold is the Gangdese arc?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: Which of the following is not a cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: underthrust beneath the southern Asian crust, or injected into this crust?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip, underthrust, or injected?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: underthrust

answers: NDQ_003391

answers: underthrust

answers: NDQ_003392

answers: underthrust

answers: NDQ_003393

answers: underthrust

answers: NDQ_003394

answers: underthrust

answers: NDQ_003395

answers: underthrust

answers: NDQ_003396

answers: underthrust

answers: NDQ_003351

answers: shortening of the Asian crust.

answers: NDQ_003352

answers: underthrust

answers: NDQ_003353

answers: Magmatism

answers: NDQ_003354

answers: Contact with India

answers: NDQ_003355

answers: arc

answers: NDQ_003356

answers: Magmatism

answers: NDQ_003357

answers: shortening of the Asian crust.

answers: NDQ_003358

answers: Magmatism

answers: NDQ_003359

answers: collision between the Indian and Eurasian plates.At

answers: NDQ_003360

answers: Magmatism

answers: NDQ_003362

answers: shortening of the Asian crust.

answers: NDQ_003363

answers: Gangdese arc

answers: NDQ_003371

answers: the Indian crust was underthrust

answers: NDQ_003373

answers: underthrust beneath the southern Asian crust,

answers: NDQ_003376

answers: underthrust beneath the southern Asian crust,

answers: NDQ_003378

answers: underthrust

answers: NDQ_003379

answers: underthrust beneath the southern Asian crust,

answers: NDQ_003380

answers: underthrust beneath the southern Asian crust,

answers: NDQ_003381

answers: underthrust beneath the southern Asian crust,

answers: NDQ_003382

answers: shortening of the Asian crust.

answers: NDQ_003383

answers: underthrust

answers: NDQ_003384

answers: Yarlung-Zangbo suture

answers: NDQ_003385

answers: Yarlung-Zangbo suture

answers: NDQ_003386

answers: tectonic

answers: NDQ_003387

answers: underthrust beneath the southern Asian crust,

answers: NDQ_003388

answers: 50 Ma during the Eocene,

answers: NDQ_003389

answers: Magmatism

answers: NDQ_003390

answers: Yarlung-Zangbo suture

answers: NDQ_003391

answers: Indian crust was underthrust beneath the southern Asian crust,

answers: NDQ_003392

answers: Yarlung-Zangbo suture

answers: NDQ_003393

answers: Indian crust was underthrust beneath the southern Asian crust,

answers: NDQ_003394

answers: Yarlung-Zangbo suture

answers: NDQ_003395

answers: Yarlung-Zangbo suture

answers: NDQ_003396

answers: Yarlung-Zangbo suture

text: Alison Games (2006) explores the convergence of the multiple strands of scholarly interest that have generated the new field of Atlantic history, which takes as its geographic unit of analysis the Atlantic Ocean and the four continents that surround it. She argues Atlantic history is best approached as a slice of world history. The Atlantic, moreover, is a region that has logic as a unit of historical analysis only within a limited chronology. An Atlantic perspective can help historians understand changes within the region that a more limited geographic framework might obscure. Attempts to write a Braudelian Atlantic history, one that includes and connects the entire region, remain elusive, driven in part by methodological impediments, by the real disjunction that characterized the Atlantic's historical and geographic components, by the disciplinary divisions that discourage historians from speaking to and writing for each other, and by the challenge of finding a vantage point that is not rooted in any single place.

text: Alison Games (2006) explores the convergence of the multiple strands of scholarly interest that have generated the new field of Atlantic history, which takes as its geographic unit of analysis the Atlantic Ocean and the four continents that surround it. She argues Atlantic history is best approached as a slice of world history. The Atlantic, moreover, is a region that has logic as a unit of historical analysis only within a limited chronology. An Atlantic perspective can help historians understand changes within the region that a more limited geographic framework might obscure. Attempts to write a Braudelian Atlantic history, one that includes and connects the entire region, remain elusive, driven in part by methodological impediments, by the real disjunction that characterized the Atlantic's historical and geographic components, by the disciplinary divisions that discourage historians from speaking to and writing for each other, and by the challenge of finding a vantage point that is not rooted in any single place.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: more likely to crack

answers: NDQ_003353

answers: igneous rocks to form

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: Braudelian

answers: NDQ_003356

answers: swell

answers: NDQ_003357

answers: An Atlantic perspective can help historians understand changes within the region that a more limited geographic framework might obscure

answers: NDQ_003358

answers: unmoving

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: continental plates

answers: NDQ_003362

answers: the San Andreas fault is not rooted in any single place

answers: NDQ_003363

answers: Atlantic

answers: NDQ_003371

answers: What may be a thrust fault in between

answers: NDQ_003373

answers: How would you describe Alison Games?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: vertical

answers: NDQ_003380

answers: What is the main idea of this passage?

answers: NDQ_003381

answers: What is the name of the new field of Atlantic history

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: Fault zone

answers: NDQ_003386

answers: movement of rock at faults

answers: NDQ_003387

answers: None of the above choices.

answers: NDQ_003388

answers: What is the name of the new field of Atlantic history?

answers: NDQ_003389

answers: the Atlantic

answers: NDQ_003390

answers: Braudelian

answers: NDQ_003391

answers: dip-slip fault

answers: NDQ_003392

answers: Braudelian

answers: NDQ_003393

answers: dip-slip fault plane

answers: NDQ_003394

answers: a Braudelian

answers: NDQ_003395

answers: Braudelian

answers: NDQ_003396

answers: Braudelian

answers: NDQ_003351

answers: Atlantic history,

answers: NDQ_003352

answers: Atlantic history,

answers: NDQ_003353

answers: Atlantic history,

answers: NDQ_003354

answers: Alison Games (2006)

answers: NDQ_003355

answers: Braudelian

answers: NDQ_003356

answers: Atlantic history,

answers: NDQ_003357

answers: disciplinary divisions that discourage historians from speaking to and writing for each other,

answers: NDQ_003358

answers: Atlantic Ocean

answers: NDQ_003359

answers: limited chronology.

answers: NDQ_003360

answers: Atlantic Ocean

answers: NDQ_003362

answers: Alison Games (2006)

answers: NDQ_003363

answers: Atlantic history, which takes as its geographic unit of analysis the Atlantic Ocean

answers: NDQ_003371

answers: Atlantic history,

answers: NDQ_003373

answers: Alison Games (2006)

answers: NDQ_003376

answers: Atlantic Ocean

answers: NDQ_003378

answers: Atlantic history,

answers: NDQ_003379

answers: Atlantic history,

answers: NDQ_003380

answers: Atlantic history,

answers: NDQ_003381

answers: Atlantic history,

answers: NDQ_003382

answers: convergence of the multiple strands of scholarly interest

answers: NDQ_003383

answers: Atlantic history,

answers: NDQ_003384

answers: Atlantic history,

answers: NDQ_003385

answers: Atlantic history,

answers: NDQ_003386

answers: Atlantic history,

answers: NDQ_003387

answers: Alison Games (2006)

answers: NDQ_003388

answers: Alison Games (2006)

answers: NDQ_003389

answers: a limited chronology.

answers: NDQ_003390

answers: Alison Games (2006)

answers: NDQ_003391

answers: Atlantic history, which takes as its geographic unit of analysis the Atlantic Ocean

answers: NDQ_003392

answers: Alison Games

answers: NDQ_003393

answers: Atlantic history, which takes as its geographic unit of analysis the Atlantic Ocean

answers: NDQ_003394

answers: Braudelian Atlantic history,

answers: NDQ_003395

answers: Atlantic history,

answers: NDQ_003396

answers: Braudelian Atlantic history,

text: Separate ocean bottom seismography and multi-channel seismic studies provide insight into the structure of the northern end of the Ryukyu trench region. Features of note include a thick (7–12 km) low velocity (4–5 km/s) zone on the landward side of the trench, the existence of subducting paleo-arc crust near the top of the trench in contrast to simple oceanic crust located at the middle of the trench, and a zone in which the Philippine Plate subducts beneath low P-wave velocity material (Vp = 5 km/s) that coincides with the location of the Mw 7.5 1968 Hyuganada earthquake.  It has been hypothesized that the above structural heterogeneity, in particular the subducting paleo-arc crust and its associated bathymetric highs, is one reason why earthquakes in this region are not larger i.e. exceeding Mw 8.0.  The exact mechanism by which the subduction of paleo-arc crust prevents sufficient stress build up for a larger earthquake is unknown.

text: Separate

text: ocean bottom seismography

text: and

text: multi-channel seismic

text: studies provide insight into the structure of the northern end of the Ryukyu trench region. Features of note include a thick (7–12 km) low velocity (4–5 km/s) zone on the landward side of the trench, the existence of subducting paleo-arc crust near the top of the trench in contrast to simple oceanic crust located at the middle of the trench, and a zone in which the Philippine Plate subducts beneath low P-wave velocity material (Vp = 5 km/s) that coincides with the location of the Mw 7.5 1968 Hyuganada earthquake.  It has been hypothesized that the above structural heterogeneity, in particular the subducting paleo-arc crust and its associated bathymetric highs, is one reason why earthquakes in this region are not larger i.e. exceeding Mw 8.0.  The exact mechanism by which the subduction of paleo-arc crust prevents sufficient stress build up for a larger earthquake is unknown.

answers: NDQ_003351

answers: P-wave velocity

answers: NDQ_003352

answers: subducts

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: trench

answers: NDQ_003356

answers: subduct

answers: NDQ_003357

answers: Subduction of paleo-arc crust prevents sufficient stress build up for a larger earthquake

answers: NDQ_003358

answers: low velocity

answers: NDQ_003359

answers: subducts

answers: NDQ_003360

answers: continental plates

answers: NDQ_003362

answers: the existence of subducting paleo-arc crust near the top of the trench

answers: NDQ_003363

answers: Ryukyu trench

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: What is one reason why earthquakes in this region are not larger?

answers: NDQ_003376

answers: What is one reason why earthquakes in this region are not larger?

answers: NDQ_003378

answers: low velocity (4–5 km/s) zone

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What is a stress?

answers: NDQ_003381

answers: What does the subduction of paleo-arc crust prevent?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is the area where faults are clustered called?

answers: NDQ_003386

answers: subducting paleo-arc crust

answers: NDQ_003387

answers: What is one reason why earthquakes in this region are not larger?

answers: NDQ_003388

answers: What type of faults are strike-slip faults?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: Ryukyu trench

answers: NDQ_003391

answers: Philippine Plate

answers: NDQ_003392

answers: Ryukyu trench

answers: NDQ_003393

answers: Philippine Plate

answers: NDQ_003394

answers: Paleo-arc crust

answers: NDQ_003395

answers: Ryukyu trench region

answers: NDQ_003396

answers: Ryukyu trench

answers: NDQ_003351

answers: subducting paleo-arc crust

answers: NDQ_003352

answers: larger earthquake

answers: NDQ_003353

answers: bathymetric highs,

answers: NDQ_003354

answers: subducting paleo-arc crust

answers: NDQ_003355

answers: Ryukyu trench

answers: NDQ_003356

answers: stress build up for a larger earthquake

answers: NDQ_003357

answers: simple oceanic crust

answers: NDQ_003358

answers: low velocity

answers: NDQ_003359

answers: stress build up

answers: NDQ_003360

answers: subducting paleo-arc crust

answers: NDQ_003362

answers: exceeding Mw 8.0.

answers: NDQ_003363

answers: Ryukyu trench

answers: NDQ_003371

answers: subducting paleo-arc crust

answers: NDQ_003373

answers: subducting paleo-arc crust

answers: NDQ_003376

answers: subducting paleo-arc crust

answers: NDQ_003378

answers: velocity

answers: NDQ_003379

answers: simple oceanic crust

answers: NDQ_003380

answers: stress build up for a larger earthquake

answers: NDQ_003381

answers: the subduction of paleo-arc crust prevents sufficient stress build up

answers: NDQ_003382

answers: subducting paleo-arc crust

answers: NDQ_003383

answers: stress build up

answers: NDQ_003384

answers: subducting paleo-arc

answers: NDQ_003385

answers: structural heterogeneity,

answers: NDQ_003386

answers: stress build up for a larger earthquake is unknown.

answers: NDQ_003387

answers: subducting paleo-arc crust

answers: NDQ_003388

answers: subducting paleo-arc crust

answers: NDQ_003389

answers: subducting paleo-arc crust

answers: NDQ_003390

answers: Philippine Plate subducts beneath low P-wave velocity material

answers: NDQ_003391

answers: paleo-arc crust

answers: NDQ_003392

answers: Philippine Plate subducts beneath low P-wave velocity material

answers: NDQ_003393

answers: paleo-arc crust

answers: NDQ_003394

answers: Ryukyu trench

answers: NDQ_003395

answers: Ryukyu trench

answers: NDQ_003396

answers: Ryukyu trench

text: ER stress can be activated by a variety of factors. In experimental conditions, excessive lipid (which can happen following obesity, a common condition preceding type 2 diabetes) and pro-inflammatory cytokines (which can occur following an inflammation, a common cause for type 1 diabetes) can activate ER stress in beta cells.

text: ER stress can be activated by a variety of factors. In experimental conditions, excessive

text: lipid

text: (which can happen following

text: obesity

text: , a common condition preceding

text: type 2 diabetes

text: ) and pro-inflammatory

text: cytokines

text: (which can occur following an

text: inflammation

text: , a common cause for

text: type 1 diabetes

text: ) can activate ER stress in beta cells.

answers: NDQ_003351

answers: ER stress

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: ER stress

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: unanswerable

answers: NDQ_003356

answers: swell

answers: NDQ_003357

answers: ER stress can be activated by a variety of factors

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: obesity is a common cause for type 1 diabetes

answers: NDQ_003363

answers: ER stress

answers: NDQ_003371

answers: Which of the following is not a cause of type 1 diabetes?

answers: NDQ_003373

answers: None of the above choices.

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: None of the above choices.

answers: NDQ_003381

answers: unanswerable

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: what is the first word in the passage?

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: Which of the following is not a cause for type 1 diabetes?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: type 2 diabetes

answers: NDQ_003391

answers: can be activated by ER stress

answers: NDQ_003392

answers: type 2 diabetes

answers: NDQ_003393

answers: a dip-slip fault plane

answers: NDQ_003394

answers: can occur following an inflammation

answers: NDQ_003395

answers: can be activated by a variety of factors

answers: NDQ_003396

answers: type 2 diabetes

answers: NDQ_003351

answers: ER stress

answers: NDQ_003352

answers: ER stress

answers: NDQ_003353

answers: ER stress in beta cells.

answers: NDQ_003354

answers: ER stress can be activated by a variety of factors.

answers: NDQ_003355

answers: ER stress

answers: NDQ_003356

answers: ER stress

answers: NDQ_003357

answers: beta cells.

answers: NDQ_003358

answers: ER stress

answers: NDQ_003359

answers: ER stress can be activated

answers: NDQ_003360

answers: ER stress

answers: NDQ_003362

answers: ER stress can be activated by a variety of factors.

answers: NDQ_003363

answers: inflammation,

answers: NDQ_003371

answers: ER stress

answers: NDQ_003373

answers: ER stress

answers: NDQ_003376

answers: ER stress

answers: NDQ_003378

answers: ER stress

answers: NDQ_003379

answers: ER stress can be activated by a variety of factors.

answers: NDQ_003380

answers: ER stress

answers: NDQ_003381

answers: ER stress

answers: NDQ_003382

answers: ER stress

answers: NDQ_003383

answers: ER stress

answers: NDQ_003384

answers: ER stress

answers: NDQ_003385

answers: ER stress can be activated by a variety of factors.

answers: NDQ_003386

answers: ER stress

answers: NDQ_003387

answers: ER stress

answers: NDQ_003388

answers: ER stress

answers: NDQ_003389

answers: ER stress

answers: NDQ_003390

answers: ER stress

answers: NDQ_003391

answers: ER stress

answers: NDQ_003392

answers: ER stress

answers: NDQ_003393

answers: ER stress

answers: NDQ_003394

answers: beta cells.

answers: NDQ_003395

answers: ER stress can be activated

answers: NDQ_003396

answers: ER stress

text: In 1980, a team of researchers consisting of Nobel prize-winning physicist Luis Alvarez, his son, geologist Walter Alvarez, and chemists Frank Asaro and Helen Michel discovered that sedimentary layers found all over the world at the K–T boundary contain a concentration of iridium many times greater than normal (30 times the average crustal content in Italy and 160 times at Stevns on the Danish island of Zealand). Iridium is extremely rare in the earth's crust because it is a siderophile element, and therefore most of it sank with iron into the earth's core during planetary differentiation. As iridium remains abundant in most asteroids and comets, the Alvarez team suggested that an asteroid struck the earth at the time of the K–T boundary. There were other earlier speculations on the possibility of an impact event, but no evidence had been uncovered at that time.

text: In 1980, a team of researchers consisting of

text: Nobel prize

text: -winning physicist

text: Luis Alvarez

text: , his son, geologist

text: Walter Alvarez

text: , and chemists

text: Frank Asaro

text: and

text: Helen Michel

text: discovered that

text: sedimentary

text: layers found all over the world at the K–T boundary contain a

text: concentration

text: of

text: iridium

text: many times greater than normal (30 times the average crustal content in Italy and 160 times at

text: Stevns

text: on the Danish island of Zealand). Iridium is extremely rare in the

text: earth's crust

text: because it is a

text: siderophile

text: element, and therefore most of it sank with

text: iron

text: into the

text: earth's core

text: during

text: planetary differentiation

text: . As iridium remains abundant in most asteroids and comets, the Alvarez team suggested that an

text: asteroid

text: struck the earth at the time of the K–T boundary. There were other earlier speculations on the possibility of an

text: impact event

text: , but no evidence had been uncovered at that time.

answers: NDQ_003351

answers: siderophile

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: igneous rocks to form

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: K–T boundary

answers: NDQ_003356

answers: sank with iron

answers: NDQ_003357

answers: sedimentary layers found all over the world at the K–T boundary contain a concentration of iridium many times greater than normal

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: no evidence had been uncovered at that time.

answers: NDQ_003363

answers: K–T boundary

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: unanswerable

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: no

answers: NDQ_003380

answers: What is a stress?

answers: NDQ_003381

answers: What is a siderophile element?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: fault zone

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip faults, strike-slip faults or shear stress?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: K–T boundary

answers: NDQ_003391

answers: sedimentary layers

answers: NDQ_003392

answers: K–T boundary

answers: NDQ_003393

answers: sedimentary layers

answers: NDQ_003394

answers: undefined

answers: NDQ_003395

answers: K–T boundary

answers: NDQ_003396

answers: K–T boundary

answers: NDQ_003351

answers: iridium

answers: NDQ_003352

answers: iridium

answers: NDQ_003353

answers: iridium

answers: NDQ_003354

answers: K–T boundary

answers: NDQ_003355

answers: layers

answers: NDQ_003356

answers: iridium

answers: NDQ_003357

answers: iridium

answers: NDQ_003358

answers: sedimentary layers

answers: NDQ_003359

answers: asteroid struck the earth at the time of the K–T boundary.

answers: NDQ_003360

answers: asteroid

answers: NDQ_003362

answers: no evidence had been uncovered at that time.

answers: NDQ_003363

answers: K–T boundary

answers: NDQ_003371

answers: K–T boundary

answers: NDQ_003373

answers: sedimentary layers

answers: NDQ_003376

answers: sedimentary layers

answers: NDQ_003378

answers: K–T boundary

answers: NDQ_003379

answers: K–T boundary

answers: NDQ_003380

answers: K–T boundary

answers: NDQ_003381

answers: planetary differentiation.

answers: NDQ_003382

answers: K–T boundary

answers: NDQ_003383

answers: iridium

answers: NDQ_003384

answers: K–T boundary

answers: NDQ_003385

answers: K–T boundary

answers: NDQ_003386

answers: K–T boundary

answers: NDQ_003387

answers: iridium

answers: NDQ_003388

answers: iridium

answers: NDQ_003389

answers: planetary differentiation.

answers: NDQ_003390

answers: K–T boundary

answers: NDQ_003391

answers: K–T boundary

answers: NDQ_003392

answers: K–T boundary

answers: NDQ_003393

answers: K–T boundary

answers: NDQ_003394

answers: K–T boundary

answers: NDQ_003395

answers: K–T boundary

answers: NDQ_003396

answers: K–T boundary

text: Geodynamics is generally concerned with processes that move materials throughout the Earth. In the Earth’s interior, movement happens when rocks melt or deform and flow in response to a stress field.  This deformation may be brittle, elastic, or plastic, depending on the magnitude of the stress and the material’s physical properties, especially the stress relaxation time scale. Rocks are structurally and compositionally heterogeneous and are subjected to variable stresses, so it is common to see different types of deformation in close spatial and temporal proximity. When working with geological timescales and lengths, it is convenient to use the continuous medium approximation and equilibrium stress fields to consider the average response to average stress.

text: Geodynamics is generally concerned with processes that move materials throughout the Earth. In the

text: Earth’s interior

text: , movement happens when rocks

text: melt

text: or

text: deform

text: and flow in response to a

text: stress field

text: .  This deformation may be

text: brittle

text: elastic

text: , or

text: plastic

text: , depending on the magnitude of the stress and the material’s physical properties, especially the stress relaxation time scale. Rocks are structurally and compositionally heterogeneous and are subjected to variable stresses, so it is common to see different types of deformation in close spatial and temporal proximity. When working with geological timescales and lengths, it is convenient to use the continuous medium approximation and equilibrium stress fields to consider the average response to average stress.

answers: NDQ_003351

answers: elastic

answers: NDQ_003352

answers: brittle

answers: NDQ_003353

answers: deformation

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: deformation

answers: NDQ_003356

answers: flow in response to

answers: NDQ_003357

answers: rocks are structurally and compositionally heterogeneous

answers: NDQ_003358

answers: stress relaxation

answers: NDQ_003359

answers: melts

answers: NDQ_003360

answers: stress fields

answers: NDQ_003362

answers: rocks are structurally and compositionally heterogeneous

answers: NDQ_003363

answers: geological timescales

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: It is convenient to use the continuous medium approximation

answers: NDQ_003376

answers: basin-and-range is caused by compressive forces

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What is a stress field?

answers: NDQ_003381

answers: In the Earth’s interior

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What type of fold is a syncline?

answers: NDQ_003385

answers: What is the term for an area where faults are clustered?

answers: NDQ_003386

answers: None of the above choices.

answers: NDQ_003387

answers: Which of the following is not a type of deformation?

answers: NDQ_003388

answers: Which of the following is not a type of deformation?

answers: NDQ_003389

answers: deform

answers: NDQ_003390

answers: a stress field

answers: NDQ_003391

answers: can be brittle

answers: NDQ_003392

answers: a stress field

answers: NDQ_003393

answers: can be brittle

answers: NDQ_003394

answers: non-vertical

answers: NDQ_003395

answers: a vertical fault plane

answers: NDQ_003396

answers: brittle

answers: NDQ_003351

answers: brittle, elastic, or plastic,

answers: NDQ_003352

answers: brittle, elastic, or plastic,

answers: NDQ_003353

answers: deform and flow

answers: NDQ_003354

answers: Geodynamics

answers: NDQ_003355

answers: Geodynamics

answers: NDQ_003356

answers: magnitude of the stress and the material’s physical properties,

answers: NDQ_003357

answers: rocks melt or deform and flow in response to a stress field.

answers: NDQ_003358

answers: brittle,

answers: NDQ_003359

answers: rocks melt or deform and flow in response to a stress field.

answers: NDQ_003360

answers: stress field.

answers: NDQ_003362

answers: rocks melt or deform and flow in response to a stress field.

answers: NDQ_003363

answers: rocks melt or deform and flow in response to a stress field.

answers: NDQ_003371

answers: Rocks are structurally and compositionally heterogeneous

answers: NDQ_003373

answers: variable stresses,

answers: NDQ_003376

answers: rocks melt or deform and flow in response to a stress field.

answers: NDQ_003378

answers: rocks melt or deform and flow in response to a stress field.

answers: NDQ_003379

answers: Geodynamics

answers: NDQ_003380

answers: stress field.

answers: NDQ_003381

answers: brittle, elastic, or plastic,

answers: NDQ_003382

answers: brittle, elastic, or plastic,

answers: NDQ_003383

answers: structurally and compositionally heterogeneous

answers: NDQ_003384

answers: Geodynamics

answers: NDQ_003385

answers: stress field.

answers: NDQ_003386

answers: rocks melt or deform and flow in response to a stress field.

answers: NDQ_003387

answers: rocks melt or deform and flow in response to a stress field.

answers: NDQ_003388

answers: rocks melt or deform and flow in response to a stress field.

answers: NDQ_003389

answers: rocks melt or deform and flow in response to a stress field.

answers: NDQ_003390

answers: Geodynamics

answers: NDQ_003391

answers: rocks melt or deform and flow in response to a stress field.

answers: NDQ_003392

answers: Geodynamics

answers: NDQ_003393

answers: rocks melt or deform and flow in response to a stress field.

answers: NDQ_003394

answers: Geodynamics

answers: NDQ_003395

answers: stress field.

answers: NDQ_003396

answers: Geodynamics

text: New Zealand lies along the boundary between the Australian and Pacific Plates. In South Island most of the relative displacement between these plates is taken up along a single dextral (right lateral) strike-slip fault with a major reverse component, the Alpine Fault. In North Island the displacement is mainly taken up along the Kermadec subduction zone, although the remaining dextral strike-slip component of the relative plate motion is accommodated by the North Island Fault System (NIFS). A group of dextral strike-slip structures, known as the Marlborough Fault System, transfer displacement between the mainly transform and convergent type plate boundaries in a complex zone at the northern end of South Island.<ref name="Van Dissen & Yeats">{{cite journal | url=http://geology.geoscienceworld.org/content/19/4/393.abstract | title=Hope fault, Jordan thrust, and uplift of the Seaward Kaikoura Range, New Zealand |author1=Van Dissen R. |author2=Yeats R.S. | journal=Geology | year=1991 | volume=19 | issue=4 | pages=393–396 | doi=10.1130/0091-7613(1991)019

text: New Zealand lies along the boundary between the

text: Australian

text: and

text: Pacific Plate

text: s. In

text: South Island

text: most of the relative displacement between these plates is taken up along a single dextral (right lateral)

text: strike-slip fault

text: with a major

text: reverse

text: component, the

text: Alpine Fault

text: . In

text: North Island

text: the displacement is mainly taken up along the

text: Kermadec subduction zone

text: , although the remaining dextral strike-slip component of the relative plate motion is accommodated by the

text: North Island Fault System

text: (NIFS). A group of dextral strike-slip structures, known as the

text: Marlborough Fault System

text: , transfer displacement between the mainly

text: transform

text: and

text: convergent type plate boundaries

text: in a complex zone at the northern end of South Island.<ref name="Van Dissen & Yeats">{{cite journal | url=http://geology.geoscienceworld.org/content/19/4/393.abstract | title=Hope fault, Jordan thrust, and uplift of the Seaward Kaikoura Range, New Zealand |author1=Van Dissen R. |author2=Yeats R.S. | journal=Geology | year=1991 | volume=19 | issue=4 | pages=393–396 | doi=10.1130/0091-7613(1991)019

answers: NDQ_003351

answers: dextral

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: Faults

answers: NDQ_003354

answers: Toroweap Formation is a formation

answers: NDQ_003355

answers: strike-slip

answers: NDQ_003356

answers: converge

answers: NDQ_003357

answers: dextral (right lateral) strike-slip

answers: NDQ_003358

answers: Fault

answers: NDQ_003359

answers: deforms

answers: NDQ_003360

answers: plate boundaries

answers: NDQ_003362

answers: The displacement is mainly taken up along the Kermadec subduction zone

answers: NDQ_003363

answers: Pacific plate boundaries

answers: NDQ_003371

answers: What is a thrust fault?

answers: NDQ_003373

answers: What is the term for this type of stress?

answers: NDQ_003376

answers: What type of terrain is basin-and-range?

answers: NDQ_003378

answers: The amount of the ground moving in an earthquake is called slip.

answers: NDQ_003379

answers: Yes

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: Van Dissen & Yeats

answers: NDQ_003382

answers: It is not possible to tell

answers: NDQ_003383

answers: What does stress cause in rock?

answers: NDQ_003384

answers: What type of fold is a syncline?

answers: NDQ_003385

answers: What is the term for an area where faults are clustered?

answers: NDQ_003386

answers: The Alpine Fault

answers: NDQ_003387

answers: Van Dissen R.

answers: NDQ_003388

answers: no

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: Alpine Fault

answers: NDQ_003391

answers: subduction zone

answers: NDQ_003392

answers: Hope fault

answers: NDQ_003393

answers: subduction zone

answers: NDQ_003394

answers: dextral

answers: NDQ_003395

answers: Alpine Fault

answers: NDQ_003396

answers: Alpine Fault

answers: NDQ_003351

answers: strike-slip fault

answers: NDQ_003352

answers: uplift

answers: NDQ_003353

answers: uplift

answers: NDQ_003354

answers: Seaward Kaikoura Range,

answers: NDQ_003355

answers: thrust,

answers: NDQ_003356

answers: uplift

answers: NDQ_003357

answers: (right lateral) strike-slip fault with a major reverse component,

answers: NDQ_003358

answers: thrust,

answers: NDQ_003359

answers: strike-slip fault

answers: NDQ_003360

answers: title=Hope fault, Jordan thrust,

answers: NDQ_003362

answers: (right lateral) strike-slip fault with a major reverse component,

answers: NDQ_003363

answers: New Zealand lies along the boundary between the Australian and Pacific Plates.

answers: NDQ_003371

answers: title=Hope fault, Jordan thrust,

answers: NDQ_003373

answers: title=Hope fault, Jordan thrust, and uplift

answers: NDQ_003376

answers: Seaward Kaikoura Range,

answers: NDQ_003378

answers: strike-slip

answers: NDQ_003379

answers: (right lateral)

answers: NDQ_003380

answers: title=Hope fault, Jordan thrust, and uplift

answers: NDQ_003381

answers: title=Hope fault, Jordan thrust, and uplift

answers: NDQ_003382

answers: title=Hope fault, Jordan thrust, and uplift

answers: NDQ_003383

answers: title=Hope fault, Jordan thrust, and uplift

answers: NDQ_003384

answers: Seaward Kaikoura Range,

answers: NDQ_003385

answers: Fault System

answers: NDQ_003386

answers: title=Hope fault, Jordan thrust, and uplift

answers: NDQ_003387

answers: strike-slip

answers: NDQ_003388

answers: strike-slip fault

answers: NDQ_003389

answers: uplift

answers: NDQ_003390

answers: title=Hope fault,

answers: NDQ_003391

answers: subduction zone,

answers: NDQ_003392

answers: title=Hope fault,

answers: NDQ_003393

answers: thrust,

answers: NDQ_003394

answers: dextral

answers: NDQ_003395

answers: Alpine Fault.

answers: NDQ_003396

answers: Alpine Fault.

text: Not all folds are equal on both sides of the axis of the fold. Those with  limbs of relatively equal length are termed symmetrical, and those with highly unequal limbs are asymmetrical. Asymmetrical folds generally have an axis at an angle to the original unfolded surface they formed on.

text: Not all folds are equal on both sides of the axis of the fold. Those with  limbs of relatively equal length are termed

text: symmetrical

text: , and those with highly unequal limbs are

text: asymmetrical

text: . Asymmetrical folds generally have an axis at an angle to the original unfolded surface they formed on.

answers: NDQ_003351

answers: asymmetrical

answers: NDQ_003352

answers: asymmetrical

answers: NDQ_003353

answers: asymmetrical folds

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: asymmetrical fold

answers: NDQ_003356

answers: asymmetrical

answers: NDQ_003357

answers: axis at an angle to the original unfolded surface they formed on

answers: NDQ_003358

answers: asymmetrical

answers: NDQ_003359

answers: unbalances

answers: NDQ_003360

answers: asymmetrical folds

answers: NDQ_003362

answers: axis at an angle to the original unfolded surface they formed on.

answers: NDQ_003363

answers: asymmetrical

answers: NDQ_003371

answers: What is a thrust fault?

answers: NDQ_003373

answers: unanswerable

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: unanswerable

answers: NDQ_003381

answers: What is the opposite of asymmetrical?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: unanswerable

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: unanswerable

answers: NDQ_003389

answers: not enough information

answers: NDQ_003390

answers: asymmetrical

answers: NDQ_003391

answers: asymmetrical

answers: NDQ_003392

answers: asymmetrical

answers: NDQ_003393

answers: asymmetrical

answers: NDQ_003394

answers: Asymmetrical folds

answers: NDQ_003395

answers: asymmetrical

answers: NDQ_003396

answers: asymmetrical

answers: NDQ_003351

answers: symmetrical,

answers: NDQ_003352

answers: asymmetrical.

answers: NDQ_003353

answers: Asymmetrical folds

answers: NDQ_003354

answers: symmetrical,

answers: NDQ_003355

answers: Asymmetrical folds

answers: NDQ_003356

answers: Asymmetrical folds

answers: NDQ_003357

answers: symmetrical,

answers: NDQ_003358

answers: asymmetrical. Asymmetrical folds

answers: NDQ_003359

answers: Asymmetrical folds

answers: NDQ_003360

answers: Asymmetrical folds

answers: NDQ_003362

answers: symmetrical,

answers: NDQ_003363

answers: asymmetrical.

answers: NDQ_003371

answers: Asymmetrical folds

answers: NDQ_003373

answers: symmetrical,

answers: NDQ_003376

answers: Asymmetrical folds

answers: NDQ_003378

answers: Asymmetrical folds

answers: NDQ_003379

answers: Asymmetrical folds generally have an axis at an angle

answers: NDQ_003380

answers: symmetrical,

answers: NDQ_003381

answers: Asymmetrical folds

answers: NDQ_003382

answers: symmetrical,

answers: NDQ_003383

answers: Asymmetrical folds

answers: NDQ_003384

answers: symmetrical,

answers: NDQ_003385

answers: symmetrical,

answers: NDQ_003386

answers: symmetrical,

answers: NDQ_003387

answers: symmetrical,

answers: NDQ_003388

answers: Asymmetrical folds

answers: NDQ_003389

answers: symmetrical,

answers: NDQ_003390

answers: Asymmetrical folds

answers: NDQ_003391

answers: Asymmetrical folds

answers: NDQ_003392

answers: Asymmetrical folds

answers: NDQ_003393

answers: Asymmetrical folds

answers: NDQ_003394

answers: Asymmetrical folds

answers: NDQ_003395

answers: Asymmetrical folds generally have an axis at an angle

answers: NDQ_003396

answers: Asymmetrical folds

text: The tectonic activity responsible for the extension in the Basin and Range is a complex and controversial issue among the geoscience community. The most accepted hypothesis suggests that crustal shearing associated with the San Andreas Fault caused spontaneous extensional faulting similar to that seen in the Great Basin. However, plate movement alone does not account for the high elevation of the Basin and Range region.  The western United States is a region of high heat flow which lowers the density of the lithosphere and stimulates isostatic uplift as a consequence. Lithospheric regions characterized by elevated heat flow are weak and extensional deformation can occur over a broad region. Basin and Range extension is therefore thought to be unrelated to the kind of extension produced by mantle upwelling which may cause narrow rift zones, such as the Afar Triple Junction. Geologic processes that elevate heat flow are varied, however some researchers suggest that heat generated at a subduction zone is transferred to the overriding plate as subduction proceeds. Fluids along fault zones then transfer heat vertically through the crust. This model has led to increasing interest in geothermal systems in the Basin and Range, and requires consideration of the continued influence of the fully subducted Farallon plate in the extension responsible for the Basin and Range Province.

text: The tectonic activity responsible for the extension in the Basin and Range is a complex and controversial issue among the geoscience community. The most accepted hypothesis suggests that crustal

text: shearing

text: associated with the

text: San Andreas Fault

text: caused spontaneous extensional faulting similar to that seen in the Great Basin. However, plate movement alone does not account for the high elevation of the Basin and Range region.  The western United States is a region of high

text: heat flow

text: which lowers the density of the lithosphere and stimulates

text: isostatic

text: uplift

text: as a consequence. Lithospheric regions characterized by elevated

text: heat flow

text: are weak and extensional

text: deformation

text: can occur over a broad region. Basin and Range extension is therefore thought to be unrelated to the kind of extension produced by

text: mantle upwelling

text: which may cause narrow rift zones, such as the

text: Afar Triple Junction

text: . Geologic processes that elevate heat flow are varied, however some researchers suggest that heat generated at a subduction zone is transferred to the overriding plate as subduction proceeds. Fluids along fault zones then transfer heat vertically through the crust. This model has led to increasing interest in

text: geothermal systems

text: in the Basin and Range, and requires consideration of the continued influence of the fully subducted Farallon plate in the extension responsible for the Basin and Range Province.

answers: NDQ_003351

answers: isostatic

answers: NDQ_003352

answers: lowers its density

answers: NDQ_003353

answers: deformation

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: rift zone

answers: NDQ_003356

answers: increase in size

answers: NDQ_003357

answers: fluids along fault zones then transfer heat vertically through the crust

answers: NDQ_003358

answers: subduction zone

answers: NDQ_003359

answers: plate movement alone

answers: NDQ_003360

answers: high heat flow

answers: NDQ_003362

answers: spontaneous extensional faulting similar to that seen in the Great Basin

answers: NDQ_003363

answers: San Andreas Fault

answers: NDQ_003371

answers: Basin and Range extension

answers: NDQ_003373

answers: What is the most accepted hypothesis?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What kind of deformation can occur over a broad region?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the most accepted hypothesis?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: Fault zones

answers: NDQ_003386

answers: San Andreas Fault

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: normal faults or plate movement?

answers: NDQ_003388

answers: crustal shearing associated with the San Andreas Fault

answers: NDQ_003389

answers: plate movement alone

answers: NDQ_003390

answers: extensional faulting

answers: NDQ_003391

answers: subduction zone

answers: NDQ_003392

answers: extensional faulting

answers: NDQ_003393

answers: rift zone

answers: NDQ_003394

answers: San Andreas

answers: NDQ_003395

answers: San Andreas Fault

answers: NDQ_003396

answers: extensional faulting

answers: NDQ_003351

answers: extensional faulting

answers: NDQ_003352

answers: lowers the density

answers: NDQ_003353

answers: extensional deformation

answers: NDQ_003354

answers: crustal shearing associated with the San Andreas Fault

answers: NDQ_003355

answers: rift zones,

answers: NDQ_003356

answers: extensional deformation can occur over a broad region.

answers: NDQ_003357

answers: Fluids along fault zones then transfer heat vertically through the crust.

answers: NDQ_003358

answers: rift zones,

answers: NDQ_003359

answers: crustal shearing

answers: NDQ_003360

answers: San Andreas Fault

answers: NDQ_003362

answers: high elevation of the Basin and Range region.

answers: NDQ_003363

answers: San Andreas Fault

answers: NDQ_003371

answers: extensional faulting

answers: NDQ_003373

answers: crustal shearing

answers: NDQ_003376

answers: plate movement alone does not account for the high elevation

answers: NDQ_003378

answers: extensional faulting

answers: NDQ_003379

answers: heat

answers: NDQ_003380

answers: extensional deformation

answers: NDQ_003381

answers: extensional deformation

answers: NDQ_003382

answers: crustal shearing associated with the San Andreas Fault

answers: NDQ_003383

answers: crustal shearing

answers: NDQ_003384

answers: crustal shearing associated with the San Andreas Fault

answers: NDQ_003385

answers: fault zones

answers: NDQ_003386

answers: crustal shearing

answers: NDQ_003387

answers: extensional faulting

answers: NDQ_003388

answers: crustal shearing

answers: NDQ_003389

answers: plate movement

answers: NDQ_003390

answers: San Andreas Fault

answers: NDQ_003391

answers: Farallon plate

answers: NDQ_003392

answers: extensional faulting

answers: NDQ_003393

answers: rift zones,

answers: NDQ_003394

answers: San Andreas Fault

answers: NDQ_003395

answers: San Andreas Fault

answers: NDQ_003396

answers: San Andreas Fault

text: By 26 February 2010 the Global Positioning System (GPS) equipment used by the Iceland Meteorological Office at Þorvaldseyri farm in the Eyjafjöll area (around  southeast of the location of the recent eruption) had shown 3 centimetres of displacement of the local crust in a southward direction, of which a 1 centimetre displacement had taken place within four days. (See the GPS Time Series page of the Nordic Volcanological Center's website for detailed information on the degree of movement detected in the Earth's crust in the Eyjafjallajökull locality.)

text: By 26 February 2010 the

text: Global Positioning System

text: (GPS) equipment used by the Iceland Meteorological Office at Þorvaldseyri farm in the Eyjafjöll area (around  southeast of the location of the recent eruption) had shown 3 centimetres of displacement of the local

text: crust

text: in a southward direction, of which a 1 centimetre displacement had taken place within four days. (See the GPS Time Series page of the Nordic Volcanological Center's website for detailed information on the degree of movement detected in the Earth's crust in the Eyjafjallajökull locality.)

answers: NDQ_003351

answers: displacement

answers: NDQ_003352

answers: displacement

answers: NDQ_003353

answers: displacement

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: displacement

answers: NDQ_003357

answers: 3 centimetres of displacement of the local crust in a southward direction

answers: NDQ_003358

answers: jökull

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: a 1 centimetre displacement had taken place within four days

answers: NDQ_003363

answers: Earth's crust

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: What type of stresses does the Earth's crust have?

answers: NDQ_003376

answers: what is the name of the terrain known as basin-and-range

answers: NDQ_003378

answers: What is the amount the ground moves in an earthquake?

answers: NDQ_003379

answers: The dip of the fault plane is

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What type of stress does the GPS Time Series page of the Nordic Volcanological Center's website describe?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: None of the above choices.

answers: NDQ_003387

answers: What are normal faults caused by?

answers: NDQ_003388

answers: What does the GPS Time Series page of the Nordic Volcanological Center's website provide detailed information on?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: dip-slip fault plane

answers: NDQ_003392

answers: Eyjafjöll

answers: NDQ_003393

answers: a dip-slip fault plane

answers: NDQ_003394

answers: isothermal

answers: NDQ_003395

answers: a fault with a vertical fault plane

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: displacement of the local crust in a southward direction,

answers: NDQ_003352

answers: displacement

answers: NDQ_003353

answers: displacement

answers: NDQ_003354

answers: By 26 February 2010

answers: NDQ_003355

answers: southeast

answers: NDQ_003356

answers: displacement of the local crust in a southward direction,

answers: NDQ_003357

answers: southward direction,

answers: NDQ_003358

answers: eruption)

answers: NDQ_003359

answers: displacement of the local crust

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: By 26 February 2010

answers: NDQ_003363

answers: Eyjafjöll

answers: NDQ_003371

answers: 3 centimetres of displacement of the local crust

answers: NDQ_003373

answers: 3 centimetres of displacement of the local crust

answers: NDQ_003376

answers: 3 centimetres of displacement of the local crust

answers: NDQ_003378

answers: displacement

answers: NDQ_003379

answers: southward

answers: NDQ_003380

answers: displacement

answers: NDQ_003381

answers: displacement of the local crust in a southward direction,

answers: NDQ_003382

answers: 3 centimetres of displacement of the local crust

answers: NDQ_003383

answers: displacement

answers: NDQ_003384

answers: <unk>orvaldseyri

answers: NDQ_003385

answers: Eyjafjöll

answers: NDQ_003386

answers: displacement of the local crust

answers: NDQ_003387

answers: 3 centimetres of displacement of the local crust

answers: NDQ_003388

answers: 3 centimetres of displacement of the local crust

answers: NDQ_003389

answers: displacement of the local crust

answers: NDQ_003390

answers: Eyjafjöll

answers: NDQ_003391

answers: crust

answers: NDQ_003392

answers: Eyjafjöll

answers: NDQ_003393

answers: eruption) had shown 3 centimetres of displacement of the local crust

answers: NDQ_003394

answers: southeast of the location of the recent eruption)

answers: NDQ_003395

answers: 3 centimetres of displacement of the local crust

answers: NDQ_003396

answers: southeast

text: A fault plane is the plane that represents the fracture surface of a fault. A fault trace  or fault line is the intersection of a fault plane with the ground surface. A fault trace is also the line commonly plotted on geologic maps to represent a fault.

text: A fault plane is the

text: plane

text: that represents the fracture surface of a fault. A fault trace  or fault line is the intersection of a fault plane with the ground surface. A fault trace is also the line commonly plotted on

text: geologic map

text: s to represent a fault.

answers: NDQ_003351

answers: fault plane

answers: NDQ_003352

answers: fractures

answers: NDQ_003353

answers: fractures

answers: NDQ_003354

answers: Toroweap Formation is a formation

answers: NDQ_003355

answers: fault

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: A fault plane is the plane that represents the fracture surface of a fault.

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: is pushed against it

answers: NDQ_003360

answers: fault lines

answers: NDQ_003362

answers: A fault trace is the intersection of a fault plane with the ground

answers: NDQ_003363

answers: fault lines

answers: NDQ_003371

answers: Which of the following is not a type of fault?

answers: NDQ_003373

answers: How would you describe a fault plane?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: What is a fault trace?

answers: NDQ_003379

answers: How is a strike-slip fault different from a normal fault?

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: Which of the following is not a type of stress?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not the cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not a type of fold?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: Which of the following is not a cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not a cause of normal faults?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip faults or fault lines?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: a fault line

answers: NDQ_003391

answers: is a fault line

answers: NDQ_003392

answers: a fault line

answers: NDQ_003393

answers: is a fault line

answers: NDQ_003394

answers: isobath

answers: NDQ_003395

answers: is a fault

answers: NDQ_003396

answers: a fault line

answers: NDQ_003351

answers: fault plane

answers: NDQ_003352

answers: fracture surface

answers: NDQ_003353

answers: fracture surface

answers: NDQ_003354

answers: A fault plane

answers: NDQ_003355

answers: fault plane

answers: NDQ_003356

answers: fault plane

answers: NDQ_003357

answers: fault plane

answers: NDQ_003358

answers: fault plane

answers: NDQ_003359

answers: fault.

answers: NDQ_003360

answers: fault plane

answers: NDQ_003362

answers: A fault plane

answers: NDQ_003363

answers: fault.

answers: NDQ_003371

answers: fault plane

answers: NDQ_003373

answers: A fault plane

answers: NDQ_003376

answers: A fault plane

answers: NDQ_003378

answers: fault plane

answers: NDQ_003379

answers: fault trace or fault line

answers: NDQ_003380

answers: A fault plane

answers: NDQ_003381

answers: A fault plane

answers: NDQ_003382

answers: A fault plane

answers: NDQ_003383

answers: A fault plane

answers: NDQ_003384

answers: fault plane

answers: NDQ_003385

answers: fault plane

answers: NDQ_003386

answers: fault plane

answers: NDQ_003387

answers: A fault plane

answers: NDQ_003388

answers: A fault plane

answers: NDQ_003389

answers: fault.

answers: NDQ_003390

answers: fault plane

answers: NDQ_003391

answers: ground surface.

answers: NDQ_003392

answers: fault plane is the plane that represents the fracture surface of a fault.

answers: NDQ_003393

answers: ground surface.

answers: NDQ_003394

answers: fault.

answers: NDQ_003395

answers: A fault plane

answers: NDQ_003396

answers: fault trace or fault line

text: In a one-dimensional relaxation test, the material is subjected to a sudden strain that is kept constant over the duration ofthe test, and the stress is measured over time. The initial stress is due to the elastic response of the material. Then, thestress relaxes over time due to the viscous effects in the material. Typically, either a tensile, compressive, bulkcompression, or shear strain is applied. The resulting stress vs. time data can be fitted with a number of equations, calledmodels. Only the notation changes depending of the type of strain applied: tensile-compressive relaxation is denoted

text: In a one-dimensional relaxation test, the material is subjected to a sudden strain that is kept constant over the duration ofthe test, and the stress is measured over time. The initial stress is due to the elastic response of the material. Then, thestress relaxes over time due to the viscous effects in the material. Typically, either a tensile, compressive, bulkcompression, or shear strain is applied. The resulting stress vs. time data can be fitted with a number of equations, calledmodels. Only the notation changes depending of the type of strain applied: tensile-compressive relaxation is denoted

answers: NDQ_003351

answers: shear

answers: NDQ_003352

answers: compresses more

answers: NDQ_003353

answers: viscous effects

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: compress.

answers: NDQ_003357

answers: tensile-compressive relaxation is denoted

answers: NDQ_003358

answers: shear

answers: NDQ_003359

answers: is pushed together

answers: NDQ_003360

answers: continental plates.

answers: NDQ_003362

answers: tensile-compressive relaxation is denoted

answers: NDQ_003363

answers: tectonic plate boundaries

answers: NDQ_003371

answers: What is a thrust fault?

answers: NDQ_003373

answers: None of the above choices .

answers: NDQ_003376

answers: basin-and-range

answers: NDQ_003378

answers: The amount the ground moves in an earthquake is called slip.

answers: NDQ_003379

answers: The dip of the fault plane is

answers: NDQ_003380

answers: None of the above choices.

answers: NDQ_003381

answers: compressive

answers: NDQ_003382

answers: compressive

answers: NDQ_003383

answers: None of the above choices are true

answers: NDQ_003384

answers: What kind of fold is a syncline?

answers: NDQ_003385

answers: Fault zones are areas where faults are clustered.

answers: NDQ_003386

answers: movement of rock at faults

answers: NDQ_003387

answers: None of the above choices.

answers: NDQ_003388

answers: tensile-compressive relaxation

answers: NDQ_003389

answers: None of the above choices.

answers: NDQ_003390

answers: Shear fault

answers: NDQ_003391

answers: a crater

answers: NDQ_003392

answers: Shear fault

answers: NDQ_003393

answers: sandstone

answers: NDQ_003394

answers: fault with a fault plane

answers: NDQ_003395

answers: a vertical fault plane

answers: NDQ_003396

answers: horizontal fault

answers: NDQ_003351

answers: tensile,

answers: NDQ_003352

answers: elastic response of the material.

answers: NDQ_003353

answers: viscous effects in the material.

answers: NDQ_003354

answers: tensile-compressive relaxation

answers: NDQ_003355

answers: shear

answers: NDQ_003356

answers: elastic response

answers: NDQ_003357

answers: tensile-compressive relaxation

answers: NDQ_003358

answers: shear

answers: NDQ_003359

answers: tensile-compressive relaxation

answers: NDQ_003360

answers: tensile-compressive relaxation

answers: NDQ_003362

answers: constant

answers: NDQ_003363

answers: tensile-compressive relaxation

answers: NDQ_003371

answers: tensile-compressive relaxation

answers: NDQ_003373

answers: tensile-compressive relaxation

answers: NDQ_003376

answers: tensile-compressive relaxation

answers: NDQ_003378

answers: tensile-compressive relaxation

answers: NDQ_003379

answers: tensile-compressive relaxation

answers: NDQ_003380

answers: tensile, compressive, bulkcompression, or shear strain

answers: NDQ_003381

answers: tensile-compressive relaxation

answers: NDQ_003382

answers: tensile-compressive relaxation

answers: NDQ_003383

answers: elastic response

answers: NDQ_003384

answers: tensile-compressive relaxation

answers: NDQ_003385

answers: tensile-compressive relaxation

answers: NDQ_003386

answers: tensile-compressive relaxation

answers: NDQ_003387

answers: tensile-compressive relaxation

answers: NDQ_003388

answers: shear strain

answers: NDQ_003389

answers: tensile-compressive relaxation

answers: NDQ_003390

answers: shear

answers: NDQ_003391

answers: tensile-compressive relaxation

answers: NDQ_003392

answers: shear

answers: NDQ_003393

answers: tensile-compressive relaxation

answers: NDQ_003394

answers: tensile-compressive relaxation

answers: NDQ_003395

answers: tensile-compressive relaxation

answers: NDQ_003396

answers: shear

text: Geologically the district forms part of the vast Indo-Gangetic alluvial tract, of which the origin is attributed to a sag in the earth's crust, formed, in the upper eocene times, between the northwardly drifting Gondwanaland and the rising Himalayan belt, and gradually filled in by sediments so as to constitute a level plane with a very gentle seaward slope. The alluvium formation of the district, comprising sand, silt & clay with occasional gravel, is of the early quaternary to sub-recent age. The older alluvium called bhangar, forms slightly elevated terraces usually above the flood levels. It is rather dark in colour generally rich in concretions and nodules of impure calcium carbonate, locally known as kankar. The newer alluvium, called khandar, forming the lowlands between the Ganga and Bhangar, is light coloured, poor in calcarious contain and composed of lenticular beds of sand, gravel and clays. The economic minerals found in the district are kankar, reh and sand.

text: Geologically

text: the district forms part of the vast Indo-Gangetic alluvial tract, of which the origin is attributed to a sag in the earth's crust, formed, in the upper eocene times, between the northwardly drifting Gondwanaland and the rising Himalayan belt, and gradually filled in by sediments so as to constitute a level plane with a very gentle seaward slope. The alluvium formation of the district, comprising sand, silt & clay with occasional gravel, is of the early quaternary to sub-recent age. The older alluvium called bhangar, forms slightly elevated terraces usually above the flood levels. It is rather dark in colour generally rich in concretions and nodules of impure calcium carbonate, locally known as kankar. The newer alluvium, called khandar, forming the lowlands between the Ganga and Bhangar, is light coloured, poor in calcarious contain and composed of lenticular beds of sand, gravel and clays. The economic minerals found in the district are kankar, reh and sand.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: is more likely to crack

answers: NDQ_003353

answers: swells

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: sag

answers: NDQ_003356

answers: elevated terraces

answers: NDQ_003357

answers: sand, silt & clay with occasional gravel

answers: NDQ_003358

answers: sag

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Himalayan belt

answers: NDQ_003362

answers: a sag in the earth's crust

answers: NDQ_003363

answers: in the upper eocene times

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: None of the above choices are true

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: no

answers: NDQ_003380

answers: What type of force applied to rock is a stress?

answers: NDQ_003381

answers: What is the sag in the earth's crust?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: None of the above choices.

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: normal faults or sag in the earth's crust?

answers: NDQ_003388

answers: Which of the following is not a type of fault: Strike-slip faults or strike-slip faults?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: sag

answers: NDQ_003391

answers: Gondwanaland

answers: NDQ_003392

answers: sag in the earth's crust

answers: NDQ_003393

answers: bhangar

answers: NDQ_003394

answers: lenticular

answers: NDQ_003395

answers: sag

answers: NDQ_003396

answers: sag

answers: NDQ_003351

answers: sag in the earth's crust,

answers: NDQ_003352

answers: elevated terraces

answers: NDQ_003353

answers: slightly elevated terraces

answers: NDQ_003354

answers: bhangar, forms slightly elevated terraces usually above the flood levels.

answers: NDQ_003355

answers: sag

answers: NDQ_003356

answers: slightly elevated terraces

answers: NDQ_003357

answers: gentle seaward slope.

answers: NDQ_003358

answers: bhangar,

answers: NDQ_003359

answers: sag in the earth's crust,

answers: NDQ_003360

answers: a sag in the earth's crust,

answers: NDQ_003362

answers: a level plane with a very gentle seaward slope.

answers: NDQ_003363

answers: Himalayan belt,

answers: NDQ_003371

answers: bhangar,

answers: NDQ_003373

answers: sag in the earth's crust,

answers: NDQ_003376

answers: a sag in the earth's crust,

answers: NDQ_003378

answers: sag in the earth's crust,

answers: NDQ_003379

answers: level plane with a very gentle seaward slope.

answers: NDQ_003380

answers: sag in the earth's crust,

answers: NDQ_003381

answers: bhangar, forms slightly elevated terraces

answers: NDQ_003382

answers: Himalayan belt,

answers: NDQ_003383

answers: a sag in the earth's crust,

answers: NDQ_003384

answers: bhangar, forms slightly elevated terraces usually above the flood levels.

answers: NDQ_003385

answers: Indo-Gangetic alluvial tract,

answers: NDQ_003386

answers: a sag in the earth's crust,

answers: NDQ_003387

answers: sag in the earth's crust,

answers: NDQ_003388

answers: a sag in the earth's crust,

answers: NDQ_003389

answers: a sag in the earth's crust,

answers: NDQ_003390

answers: sag in the earth's crust,

answers: NDQ_003391

answers: level plane with a very gentle seaward slope.

answers: NDQ_003392

answers: sag in the earth's crust,

answers: NDQ_003393

answers: bhangar,

answers: NDQ_003394

answers: level plane with a very gentle seaward slope.

answers: NDQ_003395

answers: level plane with a very gentle seaward slope.

answers: NDQ_003396

answers: level plane with a very gentle seaward slope.

text: The mountain is mostly made up of limestone formations, having risen up gradually from the Earth's crust.

text: The mountain is mostly made up of

text: limestone

text: formations, having risen up gradually from the Earth's

text: crust

answers: NDQ_003351

answers: lateral

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: igneous rocks to form.

answers: NDQ_003354

answers: the Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: glacier

answers: NDQ_003356

answers: rise up

answers: NDQ_003357

answers: limestone formations would be exposed to heat and pressure.

answers: NDQ_003358

answers: limestone formation

answers: NDQ_003359

answers: is pushed together

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: The San Andreas fault is a volcano.

answers: NDQ_003363

answers: Earth's crust

answers: NDQ_003371

answers: Which of the following is not a type of formation?

answers: NDQ_003373

answers: How would you describe the rock?

answers: NDQ_003376

answers: (iv).

answers: NDQ_003378

answers: The amount of the ground moving is called

answers: NDQ_003379

answers: The dip of the fault plane is horizontal.

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What will happen to the mountain?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: How would you describe the formations?

answers: NDQ_003384

answers: What type of formation is the mountain made up of?

answers: NDQ_003385

answers: The mountain is mostly made up of limestone formations

answers: NDQ_003386

answers: It's impossible to say

answers: NDQ_003387

answers: Which of the following is not a cause of normal faults?

answers: NDQ_003388

answers: Which of the following is not a cause of strike-slip faults?

answers: NDQ_003389

answers: It's impossible to say

answers: NDQ_003390

answers: is a fault

answers: NDQ_003391

answers: is a mountain

answers: NDQ_003392

answers: is a type of fault

answers: NDQ_003393

answers: limestone formations

answers: NDQ_003394

answers: is a fault

answers: NDQ_003395

answers: is a type of

answers: NDQ_003396

answers: NDQ_003351

answers: limestone formations, having risen up gradually from the Earth's crust.

answers: NDQ_003352

answers: risen up gradually from the Earth's crust.

answers: NDQ_003353

answers: risen up gradually from the Earth's crust.

answers: NDQ_003354

answers: risen up gradually from the Earth's crust.

answers: NDQ_003355

answers: The mountain

answers: NDQ_003356

answers: limestone formations, having risen up gradually from the Earth's crust.

answers: NDQ_003357

answers: risen up gradually from the Earth's crust.

answers: NDQ_003358

answers: The mountain

answers: NDQ_003359

answers: risen up gradually from the Earth's crust.

answers: NDQ_003360

answers: Earth's crust.

answers: NDQ_003362

answers: risen up gradually from the Earth's crust.

answers: NDQ_003363

answers: risen up gradually from the Earth's crust.

answers: NDQ_003371

answers: limestone formations, having risen up gradually from the Earth's crust.

answers: NDQ_003373

answers: risen up gradually from the Earth's crust.

answers: NDQ_003376

answers: risen up gradually from the Earth's crust.

answers: NDQ_003378

answers: risen up gradually from the Earth's crust.

answers: NDQ_003379

answers: limestone formations, having risen up gradually from the Earth's crust.

answers: NDQ_003380

answers: limestone formations, having risen up gradually from the Earth's crust.

answers: NDQ_003381

answers: limestone formations, having risen up gradually from the Earth's crust.

answers: NDQ_003382

answers: limestone formations, having risen up gradually from the Earth's crust.

answers: NDQ_003383

answers: limestone formations, having risen up gradually from the Earth's crust.

answers: NDQ_003384

answers: risen up gradually from the Earth's crust.

answers: NDQ_003385

answers: limestone formations, having risen up gradually from the Earth's crust.

answers: NDQ_003386

answers: risen up gradually from the Earth's crust.

answers: NDQ_003387

answers: limestone formations, having risen up gradually from the Earth's crust.

answers: NDQ_003388

answers: limestone formations, having risen up gradually from the Earth's crust.

answers: NDQ_003389

answers: risen up gradually from the Earth's crust.

answers: NDQ_003390

answers: limestone formations, having risen up gradually from the Earth's crust.

answers: NDQ_003391

answers: limestone

answers: NDQ_003392

answers: risen up gradually from the Earth's crust.

answers: NDQ_003393

answers: limestone

answers: NDQ_003394

answers: risen up gradually from the Earth's crust.

answers: NDQ_003395

answers: risen up gradually from the Earth's crust.

answers: NDQ_003396

answers: risen up gradually from the Earth's crust.

text: Several strands of the San Andreas Fault System in the eastern region of the San Francisco Bay Area are the Hayward–Rodgers Creek and Calaveras Faults. The Hayward Fault exhibits fault creep, but it also has potential for large earthquakes, like the 1868 M7 Hayward earthquake that occurred on its southern segment. The northern Calaveras Fault meets the Hayward Fault near the Calaveras Reservoir and can also produce large earthquakes. Except for a ~M6.5 shock that occurred in 1911, the central and southern segments might only produce smaller events and fault creep.

text: Several strands of the

text: San Andreas Fault System

text: in the

text: eastern region of the San Francisco Bay Area

text: are the

text: Hayward

text: –Rodgers Creek and

text: Calaveras Fault

text: s. The Hayward Fault exhibits

text: fault creep

text: , but it also has potential for large earthquakes, like the

text: 1868 M7 Hayward earthquake

text: that occurred on its southern segment. The northern Calaveras Fault meets the Hayward Fault near the

text: Calaveras Reservoir

text: and can also produce large earthquakes. Except for a ~M6.5 shock that occurred in 1911, the central and southern segments might only produce smaller events and fault creep.

answers: NDQ_003351

answers: fault creep

answers: NDQ_003352

answers: can crack

answers: NDQ_003353

answers: fault creep

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: Fault

answers: NDQ_003356

answers: Creep

answers: NDQ_003357

answers: the central and southern segments might only produce smaller events and fault creep

answers: NDQ_003358

answers: Reservoir

answers: NDQ_003359

answers: cracks

answers: NDQ_003360

answers: San Andreas Fault System

answers: NDQ_003362

answers: the central and southern segments might only produce smaller events and fault creep.

answers: NDQ_003363

answers: San Andreas Fault

answers: NDQ_003371

answers: Which of the following is not a strand of the San Andreas Fault System in the eastern region of the San Francisco Bay Area?

answers: NDQ_003373

answers: What type of stresses does a deeply buried rock experience?

answers: NDQ_003376

answers: What is the San Andreas Fault System?

answers: NDQ_003378

answers: what is the last word in the passage?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: How would you describe the Hayward Fault?

answers: NDQ_003381

answers: What type of stress does the Hayward Fault exhibit?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the San Andreas Fault System?

answers: NDQ_003384

answers: What is the San Andreas Fault System?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: fault creep

answers: NDQ_003387

answers: What type of stress does the Hayward Fault exhibit?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip, Hayward, or Calaveras?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: Hayward Fault

answers: NDQ_003391

answers: Hayward Fault

answers: NDQ_003392

answers: Hayward Fault

answers: NDQ_003393

answers: Calaveras Reservoir

answers: NDQ_003394

answers: Calaveras Fault

answers: NDQ_003395

answers: Hayward Fault

answers: NDQ_003396

answers: Hayward Fault

answers: NDQ_003351

answers: fault creep,

answers: NDQ_003352

answers: fault creep,

answers: NDQ_003353

answers: fault creep,

answers: NDQ_003354

answers: Several strands of the San Andreas Fault System

answers: NDQ_003355

answers: fault creep,

answers: NDQ_003356

answers: fault creep, but it also has potential for large earthquakes,

answers: NDQ_003357

answers: fault creep,

answers: NDQ_003358

answers: fault creep,

answers: NDQ_003359

answers: fault creep,

answers: NDQ_003360

answers: San Andreas Fault System

answers: NDQ_003362

answers: large earthquakes,

answers: NDQ_003363

answers: San Andreas Fault System

answers: NDQ_003371

answers: The Hayward Fault exhibits fault creep,

answers: NDQ_003373

answers: fault creep, but it also has potential for large earthquakes,

answers: NDQ_003376

answers: The Hayward Fault exhibits fault creep,

answers: NDQ_003378

answers: fault creep,

answers: NDQ_003379

answers: fault creep,

answers: NDQ_003380

answers: fault creep, but it also has potential for large earthquakes,

answers: NDQ_003381

answers: fault creep,

answers: NDQ_003382

answers: fault creep,

answers: NDQ_003383

answers: fault creep,

answers: NDQ_003384

answers: Hayward–Rodgers Creek

answers: NDQ_003385

answers: fault creep,

answers: NDQ_003386

answers: fault creep,

answers: NDQ_003387

answers: fault creep,

answers: NDQ_003388

answers: fault creep,

answers: NDQ_003389

answers: fault creep,

answers: NDQ_003390

answers: Calaveras Faults. The Hayward Fault

answers: NDQ_003391

answers: fault creep,

answers: NDQ_003392

answers: fault creep,

answers: NDQ_003393

answers: fault creep,

answers: NDQ_003394

answers: Calaveras Faults.

answers: NDQ_003395

answers: The Hayward Fault

answers: NDQ_003396

answers: Hayward–Rodgers Creek

text: The Western Carpathians are from the neotectonic point of view part of the Alcapa block. Main earthquakes in the Alcapa were located in the subduction arc of the Hellenides and Calabrids. Deep focus earthquakes are known only from the zone of Vrancea, where the subduction is still active. No deep focused earthquakes related to subduction were recorded in the Western Carpathians. A period of significant continental collision and shortening of the crust affected the area in the Miocene. Later, primarily extensional and strike-slip movement in the Neogene generated new or reactivated older faults. There are five principal earthquake zones located in the area of the Western Carpathians: the Pezinok-Pernek zone, which is a continuation of the faults responsible for formation of the Vienna Basin, the Dobrá Voda zone with the most intensive and most shallow earthquakes around the Dobrá Voda fault, the Komáro zone of earthquakes, which joins the Rába-Hurbanovo-Darnó fault (also known as Raaba linie), separating the Pelso unit from the Inner Carpathian crystalline basement, the Žilina zone of earthquakes, related to the ongoing collision and strike-slip movement in the Pieniny Klippen Belt, and the Central Slovakia zone, which is probably the result of tectonic activity of the Central Slovak fault.

text: The Western Carpathians are from the

text: neotectonic

text: point of view part of the

text: Alcapa

text: block. Main

text: earthquake

text: s in the

text: Alcapa

text: were located in the

text: subduction

text: arc of the

text: Hellenides

text: and

text: Calabrid

text: s.

text: Deep focus earthquake

text: s are known only from the zone of

text: Vrancea

text: , where the

text: subduction

text: is still active. No deep focused earthquakes related to subduction were recorded in the Western Carpathians. A period of significant

text: continental collision

text: and shortening of the crust affected the area in the

text: Miocene

text: . Later, primarily extensional and

text: strike-slip

text: movement in the Neogene generated new or reactivated older

text: fault

text: s. There are five principal earthquake zones located in the area of the Western Carpathians: the Pezinok-Pernek zone, which is a continuation of the faults responsible for formation of the

text: Vienna Basin

text: , the Dobrá Voda zone with the most intensive and most shallow earthquakes around the

text: Dobrá Voda fault

text: , the Komáro zone of earthquakes, which joins the

text: Rába

text: Hurbanovo

text: Darnó

text: fault (also known as

text: Raaba linie

text: ), separating the

text: Pelso unit

text: from the Inner Carpathian crystalline basement, the Žilina zone of earthquakes, related to the ongoing collision and strike-slip movement in the

text: Pieniny Klippen Belt

text: , and the Central Slovakia zone, which is probably the result of tectonic activity of the

text: Central Slovak fault

answers: NDQ_003351

answers: extensional

answers: NDQ_003352

answers: shortens

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: subduction arc

answers: NDQ_003356

answers: strike-slip

answers: NDQ_003357

answers: the most intense and most shallow earthquakes around the Dobrá Voda fault

answers: NDQ_003358

answers: shallow earthquakes

answers: NDQ_003359

answers: strike-slip movement

answers: NDQ_003360

answers: faults

answers: NDQ_003362

answers: deep focused earthquakes related to subduction were recorded in the Western Carpathians

answers: NDQ_003363

answers: Alcapa block

answers: NDQ_003371

answers: How many principal earthquake zones are located in the area of the Western Carpathians?

answers: NDQ_003373

answers: No deep focused earthquakes related to subduction were recorded

answers: NDQ_003376

answers: How many principal earthquake zones located in the area of the Western Carpathians?

answers: NDQ_003378

answers: strike-slip movement

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What type of stress does the Western Carpathians experience?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What type of fold is the Komáro zone of earthquakes?

answers: NDQ_003385

answers: principal earthquake zones

answers: NDQ_003386

answers: extensional and strike-slip

answers: NDQ_003387

answers: No deep focused earthquakes related to subduction were recorded in the Western Carpathians.

answers: NDQ_003388

answers: What type of movement in the Neogene generated new or reactivated older faults?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: Dobrá Voda

answers: NDQ_003391

answers: Alcapa block

answers: NDQ_003392

answers: Dobrá Voda

answers: NDQ_003393

answers: Alcapa block

answers: NDQ_003394

answers: Central Slovak fault

answers: NDQ_003395

answers: Central Slovak fault

answers: NDQ_003396

answers: Central Slovak fault

answers: NDQ_003351

answers: extensional and strike-slip movement

answers: NDQ_003352

answers: shortening

answers: NDQ_003353

answers: faults.

answers: NDQ_003354

answers: The Western Carpathians

answers: NDQ_003355

answers: subduction arc

answers: NDQ_003356

answers: strike-slip

answers: NDQ_003357

answers: No deep focused earthquakes

answers: NDQ_003358

answers: shallow earthquakes

answers: NDQ_003359

answers: strike-slip movement

answers: NDQ_003360

answers: earthquakes in the Alcapa were located in the subduction arc

answers: NDQ_003362

answers: No deep focused earthquakes

answers: NDQ_003363

answers: subduction arc

answers: NDQ_003371

answers: older faults.

answers: NDQ_003373

answers: Deep focus earthquakes

answers: NDQ_003376

answers: Vienna Basin,

answers: NDQ_003378

answers: strike-slip

answers: NDQ_003379

answers: strike-slip movement in the Neogene

answers: NDQ_003380

answers: earthquakes

answers: NDQ_003381

answers: Deep focus earthquakes

answers: NDQ_003382

answers: extensional and strike-slip

answers: NDQ_003383

answers: faults.

answers: NDQ_003384

answers: Raaba linie),

answers: NDQ_003385

answers: earthquake zones

answers: NDQ_003386

answers: extensional and strike-slip movement

answers: NDQ_003387

answers: extensional and strike-slip movement

answers: NDQ_003388

answers: strike-slip movement

answers: NDQ_003389

answers: extensional and strike-slip movement

answers: NDQ_003390

answers: Central Slovak fault.

answers: NDQ_003391

answers: crystalline basement,

answers: NDQ_003392

answers: Central Slovak fault.

answers: NDQ_003393

answers: crystalline basement,

answers: NDQ_003394

answers: Central Slovak fault.

answers: NDQ_003395

answers: Rába-Hurbanovo-Darnó

answers: NDQ_003396

answers: Central Slovak fault.

text: User-specified folding allows the user to fold sections of text using a generic selection method, but without changing the source code (out-of-band), instead being specified only in the editor. For example, a programmer may select some lines of text and specify that they  should be folded. Folded text might be anonymous or named, and this may be preserved across editing sessions or discarded. Unlike token-based folding, this does not change the source text – it thus is not shared with other editors of the file, and is not visible in the code.

text: User-specified folding allows the user to fold sections of text using a generic selection method, but without changing the source code (out-of-band), instead being specified only in the editor. For example, a programmer may select some lines of text and specify that they  should be folded. Folded text might be anonymous or named, and this may be preserved across editing sessions or discarded. Unlike token-based folding, this does not change the source text – it thus is not shared with other editors of the file, and is not visible in the code.

answers: NDQ_003351

answers: folded text

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: rocks to crack.

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: fold that bends downward

answers: NDQ_003356

answers: fold

answers: NDQ_003357

answers: user-specified folding allows the user to fold sections of text

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: continental plates.

answers: NDQ_003362

answers: does not change the source text

answers: NDQ_003363

answers: most of the worlds largest mountains

answers: NDQ_003371

answers: a thrust fault in between

answers: NDQ_003373

answers: compressive stresses

answers: NDQ_003376

answers: compressive forces

answers: NDQ_003378

answers: the ground moves

answers: NDQ_003379

answers: strike-slip fault

answers: NDQ_003380

answers: force applied to rock

answers: NDQ_003381

answers: constricting stress

answers: NDQ_003382

answers: Compression

answers: NDQ_003383

answers: Folded

answers: NDQ_003384

answers: syncline

answers: NDQ_003385

answers: fault zone

answers: NDQ_003386

answers: movement of rock

answers: NDQ_003387

answers: compression stress

answers: NDQ_003388

answers: shear stress

answers: NDQ_003389

answers: not visible in the code

answers: NDQ_003390

answers: unnamed

answers: NDQ_003391

answers: dip-slip fault plane

answers: NDQ_003392

answers: fold

answers: NDQ_003393

answers: is above a dip-slip fault plane

answers: NDQ_003394

answers: vertical

answers: NDQ_003395

answers: vertical fault plane

answers: NDQ_003396

answers: horizontal

answers: NDQ_003351

answers: User-specified folding

answers: NDQ_003352

answers: User-specified folding

answers: NDQ_003353

answers: User-specified folding

answers: NDQ_003354

answers: User-specified folding

answers: NDQ_003355

answers: anonymous

answers: NDQ_003356

answers: User-specified folding

answers: NDQ_003357

answers: token-based folding, this does not change the source text

answers: NDQ_003358

answers: (out-of-band),

answers: NDQ_003359

answers: User-specified folding

answers: NDQ_003360

answers: User-specified folding

answers: NDQ_003362

answers: User-specified folding

answers: NDQ_003363

answers: User-specified folding

answers: NDQ_003371

answers: User-specified folding

answers: NDQ_003373

answers: User-specified folding

answers: NDQ_003376

answers: User-specified folding

answers: NDQ_003378

answers: User-specified folding

answers: NDQ_003379

answers: User-specified folding

answers: NDQ_003380

answers: User-specified folding

answers: NDQ_003381

answers: User-specified folding

answers: NDQ_003382

answers: User-specified folding

answers: NDQ_003383

answers: User-specified folding

answers: NDQ_003384

answers: User-specified folding

answers: NDQ_003385

answers: User-specified folding

answers: NDQ_003386

answers: User-specified folding

answers: NDQ_003387

answers: User-specified folding

answers: NDQ_003388

answers: User-specified folding

answers: NDQ_003389

answers: User-specified folding

answers: NDQ_003390

answers: User-specified folding

answers: NDQ_003391

answers: User-specified folding

answers: NDQ_003392

answers: User-specified folding

answers: NDQ_003393

answers: User-specified folding

answers: NDQ_003394

answers: User-specified folding

answers: NDQ_003395

answers: User-specified folding

answers: NDQ_003396

answers: User-specified folding

text: A rift valley is a linear-shaped lowland between several highlands or mountain ranges created by the action of a geologic rift or fault. A rift valley is formed on a divergent plate boundary, a crustal extension, a spreading apart of the surface, which is subsequently further deepened by the forces of erosion. When the tensional forces were strong enough to cause the plate to split apart, a center block dropped between the two blocks at its flanks, forming a graben. The drop of the center creates the nearly parallel steeply dipping walls of a rift valley when it is new. That  feature is the beginning of the rift valley, but as the process continues, the valley widens, until it becomes a large basin that fills with sediment from the rift walls and the surrounding area. One of the best known examples of this process is the East African Rift. On Earth, rifts can occur at all elevations, from the sea floor to plateaus and mountain ranges in continental crust or in oceanic crust. They are often associated with a number of adjoining subsidiary or co-extensive valleys, which are typically considered part of the principal rift valley geologically.

text: A rift valley is a linear-shaped lowland between several highlands or mountain ranges created by the action of a geologic

text: rift

text: or

text: fault

text: . A rift valley is formed on a divergent plate boundary, a crustal extension, a spreading apart of the surface, which is subsequently further deepened by the forces of erosion. When the tensional forces were strong enough to cause the plate to split apart, a center block dropped between the two blocks at its flanks, forming a

text: graben

text: . The drop of the center creates the nearly parallel steeply dipping walls of a rift valley when it is new. That  feature is the beginning of the rift valley, but as the process continues, the valley widens, until it becomes a large basin that fills with sediment from the rift walls and the surrounding area. One of the best known examples of this process is the

text: East African Rift

text: . On Earth, rifts can occur at all elevations, from the sea floor to plateaus and mountain ranges in

text: continental crust

text: or in

text: oceanic crust

text: . They are often associated with a number of adjoining subsidiary or co-extensive valleys, which are typically considered part of the principal rift valley geologically.

answers: NDQ_003351

answers: tensional

answers: NDQ_003352

answers: cracks

answers: NDQ_003353

answers: tensional forces

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: graben

answers: NDQ_003356

answers: spread apart

answers: NDQ_003357

answers: a center block dropped between the two blocks at its flanks

answers: NDQ_003358

answers: graben

answers: NDQ_003359

answers: tensional forces

answers: NDQ_003360

answers: continental crust

answers: NDQ_003362

answers: rift valleys can occur at all elevations

answers: NDQ_003363

answers: rift valleys

answers: NDQ_003371

answers: Which of the following is not an example of a thrust fault?

answers: NDQ_003373

answers: Why is a deeply buried rock under compressive stresses?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What type of force applied to rock is a stress?

answers: NDQ_003381

answers: What does the drop of the center create?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: Which of the following is not a type of normal fault?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip faults, rift valleys, or faults?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: graben

answers: NDQ_003391

answers: graben

answers: NDQ_003392

answers: graben

answers: NDQ_003393

answers: graben

answers: NDQ_003394

answers: a divergent plate boundary

answers: NDQ_003395

answers: a geologic rift

answers: NDQ_003396

answers: divergent plate boundary

answers: NDQ_003351

answers: erosion.

answers: NDQ_003352

answers: a center block dropped between the two blocks at its flanks,

answers: NDQ_003353

answers: plate to split apart,

answers: NDQ_003354

answers: A rift valley

answers: NDQ_003355

answers: graben.

answers: NDQ_003356

answers: steeply dipping walls

answers: NDQ_003357

answers: a center block dropped between the two blocks at its flanks,

answers: NDQ_003358

answers: a graben.

answers: NDQ_003359

answers: tensional forces were strong enough to cause the plate to split apart,

answers: NDQ_003360

answers: a divergent plate boundary,

answers: NDQ_003362

answers: A rift valley

answers: NDQ_003363

answers: rifts can occur at all elevations,

answers: NDQ_003371

answers: rift valley

answers: NDQ_003373

answers: erosion.

answers: NDQ_003376

answers: erosion.

answers: NDQ_003378

answers: erosion.

answers: NDQ_003379

answers: steeply dipping

answers: NDQ_003380

answers: tensional forces

answers: NDQ_003381

answers: a center block dropped between the two blocks at its flanks,

answers: NDQ_003382

answers: erosion.

answers: NDQ_003383

answers: tensional forces

answers: NDQ_003384

answers: graben.

answers: NDQ_003385

answers: rift valley

answers: NDQ_003386

answers: tensional forces were strong enough to cause the plate to split apart,

answers: NDQ_003387

answers: tensional forces

answers: NDQ_003388

answers: the tensional forces

answers: NDQ_003389

answers: a geologic rift

answers: NDQ_003390

answers: graben.

answers: NDQ_003391

answers: graben.

answers: NDQ_003392

answers: graben.

answers: NDQ_003393

answers: graben.

answers: NDQ_003394

answers: fault.

answers: NDQ_003395

answers: fault. A rift valley is formed on a divergent plate boundary,

answers: NDQ_003396

answers: parallel steeply dipping walls of a rift valley

text: Dacitic magma is formed by the subduction of young oceanic crust under a thick felsic continental plate. Oceanic crust is hydrothermally altered causing addition of quartz and sodium. As the young, hot oceanic plate is subducted under continental crust, the subducted slab partially melts and interacts with the upper mantle through convection and dehydration reactions. The process of subduction creates metamorphism in the subducting slab. When this slab reaches the mantle and initiates the dehydration reactions, minerals such as talc, serpentine, mica and amphiboles break down generating a more sodic melt. The magma then continues to migrate upwards causing differentiation and becomes even more sodic and silicic as it rises. Once at the cold surface, the sodium rich magma crystallizes plagioclase, quartz and hornblende. Accessory minerals like pyroxenes provide insight to the history of the magma.

text: Dacitic magma is formed by the subduction of young oceanic crust under a thick

text: felsic

text: continental plate. Oceanic crust is hydrothermally altered causing addition of quartz and sodium. As the young, hot oceanic plate is subducted under continental crust, the subducted slab

text: partially melts

text: and interacts with the upper mantle through convection and dehydration reactions. The process of subduction creates metamorphism in the subducting slab. When this slab reaches the mantle and initiates the dehydration reactions, minerals such as

text: talc

text: serpentine

text: mica

text: and

text: amphibole

text: s break down generating a more sodic melt. The magma then continues to migrate upwards causing differentiation and becomes even more sodic and silicic as it rises. Once at the cold surface, the sodium rich magma crystallizes plagioclase, quartz and hornblende. Accessory minerals like pyroxenes provide insight to the history of the magma.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: breaks down

answers: NDQ_003353

answers: metamorphism

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: continental plate

answers: NDQ_003356

answers: break down

answers: NDQ_003357

answers: talc, serpentine, mica and amphiboles break down

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: continental plates

answers: NDQ_003362

answers: The process of subduction creates metamorphism

answers: NDQ_003363

answers: subduction

answers: NDQ_003371

answers: Which of the following is not formed by the subduction of young oceanic crust?

answers: NDQ_003373

answers: What is the main idea of this passage?

answers: NDQ_003376

answers: Which of the following is not caused by compressive forces?

answers: NDQ_003378

answers: What is the process of subduction called?

answers: NDQ_003379

answers: Which of the following is not a type of strike-slip fault?

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: Which of the following is not a type of stress: convection, subduction, or dehydration?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not a mineral: serpentine, mica or amphiboles?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: Which of the following is not a cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not caused by compression stress?

answers: NDQ_003388

answers: Which of the following is not a type of strike-slip fault?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: subduction

answers: NDQ_003391

answers: subducted slab

answers: NDQ_003392

answers: unanswerable

answers: NDQ_003393

answers: subducted slab

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: unanswerable

answers: NDQ_003396

answers: subduction

answers: NDQ_003351

answers: Dacitic magma

answers: NDQ_003352

answers: break down

answers: NDQ_003353

answers: metamorphism

answers: NDQ_003354

answers: Dacitic magma

answers: NDQ_003355

answers: Dacitic magma

answers: NDQ_003356

answers: talc, serpentine, mica and amphiboles break down

answers: NDQ_003357

answers: subducted slab partially melts and interacts with the upper mantle

answers: NDQ_003358

answers: Dacitic magma

answers: NDQ_003359

answers: Dacitic magma

answers: NDQ_003360

answers: Dacitic magma

answers: NDQ_003362

answers: Dacitic magma

answers: NDQ_003363

answers: Dacitic magma

answers: NDQ_003371

answers: Dacitic magma

answers: NDQ_003373

answers: Dacitic magma

answers: NDQ_003376

answers: Dacitic magma

answers: NDQ_003378

answers: Dacitic magma

answers: NDQ_003379

answers: Dacitic magma

answers: NDQ_003380

answers: Dacitic magma

answers: NDQ_003381

answers: subducted slab partially melts and interacts with the upper mantle

answers: NDQ_003382

answers: convection and dehydration reactions.

answers: NDQ_003383

answers: Dacitic magma

answers: NDQ_003384

answers: upwards

answers: NDQ_003385

answers: Dacitic magma

answers: NDQ_003386

answers: Dacitic magma

answers: NDQ_003387

answers: Dacitic magma

answers: NDQ_003388

answers: Dacitic magma

answers: NDQ_003389

answers: subduction creates metamorphism

answers: NDQ_003390

answers: Dacitic magma is formed by the subduction

answers: NDQ_003391

answers: Dacitic magma

answers: NDQ_003392

answers: Dacitic magma

answers: NDQ_003393

answers: Dacitic magma

answers: NDQ_003394

answers: Dacitic magma

answers: NDQ_003395

answers: Dacitic magma

answers: NDQ_003396

answers: Dacitic magma

text: As one of the requirements for stress corrosion cracking is the presence of stress in the components, one method of control is to eliminate that stress, or at least reduce it below the threshold stress for SCC. This is not usually feasible for working stresses (the stress that the component is intended to support), but it may be possible where the stress causing cracking is a residual stress introduced during welding or forming.Residual stresses can be relieved by stress-relief annealing, and this is widely used for carbon steels. These have the advantage of a relatively high threshold stress for most environments, consequently it is relatively easy to reduce the residual stresses to a low enough level. In contrast austenitic stainless steels have a very low threshold stress for chloride SCC. This, combined with the high annealing temperatures that are necessary to avoid other problems, such as sensitization and sigma phase embrittlement, means that stress relief is rarely successful as a method of controlling SCC for this system.For large structures, for which full stress-relief annealing is difficult or impossible, partial stress relief around welds and other critical areas may be of value. However, this must be done in a controlled way to avoid creating new regions of high residual stress, and expert advice is advisable if this approach is adopted.Stresses can also be relieved mechanically. For example, hydrostatic testing beyond yield will tend to ‘even-out’ the stresses and thereby reduce the peak residual stress. Similarly laser peening, shot-peening, or grit-blasting tend to introduce a surface compressive stress, and are beneficial for the control of SCC. The uniformity with which these processes are applied is important. If, for example, only the weld region is shot-peened, damaging tensile stresses may be created at the border of the peened area.  The compressive residual stresses imparted by laser peening are precisely controlled both in location and intensity, and can be applied to mitigate sharp transitions into tensile regions.  Laser peening imparts deep compressive residual stresses on the order of 10 to 20 times deeper than conventional shot peening making it significantly more beneficial at preventing SCC.  Laser peening is widely used in the aerospace and power generation industries in gas fired turbine engines.

text: As one of the requirements for stress corrosion cracking is the presence of stress in the components, one method of control is to eliminate that stress, or at least reduce it below the threshold stress for SCC. This is not usually feasible for working stresses (the stress that the component is intended to support), but it may be possible where the stress causing cracking is a

text: residual stress

text: introduced during welding or forming.Residual stresses can be relieved by stress-relief annealing, and this is widely used for carbon steels. These have the advantage of a relatively high threshold stress for most environments, consequently it is relatively easy to reduce the residual stresses to a low enough level. In contrast austenitic stainless steels have a very low threshold stress for chloride SCC. This, combined with the high annealing temperatures that are necessary to avoid other problems, such as sensitization and sigma phase embrittlement, means that stress relief is rarely successful as a method of controlling SCC for this system.For large structures, for which full stress-relief annealing is difficult or impossible, partial stress relief around welds and other critical areas may be of value. However, this must be done in a controlled way to avoid creating new regions of high residual stress, and expert advice is advisable if this approach is adopted.Stresses can also be relieved mechanically. For example, hydrostatic testing beyond yield will tend to ‘even-out’ the stresses and thereby reduce the peak residual stress. Similarly

text: laser peening

text: , shot-peening, or grit-blasting tend to introduce a surface compressive stress, and are beneficial for the control of SCC. The uniformity with which these processes are applied is important. If, for example, only the weld region is shot-peened, damaging tensile stresses may be created at the border of the peened area.  The compressive residual stresses imparted by laser peening are precisely controlled both in location and intensity, and can be applied to mitigate sharp transitions into tensile regions.  Laser peening imparts deep compressive residual stresses on the order of 10 to 20 times deeper than conventional shot peening making it significantly more beneficial at preventing SCC.  Laser peening is widely used in the aerospace and power generation industries in gas fired turbine engines.

answers: NDQ_003351

answers: tensile

answers: NDQ_003352

answers: cracks

answers: NDQ_003353

answers: compressive stresses

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: crack

answers: NDQ_003357

answers: tensile stresses are created at the border of the peened area

answers: NDQ_003358

answers: crack

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: working stresses (the stress that the component is intended to support)

answers: NDQ_003363

answers: tectonic plate boundaries

answers: NDQ_003371

answers: unanswerable

answers: NDQ_003373

answers: laser peening imparts deep compressive residual stresses

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: The amount the ground moves in an earthquake is called slip

answers: NDQ_003379

answers: unknown

answers: NDQ_003380

answers: unanswerable

answers: NDQ_003381

answers: What happens to rock when confining stress occurs?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: A fault zone is an area where faults are clustered.

answers: NDQ_003386

answers: faults are the cause of earthquakes

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: unanswerable

answers: NDQ_003389

answers: the process of folding

answers: NDQ_003390

answers: Stress corrosion cracking

answers: NDQ_003391

answers: Stress corrosion cracking

answers: NDQ_003392

answers: stress corrosion cracking

answers: NDQ_003393

answers: igneous

answers: NDQ_003394

answers: SCC

answers: NDQ_003395

answers: unanswerable

answers: NDQ_003396

answers: horizontal fault

answers: NDQ_003351

answers: tensile

answers: NDQ_003352

answers: impossible, partial stress relief

answers: NDQ_003353

answers: SCC.

answers: NDQ_003354

answers: 10 to 20 times

answers: NDQ_003355

answers: tensile regions.

answers: NDQ_003356

answers: SCC.

answers: NDQ_003357

answers: laser peening,

answers: NDQ_003358

answers: SCC.

answers: NDQ_003359

answers: partial stress relief

answers: NDQ_003360

answers: stress-relief annealing

answers: NDQ_003362

answers: ling is difficult or impossible,

answers: NDQ_003363

answers: difficult or impossible,

answers: NDQ_003371

answers: stress-relief annealing

answers: NDQ_003373

answers: laser peening

answers: NDQ_003376

answers: laser peening

answers: NDQ_003378

answers: SCC.

answers: NDQ_003379

answers: stress relief

answers: NDQ_003380

answers: partial stress relief

answers: NDQ_003381

answers: SCC.

answers: NDQ_003382

answers: surface compressive stress,

answers: NDQ_003383

answers: partial stress relief

answers: NDQ_003384

answers: partial stress relief

answers: NDQ_003385

answers: Laser peening imparts deep compressive residual stresses

answers: NDQ_003386

answers: annealing

answers: NDQ_003387

answers: SCC.

answers: NDQ_003388

answers: SCC.

answers: NDQ_003389

answers: SCC.

answers: NDQ_003390

answers: partial stress relief

answers: NDQ_003391

answers: Laser peening

answers: NDQ_003392

answers: stress corrosion cracking

answers: NDQ_003393

answers: Laser peening imparts deep compressive residual stresses

answers: NDQ_003394

answers: partial stress relief

answers: NDQ_003395

answers: impossible, partial stress relief

answers: NDQ_003396

answers: SCC.

text: This island is part of the "Kondyor-Feklistov metallogenic belt" (KD) owing to the presence of placers  which include minerals like "blacksand platinum".The "Kondyor-Feklistov metallogenic belt" is one of the major metallogenic belts of Northeast Asia. It is assumed that it formed by an oblique subduction of the oceanic crust of the Mongol-Okhotsk paleoocean under the southern margin of the Siberian continent.

text: This island is part of the "Kondyor-Feklistov

text: metallogenic

text: belt" (KD) owing to the presence of

text: placer

text: s  which include minerals like "blacksand

text: platinum

text: ".The "Kondyor-Feklistov metallogenic belt" is one of the major metallogenic belts of Northeast Asia. It is assumed that it formed by an oblique subduction of the oceanic crust of the Mongol-Okhotsk paleoocean under the southern margin of the Siberian continent.

answers: NDQ_003351

answers: subduction

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: subduction

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: oblique

answers: NDQ_003356

answers: subduct

answers: NDQ_003357

answers: the oceanic crust of the Mongol-Okhotsk paleoocean under the southern margin of the Siberian continent

answers: NDQ_003358

answers: placer

answers: NDQ_003359

answers: subducts

answers: NDQ_003360

answers: continental plates

answers: NDQ_003362

answers: it formed by an oblique subduction of the oceanic crust

answers: NDQ_003363

answers: subduction of the oceanic crust

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: What is the main idea of this passage?

answers: NDQ_003376

answers: What type of forces is the terrain known as basin-and-range?

answers: NDQ_003378

answers: What is the amount the ground moves in an earthquake?

answers: NDQ_003379

answers: What is the dip of the fault plane in a strike-slip fault?

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What type of stress does the Kondyor-Feklistov metallogenic belt experience?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What is the name of the placers that include minerals like "blacksand platinum"?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: What is the cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not a type of placer: placers or placers?

answers: NDQ_003388

answers: What type of stress is shear stress?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: subduction

answers: NDQ_003391

answers: subduction

answers: NDQ_003392

answers: oblique subduction

answers: NDQ_003393

answers: subduction

answers: NDQ_003394

answers: oblique

answers: NDQ_003395

answers: oblique subduction

answers: NDQ_003396

answers: oblique

answers: NDQ_003351

answers: oblique subduction

answers: NDQ_003352

answers: oblique subduction

answers: NDQ_003353

answers: oblique subduction

answers: NDQ_003354

answers: "Kondyor-Feklistov metallogenic belt"

answers: NDQ_003355

answers: oblique subduction

answers: NDQ_003356

answers: "blacksand platinum".The

answers: NDQ_003357

answers: oblique subduction

answers: NDQ_003358

answers: placers

answers: NDQ_003359

answers: oblique subduction

answers: NDQ_003360

answers: "Kondyor-Feklistov metallogenic belt"

answers: NDQ_003362

answers: "blacksand platinum".The

answers: NDQ_003363

answers: Mongol-Okhotsk paleoocean

answers: NDQ_003371

answers: "Kondyor-Feklistov metallogenic belt"

answers: NDQ_003373

answers: oblique subduction

answers: NDQ_003376

answers: "Kondyor-Feklistov metallogenic belt"

answers: NDQ_003378

answers: "Kondyor-Feklistov metallogenic belt"

answers: NDQ_003379

answers: oblique

answers: NDQ_003380

answers: "Kondyor-Feklistov metallogenic belt"

answers: NDQ_003381

answers: "Kondyor-Feklistov metallogenic belt"

answers: NDQ_003382

answers: "Kondyor-Feklistov metallogenic belt"

answers: NDQ_003383

answers: "Kondyor-Feklistov metallogenic belt"

answers: NDQ_003384

answers: "Kondyor-Feklistov metallogenic belt"

answers: NDQ_003385

answers: "Kondyor-Feklistov metallogenic belt"

answers: NDQ_003386

answers: oblique subduction

answers: NDQ_003387

answers: "Kondyor-Feklistov metallogenic belt"

answers: NDQ_003388

answers: "Kondyor-Feklistov metallogenic belt"

answers: NDQ_003389

answers: oblique subduction

answers: NDQ_003390

answers: oblique subduction

answers: NDQ_003391

answers: oceanic crust

answers: NDQ_003392

answers: "Kondyor-Feklistov metallogenic belt"

answers: NDQ_003393

answers: oblique subduction of the oceanic crust

answers: NDQ_003394

answers: oblique

answers: NDQ_003395

answers: oblique subduction

answers: NDQ_003396

answers: oblique subduction

text: Much of the Venusian surface appears to have been shaped by volcanic activity. Venus has several times as many volcanoes as Earth, and it has 167 large volcanoes that are over 100 km across. The only volcanic complex of this size on Earth is the Big Island of Hawaii. This is not because Venus is more volcanically active than Earth, but because its crust is older. Earth's oceanic crust is continually recycled by subduction at the boundaries of tectonic plates, and has an average age of about 100 million years, whereas the Venusian surface is estimated to be 300–600 million years old.

text: Much of the Venusian surface appears to have been shaped by volcanic activity. Venus has several times as many volcanoes as Earth, and it has 167 large volcanoes that are over 100 km across. The only volcanic complex of this size on Earth is the

text: Big Island

text: of Hawaii. This is not because Venus is more volcanically active than Earth, but because its crust is older. Earth's

text: oceanic crust

text: is continually recycled by

text: subduction

text: at the boundaries of

text: tectonic plate

text: s, and has an average age of about 100 million years, whereas the Venusian surface is estimated to be 300–600 million years old.

answers: NDQ_003351

answers: subduction

answers: NDQ_003352

answers: subducts

answers: NDQ_003353

answers: subduction

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: subduction

answers: NDQ_003356

answers: Earth's oceanic crust

answers: NDQ_003357

answers: Earth's oceanic crust is continually recycled by subduction

answers: NDQ_003358

answers: unanswerable

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth

answers: NDQ_003362

answers: Venus has several times as many volcanoes as Earth

answers: NDQ_003363

answers: Venus

answers: NDQ_003371

answers: What is the only volcanic complex of this size on Earth?

answers: NDQ_003373

answers: Why does Venus have several times as many volcanoes as Earth?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: what is the only volcanic complex of this size on Earth

answers: NDQ_003380

answers: What is the only volcanic complex of this size on Earth?

answers: NDQ_003381

answers: What is the only volcanic complex of this size on Earth

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: What is the only volcanic complex of this size on Earth?

answers: NDQ_003384

answers: What is the only volcanic complex of this size on Earth?

answers: NDQ_003385

answers: what is the only volcanic complex of this size on Earth

answers: NDQ_003386

answers: Earth's oceanic crust

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: subduction at the boundaries of tectonic plates, or normal faults?

answers: NDQ_003388

answers: What is the only volcanic complex of this size on Earth?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: subduction

answers: NDQ_003391

answers: subduction

answers: NDQ_003392

answers: subduction

answers: NDQ_003393

answers: subduction

answers: NDQ_003394

answers: tectonic plates

answers: NDQ_003395

answers: tectonic plates

answers: NDQ_003396

answers: subduction

answers: NDQ_003351

answers: subduction

answers: NDQ_003352

answers: subduction

answers: NDQ_003353

answers: subduction

answers: NDQ_003354

answers: Venus is more volcanically active than Earth,

answers: NDQ_003355

answers: subduction

answers: NDQ_003356

answers: volcanic activity.

answers: NDQ_003357

answers: subduction

answers: NDQ_003358

answers: volcanoes

answers: NDQ_003359

answers: tectonic plates,

answers: NDQ_003360

answers: volcanic activity.

answers: NDQ_003362

answers: Venus is more volcanically active than Earth,

answers: NDQ_003363

answers: volcanic activity.

answers: NDQ_003371

answers: subduction at the boundaries of tectonic plates,

answers: NDQ_003373

answers: subduction at the boundaries of tectonic plates,

answers: NDQ_003376

answers: volcanic activity.

answers: NDQ_003378

answers: subduction at the boundaries of tectonic plates,

answers: NDQ_003379

answers: Venus has several times as many volcanoes

answers: NDQ_003380

answers: volcanic activity.

answers: NDQ_003381

answers: subduction at the boundaries of tectonic plates,

answers: NDQ_003382

answers: subduction

answers: NDQ_003383

answers: tectonic plates,

answers: NDQ_003384

answers: Venus has several times as many volcanoes

answers: NDQ_003385

answers: tectonic plates,

answers: NDQ_003386

answers: tectonic plates,

answers: NDQ_003387

answers: subduction at the boundaries of tectonic plates,

answers: NDQ_003388

answers: volcanic activity.

answers: NDQ_003389

answers: subduction at the boundaries of tectonic plates,

answers: NDQ_003390

answers: subduction

answers: NDQ_003391

answers: subduction

answers: NDQ_003392

answers: subduction at the boundaries of tectonic plates,

answers: NDQ_003393

answers: subduction

answers: NDQ_003394

answers: subduction

answers: NDQ_003395

answers: subduction

answers: NDQ_003396

answers: subduction

text: The extreme cases of these two types of back-arc deformation can be found in Chile and at the Marianas arc. The shallow dipping slab subducting beneath Chile at an angle of about 10–15° causes a compressional stress on the back-arc region behind the Andes. On the other extreme, the slab going down into the mantle at the Marianas subduction zone is so steep it is nearly vertical. This is the perfect example of an oceanic back-arc basin experiencing extensional forces. The Oriente in Ecuador (the eastern part of the country covered by rainforest) is also a good example of an extensional back-arc basin, this time in a continental setting. The continental crust in this area east of the Andes has been stretched out and covered by layers of sediments.

text: The extreme cases of these two types of back-arc deformation can be found in Chile and at the

text: Marianas arc

text: . The shallow dipping slab subducting beneath Chile at an angle of about 10–15° causes a compressional stress on the back-arc region behind the Andes. On the other extreme, the slab going down into the mantle at the Marianas subduction zone is so steep it is nearly vertical. This is the perfect example of an oceanic back-arc basin experiencing extensional forces. The Oriente in Ecuador (the eastern part of the country covered by rainforest) is also a good example of an extensional back-arc basin, this time in a continental setting. The continental crust in this area east of the Andes has been stretched out and covered by layers of sediments.

answers: NDQ_003351

answers: compressional

answers: NDQ_003352

answers: compresses

answers: NDQ_003353

answers: compressional stress

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: subduction zone

answers: NDQ_003356

answers: stretch out

answers: NDQ_003357

answers: compressional stress is caused by

answers: NDQ_003358

answers: subduction zone

answers: NDQ_003359

answers: subducts

answers: NDQ_003360

answers: continental crust

answers: NDQ_003362

answers: the Marianas subduction zone is so steep it is nearly vertical

answers: NDQ_003363

answers: Marianas subduction zone

answers: NDQ_003371

answers: Which of the following is not a type of back-arc deformation?

answers: NDQ_003373

answers: unanswerable

answers: NDQ_003376

answers: Which of the following is not an example of an oceanic back-arc basin experiencing extensional forces?

answers: NDQ_003378

answers: What type of deformation can be found in Chile?

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What type of stress does the Marianas arc experience?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock: compressional stress or extensional forces?

answers: NDQ_003384

answers: What type of fold is the Marianas arc?

answers: NDQ_003385

answers: What is the name of the Marianas subduction zone?

answers: NDQ_003386

answers: What type of movement of rock is the cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not an example of an oceanic back-arc basin experiencing extensional forces?

answers: NDQ_003388

answers: Which of the following is not an example of an oceanic back-arc basin experiencing extensional forces?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: subduction zone

answers: NDQ_003391

answers: subduction zone

answers: NDQ_003392

answers: extensional

answers: NDQ_003393

answers: Marianas subduction zone

answers: NDQ_003394

answers: Marianas subduction zone

answers: NDQ_003395

answers: Marianas subduction zone

answers: NDQ_003396

answers: Marianas subduction zone

answers: NDQ_003351

answers: compressional

answers: NDQ_003352

answers: stretched out and covered by layers of sediments.

answers: NDQ_003353

answers: deformation

answers: NDQ_003354

answers: extensional forces.

answers: NDQ_003355

answers: extensional forces.

answers: NDQ_003356

answers: extensional forces.

answers: NDQ_003357

answers: compressional stress

answers: NDQ_003358

answers: extensional back-arc basin,

answers: NDQ_003359

answers: extensional forces.

answers: NDQ_003360

answers: back-arc deformation

answers: NDQ_003362

answers: stretched out and covered by layers of sediments.

answers: NDQ_003363

answers: back-arc

answers: NDQ_003371

answers: Marianas arc.

answers: NDQ_003373

answers: vertical.

answers: NDQ_003376

answers: extensional forces.

answers: NDQ_003378

answers: extensional forces.

answers: NDQ_003379

answers: Marianas subduction zone is so steep it is nearly vertical.

answers: NDQ_003380

answers: compressional stress

answers: NDQ_003381

answers: compressional stress

answers: NDQ_003382

answers: compressional stress

answers: NDQ_003383

answers: compressional stress

answers: NDQ_003384

answers: Marianas arc.

answers: NDQ_003385

answers: Marianas arc.

answers: NDQ_003386

answers: back-arc deformation

answers: NDQ_003387

answers: compressional stress

answers: NDQ_003388

answers: extensional forces.

answers: NDQ_003389

answers: extensional forces.

answers: NDQ_003390

answers: Marianas arc.

answers: NDQ_003391

answers: slab

answers: NDQ_003392

answers: Marianas arc.

answers: NDQ_003393

answers: Marianas arc.

answers: NDQ_003394

answers: Marianas subduction zone

answers: NDQ_003395

answers: Marianas subduction zone

answers: NDQ_003396

answers: vertical.

text: Sedimentary structures such as cross bedding, graded bedding and ripple marks are utilized in stratigraphic studies to indicate original position of strata in geologically complex terrains and understand the depositional environment of the sediment.

text: Sedimentary structures such as

text: cross bedding

text: graded bedding

text: and

text: ripple marks

text: are utilized in

text: stratigraphic

text: studies to indicate

text: original position

text: of

text: strata

text: in geologically complex terrains and understand the

text: depositional environment

text: of the sediment.

answers: NDQ_003351

answers: cross bedding

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: voids to form.

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: ripple mark

answers: NDQ_003356

answers: elongate

answers: NDQ_003357

answers: sedimentary structures such as cross bedding and graded bedding are utilized to indicate original position of strata

answers: NDQ_003358

answers: discontinuity

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: continental plates

answers: NDQ_003362

answers: The San Andreas fault is not a fault.

answers: NDQ_003363

answers: geologically complex terrains

answers: NDQ_003371

answers: What is a thrust fault?

answers: NDQ_003373

answers: What is the reason for this?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: The amount the ground moves in an earthquake is called slip.

answers: NDQ_003379

answers: The dip of the fault plane is horizontal

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What is the result of confining stress?

answers: NDQ_003382

answers: None of the above choices.

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: None of the above choices.

answers: NDQ_003387

answers: Which of the following is not a type of normal fault?

answers: NDQ_003388

answers: Which of the following is not a type of strike-slip fault?

answers: NDQ_003389

answers: It's impossible to say

answers: NDQ_003390

answers: can refer to:

answers: NDQ_003391

answers: is a strata

answers: NDQ_003392

answers: Ripple fault

answers: NDQ_003393

answers: is a strata

answers: NDQ_003394

answers: lateral fault

answers: NDQ_003395

answers: is a fault

answers: NDQ_003396

answers: isosceles

answers: NDQ_003351

answers: ripple marks

answers: NDQ_003352

answers: ripple marks

answers: NDQ_003353

answers: ripple marks

answers: NDQ_003354

answers: cross bedding, graded bedding and ripple marks

answers: NDQ_003355

answers: ripple marks

answers: NDQ_003356

answers: ripple marks

answers: NDQ_003357

answers: ripple marks

answers: NDQ_003358

answers: ripple marks

answers: NDQ_003359

answers: geologically complex terrains

answers: NDQ_003360

answers: Sedimentary structures

answers: NDQ_003362

answers: original position of strata in geologically complex terrains

answers: NDQ_003363

answers: geologically complex terrains

answers: NDQ_003371

answers: cross bedding, graded bedding and ripple marks

answers: NDQ_003373

answers: cross bedding, graded bedding and ripple marks

answers: NDQ_003376

answers: ripple marks

answers: NDQ_003378

answers: ripple marks

answers: NDQ_003379

answers: cross bedding, graded bedding and ripple marks

answers: NDQ_003380

answers: ripple marks

answers: NDQ_003381

answers: ripple marks

answers: NDQ_003382

answers: cross bedding, graded bedding and ripple marks

answers: NDQ_003383

answers: ripple marks

answers: NDQ_003384

answers: cross bedding, graded bedding and ripple marks

answers: NDQ_003385

answers: geologically complex terrains

answers: NDQ_003386

answers: cross bedding, graded bedding and ripple marks

answers: NDQ_003387

answers: cross bedding, graded bedding and ripple marks

answers: NDQ_003388

answers: ripple marks

answers: NDQ_003389

answers: geologically complex terrains

answers: NDQ_003390

answers: ripple marks

answers: NDQ_003391

answers: ripple marks

answers: NDQ_003392

answers: ripple marks

answers: NDQ_003393

answers: ripple marks

answers: NDQ_003394

answers: ripple marks

answers: NDQ_003395

answers: ripple marks

answers: NDQ_003396

answers: ripple marks

text: Diastrophism refers to deformation of the Earth's crust, and more especially to folding and faulting. Diastrophism can be considered part of geotectonics. Diastrophism comes from the Greek word meaning a twisting.

text: Diastrophism refers to deformation of the Earth's

text: crust

text: , and more especially to

text: folding

text: and

text: faulting

text: . Diastrophism can be considered part of

text: geotectonics

text: . Diastrophism comes from the

text: Greek

text: word meaning a twisting.

answers: NDQ_003351

answers: faulting

answers: NDQ_003352

answers: deforms

answers: NDQ_003353

answers: deformation

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: twisting

answers: NDQ_003356

answers: fold

answers: NDQ_003357

answers: Diastrophism can be considered part of

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: deforms

answers: NDQ_003360

answers: faults

answers: NDQ_003362

answers: Diastrophism comes from the Greek word meaning a twisting.

answers: NDQ_003363

answers: faulting

answers: NDQ_003371

answers: Which of the following is not a type of fault?

answers: NDQ_003373

answers: How would you describe a twisting rock?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: what is the Greek word for twisting?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: Which of the following is not a type of deformation: folding and faulting?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not a type of fold: syncline, fold or fault?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: Which of the following is not a cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not a cause of normal faults?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip faults, folding faults, or faulting?

answers: NDQ_003389

answers: It's impossible to say

answers: NDQ_003390

answers: Diastrophism

answers: NDQ_003391

answers: diastrophic

answers: NDQ_003392

answers: Diastrophism

answers: NDQ_003393

answers: diastrophic

answers: NDQ_003394

answers: Diastrophism

answers: NDQ_003395

answers: Diastrophism

answers: NDQ_003396

answers: Diastrophism

answers: NDQ_003351

answers: Diastrophism

answers: NDQ_003352

answers: folding and faulting.

answers: NDQ_003353

answers: folding and faulting.

answers: NDQ_003354

answers: Diastrophism

answers: NDQ_003355

answers: Diastrophism

answers: NDQ_003356

answers: folding and faulting.

answers: NDQ_003357

answers: twisting.

answers: NDQ_003358

answers: Diastrophism

answers: NDQ_003359

answers: folding and faulting.

answers: NDQ_003360

answers: Diastrophism

answers: NDQ_003362

answers: Diastrophism

answers: NDQ_003363

answers: Diastrophism

answers: NDQ_003371

answers: Diastrophism

answers: NDQ_003373

answers: Diastrophism

answers: NDQ_003376

answers: Diastrophism

answers: NDQ_003378

answers: Diastrophism

answers: NDQ_003379

answers: Diastrophism

answers: NDQ_003380

answers: twisting.

answers: NDQ_003381

answers: Diastrophism

answers: NDQ_003382

answers: folding and faulting.

answers: NDQ_003383

answers: Diastrophism

answers: NDQ_003384

answers: Diastrophism

answers: NDQ_003385

answers: Diastrophism

answers: NDQ_003386

answers: Diastrophism

answers: NDQ_003387

answers: Diastrophism

answers: NDQ_003388

answers: Diastrophism

answers: NDQ_003389

answers: Diastrophism

answers: NDQ_003390

answers: faulting.

answers: NDQ_003391

answers: Diastrophism

answers: NDQ_003392

answers: faulting.

answers: NDQ_003393

answers: Diastrophism

answers: NDQ_003394

answers: faulting.

answers: NDQ_003395

answers: faulting.

answers: NDQ_003396

answers: Diastrophism

text: A tectonostratigraphic terrane is not necessarily an independent microplate in origin, since it may not contain the full thickness of the lithosphere. It is a piece of crust which has been transported laterally, usually as part of a larger plate, and is relatively buoyant due to thickness or low density.  When the plate of which it was a part subducted under another plate, the terrane failed to subduct, detached from its transporting plate, and accreted onto the overriding plate.  Therefore, the terrane transferred from one plate to the other. Typically, accreting terranes are portions of continental crust which have rifted off another continental mass and been transported surrounded by oceanic crust, or old island arcs formed at some distant subduction zone.

text: A tectonostratigraphic terrane is not necessarily an independent

text: microplate

text: in origin, since it may not contain the full thickness of the

text: lithosphere

text: . It is a piece of

text: crust

text: which has been transported laterally, usually as part of a larger plate, and is relatively buoyant due to thickness or low density.  When the plate of which it was a part

text: subduct

text: ed under another plate, the terrane failed to subduct, detached from its transporting plate, and accreted onto the overriding plate.  Therefore, the terrane transferred from one plate to the other. Typically, accreting terranes are portions of

text: continental crust

text: which have

text: rifted off

text: another continental mass and been transported surrounded by oceanic crust, or old

text: island arc

text: s formed at some distant

text: subduction zone

answers: NDQ_003351

answers: subduction

answers: NDQ_003352

answers: is more buoyant

answers: NDQ_003353

answers: subduction

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: arc

answers: NDQ_003356

answers: buoyant

answers: NDQ_003357

answers: The terrane failed to subduct, detached from its transporting plate, and accreted onto the overriding plate

answers: NDQ_003358

answers: unanswerable

answers: NDQ_003359

answers: failed to subduct

answers: NDQ_003360

answers: continental crust

answers: NDQ_003362

answers: an independent microplate in origin

answers: NDQ_003363

answers: subduction zone

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: compressive stresses

answers: NDQ_003376

answers: tectonostratigraphic terrane

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: vertical

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What happens to rock when confining stress occurs?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: fault zone

answers: NDQ_003386

answers: movement of rock at faults

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: What type of stress is shear stress?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: rifting

answers: NDQ_003391

answers: terrane

answers: NDQ_003392

answers: rifting

answers: NDQ_003393

answers: terrane

answers: NDQ_003394

answers: laterally

answers: NDQ_003395

answers: tectonostatic

answers: NDQ_003396

answers: rifting

answers: NDQ_003351

answers: subducted under another plate, the terrane failed to subduct,

answers: NDQ_003352

answers: buoyant

answers: NDQ_003353

answers: accreted onto the overriding plate.

answers: NDQ_003354

answers: accreted onto the overriding plate.

answers: NDQ_003355

answers: arcs

answers: NDQ_003356

answers: buoyant

answers: NDQ_003357

answers: the terrane failed to subduct,

answers: NDQ_003358

answers: tectonostratigraphic terrane

answers: NDQ_003359

answers: accreted onto the overriding plate.

answers: NDQ_003360

answers: accreted onto the overriding plate.

answers: NDQ_003362

answers: independent microplate in origin,

answers: NDQ_003363

answers: subduction zone.

answers: NDQ_003371

answers: accreted onto the overriding plate.

answers: NDQ_003373

answers: buoyant due to thickness or low density.

answers: NDQ_003376

answers: accreted onto the overriding plate.

answers: NDQ_003378

answers: accreted onto the overriding plate.

answers: NDQ_003379

answers: accreted onto the overriding plate.

answers: NDQ_003380

answers: buoyant due to thickness or low density.

answers: NDQ_003381

answers: accreted onto the overriding plate.

answers: NDQ_003382

answers: accreted onto the overriding plate.

answers: NDQ_003383

answers: accreted onto the overriding plate.

answers: NDQ_003384

answers: old island arcs

answers: NDQ_003385

answers: tectonostratigraphic terrane

answers: NDQ_003386

answers: accreted onto the overriding plate.

answers: NDQ_003387

answers: accreted onto the overriding plate.

answers: NDQ_003388

answers: accreted onto the overriding plate.

answers: NDQ_003389

answers: accreted onto the overriding plate.

answers: NDQ_003390

answers: subduction zone.

answers: NDQ_003391

answers: tectonostratigraphic terrane

answers: NDQ_003392

answers: accreted onto the overriding plate.

answers: NDQ_003393

answers: terrane

answers: NDQ_003394

answers: tectonostratigraphic terrane

answers: NDQ_003395

answers: subducted under another plate,

answers: NDQ_003396

answers: tectonostratigraphic terrane

text: Since the Pinnacles were moved to this area, the San Andreas fault has shifted  to the east of the park.  The original location of the San Andreas can be seen in the Chalone Creek fault.  Two other large faults are known to run through the park, the Miner's Gulch and Pinnacles faults.  These faults parallel the San Andreas and were most likely caused by major movements of the main fault. The establishment of the relative movement between the Pinnacles and the Neenach rocks was a significant factor in the acceptance of plate tectonics in geology.

text: Since the Pinnacles were moved to this area, the San Andreas fault has shifted  to the east of the park.  The original location of the San Andreas can be seen in the Chalone Creek fault.  Two other large faults are known to run through the park, the Miner's Gulch and Pinnacles faults.  These faults parallel the San Andreas and were most likely caused by major movements of the main fault. The establishment of the relative movement between the Pinnacles and the Neenach rocks was a significant factor in the acceptance of

text: plate tectonics

text: in geology.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: movement

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fault

answers: NDQ_003356

answers: move

answers: NDQ_003357

answers: San Andreas fault has shifted to the east

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: major movements

answers: NDQ_003360

answers: San Andreas fault

answers: NDQ_003362

answers: the San Andreas fault has shifted to the east of the park

answers: NDQ_003363

answers: plate tectonics

answers: NDQ_003371

answers: Which of the following is not a type of fault?

answers: NDQ_003373

answers: What is the San Andreas fault?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: what is the last word in the passage?

answers: NDQ_003379

answers: What type of fault is the San Andreas fault?

answers: NDQ_003380

answers: Which of the following is not a type of force applied to rock?

answers: NDQ_003381

answers: What can be seen in the Chalone Creek fault?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: What is the San Andreas fault?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: What is the San Andreas fault

answers: NDQ_003387

answers: Which of the following is not a type of fault: Miner's Gulch, Pinnacles or San Andreas?

answers: NDQ_003388

answers: Which of the following is not an example of a strike-slip fault?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: San Andreas fault

answers: NDQ_003391

answers: Neenach rocks

answers: NDQ_003392

answers: San Andreas fault

answers: NDQ_003393

answers: Neenach rocks

answers: NDQ_003394

answers: Chalone Creek fault

answers: NDQ_003395

answers: Chalone Creek fault

answers: NDQ_003396

answers: Chalone Creek fault

answers: NDQ_003351

answers: major movements of the main fault.

answers: NDQ_003352

answers: major movements

answers: NDQ_003353

answers: faults

answers: NDQ_003354

answers: Since the Pinnacles

answers: NDQ_003355

answers: fault

answers: NDQ_003356

answers: major movements of the main fault.

answers: NDQ_003357

answers: major movements

answers: NDQ_003358

answers: fault.

answers: NDQ_003359

answers: major movements

answers: NDQ_003360

answers: plate tectonics

answers: NDQ_003362

answers: shifted to the east of the park.

answers: NDQ_003363

answers: plate tectonics

answers: NDQ_003371

answers: Miner's Gulch and Pinnacles faults.

answers: NDQ_003373

answers: Miner's Gulch and Pinnacles faults.

answers: NDQ_003376

answers: major movements of the main fault.

answers: NDQ_003378

answers: major movements of the main fault.

answers: NDQ_003379

answers: Miner's Gulch and Pinnacles faults.

answers: NDQ_003380

answers: major movements of the main fault.

answers: NDQ_003381

answers: major movements of the main fault.

answers: NDQ_003382

answers: Miner's Gulch and Pinnacles faults.

answers: NDQ_003383

answers: major movements

answers: NDQ_003384

answers: Chalone Creek fault.

answers: NDQ_003385

answers: the Miner's Gulch and Pinnacles faults.

answers: NDQ_003386

answers: major movements of the main fault.

answers: NDQ_003387

answers: major movements of the main fault.

answers: NDQ_003388

answers: major movements of the main fault.

answers: NDQ_003389

answers: plate tectonics

answers: NDQ_003390

answers: San Andreas fault

answers: NDQ_003391

answers: Neenach

answers: NDQ_003392

answers: San Andreas fault

answers: NDQ_003393

answers: Neenach

answers: NDQ_003394

answers: Chalone Creek fault.

answers: NDQ_003395

answers: Chalone Creek fault.

answers: NDQ_003396

answers: Chalone Creek fault.

text: During the Mesozoic era (about 250 to 66 million years ago) a large ocean (Tethys Ocean), floored by oceanic lithosphere existed in-between the supercontinents of Gondwana and Laurasia (which lay to the south and north respectively; Robertson & Dixon, 2006). This large oceanic plate was consumed at subduction zones (see subduction zone). At the subduction trenches the sedimentary rock layers that were deposited within the prehistoric Tethys Ocean buckled, were folded, faulted and tectonically mixed with huge blocks of crystalline basement rocks of the oceanic lithosphere. These blocks form a very complex mixture or mélange of rocks that include mainly serpentinite, basalt, dolerite and chert (e.g. Bergougnan, 1975). The Eurasian margin, now preserved in the Pontides (the Pontic Mountains along the Black Sea coast), is thought to have been geologically similar to the Western Pacific region today (e.g. Rice et al., 2006). Volcanic arcs (see volcanic arc) and backarc basins (see back-arc basin) formed and were emplaced onto Eurasia as ophiolites (see ophiolite) as they collided with microcontinents (literally relatively small plates of continental lithosphere; e.g. Ustaomer and Robertson, 1997). These microcontinents had been pulled away from the Gondwanan continent further south. Turkey is therefore made up from several different prehistorical microcontinents.

text: During the

text: Mesozoic

text: era (about 250 to 66 million years ago) a large ocean (

text: Tethys Ocean

text: ), floored by oceanic

text: lithosphere

text: existed in-between the supercontinents of

text: Gondwana

text: and

text: Laurasia

text: (which lay to the south and north respectively; Robertson & Dixon, 2006). This large oceanic plate was consumed at subduction zones (see

text: subduction zone

text: ). At the subduction trenches the

text: sedimentary rock

text: layers that were deposited within the prehistoric

text: Tethys Ocean

text: buckled, were folded, faulted and tectonically mixed with huge blocks of crystalline basement rocks of the oceanic

text: lithosphere

text: . These blocks form a very complex mixture or

text: mélange

text: of rocks that include mainly

text: serpentinite

text: basalt

text: dolerite

text: and

text: chert

text: (e.g. Bergougnan, 1975). The Eurasian margin, now preserved in the Pontides (the

text: Pontic Mountains

text: along the

text: Black Sea

text: coast), is thought to have been geologically similar to the Western Pacific region today (e.g. Rice et al., 2006). Volcanic arcs (see

text: volcanic arc

text: ) and backarc basins (see

text: back-arc basin

text: ) formed and were emplaced onto

text: Eurasia

text: as ophiolites (see

text: ophiolite

text: ) as they collided with microcontinents (literally relatively small plates of continental

text: lithosphere

text: ; e.g. Ustaomer and Robertson, 1997). These microcontinents had been pulled away from the Gondwanan continent further south. Turkey is therefore made up from several different prehistorical microcontinents.

answers: NDQ_003351

answers: faulting

answers: NDQ_003352

answers: folds

answers: NDQ_003353

answers: faulting

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: subduction zone

answers: NDQ_003356

answers: fold

answers: NDQ_003357

answers: sedimentary rock layers that were deposited within the prehistoric Tethys Ocean buckled, were folded, faulted

answers: NDQ_003358

answers: subduction zone

answers: NDQ_003359

answers: folds

answers: NDQ_003360

answers: subduction zones

answers: NDQ_003362

answers: Turkey is therefore made up from several different prehistorical microcontinents.

answers: NDQ_003363

answers: subduction zones

answers: NDQ_003371

answers: Which of the following is not a type of thrust fault?

answers: NDQ_003373

answers: What type of stresses is a deeply buried rock under?

answers: NDQ_003376

answers: What type of forces caused the terrain known as basin-and-range?

answers: NDQ_003378

answers: What is the amount the ground moves in an earthquake?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What is a stress?

answers: NDQ_003381

answers: What type of rock deforms?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is the name of the area where faults are clustered?

answers: NDQ_003386

answers: What is the cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not a cause of normal faults: compression stress, folding, or folding?

answers: NDQ_003388

answers: Which of the following is not a type of strike-slip fault: strike-slip, strike-slip, or strike-slip?

answers: NDQ_003389

answers: Which of the following is not a rock type: serpentinite, basalt, dolerite or chert?

answers: NDQ_003390

answers: subduction zone

answers: NDQ_003391

answers: basement rocks

answers: NDQ_003392

answers: subduction zone

answers: NDQ_003393

answers: crystalline basement rocks

answers: NDQ_003394

answers: faulted

answers: NDQ_003395

answers: fault with a vertical fault plane

answers: NDQ_003396

answers: back-arc basin

answers: NDQ_003351

answers: subduction zones

answers: NDQ_003352

answers: buckled, were folded, faulted

answers: NDQ_003353

answers: folded, faulted

answers: NDQ_003354

answers: Turkey

answers: NDQ_003355

answers: backarc basins (see back-arc basin)

answers: NDQ_003356

answers: tectonically mixed

answers: NDQ_003357

answers: tectonically mixed with huge blocks of crystalline basement rocks

answers: NDQ_003358

answers: subduction zones

answers: NDQ_003359

answers: folded, faulted

answers: NDQ_003360

answers: subduction zones

answers: NDQ_003362

answers: Turkey is therefore made up from several different prehistorical microcontinents.

answers: NDQ_003363

answers: subduction zones

answers: NDQ_003371

answers: Volcanic arcs

answers: NDQ_003373

answers: crystalline basement rocks

answers: NDQ_003376

answers: microcontinents

answers: NDQ_003378

answers: subduction zones

answers: NDQ_003379

answers: microcontinents

answers: NDQ_003380

answers: buckled, were folded, faulted

answers: NDQ_003381

answers: folded, faulted

answers: NDQ_003382

answers: subduction zones

answers: NDQ_003383

answers: faulted

answers: NDQ_003384

answers: volcanic arc) and backarc basins (see back-arc basin)

answers: NDQ_003385

answers: subduction zones

answers: NDQ_003386

answers: tectonically mixed

answers: NDQ_003387

answers: folded, faulted

answers: NDQ_003388

answers: the subduction trenches

answers: NDQ_003389

answers: folded,

answers: NDQ_003390

answers: subduction zones

answers: NDQ_003391

answers: crystalline basement rocks

answers: NDQ_003392

answers: backarc basins (see back-arc basin)

answers: NDQ_003393

answers: crystalline basement rocks

answers: NDQ_003394

answers: faulted

answers: NDQ_003395

answers: faulted

answers: NDQ_003396

answers: backarc basins (see back-arc basin)

text: The primary methods for dealing with faults include fault avoidance, fault tolerance, and fault detection and recovery. Fault avoidance covers proactive measures taken to minimize the occurrence of faults. These proactive measures can be in the form of transactions, replication and backups. Fault tolerance is the ability of a system to continue operation in the presence of a fault. In the event, the system should detect and recover full functionality. In any event, any actions taken should make every effort to preserve the single system image.

text: The primary methods for dealing with faults include fault avoidance,

text: fault tolerance

text: , and fault detection and recovery. Fault avoidance covers proactive measures taken to minimize the occurrence of faults. These proactive measures can be in the form of

text: transactions

text: replication

text: and

entity_section: Primary-backup and multi-primary replication

text: backups

text: . Fault tolerance is the ability of a system to continue operation in the presence of a fault. In the event, the system should detect and recover full functionality. In any event, any actions taken should make every effort to preserve the single system image.

answers: NDQ_003351

answers: Fault avoidance

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: faults

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: Fault avoidance

answers: NDQ_003357

answers: the system should detect and recover full functionality

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: faults

answers: NDQ_003362

answers: Fault avoidance covers proactive measures taken to minimize the occurrence of faults

answers: NDQ_003363

answers: faults

answers: NDQ_003371

answers: Fault avoidance

answers: NDQ_003373

answers: Fault avoidance

answers: NDQ_003376

answers: Fault avoidance

answers: NDQ_003378

answers: Fault avoidance

answers: NDQ_003379

answers: Fault tolerance

answers: NDQ_003380

answers: What does Fault avoidance cover?

answers: NDQ_003381

answers: What does Fault Tolerance cover?

answers: NDQ_003382

answers: Fault avoidance

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: Fault zone

answers: NDQ_003386

answers: Fault avoidance

answers: NDQ_003387

answers: What is the primary method for dealing with faults?

answers: NDQ_003388

answers: What is the primary method for dealing with faults?

answers: NDQ_003389

answers: Fault tolerance

answers: NDQ_003390

answers: Fault tolerance

answers: NDQ_003391

answers: Fault tolerance

answers: NDQ_003392

answers: Fault avoidance

answers: NDQ_003393

answers: fault tolerance

answers: NDQ_003394

answers: Fault tolerance

answers: NDQ_003395

answers: Fault tolerance

answers: NDQ_003396

answers: Fault tolerance

answers: NDQ_003351

answers: Fault avoidance

answers: NDQ_003352

answers: Fault avoidance

answers: NDQ_003353

answers: Fault avoidance

answers: NDQ_003354

answers: The primary methods for dealing with faults include fault avoidance,

answers: NDQ_003355

answers: The primary methods for dealing with faults include fault avoidance,

answers: NDQ_003356

answers: Fault avoidance

answers: NDQ_003357

answers: the system should detect and recover full functionality.

answers: NDQ_003358

answers: Fault tolerance

answers: NDQ_003359

answers: Fault avoidance

answers: NDQ_003360

answers: faults

answers: NDQ_003362

answers: The primary methods for dealing with faults include fault avoidance,

answers: NDQ_003363

answers: Fault avoidance

answers: NDQ_003371

answers: Fault tolerance

answers: NDQ_003373

answers: The primary methods for dealing with faults include fault avoidance,

answers: NDQ_003376

answers: Fault avoidance

answers: NDQ_003378

answers: Fault avoidance

answers: NDQ_003379

answers: Fault tolerance

answers: NDQ_003380

answers: Fault avoidance

answers: NDQ_003381

answers: Fault avoidance

answers: NDQ_003382

answers: Fault avoidance

answers: NDQ_003383

answers: Fault avoidance

answers: NDQ_003384

answers: The primary methods for dealing with faults include fault avoidance,

answers: NDQ_003385

answers: Fault tolerance

answers: NDQ_003386

answers: Fault avoidance

answers: NDQ_003387

answers: Fault tolerance

answers: NDQ_003388

answers: Fault avoidance

answers: NDQ_003389

answers: The primary methods for dealing with faults include fault avoidance,

answers: NDQ_003390

answers: Fault tolerance

answers: NDQ_003391

answers: Fault tolerance

answers: NDQ_003392

answers: fault tolerance, and fault detection and recovery.

answers: NDQ_003393

answers: Fault tolerance

answers: NDQ_003394

answers: faults.

answers: NDQ_003395

answers: fault.

answers: NDQ_003396

answers: fault tolerance, and fault detection and recovery.

text: The Frank-Read source is a mechanism based on dislocation multiplication in a slip plane under shear stress.

text: The Frank-Read source is a mechanism based on dislocation multiplication in a slip plane under

text: shear stress

answers: NDQ_003351

answers: shear

answers: NDQ_003352

answers: has more dislocations

answers: NDQ_003353

answers: dislocations

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: shear stress

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: dislocation multiplication is a mechanism based on what?

answers: NDQ_003358

answers: shear stress

answers: NDQ_003359

answers: is pushed against it

answers: NDQ_003360

answers: shear stress

answers: NDQ_003362

answers: The Frank-Read source is not a mechanism based on dislocation multiplication.

answers: NDQ_003363

answers: the Frank-Read source

answers: NDQ_003371

answers: Which of the following is not an example of a Frank-Read source?

answers: NDQ_003373

answers: no

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: Which of the following is not a type of stress?

answers: NDQ_003382

answers: None of the above choices.

answers: NDQ_003383

answers: None of the above choices.

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: no

answers: NDQ_003387

answers: Which of the following is not a type of shear stress?

answers: NDQ_003388

answers: What type of stress is shear stress?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: a slip plane

answers: NDQ_003391

answers: dislocation multiplication

answers: NDQ_003392

answers: dislocation multiplication

answers: NDQ_003393

answers: a Frank-Read source

answers: NDQ_003394

answers: a slip plane

answers: NDQ_003395

answers: a slip plane

answers: NDQ_003396

answers: frank-read

answers: NDQ_003351

answers: shear stress.

answers: NDQ_003352

answers: shear stress.

answers: NDQ_003353

answers: dislocation multiplication

answers: NDQ_003354

answers: The Frank-Read source

answers: NDQ_003355

answers: shear stress.

answers: NDQ_003356

answers: shear stress.

answers: NDQ_003357

answers: shear stress.

answers: NDQ_003358

answers: Frank-Read source

answers: NDQ_003359

answers: shear stress.

answers: NDQ_003360

answers: shear stress.

answers: NDQ_003362

answers: The Frank-Read source

answers: NDQ_003363

answers: shear stress.

answers: NDQ_003371

answers: The Frank-Read source

answers: NDQ_003373

answers: shear stress.

answers: NDQ_003376

answers: shear stress.

answers: NDQ_003378

answers: slip plane under shear stress.

answers: NDQ_003379

answers: slip plane under shear stress.

answers: NDQ_003380

answers: shear stress.

answers: NDQ_003381

answers: shear stress.

answers: NDQ_003382

answers: shear stress.

answers: NDQ_003383

answers: shear stress.

answers: NDQ_003384

answers: shear stress.

answers: NDQ_003385

answers: shear stress.

answers: NDQ_003386

answers: dislocation multiplication in a slip plane under shear stress.

answers: NDQ_003387

answers: shear stress.

answers: NDQ_003388

answers: shear stress.

answers: NDQ_003389

answers: shear stress.

answers: NDQ_003390

answers: shear stress.

answers: NDQ_003391

answers: shear stress.

answers: NDQ_003392

answers: Frank-Read source

answers: NDQ_003393

answers: shear stress.

answers: NDQ_003394

answers: slip plane

answers: NDQ_003395

answers: slip plane under shear stress.

answers: NDQ_003396

answers: slip plane under shear stress.

text: In addition to this, the way that an individual responds to stress can influence their health status. Often, individuals responding to chronic stress will develop coping behaviours, some of which have a positive influences on health and others which have a negative influence. People who cope with stress through positive behaviours such as exercise or social connections may not be as affected by the relationship between stress and health, whereas those with a coping style more prone to over consumption (i.e. emotional eating, drinking, smoking or drug use)  are more likely to be see negative health effects of stress. For example, a laboratory study has shown that, while stress did not alter calorie intake or food type eaten when averaged across the sample as a whole, when looking at a subset of the sample who were classed as emotional eaters, high stress levels were associated with eating more high fat and sweet food and a more calorie dense meal overall. Therefore, the authors conclude that stress may compromise the health of certain susceptible individuals (I.e those with an emotional eating coping style).

text: In addition to this, the way that an individual responds to stress can influence their health status. Often, individuals responding to chronic stress will develop coping behaviours, some of which have a positive influences on health and others which have a negative influence. People who cope with stress through positive behaviours such as exercise or social connections may not be as affected by the relationship between stress and health, whereas those with a coping style more prone to over consumption (i.e.

text: emotional eating

text: , drinking, smoking or drug use)  are more likely to be see negative health effects of stress. For example, a laboratory study has shown that, while stress did not alter calorie intake or food type eaten when averaged across the sample as a whole, when looking at a subset of the sample who were classed as emotional eaters, high stress levels were associated with eating more high fat and sweet food and a more calorie dense meal overall. Therefore, the authors conclude that stress may compromise the health of certain susceptible individuals (I.e those with an emotional eating coping style).

answers: NDQ_003351

answers: chronic stress

answers: NDQ_003352

answers: eats more sweet food

answers: NDQ_003353

answers: igneous rocks to form

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: swell

answers: NDQ_003357

answers: stress does not alter calorie intake or food type eaten when averaged across the sample

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: stress did not alter calorie intake or food type eaten

answers: NDQ_003363

answers: the same time

answers: NDQ_003371

answers: Which of the following is an example of a thrust fault?

answers: NDQ_003373

answers: how would you describe the stress?

answers: NDQ_003376

answers: basin-and-range

answers: NDQ_003378

answers: the amount the ground moves in an earthquake

answers: NDQ_003379

answers: strike-slip fault

answers: NDQ_003380

answers: What is the relationship between stress and health

answers: NDQ_003381

answers: How does stress affect rock?

answers: NDQ_003382

answers: what is the most common stress at convergent plates

answers: NDQ_003383

answers: no

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: earthquakes are caused by

answers: NDQ_003387

answers: Which of the following is not a cause of normal faults?

answers: NDQ_003388

answers: What is the relationship between stress and health?

answers: NDQ_003389

answers: mountain ranges

answers: NDQ_003390

answers: a fault

answers: NDQ_003391

answers: dip-slip fault

answers: NDQ_003392

answers: The hanging wall pushes up

answers: NDQ_003393

answers: dip-slip fault

answers: NDQ_003394

answers: is a

answers: NDQ_003395

answers: a vertical fault plane

answers: NDQ_003396

answers: NDQ_003351

answers: chronic stress

answers: NDQ_003352

answers: eating more high fat and sweet food

answers: NDQ_003353

answers: coping behaviours,

answers: NDQ_003354

answers: way that an individual responds to stress can influence their health status.

answers: NDQ_003355

answers: coping behaviours,

answers: NDQ_003356

answers: eating more high fat and sweet food

answers: NDQ_003357

answers: emotional eating, drinking, smoking or drug use)

answers: NDQ_003358

answers: Often, individuals responding to chronic stress

answers: NDQ_003359

answers: stress

answers: NDQ_003360

answers: stress

answers: NDQ_003362

answers: Often, individuals responding to chronic stress will develop coping behaviours,

answers: NDQ_003363

answers: stress can influence their health status. Often, individuals responding to chronic stress

answers: NDQ_003371

answers: way that an individual responds to stress can influence their health status.

answers: NDQ_003373

answers: stress can influence their health status. Often, individuals responding to chronic stress

answers: NDQ_003376

answers: stress

answers: NDQ_003378

answers: exercise or social connections

answers: NDQ_003379

answers: exercise or social connections

answers: NDQ_003380

answers: stress

answers: NDQ_003381

answers: chronic stress

answers: NDQ_003382

answers: chronic stress

answers: NDQ_003383

answers: stress

answers: NDQ_003384

answers: way that an individual responds to stress can influence their health status.

answers: NDQ_003385

answers: social connections

answers: NDQ_003386

answers: exercise or social connections

answers: NDQ_003387

answers: chronic stress

answers: NDQ_003388

answers: stress

answers: NDQ_003389

answers: Often, individuals responding to chronic stress will develop coping behaviours,

answers: NDQ_003390

answers: Often, individuals responding to chronic stress will develop coping behaviours,

answers: NDQ_003391

answers: stress

answers: NDQ_003392

answers: Often, individuals responding to chronic stress will develop coping behaviours,

answers: NDQ_003393

answers: Often, individuals responding to chronic stress

answers: NDQ_003394

answers: People who cope with stress through positive behaviours such as exercise or social connections

answers: NDQ_003395

answers: Often, individuals responding to chronic stress will develop coping behaviours,

answers: NDQ_003396

answers: stress

text: The presence of second phase particles often causes lattice distortions. These lattice distortions result when the precipitate particles  differ in size and crystallographic structure from the host atoms. Smaller precipitate particles in a host lattice leads to a tensile stress, whereas larger precipitate particles leads to a compressive stress. Dislocation defects also create a stress field. Above the dislocation there is a compressive stress and below there is a tensile stress. Consequently, there is a negative interaction energy between a dislocation and a precipitate that each respectively cause a compressive and a tensile stress or vice versa. In other words, the dislocation will be attracted to the precipitate. In addition, there is a positive interaction energy between a dislocation and a precipitate that  have the same type of stress field. This means that the dislocation will be repulsed by the precipitate.

text: The presence of second phase particles often causes lattice distortions. These lattice distortions result when the precipitate particles  differ in size and crystallographic structure from the host atoms. Smaller precipitate particles in a host lattice leads to a tensile stress, whereas larger precipitate particles leads to a compressive stress. Dislocation defects also create a stress field. Above the dislocation there is a compressive stress and below there is a tensile stress. Consequently, there is a negative interaction energy between a dislocation and a precipitate that each respectively cause a compressive and a tensile stress or vice versa. In other words, the dislocation will be attracted to the precipitate. In addition, there is a positive interaction energy between a dislocation and a precipitate that  have the same type of stress field. This means that the dislocation will be repulsed by the precipitate.

answers: NDQ_003351

answers: compressive stress

answers: NDQ_003352

answers: compresses

answers: NDQ_003353

answers: lattice distortion

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: compress

answers: NDQ_003357

answers: tensile stress

answers: NDQ_003358

answers: compressive stress

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: fault lines

answers: NDQ_003362

answers: the dislocation will be attracted to the precipitate

answers: NDQ_003363

answers: lattice distortions

answers: NDQ_003371

answers: Which of the following is not a type of stress field?

answers: NDQ_003373

answers: larger precipitate particles

answers: NDQ_003376

answers: larger precipitate particles

answers: NDQ_003378

answers: the amount the ground moves in an earthquake

answers: NDQ_003379

answers: vertical

answers: NDQ_003380

answers: compressive stress

answers: NDQ_003381

answers: compressive stress

answers: NDQ_003382

answers: larger precipitate particles

answers: NDQ_003383

answers: compressive

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: Fault zone

answers: NDQ_003386

answers: movement of rock at faults

answers: NDQ_003387

answers: Which of the following is not caused by compression stress?

answers: NDQ_003388

answers: Which of the following is not a type of stress?

answers: NDQ_003389

answers: mountain ranges

answers: NDQ_003390

answers: tensile

answers: NDQ_003391

answers: compressive stress

answers: NDQ_003392

answers: tensile

answers: NDQ_003393

answers: compressive stress

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: a vertical fault plane

answers: NDQ_003396

answers: horizontal

answers: NDQ_003351

answers: tensile

answers: NDQ_003352

answers: tensile stress,

answers: NDQ_003353

answers: lattice distortions.

answers: NDQ_003354

answers: the dislocation will be attracted to the precipitate.

answers: NDQ_003355

answers: tensile

answers: NDQ_003356

answers: tensile stress,

answers: NDQ_003357

answers: the dislocation will be attracted to the precipitate.

answers: NDQ_003358

answers: dislocation

answers: NDQ_003359

answers: second phase particles often causes lattice distortions.

answers: NDQ_003360

answers: second phase particles

answers: NDQ_003362

answers: the dislocation will be attracted to the precipitate.

answers: NDQ_003363

answers: second phase particles often causes lattice distortions.

answers: NDQ_003371

answers: The presence of second phase particles often causes lattice distortions.

answers: NDQ_003373

answers: larger precipitate particles

answers: NDQ_003376

answers: larger precipitate particles

answers: NDQ_003378

answers: the dislocation will be attracted to the precipitate.

answers: NDQ_003379

answers: tensile stress.

answers: NDQ_003380

answers: tensile stress,

answers: NDQ_003381

answers: tensile stress,

answers: NDQ_003382

answers: larger precipitate particles leads to a compressive stress.

answers: NDQ_003383

answers: Dislocation defects also create a stress field.

answers: NDQ_003384

answers: the dislocation will be attracted to the precipitate.

answers: NDQ_003385

answers: lattice distortions.

answers: NDQ_003386

answers: lattice distortions.

answers: NDQ_003387

answers: larger precipitate particles

answers: NDQ_003388

answers: tensile stress,

answers: NDQ_003389

answers: Dislocation defects also create a stress field.

answers: NDQ_003390

answers: Dislocation defects

answers: NDQ_003391

answers: tensile stress.

answers: NDQ_003392

answers: Dislocation defects

answers: NDQ_003393

answers: compressive stress

answers: NDQ_003394

answers: lattice distortions.

answers: NDQ_003395

answers: tensile stress,

answers: NDQ_003396

answers: tensile stress,

text: Environments of magma formation and compositions are commonly correlated. Environments include subduction zones, continental rift zones, mid-ocean ridges and hotspots. Despite being found in such widespread locales, the bulk of the Earth's crust and mantle is not molten. Except for the liquid outer core, most of the Earth takes the form of a rheid, a form of solid that can move or deform under pressure. Magma, as liquid, preferentially forms in high temperature, low pressure environments within several kilometers of the Earth's surface.

text: Environments of magma formation and compositions are commonly correlated. Environments include

text: subduction zone

text: s, continental

text: rift zone

text: s,

text: mid-ocean ridge

text: s and

text: hotspots

text: . Despite being found in such widespread locales, the bulk of the

text: Earth's crust

text: and

text: mantle

text: is not molten. Except for the liquid

text: outer core

text: , most of the Earth takes the form of a

text: rheid

text: , a form of solid that can move or deform under pressure. Magma, as liquid, preferentially forms in high temperature, low pressure environments within several kilometers of the Earth's surface.

answers: NDQ_003351

answers: subduction

answers: NDQ_003352

answers: deforms

answers: NDQ_003353

answers: deformation

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: continental rift zone

answers: NDQ_003356

answers: move

answers: NDQ_003357

answers: the bulk of the Earth's crust and mantle is not molten

answers: NDQ_003358

answers: subduction zone

answers: NDQ_003359

answers: under pressure

answers: NDQ_003360

answers: continental rift zones

answers: NDQ_003362

answers: the bulk of the Earth's crust and mantle is not molten

answers: NDQ_003363

answers: subduction zones

answers: NDQ_003371

answers: Which of the following is not an environment of magma formation: subduction zones, continental rift zones, mid-ocean ridges and hotspots?

answers: NDQ_003373

answers: How would you describe a rheid?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What is a form of solid that can move or deform under pressure?

answers: NDQ_003381

answers: Which of the following is not a form of solid that can move or deform under pressure?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What type of solid can move or deform under pressure?

answers: NDQ_003384

answers: Which of the following is not an environment of magma formation and compositions?

answers: NDQ_003385

answers: subduction zones

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: Which of the following is not a form of solid that can move or deform under pressure?

answers: NDQ_003388

answers: Which of the following is not a form of solid that can move or deform under pressure: strike-slip faults, mid-ocean ridges or hotspots?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: subduction zones

answers: NDQ_003391

answers: subduction zones

answers: NDQ_003392

answers: continental rift zones

answers: NDQ_003393

answers: subduction zones

answers: NDQ_003394

answers: continental rift zones

answers: NDQ_003395

answers: continental rift zones

answers: NDQ_003396

answers: continental rift zones

answers: NDQ_003351

answers: subduction zones, continental rift zones,

answers: NDQ_003352

answers: deform

answers: NDQ_003353

answers: deform

answers: NDQ_003354

answers: Environments of magma formation and compositions are commonly correlated.

answers: NDQ_003355

answers: subduction zones,

answers: NDQ_003356

answers: rheid,

answers: NDQ_003357

answers: molten.

answers: NDQ_003358

answers: rheid,

answers: NDQ_003359

answers: pressure.

answers: NDQ_003360

answers: subduction zones,

answers: NDQ_003362

answers: molten.

answers: NDQ_003363

answers: subduction zones,

answers: NDQ_003371

answers: subduction zones, continental rift zones,

answers: NDQ_003373

answers: rheid,

answers: NDQ_003376

answers: mid-ocean ridges and hotspots.

answers: NDQ_003378

answers: rheid,

answers: NDQ_003379

answers: subduction zones, continental rift zones,

answers: NDQ_003380

answers: pressure.

answers: NDQ_003381

answers: rheid,

answers: NDQ_003382

answers: pressure.

answers: NDQ_003383

answers: pressure.

answers: NDQ_003384

answers: mid-ocean ridges

answers: NDQ_003385

answers: continental rift zones,

answers: NDQ_003386

answers: rheid,

answers: NDQ_003387

answers: rheid,

answers: NDQ_003388

answers: subduction zones, continental rift zones,

answers: NDQ_003389

answers: mid-ocean ridges

answers: NDQ_003390

answers: subduction zones,

answers: NDQ_003391

answers: subduction zones,

answers: NDQ_003392

answers: subduction zones, continental rift zones,

answers: NDQ_003393

answers: subduction zones,

answers: NDQ_003394

answers: subduction zones, continental rift zones,

answers: NDQ_003395

answers: subduction zones, continental rift zones,

answers: NDQ_003396

answers: subduction zones, continental rift zones,

text: Another theory for the causes of the deep and extremely rapid exhumation of the Petermann Orogen is that it is due to isostatic instabilities caused by thermal events in the deep crust, causing accumulated stress to be released by violent thermal rebound (Sandiford, et al. 2001). This is envisaged as a kind of feedback loop between sedimentation and isostatic orogenic events. However, some authors (Camacho et al.) have called this into question with isotopic models.

text: Another theory for the causes of the deep and extremely rapid exhumation of the Petermann Orogen is that it is due to isostatic instabilities caused by thermal events in the deep crust, causing accumulated stress to be released by violent thermal rebound (Sandiford, et al. 2001). This is envisaged as a kind of feedback loop between sedimentation and

text: isostatic

text: orogenic events. However, some authors (Camacho et al.) have called this into question with

text: isotopic

text: models.

answers: NDQ_003351

answers: isostatic

answers: NDQ_003352

answers: releases more energy

answers: NDQ_003353

answers: thermal rebound

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: rebound

answers: NDQ_003357

answers: accumulated stress to be released by violent thermal rebound

answers: NDQ_003358

answers: isostatic

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: thermal rebound

answers: NDQ_003362

answers: accumulated stress to be released by violent thermal rebound

answers: NDQ_003363

answers: Petermann Orogen

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: no

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: vertical

answers: NDQ_003380

answers: What is a stress?

answers: NDQ_003381

answers: unanswerable

answers: NDQ_003382

answers: not enough information

answers: NDQ_003383

answers: no

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: Fault zone

answers: NDQ_003386

answers: accumulated stress

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: unanswerable

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: Petermann Orogen

answers: NDQ_003392

answers: isostatic

answers: NDQ_003393

answers: Petermann Orogen

answers: NDQ_003394

answers: undefined

answers: NDQ_003395

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: thermal rebound

answers: NDQ_003352

answers: accumulated stress to be released by violent thermal rebound

answers: NDQ_003353

answers: accumulated stress to be released by violent thermal rebound

answers: NDQ_003354

answers: Another theory for the causes of the deep and extremely rapid exhumation

answers: NDQ_003355

answers: thermal rebound

answers: NDQ_003356

answers: accumulated stress to be released by violent thermal rebound

answers: NDQ_003357

answers: accumulated stress to be released by violent thermal rebound

answers: NDQ_003358

answers: isostatic

answers: NDQ_003359

answers: accumulated stress to be released by violent thermal rebound

answers: NDQ_003360

answers: thermal events

answers: NDQ_003362

answers: violent thermal rebound

answers: NDQ_003363

answers: Petermann Orogen

answers: NDQ_003371

answers: isostatic instabilities

answers: NDQ_003373

answers: accumulated stress

answers: NDQ_003376

answers: thermal events

answers: NDQ_003378

answers: accumulated stress to be released by violent thermal rebound

answers: NDQ_003379

answers: thermal rebound

answers: NDQ_003380

answers: stress

answers: NDQ_003381

answers: accumulated stress to be released by violent thermal rebound

answers: NDQ_003382

answers: accumulated stress to be released by violent thermal rebound

answers: NDQ_003383

answers: stress

answers: NDQ_003384

answers: thermal rebound

answers: NDQ_003385

answers: Petermann Orogen

answers: NDQ_003386

answers: isostatic instabilities

answers: NDQ_003387

answers: thermal events

answers: NDQ_003388

answers: thermal events

answers: NDQ_003389

answers: thermal events in the deep crust,

answers: NDQ_003390

answers: Petermann Orogen

answers: NDQ_003391

answers: Petermann Orogen

answers: NDQ_003392

answers: Petermann Orogen

answers: NDQ_003393

answers: Petermann Orogen

answers: NDQ_003394

answers: isotopic models.

answers: NDQ_003395

answers: Petermann Orogen

answers: NDQ_003396

answers: Petermann Orogen

text: All three sections of the system were formed around the same time—about 2 billion years ago—and are remarkably similar. Vast quantities of molten rock from Earth's mantle were brought to the surface through long vertical cracks in Earth's crust—huge arcuate differentiated lopolithic intrusions—creating the geological intrusion known as the Bushveld Igneous Complex.

text: All three sections of the system were formed around the same time—about 2 billion years ago—and are remarkably similar. Vast quantities of molten rock from Earth's

text: mantle

text: were brought to the surface through long vertical cracks in Earth's crust—huge arcuate differentiated

text: lopolith

text: ic intrusions—creating the geological intrusion known as the Bushveld Igneous Complex.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: cracks

answers: NDQ_003353

answers: cracks

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: arcuate

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: vertical cracks in Earth's crust

answers: NDQ_003358

answers: crack

answers: NDQ_003359

answers: molten rock is brought to the surface

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: all three sections of the system were formed around the same time

answers: NDQ_003363

answers: 2 billion years ago

answers: NDQ_003371

answers: What is the Bushveld Igneous Complex?

answers: NDQ_003373

answers: Why is the Bushveld Igneous Complex unique?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: vertical cracks

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What does the Bushveld Igneous Complex contain?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: what is the first type of intrusion mentioned?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: Which of the following is not a type of normal fault?

answers: NDQ_003388

answers: Which of the following is not a type of strike-slip fault?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: vertical cracks

answers: NDQ_003391

answers: lopolithic intrusions

answers: NDQ_003392

answers: vertical cracks

answers: NDQ_003393

answers: vertical cracks

answers: NDQ_003394

answers: arcuate

answers: NDQ_003395

answers: long vertical cracks

answers: NDQ_003396

answers: arcuate

answers: NDQ_003351

answers: arcuate differentiated lopolithic intrusions—creating

answers: NDQ_003352

answers: cracks

answers: NDQ_003353

answers: cracks

answers: NDQ_003354

answers: Bushveld Igneous Complex.

answers: NDQ_003355

answers: vertical cracks in Earth's crust—huge arcuate

answers: NDQ_003356

answers: molten rock

answers: NDQ_003357

answers: vertical cracks

answers: NDQ_003358

answers: lopolithic intrusions—creating

answers: NDQ_003359

answers: molten

answers: NDQ_003360

answers: molten rock from Earth's mantle

answers: NDQ_003362

answers: 2 billion years ago—and

answers: NDQ_003363

answers: time—about 2 billion years ago—and

answers: NDQ_003371

answers: Bushveld Igneous Complex.

answers: NDQ_003373

answers: long vertical cracks

answers: NDQ_003376

answers: long vertical cracks

answers: NDQ_003378

answers: vertical cracks

answers: NDQ_003379

answers: vertical cracks

answers: NDQ_003380

answers: molten rock

answers: NDQ_003381

answers: long vertical cracks

answers: NDQ_003382

answers: 2 billion years ago—and are remarkably similar.

answers: NDQ_003383

answers: long vertical cracks

answers: NDQ_003384

answers: vertical cracks

answers: NDQ_003385

answers: Bushveld Igneous Complex.

answers: NDQ_003386

answers: long vertical cracks

answers: NDQ_003387

answers: long vertical cracks

answers: NDQ_003388

answers: Bushveld Igneous Complex.

answers: NDQ_003389

answers: long vertical cracks

answers: NDQ_003390

answers: Bushveld Igneous Complex.

answers: NDQ_003391

answers: Bushveld Igneous Complex.

answers: NDQ_003392

answers: Bushveld Igneous Complex.

answers: NDQ_003393

answers: Bushveld Igneous Complex.

answers: NDQ_003394

answers: vertical cracks

answers: NDQ_003395

answers: vertical cracks

answers: NDQ_003396

answers: vertical

text: The fault was first identified in Northern California by UC Berkeley geology professor Andrew Lawson in 1895 and named by him after the Laguna de San Andreas, a small lake which lies in a linear valley formed by the fault just south of San Francisco. Eleven years later, Lawson discovered that the San Andreas Fault stretched southward into southern California after reviewing the effects of the 1906 San Francisco earthquake. Large-scale (hundreds of miles) lateral movement along the fault was first proposed in a 1953 paper by geologists Mason Hill and Thomas Dibblee. This idea, which was considered radical at the time, has since been vindicated by modern plate tectonics.

text: The fault was first identified in Northern California by UC Berkeley geology professor

text: Andrew Lawson

text: in 1895 and named by him after the

text: Laguna de San Andreas

text: , a small lake which lies in a linear valley formed by the fault just south of San Francisco. Eleven years later, Lawson discovered that the San Andreas Fault stretched southward into southern California after reviewing the effects of the

text: 1906 San Francisco earthquake

text: . Large-scale (hundreds of miles) lateral movement along the fault was first proposed in a 1953 paper by geologists Mason Hill and

text: Thomas Dibblee

text: . This idea, which was considered radical at the time, has since been vindicated by modern

text: plate tectonics

answers: NDQ_003351

answers: lateral movement

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: lateral movement

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fault

answers: NDQ_003356

answers: lateral movement

answers: NDQ_003357

answers: Large-scale (hundreds of miles)

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: plate tectonics

answers: NDQ_003362

answers: the San Andreas Fault stretched southward into southern California after reviewing the effects of the 1906 San Francisco earthquake

answers: NDQ_003363

answers: San Andreas Fault

answers: NDQ_003371

answers: What is the San Andreas Fault?

answers: NDQ_003373

answers: How would you describe the effects of the 1906 San Francisco earthquake?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: lateral movement

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What is a stress?

answers: NDQ_003381

answers: What does the San Andreas Fault do?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What type of fold is the San Andreas Fault?

answers: NDQ_003385

answers: Fault zone

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: What is the cause of the San Andreas Fault?

answers: NDQ_003388

answers: What type of fault is the San Andreas Fault?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: San Andreas Fault

answers: NDQ_003391

answers: a linear valley

answers: NDQ_003392

answers: San Andreas Fault

answers: NDQ_003393

answers: linear valley

answers: NDQ_003394

answers: San Andreas Fault

answers: NDQ_003395

answers: San Andreas Fault

answers: NDQ_003396

answers: San Andreas Fault

answers: NDQ_003351

answers: lateral movement

answers: NDQ_003352

answers: lateral movement

answers: NDQ_003353

answers: lateral movement

answers: NDQ_003354

answers: San Andreas Fault

answers: NDQ_003355

answers: linear valley

answers: NDQ_003356

answers: lateral movement

answers: NDQ_003357

answers: lateral movement

answers: NDQ_003358

answers: The fault

answers: NDQ_003359

answers: fault

answers: NDQ_003360

answers: plate tectonics.

answers: NDQ_003362

answers: the San Andreas Fault stretched southward into southern California

answers: NDQ_003363

answers: San Andreas Fault

answers: NDQ_003371

answers: 1895

answers: NDQ_003373

answers: 1895

answers: NDQ_003376

answers: linear valley

answers: NDQ_003378

answers: lateral movement

answers: NDQ_003379

answers: 1895

answers: NDQ_003380

answers: 1906 San Francisco earthquake.

answers: NDQ_003381

answers: lateral movement

answers: NDQ_003382

answers: 1895

answers: NDQ_003383

answers: lateral movement

answers: NDQ_003384

answers: linear valley

answers: NDQ_003385

answers: Laguna de San Andreas,

answers: NDQ_003386

answers: lateral movement

answers: NDQ_003387

answers: modern plate tectonics.

answers: NDQ_003388

answers: modern plate tectonics.

answers: NDQ_003389

answers: plate tectonics.

answers: NDQ_003390

answers: San Andreas Fault

answers: NDQ_003391

answers: Laguna de San Andreas,

answers: NDQ_003392

answers: San Andreas Fault

answers: NDQ_003393

answers: Laguna de San Andreas,

answers: NDQ_003394

answers: San Andreas Fault

answers: NDQ_003395

answers: San Andreas Fault

answers: NDQ_003396

answers: San Andreas Fault

text: Geophysicists and exploration geologists who look for oil and gas fields classify the subsurface characteristics, or tectonic setting, of geological structures that contain hydrocarbons. Any one oil and gas field may reflect influences from multiple geological periods and events, but geoscientists often attempt to characterize a field based on the dominant geological event that influenced the structure's ability to trap and contain oil and gas in recoverable quantities.

text: Geophysicists

text: and exploration

text: geologists

text: who look for oil and gas fields classify the subsurface characteristics, or tectonic setting, of geological structures that contain hydrocarbons. Any one oil and gas field may reflect influences from multiple geological periods and events, but geoscientists often attempt to characterize a field based on the dominant geological event that influenced the structure's ability to trap and contain oil and gas in recoverable quantities.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: more likely to crack

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: tectonic

answers: NDQ_003356

answers: contain hydrocarbons

answers: NDQ_003357

answers: oil and gas in recoverable quantities

answers: NDQ_003358

answers: unanswerable

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: tectonic plates

answers: NDQ_003362

answers: oil and gas fields may reflect influences from multiple geological periods and events

answers: NDQ_003363

answers: tectonic setting

answers: NDQ_003371

answers: What is a thrust fault?

answers: NDQ_003373

answers: How would you describe the subsurface characteristics of a rock?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: strike-slip fault

answers: NDQ_003380

answers: Which of the following is not a stress?

answers: NDQ_003381

answers: What is the term for a rock that deforms?

answers: NDQ_003382

answers: None of the above choices.

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: None of the above choices.

answers: NDQ_003387

answers: None of the above choices.

answers: NDQ_003388

answers: Which of the following is not a type of strike-slip fault?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: tectonic setting

answers: NDQ_003391

answers: oil and gas field

answers: NDQ_003392

answers: tectonic setting

answers: NDQ_003393

answers: tectonic setting

answers: NDQ_003394

answers: tectonic

answers: NDQ_003395

answers: tectonic setting

answers: NDQ_003396

answers: tectonic

answers: NDQ_003351

answers: dominant geological event

answers: NDQ_003352

answers: ability to trap and contain oil and gas in recoverable quantities.

answers: NDQ_003353

answers: tectonic

answers: NDQ_003354

answers: Geophysicists

answers: NDQ_003355

answers: tectonic

answers: NDQ_003356

answers: trap and contain oil and gas in recoverable quantities.

answers: NDQ_003357

answers: oil and gas in recoverable quantities.

answers: NDQ_003358

answers: tectonic setting,

answers: NDQ_003359

answers: tectonic

answers: NDQ_003360

answers: tectonic

answers: NDQ_003362

answers: hydrocarbons.

answers: NDQ_003363

answers: tectonic

answers: NDQ_003371

answers: tectonic setting, of geological structures that contain hydrocarbons.

answers: NDQ_003373

answers: tectonic setting, of geological structures that contain hydrocarbons.

answers: NDQ_003376

answers: tectonic setting, of geological structures that contain hydrocarbons.

answers: NDQ_003378

answers: tectonic setting, of geological structures that contain hydrocarbons.

answers: NDQ_003379

answers: Geophysicists

answers: NDQ_003380

answers: geological structures that contain hydrocarbons.

answers: NDQ_003381

answers: tectonic setting, of geological structures that contain hydrocarbons.

answers: NDQ_003382

answers: dominant geological event

answers: NDQ_003383

answers: tectonic setting, of geological structures that contain hydrocarbons.

answers: NDQ_003384

answers: tectonic setting, of geological structures that contain hydrocarbons.

answers: NDQ_003385

answers: tectonic setting, of geological structures that contain hydrocarbons.

answers: NDQ_003386

answers: tectonic

answers: NDQ_003387

answers: geoscientists

answers: NDQ_003388

answers: tectonic setting, of geological structures that contain hydrocarbons.

answers: NDQ_003389

answers: tectonic

answers: NDQ_003390

answers: tectonic

answers: NDQ_003391

answers: oil and gas fields classify the subsurface

answers: NDQ_003392

answers: tectonic

answers: NDQ_003393

answers: tectonic setting, of geological structures that contain hydrocarbons.

answers: NDQ_003394

answers: tectonic setting, of geological structures that contain hydrocarbons.

answers: NDQ_003395

answers: tectonic setting, of geological structures that contain hydrocarbons.

answers: NDQ_003396

answers: tectonic setting, of geological structures that contain hydrocarbons.

text: The Saharan Metacraton is a term used by some geologists to describe a large area of continental crust in the north-central part of Africa. Whereas a craton is an old and stable part of the lithosphere, the term "metacraton" is used to describe a craton that has been remobilized during an orogenic event, but where the characteristics of the original craton are still identifiable. The geology of the continent has only been partially explored, and other names have been used to describe the general area that reflect different views of its nature and extent. These include "Nile Craton", "Sahara Congo Craton", "Eastern Saharan Craton" and "Central Saharan Ghost Craton".This last term is because the older rocks are almost completely covered by recent sediments and desert sands, making geological analysis difficult.

text: The Saharan Metacraton is a term used by some geologists to describe a large area of

text: continental crust

text: in the north-central part of

text: Africa

text: . Whereas a

text: craton

text: is an old and stable part of the

text: lithosphere

text: , the term "metacraton" is used to describe a craton that has been remobilized during an

text: orogenic event

text: , but where the characteristics of the original craton are still identifiable. The geology of the continent has only been partially explored, and other names have been used to describe the general area that reflect different views of its nature and extent. These include "Nile Craton", "Sahara Congo Craton", "Eastern Saharan Craton" and "Central Saharan Ghost Craton".This last term is because the older rocks are almost completely covered by recent sediments and desert sands, making geological analysis difficult.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: igneous rocks to change

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: craton

answers: NDQ_003356

answers: remobilize

answers: NDQ_003357

answers: a craton is an old and stable part of the lithosphere

answers: NDQ_003358

answers: Craton

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: orogenic events

answers: NDQ_003362

answers: the older rocks are almost completely covered by recent sediments and desert sands, making geological analysis difficult.

answers: NDQ_003363

answers: orogenic event

answers: NDQ_003371

answers: What is the term used to describe a large area of continental crust in the north-central part of Africa?

answers: NDQ_003373

answers: Why is it difficult to analyze geological analysis?

answers: NDQ_003376

answers: basin-and-range is caused by compressive forces

answers: NDQ_003378

answers: What is the last term used to describe the general area that reflect different views of its nature and extent?

answers: NDQ_003379

answers: The Saharan Metacraton

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What type of stress does the Saharan Metacraton experience?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What is a term used by some geologists to describe a large area of continental crust?

answers: NDQ_003385

answers: what is the last term used to describe the general area that reflect different views of its nature

answers: NDQ_003386

answers: orogenic event

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: normal faults, orogenic events?

answers: NDQ_003388

answers: what is the last term used to describe the general area that reflect different views of its nature and extent?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: craton

answers: NDQ_003391

answers: craton

answers: NDQ_003392

answers: craton

answers: NDQ_003393

answers: craton

answers: NDQ_003394

answers: metacraton

answers: NDQ_003395

answers: The Saharan Ghost Craton

answers: NDQ_003396

answers: Metacraton

answers: NDQ_003351

answers: orogenic event,

answers: NDQ_003352

answers: remobilized

answers: NDQ_003353

answers: orogenic event,

answers: NDQ_003354

answers: The Saharan Metacraton

answers: NDQ_003355

answers: a craton

answers: NDQ_003356

answers: remobilized during an orogenic event,

answers: NDQ_003357

answers: craton

answers: NDQ_003358

answers: craton

answers: NDQ_003359

answers: orogenic event,

answers: NDQ_003360

answers: orogenic event,

answers: NDQ_003362

answers: old and stable

answers: NDQ_003363

answers: orogenic event,

answers: NDQ_003371

answers: The Saharan Metacraton

answers: NDQ_003373

answers: The Saharan Metacraton

answers: NDQ_003376

answers: The Saharan Metacraton

answers: NDQ_003378

answers: The Saharan Metacraton

answers: NDQ_003379

answers: The Saharan Metacraton

answers: NDQ_003380

answers: orogenic event,

answers: NDQ_003381

answers: The Saharan Metacraton

answers: NDQ_003382

answers: The Saharan Metacraton

answers: NDQ_003383

answers: orogenic event,

answers: NDQ_003384

answers: The Saharan Metacraton

answers: NDQ_003385

answers: "metacraton"

answers: NDQ_003386

answers: orogenic event,

answers: NDQ_003387

answers: The Saharan Metacraton

answers: NDQ_003388

answers: The Saharan Metacraton

answers: NDQ_003389

answers: orogenic event,

answers: NDQ_003390

answers: The Saharan Metacraton

answers: NDQ_003391

answers: craton

answers: NDQ_003392

answers: The Saharan Metacraton

answers: NDQ_003393

answers: craton

answers: NDQ_003394

answers: The Saharan Metacraton

answers: NDQ_003395

answers: The Saharan Metacraton

answers: NDQ_003396

answers: The Saharan Metacraton

text: The Dictionary of Occupational Titles lists the following occupations in Geology, which it describes as "concerned with the investigation of the composition, structure, and physical and biological history of the earth's crust and the application of this knowledge in such fields as archeology, mining, construction, and environmental impact":

text: The

text: Dictionary of Occupational Titles

text: lists the following occupations in Geology, which it describes as "concerned with the investigation of the composition, structure, and physical and biological history of the earth's

text: crust

text: and the application of this knowledge in such fields as

text: archeology

text: mining

text: construction

text: , and

text: environmental impact

answers: NDQ_003351

answers: lateral

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: Earth's crust consists of igneous rocks

answers: NDQ_003358

answers: rockfall

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: fault lines

answers: NDQ_003362

answers: the San Andreas fault is a fault in the ocean

answers: NDQ_003363

answers: geological time

answers: NDQ_003371

answers: geologist

answers: NDQ_003373

answers: Geology

answers: NDQ_003376

answers: Geology

answers: NDQ_003378

answers: Geology

answers: NDQ_003379

answers: Geology

answers: NDQ_003380

answers: What is a stress?

answers: NDQ_003381

answers: Geologist

answers: NDQ_003382

answers: Geology

answers: NDQ_003383

answers: Geology

answers: NDQ_003384

answers: syncline

answers: NDQ_003385

answers: Fault zone

answers: NDQ_003386

answers: Geology

answers: NDQ_003387

answers: Geology

answers: NDQ_003388

answers: Geology

answers: NDQ_003389

answers: Geology

answers: NDQ_003390

answers: Geology

answers: NDQ_003391

answers: igneous

answers: NDQ_003392

answers: geologist

answers: NDQ_003393

answers: igneous rock

answers: NDQ_003394

answers: NDQ_003395

answers: NDQ_003396

answers: NDQ_003351

answers: Geology,

answers: NDQ_003352

answers: structure,

answers: NDQ_003353

answers: composition, structure,

answers: NDQ_003354

answers: The Dictionary of Occupational Titles lists the following occupations in Geology,

answers: NDQ_003355

answers: The Dictionary of Occupational Titles lists the following occupations in Geology,

answers: NDQ_003356

answers: physical and biological history

answers: NDQ_003357

answers: physical and biological history

answers: NDQ_003358

answers: archeology,

answers: NDQ_003359

answers: The Dictionary of Occupational Titles lists the following occupations in Geology,

answers: NDQ_003360

answers: earth's crust

answers: NDQ_003362

answers: The Dictionary of Occupational Titles

answers: NDQ_003363

answers: earth's crust

answers: NDQ_003371

answers: Geology,

answers: NDQ_003373

answers: The Dictionary of Occupational Titles lists the following occupations in Geology,

answers: NDQ_003376

answers: The Dictionary of Occupational Titles lists the following occupations in Geology,

answers: NDQ_003378

answers: The Dictionary of Occupational Titles lists the following occupations in Geology,

answers: NDQ_003379

answers: The Dictionary of Occupational Titles lists the following occupations in Geology,

answers: NDQ_003380

answers: The Dictionary of Occupational Titles lists the following occupations in Geology,

answers: NDQ_003381

answers: Geology,

answers: NDQ_003382

answers: The Dictionary of Occupational Titles lists the following occupations in Geology,

answers: NDQ_003383

answers: The Dictionary of Occupational Titles lists the following occupations in Geology,

answers: NDQ_003384

answers: The Dictionary of Occupational Titles lists the following occupations in Geology,

answers: NDQ_003385

answers: The Dictionary of Occupational Titles lists the following occupations in Geology,

answers: NDQ_003386

answers: Geology,

answers: NDQ_003387

answers: The Dictionary of Occupational Titles lists the following occupations in Geology,

answers: NDQ_003388

answers: The Dictionary of Occupational Titles lists the following occupations in Geology,

answers: NDQ_003389

answers: The Dictionary of Occupational Titles lists the following occupations in Geology,

answers: NDQ_003390

answers: The Dictionary of Occupational Titles lists the following occupations in Geology,

answers: NDQ_003391

answers: Geology,

answers: NDQ_003392

answers: The Dictionary of Occupational Titles lists the following occupations in Geology,

answers: NDQ_003393

answers: mining, construction, and environmental impact":

answers: NDQ_003394

answers: The Dictionary of Occupational Titles lists the following occupations in Geology,

answers: NDQ_003395

answers: The Dictionary of Occupational Titles lists the following occupations in Geology,

answers: NDQ_003396

answers: The Dictionary of Occupational Titles lists the following occupations in Geology,

text: The Apennine orogeny is a type of mountain-building in which two simpler types are combined in an apparently paradoxical configuration. Sometimes this is referred to as "syn-orogenic extension", but the term implies that the two processes occur simultaneously during time. Some scientists imagine that this is relatively rare but not unique in mountain building, whereas others imagine that this is fairly common in all mountain belts.

text: The Apennine orogeny is a type of mountain-building in which two simpler types are combined in an apparently paradoxical configuration. Sometimes this is referred to as "syn-orogenic extension", but the term implies that the two processes occur simultaneously during time. Some scientists imagine that this is relatively rare but not unique in mountain building, whereas others imagine that this is fairly common in all mountain belts.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: mountain-building

answers: NDQ_003356

answers: elongate

answers: NDQ_003357

answers: two processes occur simultaneously during time

answers: NDQ_003358

answers: unmoving

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Apennine

answers: NDQ_003362

answers: the two processes occur simultaneously during time

answers: NDQ_003363

answers: Apennine orogeny

answers: NDQ_003371

answers: What type of mountain-building in which two simpler types are combined in an apparently paradoxical configuration?

answers: NDQ_003373

answers: None of the above choices.

answers: NDQ_003376

answers: not

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: no

answers: NDQ_003380

answers: How would you describe the Apennine orogeny?

answers: NDQ_003381

answers: What does the term "syn-orogenic extension" mean

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: What type of mountain-building is the Apennine orogeny?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: syn-orogenic extension

answers: NDQ_003391

answers: mountain belts

answers: NDQ_003392

answers: syn-orogenic extension

answers: NDQ_003393

answers: mountain

answers: NDQ_003394

answers: unanswerable

answers: NDQ_003395

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: "syn-orogenic extension",

answers: NDQ_003352

answers: "syn-orogenic extension",

answers: NDQ_003353

answers: The Apennine orogeny

answers: NDQ_003354

answers: The Apennine orogeny

answers: NDQ_003355

answers: The Apennine orogeny

answers: NDQ_003356

answers: "syn-orogenic extension",

answers: NDQ_003357

answers: the two processes occur simultaneously during time.

answers: NDQ_003358

answers: The Apennine orogeny

answers: NDQ_003359

answers: simultaneously during time.

answers: NDQ_003360

answers: The Apennine orogeny

answers: NDQ_003362

answers: rare but not unique in mountain building,

answers: NDQ_003363

answers: Apennine orogeny

answers: NDQ_003371

answers: The Apennine orogeny

answers: NDQ_003373

answers: The Apennine orogeny

answers: NDQ_003376

answers: The Apennine orogeny

answers: NDQ_003378

answers: "syn-orogenic extension",

answers: NDQ_003379

answers: common in all mountain belts.

answers: NDQ_003380

answers: "syn-orogenic extension",

answers: NDQ_003381

answers: "syn-orogenic extension",

answers: NDQ_003382

answers: "syn-orogenic extension",

answers: NDQ_003383

answers: "syn-orogenic extension",

answers: NDQ_003384

answers: "syn-orogenic extension",

answers: NDQ_003385

answers: mountain belts.

answers: NDQ_003386

answers: The Apennine orogeny

answers: NDQ_003387

answers: The Apennine orogeny

answers: NDQ_003388

answers: The Apennine orogeny

answers: NDQ_003389

answers: The Apennine orogeny

answers: NDQ_003390

answers: The Apennine orogeny

answers: NDQ_003391

answers: Apennine orogeny

answers: NDQ_003392

answers: "syn-orogenic extension",

answers: NDQ_003393

answers: "syn-orogenic extension",

answers: NDQ_003394

answers: The Apennine orogeny

answers: NDQ_003395

answers: The Apennine orogeny

answers: NDQ_003396

answers: The Apennine orogeny

text: Following the conclusion of the original Doom series, the sole Marine who survived the horrors of Hell returned to Earth, reclaiming it from the invasion that almost eradicated the human race. Demons still lingered within the abandoned halls and complexes of Phobos and Deimos. As a last-ditch effort, the military decided to bombard the moons with extreme radiation in hopes of killing off any remaining demons. It was initially successful, however, something survived the exposure. The radiation blocked the military's sensors, and allowed something to slip past them undetected. This mysterious entity, possessing the ability to resurrect any demon it came across, recreated the entire demonic horde and made it stronger than ever before. A Marine strike force was ordered to contain the advancing armies of Hell, but was mercilessly slaughtered within moments. The player's character is the sole survivor of this group.

text: Following the conclusion of the original Doom series, the sole Marine who survived the horrors of Hell returned to Earth, reclaiming it from the invasion that almost eradicated the human race. Demons still lingered within the abandoned halls and complexes of Phobos and Deimos. As a last-ditch effort, the military decided to bombard the moons with extreme radiation in hopes of killing off any remaining demons. It was initially successful, however, something survived the exposure. The radiation blocked the military's sensors, and allowed something to slip past them undetected. This mysterious entity, possessing the ability to resurrect any demon it came across, recreated the entire demonic horde and made it stronger than ever before. A Marine strike force was ordered to contain the advancing armies of Hell, but was mercilessly slaughtered within moments. The player's character is the sole survivor of this group.

answers: NDQ_003351

answers: extreme radiation

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: resurrect

answers: NDQ_003357

answers: How many demons were resurrected?

answers: NDQ_003358

answers: unanswerable

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth?

answers: NDQ_003362

answers: unanswerable

answers: NDQ_003363

answers: Earth's surface

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: what is the last word in the passage?

answers: NDQ_003376

answers: what is the last word in the passage?

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What kind of force is applied to rock?

answers: NDQ_003381

answers: What happened to the Marine strike force?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: What happened to the marines?

answers: NDQ_003388

answers: What does shear stress result from?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: Deimos

answers: NDQ_003391

answers: Deimos

answers: NDQ_003392

answers: unanswerable

answers: NDQ_003393

answers: Deimos

answers: NDQ_003394

answers: unanswerable

answers: NDQ_003395

answers: unanswerable

answers: NDQ_003396

answers: NDQ_003351

answers: radiation

answers: NDQ_003352

answers: stronger than ever before.

answers: NDQ_003353

answers: radiation

answers: NDQ_003354

answers: something to slip past them undetected.

answers: NDQ_003355

answers: radiation

answers: NDQ_003356

answers: radiation

answers: NDQ_003357

answers: The radiation blocked the military's sensors,

answers: NDQ_003358

answers: complexes

answers: NDQ_003359

answers: radiation

answers: NDQ_003360

answers: Earth,

answers: NDQ_003362

answers: reclaiming it from the invasion that almost eradicated the human race.

answers: NDQ_003363

answers: Earth,

answers: NDQ_003371

answers: radiation

answers: NDQ_003373

answers: radiation

answers: NDQ_003376

answers: radiation

answers: NDQ_003378

answers: slip past them undetected.

answers: NDQ_003379

answers: radiation

answers: NDQ_003380

answers: radiation

answers: NDQ_003381

answers: radiation

answers: NDQ_003382

answers: radiation

answers: NDQ_003383

answers: radiation

answers: NDQ_003384

answers: reclaiming it from the invasion that almost eradicated the human race.

answers: NDQ_003385

answers: Phobos and Deimos.

answers: NDQ_003386

answers: Earth,

answers: NDQ_003387

answers: radiation

answers: NDQ_003388

answers: radiation

answers: NDQ_003389

answers: radiation

answers: NDQ_003390

answers: Doom

answers: NDQ_003391

answers: Phobos and Deimos.

answers: NDQ_003392

answers: Doom

answers: NDQ_003393

answers: Phobos

answers: NDQ_003394

answers: radiation

answers: NDQ_003395

answers: radiation

answers: NDQ_003396

answers: radiation

text: Vancouver Island is mostly made up of volcanic and sedimentary rock which was formed offshore on the now disappeared Kula oceanic plate.  Around 55 million years ago, a microplate of the Kula Plate subducted below the North American continental margin with great strain.  A volcanic arc on the surface of the Kula Plate was thus accreted and fused onto the western edge of North America.  These terranes were subjected to extreme warping from continued subduction of the Kula plate, leading to the formation of the distorted Insular Mountains.  Much of the central mountainous region around Strathcona Park is part of the Karmutsen Formation, which is a sequence of tholeiitic pillow basalts and breccias.  Since Vancouver Island has become an accretionary wedge on the North American continent, the Kula Plate has fully subducted beneath it and the remnants of the Farallon Plate, the Juan de Fuca Plate, are now subducting below the island.  This process has led to Vancouver Island being one of the most seismically active regions in Canada.  The subduction zone off the coast of the island forms a section of the Pacific Ring of Fire.  The area has been known to host megathrust earthquakes in the past, the last occurring in 1700.  In 1946, the Forbidden Plateau in the east of the Vancouver Island Ranges was the epicentre of an earthquake that registered 7.3 on the Richter magnitude scale, the strongest ever recorded on land in Canada.

text: Vancouver Island is mostly made up of

text: volcanic

text: and

text: sedimentary rock

text: which was formed offshore on the now disappeared

text: Kula

text: oceanic plate

text: .  Around 55 million years ago, a

text: microplate

text: of the Kula Plate

text: subducted

text: below the

text: North American

text: continental margin

text: with great strain.  A

text: volcanic arc

text: on the surface of the Kula Plate was thus

text: accreted

text: and fused onto the western edge of North America.  These

text: terrane

text: s were subjected to extreme warping from continued subduction of the Kula plate, leading to the formation of the distorted

text: Insular Mountains

text: .  Much of the central mountainous region around

text: Strathcona Park

text: is part of the

text: Karmutsen Formation

text: , which is a sequence of

text: tholeiitic

text: pillow basalt

text: s and

text: breccia

text: s.  Since Vancouver Island has become an

text: accretionary wedge

text: on the North American continent, the Kula Plate has fully subducted beneath it and the remnants of the

text: Farallon Plate

text: , the

text: Juan de Fuca Plate

text: , are now subducting below the island.  This process has led to Vancouver Island being one of the most seismically active regions in Canada.  The subduction zone off the coast of the island forms a section of the

text: Pacific Ring of Fire

text: .  The area has been known to host

text: megathrust

text: earthquakes in the past, the last occurring in

text: .  In

text: , the

text: Forbidden Plateau

text: in the east of the

text: Vancouver Island Ranges

text: was the

text: epicentre

text: of an

text: earthquake

text: that registered 7.3 on the

text: Richter magnitude scale

text: , the strongest ever recorded on land in Canada.

answers: NDQ_003351

answers: subduction

answers: NDQ_003352

answers: warps

answers: NDQ_003353

answers: extreme warping

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: arc

answers: NDQ_003356

answers: breccias

answers: NDQ_003357

answers: the Kula Plate has fully subducted beneath it and the remnants of what plate?

answers: NDQ_003358

answers: breccia

answers: NDQ_003359

answers: subducts

answers: NDQ_003360

answers: Kula Plate

answers: NDQ_003362

answers: the last occurring in 1700

answers: NDQ_003363

answers: Kula

answers: NDQ_003371

answers: Which of the following is not a formation: tholeiitic pillow basalts and breccias?

answers: NDQ_003373

answers: Why is Vancouver Island one of the most seismically active regions in Canada?

answers: NDQ_003376

answers: Which of the following is not a type of terrain: basin-and-range or mountainous

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: Which of the following is not a strike-slip fault?

answers: NDQ_003380

answers: What is a stress?

answers: NDQ_003381

answers: What caused the formation of the distorted Insular Mountains

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of extreme warping in rock?

answers: NDQ_003384

answers: Which of the following is not a type of fold: A volcanic arc on the surface of the Kula Plate or a volcanic arc?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: subduction

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: megathrust earthquakes, Juan de Fuca Plate or normal faults?

answers: NDQ_003388

answers: Which of the following is not a type of strike-slip fault: strike-slip, strike-slip, or strike-slip?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: megathrust

answers: NDQ_003391

answers: subduction zone

answers: NDQ_003392

answers: megathrust

answers: NDQ_003393

answers: subduction zone

answers: NDQ_003394

answers: subduction zone

answers: NDQ_003395

answers: Pacific Ring of Fire

answers: NDQ_003396

answers: megathrust

answers: NDQ_003351

answers: megathrust earthquakes

answers: NDQ_003352

answers: warping

answers: NDQ_003353

answers: warping

answers: NDQ_003354

answers: Karmutsen Formation,

answers: NDQ_003355

answers: accretionary wedge

answers: NDQ_003356

answers: warping

answers: NDQ_003357

answers: subducting

answers: NDQ_003358

answers: megathrust

answers: NDQ_003359

answers: strain.

answers: NDQ_003360

answers: subduction of the Kula plate,

answers: NDQ_003362

answers: 1700.

answers: NDQ_003363

answers: Insular Mountains.

answers: NDQ_003371

answers: megathrust earthquakes

answers: NDQ_003373

answers: extreme warping

answers: NDQ_003376

answers: distorted Insular Mountains.

answers: NDQ_003378

answers: megathrust

answers: NDQ_003379

answers: 7.3

answers: NDQ_003380

answers: strain.

answers: NDQ_003381

answers: extreme warping

answers: NDQ_003382

answers: subduction

answers: NDQ_003383

answers: extreme warping

answers: NDQ_003384

answers: volcanic arc

answers: NDQ_003385

answers: Pacific Ring of Fire.

answers: NDQ_003386

answers: megathrust earthquakes

answers: NDQ_003387

answers: megathrust

answers: NDQ_003388

answers: megathrust earthquakes in the past, the last occurring in 1700.

answers: NDQ_003389

answers: subduction

answers: NDQ_003390

answers: megathrust

answers: NDQ_003391

answers: Kula Plate

answers: NDQ_003392

answers: megathrust

answers: NDQ_003393

answers: volcanic arc

answers: NDQ_003394

answers: 7.3

answers: NDQ_003395

answers: 7.3

answers: NDQ_003396

answers: megathrust

text: As the tectonic plates migrate, oceanic crust is subducted under the leading edges of the plates at convergent boundaries. At the same time, the upwelling of mantle material at divergent boundaries creates mid-ocean ridges. The combination of these processes recycles the oceanic crust back into the mantle. Due to this recycling, most of the ocean floor is less than  old in age. The oldest oceanic crust is located in the Western Pacific and has an estimated age of . By comparison, the oldest dated continental crust is .

text: As the tectonic plates migrate, oceanic crust is

text: subducted

text: under the leading edges of the plates at convergent boundaries. At the same time, the upwelling of mantle material at divergent boundaries creates mid-ocean ridges. The combination of these processes recycles the

text: oceanic crust

text: back into the mantle. Due to this recycling, most of the ocean floor is less than  old in age. The oldest oceanic crust is located in the Western Pacific and has an estimated age of . By comparison, the oldest dated

text: continental crust

text: is .

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: subducts

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: ridge

answers: NDQ_003356

answers: subduct

answers: NDQ_003357

answers: oceanic crust is subducted

answers: NDQ_003358

answers: ridge

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: continental plates

answers: NDQ_003362

answers: the oldest dated continental crust is.

answers: NDQ_003363

answers: divergent boundaries

answers: NDQ_003371

answers: Which of the following is not a type of thrust fault?

answers: NDQ_003373

answers: It is subducted under the leading edges of the plates

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: vertical

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: How does rock deform?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: what is the last word in the passage?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: tectonic plates

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: normal faults, mid-ocean ridges, or divergent boundaries?

answers: NDQ_003388

answers: Which of the following is not a type of strike-slip fault?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: tectonic plate

answers: NDQ_003391

answers: subducted

answers: NDQ_003392

answers: Mid-ocean Ridge

answers: NDQ_003393

answers: continental crust

answers: NDQ_003394

answers: divergent

answers: NDQ_003395

answers: divergent boundaries

answers: NDQ_003396

answers: divergent boundary

answers: NDQ_003351

answers: upwelling of mantle material

answers: NDQ_003352

answers: mid-ocean ridges.

answers: NDQ_003353

answers: mid-ocean ridges.

answers: NDQ_003354

answers: As the tectonic plates

answers: NDQ_003355

answers: ridges.

answers: NDQ_003356

answers: mid-ocean ridges.

answers: NDQ_003357

answers: mid-ocean ridges.

answers: NDQ_003358

answers: mid-ocean ridges.

answers: NDQ_003359

answers: convergent boundaries.

answers: NDQ_003360

answers: tectonic plates

answers: NDQ_003362

answers: less than old in age.

answers: NDQ_003363

answers: convergent boundaries.

answers: NDQ_003371

answers: mid-ocean ridges.

answers: NDQ_003373

answers: oceanic crust

answers: NDQ_003376

answers: mid-ocean ridges.

answers: NDQ_003378

answers: oceanic crust

answers: NDQ_003379

answers: convergent boundaries.

answers: NDQ_003380

answers: oceanic crust

answers: NDQ_003381

answers: mid-ocean ridges.

answers: NDQ_003382

answers: oceanic crust

answers: NDQ_003383

answers: mid-ocean ridges.

answers: NDQ_003384

answers: mid-ocean ridges.

answers: NDQ_003385

answers: mid-ocean ridges.

answers: NDQ_003386

answers: tectonic plates

answers: NDQ_003387

answers: mid-ocean ridges.

answers: NDQ_003388

answers: mid-ocean ridges.

answers: NDQ_003389

answers: the upwelling

answers: NDQ_003390

answers: mid-ocean ridges.

answers: NDQ_003391

answers: oceanic crust

answers: NDQ_003392

answers: mid-ocean ridges.

answers: NDQ_003393

answers: mid-ocean ridges.

answers: NDQ_003394

answers: mid-ocean ridges.

answers: NDQ_003395

answers: convergent boundaries.

answers: NDQ_003396

answers: mid-ocean ridges.

text: Rhodium is one of the rarest elements in the Earth's crust, comprising an estimated 0.0002 parts per million (2 × 10).  Its rarity affects its price and its use in commercial applications.

text: Rhodium is one of the

text: rarest elements in the Earth's crust

text: , comprising an estimated 0.0002

text: parts per million

text: (2 × 10).  Its rarity affects its price and its use in commercial applications.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: increase in price

answers: NDQ_003357

answers: Rhodium is one of the rarest elements

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: the San Andreas fault is not a fault

answers: NDQ_003363

answers: Earth's crust

answers: NDQ_003371

answers: What is one of the rarest elements in the Earth's crust?

answers: NDQ_003373

answers: how would you describe compressive stresses?

answers: NDQ_003376

answers: no

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What is the reason for the rarity of rhodium?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: unanswerable

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: Rhodium or normal faults?

answers: NDQ_003388

answers: What is one of the rarest elements in the Earth's crust?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: unanswerable

answers: NDQ_003392

answers: unanswerable

answers: NDQ_003393

answers: unanswerable

answers: NDQ_003394

answers: isosceles

answers: NDQ_003395

answers: unanswerable

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: Rhodium

answers: NDQ_003352

answers: Rhodium

answers: NDQ_003353

answers: Rhodium

answers: NDQ_003354

answers: Rhodium

answers: NDQ_003355

answers: Rhodium

answers: NDQ_003356

answers: Rhodium

answers: NDQ_003357

answers: 0.0002 parts per million (2 <unk> 10).

answers: NDQ_003358

answers: Rhodium

answers: NDQ_003359

answers: 0.0002 parts per million (2 <unk> 10).

answers: NDQ_003360

answers: Rhodium

answers: NDQ_003362

answers: Rhodium

answers: NDQ_003363

answers: Rhodium

answers: NDQ_003371

answers: 0.0002 parts per million (2 <unk> 10).

answers: NDQ_003373

answers: Rhodium

answers: NDQ_003376

answers: Rhodium

answers: NDQ_003378

answers: 0.0002 parts per million (2 <unk> 10).

answers: NDQ_003379

answers: 0.0002 parts per million (2 <unk> 10).

answers: NDQ_003380

answers: 0.0002 parts per million (2 <unk> 10).

answers: NDQ_003381

answers: 0.0002 parts per million (2 <unk> 10).

answers: NDQ_003382

answers: 0.0002 parts per million (2 <unk> 10).

answers: NDQ_003383

answers: Rhodium

answers: NDQ_003384

answers: Rhodium

answers: NDQ_003385

answers: Rhodium

answers: NDQ_003386

answers: Rhodium

answers: NDQ_003387

answers: Rhodium

answers: NDQ_003388

answers: 0.0002 parts per million (2 <unk> 10).

answers: NDQ_003389

answers: Rhodium

answers: NDQ_003390

answers: 0.0002 parts per million (2 <unk> 10).

answers: NDQ_003391

answers: Rhodium

answers: NDQ_003392

answers: 0.0002 parts per million (2 <unk> 10).

answers: NDQ_003393

answers: Rhodium

answers: NDQ_003394

answers: 0.0002 parts per million (2 <unk> 10).

answers: NDQ_003395

answers: Rhodium

answers: NDQ_003396

answers: 0.0002 parts per million (2 <unk> 10).

text: Rift is the fourth official studio album by the American rock band Phish. It is the band's second concept album, the first being  The Man Who Stepped into Yesterday in 1987, which has never been officially released. Rifts songs convey the experience of a man dreaming about the rift in his relationship with his girlfriend. Recorded in September and October 1992 and produced by Muscle Shoals music veteran Barry Beckett, the album was released by Elektra Records on February 2, 1993.

text: Rift is the fourth official studio album by the American rock band

text: Phish

text: . It is the band's second

text: concept album

text: , the first being

text: The Man Who Stepped into Yesterday

text: in 1987, which has never been officially released. Rifts songs convey the experience of a man dreaming about the rift in his relationship with his girlfriend. Recorded in September and October 1992 and produced by

text: Muscle Shoals

text: music veteran

text: Barry Beckett

text: , the album was released by

text: Elektra Records

text: on February 2, 1993.

answers: NDQ_003351

answers: Rift

answers: NDQ_003352

answers: Rift

answers: NDQ_003353

answers: Rift

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: rift

answers: NDQ_003356

answers: rift

answers: NDQ_003357

answers: The Man Who Stepped into Yesterday was released in what year?

answers: NDQ_003358

answers: rift

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: has never been officially released

answers: NDQ_003363

answers: Rift

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: How would you describe Rift?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: what is the fourth official studio album by the American rock band Phish

answers: NDQ_003379

answers: vertical

answers: NDQ_003380

answers: How would you describe Rift?

answers: NDQ_003381

answers: What is the last word in the passage?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is the band's second concept album?

answers: NDQ_003386

answers: movement of rock at faults

answers: NDQ_003387

answers: Which happened first, The Man Who Stepped into Yesterday or Rift?

answers: NDQ_003388

answers: What type of stress is shear stress?

answers: NDQ_003389

answers: unknown

answers: NDQ_003390

answers: Muscle Shoals

answers: NDQ_003391

answers: Muscle Shoals

answers: NDQ_003392

answers: Muscle Shoals

answers: NDQ_003393

answers: rift

answers: NDQ_003394

answers: NDQ_003395

answers: Muscle Shoals

answers: NDQ_003396

answers: Rift

answers: NDQ_003351

answers: rift

answers: NDQ_003352

answers: rift

answers: NDQ_003353

answers: Muscle Shoals

answers: NDQ_003354

answers: 1993.

answers: NDQ_003355

answers: rift

answers: NDQ_003356

answers: rift

answers: NDQ_003357

answers: rift in his relationship with his girlfriend.

answers: NDQ_003358

answers: rift

answers: NDQ_003359

answers: rift

answers: NDQ_003360

answers: Rift

answers: NDQ_003362

answers: never been officially released.

answers: NDQ_003363

answers: Muscle Shoals

answers: NDQ_003371

answers: Rift

answers: NDQ_003373

answers: Muscle Shoals

answers: NDQ_003376

answers: Muscle Shoals

answers: NDQ_003378

answers: rift

answers: NDQ_003379

answers: 1993.

answers: NDQ_003380

answers: rock

answers: NDQ_003381

answers: rift in his relationship with his girlfriend.

answers: NDQ_003382

answers: rift in his relationship with his girlfriend.

answers: NDQ_003383

answers: rock

answers: NDQ_003384

answers: 1992 and produced by Muscle Shoals music veteran Barry Beckett,

answers: NDQ_003385

answers: rift

answers: NDQ_003386

answers: Rift

answers: NDQ_003387

answers: rift

answers: NDQ_003388

answers: Muscle Shoals music veteran Barry Beckett,

answers: NDQ_003389

answers: Rift

answers: NDQ_003390

answers: rift

answers: NDQ_003391

answers: Muscle Shoals

answers: NDQ_003392

answers: rift

answers: NDQ_003393

answers: rift

answers: NDQ_003394

answers: rift

answers: NDQ_003395

answers: rift

answers: NDQ_003396

answers: Muscle Shoals

text: On Earth, a large piece of molten iron is sufficiently denser than continental crust material to force its way down through the crust to the mantle. In the outer Solar System a similar process may take place but with lighter materials: they may be hydrocarbons such as methane, water as liquid or ice, or frozen carbon dioxide.

text: On

text: Earth

text: , a large piece of molten

text: iron

text: is sufficiently denser than

text: continental crust

text: material to force its way down through the crust to the

text: mantle

text: . In the outer Solar System a similar process may take place but with lighter materials: they may be

text: hydrocarbons

text: such as

text: methane

text: water

text: as liquid or ice, or frozen

text: carbon dioxide

answers: NDQ_003351

answers: water as liquid or ice

answers: NDQ_003352

answers: denser

answers: NDQ_003353

answers: voids to form

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: mantle

answers: NDQ_003356

answers: liquefy

answers: NDQ_003357

answers: molten iron is sufficiently dense to force its way down through the crust to the mantle

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth

answers: NDQ_003362

answers: water as liquid or ice, or frozen carbon dioxide.

answers: NDQ_003363

answers: molten iron

answers: NDQ_003371

answers: Which of the following is not a type of rock: hydrocarbons, water as liquid or ice, or frozen carbon dioxide?

answers: NDQ_003373

answers: what is the first type of rock mentioned?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a type of rock: continental crust material, water as liquid or ice, or frozen carbon dioxide?

answers: NDQ_003381

answers: what is the first type of material mentioned?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: Which of the following is not a type of normal fault?

answers: NDQ_003388

answers: Which of the following is not a result of shear stress: strike-slip faults, hydrocarbons, or frozen carbon dioxide?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: unanswerable

answers: NDQ_003392

answers: unanswerable

answers: NDQ_003393

answers: mantle

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: is a

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: molten iron

answers: NDQ_003352

answers: denser

answers: NDQ_003353

answers: denser

answers: NDQ_003354

answers: On Earth,

answers: NDQ_003355

answers: down through the crust to the mantle.

answers: NDQ_003356

answers: lighter materials:

answers: NDQ_003357

answers: force its way down through the crust to the mantle.

answers: NDQ_003358

answers: mantle.

answers: NDQ_003359

answers: denser

answers: NDQ_003360

answers: Earth,

answers: NDQ_003362

answers: a large piece of molten iron is sufficiently denser

answers: NDQ_003363

answers: molten iron

answers: NDQ_003371

answers: a similar process may take place but with lighter materials:

answers: NDQ_003373

answers: crust to the mantle.

answers: NDQ_003376

answers: lighter materials:

answers: NDQ_003378

answers: crust to the mantle.

answers: NDQ_003379

answers: lighter materials:

answers: NDQ_003380

answers: force its way down through the crust to the mantle.

answers: NDQ_003381

answers: lighter materials:

answers: NDQ_003382

answers: lighter materials:

answers: NDQ_003383

answers: lighter materials:

answers: NDQ_003384

answers: crust to the mantle.

answers: NDQ_003385

answers: Earth,

answers: NDQ_003386

answers: a large piece of molten iron

answers: NDQ_003387

answers: lighter materials:

answers: NDQ_003388

answers: lighter materials:

answers: NDQ_003389

answers: molten iron

answers: NDQ_003390

answers: Earth,

answers: NDQ_003391

answers: molten iron

answers: NDQ_003392

answers: On Earth,

answers: NDQ_003393

answers: molten iron

answers: NDQ_003394

answers: Earth,

answers: NDQ_003395

answers: crust to the mantle.

answers: NDQ_003396

answers: crust to the mantle.

text: The land on which San Diego–Tijuana sits is due west of a major transform fault. The transform fault, known as the San Andreas Fault was created during the Cenozoic Era by the movements of the Pacific Plate and North American Plate. The region experiences earthquakes and felt the shocks of the 2009 Gulf of California earthquake and 2010 Baja California earthquake.

text: The land on which San Diego–Tijuana sits is due west of a major

text: transform fault

text: . The transform fault, known as the

text: San Andreas Fault

text: was created during the

text: Cenozoic Era

text: by the movements of the

text: Pacific Plate

text: and

text: North American Plate

text: . The region experiences earthquakes and felt the shocks of the

text: 2009 Gulf of California earthquake

text: and

text: 2010 Baja California earthquake

answers: NDQ_003351

answers: shocks

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: transform fault

answers: NDQ_003356

answers: change shape

answers: NDQ_003357

answers: the land on which San Diego–Tijuana sits is due west of what?

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: moves

answers: NDQ_003360

answers: San Andreas Fault

answers: NDQ_003362

answers: The San Andreas Fault was created during the Cenozoic Era

answers: NDQ_003363

answers: Cenozoic Era

answers: NDQ_003371

answers: What type of fault is the San Andreas Fault?

answers: NDQ_003373

answers: How would you describe San Diego–Tijuana?

answers: NDQ_003376

answers: Which of the following is not caused by compressive forces: Pacific Plate and North American Plate

answers: NDQ_003378

answers: what is the last word in the passage?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: How would you describe San Diego–Tijuana?

answers: NDQ_003381

answers: What type of stress does the San Andreas Fault cause?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: How would you describe San Diego–Tijuana?

answers: NDQ_003384

answers: What type of fold is the San Diego–Tijuana sits on?

answers: NDQ_003385

answers: What is the San Andreas Fault?

answers: NDQ_003386

answers: yes

answers: NDQ_003387

answers: Which of the following is not a normal fault: San Andreas Fault, Pacific Plate or North American Plate?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip or transform?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: transform fault

answers: NDQ_003391

answers: San Diego–Tijuana

answers: NDQ_003392

answers: transform fault

answers: NDQ_003393

answers: land on which San Diego–Tijuana sits

answers: NDQ_003394

answers: transform fault

answers: NDQ_003395

answers: transform fault

answers: NDQ_003396

answers: transform fault

answers: NDQ_003351

answers: earthquakes

answers: NDQ_003352

answers: shocks

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: due west of a major transform fault.

answers: NDQ_003355

answers: transform fault.

answers: NDQ_003356

answers: earthquakes

answers: NDQ_003357

answers: due west

answers: NDQ_003358

answers: transform fault.

answers: NDQ_003359

answers: movements of the Pacific Plate and North American Plate.

answers: NDQ_003360

answers: transform fault.

answers: NDQ_003362

answers: created during the Cenozoic Era

answers: NDQ_003363

answers: Cenozoic Era

answers: NDQ_003371

answers: transform fault.

answers: NDQ_003373

answers: earthquakes

answers: NDQ_003376

answers: movements of the Pacific Plate and North American Plate.

answers: NDQ_003378

answers: shocks

answers: NDQ_003379

answers: transform fault.

answers: NDQ_003380

answers: earthquakes and felt the shocks

answers: NDQ_003381

answers: transform fault.

answers: NDQ_003382

answers: Pacific Plate and North American Plate.

answers: NDQ_003383

answers: movements of the Pacific Plate and North American Plate.

answers: NDQ_003384

answers: transform fault.

answers: NDQ_003385

answers: transform fault.

answers: NDQ_003386

answers: movements of the Pacific Plate and North American Plate.

answers: NDQ_003387

answers: transform fault.

answers: NDQ_003388

answers: transform fault.

answers: NDQ_003389

answers: movements of the Pacific Plate and North American Plate.

answers: NDQ_003390

answers: transform fault. The transform fault, known as the San Andreas Fault

answers: NDQ_003391

answers: transform fault.

answers: NDQ_003392

answers: transform fault. The transform fault, known as the San Andreas Fault

answers: NDQ_003393

answers: transform fault.

answers: NDQ_003394

answers: transform fault.

answers: NDQ_003395

answers: transform fault. The transform fault, known as the San Andreas Fault

answers: NDQ_003396

answers: transform fault.

text: The Earth formed about 4.6 billion years ago. As it cooled the lithosphere, consisting of the crust and the rigid uppermost part of the mantle solidified. The lithosphere rides on the asthenosphere, which is also solid but can flow like a liquid on geological time scales. The lithosphere is broken up into tectonic plates, which slowly move in relation to one another at speeds of 50–100 mm annually, colliding, combining into continents, splitting and drifting apart to form new continental configurations.

text: The Earth formed about 4.6 billion years ago. As it cooled the

text: lithosphere

text: , consisting of the

text: crust

text: and the rigid uppermost part of the

text: mantle

text: solidified. The lithosphere rides on the

text: asthenosphere

text: , which is also solid but can flow like a liquid on geological time scales. The lithosphere is broken up into

text: tectonic plates

text: , which slowly move in relation to one another at speeds of 50–100 mm annually, colliding, combining into

text: continents

text: , splitting and drifting apart to form new continental configurations.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: solidifies

answers: NDQ_003353

answers: tectonic plate movement

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: plate fold

answers: NDQ_003356

answers: solidify

answers: NDQ_003357

answers: speed of 50–100 mm annually

answers: NDQ_003358

answers: asthenosphere

answers: NDQ_003359

answers: collides

answers: NDQ_003360

answers: tectonic plates

answers: NDQ_003362

answers: colliding, combining into continents, splitting and drifting apart

answers: NDQ_003363

answers: 4.6 billion years ago

answers: NDQ_003371

answers: Which of the following is not a type of tectonic plate?

answers: NDQ_003373

answers: How would you describe a rock under compressive stresses?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What is the name of the part of the mantle that solidified?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not caused by stress: collapsing, combining into continents, splitting and drifting apart?

answers: NDQ_003384

answers: Which of the following is not a type of fold: tectonic plates, asthenosphere or syncline?

answers: NDQ_003385

answers: What is the name of the area where faults are clustered?

answers: NDQ_003386

answers: Which of the following is not a cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: normal faults or tectonic plates?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip, asthenosphere, or continental?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: tectonic plates

answers: NDQ_003391

answers: tectonic plates

answers: NDQ_003392

answers: tectonic plates

answers: NDQ_003393

answers: lithosphere

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: tectonic plates

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: 50–100 mm annually,

answers: NDQ_003352

answers: solid but can flow like a liquid

answers: NDQ_003353

answers: tectonic plates,

answers: NDQ_003354

answers: The Earth formed about 4.6 billion years ago.

answers: NDQ_003355

answers: tectonic plates,

answers: NDQ_003356

answers: flow like a liquid on geological time scales.

answers: NDQ_003357

answers: colliding,

answers: NDQ_003358

answers: tectonic plates,

answers: NDQ_003359

answers: colliding,

answers: NDQ_003360

answers: tectonic plates,

answers: NDQ_003362

answers: 4.6 billion years ago.

answers: NDQ_003363

answers: 4.6 billion years ago.

answers: NDQ_003371

answers: tectonic plates,

answers: NDQ_003373

answers: tectonic plates,

answers: NDQ_003376

answers: tectonic plates,

answers: NDQ_003378

answers: tectonic plates,

answers: NDQ_003379

answers: tectonic plates,

answers: NDQ_003380

answers: tectonic plates,

answers: NDQ_003381

answers: tectonic plates,

answers: NDQ_003382

answers: tectonic plates,

answers: NDQ_003383

answers: tectonic plates,

answers: NDQ_003384

answers: tectonic plates,

answers: NDQ_003385

answers: tectonic plates,

answers: NDQ_003386

answers: tectonic plates,

answers: NDQ_003387

answers: tectonic plates,

answers: NDQ_003388

answers: tectonic plates,

answers: NDQ_003389

answers: tectonic plates,

answers: NDQ_003390

answers: tectonic plates,

answers: NDQ_003391

answers: tectonic plates,

answers: NDQ_003392

answers: tectonic plates,

answers: NDQ_003393

answers: lithosphere,

answers: NDQ_003394

answers: tectonic plates,

answers: NDQ_003395

answers: tectonic plates,

answers: NDQ_003396

answers: tectonic plates,

text: In the same way as the two orogenies that followed, the Nevadan was caused by the subduction of oceanic lithosphere at a subduction zone running along the edge of the North American continent. This resulted in oceanic crust, being more dense than the mantle, descending into the lithosphere very quickly, and steeply beneath the edge of the continent.

text: In the same way as the two orogenies that followed, the Nevadan was caused by the

text: subduction

text: of

text: oceanic lithosphere

text: at a

text: subduction zone

text: running along the edge of the North American continent. This resulted in

text: oceanic crust

text: , being more dense than the mantle, descending into the

text: lithosphere

text: very quickly, and steeply beneath the edge of the

text: continent

answers: NDQ_003351

answers: subduction

answers: NDQ_003352

answers: subducts

answers: NDQ_003353

answers: subduction

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: subduction zone

answers: NDQ_003356

answers: subduct

answers: NDQ_003357

answers: oceanic crust is more dense than the mantle

answers: NDQ_003358

answers: subduction zone

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: mantle

answers: NDQ_003362

answers: the Nevadan was caused by the subduction of oceanic lithosphere

answers: NDQ_003363

answers: subduction zone

answers: NDQ_003371

answers: Which of the following is not a type of orogeny?

answers: NDQ_003373

answers: subduction

answers: NDQ_003376

answers: subduction

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: vertical

answers: NDQ_003380

answers: It's impossible to say

answers: NDQ_003381

answers: What is the reason for the Nevadan?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: subduction zone

answers: NDQ_003386

answers: no

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: Which of the following is not a type of fault?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: subduction zone

answers: NDQ_003391

answers: subduction zone

answers: NDQ_003392

answers: subduction zone

answers: NDQ_003393

answers: subduction zone

answers: NDQ_003394

answers: subduction zone

answers: NDQ_003395

answers: subduction zone

answers: NDQ_003396

answers: subduction zone

answers: NDQ_003351

answers: subduction

answers: NDQ_003352

answers: steeply beneath the edge of the continent.

answers: NDQ_003353

answers: subduction

answers: NDQ_003354

answers: steeply beneath the edge of the continent.

answers: NDQ_003355

answers: Nevadan

answers: NDQ_003356

answers: descending into the lithosphere very quickly,

answers: NDQ_003357

answers: subduction of oceanic lithosphere at a subduction zone

answers: NDQ_003358

answers: subduction zone

answers: NDQ_003359

answers: subduction

answers: NDQ_003360

answers: subduction of oceanic lithosphere

answers: NDQ_003362

answers: oceanic crust, being more dense than the mantle,

answers: NDQ_003363

answers: subduction of oceanic lithosphere at a subduction zone

answers: NDQ_003371

answers: subduction zone

answers: NDQ_003373

answers: steeply beneath the edge of the continent.

answers: NDQ_003376

answers: subduction of oceanic lithosphere

answers: NDQ_003378

answers: subduction

answers: NDQ_003379

answers: steeply beneath the edge of the continent.

answers: NDQ_003380

answers: subduction

answers: NDQ_003381

answers: subduction

answers: NDQ_003382

answers: subduction of oceanic lithosphere at a subduction zone

answers: NDQ_003383

answers: subduction of oceanic lithosphere

answers: NDQ_003384

answers: subduction zone

answers: NDQ_003385

answers: subduction zone

answers: NDQ_003386

answers: subduction of oceanic lithosphere at a subduction zone

answers: NDQ_003387

answers: subduction of oceanic lithosphere

answers: NDQ_003388

answers: subduction of oceanic lithosphere

answers: NDQ_003389

answers: subduction

answers: NDQ_003390

answers: subduction zone

answers: NDQ_003391

answers: subduction zone

answers: NDQ_003392

answers: Nevadan

answers: NDQ_003393

answers: Nevadan

answers: NDQ_003394

answers: subduction zone

answers: NDQ_003395

answers: subduction zone

answers: NDQ_003396

answers: subduction zone

text: Normally, as Earth gets colder due to natural climatic fluctuations and changes in incoming solar radiation, the cooling slows these weathering reactions. As a result, less carbon dioxide is removed from the atmosphere and Earth warms as this greenhouse gas accumulates — this 'negative feedback' process limits the magnitude of cooling. During the Cryogenian period, however, Earth's continents were all at tropical latitudes, which made this moderating process less effective, as high weathering rates continued on land even as Earth cooled. This let ice advance beyond the polar regions. Once ice advanced to within 30° of the equator, a positive feedback could ensue such that the increased reflectiveness (albedo) of the ice led to further cooling and the formation of more ice, until the whole Earth is ice-covered.

text: Normally, as Earth gets colder due to natural climatic fluctuations and changes in incoming solar radiation, the cooling slows these weathering reactions. As a result, less carbon dioxide is removed from the atmosphere and Earth warms as this greenhouse gas accumulates — this '

text: negative feedback

text: ' process limits the magnitude of cooling. During the

text: Cryogenian

text: period, however, Earth's continents were all at

text: tropical

text: latitudes, which made this moderating process less effective, as high weathering rates continued on land even as Earth cooled. This let ice advance beyond the polar regions. Once ice advanced to within 30° of the equator, a positive feedback could ensue such that the increased reflectiveness (

text: albedo

text: ) of the ice led to further cooling and the formation of more ice, until the whole Earth is ice-covered.

answers: NDQ_003351

answers: negative feedback

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: negative feedback

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: polar region

answers: NDQ_003356

answers: increase in size

answers: NDQ_003357

answers: as Earth gets colder due to natural climatic fluctuations

answers: NDQ_003358

answers: negative feedback

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's surface

answers: NDQ_003362

answers: the whole Earth is ice-covered.

answers: NDQ_003363

answers: Cryogenian

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: What is a negative feedback process?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What is a negative feedback process?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: Which of the following is not a type of fold that arches upward?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: natural climatic fluctuations

answers: NDQ_003388

answers: Which of the following is not a result of shear stress: natural climatic fluctuations and changes in incoming solar radiation

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: negative feedback

answers: NDQ_003391

answers: unanswerable

answers: NDQ_003392

answers: negative feedback

answers: NDQ_003393

answers: polar regions

answers: NDQ_003394

answers: negative feedback

answers: NDQ_003395

answers: unanswerable

answers: NDQ_003396

answers: negative feedback

answers: NDQ_003351

answers: ice

answers: NDQ_003352

answers: ice advance beyond the polar regions.

answers: NDQ_003353

answers: weathering reactions.

answers: NDQ_003354

answers: ice advance beyond the polar regions.

answers: NDQ_003355

answers: (albedo)

answers: NDQ_003356

answers: ice

answers: NDQ_003357

answers: 'negative feedback' process limits the magnitude of cooling.

answers: NDQ_003358

answers: polar regions.

answers: NDQ_003359

answers: Normally, as Earth gets colder due to natural climatic fluctuations

answers: NDQ_003360

answers: land

answers: NDQ_003362

answers: ice-covered.

answers: NDQ_003363

answers: tropical latitudes,

answers: NDQ_003371

answers: Cryogenian

answers: NDQ_003373

answers: Normally, as Earth gets colder due to natural climatic fluctuations

answers: NDQ_003376

answers: ice advance beyond the polar regions.

answers: NDQ_003378

answers: Normally, as Earth gets colder due to natural climatic fluctuations

answers: NDQ_003379

answers: tropical latitudes,

answers: NDQ_003380

answers: weathering reactions.

answers: NDQ_003381

answers: Normally, as Earth gets colder due to natural climatic fluctuations

answers: NDQ_003382

answers: Normally, as Earth gets colder due to natural climatic fluctuations

answers: NDQ_003383

answers: Normally, as Earth gets colder due to natural climatic fluctuations

answers: NDQ_003384

answers: tropical latitudes,

answers: NDQ_003385

answers: Normally, as Earth gets colder due to natural climatic fluctuations

answers: NDQ_003386

answers: Normally, as Earth gets colder due to natural climatic fluctuations

answers: NDQ_003387

answers: Normally, as Earth gets colder due to natural climatic fluctuations

answers: NDQ_003388

answers: Normally, as Earth gets colder due to natural climatic fluctuations

answers: NDQ_003389

answers: ice

answers: NDQ_003390

answers: Normally, as Earth gets colder due to natural climatic fluctuations

answers: NDQ_003391

answers: ice

answers: NDQ_003392

answers: Normally, as Earth gets colder due to natural climatic fluctuations

answers: NDQ_003393

answers: ice

answers: NDQ_003394

answers: Normally, as Earth gets colder due to natural climatic fluctuations

answers: NDQ_003395

answers: incoming solar radiation,

answers: NDQ_003396

answers: tropical latitudes,

text: A dike swarm is a large geological structure consisting of a major group of parallel, linear, or radially oriented dikes intruded within continental crust. They consist of several to hundreds of dikes emplaced more or less contemporaneously during a single intrusive event, and are magmatic and stratigraphic. Such dike swarms are the roots of a volcanic province. Examples include:

text: A dike swarm is a large geological structure consisting of a major group of parallel, linear, or radially oriented dikes intruded within continental crust. They consist of several to hundreds of dikes emplaced more or less contemporaneously during a single intrusive event, and are magmatic and stratigraphic. Such dike swarms are the roots of a volcanic province. Examples include:

answers: NDQ_003351

answers: radial

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: voids to form

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: swarm

answers: NDQ_003356

answers: swell

answers: NDQ_003357

answers: parallel, linear, or radially oriented dikes intruded

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: continental crust

answers: NDQ_003362

answers: The San Andreas fault is not a volcano

answers: NDQ_003363

answers: dike swarm

answers: NDQ_003371

answers: What is an example of a thrust fault?

answers: NDQ_003373

answers: How would you describe a rock under compressive stresses?

answers: NDQ_003376

answers: The terrain known as basin-and-range is caused by compressive forces.

answers: NDQ_003378

answers: What is the term for the amount the ground moves in an earthquake?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What is an example of a stress?

answers: NDQ_003381

answers: What is a result of confining stress?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What causes joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: Which of the following is not a type of fault?

answers: NDQ_003387

answers: What type of stress is caused by normal faults?

answers: NDQ_003388

answers: Which of the following is not an example of a strike-slip fault?

answers: NDQ_003389

answers: What is the process of folding?

answers: NDQ_003390

answers: dike swarm

answers: NDQ_003391

answers: dike

answers: NDQ_003392

answers: Hanging wall

answers: NDQ_003393

answers: dip-slip fault

answers: NDQ_003394

answers: radially

answers: NDQ_003395

answers: NDQ_003396

answers: radially

answers: NDQ_003351

answers: dike swarm

answers: NDQ_003352

answers: dike swarm

answers: NDQ_003353

answers: dike swarm

answers: NDQ_003354

answers: dike swarm

answers: NDQ_003355

answers: dike swarm

answers: NDQ_003356

answers: dike swarm

answers: NDQ_003357

answers: radially oriented dikes

answers: NDQ_003358

answers: dike swarm

answers: NDQ_003359

answers: dike swarm

answers: NDQ_003360

answers: dike swarm

answers: NDQ_003362

answers: A dike swarm

answers: NDQ_003363

answers: dike swarm

answers: NDQ_003371

answers: dike swarm

answers: NDQ_003373

answers: dike swarm

answers: NDQ_003376

answers: dike swarm

answers: NDQ_003378

answers: dike swarm

answers: NDQ_003379

answers: dike swarm

answers: NDQ_003380

answers: dike swarm

answers: NDQ_003381

answers: dike swarm

answers: NDQ_003382

answers: dike swarm

answers: NDQ_003383

answers: dike swarm

answers: NDQ_003384

answers: dike swarm

answers: NDQ_003385

answers: dike swarm

answers: NDQ_003386

answers: dike swarm

answers: NDQ_003387

answers: A dike swarm

answers: NDQ_003388

answers: dike swarm

answers: NDQ_003389

answers: dike swarm

answers: NDQ_003390

answers: dike swarm

answers: NDQ_003391

answers: dike swarm

answers: NDQ_003392

answers: dike swarm

answers: NDQ_003393

answers: dike swarm

answers: NDQ_003394

answers: radially

answers: NDQ_003395

answers: dike swarm

answers: NDQ_003396

answers: dike swarm

text: In contrast to epeirogenic movement, orogenic movement is a more complicated deformation of the Earth's crust, associated with crustal thickening, notably associated with the convergence of tectonic plates. Such plate convergence forms orogenic belts that are characterized by "the folding and faulting of layers of rock, by the intrusion of magma, and by volcanism".

text: In contrast to epeirogenic movement,

text: orogenic movement

text: is a more complicated deformation of the Earth's crust, associated with crustal thickening, notably associated with the convergence of

text: tectonic plates

text: . Such plate convergence forms

text: orogenic belts

text: that are characterized by "the folding and faulting of layers of rock, by the intrusion of magma, and by volcanism".

answers: NDQ_003351

answers: crustal thickening

answers: NDQ_003352

answers: thickens

answers: NDQ_003353

answers: faulting

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: orogenic belt

answers: NDQ_003356

answers: fold and fault

answers: NDQ_003357

answers: crustal thickening

answers: NDQ_003358

answers: unanswerable

answers: NDQ_003359

answers: folds

answers: NDQ_003360

answers: orogenic belts

answers: NDQ_003362

answers: Volcanism is a more complicated deformation of the Earth's crust

answers: NDQ_003363

answers: orogenic belts

answers: NDQ_003371

answers: Which of the following is not a type of thrust fault: folding and faulting of layers of rock, intrusion of magma, or volcanism?

answers: NDQ_003373

answers: unanswerable

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: How would you describe the folding and faulting of layers of rock?

answers: NDQ_003381

answers: Which of the following is not a type of deformation of the Earth's crust?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: no

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: Which of the following is not a type of strike-slip fault: strike-slip, strike-slip, or strike-slip?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: orogenic belts

answers: NDQ_003391

answers: layers of rock

answers: NDQ_003392

answers: orogenic belts

answers: NDQ_003393

answers: layers of rock

answers: NDQ_003394

answers: vertical

answers: NDQ_003395

answers: orogenic belts

answers: NDQ_003396

answers: orogenic belts

answers: NDQ_003351

answers: orogenic movement

answers: NDQ_003352

answers: thickening,

answers: NDQ_003353

answers: "the folding and faulting

answers: NDQ_003354

answers: orogenic movement

answers: NDQ_003355

answers: epeirogenic movement,

answers: NDQ_003356

answers: crustal thickening,

answers: NDQ_003357

answers: "the folding and faulting of layers of rock,

answers: NDQ_003358

answers: epeirogenic movement,

answers: NDQ_003359

answers: "the folding and faulting of layers of rock,

answers: NDQ_003360

answers: tectonic plates.

answers: NDQ_003362

answers: epeirogenic movement,

answers: NDQ_003363

answers: orogenic movement

answers: NDQ_003371

answers: orogenic belts

answers: NDQ_003373

answers: orogenic movement

answers: NDQ_003376

answers: orogenic movement

answers: NDQ_003378

answers: epeirogenic movement,

answers: NDQ_003379

answers: epeirogenic movement,

answers: NDQ_003380

answers: orogenic movement

answers: NDQ_003381

answers: orogenic movement

answers: NDQ_003382

answers: orogenic movement

answers: NDQ_003383

answers: "the folding and faulting

answers: NDQ_003384

answers: epeirogenic movement,

answers: NDQ_003385

answers: orogenic belts

answers: NDQ_003386

answers: orogenic movement

answers: NDQ_003387

answers: epeirogenic movement,

answers: NDQ_003388

answers: epeirogenic movement,

answers: NDQ_003389

answers: "the folding and faulting of layers of rock,

answers: NDQ_003390

answers: epeirogenic movement,

answers: NDQ_003391

answers: layers

answers: NDQ_003392

answers: epeirogenic movement,

answers: NDQ_003393

answers: layers

answers: NDQ_003394

answers: faulting of layers of rock,

answers: NDQ_003395

answers: faulting of layers of rock,

answers: NDQ_003396

answers: epeirogenic movement,

text: Oceanic lithosphere is less dense than asthenosphere for a few tens of millions of years but after this becomes increasingly denser than asthenosphere. This is because the chemically differentiated oceanic crust is lighter than asthenosphere, but thermal contraction of the mantle lithosphere makes it more dense than the asthenosphere. The gravitational instability of mature oceanic lithosphere has the effect that at subduction zones, oceanic lithosphere invariably sinks underneath the overriding lithosphere, which can be oceanic or continental. New oceanic lithosphere is constantly being produced at mid-ocean ridges and is recycled back to the mantle at subduction zones. As a result, oceanic lithosphere is much younger than continental lithosphere: the oldest oceanic lithosphere is about 170 million years old, while parts of the continental lithosphere are billions of years old. The oldest parts of continental lithosphere underlie cratons, and the mantle lithosphere there is thicker and less dense than typical; the relatively low density of such mantle "roots of cratons" helps to stabilize these regions.

text: Oceanic lithosphere is less dense than asthenosphere for a few tens of millions of years but after this becomes increasingly denser than asthenosphere. This is because the chemically differentiated oceanic crust is lighter than asthenosphere, but

text: thermal contraction

text: of the mantle lithosphere makes it more dense than the asthenosphere. The gravitational instability of mature oceanic lithosphere has the effect that at

text: subduction zone

text: s, oceanic lithosphere invariably sinks underneath the overriding lithosphere, which can be oceanic or continental. New oceanic lithosphere is constantly being produced at mid-ocean ridges and is recycled back to the mantle at subduction zones. As a result, oceanic lithosphere is much younger than continental lithosphere: the oldest oceanic lithosphere is about 170 million years old, while parts of the continental lithosphere are billions of years old. The oldest parts of continental lithosphere underlie

text: craton

text: s, and the mantle lithosphere there is thicker and less dense than typical; the relatively low density of such mantle "roots of cratons" helps to stabilize these regions.

answers: NDQ_003351

answers: subduction

answers: NDQ_003352

answers: sinks

answers: NDQ_003353

answers: thermal contraction

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: subduction zone

answers: NDQ_003356

answers: sink underneath the overriding lithosphere

answers: NDQ_003357

answers: oceanic lithosphere invariably sinks underneath the overriding lithosphere

answers: NDQ_003358

answers: craton

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: cratons

answers: NDQ_003362

answers: the oldest oceanic lithosphere is about 170 million years old, while parts of the continental lithosphere are billions of years old

answers: NDQ_003363

answers: subduction zones

answers: NDQ_003371

answers: Which of the following is not a type of crust: chemically differentiated oceanic crust or continental lithosphere?

answers: NDQ_003373

answers: subduction zones

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What type of rock deforms?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: subduction zones

answers: NDQ_003386

answers: The gravitational instability of mature oceanic lithosphere

answers: NDQ_003387

answers: Which of the following is not a type of normal fault?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip faults, mid-ocean ridges or continental lithosphere?

answers: NDQ_003389

answers: subduction zones

answers: NDQ_003390

answers: subduction zones

answers: NDQ_003391

answers: cratons

answers: NDQ_003392

answers: subduction zones

answers: NDQ_003393

answers: lithosphere

answers: NDQ_003394

answers: subduction zones

answers: NDQ_003395

answers: subduction zones

answers: NDQ_003396

answers: subduction zones

answers: NDQ_003351

answers: gravitational instability

answers: NDQ_003352

answers: denser

answers: NDQ_003353

answers: thermal contraction

answers: NDQ_003354

answers: Oceanic lithosphere

answers: NDQ_003355

answers: subduction zones,

answers: NDQ_003356

answers: sinks

answers: NDQ_003357

answers: subduction zones,

answers: NDQ_003358

answers: cratons,

answers: NDQ_003359

answers: instability

answers: NDQ_003360

answers: subduction zones,

answers: NDQ_003362

answers: 170 million years old,

answers: NDQ_003363

answers: subduction zones,

answers: NDQ_003371

answers: subduction zones,

answers: NDQ_003373

answers: subduction zones,

answers: NDQ_003376

answers: subduction zones,

answers: NDQ_003378

answers: subduction zones,

answers: NDQ_003379

answers: subduction zones,

answers: NDQ_003380

answers: thermal contraction

answers: NDQ_003381

answers: subduction zones,

answers: NDQ_003382

answers: subduction zones,

answers: NDQ_003383

answers: thermal contraction

answers: NDQ_003384

answers: mid-ocean ridges

answers: NDQ_003385

answers: subduction zones,

answers: NDQ_003386

answers: subduction zones,

answers: NDQ_003387

answers: subduction zones,

answers: NDQ_003388

answers: subduction zones,

answers: NDQ_003389

answers: cratons,

answers: NDQ_003390

answers: subduction zones,

answers: NDQ_003391

answers: cratons,

answers: NDQ_003392

answers: subduction zones,

answers: NDQ_003393

answers: cratons,

answers: NDQ_003394

answers: subduction zones,

answers: NDQ_003395

answers: subduction zones,

answers: NDQ_003396

answers: subduction zones,

text: Guangdong Province lies in a tectonically stable part of China, which has relatively low seismicity. The area forms part of the passive margin between the continental crust of China and the oceanic crust of the northern part of the South China Sea. Within the stable South China Block, there are three zones of higher earthquake activity, one of which is the Southeast China Coast seismic zone running through Guangdong and Fujian Provinces. This zone follows the South China Maritime Fold Belt, which was formed by a subduction event during the Late Jurassic to Early Cretaceous epochs. The area is currently in a compressive stress regime with the maximum horizontal stress orientated northwest-southeast. This results from a combination of the continuing collision between the Indian and Eurasian Plates and the subduction of the Philippine Sea Plate.

text: Guangdong Province

text: lies in a tectonically stable part of China, which has relatively low seismicity. The area forms part of the

text: passive margin

text: between the continental crust of China and the oceanic crust of the northern part of the

text: South China Sea

text: . Within the stable South China Block, there are three zones of higher earthquake activity, one of which is the Southeast China Coast seismic zone running through Guangdong and

text: Fujian

text: Provinces. This zone follows the South China Maritime Fold Belt, which was formed by a

text: subduction

text: event during the

text: Late Jurassic

text: to

text: Early Cretaceous

text: epochs. The area is currently in a compressive stress regime with the maximum horizontal stress orientated northwest-southeast. This results from a combination of the continuing

text: collision

text: between the

text: Indian

text: and

text: Eurasian Plate

text: s and the subduction of the

text: Philippine Sea Plate

answers: NDQ_003351

answers: compressive

answers: NDQ_003352

answers: compresses

answers: NDQ_003353

answers: compressive stress

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: Belt

answers: NDQ_003356

answers: compress

answers: NDQ_003357

answers: maximum horizontal stress orientated northwest-southeast

answers: NDQ_003358

answers: relatively low seismicity

answers: NDQ_003359

answers: collides with another

answers: NDQ_003360

answers: Indian Plates

answers: NDQ_003362

answers: The area is currently in a compressive stress regime with the maximum horizontal stress orientated northwest-southeast

answers: NDQ_003363

answers: Late Jurassic

answers: NDQ_003371

answers: What is the maximum horizontal stress orientated northwest-southeast?

answers: NDQ_003373

answers: Why is the area in a compressive stress regime?

answers: NDQ_003376

answers: What is the maximum horizontal stress orientated northwest-southeast?

answers: NDQ_003378

answers: What is the maximum horizontal stress orientated northwest-southeast?

answers: NDQ_003379

answers: What is the maximum horizontal stress orientated northwest-southeast?

answers: NDQ_003380

answers: What is the maximum horizontal stress orientated?

answers: NDQ_003381

answers: What is the result of the collision between the Indian and Eurasian Plates?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: What type of movement of rock at faults is the cause of earthquakes?

answers: NDQ_003387

answers: What is the maximum horizontal stress orientated northwest-southeast?

answers: NDQ_003388

answers: Which of the following is not a type of fault: Strike-slip faults or shear stress?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: Maritime Fold Belt

answers: NDQ_003391

answers: South China Block

answers: NDQ_003392

answers: Maritime Fold Belt

answers: NDQ_003393

answers: South China Block

answers: NDQ_003394

answers: northwest-southeast

answers: NDQ_003395

answers: a compressive stress regime with the maximum horizontal stress orientated northwest-southeast

answers: NDQ_003396

answers: northwest-southeast

answers: NDQ_003351

answers: northwest-southeast.

answers: NDQ_003352

answers: northwest-southeast.

answers: NDQ_003353

answers: earthquake activity,

answers: NDQ_003354

answers: South China Maritime Fold Belt,

answers: NDQ_003355

answers: Fold Belt,

answers: NDQ_003356

answers: compressive stress

answers: NDQ_003357

answers: northwest-southeast.

answers: NDQ_003358

answers: low seismicity.

answers: NDQ_003359

answers: collision

answers: NDQ_003360

answers: collision between the Indian and Eurasian Plates

answers: NDQ_003362

answers: Guangdong Province lies in a tectonically stable

answers: NDQ_003363

answers: subduction

answers: NDQ_003371

answers: South China Maritime Fold Belt,

answers: NDQ_003373

answers: northwest-southeast.

answers: NDQ_003376

answers: continuing collision between the Indian and Eurasian Plates

answers: NDQ_003378

answers: earthquake activity,

answers: NDQ_003379

answers: northwest-southeast.

answers: NDQ_003380

answers: compressive stress

answers: NDQ_003381

answers: compressive

answers: NDQ_003382

answers: northwest-southeast.

answers: NDQ_003383

answers: collision between the Indian and Eurasian Plates

answers: NDQ_003384

answers: South China Maritime Fold Belt,

answers: NDQ_003385

answers: Southeast China Coast seismic zone

answers: NDQ_003386

answers: collision between the Indian and Eurasian Plates

answers: NDQ_003387

answers: collision between the Indian and Eurasian Plates

answers: NDQ_003388

answers: compressive stress regime

answers: NDQ_003389

answers: subduction

answers: NDQ_003390

answers: South China Maritime Fold Belt,

answers: NDQ_003391

answers: South China Maritime Fold Belt,

answers: NDQ_003392

answers: South China Maritime Fold Belt,

answers: NDQ_003393

answers: Maritime Fold Belt,

answers: NDQ_003394

answers: northwest-southeast.

answers: NDQ_003395

answers: northwest-southeast.

answers: NDQ_003396

answers: northwest-southeast.

text: Despite always being found in combination with the other rare earth elements in minerals such as monazite and bastnäsite, cerium is easy to extract from its ores, as it can be distinguished among the lanthanides by its unique ability to be oxidised to the +4 state. It is the most common of the lanthanides, followed by neodymium, lanthanum, and praseodymium. It is the 26th most abundant element, making up 66 ppm of the Earth's crust, half as much as chlorine and five times as much as lead.

text: Despite always being found in combination with the other rare earth elements in minerals such as

text: monazite

text: and

text: bastnäsite

text: , cerium is easy to extract from its ores, as it can be distinguished among the lanthanides by its unique ability to be oxidised to the +4 state. It is the most common of the lanthanides, followed by

text: neodymium

text: lanthanum

text: , and

text: praseodymium

text: . It is the 26th most

text: abundant element

text: , making up 66

text: ppm

text: of the Earth's crust, half as much as

text: chlorine

text: and five times as much as

text: lead

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: oxidizes

answers: NDQ_003353

answers: voids to form

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: bastnäsite

answers: NDQ_003356

answers: oxidize to the +4 state

answers: NDQ_003357

answers: cerium is found in combination with the other rare earth elements

answers: NDQ_003358

answers: unanswerable

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: half as much as chlorine and five times as much as lead

answers: NDQ_003363

answers: Earth's crust

answers: NDQ_003371

answers: What is the most common of the lanthanides?

answers: NDQ_003373

answers: unanswerable

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: vertical

answers: NDQ_003380

answers: What is the most common of the lanthanides?

answers: NDQ_003381

answers: What is the most common of the lanthanides?

answers: NDQ_003382

answers: no

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: unanswerable

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: unanswerable

answers: NDQ_003389

answers: non-existent

answers: NDQ_003390

answers: bastnäsite

answers: NDQ_003391

answers: bastnäsite

answers: NDQ_003392

answers: bastnäsite

answers: NDQ_003393

answers: bastnäsite

answers: NDQ_003394

answers: bastnäsite

answers: NDQ_003395

answers: bastnäsite

answers: NDQ_003396

answers: bastnäsite

answers: NDQ_003351

answers: cerium

answers: NDQ_003352

answers: oxidised to the +4 state.

answers: NDQ_003353

answers: oxidised to the +4 state.

answers: NDQ_003354

answers: Despite always being found in combination with the other rare earth elements

answers: NDQ_003355

answers: monazite and bastnäsite,

answers: NDQ_003356

answers: oxidised to the +4 state.

answers: NDQ_003357

answers: lead.

answers: NDQ_003358

answers: bastnäsite,

answers: NDQ_003359

answers: oxidised to the +4

answers: NDQ_003360

answers: rare earth elements

answers: NDQ_003362

answers: cerium is easy to extract from its ores,

answers: NDQ_003363

answers: monazite and bastnäsite,

answers: NDQ_003371

answers: Despite always being found in combination with the other rare earth elements

answers: NDQ_003373

answers: monazite and bastnäsite,

answers: NDQ_003376

answers: monazite and bastnäsite,

answers: NDQ_003378

answers: monazite and bastnäsite,

answers: NDQ_003379

answers: +4

answers: NDQ_003380

answers: oxidised to the +4 state.

answers: NDQ_003381

answers: cerium

answers: NDQ_003382

answers: cerium

answers: NDQ_003383

answers: monazite and bastnäsite,

answers: NDQ_003384

answers: monazite and bastnäsite,

answers: NDQ_003385

answers: monazite and bastnäsite,

answers: NDQ_003386

answers: Despite always being found in combination with the other rare earth elements

answers: NDQ_003387

answers: cerium

answers: NDQ_003388

answers: monazite and bastnäsite,

answers: NDQ_003389

answers: Despite always being found in combination with the other rare earth elements

answers: NDQ_003390

answers: monazite and bastnäsite,

answers: NDQ_003391

answers: monazite and bastnäsite,

answers: NDQ_003392

answers: monazite and bastnäsite,

answers: NDQ_003393

answers: monazite and bastnäsite,

answers: NDQ_003394

answers: monazite and bastnäsite,

answers: NDQ_003395

answers: monazite and bastnäsite,

answers: NDQ_003396

answers: monazite and bastnäsite,

text: Some researchers, such as Michael Persinger of Laurentian University, Canada, have speculated that changes in geomagnetic fields (created, e.g., by tectonic stresses in the Earth's crust or solar activity) could stimulate the brain's temporal lobes and produce many of the experiences associated with hauntings. Sound is thought to be another cause of supposed sightings. Richard Lord and Richard Wiseman have concluded that infrasound can cause humans to experience bizarre feelings in a room, such as anxiety, extreme sorrow, a feeling of being watched, or even the chills. Carbon monoxide poisoning, which can cause changes in perception of the visual and auditory systems, was speculated upon as a possible explanation for haunted houses as early as 1921.

text: Some researchers, such as

text: Michael Persinger

text: of

text: Laurentian University

text: , Canada, have speculated that changes in

text: geomagnetic

text: fields (created, e.g., by tectonic stresses in the Earth's crust or

text: solar activity

text: ) could stimulate the brain's

text: temporal lobe

text: s and produce many of the experiences associated with hauntings. Sound is thought to be another cause of supposed sightings. Richard Lord and

text: Richard Wiseman

text: have concluded that

text: infrasound

text: can cause humans to experience bizarre feelings in a room, such as anxiety, extreme sorrow, a feeling of being watched, or even the chills.

text: Carbon monoxide poisoning

text: , which can cause changes in perception of the visual and auditory systems, was speculated upon as a possible explanation for

text: haunted house

text: s as early as 1921.

answers: NDQ_003351

answers: tectonic

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: tectonic stresses

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: hauntings

answers: NDQ_003357

answers: tectonic stresses in the Earth's crust

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: tectonic stresses

answers: NDQ_003362

answers: tectonic stresses in the Earth's crust or solar activity

answers: NDQ_003363

answers: Laurentian

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: unanswerable

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What can cause changes in perception of the visual and auditory systems

answers: NDQ_003381

answers: tectonic stresses

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unknown

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: fault zone

answers: NDQ_003386

answers: tectonic stresses

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: What can cause changes in perception of the visual and auditory systems?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: tectonic

answers: NDQ_003391

answers: tectonic

answers: NDQ_003392

answers: tectonic

answers: NDQ_003393

answers: stratigraphic unit

answers: NDQ_003394

answers: tectonic

answers: NDQ_003395

answers: tectonic stresses

answers: NDQ_003396

answers: horizontal fault

answers: NDQ_003351

answers: tectonic

answers: NDQ_003352

answers: tectonic stresses in the Earth's crust or solar activity)

answers: NDQ_003353

answers: geomagnetic fields

answers: NDQ_003354

answers: changes in geomagnetic fields

answers: NDQ_003355

answers: tectonic stresses

answers: NDQ_003356

answers: hauntings.

answers: NDQ_003357

answers: tectonic stresses

answers: NDQ_003358

answers: haunted houses

answers: NDQ_003359

answers: tectonic stresses

answers: NDQ_003360

answers: tectonic stresses

answers: NDQ_003362

answers: hauntings.

answers: NDQ_003363

answers: tectonic stresses

answers: NDQ_003371

answers: changes in geomagnetic fields

answers: NDQ_003373

answers: tectonic stresses

answers: NDQ_003376

answers: tectonic stresses

answers: NDQ_003378

answers: tectonic stresses

answers: NDQ_003379

answers: changes in geomagnetic fields

answers: NDQ_003380

answers: tectonic stresses

answers: NDQ_003381

answers: tectonic stresses

answers: NDQ_003382

answers: tectonic stresses

answers: NDQ_003383

answers: tectonic stresses

answers: NDQ_003384

answers: Carbon monoxide poisoning,

answers: NDQ_003385

answers: changes in geomagnetic fields

answers: NDQ_003386

answers: tectonic stresses

answers: NDQ_003387

answers: tectonic stresses

answers: NDQ_003388

answers: tectonic stresses

answers: NDQ_003389

answers: tectonic stresses

answers: NDQ_003390

answers: tectonic stresses

answers: NDQ_003391

answers: Carbon monoxide poisoning,

answers: NDQ_003392

answers: tectonic stresses

answers: NDQ_003393

answers: Carbon monoxide poisoning,

answers: NDQ_003394

answers: changes in geomagnetic fields

answers: NDQ_003395

answers: changes in geomagnetic fields

answers: NDQ_003396

answers: tectonic stresses

text: Around 35 million years ago, a rift valley of about  long and  wide came into being between the present cities of Basle and Frankfurt.  This was due to tensile stresses in the Earth's crust and mantle, which resulted in lowering the earth's surface.  The moat has been partially filled up again by sedimentation.  On the edges we find mountain ridges, the so-called "rift flanks".  On the eastern side, they are the Black Forest and Odenwald mountains, in the west the Vosges and Palatinate Forest.  During the tertiary, the High Rhine continued west from Basle and flowed via the Doubs and the Saône, into the Rhône.  The rift diverted the Rhine into the newly formed Upper Rhine Valley.

text: Around 35 million years ago, a

text: rift valley

text: of about  long and  wide came into being between the present cities of Basle and

text: Frankfurt

text: .  This was due to tensile stresses in the

text: Earth's crust

text: and

text: mantle

text: , which resulted in lowering the earth's surface.  The moat has been partially filled up again by

text: sedimentation

text: .  On the edges we find mountain ridges, the so-called "rift flanks".  On the eastern side, they are the

text: Black Forest

text: and

text: Odenwald

text: mountains, in the west the

text: Vosges

text: and

text: Palatinate Forest

text: .  During the

text: tertiary

text: , the High Rhine continued west from Basle and flowed via the

text: Doubs

text: and the

text: Saône

text: , into the

text: Rhône

text: .  The rift diverted the Rhine into the newly formed

text: Upper Rhine Valley

answers: NDQ_003351

answers: tensile

answers: NDQ_003352

answers: lowers its surface

answers: NDQ_003353

answers: rifts

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: rift flank

answers: NDQ_003356

answers: lower the earth's surface

answers: NDQ_003357

answers: tensile stresses in the Earth's crust and mantle

answers: NDQ_003358

answers: rift valley

answers: NDQ_003359

answers: tensile stresses

answers: NDQ_003360

answers: rift flanks

answers: NDQ_003362

answers: The rift diverted the Rhine into the newly formed Upper Rhine Valley.

answers: NDQ_003363

answers: 35 million years ago

answers: NDQ_003371

answers: What was the result of tensile stresses in the Earth's crust and mantle, which resulted in lowering the earth's surface?

answers: NDQ_003373

answers: unanswerable

answers: NDQ_003376

answers: Which of the following is not a type of terrain: basin-and-range or compressive forces?

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What was the result of tensile stresses in the Earth's crust and mantle?

answers: NDQ_003381

answers: What was the result of tensile stresses in the Earth's crust and mantle?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What was the result of tensile stresses in the Earth's crust and mantle

answers: NDQ_003384

answers: Which of the following is not a mountain ridge: Black Forest or Odenwald?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: What was due to tensile stresses in the Earth's crust and mantle?

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: tensile stresses in the Earth's crust and mantle, or normal faults?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip faults or strike-slip faults?

answers: NDQ_003389

answers: It's impossible to say

answers: NDQ_003390

answers: rift flanks

answers: NDQ_003391

answers: Moat

answers: NDQ_003392

answers: rift flanks

answers: NDQ_003393

answers: rift flank

answers: NDQ_003394

answers: rift flanks

answers: NDQ_003395

answers: unanswerable

answers: NDQ_003396

answers: rift flanks

answers: NDQ_003351

answers: tensile

answers: NDQ_003352

answers: lowering the earth's surface.

answers: NDQ_003353

answers: lowering the earth's surface.

answers: NDQ_003354

answers: Black Forest and Odenwald mountains,

answers: NDQ_003355

answers: "rift flanks".

answers: NDQ_003356

answers: lowering the earth's surface.

answers: NDQ_003357

answers: tensile stresses

answers: NDQ_003358

answers: rift valley

answers: NDQ_003359

answers: tensile stresses

answers: NDQ_003360

answers: tensile stresses

answers: NDQ_003362

answers: lowering the earth's surface.

answers: NDQ_003363

answers: a rift valley

answers: NDQ_003371

answers: tensile stresses

answers: NDQ_003373

answers: tensile stresses in the Earth's crust and mantle,

answers: NDQ_003376

answers: tensile stresses

answers: NDQ_003378

answers: tensile stresses

answers: NDQ_003379

answers: "rift flanks".

answers: NDQ_003380

answers: tensile stresses

answers: NDQ_003381

answers: tensile stresses

answers: NDQ_003382

answers: tensile

answers: NDQ_003383

answers: tensile stresses

answers: NDQ_003384

answers: mountain ridges,

answers: NDQ_003385

answers: "rift flanks".

answers: NDQ_003386

answers: tensile stresses

answers: NDQ_003387

answers: tensile stresses

answers: NDQ_003388

answers: tensile stresses

answers: NDQ_003389

answers: mountain ridges,

answers: NDQ_003390

answers: tensile stresses

answers: NDQ_003391

answers: mountain ridges,

answers: NDQ_003392

answers: tensile stresses

answers: NDQ_003393

answers: mountain ridges,

answers: NDQ_003394

answers: "rift flanks".

answers: NDQ_003395

answers: tensile stresses

answers: NDQ_003396

answers: "rift flanks".

text: Folds' personal life has inspired several of his songs; the hit single "Brick", co-written with Darren Jessee, was based on the experience of Folds' girlfriend having an abortion while they were in high school. Folds initially refused to discuss the story behind "Brick," thinking it was too serious for a pop song, but he eventually confirmed the inspiration for the song during a show on his Ben Folds Live tour. His telling of the story is included on the "Brick" track on the album.

text: Folds' personal life has inspired several of his songs; the hit single "Brick", co-written with Darren Jessee, was based on the experience of Folds' girlfriend having an abortion while they were in high school. Folds initially refused to discuss the story behind "Brick," thinking it was too serious for a pop song, but he eventually confirmed the inspiration for the song during a show on his Ben Folds Live tour. His telling of the story is included on the "Brick" track on the album.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: is likely to crack

answers: NDQ_003353

answers: unanswerable

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: unanswerable

answers: NDQ_003356

answers: unbalance

answers: NDQ_003357

answers: Folds' girlfriend having an abortion while they were in high school

answers: NDQ_003358

answers: Brick

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: Folds initially refused to discuss the story behind "Brick," thinking it was too serious for a pop song

answers: NDQ_003363

answers: unanswerable

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: unanswerable

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: unanswerable

answers: NDQ_003381

answers: unanswerable

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: no

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: unanswerable

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: unanswerable

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: Brick

answers: NDQ_003392

answers: unanswerable

answers: NDQ_003393

answers: Brick

answers: NDQ_003394

answers: NDQ_003395

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: abortion

answers: NDQ_003352

answers: pop song,

answers: NDQ_003353

answers: "Brick",

answers: NDQ_003354

answers: Folds' personal life has inspired several of his songs;

answers: NDQ_003355

answers: "Brick",

answers: NDQ_003356

answers: "Brick",

answers: NDQ_003357

answers: Folds initially refused to discuss the story behind "Brick,"

answers: NDQ_003358

answers: "Brick",

answers: NDQ_003359

answers: "Brick",

answers: NDQ_003360

answers: abortion while they were in high school.

answers: NDQ_003362

answers: "Brick," thinking it was too serious for a pop song,

answers: NDQ_003363

answers: abortion while they were in high school.

answers: NDQ_003371

answers: "Brick", co-written with Darren Jessee,

answers: NDQ_003373

answers: "Brick",

answers: NDQ_003376

answers: Darren Jessee,

answers: NDQ_003378

answers: "Brick", co-written with Darren Jessee,

answers: NDQ_003379

answers: "Brick", co-written with Darren Jessee,

answers: NDQ_003380

answers: "Brick",

answers: NDQ_003381

answers: "Brick",

answers: NDQ_003382

answers: Darren Jessee,

answers: NDQ_003383

answers: "Brick",

answers: NDQ_003384

answers: "Brick", co-written with Darren Jessee,

answers: NDQ_003385

answers: "Brick", co-written with Darren Jessee,

answers: NDQ_003386

answers: "Brick", co-written with Darren Jessee,

answers: NDQ_003387

answers: "Brick", co-written with Darren Jessee,

answers: NDQ_003388

answers: "Brick", co-written with Darren Jessee,

answers: NDQ_003389

answers: "Brick",

answers: NDQ_003390

answers: "Brick",

answers: NDQ_003391

answers: "Brick",

answers: NDQ_003392

answers: "Brick",

answers: NDQ_003393

answers: "Brick",

answers: NDQ_003394

answers: "Brick", co-written with Darren Jessee,

answers: NDQ_003395

answers: "Brick", co-written with Darren Jessee,

answers: NDQ_003396

answers: "Brick", co-written with Darren Jessee,

text: The SCF offsets the older NNW striking Entiat, Ross Lake, and Chewack-Pasayten faults, but not certain younger features, the period of its strike-slip activity thus being bracketed between 47 and 41 million years ago (in the Eocene epoch), just after the wedge of crust now carrying the Olympic Mountains pushed into the continental margin.  It has been suggested that initiation of the SCF may be due to events on the Kula Plate.

text: The SCF offsets the older NNW striking Entiat, Ross Lake, and Chewack-Pasayten faults, but not certain younger features, the period of its strike-slip activity thus being bracketed between 47 and 41 million years ago (in the

text: Eocene

text: epoch), just after the wedge of crust now carrying the

text: Olympic Mountains

text: pushed into the continental margin.  It has been suggested that initiation of the SCF may be due to events on the

text: Kula Plate

answers: NDQ_003351

answers: strike-slip

answers: NDQ_003352

answers: more likely to crack

answers: NDQ_003353

answers: strike-slip

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fault

answers: NDQ_003356

answers: strike

answers: NDQ_003357

answers: the wedge of crust now carrying the Olympic Mountains pushed into the continental margin

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Kula Plate

answers: NDQ_003362

answers: older NNW striking Entiat, Ross Lake, and Chewack-Pasayten faults

answers: NDQ_003363

answers: Eocene

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: What type of stresses does a deeply buried rock have?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: what is the period of its strike-slip activity

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What type of stress does the SCF offsets?

answers: NDQ_003382

answers: what is the most common stress at convergent plates

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: Fault zone

answers: NDQ_003386

answers: strike-slip activity

answers: NDQ_003387

answers: What is the cause of normal faults?

answers: NDQ_003388

answers: What type of stress is shear stress?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: strike-slip

answers: NDQ_003391

answers: wedge

answers: NDQ_003392

answers: strike-slip

answers: NDQ_003393

answers: Olympic Mountains

answers: NDQ_003394

answers: Entiat

answers: NDQ_003395

answers: Chewack-Pasayten faults

answers: NDQ_003396

answers: strike-slip

answers: NDQ_003351

answers: strike-slip

answers: NDQ_003352

answers: strike-slip

answers: NDQ_003353

answers: faults,

answers: NDQ_003354

answers: The SCF

answers: NDQ_003355

answers: strike-slip

answers: NDQ_003356

answers: strike-slip

answers: NDQ_003357

answers: strike-slip

answers: NDQ_003358

answers: faults,

answers: NDQ_003359

answers: pushed into the continental margin.

answers: NDQ_003360

answers: The SCF

answers: NDQ_003362

answers: younger features,

answers: NDQ_003363

answers: Olympic Mountains pushed into the continental margin.

answers: NDQ_003371

answers: The SCF

answers: NDQ_003373

answers: The SCF

answers: NDQ_003376

answers: The SCF

answers: NDQ_003378

answers: strike-slip

answers: NDQ_003379

answers: Chewack-Pasayten

answers: NDQ_003380

answers: strike-slip

answers: NDQ_003381

answers: The SCF

answers: NDQ_003382

answers: The SCF

answers: NDQ_003383

answers: strike-slip

answers: NDQ_003384

answers: The SCF

answers: NDQ_003385

answers: Chewack-Pasayten faults,

answers: NDQ_003386

answers: strike-slip

answers: NDQ_003387

answers: The SCF

answers: NDQ_003388

answers: Kula Plate.

answers: NDQ_003389

answers: Olympic Mountains

answers: NDQ_003390

answers: Chewack-Pasayten faults,

answers: NDQ_003391

answers: wedge of crust now carrying the Olympic Mountains

answers: NDQ_003392

answers: Chewack-Pasayten faults,

answers: NDQ_003393

answers: Olympic Mountains

answers: NDQ_003394

answers: Chewack-Pasayten faults,

answers: NDQ_003395

answers: Chewack-Pasayten faults,

answers: NDQ_003396

answers: Chewack-Pasayten faults,

text: The process of Earth's increase in atmospheric oxygen content is theorized to have started with continent-continent collision of huge land masses forming supercontinents, and therefore possibly supercontinent mountain ranges (supermountains). These supermountains would have eroded, and the mass amounts of nutrients, including iron and phosphorus, would have washed into oceans, just as we see happening today. The oceans would then be rich in nutrients essential to photosynthetic organisms, which would then be able to respire mass amounts of oxygen. (1: continents collide, 2: 'supermountains' form, 3: erosion of 'supermountains,' 4: large quantities of minerals and nutrients washed out to open ocean, 5: explosion of marine algae life (partly sourced from noted nutrients), and 6: mass amounts of oxygen produced during photosynthesis. There is an apparent direct relationship between orogeny and the atmospheric oxygen content). There is also evidence for increased sedimentation concurrent with the timing of these mass oxygenation events, meaning that the organic carbon and pyrite at these times were more likely to be buried beneath sediment and therefore unable to react with the free oxygen. This sustained the atmospheric oxygen increases.

text: The process of Earth's increase in atmospheric oxygen content is theorized to have started with continent-continent collision of huge land masses forming supercontinents, and therefore possibly supercontinent mountain ranges (supermountains). These supermountains would have eroded, and the mass amounts of nutrients, including

text: iron

text: and

text: phosphorus

text: , would have washed into oceans, just as we see happening today. The oceans would then be rich in nutrients essential to photosynthetic organisms, which would then be able to respire mass amounts of oxygen. (1: continents collide, 2: 'supermountains' form, 3: erosion of 'supermountains,' 4: large quantities of minerals and nutrients washed out to open ocean, 5: explosion of marine algae life (partly sourced from noted nutrients), and 6: mass amounts of oxygen produced during photosynthesis. There is an apparent direct relationship between orogeny and the atmospheric oxygen content). There is also evidence for increased sedimentation concurrent with the timing of these mass oxygenation events, meaning that the organic carbon and

text: pyrite

text: at these times were more likely to be buried beneath sediment and therefore unable to react with the free oxygen. This sustained the atmospheric oxygen increases.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: erosion

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: supermountains

answers: NDQ_003356

answers: erode

answers: NDQ_003357

answers: organic carbon and pyrite are more likely to be buried beneath sediment and therefore unable to react with the free oxygen.

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: continent collision

answers: NDQ_003362

answers: there is an apparent direct relationship between orogeny and the atmospheric oxygen content

answers: NDQ_003363

answers: supercontinent collision

answers: NDQ_003371

answers: What is the process of Earth's increase in atmospheric oxygen content?

answers: NDQ_003373

answers: How would you describe a rock under compressive stresses?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What is the name of the process of Earth's increase in atmospheric oxygen content

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is the name of the fold that arches upward?

answers: NDQ_003385

answers: What is the name of the area where faults are clustered

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: Which of the following is not a cause of normal faults?

answers: NDQ_003388

answers: Which of the following is not a type of strike-slip fault?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: unanswerable

answers: NDQ_003392

answers: unanswerable

answers: NDQ_003393

answers: supermountains

answers: NDQ_003394

answers: isothermal

answers: NDQ_003395

answers: continent-continent collision

answers: NDQ_003396

answers: NDQ_003351

answers: sedimentation

answers: NDQ_003352

answers: eroded,

answers: NDQ_003353

answers: eroded,

answers: NDQ_003354

answers: supercontinent mountain ranges

answers: NDQ_003355

answers: of'supermountains,'

answers: NDQ_003356

answers: sedimentation

answers: NDQ_003357

answers: buried beneath sediment and therefore unable to react with the free oxygen.

answers: NDQ_003358

answers: (supermountains).

answers: NDQ_003359

answers: continent-continent collision

answers: NDQ_003360

answers: supercontinents,

answers: NDQ_003362

answers: supercontinent mountain ranges

answers: NDQ_003363

answers: supercontinents,

answers: NDQ_003371

answers: supercontinent mountain ranges

answers: NDQ_003373

answers: sediment and therefore unable to react with the free oxygen.

answers: NDQ_003376

answers: supercontinent mountain ranges

answers: NDQ_003378

answers: sedimentation

answers: NDQ_003379

answers: iron and phosphorus,

answers: NDQ_003380

answers: eroded,

answers: NDQ_003381

answers: sedimentation

answers: NDQ_003382

answers: sedimentation

answers: NDQ_003383

answers: eroded,

answers: NDQ_003384

answers: supercontinent mountain ranges

answers: NDQ_003385

answers: supercontinent mountain ranges

answers: NDQ_003386

answers: orogeny

answers: NDQ_003387

answers: The process of Earth's increase in atmospheric oxygen content

answers: NDQ_003388

answers: continent-continent collision

answers: NDQ_003389

answers: supercontinent mountain ranges

answers: NDQ_003390

answers: supercontinent mountain ranges

answers: NDQ_003391

answers: pyrite

answers: NDQ_003392

answers: supercontinent mountain ranges

answers: NDQ_003393

answers: pyrite

answers: NDQ_003394

answers: supercontinent mountain ranges

answers: NDQ_003395

answers: continent-continent collision of huge land masses

answers: NDQ_003396

answers: supercontinent mountain ranges

text: In other languages, however, there is no possibility for confusion. For example, the Chinese word for "U.S. national" is  () is derived from a word for the United States, , where  is an abbreviation for Yàměilìjiā ("America") and  is "country". The name for the American continents is , from  plus  ("continent"). Thus, a  is an American in the continent sense, and a  is an American in the U.S. sense.

text: In other languages, however, there is no possibility for confusion. For example, the

text: Chinese

text: word for "U.S. national" is  () is derived from a word for the United States, , where  is an abbreviation for Yàměilìjiā ("America") and  is "country". The name for the American continents is , from  plus  ("continent"). Thus, a  is an American in the continent sense, and a  is an American in the U.S. sense.

answers: NDQ_003351

answers: divergent plate

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: swells

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: swell

answers: NDQ_003357

answers: a is an American in the continent sense, and a is an American in the U.S. sense

answers: NDQ_003358

answers: rockfall

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: continents

answers: NDQ_003362

answers: a is an American in the U.S. sense

answers: NDQ_003363

answers: the same time

answers: NDQ_003371

answers: What is a thrust fault?

answers: NDQ_003373

answers: compressive stresses

answers: NDQ_003376

answers: basin-and-range

answers: NDQ_003378

answers: the amount the ground moves

answers: NDQ_003379

answers: strike-slip fault

answers: NDQ_003380

answers: What is a stress?

answers: NDQ_003381

answers: confining stress

answers: NDQ_003382

answers: what is the most common stress at convergent plates

answers: NDQ_003383

answers: The answer: Stress.

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: Fault zone

answers: NDQ_003386

answers: movement of rock

answers: NDQ_003387

answers: normal faults are caused by compression stress

answers: NDQ_003388

answers: strike-slip

answers: NDQ_003389

answers: process of folding

answers: NDQ_003390

answers: a fault

answers: NDQ_003391

answers: dip-slip fault

answers: NDQ_003392

answers: The hanging wall pushes up

answers: NDQ_003393

answers: dip-slip fault

answers: NDQ_003394

answers: a fault with a fault plane that is not vertical

answers: NDQ_003395

answers: a vertical fault plane

answers: NDQ_003396

answers: Fault plane

answers: NDQ_003351

answers: In other languages, however, there is no possibility for confusion.

answers: NDQ_003352

answers: In other languages, however, there is no possibility for confusion.

answers: NDQ_003353

answers: In other languages, however, there is no possibility for confusion.

answers: NDQ_003354

answers: In other languages, however, there is no possibility for confusion.

answers: NDQ_003355

answers: a

answers: NDQ_003356

answers: confusion.

answers: NDQ_003357

answers: confusion.

answers: NDQ_003358

answers: In other languages,

answers: NDQ_003359

answers: In other languages, however, there is no possibility for confusion.

answers: NDQ_003360

answers: In other languages, however, there is no possibility for confusion.

answers: NDQ_003362

answers: there is no possibility for confusion.

answers: NDQ_003363

answers: American continents is, from plus ("continent").

answers: NDQ_003371

answers: In other languages, however, there is no possibility for confusion.

answers: NDQ_003373

answers: In other languages, however, there is no possibility for confusion.

answers: NDQ_003376

answers: In other languages, however, there is no possibility for confusion.

answers: NDQ_003378

answers: In other languages, however, there is no possibility for confusion.

answers: NDQ_003379

answers: In other languages, however, there is no possibility for confusion.

answers: NDQ_003380

answers: In other languages, however, there is no possibility for confusion.

answers: NDQ_003381

answers: In other languages, however, there is no possibility for confusion.

answers: NDQ_003382

answers: In other languages, however, there is no possibility for confusion.

answers: NDQ_003383

answers: In other languages, however, there is no possibility for confusion.

answers: NDQ_003384

answers: In other languages, however, there is no possibility for confusion.

answers: NDQ_003385

answers: In other languages, however, there is no possibility for confusion.

answers: NDQ_003386

answers: In other languages, however, there is no possibility for confusion.

answers: NDQ_003387

answers: In other languages, however, there is no possibility for confusion.

answers: NDQ_003388

answers: In other languages, however, there is no possibility for confusion.

answers: NDQ_003389

answers: American continents is, from plus ("continent").

answers: NDQ_003390

answers: In other languages, however, there is no possibility for confusion.

answers: NDQ_003391

answers: In other languages, however, there is no possibility for confusion.

answers: NDQ_003392

answers: In other languages, however, there is no possibility for confusion.

answers: NDQ_003393

answers: In other languages, however, there is no possibility for confusion.

answers: NDQ_003394

answers: In other languages, however, there is no possibility for confusion.

answers: NDQ_003395

answers: In other languages, however, there is no possibility for confusion.

answers: NDQ_003396

answers: In other languages, however, there is no possibility for confusion.

text: The San Andreas Fault Observatory at Depth (SAFOD) consists of a main borehole that cuts across the active San Andreas Fault at a depth of approximately 3 km and a pilot hole about 2 km southwest of San Andreas Fault. Data from the instruments installed in the holes, which consist of geophone sensors, data acquisition systems, and GPS clocks, as well as samples collected during drilling, will help to better understand the processes that control the behavior of the San Andreas Fault.

text: The San Andreas Fault Observatory at Depth (SAFOD) consists of a main borehole that cuts across the active

text: San Andreas Fault

text: at a depth of approximately 3 km and a pilot hole about 2 km southwest of San Andreas Fault. Data from the instruments installed in the holes, which consist of

text: geophone

text: sensors, data acquisition systems, and GPS clocks, as well as samples collected during drilling, will help to better understand the processes that control the behavior of the San Andreas Fault.

answers: NDQ_003351

answers: San Andreas Fault

answers: NDQ_003352

answers: cracks

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: crack

answers: NDQ_003357

answers: depth of approximately 3 km

answers: NDQ_003358

answers: Fault

answers: NDQ_003359

answers: cracks

answers: NDQ_003360

answers: San Andreas fault

answers: NDQ_003362

answers: The San Andreas Fault Observatory at Depth (SAFOD) consists of a main borehole that cuts across the active San Andreas Fault

answers: NDQ_003363

answers: San Andreas Fault

answers: NDQ_003371

answers: San Andreas Fault

answers: NDQ_003373

answers: How would you describe the San Andreas Fault Observatory at Depth?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: What is the San Andreas Fault?

answers: NDQ_003379

answers: What type of fault is the San Andreas Fault Observatory at Depth?

answers: NDQ_003380

answers: What is the San Andreas Fault?

answers: NDQ_003381

answers: What is the San Andreas Fault Observatory at Depth?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the San Andreas Fault Observatory at Depth?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: What is the San Andreas Fault?

answers: NDQ_003387

answers: What is the San Andreas Fault?

answers: NDQ_003388

answers: San Andreas Fault Observatory at Depth (SAFOD)

answers: NDQ_003389

answers: unknown

answers: NDQ_003390

answers: San Andreas Fault

answers: NDQ_003391

answers: San Andreas Fault

answers: NDQ_003392

answers: San Andreas Fault

answers: NDQ_003393

answers: San Andreas Fault

answers: NDQ_003394

answers: San Andreas Fault

answers: NDQ_003395

answers: San Andreas Fault

answers: NDQ_003396

answers: San Andreas Fault

answers: NDQ_003351

answers: GPS clocks,

answers: NDQ_003352

answers: depth

answers: NDQ_003353

answers: San Andreas Fault

answers: NDQ_003354

answers: The San Andreas Fault Observatory at Depth

answers: NDQ_003355

answers: The San Andreas Fault Observatory at Depth

answers: NDQ_003356

answers: San Andreas Fault.

answers: NDQ_003357

answers: 3 km

answers: NDQ_003358

answers: active San Andreas Fault

answers: NDQ_003359

answers: San Andreas Fault

answers: NDQ_003360

answers: San Andreas Fault

answers: NDQ_003362

answers: active San Andreas Fault at a depth of approximately 3 km

answers: NDQ_003363

answers: San Andreas Fault

answers: NDQ_003371

answers: The San Andreas Fault

answers: NDQ_003373

answers: 3 km

answers: NDQ_003376

answers: The San Andreas Fault Observatory at Depth

answers: NDQ_003378

answers: 3 km

answers: NDQ_003379

answers: 3 km

answers: NDQ_003380

answers: 3 km

answers: NDQ_003381

answers: geophone sensors, data acquisition systems, and GPS clocks,

answers: NDQ_003382

answers: 3

answers: NDQ_003383

answers: geophone sensors, data acquisition systems, and GPS clocks,

answers: NDQ_003384

answers: 3 km

answers: NDQ_003385

answers: The San Andreas Fault

answers: NDQ_003386

answers: San Andreas Fault.

answers: NDQ_003387

answers: The San Andreas Fault

answers: NDQ_003388

answers: The San Andreas Fault

answers: NDQ_003389

answers: The San Andreas Fault

answers: NDQ_003390

answers: San Andreas Fault

answers: NDQ_003391

answers: San Andreas Fault

answers: NDQ_003392

answers: San Andreas Fault

answers: NDQ_003393

answers: San Andreas Fault

answers: NDQ_003394

answers: San Andreas Fault

answers: NDQ_003395

answers: San Andreas Fault

answers: NDQ_003396

answers: San Andreas Fault

text: If however, a large tract of ocean intervenes between the continental margin the subduction zone, a fully developed arc and back arc basin may eventually arrive and collide with the continental margin. Further convergence may lead to overthrusting of the volcanic arc assemblage and may be followed by flipping the subduction polarity.

text: If however, a large tract of ocean intervenes between the continental margin the subduction zone, a fully developed arc and back arc basin may eventually arrive and collide with the continental margin. Further convergence may lead to overthrusting of the volcanic arc assemblage and may be followed by flipping the subduction polarity.

answers: NDQ_003351

answers: overthrusting

answers: NDQ_003352

answers: is likely to crack

answers: NDQ_003353

answers: erosion

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: subduction zone

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: flipping the subduction polarity

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: cracks

answers: NDQ_003360

answers: subduction zones

answers: NDQ_003362

answers: a fully developed arc and back arc basin may eventually arrive at the continental margin

answers: NDQ_003363

answers: subduction zone

answers: NDQ_003371

answers: Which of the following is not an example of a thrust fault?

answers: NDQ_003373

answers: How would you describe compressive stresses?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: what is the first word in the first paragraph?

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What is a result of confining stress?

answers: NDQ_003382

answers: It's impossible to say

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: no

answers: NDQ_003385

answers: yes

answers: NDQ_003386

answers: What is the cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not a type of normal fault?

answers: NDQ_003388

answers: Which of the following is not a result of shear stress?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: subduction zone

answers: NDQ_003391

answers: subduction zone

answers: NDQ_003392

answers: subduction zone

answers: NDQ_003393

answers: subduction zone

answers: NDQ_003394

answers: isobath

answers: NDQ_003395

answers: is a fault

answers: NDQ_003396

answers: isobath

answers: NDQ_003351

answers: overthrusting of the volcanic arc assemblage

answers: NDQ_003352

answers: overthrusting

answers: NDQ_003353

answers: overthrusting

answers: NDQ_003354

answers: a large tract of ocean intervenes between the continental margin

answers: NDQ_003355

answers: arc

answers: NDQ_003356

answers: overthrusting

answers: NDQ_003357

answers: subduction polarity.

answers: NDQ_003358

answers: back arc basin

answers: NDQ_003359

answers: collide with the continental margin.

answers: NDQ_003360

answers: ocean intervenes between the continental margin the subduction zone,

answers: NDQ_003362

answers: a fully developed arc

answers: NDQ_003363

answers: subduction zone,

answers: NDQ_003371

answers: overthrusting of the volcanic arc assemblage

answers: NDQ_003373

answers: large tract of ocean intervenes between the continental margin the subduction zone,

answers: NDQ_003376

answers: a fully developed arc and back arc basin

answers: NDQ_003378

answers: subduction zone,

answers: NDQ_003379

answers: flipping the subduction polarity.

answers: NDQ_003380

answers: overthrusting

answers: NDQ_003381

answers: overthrusting of the volcanic arc assemblage

answers: NDQ_003382

answers: overthrusting of the volcanic arc assemblage

answers: NDQ_003383

answers: overthrusting

answers: NDQ_003384

answers: arc

answers: NDQ_003385

answers: subduction zone,

answers: NDQ_003386

answers: overthrusting of the volcanic arc assemblage

answers: NDQ_003387

answers: flipping the subduction polarity.

answers: NDQ_003388

answers: flipping the subduction polarity.

answers: NDQ_003389

answers: a fully developed arc

answers: NDQ_003390

answers: subduction zone,

answers: NDQ_003391

answers: subduction zone,

answers: NDQ_003392

answers: subduction zone,

answers: NDQ_003393

answers: arc

answers: NDQ_003394

answers: flipping the subduction polarity.

answers: NDQ_003395

answers: subduction zone,

answers: NDQ_003396

answers: back arc basin

text: The hippocampus contains high levels of glucocorticoid receptors, which make it more vulnerable to long-term stress than most other brain areas.  Stress-related steroids affect the hippocampus in at least three ways:  first, by reducing the excitability of some hippocampal neurons; second, by inhibiting the formation of new neurons in the dentate gyrus; third, by causing atrophy of dendrites in pyramidal cells of the CA3 region.  There is evidence that humans having experienced severe, long-lasting traumatic stress show atrophy of the hippocampus more than of other parts of the brain. These effects show up in post-traumatic stress disorder, and they may contribute to the hippocampal atrophy reported in schizophrenia and severe depression. A recent study has also revealed atrophy as a result of depression, but this can be stopped with anti-depressants even if they are not effective in relieving other symptoms. Hippocampal atrophy is also frequently seen in Cushing's syndrome, a disorder caused by high levels of cortisol in the bloodstream.  At least some of these effects appear to be reversible if the stress is discontinued.  There is, however, evidence derived mainly from studies using rats that stress occurring shortly after birth can affect hippocampal function in ways that persist throughout life.

text: The hippocampus contains high levels of

text: glucocorticoid receptor

text: s, which make it more vulnerable to long-term

text: stress

text: than most other

text: brain areas

text: Stress-related steroids

text: affect the hippocampus in at least three ways:  first, by reducing the

text: excitability

text: of some hippocampal neurons; second, by inhibiting the formation of new neurons in the dentate gyrus; third, by causing atrophy of dendrites in pyramidal cells of the CA3 region.  There is evidence that humans having experienced severe, long-lasting traumatic stress show atrophy of the hippocampus more than of other parts of the brain. These effects show up in

text: post-traumatic stress disorder

text: , and they may contribute to the hippocampal atrophy reported in

text: schizophrenia

text: and

text: severe depression

text: . A recent study has also revealed atrophy as a result of depression, but this can be stopped with anti-depressants even if they are not effective in relieving other symptoms. Hippocampal atrophy is also frequently seen in

text: Cushing's syndrome

text: , a disorder caused by high levels of

text: cortisol

text: in the bloodstream.  At least some of these effects appear to be reversible if the stress is discontinued.  There is, however, evidence derived mainly from studies using rats that stress occurring shortly after birth can affect hippocampal function in ways that persist throughout life.

answers: NDQ_003351

answers: Cushing's syndrome

answers: NDQ_003352

answers: atrophys

answers: NDQ_003353

answers: atrophy of dendrites

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: unanswerable

answers: NDQ_003356

answers: atrophy

answers: NDQ_003357

answers: dendrites in pyramidal cells of the CA3 region

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: humans having experienced severe, long-lasting traumatic stress show atrophy

answers: NDQ_003363

answers: Cushing's syndrome

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: What is the main idea of this passage?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: The dip of the fault plane is vertical

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: unanswerable

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: no

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: movement of rock at faults

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: normal faults or Cushing's syndrome?

answers: NDQ_003388

answers: Which of the following is not a cause of strike-slip faults: shear stress, depression, or traumatic stress?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: Cushing's syndrome

answers: NDQ_003391

answers: dip-slip fault plane

answers: NDQ_003392

answers: Cushing's syndrome

answers: NDQ_003393

answers: dip-slip fault plane

answers: NDQ_003394

answers: a fault

answers: NDQ_003395

answers: Hippocampal atrophy

answers: NDQ_003396

answers: Cushing's syndrome

answers: NDQ_003351

answers: traumatic stress

answers: NDQ_003352

answers: hippocampus

answers: NDQ_003353

answers: atrophy of dendrites

answers: NDQ_003354

answers: glucocorticoid receptors,

answers: NDQ_003355

answers: hippocampus

answers: NDQ_003356

answers: atrophy of the hippocampus

answers: NDQ_003357

answers: stress occurring shortly after birth can affect hippocampal function

answers: NDQ_003358

answers: The hippocampus

answers: NDQ_003359

answers: stress

answers: NDQ_003360

answers: stress

answers: NDQ_003362

answers: this can be stopped with anti-depressants

answers: NDQ_003363

answers: traumatic stress

answers: NDQ_003371

answers: The hippocampus

answers: NDQ_003373

answers: The hippocampus

answers: NDQ_003376

answers: Stress-related steroids

answers: NDQ_003378

answers: atrophy of the hippocampus

answers: NDQ_003379

answers: dentate gyrus;

answers: NDQ_003380

answers: traumatic stress

answers: NDQ_003381

answers: traumatic stress

answers: NDQ_003382

answers: traumatic stress

answers: NDQ_003383

answers: Stress-related steroids

answers: NDQ_003384

answers: The hippocampus

answers: NDQ_003385

answers: The hippocampus

answers: NDQ_003386

answers: The hippocampus

answers: NDQ_003387

answers: traumatic stress

answers: NDQ_003388

answers: The hippocampus

answers: NDQ_003389

answers: glucocorticoid receptors,

answers: NDQ_003390

answers: The hippocampus

answers: NDQ_003391

answers: hippocampus

answers: NDQ_003392

answers: The hippocampus

answers: NDQ_003393

answers: hippocampus

answers: NDQ_003394

answers: The hippocampus

answers: NDQ_003395

answers: The hippocampus

answers: NDQ_003396

answers: glucocorticoid receptors,

text: Isostatic depression is the sinking of large parts of the Earth's crust into the asthenosphere. The sinking is caused by a heavy  weight placed on the Earth's surface. Often this is caused by the heavy weight of glacial ice due to continental glaciation. This is a process in which permanent ice places pressure on the Earth's crust, thereby depressing it with its weight. After continental glaciation has receded,  it is common for isostatic rebound to occur.

text: Isostatic depression is the sinking of large parts of the Earth's

text: crust

text: into the

text: asthenosphere

text: . The sinking is caused by a heavy  weight placed on the Earth's surface. Often this is caused by the heavy weight of

text: glacial ice

text: due to

text: continent

text: al

text: glaciation

text: . This is a process in which permanent ice places pressure on the Earth's crust, thereby depressing it with its weight. After continental glaciation has receded,  it is common for

text: isostatic rebound

text: to occur.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: sinks

answers: NDQ_003353

answers: pressure on it

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: glacier

answers: NDQ_003356

answers: sink

answers: NDQ_003357

answers: sinking of large parts of the Earth's crust into the asthenosphere

answers: NDQ_003358

answers: isostatic

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: continental glaciation

answers: NDQ_003362

answers: sinking of large parts of the Earth's crust into the asthenosphere

answers: NDQ_003363

answers: continental glaciation

answers: NDQ_003371

answers: Which of the following is not a process in which permanent ice places pressure on the Earth's crust?

answers: NDQ_003373

answers: How would you describe the sinking of large parts of the Earth's crust

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What does the sinking of large parts of the Earth's crust cause?

answers: NDQ_003381

answers: What is the result of the sinking of large parts of the Earth's crust into the asthenosphere

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not a type of fold?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: Which of the following is not the cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: Isostatic depression or normal faults?

answers: NDQ_003388

answers: Which of the following is not a result of shear stress: strike-slip faults, isostatic depression, or rebound?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: isostatic rebound

answers: NDQ_003391

answers: isostatic rebound

answers: NDQ_003392

answers: isostatic rebound

answers: NDQ_003393

answers: isostatic rebound

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: isostatic rebound

answers: NDQ_003396

answers: horizontal

answers: NDQ_003351

answers: Isostatic depression

answers: NDQ_003352

answers: depressing it with its weight.

answers: NDQ_003353

answers: Isostatic depression

answers: NDQ_003354

answers: Isostatic depression

answers: NDQ_003355

answers: Isostatic depression

answers: NDQ_003356

answers: Isostatic depression

answers: NDQ_003357

answers: isostatic rebound

answers: NDQ_003358

answers: Isostatic depression

answers: NDQ_003359

answers: Isostatic depression

answers: NDQ_003360

answers: continental glaciation.

answers: NDQ_003362

answers: Isostatic depression

answers: NDQ_003363

answers: continental glaciation.

answers: NDQ_003371

answers: Isostatic depression

answers: NDQ_003373

answers: Isostatic depression

answers: NDQ_003376

answers: heavy weight of glacial ice

answers: NDQ_003378

answers: Isostatic depression

answers: NDQ_003379

answers: glacial ice due to continental glaciation.

answers: NDQ_003380

answers: pressure

answers: NDQ_003381

answers: heavy weight of glacial ice

answers: NDQ_003382

answers: glacial ice

answers: NDQ_003383

answers: Isostatic depression

answers: NDQ_003384

answers: Isostatic depression

answers: NDQ_003385

answers: Isostatic depression

answers: NDQ_003386

answers: Isostatic depression

answers: NDQ_003387

answers: Isostatic depression

answers: NDQ_003388

answers: glacial ice

answers: NDQ_003389

answers: Isostatic depression

answers: NDQ_003390

answers: Isostatic depression

answers: NDQ_003391

answers: glacial ice

answers: NDQ_003392

answers: Isostatic depression

answers: NDQ_003393

answers: glacial ice

answers: NDQ_003394

answers: Isostatic depression

answers: NDQ_003395

answers: Isostatic depression

answers: NDQ_003396

answers: Isostatic depression

text: The Mohorovičić discontinuity (), usually referred to as the Moho, is the boundary between the Earth's crust and the mantle. Named after the pioneering Croatian seismologist Andrija Mohorovičić, the Moho separates both the oceanic crust and continental crust from underlying mantle. The Moho lies almost entirely within the lithosphere; only beneath mid-ocean ridges does it define the lithosphere–asthenosphere boundary. The Mohorovičić discontinuity was first identified in 1909 by Mohorovičić, when he observed that seismograms from shallow-focus earthquakes had two sets of P-waves and S-waves, one that followed a direct path near the Earth's surface and the other refracted by a high-velocity medium.

text: The Mohorovičić discontinuity (), usually referred to as the Moho, is the boundary between the

text: Earth

text: 's

text: crust

text: and the

text: mantle

text: . Named after the pioneering

text: Croatian

text: seismologist

text: Andrija Mohorovičić

text: , the Moho separates both the

text: oceanic crust

text: and

text: continental crust

text: from underlying mantle. The Moho lies almost entirely within the

text: lithosphere

text: ; only beneath

text: mid-ocean ridge

text: s does it define the lithosphere–

text: asthenosphere

text: boundary. The Mohorovičić discontinuity was first identified in 1909 by Mohorovičić, when he observed that

text: seismogram

text: s from

text: shallow-focus

text: earthquake

text: s had two sets of

text: P-wave

text: s and

text: S-wave

text: s, one that followed a direct path near the Earth's surface and the other

text: refracted

text: by a high-velocity medium.

answers: NDQ_003351

answers: high-velocity medium

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: P-waves

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: Moho

answers: NDQ_003356

answers: separate from the mantle

answers: NDQ_003357

answers: Moho lies almost entirely within the lithosphere

answers: NDQ_003358

answers: Moho

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Moho

answers: NDQ_003362

answers: the Moho lies almost entirely within the lithosphere

answers: NDQ_003363

answers: Moho

answers: NDQ_003371

answers: What is the Mohorovi i discontinuity?

answers: NDQ_003373

answers: The Mohorovi i discontinuity

answers: NDQ_003376

answers: What is the Mohorovi i discontinuity

answers: NDQ_003378

answers: The Mohorovi i discontinuity

answers: NDQ_003379

answers: The Mohorovi i discontinuity

answers: NDQ_003380

answers: What is Mohorovi i discontinuity?

answers: NDQ_003381

answers: What is the Moho?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the Mohorovi i discontinuity?

answers: NDQ_003384

answers: What is the Mohorovi i discontinuity?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: movement of rock at faults

answers: NDQ_003387

answers: What is the Mohorovi i discontinuity?

answers: NDQ_003388

answers: What is the Mohorovi i discontinuity?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: Mohorovi

answers: NDQ_003391

answers: lithosphere

answers: NDQ_003392

answers: Mohorovi

answers: NDQ_003393

answers: lithosphere

answers: NDQ_003394

answers: Moho

answers: NDQ_003395

answers: Mohorovi

answers: NDQ_003396

answers: Moho

answers: NDQ_003351

answers: P-waves and S-waves,

answers: NDQ_003352

answers: refracted by a high-velocity medium.

answers: NDQ_003353

answers: earthquakes had two sets of P-waves and S-waves,

answers: NDQ_003354

answers: The Mohorovi<unk>i<unk> discontinuity

answers: NDQ_003355

answers: ridges

answers: NDQ_003356

answers: earthquakes had two sets of P-waves and S-waves,

answers: NDQ_003357

answers: two sets of P-waves and S-waves,

answers: NDQ_003358

answers: Mohorovi<unk>i<unk> discontinuity

answers: NDQ_003359

answers: high-velocity medium.

answers: NDQ_003360

answers: Mohorovi<unk>i<unk> discontinuity

answers: NDQ_003362

answers: direct path near the Earth's surface

answers: NDQ_003363

answers: mid-ocean ridges

answers: NDQ_003371

answers: The Mohorovi<unk>i<unk> discontinuity

answers: NDQ_003373

answers: underlying mantle.

answers: NDQ_003376

answers: The Mohorovi<unk>i<unk> discontinuity

answers: NDQ_003378

answers: The Mohorovi<unk>i<unk> discontinuity

answers: NDQ_003379

answers: mid-ocean ridges

answers: NDQ_003380

answers: The Mohorovi<unk>i<unk> discontinuity

answers: NDQ_003381

answers: underlying mantle.

answers: NDQ_003382

answers: high-velocity medium.

answers: NDQ_003383

answers: high-velocity medium.

answers: NDQ_003384

answers: mid-ocean ridges

answers: NDQ_003385

answers: The Mohorovi<unk>i<unk> discontinuity

answers: NDQ_003386

answers: The Mohorovi<unk>i<unk> discontinuity

answers: NDQ_003387

answers: high-velocity medium.

answers: NDQ_003388

answers: high-velocity medium.

answers: NDQ_003389

answers: mid-ocean ridges

answers: NDQ_003390

answers: Mohorovi<unk>i<unk> discontinuity

answers: NDQ_003391

answers: mid-ocean ridges

answers: NDQ_003392

answers: Mohorovi<unk>i<unk> discontinuity

answers: NDQ_003393

answers: mid-ocean ridges

answers: NDQ_003394

answers: Mohorovi<unk>i<unk> discontinuity

answers: NDQ_003395

answers: Mohorovi<unk>i<unk> discontinuity

answers: NDQ_003396

answers: Mohorovi<unk>i<unk> discontinuity

text: One method of avoiding stress fractures is to add more stress to the bones. Though this may seem counter-intuitive (because stress fractures are caused by too much stress on the bone), moderate stress applied to the bone in a controlled manner can strengthen the bone and make it less susceptible to a stress fracture. An easy way to do this is to follow the runner's rule of increasing distance by no more than 10 percent per week. This allows the bones to adapt to the added stress so they are able to withstand greater stress in the future.

text: One method of avoiding stress fractures is to add more stress to the bones. Though this may seem counter-intuitive (because stress fractures are caused by too much stress on the bone), moderate stress applied to the bone in a controlled manner can strengthen the bone and make it less susceptible to a stress fracture. An easy way to do this is to follow the runner's rule of increasing distance by no more than 10 percent per week. This allows the bones to adapt to the added stress so they are able to withstand greater stress in the future.

answers: NDQ_003351

answers: stress fractures

answers: NDQ_003352

answers: fractures

answers: NDQ_003353

answers: stress fractures

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: stress fractures are caused by how much stress?

answers: NDQ_003358

answers: stress fracture

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: stress fractures are caused by too much stress on the bone

answers: NDQ_003363

answers: the same time

answers: NDQ_003371

answers: Which of the following is not a type of stress fracture?

answers: NDQ_003373

answers: How would you describe the stress of a rock?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: Which of the following is not a stress?

answers: NDQ_003381

answers: Which of the following is not a type of stress?

answers: NDQ_003382

answers: what is the most common stress at convergent plates

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: Which of the following is not a type of fold?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: Which of the following is not a cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not a cause of normal faults?

answers: NDQ_003388

answers: Which of the following is not a type of stress: strike-slip faults, shear stress, or stress fractures?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: stress fractures

answers: NDQ_003391

answers: a dip-slip fault

answers: NDQ_003392

answers: stress fractures

answers: NDQ_003393

answers: a dip-slip fault

answers: NDQ_003394

answers: is a

answers: NDQ_003395

answers: is a

answers: NDQ_003396

answers: NDQ_003351

answers: stress fractures

answers: NDQ_003352

answers: stress fracture.

answers: NDQ_003353

answers: stress fracture.

answers: NDQ_003354

answers: One method of avoiding stress fractures

answers: NDQ_003355

answers: stress fractures

answers: NDQ_003356

answers: stress fractures

answers: NDQ_003357

answers: increasing distance by no more than 10 percent per week.

answers: NDQ_003358

answers: stress fractures

answers: NDQ_003359

answers: too much stress

answers: NDQ_003360

answers: stress

answers: NDQ_003362

answers: One method of avoiding stress fractures is to add more stress

answers: NDQ_003363

answers: stress

answers: NDQ_003371

answers: runner's rule of increasing distance by no more than 10 percent per week.

answers: NDQ_003373

answers: runner's rule of increasing distance by no more than 10 percent per week.

answers: NDQ_003376

answers: 10 percent per week.

answers: NDQ_003378

answers: 10 percent per week.

answers: NDQ_003379

answers: 10 percent per week.

answers: NDQ_003380

answers: bones.

answers: NDQ_003381

answers: runner's rule of increasing distance by no more than 10 percent per week.

answers: NDQ_003382

answers: runner's rule of increasing distance by no more than 10 percent per week.

answers: NDQ_003383

answers: bones.

answers: NDQ_003384

answers: runner's rule of increasing distance by no more than 10 percent per week.

answers: NDQ_003385

answers: One method of avoiding stress fractures

answers: NDQ_003386

answers: runner's rule of increasing distance by no more than 10 percent per week.

answers: NDQ_003387

answers: stress fractures

answers: NDQ_003388

answers: too much stress on the bone),

answers: NDQ_003389

answers: One method of avoiding stress fractures

answers: NDQ_003390

answers: stress fractures

answers: NDQ_003391

answers: stress fractures

answers: NDQ_003392

answers: stress fractures

answers: NDQ_003393

answers: stress fractures

answers: NDQ_003394

answers: One method of avoiding stress fractures

answers: NDQ_003395

answers: 10 percent per week.

answers: NDQ_003396

answers: 10 percent per week.

text: Bombay Beach marks the southern end of the San Andreas fault.

text: Bombay Beach marks the southern end of the San Andreas fault.

answers: NDQ_003351

answers: lateral

answers: NDQ_003352

answers: is likely to crack

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: San Andreas fault

answers: NDQ_003356

answers: swell

answers: NDQ_003357

answers: Bombay Beach would be

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: is pushed together

answers: NDQ_003360

answers: faults

answers: NDQ_003362

answers: Bombay Beach marks the northern end of the San Andreas fault

answers: NDQ_003363

answers: San Andreas fault

answers: NDQ_003371

answers: Which of the following is not a type of fault?

answers: NDQ_003373

answers: What would happen to the rock if the San Andreas fault was deeper?

answers: NDQ_003376

answers: (iv)

answers: NDQ_003378

answers: What is the San Andreas fault?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: How would you describe the San Andreas fault?

answers: NDQ_003381

answers: What will happen to Bombay Beach?

answers: NDQ_003382

answers: Which of the following is not a type of stress?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not a type of fold?

answers: NDQ_003385

answers: (iv)

answers: NDQ_003386

answers: [iv]

answers: NDQ_003387

answers: What is the San Andreas fault?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip or strike-slip fault?

answers: NDQ_003389

answers: None of the above choices.

answers: NDQ_003390

answers: San Andreas fault

answers: NDQ_003391

answers: is a fault

answers: NDQ_003392

answers: San Andreas fault

answers: NDQ_003393

answers: sand

answers: NDQ_003394

answers: San Andreas fault

answers: NDQ_003395

answers: San Andreas fault

answers: NDQ_003396

answers: vertical fault

answers: NDQ_003351

answers: San Andreas fault.

answers: NDQ_003352

answers: Bombay Beach

answers: NDQ_003353

answers: San Andreas fault.

answers: NDQ_003354

answers: Bombay Beach marks the southern end of the San Andreas fault.

answers: NDQ_003355

answers: fault.

answers: NDQ_003356

answers: Bombay Beach

answers: NDQ_003357

answers: southern end

answers: NDQ_003358

answers: Beach

answers: NDQ_003359

answers: San Andreas fault.

answers: NDQ_003360

answers: San Andreas fault.

answers: NDQ_003362

answers: Bombay Beach marks the southern end

answers: NDQ_003363

answers: San Andreas fault.

answers: NDQ_003371

answers: San Andreas fault.

answers: NDQ_003373

answers: Bombay Beach marks the southern end of the San Andreas fault.

answers: NDQ_003376

answers: Bombay Beach marks the southern end of the San Andreas fault.

answers: NDQ_003378

answers: Bombay Beach marks the southern end of the San Andreas fault.

answers: NDQ_003379

answers: Bombay Beach

answers: NDQ_003380

answers: Bombay Beach marks the southern end of the San Andreas fault.

answers: NDQ_003381

answers: Bombay Beach marks the southern end of the San Andreas fault.

answers: NDQ_003382

answers: Bombay Beach marks the southern end of the San Andreas fault.

answers: NDQ_003383

answers: Bombay Beach marks the southern end of the San Andreas fault.

answers: NDQ_003384

answers: Bombay Beach marks the southern end of the San Andreas fault.

answers: NDQ_003385

answers: Bombay Beach marks the southern end of the San Andreas fault.

answers: NDQ_003386

answers: San Andreas fault.

answers: NDQ_003387

answers: Bombay Beach marks the southern end of the San Andreas fault.

answers: NDQ_003388

answers: Bombay Beach marks the southern end of the San Andreas fault.

answers: NDQ_003389

answers: San Andreas fault.

answers: NDQ_003390

answers: San Andreas fault.

answers: NDQ_003391

answers: Bombay Beach

answers: NDQ_003392

answers: San Andreas fault.

answers: NDQ_003393

answers: Bombay Beach

answers: NDQ_003394

answers: San Andreas

answers: NDQ_003395

answers: San Andreas

answers: NDQ_003396

answers: San Andreas

text: Folds form under varied conditions of stress, hydrostatic pressure, pore pressure, and temperature gradient, as evidenced by their presence in soft sediments, the full spectrum of metamorphic rocks, and even as primary flow structures in some igneous rocks. A set of folds distributed on a regional scale constitutes a fold belt, a common feature of orogenic zones. Folds are commonly formed by shortening of existing layers, but may also be formed as a result of displacement on a non-planar fault (fault bend fold), at the tip of a propagating fault (fault propagation fold), by differential compaction or due to the effects of a high-level igneous intrusion e.g. above a laccolith.

text: Folds form under varied conditions of

text: stress

text: hydrostatic pressure

text: pore pressure

text: , and

text: temperature gradient

text: , as evidenced by their presence in soft

text: sediments

text: , the full spectrum of

text: metamorphic rocks

text: , and even as primary flow structures in some

text: igneous rocks

text: . A set of folds distributed on a regional scale constitutes a fold belt, a common feature of

text: orogenic zones

text: . Folds are commonly formed by shortening of existing layers, but may also be formed as a result of displacement on a non-planar

text: fault

text: (fault bend fold), at the tip of a propagating fault (fault propagation fold), by differential

text: compaction

text: or due to the effects of a high-level

text: igneous

text: intrusion

text: e.g. above a

text: laccolith

answers: NDQ_003351

answers: hydrostatic pressure

answers: NDQ_003352

answers: folds

answers: NDQ_003353

answers: hydrostatic pressure

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fault bend fold

answers: NDQ_003356

answers: fold

answers: NDQ_003357

answers: pore pressure

answers: NDQ_003358

answers: laccolith

answers: NDQ_003359

answers: displaces

answers: NDQ_003360

answers: faults

answers: NDQ_003362

answers: the San Andreas fault is a non-planar fault

answers: NDQ_003363

answers: orogenic zones

answers: NDQ_003371

answers: What may be formed as a result of displacement on a non-planar fault

answers: NDQ_003373

answers: What type of stresses do folds form under?

answers: NDQ_003376

answers: differential compaction

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What is a stress?

answers: NDQ_003381

answers: What is a common feature of orogenic zones

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: fold belt

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: Which of the following is not a type of fold: strike-slip fault, non-planar fault, or non-planar fault?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: non-planar fault

answers: NDQ_003391

answers: laccolith

answers: NDQ_003392

answers: non-planar fault

answers: NDQ_003393

answers: laccolith

answers: NDQ_003394

answers: non-planar fault

answers: NDQ_003395

answers: non-planar

answers: NDQ_003396

answers: non-planar fault

answers: NDQ_003351

answers: hydrostatic pressure,

answers: NDQ_003352

answers: Folds

answers: NDQ_003353

answers: shortening of existing layers,

answers: NDQ_003354

answers: above a laccolith.

answers: NDQ_003355

answers: (fault bend fold),

answers: NDQ_003356

answers: shortening of existing layers,

answers: NDQ_003357

answers: shortening of existing layers,

answers: NDQ_003358

answers: laccolith.

answers: NDQ_003359

answers: displacement on a non-planar fault

answers: NDQ_003360

answers: Folds

answers: NDQ_003362

answers: laccolith.

answers: NDQ_003363

answers: orogenic zones.

answers: NDQ_003371

answers: (fault bend fold),

answers: NDQ_003373

answers: Folds

answers: NDQ_003376

answers: laccolith.

answers: NDQ_003378

answers: displacement

answers: NDQ_003379

answers: non-planar fault

answers: NDQ_003380

answers: stress, hydrostatic pressure,

answers: NDQ_003381

answers: Folds form under varied conditions of stress, hydrostatic pressure,

answers: NDQ_003382

answers: differential compaction

answers: NDQ_003383

answers: Folds form under varied conditions of stress,

answers: NDQ_003384

answers: fold belt,

answers: NDQ_003385

answers: fold belt,

answers: NDQ_003386

answers: displacement on a non-planar fault

answers: NDQ_003387

answers: Folds form under varied conditions of stress, hydrostatic pressure,

answers: NDQ_003388

answers: Folds form under varied conditions of stress, hydrostatic pressure,

answers: NDQ_003389

answers: Folds

answers: NDQ_003390

answers: (fault bend fold),

answers: NDQ_003391

answers: laccolith.

answers: NDQ_003392

answers: (fault bend fold),

answers: NDQ_003393

answers: laccolith.

answers: NDQ_003394

answers: (fault bend fold),

answers: NDQ_003395

answers: (fault bend fold),

answers: NDQ_003396

answers: (fault bend fold),

text: Silicon is a naturally occurring mineral and the second most abundant element in the earth's crust. In the soil, silicon attaches to soil colloids, helping to reduce compaction and making tied-up nutrients more available. Silicon also allows for a faster, more efficient movement of calcium and magnesium through the soil and readily ties up toxic elements, like aluminium, reducing metal toxicity. In the plant, silicon stengthens cell walls; improving plant strength, health, and productivity. Although not considered an essential element for plant growth and development, silicon is considered a beneficial element in many countries throughout the world due to its many benefits to numerous plant species when under abiotic or biotic stresses. Silicon is currently under consideration by the Association of American Plant Food Control Officials (AAPFCO) for elevation to the status of a "plant beneficial substance."

text: Silicon is a naturally occurring

text: mineral

text: and the second most abundant

text: element

text: in the earth's crust. In the

text: soil

text: , silicon attaches to soil

text: colloids

text: , helping to reduce compaction and making tied-up

text: nutrients

text: more available. Silicon also allows for a faster, more efficient movement of calcium and magnesium through the soil and readily ties up toxic elements, like

text: aluminium

text: , reducing metal toxicity. In the plant, silicon stengthens cell walls; improving plant strength, health, and productivity. Although not considered an essential element for plant growth and development, silicon is considered a beneficial element in many countries throughout the world due to its many benefits to numerous plant species when under

text: abiotic

text: or

text: biotic stress

text: es. Silicon is currently under consideration by the Association of American Plant Food Control Officials (AAPFCO) for elevation to the status of a "plant beneficial substance."

answers: NDQ_003351

answers: abiotic

answers: NDQ_003352

answers: can become more brittle

answers: NDQ_003353

answers: unanswerable

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: fold that bends downward

answers: NDQ_003356

answers: untighten

answers: NDQ_003357

answers: silicon attaches to soil colloids, helping to reduce compaction

answers: NDQ_003358

answers: unanswerable

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: silicon is considered a beneficial element in many countries throughout the world

answers: NDQ_003363

answers: Earth's crust

answers: NDQ_003371

answers: What is the second most abundant element in the earth's crust?

answers: NDQ_003373

answers: unanswerable

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What is the second most abundant element in the earth's crust?

answers: NDQ_003381

answers: What is the second most abundant element in the earth's crust?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: what is the second most abundant element in the earth's crust?

answers: NDQ_003388

answers: what is the second most abundant element in the earth's crust?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: unanswerable

answers: NDQ_003392

answers: unanswerable

answers: NDQ_003393

answers: unanswerable

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: unanswerable

answers: NDQ_003396

answers: abiotic

answers: NDQ_003351

answers: abiotic or biotic

answers: NDQ_003352

answers: silicon

answers: NDQ_003353

answers: compaction

answers: NDQ_003354

answers: Silicon

answers: NDQ_003355

answers: cell walls;

answers: NDQ_003356

answers: silicon attaches to soil colloids, helping to reduce compaction

answers: NDQ_003357

answers: silicon

answers: NDQ_003358

answers: compaction

answers: NDQ_003359

answers: stresses.

answers: NDQ_003360

answers: Silicon

answers: NDQ_003362

answers: Silicon

answers: NDQ_003363

answers: Silicon

answers: NDQ_003371

answers: Silicon

answers: NDQ_003373

answers: abiotic or biotic stresses.

answers: NDQ_003376

answers: compaction

answers: NDQ_003378

answers: compaction

answers: NDQ_003379

answers: silicon

answers: NDQ_003380

answers: abiotic or biotic stresses.

answers: NDQ_003381

answers: reducing metal toxicity.

answers: NDQ_003382

answers: compaction

answers: NDQ_003383

answers: abiotic or biotic stresses.

answers: NDQ_003384

answers: silicon attaches to soil colloids,

answers: NDQ_003385

answers: Silicon

answers: NDQ_003386

answers: Silicon

answers: NDQ_003387

answers: abiotic or biotic stresses.

answers: NDQ_003388

answers: silicon

answers: NDQ_003389

answers: Silicon

answers: NDQ_003390

answers: stresses.

answers: NDQ_003391

answers: Silicon

answers: NDQ_003392

answers: Silicon

answers: NDQ_003393

answers: Silicon

answers: NDQ_003394

answers: Silicon

answers: NDQ_003395

answers: Silicon

answers: NDQ_003396

answers: Silicon

text: See the main article on faults for a fuller treatment of fault types and nomenclature but in brief, the main types are normal faults, reverse faults, thrusts or thrust faults and strike-slip faults.

text: See the

text: main article on faults

text: for a fuller treatment of fault types and nomenclature but in brief, the main types are normal faults, reverse faults, thrusts or thrust faults and strike-slip faults.

answers: NDQ_003351

answers: strike-slip

answers: NDQ_003352

answers: increases in size.

answers: NDQ_003353

answers: Faults

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: normal fault

answers: NDQ_003356

answers: change shape

answers: NDQ_003357

answers: normal faults are caused by the movement of tectonic plates

answers: NDQ_003358

answers: normal fault

answers: NDQ_003359

answers: fractures.

answers: NDQ_003360

answers: faults

answers: NDQ_003362

answers: The San Andreas fault is a normal fault.

answers: NDQ_003363

answers: Striking faults

answers: NDQ_003371

answers: Which of the following is not a type of fault?

answers: NDQ_003373

answers: Which of the following is not a type of fault: normal faults, reverse faults, thrusts, or thrust faults?

answers: NDQ_003376

answers: Basin-and-range terrain is caused by compressive forces

answers: NDQ_003378

answers: Strike-slip faults

answers: NDQ_003379

answers: The dip of the fault plane is vertical.

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What type of stress does a normal fault have?

answers: NDQ_003382

answers: Compression is the most common stress at what plate boundary?

answers: NDQ_003383

answers: What is the main cause of joints in rock?

answers: NDQ_003384

answers: A syncline is a fold that arches upward.

answers: NDQ_003385

answers: What is the term for an area where faults are clustered?

answers: NDQ_003386

answers: The movement of rock at faults is the cause of

answers: NDQ_003387

answers: Normal faults are caused by compression stress.

answers: NDQ_003388

answers: What type of faults result from shear stress?

answers: NDQ_003389

answers: faults

answers: NDQ_003390

answers: thrust faults

answers: NDQ_003391

answers: strike-slip fault

answers: NDQ_003392

answers: thrust fault

answers: NDQ_003393

answers: strike-slip

answers: NDQ_003394

answers: normal faults

answers: NDQ_003395

answers: Strike-slip

answers: NDQ_003396

answers: thrust faults

answers: NDQ_003351

answers: strike-slip faults.

answers: NDQ_003352

answers: strike-slip faults.

answers: NDQ_003353

answers: faults

answers: NDQ_003354

answers: faults

answers: NDQ_003355

answers: thrusts

answers: NDQ_003356

answers: strike-slip faults.

answers: NDQ_003357

answers: thrusts or thrust faults and strike-slip faults.

answers: NDQ_003358

answers: strike-slip faults.

answers: NDQ_003359

answers: strike-slip faults.

answers: NDQ_003360

answers: faults

answers: NDQ_003362

answers: the main types are normal faults,

answers: NDQ_003363

answers: faults

answers: NDQ_003371

answers: thrusts

answers: NDQ_003373

answers: faults

answers: NDQ_003376

answers: strike-slip faults.

answers: NDQ_003378

answers: strike-slip faults.

answers: NDQ_003379

answers: strike-slip faults.

answers: NDQ_003380

answers: faults

answers: NDQ_003381

answers: strike-slip faults.

answers: NDQ_003382

answers: strike-slip faults.

answers: NDQ_003383

answers: faults

answers: NDQ_003384

answers: strike-slip faults.

answers: NDQ_003385

answers: strike-slip faults.

answers: NDQ_003386

answers: strike-slip faults.

answers: NDQ_003387

answers: normal faults,

answers: NDQ_003388

answers: strike-slip faults.

answers: NDQ_003389

answers: faults

answers: NDQ_003390

answers: strike-slip faults.

answers: NDQ_003391

answers: strike-slip faults.

answers: NDQ_003392

answers: thrusts or thrust faults and strike-slip faults.

answers: NDQ_003393

answers: strike-slip faults.

answers: NDQ_003394

answers: strike-slip faults.

answers: NDQ_003395

answers: strike-slip faults.

answers: NDQ_003396

answers: reverse faults,

text: Physiographically the district, which lies in a region of tectonic or folded and overthrust mountain chains, has strata are structurally marked by complex folds, reverse faults, overthrusts and nappes of great dimensions, all these as well as frequent earthquake of varying intensity give region to believe that the region is still unstable. Although any movement or tremor of the Earth's crust in the district is not produced by volcanic activity, the Chaukhamba peak a pair to be the crater of an extinct volcano.

text: Physiographically the district, which lies in a region of tectonic or folded and overthrust mountain chains, has strata are structurally marked by complex folds, reverse faults, overthrusts and nappes of great dimensions, all these as well as frequent earthquake of varying intensity give region to believe that the region is still unstable. Although any movement or tremor of the Earth's crust in the district is not produced by volcanic activity, the Chaukhamba peak a pair to be the crater of an extinct volcano.

answers: NDQ_003351

answers: overthrusts

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: movement

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: fold

answers: NDQ_003357

answers: overthrusts

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: tectonic plates

answers: NDQ_003362

answers: any movement or tremor of the Earth's crust is not produced by volcanic activity

answers: NDQ_003363

answers: tectonic

answers: NDQ_003371

answers: Which of the following is not a type of fold: complex folds, reverse faults, overthrusts and nappes of great dimensions?

answers: NDQ_003373

answers: None of the above choices.

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: what is the last word in the passage?

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What is the main idea of the passage?

answers: NDQ_003381

answers: what is the last word in the passage?

answers: NDQ_003382

answers: what is the most common stress at convergent plates

answers: NDQ_003383

answers: None of the above choices.

answers: NDQ_003384

answers: what is the first type of fold mentioned?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: yes

answers: NDQ_003387

answers: None of the above choices.

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip faults, overthrusts or nappes?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: overthrusts

answers: NDQ_003391

answers: strata

answers: NDQ_003392

answers: reverse faults

answers: NDQ_003393

answers: strata

answers: NDQ_003394

answers: reverse faults

answers: NDQ_003395

answers: reverse faults

answers: NDQ_003396

answers: overthrusts

answers: NDQ_003351

answers: earthquake

answers: NDQ_003352

answers: unstable.

answers: NDQ_003353

answers: folds, reverse faults,

answers: NDQ_003354

answers: tectonic or folded and overthrust mountain chains,

answers: NDQ_003355

answers: nappes

answers: NDQ_003356

answers: earthquake

answers: NDQ_003357

answers: reverse faults,

answers: NDQ_003358

answers: crater of an extinct volcano.

answers: NDQ_003359

answers: reverse faults,

answers: NDQ_003360

answers: tectonic

answers: NDQ_003362

answers: extinct volcano.

answers: NDQ_003363

answers: tectonic

answers: NDQ_003371

answers: reverse faults,

answers: NDQ_003373

answers: complex folds,

answers: NDQ_003376

answers: tectonic or folded and overthrust mountain chains,

answers: NDQ_003378

answers: tremor of the Earth's crust

answers: NDQ_003379

answers: reverse faults,

answers: NDQ_003380

answers: tremor

answers: NDQ_003381

answers: tectonic or folded and overthrust mountain chains,

answers: NDQ_003382

answers: folded and overthrust mountain chains,

answers: NDQ_003383

answers: complex folds,

answers: NDQ_003384

answers: tectonic or folded and overthrust mountain chains,

answers: NDQ_003385

answers: reverse faults,

answers: NDQ_003386

answers: volcanic activity,

answers: NDQ_003387

answers: reverse faults,

answers: NDQ_003388

answers: reverse faults,

answers: NDQ_003389

answers: tectonic

answers: NDQ_003390

answers: reverse faults,

answers: NDQ_003391

answers: nappes

answers: NDQ_003392

answers: reverse faults,

answers: NDQ_003393

answers: nappes

answers: NDQ_003394

answers: reverse faults,

answers: NDQ_003395

answers: reverse faults,

answers: NDQ_003396

answers: reverse faults,

text: Also, many continents can consist of several continental cratons - blocks of crust built around an initial original core of continents, that gradually grew and expanded as additional newly created terranes were added to their edges. For instance, Pangea consisted of most of the Earth's continents being accreted into one giant supercontinent. Most continents indeed have several continental cratons, in other words they are made up of the accretion of many smaller continents, such as Asia, Africa, and Europe.

text: Also, many continents can consist of several continental

text: craton

text: s - blocks of crust built around an initial original core of continents, that gradually grew and expanded as additional newly created terranes were added to their edges. For instance,

text: Pangea

text: consisted of most of the Earth's continents being accreted into one giant

text: supercontinent

text: . Most continents indeed have several continental cratons, in other words they are made up of the accretion of many smaller continents, such as

text: Asia

text: Africa

text: , and

text: Europe

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: cratons to expand

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: grow and expand

answers: NDQ_003357

answers: continents can consist of several continental cratons

answers: NDQ_003358

answers: craton

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: continents

answers: NDQ_003362

answers: most of the Earth's continents being accreted into one giant supercontinent

answers: NDQ_003363

answers: Pangea

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: how would you describe compressive stresses?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: What is the amount the ground moves in an earthquake?

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What happens to rock when confining stress occurs?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: fault zone

answers: NDQ_003386

answers: movement of rock at faults

answers: NDQ_003387

answers: Which of the following is not a cause of normal faults?

answers: NDQ_003388

answers: What type of stress is shear stress?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: craton

answers: NDQ_003391

answers: cratons

answers: NDQ_003392

answers: craton

answers: NDQ_003393

answers: cratons

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: a vertical fault plane

answers: NDQ_003396

answers: NDQ_003351

answers: continental cratons

answers: NDQ_003352

answers: grew and expanded

answers: NDQ_003353

answers: grew and expanded

answers: NDQ_003354

answers: many continents can consist of several continental cratons

answers: NDQ_003355

answers: continental cratons

answers: NDQ_003356

answers: grew and expanded

answers: NDQ_003357

answers: newly created terranes were added to their edges.

answers: NDQ_003358

answers: continental cratons

answers: NDQ_003359

answers: additional newly created terranes were added to their edges.

answers: NDQ_003360

answers: continental cratons

answers: NDQ_003362

answers: one giant supercontinent.

answers: NDQ_003363

answers: Pangea

answers: NDQ_003371

answers: many continents can consist of several continental cratons

answers: NDQ_003373

answers: continental cratons

answers: NDQ_003376

answers: continental cratons

answers: NDQ_003378

answers: continental cratons

answers: NDQ_003379

answers: continental cratons

answers: NDQ_003380

answers: continental cratons

answers: NDQ_003381

answers: continental cratons

answers: NDQ_003382

answers: continental cratons

answers: NDQ_003383

answers: continental cratons

answers: NDQ_003384

answers: continental cratons

answers: NDQ_003385

answers: continental cratons

answers: NDQ_003386

answers: continental cratons

answers: NDQ_003387

answers: many continents can consist of several continental cratons

answers: NDQ_003388

answers: continental cratons

answers: NDQ_003389

answers: accreted

answers: NDQ_003390

answers: continental cratons

answers: NDQ_003391

answers: continental cratons

answers: NDQ_003392

answers: continental cratons

answers: NDQ_003393

answers: continental cratons

answers: NDQ_003394

answers: many continents can consist of several continental cratons

answers: NDQ_003395

answers: many continents can consist of several continental cratons

answers: NDQ_003396

answers: continental cratons

text: The sedimentary cover in the SE Zagros is deforming above a layer of rock salt (acting as a ductile decollement with a low basal friction) whereas in the NW Zagros the salt layer is missing or is very thin. This different basal friction partly made different topographies in either sides of Kazerun fault. Higher topography and narrower zone of deformation in the NW Zagros is observed whereas in the SE, deformation was spread more and wider zone of deformation with lower topography was formed. Stresses induced in the Earth's crust by the collision caused extensive folding of the preexisting layered sedimentary rocks. Subsequent erosion removed softer rocks, such as mudstone (rock formed by consolidated mud) and siltstone (a slightly coarser-grained mudstone) while leaving harder rocks, such as limestone (calcium-rich rock consisting of the remains of marine organisms) and dolomite (rocks similar to limestone containing calcium and magnesium). This differential erosion formed the linear ridges of the Zagros Mountains.

text: The sedimentary cover in the SE Zagros is deforming above a layer of rock salt (acting as a

text: ductile

text: decollement

text: with a low basal

text: friction

text: ) whereas in the NW Zagros the salt layer is missing or is very thin. This different basal friction partly made different topographies in either sides of Kazerun fault. Higher topography and narrower zone of deformation in the NW Zagros is observed whereas in the SE, deformation was spread more and wider zone of deformation with lower topography was formed. Stresses induced in the Earth's crust by the collision caused extensive folding of the preexisting layered

text: sedimentary rock

text: s. Subsequent erosion removed softer rocks, such as

text: mudstone

text: (rock formed by consolidated mud) and

text: siltstone

text: (a slightly coarser-grained mudstone) while leaving harder rocks, such as

text: limestone

text: (calcium-rich rock consisting of the remains of marine organisms) and

text: dolomite

text: (rocks similar to limestone containing

text: calcium

text: and

text: magnesium

text: ). This differential

text: erosion

text: formed the linear ridges of the Zagros Mountains.

answers: NDQ_003351

answers: basal friction

answers: NDQ_003352

answers: is more likely to fold

answers: NDQ_003353

answers: extensive folding

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: ridge

answers: NDQ_003356

answers: lower topography

answers: NDQ_003357

answers: higher topography and narrower zone of deformation is observed whereas in the SE, deformation was spread more and wider zone of deformation with lower topography was formed

answers: NDQ_003358

answers: low basal friction

answers: NDQ_003359

answers: collides with another rock

answers: NDQ_003360

answers: faults

answers: NDQ_003362

answers: higher topography and narrower zone of deformation with lower topography was formed

answers: NDQ_003363

answers: Earth's crust

answers: NDQ_003371

answers: Which of the following is not a type of rock: limestone, mudstone, or siltstone?

answers: NDQ_003373

answers: Why is the salt layer missing or is very thin?

answers: NDQ_003376

answers: Which of the following is not a type of rock: mudstone, siltstone, or limestone?

answers: NDQ_003378

answers: What is the amount the ground moves in an earthquake?

answers: NDQ_003379

answers: Which of the following is not true?

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What type of rock is mudstone?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a type of rock: mudstone, siltstone or limestone?

answers: NDQ_003384

answers: Which of the following is not a type of fold: linear ridges or synclines?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: Which of the following is not a type of fault?

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: Kazerun fault or normal faults?

answers: NDQ_003388

answers: Which of the following is not a type of strike-slip fault?

answers: NDQ_003389

answers: It does not say

answers: NDQ_003390

answers: Kazerun fault

answers: NDQ_003391

answers: sedimentary cover

answers: NDQ_003392

answers: Kazerun fault

answers: NDQ_003393

answers: sedimentary cover

answers: NDQ_003394

answers: Kazerun fault

answers: NDQ_003395

answers: Kazerun fault

answers: NDQ_003396

answers: Kazerun fault

answers: NDQ_003351

answers: collision

answers: NDQ_003352

answers: folding

answers: NDQ_003353

answers: extensive folding

answers: NDQ_003354

answers: limestone

answers: NDQ_003355

answers: ductile decollement

answers: NDQ_003356

answers: folding

answers: NDQ_003357

answers: Higher topography and narrower zone of deformation

answers: NDQ_003358

answers: narrower zone of deformation

answers: NDQ_003359

answers: collision

answers: NDQ_003360

answers: collision

answers: NDQ_003362

answers: salt layer is missing or is very thin.

answers: NDQ_003363

answers: Zagros Mountains.

answers: NDQ_003371

answers: Kazerun fault.

answers: NDQ_003373

answers: layered sedimentary rocks.

answers: NDQ_003376

answers: linear ridges of the Zagros Mountains.

answers: NDQ_003378

answers: erosion

answers: NDQ_003379

answers: low basal friction)

answers: NDQ_003380

answers: Stresses

answers: NDQ_003381

answers: folding

answers: NDQ_003382

answers: collision caused extensive folding of the preexisting layered sedimentary rocks.

answers: NDQ_003383

answers: Stresses

answers: NDQ_003384

answers: linear ridges

answers: NDQ_003385

answers: fault.

answers: NDQ_003386

answers: Stresses

answers: NDQ_003387

answers: collision

answers: NDQ_003388

answers: collision caused extensive folding of the preexisting layered sedimentary rocks.

answers: NDQ_003389

answers: differential erosion

answers: NDQ_003390

answers: Kazerun

answers: NDQ_003391

answers: rock salt

answers: NDQ_003392

answers: Kazerun

answers: NDQ_003393

answers: rock salt

answers: NDQ_003394

answers: Kazerun

answers: NDQ_003395

answers: Kazerun

answers: NDQ_003396

answers: Kazerun

text: In the Just Another Band from L.A. (1972) recording, during the tornado sequence, the song alludes to The Wizard of Oz (1939) and the musical number "Over the Rainbow", which is sung by Howard Kaylan's character, while Mark Volman calls out for "Toto". Towards the middle of the recording, the band breaks out into a parody of the coda of the Crosby, Stills, and Nash song "Suite: Judy Blue Eyes", substituting the original Spanish lyrics with a series of rumors about the life of Studebacher Hoch. The famous "doot doot" backing vocals remain intact. Early in the song, we learn that Billy causes an "O Mein Papa" in the Earth's crust, a reference to Eddie Fisher who was known for his rendition of that well-known German song. The allusion is to be read, then, as "Billy causes a fissure in the Earth's crust."

text: In the

text: Just Another Band from L.A.

text: (1972) recording, during the tornado sequence, the song alludes to

text: The Wizard of Oz

text: (1939) and the musical number "

text: Over the Rainbow

text: ", which is sung by

text: Howard Kaylan

text: 's character, while

text: Mark Volman

text: calls out for "

text: Toto

text: ". Towards the middle of the recording, the band breaks out into a parody of the

text: coda

text: of the

text: Crosby, Stills, and Nash

text: song "

text: Suite: Judy Blue Eyes

text: ", substituting the original Spanish lyrics with a series of rumors about the life of Studebacher Hoch. The famous "doot doot" backing vocals remain intact. Early in the song, we learn that Billy causes an

text: "O Mein Papa"

text: in the Earth's crust, a reference to

text: Eddie Fisher

text: who was known for his rendition of that well-known German song. The allusion is to be read, then, as "Billy causes a fissure in the Earth's crust."

answers: NDQ_003351

answers: O Mein Papa

answers: NDQ_003352

answers: causes more cracks

answers: NDQ_003353

answers: a fissure

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fissure

answers: NDQ_003356

answers: fissure

answers: NDQ_003357

answers: O Mein Papa is sung by whom?

answers: NDQ_003358

answers: fissure

answers: NDQ_003359

answers: causes a fault

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: Billy causes an "O Mein Papa" in the Earth's crust

answers: NDQ_003363

answers: Earth's crust

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: unanswerable

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What does the song allude to?

answers: NDQ_003381

answers: What does the song allude to?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: What does the song allude to?

answers: NDQ_003388

answers: What does the song allude to?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: fissure in the Earth's crust

answers: NDQ_003391

answers: a fissure

answers: NDQ_003392

answers: a fissure

answers: NDQ_003393

answers: a fissure

answers: NDQ_003394

answers: a fissure

answers: NDQ_003395

answers: "Billy causes a fissure in the Earth's crust."

answers: NDQ_003396

answers: O Mein Papa

answers: NDQ_003351

answers: fissure

answers: NDQ_003352

answers: fissure

answers: NDQ_003353

answers: fissure

answers: NDQ_003354

answers: Just Another Band from L.A.

answers: NDQ_003355

answers: fissure

answers: NDQ_003356

answers: fissure

answers: NDQ_003357

answers: Billy causes an "O Mein Papa" in the Earth's crust,

answers: NDQ_003358

answers: fissure

answers: NDQ_003359

answers: fissure

answers: NDQ_003360

answers: tornado

answers: NDQ_003362

answers: "O Mein Papa"

answers: NDQ_003363

answers: fissure

answers: NDQ_003371

answers: fissure

answers: NDQ_003373

answers: "O Mein Papa" in the Earth's crust,

answers: NDQ_003376

answers: "O Mein Papa" in the Earth's crust,

answers: NDQ_003378

answers: fissure

answers: NDQ_003379

answers: "O Mein Papa" in the Earth's crust,

answers: NDQ_003380

answers: fissure

answers: NDQ_003381

answers: fissure

answers: NDQ_003382

answers: fissure

answers: NDQ_003383

answers: fissure

answers: NDQ_003384

answers: Just Another Band from L.A.

answers: NDQ_003385

answers: fissure

answers: NDQ_003386

answers: fissure

answers: NDQ_003387

answers: fissure

answers: NDQ_003388

answers: fissure

answers: NDQ_003389

answers: fissure

answers: NDQ_003390

answers: fissure

answers: NDQ_003391

answers: fissure

answers: NDQ_003392

answers: fissure

answers: NDQ_003393

answers: fissure

answers: NDQ_003394

answers: fissure

answers: NDQ_003395

answers: fissure

answers: NDQ_003396

answers: fissure

text: According to Rino and co-workers, the sum of the continental crust formed in the Pan-African orogeny and the Grenville orogeny makes the Neoproterozoic the period of Earth's history that has produced most continental crust.

text: According to Rino and co-workers, the sum of the

text: continental crust

text: formed in the

text: Pan-African orogeny

text: and the

text: Grenville orogeny

text: makes the Neoproterozoic the period of Earth's history that has produced most continental crust.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: fold that bends downward

answers: NDQ_003356

answers: change shape

answers: NDQ_003357

answers: Earth's history that has produced most continental crust

answers: NDQ_003358

answers: orogeny

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: the San Andreas fault was formed in the Neoproterozoic

answers: NDQ_003363

answers: Neoproterozoic

answers: NDQ_003371

answers: None of the above choices.

answers: NDQ_003373

answers: None of the above choices.

answers: NDQ_003376

answers: no

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: no

answers: NDQ_003380

answers: None of the above choices.

answers: NDQ_003381

answers: What will happen to the crust?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: unanswerable

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: unanswerable

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: continental crust

answers: NDQ_003392

answers: unanswerable

answers: NDQ_003393

answers: continental crust

answers: NDQ_003394

answers: Grenville

answers: NDQ_003395

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: Pan-African orogeny and the Grenville orogeny

answers: NDQ_003352

answers: most continental crust.

answers: NDQ_003353

answers: continental crust formed in the Pan-African orogeny

answers: NDQ_003354

answers: Neoproterozoic

answers: NDQ_003355

answers: Pan-African orogeny

answers: NDQ_003356

answers: Pan-African orogeny and the Grenville orogeny

answers: NDQ_003357

answers: Grenville orogeny

answers: NDQ_003358

answers: Grenville orogeny

answers: NDQ_003359

answers: Pan-African orogeny

answers: NDQ_003360

answers: Pan-African orogeny

answers: NDQ_003362

answers: the Neoproterozoic

answers: NDQ_003363

answers: Neoproterozoic

answers: NDQ_003371

answers: Pan-African orogeny and the Grenville orogeny

answers: NDQ_003373

answers: Pan-African orogeny and the Grenville orogeny

answers: NDQ_003376

answers: Grenville orogeny

answers: NDQ_003378

answers: Grenville orogeny

answers: NDQ_003379

answers: Pan-African orogeny and the Grenville orogeny

answers: NDQ_003380

answers: Pan-African orogeny and the Grenville orogeny

answers: NDQ_003381

answers: Pan-African orogeny and the Grenville orogeny

answers: NDQ_003382

answers: Pan-African orogeny and the Grenville orogeny

answers: NDQ_003383

answers: Pan-African orogeny and the Grenville orogeny

answers: NDQ_003384

answers: Pan-African orogeny and the Grenville orogeny

answers: NDQ_003385

answers: Pan-African orogeny and the Grenville orogeny

answers: NDQ_003386

answers: Pan-African orogeny and the Grenville orogeny

answers: NDQ_003387

answers: Pan-African orogeny and the Grenville orogeny

answers: NDQ_003388

answers: Pan-African orogeny and the Grenville orogeny

answers: NDQ_003389

answers: Pan-African orogeny

answers: NDQ_003390

answers: Grenville orogeny

answers: NDQ_003391

answers: continental crust

answers: NDQ_003392

answers: Grenville orogeny

answers: NDQ_003393

answers: continental crust

answers: NDQ_003394

answers: Pan-African orogeny and the Grenville orogeny

answers: NDQ_003395

answers: Grenville orogeny

answers: NDQ_003396

answers: Grenville orogeny

text: Early in the Ordovician, the continents of Laurentia (in present-day North America), Siberia, and Baltica (present-day northern Europe) were still independent continents (since the break-up of the supercontinent Pannotia earlier), but Baltica began to move towards Laurentia later in the period, causing the Iapetus Ocean between them to shrink. The small continent Avalonia separated from Gondwana and began to move north towards Baltica and Laurentia, opening the Rheic Ocean between Gondwana and Avalonia.

text: Early in the Ordovician, the continents of

text: Laurentia

text: (in present-day

text: North America

text: Siberia

text: , and

text: Baltica

text: (present-day northern Europe) were still independent continents (since the break-up of the

text: supercontinent

text: Pannotia

text: earlier), but Baltica began to move towards Laurentia later in the period, causing the

text: Iapetus Ocean

text: between them to shrink. The small continent

text: Avalonia

text: separated from Gondwana and began to move north towards Baltica and Laurentia, opening the

text: Rheic Ocean

text: between Gondwana and Avalonia.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: shrinks

answers: NDQ_003353

answers: igneous rocks to form

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: ocean

answers: NDQ_003356

answers: shrink

answers: NDQ_003357

answers: Iapetus Ocean between them to shrink

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: continents

answers: NDQ_003362

answers: Laurentia began to move towards Laurentia later in the period

answers: NDQ_003363

answers: Ordovician

answers: NDQ_003371

answers: What may have caused the Iapetus Ocean between them to shrink?

answers: NDQ_003373

answers: what is the first word in the passage?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: what is the last word in the passage?

answers: NDQ_003382

answers: what is the most common stress at convergent plates

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: fault zone

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: What type of faults result from shear stress?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: Laurentia

answers: NDQ_003391

answers: unanswerable

answers: NDQ_003392

answers: Laurentia

answers: NDQ_003393

answers: unanswerable

answers: NDQ_003394

answers: Rheic Ocean

answers: NDQ_003395

answers: unanswerable

answers: NDQ_003396

answers: Rheic Ocean

answers: NDQ_003351

answers: Iapetus Ocean

answers: NDQ_003352

answers: Baltica began to move towards Laurentia

answers: NDQ_003353

answers: Iapetus Ocean between them to shrink.

answers: NDQ_003354

answers: Early in the Ordovician,

answers: NDQ_003355

answers: Early in the Ordovician,

answers: NDQ_003356

answers: shrink.

answers: NDQ_003357

answers: Iapetus Ocean between them to shrink.

answers: NDQ_003358

answers: Iapetus Ocean

answers: NDQ_003359

answers: Baltica began to move towards Laurentia

answers: NDQ_003360

answers: Ordovician,

answers: NDQ_003362

answers: independent continents

answers: NDQ_003363

answers: Ordovician,

answers: NDQ_003371

answers: Early in the Ordovician,

answers: NDQ_003373

answers: Early in the Ordovician,

answers: NDQ_003376

answers: Iapetus Ocean

answers: NDQ_003378

answers: Baltica began to move towards Laurentia

answers: NDQ_003379

answers: Baltica began to move towards Laurentia

answers: NDQ_003380

answers: Baltica began to move towards Laurentia

answers: NDQ_003381

answers: Baltica began to move towards Laurentia

answers: NDQ_003382

answers: Baltica began to move towards Laurentia

answers: NDQ_003383

answers: Baltica began to move towards Laurentia

answers: NDQ_003384

answers: Baltica began to move towards Laurentia

answers: NDQ_003385

answers: Early in the Ordovician,

answers: NDQ_003386

answers: Baltica began to move towards Laurentia

answers: NDQ_003387

answers: Early in the Ordovician,

answers: NDQ_003388

answers: Early in the Ordovician,

answers: NDQ_003389

answers: break-up of the supercontinent Pannotia

answers: NDQ_003390

answers: Early in the Ordovician,

answers: NDQ_003391

answers: Iapetus Ocean

answers: NDQ_003392

answers: Early in the Ordovician,

answers: NDQ_003393

answers: Iapetus Ocean

answers: NDQ_003394

answers: Rheic Ocean

answers: NDQ_003395

answers: Iapetus Ocean

answers: NDQ_003396

answers: Rheic Ocean

text: In geology, a rift is a linear zone where the Earth's crust and lithosphere are being pulled apart and is an example of extensional tectonics.

text: In

text: geology

text: , a rift is a linear zone where the

text: Earth's

text: crust

text: and

text: lithosphere

text: are being pulled apart and is an example of

text: extensional tectonics

answers: NDQ_003351

answers: extensional

answers: NDQ_003352

answers: pulls apart

answers: NDQ_003353

answers: rifts

answers: NDQ_003354

answers: the Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: rift

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: Earth's crust and lithosphere are being pulled apart

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: is being pulled apart

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: The San Andreas fault is not a rift.

answers: NDQ_003363

answers: rifts

answers: NDQ_003371

answers: What is an example of extensional tectonics?

answers: NDQ_003373

answers: How would you describe compressive stresses?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: Which of the following is not an example of extensional tectonics?

answers: NDQ_003380

answers: What is an example of extensional tectonics?

answers: NDQ_003381

answers: What is an example of extensional tectonics?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: Which of the following is not a cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not an example of extensional tectonics?

answers: NDQ_003388

answers: Which of the following is not an example of extensional tectonics?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: rift

answers: NDQ_003391

answers: rift

answers: NDQ_003392

answers: rift

answers: NDQ_003393

answers: lithosphere

answers: NDQ_003394

answers: rift

answers: NDQ_003395

answers: rift

answers: NDQ_003396

answers: rift fault

answers: NDQ_003351

answers: extensional tectonics.

answers: NDQ_003352

answers: pulled apart

answers: NDQ_003353

answers: pulled apart

answers: NDQ_003354

answers: extensional tectonics.

answers: NDQ_003355

answers: rift

answers: NDQ_003356

answers: pulled apart

answers: NDQ_003357

answers: the Earth's crust and lithosphere are being pulled apart

answers: NDQ_003358

answers: rift

answers: NDQ_003359

answers: pulled apart

answers: NDQ_003360

answers: extensional tectonics.

answers: NDQ_003362

answers: extensional tectonics.

answers: NDQ_003363

answers: extensional tectonics.

answers: NDQ_003371

answers: a rift

answers: NDQ_003373

answers: In geology,

answers: NDQ_003376

answers: extensional tectonics.

answers: NDQ_003378

answers: rift

answers: NDQ_003379

answers: extensional tectonics.

answers: NDQ_003380

answers: pulled apart

answers: NDQ_003381

answers: extensional tectonics.

answers: NDQ_003382

answers: extensional tectonics.

answers: NDQ_003383

answers: extensional tectonics.

answers: NDQ_003384

answers: rift

answers: NDQ_003385

answers: rift

answers: NDQ_003386

answers: extensional tectonics.

answers: NDQ_003387

answers: extensional tectonics.

answers: NDQ_003388

answers: extensional tectonics.

answers: NDQ_003389

answers: extensional tectonics.

answers: NDQ_003390

answers: rift

answers: NDQ_003391

answers: rift

answers: NDQ_003392

answers: rift

answers: NDQ_003393

answers: rift

answers: NDQ_003394

answers: rift

answers: NDQ_003395

answers: rift

answers: NDQ_003396

answers: rift

text: The initial crust, formed when the Earth's surface first solidified, totally disappeared from a combination of this fast Hadean plate tectonics and the intense impacts of the Late Heavy Bombardment. However, it is thought that it was basaltic in composition, like today's oceanic crust, because little crustal differentiation had yet taken place. The first larger pieces of continental crust, which is a product of differentiation of lighter elements during partial melting in the lower crust, appeared at the end of the Hadean, about 4.0 Ga. What is left of these first small continents are called cratons. These pieces of late Hadean and early Archean crust form the cores around which today's continents grew.

text: The initial crust, formed when the Earth's surface first solidified, totally disappeared from a combination of this fast Hadean plate tectonics and the intense impacts of the Late Heavy Bombardment. However, it is thought that it was

text: basalt

text: ic in composition, like today's

text: oceanic crust

text: , because little crustal differentiation had yet taken place. The first larger pieces of

text: continental crust

text: , which is a product of differentiation of lighter elements during

text: partial melting

text: in the lower crust, appeared at the end of the Hadean, about 4.0 Ga. What is left of these first small continents are called

text: craton

text: s. These pieces of late Hadean and early Archean crust form the cores around which today's continents grew.

answers: NDQ_003351

answers: basaltic

answers: NDQ_003352

answers: has a harder texture

answers: NDQ_003353

answers: crustal differentiation

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: Hadean

answers: NDQ_003356

answers: solidify

answers: NDQ_003357

answers: crustal differentiation had yet taken place

answers: NDQ_003358

answers: craton

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: plates

answers: NDQ_003362

answers: it is thought that it was basaltic in composition

answers: NDQ_003363

answers: the end of the Hadean

answers: NDQ_003371

answers: What is left of these first small continents are called cratons?

answers: NDQ_003373

answers: what is the first large continents are called cratons

answers: NDQ_003376

answers: What is left of these first small continents are called cratons

answers: NDQ_003378

answers: What is left of these first small continents are called cratons

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What is the main idea of the passage?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is left of these first small continents are called cratons

answers: NDQ_003386

answers: What is the cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not a type of plate tectonics: fast Hadean plate tectonics and the intense impacts of the Late Heavy Bombardment?

answers: NDQ_003388

answers: Which of the following is not a result of shear stress: strike-slip faults, cratons, or plate tectonics?

answers: NDQ_003389

answers: What is left of these first small continents are called cratons

answers: NDQ_003390

answers: cratons

answers: NDQ_003391

answers: cratons

answers: NDQ_003392

answers: plate tectonics

answers: NDQ_003393

answers: cratons

answers: NDQ_003394

answers: cratons

answers: NDQ_003395

answers: cratons

answers: NDQ_003396

answers: Hadean

answers: NDQ_003351

answers: Late Heavy Bombardment.

answers: NDQ_003352

answers: differentiation of lighter elements

answers: NDQ_003353

answers: crustal differentiation

answers: NDQ_003354

answers: Late Heavy Bombardment.

answers: NDQ_003355

answers: cratons.

answers: NDQ_003356

answers: melting

answers: NDQ_003357

answers: partial melting in the lower crust,

answers: NDQ_003358

answers: cratons.

answers: NDQ_003359

answers: impacts

answers: NDQ_003360

answers: fast Hadean plate tectonics

answers: NDQ_003362

answers: totally disappeared

answers: NDQ_003363

answers: end of the Hadean,

answers: NDQ_003371

answers: fast Hadean plate tectonics

answers: NDQ_003373

answers: The initial crust,

answers: NDQ_003376

answers: cratons.

answers: NDQ_003378

answers: cratons.

answers: NDQ_003379

answers: cratons.

answers: NDQ_003380

answers: impacts

answers: NDQ_003381

answers: differentiation of lighter elements during partial melting in the lower crust,

answers: NDQ_003382

answers: Hadean plate tectonics

answers: NDQ_003383

answers: impacts

answers: NDQ_003384

answers: cratons.

answers: NDQ_003385

answers: cratons.

answers: NDQ_003386

answers: fast Hadean plate tectonics

answers: NDQ_003387

answers: differentiation of lighter elements during partial melting in the lower crust,

answers: NDQ_003388

answers: Late Heavy Bombardment.

answers: NDQ_003389

answers: cratons.

answers: NDQ_003390

answers: Late Heavy Bombardment.

answers: NDQ_003391

answers: cratons.

answers: NDQ_003392

answers: Late Heavy Bombardment.

answers: NDQ_003393

answers: cratons.

answers: NDQ_003394

answers: Late Heavy Bombardment.

answers: NDQ_003395

answers: Late Heavy Bombardment.

answers: NDQ_003396

answers: Late Heavy Bombardment.

text: A rift is a region where the lithosphere extends as two parts of the Earth's crust pull apart.Often a rift will form in an area of the crust that is already weakened by earlier geological activity.  Extensional faults form parallel to the axis of the rift.An extensional fault may be seen as a crack in the crust that extends down at an angle to the vertical.  As the two sides pull apart, the hanging wall ("hanging over" the sloping fault) will move downward relative to the footwall.The crust thins and sinks, forming a rift basin.  Warm mantle material wells up, melting the crust and often causing volcanoes to emerge in the rift basin.

text: A rift is a region where the

text: lithosphere

text: extends as two parts of the Earth's

text: crust

text: pull apart.Often a rift will form in an area of the crust that is already weakened by earlier geological activity.

text: Extensional fault

text: s form parallel to the axis of the rift.An extensional fault may be seen as a crack in the crust that extends down at an angle to the vertical.  As the two sides pull apart, the hanging wall ("hanging over" the sloping fault) will move downward relative to the footwall.The crust thins and sinks, forming a rift basin.  Warm mantle material wells up, melting the crust and often causing volcanoes to emerge in the rift basin.

answers: NDQ_003351

answers: extensional

answers: NDQ_003352

answers: pulls apart

answers: NDQ_003353

answers: cracks to form

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: rift

answers: NDQ_003356

answers: shrink

answers: NDQ_003357

answers: the hanging wall will move downward relative to the footwall

answers: NDQ_003358

answers: rift

answers: NDQ_003359

answers: pulls apart

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: The San Andreas fault is parallel to the axis of the rift.

answers: NDQ_003363

answers: rift basins

answers: NDQ_003371

answers: Which of the following is not a type of fault: extensional faults or thrust faults?

answers: NDQ_003373

answers: Which of the following is not a type of stress?

answers: NDQ_003376

answers: Which of the following is not caused by compressive forces?

answers: NDQ_003378

answers: Which of the following is not an example of an extensional fault?

answers: NDQ_003379

answers: Which of the following is not true of extensional faults?

answers: NDQ_003380

answers: Which of the following is not a stress?

answers: NDQ_003381

answers: Which of the following is not an example of confining stress?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not a type of fold?

answers: NDQ_003385

answers: Which of the following is not a type of fault?

answers: NDQ_003386

answers: Which of the following is not a cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: extensional faults or normal faults?

answers: NDQ_003388

answers: Which of the following is not a result of shear stress: strike-slip faults or extensional faults?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: extensional fault

answers: NDQ_003391

answers: the hanging wall

answers: NDQ_003392

answers: extensional fault

answers: NDQ_003393

answers: hanging wall

answers: NDQ_003394

answers: extensional fault

answers: NDQ_003395

answers: sloping fault

answers: NDQ_003396

answers: extensional fault

answers: NDQ_003351

answers: Extensional faults

answers: NDQ_003352

answers: move downward relative to the footwall.The

answers: NDQ_003353

answers: footwall.The crust thins and sinks,

answers: NDQ_003354

answers: weakened by earlier geological activity.

answers: NDQ_003355

answers: Extensional faults

answers: NDQ_003356

answers: footwall.The crust thins and sinks,

answers: NDQ_003357

answers: the hanging wall

answers: NDQ_003358

answers: Extensional faults

answers: NDQ_003359

answers: weakened by earlier geological activity.

answers: NDQ_003360

answers: rift

answers: NDQ_003362

answers: volcanoes to emerge in the rift basin.

answers: NDQ_003363

answers: rift

answers: NDQ_003371

answers: Extensional faults

answers: NDQ_003373

answers: footwall.The crust thins and sinks, forming a rift basin.

answers: NDQ_003376

answers: rift basin.

answers: NDQ_003378

answers: downward

answers: NDQ_003379

answers: angle to the vertical.

answers: NDQ_003380

answers: weakened by earlier geological activity.

answers: NDQ_003381

answers: footwall.The crust thins and sinks, forming a rift basin.

answers: NDQ_003382

answers: Extensional faults

answers: NDQ_003383

answers: Extensional faults

answers: NDQ_003384

answers: a crack in the crust that extends down at an angle to the vertical.

answers: NDQ_003385

answers: Extensional faults

answers: NDQ_003386

answers: the hanging wall

answers: NDQ_003387

answers: Extensional faults

answers: NDQ_003388

answers: Extensional faults

answers: NDQ_003389

answers: rift

answers: NDQ_003390

answers: sloping fault)

answers: NDQ_003391

answers: hanging wall

answers: NDQ_003392

answers: sloping fault)

answers: NDQ_003393

answers: hanging wall

answers: NDQ_003394

answers: extensional fault

answers: NDQ_003395

answers: extensional fault

answers: NDQ_003396

answers: extensional fault

text: During subduction, an oceanic plate is thrust below another tectonic plate, which may be oceanic or continental. Water and other volatiles in the down-going plate cause flux melting in the upper mantle, creating magma that rises and penetrates the overriding plate, forming a volcanic arc. The weight of the down-going slab flexes the down-going plate creating an oceanic trench. The area between the trench and the arc is the forearc region, and the area behind the arc (i.e. on the side away from the trench) is the back-arc region.

text: During

text: subduction

text: , an

text: oceanic

text: plate is thrust below another tectonic plate, which may be oceanic or

text: continental

text: . Water and other volatiles in the down-going plate cause

text: flux melting

text: in the upper mantle, creating magma that rises and penetrates the overriding plate, forming a

text: volcanic arc

text: . The weight of the down-going slab flexes the down-going plate creating an

text: oceanic trench

text: . The area between the trench and the arc is the forearc region, and the area behind the arc (i.e. on the side away from the trench) is the

text: back-arc region

answers: NDQ_003351

answers: subduction

answers: NDQ_003352

answers: more likely to crack

answers: NDQ_003353

answers: magma to rise

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: oceanic trench

answers: NDQ_003356

answers: subduct

answers: NDQ_003357

answers: the area between the trench and the arc is the forearc region

answers: NDQ_003358

answers: oceanic trench

answers: NDQ_003359

answers: down-going plate

answers: NDQ_003360

answers: oceanic plates

answers: NDQ_003362

answers: Volcanic arcs do not occur in the San Andreas fault.

answers: NDQ_003363

answers: subduction

answers: NDQ_003371

answers: What is the area between the trench and the arc called?

answers: NDQ_003373

answers: What is the area between the trench and the arc?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a stress?

answers: NDQ_003381

answers: What does the weight of the down-going slab create?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not a type of fold?

answers: NDQ_003385

answers: What is the area between the trench and the arc called?

answers: NDQ_003386

answers: Which of the following is not the cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: normal faults or subduction?

answers: NDQ_003388

answers: Which of the following is not a type of strike-slip fault?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: oceanic trench

answers: NDQ_003391

answers: oceanic trench

answers: NDQ_003392

answers: oceanic trench

answers: NDQ_003393

answers: oceanic trench

answers: NDQ_003394

answers: subduction

answers: NDQ_003395

answers: oceanic trench

answers: NDQ_003396

answers: oceanic trench

answers: NDQ_003351

answers: The weight of the down-going slab

answers: NDQ_003352

answers: oceanic trench.

answers: NDQ_003353

answers: flux melting in the upper mantle,

answers: NDQ_003354

answers: During subduction,

answers: NDQ_003355

answers: oceanic trench.

answers: NDQ_003356

answers: oceanic trench.

answers: NDQ_003357

answers: oceanic trench.

answers: NDQ_003358

answers: trench.

answers: NDQ_003359

answers: weight of the down-going slab

answers: NDQ_003360

answers: subduction,

answers: NDQ_003362

answers: volcanic arc.

answers: NDQ_003363

answers: subduction,

answers: NDQ_003371

answers: oceanic trench.

answers: NDQ_003373

answers: oceanic trench.

answers: NDQ_003376

answers: oceanic trench.

answers: NDQ_003378

answers: oceanic trench.

answers: NDQ_003379

answers: oceanic trench.

answers: NDQ_003380

answers: flexes the down-going plate creating an oceanic trench.

answers: NDQ_003381

answers: flexes the down-going plate creating an oceanic trench.

answers: NDQ_003382

answers: oceanic trench.

answers: NDQ_003383

answers: flexes the down-going plate creating an oceanic trench.

answers: NDQ_003384

answers: volcanic arc.

answers: NDQ_003385

answers: forearc region,

answers: NDQ_003386

answers: subduction,

answers: NDQ_003387

answers: oceanic trench.

answers: NDQ_003388

answers: During subduction,

answers: NDQ_003389

answers: subduction,

answers: NDQ_003390

answers: oceanic trench.

answers: NDQ_003391

answers: oceanic trench.

answers: NDQ_003392

answers: oceanic trench.

answers: NDQ_003393

answers: oceanic trench.

answers: NDQ_003394

answers: oceanic trench.

answers: NDQ_003395

answers: oceanic trench.

answers: NDQ_003396

answers: oceanic trench.

text: In detail many strike-slip faults at surface consist of en echelon and/or braided segments in many cases probably inherited from previously formed Riedel shears. In cross-section the displacements are dominantly reverse or normal in type depending on whether the overall fault geometry is transpressional (i.e. with a small component of shortening) or transtensional (with a small component of extension). As the faults tend to join downwards onto a single strand in basement, the geometry has led to these being termed flower structure. Fault zones with dominantly reverse faulting are known as positive flowers, those with dominantly normal offsets are known as negative flowers. The identification of such structures, particularly where positive and negative flowers are developed on different segments of the same fault, are regarded as reliable indicators of strike-slip.

text: In detail many strike-slip faults at surface consist of en echelon and/or braided segments in many cases probably inherited from previously formed Riedel shears. In cross-section the displacements are dominantly reverse or normal in type depending on whether the overall fault geometry is

text: transpression

text: al (i.e. with a small component of shortening) or

text: transtension

text: al (with a small component of extension). As the faults tend to join downwards onto a single strand in basement, the geometry has led to these being termed flower structure. Fault zones with dominantly reverse faulting are known as positive flowers, those with dominantly normal offsets are known as negative flowers. The identification of such structures, particularly where positive and negative flowers are developed on different segments of the same fault, are regarded as reliable indicators of strike-slip.

answers: NDQ_003351

answers: transtensional

answers: NDQ_003352

answers: shortens

answers: NDQ_003353

answers: displacements

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: negative flowers

answers: NDQ_003356

answers: join downwards

answers: NDQ_003357

answers: displacements are dominantly normal in type

answers: NDQ_003358

answers: normal

answers: NDQ_003359

answers: strike-slip

answers: NDQ_003360

answers: Riedel shears

answers: NDQ_003362

answers: positive flowers are developed on different segments of the same fault

answers: NDQ_003363

answers: strike-slip faults

answers: NDQ_003371

answers: What may be the reason for a thrust fault?

answers: NDQ_003373

answers: i.e. with a small component of shortening

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: strike-slip

answers: NDQ_003379

answers: no

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What type of stress occurs when rock deforms?

answers: NDQ_003382

answers: transpressional

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: positive flowers

answers: NDQ_003386

answers: strike-slip

answers: NDQ_003387

answers: no

answers: NDQ_003388

answers: unanswerable

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: negative flowers

answers: NDQ_003391

answers: basement

answers: NDQ_003392

answers: positive flowers

answers: NDQ_003393

answers: basement

answers: NDQ_003394

answers: transtensional

answers: NDQ_003395

answers: transtensional

answers: NDQ_003396

answers: positive flowers

answers: NDQ_003351

answers: reverse or normal

answers: NDQ_003352

answers: shortening)

answers: NDQ_003353

answers: strike-slip faults

answers: NDQ_003354

answers: inherited from previously formed Riedel shears.

answers: NDQ_003355

answers: flower structure.

answers: NDQ_003356

answers: join downwards onto a single strand in basement,

answers: NDQ_003357

answers: extension).

answers: NDQ_003358

answers: negative flowers.

answers: NDQ_003359

answers: strike-slip

answers: NDQ_003360

answers: strike-slip faults

answers: NDQ_003362

answers: positive flowers,

answers: NDQ_003363

answers: Riedel shears.

answers: NDQ_003371

answers: strike-slip faults

answers: NDQ_003373

answers: basement,

answers: NDQ_003376

answers: strike-slip faults

answers: NDQ_003378

answers: strike-slip

answers: NDQ_003379

answers: reverse

answers: NDQ_003380

answers: extension).

answers: NDQ_003381

answers: shortening)

answers: NDQ_003382

answers: transpressional

answers: NDQ_003383

answers: faults tend to join downwards onto a single strand

answers: NDQ_003384

answers: flower structure.

answers: NDQ_003385

answers: flower structure.

answers: NDQ_003386

answers: strike-slip

answers: NDQ_003387

answers: transpressional

answers: NDQ_003388

answers: Riedel shears.

answers: NDQ_003389

answers: Riedel shears.

answers: NDQ_003390

answers: strike-slip

answers: NDQ_003391

answers: basement,

answers: NDQ_003392

answers: strike-slip

answers: NDQ_003393

answers: basement,

answers: NDQ_003394

answers: positive flowers,

answers: NDQ_003395

answers: positive flowers,

answers: NDQ_003396

answers: positive flowers,

text: Workplace bullying is reported to be far more prevalent than perhaps commonly thought. For some reason, workplace bullying seems to be particularly widespread in healthcare organizations; 80% of nurses report experiencing workplace bullying. Similar to the school environment for children, the work environment typically places groups of adult peers together in a shared space on a regular basis. In such a situation, social interactions and relationships are of great importance to the function of the organizational structure and in pursuing goals. The emotional consequences of bullying put an organization at risk of losing victimized employees. Bullying also contributes to a negative work environment, is not conducive to necessary cooperation and can lessen productivity at various levels. Bullying in the workplace is associated with negative responses to stress. The ability to manage emotions, especially emotional stress, seems to be a consistently important factor in different types of bullying. The workplace in general can be a stressful environment, so a negative way of coping with stress or an inability to do so can be particularly damning. Workplace bullies may have high social intelligence and low emotional intelligence (EI). In this context, bullies tend to rank high on the social ladder and are adept at influencing others. The combination of high social intelligence and low empathy is conducive to manipulative behavior, such that Hutchinson (2013) describes workplace bullying to be. In working groups where employees have low EI, workers can be persuaded to engage in unethical behavior. With the bullies' persuasion, the work group is socialized in a way that rationalizes the behavior, and makes the group tolerant or supportive of the bullying. Hutchinson & Hurley (2013) make the case that EI and leadership skills are both necessary to bullying intervention in the workplace, and illustrates the relationship between EI, leadership and reductions in bullying. EI and ethical behavior among other members of the work team have been shown to have a significant impact on ethical behavior of nursing teams. Higher EI is linked to improvements in the work environment and is an important moderator between conflict and reactions to conflict in the workplace. The self-awareness and self-management dimensions of EI have both been illustrated to have strong positive correlations with effective leadership and the specific leadership ability to build healthy work environments and work culture.

text: Workplace bullying is reported to be far more prevalent than perhaps commonly thought. For some reason, workplace bullying seems to be particularly widespread in healthcare organizations; 80% of nurses report experiencing workplace bullying. Similar to the school environment for children, the work environment typically places groups of adult peers together in a shared space on a regular basis. In such a situation, social interactions and relationships are of great importance to the function of the

text: organizational structure

text: and in pursuing

text: goal

text: s. The emotional consequences of bullying put an organization at risk of losing victimized employees. Bullying also contributes to a negative work environment, is not conducive to necessary cooperation and can lessen productivity at various levels. Bullying in the workplace is associated with negative responses to stress. The ability to manage emotions, especially emotional

text: stress

text: , seems to be a consistently important factor in different types of bullying. The workplace in general can be a stressful environment, so a negative way of

text: coping

text: with stress or an inability to do so can be particularly damning. Workplace bullies may have high

text: social intelligence

text: and low

text: emotional intelligence

text: (EI). In this context, bullies tend to rank high on the social ladder and are adept at

text: influencing

text: others. The combination of high social intelligence and low empathy is conducive to

text: manipulative

text: behavior, such that Hutchinson (2013) describes workplace bullying to be. In working groups where employees have low EI, workers can be

text: persuaded

text: to engage in unethical behavior. With the bullies' persuasion, the work group is socialized in a way that

text: rationalizes

text: the behavior, and makes the group tolerant or supportive of the bullying. Hutchinson & Hurley (2013) make the case that EI and

text: leadership

text: skills are both necessary to bullying intervention in the workplace, and illustrates the relationship between EI, leadership and reductions in bullying. EI and ethical behavior among other members of the work team have been shown to have a significant impact on ethical behavior of nursing teams. Higher EI is linked to improvements in the work environment and is an important moderator between conflict and reactions to conflict in the workplace. The

text: self-awareness

text: and self-management dimensions of EI have both been illustrated to have strong positive correlations with effective leadership and the specific leadership ability to build healthy work environments and work culture.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: is more likely to break

answers: NDQ_003353

answers: EI to decrease.

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: swell

answers: NDQ_003357

answers: The combination of high social intelligence and low empathy is conducive to what?

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures.

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: 80% of nurses report experiencing workplace bullying

answers: NDQ_003363

answers: the same time

answers: NDQ_003371

answers: Which of the following is not an example of a thrust fault?

answers: NDQ_003373

answers: What is the main idea of this passage?

answers: NDQ_003376

answers: What type of terrain is basin-and-range?

answers: NDQ_003378

answers: What is the relationship between EI and leadership skills?

answers: NDQ_003379

answers: What is the dip of the fault plane

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: Which of the following is not an example of confining stress?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: Which of the following is not an example of a syncline?

answers: NDQ_003385

answers: What is the name of the area where faults are clustered?

answers: NDQ_003386

answers: Which of the following is not a cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not a cause of normal faults?

answers: NDQ_003388

answers: Which of the following is not a result of shear stress?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: dip-slip fault plane

answers: NDQ_003392

answers: unanswerable

answers: NDQ_003393

answers: dip-slip fault plane

answers: NDQ_003394

answers: is not vertical

answers: NDQ_003395

answers: a fault with a vertical fault plane

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: high social intelligence and low empathy is conducive to manipulative behavior,

answers: NDQ_003352

answers: manipulative behavior,

answers: NDQ_003353

answers: bullies'

answers: NDQ_003354

answers: social intelligence

answers: NDQ_003355

answers: emotional intelligence

answers: NDQ_003356

answers: high social intelligence

answers: NDQ_003357

answers: high social intelligence and low empathy

answers: NDQ_003358

answers: emotional intelligence

answers: NDQ_003359

answers: high social intelligence

answers: NDQ_003360

answers: bullies tend to rank high on the social ladder

answers: NDQ_003362

answers: the social ladder and are adept at influencing others.

answers: NDQ_003363

answers: high social intelligence

answers: NDQ_003371

answers: emotional intelligence

answers: NDQ_003373

answers: high social intelligence

answers: NDQ_003376

answers: high social intelligence and low empathy is conducive to manipulative behavior,

answers: NDQ_003378

answers: high social intelligence

answers: NDQ_003379

answers: emotional intelligence

answers: NDQ_003380

answers: high social intelligence

answers: NDQ_003381

answers: high social intelligence

answers: NDQ_003382

answers: high social intelligence

answers: NDQ_003383

answers: high social intelligence and low empathy is conducive to manipulative behavior,

answers: NDQ_003384

answers: emotional intelligence

answers: NDQ_003385

answers: high social intelligence

answers: NDQ_003386

answers: high social intelligence

answers: NDQ_003387

answers: high social intelligence

answers: NDQ_003388

answers: high social intelligence

answers: NDQ_003389

answers: high social intelligence

answers: NDQ_003390

answers: high social intelligence

answers: NDQ_003391

answers: EI and leadership skills

answers: NDQ_003392

answers: high social intelligence

answers: NDQ_003393

answers: EI and leadership skills

answers: NDQ_003394

answers: social ladder and are adept at influencing others.

answers: NDQ_003395

answers: high social intelligence and low empathy is conducive to manipulative behavior,

answers: NDQ_003396

answers: high social intelligence

text: Authentic paint craquelure occurs because paint dries and becomes less flexible as it ages and shrinks. In the case of paintings on canvas, the canvas slackens as it ages as it cannot endure the long-term stress of stretching. Paint at the center of a painting is the least cracked, whereas paint at the edges is the most cracked, or stressed. The precise pattern of craquelure depends on where, when, and under what conditions the picture was painted, and subsequently kept.  Cracks caused by stretching or slackening the canvas are quite different from cracks due to other factors, such as drying and ageing of the paint. The paint cracks when the stress upon it is greater than the breaking stress point of the paint layer and the paint will crack approximately at right-angles to the direction of the stress, relieving that stress. The stress at the corners is more than double that of the center.

text: Authentic paint craquelure occurs because paint dries and becomes less flexible as it ages and shrinks. In the case of paintings on canvas, the canvas slackens as it ages as it cannot endure the long-term stress of stretching. Paint at the center of a painting is the least cracked, whereas paint at the edges is the most cracked, or stressed. The precise pattern of craquelure depends on where, when, and under what conditions the picture was painted, and subsequently kept.  Cracks caused by stretching or slackening the canvas are quite different from cracks due to other factors, such as drying and ageing of the paint. The paint cracks when the stress upon it is greater than the breaking stress point of the paint layer and the paint will crack approximately at right-angles to the direction of the stress, relieving that stress. The stress at the corners is more than double that of the center.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: cracks

answers: NDQ_003353

answers: cracks

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: corner

answers: NDQ_003356

answers: crack

answers: NDQ_003357

answers: The stress at the corners is more than double that of the center.

answers: NDQ_003358

answers: craquelure

answers: NDQ_003359

answers: cracks

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: The stress at the corners is more than double that of the center.

answers: NDQ_003363

answers: craquelure

answers: NDQ_003371

answers: Which of the following is not an example of craquelure?

answers: NDQ_003373

answers: How would you describe the stress at the corners?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: Which of the following is not a type of stress?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: what is the most cracked, or stressed

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: Which of the following is not a type of crack?

answers: NDQ_003388

answers: What is the stress at the corners more than double that of the center?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: craquelure

answers: NDQ_003391

answers: dip-slip fault plane

answers: NDQ_003392

answers: craquelure

answers: NDQ_003393

answers: dip-slip fault plane

answers: NDQ_003394

answers: right-angles

answers: NDQ_003395

answers: crack approximately at right-angles

answers: NDQ_003396

answers: right-angles to the direction of the stress

answers: NDQ_003351

answers: edges

answers: NDQ_003352

answers: breaking stress point of the paint layer

answers: NDQ_003353

answers: paint craquelure occurs because paint dries and becomes less flexible

answers: NDQ_003354

answers: Authentic paint craquelure

answers: NDQ_003355

answers: Authentic paint craquelure

answers: NDQ_003356

answers: paint craquelure

answers: NDQ_003357

answers: breaking stress point of the paint layer

answers: NDQ_003358

answers: paint craquelure

answers: NDQ_003359

answers: paint dries and becomes less flexible as it ages and shrinks.

answers: NDQ_003360

answers: paint craquelure

answers: NDQ_003362

answers: Authentic paint craquelure

answers: NDQ_003363

answers: corners

answers: NDQ_003371

answers: Authentic paint craquelure

answers: NDQ_003373

answers: Authentic paint craquelure

answers: NDQ_003376

answers: breaking stress point of the paint layer

answers: NDQ_003378

answers: Authentic paint craquelure

answers: NDQ_003379

answers: right-angles

answers: NDQ_003380

answers: stress

answers: NDQ_003381

answers: breaking stress point of the paint layer

answers: NDQ_003382

answers: stretching.

answers: NDQ_003383

answers: stress

answers: NDQ_003384

answers: Authentic paint craquelure

answers: NDQ_003385

answers: edges

answers: NDQ_003386

answers: Authentic paint craquelure

answers: NDQ_003387

answers: Cracks

answers: NDQ_003388

answers: breaking stress point of the paint layer

answers: NDQ_003389

answers: Authentic paint craquelure

answers: NDQ_003390

answers: Authentic paint craquelure

answers: NDQ_003391

answers: Authentic paint craquelure

answers: NDQ_003392

answers: Authentic paint craquelure

answers: NDQ_003393

answers: Authentic paint craquelure

answers: NDQ_003394

answers: right-angles

answers: NDQ_003395

answers: right-angles

answers: NDQ_003396

answers: right-angles

text: The boundary between the Earth's crust and the mantle (the Moho) rises from  between the Agulhas Bank (south of South Africa) and the Agulhas passage (south of the bank), typical for a continent-ocean transition.  The Agulhas Passage consists of 120-160 Ma-old oceanic crust, whereas the 100-80 Ma-old Agulhas Plateau rises  above the surrounding ocean floor while the Moho dips to between  below it.

text: The boundary between the Earth's crust and the mantle (the

text: Moho

text: ) rises from  between the

text: Agulhas Bank

text: (south of South Africa) and the Agulhas passage (south of the bank), typical for a

text: continent-ocean transition

text: .  The

text: Agulhas Passage

text: consists of 120-160 Ma-old oceanic crust, whereas the 100-80 Ma-old Agulhas Plateau rises  above the surrounding ocean floor while the Moho dips to between  below it.

answers: NDQ_003351

answers: Moho

answers: NDQ_003352

answers: increases in hardness

answers: NDQ_003353

answers: Moho

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: Moho

answers: NDQ_003356

answers: rise above

answers: NDQ_003357

answers: Moho dips to between below it

answers: NDQ_003358

answers: Plateau

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: Agulhas Passage consists of 120-160 Ma-old oceanic crust

answers: NDQ_003363

answers: Agulhas Passage

answers: NDQ_003371

answers: How old is the Agulhas Passage?

answers: NDQ_003373

answers: What is the Moho?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What is the Moho?

answers: NDQ_003381

answers: What is the Moho?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the Moho?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is the Moho?

answers: NDQ_003386

answers: What is the Moho?

answers: NDQ_003387

answers: Which of the following is not a normal fault: Agulhas Passage, Moho or Agulhas Plateau?

answers: NDQ_003388

answers: What is the Moho?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: Agulhas Passage

answers: NDQ_003391

answers: Agulhas Plateau

answers: NDQ_003392

answers: Agulhas Passage

answers: NDQ_003393

answers: Agulhas Plateau

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: Moho dips to between below it.

answers: NDQ_003396

answers: Moho

answers: NDQ_003351

answers: continent-ocean transition.

answers: NDQ_003352

answers: rises above the surrounding ocean floor

answers: NDQ_003353

answers: The boundary between the Earth's crust and the mantle

answers: NDQ_003354

answers: the 100-80 Ma-old Agulhas Plateau

answers: NDQ_003355

answers: Moho) rises from between the Agulhas Bank

answers: NDQ_003356

answers: the 100-80 Ma-old Agulhas Plateau

answers: NDQ_003357

answers: the Moho dips to between below it.

answers: NDQ_003358

answers: Agulhas Plateau

answers: NDQ_003359

answers: The boundary between the Earth's crust and the mantle

answers: NDQ_003360

answers: continent-ocean transition.

answers: NDQ_003362

answers: The boundary between the Earth's crust and the mantle

answers: NDQ_003363

answers: Agulhas Bank

answers: NDQ_003371

answers: 100-80 Ma-old Agulhas Plateau

answers: NDQ_003373

answers: The boundary between the Earth's crust and the mantle

answers: NDQ_003376

answers: the 100-80 Ma-old Agulhas Plateau

answers: NDQ_003378

answers: The boundary between the Earth's crust and the mantle

answers: NDQ_003379

answers: Agulhas Plateau rises above the surrounding ocean floor

answers: NDQ_003380

answers: The boundary between the Earth's crust and the mantle

answers: NDQ_003381

answers: The boundary between the Earth's crust and the mantle

answers: NDQ_003382

answers: continent-ocean transition.

answers: NDQ_003383

answers: The boundary between the Earth's crust and the mantle

answers: NDQ_003384

answers: Agulhas Plateau

answers: NDQ_003385

answers: The boundary between the Earth's crust and the mantle

answers: NDQ_003386

answers: The boundary between the Earth's crust and the mantle

answers: NDQ_003387

answers: The boundary between the Earth's crust and the mantle

answers: NDQ_003388

answers: The boundary between the Earth's crust and the mantle

answers: NDQ_003389

answers: the 100-80 Ma-old Agulhas Plateau

answers: NDQ_003390

answers: Moho

answers: NDQ_003391

answers: Moho

answers: NDQ_003392

answers: Agulhas Plateau

answers: NDQ_003393

answers: Agulhas Plateau

answers: NDQ_003394

answers: The boundary between the Earth's crust and the mantle

answers: NDQ_003395

answers: The boundary between the Earth's crust and the mantle

answers: NDQ_003396

answers: continent-ocean transition.

text: Although a few mineral grains are known to be Hadean, the oldest rock formations exposed on the surface of the Earth are Archean or slightly older. Archean rocks are found in Greenland, the Canadian Shield, Montana and Wyoming (exposed parts of the Wyoming Craton), the Baltic Shield, Scotland, India, Brazil, western Australia, and southern Africa. Although the first continents formed during this eon, rock of this age makes up only 7% of the present world's cratons; even allowing for erosion and destruction of past formations, evidence suggests that continental crust equivalent to only 5-40% of the amount formed during the Archean.

text: Although a few mineral grains are known to be

text: Hadean

text: , the oldest rock formations exposed on the surface of the

text: Earth

text: are Archean or slightly older. Archean rocks are found in

text: Greenland

text: , the

text: Canadian Shield

text: Montana

text: and

text: Wyoming

text: (exposed parts of the

text: Wyoming Craton

text: ), the

text: Baltic Shield

text: Scotland

text: India

text: Brazil

text: , western

text: Australia

text: , and southern

text: Africa

text: . Although the first

text: continents

text: formed during this eon, rock of this age makes up only 7% of the present world's

text: craton

text: s; even allowing for erosion and destruction of past formations, evidence suggests that continental

text: crust

text: equivalent to only 5-40% of the amount formed during the Archean.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: causes it to age

answers: NDQ_003353

answers: erosion

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: Wyoming Craton

answers: NDQ_003356

answers: destroy formations

answers: NDQ_003357

answers: rock of this age makes up only 7%

answers: NDQ_003358

answers: craton

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Wyoming Craton

answers: NDQ_003362

answers: a few mineral grains are known to be Hadean

answers: NDQ_003363

answers: Archean

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: unanswerable

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What type of force applied to rock is stress?

answers: NDQ_003381

answers: what is the first continents formed during?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: what is the first continents formed during this eon

answers: NDQ_003385

answers: fault zone

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: what is the first continents formed during this eon?

answers: NDQ_003388

answers: what is the first continents formed during this eon?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: Wyoming Craton

answers: NDQ_003391

answers: Wyoming Craton

answers: NDQ_003392

answers: Wyoming Craton

answers: NDQ_003393

answers: Wyoming Craton

answers: NDQ_003394

answers: the Baltic Shield

answers: NDQ_003395

answers: Wyoming Craton

answers: NDQ_003396

answers: Wyoming Craton

answers: NDQ_003351

answers: Archean

answers: NDQ_003352

answers: erosion and destruction

answers: NDQ_003353

answers: erosion and destruction

answers: NDQ_003354

answers: Archean

answers: NDQ_003355

answers: Hadean,

answers: NDQ_003356

answers: erosion and destruction

answers: NDQ_003357

answers: erosion

answers: NDQ_003358

answers: Hadean,

answers: NDQ_003359

answers: Archean

answers: NDQ_003360

answers: Archean

answers: NDQ_003362

answers: Hadean,

answers: NDQ_003363

answers: Archean.

answers: NDQ_003371

answers: Archean

answers: NDQ_003373

answers: Archean

answers: NDQ_003376

answers: Archean

answers: NDQ_003378

answers: Archean

answers: NDQ_003379

answers: Archean

answers: NDQ_003380

answers: erosion

answers: NDQ_003381

answers: Archean

answers: NDQ_003382

answers: Archean

answers: NDQ_003383

answers: erosion

answers: NDQ_003384

answers: Archean

answers: NDQ_003385

answers: Archean

answers: NDQ_003386

answers: Archean

answers: NDQ_003387

answers: Archean

answers: NDQ_003388

answers: Archean

answers: NDQ_003389

answers: erosion

answers: NDQ_003390

answers: Archean

answers: NDQ_003391

answers: Archean

answers: NDQ_003392

answers: Archean

answers: NDQ_003393

answers: Archean

answers: NDQ_003394

answers: Archean

answers: NDQ_003395

answers: Archean

answers: NDQ_003396

answers: Archean

text: As explained above, tectonic plates may include continental crust or oceanic crust, and most plates contain both. For example, the African Plate includes the continent and parts of the floor of the Atlantic and Indian Oceans. The distinction between oceanic crust and continental crust is based on their modes of formation. Oceanic crust is formed at sea-floor spreading centers, and continental crust is formed through arc volcanism and accretion of terranes through tectonic processes, though some of these terranes may contain ophiolite sequences, which are pieces of oceanic crust considered to be part of the continent when they exit the standard cycle of formation and spreading centers and subduction beneath continents. Oceanic crust is also denser than continental crust owing to their different compositions. Oceanic crust is denser because it has less silicon and more heavier elements ("mafic") than continental crust ("felsic"). As a result of this density stratification, oceanic crust generally lies below sea level (for example most of the Pacific Plate), while continental crust buoyantly projects above sea level (see the page isostasy for explanation of this principle).

text: As explained above, tectonic plates may include continental crust or oceanic crust, and most plates contain both. For example, the

text: African Plate

text: includes the continent and parts of the floor of the

text: Atlantic

text: and

text: Indian

text: Oceans. The distinction between oceanic crust and continental crust is based on their modes of formation. Oceanic crust is formed at sea-floor spreading centers, and continental crust is formed through

text: arc volcanism

text: and

text: accretion

text: of

text: terrane

text: s through tectonic processes, though some of these terranes may contain

text: ophiolite

text: sequences, which are pieces of oceanic crust considered to be part of the continent when they exit the standard cycle of formation and spreading centers and subduction beneath continents. Oceanic crust is also denser than continental crust owing to their different compositions. Oceanic crust is denser because it has less silicon and more heavier elements ("

text: mafic

text: ") than continental crust ("

text: felsic

text: "). As a result of this density stratification, oceanic crust generally lies below

text: sea level

text: (for example most of the

text: Pacific Plate

text: ), while continental crust buoyantly projects above sea level (see the page

text: isostasy

text: for explanation of this principle).

answers: NDQ_003351

answers: oceanic crust

answers: NDQ_003352

answers: has less silicon and more heavier elements

answers: NDQ_003353

answers: tectonic plates

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: continental crust

answers: NDQ_003356

answers: subduct

answers: NDQ_003357

answers: oceanic crust generally lies below sea level

answers: NDQ_003358

answers: unanswerable

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: continental crust

answers: NDQ_003362

answers: oceanic crust is denser than continental crust

answers: NDQ_003363

answers: oceanic crust

answers: NDQ_003371

answers: What is the difference between continental crust and oceanic crust?

answers: NDQ_003373

answers: oceanic crust is denser than continental crust

answers: NDQ_003376

answers: oceanic crust is also denser than continental crust

answers: NDQ_003378

answers: oceanic crust is also denser than continental crust owing to their different compositions

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What is the difference between continental crust and oceanic crust?

answers: NDQ_003381

answers: What causes rock to deform?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What is the difference between oceanic crust and continental crust?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: tectonic plates

answers: NDQ_003387

answers: What is the difference between oceanic crust and continental crust?

answers: NDQ_003388

answers: What is the difference between continental crust and oceanic crust?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: subduction

answers: NDQ_003391

answers: ophiolite

answers: NDQ_003392

answers: ophiolite

answers: NDQ_003393

answers: continental crust

answers: NDQ_003394

answers: subduction

answers: NDQ_003395

answers: tectonic plate

answers: NDQ_003396

answers: tectonic

answers: NDQ_003351

answers: arc volcanism

answers: NDQ_003352

answers: oceanic crust generally lies below sea level

answers: NDQ_003353

answers: density stratification, oceanic crust generally lies below sea level

answers: NDQ_003354

answers: oceanic crust generally lies below sea level

answers: NDQ_003355

answers: ophiolite sequences,

answers: NDQ_003356

answers: oceanic crust generally lies below sea level

answers: NDQ_003357

answers: subduction

answers: NDQ_003358

answers: arc volcanism

answers: NDQ_003359

answers: arc volcanism

answers: NDQ_003360

answers: tectonic plates

answers: NDQ_003362

answers: continental crust buoyantly projects above sea level

answers: NDQ_003363

answers: sea-floor spreading centers,

answers: NDQ_003371

answers: ophiolite sequences,

answers: NDQ_003373

answers: oceanic crust generally lies below sea level

answers: NDQ_003376

answers: accretion of terranes through tectonic processes,

answers: NDQ_003378

answers: oceanic crust generally lies below sea level

answers: NDQ_003379

answers: oceanic crust generally lies below sea level

answers: NDQ_003380

answers: arc volcanism

answers: NDQ_003381

answers: oceanic crust generally lies below sea level

answers: NDQ_003382

answers: arc volcanism

answers: NDQ_003383

answers: arc volcanism

answers: NDQ_003384

answers: arc volcanism

answers: NDQ_003385

answers: tectonic plates

answers: NDQ_003386

answers: arc volcanism

answers: NDQ_003387

answers: arc volcanism

answers: NDQ_003388

answers: arc volcanism

answers: NDQ_003389

answers: arc volcanism

answers: NDQ_003390

answers: subduction

answers: NDQ_003391

answers: ophiolite sequences,

answers: NDQ_003392

answers: isostasy

answers: NDQ_003393

answers: continental crust buoyantly projects above sea level

answers: NDQ_003394

answers: arc volcanism

answers: NDQ_003395

answers: arc volcanism

answers: NDQ_003396

answers: arc volcanism

text: Continents continued to drift toward their present positions. Of the modern geologic features, only the land bridge between South America and North America was absent, although South America was approaching the western subduction zone in the Pacific Ocean, causing both the rise of the Andes and a southward extension of the Meso-American peninsula.

text: Continents continued to

text: drift

text: toward their present positions. Of the modern geologic features, only the land bridge between

text: South America

text: and

text: North America

text: was absent, although South America was approaching the western

text: subduction zone

text: in the

text: Pacific Ocean

text: , causing both the rise of the

text: Andes

text: and a southward extension of the

text: Meso-American

text: peninsula.

answers: NDQ_003351

answers: subduction zone

answers: NDQ_003352

answers: rises

answers: NDQ_003353

answers: subduction

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: subduction zone

answers: NDQ_003356

answers: extend

answers: NDQ_003357

answers: South America was approaching the western subduction zone

answers: NDQ_003358

answers: subduction zone

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: subduction zones

answers: NDQ_003362

answers: the land bridge between South America and North America was absent

answers: NDQ_003363

answers: Pacific Ocean

answers: NDQ_003371

answers: Which of the following is not an example of a thrust fault?

answers: NDQ_003373

answers: How would you describe the land bridge between South America and North America

answers: NDQ_003376

answers: What is the land bridge between South America and North America?

answers: NDQ_003378

answers: what is the last word in the passage?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: How would you describe the land bridge between South America and North America?

answers: NDQ_003381

answers: What caused the land bridge between South America and North America to be absent?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: Which of the following is not a cause of earthquakes?

answers: NDQ_003387

answers: What caused the land bridge between South America and North America to be absent?

answers: NDQ_003388

answers: What caused the rise of the Andes and a southward extension of the Meso-American peninsula

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: subduction zone

answers: NDQ_003391

answers: subduction zone

answers: NDQ_003392

answers: subduction zone

answers: NDQ_003393

answers: subduction zone

answers: NDQ_003394

answers: western subduction zone

answers: NDQ_003395

answers: subduction zone

answers: NDQ_003396

answers: subduction zone

answers: NDQ_003351

answers: subduction zone

answers: NDQ_003352

answers: the rise of the Andes

answers: NDQ_003353

answers: subduction zone

answers: NDQ_003354

answers: South America was approaching the western subduction zone

answers: NDQ_003355

answers: subduction zone

answers: NDQ_003356

answers: rise of the Andes

answers: NDQ_003357

answers: subduction zone

answers: NDQ_003358

answers: subduction zone

answers: NDQ_003359

answers: subduction zone

answers: NDQ_003360

answers: subduction zone in the Pacific Ocean,

answers: NDQ_003362

answers: the land bridge between South America and North America was absent,

answers: NDQ_003363

answers: western subduction zone in the Pacific Ocean,

answers: NDQ_003371

answers: South America was approaching the western subduction zone

answers: NDQ_003373

answers: South America was approaching the western subduction zone

answers: NDQ_003376

answers: South America was approaching the western subduction zone

answers: NDQ_003378

answers: Continents continued to drift toward their present positions.

answers: NDQ_003379

answers: South America was approaching the western subduction zone

answers: NDQ_003380

answers: South America was approaching the western subduction zone

answers: NDQ_003381

answers: South America was approaching the western subduction zone

answers: NDQ_003382

answers: subduction zone

answers: NDQ_003383

answers: South America was approaching the western subduction zone

answers: NDQ_003384

answers: South America was approaching the western subduction zone

answers: NDQ_003385

answers: subduction zone

answers: NDQ_003386

answers: South America was approaching the western subduction zone

answers: NDQ_003387

answers: South America was approaching the western subduction zone

answers: NDQ_003388

answers: South America was approaching the western subduction zone

answers: NDQ_003389

answers: subduction zone

answers: NDQ_003390

answers: subduction zone

answers: NDQ_003391

answers: subduction zone

answers: NDQ_003392

answers: subduction zone

answers: NDQ_003393

answers: subduction zone

answers: NDQ_003394

answers: subduction zone

answers: NDQ_003395

answers: subduction zone

answers: NDQ_003396

answers: subduction zone

text: Much of the Lizard peninsula is known for its botany and geology, and about 375 million years ago the molten rock, which eventually became the Lizard, was about 10 km below the surface of the earth and under immense heat and pressure. One of the rocks (peridotite) is rich in magnesium and iron, and changed through heat and pressure to serpentinite as it pushed upwards from the Moho, the boundary of the earth's crust and mantle. It finally reached the crust's surface, about 30° south of the equator as part of an ocean ridge, in the Rheic Ocean. Over the next 80 million years the Rheic Ocean disappeared and the mass of rock heads north crossing the equator about 250 million years ago. The Tropic of Cancer is passed less than 100 million years ago and the rock, which becomes the Lizard, finally reached 50° north at about the start of the last Ice Age. There are two types of serpentine at Kynance: bastite and tremolite. The rocks at the car park, cliffs to the south and the path to the cove are bastite serpentine, which is the primary serpentine on the Lizard. The rock is coarse-grained with large shiny crystals of bastite which give a flecked appearance. The islands and stacks within the cove and the valley are of tremolite serpentine which is fine-grained and banded. Tremolite is different to the bastite serpentine because it was subject to higher pressure within the crust. Kynance Cove is an important site for geologists because of the exposures of the two types of ophiolitic serpentinite, together with granite and gneiss pods within the serpentine. The area has been designated as a Geological Conservation Review site.

text: Much of the Lizard peninsula is known for its

text: botany

text: and

text: geology

text: , and about 375 million years ago the molten rock, which eventually became the Lizard, was about 10 km below the surface of the earth and under immense heat and pressure. One of the rocks (

text: peridotite

text: ) is rich in

text: magnesium

text: and

text: iron

text: , and changed through heat and pressure to

text: serpentinite

text: as it pushed upwards from the

text: Moho

text: , the boundary of the earth's

text: crust

text: and

text: mantle

text: . It finally reached the crust's surface, about 30° south of the

text: equator

text: as part of an

text: ocean ridge

text: , in the

text: Rheic Ocean

text: . Over the next 80 million years the Rheic Ocean disappeared and the mass of rock heads north crossing the equator about 250 million years ago. The

text: Tropic of Cancer

text: is passed less than 100 million years ago and the rock, which becomes the Lizard, finally reached 50° north at about the start of the last

text: Ice Age

text: . There are two types of serpentine at Kynance: bastite and tremolite. The rocks at the car park, cliffs to the south and the path to the cove are bastite serpentine, which is the primary serpentine on the Lizard. The rock is coarse-grained with large shiny crystals of bastite which give a flecked appearance. The islands and stacks within the cove and the valley are of tremolite serpentine which is fine-grained and banded. Tremolite is different to the bastite serpentine because it was subject to higher pressure within the crust. Kynance Cove is an important site for geologists because of the exposures of the two types of

text: ophiolitic

text: serpentinite, together with granite and gneiss pods within the serpentine. The area has been designated as a

text: Geological Conservation Review

text: site.

answers: NDQ_003351

answers: bastite

answers: NDQ_003352

answers: tremolite

answers: NDQ_003353

answers: heat and pressure

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: ocean ridge

answers: NDQ_003356

answers: change to what?

answers: NDQ_003357

answers: tremolite serpentine is different to the bastite serpentine because it was subjected to higher pressure within the crust

answers: NDQ_003358

answers: cliff

answers: NDQ_003359

answers: is pushed upwards

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: The Tropic of Cancer is passed less than 100 million years ago

answers: NDQ_003363

answers: 375 million years ago

answers: NDQ_003371

answers: Which of the following is not a type of serpentine: bastite or tremolite?

answers: NDQ_003373

answers: Why is tremolite different to the bastite serpentine?

answers: NDQ_003376

answers: Which of the following is not a type of serpentine: bastite or tremolite?

answers: NDQ_003378

answers: What is the primary serpentine on the Lizard?

answers: NDQ_003379

answers: What is the dip of the fault plane in a strike-slip fault?

answers: NDQ_003380

answers: Which of the following is not a type of rock: bastite or tremolite?

answers: NDQ_003381

answers: What is the primary serpentine on the Lizard?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock: heat and pressure?

answers: NDQ_003384

answers: Which of the following is not a type of serpentine: bastite, tremolite or ophiolitic?

answers: NDQ_003385

answers: Which of the following is not a type of serpentine?

answers: NDQ_003386

answers: Which of the following is not a type of serpentine?

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: bastite serpentine or tremolite serpentine?

answers: NDQ_003388

answers: Which of the following is not a type of serpentine: bastite or tremolite?

answers: NDQ_003389

answers: Which of the following is not a type of serpentine?

answers: NDQ_003390

answers: ophiolitic

answers: NDQ_003391

answers: bastite serpentine

answers: NDQ_003392

answers: Moho

answers: NDQ_003393

answers: ophiolitic

answers: NDQ_003394

answers: tremolite

answers: NDQ_003395

answers: unanswerable

answers: NDQ_003396

answers: bastite serpentine

answers: NDQ_003351

answers: tremolite

answers: NDQ_003352

answers: Tremolite

answers: NDQ_003353

answers: heat and pressure to serpentinite

answers: NDQ_003354

answers: bastite

answers: NDQ_003355

answers: ocean ridge,

answers: NDQ_003356

answers: serpentinite

answers: NDQ_003357

answers: tremolite

answers: NDQ_003358

answers: stacks

answers: NDQ_003359

answers: higher pressure

answers: NDQ_003360

answers: heat and pressure.

answers: NDQ_003362

answers: bastite serpentine,

answers: NDQ_003363

answers: the Lizard.

answers: NDQ_003371

answers: tremolite

answers: NDQ_003373

answers: tremolite

answers: NDQ_003376

answers: tremolite serpentine

answers: NDQ_003378

answers: tremolite serpentine

answers: NDQ_003379

answers: tremolite

answers: NDQ_003380

answers: pressure.

answers: NDQ_003381

answers: tremolite serpentine

answers: NDQ_003382

answers: tremolite serpentine

answers: NDQ_003383

answers: tremolite serpentine

answers: NDQ_003384

answers: tremolite

answers: NDQ_003385

answers: tremolite serpentine

answers: NDQ_003386

answers: tremolite serpentine

answers: NDQ_003387

answers: tremolite

answers: NDQ_003388

answers: tremolite serpentine

answers: NDQ_003389

answers: bastite serpentine,

answers: NDQ_003390

answers: tremolite serpentine

answers: NDQ_003391

answers: ophiolitic serpentinite,

answers: NDQ_003392

answers: tremolite serpentine

answers: NDQ_003393

answers: bastite serpentine,

answers: NDQ_003394

answers: tremolite serpentine

answers: NDQ_003395

answers: tremolite serpentine

answers: NDQ_003396

answers: tremolite serpentine

text: Near the southeast corner of the quadrangle (37° N, 225° E) lies a southward sloping, semicircular block of ancient, heavily cratered, highland crust that is dissected by numerous, arcuate troughs (Acheron Fossae). The troughs are grabens, structures formed when the crust moves downward between two faults. Grabens form in areas where the crust has undergone extensional stress. The Acheron Fossae region is partially covered by volcanic deposits from Alba Mons in the east, geologically young basaltic lava flows or sediments in the west and southeast, and the jumbled, furrowed terrain of Lycus Sulci in the south.

text: Near the southeast corner of the quadrangle (37° N, 225° E) lies a southward sloping, semicircular block of ancient, heavily cratered, highland crust that is dissected by numerous,

text: arcuate

text: troughs (

text: Acheron Fossae

text: ). The troughs are grabens, structures formed when the crust moves downward between two faults.

text: Graben

text: s form in areas where the crust has undergone extensional stress. The Acheron Fossae region is partially covered by volcanic deposits from Alba Mons in the east, geologically young

text: basalt

text: ic lava flows or sediments in the west and southeast, and the jumbled, furrowed terrain of Lycus Sulci in the south.

answers: NDQ_003351

answers: extensional

answers: NDQ_003352

answers: grabens form

answers: NDQ_003353

answers: Grabens

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: Grabens

answers: NDQ_003356

answers: grabens

answers: NDQ_003357

answers: the crust moves downward between two faults

answers: NDQ_003358

answers: trough

answers: NDQ_003359

answers: grabens

answers: NDQ_003360

answers: extensional stress

answers: NDQ_003362

answers: grabens form in areas where the crust has undergone extensional stress

answers: NDQ_003363

answers: Acheron Fossae

answers: NDQ_003371

answers: Which of the following is not a trough: grabens, structures formed when the crust moves downward between two faults

answers: NDQ_003373

answers: no

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: what is the last word in the passage?

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What is a stress?

answers: NDQ_003381

answers: What type of stress does grabens form in areas where the crust has undergone extensional stress?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not a type of fold: grabens, structures formed when the crust moves downward between two faults?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: Why do grabens form?

answers: NDQ_003387

answers: Which of the following is not caused by extensional stress: Grabens or normal faults?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip faults, grabens, or extensional stress?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: Grabens

answers: NDQ_003391

answers: grabens

answers: NDQ_003392

answers: Grabens

answers: NDQ_003393

answers: highland crust

answers: NDQ_003394

answers: arcuate

answers: NDQ_003395

answers: grabens

answers: NDQ_003396

answers: Grabens

answers: NDQ_003351

answers: extensional

answers: NDQ_003352

answers: Grabens

answers: NDQ_003353

answers: Grabens

answers: NDQ_003354

answers: (Acheron Fossae).

answers: NDQ_003355

answers: grabens,

answers: NDQ_003356

answers: Grabens form in areas where the crust has undergone extensional stress.

answers: NDQ_003357

answers: the crust moves downward

answers: NDQ_003358

answers: grabens,

answers: NDQ_003359

answers: extensional stress.

answers: NDQ_003360

answers: the crust moves downward between two faults.

answers: NDQ_003362

answers: a southward sloping,

answers: NDQ_003363

answers: the crust moves downward between two faults.

answers: NDQ_003371

answers: Grabens form in areas where the crust has undergone extensional stress.

answers: NDQ_003373

answers: extensional stress.

answers: NDQ_003376

answers: Grabens form in areas where the crust has undergone extensional stress.

answers: NDQ_003378

answers: the crust moves downward between two faults.

answers: NDQ_003379

answers: downward

answers: NDQ_003380

answers: extensional stress.

answers: NDQ_003381

answers: extensional stress.

answers: NDQ_003382

answers: extensional stress.

answers: NDQ_003383

answers: Grabens form in areas where the crust has undergone extensional stress.

answers: NDQ_003384

answers: grabens,

answers: NDQ_003385

answers: grabens, structures formed when the crust moves downward between two faults.

answers: NDQ_003386

answers: extensional stress.

answers: NDQ_003387

answers: extensional stress.

answers: NDQ_003388

answers: extensional stress.

answers: NDQ_003389

answers: the crust moves downward between two faults.

answers: NDQ_003390

answers: grabens,

answers: NDQ_003391

answers: grabens,

answers: NDQ_003392

answers: grabens,

answers: NDQ_003393

answers: grabens,

answers: NDQ_003394

answers: faults.

answers: NDQ_003395

answers: two faults.

answers: NDQ_003396

answers: grabens,

text: The Great Glen Fault is a long strike-slip (transcurrent) fault that runs through its namesake the Great Glen (Glen Albyn) in Scotland.

text: The Great Glen Fault is a long

text: strike-slip (transcurrent) fault

text: that runs through its namesake the

text: Great Glen

text: (Glen Albyn) in

text: Scotland

answers: NDQ_003351

answers: strike-slip

answers: NDQ_003352

answers: is likely to crack

answers: NDQ_003353

answers: faults

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: strike-slip

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: strike-slip is a type of

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: is moved too fast

answers: NDQ_003360

answers: faults

answers: NDQ_003362

answers: The Great Glen Fault runs through its namesake the Great Glen in Scotland.

answers: NDQ_003363

answers: Great Glen Fault

answers: NDQ_003371

answers: What type of fault is the Great Glen Fault?

answers: NDQ_003373

answers: How would you describe a rock that is deeply buried?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: what is the last word in the passage?

answers: NDQ_003379

answers: no

answers: NDQ_003380

answers: How would you describe the Great Glen Fault?

answers: NDQ_003381

answers: What type of stress does the Great Glen Fault cause?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: What kind of fold is the Great Glen Fault?

answers: NDQ_003385

answers: What type of fault is the Great Glen Fault?

answers: NDQ_003386

answers: Why is the Great Glen Fault important?

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: strike-slip or compression stress?

answers: NDQ_003388

answers: What type of fault is the Great Glen Fault?

answers: NDQ_003389

answers: None of the above choices.

answers: NDQ_003390

answers: strike-slip

answers: NDQ_003391

answers: strike-slip fault

answers: NDQ_003392

answers: strike-slip

answers: NDQ_003393

answers: strike-slip fault

answers: NDQ_003394

answers: strike-slip

answers: NDQ_003395

answers: strike-slip

answers: NDQ_003396

answers: strike-slip

answers: NDQ_003351

answers: (transcurrent)

answers: NDQ_003352

answers: strike-slip

answers: NDQ_003353

answers: strike-slip

answers: NDQ_003354

answers: The Great Glen Fault

answers: NDQ_003355

answers: strike-slip

answers: NDQ_003356

answers: strike-slip

answers: NDQ_003357

answers: strike-slip

answers: NDQ_003358

answers: strike-slip (transcurrent) fault

answers: NDQ_003359

answers: strike-slip

answers: NDQ_003360

answers: The Great Glen Fault

answers: NDQ_003362

answers: The Great Glen Fault

answers: NDQ_003363

answers: The Great Glen Fault

answers: NDQ_003371

answers: The Great Glen Fault

answers: NDQ_003373

answers: The Great Glen Fault

answers: NDQ_003376

answers: The Great Glen Fault

answers: NDQ_003378

answers: (transcurrent)

answers: NDQ_003379

answers: (transcurrent)

answers: NDQ_003380

answers: strike-slip

answers: NDQ_003381

answers: The Great Glen Fault

answers: NDQ_003382

answers: strike-slip

answers: NDQ_003383

answers: strike-slip

answers: NDQ_003384

answers: The Great Glen Fault

answers: NDQ_003385

answers: The Great Glen Fault

answers: NDQ_003386

answers: strike-slip

answers: NDQ_003387

answers: strike-slip

answers: NDQ_003388

answers: (transcurrent)

answers: NDQ_003389

answers: The Great Glen Fault is a long strike-slip

answers: NDQ_003390

answers: The Great Glen Fault

answers: NDQ_003391

answers: strike-slip

answers: NDQ_003392

answers: The Great Glen Fault

answers: NDQ_003393

answers: strike-slip

answers: NDQ_003394

answers: The Great Glen Fault

answers: NDQ_003395

answers: strike-slip

answers: NDQ_003396

answers: strike-slip

text: In 1966, Jordan published the 182 page work Die Expansion der Erde. Folgerungen aus der Diracschen Gravitationshypothese (The expansion of the Earth. Conclusions from the Dirac gravitation hypothesis) in which he developed his theory that, according to Paul Dirac's hypothesis of a steady weakening of gravitation throughout the history of the universe, the Earth may have swollen to its current size, from an initial ball of a diameter of only about . This theory could explain why the ductile lower sima layer of the Earth's crust is of a comparatively uniform thickness, while the brittle upper sial layer of the Earth's crust had broken apart into the main continental plates. The continents having to adapt to the ever flatter surface of the growing ball, the mountain ranges on the Earth's surface would, in the course of that, have come into being as constricted folds. Despite the energy Jordan invested in the expanding Earth theory, his geological work was never taken seriously by either physicists or geologists.

text: In 1966, Jordan published the 182 page work Die Expansion der Erde. Folgerungen aus der Diracschen Gravitationshypothese (The expansion of the Earth. Conclusions from the Dirac gravitation hypothesis) in which he developed his theory that, according to

text: Paul Dirac's hypothesis

text: of a steady weakening of

text: gravitation

text: throughout the history of the universe, the

text: Earth

text: may have swollen to its current size, from an initial ball of a diameter of only about . This theory could explain why the

text: ductile

text: lower

text: sima

text: layer of the

text: Earth's crust

text: is of a comparatively uniform thickness, while the brittle upper

text: sial

text: layer of the Earth's crust had broken apart into the main

text: continental plates

text: . The continents having to adapt to the ever flatter surface of the growing ball, the mountain ranges on the Earth's surface would, in the course of that, have come into being as constricted folds. Despite the energy Jordan invested in the expanding Earth theory, his geological work was never taken seriously by either physicists or geologists.

answers: NDQ_003351

answers: brittle

answers: NDQ_003352

answers: brittle

answers: NDQ_003353

answers: brittle upper sial layer

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: mountain ranges

answers: NDQ_003356

answers: swell

answers: NDQ_003357

answers: brittle upper sial layer of the Earth's crust had broken apart into the main continental plates

answers: NDQ_003358

answers: sial layer

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: continental plates

answers: NDQ_003362

answers: his geological work was never taken seriously by either physicists or geologists

answers: NDQ_003363

answers: the ever flatter surface of the growing ball

answers: NDQ_003371

answers: What may have come into being as constricted folds?

answers: NDQ_003373

answers: Why did Jordan invest in the expanding Earth theory?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What type of force applied to rock is a stress?

answers: NDQ_003381

answers: What type of rock deforms?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: fault zone

answers: NDQ_003386

answers: What is the cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: normal faults, brittle upper sial layer of the Earth's crust or gravity?

answers: NDQ_003388

answers: What type of faults result from shear stress?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: constricted folds

answers: NDQ_003391

answers: sial layer

answers: NDQ_003392

answers: constricted folds

answers: NDQ_003393

answers: sima layer

answers: NDQ_003394

answers: continental plates

answers: NDQ_003395

answers: a vertical fault plane

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: brittle upper sial layer

answers: NDQ_003352

answers: brittle

answers: NDQ_003353

answers: constricted folds.

answers: NDQ_003354

answers: never taken seriously by either physicists or geologists.

answers: NDQ_003355

answers: constricted folds.

answers: NDQ_003356

answers: constricted folds.

answers: NDQ_003357

answers: constricted folds.

answers: NDQ_003358

answers: constricted folds.

answers: NDQ_003359

answers: brittle

answers: NDQ_003360

answers: constricted folds.

answers: NDQ_003362

answers: constricted folds.

answers: NDQ_003363

answers: constricted folds.

answers: NDQ_003371

answers: Diracschen Gravitationshypothese

answers: NDQ_003373

answers: ductile lower sima layer

answers: NDQ_003376

answers: constricted folds.

answers: NDQ_003378

answers: Diracschen Gravitationshypothese

answers: NDQ_003379

answers: comparatively uniform thickness,

answers: NDQ_003380

answers: Diracschen Gravitationshypothese

answers: NDQ_003381

answers: constricted folds.

answers: NDQ_003382

answers: constricted folds.

answers: NDQ_003383

answers: brittle upper sial layer of the Earth's crust had broken apart

answers: NDQ_003384

answers: constricted folds.

answers: NDQ_003385

answers: Diracschen Gravitationshypothese

answers: NDQ_003386

answers: continental plates.

answers: NDQ_003387

answers: constricted folds.

answers: NDQ_003388

answers: brittle upper sial layer

answers: NDQ_003389

answers: constricted folds.

answers: NDQ_003390

answers: constricted folds.

answers: NDQ_003391

answers: ductile lower sima layer

answers: NDQ_003392

answers: constricted folds.

answers: NDQ_003393

answers: upper sial layer

answers: NDQ_003394

answers: constricted folds.

answers: NDQ_003395

answers: constricted folds.

answers: NDQ_003396

answers: constricted folds.

text: The Knobs are part of the same structural fold of the earth’s crust that continues to the north as Champe Knobs (with its Champe Rocks and Yellow Rocks) and to the south as River Hill and (in Virginia) Lantz Mountain.

text: The Knobs are part of the same structural fold of the earth’s crust that continues to the north as Champe Knobs (with its

text: Champe Rocks

text: and Yellow Rocks) and to the south as River Hill and (in

text: Virginia

text: Lantz Mountain

answers: NDQ_003351

answers: Lantz Mountain

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: igneous rocks to form

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: structural fold

answers: NDQ_003356

answers: change color

answers: NDQ_003357

answers: Champe Rocks and Yellow Rocks are types of what?

answers: NDQ_003358

answers: Knob

answers: NDQ_003359

answers: collapses

answers: NDQ_003360

answers: structural folds

answers: NDQ_003362

answers: The San Andreas fault is located in the Pacific Ocean.

answers: NDQ_003363

answers: the same structural fold

answers: NDQ_003371

answers: What may be the reason for the older rocks being above the younger rocks?

answers: NDQ_003373

answers: How would you describe Champe Knobs?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: (in Virginia) Lantz Mountain

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: How would you describe Champe Knobs?

answers: NDQ_003381

answers: what is the last place mentioned?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: None of the above choices.

answers: NDQ_003384

answers: What type of fold is the Knobs part of?

answers: NDQ_003385

answers: (in Virginia) Lantz Mountain

answers: NDQ_003386

answers: not enough information

answers: NDQ_003387

answers: Which of the following is not a type of normal fault?

answers: NDQ_003388

answers: Which of the following is not an example of a structural fold of the earth’s crust?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: structural fold

answers: NDQ_003391

answers: Lantz Mountain

answers: NDQ_003392

answers: structural fold

answers: NDQ_003393

answers: Lantz Mountain

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: NDQ_003396

answers: Yellow Rocks

answers: NDQ_003351

answers: Champe Rocks and Yellow Rocks)

answers: NDQ_003352

answers: Champe Rocks and Yellow Rocks)

answers: NDQ_003353

answers: Champe Rocks and Yellow Rocks)

answers: NDQ_003354

answers: Champe Knobs

answers: NDQ_003355

answers: structural fold

answers: NDQ_003356

answers: Champe Rocks and Yellow Rocks)

answers: NDQ_003357

answers: Champe Rocks and Yellow Rocks)

answers: NDQ_003358

answers: Lantz Mountain.

answers: NDQ_003359

answers: Champe Rocks and Yellow Rocks)

answers: NDQ_003360

answers: structural fold of the earth’s crust

answers: NDQ_003362

answers: The Knobs

answers: NDQ_003363

answers: structural fold of the earth’s crust

answers: NDQ_003371

answers: Champe Rocks and Yellow Rocks)

answers: NDQ_003373

answers: Champe Rocks and Yellow Rocks)

answers: NDQ_003376

answers: The Knobs are part of the same structural fold

answers: NDQ_003378

answers: Champe Knobs

answers: NDQ_003379

answers: Champe Knobs

answers: NDQ_003380

answers: Champe Rocks and Yellow Rocks)

answers: NDQ_003381

answers: Champe Rocks and Yellow Rocks)

answers: NDQ_003382

answers: Champe Rocks and Yellow Rocks)

answers: NDQ_003383

answers: Champe Rocks and Yellow Rocks)

answers: NDQ_003384

answers: Champe Knobs

answers: NDQ_003385

answers: Champe Rocks and Yellow Rocks)

answers: NDQ_003386

answers: earth’s crust

answers: NDQ_003387

answers: The Knobs

answers: NDQ_003388

answers: Champe Rocks and Yellow Rocks)

answers: NDQ_003389

answers: structural fold of the earth’s crust

answers: NDQ_003390

answers: Champe Knobs

answers: NDQ_003391

answers: Lantz Mountain.

answers: NDQ_003392

answers: Champe Knobs

answers: NDQ_003393

answers: Lantz Mountain.

answers: NDQ_003394

answers: Lantz Mountain.

answers: NDQ_003395

answers: Champe Rocks and Yellow Rocks)

answers: NDQ_003396

answers: Lantz Mountain.

text: At the beginning of the Palaeogene period of the Cenozoic era (66 to 23.8 million years ago) the formation of the Alps led to considerable tensions in the earth's crust, which, in their forelands to the north of the Alps, caused a bulge in the mantle and crust. At the apex of the arch so formed, there were considerable tensile stresses, so that the rock layers were stretched and about 35 million years ago, deep cracks and depressions in the earth's crust occurred (passive rifting). At the same time the sides of the newly created lowlands were uplifted, in the case of the Palatinate Forest, to a height of about 1000 metres.

text: At the beginning of the

text: Palaeogene

text: period of the

text: Cenozoic

text: era (66 to 23.8 million years ago) the formation of the

text: Alps

text: led to considerable tensions in the

text: earth's crust

text: , which, in their forelands to the north of the Alps, caused a bulge in the

text: mantle

text: and crust. At the apex of the arch so formed, there were considerable tensile stresses, so that the rock layers were stretched and about 35 million years ago, deep cracks and depressions in the earth's crust occurred (passive

text: rift

text: ing). At the same time the sides of the newly created lowlands were uplifted, in the case of the Palatinate Forest, to a height of about 1000 metres.

answers: NDQ_003351

answers: tensile

answers: NDQ_003352

answers: stretched

answers: NDQ_003353

answers: cracks and depressions

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: arch

answers: NDQ_003356

answers: stretch

answers: NDQ_003357

answers: deep cracks and depressions in the earth's crust occurred

answers: NDQ_003358

answers: passive rifting

answers: NDQ_003359

answers: stretched

answers: NDQ_003360

answers: passive rifting

answers: NDQ_003362

answers: deep cracks and depressions in the earth's crust occurred (passive rifting)

answers: NDQ_003363

answers: Cenozoic era

answers: NDQ_003371

answers: Which of the following is not an example of passive rifting?

answers: NDQ_003373

answers: no

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What is a stress?

answers: NDQ_003381

answers: What does passive rifting refer to?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the reason for deep cracks in the earth's crust?

answers: NDQ_003384

answers: what is the second to last word in the passage?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: What is passive rifting?

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: tensile stresses, passive rifting or compression stress?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip faults or passive rifting?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: passive rifting

answers: NDQ_003391

answers: lowlands

answers: NDQ_003392

answers: passive rifting

answers: NDQ_003393

answers: lowlands

answers: NDQ_003394

answers: passive rifting

answers: NDQ_003395

answers: passive rifting

answers: NDQ_003396

answers: passive rifting

answers: NDQ_003351

answers: tensile

answers: NDQ_003352

answers: the rock layers were stretched

answers: NDQ_003353

answers: the rock layers were stretched

answers: NDQ_003354

answers: 1000 metres.

answers: NDQ_003355

answers: arch

answers: NDQ_003356

answers: stretched

answers: NDQ_003357

answers: deep cracks and depressions

answers: NDQ_003358

answers: (passive rifting).

answers: NDQ_003359

answers: tensile stresses, so that the rock layers were stretched

answers: NDQ_003360

answers: tensile stresses,

answers: NDQ_003362

answers: 1000 metres.

answers: NDQ_003363

answers: Palaeogene period of the Cenozoic era

answers: NDQ_003371

answers: (passive rifting).

answers: NDQ_003373

answers: tensile stresses,

answers: NDQ_003376

answers: tensile stresses,

answers: NDQ_003378

answers: tensile stresses,

answers: NDQ_003379

answers: 1000 metres.

answers: NDQ_003380

answers: tensile stresses,

answers: NDQ_003381

answers: tensile stresses, so that the rock layers were stretched

answers: NDQ_003382

answers: tensile stresses,

answers: NDQ_003383

answers: tensile stresses, so that the rock layers were stretched

answers: NDQ_003384

answers: arch

answers: NDQ_003385

answers: tensile stresses,

answers: NDQ_003386

answers: tensile stresses,

answers: NDQ_003387

answers: tensile stresses,

answers: NDQ_003388

answers: tensile stresses,

answers: NDQ_003389

answers: (passive rifting).

answers: NDQ_003390

answers: (passive rifting).

answers: NDQ_003391

answers: (passive rifting).

answers: NDQ_003392

answers: tensile stresses,

answers: NDQ_003393

answers: Palatinate Forest,

answers: NDQ_003394

answers: (passive rifting).

answers: NDQ_003395

answers: (passive rifting).

answers: NDQ_003396

answers: (passive rifting).

text: A crust formed when the molten outer layer of Earth cooled to form a solid. The two models that explain land mass propose either a steady growth to the present-day forms or, more likely, a rapid growth early in Earth history followed by a long-term steady continental area. Continents formed by plate tectonics, a process ultimately driven by the continuous loss of heat from Earth's interior. On time scales lasting hundreds of millions of years, the supercontinents have assembled and broken apart. Roughly  (million years ago), one of the earliest known supercontinents, Rodinia, began to break apart. The continents later recombined to form Pannotia, 600–, then finally Pangaea, which also broke apart .

text: A crust formed when the molten outer layer of Earth cooled

text: to form

text: a solid. The two models that explain land mass propose either a steady growth to the present-day forms or, more likely, a rapid growth early in Earth history followed by a long-term steady continental area. Continents formed by

text: plate tectonics

text: , a process ultimately driven by the continuous loss of heat from Earth's interior. On

text: time scales

text: lasting hundreds of millions of years, the

text: supercontinent

text: s have assembled and broken apart. Roughly  (million years ago), one of the earliest known supercontinents,

text: Rodinia

text: , began to break apart. The continents later recombined to form

text: Pannotia

text: , 600–, then finally

text: Pangaea

text: , which also broke apart .

answers: NDQ_003351

answers: loss of heat

answers: NDQ_003352

answers: breaks apart

answers: NDQ_003353

answers: plate tectonics

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: the molten outer layer of Earth cooled to form a solid

answers: NDQ_003358

answers: unanswerable

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: plate tectonic

answers: NDQ_003362

answers: on time scales lasting hundreds of millions of years

answers: NDQ_003363

answers: plate tectonics

answers: NDQ_003371

answers: What is the process ultimately driven by the continuous loss of heat from Earth's interior

answers: NDQ_003373

answers: How would you describe the stress?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: Which of the following is not an example of a stress?

answers: NDQ_003381

answers: How does rock deform?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What type of fold is a syncline?

answers: NDQ_003385

answers: plate tectonics

answers: NDQ_003386

answers: plate tectonics

answers: NDQ_003387

answers: Which of the following is not a cause of normal faults: compression stress, plate tectonics, or plate tectonics?

answers: NDQ_003388

answers: Which of the following is not a cause of strike-slip faults: shear stress, plate tectonics, or a solid?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: tectonics

answers: NDQ_003391

answers: Continents

answers: NDQ_003392

answers: tectonics

answers: NDQ_003393

answers: Continent

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: plate tectonics

answers: NDQ_003396

answers: Pangaea

answers: NDQ_003351

answers: loss of heat

answers: NDQ_003352

answers: break apart.

answers: NDQ_003353

answers: loss of heat

answers: NDQ_003354

answers: long-term steady continental area.

answers: NDQ_003355

answers: plate tectonics,

answers: NDQ_003356

answers: solid.

answers: NDQ_003357

answers: continuous loss of heat

answers: NDQ_003358

answers: land

answers: NDQ_003359

answers: molten outer layer of Earth cooled to form a solid.

answers: NDQ_003360

answers: plate tectonics,

answers: NDQ_003362

answers: long-term steady continental area.

answers: NDQ_003363

answers: plate tectonics,

answers: NDQ_003371

answers: Continents formed by plate tectonics,

answers: NDQ_003373

answers: Continents formed by plate tectonics,

answers: NDQ_003376

answers: Continents formed by plate tectonics,

answers: NDQ_003378

answers: Continents formed by plate tectonics,

answers: NDQ_003379

answers: long-term steady continental area.

answers: NDQ_003380

answers: molten outer layer of Earth cooled to form a solid.

answers: NDQ_003381

answers: Continents formed by plate tectonics,

answers: NDQ_003382

answers: continuous loss of heat

answers: NDQ_003383

answers: continuous loss of heat

answers: NDQ_003384

answers: Continents formed by plate tectonics,

answers: NDQ_003385

answers: long-term steady continental area.

answers: NDQ_003386

answers: plate tectonics,

answers: NDQ_003387

answers: continuous loss of heat

answers: NDQ_003388

answers: plate tectonics,

answers: NDQ_003389

answers: plate tectonics,

answers: NDQ_003390

answers: plate tectonics,

answers: NDQ_003391

answers: crust

answers: NDQ_003392

answers: plate tectonics,

answers: NDQ_003393

answers: crust

answers: NDQ_003394

answers: plate tectonics,

answers: NDQ_003395

answers: plate tectonics,

answers: NDQ_003396

answers: plate tectonics,

text: San Francisco Bay is thought to represent a down-warping of the Earth's crust between the San Andreas Fault to the west and the Hayward Fault to the east, though the precise nature of this remains under study. During the last ice age, the basin now filled by the bay was a large linear valley with small hills, similar to most of the valleys of the Coast Ranges. The rivers of the Central Valley ran out to sea through a canyon that is now the Golden Gate. As the great ice sheets melted, sea level rose  over 4,000 years, and the valley filled with water from the Pacific, becoming a bay. The small hills became islands.

text: San Francisco Bay is thought to represent a down-warping of the Earth's crust between the

text: San Andreas Fault

text: to the west and the

text: Hayward Fault

text: to the east, though the precise nature of this remains under study. During the

text: last ice age

text: , the basin now filled by the bay was a large linear valley with small hills, similar to most of the valleys of the

text: Coast Ranges

text: . The rivers of the Central Valley ran out to sea through a canyon that is now the Golden Gate. As the great ice sheets melted, sea level rose  over 4,000 years, and the valley filled with water from the Pacific, becoming a bay. The small hills became islands.

answers: NDQ_003351

answers: down-warping

answers: NDQ_003352

answers: down-warping

answers: NDQ_003353

answers: down-warping

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: down-warping

answers: NDQ_003356

answers: down-warping

answers: NDQ_003357

answers: down-warping of the Earth's crust

answers: NDQ_003358

answers: valley

answers: NDQ_003359

answers: down-warping

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: the basin now filled by the bay was a large linear valley

answers: NDQ_003363

answers: San Andreas Fault

answers: NDQ_003371

answers: What is the San Andreas Fault?

answers: NDQ_003373

answers: down-warping

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: down-warping

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What type of force applied to rock is a stress?

answers: NDQ_003381

answers: What is the San Andreas Fault?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: down-warping

answers: NDQ_003384

answers: What is the opposite of down-warping?

answers: NDQ_003385

answers: San Andreas Fault

answers: NDQ_003386

answers: San Andreas Fault

answers: NDQ_003387

answers: What is the cause of the San Andreas Fault?

answers: NDQ_003388

answers: What is the San Andreas Fault to the west?

answers: NDQ_003389

answers: down-warping

answers: NDQ_003390

answers: San Andreas Fault

answers: NDQ_003391

answers: San Francisco Bay

answers: NDQ_003392

answers: San Andreas Fault

answers: NDQ_003393

answers: valley

answers: NDQ_003394

answers: San Andreas Fault

answers: NDQ_003395

answers: San Andreas Fault

answers: NDQ_003396

answers: Hayward Fault

answers: NDQ_003351

answers: down-warping

answers: NDQ_003352

answers: islands.

answers: NDQ_003353

answers: down-warping

answers: NDQ_003354

answers: San Andreas Fault

answers: NDQ_003355

answers: down-warping

answers: NDQ_003356

answers: islands.

answers: NDQ_003357

answers: San Andreas Fault to the west and the Hayward Fault

answers: NDQ_003358

answers: San Andreas Fault

answers: NDQ_003359

answers: San Andreas Fault

answers: NDQ_003360

answers: San Andreas Fault

answers: NDQ_003362

answers: a large linear valley with small hills,

answers: NDQ_003363

answers: Coast Ranges.

answers: NDQ_003371

answers: San Andreas Fault

answers: NDQ_003373

answers: San Francisco Bay is thought to represent a down-warping

answers: NDQ_003376

answers: large linear valley with small hills,

answers: NDQ_003378

answers: down-warping

answers: NDQ_003379

answers: San Andreas Fault to the west and the Hayward Fault

answers: NDQ_003380

answers: down-warping

answers: NDQ_003381

answers: down-warping

answers: NDQ_003382

answers: San Andreas Fault to the west and the Hayward Fault

answers: NDQ_003383

answers: San Andreas Fault

answers: NDQ_003384

answers: San Andreas Fault to the west and the Hayward Fault

answers: NDQ_003385

answers: San Andreas Fault

answers: NDQ_003386

answers: down-warping

answers: NDQ_003387

answers: San Andreas Fault

answers: NDQ_003388

answers: San Andreas Fault

answers: NDQ_003389

answers: down-warping

answers: NDQ_003390

answers: San Andreas Fault

answers: NDQ_003391

answers: hills,

answers: NDQ_003392

answers: San Andreas Fault

answers: NDQ_003393

answers: hills,

answers: NDQ_003394

answers: San Andreas Fault

answers: NDQ_003395

answers: San Andreas Fault

answers: NDQ_003396

answers: Hayward Fault

text: Dolenko G.N., 1984. Origin of petroleum and its accumulation in the Earth's crust. - Kiev, Naukova Dumka Publ. - 135 p. (in Russian)

text: Dolenko G.N., 1984. Origin of petroleum and its accumulation in the Earth's crust. - Kiev, Naukova Dumka Publ. - 135 p. (in Russian)

answers: NDQ_003351

answers: tensile

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: Stresses change rock

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: swell

answers: NDQ_003357

answers: 135 p.

answers: NDQ_003358

answers: rock break

answers: NDQ_003359

answers: shatters

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: petroleum and its accumulation in the Earth's crust

answers: NDQ_003363

answers: the Earth's crust

answers: NDQ_003371

answers: a thrust fault

answers: NDQ_003373

answers: A deeply buried rock is under compressive stresses

answers: NDQ_003376

answers: The terrain known as basin-and-range is caused by compressive forces

answers: NDQ_003378

answers: the amount the ground moves in an earthquake

answers: NDQ_003379

answers: In a strike-slip fault, the dip of the fault plane is vertical

answers: NDQ_003380

answers: Any force applied to rock is stress

answers: NDQ_003381

answers: When confining stress occurs, rock deforms

answers: NDQ_003382

answers: convergent plates

answers: NDQ_003383

answers: Stress is the cause of joints in rock.

answers: NDQ_003384

answers: Syncline

answers: NDQ_003385

answers: a fault zone

answers: NDQ_003386

answers: - Kiev, Naukova Dumka Publ.

answers: NDQ_003387

answers: - Kiev, Naukova Dumka Publ.

answers: NDQ_003388

answers: оректор .., 1984. Origin of petroleum and its accumulation in the Earth's crust.

answers: NDQ_003389

answers: The process of folding creates mountain ranges.

answers: NDQ_003390

answers: a fault

answers: NDQ_003391

answers: dip-slip fault plane

answers: NDQ_003392

answers: the hanging wall pushes up

answers: NDQ_003393

answers: dip-slip fault plane

answers: NDQ_003394

answers: fault with a fault plane that is not vertical

answers: NDQ_003395

answers: a vertical fault plane

answers: NDQ_003396

answers: a reverse fault

answers: NDQ_003351

answers: Origin of petroleum and its accumulation in the Earth's crust.

answers: NDQ_003352

answers: Origin of petroleum and its accumulation in the Earth's crust.

answers: NDQ_003353

answers: Origin of petroleum and its accumulation in the Earth's crust.

answers: NDQ_003354

answers: Origin of petroleum and its accumulation in the Earth's crust.

answers: NDQ_003355

answers: accumulation in the Earth's crust.

answers: NDQ_003356

answers: Origin of petroleum and its accumulation in the Earth's crust.

answers: NDQ_003357

answers: petroleum and its accumulation in the Earth's crust.

answers: NDQ_003358

answers: Earth's crust.

answers: NDQ_003359

answers: Origin of petroleum and its accumulation in the Earth's crust.

answers: NDQ_003360

answers: Earth's crust.

answers: NDQ_003362

answers: Origin of petroleum and its accumulation in the Earth's crust.

answers: NDQ_003363

answers: Earth's crust.

answers: NDQ_003371

answers: Origin of petroleum and its accumulation in the Earth's crust.

answers: NDQ_003373

answers: Origin of petroleum and its accumulation in the Earth's crust.

answers: NDQ_003376

answers: Origin of petroleum and its accumulation in the Earth's crust.

answers: NDQ_003378

answers: Origin of petroleum and its accumulation in the Earth's crust.

answers: NDQ_003379

answers: Origin of petroleum and its accumulation in the Earth's crust.

answers: NDQ_003380

answers: Origin of petroleum and its accumulation in the Earth's crust.

answers: NDQ_003381

answers: Origin of petroleum and its accumulation in the Earth's crust.

answers: NDQ_003382

answers: Dolenko G.N.,

answers: NDQ_003383

answers: Origin of petroleum and its accumulation in the Earth's crust.

answers: NDQ_003384

answers: Origin of petroleum and its accumulation in the Earth's crust.

answers: NDQ_003385

answers: Origin of petroleum and its accumulation in the Earth's crust.

answers: NDQ_003386

answers: Origin of petroleum and its accumulation in the Earth's crust.

answers: NDQ_003387

answers: Origin of petroleum and its accumulation in the Earth's crust.

answers: NDQ_003388

answers: Dolenko G.N.,

answers: NDQ_003389

answers: Origin of petroleum and its accumulation in the Earth's crust.

answers: NDQ_003390

answers: Origin of petroleum and its accumulation in the Earth's crust.

answers: NDQ_003391

answers: petroleum and its accumulation in the Earth's crust.

answers: NDQ_003392

answers: Origin of petroleum and its accumulation in the Earth's crust.

answers: NDQ_003393

answers: petroleum and its accumulation in the Earth's crust.

answers: NDQ_003394

answers: Origin of petroleum and its accumulation in the Earth's crust.

answers: NDQ_003395

answers: Origin of petroleum and its accumulation in the Earth's crust.

answers: NDQ_003396

answers: Origin of petroleum and its accumulation in the Earth's crust.

text: The station is currently the home base for two permanent monitoring projects: continual geodetic measurement using GPS technology, run by the Royal Institute of Technology in Stockholm, and a seismograph that records movements in the earth’s crust, run by the German Alfred Wegener Institute.

text: The station is currently the home base for two permanent monitoring projects: continual

text: geodetic

text: measurement using

text: GPS technology

text: , run by the

text: Royal Institute of Technology

text: in

text: Stockholm

text: , and a

text: seismograph

text: that records movements in the earth’s crust, run by the

text: German

entity_name: Alfred Wegener Institute for Polar and Marine Research

text: Alfred Wegener Institute

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: movement

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: change shape

answers: NDQ_003357

answers: seismograph that records movements in the earth’s crust

answers: NDQ_003358

answers: seismograph

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: the station is currently the home base for two permanent monitoring projects

answers: NDQ_003363

answers: the same time

answers: NDQ_003371

answers: what may be a thrust fault in between?

answers: NDQ_003373

answers: None of the above choices.

answers: NDQ_003376

answers: unknown

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: no

answers: NDQ_003380

answers: None of the above choices.

answers: NDQ_003381

answers: what is the last word in the passage?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: what is the second to last word in the passage?

answers: NDQ_003385

answers: unanswerable

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: unanswerable

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: NDQ_003391

answers: unanswerable

answers: NDQ_003392

answers: unanswerable

answers: NDQ_003393

answers: dip-slip fault plane

answers: NDQ_003394

answers: isobath

answers: NDQ_003395

answers: a seismograph

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: seismograph

answers: NDQ_003352

answers: seismograph

answers: NDQ_003353

answers: seismograph

answers: NDQ_003354

answers: The station is currently the home base for two permanent monitoring projects:

answers: NDQ_003355

answers: seismograph

answers: NDQ_003356

answers: seismograph

answers: NDQ_003357

answers: seismograph that records movements in the earth’s crust,

answers: NDQ_003358

answers: seismograph

answers: NDQ_003359

answers: movements in the earth’s crust,

answers: NDQ_003360

answers: seismograph that records movements in the earth’s crust,

answers: NDQ_003362

answers: continual geodetic measurement

answers: NDQ_003363

answers: earth’s crust,

answers: NDQ_003371

answers: seismograph

answers: NDQ_003373

answers: seismograph that records movements in the earth’s crust,

answers: NDQ_003376

answers: German Alfred Wegener Institute.

answers: NDQ_003378

answers: seismograph that records movements in the earth’s crust,

answers: NDQ_003379

answers: GPS technology, run by the Royal Institute of Technology in Stockholm,

answers: NDQ_003380

answers: seismograph

answers: NDQ_003381

answers: seismograph

answers: NDQ_003382

answers: German Alfred Wegener Institute.

answers: NDQ_003383

answers: seismograph

answers: NDQ_003384

answers: Royal Institute of Technology in Stockholm, and a seismograph

answers: NDQ_003385

answers: seismograph

answers: NDQ_003386

answers: seismograph that records movements in the earth’s crust,

answers: NDQ_003387

answers: seismograph

answers: NDQ_003388

answers: seismograph

answers: NDQ_003389

answers: earth’s crust,

answers: NDQ_003390

answers: seismograph

answers: NDQ_003391

answers: seismograph

answers: NDQ_003392

answers: seismograph

answers: NDQ_003393

answers: seismograph

answers: NDQ_003394

answers: seismograph

answers: NDQ_003395

answers: seismograph

answers: NDQ_003396

answers: seismograph

text: Within the Precambrian rocks beneath and just west of the center of the basin lies a generally north to northwest trending linear feature that appears to be an ancient rift in the Earth's crust. This rift appears to be contiguous with the rift zone under Lake Superior. This, the Midcontinent Rift System, turns west under Lake Superior and then southwest through southern Minnesota, central and western Iowa and on through southeastern Nebraska and into eastern Kansas.

text: Within the Precambrian rocks beneath and just west of the center of the basin lies a generally north to northwest trending linear feature that appears to be an ancient

text: rift

text: in the Earth's

text: crust

text: . This rift appears to be contiguous with the rift zone under

text: Lake Superior

text: . This, the

text: Midcontinent Rift System

text: , turns west under Lake Superior and then southwest through southern

text: Minnesota

text: , central and western

text: Iowa

text: and on through southeastern

text: Nebraska

text: and into eastern

text: Kansas

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: more likely to crack

answers: NDQ_003353

answers: rifts

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: rift

answers: NDQ_003356

answers: change shape

answers: NDQ_003357

answers: the midcontinent rift system turns west under Lake Superior

answers: NDQ_003358

answers: rift zone

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Precambrian rocks

answers: NDQ_003362

answers: an ancient rift in the Earth's crust

answers: NDQ_003363

answers: Lake Superior

answers: NDQ_003371

answers: What is the Midcontinent Rift System?

answers: NDQ_003373

answers: Why would a rock be deeply buried?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What is the Midcontinent Rift System?

answers: NDQ_003381

answers: What is the Midcontinent Rift System?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: None of the above choices.

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: normal faults or compression stress?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip faults, strike-slip faults or strike-slip faults?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: rift zone

answers: NDQ_003392

answers: unanswerable

answers: NDQ_003393

answers: rift zone

answers: NDQ_003394

answers: unanswerable

answers: NDQ_003395

answers: rift with a vertical fault plane

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: north to northwest trending linear feature

answers: NDQ_003352

answers: rift

answers: NDQ_003353

answers: rift in the Earth's crust.

answers: NDQ_003354

answers: Within the Precambrian rocks

answers: NDQ_003355

answers: rift

answers: NDQ_003356

answers: rift in the Earth's crust.

answers: NDQ_003357

answers: rift

answers: NDQ_003358

answers: rift

answers: NDQ_003359

answers: rift

answers: NDQ_003360

answers: rift in the Earth's crust.

answers: NDQ_003362

answers: contiguous with the rift zone under Lake Superior.

answers: NDQ_003363

answers: Precambrian

answers: NDQ_003371

answers: rift

answers: NDQ_003373

answers: Within the Precambrian rocks

answers: NDQ_003376

answers: rift in the Earth's crust.

answers: NDQ_003378

answers: rift in the Earth's crust.

answers: NDQ_003379

answers: north to northwest

answers: NDQ_003380

answers: rift in the Earth's crust.

answers: NDQ_003381

answers: rift

answers: NDQ_003382

answers: southeastern Nebraska and into eastern Kansas.

answers: NDQ_003383

answers: rift in the Earth's crust.

answers: NDQ_003384

answers: north to northwest trending linear feature

answers: NDQ_003385

answers: rift zone

answers: NDQ_003386

answers: rift

answers: NDQ_003387

answers: rift in the Earth's crust.

answers: NDQ_003388

answers: southeastern Nebraska and into eastern Kansas.

answers: NDQ_003389

answers: rift in the Earth's crust.

answers: NDQ_003390

answers: rift

answers: NDQ_003391

answers: Precambrian

answers: NDQ_003392

answers: rift

answers: NDQ_003393

answers: rift

answers: NDQ_003394

answers: rift

answers: NDQ_003395

answers: rift

answers: NDQ_003396

answers: north to northwest trending linear feature that appears to be an ancient rift

text: However the failure of the strike was not solely from violence, well-organized public relations, or the failing morale of the strikers. Right before the Little Steel strike began, the economy had slipped back into a slight depression, causing less demand for steel. Fewer employees were needed to satisfy the decreased demand. The SWOC was not able to use lost profits as a bargaining tool. It was aggressive strike breaking tactics from Little Steel, lack of organization from SWOC, and demoralized unionists that made the strike end by the end of the summer of 1937 with the companies victorious.

text: However the failure of the strike was not solely from violence, well-organized public relations, or the failing morale of the strikers. Right before the Little Steel strike began, the economy had slipped back into a slight depression, causing less demand for steel. Fewer employees were needed to satisfy the decreased demand. The SWOC was not able to use lost profits as a bargaining tool. It was aggressive strike breaking tactics from Little Steel, lack of organization from SWOC, and demoralized unionists that made the strike end by the end of the summer of 1937 with the companies victorious.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: igneous rocks to form

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: unanswerable

answers: NDQ_003356

answers: deform

answers: NDQ_003357

answers: Fewer employees were needed to satisfy the decreased demand.

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's surface

answers: NDQ_003362

answers: violence, well-organized public relations, or the failure of the strikers

answers: NDQ_003363

answers: unanswerable

answers: NDQ_003371

answers: What may be the reason for the strike?

answers: NDQ_003373

answers: Why did the strike end?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: no

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What may be the reason for the strike?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: Which of the following is not a type of fold: syncline, fold, or fold?

answers: NDQ_003385

answers: what is the first word in the passage?

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: normal faults, SWOC, or demoralized unionists?

answers: NDQ_003388

answers: Which of the following is not a result of shear stress: strike-slip faults, shear stress, or the economy?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: dip-slip fault plane

answers: NDQ_003392

answers: unanswerable

answers: NDQ_003393

answers: dip-slip fault plane

answers: NDQ_003394

answers: unanswerable

answers: NDQ_003395

answers: unanswerable

answers: NDQ_003396

answers: NDQ_003351

answers: violence,

answers: NDQ_003352

answers: aggressive strike breaking tactics

answers: NDQ_003353

answers: less demand for steel.

answers: NDQ_003354

answers: aggressive strike breaking tactics from Little Steel,

answers: NDQ_003355

answers: depression,

answers: NDQ_003356

answers: aggressive strike breaking tactics

answers: NDQ_003357

answers: failing morale of the strikers.

answers: NDQ_003358

answers: violence,

answers: NDQ_003359

answers: violence,

answers: NDQ_003360

answers: violence,

answers: NDQ_003362

answers: violence, well-organized public relations,

answers: NDQ_003363

answers: depression,

answers: NDQ_003371

answers: violence, well-organized public relations,

answers: NDQ_003373

answers: aggressive strike breaking tactics from Little Steel,

answers: NDQ_003376

answers: violence,

answers: NDQ_003378

answers: slipped

answers: NDQ_003379

answers: slight depression,

answers: NDQ_003380

answers: violence,

answers: NDQ_003381

answers: aggressive strike breaking tactics

answers: NDQ_003382

answers: violence,

answers: NDQ_003383

answers: violence,

answers: NDQ_003384

answers: depression,

answers: NDQ_003385

answers: violence,

answers: NDQ_003386

answers: violence,

answers: NDQ_003387

answers: violence,

answers: NDQ_003388

answers: violence,

answers: NDQ_003389

answers: violence,

answers: NDQ_003390

answers: Little Steel,

answers: NDQ_003391

answers: Little Steel,

answers: NDQ_003392

answers: aggressive strike breaking tactics from Little Steel,

answers: NDQ_003393

answers: Little Steel,

answers: NDQ_003394

answers: aggressive strike breaking tactics from Little Steel,

answers: NDQ_003395

answers: aggressive strike breaking tactics from Little Steel,

answers: NDQ_003396

answers: depression,

text: A geologic or geomorphic province is a spatial entity with common geologic or geomorphic attributes. A province may include a single dominant structural element such as a basin or a fold belt, or a number of contiguous related elements.  Adjoining provinces may be similar in structure but be considered separate due to differing histories.

text: A geologic or geomorphic province is a spatial entity with common

text: geologic

text: or

text: geomorphic

text: attributes. A province may include a single dominant structural element such as a

text: basin

text: or a

text: fold belt

text: , or a number of contiguous related elements.  Adjoining provinces may be similar in structure but be considered separate due to differing

text: histories

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: erosion

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: fold belt

answers: NDQ_003356

answers: fold

answers: NDQ_003357

answers: provinces may include a single dominant structural element

answers: NDQ_003358

answers: basin

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: continents

answers: NDQ_003362

answers: separate due to differing histories

answers: NDQ_003363

answers: geologic province

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: compressive stresses

answers: NDQ_003376

answers: compressive forces

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: strike-slip fault

answers: NDQ_003380

answers: What is a stress?

answers: NDQ_003381

answers: What happens to rock when confining stress occurs?

answers: NDQ_003382

answers: None of the above choices.

answers: NDQ_003383

answers: What causes joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: Fault zone

answers: NDQ_003386

answers: movement of rock at faults

answers: NDQ_003387

answers: normal faults are caused by compression stress

answers: NDQ_003388

answers: What causes strike-slip faults?

answers: NDQ_003389

answers: fold belt

answers: NDQ_003390

answers: a fold

answers: NDQ_003391

answers: a basin

answers: NDQ_003392

answers: a fold

answers: NDQ_003393

answers: a basin

answers: NDQ_003394

answers: a fold belt

answers: NDQ_003395

answers: is a type of fault

answers: NDQ_003396

answers: horizontal

answers: NDQ_003351

answers: fold belt,

answers: NDQ_003352

answers: fold belt,

answers: NDQ_003353

answers: geomorphic province

answers: NDQ_003354

answers: Adjoining provinces

answers: NDQ_003355

answers: fold belt,

answers: NDQ_003356

answers: fold belt,

answers: NDQ_003357

answers: a single dominant structural element

answers: NDQ_003358

answers: a basin or a fold belt,

answers: NDQ_003359

answers: geologic or geomorphic province

answers: NDQ_003360

answers: geologic or geomorphic province

answers: NDQ_003362

answers: a single dominant structural element

answers: NDQ_003363

answers: a basin or a fold belt,

answers: NDQ_003371

answers: Adjoining provinces

answers: NDQ_003373

answers: geologic or geomorphic province

answers: NDQ_003376

answers: basin or a fold belt,

answers: NDQ_003378

answers: A geologic or geomorphic province

answers: NDQ_003379

answers: single dominant structural element such as a basin or a fold belt,

answers: NDQ_003380

answers: A geologic or geomorphic province

answers: NDQ_003381

answers: basin or a fold belt,

answers: NDQ_003382

answers: fold belt,

answers: NDQ_003383

answers: basin or a fold belt,

answers: NDQ_003384

answers: fold belt,

answers: NDQ_003385

answers: geologic or geomorphic province

answers: NDQ_003386

answers: A geologic or geomorphic province

answers: NDQ_003387

answers: A geologic or geomorphic province

answers: NDQ_003388

answers: A geologic or geomorphic province

answers: NDQ_003389

answers: a single dominant structural element such as a basin or a fold belt,

answers: NDQ_003390

answers: fold belt,

answers: NDQ_003391

answers: basin or a fold belt,

answers: NDQ_003392

answers: fold belt,

answers: NDQ_003393

answers: fold belt,

answers: NDQ_003394

answers: fold belt,

answers: NDQ_003395

answers: fold belt,

answers: NDQ_003396

answers: fold belt,

text: In plate tectonics theory during the breakup of a continent, three divergent boundaries form, radiating out from a central point (the triple junction). One of these divergent plate boundaries fails (see aulacogen) and the other two continue spreading to form an ocean. The opening of the south Atlantic Ocean started at the south of the South American and African continents, reaching a triple junction in the present Gulf of Guinea, from where it continued to the west. The NE-trending Benue Trough is the failed arm of this junction.

text: In

text: plate tectonics

text: theory during the breakup of a continent, three divergent boundaries form, radiating out from a central point (the triple junction). One of these divergent plate boundaries fails (see

text: aulacogen

text: ) and the other two continue spreading to form an ocean. The

text: opening

text: of the south

text: Atlantic Ocean

text: started at the south of the

text: South America

text: n and

text: Africa

text: n continents, reaching a triple junction in the present

text: Gulf of Guinea

text: , from where it continued to the west. The NE-trending

text: Benue Trough

text: is the failed arm of this junction.

answers: NDQ_003351

answers: aulacogen

answers: NDQ_003352

answers: is likely to crack

answers: NDQ_003353

answers: divergent boundaries

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: divergent boundary

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: one of these divergent plate boundaries fails

answers: NDQ_003358

answers: aulacogen

answers: NDQ_003359

answers: fails

answers: NDQ_003360

answers: plate tectonics

answers: NDQ_003362

answers: Benue Trough is the failed arm of this junction.

answers: NDQ_003363

answers: the opening of the south Atlantic Ocean

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: How would you describe a rock that is deeply buried?

answers: NDQ_003376

answers: compressive forces

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What is a stress?

answers: NDQ_003381

answers: What happens to rock when confining stress occurs?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: unanswerable

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: aulacogen

answers: NDQ_003391

answers: aulacogen

answers: NDQ_003392

answers: aulacogen

answers: NDQ_003393

answers: aulacogen

answers: NDQ_003394

answers: Benue Trough

answers: NDQ_003395

answers: NE-trending Benue Trough

answers: NDQ_003396

answers: Benue Trough

answers: NDQ_003351

answers: aulacogen)

answers: NDQ_003352

answers: fails (see aulacogen)

answers: NDQ_003353

answers: aulacogen)

answers: NDQ_003354

answers: In plate tectonics

answers: NDQ_003355

answers: aulacogen)

answers: NDQ_003356

answers: ocean.

answers: NDQ_003357

answers: One of these divergent plate boundaries fails (see aulacogen)

answers: NDQ_003358

answers: aulacogen)

answers: NDQ_003359

answers: fails

answers: NDQ_003360

answers: plate tectonics

answers: NDQ_003362

answers: ocean.

answers: NDQ_003363

answers: breakup of a continent,

answers: NDQ_003371

answers: In plate tectonics

answers: NDQ_003373

answers: In plate tectonics

answers: NDQ_003376

answers: In plate tectonics

answers: NDQ_003378

answers: In plate tectonics

answers: NDQ_003379

answers: In plate tectonics

answers: NDQ_003380

answers: In plate tectonics

answers: NDQ_003381

answers: In plate tectonics

answers: NDQ_003382

answers: ocean.

answers: NDQ_003383

answers: In plate tectonics

answers: NDQ_003384

answers: aulacogen)

answers: NDQ_003385

answers: three divergent boundaries form, radiating out from a central point

answers: NDQ_003386

answers: plate tectonics

answers: NDQ_003387

answers: aulacogen)

answers: NDQ_003388

answers: In plate tectonics

answers: NDQ_003389

answers: ocean.

answers: NDQ_003390

answers: Benue Trough

answers: NDQ_003391

answers: aulacogen)

answers: NDQ_003392

answers: Benue Trough

answers: NDQ_003393

answers: aulacogen)

answers: NDQ_003394

answers: Benue Trough

answers: NDQ_003395

answers: Benue Trough

answers: NDQ_003396

answers: aulacogen)

text: The 1997 Manyi earthquake (玛尼地震) occurred on November 8 at 10:02 UTC. The epicenter was in Nagqu Prefecture (那曲地區) in northern Tibet, China. The focal mechanism indicates a lift-lateral strike-slip movement. This earthquake had a surface rupture of  long with up to  of left-lateral slip along the Manyi fault, a westward continuation of the Kunlun fault, offset about  to the south. Normally, the continental crust is about  thick, but it reaches  thick under the Tibetan Plateau. This earthquake ruptured up to  of the top part of the local continental crust.

text: The 1997 Manyi earthquake (玛尼地震) occurred on November 8 at 10:02 UTC. The epicenter was in

text: Nagqu Prefecture

text: (那曲地區) in northern

text: Tibet

text: China

text: . The focal mechanism indicates a lift-lateral strike-slip movement. This earthquake had a surface rupture of  long with up to  of left-lateral slip along the Manyi fault, a westward continuation of the

text: Kunlun fault

text: , offset about  to the south. Normally, the

text: continental crust

text: is about  thick, but it reaches  thick under the Tibetan Plateau. This earthquake ruptured up to  of the top part of the local continental crust.

answers: NDQ_003351

answers: left-lateral slip

answers: NDQ_003352

answers: is likely to crack

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: fault

answers: NDQ_003356

answers: slip

answers: NDQ_003357

answers: the continental crust is about how thick?

answers: NDQ_003358

answers: epicenter

answers: NDQ_003359

answers: ruptures

answers: NDQ_003360

answers: faults

answers: NDQ_003362

answers: This earthquake ruptured up to of the top part of the local continental crust.

answers: NDQ_003363

answers: The 1997 Manyi earthquake

answers: NDQ_003371

answers: What type of movement does the focal mechanism indicate?

answers: NDQ_003373

answers: How would you describe the earthquake?

answers: NDQ_003376

answers: What type of forces caused the terrain known as basin-and-range?

answers: NDQ_003378

answers: what is the last word in the passage?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What was the cause of the earthquake?

answers: NDQ_003381

answers: What type of stress does the earthquake cause?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What was the epicenter of the 1997 Manyi earthquake?

answers: NDQ_003385

answers: What is the name of the area where faults are clustered?

answers: NDQ_003386

answers: What is the cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: lift-lateral strike-slip movement or normal faults?

answers: NDQ_003388

answers: Which of the following is not an example of a strike-slip fault?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: Manyi fault

answers: NDQ_003391

answers: Tibetan Plateau

answers: NDQ_003392

answers: Manyi fault

answers: NDQ_003393

answers: the Tibetan Plateau

answers: NDQ_003394

answers: Manyi fault

answers: NDQ_003395

answers: Manyi fault

answers: NDQ_003396

answers: Manyi fault

answers: NDQ_003351

answers: lift-lateral strike-slip

answers: NDQ_003352

answers: thick, but it reaches thick

answers: NDQ_003353

answers: lift-lateral strike-slip movement.

answers: NDQ_003354

answers: thick, but it reaches thick under the Tibetan Plateau.

answers: NDQ_003355

answers: fault,

answers: NDQ_003356

answers: lift-lateral strike-slip

answers: NDQ_003357

answers: the continental crust is about thick,

answers: NDQ_003358

answers: surface rupture

answers: NDQ_003359

answers: fault,

answers: NDQ_003360

answers: Manyi fault,

answers: NDQ_003362

answers: thick, but it reaches thick under the Tibetan Plateau.

answers: NDQ_003363

answers: Tibetan Plateau.

answers: NDQ_003371

answers: Manyi fault,

answers: NDQ_003373

answers: thick under the Tibetan Plateau.

answers: NDQ_003376

answers: Tibetan Plateau.

answers: NDQ_003378

answers: slip

answers: NDQ_003379

answers: lift-lateral

answers: NDQ_003380

answers: lift-lateral strike-slip

answers: NDQ_003381

answers: lift-lateral strike-slip movement.

answers: NDQ_003382

answers: lift-lateral strike-slip

answers: NDQ_003383

answers: lift-lateral strike-slip movement.

answers: NDQ_003384

answers: Manyi fault,

answers: NDQ_003385

answers: Manyi fault,

answers: NDQ_003386

answers: lift-lateral strike-slip

answers: NDQ_003387

answers: Normally, the continental crust is about thick,

answers: NDQ_003388

answers: lift-lateral strike-slip

answers: NDQ_003389

answers: Tibetan Plateau.

answers: NDQ_003390

answers: Manyi fault,

answers: NDQ_003391

answers: Tibetan Plateau.

answers: NDQ_003392

answers: Manyi fault,

answers: NDQ_003393

answers: Tibetan Plateau.

answers: NDQ_003394

answers: Kunlun fault,

answers: NDQ_003395

answers: Kunlun fault,

answers: NDQ_003396

answers: Kunlun fault,

text: Tilted block faulting, also called rotational block faulting, is a mode of structural evolution in extensional tectonic events, a result of tectonic plates stretching apart. When the upper lithospheric crust experiences extensional pressures, the brittle crust fractures, creating detachment faults. These normal faults express themselves on a regional scale; upper crust fractures into tilted fault blocks, and ductile lower crust ascends. This results in uplift, cooling, and exhumation of ductily deformed deeper crust. The large unit of tilted blocks and associated crust can help form an integral part of metamorphic core complexes and can occur on both continental and oceanic crust.

text: Tilted block faulting, also called rotational block faulting, is a mode of structural evolution in

text: extensional tectonic

text: events, a result of tectonic plates stretching apart. When the upper

text: lithospheric

text: crust experiences extensional pressures, the brittle crust fractures, creating

text: detachment fault

text: s. These normal

text: fault

text: s express themselves on a regional scale; upper crust fractures into tilted fault blocks, and

text: ductile

text: lower crust ascends. This results in uplift, cooling, and exhumation of ductily deformed deeper crust. The large unit of tilted blocks and associated crust can help form an integral part of

text: metamorphic core complexes

text: and can occur on both continental and oceanic crust.

answers: NDQ_003351

answers: extensional

answers: NDQ_003352

answers: fractures

answers: NDQ_003353

answers: detachment faults

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: detachment fault

answers: NDQ_003356

answers: exhume

answers: NDQ_003357

answers: upper crust fractures into tilted fault blocks

answers: NDQ_003358

answers: detachment

answers: NDQ_003359

answers: extensional pressures

answers: NDQ_003360

answers: a regional scale

answers: NDQ_003362

answers: ductile lower crust ascends. This results in uplift, cooling, and exhumation of ductily deformed deeper crust.

answers: NDQ_003363

answers: extensional tectonic events

answers: NDQ_003371

answers: Which of the following is not a type of fault: tilted fault blocks, and ductile lower crust ascends

answers: NDQ_003373

answers: unanswerable

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: When the upper lithospheric crust experiences extensional pressures

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What type of fold is a syncline?

answers: NDQ_003385

answers: What is the large unit of tilted blocks and associated crust?

answers: NDQ_003386

answers: Tilted block faulting

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: Which of the following is not a result of extensional pressures, the brittle crust fractures, creating detachment faults

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: detachment faulting

answers: NDQ_003391

answers: tilted fault

answers: NDQ_003392

answers: detachment faulting

answers: NDQ_003393

answers: tilted fault

answers: NDQ_003394

answers: tilted faulting

answers: NDQ_003395

answers: detachment

answers: NDQ_003396

answers: detachment faulting

answers: NDQ_003351

answers: extensional pressures,

answers: NDQ_003352

answers: brittle crust fractures,

answers: NDQ_003353

answers: the brittle crust fractures,

answers: NDQ_003354

answers: Tilted block faulting,

answers: NDQ_003355

answers: detachment faults.

answers: NDQ_003356

answers: uplift, cooling, and exhumation of ductily

answers: NDQ_003357

answers: ductile lower crust ascends.

answers: NDQ_003358

answers: detachment faults.

answers: NDQ_003359

answers: extensional pressures,

answers: NDQ_003360

answers: Tilted block faulting,

answers: NDQ_003362

answers: Tilted block faulting,

answers: NDQ_003363

answers: extensional tectonic events,

answers: NDQ_003371

answers: Tilted block faulting,

answers: NDQ_003373

answers: ductily deformed deeper crust.

answers: NDQ_003376

answers: extensional pressures,

answers: NDQ_003378

answers: uplift,

answers: NDQ_003379

answers: Tilted block faulting, also called rotational block faulting,

answers: NDQ_003380

answers: extensional pressures,

answers: NDQ_003381

answers: extensional pressures,

answers: NDQ_003382

answers: extensional pressures,

answers: NDQ_003383

answers: extensional pressures,

answers: NDQ_003384

answers: ductile lower crust ascends.

answers: NDQ_003385

answers: tilted fault blocks,

answers: NDQ_003386

answers: When the upper lithospheric crust experiences extensional pressures,

answers: NDQ_003387

answers: extensional pressures,

answers: NDQ_003388

answers: detachment faults.

answers: NDQ_003389

answers: Tilted block faulting,

answers: NDQ_003390

answers: detachment faults.

answers: NDQ_003391

answers: tilted fault blocks,

answers: NDQ_003392

answers: detachment faults.

answers: NDQ_003393

answers: tilted fault blocks,

answers: NDQ_003394

answers: Tilted block faulting,

answers: NDQ_003395

answers: detachment faults.

answers: NDQ_003396

answers: detachment faults.

text: The crust ranges from 5–70 km (~3–44 miles) in depth and is the outermost layer. The thin parts are the oceanic crust, which underlie the ocean basins (5–10 km) and are composed of dense  (mafic) iron magnesium silicate igneous rocks, like basalt. The thicker crust is continental crust, which is less dense and composed of (felsic) sodium potassium aluminium silicate rocks, like granite. The rocks of the crust fall into two major categories –  sial and sima (Suess,1831–1914). It is estimated that sima starts about 11 km below the Conrad discontinuity (a second order discontinuity). The uppermost mantle together with the crust constitutes the lithosphere. The crust-mantle boundary occurs as two physically different events. First, there is a discontinuity in the seismic velocity, which is most commonly known as the Mohorovičić discontinuity or Moho. The cause of the Moho is thought to be a change in rock composition from rocks containing plagioclase feldspar (above) to rocks that contain no feldspars (below). Second, in oceanic crust, there is a chemical discontinuity between ultramafic cumulates and tectonized harzburgites, which has been observed from deep parts of the oceanic crust that have been obducted onto the continental crust and preserved as ophiolite sequences.

text: The crust ranges from 5–70 km (~3–44 miles) in depth and is the outermost layer. The thin parts are the

text: oceanic crust

text: , which underlie the ocean basins (5–10 km) and are composed of dense  (

text: mafic

text: ) iron magnesium

text: silicate

text: igneous rock

text: s, like

text: basalt

text: . The thicker crust is

text: continental crust

text: , which is less dense and composed of (

text: felsic

text: sodium

text: potassium

text: aluminium

text: silicate rocks, like

text: granite

text: . The rocks of the crust fall into two major categories –  sial and sima (Suess,1831–1914). It is estimated that sima starts about 11 km below the

text: Conrad discontinuity

text: (a second order discontinuity). The uppermost mantle together with the crust constitutes the

text: lithosphere

text: . The crust-mantle boundary occurs as two physically different events. First, there is a discontinuity in the

text: seismic

text: velocity, which is most commonly known as the

text: Mohorovičić discontinuity

text: or Moho. The cause of the Moho is thought to be a change in rock composition from rocks containing

text: plagioclase feldspar

text: (above) to rocks that contain no feldspars (below). Second, in oceanic crust, there is a

text: chemical

text: discontinuity between

text: ultramafic

text: cumulates and tectonized

text: harzburgite

text: s, which has been observed from deep parts of the oceanic crust that have been

text: obducted

text: onto the continental crust and preserved as

text: ophiolite sequences

answers: NDQ_003351

answers: Moho

answers: NDQ_003352

answers: is likely to contain more silicates

answers: NDQ_003353

answers: Moho

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: Moho

answers: NDQ_003356

answers: contain no feldspar

answers: NDQ_003357

answers: rocks containing plagioclase feldspar

answers: NDQ_003358

answers: discontinuity

answers: NDQ_003359

answers: change in rock composition

answers: NDQ_003360

answers: tectonic plates

answers: NDQ_003362

answers: sima starts about 11 km below the Conrad discontinuity

answers: NDQ_003363

answers: oceanic crust

answers: NDQ_003371

answers: What is the cause of the Moho?

answers: NDQ_003373

answers: What is the cause of the Moho?

answers: NDQ_003376

answers: What is the thickness of the continental crust?

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What is the Moho?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of the Moho?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: tectonized harzburgites

answers: NDQ_003387

answers: What is the cause of the Moho?

answers: NDQ_003388

answers: What is the cause of the Moho?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: Conrad discontinuity

answers: NDQ_003391

answers: ophiolite

answers: NDQ_003392

answers: Conrad discontinuity

answers: NDQ_003393

answers: lithosphere

answers: NDQ_003394

answers: Conrad discontinuity

answers: NDQ_003395

answers: Conrad discontinuity

answers: NDQ_003396

answers: Moho

answers: NDQ_003351

answers: seismic velocity,

answers: NDQ_003352

answers: rocks that contain no feldspars

answers: NDQ_003353

answers: composition

answers: NDQ_003354

answers: Conrad discontinuity

answers: NDQ_003355

answers: Conrad discontinuity

answers: NDQ_003356

answers: rocks that contain no feldspars

answers: NDQ_003357

answers: Conrad discontinuity

answers: NDQ_003358

answers: Conrad discontinuity

answers: NDQ_003359

answers: change in rock composition

answers: NDQ_003360

answers: tectonized

answers: NDQ_003362

answers: no feldspars

answers: NDQ_003363

answers: oceanic crust,

answers: NDQ_003371

answers: Mohorovi<unk>i<unk> discontinuity

answers: NDQ_003373

answers: The crust ranges from 5–70 km (<unk>3–44 miles)

answers: NDQ_003376

answers: oceanic crust,

answers: NDQ_003378

answers: seismic velocity,

answers: NDQ_003379

answers: Mohorovi<unk>i<unk> discontinuity

answers: NDQ_003380

answers: oceanic crust,

answers: NDQ_003381

answers: a change in rock composition

answers: NDQ_003382

answers: Conrad discontinuity

answers: NDQ_003383

answers: a change in rock composition

answers: NDQ_003384

answers: Mohorovi<unk>i<unk> discontinuity

answers: NDQ_003385

answers: Mohorovi<unk>i<unk> discontinuity

answers: NDQ_003386

answers: Mohorovi<unk>i<unk> discontinuity

answers: NDQ_003387

answers: a change in rock composition

answers: NDQ_003388

answers: a change in rock composition

answers: NDQ_003389

answers: ophiolite sequences.

answers: NDQ_003390

answers: Conrad discontinuity

answers: NDQ_003391

answers: Conrad discontinuity

answers: NDQ_003392

answers: Mohorovi<unk>i<unk> discontinuity

answers: NDQ_003393

answers: Conrad discontinuity

answers: NDQ_003394

answers: Conrad discontinuity

answers: NDQ_003395

answers: Conrad discontinuity

answers: NDQ_003396

answers: Conrad discontinuity

text: The effects of stress on memory include interference with a person's capacity to encode memory and the ability to retrieve information. During times of stress, the body reacts by secreting stress hormones into the bloodstream. Stress can cause acute and chronic changes in certain brain areas which can cause long-term damage.  Over-secretion of stress hormones most frequently impairs memory, but in a few cases can enhance it. In particular, the hippocampus, prefrontal cortex and the amygdala are affected. One class of stress hormone responsible for negatively affecting memory is the glucocorticoids (GCs), the most notable of which is cortisol. Glucocorticoids facilitate and impair the actions of stress in the brain memory process. Cortisol is a known biomarker for stress. Under normal circumstances, the hippocampus regulates the production of cortisol through negative feedback because it has many receptors that are sensitive to these stress hormones. However, an excess of cortisol can impair the ability of the hippocampus to both encode and recall memories. These stress hormones are also hindering the hippocampus from receiving enough energy by diverting glucose levels to surrounding muscles.

text: The effects of stress on memory include interference with a person's capacity to

text: encode

text: memory

text: and the ability to retrieve information. During times of

text: stress

text: , the body reacts by secreting

text: stress hormone

text: s into the bloodstream. Stress can cause acute and chronic changes in certain brain areas which can cause long-term damage.  Over-secretion of stress hormones most frequently impairs memory, but in a few cases can enhance it. In particular, the

text: hippocampus

text: prefrontal cortex

text: and the amygdala are affected. One class of stress hormone responsible for negatively affecting memory is the

text: glucocorticoids

text: (GCs), the most notable of which is

text: cortisol

text: . Glucocorticoids facilitate and impair the actions of stress in the brain memory process. Cortisol is a known biomarker for stress. Under normal circumstances, the hippocampus regulates the production of cortisol through

text: negative feedback

text: because it has many

text: receptors

text: that are sensitive to these stress hormones. However, an excess of cortisol can impair the ability of the hippocampus to both encode and recall memories. These stress hormones are also hindering the hippocampus from receiving enough energy by diverting glucose levels to surrounding muscles.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: can cause more damage

answers: NDQ_003353

answers: cortisol

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: unanswerable

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: the hippocampus regulates the production of cortisol

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: stress

answers: NDQ_003362

answers: over-secretion of stress hormones most frequently impairs memory

answers: NDQ_003363

answers: stress

answers: NDQ_003371

answers: Which of the following is not a type of stress hormone?

answers: NDQ_003373

answers: What is the best title for this passage?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: Which of the following is not a class of stress hormone responsible for negatively affecting memory?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: What is the most notable of which is cortisol?

answers: NDQ_003386

answers: What is the most notable of which is cortisol?

answers: NDQ_003387

answers: Which is not a class of stress hormone responsible for negatively affecting memory?

answers: NDQ_003388

answers: Which is not a class of stress hormone responsible for negatively affecting memory?

answers: NDQ_003389

answers: process of folding

answers: NDQ_003390

answers: negative feedback

answers: NDQ_003391

answers: dip-slip fault plane

answers: NDQ_003392

answers: cortisol

answers: NDQ_003393

answers: dip-slip fault plane

answers: NDQ_003394

answers: is a

answers: NDQ_003395

answers: a vertical fault plane

answers: NDQ_003396

answers: NDQ_003351

answers: glucocorticoids

answers: NDQ_003352

answers: damage.

answers: NDQ_003353

answers: secreting stress hormones

answers: NDQ_003354

answers: glucocorticoids

answers: NDQ_003355

answers: glucocorticoids

answers: NDQ_003356

answers: glucocorticoids

answers: NDQ_003357

answers: the hippocampus regulates the production of cortisol

answers: NDQ_003358

answers: The effects of stress

answers: NDQ_003359

answers: stress

answers: NDQ_003360

answers: stress

answers: NDQ_003362

answers: The effects of stress

answers: NDQ_003363

answers: stress

answers: NDQ_003371

answers: glucocorticoids

answers: NDQ_003373

answers: The effects of stress

answers: NDQ_003376

answers: glucocorticoids

answers: NDQ_003378

answers: glucocorticoids

answers: NDQ_003379

answers: glucocorticoids

answers: NDQ_003380

answers: stress

answers: NDQ_003381

answers: secreting stress hormones into the bloodstream.

answers: NDQ_003382

answers: glucocorticoids

answers: NDQ_003383

answers: Stress can cause acute and chronic changes in certain brain areas

answers: NDQ_003384

answers: glucocorticoids

answers: NDQ_003385

answers: Stress can cause acute and chronic changes in certain brain areas

answers: NDQ_003386

answers: glucocorticoids

answers: NDQ_003387

answers: hippocampus regulates the production of cortisol

answers: NDQ_003388

answers: glucocorticoids

answers: NDQ_003389

answers: glucocorticoids

answers: NDQ_003390

answers: feedback

answers: NDQ_003391

answers: glucocorticoids

answers: NDQ_003392

answers: feedback

answers: NDQ_003393

answers: glucocorticoids

answers: NDQ_003394

answers: Glucocorticoids

answers: NDQ_003395

answers: Glucocorticoids

answers: NDQ_003396

answers: glucocorticoids

text: This effect is not restricted to astronauts in space; a climber's time is passing slightly faster at the top of a mountain (a high altitude, farther from the Earth's center of gravity) compared to people at sea level. It has also been calculated that due to time dilation, the core of the Earth is 2.5 years younger than the crust.

text: This effect is not restricted to astronauts in space; a climber's time is passing slightly faster at the top of a mountain (a high altitude, farther from the Earth's center of gravity) compared to people at sea level. It has also been calculated that due to time dilation, the

text: core of the Earth

text: is 2.5 years younger than the

text: crust

answers: NDQ_003351

answers: time dilation

answers: NDQ_003352

answers: is likely to crack

answers: NDQ_003353

answers: time dilation

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: mountain

answers: NDQ_003356

answers: swell

answers: NDQ_003357

answers: the core of the Earth is 2.5 years younger than the crust

answers: NDQ_003358

answers: rockfall

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's surface

answers: NDQ_003362

answers: the core of the Earth is 2.5 years younger than the crust

answers: NDQ_003363

answers: a high altitude

answers: NDQ_003371

answers: Which of the following is not an example of a thrust fault?

answers: NDQ_003373

answers: not enough information

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: no

answers: NDQ_003380

answers: Which of the following is not a stress?

answers: NDQ_003381

answers: what is the second to last word in the passage?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: what is the first word in the passage?

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: normal faults or time dilation?

answers: NDQ_003388

answers: Which of the following is not a result of shear stress: strike-slip faults, earthquakes, or time dilation?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: time dilation

answers: NDQ_003391

answers: a mountain

answers: NDQ_003392

answers: time dilation

answers: NDQ_003393

answers: a mountain

answers: NDQ_003394

answers: is not vertical

answers: NDQ_003395

answers: is a type of

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: time dilation,

answers: NDQ_003352

answers: faster at the top of a mountain

answers: NDQ_003353

answers: time dilation,

answers: NDQ_003354

answers: a climber's time is passing slightly faster

answers: NDQ_003355

answers: mountain

answers: NDQ_003356

answers: the core of the Earth is 2.5 years younger than the crust.

answers: NDQ_003357

answers: the core of the Earth is 2.5 years younger than the crust.

answers: NDQ_003358

answers: mountain

answers: NDQ_003359

answers: gravity)

answers: NDQ_003360

answers: Earth's center of gravity)

answers: NDQ_003362

answers: astronauts in space;

answers: NDQ_003363

answers: Earth's center of gravity) compared to people at sea level.

answers: NDQ_003371

answers: This effect is not restricted to astronauts in space;

answers: NDQ_003373

answers: (a high altitude, farther from the Earth's center of gravity)

answers: NDQ_003376

answers: mountain

answers: NDQ_003378

answers: Earth's center of gravity)

answers: NDQ_003379

answers: farther from the Earth's center of gravity)

answers: NDQ_003380

answers: (a high altitude, farther from the Earth's center of gravity)

answers: NDQ_003381

answers: (a high altitude, farther from the Earth's center of gravity)

answers: NDQ_003382

answers: Earth's center of gravity)

answers: NDQ_003383

answers: This effect is not restricted to astronauts

answers: NDQ_003384

answers: mountain

answers: NDQ_003385

answers: Earth's center of gravity)

answers: NDQ_003386

answers: Earth's center of gravity)

answers: NDQ_003387

answers: This effect is not restricted to astronauts

answers: NDQ_003388

answers: (a high altitude, farther from the Earth's center of gravity)

answers: NDQ_003389

answers: mountain

answers: NDQ_003390

answers: gravity)

answers: NDQ_003391

answers: core of the Earth is 2.5 years younger than the crust.

answers: NDQ_003392

answers: gravity)

answers: NDQ_003393

answers: mountain

answers: NDQ_003394

answers: mountain

answers: NDQ_003395

answers: Earth's center of gravity)

answers: NDQ_003396

answers: Earth's center of gravity)

text: The new data that had been collected on the ocean basins also showed particular characteristics regarding the bathymetry. One of the major outcomes of these datasets was that all along the globe, a system of mid-oceanic ridges was detected. An important conclusion was that along this system, new ocean floor was being created, which led to the concept of the "Great Global Rift". This was described in the crucial paper of Bruce Heezen (1960), which would trigger a real revolution in thinking. A profound consequence of seafloor spreading is that new crust was, and still is, being continually created along the oceanic ridges. Therefore, Heezen advocated the so-called "expanding Earth" hypothesis of S. Warren Carey (see above). So, still the question remained: how can new crust be continuously added along the oceanic ridges without increasing the size of the Earth? In reality, this question had been solved already by numerous scientists during the forties and the fifties, like Arthur Holmes, Vening-Meinesz, Coates and many others: The crust in excess disappeared along what were called the oceanic trenches, where so-called "subduction" occurred. Therefore, when various scientists during the early sixties started to reason on the data at their disposal regarding the ocean floor, the pieces of the theory quickly fell into place.

text: The new data that had been collected on the ocean basins also showed particular characteristics regarding the bathymetry. One of the major outcomes of these datasets was that all along the globe, a system of mid-oceanic ridges was detected. An important conclusion was that along this system, new ocean floor was being created, which led to the concept of the "

text: Great Global Rift

text: ". This was described in the crucial paper of

text: Bruce Heezen

text: (1960), which would trigger a real revolution in thinking. A profound consequence of seafloor spreading is that new crust was, and still is, being continually created along the oceanic ridges. Therefore, Heezen advocated the so-called "

text: expanding Earth

text: " hypothesis of S. Warren Carey (see above). So, still the question remained: how can new crust be continuously added along the oceanic ridges without increasing the size of the Earth? In reality, this question had been solved already by numerous scientists during the forties and the fifties, like Arthur Holmes, Vening-Meinesz, Coates and many others: The crust in excess disappeared along what were called the oceanic trenches, where so-called "subduction" occurred. Therefore, when various scientists during the early sixties started to reason on the data at their disposal regarding the ocean floor, the pieces of the theory quickly fell into place.

answers: NDQ_003351

answers: subduction

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: subduction

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: ridge

answers: NDQ_003356

answers: subduct

answers: NDQ_003357

answers: new crust was, and still is, being continually created

answers: NDQ_003358

answers: ridge

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: oceanic ridges

answers: NDQ_003362

answers: the crust in excess disappeared along what were called the oceanic trenches

answers: NDQ_003363

answers: Great Global Rift

answers: NDQ_003371

answers: How can new crust be continually added along the oceanic ridges without increasing the size of the Earth?

answers: NDQ_003373

answers: What is a profound consequence of seafloor spreading?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: strike-slip fault

answers: NDQ_003380

answers: Which of the following is not a consequence of seafloor spreading?

answers: NDQ_003381

answers: What is a profound consequence of seafloor spreading?

answers: NDQ_003382

answers: new crust was, and still is, being continually created

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: what were called the oceanic trenches

answers: NDQ_003386

answers: movement of rock at faults

answers: NDQ_003387

answers: How can new crust be continually added along the oceanic ridges without increasing the size of the Earth?

answers: NDQ_003388

answers: How can new crust be continually added along the oceanic ridges without increasing the size of the Earth?

answers: NDQ_003389

answers: seafloor spreading

answers: NDQ_003390

answers: subduction

answers: NDQ_003391

answers: oceanic trenches

answers: NDQ_003392

answers: oceanic trenches

answers: NDQ_003393

answers: mid-oceanic ridges

answers: NDQ_003394

answers: "Great Global Rift"

answers: NDQ_003395

answers: "Great Global Rift"

answers: NDQ_003396

answers: "Great Global Rift"

answers: NDQ_003351

answers: seafloor spreading

answers: NDQ_003352

answers: The crust in excess disappeared along what were called the oceanic trenches,

answers: NDQ_003353

answers: new crust

answers: NDQ_003354

answers: oceanic trenches,

answers: NDQ_003355

answers: oceanic trenches,

answers: NDQ_003356

answers: new crust

answers: NDQ_003357

answers: "subduction"

answers: NDQ_003358

answers: oceanic trenches,

answers: NDQ_003359

answers: excess

answers: NDQ_003360

answers: seafloor spreading

answers: NDQ_003362

answers: "expanding Earth"

answers: NDQ_003363

answers: "subduction"

answers: NDQ_003371

answers: oceanic trenches,

answers: NDQ_003373

answers: oceanic trenches,

answers: NDQ_003376

answers: seafloor spreading

answers: NDQ_003378

answers: oceanic trenches,

answers: NDQ_003379

answers: oceanic trenches,

answers: NDQ_003380

answers: new crust

answers: NDQ_003381

answers: oceanic trenches,

answers: NDQ_003382

answers: oceanic trenches,

answers: NDQ_003383

answers: seafloor spreading

answers: NDQ_003384

answers: oceanic trenches,

answers: NDQ_003385

answers: oceanic trenches,

answers: NDQ_003386

answers: seafloor spreading

answers: NDQ_003387

answers: oceanic trenches,

answers: NDQ_003388

answers: seafloor spreading

answers: NDQ_003389

answers: seafloor spreading

answers: NDQ_003390

answers: "subduction"

answers: NDQ_003391

answers: oceanic trenches,

answers: NDQ_003392

answers: oceanic trenches,

answers: NDQ_003393

answers: oceanic trenches,

answers: NDQ_003394

answers: oceanic trenches,

answers: NDQ_003395

answers: oceanic trenches,

answers: NDQ_003396

answers: oceanic trenches,

text: When the body undergoes a stressful situation, the stress hormone cortisol is released. Cortisol helps the body prepare for stressful and dangerous situation. It gives a quick burst of energy, heightened memory and lower sensitivity to pain, among other things. When cortisol is present in the body at high levels and for extended periods of time, however, the body’s immune response may be suppressed. This leaves the developing bodies of children extremely vulnerable to damage and illness.  Cortisol is usually bound to proteins in adults. The protein is called the corticosteroid-binding globulin (CBG). In newborn babies, CBGs remain low and increase during the first six months after birth. Therefore, as the amount of CBGs increase, more cortisol becomes bound to the CBGs. Due to this occurrence, plasma and total cortisol levels increase. Although, there are low levels of cortisol at birth, the levels are sufficient to have serious physiological effects. Newborns do not manifest typical adult circadian rhythms in cortisol production. Usually, newborns have peak cortisol levels every 12 hours and this does not depend on the time of day. After 3 months of life, babies begin to experience the adult cortisol production patterns, an early morning cortisol peak and low evening levels of cortisol. These cortisol rhythmic changes occur throughout infancy and early childhood, along with changes in sleep patterns. The activity of the HPA stress system adapts by repeated exposure to stressful stimulation.  As newborns progress through the early months of life, babies experience increased cortisol levels during medical examinations. This is physically characterized by the fussing and crying of babies. After three months of life, babies do not respond to physical examinations with the HPA stress response system. However, babies can still respond to behavioral distress. As another example, if blood is drawn from a baby, the baby experiences an increased cortisol level. When this process is repeated 24 hours later, the same increase in cortisol is observed. In addition, during the first year of life, it becomes difficult to induce cortisol level increases to some mild stressors. These stressors include the approach of a stranger, strange events, few-minute separations from parents, and more. The decreased sensitivity of the HPA stress response may be due to physiological changes that occur in the system during early ages. The physiological changes that may occur include improved negative feedback regulation of the HPA system, and decreased sensitivity of the adrenal cortex to ACTH. Also, the availability of adult support for young children helps safeguard the activity of the HPA stress system. Many experiences can cause structural changes in the HPA system. The effects of repeated increases in cortisol levels have been researched in many animal studies, but these outcomes are also representative of humans, including young children. It has been determined that when glucocorticoids, including cortisol, are placed into various parts of the brain for many days, CRH is produced in increased quantities. In turn, this causes fear behaviors, increased caution, and activation of the SAM system. Eventually, these effects may cause  PTSD or Post-Traumatic Stress Disorder, in young children. A more serious psychological symptom seen in children, PTSD manifests symptoms such as, heightened fear and anxiety, loss of interests, flashbacks, lacking some emotions, paranoia. Other serious psychological symptoms of stress seen in children are depression, anxiety, low self-confidence and dysregulated aggression.

text: When the body undergoes a stressful situation, the stress hormone

entity_section: Factors generally increasing cortisol le

text: cortisol

text: is released. Cortisol helps the body prepare for stressful and dangerous situation. It gives a quick burst of energy, heightened memory and lower sensitivity to pain, among other things. When cortisol is present in the body at high levels and for extended periods of time, however, the body’s immune response may be suppressed. This leaves the developing bodies of children extremely vulnerable to damage and illness.  Cortisol is usually bound to proteins in adults. The protein is called the

text: corticosteroid-binding globulin

text: PTSD or Post-Traumatic Stress Disorder

text: , in young children. A more serious psychological symptom seen in children, PTSD manifests symptoms such as, heightened fear and anxiety, loss of interests, flashbacks, lacking some emotions, paranoia. Other serious psychological symptoms of stress seen in children are depression, anxiety, low self-confidence and dysregulated aggression.

answers: NDQ_003351

answers: cortisol

answers: NDQ_003352

answers: is more likely to crack

answers: NDQ_003353

answers: cortisol to increase

answers: NDQ_003354

answers: Toroweap Formation is a formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: damage and illness

answers: NDQ_003357

answers: cortisol is bound to proteins in adults.

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: cortisol

answers: NDQ_003362

answers: Newborns do not manifest typical adult circadian rhythms in cortisol production

answers: NDQ_003363

answers: cortisol

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: Which of the following is not a type of stress?

answers: NDQ_003376

answers: Which of the following is not a characteristic of basin-and-range terrain?

answers: NDQ_003378

answers: What is the stress hormone cortisol released to?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: None of the above choices.

answers: NDQ_003381

answers: unanswerable

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: Which of the following is not a type of fold that arches upward?

answers: NDQ_003385

answers: What is the term for an area where faults are clustered?

answers: NDQ_003386

answers: Which of the following is not a cause of earthquakes?

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: Which of the following is not an example of shear stress?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: a fault

answers: NDQ_003391

answers: igneous rock

answers: NDQ_003392

answers: The hanging wall

answers: NDQ_003393

answers: igneous rock

answers: NDQ_003394

answers: fault with a fault plane that is not vertical

answers: NDQ_003395

answers: cortisol

answers: NDQ_003396

answers: cortisol

answers: NDQ_003351

answers: isol production.

answers: NDQ_003352

answers: cortisol

answers: NDQ_003353

answers: cortisol

answers: NDQ_003354

answers: infancy and early childhood,

answers: NDQ_003355

answers: newborns have peak cortisol levels every 12 hours

answers: NDQ_003356

answers: stressful stimulation.

answers: NDQ_003357

answers: fussing and crying

answers: NDQ_003358

answers: newborns have peak cortisol levels every 12 hours

answers: NDQ_003359

answers: cortisol

answers: NDQ_003360

answers: babies begin to experience the adult cortisol production patterns,

answers: NDQ_003362

answers: tisol production.

answers: NDQ_003363

answers: cortisol

answers: NDQ_003371

answers: babies begin to experience the adult cortisol production patterns,

answers: NDQ_003373

answers: HPA stress system adapts by repeated exposure to stressful stimulation.

answers: NDQ_003376

answers: HPA stress system adapts by repeated exposure to stressful stimulation.

answers: NDQ_003378

answers: newborns have peak cortisol levels every 12 hours

answers: NDQ_003379

answers: adult cortisol production patterns,

answers: NDQ_003380

answers: repeated exposure to stressful stimulation.

answers: NDQ_003381

answers: HPA stress system adapts by repeated exposure to stressful stimulation.

answers: NDQ_003382

answers: changes in sleep patterns.

answers: NDQ_003383

answers: cortisol

answers: NDQ_003384

answers: newborns have peak cortisol levels every 12 hours

answers: NDQ_003385

answers: HPA stress system adapts by repeated exposure to stressful stimulation.

answers: NDQ_003386

answers: peak cortisol levels every 12 hours

answers: NDQ_003387

answers: cortisol

answers: NDQ_003388

answers: low evening levels of cortisol.

answers: NDQ_003389

answers: cortisol levels

answers: NDQ_003390

answers: changes in sleep patterns.

answers: NDQ_003391

answers: newborns have peak cortisol levels every 12 hours

answers: NDQ_003392

answers: cortisol rhythmic changes

answers: NDQ_003393

answers: newborns have peak cortisol levels every 12 hours

answers: NDQ_003394

answers: repeated exposure to stressful stimulation.

answers: NDQ_003395

answers: corticosteroid-binding globulin

answers: NDQ_003396

answers: stressful stimulation.

text: Santa Clara Valley was created by the sudden growth of the Santa Cruz Mountains and the Diablo Range during the later Cenozoic era. This was a period of intense mountain building in California when the folding and thrusting of the Earth's crust, combined with active volcanism, gave shape to the present state of California. Hence, Santa Clara Valley is a structural valley, created by mountain building as opposed to an erosional valley, or a valley which has undergone the wearing away of the Earth's surface by natural agents. The underlying geology of the Santa Cruz Mountains was also formed by the sediment of the ancient seas, where marine shale points to Miocene origin. Today one can still find evidence of this in the Santa Cruz Mountains, where shark's teeth and the remains of maritime life are still found as high as Scotts Valley, a city nestled in the mountains. The highest peak on the Santa Cruz Mountains side of the valley is Loma Prieta at 3,790 feet. The highest peak in the Diablo Range side of the valley is Mount Hamilton, specifically Copernicus Peak at 4,370 feet elevation. This is the highest peak in Santa Clara County.

text: Santa Clara Valley was created by the sudden growth of the

text: Santa Cruz Mountains

text: and the

text: Diablo Range

text: during the later

text: Cenozoic

text: era. This was a period of intense mountain building in California when the folding and thrusting of the Earth's

text: crust

text: , combined with active

text: volcanism

text: , gave shape to the present state of California. Hence, Santa Clara Valley is a structural valley, created by mountain building as opposed to an erosional valley, or a valley which has undergone the wearing away of the Earth's surface by natural agents. The underlying geology of the Santa Cruz Mountains was also formed by the

text: sediment

text: of the ancient seas, where marine

text: shale

text: points to

text: Miocene

text: origin. Today one can still find evidence of this in the Santa Cruz Mountains, where

text: shark

text: 's teeth and the remains of maritime life are still found as high as

text: Scotts Valley

text: , a city nestled in the mountains. The highest peak on the Santa Cruz Mountains side of the valley is

text: Loma Prieta

text: at 3,790 feet. The highest peak in the

text: Diablo Range

text: side of the valley is

text: Mount Hamilton

text: , specifically Copernicus Peak at 4,370 feet elevation. This is the highest peak in

text: Santa Clara County

answers: NDQ_003351

answers: thrusting

answers: NDQ_003352

answers: folds and thrusts

answers: NDQ_003353

answers: folding and thrusting

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: thrusting

answers: NDQ_003356

answers: wear away

answers: NDQ_003357

answers: folds and thrusts of the Earth's crust

answers: NDQ_003358

answers: structural valley

answers: NDQ_003359

answers: folds

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: Santa Clara Valley is a structural valley

answers: NDQ_003363

answers: Cenozoic era

answers: NDQ_003371

answers: Which of the following is not a type of valley: structural valley, created by mountain building, or erosional valley?

answers: NDQ_003373

answers: What is the highest peak in Santa Clara County?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: what is the highest peak in Santa Clara County?

answers: NDQ_003379

answers: What is the highest peak in Santa Clara County?

answers: NDQ_003380

answers: What is Loma Prieta?

answers: NDQ_003381

answers: What is the highest peak in Santa Clara County?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: folding and thrusting

answers: NDQ_003384

answers: What is the highest peak in Santa Clara County?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: active volcanism

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: folding and thrusting of the Earth's crust, combined with active volcanism, gave shape to the present state of California?

answers: NDQ_003388

answers: Which of the following is not a type of fault: Strike-slip faults, active volcanism, or structural valley?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: fold and thrusting

answers: NDQ_003391

answers: underlying geology

answers: NDQ_003392

answers: thrusting

answers: NDQ_003393

answers: mountain

answers: NDQ_003394

answers: active volcanism

answers: NDQ_003395

answers: active volcanism

answers: NDQ_003396

answers: active volcanism

answers: NDQ_003351

answers: thrusting of the Earth's crust, combined with active volcanism,

answers: NDQ_003352

answers: thrusting

answers: NDQ_003353

answers: folding and thrusting

answers: NDQ_003354

answers: Loma Prieta

answers: NDQ_003355

answers: erosional valley,

answers: NDQ_003356

answers: erosional valley,

answers: NDQ_003357

answers: erosional valley,

answers: NDQ_003358

answers: erosional valley,

answers: NDQ_003359

answers: active volcanism,

answers: NDQ_003360

answers: volcanism,

answers: NDQ_003362

answers: erosional valley,

answers: NDQ_003363

answers: active volcanism,

answers: NDQ_003371

answers: thrusting of the Earth's crust, combined with active volcanism,

answers: NDQ_003373

answers: erosional valley,

answers: NDQ_003376

answers: mountain building

answers: NDQ_003378

answers: active volcanism,

answers: NDQ_003379

answers: 3,790 feet.

answers: NDQ_003380

answers: thrusting

answers: NDQ_003381

answers: thrusting of the Earth's crust, combined with active volcanism,

answers: NDQ_003382

answers: thrusting of the Earth's crust, combined with active volcanism,

answers: NDQ_003383

answers: thrusting of the Earth's crust, combined with active volcanism,

answers: NDQ_003384

answers: erosional valley,

answers: NDQ_003385

answers: thrusting of the Earth's crust, combined with active volcanism,

answers: NDQ_003386

answers: active volcanism,

answers: NDQ_003387

answers: erosional valley,

answers: NDQ_003388

answers: active volcanism,

answers: NDQ_003389

answers: folding and thrusting of the Earth's crust,

answers: NDQ_003390

answers: thrusting of the Earth's crust, combined with active volcanism,

answers: NDQ_003391

answers: Santa Cruz Mountains

answers: NDQ_003392

answers: thrusting of the Earth's crust, combined with active volcanism,

answers: NDQ_003393

answers: erosional valley,

answers: NDQ_003394

answers: active volcanism,

answers: NDQ_003395

answers: active volcanism,

answers: NDQ_003396

answers: erosional valley,

text: Earth's lithosphere includes the crust and the uppermost mantle, which constitute the hard and rigid outer layer of the Earth. The lithosphere is subdivided into tectonic plates. The uppermost part of the lithosphere that chemically reacts to the atmosphere, hydrosphere and biosphere through the soil forming process is called the pedosphere. The lithosphere is underlain by the asthenosphere which is the weaker, hotter, and deeper part of the upper mantle. The boundary between the lithosphere and the underlying asthenosphere is known as the Lithosphere-Asthenosphere boundary and is defined by a difference in response to stress: the lithosphere remains rigid for very long periods of geologic time in which it deforms elastically and through brittle failure, while the asthenosphere deforms viscously and accommodates strain through plastic deformation. The study of past and current formations of landscapes is called geomorphology.

text: Earth's lithosphere includes the crust and the uppermost mantle, which constitute the hard and rigid outer layer of the Earth. The lithosphere is subdivided into

text: tectonic plates

text: . The uppermost part of the lithosphere that chemically reacts to the

text: atmosphere

text: hydrosphere

text: and

text: biosphere

text: through the

text: soil forming process

text: is called the

text: pedosphere

text: . The lithosphere is underlain by the

text: asthenosphere

text: which is the weaker, hotter, and deeper part of the upper mantle. The boundary between the lithosphere and the underlying asthenosphere is known as the

text: Lithosphere-Asthenosphere boundary

text: and is defined by a difference in response to stress: the lithosphere remains rigid for very long periods of geologic time in which it deforms elastically and through brittle failure, while the asthenosphere deforms viscously and accommodates strain through plastic deformation. The study of past and current formations of landscapes is called

text: geomorphology

answers: NDQ_003351

answers: brittle failure

answers: NDQ_003352

answers: brittle

answers: NDQ_003353

answers: brittle failure

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: tectonic plate

answers: NDQ_003356

answers: accommodate strain

answers: NDQ_003357

answers: asthenosphere deforms viscously and accommodates strain through plastic deformation

answers: NDQ_003358

answers: asthenosphere

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: plates

answers: NDQ_003362

answers: the study of past and current formations of landscapes is called geomorphology

answers: NDQ_003363

answers: tectonic plates

answers: NDQ_003371

answers: What is the study of past and current formations of landscapes called?

answers: NDQ_003373

answers: How would you describe the asthenosphere?

answers: NDQ_003376

answers: What is the study of past and current formations of landscapes called?

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: How does the lithosphere deform?

answers: NDQ_003382

answers: Which of the following is not a type of stress?

answers: NDQ_003383

answers: What is the relationship between lithosphere and asthenosphere?

answers: NDQ_003384

answers: What is the study of past and current formations of landscapes?

answers: NDQ_003385

answers: What is the study of past and current formations of landscapes called?

answers: NDQ_003386

answers: What is the study of past and current formations of landscapes called?

answers: NDQ_003387

answers: Which of the following is not a type of normal fault?

answers: NDQ_003388

answers: What is the boundary between the lithosphere and the underlying asthenosphere?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: tectonic plate

answers: NDQ_003391

answers: asthenosphere

answers: NDQ_003392

answers: tectonic plate

answers: NDQ_003393

answers: asthenosphere

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: tectonic plates

answers: NDQ_003396

answers: tectonic plates

answers: NDQ_003351

answers: brittle failure,

answers: NDQ_003352

answers: it deforms elastically and through brittle failure,

answers: NDQ_003353

answers: brittle failure,

answers: NDQ_003354

answers: geomorphology.

answers: NDQ_003355

answers: pedosphere.

answers: NDQ_003356

answers: accommodates strain

answers: NDQ_003357

answers: brittle failure,

answers: NDQ_003358

answers: brittle failure,

answers: NDQ_003359

answers: stress:

answers: NDQ_003360

answers: tectonic plates.

answers: NDQ_003362

answers: lithosphere remains rigid for very long periods of geologic time

answers: NDQ_003363

answers: tectonic plates.

answers: NDQ_003371

answers: Lithosphere-Asthenosphere boundary

answers: NDQ_003373

answers: asthenosphere

answers: NDQ_003376

answers: geomorphology.

answers: NDQ_003378

answers: geomorphology.

answers: NDQ_003379

answers: tectonic plates.

answers: NDQ_003380

answers: stress:

answers: NDQ_003381

answers: elastically

answers: NDQ_003382

answers: brittle failure,

answers: NDQ_003383

answers: brittle failure,

answers: NDQ_003384

answers: geomorphology.

answers: NDQ_003385

answers: tectonic plates.

answers: NDQ_003386

answers: tectonic plates.

answers: NDQ_003387

answers: brittle failure,

answers: NDQ_003388

answers: Lithosphere-Asthenosphere boundary

answers: NDQ_003389

answers: geomorphology.

answers: NDQ_003390

answers: tectonic plates.

answers: NDQ_003391

answers: asthenosphere

answers: NDQ_003392

answers: tectonic plates.

answers: NDQ_003393

answers: lithosphere

answers: NDQ_003394

answers: tectonic plates.

answers: NDQ_003395

answers: tectonic plates.

answers: NDQ_003396

answers: tectonic plates.

text: In the field of civil engineering, geological principles and analyses are used in order to ascertain the mechanical principles of the material on which structures are built. This allows tunnels to be built without collapsing, bridges and skyscrapers to be built with sturdy foundations, and buildings to be built that will not settle in clay and mud.

text: In the field of

text: civil engineering

text: , geological principles and analyses are used in order to ascertain the mechanical principles of the material on which structures are built. This allows tunnels to be built without collapsing, bridges and skyscrapers to be built with sturdy foundations, and buildings to be built that will not settle in clay and mud.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: collapses

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: tunnel

answers: NDQ_003356

answers: collapse

answers: NDQ_003357

answers: tunnels can be built without collapsing

answers: NDQ_003358

answers: tunnel

answers: NDQ_003359

answers: collapses

answers: NDQ_003360

answers: geological principles

answers: NDQ_003362

answers: tunnels can be built without collapsing

answers: NDQ_003363

answers: geological principles

answers: NDQ_003371

answers: Which of the following is not an example of a thrust fault?

answers: NDQ_003373

answers: what is the reason for this?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: Which of the following is not a result of confining stress?

answers: NDQ_003382

answers: what is the most common stress at convergent plates

answers: NDQ_003383

answers: None of the above choices.

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: what is the first word in the passage?

answers: NDQ_003386

answers: None of the above choices.

answers: NDQ_003387

answers: Which of the following is not a cause of normal faults?

answers: NDQ_003388

answers: Which of the following is not a result of shear stress?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: collapsing

answers: NDQ_003391

answers: mud

answers: NDQ_003392

answers: collapsing

answers: NDQ_003393

answers: is a crater

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: is a

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: collapsing,

answers: NDQ_003352

answers: collapsing,

answers: NDQ_003353

answers: collapsing,

answers: NDQ_003354

answers: In the field of civil engineering,

answers: NDQ_003355

answers: tunnels to be built without collapsing,

answers: NDQ_003356

answers: collapsing,

answers: NDQ_003357

answers: collapsing,

answers: NDQ_003358

answers: tunnels

answers: NDQ_003359

answers: tunnels to be built without collapsing,

answers: NDQ_003360

answers: geological principles

answers: NDQ_003362

answers: tunnels to be built without collapsing,

answers: NDQ_003363

answers: geological principles

answers: NDQ_003371

answers: In the field of civil engineering,

answers: NDQ_003373

answers: tunnels to be built without collapsing,

answers: NDQ_003376

answers: clay and mud.

answers: NDQ_003378

answers: In the field of civil engineering,

answers: NDQ_003379

answers: tunnels to be built without collapsing,

answers: NDQ_003380

answers: tunnels to be built without collapsing,

answers: NDQ_003381

answers: tunnels to be built without collapsing,

answers: NDQ_003382

answers: tunnels to be built without collapsing,

answers: NDQ_003383

answers: geological principles and analyses are used in order to ascertain the mechanical principles

answers: NDQ_003384

answers: skyscrapers

answers: NDQ_003385

answers: In the field of civil engineering,

answers: NDQ_003386

answers: geological principles

answers: NDQ_003387

answers: geological principles and analyses are used in order to ascertain the mechanical principles

answers: NDQ_003388

answers: In the field of civil engineering,

answers: NDQ_003389

answers: tunnels to be built without collapsing,

answers: NDQ_003390

answers: collapsing,

answers: NDQ_003391

answers: tunnels to be built without collapsing,

answers: NDQ_003392

answers: tunnels to be built without collapsing,

answers: NDQ_003393

answers: tunnels to be built without collapsing,

answers: NDQ_003394

answers: tunnels to be built without collapsing,

answers: NDQ_003395

answers: tunnels to be built without collapsing,

answers: NDQ_003396

answers: tunnels to be built without collapsing,

text: Modern soil science offers the following definition: "Primary Minerals: The thickness of the earth's crust varies from 10 km under the ocean to 30 km under the continents. Of the 88 naturally occurring elements on earth, only 8 make [up] most of the crust. The earth's crust and soils are dominated by the silicic acid in combination with Na, Al, K, Ca, Fe and O ions. ...Those elements are components of primary minerals, whereas primary minerals are components of parent rocks. There are almost 3000 known minerals, but only 20 are common and just 10 minerals make up 90 % of the earth's crust. Primary minerals are defined as minerals found in soil but not formed in soil. This definition is different from that of secondary minerals, which are defined as minerals formed in soils." This is further defined by Dr. Broome of North Carolina State:

text: Modern soil science offers the following definition: "Primary Minerals: The thickness of the earth's crust varies from 10 km under the ocean to 30 km under the continents. Of the 88 naturally occurring elements on earth, only 8 make [up] most of the crust. The earth's crust and soils are dominated by the silicic acid in combination with Na, Al, K, Ca, Fe and O ions. ...Those elements are components of primary minerals, whereas primary minerals are components of parent rocks. There are almost 3000 known minerals, but only 20 are common and just 10 minerals make up 90 % of the earth's crust. Primary minerals are defined as minerals found in soil but not formed in soil. This definition is different from that of secondary minerals, which are defined as minerals formed in soils." This is further defined by Dr. Broome of North Carolina State:

answers: NDQ_003351

answers: primary minerals

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: primary minerals to form

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: form in soil

answers: NDQ_003357

answers: primary minerals are found in soil but not formed in soil.

answers: NDQ_003358

answers: rock pocket

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: continental plates

answers: NDQ_003362

answers: primary minerals are components of parent rocks

answers: NDQ_003363

answers: primary minerals

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: primary minerals are components of parent rocks

answers: NDQ_003376

answers: primary minerals

answers: NDQ_003378

answers: the thickness of the earth's crust

answers: NDQ_003379

answers: strike-slip fault

answers: NDQ_003380

answers: Which of the following is not a stress?

answers: NDQ_003381

answers: primary minerals are components of parent rocks

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: primary minerals are components of parent rocks

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: The thickness of the earth's crust

answers: NDQ_003386

answers: primary minerals are components of parent rocks

answers: NDQ_003387

answers: primary minerals are components of parent rocks

answers: NDQ_003388

answers: primary minerals are components of parent rocks

answers: NDQ_003389

answers: secondary minerals

answers: NDQ_003390

answers: a fault

answers: NDQ_003391

answers: parent rocks

answers: NDQ_003392

answers: tectonic

answers: NDQ_003393

answers: parent rocks

answers: NDQ_003394

answers: horizontal fault

answers: NDQ_003395

answers: NDQ_003396

answers: horizontal fault

answers: NDQ_003351

answers: silicic acid

answers: NDQ_003352

answers: primary minerals are components of parent rocks.

answers: NDQ_003353

answers: primary minerals, whereas primary minerals are components of parent rocks.

answers: NDQ_003354

answers: Primary minerals are defined as minerals found in soil but not formed in soil.

answers: NDQ_003355

answers: secondary minerals,

answers: NDQ_003356

answers: primary minerals are components of parent rocks.

answers: NDQ_003357

answers: primary minerals are components of parent rocks.

answers: NDQ_003358

answers: Primary minerals

answers: NDQ_003359

answers: primary minerals are components of parent rocks.

answers: NDQ_003360

answers: ocean to 30 km under the continents.

answers: NDQ_003362

answers: Modern soil science offers the following definition: "Primary Minerals:

answers: NDQ_003363

answers: 10 km under the ocean to 30 km under the continents.

answers: NDQ_003371

answers: primary minerals are components of parent rocks.

answers: NDQ_003373

answers: primary minerals are components of parent rocks.

answers: NDQ_003376

answers: North Carolina State:

answers: NDQ_003378

answers: secondary minerals,

answers: NDQ_003379

answers: secondary minerals,

answers: NDQ_003380

answers: primary minerals are components of parent rocks.

answers: NDQ_003381

answers: primary minerals are components of parent rocks.

answers: NDQ_003382

answers: 88

answers: NDQ_003383

answers: primary minerals are components of parent rocks.

answers: NDQ_003384

answers: secondary minerals,

answers: NDQ_003385

answers: North Carolina State:

answers: NDQ_003386

answers: primary minerals are components of parent rocks.

answers: NDQ_003387

answers: secondary minerals,

answers: NDQ_003388

answers: secondary minerals,

answers: NDQ_003389

answers: rocks.

answers: NDQ_003390

answers: North Carolina State:

answers: NDQ_003391

answers: parent rocks.

answers: NDQ_003392

answers: North Carolina State:

answers: NDQ_003393

answers: primary minerals are components of parent rocks.

answers: NDQ_003394

answers: secondary minerals,

answers: NDQ_003395

answers: 10 km under the ocean to 30 km under the continents.

answers: NDQ_003396

answers: secondary minerals,

text: Several known earthquake faults criss-cross the Glendale area and adjacent mountains, as in much of Southern California. Among the more recognized faults are the Sierra Madre and Hollywood faults, situated in the city's northern and southwestern portions, respectively. Additionally, the Verdugo and Raymond faults intersect through the city's central and southeastern areas. The San Gabriel fault, meanwhile, is located northeast of the city. Roughly  northeast of Glendale is a major portion of the San Andreas Fault known as the "Big Bend", where quake-recurrence tracking shows major activity roughly every 140–160 years. The closest portion of the San Andreas is actually  from Glendale. The last major quake along the southern San Andreas was recorded in 1857.

text: Several known earthquake faults criss-cross the Glendale area and adjacent mountains, as in much of Southern California. Among the more recognized faults are the Sierra Madre and Hollywood faults, situated in the city's northern and southwestern portions, respectively. Additionally, the Verdugo and Raymond faults intersect through the city's central and southeastern areas. The San Gabriel fault, meanwhile, is located northeast of the city. Roughly  northeast of Glendale is a major portion of the

text: San Andreas Fault

text: known as the "Big Bend", where quake-recurrence tracking shows major activity roughly every 140–160 years. The closest portion of the San Andreas is actually  from Glendale. The last major quake along the southern San Andreas was recorded in 1857.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: more likely to crack

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: Big Bend

answers: NDQ_003356

answers: quake

answers: NDQ_003357

answers: quake-recurrence tracking shows major activity

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: San Andreas fault

answers: NDQ_003362

answers: The closest portion of the San Andreas is actually from Glendale

answers: NDQ_003363

answers: Southern California

answers: NDQ_003371

answers: What type of fault is the San Gabriel fault?

answers: NDQ_003373

answers: How would you describe a rock that is deeply buried?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: How does rock deform?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: yes

answers: NDQ_003387

answers: What are normal faults caused by?

answers: NDQ_003388

answers: What type of faults are strike-slip faults?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: San Andreas Fault

answers: NDQ_003391

answers: unanswerable

answers: NDQ_003392

answers: San Andreas

answers: NDQ_003393

answers: The San Gabriel fault

answers: NDQ_003394

answers: San Andreas Fault

answers: NDQ_003395

answers: San Andreas Fault

answers: NDQ_003396

answers: Raymond faults

answers: NDQ_003351

answers: earthquake faults

answers: NDQ_003352

answers: major activity roughly every 140–160 years.

answers: NDQ_003353

answers: earthquake faults

answers: NDQ_003354

answers: Several known earthquake faults

answers: NDQ_003355

answers: "Big Bend",

answers: NDQ_003356

answers: earthquake faults

answers: NDQ_003357

answers: every 140–160 years.

answers: NDQ_003358

answers: earthquake faults

answers: NDQ_003359

answers: earthquake faults

answers: NDQ_003360

answers: earthquake faults

answers: NDQ_003362

answers: The closest portion of the San Andreas is actually from Glendale.

answers: NDQ_003363

answers: Southern California.

answers: NDQ_003371

answers: earthquake faults

answers: NDQ_003373

answers: Several known earthquake faults

answers: NDQ_003376

answers: mountains,

answers: NDQ_003378

answers: earthquake faults

answers: NDQ_003379

answers: Sierra Madre and Hollywood faults,

answers: NDQ_003380

answers: earthquake faults

answers: NDQ_003381

answers: earthquake faults

answers: NDQ_003382

answers: San Andreas Fault

answers: NDQ_003383

answers: earthquake faults

answers: NDQ_003384

answers: mountains,

answers: NDQ_003385

answers: earthquake faults

answers: NDQ_003386

answers: faults

answers: NDQ_003387

answers: earthquake faults

answers: NDQ_003388

answers: earthquake faults

answers: NDQ_003389

answers: earthquake faults

answers: NDQ_003390

answers: San Andreas Fault

answers: NDQ_003391

answers: mountains,

answers: NDQ_003392

answers: San Andreas Fault

answers: NDQ_003393

answers: mountains,

answers: NDQ_003394

answers: San Gabriel fault,

answers: NDQ_003395

answers: San Andreas Fault

answers: NDQ_003396

answers: San Gabriel fault,

text: In some situations, a single subduction zone may show both aspects along its length, as part of a plate subducts beneath a continent and part beneath adjacent oceanic crust.

text: In some situations, a single subduction zone may show both aspects along its length, as part of a plate subducts beneath a continent and part beneath adjacent oceanic crust.

answers: NDQ_003351

answers: subduction

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: subduction

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: subduction zone

answers: NDQ_003356

answers: subduct

answers: NDQ_003357

answers: a plate subducts beneath the oceanic crust

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: is pushed together

answers: NDQ_003360

answers: subduction zones

answers: NDQ_003362

answers: a single subduction zone may show both aspects along its length

answers: NDQ_003363

answers: subduction zones

answers: NDQ_003371

answers: What is a thrust fault?

answers: NDQ_003373

answers: Why would a rock be deeply buried?

answers: NDQ_003376

answers: subduction zone

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: The dip of the fault plane is horizontal

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What would happen if a plate subducts beneath a continent?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: None of the above choices.

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: NDQ_003386

answers: None of the above choices.

answers: NDQ_003387

answers: Which of the following is not caused by compression stress?

answers: NDQ_003388

answers: Which of the following is not a type of strike-slip fault?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: subduction zone

answers: NDQ_003391

answers: subduction zone

answers: NDQ_003392

answers: subduction zone

answers: NDQ_003393

answers: subduction zone

answers: NDQ_003394

answers: isosceles

answers: NDQ_003395

answers: is a type of fault

answers: NDQ_003396

answers: isosceles

answers: NDQ_003351

answers: oceanic crust.

answers: NDQ_003352

answers: oceanic crust.

answers: NDQ_003353

answers: subduction zone

answers: NDQ_003354

answers: beneath adjacent oceanic crust.

answers: NDQ_003355

answers: subduction zone

answers: NDQ_003356

answers: subducts beneath a continent and part beneath adjacent oceanic crust.

answers: NDQ_003357

answers: plate subducts beneath a continent and part beneath adjacent oceanic crust.

answers: NDQ_003358

answers: subduction zone

answers: NDQ_003359

answers: plate subducts beneath a continent and part beneath adjacent oceanic crust.

answers: NDQ_003360

answers: subduction zone

answers: NDQ_003362

answers: part of a plate subducts beneath a continent

answers: NDQ_003363

answers: subduction zone

answers: NDQ_003371

answers: a single subduction zone

answers: NDQ_003373

answers: oceanic crust.

answers: NDQ_003376

answers: oceanic crust.

answers: NDQ_003378

answers: oceanic crust.

answers: NDQ_003379

answers: a single subduction zone may show both aspects along its length,

answers: NDQ_003380

answers: oceanic crust.

answers: NDQ_003381

answers: oceanic crust.

answers: NDQ_003382

answers: oceanic crust.

answers: NDQ_003383

answers: oceanic crust.

answers: NDQ_003384

answers: subduction zone

answers: NDQ_003385

answers: subduction zone

answers: NDQ_003386

answers: subduction zone

answers: NDQ_003387

answers: In some situations, a single subduction zone

answers: NDQ_003388

answers: oceanic crust.

answers: NDQ_003389

answers: plate subducts beneath a continent and part beneath adjacent oceanic crust.

answers: NDQ_003390

answers: subduction zone

answers: NDQ_003391

answers: oceanic crust.

answers: NDQ_003392

answers: subduction zone

answers: NDQ_003393

answers: oceanic crust.

answers: NDQ_003394

answers: a single subduction zone

answers: NDQ_003395

answers: a single subduction zone

answers: NDQ_003396

answers: subduction zone

text: Adult-born neurons appear to have a role in the regulation of stress. Studies have linked neurogenesis to the beneficial actions of specific antidepressants, suggesting a connection between decreased hippocampal neurogenesis and depression. In a pioneer study, scientists demonstrated that the behavioral benefits of antidepressant administration in mice is reversed when neurogenesis is prevented with x-irradiation techniques. In fact, newborn neurons are more excitable than older neurons due to a differential expression of GABA receptors. A plausible model, therefore, is that these neurons augment the role of the hippocampus in the negative feedback mechanism of the HPA-axis (physiological stress) and perhaps in inhibiting the amygdala (the region of brain responsible for fearful responses to stimuli). Indeed, suppression of adult neurogenesis can lead to an increased HPA-axis stress response in mildly stressful situations. This is consistent with numerous findings linking stress-relieving activities (learning, exposure to a new yet benign environment, and exercise) to increased levels of neurogenesis, as well as the observation that animals exposed to physiological stress (cortisol) or psychological stress (e.g. isolation) show markedly decreased levels of newborn neurons. Interestingly, under chronic stress conditions, the elevation of newborn neurons by antidepressants improves the hippocampal-dependent control on the stress response; without newborn neurons, antidepressants are unable to restore the regulation of the stress response and recovery becomes impossible.

text: Adult-born neurons appear to have a role in the regulation of

text: stress

text: . Studies have linked neurogenesis to the beneficial actions of specific

text: antidepressant

text: s, suggesting a connection between decreased hippocampal neurogenesis and

text: depression

text: . In a pioneer study, scientists demonstrated that the behavioral benefits of antidepressant administration in

text: mice

text: is reversed when neurogenesis is prevented with

text: x-irradiation

text: techniques. In fact, newborn neurons are more excitable than older neurons due to a differential expression of

text: GABA

text: receptors. A plausible model, therefore, is that these neurons augment the role of the hippocampus in the negative feedback mechanism of the

text: HPA-axis

text: (physiological stress) and perhaps in inhibiting the

text: amygdala

text: (the region of brain responsible for fearful responses to stimuli). Indeed, suppression of adult neurogenesis can lead to an increased

text: HPA-axis

text: stress response in mildly stressful situations. This is consistent with numerous findings linking stress-relieving activities (learning, exposure to a new yet benign environment, and exercise) to increased levels of neurogenesis, as well as the observation that animals exposed to physiological stress (

text: cortisol

text: ) or

text: psychological stress

text: (e.g. isolation) show markedly decreased levels of newborn neurons. Interestingly, under chronic stress conditions, the elevation of newborn neurons by antidepressants improves the hippocampal-dependent control on the stress response; without newborn neurons, antidepressants are unable to restore the regulation of the stress response and recovery becomes impossible.

answers: NDQ_003351

answers: cortisol

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: cortisol to increase

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: increase in size

answers: NDQ_003357

answers: neurons augment the role of the hippocampus

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: x-irradiation techniques

answers: NDQ_003363

answers: the same time

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: What is the main idea of this passage?

answers: NDQ_003376

answers: basin-and-range is caused by compressive forces

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What is the HPA-axis?

answers: NDQ_003381

answers: What is the name of the region of brain responsible for fearful responses to stimuli?

answers: NDQ_003382

answers: what is the most common stress at convergent plates

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: Fault zones are areas where faults are clustered.

answers: NDQ_003386

answers: movement of rock at faults

answers: NDQ_003387

answers: Which of the following is not caused by compression stress?

answers: NDQ_003388

answers: What is the primary cause of strike-slip faults?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: The hanging wall

answers: NDQ_003391

answers: dip-slip fault

answers: NDQ_003392

answers: The hanging wall

answers: NDQ_003393

answers: dip-slip fault

answers: NDQ_003394

answers: lateral

answers: NDQ_003395

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: (physiological stress)

answers: NDQ_003352

answers: suppression of adult neurogenesis

answers: NDQ_003353

answers: Adult-born neurons

answers: NDQ_003354

answers: newborn neurons are more excitable than older neurons

answers: NDQ_003355

answers: hippocampus

answers: NDQ_003356

answers: x-irradiation

answers: NDQ_003357

answers: suppression of adult neurogenesis

answers: NDQ_003358

answers: Adult-born neurons

answers: NDQ_003359

answers: x-irradiation

answers: NDQ_003360

answers: stress.

answers: NDQ_003362

answers: x-irradiation

answers: NDQ_003363

answers: Adult-born neurons

answers: NDQ_003371

answers: newborn neurons are more excitable than older neurons

answers: NDQ_003373

answers: Adult-born neurons

answers: NDQ_003376

answers: newborn neurons are more excitable than older neurons

answers: NDQ_003378

answers: HPA-axis

answers: NDQ_003379

answers: negative feedback mechanism of the HPA-axis

answers: NDQ_003380

answers: (physiological stress)

answers: NDQ_003381

answers: psychological stress

answers: NDQ_003382

answers: HPA-axis

answers: NDQ_003383

answers: Adult-born neurons

answers: NDQ_003384

answers: HPA-axis

answers: NDQ_003385

answers: HPA-axis

answers: NDQ_003386

answers: Adult-born neurons

answers: NDQ_003387

answers: HPA-axis

answers: NDQ_003388

answers: Adult-born neurons

answers: NDQ_003389

answers: Adult-born neurons

answers: NDQ_003390

answers: Adult-born neurons

answers: NDQ_003391

answers: Adult-born neurons

answers: NDQ_003392

answers: Adult-born neurons

answers: NDQ_003393

answers: Adult-born neurons

answers: NDQ_003394

answers: x-irradiation

answers: NDQ_003395

answers: x-irradiation techniques.

answers: NDQ_003396

answers: x-irradiation techniques.

text: A major shift in the Earth's crust had severed the city from its surrounding landform, leaving it an island with virtually no outside contact. Money-crazed inhabitants soon lashed out for the city's remaining but useless vestiges of power, preaching salvation while hiding their wicked motives.

text: A major shift in the Earth's crust had severed the city from its surrounding landform, leaving it an island with virtually no outside contact. Money-crazed inhabitants soon lashed out for the city's remaining but useless vestiges of power, preaching salvation while hiding their wicked motives.

answers: NDQ_003351

answers: earthquakes

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: movement

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: landform

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: a major shift in the Earth's crust would have left the city with virtually no outside contact

answers: NDQ_003358

answers: island

answers: NDQ_003359

answers: has shifted

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: a major shift in the Earth's crust had severed the city from its surrounding landform

answers: NDQ_003363

answers: the same time as the city

answers: NDQ_003371

answers: What may be a plausible fact about the city?

answers: NDQ_003373

answers: How would you describe the island?

answers: NDQ_003376

answers: None of the above choices.

answers: NDQ_003378

answers: what is the last option?

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: How would you describe the city?

answers: NDQ_003381

answers: What will happen to the surrounding landform?

answers: NDQ_003382

answers: None of the above choices.

answers: NDQ_003383

answers: None of the above choices.

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: what is the last word in the passage?

answers: NDQ_003386

answers: None of the above choices.

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: normal faults or money-crazed inhabitants?

answers: NDQ_003388

answers: Which of the following is not a type of fault?

answers: NDQ_003389

answers: not enough information

answers: NDQ_003390

answers: Earth's crust

answers: NDQ_003391

answers: is an island

answers: NDQ_003392

answers: a major shift

answers: NDQ_003393

answers: is an island

answers: NDQ_003394

answers: isobath

answers: NDQ_003395

answers: NDQ_003396

answers: NDQ_003351

answers: shift in the Earth's crust

answers: NDQ_003352

answers: severed the city from its surrounding landform,

answers: NDQ_003353

answers: shift in the Earth's crust

answers: NDQ_003354

answers: A major shift in the Earth's crust

answers: NDQ_003355

answers: island

answers: NDQ_003356

answers: island with virtually no outside contact.

answers: NDQ_003357

answers: Earth's crust had severed the city from its surrounding landform,

answers: NDQ_003358

answers: island

answers: NDQ_003359

answers: shift in the Earth's crust

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: leaving it an island with virtually no outside contact.

answers: NDQ_003363

answers: Earth's crust

answers: NDQ_003371

answers: major shift in the Earth's crust

answers: NDQ_003373

answers: major shift in the Earth's crust

answers: NDQ_003376

answers: A major shift in the Earth's crust

answers: NDQ_003378

answers: shift in the Earth's crust

answers: NDQ_003379

answers: island with virtually no outside contact.

answers: NDQ_003380

answers: A major shift in the Earth's crust

answers: NDQ_003381

answers: Earth's crust had severed the city from its surrounding landform,

answers: NDQ_003382

answers: Earth's crust had severed the city from its surrounding landform,

answers: NDQ_003383

answers: shift in the Earth's crust

answers: NDQ_003384

answers: major shift in the Earth's crust

answers: NDQ_003385

answers: major shift in the Earth's crust

answers: NDQ_003386

answers: Earth's crust

answers: NDQ_003387

answers: A major shift in the Earth's crust

answers: NDQ_003388

answers: A major shift in the Earth's crust

answers: NDQ_003389

answers: Earth's crust

answers: NDQ_003390

answers: Earth's crust

answers: NDQ_003391

answers: Earth's crust had severed the city from its surrounding landform,

answers: NDQ_003392

answers: shift in the Earth's crust

answers: NDQ_003393

answers: Earth's crust had severed the city from its surrounding landform,

answers: NDQ_003394

answers: major shift in the Earth's crust

answers: NDQ_003395

answers: Earth's crust had severed the city from its surrounding landform,

answers: NDQ_003396

answers: major shift in the Earth's crust

text: When the theory of plate tectonics became established in the 1960s, it became clear Suess's "sea" had in fact been an ocean. Plate tectonics also provided the mechanism by which the former ocean disappeared: oceanic crust can subduct under continental crust.

text: When the theory of

text: plate tectonics

text: became established in the 1960s, it became clear Suess's "sea" had in fact been an

text: ocean

text: . Plate tectonics also provided the mechanism by which the former ocean disappeared:

text: oceanic crust

text: can

text: subduct

text: under

text: continental crust

answers: NDQ_003351

answers: subducting

answers: NDQ_003352

answers: subducts

answers: NDQ_003353

answers: subducting

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: subduct

answers: NDQ_003357

answers: oceanic crust can subduct

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: subducts

answers: NDQ_003360

answers: continental crust

answers: NDQ_003362

answers: oceanic crust can subduct under continental crust

answers: NDQ_003363

answers: plate tectonics

answers: NDQ_003371

answers: Which of the following is not a type of plate tectonics?

answers: NDQ_003373

answers: What is the reason for this?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What does the theory of plate tectonics provide?

answers: NDQ_003382

answers: what is the most common stress at convergent plates?

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: Which of the following is not a type of normal fault?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip, strike-slip or strike-slip?

answers: NDQ_003389

answers: not enough information

answers: NDQ_003390

answers: subduct

answers: NDQ_003391

answers: continental crust

answers: NDQ_003392

answers: subduct

answers: NDQ_003393

answers: continental crust

answers: NDQ_003394

answers: subduct

answers: NDQ_003395

answers: subduct under continental crust

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: oceanic crust can subduct under continental crust.

answers: NDQ_003352

answers: oceanic crust can subduct under continental crust.

answers: NDQ_003353

answers: subduct under continental crust.

answers: NDQ_003354

answers: oceanic crust can subduct under continental crust.

answers: NDQ_003355

answers: ocean.

answers: NDQ_003356

answers: subduct under continental crust.

answers: NDQ_003357

answers: oceanic crust can subduct under continental crust.

answers: NDQ_003358

answers: ocean.

answers: NDQ_003359

answers: subduct under continental crust.

answers: NDQ_003360

answers: plate tectonics

answers: NDQ_003362

answers: "sea"

answers: NDQ_003363

answers: plate tectonics

answers: NDQ_003371

answers: oceanic crust can subduct under continental crust.

answers: NDQ_003373

answers: oceanic crust can subduct under continental crust.

answers: NDQ_003376

answers: oceanic crust can subduct under continental crust.

answers: NDQ_003378

answers: When the theory of plate tectonics

answers: NDQ_003379

answers: oceanic crust can subduct under continental crust.

answers: NDQ_003380

answers: ocean.

answers: NDQ_003381

answers: oceanic crust can subduct under continental crust.

answers: NDQ_003382

answers: oceanic crust can subduct under continental crust.

answers: NDQ_003383

answers: When the theory of plate tectonics

answers: NDQ_003384

answers: ocean.

answers: NDQ_003385

answers: plate tectonics

answers: NDQ_003386

answers: plate tectonics

answers: NDQ_003387

answers: When the theory of plate tectonics

answers: NDQ_003388

answers: When the theory of plate tectonics

answers: NDQ_003389

answers: oceanic crust can subduct under continental crust.

answers: NDQ_003390

answers: plate tectonics

answers: NDQ_003391

answers: oceanic crust can subduct under continental crust.

answers: NDQ_003392

answers: plate tectonics

answers: NDQ_003393

answers: oceanic crust can subduct under continental crust.

answers: NDQ_003394

answers: oceanic crust can subduct under continental crust.

answers: NDQ_003395

answers: oceanic crust can subduct under continental crust.

answers: NDQ_003396

answers: oceanic crust can subduct under continental crust.

text: When a plate of oceanic crust is subducted beneath an overriding plate of oceanic crust, as the underthrusting crust melts, it can cause upwelling of magma that can cause volcanism along the subduction front on the overridding plate. This produces an oceanic chain of volcanoes, like Japan. This volcanism causes metamorphosis of rocks, intrusions of magma that produce  rocks such as granite, and thickens the crust by depositing additional layers of rock from volcanoes. This tends to make the crust lighter and thicker, as a result making it immune to subduction.

text: When a plate of oceanic crust is subducted beneath an overriding plate of oceanic crust, as the underthrusting crust melts, it can cause upwelling of magma that can cause

text: volcanism

text: along the subduction front on the overridding plate. This produces an oceanic chain of

text: volcano

text: es, like

text: Japan

text: . This volcanism causes

text: metamorphosis

text: of

text: rocks

text: , intrusions of

text: magma

text: that produce  rocks such as granite, and thickens the crust by depositing additional layers of rock from volcanoes. This tends to make the crust lighter and thicker, as a result making it immune to subduction.

answers: NDQ_003351

answers: subduction

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: metamorphosis

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: subduction front

answers: NDQ_003356

answers: make the crust lighter

answers: NDQ_003357

answers: a plate of oceanic crust is subducted beneath an overriding plate

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: metamorphoses

answers: NDQ_003360

answers: oceanic crust

answers: NDQ_003362

answers: Japan is an oceanic chain of volcanoes

answers: NDQ_003363

answers: subduction

answers: NDQ_003371

answers: Which of the following is not a type of volcano?

answers: NDQ_003373

answers: what is the last word in the passage?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What is the result of subduction?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not a type of fold that arches upward?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: Which of the following is not the cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not a type of normal fault?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip faults or strike-slip faults?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: subduction front

answers: NDQ_003391

answers: unanswerable

answers: NDQ_003392

answers: subduction front

answers: NDQ_003393

answers: overriding plate

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: subduction front

answers: NDQ_003396

answers: subduction front

answers: NDQ_003351

answers: volcanism

answers: NDQ_003352

answers: metamorphosis

answers: NDQ_003353

answers: metamorphosis

answers: NDQ_003354

answers: When a plate of oceanic crust is subducted

answers: NDQ_003355

answers: subduction front

answers: NDQ_003356

answers: lighter and thicker,

answers: NDQ_003357

answers: subduction.

answers: NDQ_003358

answers: volcanoes,

answers: NDQ_003359

answers: subduction.

answers: NDQ_003360

answers: subduction.

answers: NDQ_003362

answers: immune to subduction.

answers: NDQ_003363

answers: When a plate of oceanic crust is subducted

answers: NDQ_003371

answers: upwelling of magma that can cause volcanism

answers: NDQ_003373

answers: metamorphosis of rocks,

answers: NDQ_003376

answers: oceanic chain of volcanoes,

answers: NDQ_003378

answers: volcanism

answers: NDQ_003379

answers: subduction front

answers: NDQ_003380

answers: metamorphosis of rocks,

answers: NDQ_003381

answers: volcanism causes metamorphosis of rocks,

answers: NDQ_003382

answers: subduction.

answers: NDQ_003383

answers: metamorphosis of rocks,

answers: NDQ_003384

answers: oceanic chain of volcanoes,

answers: NDQ_003385

answers: subduction front

answers: NDQ_003386

answers: volcanism

answers: NDQ_003387

answers: volcanism

answers: NDQ_003388

answers: volcanism

answers: NDQ_003389

answers: oceanic chain of volcanoes,

answers: NDQ_003390

answers: subduction.

answers: NDQ_003391

answers: granite,

answers: NDQ_003392

answers: subduction front

answers: NDQ_003393

answers: granite,

answers: NDQ_003394

answers: upwelling of magma that can cause volcanism

answers: NDQ_003395

answers: subduction front

answers: NDQ_003396

answers: subduction front

text: The Sumozero-Kenozero greenstone belt displays fragments of unsubductable oceanic crust, represented by the lower mafic-ultramafic volcanic sequence, and also displays the products of subduction-related magmatism. This implies that the  thick plume-derived oceanic crust reached an intraoceanic convergent plate boundary and was intruded and overlain by felsic melts coming from both a subducting slab and an overlying mantle wedge. Later, the oceanic plateau, together with the volcanic arc complex built on top of it, were accreted to and obducted onto the continental crust of the Vodla block. (Hofmann et al., 1999)

text: The Sumozero-Kenozero greenstone belt displays fragments of unsubductable oceanic

text: crust

text: , represented by the lower mafic-ultramafic volcanic sequence, and also displays the products of subduction-related

text: magma

text: tism. This implies that the  thick plume-derived oceanic

text: crust

text: reached an intraoceanic

text: convergent plate boundary

text: and was intruded and overlain by felsic melts coming from both a subducting

text: slab

text: and an overlying mantle wedge. Later, the oceanic

text: plateau

text: , together with the volcanic arc complex built on top of it, were

text: accreted

text: to and obducted onto the continental crust of the Vodla block. (Hofmann et al., 1999)

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: subducts

answers: NDQ_003353

answers: subduction

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: plate boundary

answers: NDQ_003356

answers: subduct

answers: NDQ_003357

answers: subducting slab and an overlying mantle wedge

answers: NDQ_003358

answers: plate boundary

answers: NDQ_003359

answers: unsubductable

answers: NDQ_003360

answers: continental crust

answers: NDQ_003362

answers: unsubductable oceanic crust

answers: NDQ_003363

answers: Subduction

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: What is the main idea of this passage?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: What is the amount the ground moves in an earthquake?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What type of rock deforms?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: subduction-related magmatism

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: normal faults, subduction, or magmatism?

answers: NDQ_003388

answers: Which of the following is not a type of strike-slip fault: strike-slip, strike-slip, or strike-slip?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: subducting slab

answers: NDQ_003391

answers: Vodla block

answers: NDQ_003392

answers: subducting slab

answers: NDQ_003393

answers: Vodla block

answers: NDQ_003394

answers: subducting slab

answers: NDQ_003395

answers: convergent plate boundary

answers: NDQ_003396

answers: subducting slab

answers: NDQ_003351

answers: felsic melts

answers: NDQ_003352

answers: subduction-related magmatism.

answers: NDQ_003353

answers: magmatism.

answers: NDQ_003354

answers: The Sumozero-Kenozero greenstone belt

answers: NDQ_003355

answers: wedge.

answers: NDQ_003356

answers: subduction-related magmatism.

answers: NDQ_003357

answers: subducting slab and an overlying mantle wedge.

answers: NDQ_003358

answers: unsubductable

answers: NDQ_003359

answers: unsubductable

answers: NDQ_003360

answers: subduction-related magmatism.

answers: NDQ_003362

answers: unsubductable

answers: NDQ_003363

answers: intraoceanic convergent plate boundary

answers: NDQ_003371

answers: subducting slab and an overlying mantle wedge.

answers: NDQ_003373

answers: subduction-related magmatism.

answers: NDQ_003376

answers: subduction-related magmatism.

answers: NDQ_003378

answers: subduction-related magmatism.

answers: NDQ_003379

answers: subduction-related magmatism.

answers: NDQ_003380

answers: subduction-related magmatism.

answers: NDQ_003381

answers: subduction-related magmatism.

answers: NDQ_003382

answers: subduction-related magmatism.

answers: NDQ_003383

answers: subduction-related magmatism.

answers: NDQ_003384

answers: volcanic arc

answers: NDQ_003385

answers: convergent plate boundary

answers: NDQ_003386

answers: subduction-related magmatism.

answers: NDQ_003387

answers: subduction-related magmatism.

answers: NDQ_003388

answers: subduction-related magmatism.

answers: NDQ_003389

answers: subduction-related magmatism.

answers: NDQ_003390

answers: subduction-related magmatism.

answers: NDQ_003391

answers: Vodla block.

answers: NDQ_003392

answers: convergent plate boundary

answers: NDQ_003393

answers: Vodla block.

answers: NDQ_003394

answers: convergent plate boundary

answers: NDQ_003395

answers: convergent plate boundary

answers: NDQ_003396

answers: convergent plate boundary

text: Reluctantly, believing that any other similarly senescent star will offer no better option, the people accede to the new captain's order to land on Earth despite the lack of an atmosphere. However, this is not a haphazard decision by the new captain, who is an astrophysicist. He is convinced that there is a remnant atmosphere frozen on the dark side, and uses the ship's drive to begin to re-spin Earth. (The drive really is powerful enough to achieve this within a reasonable timescale, if only the planet's crust can withstand the seismic stresses without catastrophic earthquakes.) This will, he hopes, convert this frozen gas back to a breathable atmosphere.

text: Reluctantly, believing that any other similarly senescent star will offer no better option, the people accede to the new captain's order to land on Earth despite the lack of an atmosphere. However, this is not a haphazard decision by the new captain, who is an astrophysicist. He is convinced that there is a remnant atmosphere frozen on the dark side, and uses the ship's drive to begin to re-spin Earth. (The drive really is powerful enough to achieve this within a reasonable timescale, if only the planet's crust can withstand the seismic stresses without catastrophic earthquakes.) This will, he hopes, convert this frozen gas back to a breathable atmosphere.

answers: NDQ_003351

answers: seismic

answers: NDQ_003352

answers: more likely to crack

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: catastrophic earthquakes

answers: NDQ_003357

answers: Earth can withstand the seismic stresses without catastrophic earthquakes.

answers: NDQ_003358

answers: earthquake

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth

answers: NDQ_003362

answers: catastrophic earthquakes

answers: NDQ_003363

answers: unanswerable

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: None of the above choices.

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: What will the new captain hope to convert?

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What will the new captain hope to convert?

answers: NDQ_003381

answers: What will the new captain hope to convert?

answers: NDQ_003382

answers: what is the most common stress at convergent plates

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: normal faults, earthquakes, or gas?

answers: NDQ_003388

answers: What will the new captain hope to convert this frozen gas back to a breathable atmosphere?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: earthquakes

answers: NDQ_003391

answers: Earth's crust

answers: NDQ_003392

answers: earthquakes

answers: NDQ_003393

answers: Earth's crust

answers: NDQ_003394

answers: earthquakes

answers: NDQ_003395

answers: earthquakes

answers: NDQ_003396

answers: earthquakes

answers: NDQ_003351

answers: earthquakes.)

answers: NDQ_003352

answers: earthquakes.)

answers: NDQ_003353

answers: earthquakes.)

answers: NDQ_003354

answers: earthquakes.)

answers: NDQ_003355

answers: earthquakes.)

answers: NDQ_003356

answers: earthquakes.)

answers: NDQ_003357

answers: catastrophic earthquakes.)

answers: NDQ_003358

answers: earthquakes.)

answers: NDQ_003359

answers: seismic stresses

answers: NDQ_003360

answers: Earth

answers: NDQ_003362

answers: catastrophic earthquakes.)

answers: NDQ_003363

answers: Earth

answers: NDQ_003371

answers: earthquakes.)

answers: NDQ_003373

answers: seismic stresses

answers: NDQ_003376

answers: seismic stresses without catastrophic earthquakes.)

answers: NDQ_003378

answers: seismic stresses

answers: NDQ_003379

answers: earthquakes.)

answers: NDQ_003380

answers: seismic stresses

answers: NDQ_003381

answers: earthquakes.)

answers: NDQ_003382

answers: seismic stresses

answers: NDQ_003383

answers: seismic stresses without catastrophic earthquakes.)

answers: NDQ_003384

answers: earthquakes.)

answers: NDQ_003385

answers: earthquakes.)

answers: NDQ_003386

answers: seismic stresses

answers: NDQ_003387

answers: seismic stresses

answers: NDQ_003388

answers: seismic stresses

answers: NDQ_003389

answers: planet's crust can withstand the seismic stresses without catastrophic earthquakes.)

answers: NDQ_003390

answers: earthquakes.)

answers: NDQ_003391

answers: earthquakes.)

answers: NDQ_003392

answers: earthquakes.)

answers: NDQ_003393

answers: earthquakes.)

answers: NDQ_003394

answers: earthquakes.)

answers: NDQ_003395

answers: earthquakes.)

answers: NDQ_003396

answers: earthquakes.)

text: When copulation is achieved, a male implements a coercive mating strategy known as caudocephalic waving.  The male garter snake strikes his own body against the female in quick repeated intervals.  These strikes drive anoxic air from the non-respiratory lung of the female into her respiratory lungs, causing an increase in her stress level. The increase in stress level causes cloacal gaping, allowing for the courting male to more easily insert his reproductive organ into the female.

text: When copulation is achieved, a male implements a coercive mating strategy known as caudocephalic waving.  The male garter snake strikes his own body against the female in quick repeated intervals.  These strikes drive anoxic air from the non-respiratory lung of the female into her respiratory lungs, causing an increase in her stress level. The increase in stress level causes cloacal gaping, allowing for the courting male to more easily insert his reproductive organ into the female.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: is more likely to crack

answers: NDQ_003353

answers: cloacal gaping

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: caudocephalic

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: male garter snake strikes his own body against the female

answers: NDQ_003358

answers: rockfall

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's surface

answers: NDQ_003362

answers: a male garter snake strikes his own body against the female

answers: NDQ_003363

answers: the same time

answers: NDQ_003371

answers: Which of the following is not an example of a thrust fault?

answers: NDQ_003373

answers: How would you describe a rock under compressive stresses?

answers: NDQ_003376

answers: Which of the following is not a cause of basin-and-range terrain?

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What does the male garter snake strike his own body against?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: Which of the following is not a type of fold that arches upward?

answers: NDQ_003385

answers: Which of the following is not an example of a fault zone?

answers: NDQ_003386

answers: Which of the following is not a cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not a cause of normal faults?

answers: NDQ_003388

answers: Which of the following is not a result of shear stress: strike-slip faults or strike-slip faults?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: caudocephalic

answers: NDQ_003391

answers: dip-slip fault plane

answers: NDQ_003392

answers: caudocephalic

answers: NDQ_003393

answers: dip-slip fault plane

answers: NDQ_003394

answers: isobath

answers: NDQ_003395

answers: is a fault

answers: NDQ_003396

answers: NDQ_003351

answers: cloacal gaping,

answers: NDQ_003352

answers: cloacal gaping,

answers: NDQ_003353

answers: cloacal gaping,

answers: NDQ_003354

answers: caudocephalic waving.

answers: NDQ_003355

answers: cloacal gaping,

answers: NDQ_003356

answers: cloacal gaping,

answers: NDQ_003357

answers: cloacal gaping,

answers: NDQ_003358

answers: caudocephalic waving.

answers: NDQ_003359

answers: caudocephalic waving.

answers: NDQ_003360

answers: When copulation

answers: NDQ_003362

answers: caudocephalic waving.

answers: NDQ_003363

answers: caudocephalic waving.

answers: NDQ_003371

answers: caudocephalic waving.

answers: NDQ_003373

answers: When copulation

answers: NDQ_003376

answers: caudocephalic waving.

answers: NDQ_003378

answers: caudocephalic waving.

answers: NDQ_003379

answers: caudocephalic waving.

answers: NDQ_003380

answers: stress level.

answers: NDQ_003381

answers: cloacal gaping,

answers: NDQ_003382

answers: female into her respiratory lungs,

answers: NDQ_003383

answers: cloacal gaping,

answers: NDQ_003384

answers: caudocephalic waving.

answers: NDQ_003385

answers: caudocephalic waving.

answers: NDQ_003386

answers: caudocephalic waving.

answers: NDQ_003387

answers: cloacal gaping,

answers: NDQ_003388

answers: cloacal gaping,

answers: NDQ_003389

answers: caudocephalic waving.

answers: NDQ_003390

answers: caudocephalic waving.

answers: NDQ_003391

answers: caudocephalic waving.

answers: NDQ_003392

answers: caudocephalic waving.

answers: NDQ_003393

answers: caudocephalic waving.

answers: NDQ_003394

answers: caudocephalic waving.

answers: NDQ_003395

answers: caudocephalic waving.

answers: NDQ_003396

answers: caudocephalic waving.

text: O’Rourke is a Geotechnical engineer and a subject-matter expert on natural disasters and their impact on the infrastructure supporting civil society.  Geotechnical engineers study the Earth’s near-surface crust and its performance under stress. They analyze how structures buried in the ground behave in an environment of change, structures such as subway systems, water and gas pipelines, etc. They, for instance, study underground spaces such as parking garages, skyscraper foundations and subfloors and they also evaluate how structures made of soil and/or rock behave, structures such as earth dams, highway embankments, and levies.  O’Rourke served on the National Academy of Engineering (NAE) team studying Hurricane Katrina and its effect on the Gulf Coast.  Funded in part by the Charles L. Crandall Fund, O’Rourke reviewed the Armenia earthquake (1988), the Kobe, Japan earthquake (1995), and the Kocaeli, Turkey earthquake (1999).  A specialist in geotechnical engineering including foundations, earth retaining structures, slope stability, soil/structure interaction, underground construction, laboratory testing, and elements of earthquake engineering, O’Rourke has written extensively on geotechnical, underground, and earthquake engineering. O'Rourke was an early specialist in the field of monitoring large construction projects.

text: O’Rourke is a

text: Geotechnical engineer

text: and a subject-matter expert on natural disasters and their impact on the infrastructure supporting civil society.

text: Geotechnical

text: engineers study the Earth’s near-surface crust and its performance under stress. They analyze how structures buried in the ground behave in an environment of change, structures such as subway systems, water and gas pipelines, etc. They, for instance, study underground spaces such as parking garages, skyscraper foundations and subfloors and they also evaluate how structures made of soil and/or rock behave, structures such as earth dams, highway embankments, and levies.  O’Rourke served on the

text: National Academy of Engineering

text: (NAE) team studying

text: Hurricane Katrina

text: and its effect on the Gulf Coast.  Funded in part by the Charles L. Crandall Fund, O’Rourke reviewed the

text: Armenia

text: earthquake (1988), the Kobe, Japan earthquake (1995), and the Kocaeli, Turkey earthquake (1999).  A specialist in

text: geotechnical engineering

text: including foundations, earth retaining structures, slope stability, soil/structure interaction, underground construction, laboratory testing, and elements of earthquake engineering, O’Rourke has written extensively on geotechnical, underground, and earthquake engineering. O'Rourke was an early specialist in the field of monitoring large construction projects.

answers: NDQ_003351

answers: slope stability

answers: NDQ_003352

answers: is more likely to crack

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: slope

answers: NDQ_003356

answers: collapse

answers: NDQ_003357

answers: Earth dams, highway embankments, and levies

answers: NDQ_003358

answers: earth dam

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's near-surface crust

answers: NDQ_003362

answers: buried in the ground behave in an environment of change

answers: NDQ_003363

answers: Earth's near-surface crust

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: structures such as subway systems

answers: NDQ_003376

answers: what is the last word in the passage?

answers: NDQ_003378

answers: what is the last word in the passage?

answers: NDQ_003379

answers: strike-slip fault

answers: NDQ_003380

answers: What is a stress?

answers: NDQ_003381

answers: What does O'Rourke study?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: fault zone

answers: NDQ_003386

answers: earthquakes

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: Armenia earthquake (1988), the Kobe, Japan earthquake (1995), and the Kocaeli, Turkey earthquake (1999)

answers: NDQ_003388

answers: Which of the following is not a type of earthquake: strike-slip faults or earthquake engineering?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: slope stability

answers: NDQ_003391

answers: earth dams

answers: NDQ_003392

answers: slope stability

answers: NDQ_003393

answers: earth dams

answers: NDQ_003394

answers: slope

answers: NDQ_003395

answers: Kobe, Japan earthquake

answers: NDQ_003396

answers: slope stability

answers: NDQ_003351

answers: earthquake

answers: NDQ_003352

answers: earth dams, highway embankments, and levies.

answers: NDQ_003353

answers: earth dams, highway embankments, and levies.

answers: NDQ_003354

answers: O’Rourke

answers: NDQ_003355

answers: slope

answers: NDQ_003356

answers: slope stability,

answers: NDQ_003357

answers: slope stability,

answers: NDQ_003358

answers: earth dams,

answers: NDQ_003359

answers: stress.

answers: NDQ_003360

answers: Earth’s near-surface crust

answers: NDQ_003362

answers: Hurricane Katrina

answers: NDQ_003363

answers: Earth’s near-surface crust

answers: NDQ_003371

answers: Geotechnical engineers

answers: NDQ_003373

answers: earth dams, highway embankments, and levies.

answers: NDQ_003376

answers: earth dams, highway embankments, and levies.

answers: NDQ_003378

answers: slope stability,

answers: NDQ_003379

answers: slope stability,

answers: NDQ_003380

answers: stress.

answers: NDQ_003381

answers: earth dams, highway embankments, and levies.

answers: NDQ_003382

answers: Armenia earthquake (1988), the Kobe, Japan earthquake (1995),

answers: NDQ_003383

answers: earth dams, highway embankments, and levies.

answers: NDQ_003384

answers: slope stability,

answers: NDQ_003385

answers: Geotechnical engineers

answers: NDQ_003386

answers: earth dams, highway embankments, and levies.

answers: NDQ_003387

answers: earthquake engineering,

answers: NDQ_003388

answers: Geotechnical engineers

answers: NDQ_003389

answers: earth dams, highway embankments, and levies.

answers: NDQ_003390

answers: slope stability,

answers: NDQ_003391

answers: earth dams,

answers: NDQ_003392

answers: slope stability,

answers: NDQ_003393

answers: earth dams,

answers: NDQ_003394

answers: slope stability,

answers: NDQ_003395

answers: slope stability,

answers: NDQ_003396

answers: slope stability,

text: When a strike-slip fault is offset along strike such as to create a gap i.e. a left-stepping bend on a sinistral fault, a zone of extension or transtension is generated. Such bends are known as releasing bends or extensional stepovers and often form pull-apart basins or rhombochasms. Examples of active pull-apart basins include the Dead Sea, formed at a left-stepping offset of the sinistral sense Dead Sea Transform system, and the Sea of Marmara, formed at a right-stepping offset on the dextral sense North Anatolian Fault system.

text: When a

text: strike-slip fault

text: is offset along strike such as to create a gap i.e. a left-stepping bend on a sinistral fault, a zone of extension or

text: transtension

text: is generated. Such bends are known as releasing bends or extensional stepovers and often form

text: pull-apart basin

text: s or rhombochasms. Examples of active pull-apart basins include the

text: Dead Sea

text: , formed at a left-stepping offset of the sinistral sense

text: Dead Sea Transform

text: system, and the

text: Sea of Marmara

text: , formed at a right-stepping offset on the dextral sense

text: North Anatolian Fault

text: system.

answers: NDQ_003351

answers: transtension

answers: NDQ_003352

answers: pulls apart

answers: NDQ_003353

answers: transtension

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: releasing bends

answers: NDQ_003356

answers: pull apart

answers: NDQ_003357

answers: zone of extension or transtension is generated

answers: NDQ_003358

answers: dextral sense

answers: NDQ_003359

answers: strike-slip

answers: NDQ_003360

answers: strike-slip faults

answers: NDQ_003362

answers: Dead Sea Transform system

answers: NDQ_003363

answers: strike-slip faults

answers: NDQ_003371

answers: Which of the following is not a type of fault: strike-slip fault, dextral sense North Anatolian Fault system, or thrust fault?

answers: NDQ_003373

answers: None of the above choices are true

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: no

answers: NDQ_003380

answers: What is a zone of extension or transtension generated?

answers: NDQ_003381

answers: What is a zone of extension or transtension generated?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: unanswerable

answers: NDQ_003386

answers: what is the cause of earthquakes

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: unanswerable

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: strike-slip fault

answers: NDQ_003391

answers: dextral sense

answers: NDQ_003392

answers: strike-slip fault

answers: NDQ_003393

answers: dextral sense

answers: NDQ_003394

answers: sinistral fault

answers: NDQ_003395

answers: sinistral

answers: NDQ_003396

answers: sinistral fault

answers: NDQ_003351

answers: extension or transtension

answers: NDQ_003352

answers: extension or transtension

answers: NDQ_003353

answers: extension or transtension

answers: NDQ_003354

answers: Dead Sea,

answers: NDQ_003355

answers: releasing bends

answers: NDQ_003356

answers: pull-apart basins or rhombochasms.

answers: NDQ_003357

answers: a zone of extension or transtension

answers: NDQ_003358

answers: pull-apart basins or rhombochasms.

answers: NDQ_003359

answers: offset along strike

answers: NDQ_003360

answers: strike-slip fault

answers: NDQ_003362

answers: create a gap

answers: NDQ_003363

answers: strike-slip fault

answers: NDQ_003371

answers: strike-slip fault

answers: NDQ_003373

answers: extension or transtension

answers: NDQ_003376

answers: pull-apart basins or rhombochasms.

answers: NDQ_003378

answers: strike-slip

answers: NDQ_003379

answers: left-stepping bend on a sinistral

answers: NDQ_003380

answers: extension or transtension

answers: NDQ_003381

answers: releasing bends

answers: NDQ_003382

answers: extension or transtension

answers: NDQ_003383

answers: extension or transtension

answers: NDQ_003384

answers: sinistral fault,

answers: NDQ_003385

answers: zone of extension or transtension

answers: NDQ_003386

answers: When a strike-slip

answers: NDQ_003387

answers: extension or transtension

answers: NDQ_003388

answers: extension or transtension

answers: NDQ_003389

answers: pull-apart basins or rhombochasms.

answers: NDQ_003390

answers: strike-slip

answers: NDQ_003391

answers: extension or transtension

answers: NDQ_003392

answers: strike-slip

answers: NDQ_003393

answers: sinistral fault, a zone of extension or transtension

answers: NDQ_003394

answers: sinistral

answers: NDQ_003395

answers: sinistral

answers: NDQ_003396

answers: sinistral

text: The main features of passive margins lie underneath the external characters. Beneath passive margins the transition between the continental and oceanic crust is a broad transition known as transitional crust. The subsided continental crust is marked by normal faults that dip seaward. The faulted crust transitions into oceanic crust and may be deeply buried due to thermal subsidence and the mass of sediment that collects above it. The lithosphere beneath passive margins is known as transitional lithosphere. The lithosphere thins seaward as it transitions seaward to oceanic crust. Different kinds of transitional crust form, depending on how fast rifting occurs and how hot the underlying mantle was at the time of rifting. Volcanic passive margins represent one endmember transitional crust type, the other endmember (amagmatic) type is the rifted passive margin. Volcanic passive margins they also are marked by numerous dykes and igneous intrusions within the subsided continental crust. There are typically a lot of dykes formed perpendicular to the seaward-dipping lava flows and sills. Igneous intrusions within the crust cause lava flows along the top the subsided continental crust and form seaward-dipping reflectors.

text: The main features of passive margins lie underneath the external characters. Beneath passive margins the transition between the continental and oceanic crust is a broad transition known as transitional crust. The subsided continental crust is marked by

text: normal fault

text: s that dip seaward. The faulted crust transitions into oceanic crust and may be deeply buried due to

text: thermal subsidence

text: and the mass of sediment that collects above it. The

text: lithosphere

text: beneath passive margins is known as transitional lithosphere. The lithosphere thins seaward as it transitions seaward to oceanic crust. Different kinds of transitional crust form, depending on how fast rifting occurs and how hot the underlying mantle was at the time of rifting. Volcanic passive margins represent one endmember transitional crust type, the other endmember (amagmatic) type is the rifted passive margin. Volcanic passive margins they also are marked by numerous

text: dykes

text: and

text: igneous intrusions

text: within the subsided continental crust. There are typically a lot of dykes formed perpendicular to the seaward-dipping lava flows and sills. Igneous intrusions within the crust cause lava flows along the top the subsided continental crust and form seaward-dipping reflectors.

answers: NDQ_003351

answers: normal faults

answers: NDQ_003352

answers: erodes more

answers: NDQ_003353

answers: normal faults

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: fault

answers: NDQ_003356

answers: subsided

answers: NDQ_003357

answers: The lithosphere thins seaward as it transitions seaward to oceanic crust

answers: NDQ_003358

answers: passive margin

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: passive margins

answers: NDQ_003362

answers: normal faults that dip seaward

answers: NDQ_003363

answers: passive margins

answers: NDQ_003371

answers: Which of the following is not a type of endmember transitional crust?

answers: NDQ_003373

answers: Which of the following is not a cause of thermal subsidence?

answers: NDQ_003376

answers: Which of the following is not caused by compressive forces?

answers: NDQ_003378

answers: What is the mass of sediment that collects above it?

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: Which of the following is not a type of crust: normal faults, igneous intrusions, or rifted?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not a type of fold?

answers: NDQ_003385

answers: Which of the following is not a type of transitional crust?

answers: NDQ_003386

answers: Which of the following is not a cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not a cause of normal faults: compression stress or thermal subsidence?

answers: NDQ_003388

answers: Which of the following is not a type of strike-slip fault?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: normal faults

answers: NDQ_003391

answers: Subsided continental crust

answers: NDQ_003392

answers: dykes

answers: NDQ_003393

answers: Subsided continental crust

answers: NDQ_003394

answers: dip seaward

answers: NDQ_003395

answers: normal faults

answers: NDQ_003396

answers: Volcanic passive margins

answers: NDQ_003351

answers: normal faults

answers: NDQ_003352

answers: deeply buried

answers: NDQ_003353

answers: faults

answers: NDQ_003354

answers: The main features of passive margins lie underneath the external characters.

answers: NDQ_003355

answers: faults

answers: NDQ_003356

answers: deeply buried

answers: NDQ_003357

answers: dip seaward.

answers: NDQ_003358

answers: passive margins

answers: NDQ_003359

answers: faults that dip seaward.

answers: NDQ_003360

answers: faults

answers: NDQ_003362

answers: deeply buried

answers: NDQ_003363

answers: Volcanic passive margins

answers: NDQ_003371

answers: normal faults

answers: NDQ_003373

answers: thermal subsidence

answers: NDQ_003376

answers: normal faults that dip seaward.

answers: NDQ_003378

answers: subsidence

answers: NDQ_003379

answers: seaward.

answers: NDQ_003380

answers: faults that dip seaward.

answers: NDQ_003381

answers: thermal subsidence

answers: NDQ_003382

answers: normal faults that dip seaward.

answers: NDQ_003383

answers: faults

answers: NDQ_003384

answers: faults that dip seaward.

answers: NDQ_003385

answers: faults that dip seaward.

answers: NDQ_003386

answers: faults that dip seaward.

answers: NDQ_003387

answers: normal faults that dip seaward.

answers: NDQ_003388

answers: normal faults

answers: NDQ_003389

answers: rifting.

answers: NDQ_003390

answers: normal faults

answers: NDQ_003391

answers: transitional lithosphere.

answers: NDQ_003392

answers: normal faults

answers: NDQ_003393

answers: transitional lithosphere.

answers: NDQ_003394

answers: faults

answers: NDQ_003395

answers: normal faults that dip seaward.

answers: NDQ_003396

answers: rifted passive margin.

text: Another way bays form is via glacial and river erosion. A bay formed by a glacier is a fjord. Rias are created by rivers and are characterised by more gradual slopes. Most gulf and bays form by the folding of the earth's crust, and by coastal erosion due to waves and currents. Currents can make waves more constant, and soft rocks speed erosion. Hard rock eroded less quickly, leaving headlands. The Gulf of California is an example of a bay created by the geological process of folding.

text: Another way bays form is via glacial and river erosion. A bay formed by a glacier is a

text: fjord

text: Ria

text: s are created by rivers and are characterised by more gradual slopes. Most gulf and bays form by the

text: folding

text: of the earth's

text: crust

text: , and by coastal erosion due to

text: waves

text: and

text: currents

text: . Currents can make waves more constant, and soft rocks speed erosion. Hard rock eroded less quickly, leaving

text: headland

text: s. The

text: Gulf of California

text: is an example of a bay created by the geological process of folding.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: erodes more quickly

answers: NDQ_003353

answers: erosion

answers: NDQ_003354

answers: Toroweap Formation is a soft rock

answers: NDQ_003355

answers: Rias

answers: NDQ_003356

answers: speed up erosion

answers: NDQ_003357

answers: Hard rock eroded less quickly, leaving headlands.

answers: NDQ_003358

answers: headlands

answers: NDQ_003359

answers: hard rock eroded less quickly

answers: NDQ_003360

answers: glaciers

answers: NDQ_003362

answers: Hard rock eroded less quickly, leaving headlands.

answers: NDQ_003363

answers: glacial and river erosion

answers: NDQ_003371

answers: Which of the following is not an example of a bay created by the geological process of folding?

answers: NDQ_003373

answers: Which of the following is not an example of a geological process of folding?

answers: NDQ_003376

answers: Which of the following is not an example of a bay created by the geological process of folding?

answers: NDQ_003378

answers: What is the term for the amount the ground moves in an earthquake?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: Which of the following is not a type of erosion: glacial or river?

answers: NDQ_003381

answers: Which of the following is not an example of the geological process of folding?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not an example of a bay created by the folding of the earth's crust?

answers: NDQ_003385

answers: Which of the following is not an example of a fault zone?

answers: NDQ_003386

answers: Which of the following is not a cause of earthquakes: folding of the earth's crust, waves and currents, or movement of rock at faults?

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: folding of the earth's crust, waves, or currents?

answers: NDQ_003388

answers: Which of the following is not an example of a strike-slip fault?

answers: NDQ_003389

answers: It's impossible to say

answers: NDQ_003390

answers: Rias

answers: NDQ_003391

answers: hard rock

answers: NDQ_003392

answers: Rias

answers: NDQ_003393

answers: hard rock

answers: NDQ_003394

answers: Rias

answers: NDQ_003395

answers: a fault with a vertical fault plane

answers: NDQ_003396

answers: Rias

answers: NDQ_003351

answers: waves and currents.

answers: NDQ_003352

answers: Hard rock eroded less quickly,

answers: NDQ_003353

answers: soft rocks

answers: NDQ_003354

answers: The Gulf of California

answers: NDQ_003355

answers: Rias

answers: NDQ_003356

answers: soft rocks speed erosion.

answers: NDQ_003357

answers: Hard rock

answers: NDQ_003358

answers: headlands.

answers: NDQ_003359

answers: Hard rock eroded less quickly,

answers: NDQ_003360

answers: folding of the earth's crust,

answers: NDQ_003362

answers: a glacier

answers: NDQ_003363

answers: folding of the earth's crust,

answers: NDQ_003371

answers: folding of the earth's crust,

answers: NDQ_003373

answers: Hard rock eroded less quickly,

answers: NDQ_003376

answers: folding of the earth's crust,

answers: NDQ_003378

answers: folding of the earth's crust,

answers: NDQ_003379

answers: gradual slopes.

answers: NDQ_003380

answers: soft rocks speed erosion.

answers: NDQ_003381

answers: folding of the earth's crust,

answers: NDQ_003382

answers: folding of the earth's crust,

answers: NDQ_003383

answers: Hard rock eroded less quickly, leaving headlands.

answers: NDQ_003384

answers: folding of the earth's crust,

answers: NDQ_003385

answers: fjord.

answers: NDQ_003386

answers: folding of the earth's crust,

answers: NDQ_003387

answers: folding of the earth's crust,

answers: NDQ_003388

answers: folding of the earth's crust,

answers: NDQ_003389

answers: folding of the earth's crust,

answers: NDQ_003390

answers: fjord.

answers: NDQ_003391

answers: Hard rock eroded less quickly, leaving headlands.

answers: NDQ_003392

answers: fjord.

answers: NDQ_003393

answers: headlands.

answers: NDQ_003394

answers: fjord.

answers: NDQ_003395

answers: folding of the earth's crust,

answers: NDQ_003396

answers: fjord.

text: Lake Hughes is generally centered on the intersection of Elizabeth Lake Road and Lake Hughes Road, both of which are county highways. Hughes Lake and Munz Lakes are located within the community. In addition, a third lake, Lake Elizabeth is located just to the east within the community of Elizabeth Lake.  Lakes Hughes and Lake Elizabeth are in the canyons along the San Andreas Fault. Both lakes periodically dry up depending on rainfall cycles. Lake Hughes was previously known as West Elizabeth Lake.

text: Lake Hughes is generally centered on the intersection of Elizabeth Lake Road and Lake Hughes Road, both of which are county highways. Hughes Lake and Munz Lakes are located within the community. In addition, a third lake,

entity_name: Elizabeth Lake (Los Angeles County, California)

text: Lake Elizabeth

text: is located just to the east within the community of Elizabeth Lake.  Lakes Hughes and Lake Elizabeth are in the canyons along the

text: San Andreas Fault

text: . Both lakes periodically dry up depending on rainfall cycles. Lake Hughes was previously known as West Elizabeth Lake.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: dry up

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: canyon

answers: NDQ_003356

answers: dry up

answers: NDQ_003357

answers: Lake Hughes and Lake Elizabeth are in the canyons along what fault?

answers: NDQ_003358

answers: canyon

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: San Andreas fault

answers: NDQ_003362

answers: Lake Hughes was previously known as West Elizabeth Lake.

answers: NDQ_003363

answers: San Andreas Fault

answers: NDQ_003371

answers: Which of the following is not a type of fault: San Andreas Fault, Hughes Lake or Munz Lake?

answers: NDQ_003373

answers: How would you describe Hughes Lake?

answers: NDQ_003376

answers: Which of the following is not a type of terrain: basin-and-range or mountain?

answers: NDQ_003378

answers: what is the first lake mentioned?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What type of stress does Lake Hughes and Lake Elizabeth experience?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: How would you describe Lake Hughes?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: The San Andreas Fault

answers: NDQ_003387

answers: Which of the following is not a normal fault: San Andreas Fault, Hughes Lake or Munz Lake?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip, strike-slip, or strike-slip?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: San Andreas Fault

answers: NDQ_003391

answers: Lake Elizabeth

answers: NDQ_003392

answers: San Andreas Fault

answers: NDQ_003393

answers: Lake Elizabeth

answers: NDQ_003394

answers: San Andreas Fault

answers: NDQ_003395

answers: San Andreas Fault

answers: NDQ_003396

answers: San Andreas Fault

answers: NDQ_003351

answers: San Andreas Fault.

answers: NDQ_003352

answers: dry up

answers: NDQ_003353

answers: San Andreas Fault.

answers: NDQ_003354

answers: San Andreas Fault.

answers: NDQ_003355

answers: canyons

answers: NDQ_003356

answers: dry up

answers: NDQ_003357

answers: San Andreas Fault.

answers: NDQ_003358

answers: canyons

answers: NDQ_003359

answers: San Andreas Fault.

answers: NDQ_003360

answers: San Andreas Fault.

answers: NDQ_003362

answers: Both lakes periodically dry up depending on rainfall cycles.

answers: NDQ_003363

answers: San Andreas Fault.

answers: NDQ_003371

answers: San Andreas Fault.

answers: NDQ_003373

answers: San Andreas Fault.

answers: NDQ_003376

answers: San Andreas Fault.

answers: NDQ_003378

answers: San Andreas Fault.

answers: NDQ_003379

answers: San Andreas Fault.

answers: NDQ_003380

answers: San Andreas Fault.

answers: NDQ_003381

answers: San Andreas Fault.

answers: NDQ_003382

answers: San Andreas Fault.

answers: NDQ_003383

answers: San Andreas Fault.

answers: NDQ_003384

answers: San Andreas Fault.

answers: NDQ_003385

answers: San Andreas Fault.

answers: NDQ_003386

answers: San Andreas Fault.

answers: NDQ_003387

answers: San Andreas Fault.

answers: NDQ_003388

answers: San Andreas Fault.

answers: NDQ_003389

answers: San Andreas Fault.

answers: NDQ_003390

answers: San Andreas Fault.

answers: NDQ_003391

answers: San Andreas Fault.

answers: NDQ_003392

answers: San Andreas Fault.

answers: NDQ_003393

answers: San Andreas Fault.

answers: NDQ_003394

answers: San Andreas Fault.

answers: NDQ_003395

answers: San Andreas Fault.

answers: NDQ_003396

answers: San Andreas Fault.

text: Seven pairs of hotspots and LIPs located on opposite sides of the earth have been noted; analyses indicate this coincident antipodal location is highly unlikely to be random. The hotspot pairs include a large igneous province with continental volcanism opposite an oceanic hotspot. Oceanic impacts of large meteorites are expected to have high efficiency in converting energy into seismic waves. These waves would propagate around the world and reconverge close to the antipodal position; small variations are expected as the seismic velocity varies depending upon the route characteristics along which the waves propagate. As the waves focus on the antipodal position, they put the crust at the focal point under significant stress and are proposed to rupture it, creating antipodal pairs. When the meteorite impacts a continent, the lower efficiency of kinetic energy conversion into seismic energy is not expected to create an antipodal hotspot.

text: Seven pairs of hotspots and LIPs located on opposite sides of the earth have been noted; analyses indicate this coincident antipodal location is highly unlikely to be random. The hotspot pairs include a large igneous province with continental volcanism opposite an oceanic hotspot. Oceanic impacts of large meteorites are expected to have high efficiency in converting energy into seismic waves. These waves would propagate around the world and reconverge close to the antipodal position; small variations are expected as the seismic velocity varies depending upon the route characteristics along which the waves propagate. As the waves focus on the antipodal position, they put the crust at the focal point under significant stress and are proposed to rupture it, creating antipodal pairs. When the meteorite impacts a continent, the lower efficiency of kinetic energy conversion into seismic energy is not expected to create an antipodal hotspot.

answers: NDQ_003351

answers: seismic

answers: NDQ_003352

answers: ruptures

answers: NDQ_003353

answers: seismic waves

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: antipodal

answers: NDQ_003356

answers: rupture

answers: NDQ_003357

answers: oceanic impacts of large meteorites are expected to have high

answers: NDQ_003358

answers: hotspot

answers: NDQ_003359

answers: is put under significant stress

answers: NDQ_003360

answers: antipodal

answers: NDQ_003362

answers: oceanic impacts of large meteorites are expected to have high efficiency in converting energy into seismic

answers: NDQ_003363

answers: antipodal

answers: NDQ_003371

answers: Which of the following is not a type of thrust fault?

answers: NDQ_003373

answers: How would the waves focus on the antipodal position?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What is the main idea of the passage?

answers: NDQ_003381

answers: Which of the following is not expected to create an antipodal hotspot?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not a type of fold that arches upward?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: significant stress and are proposed to rupture it

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: oceanic impacts of large meteorites or normal faults?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip faults, LIPs, or hotspots?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: antipodal pairs

answers: NDQ_003391

answers: antipodal pairs

answers: NDQ_003392

answers: antipodal pairs

answers: NDQ_003393

answers: antipodal pairs

answers: NDQ_003394

answers: antipodal

answers: NDQ_003395

answers: antipodal pairs

answers: NDQ_003396

answers: antipodal

answers: NDQ_003351

answers: Oceanic impacts of large meteorites

answers: NDQ_003352

answers: rupture it,

answers: NDQ_003353

answers: rupture it,

answers: NDQ_003354

answers: Seven pairs of hotspots

answers: NDQ_003355

answers: antipodal

answers: NDQ_003356

answers: rupture it,

answers: NDQ_003357

answers: reconverge close to the antipodal position;

answers: NDQ_003358

answers: antipodal hotspot.

answers: NDQ_003359

answers: stress

answers: NDQ_003360

answers: continental volcanism

answers: NDQ_003362

answers: random.

answers: NDQ_003363

answers: antipodal

answers: NDQ_003371

answers: antipodal pairs.

answers: NDQ_003373

answers: crust at the focal point under significant stress

answers: NDQ_003376

answers: stress

answers: NDQ_003378

answers: seismic velocity

answers: NDQ_003379

answers: continental volcanism

answers: NDQ_003380

answers: stress

answers: NDQ_003381

answers: rupture it,

answers: NDQ_003382

answers: stress

answers: NDQ_003383

answers: rupture it, creating antipodal pairs.

answers: NDQ_003384

answers: Seven pairs of hotspots and LIPs

answers: NDQ_003385

answers: antipodal pairs.

answers: NDQ_003386

answers: they put the crust at the focal point under significant stress

answers: NDQ_003387

answers: they put the crust at the focal point under significant stress

answers: NDQ_003388

answers: they put the crust at the focal point under significant stress

answers: NDQ_003389

answers: continental volcanism

answers: NDQ_003390

answers: antipodal pairs.

answers: NDQ_003391

answers: antipodal hotspot.

answers: NDQ_003392

answers: antipodal pairs.

answers: NDQ_003393

answers: antipodal hotspot.

answers: NDQ_003394

answers: LIPs

answers: NDQ_003395

answers: continental volcanism

answers: NDQ_003396

answers: LIPs

text: Gravity data provides information about the subsurface density distribution. The most important gravity feature associated with any continent-ocean transition, including NVPM, is the free-air edge effect anomaly, which consists of a gravity high and a gravity low associated with the contrast between the thick continental and thin oceanic crust. There are also subsurface variations in density that cause significant variations across the continent-ocean transition.  The crust, as well as the entire lithosphere, is thinned due to mechanical extension. The Moho marks a large density contrast between crust and mantle, typically at least 0.35 g/cm3. The highest amplitudes of the gravity anomaly occur seaward of the continent-ocean transition. High-density upper mantle material is elevated relative to the more landward crustal root. The oceanic crust density is then further enhanced with gabbros and basalts and additionally contributes to the regional gravity trend.

text: Gravity data provides information about the subsurface density distribution. The most important

text: gravit

text: y feature associated with any

text: continent-ocean transition

text: , including NVPM, is the free-air edge effect anomaly, which consists of a gravity high and a gravity low associated with the contrast between the thick continental and thin oceanic crust. There are also subsurface variations in density that cause significant variations across the continent-ocean transition.  The crust, as well as the entire

text: lithosphere

text: , is thinned due to mechanical extension. The

text: Moho

text: marks a large density contrast between

text: crust

text: and

text: mantle

text: , typically at least 0.35 g/cm3. The highest amplitudes of the

text: gravity anomaly

text: occur seaward of the continent-ocean transition. High-density upper mantle material is elevated relative to the more landward crustal root. The oceanic crust density is then further enhanced with gabbros and basalts and additionally contributes to the regional gravity trend.

answers: NDQ_003351

answers: mechanical extension

answers: NDQ_003352

answers: thinned

answers: NDQ_003353

answers: mechanical extension

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: Moho

answers: NDQ_003356

answers: thin

answers: NDQ_003357

answers: The crust, as well as the entire lithosphere is thinned due to mechanical extension.

answers: NDQ_003358

answers: Moho

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: continental plates

answers: NDQ_003362

answers: The crust, as well as the entire lithosphere, is thinned due to mechanical extension

answers: NDQ_003363

answers: NVPM

answers: NDQ_003371

answers: What is the Moho?

answers: NDQ_003373

answers: Why is the crust thinned due to mechanical extension?

answers: NDQ_003376

answers: What is the most important gravity feature associated with any continent-ocean transition?

answers: NDQ_003378

answers: The crust, as well as the entire lithosphere is thinned due to mechanical extension

answers: NDQ_003379

answers: What is the Moho?

answers: NDQ_003380

answers: What is the Moho?

answers: NDQ_003381

answers: What is the Moho?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the Moho?

answers: NDQ_003384

answers: What is the Moho?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: What is thinned due to mechanical extension?

answers: NDQ_003387

answers: What is thinned due to mechanical extension?

answers: NDQ_003388

answers: What is the Moho?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: Moho

answers: NDQ_003391

answers: gabbros

answers: NDQ_003392

answers: Moho

answers: NDQ_003393

answers: High-density upper mantle

answers: NDQ_003394

answers: Moho

answers: NDQ_003395

answers: Moho marks a large density contrast between crust and mantle

answers: NDQ_003396

answers: Moho

answers: NDQ_003351

answers: free-air edge effect anomaly,

answers: NDQ_003352

answers: thinned

answers: NDQ_003353

answers: thinned

answers: NDQ_003354

answers: elevated relative to the more landward crustal root.

answers: NDQ_003355

answers: The Moho

answers: NDQ_003356

answers: thinned due to mechanical extension.

answers: NDQ_003357

answers: landward crustal root.

answers: NDQ_003358

answers: The Moho

answers: NDQ_003359

answers: mechanical extension.

answers: NDQ_003360

answers: mechanical extension.

answers: NDQ_003362

answers: thinned due to mechanical extension.

answers: NDQ_003363

answers: continent-ocean transition,

answers: NDQ_003371

answers: free-air edge effect anomaly,

answers: NDQ_003373

answers: mechanical extension.

answers: NDQ_003376

answers: mechanical extension.

answers: NDQ_003378

answers: extension.

answers: NDQ_003379

answers: 0.35 g/cm3.

answers: NDQ_003380

answers: mechanical extension.

answers: NDQ_003381

answers: mechanical extension.

answers: NDQ_003382

answers: mechanical extension.

answers: NDQ_003383

answers: mechanical extension.

answers: NDQ_003384

answers: free-air edge effect anomaly,

answers: NDQ_003385

answers: free-air edge effect anomaly,

answers: NDQ_003386

answers: mechanical extension.

answers: NDQ_003387

answers: mechanical extension.

answers: NDQ_003388

answers: mechanical extension.

answers: NDQ_003389

answers: mechanical extension.

answers: NDQ_003390

answers: NVPM,

answers: NDQ_003391

answers: The Moho

answers: NDQ_003392

answers: NVPM,

answers: NDQ_003393

answers: crustal root.

answers: NDQ_003394

answers: free-air edge effect anomaly,

answers: NDQ_003395

answers: The Moho

answers: NDQ_003396

answers: The Moho

text: Intraplate deformation is the folding, breaking, or flow of the Earth's crust within plates instead of at their margins. This process usually occurs in areas with especially weak crust and upper mantle, such as the Tibetan Plateau (Figure 1). Intraplate deformation brings another aspect to plate tectonic theory.

text: Intraplate deformation is the folding, breaking, or flow of the

text: Earth's crust

text: within plates instead of at their margins. This process usually occurs in areas with especially weak crust and upper

text: mantle

text: , such as the

text: Tibetan Plateau

text: (Figure 1). Intraplate deformation brings another aspect to

text: plate tectonic

text: theory.

answers: NDQ_003351

answers: Intraplate deformation

answers: NDQ_003352

answers: breaks

answers: NDQ_003353

answers: deformation

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: Tibetan Plateau

answers: NDQ_003356

answers: fold

answers: NDQ_003357

answers: intraplate deformation is the folding, breaking, or flow

answers: NDQ_003358

answers: Plateau

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: plates

answers: NDQ_003362

answers: the Tibetan Plateau

answers: NDQ_003363

answers: the Tibetan Plateau

answers: NDQ_003371

answers: Which of the following is not a type of plate tectonic theory?

answers: NDQ_003373

answers: unanswerable

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: Which of the following is not a type of deformation: folding, breaking, or flow of the Earth's crust

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: Which of the following is not a result of shear stress: strike-slip faults, intraplate deformation, or strike-slip faults?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: The Tibetan Plateau

answers: NDQ_003391

answers: Tibetan Plateau

answers: NDQ_003392

answers: The Tibetan Plateau

answers: NDQ_003393

answers: Upper mantle

answers: NDQ_003394

answers: Tibetan Plateau

answers: NDQ_003395

answers: tectonic theory

answers: NDQ_003396

answers: Tibetan Plateau

answers: NDQ_003351

answers: Intraplate deformation

answers: NDQ_003352

answers: breaking,

answers: NDQ_003353

answers: folding, breaking, or flow

answers: NDQ_003354

answers: Intraplate deformation

answers: NDQ_003355

answers: Intraplate deformation

answers: NDQ_003356

answers: breaking,

answers: NDQ_003357

answers: margins.

answers: NDQ_003358

answers: Tibetan Plateau

answers: NDQ_003359

answers: weak crust

answers: NDQ_003360

answers: Intraplate deformation

answers: NDQ_003362

answers: Intraplate deformation

answers: NDQ_003363

answers: Tibetan Plateau

answers: NDQ_003371

answers: Intraplate deformation

answers: NDQ_003373

answers: Intraplate deformation

answers: NDQ_003376

answers: Tibetan Plateau

answers: NDQ_003378

answers: Intraplate deformation

answers: NDQ_003379

answers: (Figure 1).

answers: NDQ_003380

answers: Intraplate deformation

answers: NDQ_003381

answers: Intraplate deformation

answers: NDQ_003382

answers: Intraplate deformation

answers: NDQ_003383

answers: Intraplate deformation

answers: NDQ_003384

answers: Tibetan Plateau

answers: NDQ_003385

answers: Intraplate deformation

answers: NDQ_003386

answers: Intraplate deformation

answers: NDQ_003387

answers: Intraplate deformation

answers: NDQ_003388

answers: Intraplate deformation

answers: NDQ_003389

answers: Tibetan Plateau

answers: NDQ_003390

answers: Tibetan Plateau

answers: NDQ_003391

answers: Tibetan Plateau

answers: NDQ_003392

answers: Intraplate deformation

answers: NDQ_003393

answers: Tibetan Plateau

answers: NDQ_003394

answers: Intraplate deformation

answers: NDQ_003395

answers: Intraplate deformation

answers: NDQ_003396

answers: Intraplate deformation

text: Rifting is said to have begun in the Late Cretaceous epoch to Paleogene period. At that time the African plate was experiencing far-field stresses caused by portions of the northern boundary of the African plate subducting under the Eurasian plate. Today, the Arabian plate is experiencing a crustal down pull, or slab pull, that has separated from the African plate. At the same time of the subduction in the north there was mantle upwelling causing the crust to down warp and swell into domes. There are many domes throughout the East African Rift System. The plume is thought to have begun under Lake Tana in Ethiopia. The Kenyan dome has been studied extensively.

text: Rifting is said to have begun in the

text: Late Cretaceous

text: epoch to Paleogene period. At that time the African plate was experiencing far-field stresses caused by portions of the northern boundary of the African plate subducting under the Eurasian plate. Today, the Arabian plate is experiencing a crustal down pull, or

text: slab pull

text: , that has separated from the African plate. At the same time of the

text: subduction

text: in the north there was mantle upwelling causing the crust to down warp and swell into

text: domes

text: . There are many domes throughout the East African Rift System. The plume is thought to have begun under

text: Lake Tana

text: in

text: Ethiopia

text: . The Kenyan dome has been studied extensively.

answers: NDQ_003351

answers: far-field stresses

answers: NDQ_003352

answers: warps

answers: NDQ_003353

answers: rifting

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: slab pull

answers: NDQ_003356

answers: swell

answers: NDQ_003357

answers: subducting under the Eurasian plate

answers: NDQ_003358

answers: dome

answers: NDQ_003359

answers: subducts

answers: NDQ_003360

answers: Eurasian plates

answers: NDQ_003362

answers: Lake Tana in Ethiopia

answers: NDQ_003363

answers: Late Cretaceous

answers: NDQ_003371

answers: Which of the following is not a type of thrust fault?

answers: NDQ_003373

answers: what is the last word in the passage?

answers: NDQ_003376

answers: Which of the following is not caused by compressive forces: basin-and-range or mantle upwelling?

answers: NDQ_003378

answers: what is the last word in the passage?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: Which of the following is not a type of stress: far-field stresses or slab pull?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock: subducting under the Eurasian plate?

answers: NDQ_003384

answers: Which of the following is not a type of fold?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: Which of the following is not a cause of earthquakes?

answers: NDQ_003387

answers: Which plate is experiencing a crustal down pull, or slab pull, that has separated from the African plate

answers: NDQ_003388

answers: Which of the following is not a result of shear stress: strike-slip faults, subducting under the Eurasian plate or slab pull?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: slab pull

answers: NDQ_003391

answers: subducting

answers: NDQ_003392

answers: slab pull

answers: NDQ_003393

answers: subducting

answers: NDQ_003394

answers: subducting

answers: NDQ_003395

answers: subducting

answers: NDQ_003396

answers: slab pull

answers: NDQ_003351

answers: far-field stresses

answers: NDQ_003352

answers: down warp and swell into domes.

answers: NDQ_003353

answers: down warp and swell into domes.

answers: NDQ_003354

answers: Rifting

answers: NDQ_003355

answers: domes.

answers: NDQ_003356

answers: warp and swell into domes.

answers: NDQ_003357

answers: mantle upwelling

answers: NDQ_003358

answers: domes.

answers: NDQ_003359

answers: mantle upwelling

answers: NDQ_003360

answers: mantle upwelling

answers: NDQ_003362

answers: Rifting

answers: NDQ_003363

answers: Rifting

answers: NDQ_003371

answers: Rifting

answers: NDQ_003373

answers: far-field stresses

answers: NDQ_003376

answers: domes.

answers: NDQ_003378

answers: crustal down pull,

answers: NDQ_003379

answers: Late Cretaceous epoch to Paleogene period.

answers: NDQ_003380

answers: stresses

answers: NDQ_003381

answers: down warp and swell into domes.

answers: NDQ_003382

answers: far-field stresses

answers: NDQ_003383

answers: domes.

answers: NDQ_003384

answers: domes.

answers: NDQ_003385

answers: far-field stresses

answers: NDQ_003386

answers: Rifting

answers: NDQ_003387

answers: far-field stresses

answers: NDQ_003388

answers: far-field stresses

answers: NDQ_003389

answers: domes.

answers: NDQ_003390

answers: crustal down pull,

answers: NDQ_003391

answers: domes.

answers: NDQ_003392

answers: Rifting

answers: NDQ_003393

answers: domes.

answers: NDQ_003394

answers: far-field stresses

answers: NDQ_003395

answers: Eurasian plate.

answers: NDQ_003396

answers: crustal down pull,

text: V. carteri can reproduce either asexually or sexually. Thus, it is a facultatively sexual organism.  In nature, Volvox reproduces asexually in temporary ponds in spring, but becomes sexual and produces dormant over-wintering zygotes before the ponds dry up in the summer heat.  V. carteri can be induced to reproduce sexually by heat shock treatment.  However, this induction can be inhibited by antioxidants indicating that the induction of sex by heat shock is mediated by oxidative stress.  Nedelcu et al. further found that an inhibitor of the mitochondrial electron transport chain that induces oxidative stress also induced sex in V. carteri.  Nedelcu and Michod and Nedelcu et al. suggested that oxidative DNA damage caused by oxidative stress may be the underlying cause of the induction of sex in their experiments.  Other agents that cause DNA damage (i.e. glutaraldehyde, formaldehyde and UV) also induce sex in V. carteri.  These findings lend support to the general idea that a principal adaptive function of sex is repair of DNA damages.

text: V. carteri can reproduce either asexually or sexually. Thus, it is a facultatively sexual organism.  In nature, Volvox reproduces asexually in temporary ponds in spring, but becomes sexual and produces dormant over-wintering zygotes before the ponds dry up in the summer heat.  V. carteri can be induced to reproduce sexually by heat shock treatment.  However, this induction can be inhibited by antioxidants indicating that the induction of sex by heat shock is mediated by oxidative stress.  Nedelcu et al. further found that an inhibitor of the mitochondrial electron transport chain that induces oxidative stress also induced sex in V. carteri.  Nedelcu and Michod and Nedelcu et al. suggested that oxidative DNA damage caused by oxidative stress may be the underlying cause of the induction of sex in their experiments.  Other agents that cause DNA damage (i.e. glutaraldehyde, formaldehyde and UV) also induce sex in V. carteri.  These findings lend support to the general idea that a principal adaptive function of sex is repair of DNA damages.

answers: NDQ_003351

answers: oxidative

answers: NDQ_003352

answers: oxidizes

answers: NDQ_003353

answers: DNA damage

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: oxidize

answers: NDQ_003357

answers: V. carteri can be induced to reproduce sexually

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: induction can be inhibited by antioxidants

answers: NDQ_003363

answers: the same time

answers: NDQ_003371

answers: What is a thrust fault?

answers: NDQ_003373

answers: How would you describe the stress?

answers: NDQ_003376

answers: What type of terrain is caused by compressive forces?

answers: NDQ_003378

answers: What is the amount the ground moves in an earthquake?

answers: NDQ_003379

answers: The dip of the fault plane is vertical

answers: NDQ_003380

answers: What is the main idea of this passage?

answers: NDQ_003381

answers: What is the main idea of this passage?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the main idea of this passage?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: movement of rock at faults

answers: NDQ_003387

answers: Which of the following is not a cause of normal faults?

answers: NDQ_003388

answers: Which of the following is not an example of a strike-slip fault?

answers: NDQ_003389

answers: mountains

answers: NDQ_003390

answers: footwall

answers: NDQ_003391

answers: igneous rock

answers: NDQ_003392

answers: asymmetrical fault

answers: NDQ_003393

answers: dip-slip fault

answers: NDQ_003394

answers: vertical fault

answers: NDQ_003395

answers: a vertical fault plane

answers: NDQ_003396

answers: horizontal fault

answers: NDQ_003351

answers: oxidative stress.

answers: NDQ_003352

answers: mitochondrial electron transport chain

answers: NDQ_003353

answers: oxidative DNA damage

answers: NDQ_003354

answers: oxidative stress.

answers: NDQ_003355

answers: V. carteri

answers: NDQ_003356

answers: oxidative stress.

answers: NDQ_003357

answers: asexually

answers: NDQ_003358

answers: ponds

answers: NDQ_003359

answers: oxidative DNA damage

answers: NDQ_003360

answers: oxidative stress.

answers: NDQ_003362

answers: V. carteri can reproduce either asexually or sexually.

answers: NDQ_003363

answers: heat.

answers: NDQ_003371

answers: oxidative DNA damage

answers: NDQ_003373

answers: oxidative stress.

answers: NDQ_003376

answers: oxidative stress.

answers: NDQ_003378

answers: oxidative DNA damage

answers: NDQ_003379

answers: oxidative DNA damage

answers: NDQ_003380

answers: oxidative stress.

answers: NDQ_003381

answers: oxidative stress.

answers: NDQ_003382

answers: oxidative stress.

answers: NDQ_003383

answers: oxidative stress.

answers: NDQ_003384

answers: oxidative DNA damage

answers: NDQ_003385

answers: oxidative stress.

answers: NDQ_003386

answers: oxidative DNA damage

answers: NDQ_003387

answers: oxidative stress.

answers: NDQ_003388

answers: oxidative stress.

answers: NDQ_003389

answers: oxidative stress.

answers: NDQ_003390

answers: V. carteri

answers: NDQ_003391

answers: V. carteri

answers: NDQ_003392

answers: V. carteri

answers: NDQ_003393

answers: V. carteri

answers: NDQ_003394

answers: mitochondrial electron transport chain

answers: NDQ_003395

answers: mitochondrial electron transport chain

answers: NDQ_003396

answers: mitochondrial electron transport chain

text: The term cryptoexplosion structure (or cryptovolcanic structure) means an explosion of unknown cause.  The term is now largely obsolete. It was once commonly used to describe sites where there was geological evidence of a large-scale explosion within the Earth's crust, but no definitive evidence for the cause such as normal volcanic rocks. These sites are usually circular with signs of anomalous rock deformation contrasting with the surrounding region, and often showing evidence that crustal material had been uplifted and/or blown outwards. The assumption was that some unusual form of volcanism, or a gas explosion originating within the crust, was the cause. The use of the term went away with the rise of the science of impact crater recognition in the late 20th century. Most structures described as cryptoexplosions turned out to be eroded impact craters, caused by the impact of meteorites. Today geologists discount former cryptoexplosion theories.

text: The term cryptoexplosion structure (or cryptovolcanic structure) means an explosion of unknown cause.  The term is now largely obsolete. It was once commonly used to describe sites where there was geological evidence of a large-scale explosion within the

text: Earth's crust

text: , but no definitive evidence for the cause such as normal

text: volcanic rocks

text: . These sites are usually circular with signs of anomalous rock deformation contrasting with the surrounding region, and often showing evidence that crustal material had been uplifted and/or blown outwards. The assumption was that some unusual form of volcanism, or a gas explosion originating within the crust, was the cause. The use of the term went away with the rise of the science of impact crater recognition in the late 20th century. Most structures described as cryptoexplosions turned out to be eroded

text: impact crater

text: s, caused by the impact of

text: meteorite

text: s. Today geologists discount former cryptoexplosion theories.

answers: NDQ_003351

answers: anomalous rock deformation

answers: NDQ_003352

answers: deforms

answers: NDQ_003353

answers: anomalous rock deformation

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: unanswerable

answers: NDQ_003356

answers: contrasting with the surrounding region

answers: NDQ_003357

answers: geological evidence of a large-scale explosion

answers: NDQ_003358

answers: impact crater

answers: NDQ_003359

answers: deformation

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: the term cryptoexplosion structure means an explosion of unknown cause

answers: NDQ_003363

answers: large-scale explosions

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: Why is the term cryptoexplosion structure now largely obsolete?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What does the term cryptoexplosion structure mean?

answers: NDQ_003381

answers: What does the term cryptoexplosion structure mean?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: Fault zones are areas where faults are clustered

answers: NDQ_003386

answers: geologists discount former cryptoexplosion theories

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: What does the term cryptoexplosion structure mean?

answers: NDQ_003389

answers: rock deformation

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: unanswerable

answers: NDQ_003392

answers: unanswerable

answers: NDQ_003393

answers: uplifted

answers: NDQ_003394

answers: lateral

answers: NDQ_003395

answers: unanswerable

answers: NDQ_003396

answers: Cryptoexplosion structure

answers: NDQ_003351

answers: meteorites.

answers: NDQ_003352

answers: deformation

answers: NDQ_003353

answers: deformation

answers: NDQ_003354

answers: volcanic rocks.

answers: NDQ_003355

answers: cryptoexplosion structure

answers: NDQ_003356

answers: blown outwards.

answers: NDQ_003357

answers: volcanic rocks.

answers: NDQ_003358

answers: impact crater

answers: NDQ_003359

answers: uplifted and/or blown outwards.

answers: NDQ_003360

answers: volcanism,

answers: NDQ_003362

answers: some unusual form of volcanism,

answers: NDQ_003363

answers: explosion within the Earth's crust,

answers: NDQ_003371

answers: anomalous rock deformation

answers: NDQ_003373

answers: rock deformation contrasting with the surrounding region,

answers: NDQ_003376

answers: the impact of meteorites.

answers: NDQ_003378

answers: crustal material had been uplifted

answers: NDQ_003379

answers: circular with signs of anomalous rock deformation contrasting with the surrounding region,

answers: NDQ_003380

answers: rock deformation

answers: NDQ_003381

answers: rock deformation contrasting with the surrounding region,

answers: NDQ_003382

answers: meteorites.

answers: NDQ_003383

answers: rock deformation

answers: NDQ_003384

answers: blown outwards.

answers: NDQ_003385

answers: circular with signs of anomalous rock deformation contrasting with the surrounding region,

answers: NDQ_003386

answers: uplifted and/or blown outwards.

answers: NDQ_003387

answers: volcanic rocks.

answers: NDQ_003388

answers: eroded impact craters, caused by the impact of meteorites.

answers: NDQ_003389

answers: uplifted

answers: NDQ_003390

answers: cryptoexplosion structure

answers: NDQ_003391

answers: impact craters,

answers: NDQ_003392

answers: uplifted

answers: NDQ_003393

answers: impact craters,

answers: NDQ_003394

answers: circular with signs of anomalous rock deformation contrasting with the surrounding region,

answers: NDQ_003395

answers: circular with signs of anomalous rock deformation contrasting with the surrounding region,

answers: NDQ_003396

answers: circular with signs of anomalous rock deformation contrasting with the surrounding region,

text: Carefully Lurking Into Mountainous Building Is Tricky

text: Carefully Lurking Into Mountainous Building Is Tricky

answers: NDQ_003351

answers: mountainous

answers: NDQ_003352

answers: can crack

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: crease

answers: NDQ_003356

answers: fall down

answers: NDQ_003357

answers: a person would not be able to escape a building

answers: NDQ_003358

answers: mountain

answers: NDQ_003359

answers: is in contact with it

answers: NDQ_003360

answers: tectonic plates

answers: NDQ_003362

answers: The San Andreas fault is not a mountain.

answers: NDQ_003363

answers: volcanoes

answers: NDQ_003371

answers: How do you know if you are in a mountainous building?

answers: NDQ_003373

answers: Which of the following is not a type of stress?

answers: NDQ_003376

answers: How would you describe the terrain known as basin-and-range?

answers: NDQ_003378

answers: How does the ground move in an earthquake?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What is the best way to avoid this problem?

answers: NDQ_003382

answers: None of the above choices.

answers: NDQ_003383

answers: What is the best title for this passage?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a mountainous building?

answers: NDQ_003386

answers: What is a mountainous building?

answers: NDQ_003387

answers: Which of the following is not a cause of normal faults?

answers: NDQ_003388

answers: How does shear stress affect mountainous buildings?

answers: NDQ_003389

answers: The process of folding creates mountains

answers: NDQ_003390

answers: is a mountainous building

answers: NDQ_003391

answers: is a mountainous building

answers: NDQ_003392

answers: can be used to describe

answers: NDQ_003393

answers: can be buried

answers: NDQ_003394

answers: is tricky

answers: NDQ_003395

answers: a mountainous building

answers: NDQ_003396

answers: can be used to describe

answers: NDQ_003351

answers: Mountainous Building Is Tricky

answers: NDQ_003352

answers: Carefully Lurking Into Mountainous Building Is Tricky

answers: NDQ_003353

answers: Carefully Lurking Into Mountainous Building

answers: NDQ_003354

answers: Carefully Lurking Into Mountainous Building Is Tricky

answers: NDQ_003355

answers: Carefully Lurking Into Mountainous Building

answers: NDQ_003356

answers: Carefully Lurking Into Mountainous Building

answers: NDQ_003357

answers: Carefully Lurking Into Mountainous Building Is Tricky

answers: NDQ_003358

answers: Mountainous Building

answers: NDQ_003359

answers: Mountainous Building

answers: NDQ_003360

answers: Carefully Lurking Into Mountainous Building Is Tricky

answers: NDQ_003362

answers: Carefully Lurking Into Mountainous Building Is Tricky

answers: NDQ_003363

answers: Carefully Lurking Into Mountainous Building Is Tricky

answers: NDQ_003371

answers: Carefully Lurking Into Mountainous Building Is Tricky

answers: NDQ_003373

answers: Carefully Lurking Into Mountainous Building Is Tricky

answers: NDQ_003376

answers: Carefully Lurking Into Mountainous Building Is Tricky

answers: NDQ_003378

answers: Carefully Lurking Into Mountainous Building

answers: NDQ_003379

answers: Carefully Lurking Into Mountainous Building Is Tricky

answers: NDQ_003380

answers: Carefully Lurking Into Mountainous Building Is Tricky

answers: NDQ_003381

answers: Carefully Lurking Into Mountainous Building Is Tricky

answers: NDQ_003382

answers: Carefully Lurking Into Mountainous Building Is Tricky

answers: NDQ_003383

answers: Carefully Lurking Into Mountainous Building

answers: NDQ_003384

answers: Carefully Lurking Into Mountainous Building Is Tricky

answers: NDQ_003385

answers: Carefully Lurking Into Mountainous Building Is Tricky

answers: NDQ_003386

answers: Carefully Lurking Into Mountainous Building Is Tricky

answers: NDQ_003387

answers: Carefully Lurking Into Mountainous Building Is Tricky

answers: NDQ_003388

answers: Carefully Lurking Into Mountainous Building Is Tricky

answers: NDQ_003389

answers: Mountainous Building Is Tricky

answers: NDQ_003390

answers: Carefully Lurking Into Mountainous Building Is Tricky

answers: NDQ_003391

answers: Mountainous Building

answers: NDQ_003392

answers: Carefully Lurking Into Mountainous Building Is Tricky

answers: NDQ_003393

answers: Mountainous Building

answers: NDQ_003394

answers: Mountainous Building Is Tricky

answers: NDQ_003395

answers: Carefully Lurking Into Mountainous Building Is Tricky

answers: NDQ_003396

answers: Carefully Lurking Into Mountainous Building Is Tricky

text: Lake Turkana is an East African Rift feature. A rift is a weak place in the Earth's crust due to the separation of two tectonic plates, often accompanied by a graben, or trough, in which lake water can collect. The rift began when East Africa, impelled by currents in the mantle, began separating from the rest of Africa, moving to the northeast. Currently, the graben is 320 km wide in the north of the lake, 170 km in the south. This rift is one of two, and is called the Great or Eastern Rift. There is another to the west, the Western Rift.

text: Lake Turkana is an

text: East African Rift

text: feature. A

text: rift

text: is a weak place in the Earth's crust due to the separation of two

text: tectonic plate

text: s, often accompanied by a

text: graben

text: , or trough, in which lake water can collect. The rift began when East Africa, impelled by currents in the

text: mantle

text: , began separating from the rest of Africa, moving to the northeast. Currently, the graben is 320 km wide in the north of the lake, 170 km in the south. This rift is one of two, and is called the Great or Eastern Rift. There is another to the west, the Western Rift.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: is more likely to crack

answers: NDQ_003353

answers: rifts

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: graben

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: a tectonic plate separates from another plate

answers: NDQ_003358

answers: rift

answers: NDQ_003359

answers: separates

answers: NDQ_003360

answers: tectonic plates

answers: NDQ_003362

answers: Lake Turkana is an East African Rift feature

answers: NDQ_003363

answers: East African Rift

answers: NDQ_003371

answers: Which of the following is not a type of rift: Great or Eastern Rift?

answers: NDQ_003373

answers: what is the last word in the passage?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: How many tectonic plates are mentioned?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What would happen if there was no rift?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not a type of fold: rift, graben, or trough?

answers: NDQ_003385

answers: what is the last word in the passage?

answers: NDQ_003386

answers: Which of the following is not a cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: tectonic plates, graben, or trough?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip faults, graben, or trough?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: graben

answers: NDQ_003391

answers: graben

answers: NDQ_003392

answers: rift

answers: NDQ_003393

answers: graben

answers: NDQ_003394

answers: trough

answers: NDQ_003395

answers: tectonic plates

answers: NDQ_003396

answers: graben

answers: NDQ_003351

answers: currents

answers: NDQ_003352

answers: weak

answers: NDQ_003353

answers: separation of two tectonic plates,

answers: NDQ_003354

answers: Great or Eastern Rift.

answers: NDQ_003355

answers: graben,

answers: NDQ_003356

answers: separation of two tectonic plates,

answers: NDQ_003357

answers: separation of two tectonic plates,

answers: NDQ_003358

answers: rift

answers: NDQ_003359

answers: separation of two tectonic plates,

answers: NDQ_003360

answers: tectonic plates,

answers: NDQ_003362

answers: Lake Turkana is an East African Rift feature.

answers: NDQ_003363

answers: East African Rift

answers: NDQ_003371

answers: East African Rift

answers: NDQ_003373

answers: rift is a weak place in the Earth's crust

answers: NDQ_003376

answers: separation of two tectonic plates,

answers: NDQ_003378

answers: rift

answers: NDQ_003379

answers: northeast.

answers: NDQ_003380

answers: rift is a weak place in the Earth's crust

answers: NDQ_003381

answers: rift

answers: NDQ_003382

answers: tectonic plates,

answers: NDQ_003383

answers: separation of two tectonic plates,

answers: NDQ_003384

answers: a graben,

answers: NDQ_003385

answers: rift

answers: NDQ_003386

answers: separation of two tectonic plates,

answers: NDQ_003387

answers: separation of two tectonic plates,

answers: NDQ_003388

answers: separation of two tectonic plates,

answers: NDQ_003389

answers: separation of two tectonic plates,

answers: NDQ_003390

answers: East African Rift

answers: NDQ_003391

answers: graben,

answers: NDQ_003392

answers: East African Rift

answers: NDQ_003393

answers: graben,

answers: NDQ_003394

answers: two tectonic plates,

answers: NDQ_003395

answers: tectonic plates,

answers: NDQ_003396

answers: East African Rift

text: Many longitudinal valleys follow the strike of the rock strata or significant geological fault lines. These are formed in conjunction with the tectonic movements during the mountain building, which in turn are due to plate tectonic processes. The faults be structures that reach deep into the lower part of the earth's crust, that are already in place before the actual mountain building phase and are later reactivated as, for example, is the case in the Periadriatic Seam in the Alps. For the formation of longitudinal valleys, however, nappe overthrusts also play a major, if not the most important, role. The nappes that are present in many young fold mountain ranges is responsible to a large extent for the morphological division of a mountain belt into more or less parallel chains. In such cases, longitudinal valleys generally run along the so-called leading edge of the napped (the overthrust front), that are oriented at right angles to the direction of movement of the tectonic nappes, which in turn corresponds to the direction of movement of the colliding continental blocks. From this configuration results a course that runs  with the strike of the geological units, which is an important criterion for the definition of a longitudinal valley. By contrast a transverse valley cuts across the strike.

text: Many longitudinal valleys follow the

text: strike

text: of the

text: rock strata

text: or significant

text: geological fault lines

text: . These are formed in conjunction with the tectonic movements during the

text: mountain building

text: , which in turn are due to

text: plate tectonic

text: processes. The faults be structures that reach deep into the lower part of the

text: earth's crust

text: , that are already in place before the actual mountain building phase and are later reactivated as, for example, is the case in the

text: Periadriatic Seam

text: in the Alps. For the formation of longitudinal valleys, however,

text: nappe

text: overthrust

text: s also play a major, if not the most important, role. The nappes that are present in many young fold mountain ranges is responsible to a large extent for the morphological division of a mountain belt into more or less parallel chains. In such cases, longitudinal valleys generally run along the so-called leading edge of the napped (the overthrust front), that are oriented at right angles to the direction of movement of the tectonic nappes, which in turn corresponds to the direction of movement of the colliding

text: continental blocks

text: . From this configuration results a course that runs  with the

text: strike

text: of the geological units, which is an important criterion for the definition of a longitudinal valley. By contrast a transverse valley cuts across the strike.

answers: NDQ_003351

answers: overthrusts

answers: NDQ_003352

answers: runs with the strike

answers: NDQ_003353

answers: faults

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: transverse valley

answers: NDQ_003356

answers: run along the leading edge

answers: NDQ_003357

answers: direction of movement of the colliding continental blocks

answers: NDQ_003358

answers: transverse valley

answers: NDQ_003359

answers: is displaced

answers: NDQ_003360

answers: tectonic movements

answers: NDQ_003362

answers: transverse valley cuts across the strike.

answers: NDQ_003363

answers: tectonic movements

answers: NDQ_003371

answers: What is the case in the Periadriatic Seam in the Alps?

answers: NDQ_003373

answers: what is the most important criterion for the definition of a longitudinal valley

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What is the most important criterion for the definition of a longitudinal valley

answers: NDQ_003381

answers: What is the most important criterion for the definition of a longitudinal valley?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: plate tectonic processes

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: normal faults or plate tectonic processes?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip faults, overthrusts, or nappes?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: transverse valley

answers: NDQ_003391

answers: the overthrust front

answers: NDQ_003392

answers: transverse valley

answers: NDQ_003393

answers: rock strata

answers: NDQ_003394

answers: transverse valley

answers: NDQ_003395

answers: significant geological fault lines

answers: NDQ_003396

answers: transverse valley

answers: NDQ_003351

answers: nappe overthrusts

answers: NDQ_003352

answers: geological fault lines.

answers: NDQ_003353

answers: fault lines.

answers: NDQ_003354

answers: Many longitudinal valleys follow the strike of the rock strata

answers: NDQ_003355

answers: transverse valley

answers: NDQ_003356

answers: transverse valley

answers: NDQ_003357

answers: runs with the strike of the geological units,

answers: NDQ_003358

answers: transverse valley

answers: NDQ_003359

answers: strike of the rock strata or significant geological fault lines.

answers: NDQ_003360

answers: geological fault lines.

answers: NDQ_003362

answers: a transverse valley cuts across the strike.

answers: NDQ_003363

answers: follow the strike of the rock strata or significant geological fault lines.

answers: NDQ_003371

answers: nappe overthrusts

answers: NDQ_003373

answers: deep into the lower part of the earth's crust,

answers: NDQ_003376

answers: nappe overthrusts

answers: NDQ_003378

answers: strike of the rock strata or significant geological fault lines.

answers: NDQ_003379

answers: right angles

answers: NDQ_003380

answers: strike of the rock strata or significant geological fault lines.

answers: NDQ_003381

answers: nappe overthrusts

answers: NDQ_003382

answers: nappe overthrusts

answers: NDQ_003383

answers: nappe overthrusts

answers: NDQ_003384

answers: nappe overthrusts

answers: NDQ_003385

answers: fault lines.

answers: NDQ_003386

answers: plate tectonic processes.

answers: NDQ_003387

answers: nappe overthrusts

answers: NDQ_003388

answers: plate tectonic processes.

answers: NDQ_003389

answers: nappe overthrusts

answers: NDQ_003390

answers: transverse valley

answers: NDQ_003391

answers: rock strata

answers: NDQ_003392

answers: transverse valley

answers: NDQ_003393

answers: rock strata

answers: NDQ_003394

answers: transverse

answers: NDQ_003395

answers: geological fault lines.

answers: NDQ_003396

answers: transverse valley

text: Tectonic boundaries have been discovered on Mars. Valles Marineris is a horizontally sliding tectonic boundary that divides two major partial or complete plates of Mars. The recent finding suggests that Mars is geologically active with occurrences in the millions of years, and there is additional speculation.There has been previous evidence of Mars' geologic activity. The Mars Global Surveyor (MGS) discovered magnetic stripes in the crust of Mars, especially in the Phaethontis and Eridania quadrangles. The magnetometer on MGS discovered 100 km wide stripes of magnetized crust running roughly parallel for up to 2000 km. These stripes alternate in polarity with the north magnetic pole of one pointing up from the surface and the north magnetic pole of the next pointing down. When similar stripes were discovered on Earth in the 1960s, they were taken as evidence of plate tectonics. However, there are some differences, between the magnetic stripes on Earth and those on Mars. The Martian stripes are wider, much more strongly magnetized, and do not appear to spread out from a middle crustal spreading zone.Because the area with the magnetic stripes is about 4 billion years old, it is believed that the global magnetic field probably lasted for only the first few hundred million years of Mars' life. At that time the temperature of the molten iron in the planet's core might have been high enough to mix it into a magnetic dynamo. Younger rock does not show any stripes.When molten rock containing magnetic material, such as hematite (Fe2O3), cools and solidifies in the presence of a magnetic field, it becomes magnetized and takes on the polarity of the background field. This magnetism is lost only if the rock is subsequently heated above the Curie temperature, which is 770 °C for pure iron, but lower for oxides such as hematite (approximately 650 °C) or magnetite (approximately 580 °C). The magnetism left in rocks is a record of the magnetic field when the rock solidified.

text: Tectonic boundaries have been discovered on Mars. Valles Marineris is a horizontally sliding tectonic boundary that divides two major partial or complete plates of Mars. The recent finding suggests that Mars is geologically active with occurrences in the millions of years, and there is additional speculation.There has been previous evidence of Mars' geologic activity. The

text: Mars Global Surveyor

text: (MGS) discovered magnetic stripes in the crust of Mars, especially in the Phaethontis and

text: Eridania quadrangle

text: s. The magnetometer on MGS discovered 100 km wide stripes of magnetized crust running roughly parallel for up to 2000 km. These stripes alternate in polarity with the north magnetic pole of one pointing up from the surface and the north magnetic pole of the next pointing down. When similar stripes were discovered on Earth in the 1960s, they were taken as evidence of

text: plate tectonics

text: . However, there are some differences, between the

text: magnetic stripes

text: on Earth and those on Mars. The Martian stripes are wider, much more strongly magnetized, and do not appear to spread out from a middle crustal spreading zone.Because the area with the magnetic stripes is about 4 billion years old, it is believed that the global magnetic field probably lasted for only the first few hundred million years of Mars' life. At that time the temperature of the molten iron in the planet's core might have been high enough to mix it into a magnetic dynamo. Younger rock does not show any stripes.When molten rock containing magnetic material, such as

text: hematite

text: (Fe2O3), cools and solidifies in the presence of a magnetic field, it becomes magnetized and takes on the polarity of the background field. This magnetism is lost only if the rock is subsequently heated above the Curie temperature, which is 770 °C for pure iron, but lower for oxides such as hematite (approximately 650 °C) or magnetite (approximately 580 °C). The magnetism left in rocks is a record of the magnetic field when the rock solidified.

answers: NDQ_003351

answers: horizontally sliding

answers: NDQ_003352

answers: magnetizes more

answers: NDQ_003353

answers: Magnetism

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: vertical fold

answers: NDQ_003356

answers: magnetize

answers: NDQ_003357

answers: Younger rock does not show any stripes.

answers: NDQ_003358

answers: Tectonic boundary

answers: NDQ_003359

answers: is subsequently heated

answers: NDQ_003360

answers: Earth

answers: NDQ_003362

answers: Younger rock does not show any stripes

answers: NDQ_003363

answers: Valles Marineris

answers: NDQ_003371

answers: Which of the following is not a type of rock: hematite, iron, or magnetite?

answers: NDQ_003373

answers: Which of the following is not a type of rock: Younger rock does not show any stripes.

answers: NDQ_003376

answers: Which of the following is not a type of terrain: basin-and-range or plate tectonics?

answers: NDQ_003378

answers: What is the difference between the magnetic stripes on Earth and those on Mars?

answers: NDQ_003379

answers: What is the difference between the magnetic stripes on Earth and those on Mars?

answers: NDQ_003380

answers: Which of the following is not a type of force applied to rock?

answers: NDQ_003381

answers: Which of the following is not a type of rock: hematite, iron, or magnetite?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not a type of fold that arches upward?

answers: NDQ_003385

answers: Which of the following is not a type of plate tectonics: plate tectonics, plate tectonics, or crustal spreading zone?

answers: NDQ_003386

answers: Which of the following is not a cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not a type of plate tectonics: plate tectonics, plate tectonics, or normal faults?

answers: NDQ_003388

answers: Which of the following is not a result of shear stress: strike-slip faults, plate tectonics, or strike-slip faults?

answers: NDQ_003389

answers: What is the difference between the magnetic stripes on Earth and those on Mars

answers: NDQ_003390

answers: Valles Marineris

answers: NDQ_003391

answers: Valles Marineris

answers: NDQ_003392

answers: Valles Marineris

answers: NDQ_003393

answers: Valles Marineris

answers: NDQ_003394

answers: Valles Marineris

answers: NDQ_003395

answers: Valles Marineris

answers: NDQ_003396

answers: Valles Marineris

answers: NDQ_003351

answers: zone.Because the area with the magnetic stripes

answers: NDQ_003352

answers: it becomes magnetized

answers: NDQ_003353

answers: magnetized

answers: NDQ_003354

answers: do not appear to spread out from a middle crustal spreading zone.Because

answers: NDQ_003355

answers: middle crustal spreading zone.Because

answers: NDQ_003356

answers: magnetized

answers: NDQ_003357

answers: Younger rock does not show any stripes.When

answers: NDQ_003358

answers: middle crustal spreading zone.Because

answers: NDQ_003359

answers: heated above the Curie temperature,

answers: NDQ_003360

answers: spread out from a middle crustal spreading zone.Because

answers: NDQ_003362

answers: spreading zone.Because

answers: NDQ_003363

answers: 4 billion years old,

answers: NDQ_003371

answers: middle crustal spreading zone.Because

answers: NDQ_003373

answers: magnetic stripes

answers: NDQ_003376

answers: middle crustal spreading zone.Because

answers: NDQ_003378

answers: al spreading zone.Because

answers: NDQ_003379

answers: middle crustal spreading zone.Because

answers: NDQ_003380

answers: magnetized

answers: NDQ_003381

answers: magnet

answers: NDQ_003382

answers: middle crustal spreading zone.Because

answers: NDQ_003383

answers: magnetized

answers: NDQ_003384

answers: crustal spreading zone.Because

answers: NDQ_003385

answers: middle crustal spreading zone.Because

answers: NDQ_003386

answers: magnetic dynamo.

answers: NDQ_003387

answers: magnetized

answers: NDQ_003388

answers: magnetic material,

answers: NDQ_003389

answers: magnetic stripes

answers: NDQ_003390

answers: crustal spreading zone.Because

answers: NDQ_003391

answers: middle crustal spreading zone.Because

answers: NDQ_003392

answers: middle crustal spreading zone.Because

answers: NDQ_003393

answers: middle crustal spreading zone.Because

answers: NDQ_003394

answers: Valles Marineris

answers: NDQ_003395

answers: Valles Marineris

answers: NDQ_003396

answers: Valles Marineris

text: Plate tectonics, mountain ranges, volcanoes, and earthquakes are geological phenomena that can be explained in terms of energy transformations in Earth's crust.

text: Plate tectonics

text: mountain

text: ranges,

text: volcano

text: es, and

text: earthquake

text: s are

text: geological phenomena

text: that can be explained in terms of

text: energy transformation

text: s in

text: Earth's crust

answers: NDQ_003351

answers: earthquakes

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: mountain range

answers: NDQ_003356

answers: change shape

answers: NDQ_003357

answers: energy transformations occur in the Earth's crust.

answers: NDQ_003358

answers: volcano

answers: NDQ_003359

answers: is pushed together

answers: NDQ_003360

answers: plate tectonics

answers: NDQ_003362

answers: The San Andreas fault is not a volcano.

answers: NDQ_003363

answers: plate tectonics

answers: NDQ_003371

answers: Which of the following is not a geological phenomenon?

answers: NDQ_003373

answers: How would you describe a rock that is deeply buried?

answers: NDQ_003376

answers: The terrain known as basin-and-range is caused by compressive forces

answers: NDQ_003378

answers: What is a type of energy transformation in Earth's crust?

answers: NDQ_003379

answers: The dip of the fault plane is horizontal.

answers: NDQ_003380

answers: Which of the following is not a geological phenomenon?

answers: NDQ_003381

answers: Which of the following is not a geological phenomenon?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not a geological phenomenon that can be explained in terms of energy transformations in Earth's crust?

answers: NDQ_003385

answers: Which of the following is not a type of geological phenomenon?

answers: NDQ_003386

answers: Which of the following is not a type of geological phenomenon?

answers: NDQ_003387

answers: Which of the following is not a geological phenomenon?

answers: NDQ_003388

answers: Which of the following is an example of a geological phenomenon that can be explained by energy transformations in Earth's crust?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: tectonics

answers: NDQ_003391

answers: can be described as a

answers: NDQ_003392

answers: tectonics

answers: NDQ_003393

answers: is a mountain range

answers: NDQ_003394

answers: isobath

answers: NDQ_003395

answers: can cause earthquakes

answers: NDQ_003396

answers: isosceles

answers: NDQ_003351

answers: earthquakes

answers: NDQ_003352

answers: earthquakes

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Plate tectonics,

answers: NDQ_003355

answers: mountain ranges, volcanoes, and earthquakes

answers: NDQ_003356

answers: earthquakes

answers: NDQ_003357

answers: energy transformations

answers: NDQ_003358

answers: earthquakes

answers: NDQ_003359

answers: energy transformations

answers: NDQ_003360

answers: Plate tectonics,

answers: NDQ_003362

answers: energy transformations in Earth's crust.

answers: NDQ_003363

answers: Plate tectonics,

answers: NDQ_003371

answers: Plate tectonics,

answers: NDQ_003373

answers: earthquakes

answers: NDQ_003376

answers: mountain ranges, volcanoes, and earthquakes

answers: NDQ_003378

answers: earthquakes

answers: NDQ_003379

answers: earthquakes

answers: NDQ_003380

answers: earthquakes

answers: NDQ_003381

answers: earthquakes

answers: NDQ_003382

answers: earthquakes

answers: NDQ_003383

answers: earthquakes

answers: NDQ_003384

answers: Plate tectonics,

answers: NDQ_003385

answers: earthquakes

answers: NDQ_003386

answers: energy transformations in Earth's crust.

answers: NDQ_003387

answers: energy transformations in Earth's crust.

answers: NDQ_003388

answers: energy transformations in Earth's crust.

answers: NDQ_003389

answers: Plate tectonics,

answers: NDQ_003390

answers: earthquakes

answers: NDQ_003391

answers: mountain ranges, volcanoes, and earthquakes

answers: NDQ_003392

answers: earthquakes

answers: NDQ_003393

answers: mountain ranges, volcanoes,

answers: NDQ_003394

answers: earthquakes

answers: NDQ_003395

answers: earthquakes

answers: NDQ_003396

answers: earthquakes

text: In plate tectonics, a convergent boundary, also known as a destructive plate boundary (because of subduction), is an actively deforming  region where two (or more) tectonic plates or fragments of the lithosphere move toward one another and collide.  As a result of pressure, friction, and plate material melting in the mantle, earthquakes and volcanoes are common near convergent boundaries. When two plates move towards one another, they form either a subduction zone or a continental collision. This depends on the nature of the plates involved.  In a subduction zone, the subducting plate, which is normally a plate with oceanic crust, moves beneath the other plate, which can be made of either oceanic or continental crust.  During collisions between two continental plates, large mountain ranges, such as the Himalayas are formed.

text: In

text: plate tectonics

text: , a convergent boundary, also known as a destructive plate boundary (because of

text: subduction

text: ), is an actively deforming  region where two (or more) tectonic plates or fragments of the

text: lithosphere

text: move toward one another and collide.  As a result of pressure, friction, and plate material melting in the

text: mantle

text: earthquake

text: s and

text: volcano

text: es are common near convergent boundaries. When two plates move towards one another, they form either a subduction zone or a

text: continental collision

text: . This depends on the nature of the plates involved.  In a subduction zone, the subducting plate, which is normally a plate with

text: oceanic crust

text: , moves beneath the other plate, which can be made of either oceanic or

text: continental crust

text: .  During collisions between two continental plates, large mountain ranges, such as the

text: Himalayas

text: are formed.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: is likely to crack

answers: NDQ_003353

answers: pressure

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: subduction zone

answers: NDQ_003356

answers: collide

answers: NDQ_003357

answers: plate material melting in the mantle are common near convergent boundaries

answers: NDQ_003358

answers: unanswerable

answers: NDQ_003359

answers: collide

answers: NDQ_003360

answers: collisions

answers: NDQ_003362

answers: earthquakes and volcanoes are common near convergent boundaries

answers: NDQ_003363

answers: collisions between two continental plates

answers: NDQ_003371

answers: What is a subduction zone?

answers: NDQ_003373

answers: subduction zone or a continental collision

answers: NDQ_003376

answers: collisions between two continental plates

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: vertical

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What happens to rock when confining stress occurs?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: As a result of pressure, friction, and plate material melting in the mantle,

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: unanswerable

answers: NDQ_003386

answers: convergent boundary

answers: NDQ_003387

answers: Which is not a result of pressure, friction, and plate material melting in the mantle?

answers: NDQ_003388

answers: Which of the following is not a result of pressure, friction, and plate material melting in the mantle

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: subduction zone

answers: NDQ_003391

answers: subduction zone

answers: NDQ_003392

answers: subduction zone

answers: NDQ_003393

answers: subduction zone

answers: NDQ_003394

answers: tectonic

answers: NDQ_003395

answers: tectonic plates

answers: NDQ_003396

answers: subduction zone

answers: NDQ_003351

answers: earthquakes and volcanoes

answers: NDQ_003352

answers: earthquakes and volcanoes

answers: NDQ_003353

answers: earthquakes and volcanoes

answers: NDQ_003354

answers: subduction zone,

answers: NDQ_003355

answers: subduction zone

answers: NDQ_003356

answers: earthquakes and volcanoes

answers: NDQ_003357

answers: the subducting plate,

answers: NDQ_003358

answers: subduction zone

answers: NDQ_003359

answers: collide.

answers: NDQ_003360

answers: During collisions between two continental plates,

answers: NDQ_003362

answers: earthquakes and volcanoes

answers: NDQ_003363

answers: During collisions between two continental plates,

answers: NDQ_003371

answers: subduction zone,

answers: NDQ_003373

answers: pressure, friction, and plate material melting in the mantle,

answers: NDQ_003376

answers: During collisions between two continental plates, large mountain ranges,

answers: NDQ_003378

answers: earthquakes

answers: NDQ_003379

answers: subduction zone,

answers: NDQ_003380

answers: pressure, friction,

answers: NDQ_003381

answers: earthquakes and volcanoes

answers: NDQ_003382

answers: earthquakes and volcanoes

answers: NDQ_003383

answers: pressure, friction,

answers: NDQ_003384

answers: convergent boundary,

answers: NDQ_003385

answers: subduction zone

answers: NDQ_003386

answers: pressure, friction, and plate material melting in the mantle,

answers: NDQ_003387

answers: pressure, friction, and plate material melting in the mantle,

answers: NDQ_003388

answers: pressure, friction, and plate material melting in the mantle,

answers: NDQ_003389

answers: During collisions between two continental plates,

answers: NDQ_003390

answers: subduction),

answers: NDQ_003391

answers: subduction zone,

answers: NDQ_003392

answers: convergent boundary,

answers: NDQ_003393

answers: subduction zone,

answers: NDQ_003394

answers: convergent boundary,

answers: NDQ_003395

answers: subduction zone,

answers: NDQ_003396

answers: subduction zone,

text: About fifty strong motion stations recorded the event, including an array of units along the rupture zone, and instruments at the Berkeley Seismological Laboratory (about  away). The records revealed that strike-slip motion occurred over  on a vertical fault, and that the total amount of slip varied with depth, with more slip occurring in the shallower regions. The two closest stations at Coyote Creek and Gilroy, as well as the Berkeley stations, were used to refine the overall fault length, slip, and depth of faulting.

text: About fifty strong motion stations recorded the event, including an array of units along the rupture zone, and instruments at the

text: Berkeley Seismological Laboratory

text: (about  away). The records revealed that

text: strike-slip

text: motion occurred over  on a vertical fault, and that the total amount of slip varied with depth, with more slip occurring in the shallower regions. The two closest stations at Coyote Creek and Gilroy, as well as the Berkeley stations, were used to refine the overall fault length, slip, and depth of faulting.

answers: NDQ_003351

answers: vertical fault

answers: NDQ_003352

answers: slips

answers: NDQ_003353

answers: slip

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: vertical fault

answers: NDQ_003356

answers: slip

answers: NDQ_003357

answers: more slip occurs in the shallower regions

answers: NDQ_003358

answers: rupture zone

answers: NDQ_003359

answers: ruptures

answers: NDQ_003360

answers: faulting

answers: NDQ_003362

answers: more slip occurring in the shallower regions

answers: NDQ_003363

answers: Berkeley Seismological Laboratory

answers: NDQ_003371

answers: Which of the following is not a type of fault: vertical fault, thrust fault, or horizontal fault?

answers: NDQ_003373

answers: What type of stresses does the rock have?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: yes

answers: NDQ_003380

answers: What type of force applied to rock is a stress?

answers: NDQ_003381

answers: What type of stress does the rock experience?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: yes

answers: NDQ_003386

answers: yes

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: strike-slip motion or normal faults?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip, strike-slip motion, or shear stress?

answers: NDQ_003389

answers: faulting

answers: NDQ_003390

answers: vertical fault

answers: NDQ_003391

answers: rupture zone

answers: NDQ_003392

answers: vertical fault

answers: NDQ_003393

answers: rupture zone

answers: NDQ_003394

answers: unanswerable

answers: NDQ_003395

answers: strike-slip motion

answers: NDQ_003396

answers: vertical fault

answers: NDQ_003351

answers: strike-slip

answers: NDQ_003352

answers: depth, with more slip occurring in the shallower regions.

answers: NDQ_003353

answers: strike-slip motion

answers: NDQ_003354

answers: vertical fault,

answers: NDQ_003355

answers: vertical fault,

answers: NDQ_003356

answers: slip varied with depth, with more slip occurring in the shallower regions.

answers: NDQ_003357

answers: more slip occurring in the shallower regions.

answers: NDQ_003358

answers: rupture zone,

answers: NDQ_003359

answers: vertical fault,

answers: NDQ_003360

answers: vertical fault,

answers: NDQ_003362

answers: more slip occurring in the shallower regions.

answers: NDQ_003363

answers: vertical fault,

answers: NDQ_003371

answers: vertical fault,

answers: NDQ_003373

answers: depth, with more slip occurring in the shallower regions.

answers: NDQ_003376

answers: strike-slip motion occurred over on a vertical fault,

answers: NDQ_003378

answers: strike-slip motion

answers: NDQ_003379

answers: vertical

answers: NDQ_003380

answers: strike-slip motion

answers: NDQ_003381

answers: strike-slip motion

answers: NDQ_003382

answers: strike-slip

answers: NDQ_003383

answers: strike-slip motion occurred over on a vertical fault,

answers: NDQ_003384

answers: vertical fault,

answers: NDQ_003385

answers: rupture zone,

answers: NDQ_003386

answers: strike-slip

answers: NDQ_003387

answers: vertical fault,

answers: NDQ_003388

answers: vertical fault,

answers: NDQ_003389

answers: vertical fault,

answers: NDQ_003390

answers: vertical fault,

answers: NDQ_003391

answers: vertical fault,

answers: NDQ_003392

answers: vertical fault,

answers: NDQ_003393

answers: vertical fault,

answers: NDQ_003394

answers: vertical fault,

answers: NDQ_003395

answers: strike-slip motion occurred over on a vertical fault,

answers: NDQ_003396

answers: vertical fault,

text: In geology, transpression is a type of strike-slip deformation that deviates from simple shear because of a simultaneous component of shortening perpendicular to the fault plane. This movement ends up resulting in oblique shear. It is generally very unlikely that a deforming body will experience "pure" shortening or "pure" strike-slip. The relative amounts of shortening and strike-slip can be expressed in the convergence angle alpha which ranges from zero (ideal strike-slip) to 90 degrees (ideal convergence). During shortening, unless material is lost, transpression produces vertical thickening in the crust. Transpression that occurs on a regional scale along plate boundaries is characterized by oblique convergence.  More locally, transpression occurs within restraining bends in strike-slip fault zones.

text: In

text: geology

text: , transpression is a type of

text: strike-slip

text: deformation that deviates from simple shear because of a simultaneous component of shortening perpendicular to the fault plane. This movement ends up resulting in oblique shear. It is generally very unlikely that a deforming body will experience "pure" shortening or "pure" strike-slip. The relative amounts of shortening and strike-slip can be expressed in the convergence angle alpha which ranges from zero (ideal strike-slip) to 90 degrees (ideal convergence). During shortening, unless material is lost, transpression produces vertical thickening in the crust. Transpression that occurs on a regional scale along

text: plate boundaries

text: is characterized by oblique convergence.  More locally, transpression occurs within restraining bends in strike-slip

text: fault zones

answers: NDQ_003351

answers: oblique convergence

answers: NDQ_003352

answers: vertical thickening

answers: NDQ_003353

answers: oblique shear

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: restraining bend

answers: NDQ_003356

answers: oblique shear

answers: NDQ_003357

answers: shortening perpendicular to the fault plane

answers: NDQ_003358

answers: simple shear

answers: NDQ_003359

answers: shortening

answers: NDQ_003360

answers: plate boundaries

answers: NDQ_003362

answers: pure shear

answers: NDQ_003363

answers: plate boundaries

answers: NDQ_003371

answers: What is a type of strike-slip deformation?

answers: NDQ_003373

answers: oblique shear

answers: NDQ_003376

answers: basin-and-range

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: no

answers: NDQ_003380

answers: What type of force applied to rock is a stress?

answers: NDQ_003381

answers: What is a type of strike-slip deformation

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: What type of fold is a syncline?

answers: NDQ_003385

answers: strike-slip fault zones

answers: NDQ_003386

answers: strike-slip deformation

answers: NDQ_003387

answers: Which of the following is not a type of strike-slip deformation?

answers: NDQ_003388

answers: Which of the following is not a type of strike-slip deformation that deviates from simple shear?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: strike-slip fault

answers: NDQ_003391

answers: strike-slip fault zones

answers: NDQ_003392

answers: strike-slip fault

answers: NDQ_003393

answers: strike-slip fault zones

answers: NDQ_003394

answers: oblique

answers: NDQ_003395

answers: strike-slip fault zones

answers: NDQ_003396

answers: oblique

answers: NDQ_003351

answers: oblique convergence.

answers: NDQ_003352

answers: vertical thickening

answers: NDQ_003353

answers: shortening

answers: NDQ_003354

answers: In geology,

answers: NDQ_003355

answers: restraining bends

answers: NDQ_003356

answers: vertical thickening

answers: NDQ_003357

answers: shortening perpendicular to the fault plane.

answers: NDQ_003358

answers: restraining bends

answers: NDQ_003359

answers: shortening perpendicular to the fault plane.

answers: NDQ_003360

answers: plate boundaries

answers: NDQ_003362

answers: "pure" shortening or "pure" strike-slip.

answers: NDQ_003363

answers: plate boundaries

answers: NDQ_003371

answers: restraining bends in strike-slip fault zones.

answers: NDQ_003373

answers: transpression

answers: NDQ_003376

answers: transpression

answers: NDQ_003378

answers: strike-slip

answers: NDQ_003379

answers: vertical thickening

answers: NDQ_003380

answers: transpression is a type of strike-slip deformation

answers: NDQ_003381

answers: restraining bends

answers: NDQ_003382

answers: shortening perpendicular to the fault plane.

answers: NDQ_003383

answers: restraining bends

answers: NDQ_003384

answers: restraining bends

answers: NDQ_003385

answers: strike-slip fault zones.

answers: NDQ_003386

answers: transpression is a type of strike-slip deformation

answers: NDQ_003387

answers: shortening perpendicular to the fault plane.

answers: NDQ_003388

answers: simple shear

answers: NDQ_003389

answers: vertical thickening

answers: NDQ_003390

answers: strike-slip

answers: NDQ_003391

answers: restraining bends

answers: NDQ_003392

answers: transpression

answers: NDQ_003393

answers: strike-slip fault zones.

answers: NDQ_003394

answers: strike-slip fault zones.

answers: NDQ_003395

answers: strike-slip fault zones.

answers: NDQ_003396

answers: transpression

text: Vocal fold nodules are thought to be the result of vocal fold tissue trauma caused by excessive mechanical stress. During phonation, the vocal folds undergo many forms of mechanical stress. One example of such stress is the impact stress caused by the collision between the left and right vocal fold surfaces during vibration. This stress is thought to reach its maximum in the mid-membranous region of the vocal folds, a common site of nodule formation. Vocal overuse (speaking for long periods), abuse (yelling), or misuse (hyperfunction) may produce excessive amounts of mechanical stress by increasing the rate and/or force with which the vocal folds collide. This may lead to trauma that is focalized to the mid-membranous vocal fold and subsequent wound formation. Repeated or chronic mechanical stress is thought to lead to the remodeling of the superficial layer of the lamina propria. It is this process of tissue remodeling that results in the formation of benign lesions of the vocal folds such as nodules.

text: Vocal fold nodules are thought to be the result of vocal fold tissue trauma caused by excessive

text: mechanical stress

text: . During phonation, the vocal folds undergo many forms of mechanical stress. One example of such stress is the impact stress caused by the collision between the left and right vocal fold surfaces during vibration. This stress is thought to reach its maximum in the mid-membranous region of the vocal folds, a common site of nodule formation. Vocal overuse (speaking for long periods), abuse (yelling), or misuse (hyperfunction) may produce excessive amounts of mechanical stress by increasing the rate and/or force with which the vocal folds collide. This may lead to trauma that is focalized to the mid-membranous vocal fold and subsequent wound formation. Repeated or chronic mechanical stress is thought to lead to the remodeling of the superficial layer of the

text: lamina propria

text: . It is this process of tissue remodeling that results in the formation of benign lesions of the vocal folds such as nodules.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: unanswerable

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: vocal fold

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: the left and right vocal fold surfaces collide

answers: NDQ_003358

answers: nodule

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: unanswerable

answers: NDQ_003363

answers: unanswerable

answers: NDQ_003371

answers: What is a common site of nodule formation?

answers: NDQ_003373

answers: How would you describe compressive stresses?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: Which of the following is not a form of mechanical stress?

answers: NDQ_003381

answers: Which of the following is not a form of mechanical stress?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is a common site of nodule formation?

answers: NDQ_003385

answers: What is the common site of nodule formation?

answers: NDQ_003386

answers: Which of the following is not a cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not a form of mechanical stress?

answers: NDQ_003388

answers: Which of the following is not a form of mechanical stress: impact stress, shear stress, or vibration?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: dip-slip fault plane

answers: NDQ_003392

answers: Fracture

answers: NDQ_003393

answers: dip-slip fault plane

answers: NDQ_003394

answers: non-vertical

answers: NDQ_003395

answers: unanswerable

answers: NDQ_003396

answers: NDQ_003351

answers: impact stress

answers: NDQ_003352

answers: impact stress

answers: NDQ_003353

answers: superficial layer of the lamina propria.

answers: NDQ_003354

answers: Vocal fold nodules

answers: NDQ_003355

answers: Vocal fold nodules

answers: NDQ_003356

answers: Vocal fold nodules

answers: NDQ_003357

answers: (speaking for long periods), abuse (yelling),

answers: NDQ_003358

answers: wound

answers: NDQ_003359

answers: excessive mechanical stress.

answers: NDQ_003360

answers: mechanical stress.

answers: NDQ_003362

answers: Vocal fold nodules

answers: NDQ_003363

answers: excessive mechanical stress.

answers: NDQ_003371

answers: Vocal fold nodules

answers: NDQ_003373

answers: Vocal fold nodules

answers: NDQ_003376

answers: excessive mechanical stress.

answers: NDQ_003378

answers: Vocal fold nodules

answers: NDQ_003379

answers: mid-membranous vocal fold

answers: NDQ_003380

answers: impact stress

answers: NDQ_003381

answers: Vocal fold nodules

answers: NDQ_003382

answers: impact stress

answers: NDQ_003383

answers: Vocal fold nodules

answers: NDQ_003384

answers: Vocal fold nodules

answers: NDQ_003385

answers: mid-membranous vocal fold

answers: NDQ_003386

answers: Vocal fold nodules

answers: NDQ_003387

answers: excessive mechanical stress.

answers: NDQ_003388

answers: Vocal fold nodules

answers: NDQ_003389

answers: Vocal fold nodules

answers: NDQ_003390

answers: Vocal fold nodules

answers: NDQ_003391

answers: Vocal fold nodules

answers: NDQ_003392

answers: Vocal fold nodules

answers: NDQ_003393

answers: Vocal fold nodules

answers: NDQ_003394

answers: Vocal fold nodules

answers: NDQ_003395

answers: left and right vocal fold surfaces

answers: NDQ_003396

answers: Vocal fold nodules

text: The length of time since occurrence and whether or not it is a positive or negative event are factors in whether or not it causes stress and how much stress it causes. Researchers have found that events that have occurred within the past month generally are not linked to stress or illness, while chronic events that occurred more than several months ago are linked to stress and illness  and personality change. Additionally, positive life events are typically not linked to stress—and if so, generally only trivial stress—while negative life events can be linked to stress and the health problems that accompany it. However, positive experiences and positive life changes can predict decreases in neuroticism.

text: The length of time since occurrence and whether or not it is a positive or negative event are factors in whether or not it causes stress and how much stress it causes. Researchers have found that events that have occurred within the past month generally are not linked to stress or illness, while chronic events that occurred more than several months ago are linked to stress and illness  and personality change. Additionally, positive life events are typically not linked to stress—and if so, generally only trivial stress—while negative life events can be linked to stress and the health problems that accompany it. However, positive experiences and positive life changes can predict decreases in neuroticism.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: causes more health problems

answers: NDQ_003353

answers: negative life events

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: negative

answers: NDQ_003356

answers: stress

answers: NDQ_003357

answers: positive experiences and positive life changes can predict decreases in neuroticism

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: stress

answers: NDQ_003362

answers: positive experiences and positive life changes can predict decreases in neuroticism

answers: NDQ_003363

answers: stress

answers: NDQ_003371

answers: what may be a thrust fault in between

answers: NDQ_003373

answers: stress and illness

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: strike-slip fault

answers: NDQ_003380

answers: negative

answers: NDQ_003381

answers: negative

answers: NDQ_003382

answers: negative experiences and positive life changes can predict decreases in neuroticism

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: Fault zone

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: unanswerable

answers: NDQ_003389

answers: process of folding

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: dip-slip fault plane

answers: NDQ_003392

answers: unanswerable

answers: NDQ_003393

answers: a dip-slip fault plane

answers: NDQ_003394

answers: isosceles

answers: NDQ_003395

answers: can cause stress

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: chronic events

answers: NDQ_003352

answers: chronic events

answers: NDQ_003353

answers: illness and personality change.

answers: NDQ_003354

answers: chronic events that occurred more than several months ago

answers: NDQ_003355

answers: chronic events

answers: NDQ_003356

answers: stress and illness and personality change.

answers: NDQ_003357

answers: positive experiences and positive life changes can predict decreases in neuroticism.

answers: NDQ_003358

answers: chronic events

answers: NDQ_003359

answers: positive or negative event

answers: NDQ_003360

answers: chronic events

answers: NDQ_003362

answers: events that have occurred within the past month

answers: NDQ_003363

answers: more than several months ago

answers: NDQ_003371

answers: The length of time since occurrence

answers: NDQ_003373

answers: chronic events

answers: NDQ_003376

answers: chronic events

answers: NDQ_003378

answers: chronic events

answers: NDQ_003379

answers: chronic events that occurred more than several months ago

answers: NDQ_003380

answers: chronic events

answers: NDQ_003381

answers: chronic events

answers: NDQ_003382

answers: chronic events

answers: NDQ_003383

answers: chronic events

answers: NDQ_003384

answers: chronic events

answers: NDQ_003385

answers: stress and illness and personality change.

answers: NDQ_003386

answers: chronic events

answers: NDQ_003387

answers: chronic events

answers: NDQ_003388

answers: chronic events

answers: NDQ_003389

answers: events that have occurred within the past month

answers: NDQ_003390

answers: chronic events

answers: NDQ_003391

answers: chronic events

answers: NDQ_003392

answers: chronic events

answers: NDQ_003393

answers: chronic events

answers: NDQ_003394

answers: linked to stress and illness and personality change.

answers: NDQ_003395

answers: chronic events

answers: NDQ_003396

answers: chronic events

text: Fictional locations vary greatly in their size. Very small places like a single room are kept out of the umbrella of fictional locations by convention, as are most single buildings. A fictional location can be the size of a university (H.P. Lovecraft's Miskatonic University), a town (Stephen King's Salem's Lot), a county (Raintree County), a state (Winnemac in various Sinclair Lewis stories), a large section of continent (as in north-western Middle-earth, which supposedly represents Europe), a whole planet (Anne McCaffrey's Pern), a whole galaxy (Isaac Asimov's Foundation books), even a multiverse (His Dark Materials). In a larger scale, occasionally the term alternate reality is used, but only if it is considered a variant of Earth rather than an original world. Austin Tappan Wright's Islandia has an invented continent, Karain, on our world.

text: Fictional locations vary greatly in their size. Very small places like a single room are kept out of the umbrella of fictional locations by convention, as are most single buildings. A fictional location can be the size of a university (

text: H.P. Lovecraft

text: 's

text: Miskatonic University

text: ), a town (

text: Stephen King

text: 's

text: Salem's Lot

text: ), a county (

text: Raintree County

text: ), a state (

text: Winnemac

text: in various

text: Sinclair Lewis

text: stories), a large section of continent (as in north-western

text: Middle-earth

text: , which supposedly represents Europe), a whole planet (

text: Anne McCaffrey

text: 's

text: Pern

text: ), a whole galaxy (

text: Isaac Asimov

text: 's

text: Foundation

text: books), even a

text: multiverse

text: His Dark Materials

text: ). In a larger scale, occasionally the term

text: alternate reality

text: is used, but only if it is considered a variant of Earth rather than an original world.

text: Austin Tappan Wright

text: 's

text: Islandia

text: has an invented continent, Karain, on our world.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: unanswerable

answers: NDQ_003356

answers: swell

answers: NDQ_003357

answers: Earth is considered a variant of Earth rather than an original world.

answers: NDQ_003358

answers: unanswerable

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: continent

answers: NDQ_003362

answers: the San Andreas fault is on our world

answers: NDQ_003363

answers: Middle-earth

answers: NDQ_003371

answers: What is the term alternate reality used for?

answers: NDQ_003373

answers: None of the above choices

answers: NDQ_003376

answers: basin-and-range

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: strike-slip fault

answers: NDQ_003380

answers: What is an example of a stress?

answers: NDQ_003381

answers: What can be kept out of the umbrella of fictional locations?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: fault zone

answers: NDQ_003386

answers: movement of rock at faults

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: How are strike-slip faults classified?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: Salem's Lot

answers: NDQ_003391

answers: a large section of continent

answers: NDQ_003392

answers: Salem's Lot

answers: NDQ_003393

answers: a large section of continent

answers: NDQ_003394

answers: unanswerable

answers: NDQ_003395

answers: north-western Middle-earth

answers: NDQ_003396

answers: north-western Middle-earth

answers: NDQ_003351

answers: north-western Middle-earth,

answers: NDQ_003352

answers: north-western Middle-earth,

answers: NDQ_003353

answers: continent (as in north-western Middle-earth,

answers: NDQ_003354

answers: Fictional locations vary greatly in their size.

answers: NDQ_003355

answers: alternate reality

answers: NDQ_003356

answers: north-western Middle-earth,

answers: NDQ_003357

answers: alternate reality

answers: NDQ_003358

answers: alternate reality

answers: NDQ_003359

answers: Fictional locations vary greatly in their size.

answers: NDQ_003360

answers: north-western Middle-earth,

answers: NDQ_003362

answers: fictional locations

answers: NDQ_003363

answers: north-western Middle-earth,

answers: NDQ_003371

answers: Fictional locations vary greatly in their size.

answers: NDQ_003373

answers: Fictional locations vary greatly in their size.

answers: NDQ_003376

answers: north-western Middle-earth,

answers: NDQ_003378

answers: Fictional locations vary greatly in their size.

answers: NDQ_003379

answers: north-western Middle-earth,

answers: NDQ_003380

answers: buildings.

answers: NDQ_003381

answers: continent (as in north-western Middle-earth,

answers: NDQ_003382

answers: continent (as in north-western Middle-earth,

answers: NDQ_003383

answers: Fictional locations vary greatly in their size.

answers: NDQ_003384

answers: continent (as in north-western Middle-earth,

answers: NDQ_003385

answers: Fictional locations

answers: NDQ_003386

answers: Fictional locations vary greatly in their size.

answers: NDQ_003387

answers: Fictional locations vary greatly in their size.

answers: NDQ_003388

answers: Fictional locations vary greatly in their size.

answers: NDQ_003389

answers: continent (as in north-western Middle-earth,

answers: NDQ_003390

answers: Fictional locations vary greatly in their size.

answers: NDQ_003391

answers: north-western Middle-earth,

answers: NDQ_003392

answers: Fictional locations vary greatly in their size.

answers: NDQ_003393

answers: north-western Middle-earth,

answers: NDQ_003394

answers: north-western Middle-earth,

answers: NDQ_003395

answers: north-western Middle-earth,

answers: NDQ_003396

answers: north-western Middle-earth,

text: There is no evidence of continued subduction of oceanic crust beneath the Eurasian Plate along this part of the plate boundary, in contrast to the neighbouring segment along the Makran Trench, an active subduction zone, where a dipping slab is well imaged by seismic tomography. The ending of subduction has been linked to evidence that the Main Zagros Reverse Fault is no longer active, suggesting that further deformation is occurring by distributed deformation of the leading edge of the Arabian Plate. This is consistent with observations of recent seismicity.

text: There is no evidence of continued subduction of oceanic crust beneath the Eurasian Plate along this part of the plate boundary, in contrast to the neighbouring segment along the

text: Makran Trench

text: , an active subduction zone, where a dipping slab is well imaged by

text: seismic tomography

text: . The ending of subduction has been linked to evidence that the Main Zagros Reverse Fault is no longer active, suggesting that further deformation is occurring by distributed deformation of the leading edge of the Arabian Plate. This is consistent with observations of recent seismicity.

answers: NDQ_003351

answers: subduction

answers: NDQ_003352

answers: deforms

answers: NDQ_003353

answers: deformation

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: dipping slab

answers: NDQ_003356

answers: dip

answers: NDQ_003357

answers: subduction of oceanic crust beneath the Eurasian Plate

answers: NDQ_003358

answers: active subduction zone

answers: NDQ_003359

answers: deforms

answers: NDQ_003360

answers: Eurasian Plate

answers: NDQ_003362

answers: the Main Zagros Reverse Fault is no longer active

answers: NDQ_003363

answers: Makran Trench

answers: NDQ_003371

answers: What may be the reason for the ending of subduction?

answers: NDQ_003373

answers: subduction of oceanic crust

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: deformation

answers: NDQ_003379

answers: no

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What happens to the leading edge of the Arabian Plate?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the main cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: active subduction zone

answers: NDQ_003386

answers: subduction

answers: NDQ_003387

answers: What type of stress does the Main Zagros Reverse Fault cause?

answers: NDQ_003388

answers: What type of stress does the Main Zagros Reverse Fault result from?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: Main Zagros Reverse Fault

answers: NDQ_003391

answers: dipping slab

answers: NDQ_003392

answers: Reverse Fault

answers: NDQ_003393

answers: dipping slab

answers: NDQ_003394

answers: Main Zagros Reverse Fault

answers: NDQ_003395

answers: Main Zagros Reverse

answers: NDQ_003396

answers: main zagros reverse fault

answers: NDQ_003351

answers: subduction

answers: NDQ_003352

answers: dipping slab

answers: NDQ_003353

answers: dipping slab

answers: NDQ_003354

answers: There is no evidence of continued subduction

answers: NDQ_003355

answers: dipping slab

answers: NDQ_003356

answers: dipping slab

answers: NDQ_003357

answers: dipping slab

answers: NDQ_003358

answers: active subduction zone,

answers: NDQ_003359

answers: subduction

answers: NDQ_003360

answers: subduction

answers: NDQ_003362

answers: active subduction zone,

answers: NDQ_003363

answers: subduction

answers: NDQ_003371

answers: subduction

answers: NDQ_003373

answers: subduction

answers: NDQ_003376

answers: subduction

answers: NDQ_003378

answers: subduction

answers: NDQ_003379

answers: dipping slab

answers: NDQ_003380

answers: deformation

answers: NDQ_003381

answers: subduction

answers: NDQ_003382

answers: subduction

answers: NDQ_003383

answers: subduction

answers: NDQ_003384

answers: subduction

answers: NDQ_003385

answers: active subduction zone,

answers: NDQ_003386

answers: subduction

answers: NDQ_003387

answers: distributed deformation

answers: NDQ_003388

answers: subduction

answers: NDQ_003389

answers: subduction

answers: NDQ_003390

answers: Main Zagros Reverse Fault

answers: NDQ_003391

answers: dipping slab

answers: NDQ_003392

answers: Main Zagros Reverse Fault

answers: NDQ_003393

answers: dipping slab

answers: NDQ_003394

answers: Main Zagros Reverse Fault

answers: NDQ_003395

answers: Main Zagros Reverse Fault

answers: NDQ_003396

answers: Main Zagros Reverse Fault

text: Two common types of forced folds are, namely, fault-bend fold and fault-propagation fold. Folding occurs above the hanging wall of a fold ramp in a fault-bend fold, while folding occurs above the truncation of a thrust fault(fault tip) in a fault-propagation fold. They are usually highly asymmetric with one side of the limb much steeper than the other side, or like monocline. Shortening stress is usually at a high angle to the strata and is concentrated along the slipping plane and in the hanging wall of the thrust fault. A fold acquires higher amplitude, longer wavelength and broader width as rock slips along the fault plane of underlying coeval thrust fault, casting major influence on the three dimensional growth of fold other than stress parameters. Therefore, forced folds are controlled by the fault structure in the basement rocks along planar or listric fault surface and folding of the overlying sedimentary cover only acts as a reaction to underlying fault structure. The amount of fault displacement would control the amplitude of a fold, the lateral growth of fault would implies lateral growth of fold and fault linkage implies fold linkage on the surface. ‘When compared to detachment folds, contrasting competency across strata is not as pronounced and the tectonic environments that they are found in are often more diverse.

text: Two common types of forced folds are, namely,

text: fault-bend fold

text: and

text: fault-propagation fold

text: . Folding occurs above the hanging wall of a fold ramp in a fault-bend fold, while folding occurs above the truncation of a thrust fault(fault tip) in a fault-propagation fold. They are usually highly asymmetric with one side of the limb much steeper than the other side, or like monocline. Shortening stress is usually at a high angle to the strata and is concentrated along the slipping plane and in the hanging wall of the thrust fault. A fold acquires higher amplitude, longer

text: wavelength

text: and broader width as rock slips along the fault plane of underlying coeval thrust fault, casting major influence on the three dimensional growth of fold other than stress parameters. Therefore, forced folds are controlled by the fault structure in the basement rocks along planar or

text: listric fault

text: surface and folding of the overlying sedimentary cover only acts as a reaction to underlying fault structure. The amount of fault displacement would control the amplitude of a fold, the lateral growth of fault would implies lateral growth of fold and fault linkage implies fold linkage on the surface. ‘When compared to detachment folds, contrasting competency across strata is not as pronounced and the tectonic environments that they are found in are often more diverse.

answers: NDQ_003351

answers: Shortening stress

answers: NDQ_003352

answers: slips along the fault

answers: NDQ_003353

answers: Faults

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fault-bend fold

answers: NDQ_003356

answers: slip

answers: NDQ_003357

answers: the hanging wall of the thrust fault

answers: NDQ_003358

answers: detachment fold

answers: NDQ_003359

answers: slips

answers: NDQ_003360

answers: faults

answers: NDQ_003362

answers: contrasting competency across strata is not as pronounced

answers: NDQ_003363

answers: fault-propagation fold

answers: NDQ_003371

answers: What type of fold is a thrust fault?

answers: NDQ_003373

answers: unanswerable

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What is shortening stress?

answers: NDQ_003381

answers: unanswerable

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: unanswerable

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: thrust fault

answers: NDQ_003391

answers: basement rocks

answers: NDQ_003392

answers: thrust fault

answers: NDQ_003393

answers: hanging wall

answers: NDQ_003394

answers: thrust fault

answers: NDQ_003395

answers: thrust fault

answers: NDQ_003396

answers: thrust fault

answers: NDQ_003351

answers: Shortening stress

answers: NDQ_003352

answers: A fold acquires higher amplitude, longer wavelength and broader width

answers: NDQ_003353

answers: A fold acquires higher amplitude, longer wavelength and broader width

answers: NDQ_003354

answers: Two common types of forced folds

answers: NDQ_003355

answers: fault-bend fold

answers: NDQ_003356

answers: A fold acquires higher amplitude, longer wavelength and broader width

answers: NDQ_003357

answers: Shortening stress

answers: NDQ_003358

answers: detachment folds,

answers: NDQ_003359

answers: slips

answers: NDQ_003360

answers: forced folds

answers: NDQ_003362

answers: contrasting competency across strata is not as pronounced

answers: NDQ_003363

answers: forced folds

answers: NDQ_003371

answers: thrust fault(fault

answers: NDQ_003373

answers: forced folds are controlled by the fault structure in the basement rocks

answers: NDQ_003376

answers: detachment folds,

answers: NDQ_003378

answers: slips along the fault plane

answers: NDQ_003379

answers: one side of the limb much steeper than the other side,

answers: NDQ_003380

answers: stress

answers: NDQ_003381

answers: Shortening stress

answers: NDQ_003382

answers: Shortening stress

answers: NDQ_003383

answers: fault linkage

answers: NDQ_003384

answers: monocline.

answers: NDQ_003385

answers: fault-propagation

answers: NDQ_003386

answers: slips along the fault plane

answers: NDQ_003387

answers: Shortening stress

answers: NDQ_003388

answers: thrust fault.

answers: NDQ_003389

answers: folding of the overlying sedimentary cover

answers: NDQ_003390

answers: thrust fault.

answers: NDQ_003391

answers: sedimentary cover

answers: NDQ_003392

answers: fault-bend fold,

answers: NDQ_003393

answers: hanging wall

answers: NDQ_003394

answers: thrust fault(fault

answers: NDQ_003395

answers: coeval thrust fault,

answers: NDQ_003396

answers: monocline.

text: The crystallization order of feldspar and pyroxene (clino- and orthopyroxene) in the gabbros is reversed, and ophiolites also appear to have a multi-phase magmatic complexity on par with subduction zones. Indeed, there is increasing evidence that most ophiolites are generated when subduction begins and thus represent fragments of fore-arc lithosphere. This led to introduction of the term "supra-subduction zone" (SSZ) ophiolite in the 1980s to acknowledge that some ophiolites are more closely related to island arcs than ocean ridges. Consequently, some of the classic ophiolite occurrences  thought of as being related to seafloor spreading (Troodos in Cyprus, Semail in Oman) were found to be "SSZ" ophiolites, formed by rapid extension of fore-arc crust during subduction initiation.

text: The crystallization order of

text: feldspar

text: and

text: pyroxene

text: (clino- and orthopyroxene) in the gabbros is reversed, and ophiolites also appear to have a multi-phase magmatic complexity on par with subduction zones. Indeed, there is increasing evidence that most ophiolites are generated when subduction begins and thus represent fragments of

text: fore-arc

text: lithosphere. This led to introduction of the term "supra-subduction zone" (SSZ) ophiolite in the 1980s to acknowledge that some ophiolites are more closely related to island arcs than ocean ridges. Consequently, some of the classic ophiolite occurrences  thought of as being related to seafloor spreading (Troodos in Cyprus, Semail in Oman) were found to be "SSZ" ophiolites, formed by rapid extension of fore-arc crust during subduction initiation.

answers: NDQ_003351

answers: subduction

answers: NDQ_003352

answers: ophiolites are generated

answers: NDQ_003353

answers: subduction

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: subduction zone

answers: NDQ_003356

answers: subduction

answers: NDQ_003357

answers: rapid extension of fore-arc crust

answers: NDQ_003358

answers: unanswerable

answers: NDQ_003359

answers: subduction begins

answers: NDQ_003360

answers: subduction zones

answers: NDQ_003362

answers: some of the classic ophiolites occurrences thought of as being related to seafloor spreading

answers: NDQ_003363

answers: subduction

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: What is the reason for this?

answers: NDQ_003376

answers: subduction zones

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What type of force applied to rock is a stress?

answers: NDQ_003381

answers: What is the term for ophiolites generated when subduction begins?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: subduction zones

answers: NDQ_003386

answers: subduction

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: unanswerable

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: subduction zone

answers: NDQ_003391

answers: subduction zone

answers: NDQ_003392

answers: Troodos

answers: NDQ_003393

answers: supra-subduction zone

answers: NDQ_003394

answers: subduction zone

answers: NDQ_003395

answers: unanswerable

answers: NDQ_003396

answers: gabbros

answers: NDQ_003351

answers: subduction zones.

answers: NDQ_003352

answers: extension

answers: NDQ_003353

answers: crystallization order

answers: NDQ_003354

answers: The crystallization order

answers: NDQ_003355

answers: fore-arc

answers: NDQ_003356

answers: ophiolites

answers: NDQ_003357

answers: reversed,

answers: NDQ_003358

answers: ophiolites

answers: NDQ_003359

answers: rapid extension

answers: NDQ_003360

answers: subduction zones.

answers: NDQ_003362

answers: reversed,

answers: NDQ_003363

answers: subduction begins

answers: NDQ_003371

answers: subduction zones.

answers: NDQ_003373

answers: subduction zones.

answers: NDQ_003376

answers: subduction zones.

answers: NDQ_003378

answers: subduction zones.

answers: NDQ_003379

answers: reversed,

answers: NDQ_003380

answers: extension of fore-arc crust

answers: NDQ_003381

answers: subduction zones.

answers: NDQ_003382

answers: subduction zones.

answers: NDQ_003383

answers: (clino- and orthopyroxene)

answers: NDQ_003384

answers: "supra-subduction zone"

answers: NDQ_003385

answers: "supra-subduction zone"

answers: NDQ_003386

answers: subduction zones.

answers: NDQ_003387

answers: subduction zones.

answers: NDQ_003388

answers: subduction zones.

answers: NDQ_003389

answers: subduction zones.

answers: NDQ_003390

answers: subduction zones.

answers: NDQ_003391

answers: "supra-subduction zone"

answers: NDQ_003392

answers: subduction zones.

answers: NDQ_003393

answers: "supra-subduction zone"

answers: NDQ_003394

answers: reversed,

answers: NDQ_003395

answers: subduction zones.

answers: NDQ_003396

answers: gabbros

text: Geologic tension is also found in the tectonic regions of divergent boundaries.  Here, a magma chamber forms underneath oceanic crust and causes sea-floor spreading in the creation of new oceanic crust.<ref>Watson, J. M. "Understanding Plate Motions [This Dynamic Earth, USGS]." Understanding Plate Motions. USGS Publications Warehouse, 5 May 1999. Web.

text: Geologic tension is also found in the tectonic regions of

text: divergent boundaries

text: .  Here, a

text: magma chamber

text: forms underneath

text: oceanic crust

text: and causes sea-floor spreading in the creation of new oceanic crust.<ref>Watson, J. M. "Understanding Plate Motions [This Dynamic Earth, USGS]." Understanding Plate Motions. USGS Publications Warehouse, 5 May 1999. Web.

answers: NDQ_003351

answers: magma

answers: NDQ_003352

answers: is more likely to crack

answers: NDQ_003353

answers: earthquakes.

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: horizontal fold

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: a magma chamber forms underneath oceanic crust

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: fractures.

answers: NDQ_003360

answers: plates.

answers: NDQ_003362

answers: sea-floor spreading in the creation of new oceanic crust

answers: NDQ_003363

answers: divergent boundaries

answers: NDQ_003371

answers: What is a thrust fault?

answers: NDQ_003373

answers: Which of the following is an example of a compressive stress?

answers: NDQ_003376

answers: The terrain known as basin-and-range is caused by compressive forces.

answers: NDQ_003378

answers: What is the amount the ground moves in an earthquake?

answers: NDQ_003379

answers: The dip of the fault plane is horizontal.

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What is the result of confining stress?

answers: NDQ_003382

answers: What is the most common stress at divergent plates?

answers: NDQ_003383

answers: What causes joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is the term for an area where faults are clustered?

answers: NDQ_003386

answers: What is the cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not caused by compression stress?

answers: NDQ_003388

answers: How do strike-slip faults form?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: tectonic fault

answers: NDQ_003391

answers: dip-slip fault

answers: NDQ_003392

answers: Fault in which the hanging wall pushes up

answers: NDQ_003393

answers: dip-slip fault

answers: NDQ_003394

answers: Fault with a fault plane

answers: NDQ_003395

answers: Faults with a vertical fault plane

answers: NDQ_003396

answers: elongated

answers: NDQ_003351

answers: Geologic tension

answers: NDQ_003352

answers: sea-floor spreading in the creation of new oceanic crust.

answers: NDQ_003353

answers: sea-floor spreading in the creation of new oceanic crust.

answers: NDQ_003354

answers: Geologic tension

answers: NDQ_003355

answers: Geologic tension

answers: NDQ_003356

answers: Geologic tension

answers: NDQ_003357

answers: a magma chamber forms underneath oceanic crust

answers: NDQ_003358

answers: Geologic tension

answers: NDQ_003359

answers: divergent boundaries.

answers: NDQ_003360

answers: Geologic tension

answers: NDQ_003362

answers: sea-floor spreading in the creation of new oceanic crust.

answers: NDQ_003363

answers: tectonic regions of divergent boundaries.

answers: NDQ_003371

answers: Geologic tension

answers: NDQ_003373

answers: Geologic tension

answers: NDQ_003376

answers: Geologic tension

answers: NDQ_003378

answers: Geologic tension

answers: NDQ_003379

answers: divergent boundaries.

answers: NDQ_003380

answers: tension

answers: NDQ_003381

answers: Geologic tension

answers: NDQ_003382

answers: divergent boundaries.

answers: NDQ_003383

answers: Geologic tension

answers: NDQ_003384

answers: divergent boundaries.

answers: NDQ_003385

answers: tectonic regions of divergent boundaries.

answers: NDQ_003386

answers: Geologic tension

answers: NDQ_003387

answers: Geologic tension

answers: NDQ_003388

answers: Geologic tension

answers: NDQ_003389

answers: Geologic tension

answers: NDQ_003390

answers: Geologic tension

answers: NDQ_003391

answers: magma chamber

answers: NDQ_003392

answers: Geologic tension

answers: NDQ_003393

answers: oceanic crust

answers: NDQ_003394

answers: divergent boundaries.

answers: NDQ_003395

answers: divergent boundaries.

answers: NDQ_003396

answers: divergent boundaries.

text: The oldest rocks are hard, grey, often shelly, Carboniferous limestones. These were laid down in a warm, shallow sea during the early part of the Carboniferous Period when Wales lay just south of the equator. Subsequent earth movements have folded and fractured the crust, and during the next 100 million years they suffered extensive erosion. These earth movements left the upfolded Carboniferous limestones as an area of high ground, extending through what is now the Vale of Glamorgan.

text: The oldest rocks are hard, grey, often shelly,

text: Carboniferous limestones

text: . These were laid down in a warm, shallow sea during the early part of the

text: Carboniferous

text: Period when

text: Wales

text: lay just south of the equator. Subsequent earth movements have folded and fractured the crust, and during the next 100 million years they suffered extensive erosion. These earth movements left the upfolded Carboniferous limestones as an area of high ground, extending through what is now the

text: Vale of Glamorgan

answers: NDQ_003351

answers: earthquakes

answers: NDQ_003352

answers: more likely to crack

answers: NDQ_003353

answers: Earth movements

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: upfolded

answers: NDQ_003356

answers: fold

answers: NDQ_003357

answers: earth movements have folded and fractured the crust

answers: NDQ_003358

answers: high ground

answers: NDQ_003359

answers: folds

answers: NDQ_003360

answers: earth movements

answers: NDQ_003362

answers: the San Andreas fault is located in the Pacific Ocean

answers: NDQ_003363

answers: Carboniferous Period

answers: NDQ_003371

answers: Which of the following is not a type of rock: Carboniferous limestones, upfolded Carboniferous limestones, or limestones?

answers: NDQ_003373

answers: How would you describe a rock that is deeply buried?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What type of force applied to rock is a stress?

answers: NDQ_003381

answers: Which of the following is not a type of rock: Carboniferous limestones, upfolded limestones, or Wales lay just south of the equator?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not a type of fold: Carboniferous limestones, upfolded Carboniferous limestones or Vale of Glamorgan?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: Which of the following is not the cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not a type of normal fault?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip, strike-slip, or strike-slip?

answers: NDQ_003389

answers: It's impossible to say

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: Vale of Glamorgan

answers: NDQ_003392

answers: upfolded Carboniferous limestones

answers: NDQ_003393

answers: high ground

answers: NDQ_003394

answers: undefined

answers: NDQ_003395

answers: fault with a vertical fault plane

answers: NDQ_003396

answers: Vale of Glamorgan

answers: NDQ_003351

answers: erosion.

answers: NDQ_003352

answers: erosion.

answers: NDQ_003353

answers: fractured the crust,

answers: NDQ_003354

answers: Carboniferous limestones

answers: NDQ_003355

answers: upfolded

answers: NDQ_003356

answers: erosion.

answers: NDQ_003357

answers: fractured the crust,

answers: NDQ_003358

answers: erosion.

answers: NDQ_003359

answers: earth movements

answers: NDQ_003360

answers: earth movements

answers: NDQ_003362

answers: Wales lay just south of the equator.

answers: NDQ_003363

answers: Wales lay just south of the equator.

answers: NDQ_003371

answers: earth movements

answers: NDQ_003373

answers: earth movements

answers: NDQ_003376

answers: earth movements

answers: NDQ_003378

answers: earth movements have folded and fractured the crust,

answers: NDQ_003379

answers: south of the equator.

answers: NDQ_003380

answers: erosion.

answers: NDQ_003381

answers: fractured the crust,

answers: NDQ_003382

answers: erosion.

answers: NDQ_003383

answers: earth movements

answers: NDQ_003384

answers: the upfolded

answers: NDQ_003385

answers: folded and fractured the crust,

answers: NDQ_003386

answers: earth movements

answers: NDQ_003387

answers: earth movements

answers: NDQ_003388

answers: folded and fractured the crust,

answers: NDQ_003389

answers: earth movements

answers: NDQ_003390

answers: erosion.

answers: NDQ_003391

answers: Carboniferous limestones

answers: NDQ_003392

answers: the upfolded

answers: NDQ_003393

answers: high ground,

answers: NDQ_003394

answers: folded and fractured the crust,

answers: NDQ_003395

answers: folded and fractured the crust,

answers: NDQ_003396

answers: south of the equator.

text: Major changes came to the conference in 1992. First, Akron left for the Mid-American Conference (MAC) and was replaced by another Ohio school, Youngstown State University. More significantly, the Mid-Continent added women's sports by absorbing the North Star Conference (NSC), a women's-only league whose final seven members had all been in the Mid-Continent. All of the final NSC members except for Akron moved their women's sports into the Mid-Continent. At the same time, Eastern Illinois and Western Illinois moved their women's sports into the Mid-Continent when their former women's sports home, the Gateway Conference, merged into the Missouri Valley Conference. A year later, the University of Wisconsin–Milwaukee joined the Mid-Continent.

text: Major changes came to the conference in 1992. First, Akron left for the

text: Mid-American Conference

text: (MAC) and was replaced by another Ohio school,

text: Youngstown State University

text: . More significantly, the Mid-Continent added women's sports by absorbing the

text: North Star Conference

text: (NSC), a women's-only league whose final seven members had all been in the Mid-Continent. All of the final NSC members except for Akron moved their women's sports into the Mid-Continent. At the same time, Eastern Illinois and Western Illinois moved their women's sports into the Mid-Continent when their former women's sports home, the

text: Gateway Conference

text: , merged into the

text: Missouri Valley Conference

text: . A year later, the

text: University of Wisconsin–Milwaukee

text: joined the Mid-Continent.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: is likely to crack

answers: NDQ_003353

answers: igneous rocks to form

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: unanswerable

answers: NDQ_003356

answers: swell

answers: NDQ_003357

answers: Akron left for the Mid-American Conference

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: Akron left for the Mid-American Conference (MAC)

answers: NDQ_003363

answers: Mid-Continent

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: What is the best title for this passage?

answers: NDQ_003376

answers: What type of terrain is caused by compressive forces?

answers: NDQ_003378

answers: What did the Mid-Continent add women's sports by absorbing?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: How would you describe Youngstown State University?

answers: NDQ_003381

answers: What happened to Akron in 1992?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: what is the last word in the passage?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: What type of movement of rock at faults is the cause of earthquakes?

answers: NDQ_003387

answers: Which happened first, Akron left for the Mid-American Conference (MAC) or the University of Wisconsin–Milwaukee joined the Mid-Continent?

answers: NDQ_003388

answers: Which happened first, Akron left for the Mid-American Conference (MAC) or the University of Wisconsin–Milwaukee joined the Mid-Continent?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: unanswerable

answers: NDQ_003392

answers: unanswerable

answers: NDQ_003393

answers: dip-slip fault plane

answers: NDQ_003394

answers: unanswerable

answers: NDQ_003395

answers: unanswerable

answers: NDQ_003396

answers: Missouri Valley Conference

answers: NDQ_003351

answers: women's sports by absorbing the North Star Conference

answers: NDQ_003352

answers: North Star Conference

answers: NDQ_003353

answers: North Star Conference

answers: NDQ_003354

answers: Major changes came to the conference in 1992.

answers: NDQ_003355

answers: North Star Conference

answers: NDQ_003356

answers: North Star Conference

answers: NDQ_003357

answers: Akron moved their women's sports into the Mid-Continent.

answers: NDQ_003358

answers: Mid-American Conference

answers: NDQ_003359

answers: North Star Conference

answers: NDQ_003360

answers: North Star Conference

answers: NDQ_003362

answers: Major changes came to the conference in 1992.

answers: NDQ_003363

answers: Mid-Continent

answers: NDQ_003371

answers: Major changes came to the conference in 1992.

answers: NDQ_003373

answers: Major changes came to the conference in 1992.

answers: NDQ_003376

answers: North Star Conference

answers: NDQ_003378

answers: North Star Conference

answers: NDQ_003379

answers: North Star Conference

answers: NDQ_003380

answers: 1992. First, Akron left for the Mid-American Conference

answers: NDQ_003381

answers: North Star Conference

answers: NDQ_003382

answers: women's sports by absorbing the North Star Conference

answers: NDQ_003383

answers: North Star Conference

answers: NDQ_003384

answers: North Star Conference

answers: NDQ_003385

answers: Mid-American Conference

answers: NDQ_003386

answers: Mid-American Conference

answers: NDQ_003387

answers: North Star Conference

answers: NDQ_003388

answers: North Star Conference

answers: NDQ_003389

answers: North Star Conference

answers: NDQ_003390

answers: Mid-American Conference

answers: NDQ_003391

answers: North Star Conference

answers: NDQ_003392

answers: North Star Conference

answers: NDQ_003393

answers: North Star Conference

answers: NDQ_003394

answers: North Star Conference

answers: NDQ_003395

answers: North Star Conference

answers: NDQ_003396

answers: North Star Conference

text: Geological structures can be mapped by observing how they affect seismic waves from local and distant earthquakes, a process known as seismic tomography.  The density of the TA network — typical station spacing of about 70 km — provides a level of resolution not previously available in many parts of the country, and is providing finer details of the lithosphere under parts of North America.

text: Geological structures can be mapped by observing how they affect seismic waves from local and distant earthquakes, a process known as

text: seismic tomography

text: .  The density of the TA network — typical station spacing of about 70 km — provides a level of resolution not previously available in many parts of the country, and is providing finer details of the

text: lithosphere

text: under parts of North America.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: affect seismic waves

answers: NDQ_003357

answers: seismic waves from local and distant earthquakes

answers: NDQ_003358

answers: unmoving

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: earthquakes

answers: NDQ_003362

answers: the density of the TA network — typical station spacing of about 70 km

answers: NDQ_003363

answers: North America

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: What is the density of the TA network?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: what is the density of the TA network

answers: NDQ_003379

answers: what is the density of the TA network

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What does the density of the TA network provide?

answers: NDQ_003382

answers: what is the most common stress at convergent plates

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: What is the density of the TA network?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip, strike-slip, or strike-slip?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: seismic tomography

answers: NDQ_003391

answers: lithosphere

answers: NDQ_003392

answers: a hanging wall

answers: NDQ_003393

answers: lithosphere

answers: NDQ_003394

answers: lateral

answers: NDQ_003395

answers: is a process known as seismic tomography

answers: NDQ_003396

answers: TA network

answers: NDQ_003351

answers: earthquakes,

answers: NDQ_003352

answers: lithosphere

answers: NDQ_003353

answers: seismic waves

answers: NDQ_003354

answers: Geological structures can be mapped by observing how they affect seismic waves

answers: NDQ_003355

answers: Geological structures

answers: NDQ_003356

answers: seismic waves from local and distant earthquakes,

answers: NDQ_003357

answers: seismic waves

answers: NDQ_003358

answers: earthquakes,

answers: NDQ_003359

answers: earthquakes,

answers: NDQ_003360

answers: earthquakes,

answers: NDQ_003362

answers: Geological structures can be mapped by observing how they affect seismic waves

answers: NDQ_003363

answers: earthquakes,

answers: NDQ_003371

answers: Geological structures can be mapped by observing how they affect seismic waves

answers: NDQ_003373

answers: lithosphere

answers: NDQ_003376

answers: Geological structures can be mapped by observing how they affect seismic waves

answers: NDQ_003378

answers: seismic tomography.

answers: NDQ_003379

answers: seismic tomography.

answers: NDQ_003380

answers: Geological structures can be mapped by observing how they affect seismic waves

answers: NDQ_003381

answers: Geological structures can be mapped by observing how they affect seismic waves

answers: NDQ_003382

answers: seismic tomography.

answers: NDQ_003383

answers: Geological structures can be mapped by observing how they affect seismic waves

answers: NDQ_003384

answers: seismic tomography.

answers: NDQ_003385

answers: seismic tomography.

answers: NDQ_003386

answers: Geological structures can be mapped by observing how they affect seismic waves

answers: NDQ_003387

answers: Geological structures can be mapped by observing how they affect seismic waves

answers: NDQ_003388

answers: Geological structures

answers: NDQ_003389

answers: Geological structures

answers: NDQ_003390

answers: seismic tomography.

answers: NDQ_003391

answers: lithosphere

answers: NDQ_003392

answers: seismic tomography.

answers: NDQ_003393

answers: lithosphere

answers: NDQ_003394

answers: earthquakes,

answers: NDQ_003395

answers: earthquakes,

answers: NDQ_003396

answers: seismic tomography.

text: Leaflets that are folded are usually used for advertising or marketing purposes, or for information supplementary to labels. There are many types of folds; only the most popular types are listed here. Although it is difficult to put a date on when some of these folds were first used, it is evident that their popularity boomed when the first mass production printers were introduced.

text: Leaflets that are folded are usually used for advertising or marketing purposes, or for information supplementary to

text: label

text: s. There are many types of folds; only the most popular types are listed here. Although it is difficult to put a date on when some of these folds were first used, it is evident that their popularity boomed when the first mass production printers were introduced.

answers: NDQ_003351

answers: folds

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: erosion

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: type of fold

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: mass production printers were introduced

answers: NDQ_003358

answers: rockfall

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: it is difficult to put a date when some of these folds were first used

answers: NDQ_003363

answers: the same time

answers: NDQ_003371

answers: What is the most common type of fold?

answers: NDQ_003373

answers: how would you describe compressive stresses?

answers: NDQ_003376

answers: compressive forces

answers: NDQ_003378

answers: the amount the ground moves in an earthquake

answers: NDQ_003379

answers: answer: vertical

answers: NDQ_003380

answers: What is the most common type of fold?

answers: NDQ_003381

answers: how does rock deform?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: What does stress cause in rock?

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: what is the first mass production printers introduced

answers: NDQ_003386

answers: movement of rock at faults

answers: NDQ_003387

answers: Which of the following is not a type of fold?

answers: NDQ_003388

answers: Which of the following is not a type of fold?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: dip-slip fault

answers: NDQ_003392

answers: unanswerable

answers: NDQ_003393

answers: dip-slip fault plane

answers: NDQ_003394

answers: isosceles

answers: NDQ_003395

answers: is a type of fault

answers: NDQ_003396

answers: NDQ_003351

answers: Leaflets

answers: NDQ_003352

answers: mass production printers

answers: NDQ_003353

answers: Leaflets that are folded

answers: NDQ_003354

answers: their popularity boomed when the first mass production printers were introduced.

answers: NDQ_003355

answers: Leaflets

answers: NDQ_003356

answers: mass production printers

answers: NDQ_003357

answers: Leaflets that are folded are usually used for advertising or marketing purposes,

answers: NDQ_003358

answers: Leaflets

answers: NDQ_003359

answers: first mass production printers were introduced.

answers: NDQ_003360

answers: first mass production printers were introduced.

answers: NDQ_003362

answers: Leaflets that are folded are usually used for advertising or marketing purposes,

answers: NDQ_003363

answers: first mass production printers were introduced.

answers: NDQ_003371

answers: Leaflets that are folded are usually used for advertising or marketing purposes,

answers: NDQ_003373

answers: Leaflets

answers: NDQ_003376

answers: first mass production printers

answers: NDQ_003378

answers: Leaflets that are folded

answers: NDQ_003379

answers: mass production printers

answers: NDQ_003380

answers: Leaflets

answers: NDQ_003381

answers: mass production printers

answers: NDQ_003382

answers: Leaflets that are folded are usually used for advertising or marketing purposes,

answers: NDQ_003383

answers: Leaflets

answers: NDQ_003384

answers: many types of folds;

answers: NDQ_003385

answers: Leaflets

answers: NDQ_003386

answers: Leaflets

answers: NDQ_003387

answers: first mass production printers

answers: NDQ_003388

answers: Leaflets that are folded

answers: NDQ_003389

answers: Leaflets

answers: NDQ_003390

answers: Leaflets that are folded are usually used for advertising or marketing purposes,

answers: NDQ_003391

answers: Leaflets that are folded

answers: NDQ_003392

answers: Leaflets

answers: NDQ_003393

answers: Leaflets

answers: NDQ_003394

answers: Leaflets

answers: NDQ_003395

answers: Leaflets that are folded are usually used for advertising or marketing purposes,

answers: NDQ_003396

answers: Leaflets

text: Another area of application for Poisson's effect is in the realm of structural geology. Rocks, like most materials, are subject to Poisson's effect while under stress. In a geological timescale, excessive erosion or sedimentation of Earth's crust can either create or remove large vertical stresses upon the underlying rock. This rock will expand or contract in the vertical direction as a direct result of the applied stress, and it will also deform in the horizontal direction as a result of Poisson's effect. This change in strain in the horizontal direction can affect or form joints and dormant stresses in the rock.

text: Another area of application for Poisson's effect is in the realm of

text: structural geology

text: . Rocks, like most materials, are subject to Poisson's effect while under stress. In a geological timescale, excessive erosion or sedimentation of Earth's crust can either create or remove large vertical stresses upon the underlying rock. This rock will expand or contract in the vertical direction as a direct result of the applied stress, and it will also deform in the horizontal direction as a result of Poisson's effect. This change in strain in the horizontal direction can affect or form joints and dormant stresses in the rock.

answers: NDQ_003351

answers: large vertical stresses

answers: NDQ_003352

answers: expand or contract in the vertical direction

answers: NDQ_003353

answers: expansion or contraction

answers: NDQ_003354

answers: Toroweap Formation is the underlying rock

answers: NDQ_003355

answers: horizontal direction

answers: NDQ_003356

answers: expand or contract

answers: NDQ_003357

answers: horizontal direction can affect or form joints and dormant stresses

answers: NDQ_003358

answers: joints

answers: NDQ_003359

answers: under stress

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: rocks are subject to Poisson's effect while under stress

answers: NDQ_003363

answers: Poisson's effect

answers: NDQ_003371

answers: What can joints and dormant stresses form?

answers: NDQ_003373

answers: It will expand or contract in the vertical direction

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: horizontal direction

answers: NDQ_003380

answers: Yes

answers: NDQ_003381

answers: Which of the following is not a result of Poisson's effect?

answers: NDQ_003382

answers: what is the most common stress at convergent plates

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: Which of the following is not a cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not a cause of normal faults?

answers: NDQ_003388

answers: Which of the following is not a form of Poisson's effect?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: Poisson's

answers: NDQ_003391

answers: underlying rock

answers: NDQ_003392

answers: horizontal direction

answers: NDQ_003393

answers: underlying rock

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: Poisson's effect

answers: NDQ_003396

answers: Poisson's effect

answers: NDQ_003351

answers: excessive erosion

answers: NDQ_003352

answers: expand or contract in the vertical direction

answers: NDQ_003353

answers: expand or contract in the vertical direction

answers: NDQ_003354

answers: Poisson's effect is in the realm of structural geology.

answers: NDQ_003355

answers: joints

answers: NDQ_003356

answers: joints and dormant stresses

answers: NDQ_003357

answers: large vertical stresses upon the underlying rock.

answers: NDQ_003358

answers: joints and dormant stresses

answers: NDQ_003359

answers: stress.

answers: NDQ_003360

answers: excessive erosion or sedimentation of Earth's crust

answers: NDQ_003362

answers: Poisson's effect is in the realm of structural geology.

answers: NDQ_003363

answers: excessive erosion or sedimentation of Earth's crust

answers: NDQ_003371

answers: Poisson's effect is in the realm of structural geology.

answers: NDQ_003373

answers: vertical stresses upon the underlying rock.

answers: NDQ_003376

answers: excessive erosion

answers: NDQ_003378

answers: expand or contract in the vertical direction

answers: NDQ_003379

answers: vertical

answers: NDQ_003380

answers: stress.

answers: NDQ_003381

answers: horizontal direction

answers: NDQ_003382

answers: vertical stresses upon the underlying rock.

answers: NDQ_003383

answers: change in strain in the horizontal direction

answers: NDQ_003384

answers: structural geology.

answers: NDQ_003385

answers: structural geology.

answers: NDQ_003386

answers: Poisson's effect is in the realm of structural geology.

answers: NDQ_003387

answers: vertical stresses upon the underlying rock.

answers: NDQ_003388

answers: Poisson's effect is in the realm of structural geology.

answers: NDQ_003389

answers: erosion

answers: NDQ_003390

answers: Poisson's effect is in the realm of structural geology.

answers: NDQ_003391

answers: underlying rock.

answers: NDQ_003392

answers: Poisson's effect is in the realm of structural geology.

answers: NDQ_003393

answers: joints and dormant stresses

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: expand or contract in the vertical direction

answers: NDQ_003396

answers: deform in the horizontal direction

text: The subducted oceanic crust triggers volcanism, although the basic mechanisms are varied. Volcanism  may occur due to processes that add buoyancy to partially melted mantle causing an upward flow due to a decrease in density of the partial melt.

text: The subducted oceanic crust triggers

text: volcanism

text: , although the basic mechanisms are varied. Volcanism  may occur due to processes that add buoyancy to partially melted mantle causing an upward flow due to a decrease in density of the partial melt.

answers: NDQ_003351

answers: Volcanism

answers: NDQ_003352

answers: decreases in size

answers: NDQ_003353

answers: density to decrease

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: volcanism

answers: NDQ_003356

answers: decrease in density

answers: NDQ_003357

answers: Volcanism may occur due to processes that add buoyancy to partially melted mantle

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: is subducted

answers: NDQ_003360

answers: Volcanism

answers: NDQ_003362

answers: Volcanism may occur due to processes that add buoyancy to partially melted mantle

answers: NDQ_003363

answers: subducted oceanic crust

answers: NDQ_003371

answers: What may occur due to processes that add buoyancy to partially melted mantle?

answers: NDQ_003373

answers: How would you describe a subducted oceanic crust?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: Which of the following is not a process that add buoyancy to partially melted mantle?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not an example of a fold that arches upward?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: Which of the following is not the cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: Volcanism or normal faults?

answers: NDQ_003388

answers: Which of the following is not a result of shear stress: strike-slip faults, subducted oceanic crust, or volcanism?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: Volcanism

answers: NDQ_003391

answers: subducted oceanic crust

answers: NDQ_003392

answers: Volcanism

answers: NDQ_003393

answers: subducted oceanic crust

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: unanswerable

answers: NDQ_003396

answers: horizontal

answers: NDQ_003351

answers: volcanism,

answers: NDQ_003352

answers: upward flow due to a decrease in density

answers: NDQ_003353

answers: buoyancy

answers: NDQ_003354

answers: The subducted oceanic crust triggers volcanism,

answers: NDQ_003355

answers: volcanism,

answers: NDQ_003356

answers: buoyancy

answers: NDQ_003357

answers: upward flow

answers: NDQ_003358

answers: The subducted oceanic crust triggers volcanism,

answers: NDQ_003359

answers: The subducted oceanic crust triggers volcanism,

answers: NDQ_003360

answers: volcanism,

answers: NDQ_003362

answers: The subducted oceanic crust triggers volcanism,

answers: NDQ_003363

answers: subducted oceanic crust triggers volcanism,

answers: NDQ_003371

answers: The subducted oceanic crust triggers volcanism,

answers: NDQ_003373

answers: The subducted oceanic crust triggers volcanism,

answers: NDQ_003376

answers: The subducted oceanic crust triggers volcanism,

answers: NDQ_003378

answers: volcanism,

answers: NDQ_003379

answers: The subducted oceanic crust triggers volcanism,

answers: NDQ_003380

answers: Volcanism may occur due to processes that add buoyancy

answers: NDQ_003381

answers: The subducted oceanic crust triggers volcanism,

answers: NDQ_003382

answers: volcanism,

answers: NDQ_003383

answers: The subducted oceanic crust triggers volcanism,

answers: NDQ_003384

answers: The subducted oceanic crust triggers volcanism,

answers: NDQ_003385

answers: The subducted oceanic crust triggers volcanism,

answers: NDQ_003386

answers: The subducted oceanic crust triggers volcanism,

answers: NDQ_003387

answers: The subducted oceanic crust triggers volcanism,

answers: NDQ_003388

answers: The subducted oceanic crust triggers volcanism,

answers: NDQ_003389

answers: The subducted oceanic crust triggers volcanism,

answers: NDQ_003390

answers: The subducted oceanic crust triggers volcanism,

answers: NDQ_003391

answers: oceanic crust

answers: NDQ_003392

answers: volcanism,

answers: NDQ_003393

answers: The subducted oceanic crust triggers volcanism,

answers: NDQ_003394

answers: The subducted oceanic crust triggers volcanism,

answers: NDQ_003395

answers: The subducted oceanic crust triggers volcanism,

answers: NDQ_003396

answers: volcanism,

text: As new seafloor forms and spreads apart from the mid-ocean ridge it slowly cools over time. Older seafloor is therefore colder than new seafloor, and older oceanic basins deeper than new oceanic basins due to isostasy. If the diameter of the earth remains relatively constant despite the production of new crust, a mechanism must exist by which crust is also destroyed. The destruction of oceanic crust occurs at subduction zones where oceanic crust is forced under either continental crust or oceanic crust. Today, the Atlantic basin is actively spreading at the Mid-Atlantic Ridge. Only a small portion of the oceanic crust produced in the Atlantic is subducted. However, the plates making up the Pacific Ocean are experiencing subduction along many of their boundaries which causes the volcanic activity in what has been termed the Ring of Fire of the Pacific Ocean. The Pacific is also home to one of the world's most active spreading centres (the East Pacific Rise) with spreading rates of up to 13 cm/yr. The Mid-Atlantic Ridge is a "textbook" slow-spreading centre, while the East Pacific Rise is used as an example of fast spreading. The differences in spreading rates affect not only the geometries of the ridges but also the geochemistry of the basalts that are produced.

text: As new seafloor forms and spreads apart from the

text: mid-ocean ridge

text: it slowly cools over time. Older seafloor is therefore colder than new seafloor, and older oceanic basins deeper than new oceanic basins due to

text: isostasy

text: . If the diameter of the earth remains relatively constant despite the production of new crust, a mechanism must exist by which crust is also destroyed. The destruction of oceanic crust occurs at

text: subduction

text: zones where oceanic crust is forced under either continental crust or oceanic crust. Today, the Atlantic basin is actively spreading at the Mid-Atlantic Ridge. Only a small portion of the oceanic crust produced in the Atlantic is subducted. However, the plates making up the Pacific Ocean are experiencing subduction along many of their boundaries which causes the volcanic activity in what has been termed the

text: Ring of Fire

text: of the Pacific Ocean. The Pacific is also home to one of the world's most active spreading centres (the

text: East Pacific Rise

text: ) with spreading rates of up to 13 cm/yr. The Mid-Atlantic Ridge is a "

text: textbook

text: " slow-spreading centre, while the East Pacific Rise is used as an example of fast spreading. The differences in spreading rates affect not only the geometries of the ridges but also the geochemistry of the basalts that are produced.

answers: NDQ_003351

answers: subduction

answers: NDQ_003352

answers: subducts

answers: NDQ_003353

answers: subduction

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: ridge

answers: NDQ_003356

answers: subduct

answers: NDQ_003357

answers: oceanic crust is forced under either continental crust or oceanic crust

answers: NDQ_003358

answers: unanswerable

answers: NDQ_003359

answers: subducts

answers: NDQ_003360

answers: continental plates

answers: NDQ_003362

answers: Older seafloor is therefore colder than new seafloor

answers: NDQ_003363

answers: Subduction zones

answers: NDQ_003371

answers: What causes the volcanic activity in what has been termed the Ring of Fire

answers: NDQ_003373

answers: Why is older seafloor is therefore colder than new seafloor?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What does the destruction of oceanic crust occur at?

answers: NDQ_003381

answers: What does the destruction of oceanic crust occur at?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: unanswerable

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: What causes the volcanic activity in what has been termed the Ring of Fire of the Pacific Ocean?

answers: NDQ_003388

answers: What causes the volcanic activity in what has been termed the Ring of Fire of the Pacific Ocean?

answers: NDQ_003389

answers: subduction

answers: NDQ_003390

answers: subduction zones

answers: NDQ_003391

answers: subduction zones

answers: NDQ_003392

answers: subduction zones

answers: NDQ_003393

answers: subduction zones

answers: NDQ_003394

answers: subduction zones

answers: NDQ_003395

answers: subduction zones

answers: NDQ_003396

answers: subduction zones

answers: NDQ_003351

answers: subduction

answers: NDQ_003352

answers: cools over time.

answers: NDQ_003353

answers: subduction zones

answers: NDQ_003354

answers: Older seafloor is therefore colder than new seafloor,

answers: NDQ_003355

answers: subduction zones

answers: NDQ_003356

answers: subduction zones

answers: NDQ_003357

answers: subduction zones

answers: NDQ_003358

answers: subduction zones

answers: NDQ_003359

answers: destroyed.

answers: NDQ_003360

answers: subduction zones

answers: NDQ_003362

answers: Older seafloor is therefore colder than new seafloor,

answers: NDQ_003363

answers: mid-ocean ridge

answers: NDQ_003371

answers: subduction zones

answers: NDQ_003373

answers: isostasy.

answers: NDQ_003376

answers: older oceanic basins deeper than new oceanic basins

answers: NDQ_003378

answers: 13 cm/yr.

answers: NDQ_003379

answers: 13 cm/yr.

answers: NDQ_003380

answers: destroyed.

answers: NDQ_003381

answers: The destruction of oceanic crust occurs at subduction zones

answers: NDQ_003382

answers: subduction zones

answers: NDQ_003383

answers: subduction

answers: NDQ_003384

answers: mid-ocean ridge

answers: NDQ_003385

answers: subduction zones

answers: NDQ_003386

answers: The destruction of oceanic crust occurs at subduction zones

answers: NDQ_003387

answers: subduction zones

answers: NDQ_003388

answers: subduction zones

answers: NDQ_003389

answers: subduction zones

answers: NDQ_003390

answers: subduction zones

answers: NDQ_003391

answers: subduction zones

answers: NDQ_003392

answers: subduction zones

answers: NDQ_003393

answers: subduction zones

answers: NDQ_003394

answers: subduction zones

answers: NDQ_003395

answers: subduction zones

answers: NDQ_003396

answers: subduction zones

text: Asylum decisions in the UK based on particular social groups have stressed the need to make a two-fold case:

text: Asylum decisions in the UK based on particular social groups have stressed the need to make a two-fold case:

answers: NDQ_003351

answers: lateral

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation is a geologic formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: Asylum decisions in the UK based on particular social groups have stressed the need

answers: NDQ_003358

answers: rockfall

answers: NDQ_003359

answers: breaks apart.

answers: NDQ_003360

answers: continental plates.

answers: NDQ_003362

answers: The San Andreas fault is not a fault.

answers: NDQ_003363

answers: volcanoes

answers: NDQ_003371

answers: What is a thrust fault?

answers: NDQ_003373

answers: What is the best way to describe this situation?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: The amount the ground moves in an earthquake is called slip

answers: NDQ_003379

answers: The dip of the fault plane is horizontal.

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: Which of the following is not a type of stress?

answers: NDQ_003382

answers: description

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: Faults are clustered where there are fault lines.

answers: NDQ_003386

answers: (4).

answers: NDQ_003387

answers: None of the above choices.

answers: NDQ_003388

answers: Which of the following is not an example of shear stress?

answers: NDQ_003389

answers: None of the above choices .

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: is a crater

answers: NDQ_003392

answers: unanswerable

answers: NDQ_003393

answers: is a crater

answers: NDQ_003394

answers: isosceles

answers: NDQ_003395

answers: NDQ_003396

answers: NDQ_003351

answers: two-fold case:

answers: NDQ_003352

answers: two-fold

answers: NDQ_003353

answers: two-fold case:

answers: NDQ_003354

answers: two-fold case:

answers: NDQ_003355

answers: two-fold

answers: NDQ_003356

answers: two-fold case:

answers: NDQ_003357

answers: two-fold case:

answers: NDQ_003358

answers: two-fold

answers: NDQ_003359

answers: two-fold case:

answers: NDQ_003360

answers: Asylum decisions in the UK based on particular social groups

answers: NDQ_003362

answers: Asylum decisions in the UK based on particular social groups

answers: NDQ_003363

answers: Asylum decisions in the UK based on particular social groups

answers: NDQ_003371

answers: Asylum decisions in the UK based on particular social groups

answers: NDQ_003373

answers: Asylum decisions in the UK

answers: NDQ_003376

answers: Asylum decisions in the UK

answers: NDQ_003378

answers: two-fold case:

answers: NDQ_003379

answers: two-fold case:

answers: NDQ_003380

answers: stressed the need to make a two-fold case:

answers: NDQ_003381

answers: Asylum decisions in the UK based on particular social groups

answers: NDQ_003382

answers: two-fold case:

answers: NDQ_003383

answers: Asylum decisions in the UK based on particular social groups

answers: NDQ_003384

answers: two-fold

answers: NDQ_003385

answers: two-fold case:

answers: NDQ_003386

answers: Asylum decisions in the UK

answers: NDQ_003387

answers: Asylum decisions in the UK based on particular social groups

answers: NDQ_003388

answers: Asylum decisions in the UK based on particular social groups

answers: NDQ_003389

answers: two-fold

answers: NDQ_003390

answers: two-fold case:

answers: NDQ_003391

answers: two-fold case:

answers: NDQ_003392

answers: two-fold case:

answers: NDQ_003393

answers: two-fold case:

answers: NDQ_003394

answers: two-fold case:

answers: NDQ_003395

answers: two-fold case:

answers: NDQ_003396

answers: two-fold case:

text: The geometrical properties of conjugate faults are indicative of the sense of stress, but they may not appear in the actual fault patterns.

text: The geometrical properties of conjugate faults are indicative of the sense of stress, but they may not appear in the actual fault patterns.

answers: NDQ_003351

answers: conjugate

answers: NDQ_003352

answers: is more likely to crack

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation is a formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: shrink

answers: NDQ_003357

answers: the geometrical properties are indicative of

answers: NDQ_003358

answers: unmoving fault

answers: NDQ_003359

answers: stress is applied to it

answers: NDQ_003360

answers: faults

answers: NDQ_003362

answers: The geometrical properties of conjugate faults indicate the sense of stress.

answers: NDQ_003363

answers: conjugate faults

answers: NDQ_003371

answers: Which of the following is not an example of a conjugate fault?

answers: NDQ_003373

answers: how would you describe the stress?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: It's impossible to say

answers: NDQ_003381

answers: Which of the following is not a type of stress: conjugate faults or confining stress?

answers: NDQ_003382

answers: None of the above choices.

answers: NDQ_003383

answers: no

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: NDQ_003386

answers: no

answers: NDQ_003387

answers: no

answers: NDQ_003388

answers: Which of the following is not a type of fault?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: conjugate faults

answers: NDQ_003391

answers: can not be seen

answers: NDQ_003392

answers: conjugate faults

answers: NDQ_003393

answers: can not be seen

answers: NDQ_003394

answers: conjugate faults

answers: NDQ_003395

answers: conjugate faults

answers: NDQ_003396

answers: conjugate faults

answers: NDQ_003351

answers: conjugate faults

answers: NDQ_003352

answers: conjugate faults

answers: NDQ_003353

answers: conjugate faults

answers: NDQ_003354

answers: The geometrical properties of conjugate faults

answers: NDQ_003355

answers: conjugate faults

answers: NDQ_003356

answers: stress,

answers: NDQ_003357

answers: stress,

answers: NDQ_003358

answers: conjugate faults

answers: NDQ_003359

answers: stress,

answers: NDQ_003360

answers: stress,

answers: NDQ_003362

answers: they may not appear in the actual fault patterns.

answers: NDQ_003363

answers: conjugate faults

answers: NDQ_003371

answers: conjugate faults

answers: NDQ_003373

answers: The geometrical properties of conjugate faults

answers: NDQ_003376

answers: The geometrical properties of conjugate faults

answers: NDQ_003378

answers: stress,

answers: NDQ_003379

answers: they may not appear in the actual fault patterns.

answers: NDQ_003380

answers: stress,

answers: NDQ_003381

answers: conjugate faults

answers: NDQ_003382

answers: they may not appear in the actual fault patterns.

answers: NDQ_003383

answers: The geometrical properties of conjugate faults

answers: NDQ_003384

answers: The geometrical properties of conjugate faults

answers: NDQ_003385

answers: fault patterns.

answers: NDQ_003386

answers: stress,

answers: NDQ_003387

answers: The geometrical properties of conjugate faults

answers: NDQ_003388

answers: conjugate faults

answers: NDQ_003389

answers: The geometrical properties of conjugate faults

answers: NDQ_003390

answers: conjugate faults

answers: NDQ_003391

answers: stress,

answers: NDQ_003392

answers: conjugate faults

answers: NDQ_003393

answers: stress,

answers: NDQ_003394

answers: conjugate faults

answers: NDQ_003395

answers: conjugate faults

answers: NDQ_003396

answers: conjugate faults

text: Stressors have physical, chemical and mental responses inside of the body. Physical stressors produce mechanical stresses on skin, bones, ligaments, tendons, muscles and nerves that cause tissue deformation and in extreme cases tissue failure.  Chemical stresses also produce biomechanical responses associated with metabolism and tissue repair. Physical stressors may produce pain and impair work performance.  Chronic pain and impairment requiring medical attention may result from extreme physical stressors or if there is not sufficient recovery time between successive exposures.

text: Stressors have physical, chemical and mental responses inside of the body. Physical stressors produce mechanical stresses on skin, bones, ligaments, tendons, muscles and nerves that cause tissue deformation and in extreme cases tissue failure.  Chemical stresses also produce biomechanical responses associated with

text: metabolism

text: and tissue repair. Physical stressors may produce pain and impair work performance.  Chronic pain and impairment requiring medical attention may result from extreme physical stressors or if there is not sufficient recovery time between successive exposures.

answers: NDQ_003351

answers: chemical

answers: NDQ_003352

answers: deforms

answers: NDQ_003353

answers: tissue deformation

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: tendons

answers: NDQ_003356

answers: fail

answers: NDQ_003357

answers: tissue deformation is caused by

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: physical stresses

answers: NDQ_003362

answers: there is not sufficient recovery time between successive exposures.

answers: NDQ_003363

answers: physical stressors

answers: NDQ_003371

answers: Which of the following is not a type of stressor?

answers: NDQ_003373

answers: What is a physical stressor?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: Which of the following is not a type of stress?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: Which of the following is not a type of fold that arches upward?

answers: NDQ_003385

answers: Which of the following is not a type of stressor?

answers: NDQ_003386

answers: Which of the following is not a type of stressor?

answers: NDQ_003387

answers: Which of the following is not a type of tissue failure?

answers: NDQ_003388

answers: Which of the following is not a type of stressor?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: tissue failure

answers: NDQ_003391

answers: is not sufficient recovery time

answers: NDQ_003392

answers: tissue failure

answers: NDQ_003393

answers: Bones

answers: NDQ_003394

answers: can result from extreme physical stressors

answers: NDQ_003395

answers: tissue failure

answers: NDQ_003396

answers: tissue failure

answers: NDQ_003351

answers: Physical stressors

answers: NDQ_003352

answers: tissue failure.

answers: NDQ_003353

answers: tissue deformation

answers: NDQ_003354

answers: Stressors

answers: NDQ_003355

answers: tendons,

answers: NDQ_003356

answers: tissue failure.

answers: NDQ_003357

answers: sufficient recovery time between successive exposures.

answers: NDQ_003358

answers: Stressors

answers: NDQ_003359

answers: stresses

answers: NDQ_003360

answers: Stressors

answers: NDQ_003362

answers: tissue failure.

answers: NDQ_003363

answers: extreme physical stressors

answers: NDQ_003371

answers: Physical stressors

answers: NDQ_003373

answers: Physical stressors produce mechanical stresses

answers: NDQ_003376

answers: Physical stressors

answers: NDQ_003378

answers: Physical stressors produce mechanical stresses

answers: NDQ_003379

answers: tendons, muscles and nerves

answers: NDQ_003380

answers: mechanical stresses

answers: NDQ_003381

answers: Physical stressors

answers: NDQ_003382

answers: Physical stressors

answers: NDQ_003383

answers: Physical stressors

answers: NDQ_003384

answers: tendons, muscles and nerves

answers: NDQ_003385

answers: tissue failure.

answers: NDQ_003386

answers: Physical stressors

answers: NDQ_003387

answers: tissue failure.

answers: NDQ_003388

answers: tissue failure.

answers: NDQ_003389

answers: Physical stressors

answers: NDQ_003390

answers: tissue failure.

answers: NDQ_003391

answers: tissue failure.

answers: NDQ_003392

answers: tissue failure.

answers: NDQ_003393

answers: tissue failure.

answers: NDQ_003394

answers: tissue failure.

answers: NDQ_003395

answers: tissue failure.

answers: NDQ_003396

answers: tissue failure.

text: The Rideau Lake Fault (an ancient fracture in the Earth's crust due to tension) explains the large exposure of granite that can be observed on much of Upper Rideau Lake's northern shore.The northern half of Upper Rideau Lake is located in the Algonquin Highlands. Bedrock in this hilly, Precambrian landscape consists mostly of gneisses and marble and is covered in a very thin layer of mixed glacial sediment. The southern half of Upper Rideau Lake is located between the Algonquin Highlands and the Smiths Falls Limestone Plain. Bedrock here consists of Paleozonic quartzose sandstone, dolostone, and conglomerate covered in a variety of sediment; mixed glacial sediment, sandy glacial till, silt and clay, organic deposits, and sand.

text: The Rideau Lake Fault (an ancient fracture in the Earth's crust due to tension) explains the large exposure of granite that can be observed on much of Upper Rideau Lake's northern shore.The northern half of Upper Rideau Lake is located in the Algonquin Highlands. Bedrock in this hilly, Precambrian landscape consists mostly of gneisses and marble and is covered in a very thin layer of mixed glacial sediment. The southern half of Upper Rideau Lake is located between the Algonquin Highlands and the Smiths Falls Limestone Plain. Bedrock here consists of Paleozonic quartzose sandstone, dolostone, and conglomerate covered in a variety of sediment; mixed glacial sediment, sandy glacial till, silt and clay, organic deposits, and sand.

answers: NDQ_003351

answers: tension

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: fractures

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: Fault

answers: NDQ_003356

answers: erode

answers: NDQ_003357

answers: tension causes a fracture in the Earth's crust

answers: NDQ_003358

answers: Fault

answers: NDQ_003359

answers: tension is applied

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: The Rideau Lake Fault is an ancient fracture in the Earth's crust due to tension

answers: NDQ_003363

answers: Precambrian

answers: NDQ_003371

answers: What type of fault is the Rideau Lake Fault?

answers: NDQ_003373

answers: Why does the Rideau Lake Fault explain the large exposure of granite?

answers: NDQ_003376

answers: Which of the following is not a type of terrain: basin-and-range or hilly?

answers: NDQ_003378

answers: What is the last word in the passage?

answers: NDQ_003379

answers: What type of fault is the Rideau Lake Fault?

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What type of stress does the Rideau Lake Fault cause?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What causes the Rideau Lake Fault?

answers: NDQ_003384

answers: Which of the following is not a type of fold?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: Why is granite exposed on much of Upper Rideau Lake's northern shore?

answers: NDQ_003387

answers: Which of the following is not the cause of the Rideau Lake Fault: tension or compression stress?

answers: NDQ_003388

answers: Which of the following is not a type of fault: Rideau Lake Fault, Smiths Falls Limestone Plain, or Rideau Lake Fault?

answers: NDQ_003389

answers: It is not possible to tell

answers: NDQ_003390

answers: Rideau Lake Fault

answers: NDQ_003391

answers: Algonquin Highlands

answers: NDQ_003392

answers: Rideau Lake Fault

answers: NDQ_003393

answers: Algonquin Highlands

answers: NDQ_003394

answers: Rideau Lake Fault

answers: NDQ_003395

answers: Rideau Lake Fault

answers: NDQ_003396

answers: Rideau Lake Fault

answers: NDQ_003351

answers: tension)

answers: NDQ_003352

answers: granite

answers: NDQ_003353

answers: fracture in the Earth's crust

answers: NDQ_003354

answers: Smiths Falls Limestone Plain.

answers: NDQ_003355

answers: The Rideau Lake Fault

answers: NDQ_003356

answers: tension) explains the large exposure of granite

answers: NDQ_003357

answers: tension)

answers: NDQ_003358

answers: The Rideau Lake Fault

answers: NDQ_003359

answers: tension)

answers: NDQ_003360

answers: The Rideau Lake Fault

answers: NDQ_003362

answers: The Rideau Lake Fault

answers: NDQ_003363

answers: Rideau Lake Fault

answers: NDQ_003371

answers: The Rideau Lake Fault

answers: NDQ_003373

answers: The Rideau Lake Fault

answers: NDQ_003376

answers: The Rideau Lake Fault

answers: NDQ_003378

answers: The Rideau Lake Fault

answers: NDQ_003379

answers: Rideau Lake Fault

answers: NDQ_003380

answers: tension)

answers: NDQ_003381

answers: tension)

answers: NDQ_003382

answers: tension)

answers: NDQ_003383

answers: tension)

answers: NDQ_003384

answers: The Rideau Lake Fault

answers: NDQ_003385

answers: The Rideau Lake Fault

answers: NDQ_003386

answers: tension)

answers: NDQ_003387

answers: tension)

answers: NDQ_003388

answers: tension)

answers: NDQ_003389

answers: The Rideau Lake Fault

answers: NDQ_003390

answers: Rideau Lake Fault

answers: NDQ_003391

answers: granite

answers: NDQ_003392

answers: Rideau Lake Fault

answers: NDQ_003393

answers: granite

answers: NDQ_003394

answers: The Rideau Lake Fault

answers: NDQ_003395

answers: Rideau Lake Fault

answers: NDQ_003396

answers: Rideau Lake Fault

text: Biotic stress is stress that occurs as a result of damage done to plants by other living organisms, such as bacteria, viruses, fungi, parasites, beneficial and harmful insects, weeds, and cultivated or native plants. Not to be confused with abiotic stress, which is the negative impact of non-living factors on the organisms in a specific environment such as sunlight, wind, salinity, over watering and drought. The types of biotic stresses imposed on a plant depend on both geography and climate and on the host plant and its ability to resist particular stresses. Although there are many kinds of biotic stress, the majority of plant diseases are caused by fungi. Biotic stress remains a broadly defined term and those who study it face many challenges, such as the greater difficulty in controlling biotic stresses in an experimental context compared to abiotic stress.

text: Biotic stress is

text: stress

text: that occurs as a result of damage done to plants by other living organisms, such as bacteria, viruses, fungi, parasites, beneficial and harmful insects, weeds, and cultivated or

text: native plant

text: s. Not to be confused with

text: abiotic stress

text: , which is the negative impact of non-living factors on the organisms in a specific environment such as sunlight, wind, salinity, over watering and drought. The types of biotic stresses imposed on a plant depend on both geography and climate and on the host plant and its ability to resist particular stresses. Although there are many kinds of biotic stress, the majority of plant diseases are caused by fungi. Biotic stress remains a broadly defined term and those who study it face many challenges, such as the greater difficulty in controlling biotic stresses in an experimental context compared to abiotic stress.

answers: NDQ_003351

answers: abiotic stress

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: abiotic stress

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: deteriorate

answers: NDQ_003357

answers: abiotic stress is the negative impact of non-living factors on the organisms

answers: NDQ_003358

answers: Abiotic stress

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: biotic stresses

answers: NDQ_003362

answers: Biotic stress remains a broadly defined term

answers: NDQ_003363

answers: biotic stress

answers: NDQ_003371

answers: Which of the following is not a type of stress?

answers: NDQ_003373

answers: None of the above choices.

answers: NDQ_003376

answers: basin-and-range

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: unanswerable

answers: NDQ_003381

answers: What is abiotic stress?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: Fault zone

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: Which of the following is not a cause of normal faults?

answers: NDQ_003388

answers: What type of stress is shear stress?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: abiotic stress

answers: NDQ_003391

answers: unanswerable

answers: NDQ_003392

answers: a fault

answers: NDQ_003393

answers: dip-slip fault

answers: NDQ_003394

answers: isobath

answers: NDQ_003395

answers: a fault with a vertical fault plane

answers: NDQ_003396

answers: asymmetric

answers: NDQ_003351

answers: fungi.

answers: NDQ_003352

answers: Biotic stress

answers: NDQ_003353

answers: Biotic stress

answers: NDQ_003354

answers: Biotic stress

answers: NDQ_003355

answers: Biotic stress

answers: NDQ_003356

answers: fungi.

answers: NDQ_003357

answers: over watering and drought.

answers: NDQ_003358

answers: abiotic stress,

answers: NDQ_003359

answers: stresses.

answers: NDQ_003360

answers: Biotic stress

answers: NDQ_003362

answers: Biotic stress

answers: NDQ_003363

answers: climate

answers: NDQ_003371

answers: Biotic stress

answers: NDQ_003373

answers: Biotic stress

answers: NDQ_003376

answers: Biotic stress

answers: NDQ_003378

answers: Biotic stress

answers: NDQ_003379

answers: fungi.

answers: NDQ_003380

answers: abiotic stress,

answers: NDQ_003381

answers: abiotic stress,

answers: NDQ_003382

answers: Biotic stress

answers: NDQ_003383

answers: Biotic stress

answers: NDQ_003384

answers: Biotic stress

answers: NDQ_003385

answers: Biotic stress

answers: NDQ_003386

answers: Biotic stress

answers: NDQ_003387

answers: fungi.

answers: NDQ_003388

answers: Biotic stress

answers: NDQ_003389

answers: Biotic stress

answers: NDQ_003390

answers: Biotic stress

answers: NDQ_003391

answers: Biotic stress

answers: NDQ_003392

answers: Biotic stress

answers: NDQ_003393

answers: Biotic stress

answers: NDQ_003394

answers: Biotic stress

answers: NDQ_003395

answers: Biotic stress

answers: NDQ_003396

answers: Biotic stress

text: Earthquakes in California are common occurrences since the state is traversed by six major strike-slip fault systems with hundreds of related faults, many of which are "sister faults" of the infamous San Andreas Fault that runs nearly the full length of California at the juncture of the Pacific Plate and the North American Plate. The fault systems include the Hayward Fault Zone, Calaveras Fault, Clayton-Marsh Creek-Greenville Fault, and the San Gregorio Fault. Significant blind thrust faults (faults with near vertical motion and no surface ruptures) are associated with portions of the Santa Cruz Mountains and the northern reaches of the Diablo Range and Mount Diablo. The California earthquake forecast gives a rough estimate of where the main earthquake zones in California are. Earthquake damage depends on what area is hit, how close to the surface the center of the earthquake is located, and its magnitude. Earthquake damage, for a given magnitude earthquake, to human structures depends on how well the buildings are built and what the structures are located on. Buildings on soft or filled-in soil suffer the most because they feel shock waves most strongly. Buildings on bedrock suffer less damage because the ground is firmer. Sometimes the ensuing fires, floods or tsunamis caused by the earthquake are often where the greatest damage occurs.

text: Earthquake

text: s in California are common occurrences since the state is traversed by six major

text: strike-slip fault

text: systems with hundreds of related faults, many of which are "sister faults" of the infamous

text: San Andreas Fault

text: that runs nearly the full length of California at the juncture of the

text: Pacific Plate

text: and the

text: North American Plate

text: . The fault systems include the

text: Hayward Fault Zone

text: Calaveras Fault

text: Clayton-Marsh Creek-Greenville Fault

text: , and the

text: San Gregorio Fault

text: . Significant blind

text: thrust fault

text: s (faults with near vertical motion and no surface ruptures) are associated with portions of the

text: Santa Cruz Mountains

text: and the northern reaches of the

text: Diablo Range

text: and

text: Mount Diablo

text: . The

text: California earthquake forecast

text: gives a rough estimate of where the main earthquake zones in California are. Earthquake damage depends on what area is hit, how close to the surface the center of the earthquake is located, and its magnitude. Earthquake damage, for a given magnitude earthquake, to human structures depends on how well the buildings are built and what the structures are located on. Buildings on soft or filled-in soil suffer the most because they feel shock waves most strongly. Buildings on bedrock suffer less damage because the ground is firmer. Sometimes the ensuing fires, floods or

text: tsunami

text: s caused by the earthquake are often where the greatest damage occurs.

answers: NDQ_003351

answers: blind thrust faults

answers: NDQ_003352

answers: more likely to crack

answers: NDQ_003353

answers: Earthquake damage

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: blind thrust fault

answers: NDQ_003356

answers: swell

answers: NDQ_003357

answers: surface ruptures are caused by

answers: NDQ_003358

answers: blind thrust fault

answers: NDQ_003359

answers: surface ruptures

answers: NDQ_003360

answers: Pacific Plate

answers: NDQ_003362

answers: the San Andreas Fault runs nearly the full length of California

answers: NDQ_003363

answers: San Andreas Fault

answers: NDQ_003371

answers: How old rocks are above much younger rocks there may be a thrust fault in between

answers: NDQ_003373

answers: what is the last word in the passage?

answers: NDQ_003376

answers: What type of terrain is caused by compressive forces?

answers: NDQ_003378

answers: strike-slip fault systems

answers: NDQ_003379

answers: blind thrust faults

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What type of stress does the San Andreas Fault cause?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: What type of fold is the San Gregorio Fault?

answers: NDQ_003385

answers: The Hayward Fault Zone

answers: NDQ_003386

answers: strike-slip faults

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: strike-slip faults, blind thrust faults, or surface ruptures?

answers: NDQ_003388

answers: Which of the following is not an example of a strike-slip fault?

answers: NDQ_003389

answers: not enough information

answers: NDQ_003390

answers: blind thrust faults

answers: NDQ_003391

answers: bedrock

answers: NDQ_003392

answers: blind thrust faults

answers: NDQ_003393

answers: bedrock

answers: NDQ_003394

answers: blind thrust faults

answers: NDQ_003395

answers: blind thrust faults

answers: NDQ_003396

answers: blind thrust faults

answers: NDQ_003351

answers: shock waves

answers: NDQ_003352

answers: soft or filled-in soil suffer the most because they feel shock waves

answers: NDQ_003353

answers: shock waves

answers: NDQ_003354

answers: Buildings on bedrock

answers: NDQ_003355

answers: blind thrust faults

answers: NDQ_003356

answers: soft or filled-in soil suffer the most because they feel shock waves

answers: NDQ_003357

answers: near vertical motion and no surface ruptures)

answers: NDQ_003358

answers: blind thrust faults

answers: NDQ_003359

answers: vertical motion

answers: NDQ_003360

answers: Pacific Plate

answers: NDQ_003362

answers: no surface ruptures)

answers: NDQ_003363

answers: Pacific Plate and the North American Plate.

answers: NDQ_003371

answers: thrust faults

answers: NDQ_003373

answers: Buildings on bedrock

answers: NDQ_003376

answers: Buildings on soft or filled-in soil

answers: NDQ_003378

answers: strike-slip

answers: NDQ_003379

answers: blind thrust faults

answers: NDQ_003380

answers: shock waves

answers: NDQ_003381

answers: Buildings on bedrock

answers: NDQ_003382

answers: Buildings on soft or filled-in soil

answers: NDQ_003383

answers: shock waves most strongly. Buildings on bedrock

answers: NDQ_003384

answers: blind thrust faults

answers: NDQ_003385

answers: strike-slip fault systems

answers: NDQ_003386

answers: strike-slip fault systems

answers: NDQ_003387

answers: blind thrust faults

answers: NDQ_003388

answers: six major strike-slip fault systems with hundreds of related faults,

answers: NDQ_003389

answers: blind thrust faults

answers: NDQ_003390

answers: blind thrust faults

answers: NDQ_003391

answers: bedrock

answers: NDQ_003392

answers: blind thrust faults

answers: NDQ_003393

answers: bedrock

answers: NDQ_003394

answers: blind thrust faults

answers: NDQ_003395

answers: blind thrust faults

answers: NDQ_003396

answers: blind thrust faults

text: Post-perovskite has the same crystal structure as the synthetic solid compound CaIrO, and is often referred to as the "CaIrO-type phase of MgSiO" in the literature. The crystal system of post-perovskite is orthorhombic, its space group is Cmcm, and its structure is a stacked SiO-octahedral sheet along the b axis. The name "post-perovskite" derives from silicate perovskite, the stable phase of MgSiO throughout most of Earth's mantle, which has the perovskite structure. The prefix "post-" refers to the fact that it occurs after perovskite structured MgSiO as pressure increases (and historically, the progression of high pressure mineral physics). At upper mantle pressures, nearest Earth's surface, MgSiO persists as the silicate mineral enstatite, a pyroxene rock forming mineral found in igneous and metamorphic rocks of the crust.

text: Post-perovskite has the same crystal structure as the synthetic solid compound CaIrO, and is often referred to as the "CaIrO-type phase of MgSiO" in the literature. The

text: crystal system

text: of post-perovskite is

text: orthorhombic

text: , its

text: space group

text: is Cmcm, and its structure is a stacked SiO-octahedral sheet along the b axis. The name "post-perovskite" derives from

text: silicate perovskite

text: , the stable phase of MgSiO throughout most of Earth's mantle, which has the

text: perovskite structure

text: . The prefix "post-" refers to the fact that it occurs after perovskite structured MgSiO as pressure increases (and historically, the progression of high pressure mineral physics). At upper mantle pressures, nearest Earth's surface, MgSiO persists as the

text: silicate mineral

text: enstatite

text: , a

text: pyroxene

text: rock forming mineral found in

text: igneous

text: and

text: metamorphic rock

text: s of the

text: crust

answers: NDQ_003351

answers: post-perovskite

answers: NDQ_003352

answers: perovskite structure

answers: NDQ_003353

answers: metamorphism

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: unanswerable

answers: NDQ_003356

answers: enstatite

answers: NDQ_003357

answers: MgSiO persists as the silicate mineral enstatite, a pyroxene rock forming mineral found in igneous and metamorphic rocks of the crust

answers: NDQ_003358

answers: unanswerable

answers: NDQ_003359

answers: pressure increases

answers: NDQ_003360

answers: mantle

answers: NDQ_003362

answers: At upper mantle pressures, nearest Earth's surface,

answers: NDQ_003363

answers: high pressure

answers: NDQ_003371

answers: What is the name of the crystal system of post-perovskite?

answers: NDQ_003373

answers: How would you describe compressive stresses?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What type of force applied to rock is a stress?

answers: NDQ_003381

answers: What is the name of the crystal system of post-perovskite?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the name of the crystal system of post-perovskite?

answers: NDQ_003384

answers: What is the crystal system of post-perovskite?

answers: NDQ_003385

answers: What is the name of an area where faults are clustered?

answers: NDQ_003386

answers: What is the cause of earthquakes?

answers: NDQ_003387

answers: What is the name of the crystal system of post-perovskite?

answers: NDQ_003388

answers: What is the name of the silicate mineral enstatite?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: perovskite

answers: NDQ_003391

answers: perovskite

answers: NDQ_003392

answers: perovskite

answers: NDQ_003393

answers: enstatite

answers: NDQ_003394

answers: b axis

answers: NDQ_003395

answers: post-perovskite

answers: NDQ_003396

answers: post-perovskite

answers: NDQ_003351

answers: Post-perovskite

answers: NDQ_003352

answers: perovskite structured MgSiO

answers: NDQ_003353

answers: pressure increases (and historically, the progression of high pressure mineral physics).

answers: NDQ_003354

answers: Post-perovskite

answers: NDQ_003355

answers: Post-perovskite

answers: NDQ_003356

answers: metamorphic rocks

answers: NDQ_003357

answers: pressure increases

answers: NDQ_003358

answers: igneous and metamorphic rocks

answers: NDQ_003359

answers: pressure increases

answers: NDQ_003360

answers: high pressure mineral physics). At upper mantle pressures,

answers: NDQ_003362

answers: Post-perovskite

answers: NDQ_003363

answers: high pressure mineral physics). At upper mantle pressures,

answers: NDQ_003371

answers: Post-perovskite

answers: NDQ_003373

answers: pressure increases

answers: NDQ_003376

answers: Post-perovskite

answers: NDQ_003378

answers: Post-perovskite

answers: NDQ_003379

answers: b axis.

answers: NDQ_003380

answers: pressure

answers: NDQ_003381

answers: pressure increases

answers: NDQ_003382

answers: Post-perovskite

answers: NDQ_003383

answers: pressure increases

answers: NDQ_003384

answers: Post-perovskite

answers: NDQ_003385

answers: Post-perovskite

answers: NDQ_003386

answers: Post-perovskite

answers: NDQ_003387

answers: Post-perovskite

answers: NDQ_003388

answers: Post-perovskite

answers: NDQ_003389

answers: igneous and metamorphic rocks

answers: NDQ_003390

answers: Post-perovskite

answers: NDQ_003391

answers: enstatite,

answers: NDQ_003392

answers: Post-perovskite

answers: NDQ_003393

answers: enstatite,

answers: NDQ_003394

answers: b axis.

answers: NDQ_003395

answers: b axis.

answers: NDQ_003396

answers: Post-perovskite

text: The Afar Depression is the product of a tectonic triple-rifts junction (the Afar Triple Junction), where the spreading ridges forming the Red Sea and the Gulf of Aden emerge on land and meet the East African Rift. The conjunction of these three plates of Earth's crust is near Lake Abbe. The Afar Depression is one of two places on Earth where a mid-ocean ridge can be studied on land, the other being Iceland.

text: The Afar Depression is the product of a

text: tectonic

text: triple-rifts junction

text: (the

text: Afar Triple Junction

text: ), where the spreading ridges forming the

text: Red Sea

text: and the

text: Gulf of Aden

text: emerge on land and meet the

text: East African Rift

text: . The conjunction of these three plates of Earth's crust is near

text: Lake Abbe

text: . The Afar Depression is one of two places on Earth where a

text: mid-ocean ridge

text: can be studied on land, the other being

text: Iceland

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: rifts

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: rift

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: a mid-ocean ridge can be studied on land

answers: NDQ_003358

answers: Depression

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: plates

answers: NDQ_003362

answers: The Afar Depression is one of two places on Earth where a mid-ocean ridge can be studied on land, the other being Iceland

answers: NDQ_003363

answers: Afar Depression

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: How would you describe the stress?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: what is the product of a tectonic triple-rifts junction

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What type of stress does the Afar Depression experience?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: Fault zone

answers: NDQ_003386

answers: What is the cause of earthquakes?

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: What type of stress is shear stress?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: The Afar Depression

answers: NDQ_003391

answers: plate

answers: NDQ_003392

answers: The Afar Depression

answers: NDQ_003393

answers: plate

answers: NDQ_003394

answers: Afar Triple Junction

answers: NDQ_003395

answers: tectonic triple-rifts

answers: NDQ_003396

answers: East African Rift

answers: NDQ_003351

answers: East African Rift.

answers: NDQ_003352

answers: The Afar Depression

answers: NDQ_003353

answers: tectonic triple-rifts junction

answers: NDQ_003354

answers: Iceland.

answers: NDQ_003355

answers: mid-ocean ridge

answers: NDQ_003356

answers: The Afar Depression

answers: NDQ_003357

answers: East African Rift.

answers: NDQ_003358

answers: The Afar Depression

answers: NDQ_003359

answers: tectonic

answers: NDQ_003360

answers: land

answers: NDQ_003362

answers: The Afar Depression

answers: NDQ_003363

answers: tectonic triple-rifts junction

answers: NDQ_003371

answers: The Afar Depression

answers: NDQ_003373

answers: The Afar Depression

answers: NDQ_003376

answers: the spreading ridges

answers: NDQ_003378

answers: The Afar Depression

answers: NDQ_003379

answers: Iceland.

answers: NDQ_003380

answers: The Afar Depression

answers: NDQ_003381

answers: The Afar Depression

answers: NDQ_003382

answers: East African Rift.

answers: NDQ_003383

answers: tectonic triple-rifts junction

answers: NDQ_003384

answers: East African Rift.

answers: NDQ_003385

answers: tectonic triple-rifts junction

answers: NDQ_003386

answers: tectonic

answers: NDQ_003387

answers: The Afar Depression

answers: NDQ_003388

answers: The Afar Depression

answers: NDQ_003389

answers: the spreading ridges

answers: NDQ_003390

answers: The Afar Depression

answers: NDQ_003391

answers: mid-ocean ridge

answers: NDQ_003392

answers: The Afar Depression

answers: NDQ_003393

answers: mid-ocean ridge

answers: NDQ_003394

answers: The Afar Depression

answers: NDQ_003395

answers: East African Rift.

answers: NDQ_003396

answers: East African Rift.

text: A permanent meteorological station and a laboratory of the Siberian Institute of the Earth's crust are operating in the village.Population:  consists mainly of the staff of meteorological station.

text: A permanent meteorological station and a laboratory of the Siberian Institute of the Earth's crust are operating in the village.Population:  consists mainly of the staff of meteorological station.

answers: NDQ_003351

answers: lateral

answers: NDQ_003352

answers: increases in size.

answers: NDQ_003353

answers: igneous rocks to form.

answers: NDQ_003354

answers: Toroweap Formation is a formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: Siberian Institute of the Earth's crust is

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: breaks apart.

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: Population: consists mainly of the staff of meteorological station.

answers: NDQ_003363

answers: Earth's crust

answers: NDQ_003371

answers: Which of the following is not a type of fault?

answers: NDQ_003373

answers: It is more likely to be buried under a layer of soil.

answers: NDQ_003376

answers: None of the above choices .

answers: NDQ_003378

answers: The amount the ground moves in an earthquake is called slip

answers: NDQ_003379

answers: The dip of the fault plane is horizontal.

answers: NDQ_003380

answers: What is the best title for this passage?

answers: NDQ_003381

answers: What will happen to the rock?

answers: NDQ_003382

answers: None of the above choices .

answers: NDQ_003383

answers: None of the above choices .

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: It is not possible to tell

answers: NDQ_003386

answers: None of the above choices .

answers: NDQ_003387

answers: Which of the following is not a cause of normal faults?

answers: NDQ_003388

answers: Which of the following is not a cause of strike-slip faults?

answers: NDQ_003389

answers: None of the above choices .

answers: NDQ_003390

answers: is a fault

answers: NDQ_003391

answers: dip-slip fault

answers: NDQ_003392

answers: is a fault

answers: NDQ_003393

answers: dip-slip fault

answers: NDQ_003394

answers: is a

answers: NDQ_003395

answers: is a fault

answers: NDQ_003396

answers: NDQ_003351

answers: Earth's crust

answers: NDQ_003352

answers: Earth's crust

answers: NDQ_003353

answers: Earth's crust

answers: NDQ_003354

answers: A permanent meteorological station

answers: NDQ_003355

answers: Earth's crust

answers: NDQ_003356

answers: Earth's crust

answers: NDQ_003357

answers: Earth's crust

answers: NDQ_003358

answers: Earth's crust

answers: NDQ_003359

answers: Earth's crust

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: A permanent meteorological station

answers: NDQ_003363

answers: Siberian Institute of the Earth's crust

answers: NDQ_003371

answers: Siberian Institute of the Earth's crust

answers: NDQ_003373

answers: Earth's crust

answers: NDQ_003376

answers: Siberian Institute of the Earth's crust

answers: NDQ_003378

answers: Earth's crust

answers: NDQ_003379

answers: Siberian Institute of the Earth's crust

answers: NDQ_003380

answers: Earth's crust

answers: NDQ_003381

answers: Siberian Institute of the Earth's crust

answers: NDQ_003382

answers: Siberian Institute of the Earth's crust

answers: NDQ_003383

answers: Siberian Institute of the Earth's crust

answers: NDQ_003384

answers: Siberian Institute of the Earth's crust

answers: NDQ_003385

answers: Earth's crust

answers: NDQ_003386

answers: Siberian Institute of the Earth's crust

answers: NDQ_003387

answers: Siberian Institute of the Earth's crust

answers: NDQ_003388

answers: Siberian Institute of the Earth's crust

answers: NDQ_003389

answers: Earth's crust

answers: NDQ_003390

answers: Siberian Institute of the Earth's crust

answers: NDQ_003391

answers: Earth's crust

answers: NDQ_003392

answers: Siberian Institute of the Earth's crust

answers: NDQ_003393

answers: Earth's crust

answers: NDQ_003394

answers: Earth's crust

answers: NDQ_003395

answers: Earth's crust

answers: NDQ_003396

answers: Siberian Institute of the Earth's crust

text: The Ceraunius Fossae fractures are extensional features produced when the crust is stretched apart. The fractures are oriented north-south, radial to an early center of volcano-tectonic activity in Syria Planum, a region in southern Tharsis. A large number of extensional structures, including graben and rifts, radiate outward from the center of Tharsis. Mechanical studies indicate that a regional pattern of radiating graben and rifts is consistent with stresses caused by loading of the lithosphere by the enormous weight of the Tharsis bulge. The immense Valles Marineris is probably the best known example of a rift system that lies radial to Tharsis. Several generations of grabens with slightly different orientations are present in Ceraunius Fossae, indicating that stress fields have changed somewhat over time.

text: The Ceraunius Fossae fractures are

text: extensional

text: features produced when the crust is stretched apart. The fractures are oriented north-south, radial to an early center of volcano-tectonic activity in

text: Syria Planum

text: , a region in southern Tharsis. A large number of extensional structures, including

text: graben

text: and

text: rift

text: s, radiate outward from the center of Tharsis.

text: Mechanical

text: studies indicate that a regional pattern of radiating graben and rifts is consistent with stresses caused by loading of the lithosphere by the enormous weight of the Tharsis bulge. The immense

text: Valles Marineris

text: is probably the best known example of a rift system that lies radial to Tharsis. Several generations of grabens with slightly different orientations are present in Ceraunius Fossae, indicating that

text: stress field

text: s have changed somewhat over time.

answers: NDQ_003351

answers: loading of the lithosphere

answers: NDQ_003352

answers: is more likely to have cracks

answers: NDQ_003353

answers: rifts

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: graben

answers: NDQ_003356

answers: stretch apart

answers: NDQ_003357

answers: Ceraunius Fossae fractures are oriented which direction?

answers: NDQ_003358

answers: graben

answers: NDQ_003359

answers: stretched apart

answers: NDQ_003360

answers: Tharsis

answers: NDQ_003362

answers: stress fields have changed somewhat over time.

answers: NDQ_003363

answers: Tharsis

answers: NDQ_003371

answers: What is the best known example of a rift system that lies radial to Tharsis

answers: NDQ_003373

answers: Which of the following is not a type of stress?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What is an example of a stress field that has changed somewhat over time?

answers: NDQ_003381

answers: Which of the following is not an example of an extensional structure: graben or rifts?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a type of structure: graben or rifts?

answers: NDQ_003384

answers: What is the best known example of a rift system that lies radial to Tharsis?

answers: NDQ_003385

answers: What is the name of the area where faults are clustered?

answers: NDQ_003386

answers: What type of movement of rock at faults is the cause of earthquakes?

answers: NDQ_003387

answers: Which is not caused by loading of the lithosphere by the enormous weight of the Tharsis bulge

answers: NDQ_003388

answers: Which of the following is not an example of an extensional structure: graben or rifts?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: graben

answers: NDQ_003391

answers: graben

answers: NDQ_003392

answers: graben

answers: NDQ_003393

answers: graben

answers: NDQ_003394

answers: radial

answers: NDQ_003395

answers: a rift system that lies radial to Tharsis

answers: NDQ_003396

answers: graben

answers: NDQ_003351

answers: loading of the lithosphere by the enormous weight

answers: NDQ_003352

answers: stress fields have changed somewhat over time.

answers: NDQ_003353

answers: Several generations of grabens with slightly different orientations

answers: NDQ_003354

answers: The Ceraunius Fossae

answers: NDQ_003355

answers: graben

answers: NDQ_003356

answers: stretched apart.

answers: NDQ_003357

answers: north-south,

answers: NDQ_003358

answers: graben

answers: NDQ_003359

answers: stretched apart.

answers: NDQ_003360

answers: weight of the Tharsis bulge.

answers: NDQ_003362

answers: stress fields have changed somewhat over time.

answers: NDQ_003363

answers: Tharsis bulge.

answers: NDQ_003371

answers: rift system

answers: NDQ_003373

answers: loading of the lithosphere by the enormous weight

answers: NDQ_003376

answers: loading of the lithosphere by the enormous weight

answers: NDQ_003378

answers: extensional features produced when the crust is stretched apart.

answers: NDQ_003379

answers: north-south,

answers: NDQ_003380

answers: loading of the lithosphere by the enormous weight

answers: NDQ_003381

answers: stretched apart.

answers: NDQ_003382

answers: loading of the lithosphere

answers: NDQ_003383

answers: loading of the lithosphere by the enormous weight

answers: NDQ_003384

answers: graben

answers: NDQ_003385

answers: rift system

answers: NDQ_003386

answers: stretched apart.

answers: NDQ_003387

answers: extensional features produced when the crust is stretched apart.

answers: NDQ_003388

answers: loading of the lithosphere

answers: NDQ_003389

answers: the crust is stretched apart.

answers: NDQ_003390

answers: Ceraunius Fossae

answers: NDQ_003391

answers: Tharsis bulge.

answers: NDQ_003392

answers: Ceraunius Fossae

answers: NDQ_003393

answers: graben

answers: NDQ_003394

answers: rift system that lies radial

answers: NDQ_003395

answers: north-south,

answers: NDQ_003396

answers: Valles Marineris

text: "There are rifts and rifts," wrote Pisarev of the rift between dreams and reality. "My dream may run ahead of the natural march of events or may fly off at a tangent in a direction in which no natural march of events will ever proceed. In the first case my dream will not cause any harm; it may even support and augment the energy of the working men.... There is nothing in such dreams that would distort or paralyse labour-power. On the contrary, if man were completely deprived of the ability to dream in this way, if he could not from time to time run ahead and mentally conceive, in an entire and completed picture, the product to which his hands are only just beginning to lend shape, then I cannot at all imagine what stimulus there would be to induce man to undertake and complete extensive and strenuous work in the sphere of art, science, and practical endeavour....

text: "There are rifts and rifts," wrote Pisarev of the rift between dreams and reality. "My dream may run ahead of the natural march of events or may fly off at a tangent in a direction in which no natural march of events will ever proceed. In the first case my dream will not cause any harm; it may even support and augment the energy of the working men.... There is nothing in such dreams that would distort or paralyse labour-power. On the contrary, if man were completely deprived of the ability to dream in this way, if he could not from time to time run ahead and mentally conceive, in an entire and completed picture, the product to which his hands are only just beginning to lend shape, then I cannot at all imagine what stimulus there would be to induce man to undertake and complete extensive and strenuous work in the sphere of art, science, and practical endeavour....

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: has more cracks

answers: NDQ_003353

answers: rifts

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: tangent

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: In the first case my dream will not cause any harm

answers: NDQ_003358

answers: rift

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: no natural march of events will ever proceed

answers: NDQ_003363

answers: a tangent

answers: NDQ_003371

answers: what may cause any harm

answers: NDQ_003373

answers: None of the above choices .

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: None of the above choices.

answers: NDQ_003379

answers: vertical

answers: NDQ_003380

answers: What is Pisarev talking about?

answers: NDQ_003381

answers: It may even support and augment the energy of the working men

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: no

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: NDQ_003386

answers: no

answers: NDQ_003387

answers: None of the above choices.

answers: NDQ_003388

answers: unanswerable

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: rift

answers: NDQ_003391

answers: unanswerable

answers: NDQ_003392

answers: rift

answers: NDQ_003393

answers: unanswerable

answers: NDQ_003394

answers: tangent

answers: NDQ_003395

answers: fly off at a tangent

answers: NDQ_003396

answers: tangent

answers: NDQ_003351

answers: natural march of events

answers: NDQ_003352

answers: tangent

answers: NDQ_003353

answers: rifts and rifts,"

answers: NDQ_003354

answers: rifts and rifts,"

answers: NDQ_003355

answers: tangent

answers: NDQ_003356

answers: distort or paralyse labour-power.

answers: NDQ_003357

answers: my dream will not cause any harm;

answers: NDQ_003358

answers: tangent

answers: NDQ_003359

answers: no natural march of events will ever proceed.

answers: NDQ_003360

answers: dreams

answers: NDQ_003362

answers: no natural march of events will ever proceed.

answers: NDQ_003363

answers: natural march of events

answers: NDQ_003371

answers: rifts

answers: NDQ_003373

answers: "There are rifts and rifts,"

answers: NDQ_003376

answers: rifts and rifts," wrote Pisarev

answers: NDQ_003378

answers: natural march of events or may fly off at a tangent

answers: NDQ_003379

answers: tangent

answers: NDQ_003380

answers: strenuous work

answers: NDQ_003381

answers: rifts and rifts,"

answers: NDQ_003382

answers: rifts and rifts," wrote Pisarev

answers: NDQ_003383

answers: rifts and rifts," wrote Pisarev

answers: NDQ_003384

answers: tangent

answers: NDQ_003385

answers: rifts and rifts,"

answers: NDQ_003386

answers: rifts and rifts," wrote Pisarev

answers: NDQ_003387

answers: distort or paralyse labour-power.

answers: NDQ_003388

answers: rifts and rifts," wrote Pisarev

answers: NDQ_003389

answers: rifts and rifts," wrote Pisarev

answers: NDQ_003390

answers: rifts and rifts,"

answers: NDQ_003391

answers: rifts and rifts," wrote Pisarev

answers: NDQ_003392

answers: rifts and rifts,"

answers: NDQ_003393

answers: rifts and rifts,"

answers: NDQ_003394

answers: tangent

answers: NDQ_003395

answers: tangent

answers: NDQ_003396

answers: tangent

text: An orogeny is underway when mountains begin to grow in the collision zone. There are other modes of mountain formation and orogeny but certainly continental collision is one of the most important. Rainfall and snowfall increase on the mountains as these rise, perhaps at a rate of a few millimeters per year (at a growth rate of 1 mm/year, a 5,000 m tall mountain can form in 5 million years, a time period that is less than 10% of the life of a typical collision zone). River systems form, and glaciers may grow on the highest peaks. Erosion accelerates as the mountains rise, and great volumes of sediment are shed into the rivers, which carry sediment away from the mountains to be deposited in sedimentary basins in the surrounding lowlands. Crustal rocks are thrust faulted over the sediments and the mountain belt broadens as it rises in height. A crustal root also develops, as required by isostasy; mountains can be high if underlain by thicker crust. Crustal thickening may happen as a result of crustal shortening or when one crust overthrusts the other. Thickening is accompanied by heating, so the crust becomes weaker as it thickens. The lower crust begins to flow and collapse under the growing mountain mass, forming rifts near the crest of the mountain range. The lower crust may partially melt, forming anatectic granites which then rise into the overlying units, forming granite intrusions. Crustal thickening provides one of two negative feedbacks on mountain growth in collision zones, the other being erosion. The popular notion that erosion is responsible for destroying mountains is only half correct - viscous flow of weak lower mantle also reduces relief with time, especially once the collision is complete and  the two continents are completely sutured.  Convergence between the continents continues because the crust is still being pulled down by oceanic lithosphere sinking in the subduction zone to either side of the collision as well as beneath the impinging continent.

text: An

text: orogeny

text: is underway when mountains begin to grow in the collision zone. There are other modes of mountain formation and orogeny but certainly continental collision is one of the most important.

text: Rain

text: fall and

text: snow

text: fall increase on the mountains as these rise, perhaps at a rate of a few millimeters per year (at a growth rate of 1 mm/year, a 5,000 m tall mountain can form in 5 million years, a time period that is less than 10% of the life of a typical collision zone).

text: River

text: systems form, and

text: glaciers

text: may grow on the highest peaks.

text: Erosion

text: accelerates as the mountains rise, and great volumes of

text: sediment

text: are shed into the rivers, which carry sediment away from the mountains to be deposited in

text: sedimentary basins

text: in the surrounding lowlands. Crustal rocks are

text: thrust fault

text: ed over the sediments and the mountain belt broadens as it rises in height. A crustal root also develops, as required by

text: isostasy

text: ; mountains can be high if underlain by thicker crust. Crustal thickening may happen as a result of crustal shortening or when one crust overthrusts the other. Thickening is accompanied by heating, so the crust becomes weaker as it thickens. The lower crust begins to flow and collapse under the growing mountain mass, forming

text: rifts

text: near the crest of the mountain range. The lower crust may partially

text: melt

text: , forming anatectic granites which then rise into the overlying units, forming

text: granite

text: intrusion

text: s. Crustal thickening provides one of two negative feedbacks on mountain growth in collision zones, the other being erosion. The popular notion that erosion is responsible for destroying mountains is only half correct - viscous flow of weak lower mantle also reduces relief with time, especially once the collision is complete and  the two continents are completely sutured.  Convergence between the continents continues because the crust is still being pulled down by oceanic lithosphere sinking in the subduction zone to either side of the collision as well as beneath the impinging continent.

answers: NDQ_003351

answers: crustal shortening

answers: NDQ_003352

answers: becomes weaker

answers: NDQ_003353

answers: Crustal thickening

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: rift

answers: NDQ_003356

answers: increase in height

answers: NDQ_003357

answers: crustal shortening or when one crust overthrusts the other

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: thrust faulted

answers: NDQ_003360

answers: continental collision

answers: NDQ_003362

answers: the San Andreas fault is responsible for destroying mountains

answers: NDQ_003363

answers: continental collision

answers: NDQ_003371

answers: What may happen if one crust overthrusts the other?

answers: NDQ_003373

answers: What is one of the negative feedbacks on mountain growth in collision zones?

answers: NDQ_003376

answers: Which of the following is not caused by compressive forces:

answers: NDQ_003378

answers: What is one of two negative feedbacks on mountain growth in collision zones, the other being erosion

answers: NDQ_003379

answers: Which of the following is not a type of strike-slip fault?

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What happens when the lower crust begins to flow and collapse under the growing mountain mass?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What happens when one crust overthrusts the other?

answers: NDQ_003384

answers: Which of the following is not a type of fold?

answers: NDQ_003385

answers: What is the name of the area where faults are clustered?

answers: NDQ_003386

answers: Which of the following is not a cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not a cause of normal faults?

answers: NDQ_003388

answers: Which of the following is not a result of shear stress: thrust faults, strike-slip faults, or erosion?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: thrust fault

answers: NDQ_003391

answers: subduction zone

answers: NDQ_003392

answers: thrust fault

answers: NDQ_003393

answers: a crustal root

answers: NDQ_003394

answers: thrust fault

answers: NDQ_003395

answers: thrust fault

answers: NDQ_003396

answers: thrust fault

answers: NDQ_003351

answers: crustal shortening or when one crust overthrusts the other.

answers: NDQ_003352

answers: the crust becomes weaker

answers: NDQ_003353

answers: Crustal rocks are thrust faulted

answers: NDQ_003354

answers: Crustal thickening

answers: NDQ_003355

answers: rifts

answers: NDQ_003356

answers: erosion.

answers: NDQ_003357

answers: Crustal thickening

answers: NDQ_003358

answers: rifts

answers: NDQ_003359

answers: one crust overthrusts the other.

answers: NDQ_003360

answers: thickening

answers: NDQ_003362

answers: erosion is responsible for destroying mountains

answers: NDQ_003363

answers: continental collision

answers: NDQ_003371

answers: thickening

answers: NDQ_003373

answers: Thickening

answers: NDQ_003376

answers: Thickening

answers: NDQ_003378

answers: The lower crust begins to flow and collapse under the growing mountain mass,

answers: NDQ_003379

answers: Thickening

answers: NDQ_003380

answers: erosion.

answers: NDQ_003381

answers: Thickening

answers: NDQ_003382

answers: Thickening

answers: NDQ_003383

answers: rifts

answers: NDQ_003384

answers: Thickening

answers: NDQ_003385

answers: one crust overthrusts the other.

answers: NDQ_003386

answers: crustal shortening or when one crust overthrusts the other.

answers: NDQ_003387

answers: Thickening

answers: NDQ_003388

answers: crustal shortening

answers: NDQ_003389

answers: Thickening

answers: NDQ_003390

answers: rifts

answers: NDQ_003391

answers: Crustal rocks

answers: NDQ_003392

answers: rifts

answers: NDQ_003393

answers: Crustal rocks

answers: NDQ_003394

answers: crustal shortening or when one crust overthrusts the other.

answers: NDQ_003395

answers: Thickening

answers: NDQ_003396

answers: Thickening

text: The opposite effect is that of transpression, where converging movement of a curved fault plane causes collision of the opposing sides of the fault.  An example is the San Bernardino Mountains north of Los Angeles, which result from convergence along a curve in the San Andreas fault system.  The Northridge earthquake was caused by vertical movement along local thrust and reverse faults bunching up against the bend in the otherwise strike-slip fault environment.In Nigeria, the dominant type of basement rock intersected by wells drilled for hydrocarbons, limestone, or water is granite. The three sedimentary basins in Nigeria are underlain by continental crust except in the Niger delta, where the basement rock is interpreted to be oceanic crust. Most of the wells that penetrated the basement are in the Eastern Dahomey embayment of western Nigeria. A maximum thickness of about 12,000 m of sedimentary rocks is attained in the offshore western Niger delta, but maximum thicknesses of sedimentary rocks are about 2,000 m in the Chad basin and only 500 m in the Sokoto embayment.

text: The opposite effect is that of transpression, where converging movement of a curved fault plane causes collision of the opposing sides of the fault.  An example is the

text: San Bernardino Mountains

text: north of

text: Los Angeles

text: , which result from convergence along a curve in the

text: San Andreas fault

text: system.  The

text: Northridge earthquake

text: was caused by vertical movement along local thrust and reverse faults bunching up against the bend in the otherwise strike-slip fault environment.In Nigeria, the dominant type of basement rock intersected by wells drilled for hydrocarbons, limestone, or water is granite. The three sedimentary basins in Nigeria are underlain by continental crust except in the Niger delta, where the basement rock is interpreted to be oceanic crust. Most of the wells that penetrated the basement are in the Eastern Dahomey embayment of western Nigeria. A maximum thickness of about 12,000 m of sedimentary rocks is attained in the offshore western Niger delta, but maximum thicknesses of sedimentary rocks are about 2,000 m in the

text: Chad basin

text: and only 500 m in the Sokoto embayment.

answers: NDQ_003351

answers: transpression

answers: NDQ_003352

answers: increases in thickness

answers: NDQ_003353

answers: collapsing movement

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: strike fault

answers: NDQ_003356

answers: collide

answers: NDQ_003357

answers: vertical movement along local thrust and reverse faults bunching up against the bend

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: converging movement

answers: NDQ_003360

answers: faults

answers: NDQ_003362

answers: the San Bernardino Mountains north of Los Angeles, which result from convergence along a curve in the San Andreas fault system

answers: NDQ_003363

answers: San Andreas fault

answers: NDQ_003371

answers: What is the opposite effect of transpression?

answers: NDQ_003373

answers: What is the opposite effect of transpression?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: no

answers: NDQ_003380

answers: What is the opposite effect of transpression?

answers: NDQ_003381

answers: What is the opposite effect of transpression?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: What is the opposite effect of transpression

answers: NDQ_003384

answers: What is the opposite effect of transpression?

answers: NDQ_003385

answers: fault zone

answers: NDQ_003386

answers: vertical movement

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: What is the opposite effect of transpression?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: strike-slip

answers: NDQ_003391

answers: basement

answers: NDQ_003392

answers: strike-slip

answers: NDQ_003393

answers: basement

answers: NDQ_003394

answers: curved fault

answers: NDQ_003395

answers: The Northridge earthquake was caused by vertical movement

answers: NDQ_003396

answers: strike-slip fault

answers: NDQ_003351

answers: transpression,

answers: NDQ_003352

answers: transpression,

answers: NDQ_003353

answers: transpression,

answers: NDQ_003354

answers: The opposite effect is that of transpression,

answers: NDQ_003355

answers: strike-slip

answers: NDQ_003356

answers: transpression,

answers: NDQ_003357

answers: strike-slip

answers: NDQ_003358

answers: transpression,

answers: NDQ_003359

answers: converging movement

answers: NDQ_003360

answers: San Andreas fault system.

answers: NDQ_003362

answers: transpression,

answers: NDQ_003363

answers: convergence along a curve in the San Andreas fault system.

answers: NDQ_003371

answers: thrust

answers: NDQ_003373

answers: granite.

answers: NDQ_003376

answers: transpression,

answers: NDQ_003378

answers: strike-slip

answers: NDQ_003379

answers: vertical

answers: NDQ_003380

answers: transpression,

answers: NDQ_003381

answers: transpression,

answers: NDQ_003382

answers: transpression,

answers: NDQ_003383

answers: transpression,

answers: NDQ_003384

answers: The opposite effect is that of transpression,

answers: NDQ_003385

answers: strike-slip fault environment.In

answers: NDQ_003386

answers: strike-slip fault environment.In

answers: NDQ_003387

answers: transpression,

answers: NDQ_003388

answers: strike-slip fault environment.In

answers: NDQ_003389

answers: transpression,

answers: NDQ_003390

answers: strike-slip

answers: NDQ_003391

answers: granite.

answers: NDQ_003392

answers: strike-slip

answers: NDQ_003393

answers: granite.

answers: NDQ_003394

answers: curved

answers: NDQ_003395

answers: strike-slip fault environment.In

answers: NDQ_003396

answers: strike-slip fault

text: In geology, a fault is a planar fracture or discontinuity in a volume of rock, across which there has been significant displacement as a result of rock mass movement. Large faults within the Earth's crust result from the action of plate tectonic forces, with the largest forming the boundaries between the plates, such as subduction zones or transform faults. Energy release associated with rapid movement on active faults is the cause of most earthquakes.

text: In

text: geology

text: , a fault is a

text: planar

text: fracture

text: or discontinuity in a volume of

text: rock

text: , across which there has been significant displacement as a result of rock mass movement. Large faults within the Earth's

text: crust

text: result from the action of

text: plate tectonic

text: forces, with the largest forming the boundaries between the plates, such as

text: subduction zones

text: or

text: transform fault

text: s. Energy release associated with rapid movement on

text: active fault

text: s is the cause of most

text: earthquake

text: s.

answers: NDQ_003351

answers: transform faults

answers: NDQ_003352

answers: causes more displacement

answers: NDQ_003353

answers: significant displacement

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: subduction zone

answers: NDQ_003356

answers: move

answers: NDQ_003357

answers: significant displacement as a result of rock mass movement

answers: NDQ_003358

answers: discontinuity

answers: NDQ_003359

answers: mass movement

answers: NDQ_003360

answers: active faults

answers: NDQ_003362

answers: Energy release associated with rapid movement on active faults is the cause of most earthquakes.

answers: NDQ_003363

answers: subduction zones

answers: NDQ_003371

answers: What may be the cause of most earthquakes?

answers: NDQ_003373

answers: unanswerable

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: significant displacement

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What is the cause of most earthquakes?

answers: NDQ_003381

answers: Which of the following is not a cause of most earthquakes?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: Fault zone

answers: NDQ_003386

answers: yes

answers: NDQ_003387

answers: Which of the following is not the cause of most earthquakes?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip faults, subduction zones, or transform faults?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: transform faults

answers: NDQ_003391

answers: subduction zones

answers: NDQ_003392

answers: transform faults

answers: NDQ_003393

answers: subduction zones

answers: NDQ_003394

answers: transform faults

answers: NDQ_003395

answers: transform faults

answers: NDQ_003396

answers: transform faults

answers: NDQ_003351

answers: earthquakes.

answers: NDQ_003352

answers: displacement

answers: NDQ_003353

answers: displacement

answers: NDQ_003354

answers: In geology,

answers: NDQ_003355

answers: fault

answers: NDQ_003356

answers: earthquakes.

answers: NDQ_003357

answers: significant displacement

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: significant displacement as a result of rock mass movement.

answers: NDQ_003360

answers: plate tectonic forces,

answers: NDQ_003362

answers: significant displacement as a result of rock mass movement.

answers: NDQ_003363

answers: plate tectonic forces,

answers: NDQ_003371

answers: transform faults.

answers: NDQ_003373

answers: fault

answers: NDQ_003376

answers: plate tectonic forces,

answers: NDQ_003378

answers: Energy release

answers: NDQ_003379

answers: subduction zones or transform faults.

answers: NDQ_003380

answers: displacement

answers: NDQ_003381

answers: displacement as a result of rock mass movement.

answers: NDQ_003382

answers: subduction zones or transform faults.

answers: NDQ_003383

answers: displacement as a result of rock mass movement.

answers: NDQ_003384

answers: fault

answers: NDQ_003385

answers: subduction zones or transform faults.

answers: NDQ_003386

answers: Energy release

answers: NDQ_003387

answers: plate tectonic forces,

answers: NDQ_003388

answers: plate tectonic forces,

answers: NDQ_003389

answers: plate tectonic forces,

answers: NDQ_003390

answers: transform faults.

answers: NDQ_003391

answers: subduction zones

answers: NDQ_003392

answers: transform faults.

answers: NDQ_003393

answers: subduction zones

answers: NDQ_003394

answers: transform faults.

answers: NDQ_003395

answers: transform faults.

answers: NDQ_003396

answers: transform faults.

text: The Andean Volcanic Belt consists of three main volcanic zones: the Northern Volcanic Zone (from 2° N to 5° S), the Central Volcanic Zone (16° to 28° S) and the Southern Volcanic Zone (33° to 46° S). Active volcanism occurs where the Nazca Plate subducts beneath the South American Plate. The plates are separated by shallower  subduction zones, with no present-day volcanism. These shallower zones have been attributed to the high speed of the plate collision, the young age of the subducting oceanic lithosphere and the curvature of the subducting plate. The most plausible theory is that variations in buoyancy of a subducting plate creates a flat subduction zone. The Cocos, Juan Fernandez and Nazca Ridges are associated with such volcanic gaps where they collide with the oceanic trench. The subduction of spreading ridges can also diminish volcanism, as observed in the Chile Rise farther south. The buoyancy of these crustal structures may hinder subduction, reducing water supply to the mantle and inducing the formation of melts.

text: The

text: Andean Volcanic Belt

text: consists of three main volcanic zones: the

text: Northern Volcanic Zone

text: (from 2° N to 5° S), the Central Volcanic Zone (16° to 28° S) and the

text: Southern Volcanic Zone

text: (33° to 46° S). Active volcanism occurs where the

text: Nazca Plate

text: subducts

text: beneath the

text: South American Plate

text: . The plates are separated by shallower  subduction zones, with no present-day volcanism. These shallower zones have been attributed to the high speed of the plate collision, the young age of the subducting oceanic

text: lithosphere

text: and the curvature of the subducting plate. The most plausible theory is that variations in

text: buoyancy

text: of a subducting plate creates a flat subduction zone. The

text: Cocos

text: Juan Fernandez

text: and

text: Nazca Ridge

text: s are associated with such volcanic gaps where they collide with the

text: oceanic trench

text: . The subduction of

text: spreading ridge

text: s can also diminish volcanism, as observed in the

text: Chile Rise

text: farther south. The buoyancy of these crustal structures may hinder subduction, reducing water supply to the

text: mantle

text: and inducing the formation of

text: melts

answers: NDQ_003351

answers: buoyancy

answers: NDQ_003352

answers: subducts

answers: NDQ_003353

answers: water supply to the mantle

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: ridge

answers: NDQ_003356

answers: subduct

answers: NDQ_003357

answers: The plates are separated by shallower subduction zones, with no present-day volcanism

answers: NDQ_003358

answers: subduction zone

answers: NDQ_003359

answers: collides with another rock

answers: NDQ_003360

answers: Andean Volcanic Belt

answers: NDQ_003362

answers: present-day volcanism

answers: NDQ_003363

answers: Andean Volcanic Belt

answers: NDQ_003371

answers: What may hinder subduction, reducing water supply to the mantle

answers: NDQ_003373

answers: What is the most plausible theory about the flat subduction zone?

answers: NDQ_003376

answers: How many main volcanic zones does the Andean Volcanic Belt consist of?

answers: NDQ_003378

answers: How many main volcanic zones does the Andean Volcanic Belt consist of

answers: NDQ_003379

answers: How many main volcanic zones does the Andean Volcanic Belt consist of?

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What is the most likely reason for the shallower zones?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not a type of fold: Cocos, Juan Fernandez and Nazca Ridges?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: active volcanism

answers: NDQ_003387

answers: How many main volcanic zones does the Andean Volcanic Belt contain?

answers: NDQ_003388

answers: How many main volcanic zones does the Andean Volcanic Belt consist of?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: subduction zone

answers: NDQ_003391

answers: subduction zone

answers: NDQ_003392

answers: subduction zone

answers: NDQ_003393

answers: subduction zone

answers: NDQ_003394

answers: spreading ridges

answers: NDQ_003395

answers: Nazca Ridges are associated with such volcanic gaps

answers: NDQ_003396

answers: flat subduction zone

answers: NDQ_003351

answers: buoyancy

answers: NDQ_003352

answers: melts.

answers: NDQ_003353

answers: melts.

answers: NDQ_003354

answers: Active volcanism

answers: NDQ_003355

answers: ridges

answers: NDQ_003356

answers: melts.

answers: NDQ_003357

answers: subduction,

answers: NDQ_003358

answers: shallower subduction zones,

answers: NDQ_003359

answers: collide with the oceanic trench.

answers: NDQ_003360

answers: Active volcanism

answers: NDQ_003362

answers: no present-day volcanism.

answers: NDQ_003363

answers: Nazca Plate subducts beneath the South American Plate.

answers: NDQ_003371

answers: volcanic gaps where they collide with the oceanic trench.

answers: NDQ_003373

answers: reducing water supply to the mantle

answers: NDQ_003376

answers: shallower subduction zones,

answers: NDQ_003378

answers: Active volcanism

answers: NDQ_003379

answers: flat subduction zone.

answers: NDQ_003380

answers: Active volcanism

answers: NDQ_003381

answers: The buoyancy of these crustal structures may hinder subduction,

answers: NDQ_003382

answers: Active volcanism

answers: NDQ_003383

answers: The Cocos, Juan Fernandez and Nazca Ridges

answers: NDQ_003384

answers: Nazca Ridges

answers: NDQ_003385

answers: volcanic zones: the Northern Volcanic Zone

answers: NDQ_003386

answers: Active volcanism

answers: NDQ_003387

answers: buoyancy

answers: NDQ_003388

answers: high speed of the plate collision,

answers: NDQ_003389

answers: Active volcanism

answers: NDQ_003390

answers: Chile Rise

answers: NDQ_003391

answers: South American Plate.

answers: NDQ_003392

answers: Chile Rise

answers: NDQ_003393

answers: Nazca Ridges

answers: NDQ_003394

answers: oceanic trench.

answers: NDQ_003395

answers: oceanic trench.

answers: NDQ_003396

answers: flat subduction zone.

text: In the 60s and 70s a simple creationist model proposed that, "The Flood split the land mass into the present continents." Steve Austin and other creationists proposed a preliminary model of catastrophic plate tectonics (CPT) in 1994. Their work built on earlier papers by John Baumgardner and Russell Humphreys in 1986. Baumgardner proposed a model of mantel convection that allows for runaway subduction and Humphrey associated mantle convection with rapid magnetic reversals in earth history. Baumgardner's proposal holds that the rapid plunge of former oceanic plates into the mantle (caused by an unknown trigger-mechanism) increased local mantle pressures to the point that its viscosity dropped several magnitudes according to known properties of mantle silicates.  Once initiated, sinking plates caused the spread of low viscosity throughout the mantle resulting in runaway mantle-convection and catastrophic tectonic motion which dragged continents across the surface of the earth. Once the former ocean plates, which are thought to be denser than the mantle, reached the bottom of the mantle an equilibrium resulted.  Pressures dropped, viscosity increased, runaway mantle-convection stopped, leaving the surface of the earth rearranged.  Proponents point to subducted slabs in the mantle which are still relatively cool, which they regard as evidence that they have not been there for millions of years which would result in temperature equilibration.

text: In the 60s and 70s a simple creationist model proposed that, "The Flood split the land mass into the present continents." Steve Austin and other creationists proposed a preliminary model of catastrophic plate tectonics (CPT) in 1994. Their work built on earlier papers by

text: John Baumgardner

text: and

text: Russell Humphreys

text: in 1986. Baumgardner proposed a model of mantel convection that allows for runaway subduction and Humphrey associated mantle convection with rapid magnetic reversals in earth history. Baumgardner's proposal holds that the rapid plunge of former oceanic plates into the

text: mantle

text: (caused by an unknown trigger-mechanism) increased local mantle pressures to the point that its viscosity dropped several magnitudes according to known properties of mantle silicates.  Once initiated, sinking plates caused the spread of low viscosity throughout the mantle resulting in runaway mantle-convection and catastrophic

text: tectonic

text: motion which dragged continents across the surface of the earth. Once the former ocean plates, which are thought to be denser than the mantle, reached the bottom of the mantle an equilibrium resulted.  Pressures dropped, viscosity increased, runaway mantle-convection stopped, leaving the surface of the earth rearranged.  Proponents point to subducted slabs in the mantle which are still relatively cool, which they regard as evidence that they have not been there for millions of years which would result in temperature equilibration.

answers: NDQ_003351

answers: runaway subduction

answers: NDQ_003352

answers: viscosity drops

answers: NDQ_003353

answers: pressures to drop

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: subduction

answers: NDQ_003356

answers: runaway

answers: NDQ_003357

answers: runaway mantle-convection stopped

answers: NDQ_003358

answers: equilibrium

answers: NDQ_003359

answers: runaway

answers: NDQ_003360

answers: plate tectonics

answers: NDQ_003362

answers: runaway mantle-convection stopped

answers: NDQ_003363

answers: Subduction

answers: NDQ_003371

answers: What would result in temperature equilibration?

answers: NDQ_003373

answers: Why would a deeply buried rock be under compressive stresses

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a type of pressure: pressures, pressures, or pressures?

answers: NDQ_003381

answers: What is a result of confining stress?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What caused the spread of low viscosity throughout the mantle

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: plate tectonics

answers: NDQ_003387

answers: What caused the spread of low viscosity throughout the mantle?

answers: NDQ_003388

answers: What caused the spread of low viscosity throughout the mantle

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: subduction

answers: NDQ_003391

answers: subducted slabs

answers: NDQ_003392

answers: mantel convection

answers: NDQ_003393

answers: slabs

answers: NDQ_003394

answers: subduction

answers: NDQ_003395

answers: runaway mantle-convection

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: runaway subduction

answers: NDQ_003352

answers: viscosity

answers: NDQ_003353

answers: viscosity

answers: NDQ_003354

answers: In the 60s and 70s

answers: NDQ_003355

answers: subduction

answers: NDQ_003356

answers: low viscosity

answers: NDQ_003357

answers: runaway subduction

answers: NDQ_003358

answers: subducted slabs

answers: NDQ_003359

answers: sinking plates caused the spread of low viscosity

answers: NDQ_003360

answers: oceanic plates

answers: NDQ_003362

answers: "The Flood split the land mass into the present continents."

answers: NDQ_003363

answers: "The Flood

answers: NDQ_003371

answers: runaway subduction

answers: NDQ_003373

answers: subducted slabs in the mantle which are still relatively cool,

answers: NDQ_003376

answers: runaway mantle-convection

answers: NDQ_003378

answers: catastrophic tectonic motion

answers: NDQ_003379

answers: magnetic reversals

answers: NDQ_003380

answers: pressures

answers: NDQ_003381

answers: low viscosity

answers: NDQ_003382

answers: runaway subduction

answers: NDQ_003383

answers: mantle pressures to the point that its viscosity

answers: NDQ_003384

answers: mantel convection

answers: NDQ_003385

answers: catastrophic plate tectonics

answers: NDQ_003386

answers: catastrophic plate tectonics

answers: NDQ_003387

answers: mantel convection

answers: NDQ_003388

answers: runaway mantle-convection

answers: NDQ_003389

answers: runaway mantle-convection

answers: NDQ_003390

answers: subduction

answers: NDQ_003391

answers: subducted slabs

answers: NDQ_003392

answers: mantel convection

answers: NDQ_003393

answers: subducted slabs

answers: NDQ_003394

answers: magnetic reversals

answers: NDQ_003395

answers: magnetic reversals

answers: NDQ_003396

answers: magnetic reversals

text: The Lord Howe Rise is a deep sea plateau which extends from south west of New Caledonia to the Challenger Plateau, west of New Zealand in the south west of the Pacific Ocean. To its west is the Tasman Basin and to the east is the New Caledonia Basin. Lord Howe Rise has a total area of about 1,500,000 square km, and generally lies about 750 to 1,200 metres under water.  It is part of Zealandia, a much larger continent that is now mostly submerged, and so is composed of continental crust.

text: The Lord Howe Rise is a

text: deep sea

text: plateau

text: which extends from south west of

text: New Caledonia

text: to the

text: Challenger Plateau

text: , west of

text: New Zealand

text: in the south west of the

text: Pacific Ocean

text: . To its west is the

text: Tasman Basin

text: and to the east is the

text: New Caledonia Basin

text: . Lord Howe Rise has a total area of about 1,500,000 square km, and generally lies about 750 to 1,200 metres under water.  It is part of

text: Zealandia

text: , a much larger

text: continent

text: that is now mostly submerged, and so is composed of

text: continental crust

answers: NDQ_003351

answers: Lord Howe Rise

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: Lord Howe Rise

answers: NDQ_003356

answers: lie under water

answers: NDQ_003357

answers: Lord Howe Rise has a total area of about 1,500,000 square km

answers: NDQ_003358

answers: plateau

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: continental crust

answers: NDQ_003362

answers: Lord Howe Rise has a total area of about 1,500,000 square km

answers: NDQ_003363

answers: Pacific Ocean

answers: NDQ_003371

answers: What is the Lord Howe Rise?

answers: NDQ_003373

answers: How would you describe Lord Howe Rise?

answers: NDQ_003376

answers: What is the Lord Howe Rise?

answers: NDQ_003378

answers: What is Lord Howe Rise?

answers: NDQ_003379

answers: What is the dip of the fault plane in Lord Howe Rise?

answers: NDQ_003380

answers: What is Lord Howe Rise?

answers: NDQ_003381

answers: How does Lord Howe Rise deform?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the Lord Howe Rise?

answers: NDQ_003384

answers: What does Lord Howe Rise have a total area of about 1,500,000 square km?

answers: NDQ_003385

answers: What is Lord Howe Rise?

answers: NDQ_003386

answers: What is the Lord Howe Rise?

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: Lord Howe Rise or Tasman Basin?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip faults, Tasman Basin or Lord Howe Rise?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: Lord Howe Rise

answers: NDQ_003392

answers: Lord Howe Rise

answers: NDQ_003393

answers: The Lord Howe Rise

answers: NDQ_003394

answers: lateral fault

answers: NDQ_003395

answers: Lord Howe Rise has a total area of about 1,500,000 square km

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: south west of the Pacific Ocean.

answers: NDQ_003352

answers: 750 to 1,200 metres under water.

answers: NDQ_003353

answers: continental crust.

answers: NDQ_003354

answers: The Lord Howe Rise

answers: NDQ_003355

answers: Challenger Plateau,

answers: NDQ_003356

answers: 750 to 1,200 metres under water.

answers: NDQ_003357

answers: 750 to 1,200 metres under water.

answers: NDQ_003358

answers: deep sea plateau

answers: NDQ_003359

answers: crust.

answers: NDQ_003360

answers: Pacific Ocean.

answers: NDQ_003362

answers: a much larger continent that is now mostly submerged,

answers: NDQ_003363

answers: Pacific Ocean.

answers: NDQ_003371

answers: The Lord Howe Rise

answers: NDQ_003373

answers: 750 to 1,200 metres under water.

answers: NDQ_003376

answers: New Caledonia Basin.

answers: NDQ_003378

answers: 1,500,000 square km,

answers: NDQ_003379

answers: south west of the Pacific Ocean.

answers: NDQ_003380

answers: continental crust.

answers: NDQ_003381

answers: 750 to 1,200 metres under water.

answers: NDQ_003382

answers: Challenger Plateau,

answers: NDQ_003383

answers: The Lord Howe Rise

answers: NDQ_003384

answers: Challenger Plateau,

answers: NDQ_003385

answers: The Lord Howe Rise

answers: NDQ_003386

answers: south west of the Pacific Ocean.

answers: NDQ_003387

answers: The Lord Howe Rise

answers: NDQ_003388

answers: south west of the Pacific Ocean.

answers: NDQ_003389

answers: continental crust.

answers: NDQ_003390

answers: The Lord Howe Rise

answers: NDQ_003391

answers: The Lord Howe Rise

answers: NDQ_003392

answers: The Lord Howe Rise

answers: NDQ_003393

answers: Lord Howe Rise

answers: NDQ_003394

answers: Challenger Plateau,

answers: NDQ_003395

answers: south west of the Pacific Ocean.

answers: NDQ_003396

answers: Challenger Plateau,

text: The term 'megalineament' has been used to describe such features on a continental scale. The trace of the San Andreas Fault might be considered an example.The Trans Brazilian Lineament and the Trans-Saharan Belt, taken together, form perhaps the longest coherent shear zone on the Earth, extending for about 4,000 km.

text: The term 'megalineament' has been used to describe such features on a continental scale. The trace of the

text: San Andreas Fault

text: might be considered an example.The

text: Trans Brazilian Lineament

text: and the

text: Trans-Saharan Belt

text: , taken together, form perhaps the longest coherent shear zone on the Earth, extending for about 4,000 km.

answers: NDQ_003351

answers: shear

answers: NDQ_003352

answers: shears

answers: NDQ_003353

answers: shear

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: megalineament

answers: NDQ_003356

answers: shear

answers: NDQ_003357

answers: shear zone

answers: NDQ_003358

answers: shear zone

answers: NDQ_003359

answers: shears

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: The San Andreas Fault might be considered an example

answers: NDQ_003363

answers: San Andreas Fault

answers: NDQ_003371

answers: Which of the following is not an example of a megalineament: the San Andreas Fault or the Trans Brazilian Lineament?

answers: NDQ_003373

answers: What is the main idea of this passage?

answers: NDQ_003376

answers: What is the term used to describe features on a continental scale?

answers: NDQ_003378

answers: What is the term used to describe features on a continental scale?

answers: NDQ_003379

answers: What is the dip of the fault plane in a strike-slip fault

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What is a consequence of confining stress?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: What is the term for a fold that arches upward?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: Which of the following is not the cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not a normal fault: San Andreas Fault, Trans Brazilian Lineament or Trans Saharan Belt?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip faults, megalineament or strike-slip faults?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: San Andreas Fault

answers: NDQ_003391

answers: megalineament

answers: NDQ_003392

answers: San Andreas Fault

answers: NDQ_003393

answers: megalineament

answers: NDQ_003394

answers: San Andreas Fault

answers: NDQ_003395

answers: San Andreas Fault

answers: NDQ_003396

answers: San Andreas Fault

answers: NDQ_003351

answers: shear zone

answers: NDQ_003352

answers: shear zone

answers: NDQ_003353

answers: shear

answers: NDQ_003354

answers: The term'megalineament'

answers: NDQ_003355

answers: term'megalineament'

answers: NDQ_003356

answers: shear zone

answers: NDQ_003357

answers: coherent shear zone

answers: NDQ_003358

answers: term'megalineament'

answers: NDQ_003359

answers: San Andreas Fault

answers: NDQ_003360

answers: term'megalineament'

answers: NDQ_003362

answers: term'megalineament'

answers: NDQ_003363

answers: term'megalineament'

answers: NDQ_003371

answers: term'megalineament'

answers: NDQ_003373

answers: The term'megalineament'

answers: NDQ_003376

answers: The term'megalineament'

answers: NDQ_003378

answers: shear

answers: NDQ_003379

answers: San Andreas Fault

answers: NDQ_003380

answers: shear zone

answers: NDQ_003381

answers: term'megalineament'

answers: NDQ_003382

answers: The term'megalineament'

answers: NDQ_003383

answers: The term'megalineament'

answers: NDQ_003384

answers: term'megalineament'

answers: NDQ_003385

answers: term'megalineament'

answers: NDQ_003386

answers: San Andreas Fault

answers: NDQ_003387

answers: San Andreas Fault

answers: NDQ_003388

answers: The term'megalineament'

answers: NDQ_003389

answers: The term'megalineament'

answers: NDQ_003390

answers: San Andreas Fault

answers: NDQ_003391

answers: term'megalineament'

answers: NDQ_003392

answers: San Andreas Fault

answers: NDQ_003393

answers: term'megalineament'

answers: NDQ_003394

answers: San Andreas Fault

answers: NDQ_003395

answers: San Andreas Fault

answers: NDQ_003396

answers: San Andreas Fault

text: An example of a convergence zone is the Intertropical Convergence Zone (ITCZ), a low pressure area which girdles the Earth at the Equator. Another example is the South Pacific convergence zone that extends from the western Pacific Ocean toward French Polynesia.

text: An example of a convergence zone is the

text: Intertropical Convergence Zone

text: (ITCZ), a

text: low pressure area

text: which girdles the

text: Earth

text: at the

text: Equator

text: . Another example is the

text: South Pacific convergence zone

text: that extends from the western

text: Pacific Ocean

text: toward

text: French Polynesia

answers: NDQ_003351

answers: low pressure

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: pressure to increase

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: Convergence Zone

answers: NDQ_003356

answers: converge

answers: NDQ_003357

answers: ITCZ is a low pressure area

answers: NDQ_003358

answers: Convergence Zone

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's surface

answers: NDQ_003362

answers: girdles the Earth at the Equator

answers: NDQ_003363

answers: the Equator

answers: NDQ_003371

answers: Which of the following is not an example of a convergence zone?

answers: NDQ_003373

answers: How would you describe a rock that is deeply buried?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: The dip of the fault plane is vertical

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What is the result of confining stress?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: unanswerable

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: Which of the following is not an example of a convergence zone: the Intertropical Convergence Zone or the South Pacific convergence zone?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: Convergence zone

answers: NDQ_003391

answers: Convergence zone

answers: NDQ_003392

answers: Convergence zone

answers: NDQ_003393

answers: Convergence zone

answers: NDQ_003394

answers: converging zone

answers: NDQ_003395

answers: a fault with a vertical fault plane

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: convergence zone

answers: NDQ_003352

answers: convergence zone

answers: NDQ_003353

answers: low pressure

answers: NDQ_003354

answers: Intertropical Convergence Zone

answers: NDQ_003355

answers: convergence zone

answers: NDQ_003356

answers: convergence zone

answers: NDQ_003357

answers: convergence zone

answers: NDQ_003358

answers: convergence zone

answers: NDQ_003359

answers: convergence zone

answers: NDQ_003360

answers: convergence zone

answers: NDQ_003362

answers: a low pressure area which girdles the Earth at the Equator.

answers: NDQ_003363

answers: the Equator.

answers: NDQ_003371

answers: convergence zone

answers: NDQ_003373

answers: convergence zone

answers: NDQ_003376

answers: convergence zone

answers: NDQ_003378

answers: convergence zone

answers: NDQ_003379

answers: convergence zone

answers: NDQ_003380

answers: convergence zone

answers: NDQ_003381

answers: convergence zone

answers: NDQ_003382

answers: Intertropical Convergence Zone

answers: NDQ_003383

answers: convergence zone is the Intertropical Convergence Zone

answers: NDQ_003384

answers: convergence zone

answers: NDQ_003385

answers: convergence zone

answers: NDQ_003386

answers: convergence zone

answers: NDQ_003387

answers: convergence zone

answers: NDQ_003388

answers: convergence zone

answers: NDQ_003389

answers: convergence zone

answers: NDQ_003390

answers: convergence zone

answers: NDQ_003391

answers: convergence zone

answers: NDQ_003392

answers: convergence zone

answers: NDQ_003393

answers: convergence zone

answers: NDQ_003394

answers: convergence zone

answers: NDQ_003395

answers: convergence zone

answers: NDQ_003396

answers: convergence zone

text: The stable form of cobalt is produced in supernovas through the r-process. It comprises 0.0029% of the Earth's crust and is one of the first transition metals.

text: The stable form of cobalt is produced in

text: supernova

text: s through the

text: r-process

text: . It comprises

text: 0.0029% of the Earth's crust

text: and is one of the first

text: transition metal

text: s.

answers: NDQ_003351

answers: cobalt

answers: NDQ_003352

answers: is exposed to more heat

answers: NDQ_003353

answers: voids to form

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: cobalt is present in what form?

answers: NDQ_003358

answers: crack

answers: NDQ_003359

answers: is pushed together

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: cobalt is produced in supernovas

answers: NDQ_003363

answers: supernovas

answers: NDQ_003371

answers: What is one of the first transition metals produced in supernovas through the r-process?

answers: NDQ_003373

answers: How would you describe the stress?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: what is the second to last transition metal mentioned?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: Which of the following is not a type of stress?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not caused by stress: supernovas, cobalt, or the r-process?

answers: NDQ_003384

answers: What is one of the first transition metals?

answers: NDQ_003385

answers: What is one of the first transition metals?

answers: NDQ_003386

answers: Which is not the reason for earthquakes?

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: normal faults or supernovas?

answers: NDQ_003388

answers: Which of the following is not a result of shear stress: strike-slip faults, supernovas or shear stress?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: unanswerable

answers: NDQ_003392

answers: r-process

answers: NDQ_003393

answers: unanswerable

answers: NDQ_003394

answers: isobath

answers: NDQ_003395

answers: is a type of

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: r-process.

answers: NDQ_003352

answers: r-process.

answers: NDQ_003353

answers: r-process.

answers: NDQ_003354

answers: The stable form of cobalt

answers: NDQ_003355

answers: r-process.

answers: NDQ_003356

answers: r-process.

answers: NDQ_003357

answers: The stable form of cobalt

answers: NDQ_003358

answers: The stable form of cobalt is produced in supernovas

answers: NDQ_003359

answers: r-process.

answers: NDQ_003360

answers: supernovas

answers: NDQ_003362

answers: The stable form of cobalt is produced in supernovas

answers: NDQ_003363

answers: supernovas

answers: NDQ_003371

answers: r-process.

answers: NDQ_003373

answers: The stable form of cobalt is produced in supernovas

answers: NDQ_003376

answers: The stable form of cobalt is produced in supernovas

answers: NDQ_003378

answers: r-process.

answers: NDQ_003379

answers: r-process.

answers: NDQ_003380

answers: r-process.

answers: NDQ_003381

answers: The stable form of cobalt is produced in supernovas

answers: NDQ_003382

answers: r-process.

answers: NDQ_003383

answers: r-process.

answers: NDQ_003384

answers: r-process.

answers: NDQ_003385

answers: r-process.

answers: NDQ_003386

answers: r-process.

answers: NDQ_003387

answers: r-process.

answers: NDQ_003388

answers: r-process.

answers: NDQ_003389

answers: r-process.

answers: NDQ_003390

answers: r-process.

answers: NDQ_003391

answers: r-process.

answers: NDQ_003392

answers: r-process.

answers: NDQ_003393

answers: r-process.

answers: NDQ_003394

answers: r-process.

answers: NDQ_003395

answers: r-process.

answers: NDQ_003396

answers: r-process.

text: Some rifts show a complex and prolonged history of rifting, with several distinct phases. The North Sea rift shows evidence of several separate rift phases from the Permian through to the Earliest Cretaceous, a period of over 100 million years.

text: Some rifts show a complex and prolonged history of rifting, with several distinct phases. The North Sea rift shows evidence of several separate rift phases from the

text: Permian

text: through to the Earliest

text: Cretaceous

text: , a period of over 100 million years.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: more likely to crack

answers: NDQ_003353

answers: rifting

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: rift

answers: NDQ_003356

answers: change shape

answers: NDQ_003357

answers: several distinct phases of rifting

answers: NDQ_003358

answers: rift

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: The North Sea rift shows evidence of several separate rift phases from the Permian to the Earliest Cretaceous

answers: NDQ_003363

answers: the Permian

answers: NDQ_003371

answers: Which of the following is not a type of rift: Permian through to the Earliest Cretaceous

answers: NDQ_003373

answers: What is the best title for this passage?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What does the North Sea rift show evidence of?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: what is the first time period mentioned?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: Which of the following is not the cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: normal faults, rifting or rifting?

answers: NDQ_003388

answers: Which of the following is not a type of fault: Strike-slip faults or shear stress?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: rifting

answers: NDQ_003391

answers: rifting

answers: NDQ_003392

answers: rifting

answers: NDQ_003393

answers: rifting

answers: NDQ_003394

answers: rifting

answers: NDQ_003395

answers: The North Sea rift

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: rifting,

answers: NDQ_003352

answers: rifting,

answers: NDQ_003353

answers: rifting,

answers: NDQ_003354

answers: Some rifts show a complex and prolonged history of rifting,

answers: NDQ_003355

answers: rifts

answers: NDQ_003356

answers: rifting,

answers: NDQ_003357

answers: rifting,

answers: NDQ_003358

answers: rifts

answers: NDQ_003359

answers: rifting,

answers: NDQ_003360

answers: rifts

answers: NDQ_003362

answers: 100 million years.

answers: NDQ_003363

answers: rifting,

answers: NDQ_003371

answers: Some rifts show a complex and prolonged history of rifting,

answers: NDQ_003373

answers: Some rifts show a complex and prolonged history of rifting,

answers: NDQ_003376

answers: Some rifts show a complex and prolonged history of rifting,

answers: NDQ_003378

answers: rifting,

answers: NDQ_003379

answers: Some rifts show a complex and prolonged history of rifting,

answers: NDQ_003380

answers: rifting,

answers: NDQ_003381

answers: Some rifts show a complex and prolonged history of rifting,

answers: NDQ_003382

answers: Some rifts show a complex and prolonged history of rifting,

answers: NDQ_003383

answers: rifting,

answers: NDQ_003384

answers: Some rifts show a complex and prolonged history of rifting,

answers: NDQ_003385

answers: rifts

answers: NDQ_003386

answers: rifting,

answers: NDQ_003387

answers: Some rifts show a complex and prolonged history of rifting,

answers: NDQ_003388

answers: Some rifts show a complex and prolonged history of rifting,

answers: NDQ_003389

answers: rifting,

answers: NDQ_003390

answers: rifts

answers: NDQ_003391

answers: rifts

answers: NDQ_003392

answers: rifts show a complex and prolonged history of rifting,

answers: NDQ_003393

answers: rifts

answers: NDQ_003394

answers: Some rifts

answers: NDQ_003395

answers: Some rifts show a complex and prolonged history of rifting,

answers: NDQ_003396

answers: rifts

text: Lake Baikal is in a rift valley, created by the Baikal Rift Zone, where the Earth's crust is slowly pulling apart. At  long and  wide, Lake Baikal has the largest surface area of any freshwater lake in Asia, at , and is the deepest lake in the world at . The bottom of the lake is  below sea level, but below this lies some  of sediment, placing the rift floor some  below the surface: the deepest continental rift on Earth. In geological terms, the rift is young and active—it widens about 2 cm (0.79 in) per year. The fault zone is also seismically active; hot springs occur in the area and notable earthquakes happen every few years. The lake is divided into three basins: North, Central, and South, with depths about , , and , respectively. Fault-controlled accommodation zones rising to depths about  separate the basins. The North and Central basins are separated by Academician Ridge, while the area around the Selenga Delta and the Buguldeika Saddle separates the Central and South basins. The lake drains into the Angara tributary of the Yenisei. Notable landforms include Cape Ryty on Baikal's northwest coast.

text: Lake Baikal is in a rift valley, created by the

text: Baikal Rift Zone

text: , where the Earth's crust is slowly pulling apart. At  long and  wide, Lake Baikal has the largest surface area of any freshwater lake in Asia, at , and is the deepest lake in the world at . The bottom of the lake is  below sea level, but below this lies some  of

text: sediment

text: , placing the rift floor some  below the surface: the deepest continental

text: rift

text: on Earth. In geological terms, the rift is young and active—it widens about 2 cm (0.79 in) per year. The fault zone is also seismically active; hot springs occur in the area and notable

text: earthquake

text: s happen every few years. The lake is divided into three basins: North, Central, and South, with depths about , , and , respectively. Fault-controlled accommodation zones rising to depths about  separate the basins. The North and Central basins are separated by

text: Academician Ridge

text: , while the area around the Selenga Delta and the Buguldeika Saddle separates the Central and South basins. The lake drains into the

text: Angara

text: tributary of the

text: Yenisei

text: . Notable landforms include

text: Cape Ryty

text: on Baikal's northwest coast.

answers: NDQ_003351

answers: seismically active

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: rift valley

answers: NDQ_003356

answers: widens about 2 cm

answers: NDQ_003357

answers: Fault-controlled accommodation zones rising to depths about separate the basins

answers: NDQ_003358

answers: fault zone

answers: NDQ_003359

answers: pulls apart

answers: NDQ_003360

answers: faults

answers: NDQ_003362

answers: unanswerable

answers: NDQ_003363

answers: Baikal Rift Zone

answers: NDQ_003371

answers: How many basins does Lake Baikal have?

answers: NDQ_003373

answers: Why is the bottom of the lake below sea level?

answers: NDQ_003376

answers: How many basins does Lake Baikal have?

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What type of stress occurs when the Earth's crust is pulling apart?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What type of fold is Academician Ridge?

answers: NDQ_003385

answers: Fault-controlled accommodation zones

answers: NDQ_003386

answers: What is the cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: hot springs, hot springs, or normal faults?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip faults, rift faults, or rift valleys?

answers: NDQ_003389

answers: The Baikal Rift Zone

answers: NDQ_003390

answers: Fault-controlled accommodation zones

answers: NDQ_003391

answers: rift valley

answers: NDQ_003392

answers: Academician Ridge

answers: NDQ_003393

answers: Academician Ridge

answers: NDQ_003394

answers: The fault zone

answers: NDQ_003395

answers: Fault-controlled accommodation zones

answers: NDQ_003396

answers: Fault-controlled accommodation zones

answers: NDQ_003351

answers: hot springs occur in the area and notable earthquakes

answers: NDQ_003352

answers: hot springs occur in the area and notable earthquakes

answers: NDQ_003353

answers: hot springs occur in the area and notable earthquakes

answers: NDQ_003354

answers: Baikal Rift Zone,

answers: NDQ_003355

answers: rift valley,

answers: NDQ_003356

answers: hot springs occur in the area and notable earthquakes

answers: NDQ_003357

answers: hot springs occur in the area and notable earthquakes happen every few years.

answers: NDQ_003358

answers: fault zone

answers: NDQ_003359

answers: pulling apart.

answers: NDQ_003360

answers: Baikal Rift Zone,

answers: NDQ_003362

answers: hot springs occur in the area and notable earthquakes happen every few years.

answers: NDQ_003363

answers: Baikal Rift Zone,

answers: NDQ_003371

answers: Baikal Rift Zone,

answers: NDQ_003373

answers: sediment,

answers: NDQ_003376

answers: Fault-controlled accommodation zones

answers: NDQ_003378

answers: earthquakes happen every few years.

answers: NDQ_003379

answers: Baikal Rift Zone,

answers: NDQ_003380

answers: earthquakes

answers: NDQ_003381

answers: Fault-controlled accommodation zones

answers: NDQ_003382

answers: Baikal Rift Zone,

answers: NDQ_003383

answers: Fault-controlled accommodation zones

answers: NDQ_003384

answers: Academician Ridge,

answers: NDQ_003385

answers: Fault-controlled accommodation zones

answers: NDQ_003386

answers: hot springs occur in the area and notable earthquakes happen every few years.

answers: NDQ_003387

answers: Baikal Rift Zone,

answers: NDQ_003388

answers: Baikal Rift Zone,

answers: NDQ_003389

answers: Baikal Rift Zone,

answers: NDQ_003390

answers: Baikal Rift Zone,

answers: NDQ_003391

answers: Baikal Rift Zone,

answers: NDQ_003392

answers: Baikal Rift Zone,

answers: NDQ_003393

answers: Academician Ridge,

answers: NDQ_003394

answers: Baikal Rift Zone,

answers: NDQ_003395

answers: Baikal Rift Zone,

answers: NDQ_003396

answers: Baikal Rift Zone,

text: The North American Plate is a tectonic plate covering most of North America, Greenland, Cuba, the Bahamas, extreme northeastern Russia, and parts of Iceland and the Azores.  It extends eastward to the Mid-Atlantic Ridge and westward to the Chersky Range in eastern Siberia.  The plate includes both continental and oceanic crust.  The interior of the main continental landmass includes an extensive granitic core called a craton.  Along most of the edges of this craton are fragments of crustal material called  terranes, accreted to the craton by tectonic actions over the long span of geologic time. It is thought that much of North America west of the Rocky Mountains is composed of such terranes.

text: The North American Plate is a

text: tectonic plate

text: covering most of

text: North America

text: Greenland

text: Cuba

text: , the

text: Bahamas

text: , extreme northeastern

text: Russia

text: , and parts of

text: Iceland

text: and

text: the Azores

text: .  It extends eastward to the

text: Mid-Atlantic Ridge

text: and westward to the

text: Chersky Range

text: in eastern Siberia.  The plate includes both

text: continental

text: and

text: oceanic crust

text: .  The interior of the main continental landmass includes an extensive

text: granitic

text: core called a

text: craton

text: .  Along most of the edges of this craton are fragments of crustal material called

text: terrane

text: s, accreted to the craton by tectonic actions over the long span of geologic time. It is thought that much of North America west of the

text: Rocky Mountains

text: is composed of such terranes.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: more likely to crack

answers: NDQ_003353

answers: tectonic actions

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: craton

answers: NDQ_003356

answers: accret

answers: NDQ_003357

answers: fragments of crustal material are accreted to the craton by tectonic actions

answers: NDQ_003358

answers: Ridge

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: tectonic plates

answers: NDQ_003362

answers: much of North America west of the Rocky Mountains is composed of such terranes.

answers: NDQ_003363

answers: The North American Plate

answers: NDQ_003371

answers: Which of the following is not a craton: continental, oceanic, or granitic?

answers: NDQ_003373

answers: What is a craton?

answers: NDQ_003376

answers: Which of the following is not a type of terrain: basin-and-range or craton?

answers: NDQ_003378

answers: What is the amount of the ground moving in an earthquake?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What type of stress does the craton have?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not a type of fold: Mid-Atlantic Ridge or Chersky Range?

answers: NDQ_003385

answers: What is the term for an area where faults are clustered?

answers: NDQ_003386

answers: Which of the following is not a cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not a type of normal fault?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip, Mid-Atlantic Ridge or Chersky Range?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: tectonic plate

answers: NDQ_003391

answers: craton

answers: NDQ_003392

answers: tectonic plate

answers: NDQ_003393

answers: craton

answers: NDQ_003394

answers: tectonic plate

answers: NDQ_003395

answers: The Mid-Atlantic Ridge

answers: NDQ_003396

answers: Mid-Atlantic Ridge

answers: NDQ_003351

answers: tectonic actions

answers: NDQ_003352

answers: terranes,

answers: NDQ_003353

answers: terranes,

answers: NDQ_003354

answers: The North American Plate

answers: NDQ_003355

answers: terranes,

answers: NDQ_003356

answers: granitic

answers: NDQ_003357

answers: tectonic actions

answers: NDQ_003358

answers: craton.

answers: NDQ_003359

answers: tectonic actions

answers: NDQ_003360

answers: tectonic actions

answers: NDQ_003362

answers: The North American Plate

answers: NDQ_003363

answers: tectonic actions

answers: NDQ_003371

answers: The North American Plate

answers: NDQ_003373

answers: terranes,

answers: NDQ_003376

answers: accreted to the craton by tectonic actions

answers: NDQ_003378

answers: terranes,

answers: NDQ_003379

answers: craton.

answers: NDQ_003380

answers: tectonic actions

answers: NDQ_003381

answers: granitic core called a craton.

answers: NDQ_003382

answers: Mid-Atlantic Ridge

answers: NDQ_003383

answers: tectonic actions

answers: NDQ_003384

answers: terranes,

answers: NDQ_003385

answers: craton.

answers: NDQ_003386

answers: tectonic actions

answers: NDQ_003387

answers: tectonic actions

answers: NDQ_003388

answers: tectonic actions

answers: NDQ_003389

answers: tectonic actions

answers: NDQ_003390

answers: The North American Plate is a tectonic plate

answers: NDQ_003391

answers: terranes,

answers: NDQ_003392

answers: The North American Plate

answers: NDQ_003393

answers: granitic core called a craton.

answers: NDQ_003394

answers: The North American Plate

answers: NDQ_003395

answers: The North American Plate

answers: NDQ_003396

answers: Mid-Atlantic Ridge

text: The Earth's crust is made of approximately 5% of heavy metals by weight, with iron comprising 95% of this quantity. Light metals (~20%) and nonmetals (~75%) make up the other 95% of the crust. Despite their overall scarcity, heavy metals can become concentrated in economically extractable quantities as a result of mountain building, erosion, or other geological processes.

text: The Earth's crust is made of approximately 5% of heavy metals by weight, with iron comprising 95% of this quantity. Light metals (~20%) and nonmetals (~75%) make up the other 95% of the crust. Despite their overall scarcity, heavy metals can become concentrated in economically extractable quantities as a result of

text: mountain building

text: erosion

text: , or other

text: geological processes

answers: NDQ_003351

answers: nonmetals

answers: NDQ_003352

answers: metals can become concentrated

answers: NDQ_003353

answers: erosion

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: mountain

answers: NDQ_003356

answers: oxidize

answers: NDQ_003357

answers: iron comprises 95% of this quantity

answers: NDQ_003358

answers: unmoving

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: heavy metals

answers: NDQ_003362

answers: heavy metals can become concentrated in economically extractable quantities

answers: NDQ_003363

answers: heavy metals

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: heavy metals can become concentrated

answers: NDQ_003376

answers: heavy metals

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: vertical

answers: NDQ_003380

answers: What can become concentrated in economically extractable quantities as a result of mountain building

answers: NDQ_003381

answers: What is a result of mountain building?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: unanswerable

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: heavy metals can become concentrated in economically extractable quantities

answers: NDQ_003389

answers: nonmetals

answers: NDQ_003390

answers: Erosion

answers: NDQ_003391

answers: mountain

answers: NDQ_003392

answers: unanswerable

answers: NDQ_003393

answers: mountain

answers: NDQ_003394

answers: mountain building

answers: NDQ_003395

answers: NDQ_003396

answers: NDQ_003351

answers: 5% of heavy metals

answers: NDQ_003352

answers: heavy metals can become concentrated in economically extractable quantities

answers: NDQ_003353

answers: erosion,

answers: NDQ_003354

answers: 5% of heavy metals

answers: NDQ_003355

answers: mountain building, erosion,

answers: NDQ_003356

answers: heavy metals can become concentrated in economically extractable quantities

answers: NDQ_003357

answers: heavy metals

answers: NDQ_003358

answers: mountain

answers: NDQ_003359

answers: 5% of heavy metals

answers: NDQ_003360

answers: geological processes.

answers: NDQ_003362

answers: heavy metals can become concentrated in economically extractable quantities

answers: NDQ_003363

answers: heavy metals

answers: NDQ_003371

answers: 5% of heavy metals

answers: NDQ_003373

answers: The Earth's crust is made of approximately 5% of heavy metals

answers: NDQ_003376

answers: mountain building, erosion, or other geological processes.

answers: NDQ_003378

answers: 5% of heavy metals

answers: NDQ_003379

answers: 5% of heavy metals

answers: NDQ_003380

answers: erosion, or other geological processes.

answers: NDQ_003381

answers: 5% of heavy metals

answers: NDQ_003382

answers: 5% of heavy metals

answers: NDQ_003383

answers: erosion, or other geological processes.

answers: NDQ_003384

answers: The Earth's crust is made of approximately 5% of heavy metals

answers: NDQ_003385

answers: mountain building, erosion, or other geological processes.

answers: NDQ_003386

answers: The Earth's crust is made of approximately 5% of heavy metals

answers: NDQ_003387

answers: heavy metals

answers: NDQ_003388

answers: 5% of heavy metals

answers: NDQ_003389

answers: mountain building,

answers: NDQ_003390

answers: erosion, or other geological processes.

answers: NDQ_003391

answers: mountain building,

answers: NDQ_003392

answers: erosion, or other geological processes.

answers: NDQ_003393

answers: mountain

answers: NDQ_003394

answers: mountain building, erosion, or other geological processes.

answers: NDQ_003395

answers: The Earth's crust is made of approximately 5% of heavy metals

answers: NDQ_003396

answers: The Earth's crust is made of approximately 5% of heavy metals

text: All of Maria Gordon's geological research was carried out in the South Tyrol, an area of the Italian Alps close to the border with Austria. This area of the Alps is part of the geologically-complex Dolomites. The Dolomites  are a very distinct range of mountains, characterised by high, dramatic peaks, which were thought to have been formed from the remains of coral atolls in an ancient sea. Gordon challenged this idea with her theory of 'crust-torsion', the notion that the mountains had been formed by the pushing, twisting and folding of the earth's crust. Through observation and measurement of the geological structures in the Dolomites, she was able to determine that there were two phases of folding and structural deformation, leading to a new interpretation of the tectonic structure of the Alps.

text: All of Maria Gordon's geological research was carried out in the South Tyrol, an area of the Italian Alps close to the border with Austria. This area of the Alps is part of the geologically-complex

text: Dolomites

text: . The Dolomites  are a very distinct range of mountains, characterised by high, dramatic peaks, which were thought to have been formed from the remains of

text: coral atolls

text: in an ancient sea. Gordon challenged this idea with her theory of 'crust-torsion', the notion that the mountains had been formed by the pushing, twisting and folding of the earth's crust. Through observation and measurement of the geological structures in the Dolomites, she was able to determine that there were two phases of folding and structural deformation, leading to a new interpretation of the tectonic structure of the Alps.

answers: NDQ_003351

answers: crust-torsion

answers: NDQ_003352

answers: deforms

answers: NDQ_003353

answers: deformation

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: Alps

answers: NDQ_003356

answers: fold

answers: NDQ_003357

answers: pushing and twisting of the earth's crust

answers: NDQ_003358

answers: atoll

answers: NDQ_003359

answers: folds

answers: NDQ_003360

answers: tectonic plates

answers: NDQ_003362

answers: formed from the remains of coral atolls in an ancient sea

answers: NDQ_003363

answers: crust-torsion

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: unanswerable

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: vertical

answers: NDQ_003380

answers: Which of the following is not a type of stress: pushing, twisting and folding

answers: NDQ_003381

answers: Which of the following is not a phase of folding and structural deformation?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not a phase of folding and structural deformation?

answers: NDQ_003385

answers: fault zone

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: normal faults, folding of the earth's crust

answers: NDQ_003388

answers: What does Gordon's theory of 'crust-torsion' refer to?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: tectonic

answers: NDQ_003391

answers: Dolomites

answers: NDQ_003392

answers: crust-torsion

answers: NDQ_003393

answers: Dolomites

answers: NDQ_003394

answers: tectonic

answers: NDQ_003395

answers: tectonic

answers: NDQ_003396

answers: crust-torsion

answers: NDQ_003351

answers: 'crust-torsion',

answers: NDQ_003352

answers: folding

answers: NDQ_003353

answers: folding

answers: NDQ_003354

answers: South Tyrol,

answers: NDQ_003355

answers: 'crust-torsion',

answers: NDQ_003356

answers: folding

answers: NDQ_003357

answers: pushing, twisting and folding of the earth's crust.

answers: NDQ_003358

answers: 'crust-torsion',

answers: NDQ_003359

answers: pushing, twisting and folding

answers: NDQ_003360

answers: the pushing, twisting and folding of the earth's crust.

answers: NDQ_003362

answers: coral atolls in an ancient sea.

answers: NDQ_003363

answers: 'crust-torsion',

answers: NDQ_003371

answers: 'crust-torsion',

answers: NDQ_003373

answers: 'crust-torsion',

answers: NDQ_003376

answers: pushing, twisting and folding of the earth's crust.

answers: NDQ_003378

answers: 'crust-torsion',

answers: NDQ_003379

answers: 'crust-torsion',

answers: NDQ_003380

answers: pushing, twisting and folding of the earth's crust.

answers: NDQ_003381

answers: folding of the earth's crust.

answers: NDQ_003382

answers: 'crust-torsion',

answers: NDQ_003383

answers: pushing, twisting and folding

answers: NDQ_003384

answers: 'crust-torsion',

answers: NDQ_003385

answers: South Tyrol,

answers: NDQ_003386

answers: pushing, twisting and folding of the earth's crust.

answers: NDQ_003387

answers: 'crust-torsion',

answers: NDQ_003388

answers: 'crust-torsion',

answers: NDQ_003389

answers: pushing, twisting and folding of the earth's crust.

answers: NDQ_003390

answers: 'crust-torsion',

answers: NDQ_003391

answers: 'crust-torsion',

answers: NDQ_003392

answers: 'crust-torsion',

answers: NDQ_003393

answers: 'crust-torsion',

answers: NDQ_003394

answers: 'crust-torsion',

answers: NDQ_003395

answers: 'crust-torsion',

answers: NDQ_003396

answers: 'crust-torsion',

text: The Böllstein gneiss and basalt Otzberg caused by large movements of the earth's crust in two different geological eras:

text: The Böllstein gneiss and basalt Otzberg caused by large movements of the earth's crust in two different geological eras:

answers: NDQ_003351

answers: deformation

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: movement

answers: NDQ_003354

answers: Toroweap Formation is a geological formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: change shape

answers: NDQ_003357

answers: movement of the earth's crust causes what?

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: is pushed together

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: The San Andreas fault is a fault in the Earth's crust.

answers: NDQ_003363

answers: geological epochs

answers: NDQ_003371

answers: Which of the following is an example of a thrust fault?

answers: NDQ_003373

answers: How would you describe a rock that is deeply buried?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: The amount of the ground moving in an earthquake is called

answers: NDQ_003379

answers: The dip of the fault plane is horizontal.

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What happens to the rock when confining stress occurs?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: (d).

answers: NDQ_003387

answers: Which of the following is not a type of fault?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip faults or basalt Otzberg?

answers: NDQ_003389

answers: It's impossible to say

answers: NDQ_003390

answers: a fault in which the hanging wall descends

answers: NDQ_003391

answers: gneiss

answers: NDQ_003392

answers: tectonic plate movement

answers: NDQ_003393

answers: gneiss

answers: NDQ_003394

answers: horizontal fault

answers: NDQ_003395

answers: a fault with a vertical fault plane

answers: NDQ_003396

answers: NDQ_003351

answers: large movements

answers: NDQ_003352

answers: movements

answers: NDQ_003353

answers: large movements

answers: NDQ_003354

answers: The Böllstein gneiss and basalt Otzberg

answers: NDQ_003355

answers: The Böllstein gneiss and basalt Otzberg

answers: NDQ_003356

answers: large movements

answers: NDQ_003357

answers: large movements of the earth's crust

answers: NDQ_003358

answers: gneiss

answers: NDQ_003359

answers: large movements

answers: NDQ_003360

answers: large movements of the earth's crust

answers: NDQ_003362

answers: two different geological eras:

answers: NDQ_003363

answers: two different geological eras:

answers: NDQ_003371

answers: movements of the earth's crust in two different geological eras:

answers: NDQ_003373

answers: The Böllstein gneiss and basalt Otzberg

answers: NDQ_003376

answers: large movements of the earth's crust

answers: NDQ_003378

answers: large movements of the earth's crust

answers: NDQ_003379

answers: The Böllstein gneiss and basalt Otzberg

answers: NDQ_003380

answers: large movements

answers: NDQ_003381

answers: large movements

answers: NDQ_003382

answers: The Böllstein gneiss and basalt Otzberg

answers: NDQ_003383

answers: large movements

answers: NDQ_003384

answers: The Böllstein gneiss and basalt Otzberg

answers: NDQ_003385

answers: The Böllstein gneiss and basalt Otzberg

answers: NDQ_003386

answers: large movements of the earth's crust

answers: NDQ_003387

answers: large movements of the earth's crust

answers: NDQ_003388

answers: The Böllstein gneiss and basalt Otzberg

answers: NDQ_003389

answers: large movements of the earth's crust

answers: NDQ_003390

answers: The Böllstein gneiss and basalt Otzberg

answers: NDQ_003391

answers: basalt Otzberg

answers: NDQ_003392

answers: The Böllstein gneiss and basalt Otzberg

answers: NDQ_003393

answers: basalt Otzberg

answers: NDQ_003394

answers: The Böllstein gneiss and basalt Otzberg

answers: NDQ_003395

answers: The Böllstein gneiss and basalt Otzberg

answers: NDQ_003396

answers: The Böllstein gneiss and basalt Otzberg

text: A chiffon pie is a type of pie that consists of a special type of airy mousse-like filling in a crust.  The filling is typically produced by folding meringue and/or whipped cream into a mixture resembling fruit curd (most commonly lemon) that has been thickened with unflavored gelatin.  This filling is then put into a pre-baked pie shell of variable composition.  This same technique can also be used with canned pumpkin to produce pumpkin chiffon pie.

text: A chiffon pie is a type of pie that consists of a special type of airy

text: mousse

text: -like filling in a crust.  The filling is typically produced by folding

text: meringue

text: and/or whipped cream into a mixture resembling

text: fruit curd

text: (most commonly lemon) that has been thickened with unflavored

text: gelatin

text: .  This filling is then put into a pre-baked pie shell of variable composition.  This same technique can also be used with canned pumpkin to produce pumpkin chiffon pie.

answers: NDQ_003351

answers: unflavored gelatin

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: igneous rocks to form

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: chiffon

answers: NDQ_003356

answers: swell

answers: NDQ_003357

answers: fruit curd is thickened with unflavored gelatin

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: a chiffon pie consists of a special type of airy mousse-like filling in a crust

answers: NDQ_003363

answers: unanswerable

answers: NDQ_003371

answers: What type of pie is a chiffon pie?

answers: NDQ_003373

answers: How would you describe a chiffon pie?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: The dip of the fault plane is vertical

answers: NDQ_003380

answers: What is a stress?

answers: NDQ_003381

answers: What type of pie is a chiffon pie?

answers: NDQ_003382

answers: what is the most common stress at convergent plates

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: movement of rock at faults

answers: NDQ_003387

answers: Which of the following is not a cause of normal faults?

answers: NDQ_003388

answers: Which of the following is not a type of pie: strike-slip faults or chiffon pie?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: a fault

answers: NDQ_003391

answers: dip-slip fault plane

answers: NDQ_003392

answers: a hanging wall

answers: NDQ_003393

answers: dip-slip fault plane

answers: NDQ_003394

answers: vertical

answers: NDQ_003395

answers: vertical fault plane

answers: NDQ_003396

answers: NDQ_003351

answers: lemon) that has been thickened with unflavored gelatin.

answers: NDQ_003352

answers: A chiffon pie

answers: NDQ_003353

answers: A chiffon pie

answers: NDQ_003354

answers: pumpkin chiffon pie.

answers: NDQ_003355

answers: chiffon

answers: NDQ_003356

answers: unflavored gelatin.

answers: NDQ_003357

answers: unflavored gelatin.

answers: NDQ_003358

answers: A chiffon pie

answers: NDQ_003359

answers: chiffon pie

answers: NDQ_003360

answers: A chiffon pie

answers: NDQ_003362

answers: A chiffon pie

answers: NDQ_003363

answers: A chiffon pie

answers: NDQ_003371

answers: A chiffon pie

answers: NDQ_003373

answers: chiffon pie

answers: NDQ_003376

answers: A chiffon pie

answers: NDQ_003378

answers: A chiffon pie

answers: NDQ_003379

answers: pumpkin chiffon pie.

answers: NDQ_003380

answers: A chiffon pie

answers: NDQ_003381

answers: A chiffon pie

answers: NDQ_003382

answers: pumpkin chiffon pie.

answers: NDQ_003383

answers: A chiffon pie

answers: NDQ_003384

answers: chiffon pie

answers: NDQ_003385

answers: pumpkin chiffon pie.

answers: NDQ_003386

answers: A chiffon pie

answers: NDQ_003387

answers: A chiffon pie

answers: NDQ_003388

answers: A chiffon pie

answers: NDQ_003389

answers: A chiffon pie

answers: NDQ_003390

answers: A chiffon pie

answers: NDQ_003391

answers: chiffon pie

answers: NDQ_003392

answers: A chiffon pie

answers: NDQ_003393

answers: A chiffon pie

answers: NDQ_003394

answers: A chiffon pie

answers: NDQ_003395

answers: A chiffon pie

answers: NDQ_003396

answers: A chiffon pie

text: The mountain is formed by the same structural fold in the Earth's crust which continues north from Laurel as Briery Mountains (north of Cheat River) and south as Rich Mountain (south of the Tygart Valley River). The mountain is characteristic of the long, folded mountains of the Appalachian Valley and Ridge Region and is located at the western edge of that physiographic province.

text: The mountain is formed by the same structural fold in the Earth's crust which continues north from Laurel as

text: Briery Mountains

text: (north of

text: Cheat River

text: ) and south as

text: Rich Mountain

text: (south of the

text: Tygart Valley River

text: ). The mountain is characteristic of the long, folded mountains of the Appalachian

text: Valley and Ridge Region

text: and is located at the western edge of that

text: physiographic province

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: more likely to fold

answers: NDQ_003353

answers: structural folds

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: structural fold

answers: NDQ_003356

answers: fold

answers: NDQ_003357

answers: Briery Mountains is formed by the same structural fold

answers: NDQ_003358

answers: valley

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: Briery Mountains (north of Cheat River) and south as Rich Mountain

answers: NDQ_003363

answers: Appalachian Valley and Ridge Region

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: What is the best title for this passage?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What may be the reason for the mountain's formation?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: None of the above choices.

answers: NDQ_003384

answers: What type of fold is the mountain formed by?

answers: NDQ_003385

answers: What is the mountain characteristic of?

answers: NDQ_003386

answers: None of the above choices.

answers: NDQ_003387

answers: Which of the following is not a normal fault: Briery Mountains (north of Cheat River) or Rich Mountain?

answers: NDQ_003388

answers: Which of the following is not a result of shear stress: strike-slip faults, Tygart Valley River, or Appalachian Valley and Ridge Region?

answers: NDQ_003389

answers: Yes

answers: NDQ_003390

answers: structural fold

answers: NDQ_003391

answers: Ridge Region

answers: NDQ_003392

answers: structural fold

answers: NDQ_003393

answers: mountain

answers: NDQ_003394

answers: structural fold

answers: NDQ_003395

answers: structural fold in the Earth's crust

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: folded mountains of the Appalachian Valley and Ridge Region

answers: NDQ_003352

answers: folded mountains

answers: NDQ_003353

answers: folded mountains

answers: NDQ_003354

answers: Briery Mountains

answers: NDQ_003355

answers: structural fold

answers: NDQ_003356

answers: folded mountains

answers: NDQ_003357

answers: north from Laurel

answers: NDQ_003358

answers: The mountain

answers: NDQ_003359

answers: fold in the Earth's crust

answers: NDQ_003360

answers: structural fold in the Earth's crust

answers: NDQ_003362

answers: The mountain is formed by the same structural fold in the Earth's crust

answers: NDQ_003363

answers: structural fold in the Earth's crust

answers: NDQ_003371

answers: Briery Mountains

answers: NDQ_003373

answers: The mountain is formed by the same structural fold in the Earth's crust

answers: NDQ_003376

answers: folded mountains

answers: NDQ_003378

answers: folded mountains of the Appalachian Valley and Ridge Region

answers: NDQ_003379

answers: Briery Mountains

answers: NDQ_003380

answers: folded mountains of the Appalachian Valley and Ridge Region

answers: NDQ_003381

answers: folded mountains of the Appalachian Valley and Ridge Region

answers: NDQ_003382

answers: Briery Mountains

answers: NDQ_003383

answers: folded mountains

answers: NDQ_003384

answers: long, folded mountains of the Appalachian Valley and Ridge Region

answers: NDQ_003385

answers: physiographic province.

answers: NDQ_003386

answers: Earth's crust

answers: NDQ_003387

answers: The mountain is formed by the same structural fold in the Earth's crust

answers: NDQ_003388

answers: Briery Mountains

answers: NDQ_003389

answers: structural fold in the Earth's crust

answers: NDQ_003390

answers: fold

answers: NDQ_003391

answers: structural fold

answers: NDQ_003392

answers: fold

answers: NDQ_003393

answers: Ridge Region

answers: NDQ_003394

answers: The mountain is formed by the same structural fold in the Earth's crust

answers: NDQ_003395

answers: The mountain is formed by the same structural fold in the Earth's crust

answers: NDQ_003396

answers: Appalachian Valley and Ridge Region

text: Modern regional structure is being investigated using seismic tomography and seismic reflection in three dimensions, providing unrivaled images of the Earth's interior, its faults and the deep crust. Further information from geophysics such as gravity and airborne magnetics can provide information on the nature of rocks imaged to be in the deep crust.

text: Modern regional structure is being investigated using

text: seismic tomography

text: and

text: seismic

text: reflection in three dimensions, providing unrivaled images of the Earth's interior, its faults and the deep crust. Further information from

text: geophysics

text: such as

text: gravity

text: and airborne magnetics can provide information on the nature of rocks imaged to be in the deep crust.

answers: NDQ_003351

answers: gravity

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fault

answers: NDQ_003356

answers: swell

answers: NDQ_003357

answers: rocks imaged to be in the deep crust

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: faults

answers: NDQ_003362

answers: rocks imaged to be in the deep crust

answers: NDQ_003363

answers: Earth's interior

answers: NDQ_003371

answers: Which of the following is not an example of a thrust fault?

answers: NDQ_003373

answers: None of the above choices.

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: Which of the following is not a type of seismic tomography?

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: Which of the following is not a type of stress: confining, gravity, or airborne magnetics?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not a type of fold that arches upward?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: None of the above choices.

answers: NDQ_003387

answers: None of the above choices.

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip, gravity, or magnetic?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: a hanging wall

answers: NDQ_003391

answers: airborne magnetics

answers: NDQ_003392

answers: a hanging wall

answers: NDQ_003393

answers: rock imaged to be in the deep crust

answers: NDQ_003394

answers: isobath

answers: NDQ_003395

answers: Earth's interior, its faults

answers: NDQ_003396

answers: seismic reflection

answers: NDQ_003351

answers: faults

answers: NDQ_003352

answers: faults

answers: NDQ_003353

answers: faults

answers: NDQ_003354

answers: seismic tomography and seismic reflection

answers: NDQ_003355

answers: faults

answers: NDQ_003356

answers: gravity and airborne magnetics

answers: NDQ_003357

answers: seismic reflection

answers: NDQ_003358

answers: faults

answers: NDQ_003359

answers: faults and the deep crust.

answers: NDQ_003360

answers: faults and the deep crust.

answers: NDQ_003362

answers: rocks imaged to be in the deep crust.

answers: NDQ_003363

answers: deep crust.

answers: NDQ_003371

answers: faults

answers: NDQ_003373

answers: gravity and airborne magnetics

answers: NDQ_003376

answers: seismic tomography and seismic reflection

answers: NDQ_003378

answers: seismic tomography and seismic reflection

answers: NDQ_003379

answers: seismic tomography and seismic reflection

answers: NDQ_003380

answers: gravity and airborne magnetics

answers: NDQ_003381

answers: gravity and airborne magnetics

answers: NDQ_003382

answers: gravity and airborne magnetics

answers: NDQ_003383

answers: seismic tomography and seismic reflection

answers: NDQ_003384

answers: seismic tomography and seismic reflection

answers: NDQ_003385

answers: faults

answers: NDQ_003386

answers: seismic tomography and seismic reflection

answers: NDQ_003387

answers: seismic tomography and seismic reflection

answers: NDQ_003388

answers: seismic tomography and seismic reflection

answers: NDQ_003389

answers: faults

answers: NDQ_003390

answers: faults

answers: NDQ_003391

answers: deep crust.

answers: NDQ_003392

answers: faults

answers: NDQ_003393

answers: rocks imaged to be in the deep crust.

answers: NDQ_003394

answers: faults

answers: NDQ_003395

answers: faults

answers: NDQ_003396

answers: faults

text: A torsion spring is a spring that works by torsion or twisting; that is, a flexible elastic object that stores mechanical energy when it is twisted.  When it is twisted, it exerts a force (actually torque) in the opposite direction, proportional to the amount (angle) it is twisted.  There are two types.  A torsion bar is a straight bar of metal or rubber that is subjected to twisting (shear stress) about its axis by torque applied at its ends.  A more delicate form used in sensitive instruments, called a torsion fiber consists of a fiber of silk, glass, or quartz under tension, that is twisted about its axis.  The other type, a helical torsion spring, is a metal rod or wire in the shape of a helix (coil) that is subjected to twisting about the axis of the coil by sideways forces (bending moments) applied to its ends, twisting the coil tighter.  This terminology can be confusing because in a helical torsion spring the forces acting on the wire are actually bending stresses, not torsional (shear) stresses.

text: A torsion spring is a

text: spring

text: that works by

text: torsion

text: or twisting; that is, a flexible

text: elastic

text: object that stores

text: mechanical energy

text: when it is twisted.  When it is twisted, it exerts a force (actually

text: torque

text: ) in the opposite direction, proportional to the amount (angle) it is twisted.  There are two types.  A torsion bar is a straight bar of metal or rubber that is subjected to twisting (

text: shear stress

text: ) about its axis by torque applied at its ends.  A more delicate form used in sensitive instruments, called a torsion fiber consists of a

text: fiber

text: of silk, glass, or

text: quartz

text: under tension, that is twisted about its axis.  The other type, a helical torsion spring, is a metal rod or wire in the shape of a

text: helix

text: (coil) that is subjected to twisting about the axis of the coil by sideways forces (

text: bending moment

text: s) applied to its ends, twisting the coil tighter.  This terminology can be confusing because in a helical torsion spring the forces acting on the wire are actually bending stresses, not

text: torsional

text: (shear) stresses.

answers: NDQ_003351

answers: twisting

answers: NDQ_003352

answers: twists more

answers: NDQ_003353

answers: twisting

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: helix

answers: NDQ_003356

answers: twist

answers: NDQ_003357

answers: A torsion bar is subjected to twisting (shear stress) about its axis by torque applied at its ends

answers: NDQ_003358

answers: shear

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: sideways forces

answers: NDQ_003362

answers: a helical torsion spring

answers: NDQ_003363

answers: a torsion spring

answers: NDQ_003371

answers: What type of spring is a torsion bar?

answers: NDQ_003373

answers: None of the above choices are right

answers: NDQ_003376

answers: basin-and-range

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: vertical

answers: NDQ_003380

answers: What is a torsion spring?

answers: NDQ_003381

answers: What is the opposite of twisting?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: movement of rock at faults

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: twisting (shear stress) about its axis by torque applied at its ends

answers: NDQ_003388

answers: What type of spring is a torsion bar?

answers: NDQ_003389

answers: mountains

answers: NDQ_003390

answers: torsion spring

answers: NDQ_003391

answers: dip-slip fault plane

answers: NDQ_003392

answers: torsion spring

answers: NDQ_003393

answers: dip-slip fault plane

answers: NDQ_003394

answers: sideways

answers: NDQ_003395

answers: a torsion spring

answers: NDQ_003396

answers: helical

answers: NDQ_003351

answers: (shear stress)

answers: NDQ_003352

answers: twisting (shear stress) about its axis

answers: NDQ_003353

answers: twisting

answers: NDQ_003354

answers: A torsion spring

answers: NDQ_003355

answers: torsion fiber

answers: NDQ_003356

answers: twisting (shear stress)

answers: NDQ_003357

answers: bending stresses,

answers: NDQ_003358

answers: torsion fiber

answers: NDQ_003359

answers: twisted.

answers: NDQ_003360

answers: energy

answers: NDQ_003362

answers: A torsion spring

answers: NDQ_003363

answers: twisting (shear stress) about its axis

answers: NDQ_003371

answers: A torsion spring

answers: NDQ_003373

answers: A torsion spring

answers: NDQ_003376

answers: bending stresses,

answers: NDQ_003378

answers: A torsion spring

answers: NDQ_003379

answers: torsion bar

answers: NDQ_003380

answers: (shear stress)

answers: NDQ_003381

answers: (shear stress)

answers: NDQ_003382

answers: (shear stress)

answers: NDQ_003383

answers: twisting

answers: NDQ_003384

answers: torsion spring

answers: NDQ_003385

answers: torsion fiber

answers: NDQ_003386

answers: A torsion spring

answers: NDQ_003387

answers: bending stresses,

answers: NDQ_003388

answers: torsion bar

answers: NDQ_003389

answers: twisted.

answers: NDQ_003390

answers: A torsion spring

answers: NDQ_003391

answers: torsion bar

answers: NDQ_003392

answers: A torsion spring

answers: NDQ_003393

answers: torsion bar

answers: NDQ_003394

answers: sideways

answers: NDQ_003395

answers: (angle) it is twisted.

answers: NDQ_003396

answers: helical torsion spring,

text: One of the three models for the thinning and rifting of the continental crust of the South China Sea is initiated by Java and Sumatra subduction causing extrusion and slab roll back along the margin. The stresses from these were experienced in the South China Sea and together they caused the southward extension of the South China Sea. This model indicates subduction to the south of Borneo near Java and Sumatra but not subduction of Borneo or beneath Borneo. This is unlikely to have caused South China Sea spreading singlehandedly but probably contributed to the forces involved.

text: One of the three models for the thinning and rifting of the

text: continental crust

text: of the South China Sea is initiated by Java and Sumatra subduction causing extrusion and slab roll back along the margin. The stresses from these were experienced in the South China Sea and together they caused the southward extension of the South China Sea. This model indicates subduction to the south of Borneo near Java and Sumatra but not subduction of Borneo or beneath Borneo. This is unlikely to have caused South China Sea spreading singlehandedly but probably contributed to the forces involved.

answers: NDQ_003351

answers: slab roll back

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: extrusion

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: margin

answers: NDQ_003356

answers: extrude

answers: NDQ_003357

answers: subduction of Borneo or beneath Borneo

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: subducts

answers: NDQ_003360

answers: continental crust

answers: NDQ_003362

answers: subduction of Borneo or beneath Borneo

answers: NDQ_003363

answers: South China Sea

answers: NDQ_003371

answers: What may have caused South China Sea spreading singlehandedly?

answers: NDQ_003373

answers: What is the main idea of the passage?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: What is the dip of the fault plane

answers: NDQ_003380

answers: Which of the following is not a stress?

answers: NDQ_003381

answers: Which of the following is not a type of stress: extrusion and slab roll back

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: subduction

answers: NDQ_003387

answers: Which of the following is not a normal fault: extrusion and slab roll back?

answers: NDQ_003388

answers: Which of the following is not a model for the thinning and rifting of the continental crust of the South China Sea?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: subduction

answers: NDQ_003391

answers: subduction

answers: NDQ_003392

answers: extrusion

answers: NDQ_003393

answers: slab

answers: NDQ_003394

answers: subduction

answers: NDQ_003395

answers: Java and Sumatra subduction

answers: NDQ_003396

answers: subduction

answers: NDQ_003351

answers: extrusion and slab roll back

answers: NDQ_003352

answers: southward extension of the South China Sea.

answers: NDQ_003353

answers: southward extension of the South China Sea.

answers: NDQ_003354

answers: subduction of Borneo or beneath Borneo.

answers: NDQ_003355

answers: slab roll back

answers: NDQ_003356

answers: slab roll back

answers: NDQ_003357

answers: subduction of Borneo or beneath Borneo.

answers: NDQ_003358

answers: slab roll back

answers: NDQ_003359

answers: Java and Sumatra subduction

answers: NDQ_003360

answers: subduction

answers: NDQ_003362

answers: subduction of Borneo or beneath Borneo.

answers: NDQ_003363

answers: Java and Sumatra subduction

answers: NDQ_003371

answers: Java and Sumatra subduction

answers: NDQ_003373

answers: Java and Sumatra subduction

answers: NDQ_003376

answers: Java and Sumatra subduction

answers: NDQ_003378

answers: slab roll back

answers: NDQ_003379

answers: Java and Sumatra subduction

answers: NDQ_003380

answers: stresses

answers: NDQ_003381

answers: extrusion

answers: NDQ_003382

answers: Java and Sumatra subduction

answers: NDQ_003383

answers: stresses

answers: NDQ_003384

answers: Java and Sumatra subduction

answers: NDQ_003385

answers: Java and Sumatra subduction

answers: NDQ_003386

answers: Java and Sumatra subduction

answers: NDQ_003387

answers: Java and Sumatra subduction

answers: NDQ_003388

answers: Java and Sumatra subduction

answers: NDQ_003389

answers: This is unlikely to have caused South China Sea spreading singlehandedly

answers: NDQ_003390

answers: slab roll back

answers: NDQ_003391

answers: Borneo

answers: NDQ_003392

answers: slab roll back

answers: NDQ_003393

answers: slab

answers: NDQ_003394

answers: Java and Sumatra subduction

answers: NDQ_003395

answers: Java and Sumatra subduction

answers: NDQ_003396

answers: Java and Sumatra subduction

text: When one or more salt layers are present during extensional tectonics, a characteristic set of structures are formed. Extensional faults propagate up from the middle part of the crust until they encounter the salt layer. The weakness of the salt prevents the fault from propagating through. However, continuing displacement on the fault offsets the base of the salt and causes bending of the overburden layer. Eventually the stresses caused by this bending will be sufficient to fault the overburden. The types of structures developed depend on the initial salt thickness. In the case of a very thick salt layer there is no direct spatial relationship between the faulting beneath the salt and that in the overburden, such a system is said to be unlinked. For intermediate salt thicknesses, the overburden faults are spatially related to the deeper faults, but offset from them, normally into the footwall; these are known as soft-linked systems. When the salt layer becomes thin enough, the fault that develops in the overburden is closely aligned with that beneath the salt, and forms a continuous fault surface after only a relatively small displacement, forming a hard-linked fault.

text: When one or more salt layers are present during

text: extensional tectonics

text: , a characteristic set of structures are formed. Extensional faults propagate up from the middle part of the crust until they encounter the salt layer. The weakness of the salt prevents the fault from propagating through. However, continuing displacement on the fault offsets the base of the salt and causes bending of the overburden layer. Eventually the stresses caused by this bending will be sufficient to fault the overburden. The types of structures developed depend on the initial salt thickness. In the case of a very thick salt layer there is no direct spatial relationship between the faulting beneath the salt and that in the overburden, such a system is said to be unlinked. For intermediate salt thicknesses, the overburden faults are spatially related to the deeper faults, but offset from them, normally into the footwall; these are known as soft-linked systems. When the salt layer becomes thin enough, the fault that develops in the overburden is closely aligned with that beneath the salt, and forms a continuous fault surface after only a relatively small displacement, forming a hard-linked fault.

answers: NDQ_003351

answers: unlinked

answers: NDQ_003352

answers: bends

answers: NDQ_003353

answers: bending

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: hard-linked fault

answers: NDQ_003356

answers: bend

answers: NDQ_003357

answers: The weakness of the salt prevents the fault from propagating

answers: NDQ_003358

answers: unlinked

answers: NDQ_003359

answers: bending

answers: NDQ_003360

answers: extensional faults

answers: NDQ_003362

answers: The weakness of the salt prevents the fault from propagating

answers: NDQ_003363

answers: extensional tectonics

answers: NDQ_003371

answers: What type of structures are formed depending on the initial salt thickness?

answers: NDQ_003373

answers: unanswerable

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What happens when the salt layer becomes thin enough?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is the term for an area where faults are clustered?

answers: NDQ_003386

answers: What is the cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: extensional faults or normal faults?

answers: NDQ_003388

answers: Which of the following is not a type of fault: extensional faults, soft-linked systems, or hard-linked systems?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: hard-linked fault

answers: NDQ_003391

answers: salt layer

answers: NDQ_003392

answers: hard-linked fault

answers: NDQ_003393

answers: overburden

answers: NDQ_003394

answers: hard-linked fault

answers: NDQ_003395

answers: hard-linked fault

answers: NDQ_003396

answers: hard-linked fault

answers: NDQ_003351

answers: Extensional faults

answers: NDQ_003352

answers: fault the overburden.

answers: NDQ_003353

answers: bending

answers: NDQ_003354

answers: When one or more salt layers

answers: NDQ_003355

answers: soft-linked systems.

answers: NDQ_003356

answers: bending

answers: NDQ_003357

answers: closely aligned with that beneath the salt,

answers: NDQ_003358

answers: unlinked.

answers: NDQ_003359

answers: stresses caused by this bending

answers: NDQ_003360

answers: extensional tectonics,

answers: NDQ_003362

answers: unlinked.

answers: NDQ_003363

answers: extensional tectonics,

answers: NDQ_003371

answers: hard-linked fault.

answers: NDQ_003373

answers: bending of the overburden layer.

answers: NDQ_003376

answers: salt layers are present during extensional tectonics,

answers: NDQ_003378

answers: displacement

answers: NDQ_003379

answers: hard-linked fault.

answers: NDQ_003380

answers: stresses

answers: NDQ_003381

answers: bending of the overburden layer.

answers: NDQ_003382

answers: bending

answers: NDQ_003383

answers: bending

answers: NDQ_003384

answers: soft-linked systems.

answers: NDQ_003385

answers: hard-linked fault.

answers: NDQ_003386

answers: bending of the overburden layer.

answers: NDQ_003387

answers: hard-linked fault.

answers: NDQ_003388

answers: bending

answers: NDQ_003389

answers: bending of the overburden layer.

answers: NDQ_003390

answers: soft-linked systems.

answers: NDQ_003391

answers: overburden

answers: NDQ_003392

answers: soft-linked systems.

answers: NDQ_003393

answers: overburden

answers: NDQ_003394

answers: hard-linked fault.

answers: NDQ_003395

answers: hard-linked fault.

answers: NDQ_003396

answers: hard-linked fault.

text: Fold mountains are mountains that form mainly by the effects of folding on layers within the upper part of the Earth's crust. Before either plate tectonic theory developed, or the internal architecture of thrust belts became well understood, the term was used for most mountain belts, such as the Himalayas. The term is still fairly common in physical geography literature but has otherwise generally fallen out of use except as described below. The forces responsible for formation of fold mountains are called orogenic movements. The term orogenic has derived from a Greek word meaning mountain building. These forces act at tangent to the surface of the earth and are primarily a result of plate tectonics.

text: Fold mountains are

text: mountain

text: s that form mainly by the effects of

text: folding

text: on layers within the upper part of the

text: Earth's crust

text: . Before either

text: plate tectonic

text: theory developed, or the internal architecture of

text: thrust belts

text: became well understood, the term was used for most mountain belts, such as the

text: Himalayas

text: . The term is still fairly common in

text: physical geography

text: literature but has otherwise generally fallen out of use except as described below. The forces responsible for formation of fold mountains are called

text: orogenic

text: movements. The term orogenic has derived from a Greek word meaning mountain building. These forces act at tangent to the surface of the earth and are primarily a result of

text: plate tectonics

answers: NDQ_003351

answers: orogenic movements

answers: NDQ_003352

answers: folds

answers: NDQ_003353

answers: orogenic movements

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: Himalayas

answers: NDQ_003356

answers: fold

answers: NDQ_003357

answers: orogenic movements act at tangent to the surface of the earth

answers: NDQ_003358

answers: unanswerable

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: plates

answers: NDQ_003362

answers: the term was used for most mountain belts, such as the Himalayas

answers: NDQ_003363

answers: plate tectonics

answers: NDQ_003371

answers: What is the term used for most mountain belts, such as the Himalayas

answers: NDQ_003373

answers: What is the term used for most mountain belts, such as the Himalayas?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: Which of the following is not a type of strike-slip fault?

answers: NDQ_003380

answers: What is the term used for most mountain belts, such as the Himalayas?

answers: NDQ_003381

answers: What is a result of plate tectonics?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the term used for most mountain belts, such as the Himalayas?

answers: NDQ_003384

answers: What is the term used for most mountain belts, such as the Himalayas

answers: NDQ_003385

answers: What term has otherwise generally fallen out of use except for the following?

answers: NDQ_003386

answers: Which of the following is not a cause of earthquakes?

answers: NDQ_003387

answers: What is the term used for most mountain belts, such as the Himalayas?

answers: NDQ_003388

answers: What is the term for mountains that form mainly by the effects of folding on layers within the upper part of the Earth's crust?

answers: NDQ_003389

answers: It's impossible to say

answers: NDQ_003390

answers: thrust belt

answers: NDQ_003391

answers: fold mountain

answers: NDQ_003392

answers: thrust belt

answers: NDQ_003393

answers: mountain

answers: NDQ_003394

answers: tangent

answers: NDQ_003395

answers: plate tectonic

answers: NDQ_003396

answers: thrust belt

answers: NDQ_003351

answers: orogenic movements.

answers: NDQ_003352

answers: orogenic movements.

answers: NDQ_003353

answers: orogenic movements.

answers: NDQ_003354

answers: Fold mountains

answers: NDQ_003355

answers: Fold mountains

answers: NDQ_003356

answers: folding

answers: NDQ_003357

answers: tangent to the surface of the earth

answers: NDQ_003358

answers: Fold mountains

answers: NDQ_003359

answers: Fold mountains

answers: NDQ_003360

answers: plate tectonic

answers: NDQ_003362

answers: Fold mountains

answers: NDQ_003363

answers: Fold mountains

answers: NDQ_003371

answers: thrust belts

answers: NDQ_003373

answers: orogenic movements.

answers: NDQ_003376

answers: orogenic movements.

answers: NDQ_003378

answers: orogenic movements.

answers: NDQ_003379

answers: orogenic movements.

answers: NDQ_003380

answers: orogenic movements.

answers: NDQ_003381

answers: orogenic movements.

answers: NDQ_003382

answers: orogenic movements.

answers: NDQ_003383

answers: orogenic movements.

answers: NDQ_003384

answers: orogenic movements.

answers: NDQ_003385

answers: orogenic movements.

answers: NDQ_003386

answers: orogenic movements.

answers: NDQ_003387

answers: orogenic movements.

answers: NDQ_003388

answers: orogenic movements.

answers: NDQ_003389

answers: Fold mountains

answers: NDQ_003390

answers: orogenic movements.

answers: NDQ_003391

answers: Fold mountains

answers: NDQ_003392

answers: orogenic movements.

answers: NDQ_003393

answers: Fold mountains

answers: NDQ_003394

answers: tangent

answers: NDQ_003395

answers: thrust belts

answers: NDQ_003396

answers: thrust belts

text: Discharge's influence can also be seen in the range of cover versions recorded by hardcore punk and metal groups. The Scottish anarcho-punk band Oi Polloi covered the song "State Violence, State Control". During the same period, the Swedish hardcore punk band Mob 47 covered "Never Again" on their Ultimate Attack recording. New York City anarchist crust band Nausea, active from 1985–1992, recorded "Ain't No Feeble Bastard" along with "Hear Nothing, See Nothing, Say Nothing", on The Punk Terrorist Anthology, Vol. 1. Swedish grindcore band Nasum covered "Visions of War" for a tribute compilation. The Southern American punk metal band The Cooters covered "A Hell on Earth/Cries of Help" on their 2005 album Chaos or Bust. D-beat/hardcore punk band From Ashes Rise recorded the nuclear war-themed "Hell on Earth". In 2003, US hardcore band Ensign covered "Protest and Survive" on their album of covers Love the Music, Hate the Kids. In 2009 Peruvian crust punk band Reciklaje cover "The Nightmare Continues" for their album El Declive de las Estructuras

text: Discharge's influence can also be seen in the range of cover versions recorded by hardcore punk and metal groups. The Scottish anarcho-punk band

text: Oi Polloi

text: covered the song "State Violence, State Control". During the same period, the Swedish hardcore punk band

text: Mob 47

text: covered "Never Again" on their Ultimate Attack recording. New York City anarchist crust band

text: Nausea

text: , active from 1985–1992, recorded "Ain't No Feeble Bastard" along with "Hear Nothing, See Nothing, Say Nothing", on The Punk Terrorist Anthology, Vol. 1. Swedish

text: grindcore

text: band

text: Nasum

text: covered "Visions of War" for a tribute compilation. The Southern American

text: punk metal

text: band

text: The Cooters

text: covered "A Hell on Earth/Cries of Help" on their 2005 album Chaos or Bust. D-beat/hardcore punk band

text: From Ashes Rise

text: recorded the nuclear war-themed "Hell on Earth". In 2003, US hardcore band

text: Ensign

text: covered "Protest and Survive" on their album of covers

text: Love the Music, Hate the Kids

text: . In 2009 Peruvian crust punk band

text: Reciklaje

text: cover "The Nightmare Continues" for their album El Declive de las Estructuras

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: more likely to crack

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fold that bends downward

answers: NDQ_003356

answers: cover

answers: NDQ_003357

answers: State Violence, State Control

answers: NDQ_003358

answers: Hell

answers: NDQ_003359

answers: collapses

answers: NDQ_003360

answers: volcanic eruptions

answers: NDQ_003362

answers: Nuclear war-themed "Hell on Earth"

answers: NDQ_003363

answers: nuclear war

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: not enough information

answers: NDQ_003376

answers: What kind of terrain is caused by compressive forces?

answers: NDQ_003378

answers: What is the amount the ground moves in an earthquake?

answers: NDQ_003379

answers: strike-slip fault

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: El Declive de las Estructuras

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: Which band covered "A Hell on Earth/Cries of Help"

answers: NDQ_003388

answers: What type of stress is shear stress?

answers: NDQ_003389

answers: NDQ_003390

answers: a fault

answers: NDQ_003391

answers: unanswerable

answers: NDQ_003392

answers: a fault

answers: NDQ_003393

answers: unanswerable

answers: NDQ_003394

answers: non-vertical

answers: NDQ_003395

answers: a vertical fault plane

answers: NDQ_003396

answers: Visions of War

answers: NDQ_003351

answers: nuclear war-themed

answers: NDQ_003352

answers: metal

answers: NDQ_003353

answers: Discharge's

answers: NDQ_003354

answers: Discharge's

answers: NDQ_003355

answers: Feeble Bastard"

answers: NDQ_003356

answers: Discharge's

answers: NDQ_003357

answers: Discharge's

answers: NDQ_003358

answers: Hell on Earth/Cries

answers: NDQ_003359

answers: Declive de las Estructuras

answers: NDQ_003360

answers: Discharge's

answers: NDQ_003362

answers: "Ain't No Feeble Bastard"

answers: NDQ_003363

answers: nuclear war-themed

answers: NDQ_003371

answers: Discharge's

answers: NDQ_003373

answers: Discharge's

answers: NDQ_003376

answers: Discharge's

answers: NDQ_003378

answers: Discharge's

answers: NDQ_003379

answers: cover versions recorded by hardcore punk and metal groups.

answers: NDQ_003380

answers: metal

answers: NDQ_003381

answers: Discharge's

answers: NDQ_003382

answers: Discharge's

answers: NDQ_003383

answers: metal

answers: NDQ_003384

answers: Discharge's

answers: NDQ_003385

answers: Discharge's

answers: NDQ_003386

answers: Discharge's

answers: NDQ_003387

answers: Discharge's

answers: NDQ_003388

answers: Discharge's

answers: NDQ_003389

answers: Discharge's

answers: NDQ_003390

answers: Discharge's

answers: NDQ_003391

answers: Discharge's

answers: NDQ_003392

answers: Discharge's

answers: NDQ_003393

answers: Discharge's

answers: NDQ_003394

answers: Discharge's

answers: NDQ_003395

answers: Discharge's

answers: NDQ_003396

answers: Discharge's

text: The second view (Protopangea-Paleopangea), based on both palaeomagnetic and geological evidence, is that supercontinent cycles did not occur before about 0.6 Ga (during the Ediacaran Period). Instead, the continental crust comprised a single supercontinent from about 2.7 Ga (Gigaanum, or "billion years ago") until it broke up for the first time, somewhere around 0.6 Ga. This reconstruction is based on the observation that if only small peripheral modifications are made to the primary reconstruction, the data show that the palaeomagnetic poles converged to quasi-static positions for long intervals between about 2.7–2.2, 1.5–1.25 and 0.75–0.6 Ga. During the intervening periods, the poles appear to have conformed to a unified apparent polar wander path. Thus the paleomagnetic data are adequately explained by the existence of a single Protopangea–Paleopangea supercontinent with prolonged quasi-integrity. The prolonged duration of this supercontinent could be explained by the operation of lid tectonics (comparable to the tectonics operating on Mars and Venus) during Precambrian times, as opposed to the plate tectonics seen on the contemporary Earth.

text: The second view (Protopangea-Paleopangea), based on both

text: palaeomagnetic

text: and geological evidence, is that supercontinent cycles did not occur before about 0.6

text: Ga

text: (during the

text: Ediacaran

text: Period). Instead, the continental crust comprised a single supercontinent from about 2.7 Ga (Gigaanum, or "billion years ago") until it broke up for the first time, somewhere around 0.6 Ga. This reconstruction is based on the observation that if only small peripheral modifications are made to the primary reconstruction, the data show that the palaeomagnetic poles converged to quasi-static positions for long intervals between about 2.7–2.2, 1.5–1.25 and 0.75–0.6 Ga. During the intervening periods, the poles appear to have conformed to a unified

text: apparent polar wander

text: path. Thus the paleomagnetic data are adequately explained by the existence of a single Protopangea–Paleopangea supercontinent with prolonged quasi-integrity. The prolonged duration of this supercontinent could be explained by the operation of lid tectonics (comparable to the tectonics operating on Mars and Venus) during

text: Precambrian

text: times, as opposed to the plate tectonics seen on the contemporary Earth.

answers: NDQ_003351

answers: lid tectonics

answers: NDQ_003352

answers: breaks up

answers: NDQ_003353

answers: plates to break apart

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fold that bends downward

answers: NDQ_003356

answers: break up

answers: NDQ_003357

answers: During the intervening periods, the poles appear to have conformed to what?

answers: NDQ_003358

answers: quasi-static

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's surface

answers: NDQ_003362

answers: supercontinent cycles did not occur before about 0.6 Ga

answers: NDQ_003363

answers: 2.7–2.2

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: Why would a rock be deeply buried?

answers: NDQ_003376

answers: plate tectonics

answers: NDQ_003378

answers: What is the amount the ground moves in an earthquake?

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What is a stress?

answers: NDQ_003381

answers: What type of stress occurs when rock deforms?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: plate tectonics

answers: NDQ_003387

answers: What are normal faults caused by?

answers: NDQ_003388

answers: What type of stress is shear stress?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: tectonics

answers: NDQ_003391

answers: supercontinent

answers: NDQ_003392

answers: tectonics

answers: NDQ_003393

answers: supercontinent

answers: NDQ_003394

answers: plate tectonics

answers: NDQ_003395

answers: plate tectonics

answers: NDQ_003396

answers: plate tectonics

answers: NDQ_003351

answers: lid tectonics

answers: NDQ_003352

answers: broke up

answers: NDQ_003353

answers: quasi-static positions

answers: NDQ_003354

answers: 0.6 Ga.

answers: NDQ_003355

answers: lid tectonics

answers: NDQ_003356

answers: quasi-static

answers: NDQ_003357

answers: 2.7–2.2, 1.5–1.25 and 0.75–0.6 Ga.

answers: NDQ_003358

answers: quasi-static

answers: NDQ_003359

answers: small peripheral modifications

answers: NDQ_003360

answers: plate tectonics

answers: NDQ_003362

answers: supercontinent cycles did not occur before about 0.6 Ga

answers: NDQ_003363

answers: Precambrian

answers: NDQ_003371

answers: 2.7–2.2, 1.5–1.25 and 0.75–0.6 Ga.

answers: NDQ_003373

answers: lid tectonics

answers: NDQ_003376

answers: lid tectonics

answers: NDQ_003378

answers: polar wander path.

answers: NDQ_003379

answers: 0.6 Ga

answers: NDQ_003380

answers: 0.6 Ga

answers: NDQ_003381

answers: quasi-static

answers: NDQ_003382

answers: palaeomagnetic poles converged to quasi-static

answers: NDQ_003383

answers: lid tectonics

answers: NDQ_003384

answers: 0.6 Ga (during the Ediacaran Period).

answers: NDQ_003385

answers: (Protopangea-Paleopangea),

answers: NDQ_003386

answers: plate tectonics

answers: NDQ_003387

answers: lid tectonics

answers: NDQ_003388

answers: lid tectonics

answers: NDQ_003389

answers: lid tectonics

answers: NDQ_003390

answers: (Protopangea-Paleopangea),

answers: NDQ_003391

answers: lid tectonics

answers: NDQ_003392

answers: (Protopangea-Paleopangea),

answers: NDQ_003393

answers: lid tectonics

answers: NDQ_003394

answers: (Protopangea-Paleopangea),

answers: NDQ_003395

answers: (Protopangea-Paleopangea),

answers: NDQ_003396

answers: (Protopangea-Paleopangea),

text: When differential stresses exist in the Earth, these can be accommodated either by geological faulting in the brittle crust, or by ductile flow in the hotter and more fluid mantle.  Where faults occur, absolute subsidence may occur in the hanging wall of normal faults.  In reverse, or thrust, faults, relative subsidence may be measured in the footwall.

text: When differential stresses exist in the Earth, these can be accommodated either by

text: geological faulting

text: in the brittle

text: crust

text: , or by

text: ductile

text: flow in the hotter and more fluid

text: mantle

text: .  Where faults occur, absolute subsidence may occur in the hanging wall of normal faults.  In reverse, or thrust, faults, relative subsidence may be measured in the footwall.

answers: NDQ_003351

answers: differential stresses

answers: NDQ_003352

answers: subsidence may occur

answers: NDQ_003353

answers: subsidence

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: footwall

answers: NDQ_003356

answers: submerge

answers: NDQ_003357

answers: absolute subsidence may occur

answers: NDQ_003358

answers: normal fault

answers: NDQ_003359

answers: brittle

answers: NDQ_003360

answers: faults

answers: NDQ_003362

answers: absolute subsidence may occur in the hanging wall

answers: NDQ_003363

answers: faulting

answers: NDQ_003371

answers: relative subsidence may be measured in the footwall

answers: NDQ_003373

answers: no

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: relative subsidence

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a stress?

answers: NDQ_003381

answers: unanswerable

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: no

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip, normal, or thrust?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: thrust, faults

answers: NDQ_003391

answers: footwall

answers: NDQ_003392

answers: thrust

answers: NDQ_003393

answers: footwall

answers: NDQ_003394

answers: reverse, or thrust

answers: NDQ_003395

answers: normal faults

answers: NDQ_003396

answers: thrust

answers: NDQ_003351

answers: geological faulting

answers: NDQ_003352

answers: subsidence

answers: NDQ_003353

answers: subsidence

answers: NDQ_003354

answers: relative subsidence may be measured in the footwall.

answers: NDQ_003355

answers: thrust,

answers: NDQ_003356

answers: absolute subsidence

answers: NDQ_003357

answers: absolute subsidence may occur in the hanging wall

answers: NDQ_003358

answers: faults.

answers: NDQ_003359

answers: differential stresses

answers: NDQ_003360

answers: geological faulting

answers: NDQ_003362

answers: absolute subsidence may occur in the hanging wall of normal faults.

answers: NDQ_003363

answers: geological faulting

answers: NDQ_003371

answers: reverse, or thrust, faults,

answers: NDQ_003373

answers: brittle crust,

answers: NDQ_003376

answers: geological faulting

answers: NDQ_003378

answers: subsidence

answers: NDQ_003379

answers: thrust, faults, relative subsidence may be measured in the footwall.

answers: NDQ_003380

answers: stresses

answers: NDQ_003381

answers: absolute subsidence

answers: NDQ_003382

answers: geological faulting in the brittle crust,

answers: NDQ_003383

answers: geological faulting

answers: NDQ_003384

answers: geological faulting in the brittle crust,

answers: NDQ_003385

answers: Where faults occur, absolute subsidence may occur in the hanging wall

answers: NDQ_003386

answers: absolute subsidence

answers: NDQ_003387

answers: absolute subsidence may occur in the hanging wall of normal faults.

answers: NDQ_003388

answers: reverse, or thrust, faults,

answers: NDQ_003389

answers: geological faulting

answers: NDQ_003390

answers: reverse, or thrust, faults,

answers: NDQ_003391

answers: footwall.

answers: NDQ_003392

answers: reverse, or thrust, faults,

answers: NDQ_003393

answers: footwall.

answers: NDQ_003394

answers: reverse, or thrust, faults,

answers: NDQ_003395

answers: reverse, or thrust, faults,

answers: NDQ_003396

answers: thrust,

text: When a transverse shear force is applied to a structure, such as a beam, the result is variation in bending normal stresses along the length of the beam. This variation necessitates an internal horizontal shear stress within the beam that varies with position y’ from the neutral axis in the beam. The concept of complementary shear then dictates that a shear stress also exists along the front face of the beam. As described above, in thin-walled structures the variation with thickness can be neglected, and the shear stress along the front face of the structure can be examined as shear flow, or the shear stress multiplied by the thickness of the element.

text: When a transverse shear force is applied to a structure, such as a beam, the result is variation in bending normal stresses along the length of the beam. This variation necessitates an internal horizontal shear stress within the beam that varies with position y’ from the neutral axis in the beam. The concept of complementary shear then dictates that a shear stress also exists along the front face of the beam. As described above, in thin-walled structures the variation with thickness can be neglected, and the shear stress along the front face of the structure can be examined as shear flow, or the shear stress multiplied by the thickness of the element.

answers: NDQ_003351

answers: shear flow

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: shear flow

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: shear

answers: NDQ_003356

answers: swell

answers: NDQ_003357

answers: bending normal stresses along the length of the beam

answers: NDQ_003358

answers: neutral

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: transverse shear forces

answers: NDQ_003362

answers: thin-walled structures the variation with thickness can be neglected

answers: NDQ_003363

answers: transverse shear

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: how would you describe compressive stresses?

answers: NDQ_003376

answers: Shear stress multiplied by the thickness of the element

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: vertical

answers: NDQ_003380

answers: What is the main idea of this passage?

answers: NDQ_003381

answers: What is the result of a transverse shear force?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: Fault zone

answers: NDQ_003386

answers: what is the cause of earthquakes

answers: NDQ_003387

answers: Which of the following is not caused by compression stress?

answers: NDQ_003388

answers: Which of the following is not a type of strike-slip fault?

answers: NDQ_003389

answers: mountains

answers: NDQ_003390

answers: transverse shear

answers: NDQ_003391

answers: neutral axis

answers: NDQ_003392

answers: transverse shear

answers: NDQ_003393

answers: neutral axis

answers: NDQ_003394

answers: transverse

answers: NDQ_003395

answers: y’ from the neutral axis in the beam

answers: NDQ_003396

answers: transverse shear

answers: NDQ_003351

answers: bending normal stresses

answers: NDQ_003352

answers: thickness

answers: NDQ_003353

answers: bending

answers: NDQ_003354

answers: When a transverse shear force

answers: NDQ_003355

answers: transverse shear force

answers: NDQ_003356

answers: bending normal stresses

answers: NDQ_003357

answers: bending normal stresses

answers: NDQ_003358

answers: transverse shear force

answers: NDQ_003359

answers: transverse shear force

answers: NDQ_003360

answers: transverse shear force

answers: NDQ_003362

answers: thin-walled structures the variation with thickness can be neglected,

answers: NDQ_003363

answers: transverse shear force

answers: NDQ_003371

answers: When a transverse shear force

answers: NDQ_003373

answers: When a transverse shear force

answers: NDQ_003376

answers: transverse shear force

answers: NDQ_003378

answers: shear flow,

answers: NDQ_003379

answers: y’ from the neutral axis

answers: NDQ_003380

answers: transverse shear force

answers: NDQ_003381

answers: transverse shear force

answers: NDQ_003382

answers: bending normal stresses

answers: NDQ_003383

answers: bending normal stresses

answers: NDQ_003384

answers: y’ from the neutral axis

answers: NDQ_003385

answers: transverse shear force

answers: NDQ_003386

answers: When a transverse shear force

answers: NDQ_003387

answers: bending normal stresses

answers: NDQ_003388

answers: transverse shear force

answers: NDQ_003389

answers: When a transverse shear force

answers: NDQ_003390

answers: transverse shear force

answers: NDQ_003391

answers: transverse shear force

answers: NDQ_003392

answers: transverse shear force

answers: NDQ_003393

answers: beam,

answers: NDQ_003394

answers: transverse shear force

answers: NDQ_003395

answers: y’ from the neutral axis

answers: NDQ_003396

answers: horizontal shear stress

text: The calc-alkaline magma series is one of two main subdivisions of the subalkaline magma series, the other subalkaline magma series being the tholeiitic. A magma series is a series of compositions that describes the evolution of a mafic magma, which is high in magnesium and iron and produces basalt or gabbro, as it fractionally crystallizes to become a felsic magma, which is low in magnesium and iron and produces rhyolite or granite. Calc-alkaline rocks are rich in alkaline earths (magnesia and calcium oxide) and alkali metals and make up a major part of the crust of the continents.

text: The calc-alkaline magma series is one of two main subdivisions of the subalkaline

text: magma series

text: , the other subalkaline magma series being the

text: tholeiitic

text: . A magma series is a series of compositions that describes the evolution of a

text: mafic

text: magma, which is high in

text: magnesium

text: and

text: iron

text: and produces

text: basalt

text: or

text: gabbro

text: , as it

text: fractionally crystallizes

text: to become a

text: felsic

text: magma, which is low in magnesium and iron and produces

text: rhyolite

text: or

text: granite

text: . Calc-alkaline

text: rocks

text: are rich in

text: alkaline earths

text: magnesia

text: and

text: calcium oxide

text: ) and

text: alkali metal

text: s and make up a major part of the

text: crust of the continents

answers: NDQ_003351

answers: tholeiitic

answers: NDQ_003352

answers: produces more magma

answers: NDQ_003353

answers: magma

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: gabbro

answers: NDQ_003356

answers: crystallize

answers: NDQ_003357

answers: basalt or gabbro

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: magma

answers: NDQ_003362

answers: basalt or gabbro

answers: NDQ_003363

answers: subalkaline magma

answers: NDQ_003371

answers: What is one of the main subdivisions of the subalkaline magma series?

answers: NDQ_003373

answers: How would you describe a rock under compressive stresses?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What is a stress?

answers: NDQ_003381

answers: What type of rocks are rich in alkaline earths?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the main cause of joints in rock?

answers: NDQ_003384

answers: What is one of two main subdivisions of the subalkaline magma series

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: What is the cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: basalt or gabbro?

answers: NDQ_003388

answers: What is one of the two main subdivisions of the subalkaline magma series?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: gabbro

answers: NDQ_003391

answers: gabbro

answers: NDQ_003392

answers: gabbro

answers: NDQ_003393

answers: gabbro

answers: NDQ_003394

answers: gabbro

answers: NDQ_003395

answers: tholeiitic

answers: NDQ_003396

answers: gabbro

answers: NDQ_003351

answers: tholeiitic.

answers: NDQ_003352

answers: rhyolite or granite.

answers: NDQ_003353

answers: crystallizes to become a felsic magma,

answers: NDQ_003354

answers: The calc-alkaline

answers: NDQ_003355

answers: tholeiitic.

answers: NDQ_003356

answers: basalt or gabbro,

answers: NDQ_003357

answers: basalt or gabbro,

answers: NDQ_003358

answers: gabbro,

answers: NDQ_003359

answers: The calc-alkaline magma series

answers: NDQ_003360

answers: calc-alkaline magma

answers: NDQ_003362

answers: The calc-alkaline magma series

answers: NDQ_003363

answers: Calc-alkaline

answers: NDQ_003371

answers: The calc-alkaline magma series

answers: NDQ_003373

answers: The calc-alkaline

answers: NDQ_003376

answers: The calc-alkaline magma series

answers: NDQ_003378

answers: tholeiitic.

answers: NDQ_003379

answers: tholeiitic.

answers: NDQ_003380

answers: tholeiitic.

answers: NDQ_003381

answers: The calc-alkaline

answers: NDQ_003382

answers: tholeiitic.

answers: NDQ_003383

answers: The calc-alkaline

answers: NDQ_003384

answers: tholeiitic.

answers: NDQ_003385

answers: tholeiitic.

answers: NDQ_003386

answers: The calc-alkaline magma series

answers: NDQ_003387

answers: tholeiitic.

answers: NDQ_003388

answers: tholeiitic.

answers: NDQ_003389

answers: rhyolite or granite. Calc-alkaline rocks

answers: NDQ_003390

answers: tholeiitic.

answers: NDQ_003391

answers: rhyolite or granite. Calc-alkaline

answers: NDQ_003392

answers: tholeiitic.

answers: NDQ_003393

answers: gabbro,

answers: NDQ_003394

answers: tholeiitic.

answers: NDQ_003395

answers: tholeiitic.

answers: NDQ_003396

answers: tholeiitic.

text: Evidence of both thrust faulting and strike-slip faulting is present in the Plomosa Mountains.

text: Evidence of both

text: thrust fault

text: ing and

text: strike-slip faulting

text: is present in the Plomosa Mountains.

answers: NDQ_003351

answers: strike-slip

answers: NDQ_003352

answers: is likely to crack

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: Strike fault

answers: NDQ_003356

answers: change shape

answers: NDQ_003357

answers: Strike-slip faulting is a type of

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: is pushed against it

answers: NDQ_003360

answers: faulting

answers: NDQ_003362

answers: the San Andreas fault is not present in the Plomosa Mountains

answers: NDQ_003363

answers: tectonic plates

answers: NDQ_003371

answers: Which of the following is not a type of faulting?

answers: NDQ_003373

answers: Why would the Plomosa Mountains have evidence of thrust faulting?

answers: NDQ_003376

answers: Which of the following is not caused by compressive forces?

answers: NDQ_003378

answers: (d).

answers: NDQ_003379

answers: (iv)

answers: NDQ_003380

answers: How would you describe the Plomosa Mountains?

answers: NDQ_003381

answers: What would happen to the Plomosa Mountains?

answers: NDQ_003382

answers: None of the above choices.

answers: NDQ_003383

answers: Which of the following is not a type of faulting?

answers: NDQ_003384

answers: Which of the following is not a type of fold that arches upward?

answers: NDQ_003385

answers: (iv)

answers: NDQ_003386

answers: (d).

answers: NDQ_003387

answers: Which of the following is not a type of fault?

answers: NDQ_003388

answers: It's impossible to say

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: strike-slip

answers: NDQ_003391

answers: is a block of rock

answers: NDQ_003392

answers: thrust faulting

answers: NDQ_003393

answers: strike-slip fault

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: strike-slip

answers: NDQ_003396

answers: thrust faulting

answers: NDQ_003351

answers: thrust faulting

answers: NDQ_003352

answers: thrust faulting and strike-slip faulting

answers: NDQ_003353

answers: thrust faulting

answers: NDQ_003354

answers: Evidence of both thrust faulting and strike-slip faulting

answers: NDQ_003355

answers: thrust faulting

answers: NDQ_003356

answers: thrust faulting and strike-slip faulting

answers: NDQ_003357

answers: thrust faulting and strike-slip

answers: NDQ_003358

answers: thrust faulting and strike-slip faulting

answers: NDQ_003359

answers: thrust faulting and strike-slip faulting

answers: NDQ_003360

answers: thrust faulting

answers: NDQ_003362

answers: thrust faulting and strike-slip faulting

answers: NDQ_003363

answers: thrust faulting

answers: NDQ_003371

answers: thrust faulting and strike-slip faulting

answers: NDQ_003373

answers: thrust faulting and strike-slip faulting

answers: NDQ_003376

answers: thrust faulting and strike-slip faulting

answers: NDQ_003378

answers: strike-slip

answers: NDQ_003379

answers: thrust faulting and strike-slip faulting

answers: NDQ_003380

answers: thrust faulting and strike-slip faulting

answers: NDQ_003381

answers: thrust faulting and strike-slip faulting

answers: NDQ_003382

answers: thrust faulting and strike-slip faulting

answers: NDQ_003383

answers: thrust faulting and strike-slip faulting

answers: NDQ_003384

answers: thrust faulting and strike-slip faulting

answers: NDQ_003385

answers: thrust faulting and strike-slip faulting

answers: NDQ_003386

answers: thrust faulting and strike-slip faulting

answers: NDQ_003387

answers: thrust faulting and strike-slip faulting

answers: NDQ_003388

answers: strike-slip faulting is present in the Plomosa Mountains.

answers: NDQ_003389

answers: thrust faulting and strike-slip faulting

answers: NDQ_003390

answers: thrust faulting and strike-slip

answers: NDQ_003391

answers: strike-slip faulting is present in the Plomosa Mountains.

answers: NDQ_003392

answers: thrust faulting

answers: NDQ_003393

answers: thrust faulting and strike-slip faulting

answers: NDQ_003394

answers: strike-slip faulting

answers: NDQ_003395

answers: strike-slip faulting

answers: NDQ_003396

answers: strike-slip faulting

text: Many chaperones are  heat shock proteins, that is, proteins expressed in response to elevated temperatures or other cellular stresses. The reason for this behaviour is that protein folding is severely affected by heat and, therefore, some chaperones act to prevent or correct damage caused by misfolding. Other chaperones are involved in folding newly made proteins as they are extruded from the ribosome. Although most newly synthesized proteins can fold in absence of chaperones, a minority strictly requires them for the same.

text: Many chaperones are

text: heat shock protein

text: s, that is, proteins

text: expressed

text: in response to elevated temperatures or other cellular stresses. The reason for this behaviour is that

text: protein folding

text: is severely affected by heat and, therefore, some chaperones act to prevent or correct damage caused by misfolding. Other chaperones are involved in folding newly made proteins as they are extruded from the ribosome. Although most newly synthesized proteins can fold in absence of chaperones, a minority strictly requires them for the same.

answers: NDQ_003351

answers: elevated temperatures

answers: NDQ_003352

answers: cracks

answers: NDQ_003353

answers: misfolding

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: misfolding

answers: NDQ_003356

answers: misfold

answers: NDQ_003357

answers: protein folding is severely affected by heat

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: most newly synthesized proteins can fold in absence of chaperones

answers: NDQ_003363

answers: elevated temperatures

answers: NDQ_003371

answers: Which of the following is not a type of thrust fault?

answers: NDQ_003373

answers: how would you describe the stress?

answers: NDQ_003376

answers: compressive forces

answers: NDQ_003378

answers: the amount the ground moves in an earthquake

answers: NDQ_003379

answers: strike-slip fault

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What is the reason for this behaviour?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: movement of rock at faults

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: What type of stress is shear stress?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: a fault

answers: NDQ_003391

answers: dip-slip fault

answers: NDQ_003392

answers: wall-to-wall

answers: NDQ_003393

answers: dip-slip fault

answers: NDQ_003394

answers: isobath

answers: NDQ_003395

answers: a vertical fault plane

answers: NDQ_003396

answers: horizontal fault

answers: NDQ_003351

answers: elevated temperatures

answers: NDQ_003352

answers: damage caused by misfolding.

answers: NDQ_003353

answers: misfolding.

answers: NDQ_003354

answers: Many chaperones are heat shock proteins,

answers: NDQ_003355

answers: misfolding.

answers: NDQ_003356

answers: misfolding.

answers: NDQ_003357

answers: most newly synthesized proteins can fold in absence of chaperones,

answers: NDQ_003358

answers: Many chaperones are heat shock proteins,

answers: NDQ_003359

answers: stresses.

answers: NDQ_003360

answers: elevated temperatures

answers: NDQ_003362

answers: Many chaperones are heat shock proteins,

answers: NDQ_003363

answers: elevated temperatures

answers: NDQ_003371

answers: Many chaperones are heat shock proteins,

answers: NDQ_003373

answers: Many chaperones are heat shock proteins,

answers: NDQ_003376

answers: cellular stresses.

answers: NDQ_003378

answers: Many chaperones are heat shock proteins,

answers: NDQ_003379

answers: temperatures or other cellular stresses.

answers: NDQ_003380

answers: cellular stresses.

answers: NDQ_003381

answers: cellular stresses.

answers: NDQ_003382

answers: temperatures

answers: NDQ_003383

answers: cellular stresses.

answers: NDQ_003384

answers: Many chaperones are heat shock proteins,

answers: NDQ_003385

answers: cellular stresses.

answers: NDQ_003386

answers: Many chaperones are heat shock proteins,

answers: NDQ_003387

answers: misfolding.

answers: NDQ_003388

answers: cellular stresses.

answers: NDQ_003389

answers: most newly synthesized proteins

answers: NDQ_003390

answers: stresses.

answers: NDQ_003391

answers: Many chaperones are heat shock proteins,

answers: NDQ_003392

answers: stresses.

answers: NDQ_003393

answers: Many chaperones are heat shock proteins,

answers: NDQ_003394

answers: cellular stresses.

answers: NDQ_003395

answers: Many chaperones are heat shock proteins,

answers: NDQ_003396

answers: Many chaperones are heat shock proteins,

text: The use of reflection seismology in studies of tectonics and the Earth's crust was pioneered in the 1970s by groups such as the Consortium for Continental Reflection Profiling (COCORP), who inspired deep seismic exploration in other countries such as BIRPS in Great Britain and ECORS in France. The British Institutions Reflection Profiling Syndicate (BIRPS) was started up as a result of oil hydrocarbon exploration in the North Sea.  It became clear that there was a lack of understanding of the tectonic processes that had formed the geological structures and sedimentary basins which were being explored.  The effort produced some significant results and showed that it is possible to profile features such as thrust faults that penetrate through the crust to the upper mantle with marine seismic surveys.

text: The use of reflection seismology in studies of

text: tectonics

text: and the Earth's crust was pioneered in the 1970s by groups such as the Consortium for Continental Reflection Profiling (COCORP), who inspired deep seismic exploration in other countries such as BIRPS in Great Britain and ECORS in France. The British Institutions Reflection Profiling Syndicate (BIRPS) was started up as a result of oil hydrocarbon exploration in the North Sea.  It became clear that there was a lack of understanding of the tectonic processes that had formed the geological structures and

text: sedimentary basin

text: s which were being explored.  The effort produced some significant results and showed that it is possible to profile features such as

text: thrust fault

text: s that penetrate through the crust to the

text: upper mantle

text: with marine seismic surveys.

answers: NDQ_003351

answers: thrust faults

answers: NDQ_003352

answers: is likely to crack

answers: NDQ_003353

answers: thrust faults

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: thrust fault

answers: NDQ_003356

answers: erode

answers: NDQ_003357

answers: penetrate through the crust to the upper mantle

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: penetrate through the crust

answers: NDQ_003360

answers: tectonics

answers: NDQ_003362

answers: penetrate through the crust to the upper mantle with marine seismic surveys

answers: NDQ_003363

answers: tectonics

answers: NDQ_003371

answers: Which of the following is not a type of thrust fault?

answers: NDQ_003373

answers: What is the main idea of this passage?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What is the main idea of this passage?

answers: NDQ_003382

answers: what is the most common stress at convergent plates

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: thrust faults

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: thrust faults or normal faults?

answers: NDQ_003388

answers: Which of the following is not a type of fault: thrust faults, strike-slip faults, or strike-slip faults?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: thrust faults

answers: NDQ_003391

answers: sedimentary basin

answers: NDQ_003392

answers: thrust faults

answers: NDQ_003393

answers: sedimentary basins

answers: NDQ_003394

answers: thrust faults

answers: NDQ_003395

answers: thrust faults

answers: NDQ_003396

answers: thrust faults

answers: NDQ_003351

answers: thrust faults

answers: NDQ_003352

answers: thrust faults

answers: NDQ_003353

answers: thrust faults

answers: NDQ_003354

answers: The use of reflection seismology

answers: NDQ_003355

answers: thrust faults

answers: NDQ_003356

answers: thrust faults that penetrate through the crust to the upper mantle

answers: NDQ_003357

answers: thrust faults that penetrate through the crust to the upper mantle

answers: NDQ_003358

answers: thrust faults

answers: NDQ_003359

answers: thrust faults that penetrate through the crust to the upper mantle

answers: NDQ_003360

answers: tectonics

answers: NDQ_003362

answers: thrust faults that penetrate through the crust to the upper mantle

answers: NDQ_003363

answers: tectonic processes

answers: NDQ_003371

answers: thrust faults that penetrate through the crust to the upper mantle

answers: NDQ_003373

answers: thrust faults that penetrate through the crust to the upper mantle

answers: NDQ_003376

answers: sedimentary basins

answers: NDQ_003378

answers: reflection seismology

answers: NDQ_003379

answers: thrust faults that penetrate through the crust to the upper mantle

answers: NDQ_003380

answers: thrust faults

answers: NDQ_003381

answers: thrust faults that penetrate through the crust to the upper mantle

answers: NDQ_003382

answers: thrust faults

answers: NDQ_003383

answers: thrust faults

answers: NDQ_003384

answers: thrust faults

answers: NDQ_003385

answers: thrust faults

answers: NDQ_003386

answers: thrust faults that penetrate through the crust to the upper mantle

answers: NDQ_003387

answers: thrust faults

answers: NDQ_003388

answers: thrust faults

answers: NDQ_003389

answers: tectonic processes

answers: NDQ_003390

answers: thrust faults

answers: NDQ_003391

answers: thrust faults that penetrate through the crust to the upper mantle

answers: NDQ_003392

answers: thrust faults

answers: NDQ_003393

answers: thrust faults that penetrate through the crust to the upper mantle

answers: NDQ_003394

answers: thrust faults

answers: NDQ_003395

answers: thrust faults

answers: NDQ_003396

answers: thrust faults

text: The San Gabriel Fault was once part of the San Andreas Fault, and is believed to be the former path of it. It is also believed that the northwestern end of this fault zone meets the current San Andreas Fault zone beneath the Frazier Mountain Thrust, near the juncture of the San Andreas with the Garlock Fault and Big Pine Fault.

text: The San Gabriel Fault was once part of the

text: San Andreas Fault

text: , and is believed to be the former path of it. It is also believed that the northwestern end of this fault zone meets the current San Andreas Fault zone beneath the Frazier Mountain Thrust, near the juncture of the San Andreas with the

text: Garlock Fault

text: and Big Pine Fault.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: cracks

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: San Gabriel Fault

answers: NDQ_003356

answers: crack

answers: NDQ_003357

answers: Frazier Mountain Thrust is a type of

answers: NDQ_003358

answers: Thrust

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: San Andreas fault

answers: NDQ_003362

answers: San Gabriel Fault was once part of the San Andreas Fault

answers: NDQ_003363

answers: San Andreas Fault

answers: NDQ_003371

answers: What type of fault is Frazier Mountain Thrust?

answers: NDQ_003373

answers: How would you describe a rock that is deeply buried?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: What is the San Gabriel Fault?

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: How would you describe the San Gabriel Fault?

answers: NDQ_003381

answers: What type of stress does the San Gabriel Fault experience?

answers: NDQ_003382

answers: None of the above choices.

answers: NDQ_003383

answers: What is the San Gabriel Fault?

answers: NDQ_003384

answers: What type of fold is the San Gabriel Fault?

answers: NDQ_003385

answers: yes

answers: NDQ_003386

answers: What is the San Gabriel Fault?

answers: NDQ_003387

answers: None of the above choices.

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip, Garlock or Big Pine?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: San Andreas Fault

answers: NDQ_003391

answers: Frazier Mountain

answers: NDQ_003392

answers: San Andreas Fault

answers: NDQ_003393

answers: Frazier Mountain

answers: NDQ_003394

answers: Frazier Mountain Thrust

answers: NDQ_003395

answers: San Andreas Fault

answers: NDQ_003396

answers: Frazier Mountain Thrust

answers: NDQ_003351

answers: The San Gabriel Fault was once part of the San Andreas Fault,

answers: NDQ_003352

answers: Frazier Mountain Thrust,

answers: NDQ_003353

answers: The San Gabriel Fault was once part of the San Andreas Fault,

answers: NDQ_003354

answers: Frazier Mountain Thrust,

answers: NDQ_003355

answers: Thrust,

answers: NDQ_003356

answers: Frazier Mountain Thrust,

answers: NDQ_003357

answers: Frazier Mountain Thrust,

answers: NDQ_003358

answers: Thrust,

answers: NDQ_003359

answers: The San Gabriel Fault was once part of the San Andreas Fault,

answers: NDQ_003360

answers: The San Gabriel Fault

answers: NDQ_003362

answers: The San Gabriel Fault was once part of the San Andreas Fault,

answers: NDQ_003363

answers: San Andreas Fault,

answers: NDQ_003371

answers: Frazier Mountain Thrust,

answers: NDQ_003373

answers: The San Gabriel Fault

answers: NDQ_003376

answers: The San Gabriel Fault

answers: NDQ_003378

answers: The San Gabriel Fault was once part of the San Andreas Fault,

answers: NDQ_003379

answers: The San Gabriel Fault was once part of the San Andreas Fault,

answers: NDQ_003380

answers: The San Gabriel Fault was once part of the San Andreas Fault,

answers: NDQ_003381

answers: The San Gabriel Fault was once part of the San Andreas Fault,

answers: NDQ_003382

answers: The San Gabriel Fault was once part of the San Andreas Fault,

answers: NDQ_003383

answers: The San Gabriel Fault

answers: NDQ_003384

answers: San Gabriel Fault was once part of the San Andreas Fault,

answers: NDQ_003385

answers: fault zone

answers: NDQ_003386

answers: The San Gabriel Fault was once part of the San Andreas Fault,

answers: NDQ_003387

answers: The San Gabriel Fault was once part of the San Andreas Fault,

answers: NDQ_003388

answers: The San Gabriel Fault

answers: NDQ_003389

answers: The San Gabriel Fault

answers: NDQ_003390

answers: San Gabriel Fault

answers: NDQ_003391

answers: Frazier Mountain Thrust,

answers: NDQ_003392

answers: San Gabriel Fault

answers: NDQ_003393

answers: Frazier Mountain Thrust,

answers: NDQ_003394

answers: San Gabriel Fault

answers: NDQ_003395

answers: San Gabriel Fault

answers: NDQ_003396

answers: San Gabriel Fault

text: The second group of younger Early Paleoproterozoic igneous intrusive rocks is quite different in style, age, and significance. These igneous intrusive rocks consist of granitic and pegmatitic dike swarms, i.e. the Cottonwood, Cremation, Sapphire, and Garnet pegmatite complexes, that cut the Granite Gorge Metamorphic Suite from east to west. They formed as granite magma, and related pegmatite fluids, filled crack-systems as magma migrated through the crust. The chemical composition of the granite and pegmatite comprising these dike swarms is indicative of the partial melting of the metasedimetary and metavolcanic rocks of the Granite Gorge Metamorphic Suite both in-place and at greater depth, in the crust. These dikes exhibit a wide variability in the degree that they have been deformed from straight and nearly undeformed – to varying degrees of folding, stretching, and shearing. The variable degree of the deformation of these structures is interpreted to indicate that these dike swarms were emplaced during a period of significant mountain building and crustal thickening that was possibly associated with continental collision.

text: The second group of younger Early Paleoproterozoic igneous intrusive rocks is quite different in style, age, and significance. These igneous intrusive rocks consist of granitic and pegmatitic dike swarms, i.e. the Cottonwood, Cremation, Sapphire, and Garnet pegmatite complexes, that cut the Granite Gorge Metamorphic Suite from east to west. They formed as granite

text: magma

text: , and related pegmatite fluids, filled crack-systems as magma migrated through the crust. The chemical composition of the granite and pegmatite comprising these dike swarms is indicative of the partial melting of the metasedimetary and metavolcanic rocks of the Granite Gorge Metamorphic Suite both in-place and at greater depth, in the crust. These dikes exhibit a wide variability in the degree that they have been deformed from straight and nearly undeformed – to varying degrees of folding, stretching, and shearing. The variable degree of the deformation of these structures is interpreted to indicate that these dike swarms were emplaced during a period of significant mountain building and crustal thickening that was possibly associated with continental collision.

answers: NDQ_003351

answers: shearing

answers: NDQ_003352

answers: deforms

answers: NDQ_003353

answers: deformation

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: dikes

answers: NDQ_003356

answers: folding, stretching, and shearing

answers: NDQ_003357

answers: crack-systems as magma migrated through the crust

answers: NDQ_003358

answers: undeformed

answers: NDQ_003359

answers: crack-systems

answers: NDQ_003360

answers: continental collision

answers: NDQ_003362

answers: the San Andreas fault is not active

answers: NDQ_003363

answers: continental collision

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: What is the reason for the variable degree of deformation?

answers: NDQ_003376

answers: What was possibly associated with continental collision?

answers: NDQ_003378

answers: What is the variable degree of the deformation of these structures?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What type of force applied to rock is a stress?

answers: NDQ_003381

answers: What type of stress does the rock exhibit?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of cracks in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is the name of the area where faults are clustered?

answers: NDQ_003386

answers: What was possibly associated with continental collision?

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: folding, stretching, and shearing

answers: NDQ_003388

answers: Which of the following is not a type of deformation: folding, stretching, or shear stress?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: Granite Gorge Metamorphic Suite

answers: NDQ_003391

answers: dike

answers: NDQ_003392

answers: Granite Gorge Metamorphic Suite

answers: NDQ_003393

answers: mountain

answers: NDQ_003394

answers: Granite Gorge Metamorphic Suite

answers: NDQ_003395

answers: crack-systems as magma migrated through the crust

answers: NDQ_003396

answers: Straight and nearly undeformed

answers: NDQ_003351

answers: folding, stretching, and shearing.

answers: NDQ_003352

answers: folding, stretching, and shearing.

answers: NDQ_003353

answers: folding, stretching, and shearing.

answers: NDQ_003354

answers: Granite Gorge Metamorphic Suite

answers: NDQ_003355

answers: folding, stretching, and shearing.

answers: NDQ_003356

answers: folding, stretching, and shearing.

answers: NDQ_003357

answers: straight and nearly undeformed

answers: NDQ_003358

answers: undeformed

answers: NDQ_003359

answers: continental collision.

answers: NDQ_003360

answers: continental collision.

answers: NDQ_003362

answers: straight and nearly undeformed

answers: NDQ_003363

answers: continental collision.

answers: NDQ_003371

answers: continental collision.

answers: NDQ_003373

answers: folding, stretching, and shearing.

answers: NDQ_003376

answers: mountain building

answers: NDQ_003378

answers: folding, stretching, and shearing.

answers: NDQ_003379

answers: east to west.

answers: NDQ_003380

answers: folding, stretching, and shearing.

answers: NDQ_003381

answers: folding, stretching, and shearing.

answers: NDQ_003382

answers: folding, stretching, and shearing.

answers: NDQ_003383

answers: folding, stretching, and shearing.

answers: NDQ_003384

answers: folding, stretching, and shearing.

answers: NDQ_003385

answers: continental collision.

answers: NDQ_003386

answers: continental collision.

answers: NDQ_003387

answers: folding, stretching, and shearing.

answers: NDQ_003388

answers: varying degrees of folding, stretching, and shearing.

answers: NDQ_003389

answers: folding,

answers: NDQ_003390

answers: folding, stretching, and shearing.

answers: NDQ_003391

answers: granitic and pegmatitic dike swarms,

answers: NDQ_003392

answers: folding, stretching, and shearing.

answers: NDQ_003393

answers: granitic and pegmatitic dike swarms,

answers: NDQ_003394

answers: continental collision.

answers: NDQ_003395

answers: east to west.

answers: NDQ_003396

answers: straight and nearly undeformed

text: Radiogenic isotope tracers are most powerful when used together with other tracers: The more tracers used, the more control on mixing processes. An example of this application is to the evolution of the Earth's crust and Earth's mantle through geological time.

text: Radiogenic isotope tracers are most powerful when used together with other tracers: The more tracers used, the more control on mixing processes. An example of this application is to the evolution of the

text: Earth's crust

text: and

text: Earth's mantle

text: through geological time.

answers: NDQ_003351

answers: radiogenic

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: voids to form

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: mix

answers: NDQ_003357

answers: Radiogenic isotope tracers are most powerful when used together with what?

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: radiogenic isotope tracers are most powerful when used alone

answers: NDQ_003363

answers: Earth's mantle

answers: NDQ_003371

answers: Which of the following is not an example of an application of radiogenic isotope tracers?

answers: NDQ_003373

answers: how would you describe compressive stresses?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: The amount the ground moves in an earthquake is called slip

answers: NDQ_003379

answers: The dip of the fault plane is vertical

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: Which of the following is not an example of confining stress?

answers: NDQ_003382

answers: None of the above choices.

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: Which of the following is not an example of movement of rock at faults?

answers: NDQ_003387

answers: Which of the following is not a type of normal fault?

answers: NDQ_003388

answers: Which of the following is not a type of strike-slip fault?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: isotope tracers

answers: NDQ_003391

answers: isotope

answers: NDQ_003392

answers: isotope tracers

answers: NDQ_003393

answers: isotope

answers: NDQ_003394

answers: isotopic

answers: NDQ_003395

answers: isotope tracers

answers: NDQ_003396

answers: isotope

answers: NDQ_003351

answers: mixing processes.

answers: NDQ_003352

answers: mixing processes.

answers: NDQ_003353

answers: mixing processes.

answers: NDQ_003354

answers: Radiogenic isotope tracers

answers: NDQ_003355

answers: Radiogenic isotope tracers

answers: NDQ_003356

answers: mixing processes.

answers: NDQ_003357

answers: mixing processes.

answers: NDQ_003358

answers: crust and Earth's mantle

answers: NDQ_003359

answers: mixing processes.

answers: NDQ_003360

answers: Radiogenic isotope tracers

answers: NDQ_003362

answers: The more tracers used, the more control on mixing processes.

answers: NDQ_003363

answers: Earth's crust and Earth's mantle through geological time.

answers: NDQ_003371

answers: Radiogenic isotope tracers

answers: NDQ_003373

answers: Radiogenic isotope tracers

answers: NDQ_003376

answers: Radiogenic isotope tracers

answers: NDQ_003378

answers: Radiogenic isotope tracers

answers: NDQ_003379

answers: Radiogenic isotope tracers

answers: NDQ_003380

answers: Radiogenic isotope tracers

answers: NDQ_003381

answers: Radiogenic isotope tracers

answers: NDQ_003382

answers: Radiogenic isotope tracers

answers: NDQ_003383

answers: Radiogenic isotope tracers

answers: NDQ_003384

answers: Radiogenic isotope tracers

answers: NDQ_003385

answers: Radiogenic

answers: NDQ_003386

answers: Radiogenic isotope tracers

answers: NDQ_003387

answers: Radiogenic isotope tracers

answers: NDQ_003388

answers: Radiogenic isotope tracers

answers: NDQ_003389

answers: Earth's crust and Earth's mantle

answers: NDQ_003390

answers: Radiogenic isotope tracers

answers: NDQ_003391

answers: mantle

answers: NDQ_003392

answers: Radiogenic isotope tracers

answers: NDQ_003393

answers: crust and Earth's mantle

answers: NDQ_003394

answers: Radiogenic isotope tracers

answers: NDQ_003395

answers: Radiogenic isotope tracers

answers: NDQ_003396

answers: Radiogenic

text: This earthquake occurred three hours after the 7.3 magnitude Landers earthquake, which was centered  to the east.  The closely timed occurrence of these earthquakes is an often-cited example of a regional earthquake sequence. Both earthquakes had occurred significantly close to the southern portion of the San Andreas Fault, and the Landers event may have reduced the compressional stress in that area.

text: This earthquake occurred three hours after the 7.3 magnitude

text: Landers earthquake

text: , which was centered  to the east.  The closely timed occurrence of these earthquakes is an often-cited example of a regional earthquake sequence. Both earthquakes had occurred significantly close to the southern portion of the

text: San Andreas Fault

text: , and the Landers event may have reduced the compressional stress in that area.

answers: NDQ_003351

answers: compressional stress

answers: NDQ_003352

answers: compresses

answers: NDQ_003353

answers: compressional stress

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: increase in size

answers: NDQ_003357

answers: compressional stress is the amount of

answers: NDQ_003358

answers: Landers earthquake

answers: NDQ_003359

answers: cracks

answers: NDQ_003360

answers: San Andreas fault

answers: NDQ_003362

answers: the Landers earthquake was centered to the east

answers: NDQ_003363

answers: San Andreas Fault

answers: NDQ_003371

answers: What may have reduced the compressional stress in that area?

answers: NDQ_003373

answers: Why would the Landers event have reduced the compressional stress?

answers: NDQ_003376

answers: Which of the following is not a type of terrain: basin-and-range or land?

answers: NDQ_003378

answers: What was the magnitude of the Landers earthquake?

answers: NDQ_003379

answers: What type of fault is the San Andreas Fault?

answers: NDQ_003380

answers: What type of stress is the Landers earthquake?

answers: NDQ_003381

answers: How would the Landers earthquake affect the San Andreas Fault?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: What type of fold is the San Andreas Fault?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: What is the San Andreas fault?

answers: NDQ_003387

answers: What may have reduced the compressional stress in that area?

answers: NDQ_003388

answers: What type of fault is the San Andreas Fault?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: San Andreas Fault

answers: NDQ_003391

answers: San Andreas Fault

answers: NDQ_003392

answers: San Andreas Fault

answers: NDQ_003393

answers: San Andreas Fault

answers: NDQ_003394

answers: San Andreas Fault

answers: NDQ_003395

answers: San Andreas Fault

answers: NDQ_003396

answers: San Andreas Fault

answers: NDQ_003351

answers: compressional

answers: NDQ_003352

answers: compressional stress

answers: NDQ_003353

answers: compressional stress

answers: NDQ_003354

answers: 7.3 magnitude Landers earthquake, which was centered to the east.

answers: NDQ_003355

answers: San Andreas Fault,

answers: NDQ_003356

answers: compressional stress

answers: NDQ_003357

answers: compressional stress

answers: NDQ_003358

answers: compressional stress

answers: NDQ_003359

answers: San Andreas Fault,

answers: NDQ_003360

answers: San Andreas Fault,

answers: NDQ_003362

answers: the Landers event may have reduced the compressional stress

answers: NDQ_003363

answers: San Andreas Fault,

answers: NDQ_003371

answers: San Andreas Fault,

answers: NDQ_003373

answers: compressional stress

answers: NDQ_003376

answers: compressional stress

answers: NDQ_003378

answers: compressional stress

answers: NDQ_003379

answers: 7.3 magnitude Landers earthquake, which was centered to the east.

answers: NDQ_003380

answers: compressional stress

answers: NDQ_003381

answers: compressional stress

answers: NDQ_003382

answers: compressional stress

answers: NDQ_003383

answers: compressional stress

answers: NDQ_003384

answers: 7.3 magnitude Landers earthquake, which was centered to the east.

answers: NDQ_003385

answers: San Andreas Fault,

answers: NDQ_003386

answers: compressional stress

answers: NDQ_003387

answers: compressional stress

answers: NDQ_003388

answers: compressional stress

answers: NDQ_003389

answers: San Andreas Fault,

answers: NDQ_003390

answers: San Andreas Fault,

answers: NDQ_003391

answers: San Andreas Fault,

answers: NDQ_003392

answers: San Andreas Fault,

answers: NDQ_003393

answers: San Andreas Fault,

answers: NDQ_003394

answers: San Andreas Fault,

answers: NDQ_003395

answers: San Andreas Fault,

answers: NDQ_003396

answers: San Andreas Fault,

text: Purdue Pharma makes pain medicines such as hydromorphone, oxycodone, fentanyl, codeine, and hydrocodone. It is widely known for the production of drugs such as MS Contin, Oxycontin, and Ryzolt. In 1972, Contin (a controlled drug-release system) was developed. In 1984, its extended-release formulation of morphine, MS Contin, was released. In 1996 its extended-release formulation of oxycodone, OxyContin, was released.

text: Purdue Pharma makes pain medicines such as

text: hydromorphone

text: oxycodone

text: fentanyl

text: codeine

text: , and

text: hydrocodone

text: . It is widely known for the production of drugs such as MS Contin, Oxycontin, and Ryzolt. In 1972, Contin (a controlled drug-release system) was developed. In 1984, its extended-release formulation of morphine, MS Contin, was released. In 1996 its extended-release formulation of oxycodone, OxyContin, was released.

answers: NDQ_003351

answers: fentanyl

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: voids to form

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: swell

answers: NDQ_003357

answers: OxyContin was released in what year?

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: tectonic plates

answers: NDQ_003362

answers: fentanyl, codeine, and hydrocodone

answers: NDQ_003363

answers: unanswerable

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: How would you describe Purdue Pharma?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: How many years after MS Contin was released was OxyContin released?

answers: NDQ_003381

answers: Which happened first, MS Contin was released or OxyContin was released?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: What does Purdue Pharma make?

answers: NDQ_003387

answers: Which happened first, MS Contin was released or OxyContin was released?

answers: NDQ_003388

answers: What does Purdue Pharma make?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: dip-slip fault plane

answers: NDQ_003392

answers: fentanyl

answers: NDQ_003393

answers: dip-slip fault plane

answers: NDQ_003394

answers: fentanyl

answers: NDQ_003395

answers: a vertical fault plane

answers: NDQ_003396

answers: fentanyl

answers: NDQ_003351

answers: fentanyl,

answers: NDQ_003352

answers: fentanyl, codeine, and hydrocodone.

answers: NDQ_003353

answers: fentanyl, codeine, and hydrocodone.

answers: NDQ_003354

answers: MS Contin,

answers: NDQ_003355

answers: Contin (a controlled drug-release system)

answers: NDQ_003356

answers: 1996

answers: NDQ_003357

answers: Purdue Pharma makes pain medicines such as hydromorphone,

answers: NDQ_003358

answers: Purdue Pharma makes pain medicines such as hydromorphone,

answers: NDQ_003359

answers: fentanyl, codeine, and hydrocodone.

answers: NDQ_003360

answers: Purdue Pharma

answers: NDQ_003362

answers: Purdue Pharma makes pain medicines such as hydromorphone,

answers: NDQ_003363

answers: Purdue Pharma

answers: NDQ_003371

answers: Purdue Pharma makes pain medicines such as hydromorphone,

answers: NDQ_003373

answers: Purdue Pharma makes pain medicines such as hydromorphone,

answers: NDQ_003376

answers: fentanyl, codeine, and hydrocodone.

answers: NDQ_003378

answers: MS Contin, Oxycontin,

answers: NDQ_003379

answers: fentanyl, codeine, and hydrocodone.

answers: NDQ_003380

answers: fentanyl, codeine, and hydrocodone.

answers: NDQ_003381

answers: Contin (a controlled drug-release system)

answers: NDQ_003382

answers: fentanyl, codeine, and hydrocodone.

answers: NDQ_003383

answers: Purdue Pharma makes pain medicines

answers: NDQ_003384

answers: fentanyl, codeine, and hydrocodone.

answers: NDQ_003385

answers: fentanyl, codeine, and hydrocodone.

answers: NDQ_003386

answers: Purdue Pharma makes pain medicines such as hydromorphone,

answers: NDQ_003387

answers: Purdue Pharma makes pain medicines such as hydromorphone,

answers: NDQ_003388

answers: fentanyl, codeine, and hydrocodone.

answers: NDQ_003389

answers: fentanyl, codeine, and hydrocodone.

answers: NDQ_003390

answers: fentanyl, codeine, and hydrocodone.

answers: NDQ_003391

answers: fentanyl, codeine, and hydrocodone.

answers: NDQ_003392

answers: fentanyl, codeine, and hydrocodone.

answers: NDQ_003393

answers: fentanyl, codeine, and hydrocodone.

answers: NDQ_003394

answers: fentanyl, codeine, and hydrocodone.

answers: NDQ_003395

answers: fentanyl, codeine, and hydrocodone.

answers: NDQ_003396

answers: fentanyl, codeine, and hydrocodone.

text: Those who favour non-existent subduction in the Archean point to the well-established model that the Archean Earth was significantly hotter than it is today, which would have affected lithospheric density in such a way as to perhaps prohibit subduction. The higher temperatures of the Archean Earth can be attributed to the release of tremendous amounts of energy from the accretion of solar system material and subsequent differentiation into core and mantle. This energy, coupled with a greater concentration of heat-producing elements, led to the Earth being 200 K hotter in the Archean than it is today. Assuming seafloor spreading generated oceanic lithosphere in the Archean, higher temperatures led to greater melting of mantle material rising at oceanic spreading centres. This in turn produced thicker oceanic crust and thicker regions of underlying depleted lithospheric mantle. As such, the density of the lithosphere was reduced due to both differentiation of the crust from the mantle and the ensuing relative depletion of the residual mantle in Fe and Al. These expected properties have led to suggestions that oceanic lithosphere was so light that it subducted very shallowly or not at all. Scientists who favour this hypothesis argue that felsic material formed from hydrous partial melting of thickened oceanic crust in the root zones of oceanic plateaus, and not from subduction zones as generally believed.

text: Those who favour non-existent subduction in the Archean point to the well-established model that the Archean Earth was significantly hotter than it is today, which would have affected lithospheric

text: density

text: in such a way as to perhaps prohibit subduction. The higher

text: temperatures

text: of the Archean Earth can be attributed to the release of tremendous amounts of

text: energy

text: from the

text: accretion

text: of

text: solar system

text: material and subsequent differentiation into

text: core

text: and

text: mantle

text: . This energy, coupled with a greater concentration of heat-producing

text: elements

text: , led to the Earth being 200 K hotter in the Archean than it is today. Assuming

text: seafloor spreading

text: generated oceanic

text: lithosphere

text: in the Archean, higher temperatures led to greater

text: melting

text: of mantle material rising at oceanic spreading centres. This in turn produced thicker

text: oceanic crust

text: and thicker regions of underlying depleted lithospheric mantle. As such, the density of the lithosphere was reduced due to both differentiation of the crust from the mantle and the ensuing relative depletion of the residual mantle in

text: Fe

text: and

text: Al

text: . These expected properties have led to suggestions that oceanic lithosphere was so light that it subducted very shallowly or not at all. Scientists who favour this hypothesis argue that

text: felsic

text: material formed from hydrous

text: partial melting

text: of thickened oceanic crust in the root zones of

text: oceanic plateau

text: s, and not from subduction zones as generally believed.

answers: NDQ_003351

answers: subduction

answers: NDQ_003352

answers: melts

answers: NDQ_003353

answers: melting

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: subduction zone

answers: NDQ_003356

answers: subduct

answers: NDQ_003357

answers: melting of mantle material rising at oceanic spreading centres

answers: NDQ_003358

answers: plateau

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: oceanic spreading centres

answers: NDQ_003362

answers: non-existent subduction

answers: NDQ_003363

answers: Archean

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: thicker oceanic crust

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: vertical

answers: NDQ_003380

answers: What is the density of the lithosphere?

answers: NDQ_003381

answers: the density of the lithosphere was reduced

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: subduction zones

answers: NDQ_003386

answers: subduction

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: unanswerable

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: subduction zones

answers: NDQ_003391

answers: seafloor

answers: NDQ_003392

answers: subduction zones

answers: NDQ_003393

answers: oceanic crust

answers: NDQ_003394

answers: subduction zones

answers: NDQ_003395

answers: subduction zones as generally believed

answers: NDQ_003396

answers: subduction zones

answers: NDQ_003351

answers: subduction

answers: NDQ_003352

answers: thicker

answers: NDQ_003353

answers: melting of mantle material

answers: NDQ_003354

answers: Those who favour non-existent subduction in the Archean

answers: NDQ_003355

answers: Those who favour non-existent subduction

answers: NDQ_003356

answers: thicker oceanic crust

answers: NDQ_003357

answers: subduction zones

answers: NDQ_003358

answers: subduction zones

answers: NDQ_003359

answers: Those who favour non-existent subduction

answers: NDQ_003360

answers: seafloor spreading

answers: NDQ_003362

answers: subduction zones

answers: NDQ_003363

answers: oceanic spreading centres.

answers: NDQ_003371

answers: Those who favour non-existent subduction in the Archean

answers: NDQ_003373

answers: thicker oceanic crust

answers: NDQ_003376

answers: oceanic spreading centres.

answers: NDQ_003378

answers: Those who favour non-existent subduction

answers: NDQ_003379

answers: Those who favour non-existent subduction in the Archean

answers: NDQ_003380

answers: melting

answers: NDQ_003381

answers: thicker oceanic crust

answers: NDQ_003382

answers: melting

answers: NDQ_003383

answers: melting of mantle material rising at oceanic spreading centres.

answers: NDQ_003384

answers: oceanic spreading centres.

answers: NDQ_003385

answers: subduction zones

answers: NDQ_003386

answers: subduction

answers: NDQ_003387

answers: melting of mantle material rising at oceanic spreading centres.

answers: NDQ_003388

answers: melting of mantle material rising at oceanic spreading centres.

answers: NDQ_003389

answers: seafloor spreading

answers: NDQ_003390

answers: subduction

answers: NDQ_003391

answers: oceanic lithosphere

answers: NDQ_003392

answers: Those who favour non-existent subduction

answers: NDQ_003393

answers: oceanic lithosphere

answers: NDQ_003394

answers: Those who favour non-existent subduction

answers: NDQ_003395

answers: Those who favour non-existent subduction

answers: NDQ_003396

answers: subduction

text: Several enormous, circular impact basins are present on Mars. The largest one that is readily visible is the Hellas basin located in the southern hemisphere. It is the second largest confirmed impact structure on the planet, centered at about 64°E longitude and 40°S latitude. The central part of the basin (Hellas Planitia) is 1,800 km in diameter and surrounded by a broad, heavily eroded annular rim structure characterized by closely spaced rugged irregular mountains (massifs), which probably represent uplifted, jostled blocks of old pre-basin crust. (See Anseris Mons, for example.) Ancient, low-relief volcanic constructs (highland paterae) are located on the northeastern and southwestern portions of the rim. The basin floor contains thick, structurally complex sedimentary deposits that have a long geologic history of deposition, erosion, and internal deformation. The lowest elevations on the planet are located within the Hellas basin, with some areas of the basin floor lying over 8 km below datum.

text: Several enormous, circular impact basins are present on Mars. The largest one that is readily visible is the

text: Hellas basin

text: located in the southern hemisphere. It is the second largest confirmed impact structure on the planet, centered at about 64°E longitude and 40°S latitude. The central part of the basin (Hellas Planitia) is 1,800 km in diameter and surrounded by a broad, heavily eroded

text: annular

text: rim structure characterized by closely spaced rugged irregular mountains (

text: massif

text: s), which probably represent uplifted, jostled blocks of old pre-basin crust. (See

text: Anseris Mons

text: , for example.) Ancient, low-relief volcanic constructs (highland paterae) are located on the northeastern and southwestern portions of the rim. The basin floor contains thick, structurally complex sedimentary deposits that have a long geologic history of deposition, erosion, and internal deformation. The lowest elevations on the planet are located within the Hellas basin, with some areas of the basin floor lying over 8 km below datum.

answers: NDQ_003351

answers: internal deformation

answers: NDQ_003352

answers: deforms

answers: NDQ_003353

answers: internal deformation

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: massif

answers: NDQ_003356

answers: internal deformation

answers: NDQ_003357

answers: Hellas Planitia is located on the northeastern and southwestern portions of the rim

answers: NDQ_003358

answers: impact

answers: NDQ_003359

answers: deforms

answers: NDQ_003360

answers: Mars

answers: NDQ_003362

answers: ancient, low-relief volcanic constructs are located on the northeastern and southwestern portions of the rim

answers: NDQ_003363

answers: Hellas Basin

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: Why is the lowest elevations on the planet located within the Hellas basin?

answers: NDQ_003376

answers: what is the second largest confirmed impact structure on the planet

answers: NDQ_003378

answers: What is the second largest confirmed impact structure on the planet?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What is the lowest elevations on the planet?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What type of fold is the Hellas Planitia?

answers: NDQ_003385

answers: What is the second largest confirmed impact structure on the planet?

answers: NDQ_003386

answers: What is the cause of earthquakes?

answers: NDQ_003387

answers: What are the lowest elevations on the planet located within the Hellas basin?

answers: NDQ_003388

answers: Which of the following is not a type of strike-slip fault: strike-slip, strike-slip, or strike-slip?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: annular rim structure

answers: NDQ_003391

answers: pre-basin crust

answers: NDQ_003392

answers: Anseris Mons

answers: NDQ_003393

answers: pre-basin crust

answers: NDQ_003394

answers: annular

answers: NDQ_003395

answers: Anseris Mons

answers: NDQ_003396

answers: annular rim structure

answers: NDQ_003351

answers: erosion, and internal deformation.

answers: NDQ_003352

answers: eroded

answers: NDQ_003353

answers: erosion, and internal deformation.

answers: NDQ_003354

answers: low-relief volcanic constructs

answers: NDQ_003355

answers: (highland paterae)

answers: NDQ_003356

answers: internal deformation.

answers: NDQ_003357

answers: jostled blocks of old pre-basin crust.

answers: NDQ_003358

answers: impact basins

answers: NDQ_003359

answers: jostled

answers: NDQ_003360

answers: jostled blocks of old pre-basin crust.

answers: NDQ_003362

answers: Several enormous, circular impact basins are present on Mars.

answers: NDQ_003363

answers: jostled blocks of old pre-basin crust.

answers: NDQ_003371

answers: jostled blocks of old pre-basin crust.

answers: NDQ_003373

answers: internal deformation.

answers: NDQ_003376

answers: closely spaced rugged irregular mountains

answers: NDQ_003378

answers: erosion, and internal deformation.

answers: NDQ_003379

answers: 64°E

answers: NDQ_003380

answers: erosion, and internal deformation.

answers: NDQ_003381

answers: internal deformation.

answers: NDQ_003382

answers: uplifted,

answers: NDQ_003383

answers: jostled

answers: NDQ_003384

answers: eroded annular rim structure

answers: NDQ_003385

answers: Hellas basin

answers: NDQ_003386

answers: uplifted,

answers: NDQ_003387

answers: uplifted, jostled blocks

answers: NDQ_003388

answers: Hellas basin located in the southern hemisphere.

answers: NDQ_003389

answers: uplifted,

answers: NDQ_003390

answers: Hellas basin

answers: NDQ_003391

answers: old pre-basin crust.

answers: NDQ_003392

answers: Hellas basin located in the southern hemisphere.

answers: NDQ_003393

answers: pre-basin crust.

answers: NDQ_003394

answers: 64°E longitude and 40°S latitude.

answers: NDQ_003395

answers: 64°E longitude and 40°S latitude.

answers: NDQ_003396

answers: 64°E longitude and 40°S latitude.

text: Psychological and physical stress can induce a variety of alterations in intestinal function. These include changes in gut motility, intestinal permeability, ion flux, fluid balance and mucus secretion. Furthermore, acute and chronic stress in animal models has shown that stress can cause degradation of intestinal barrier function. Psychological stress can influence the clinical outcome of inflammatory bowel disease and irritable bowel syndrome. Long-term stress has been shown to be positively associated with an increased propensity for relapse of ulcerative colitis.

text: Psychological

text: and

text: physical stress

text: can induce a variety of alterations in intestinal function. These include changes in

text: gut motility

text: intestinal permeability

text: , ion flux,

text: fluid balance

text: and mucus secretion. Furthermore, acute and chronic stress in

text: animal models

text: has shown that stress can cause degradation of intestinal barrier function. Psychological stress can influence the clinical outcome of

text: inflammatory bowel disease

text: and

text: irritable bowel syndrome

text: . Long-term stress has been shown to be positively associated with an increased propensity for relapse of

text: ulcerative colitis

answers: NDQ_003351

answers: ion flux

answers: NDQ_003352

answers: can cause digestive permeability

answers: NDQ_003353

answers: degradation of intestinal barrier function

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: unanswerable

answers: NDQ_003356

answers: relapse

answers: NDQ_003357

answers: mucus secretion

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: long-term stress has been positively associated with an increased propensity for relapse of ulcerative colitis.

answers: NDQ_003363

answers: long-term stress

answers: NDQ_003371

answers: Which of the following is not an example of a thrust fault?

answers: NDQ_003373

answers: Which of the following is not a stress?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What can cause degradation of intestinal barrier function?

answers: NDQ_003381

answers: Which of the following is not a type of stress: psychological or physical?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: Which of the following is not a type of fold that arches upward?

answers: NDQ_003385

answers: Fault zones are areas where faults are clustered.

answers: NDQ_003386

answers: Which of the following is not the cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: ion flux, fluid balance, or mucus secretion?

answers: NDQ_003388

answers: Which of the following is not a result of shear stress: strike-slip faults, ion flux, or fluid balance?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: permeability

answers: NDQ_003391

answers: dip-slip fault plane

answers: NDQ_003392

answers: a hanging wall

answers: NDQ_003393

answers: a dip-slip fault plane

answers: NDQ_003394

answers: isosceles

answers: NDQ_003395

answers: a vertical fault plane

answers: NDQ_003396

answers: NDQ_003351

answers: chronic stress

answers: NDQ_003352

answers: stress can cause degradation of intestinal barrier function.

answers: NDQ_003353

answers: degradation of intestinal barrier function.

answers: NDQ_003354

answers: irritable bowel syndrome.

answers: NDQ_003355

answers: irritable bowel syndrome.

answers: NDQ_003356

answers: stress can cause degradation of intestinal barrier function.

answers: NDQ_003357

answers: ion flux, fluid balance and mucus secretion.

answers: NDQ_003358

answers: Psychological and physical stress

answers: NDQ_003359

answers: stress

answers: NDQ_003360

answers: stress

answers: NDQ_003362

answers: Psychological and physical stress

answers: NDQ_003363

answers: stress

answers: NDQ_003371

answers: stress can cause degradation of intestinal barrier function.

answers: NDQ_003373

answers: Psychological and physical stress

answers: NDQ_003376

answers: Psychological and physical stress

answers: NDQ_003378

answers: Psychological and physical stress

answers: NDQ_003379

answers: stress can cause degradation of intestinal barrier function.

answers: NDQ_003380

answers: stress

answers: NDQ_003381

answers: stress can cause degradation of intestinal barrier function.

answers: NDQ_003382

answers: Psychological and physical stress

answers: NDQ_003383

answers: stress

answers: NDQ_003384

answers: irritable bowel syndrome.

answers: NDQ_003385

answers: ion flux,

answers: NDQ_003386

answers: Psychological and physical stress

answers: NDQ_003387

answers: Psychological and physical stress

answers: NDQ_003388

answers: Psychological and physical stress

answers: NDQ_003389

answers: Psychological and physical stress

answers: NDQ_003390

answers: irritable bowel syndrome.

answers: NDQ_003391

answers: irritable bowel syndrome.

answers: NDQ_003392

answers: irritable bowel syndrome.

answers: NDQ_003393

answers: irritable bowel syndrome.

answers: NDQ_003394

answers: inflammatory bowel disease and irritable bowel syndrome.

answers: NDQ_003395

answers: ion flux, fluid balance and mucus secretion.

answers: NDQ_003396

answers: irritable bowel syndrome.

text: The duo would frequently promise a celebrity guest such as Burt Reynolds, who turned out to be Vic in a bizarre outfit yelling about his book Coping With Stress, Cuban soap star Juan Nelly The Elephant (Vic), who kept intermittently turning into an electrical salesman, and Ian Crust, the Inventor of the Bag (Bob).

text: The duo would frequently promise a celebrity guest such as

text: Burt Reynolds

text: , who turned out to be Vic in a bizarre outfit yelling about his book Coping With Stress, Cuban soap star Juan Nelly The Elephant (Vic), who kept intermittently turning into an electrical salesman, and Ian Crust, the Inventor of the Bag (Bob).

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: has more cracks

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: crease

answers: NDQ_003356

answers: turn into electrical

answers: NDQ_003357

answers: Juan Nelly The Elephant would turn into an electrical salesman

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: continental plates

answers: NDQ_003362

answers: Inventor of the Bag

answers: NDQ_003363

answers: the same time

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: How would you describe Burt Reynolds?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: What is the last word in the passage?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: How would you describe Burt Reynolds?

answers: NDQ_003381

answers: what is the last word in the passage?

answers: NDQ_003382

answers: None of the above choices.

answers: NDQ_003383

answers: not enough information

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: what is the first word in the passage?

answers: NDQ_003386

answers: None of the above choices.

answers: NDQ_003387

answers: Which of the following is not a celebrity guest: Burt Reynolds, Ian Crust, or Vic?

answers: NDQ_003388

answers: Which of the following is not a type of stress: strike-slip faults, shear stress, or electrical salesman?

answers: NDQ_003389

answers: Ian Crust

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: dip-slip fault plane

answers: NDQ_003392

answers: the Inventor of the Bag

answers: NDQ_003393

answers: dip-slip fault plane

answers: NDQ_003394

answers: is not vertical

answers: NDQ_003395

answers: does not

answers: NDQ_003396

answers: NDQ_003351

answers: Stress,

answers: NDQ_003352

answers: Ian Crust,

answers: NDQ_003353

answers: electrical salesman, and Ian Crust,

answers: NDQ_003354

answers: Burt Reynolds,

answers: NDQ_003355

answers: Bag

answers: NDQ_003356

answers: electrical salesman,

answers: NDQ_003357

answers: intermittently turning into an electrical salesman,

answers: NDQ_003358

answers: Crust,

answers: NDQ_003359

answers: Vic

answers: NDQ_003360

answers: Stress,

answers: NDQ_003362

answers: Burt Reynolds,

answers: NDQ_003363

answers: Cuban

answers: NDQ_003371

answers: Coping With Stress,

answers: NDQ_003373

answers: Coping With Stress,

answers: NDQ_003376

answers: Coping With Stress,

answers: NDQ_003378

answers: Coping With Stress,

answers: NDQ_003379

answers: Vic

answers: NDQ_003380

answers: Stress,

answers: NDQ_003381

answers: Stress,

answers: NDQ_003382

answers: Coping With Stress,

answers: NDQ_003383

answers: Stress,

answers: NDQ_003384

answers: Burt Reynolds,

answers: NDQ_003385

answers: Coping With Stress,

answers: NDQ_003386

answers: Burt Reynolds,

answers: NDQ_003387

answers: Stress,

answers: NDQ_003388

answers: Coping With Stress,

answers: NDQ_003389

answers: Bag

answers: NDQ_003390

answers: Coping With Stress,

answers: NDQ_003391

answers: Ian Crust,

answers: NDQ_003392

answers: Coping With Stress,

answers: NDQ_003393

answers: Bag

answers: NDQ_003394

answers: electrical salesman,

answers: NDQ_003395

answers: Coping With Stress,

answers: NDQ_003396

answers: Coping With Stress,

text: A subduction zone is a region of the earth's crust where one tectonic plate moves under another tectonic plate; oceanic crust gets recycled back into the mantle and continental crust gets created by the formation of arc magmas. Arc magmas account for more than 20% of terrestrially produced magmas and are produced by the dehydration of minerals within the subducting slab as it descends into the mantle and are accreted onto the base of the overriding continental plate. Subduction zones host a unique variety of rock types created by the high-pressure, low-temperature conditions a subducting slab encounters during its descent. The metamorphic conditions the slab passes through in this process creates and destroys water bearing (hydrous) mineral phases, releasing water into the mantle. This water lowers the melting point of mantle rock, initiating melting. Understanding the timing and conditions in which these dehydration reactions occur, is key to interpreting mantle melting, volcanic arc magmatism, and the formation of continental crust.

text: A

text: subduction zone

text: is a region of the earth's crust where one

text: tectonic plate

text: moves under another tectonic plate;

text: oceanic crust

text: gets recycled back into the mantle and

text: continental crust

text: gets created by the formation of arc

text: magma

text: s. Arc magmas account for more than 20% of terrestrially produced magmas and are produced by the dehydration of minerals within the subducting slab as it descends into the mantle and are accreted onto the base of the overriding continental plate. Subduction zones host a unique variety of rock types created by the high-pressure, low-temperature conditions a subducting slab encounters during its descent. The metamorphic conditions the slab passes through in this process creates and destroys water bearing (hydrous) mineral phases, releasing water into the mantle. This water lowers the melting point of mantle rock, initiating melting. Understanding the timing and conditions in which these dehydration reactions occur, is key to interpreting mantle melting, volcanic arc magmatism, and the formation of continental crust.

answers: NDQ_003351

answers: high-pressure

answers: NDQ_003352

answers: melts

answers: NDQ_003353

answers: metamorphic reactions

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: subduction zone

answers: NDQ_003356

answers: lower the melting point

answers: NDQ_003357

answers: water lowers the melting point of mantle rock

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: low-temperature conditions

answers: NDQ_003360

answers: subduction zones

answers: NDQ_003362

answers: melting point of mantle rock, initiating melting

answers: NDQ_003363

answers: Subduction zones

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: What is the main idea of this passage?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What happens to rock when confining stress occurs?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: What type of fold is a syncline?

answers: NDQ_003385

answers: Which of the following is not a type of fault zone?

answers: NDQ_003386

answers: Which of the following is not a cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: normal faults or subduction zones?

answers: NDQ_003388

answers: Which of the following is not a result of shear stress: strike-slip faults, subduction zones, or continental crust?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: Subduction zone

answers: NDQ_003391

answers: subducting slab

answers: NDQ_003392

answers: subducting

answers: NDQ_003393

answers: subducting slab

answers: NDQ_003394

answers: subducting

answers: NDQ_003395

answers: subducting slab

answers: NDQ_003396

answers: Subduction zone

answers: NDQ_003351

answers: high-pressure, low-temperature

answers: NDQ_003352

answers: creates and destroys water bearing (hydrous) mineral phases,

answers: NDQ_003353

answers: creates and destroys water bearing (hydrous) mineral phases,

answers: NDQ_003354

answers: subduction zone

answers: NDQ_003355

answers: subduction zone

answers: NDQ_003356

answers: melting.

answers: NDQ_003357

answers: oceanic crust gets recycled back into the mantle

answers: NDQ_003358

answers: subduction zone

answers: NDQ_003359

answers: high-pressure, low-temperature

answers: NDQ_003360

answers: subduction zone

answers: NDQ_003362

answers: A subduction zone

answers: NDQ_003363

answers: subduction zone

answers: NDQ_003371

answers: subduction zone

answers: NDQ_003373

answers: high-pressure, low-temperature

answers: NDQ_003376

answers: subduction zone

answers: NDQ_003378

answers: subduction zone

answers: NDQ_003379

answers: subduction zone

answers: NDQ_003380

answers: high-pressure,

answers: NDQ_003381

answers: high-pressure, low-temperature

answers: NDQ_003382

answers: high-pressure, low-temperature

answers: NDQ_003383

answers: high-pressure,

answers: NDQ_003384

answers: subduction zone

answers: NDQ_003385

answers: subduction zone

answers: NDQ_003386

answers: subduction zone

answers: NDQ_003387

answers: high-pressure, low-temperature

answers: NDQ_003388

answers: high-pressure, low-temperature conditions

answers: NDQ_003389

answers: high-pressure, low-temperature

answers: NDQ_003390

answers: subduction zone

answers: NDQ_003391

answers: subduction zone

answers: NDQ_003392

answers: subduction zone

answers: NDQ_003393

answers: subduction zone

answers: NDQ_003394

answers: subduction zone

answers: NDQ_003395

answers: subduction zone

answers: NDQ_003396

answers: subduction zone

text: However, when a plate carrying oceanic crust subducts under a plate carrying an igneous oceanic plateau, the volcanism which erupts on the plateau as the oceanic crust heats up on its descent into the mantle erupts material which is more felsic than the material which makes up the plateau.  This represents a step toward creating crust which is increasingly continental in character, being less dense and more buoyant.  If an igneous oceanic plateau is subducted underneath another one, or under existing continental crust, the eruptions produced thereby produce material that is yet more felsic, and so on through geologic time.

text: However, when a

text: plate

text: carrying oceanic crust

text: subducts

text: under a plate carrying an igneous oceanic plateau, the volcanism which erupts on the plateau as the oceanic crust heats up on its descent into the mantle erupts material which is more felsic than the material which makes up the plateau.  This represents a step toward creating crust which is increasingly continental in character, being less dense and more buoyant.  If an igneous oceanic plateau is subducted underneath another one, or under existing continental crust, the eruptions produced thereby produce material that is yet more felsic, and so on through geologic time.

answers: NDQ_003351

answers: buoyant

answers: NDQ_003352

answers: more felsic

answers: NDQ_003353

answers: eruptions

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: plate

answers: NDQ_003356

answers: subduct

answers: NDQ_003357

answers: a plate carrying oceanic crust subducts under a plate carrying an igneous oceanic plateau

answers: NDQ_003358

answers: plateau

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: plates

answers: NDQ_003362

answers: a step toward creating crust which is increasingly continental in character

answers: NDQ_003363

answers: igneous oceanic plateau

answers: NDQ_003371

answers: What may be a step toward creating crust which is increasingly continental in character?

answers: NDQ_003373

answers: What is the main idea of this passage?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a stress?

answers: NDQ_003381

answers: What happens to rock when confining stress occurs?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: What is the cause of joints in rock

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: What is the cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not a type of normal fault?

answers: NDQ_003388

answers: What does shear stress result from?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: continental crust

answers: NDQ_003392

answers: unanswerable

answers: NDQ_003393

answers: continental crust

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: is a fault

answers: NDQ_003396

answers: horizontal

answers: NDQ_003351

answers: volcanism

answers: NDQ_003352

answers: more felsic

answers: NDQ_003353

answers: less dense and more buoyant.

answers: NDQ_003354

answers: igneous oceanic plateau,

answers: NDQ_003355

answers: igneous oceanic plateau,

answers: NDQ_003356

answers: less dense and more buoyant.

answers: NDQ_003357

answers: less dense and more buoyant.

answers: NDQ_003358

answers: igneous oceanic plateau,

answers: NDQ_003359

answers: when a plate carrying oceanic crust subducts

answers: NDQ_003360

answers: a plate

answers: NDQ_003362

answers: the volcanism

answers: NDQ_003363

answers: igneous oceanic plateau,

answers: NDQ_003371

answers: the volcanism

answers: NDQ_003373

answers: less dense and more buoyant.

answers: NDQ_003376

answers: igneous oceanic plateau,

answers: NDQ_003378

answers: igneous oceanic plateau, the volcanism

answers: NDQ_003379

answers: igneous oceanic plateau,

answers: NDQ_003380

answers: less dense and more buoyant.

answers: NDQ_003381

answers: less dense and more buoyant.

answers: NDQ_003382

answers: igneous oceanic plateau,

answers: NDQ_003383

answers: igneous oceanic plateau,

answers: NDQ_003384

answers: igneous oceanic plateau,

answers: NDQ_003385

answers: igneous oceanic plateau,

answers: NDQ_003386

answers: the volcanism

answers: NDQ_003387

answers: igneous oceanic plateau, the volcanism

answers: NDQ_003388

answers: igneous oceanic plateau,

answers: NDQ_003389

answers: igneous oceanic plateau,

answers: NDQ_003390

answers: igneous oceanic plateau,

answers: NDQ_003391

answers: igneous oceanic plateau,

answers: NDQ_003392

answers: igneous oceanic plateau,

answers: NDQ_003393

answers: igneous oceanic plateau,

answers: NDQ_003394

answers: igneous oceanic plateau, the volcanism

answers: NDQ_003395

answers: igneous oceanic plateau,

answers: NDQ_003396

answers: igneous oceanic plateau,

text: Nonetheless, Earth remains the only place in the Universe known to harbour life, and fossil evidence from the Earth supplies most studies of abiogenesis. The age of the Earth is about 4.54 billion years; the earliest undisputed evidence of life on Earth dates from at least 3.5 billion years ago, and possibly as early as the Eoarchean Era, after a geological crust started to solidify following the earlier molten Hadean Eon. Microbial mat fossils have been found in 3.48 billion-year-old sandstone in Western Australia. Other early physical evidence of biogenic substances includes graphite and possibly stromatolites discovered in 3.7 billion-year-old metasedimentary rocks in southwestern Greenland, as well as "remains of biotic life" found in 4.1 billion-year-old rocks in Western Australia. According to a scientist who commented on the study, "If life arose relatively quickly on Earth … then it could be common in the universe."

text: Nonetheless, Earth remains the only place in the Universe known to harbour life, and fossil evidence from the Earth supplies most studies of abiogenesis. The

text: age of the Earth

text: is about 4.54 billion years; the earliest undisputed evidence of life on Earth dates from at least 3.5 billion years ago, and possibly as early as the

text: Eoarchean

text: Era, after a geological

text: crust

text: started to solidify following the earlier molten

text: Hadean

text: Eon

text: Microbial mat

text: fossil

text: s have been found in 3.48 billion-year-old

text: sandstone

text: in

text: Western Australia

text: . Other early physical evidence of

text: biogenic substance

text: s includes

text: graphite

text: and possibly

text: stromatolites

text: discovered in 3.7 billion-year-old

text: metasedimentary rocks

text: in southwestern

text: Greenland

text: , as well as "remains of

text: biotic life

text: " found in 4.1 billion-year-old rocks in Western Australia. According to a scientist who commented on the study, "If life arose relatively quickly on Earth … then it could be common in the

text: universe

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: solidify

answers: NDQ_003353

answers: solidification

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: fold that bends downward

answers: NDQ_003356

answers: solidify

answers: NDQ_003357

answers: a geological crust started to solidify

answers: NDQ_003358

answers: unanswerable

answers: NDQ_003359

answers: solidify

answers: NDQ_003360

answers: Earth

answers: NDQ_003362

answers: Earth remains the only place in the Universe known to harbour life

answers: NDQ_003363

answers: Hadean Eon

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: unanswerable

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What is a stress?

answers: NDQ_003381

answers: What type of rock deforms?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: fault zone

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: unanswerable

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: a geological crust

answers: NDQ_003391

answers: a geological crust

answers: NDQ_003392

answers: a hanging wall

answers: NDQ_003393

answers: sandstone

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: southwestern Greenland

answers: NDQ_003396

answers: Hadean Eon

answers: NDQ_003351

answers: molten Hadean Eon.

answers: NDQ_003352

answers: solidify

answers: NDQ_003353

answers: solidify

answers: NDQ_003354

answers: Earth

answers: NDQ_003355

answers: abiogenesis.

answers: NDQ_003356

answers: solidify

answers: NDQ_003357

answers: molten Hadean Eon.

answers: NDQ_003358

answers: metasedimentary

answers: NDQ_003359

answers: molten

answers: NDQ_003360

answers: Earth

answers: NDQ_003362

answers: "If life arose relatively quickly on Earth...

answers: NDQ_003363

answers: molten Hadean Eon.

answers: NDQ_003371

answers: 4.54 billion years;

answers: NDQ_003373

answers: 3.7 billion-year-old metasedimentary rocks

answers: NDQ_003376

answers: molten Hadean Eon.

answers: NDQ_003378

answers: Earth remains the only place in the Universe known to harbour life,

answers: NDQ_003379

answers: Earth remains the only place in the Universe known to harbour life,

answers: NDQ_003380

answers: Earth remains the only place in the Universe known to harbour life,

answers: NDQ_003381

answers: a geological crust started to solidify

answers: NDQ_003382

answers: Earth remains the only place in the Universe known to harbour life,

answers: NDQ_003383

answers: Earth remains the only place in the Universe known to harbour life,

answers: NDQ_003384

answers: Earth remains the only place in the Universe known to harbour life,

answers: NDQ_003385

answers: fossil evidence from the Earth supplies most studies of abiogenesis.

answers: NDQ_003386

answers: Earth remains the only place in the Universe known to harbour life,

answers: NDQ_003387

answers: Earth remains the only place in the Universe known to harbour life,

answers: NDQ_003388

answers: Earth remains the only place in the Universe known to harbour life,

answers: NDQ_003389

answers: Earth remains the only place in the Universe known to harbour life,

answers: NDQ_003390

answers: Earth remains the only place in the Universe known to harbour life,

answers: NDQ_003391

answers: 3.7 billion-year-old metasedimentary rocks

answers: NDQ_003392

answers: Earth remains the only place in the Universe known to harbour life,

answers: NDQ_003393

answers: 3.7 billion-year-old metasedimentary rocks

answers: NDQ_003394

answers: abiogenesis.

answers: NDQ_003395

answers: molten Hadean Eon.

answers: NDQ_003396

answers: Earth remains the only place in the Universe known to harbour life,

text: In geology, the sial refers to the composition of the upper layer of the Earth's crust, namely rocks rich in silicates and aluminium minerals.  It is sometimes equated with the continental crust because it is absent in the wide oceanic basins, but "sial" is a geochemical term rather than a plate tectonic term. As these elements are less dense than the majority of the earth's elements, they tend to be concentrated in the upper layer of the crust.

text: In

text: geology

text: , the sial refers to the composition of the upper layer of the

text: Earth

text: 's

text: crust

text: , namely rocks rich in

text: silicate

text: s and

text: aluminium

text: minerals.  It is sometimes equated with the

text: continental crust

text: because it is absent in the wide

text: oceanic basin

text: s, but "sial" is a

text: geochemical

text: term rather than a

text: plate tectonic

text: term. As these elements are less dense than the majority of the earth's elements, they tend to be concentrated in the upper layer of the crust.

answers: NDQ_003351

answers: sial

answers: NDQ_003352

answers: is more likely to contain silicates

answers: NDQ_003353

answers: silicates to break down

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: continental crust

answers: NDQ_003356

answers: concentrate in the upper layer of the crust

answers: NDQ_003357

answers: rock rich in silicates and aluminium minerals

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: plates

answers: NDQ_003362

answers: sial is a geochemical term rather than a plate tectonic term

answers: NDQ_003363

answers: plate tectonic

answers: NDQ_003371

answers: What may be the reason for a thrust fault?

answers: NDQ_003373

answers: unanswerable

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: vertical

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: what is the first type of stress mentioned?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: what is sometimes equated with the continental crust

answers: NDQ_003386

answers: plate tectonic

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: unanswerable

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: plate tectonic

answers: NDQ_003391

answers: continental crust

answers: NDQ_003392

answers: plate tectonic

answers: NDQ_003393

answers: continental crust

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: unanswerable

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: silicates and aluminium minerals.

answers: NDQ_003352

answers: concentrated in the upper layer of the crust.

answers: NDQ_003353

answers: rocks rich in silicates and aluminium minerals.

answers: NDQ_003354

answers: In geology,

answers: NDQ_003355

answers: continental crust because it is absent in the wide oceanic basins,

answers: NDQ_003356

answers: concentrated in the upper layer of the crust.

answers: NDQ_003357

answers: concentrated in the upper layer of the crust.

answers: NDQ_003358

answers: oceanic basins,

answers: NDQ_003359

answers: rocks rich in silicates and aluminium minerals.

answers: NDQ_003360

answers: plate tectonic

answers: NDQ_003362

answers: absent in the wide oceanic basins,

answers: NDQ_003363

answers: oceanic basins,

answers: NDQ_003371

answers: In geology,

answers: NDQ_003373

answers: rocks rich in silicates and aluminium minerals.

answers: NDQ_003376

answers: oceanic basins,

answers: NDQ_003378

answers: In geology,

answers: NDQ_003379

answers: absent in the wide oceanic basins,

answers: NDQ_003380

answers: rocks rich in silicates and aluminium minerals.

answers: NDQ_003381

answers: rocks rich in silicates and aluminium minerals.

answers: NDQ_003382

answers: rocks rich in silicates and aluminium minerals.

answers: NDQ_003383

answers: rocks rich in silicates and aluminium minerals.

answers: NDQ_003384

answers: In geology,

answers: NDQ_003385

answers: In geology,

answers: NDQ_003386

answers: plate tectonic

answers: NDQ_003387

answers: In geology,

answers: NDQ_003388

answers: In geology,

answers: NDQ_003389

answers: plate tectonic

answers: NDQ_003390

answers: plate tectonic

answers: NDQ_003391

answers: sial

answers: NDQ_003392

answers: plate tectonic

answers: NDQ_003393

answers: sial

answers: NDQ_003394

answers: plate tectonic

answers: NDQ_003395

answers: plate tectonic

answers: NDQ_003396

answers: plate tectonic

text: The Horn of Africa is almost equidistant from the equator and the Tropic of Cancer. It consists chiefly of mountains uplifted through the formation of the Great Rift Valley, a fissure in the Earth's crust extending from Turkey to Mozambique and marking the separation of the African and Arabian tectonic plates. Mostly mountainous, the region arose through faults resulting from the Rift Valley.

text: The Horn of Africa is almost

text: equidistant

text: from the

text: equator

text: and the

text: Tropic of Cancer

text: . It consists chiefly of mountains uplifted through the formation of the

text: Great Rift Valley

text: , a fissure in the Earth's

text: crust

text: extending from

text: Turkey

text: to

text: Mozambique

text: and marking the separation of the African and Arabian

text: tectonic plates

text: . Mostly mountainous, the region arose through faults resulting from the Rift Valley.

answers: NDQ_003351

answers: faults

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: faults

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fissure

answers: NDQ_003356

answers: uplift

answers: NDQ_003357

answers: a fissure in the Earth's crust

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: uplifted

answers: NDQ_003360

answers: faults

answers: NDQ_003362

answers: The Horn of Africa is almost equidistant from the equator

answers: NDQ_003363

answers: the Great Rift Valley

answers: NDQ_003371

answers: Which of the following is not a tectonic plate: African or Arabian?

answers: NDQ_003373

answers: Why is the Horn of Africa almost equidistant from the equator

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: How does the Horn of Africa differ from the equator?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not a tectonic plate: African or Arabian?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: Which of the following is not a type of fault?

answers: NDQ_003387

answers: Which of the following is not a tectonic plate: African or Arabian?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip faults, tectonic plates, or faults?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: mountainous

answers: NDQ_003392

answers: unanswerable

answers: NDQ_003393

answers: mountainous

answers: NDQ_003394

answers: unanswerable

answers: NDQ_003395

answers: faults resulting from the Rift Valley

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: faults

answers: NDQ_003352

answers: faults

answers: NDQ_003353

answers: faults

answers: NDQ_003354

answers: The Horn of Africa

answers: NDQ_003355

answers: faults

answers: NDQ_003356

answers: mountainous,

answers: NDQ_003357

answers: separation of the African and Arabian tectonic plates.

answers: NDQ_003358

answers: faults

answers: NDQ_003359

answers: fissure in the Earth's crust

answers: NDQ_003360

answers: Great Rift Valley,

answers: NDQ_003362

answers: equidistant from the equator

answers: NDQ_003363

answers: Great Rift Valley,

answers: NDQ_003371

answers: faults resulting from the Rift Valley.

answers: NDQ_003373

answers: Great Rift Valley,

answers: NDQ_003376

answers: faults

answers: NDQ_003378

answers: Great Rift Valley,

answers: NDQ_003379

answers: Great Rift Valley,

answers: NDQ_003380

answers: faults

answers: NDQ_003381

answers: faults resulting from the Rift Valley.

answers: NDQ_003382

answers: African and Arabian tectonic plates.

answers: NDQ_003383

answers: faults

answers: NDQ_003384

answers: Great Rift Valley,

answers: NDQ_003385

answers: faults resulting from the Rift Valley.

answers: NDQ_003386

answers: faults

answers: NDQ_003387

answers: Rift Valley.

answers: NDQ_003388

answers: the Rift Valley.

answers: NDQ_003389

answers: faults

answers: NDQ_003390

answers: faults resulting from the Rift Valley.

answers: NDQ_003391

answers: mountains uplifted through the formation of the Great Rift Valley,

answers: NDQ_003392

answers: Great Rift Valley,

answers: NDQ_003393

answers: mountains uplifted through the formation of the Great Rift Valley,

answers: NDQ_003394

answers: faults

answers: NDQ_003395

answers: faults resulting from the Rift Valley.

answers: NDQ_003396

answers: Great Rift Valley,

text: Tectonics (from the Late Latin tectonicus from the Greek τεκτονικός, "pertaining to building") is concerned with the processes which control the structure and properties of the Earth's crust, and its evolution through time. In particular, it describes the processes of mountain building, the growth and behavior of the strong, old cores of continents known as cratons, and the ways in which the relatively rigid plates that constitute the Earth's outer shell interact with each other. Tectonics also provides a framework to understand the earthquake and volcanic belts which directly affect much of the global population. Tectonic studies are important for understanding erosion patterns in geomorphology and as guides for the economic geologist searching for petroleum and metallic ores.

text: Tectonics (from the

text: Late Latin

text: tectonicus

text: from the

text: Greek

text: τεκτονικός, "pertaining to

text: building

text: ") is concerned with the processes which control the structure and properties of the Earth's crust, and its evolution through time. In particular, it describes the processes of

text: mountain building

text: , the growth and behavior of the strong, old cores of continents known as

text: craton

text: s, and the ways in which the relatively rigid

text: plates

text: that constitute the Earth's outer shell interact with each other. Tectonics also provides a framework to understand the

text: earthquake

text: and

text: volcanic belt

text: s which directly affect much of the global population. Tectonic studies are important for understanding

text: erosion

text: patterns in

text: geomorphology

text: and as guides for the

text: economic geologist

text: searching for

text: petroleum

text: and

text: metal

text: lic

text: ore

text: s.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: more likely to crack

answers: NDQ_003353

answers: erosion

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: cratons

answers: NDQ_003356

answers: erode

answers: NDQ_003357

answers: Earth's outer shell interacts with each other

answers: NDQ_003358

answers: cratons

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: cratons

answers: NDQ_003362

answers: directly affect much of the global population

answers: NDQ_003363

answers: cratons

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: How would you describe Tectonics?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: what is the dip of the fault plane

answers: NDQ_003380

answers: What does Tectonics describe?

answers: NDQ_003381

answers: What does Tectonics describe?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: Tectonics

answers: NDQ_003387

answers: What type of stress is caused by normal faults?

answers: NDQ_003388

answers: What does tectonics describe?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: Tectonic

answers: NDQ_003391

answers: mountain

answers: NDQ_003392

answers: Tectonics

answers: NDQ_003393

answers: mountain

answers: NDQ_003394

answers: non-vertical

answers: NDQ_003395

answers: cratons

answers: NDQ_003396

answers: horizontal fault

answers: NDQ_003351

answers: earthquake and volcanic belts

answers: NDQ_003352

answers: erosion

answers: NDQ_003353

answers: erosion

answers: NDQ_003354

answers: Tectonics

answers: NDQ_003355

answers: erosion

answers: NDQ_003356

answers: erosion

answers: NDQ_003357

answers: rigid plates that constitute the Earth's outer shell interact with each other.

answers: NDQ_003358

answers: cratons,

answers: NDQ_003359

answers: each other.

answers: NDQ_003360

answers: cratons,

answers: NDQ_003362

answers: directly affect much of the global population.

answers: NDQ_003363

answers: cratons,

answers: NDQ_003371

answers: Tectonics

answers: NDQ_003373

answers: Tectonics

answers: NDQ_003376

answers: cratons,

answers: NDQ_003378

answers: earthquake and volcanic belts which directly affect much of the global population.

answers: NDQ_003379

answers: petroleum and metallic ores.

answers: NDQ_003380

answers: earthquake and volcanic belts which directly affect much of the global population.

answers: NDQ_003381

answers: relatively rigid plates

answers: NDQ_003382

answers: cratons,

answers: NDQ_003383

answers: rigid plates that constitute the Earth's outer shell interact with each other.

answers: NDQ_003384

answers: cratons,

answers: NDQ_003385

answers: Tectonics

answers: NDQ_003386

answers: earthquake and volcanic belts which directly affect much of the global population.

answers: NDQ_003387

answers: earthquake and volcanic belts

answers: NDQ_003388

answers: Tectonics

answers: NDQ_003389

answers: Tectonics

answers: NDQ_003390

answers: Tectonics

answers: NDQ_003391

answers: cratons,

answers: NDQ_003392

answers: Tectonics

answers: NDQ_003393

answers: cratons,

answers: NDQ_003394

answers: volcanic belts

answers: NDQ_003395

answers: volcanic belts

answers: NDQ_003396

answers: volcanic belts

text: The Indian plate continues to move north relative to Asia at the rate of approximately  per year. This is approximately twice the speed at which human fingernails grow, which is very fast given the size of the blocks of Earth's crust involved. As the strong Indian continental crust subducts beneath the relatively weak Tibetan crust, it pushes up the Himalayan Mountains. This collision zone has accommodated huge amounts of crustal shortening as the rock sequences slide one over another.

text: The Indian plate continues to move north relative to Asia at the rate of approximately  per year. This is approximately twice the speed at which human fingernails grow, which is very fast given the size of the blocks of Earth's crust involved. As the strong Indian continental crust subducts beneath the relatively weak Tibetan crust, it pushes up the Himalayan Mountains. This collision zone has accommodated huge amounts of crustal shortening as the rock sequences slide one over another.

answers: NDQ_003351

answers: crustal shortening

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: crustal shortening

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: Indian plate

answers: NDQ_003356

answers: slide one over another

answers: NDQ_003357

answers: rock sequences slide one over another

answers: NDQ_003358

answers: collision zone

answers: NDQ_003359

answers: slide one over another

answers: NDQ_003360

answers: Indian plate

answers: NDQ_003362

answers: strong Indian continental crust subducts beneath the relatively weak Tibetan crust

answers: NDQ_003363

answers: the rate of approximately per year

answers: NDQ_003371

answers: Which of the following is not a type of rock sequence: rock sequences slide one over another or rock sequences slide one over another?

answers: NDQ_003373

answers: Why is the rock sequences slide one over another?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What happens to the rock sequences slide one over another?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What type of rock sequences slide one over another?

answers: NDQ_003384

answers: What does the Indian plate continue to move north relative to Asia?

answers: NDQ_003385

answers: what is the last word in the passage?

answers: NDQ_003386

answers: what is the last word in the passage?

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: normal faults, Indian plate, or Himalayan Mountains?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip faults, earthquake faults, or earthquake faults?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: collapsing zone

answers: NDQ_003391

answers: weak Tibetan crust

answers: NDQ_003392

answers: collision zone

answers: NDQ_003393

answers: weak Tibetan crust

answers: NDQ_003394

answers: subduct

answers: NDQ_003395

answers: subducts beneath the relatively weak Tibetan crust, it pushes up the Himalayan Mountains

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: crustal shortening

answers: NDQ_003352

answers: crustal shortening

answers: NDQ_003353

answers: crustal shortening

answers: NDQ_003354

answers: Indian continental crust subducts beneath the relatively weak Tibetan crust,

answers: NDQ_003355

answers: The Indian plate

answers: NDQ_003356

answers: crustal shortening

answers: NDQ_003357

answers: rock sequences slide one over another.

answers: NDQ_003358

answers: collision zone

answers: NDQ_003359

answers: slide one over another.

answers: NDQ_003360

answers: the strong Indian continental crust subducts beneath the relatively weak Tibetan crust,

answers: NDQ_003362

answers: human fingernails grow,

answers: NDQ_003363

answers: As the strong Indian continental crust subducts beneath the relatively weak Tibetan crust,

answers: NDQ_003371

answers: rock sequences slide one over another.

answers: NDQ_003373

answers: crustal shortening

answers: NDQ_003376

answers: Himalayan Mountains.

answers: NDQ_003378

answers: slide one over another.

answers: NDQ_003379

answers: per year.

answers: NDQ_003380

answers: crustal shortening

answers: NDQ_003381

answers: crustal shortening

answers: NDQ_003382

answers: crustal shortening

answers: NDQ_003383

answers: slide one over another.

answers: NDQ_003384

answers: Himalayan Mountains.

answers: NDQ_003385

answers: collision zone

answers: NDQ_003386

answers: the rock sequences slide one over another.

answers: NDQ_003387

answers: crustal shortening

answers: NDQ_003388

answers: crustal shortening

answers: NDQ_003389

answers: crustal shortening

answers: NDQ_003390

answers: Tibetan crust, it pushes up the Himalayan Mountains.

answers: NDQ_003391

answers: Tibetan crust,

answers: NDQ_003392

answers: Himalayan Mountains.

answers: NDQ_003393

answers: Tibetan crust,

answers: NDQ_003394

answers: per year.

answers: NDQ_003395

answers: per year.

answers: NDQ_003396

answers: Tibetan crust, it pushes up the Himalayan Mountains.

text: Also in 1989, the National Endowment for the Humanities chose him as the winner for the Jefferson Lecture in the Humanities. He read his essay, "The Fateful Rift: The San Andreas Fault in the Modern Mind."

text: Also in 1989, the

text: National Endowment for the Humanities

text: chose him as the winner for the

text: Jefferson Lecture

text: in the Humanities. He read his essay, "The Fateful Rift: The San Andreas Fault in the Modern Mind."

answers: NDQ_003351

answers: San Andreas Fault

answers: NDQ_003352

answers: more likely breaks

answers: NDQ_003353

answers: rifts

answers: NDQ_003354

answers: Toroweap Formation is above

answers: NDQ_003355

answers: Rift

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: The San Andreas Fault in the Modern Mind

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: San Andreas faults

answers: NDQ_003362

answers: The San Andreas Fault in the Modern Mind.

answers: NDQ_003363

answers: San Andreas fault

answers: NDQ_003371

answers: Which of the following is not a type of thrust fault: San Andreas Fault in the Modern Mind?

answers: NDQ_003373

answers: What is the best title for this passage?

answers: NDQ_003376

answers: The San Andreas Fault in the Modern Mind

answers: NDQ_003378

answers: what is the second to last word in the passage?

answers: NDQ_003379

answers: The dip of the fault plane is vertical

answers: NDQ_003380

answers: Which of the following is not a type of force applied to rock?

answers: NDQ_003381

answers: What type of stress occurs when rock deforms?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the reason for joints in rock?

answers: NDQ_003384

answers: What type of fold is the Jefferson Lecture in the Humanities?

answers: NDQ_003385

answers: The Fateful Rift

answers: NDQ_003386

answers: The San Andreas Fault

answers: NDQ_003387

answers: Which of the following is not a type of fault: San Andreas Fault in the Modern Mind?

answers: NDQ_003388

answers: What is the cause of strike-slip faults?

answers: NDQ_003389

answers: The Fateful Rift

answers: NDQ_003390

answers: San Andreas Fault

answers: NDQ_003391

answers: rift zone

answers: NDQ_003392

answers: San Andreas Fault

answers: NDQ_003393

answers: rift zone

answers: NDQ_003394

answers: San Andreas Fault

answers: NDQ_003395

answers: San Andreas Fault

answers: NDQ_003396

answers: San Andreas Fault

answers: NDQ_003351

answers: The San Andreas

answers: NDQ_003352

answers: "The Fateful Rift:

answers: NDQ_003353

answers: Rift:

answers: NDQ_003354

answers: Jefferson Lecture in the Humanities.

answers: NDQ_003355

answers: Rift:

answers: NDQ_003356

answers: "The Fateful Rift:

answers: NDQ_003357

answers: The San Andreas

answers: NDQ_003358

answers: Rift:

answers: NDQ_003359

answers: The San Andreas Fault in the Modern Mind."

answers: NDQ_003360

answers: The San Andreas

answers: NDQ_003362

answers: The San Andreas Fault in the Modern Mind."

answers: NDQ_003363

answers: The San Andreas

answers: NDQ_003371

answers: The San Andreas Fault in the Modern Mind."

answers: NDQ_003373

answers: Jefferson Lecture in the Humanities.

answers: NDQ_003376

answers: The San Andreas Fault in the Modern Mind."

answers: NDQ_003378

answers: "The Fateful Rift:

answers: NDQ_003379

answers: The San Andreas Fault in the Modern Mind."

answers: NDQ_003380

answers: Jefferson Lecture in the Humanities.

answers: NDQ_003381

answers: The San Andreas Fault in the Modern Mind."

answers: NDQ_003382

answers: The San Andreas Fault in the Modern Mind."

answers: NDQ_003383

answers: The San Andreas Fault in the Modern Mind."

answers: NDQ_003384

answers: Jefferson Lecture in the Humanities.

answers: NDQ_003385

answers: The San Andreas Fault in the Modern Mind."

answers: NDQ_003386

answers: The San Andreas Fault in the Modern Mind."

answers: NDQ_003387

answers: The San Andreas Fault in the Modern Mind."

answers: NDQ_003388

answers: The San Andreas Fault in the Modern Mind."

answers: NDQ_003389

answers: "The Fateful Rift:

answers: NDQ_003390

answers: The San Andreas

answers: NDQ_003391

answers: The San Andreas Fault

answers: NDQ_003392

answers: The San Andreas Fault

answers: NDQ_003393

answers: The San Andreas Fault

answers: NDQ_003394

answers: The San Andreas Fault

answers: NDQ_003395

answers: The San Andreas

answers: NDQ_003396

answers: The San Andreas Fault

text: The Sawatch Uplift  is a prominent geologic anticline in the Rocky Mountains in central Colorado in the United States. It was formed as a bulge in the North American Plate approximately 70–65 MYA during the Laramide orogeny that created the modern Rocky Mountains. The uplift runs north-south for several hundred miles from central Colorado into northern New Mexico. The Sawatch Range and Mosquito Range were both formed as part of the uplift. Approximately 35 MYA, stresses in the continental plate in the center of the uplift caused the center to collapse, forming a trough between the Sawatch and Mosquito Range that is part of the larger Rio Grande Rift. The trough runs southward from Leadville, CO into New Mexico. The northern part of the rift forms the headwater valley of the Arkansas River.

text: The Sawatch Uplift  is a prominent

text: geologic

text: anticline

text: in the

text: Rocky Mountains

text: in central

text: Colorado

text: in the

text: United States

text: . It was formed as a bulge in the

text: North American Plate

text: approximately 70–65

text: MYA

text: during the

text: Laramide orogeny

text: that created the modern Rocky Mountains. The uplift runs north-south for several hundred miles from central Colorado into northern

text: New Mexico

text: . The

text: Sawatch Range

text: and

text: Mosquito Range

text: were both formed as part of the uplift. Approximately 35 MYA, stresses in the continental plate in the center of the uplift caused the center to collapse, forming a trough between the Sawatch and Mosquito Range that is part of the larger

text: Rio Grande Rift

text: . The trough runs southward from

text: Leadville, CO

text: into New Mexico. The northern part of the rift forms the headwater valley of the

text: Arkansas River

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: collapses

answers: NDQ_003353

answers: collapse

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: anticline

answers: NDQ_003356

answers: collapse

answers: NDQ_003357

answers: a trough runs southward from Leadville, CO into New Mexico

answers: NDQ_003358

answers: trough

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: North American Plate

answers: NDQ_003362

answers: trough runs southward from Leadville, CO into New Mexico

answers: NDQ_003363

answers: Laramide orogeny

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: How would you describe the Sawatch Uplift?

answers: NDQ_003376

answers: What type of forces caused the terrain known as basin-and-range?

answers: NDQ_003378

answers: How many miles does the uplift run north-south?

answers: NDQ_003379

answers: What is the dip of the fault plane in a strike-slip fault

answers: NDQ_003380

answers: What caused the center to collapse?

answers: NDQ_003381

answers: How did the Sawatch Uplift deform?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What type of fold is the Sawatch Uplift?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: Which of the following is not a cause of earthquakes?

answers: NDQ_003387

answers: Which happened first, the Sawatch Uplift or the Rio Grande Rift?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip, Mosquito, or uplift?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: anticline

answers: NDQ_003391

answers: anticline

answers: NDQ_003392

answers: anticline

answers: NDQ_003393

answers: anticline

answers: NDQ_003394

answers: Rift

answers: NDQ_003395

answers: Rio Grande Rift

answers: NDQ_003396

answers: Rift

answers: NDQ_003351

answers: continental plate

answers: NDQ_003352

answers: collapse,

answers: NDQ_003353

answers: the center to collapse,

answers: NDQ_003354

answers: Rio Grande Rift.

answers: NDQ_003355

answers: anticline

answers: NDQ_003356

answers: collapse,

answers: NDQ_003357

answers: Rio Grande Rift.

answers: NDQ_003358

answers: trough

answers: NDQ_003359

answers: stresses

answers: NDQ_003360

answers: Laramide orogeny

answers: NDQ_003362

answers: Rio Grande Rift.

answers: NDQ_003363

answers: Laramide orogeny

answers: NDQ_003371

answers: Rio Grande Rift.

answers: NDQ_003373

answers: stresses in the continental plate

answers: NDQ_003376

answers: trough

answers: NDQ_003378

answers: The Sawatch Uplift

answers: NDQ_003379

answers: Rio Grande Rift.

answers: NDQ_003380

answers: stresses

answers: NDQ_003381

answers: stresses in the continental plate

answers: NDQ_003382

answers: Rio Grande Rift.

answers: NDQ_003383

answers: stresses

answers: NDQ_003384

answers: anticline

answers: NDQ_003385

answers: Rio Grande Rift.

answers: NDQ_003386

answers: stresses in the continental plate

answers: NDQ_003387

answers: stresses in the continental plate

answers: NDQ_003388

answers: stresses in the continental plate

answers: NDQ_003389

answers: Laramide orogeny

answers: NDQ_003390

answers: Sawatch Uplift

answers: NDQ_003391

answers: Rio Grande Rift.

answers: NDQ_003392

answers: The Sawatch Uplift

answers: NDQ_003393

answers: The Sawatch Uplift

answers: NDQ_003394

answers: Rio Grande Rift.

answers: NDQ_003395

answers: Rio Grande Rift.

answers: NDQ_003396

answers: Rio Grande Rift.

text: Anticlines are usually developed above thrust faults, so any small compression and motion within the inner crust can have large effects on the upper rock stratum.  Stresses developed during mountain building or during other tectonic processes can similarly warp or bend bedding and foliation (or other planar features).  The more the underlying fault is tectonically uplifted, the more the strata will be deformed and must adapt to new shapes.  The shape formed will also be very dependent on the properties and cohesion of the different types of rock within each layer.

text: Anticlines are usually developed above thrust faults, so any small

text: compression

text: and motion within the inner crust can have large effects on the upper rock stratum.  Stresses developed during mountain building or during other tectonic processes can similarly warp or bend bedding and

text: foliation

text: (or other planar features).  The more the underlying fault is tectonically uplifted, the more the strata will be deformed and must adapt to new shapes.  The shape formed will also be very dependent on the properties and cohesion of the different types of rock within each layer.

answers: NDQ_003351

answers: thrust faults

answers: NDQ_003352

answers: warp or bend

answers: NDQ_003353

answers: warp or bend

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: Anticlines

answers: NDQ_003356

answers: change shape

answers: NDQ_003357

answers: any small compression and motion within the inner crust can have large effects

answers: NDQ_003358

answers: anticline

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: faults

answers: NDQ_003362

answers: any small compression and motion within the inner crust can have large effects on the upper rock stratum

answers: NDQ_003363

answers: tectonic processes

answers: NDQ_003371

answers: Which of the following is not a type of rock?

answers: NDQ_003373

answers: any small compression and motion within the inner crust

answers: NDQ_003376

answers: What type of terrain is caused by compressive forces?

answers: NDQ_003378

answers: any small compression and motion within the inner crust

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What is a stress?

answers: NDQ_003381

answers: What happens to the strata when the underlying fault is uplifted?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: warp or bend bedding and foliation

answers: NDQ_003384

answers: Which of the following is not a type of fold?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: what is the cause of earthquakes

answers: NDQ_003387

answers: Which of the following is not caused by compression stress?

answers: NDQ_003388

answers: Which of the following is not a type of strike-slip fault?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: thrust fault

answers: NDQ_003391

answers: stratum

answers: NDQ_003392

answers: thrust fault

answers: NDQ_003393

answers: stratum

answers: NDQ_003394

answers: thrust fault

answers: NDQ_003395

answers: thrust faults

answers: NDQ_003396

answers: thrust fault

answers: NDQ_003351

answers: thrust faults,

answers: NDQ_003352

answers: warp or bend bedding and foliation

answers: NDQ_003353

answers: warp or bend bedding and foliation

answers: NDQ_003354

answers: Anticlines are usually developed above thrust faults,

answers: NDQ_003355

answers: Anticlines

answers: NDQ_003356

answers: new shapes.

answers: NDQ_003357

answers: motion within the inner crust can have large effects on the upper rock stratum.

answers: NDQ_003358

answers: Anticlines

answers: NDQ_003359

answers: tectonically uplifted,

answers: NDQ_003360

answers: thrust faults,

answers: NDQ_003362

answers: Anticlines are usually developed above thrust faults,

answers: NDQ_003363

answers: thrust faults,

answers: NDQ_003371

answers: Anticlines are usually developed above thrust faults,

answers: NDQ_003373

answers: Anticlines are usually developed above thrust faults,

answers: NDQ_003376

answers: Anticlines are usually developed above thrust faults,

answers: NDQ_003378

answers: motion within the inner crust can have large effects on the upper rock stratum.

answers: NDQ_003379

answers: thrust faults,

answers: NDQ_003380

answers: Stresses

answers: NDQ_003381

answers: warp or bend bedding and foliation

answers: NDQ_003382

answers: thrust faults,

answers: NDQ_003383

answers: Stresses

answers: NDQ_003384

answers: Anticlines

answers: NDQ_003385

answers: thrust faults,

answers: NDQ_003386

answers: motion within the inner crust can have large effects on the upper rock stratum.

answers: NDQ_003387

answers: thrust faults,

answers: NDQ_003388

answers: thrust faults,

answers: NDQ_003389

answers: mountain building

answers: NDQ_003390

answers: thrust faults,

answers: NDQ_003391

answers: Anticlines

answers: NDQ_003392

answers: thrust faults,

answers: NDQ_003393

answers: Anticlines

answers: NDQ_003394

answers: thrust faults,

answers: NDQ_003395

answers: thrust faults,

answers: NDQ_003396

answers: thrust faults,

text: In the simplest example, isostasy is the principle of buoyancy wherein an object immersed in a fluid is buoyed with a force equal to the weight of the displaced fluid. On a geological scale, isostasy can be observed where Earth's strong crust or lithosphere exerts stress on the weaker mantle or asthenosphere, which, over geological time, flows laterally such that the load is accommodated by height adjustments.

text: In the simplest example, isostasy is the principle of

text: buoyancy

text: wherein an object immersed in a

text: fluid

text: is buoyed with a force equal to the weight of the displaced fluid. On a geological scale, isostasy can be observed where Earth's strong crust or lithosphere exerts stress on the weaker mantle or asthenosphere, which, over

text: geological time

text: , flows laterally such that the load is accommodated by height adjustments.

answers: NDQ_003351

answers: isostasy

answers: NDQ_003352

answers: is more likely to crack

answers: NDQ_003353

answers: height adjustments

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: isostatic

answers: NDQ_003356

answers: buoyant

answers: NDQ_003357

answers: Earth's strong crust or lithosphere exerts stress on the weaker mantle

answers: NDQ_003358

answers: isostasy

answers: NDQ_003359

answers: is weaker

answers: NDQ_003360

answers: Earth's strong crust

answers: NDQ_003362

answers: buoyant with a force equal to the weight of the displaced fluid

answers: NDQ_003363

answers: isostasy

answers: NDQ_003371

answers: What is the principle of buoyancy?

answers: NDQ_003373

answers: isostasy

answers: NDQ_003376

answers: Earth's strong crust or lithosphere exerts stress on the weaker mantle

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: vertical

answers: NDQ_003380

answers: It's impossible to say

answers: NDQ_003381

answers: Where does isostasy occur?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: fault zone

answers: NDQ_003386

answers: stress on the weaker mantle or asthenosphere

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: isostasy can be observed where Earth's strong crust or lithosphere exerts stress

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: isostasy

answers: NDQ_003391

answers: isostasy

answers: NDQ_003392

answers: isostasy

answers: NDQ_003393

answers: lithosphere

answers: NDQ_003394

answers: flow laterally

answers: NDQ_003395

answers: isostasy

answers: NDQ_003396

answers: lateral

answers: NDQ_003351

answers: isostasy

answers: NDQ_003352

answers: flows laterally such that the load is accommodated by height adjustments.

answers: NDQ_003353

answers: flows laterally

answers: NDQ_003354

answers: isostasy

answers: NDQ_003355

answers: isostasy

answers: NDQ_003356

answers: height adjustments.

answers: NDQ_003357

answers: Earth's strong crust or lithosphere exerts stress

answers: NDQ_003358

answers: isostasy

answers: NDQ_003359

answers: stress

answers: NDQ_003360

answers: Earth's strong crust

answers: NDQ_003362

answers: height adjustments.

answers: NDQ_003363

answers: geological time, flows laterally

answers: NDQ_003371

answers: isostasy

answers: NDQ_003373

answers: isostasy

answers: NDQ_003376

answers: Earth's strong crust

answers: NDQ_003378

answers: height adjustments.

answers: NDQ_003379

answers: laterally

answers: NDQ_003380

answers: stress

answers: NDQ_003381

answers: lithosphere exerts stress on the weaker mantle

answers: NDQ_003382

answers: isostasy

answers: NDQ_003383

answers: Earth's strong crust or lithosphere exerts stress

answers: NDQ_003384

answers: isostasy

answers: NDQ_003385

answers: isostasy

answers: NDQ_003386

answers: stress on the weaker mantle

answers: NDQ_003387

answers: isostasy

answers: NDQ_003388

answers: isostasy

answers: NDQ_003389

answers: height adjustments.

answers: NDQ_003390

answers: isostasy

answers: NDQ_003391

answers: lithosphere exerts stress on the weaker mantle

answers: NDQ_003392

answers: isostasy

answers: NDQ_003393

answers: lithosphere exerts stress on the weaker mantle

answers: NDQ_003394

answers: laterally

answers: NDQ_003395

answers: laterally

answers: NDQ_003396

answers: laterally

text: The early Paleozoic geology of northern England records the convergence and eventual collision of the Avalonia microcontinent with the continent of Laurentia. The underlying Borrowdale Volcanic Group formed in an island arc, caused by the southerly subduction of the crust of the now vanished Iapetus Ocean. At the end of active arc volcanism, the area began to subside, allowing deposition of the shallow marine Dent Group. The final closure of Iapetus occurred during the Devonian Acadian orogeny, with the resulting continental collision causing deformation of the Ordovician rocks, including folding, thrusting and cleavage development.

text: The early

text: Paleozoic

text: geology of northern England records the convergence and eventual collision of the Avalonia microcontinent with the continent of Laurentia. The underlying

text: Borrowdale Volcanic Group

text: formed in an

text: island arc

text: , caused by the southerly

text: subduction

text: of the

text: crust

text: of the now vanished

text: Iapetus Ocean

text: . At the end of active arc volcanism, the area began to subside, allowing deposition of the shallow marine Dent Group. The final closure of Iapetus occurred during the

text: Devonian

text: Acadian orogeny

text: , with the resulting

text: continental collision

text: causing deformation of the Ordovician rocks, including

text: folding

text: thrusting

text: and

text: cleavage

text: development.

answers: NDQ_003351

answers: thrusting

answers: NDQ_003352

answers: deforms

answers: NDQ_003353

answers: deformation

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: arc

answers: NDQ_003356

answers: fold

answers: NDQ_003357

answers: subduction of the crust of the now vanished Iapetus Ocean

answers: NDQ_003358

answers: cleavage

answers: NDQ_003359

answers: deforms

answers: NDQ_003360

answers: continental collision

answers: NDQ_003362

answers: the area began to subside

answers: NDQ_003363

answers: Devonian

answers: NDQ_003371

answers: What is the underlying Borrowdale Volcanic Group?

answers: NDQ_003373

answers: What is the main idea of this passage?

answers: NDQ_003376

answers: Which of the following is not a type of terrain: basin-and-range or continental collision?

answers: NDQ_003378

answers: what is the last word in the passage?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What type of force applied to rock is a stress?

answers: NDQ_003381

answers: What happened to the Ordovician rocks?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of cleavage development?

answers: NDQ_003384

answers: Which of the following is not a type of fold that arches upward?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: What is the cause of active arc volcanism?

answers: NDQ_003387

answers: Which of the following is not a type of normal fault: folding, thrusting or cleavage?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip, thrust, or cleavage?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: cleavage

answers: NDQ_003391

answers: subduction

answers: NDQ_003392

answers: thrusting

answers: NDQ_003393

answers: Ordovician rocks

answers: NDQ_003394

answers: southerly

answers: NDQ_003395

answers: cleavage development

answers: NDQ_003396

answers: Devonian

answers: NDQ_003351

answers: thrusting

answers: NDQ_003352

answers: folding, thrusting and cleavage development.

answers: NDQ_003353

answers: folding, thrusting and cleavage development.

answers: NDQ_003354

answers: Borrowdale Volcanic Group

answers: NDQ_003355

answers: thrusting

answers: NDQ_003356

answers: folding, thrusting and cleavage development.

answers: NDQ_003357

answers: subduction

answers: NDQ_003358

answers: shallow marine Dent Group.

answers: NDQ_003359

answers: collision

answers: NDQ_003360

answers: arc volcanism,

answers: NDQ_003362

answers: now vanished Iapetus Ocean.

answers: NDQ_003363

answers: island arc,

answers: NDQ_003371

answers: thrusting

answers: NDQ_003373

answers: deformation

answers: NDQ_003376

answers: southerly subduction

answers: NDQ_003378

answers: active arc volcanism,

answers: NDQ_003379

answers: Avalonia microcontinent with the continent of Laurentia.

answers: NDQ_003380

answers: deformation

answers: NDQ_003381

answers: folding, thrusting and cleavage development.

answers: NDQ_003382

answers: folding, thrusting

answers: NDQ_003383

answers: cleavage

answers: NDQ_003384

answers: island arc,

answers: NDQ_003385

answers: island arc,

answers: NDQ_003386

answers: deformation

answers: NDQ_003387

answers: subduction

answers: NDQ_003388

answers: Avalonia microcontinent with the continent of Laurentia.

answers: NDQ_003389

answers: folding,

answers: NDQ_003390

answers: Borrowdale Volcanic Group

answers: NDQ_003391

answers: Borrowdale Volcanic Group

answers: NDQ_003392

answers: thrusting and cleavage

answers: NDQ_003393

answers: Dent Group.

answers: NDQ_003394

answers: southerly subduction

answers: NDQ_003395

answers: Borrowdale Volcanic Group

answers: NDQ_003396

answers: southerly subduction

text: The town is adjacent to the San Andreas Fault.

text: The town is adjacent to the

text: San Andreas Fault

answers: NDQ_003351

answers: lateral

answers: NDQ_003352

answers: is likely to crack

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: swell

answers: NDQ_003357

answers: San Andreas Fault is a type of

answers: NDQ_003358

answers: Fault

answers: NDQ_003359

answers: is pushed together

answers: NDQ_003360

answers: faults

answers: NDQ_003362

answers: The San Andreas Fault is located in the Pacific Ocean.

answers: NDQ_003363

answers: San Andreas Fault

answers: NDQ_003371

answers: Which of the following is not a type of fault?

answers: NDQ_003373

answers: If the town is adjacent to the San Andreas Fault, then the rock is

answers: NDQ_003376

answers: The San Andreas Fault

answers: NDQ_003378

answers: The San Andreas Fault is a fault.

answers: NDQ_003379

answers: The dip of the fault plane is horizontal.

answers: NDQ_003380

answers: How would you describe the town?

answers: NDQ_003381

answers: What will happen to the town?

answers: NDQ_003382

answers: None of the above choices.

answers: NDQ_003383

answers: None of the above choices.

answers: NDQ_003384

answers: The San Andreas Fault is a

answers: NDQ_003385

answers: What is the San Andreas Fault?

answers: NDQ_003386

answers: (iii).

answers: NDQ_003387

answers: How would you describe the San Andreas Fault?

answers: NDQ_003388

answers: How would you describe the San Andreas Fault?

answers: NDQ_003389

answers: None of the above choices .

answers: NDQ_003390

answers: San Andreas Fault

answers: NDQ_003391

answers: is a town

answers: NDQ_003392

answers: San Andreas Fault

answers: NDQ_003393

answers: is a town

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: san andreas

answers: NDQ_003396

answers: horizontal fault

answers: NDQ_003351

answers: San Andreas Fault.

answers: NDQ_003352

answers: San Andreas Fault.

answers: NDQ_003353

answers: San Andreas Fault.

answers: NDQ_003354

answers: The town is adjacent to the San Andreas Fault.

answers: NDQ_003355

answers: San Andreas Fault.

answers: NDQ_003356

answers: San Andreas Fault.

answers: NDQ_003357

answers: San Andreas Fault.

answers: NDQ_003358

answers: San Andreas Fault.

answers: NDQ_003359

answers: San Andreas Fault.

answers: NDQ_003360

answers: San Andreas Fault.

answers: NDQ_003362

answers: The town is adjacent to the San Andreas Fault.

answers: NDQ_003363

answers: San Andreas Fault.

answers: NDQ_003371

answers: San Andreas Fault.

answers: NDQ_003373

answers: The town is adjacent to the San Andreas Fault.

answers: NDQ_003376

answers: The town is adjacent to the San Andreas Fault.

answers: NDQ_003378

answers: San Andreas Fault.

answers: NDQ_003379

answers: San Andreas Fault.

answers: NDQ_003380

answers: San Andreas Fault.

answers: NDQ_003381

answers: The town is adjacent to the San Andreas Fault.

answers: NDQ_003382

answers: San Andreas Fault.

answers: NDQ_003383

answers: San Andreas Fault.

answers: NDQ_003384

answers: San Andreas Fault.

answers: NDQ_003385

answers: San Andreas Fault.

answers: NDQ_003386

answers: San Andreas Fault.

answers: NDQ_003387

answers: San Andreas Fault.

answers: NDQ_003388

answers: San Andreas Fault.

answers: NDQ_003389

answers: San Andreas Fault.

answers: NDQ_003390

answers: San Andreas Fault.

answers: NDQ_003391

answers: San Andreas Fault.

answers: NDQ_003392

answers: San Andreas Fault.

answers: NDQ_003393

answers: San Andreas Fault.

answers: NDQ_003394

answers: San Andreas Fault.

answers: NDQ_003395

answers: San Andreas Fault.

answers: NDQ_003396

answers: San Andreas Fault.

text: Due to the similarities between Earth and Venus, it is suggested that they have a similar lithospheric elastic thickness of ~30 km. East African Rift is the only rift that can be compared to Devana Chasma.  Both rifts have fault segments length around ~100 km, which makes them stronger than any extensional system on Earth. However, they differ in their half grabens, East African Rifts' half grabens are around 50 km wide while on Venus it is around 150 km. In East African Rift, the higher elastic thickness can explain the wide half grabens. However, on Venus the main force is the high shear stress due to the cold lithosphere, which require the faults to be stronger in order to move. As a result, it has a wider half grabens than the one on Earth. Studying and comparing these two rift systems help us to understand how volcanism and tectonic activities affected the development and formation of the Beta Regio region on Venus.

text: Due to the similarities between Earth and Venus, it is suggested that they have a similar lithospheric elastic thickness of ~30 km.

text: East African Rift

text: is the only rift that can be compared to Devana Chasma.  Both rifts have fault segments length around ~100 km, which makes them stronger than any extensional system on

text: Earth

text: . However, they differ in their

text: half grabens

text: East African Rift

text: s'

text: half grabens

text: are around 50 km wide while on

text: Venus

text: it is around 150 km. In

text: East African Rift

text: , the higher

text: elastic thickness

text: can explain the wide

text: half grabens

text: . However, on

text: Venus

text: the main force is the high

text: shear stress

text: due to the cold lithosphere, which require the faults to be stronger in order to move. As a result, it has a wider

text: half grabens

text: than the one on Earth. Studying and comparing these two rift systems help us to understand how volcanism and tectonic activities affected the development and formation of the

text: Beta Regio

text: region on

text: Venus

answers: NDQ_003351

answers: shear stress

answers: NDQ_003352

answers: is more likely to crack

answers: NDQ_003353

answers: shear

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: grabens

answers: NDQ_003356

answers: shear

answers: NDQ_003357

answers: Fault segments length around  100 km

answers: NDQ_003358

answers: grabens

answers: NDQ_003359

answers: shear stress

answers: NDQ_003360

answers: Earth

answers: NDQ_003362

answers: the San Andreas fault is stronger than any extensional system on Earth

answers: NDQ_003363

answers: East African Rift

answers: NDQ_003371

answers: What is the only rift that can be compared to Devana Chasma

answers: NDQ_003373

answers: The main force is the high shear stress

answers: NDQ_003376

answers: basin-and-range

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: How does East African Rift differ from Devana Chasma?

answers: NDQ_003382

answers: What is the most common stress at convergent plates

answers: NDQ_003383

answers: What is the reason for the wide half grabens on Venus?

answers: NDQ_003384

answers: What is the only rift that can be compared to Devana Chasma?

answers: NDQ_003385

answers: Fault zones are areas where faults are clustered

answers: NDQ_003386

answers: Volcanism and tectonic activities

answers: NDQ_003387

answers: Which is not the reason for the wide half grabens on Venus?

answers: NDQ_003388

answers: Why does Venus have a wider half grabens than Earth?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: grabens

answers: NDQ_003391

answers: graben

answers: NDQ_003392

answers: extensional system

answers: NDQ_003393

answers: graben

answers: NDQ_003394

answers: East African Rift

answers: NDQ_003395

answers: East African Rift

answers: NDQ_003396

answers: East African Rift

answers: NDQ_003351

answers: shear stress

answers: NDQ_003352

answers: cold lithosphere,

answers: NDQ_003353

answers: faults to be stronger in order to move.

answers: NDQ_003354

answers: East African Rift

answers: NDQ_003355

answers: half grabens,

answers: NDQ_003356

answers: high shear stress

answers: NDQ_003357

answers: fault segments length around <unk>100 km,

answers: NDQ_003358

answers: rift that can be compared to Devana Chasma.

answers: NDQ_003359

answers: high shear stress

answers: NDQ_003360

answers: Venus.

answers: NDQ_003362

answers: stronger than any extensional system

answers: NDQ_003363

answers: volcanism

answers: NDQ_003371

answers: East African Rift

answers: NDQ_003373

answers: cold lithosphere,

answers: NDQ_003376

answers: high shear stress

answers: NDQ_003378

answers: shear stress

answers: NDQ_003379

answers: 50 km wide while on Venus

answers: NDQ_003380

answers: shear stress

answers: NDQ_003381

answers: high shear stress

answers: NDQ_003382

answers: shear stress

answers: NDQ_003383

answers: high shear stress

answers: NDQ_003384

answers: East African Rift

answers: NDQ_003385

answers: fault segments

answers: NDQ_003386

answers: high shear stress

answers: NDQ_003387

answers: shear stress

answers: NDQ_003388

answers: Venus

answers: NDQ_003389

answers: East African Rift

answers: NDQ_003390

answers: Devana Chasma.

answers: NDQ_003391

answers: half grabens,

answers: NDQ_003392

answers: Devana Chasma.

answers: NDQ_003393

answers: half grabens,

answers: NDQ_003394

answers: East African Rift

answers: NDQ_003395

answers: Devana Chasma.

answers: NDQ_003396

answers: Devana Chasma.

text: Porphyry copper deposits represent an important resource and the dominant source of copper that is mined today to satisfy global demand. Via compilation of geological data, it has been found that the majority of porphyry deposits are Phanerozoic in age and were emplaced at depths of approximately 1 to 6 kilometres with vertical thicknesses on average of 2 kilometres. Throughout the Phanerozoic an estimated 125,895 porphyry copper deposits were formed; however, 62% of them (78,106) have been removed by uplift and erosion. Thus, 38% (47,789) remain in the crust, of which there are 574 known deposits that are at the surface. It is estimated that the Earth’s porphyry copper deposits contain approximately 1.7×10 tonnes of copper.

text: Porphyry copper deposits represent an important resource and the dominant source of copper that is mined today to satisfy global demand. Via compilation of geological data, it has been found that the majority of porphyry deposits are

text: Phanerozoic

text: in age and were emplaced at depths of approximately 1 to 6 kilometres with vertical thicknesses on average of 2 kilometres. Throughout the Phanerozoic an estimated 125,895 porphyry copper deposits were formed; however, 62% of them (78,106) have been removed by uplift and erosion. Thus, 38% (47,789) remain in the crust, of which there are 574 known deposits that are at the surface. It is estimated that the Earth’s porphyry copper deposits contain approximately 1.7×10 tonnes of copper.

answers: NDQ_003351

answers: uplift

answers: NDQ_003352

answers: uplifts

answers: NDQ_003353

answers: erosion

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: uplift

answers: NDQ_003356

answers: erode

answers: NDQ_003357

answers: 38% (47,789) remain in the crust

answers: NDQ_003358

answers: unanswerable

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: 62% of them (78,106) have been removed by uplift and erosion

answers: NDQ_003363

answers: Phanerozoic

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: What is the main idea of the passage?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What type of force applied to rock is a stress?

answers: NDQ_003381

answers: What is the primary cause of rock deforms?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: movement of rock at faults

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: uplift and erosion

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip, uplift, or erosion?

answers: NDQ_003389

answers: geological

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: porphyry deposits

answers: NDQ_003392

answers: uplift and erosion

answers: NDQ_003393

answers: porphyry deposits

answers: NDQ_003394

answers: lateral

answers: NDQ_003395

answers: a vertical fault plane

answers: NDQ_003396

answers: vertical thicknesses

answers: NDQ_003351

answers: uplift and erosion.

answers: NDQ_003352

answers: uplift and erosion.

answers: NDQ_003353

answers: erosion.

answers: NDQ_003354

answers: 1 to 6 kilometres

answers: NDQ_003355

answers: erosion.

answers: NDQ_003356

answers: removed by uplift and erosion.

answers: NDQ_003357

answers: 2 kilometres.

answers: NDQ_003358

answers: erosion.

answers: NDQ_003359

answers: 1 to 6 kilometres

answers: NDQ_003360

answers: uplift

answers: NDQ_003362

answers: 62% of them (78,106) have been removed by uplift

answers: NDQ_003363

answers: depths of approximately 1 to 6 kilometres

answers: NDQ_003371

answers: 1 to 6 kilometres

answers: NDQ_003373

answers: vertical thicknesses on average of 2 kilometres.

answers: NDQ_003376

answers: uplift and erosion.

answers: NDQ_003378

answers: uplift and erosion.

answers: NDQ_003379

answers: vertical thicknesses on average of 2 kilometres.

answers: NDQ_003380

answers: uplift and erosion.

answers: NDQ_003381

answers: vertical thicknesses on average of 2 kilometres.

answers: NDQ_003382

answers: uplift and erosion.

answers: NDQ_003383

answers: erosion.

answers: NDQ_003384

answers: vertical thicknesses on average of 2 kilometres.

answers: NDQ_003385

answers: 1 to 6 kilometres

answers: NDQ_003386

answers: uplift

answers: NDQ_003387

answers: 1 to 6 kilometres

answers: NDQ_003388

answers: 1 to 6 kilometres

answers: NDQ_003389

answers: uplift and erosion.

answers: NDQ_003390

answers: vertical thicknesses on average of 2 kilometres.

answers: NDQ_003391

answers: Porphyry copper deposits

answers: NDQ_003392

answers: vertical thicknesses on average of 2 kilometres.

answers: NDQ_003393

answers: Porphyry copper deposits

answers: NDQ_003394

answers: 2 kilometres.

answers: NDQ_003395

answers: 2 kilometres.

answers: NDQ_003396

answers: vertical thicknesses on average of 2 kilometres.

text: A counter-intuitive method of reducing one of the worst types of stress concentrations, a crack, is to drill a large hole at the end of the crack.  The drilled hole, with its relatively large diameter, causes a smaller stress concentration than the sharp end of a crack.  This is however, a temporary solution that must be corrected at the first opportune time.

text: A counter-intuitive method of reducing one of the worst types of stress concentrations, a

text: crack

text: , is to

text: drill

text: a large hole at the end of the crack.  The drilled hole, with its relatively large

text: diameter

text: , causes a smaller stress concentration than the sharp end of a crack.  This is however, a temporary solution that must be corrected at the first opportune time.

answers: NDQ_003351

answers: crack

answers: NDQ_003352

answers: cracks

answers: NDQ_003353

answers: cracks

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: crack

answers: NDQ_003357

answers: the sharp end of a crack is more likely to be

answers: NDQ_003358

answers: crack

answers: NDQ_003359

answers: cracks

answers: NDQ_003360

answers: fault lines

answers: NDQ_003362

answers: Drill a large hole at the end of the crack.

answers: NDQ_003363

answers: the same time

answers: NDQ_003371

answers: Which of the following is not a type of stress concentration?

answers: NDQ_003373

answers: None of the above choices .

answers: NDQ_003376

answers: compressive forces

answers: NDQ_003378

answers: the sharp end of a crack

answers: NDQ_003379

answers: vertical

answers: NDQ_003380

answers: unanswerable

answers: NDQ_003381

answers: How does rock deform?

answers: NDQ_003382

answers: NDQ_003383

answers: no

answers: NDQ_003384

answers: what is the first type of stress concentrations

answers: NDQ_003385

answers: fault zone

answers: NDQ_003386

answers: faults

answers: NDQ_003387

answers: None of the above choices.

answers: NDQ_003388

answers: The drilled hole, with its relatively large diameter, causes a smaller stress concentration

answers: NDQ_003389

answers: mountains

answers: NDQ_003390

answers: a crack

answers: NDQ_003391

answers: is a crack

answers: NDQ_003392

answers: a crack

answers: NDQ_003393

answers: a crack

answers: NDQ_003394

answers: is a crack

answers: NDQ_003395

answers: is

answers: NDQ_003396

answers: a crack

answers: NDQ_003351

answers: crack,

answers: NDQ_003352

answers: crack,

answers: NDQ_003353

answers: crack,

answers: NDQ_003354

answers: A counter-intuitive

answers: NDQ_003355

answers: crack,

answers: NDQ_003356

answers: crack,

answers: NDQ_003357

answers: sharp end of a crack.

answers: NDQ_003358

answers: crack,

answers: NDQ_003359

answers: crack,

answers: NDQ_003360

answers: stress concentrations,

answers: NDQ_003362

answers: smaller stress concentration than the sharp end of a crack.

answers: NDQ_003363

answers: stress concentrations,

answers: NDQ_003371

answers: drilled hole,

answers: NDQ_003373

answers: drilled hole,

answers: NDQ_003376

answers: drilled hole,

answers: NDQ_003378

answers: crack,

answers: NDQ_003379

answers: drilled hole,

answers: NDQ_003380

answers: stress concentrations, a crack,

answers: NDQ_003381

answers: crack,

answers: NDQ_003382

answers: crack,

answers: NDQ_003383

answers: crack,

answers: NDQ_003384

answers: crack,

answers: NDQ_003385

answers: crack. The drilled hole,

answers: NDQ_003386

answers: stress concentrations,

answers: NDQ_003387

answers: crack,

answers: NDQ_003388

answers: crack,

answers: NDQ_003389

answers: A counter-intuitive

answers: NDQ_003390

answers: crack,

answers: NDQ_003391

answers: crack,

answers: NDQ_003392

answers: crack,

answers: NDQ_003393

answers: crack,

answers: NDQ_003394

answers: crack,

answers: NDQ_003395

answers: crack,

answers: NDQ_003396

answers: crack,

text: Many existing continental rift valleys are the result of a failed arm (aulacogen) of a triple junction, although there are two, the East African Rift and the Baikal Rift Zone, which are currently active, as well as a third which may be, the West Antarctic Rift.  In these instances, not only the crust, but also entire tectonic plates, are in the process of breaking apart to create new plates.  If they continue, continental rifts will eventually become oceanic rifts.

text: Many existing continental rift valleys are the result of a failed arm (

text: aulacogen

text: ) of a

text: triple junction

text: , although there are two, the

text: East African Rift

text: and the

text: Baikal Rift Zone

text: , which are currently active, as well as a third which may be, the

text: West Antarctic Rift

text: .  In these instances, not only the crust, but also entire

text: tectonic plate

text: s, are in the process of breaking apart to create new plates.  If they continue, continental rifts will eventually become oceanic rifts.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: breaks apart

answers: NDQ_003353

answers: fractures

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: rift valley

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: a failed arm (aulacogen) of a triple junction

answers: NDQ_003358

answers: valley

answers: NDQ_003359

answers: breaks apart

answers: NDQ_003360

answers: continental rifts

answers: NDQ_003362

answers: oceanic rifts will eventually become oceanic rifts

answers: NDQ_003363

answers: the West Antarctic Rift

answers: NDQ_003371

answers: What may be, the West Antarctic Rift?

answers: NDQ_003373

answers: How would you describe compressive stresses?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What is the third which may be, the West Antarctic Rift?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: What is the cause of earthquakes?

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: what is the third which may be, the West Antarctic Rift?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: aulacogen

answers: NDQ_003391

answers: unanswerable

answers: NDQ_003392

answers: aulacogen

answers: NDQ_003393

answers: unanswerable

answers: NDQ_003394

answers: aulacogen

answers: NDQ_003395

answers: unanswerable

answers: NDQ_003396

answers: aulacogen

answers: NDQ_003351

answers: (aulacogen)

answers: NDQ_003352

answers: breaking apart

answers: NDQ_003353

answers: breaking apart to create new plates.

answers: NDQ_003354

answers: Many existing continental rift valleys

answers: NDQ_003355

answers: (aulacogen)

answers: NDQ_003356

answers: breaking apart to create new plates.

answers: NDQ_003357

answers: triple junction,

answers: NDQ_003358

answers: rift valleys

answers: NDQ_003359

answers: breaking apart to create new plates.

answers: NDQ_003360

answers: tectonic plates,

answers: NDQ_003362

answers: currently active,

answers: NDQ_003363

answers: a failed arm (aulacogen) of a triple junction,

answers: NDQ_003371

answers: triple junction,

answers: NDQ_003373

answers: Many existing continental rift valleys

answers: NDQ_003376

answers: a failed arm (aulacogen) of a triple junction,

answers: NDQ_003378

answers: (aulacogen)

answers: NDQ_003379

answers: triple junction,

answers: NDQ_003380

answers: breaking apart to create new plates.

answers: NDQ_003381

answers: entire tectonic plates,

answers: NDQ_003382

answers: triple junction,

answers: NDQ_003383

answers: triple junction,

answers: NDQ_003384

answers: (aulacogen)

answers: NDQ_003385

answers: triple junction,

answers: NDQ_003386

answers: breaking apart to create new plates.

answers: NDQ_003387

answers: failed arm (aulacogen) of a triple junction,

answers: NDQ_003388

answers: a failed arm (aulacogen) of a triple junction,

answers: NDQ_003389

answers: plates.

answers: NDQ_003390

answers: (aulacogen)

answers: NDQ_003391

answers: (aulacogen)

answers: NDQ_003392

answers: (aulacogen)

answers: NDQ_003393

answers: (aulacogen)

answers: NDQ_003394

answers: triple junction,

answers: NDQ_003395

answers: triple junction,

answers: NDQ_003396

answers: (aulacogen)

text: The central segment of the San Andreas fault runs in a northwestern direction from Parkfield to Hollister. While the southern section of the fault and the parts through Parkfield experience earthquakes, the rest of the central section of the fault exhibits a phenomenon called aseismic creep, where the fault slips continuously without causing earthquakes.

text: The central segment of the San Andreas fault runs in a northwestern direction from Parkfield to

text: Hollister

text: . While the southern section of the fault and the parts through Parkfield experience earthquakes, the rest of the central section of the fault exhibits a phenomenon called

text: aseismic creep

text: , where the fault slips continuously without causing earthquakes.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: cracks

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fold that bends downward

answers: NDQ_003356

answers: crack

answers: NDQ_003357

answers: aseismic creep occurs when the fault slips without causing earthquakes

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: slips

answers: NDQ_003360

answers: San Andreas fault

answers: NDQ_003362

answers: the southern section of the fault and the parts through Parkfield experience earthquakes

answers: NDQ_003363

answers: San Andreas fault

answers: NDQ_003371

answers: Which of the following is not an example of a thrust fault?

answers: NDQ_003373

answers: what is the last word in the passage?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What does the central segment of the San Andreas fault exhibit?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not a type of fold?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: yes

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: San Andreas fault or aseismic creep?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip faults or aseismic creep?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: aseismic creep

answers: NDQ_003391

answers: aseismic creep

answers: NDQ_003392

answers: aseismic creep

answers: NDQ_003393

answers: aseismic creep

answers: NDQ_003394

answers: northwestern

answers: NDQ_003395

answers: San Andreas fault

answers: NDQ_003396

answers: San Andreas fault

answers: NDQ_003351

answers: earthquakes,

answers: NDQ_003352

answers: earthquakes,

answers: NDQ_003353

answers: earthquakes,

answers: NDQ_003354

answers: aseismic creep,

answers: NDQ_003355

answers: aseismic creep,

answers: NDQ_003356

answers: earthquakes,

answers: NDQ_003357

answers: earthquakes,

answers: NDQ_003358

answers: aseismic creep,

answers: NDQ_003359

answers: aseismic creep,

answers: NDQ_003360

answers: San Andreas fault

answers: NDQ_003362

answers: the southern section of the fault and the parts through Parkfield experience earthquakes,

answers: NDQ_003363

answers: San Andreas fault

answers: NDQ_003371

answers: aseismic creep,

answers: NDQ_003373

answers: aseismic creep,

answers: NDQ_003376

answers: aseismic creep,

answers: NDQ_003378

answers: aseismic creep,

answers: NDQ_003379

answers: aseismic creep,

answers: NDQ_003380

answers: earthquakes,

answers: NDQ_003381

answers: aseismic creep,

answers: NDQ_003382

answers: aseismic creep,

answers: NDQ_003383

answers: aseismic creep,

answers: NDQ_003384

answers: aseismic creep,

answers: NDQ_003385

answers: aseismic creep,

answers: NDQ_003386

answers: the fault slips continuously without causing earthquakes.

answers: NDQ_003387

answers: aseismic creep,

answers: NDQ_003388

answers: aseismic creep,

answers: NDQ_003389

answers: aseismic creep,

answers: NDQ_003390

answers: aseismic creep,

answers: NDQ_003391

answers: aseismic creep,

answers: NDQ_003392

answers: aseismic creep,

answers: NDQ_003393

answers: aseismic creep,

answers: NDQ_003394

answers: San Andreas fault

answers: NDQ_003395

answers: San Andreas fault

answers: NDQ_003396

answers: aseismic creep,

text: Georgescu argues that Daly's steady-state economy will provide no ecological salvation for mankind, especially not in the longer run. Due to the geologic fact that mineral ores are deposited and concentrated very unevenly in the crust of the Earth, exploration and extraction of mineral resources will sooner or later be faced with the principle of diminishing returns, whereby extraction activities are pushed to still less accessible sites and still lower grades of ores. In the course of time, then, extraction costs and market prices of the incremental amount of resources will tend to increase. Eventually, all minerals will be exhausted, but the economic exhaustion will manifest itself long before the physical exhaustion provides the ultimate backstop for further activity: There will still be deposits of resources left in the crust, but the geologic concentration of these deposits will remain below the critical cutoff grade; hence, continued extraction will no longer pay off, and the market for these resources will then collapse. This long-term dynamics works itself through any economic (sub-)system, regardless of the system's geographical location, its size and its state of development (whether a progressive, a steady or a declining state). In effect, the arguments advanced by Daly in support of his steady-state economy apply with even greater force in support of a declining-state economy, Georgescu points out: When the overall purpose is to ration and stretch mineral resource use for as long time into the future as possible, zero economic growth is more desirable than growth is, true; but negative growth is better still! In this context, Georgescu also criticises Daly for not specifying at what levels man-made capital and human population are to be kept constant in the steady-state.

text: Georgescu argues that Daly's steady-state economy will provide no ecological salvation for mankind, especially not in the longer run. Due to the geologic fact that

text: mineral ores are deposited and concentrated very unevenly in the crust of the Earth

text: exploration and extraction of mineral resources

text: will sooner or later be faced with the principle of

text: diminishing returns

text: , whereby extraction activities are pushed to

text: still less accessible sites and still lower grades of ores

text: . In the course of time, then, extraction costs and market prices of the incremental amount of resources will tend to increase. Eventually, all minerals will be exhausted, but the economic exhaustion will manifest itself long before the physical exhaustion provides the ultimate backstop for further activity: There will still be deposits of resources left in the crust, but the geologic concentration of these deposits will remain below the critical

text: cutoff grade

text: ; hence, continued extraction will no longer pay off, and the market for these resources will then collapse. This long-term dynamics works itself through any economic (sub-)system, regardless of the system's geographical location, its size and its state of development (whether a progressive, a steady or a declining state). In effect, the arguments advanced by Daly in support of his steady-state economy apply with even greater force in support of a declining-state economy, Georgescu points out: When the overall purpose is to ration and stretch mineral resource use for as long time into the future as possible, zero economic growth is more desirable than growth is, true; but negative growth is better still! In this context, Georgescu also criticises Daly for not specifying at what levels man-made capital and human population are to be kept constant in the steady-state.

answers: NDQ_003351

answers: negative growth

answers: NDQ_003352

answers: decreases in size

answers: NDQ_003353

answers: igneous rocks to form

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: negative growth

answers: NDQ_003356

answers: diminishing returns

answers: NDQ_003357

answers: the market for these resources will then collapse

answers: NDQ_003358

answers: steady-state

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: zero economic growth is more desirable than growth is

answers: NDQ_003363

answers: the same time

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: due to the geologic fact that mineral ores are deposited

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: vertical

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What will still be deposits of resources left in the crust

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: geologic

answers: NDQ_003386

answers: geologic

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: unanswerable

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: critical cutoff grade

answers: NDQ_003391

answers: critical cutoff grade

answers: NDQ_003392

answers: critical cutoff grade

answers: NDQ_003393

answers: critical cutoff grade

answers: NDQ_003394

answers: undefined

answers: NDQ_003395

answers: a vertical fault plane

answers: NDQ_003396

answers: negative growth

answers: NDQ_003351

answers: principle of diminishing returns,

answers: NDQ_003352

answers: diminishing returns,

answers: NDQ_003353

answers: geologic concentration of these deposits will remain below the critical cutoff grade;

answers: NDQ_003354

answers: its size and its state of development

answers: NDQ_003355

answers: negative growth

answers: NDQ_003356

answers: increase.

answers: NDQ_003357

answers: zero economic growth is more desirable than growth is, true; but negative growth

answers: NDQ_003358

answers: declining-state economy,

answers: NDQ_003359

answers: deposited and concentrated very unevenly in the crust of the Earth,

answers: NDQ_003360

answers: zero economic growth

answers: NDQ_003362

answers: zero economic growth is more desirable than growth

answers: NDQ_003363

answers: crust of the Earth,

answers: NDQ_003371

answers: steady-state

answers: NDQ_003373

answers: mineral ores are deposited and concentrated very unevenly in the crust

answers: NDQ_003376

answers: steady-state

answers: NDQ_003378

answers: negative growth

answers: NDQ_003379

answers: zero economic growth

answers: NDQ_003380

answers: negative growth

answers: NDQ_003381

answers: zero economic growth is more desirable than growth is, true; but negative growth

answers: NDQ_003382

answers: zero economic growth is more desirable than growth is, true; but negative growth

answers: NDQ_003383

answers: mineral ores are deposited and concentrated very unevenly

answers: NDQ_003384

answers: negative growth

answers: NDQ_003385

answers: declining-state economy,

answers: NDQ_003386

answers: mineral ores are deposited and concentrated very unevenly

answers: NDQ_003387

answers: deposited and concentrated very unevenly in the crust of the Earth,

answers: NDQ_003388

answers: zero economic growth is more desirable than growth is, true; but negative growth

answers: NDQ_003389

answers: deposited and concentrated very unevenly in the crust of the Earth,

answers: NDQ_003390

answers: negative growth

answers: NDQ_003391

answers: critical cutoff grade;

answers: NDQ_003392

answers: progressive, a steady or a declining state).

answers: NDQ_003393

answers: critical cutoff grade;

answers: NDQ_003394

answers: negative growth

answers: NDQ_003395

answers: negative growth

answers: NDQ_003396

answers: negative growth

text: The St. Elias Mountains is the highest coastal mountain range on Earth. It formed due to the subduction of the Yakutat plate underneath the North American plate. The Yakutat microplate is a wedge shaped oceanic plateau with 20–30 km thickness. Similar to the adjacent Pacific plate (7 km crustal thickness) the Yakutat plate is currently moving northwestward with a rate of ~50 mm/year with respect to stable North America. The Yakutat plate is transported northwards along the active Fairweather Fault, which probably started more than 35 million years ago. Due to its thickness the Yakutat plate is buoyant resulting in surface uplift of the overriding North American plate, which formed the Talkeetna Mountains and the Alaska Range in southcentral Alaska located above the subducted part of the Yakutat plate. The St. Elias Mountains formed at the plate boundary between the Yakutat and North American plate. The up to 12 km thick sediments that have been deposited on top of the Yakutat plate are imbricated and deformed as they became scraped off and compose today the southern (coastal) flanks of the St. Elias Mountains. In contrast the high elevated regions of the drainage divide (Bagley Ice Field, Seward Glacier) and north of it comprise rocks that are part of the North American plate.The highest peaks of the St. Elias Mountains are located in the high ice field region of the Kluane National Park (Mt. Logan, Mt. Vancouver) and north of the Malaspina Glacier (Mt. St. Elias, Mt. Cook), in the region known as the St. Elias syntaxis. At the syntaxis region the tectonic style changes from strike-slip motion along the Fairweather Fault to collision west of Malaspina. This tectonic transition concentrates stress in the crust at the syntaxis that together with efficient glacial erosion results in positive feedback processes that through time forms extreme high mountain peaks and local relief, and rapid exhumation of rocks from up to 10 km depths to the surface.

answers: NDQ_003351

answers: strike-slip motion

answers: NDQ_003352

answers: increases in thickness

answers: NDQ_003353

answers: positive feedback processes

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: syntactic

answers: NDQ_003356

answers: exhume from what depths?

answers: NDQ_003357

answers: How many kilometers thick is the Yakutat plate?

answers: NDQ_003358

answers: unanswerable

answers: NDQ_003359

answers: subducts

answers: NDQ_003360

answers: Yakutat plate

answers: NDQ_003362

answers: The St. Elias Mountains formed at the plate boundary between the Yakutat and North American plate

answers: NDQ_003363

answers: Yakutat

answers: NDQ_003371

answers: What type of fault is the Fairweather Fault?

answers: NDQ_003373

answers: Why is the St. Elias Mountains highest coastal mountain range on Earth?

answers: NDQ_003376

answers: Which of the following is not caused by compressive forces: basin-and-range or glacial erosion?

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What is the highest coastal mountain range on Earth?

answers: NDQ_003381

answers: What happens to rocks from up to 10 km depths to the surface?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not a type of fold: St. Elias syntaxis or Malaspina Glacier?

answers: NDQ_003385

answers: What is the region known as the St. Elias syntaxis?

answers: NDQ_003386

answers: What type of movement is the Fairweather Fault?

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: strike-slip motion along the Fairweather Fault to collision

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip motion, collision, or shear stress?

answers: NDQ_003389

answers: What is the highest coastal mountain range on Earth?

answers: NDQ_003390

answers: Fairweather Fault

answers: NDQ_003391

answers: Yakutat plate

answers: NDQ_003392

answers: Fairweather Fault

answers: NDQ_003393

answers: The St. Elias Mountains

answers: NDQ_003394

answers: Fairweather Fault

answers: NDQ_003395

answers: Fairweather Fault

answers: NDQ_003396

answers: Fairweather Fault

answers: NDQ_003351

answers: strike-slip motion

answers: NDQ_003352

answers: deformed

answers: NDQ_003353

answers: positive feedback processes

answers: NDQ_003354

answers: Yakutat plate

answers: NDQ_003355

answers: drainage divide

answers: NDQ_003356

answers: scraped off

answers: NDQ_003357

answers: strike-slip

answers: NDQ_003358

answers: strike-slip motion along the Fairweather Fault

answers: NDQ_003359

answers: Fairweather Fault,

answers: NDQ_003360

answers: Yakutat plate

answers: NDQ_003362

answers: cated and deformed

answers: NDQ_003363

answers: plate boundary between the Yakutat and North American plate.

answers: NDQ_003371

answers: Fairweather Fault

answers: NDQ_003373

answers: imbricated and deformed

answers: NDQ_003376

answers: North American plate.The

answers: NDQ_003378

answers: strike-slip

answers: NDQ_003379

answers: strike-slip motion along the Fairweather Fault

answers: NDQ_003380

answers: stress

answers: NDQ_003381

answers: bricated

answers: NDQ_003382

answers: rocks

answers: NDQ_003383

answers: deformed

answers: NDQ_003384

answers: St. Elias syntaxis.

answers: NDQ_003385

answers: St. Elias syntaxis.

answers: NDQ_003386

answers: strike-slip

answers: NDQ_003387

answers: strike-slip motion along the Fairweather Fault

answers: NDQ_003388

answers: strike-slip motion along the Fairweather Fault

answers: NDQ_003389

answers: subduction

answers: NDQ_003390

answers: Fairweather Fault

answers: NDQ_003391

answers: Yakutat plate

answers: NDQ_003392

answers: Fairweather Fault

answers: NDQ_003393

answers: drainage divide

answers: NDQ_003394

answers: Fairweather Fault

answers: NDQ_003395

answers: Fairweather Fault,

answers: NDQ_003396

answers: Fairweather Fault,

text: A number of mechanisms have been proposed to interpret the origin of volcanism in the NCVP. This includes slab windows, mantle plumes, crustal extension and deglaciation. The most common and best mechanism used to explain NCVP volcanic activity is incipient rifting of the North American Plate caused by crustal extension. As the continental crust stretches, the near surface rocks fracture along steeply dipping cracks parallel to the rift known as faults. Mafic magma rises along these fractures to create passive lava flows, although more viscous felsic magma also makes its way to the surface and can produce explosive eruptions. Two major structural features, the Tintina and Denali-Coast fault systems, run parallel with the NCVP. Both structures have had strike-slip motions since the Cretaceous period and has resulted in several hundred kilometres of crustal displacement.<ref name="SL">{{cite journal|title=Distribution, nature, and origin of Neogene–Quaternary magmatism in the northern Cordilleran volcanic province, Canada|last=Edwards|first=Benjamin R.|last2=Russell|first2=James K.|journal=Geological Society of America Bulletin|publisher=Geological Society of America|pages=1280, 1281, 1283, 1284, 1286, 1291|volume=112|issue=8|year=2000|issn=0016-7606|doi=10.1130/0016-7606(2000)112

text: A number of mechanisms have been proposed to interpret the origin of volcanism in the NCVP. This includes

text: slab window

text: s,

text: mantle plume

text: s,

text: crustal

text: extension and

text: deglaciation

text: . The most common and best mechanism used to explain NCVP volcanic activity is incipient

text: rift

text: ing of the

text: North American Plate

text: caused by crustal extension. As the

text: continental crust

text: stretches, the near surface rocks fracture along steeply dipping cracks parallel to the rift known as

text: faults

text: Mafic

text: magma rises along these fractures to create passive lava flows, although more viscous

text: felsic

text: magma also makes its way to the surface and can produce explosive eruptions. Two major structural features, the

text: Tintina

text: and

text: Denali

text: -Coast fault systems, run parallel with the NCVP. Both structures have had

text: strike-slip

text: motions since the

text: Cretaceous

text: period

text: and has resulted in several hundred kilometres of crustal displacement.<ref name="SL">{{cite journal|title=Distribution, nature, and origin of Neogene–Quaternary magmatism in the northern Cordilleran volcanic province, Canada|last=Edwards|first=Benjamin R.|last2=Russell|first2=James K.|journal=

text: Geological Society of America Bulletin

text: |publisher=

text: Geological Society of America

text: |pages=1280, 1281, 1283, 1284, 1286, 1291|volume=112|issue=8|year=2000|issn=0016-7606|doi=10.1130/0016-7606(2000)112

answers: NDQ_003351

answers: strike-slip

answers: NDQ_003352

answers: fractures

answers: NDQ_003353

answers: cracks

answers: NDQ_003354

answers: Toroweap Formation is a formation

answers: NDQ_003355

answers: fault

answers: NDQ_003356

answers: crack

answers: NDQ_003357

answers: Mafic magma rises along these cracks to create passive lava flows

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: stretches

answers: NDQ_003360

answers: North American Plate

answers: NDQ_003362

answers: The most common and best mechanism used to explain NCVP volcanic activity

answers: NDQ_003363

answers: the Cretaceous

answers: NDQ_003371

answers: What is the most common and best mechanism used to explain NCVP volcanic activity?

answers: NDQ_003373

answers: What is the most common and best mechanism used to explain NCVP volcanic activity?

answers: NDQ_003376

answers: The terrain known as basin-and-range is caused by compressive forces.

answers: NDQ_003378

answers: What is the difference between strike and slip?

answers: NDQ_003379

answers: yes

answers: NDQ_003380

answers: Which of the following is not an example of a stress?

answers: NDQ_003381

answers: What is the most common and best mechanism used to explain NCVP volcanic activity?

answers: NDQ_003382

answers: The most common stress at convergent plates is compression

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: as the continental crust stretches

answers: NDQ_003387

answers: no

answers: NDQ_003388

answers: It's impossible to say

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: deglaciation

answers: NDQ_003391

answers: rift

answers: NDQ_003392

answers: denali-coast fault

answers: NDQ_003393

answers: surface rocks

answers: NDQ_003394

answers: steeply dipping cracks

answers: NDQ_003395

answers: Denali-Coast

answers: NDQ_003396

answers: Denali-Coast

answers: NDQ_003351

answers: crustal extension.

answers: NDQ_003352

answers: fracture along steeply dipping cracks

answers: NDQ_003353

answers: faults.

answers: NDQ_003354

answers: K.|journal=Geological Society of America Bulletin|publisher=Geological

answers: NDQ_003355

answers: faults.

answers: NDQ_003356

answers: Mafic magma

answers: NDQ_003357

answers: steeply dipping cracks

answers: NDQ_003358

answers: faults.

answers: NDQ_003359

answers: As the continental crust stretches,

answers: NDQ_003360

answers: ogene–Quaternary magmatism

answers: NDQ_003362

answers: explosive eruptions.

answers: NDQ_003363

answers: northern Cordilleran volcanic province,

answers: NDQ_003371

answers: faults.

answers: NDQ_003373

answers: faults.

answers: NDQ_003376

answers: faults.

answers: NDQ_003378

answers: strike-slip

answers: NDQ_003379

answers: steeply dipping

answers: NDQ_003380

answers: faults.

answers: NDQ_003381

answers: faults.

answers: NDQ_003382

answers: crustal extension.

answers: NDQ_003383

answers: faults.

answers: NDQ_003384

answers: faults.

answers: NDQ_003385

answers: steeply dipping cracks parallel to the rift known as faults.

answers: NDQ_003386

answers: the near surface rocks fracture along steeply dipping cracks

answers: NDQ_003387

answers: faults.

answers: NDQ_003388

answers: Tintina and Denali-Coast fault systems,

answers: NDQ_003389

answers: crustal extension.

answers: NDQ_003390

answers: Denali-Coast fault systems,

answers: NDQ_003391

answers: near surface rocks

answers: NDQ_003392

answers: Tintina and Denali-Coast fault systems,

answers: NDQ_003393

answers: near surface rocks

answers: NDQ_003394

answers: steeply dipping cracks

answers: NDQ_003395

answers: steeply dipping cracks parallel to the rift known as faults.

answers: NDQ_003396

answers: faults.

text: A paper written by Gerya theorizes that the creation of the transform faults between the ridges of the mid-oceanic ridge is attributed to rotated and stretched sections of the mid-oceanic ridge. This occurs over a long period of time with the spreading center or ridge slowly deforming from a straight line to a curved line. Finally, fracturing along these planes forms transform faults. As this takes place, the fault changes from a normal fault with extensional stress to a strike slip fault with lateral stress. In the study done by Bonatti & Crane, peridotite and gabbro rocks were discovered in the edges of the transform ridges.  These rocks are created deep inside the Earth’s mantle and then rapidly exhumed to the surface.  This evidence helps to prove that new seafloor is being created at the mid-oceanic ridges and further supports the theory of plate tectonics.

text: A paper written by Gerya theorizes that the creation of the transform faults between the ridges of the mid-oceanic ridge is attributed to rotated and stretched sections of the mid-oceanic ridge. This occurs over a long period of time with the spreading center or ridge slowly deforming from a straight line to a curved line. Finally, fracturing along these planes forms transform faults. As this takes place, the fault changes from a normal fault with extensional stress to a strike slip fault with lateral stress. In the study done by Bonatti & Crane,

text: peridotite

text: and

text: gabbro

text: rocks were discovered in the edges of the transform ridges.  These rocks are created deep inside the Earth’s mantle and then rapidly exhumed to the surface.  This evidence helps to prove that new seafloor is being created at the mid-oceanic ridges and further supports the theory of plate tectonics.

answers: NDQ_003351

answers: lateral stress

answers: NDQ_003352

answers: is more likely to crack

answers: NDQ_003353

answers: lateral stress

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: strike slip fault

answers: NDQ_003356

answers: form transform faults

answers: NDQ_003357

answers: extensional stress is

answers: NDQ_003358

answers: normal fault

answers: NDQ_003359

answers: deforms

answers: NDQ_003360

answers: plate faults

answers: NDQ_003362

answers: peridotite and gabbro rocks were discovered in the edges of the transform ridges

answers: NDQ_003363

answers: plate tectonics

answers: NDQ_003371

answers: Which of the following is not a type of strike slip fault?

answers: NDQ_003373

answers: Which of the following is not a type of stress?

answers: NDQ_003376

answers: Which of the following is not a type of terrain: basin-and-range or plate tectonics?

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: Which of the following is not a type of stress: extensional stress, strike slip stress, or lateral stress?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not a type of fold that arches upward?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: Why do earthquakes occur?

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: normal faults or strike slip faults?

answers: NDQ_003388

answers: Which of the following is not a type of strike-slip fault?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: strike slip fault

answers: NDQ_003391

answers: strike slip fault

answers: NDQ_003392

answers: strike slip fault

answers: NDQ_003393

answers: strike slip fault

answers: NDQ_003394

answers: strike slip fault

answers: NDQ_003395

answers: strike slip fault

answers: NDQ_003396

answers: strike slip fault

answers: NDQ_003351

answers: extensional

answers: NDQ_003352

answers: lateral stress.

answers: NDQ_003353

answers: fracturing

answers: NDQ_003354

answers: curved line.

answers: NDQ_003355

answers: strike slip fault

answers: NDQ_003356

answers: fracturing along these planes forms transform faults.

answers: NDQ_003357

answers: extensional stress

answers: NDQ_003358

answers: strike slip fault

answers: NDQ_003359

answers: fracturing along these planes

answers: NDQ_003360

answers: plate tectonics.

answers: NDQ_003362

answers: rotated and stretched sections of the mid-oceanic ridge.

answers: NDQ_003363

answers: mid-oceanic ridge

answers: NDQ_003371

answers: strike slip fault with lateral stress.

answers: NDQ_003373

answers: deep inside the Earth’s mantle

answers: NDQ_003376

answers: extensional stress to a strike slip fault with lateral stress.

answers: NDQ_003378

answers: strike slip fault with lateral stress.

answers: NDQ_003379

answers: lateral stress.

answers: NDQ_003380

answers: extensional stress

answers: NDQ_003381

answers: extensional stress to a strike slip fault with lateral stress.

answers: NDQ_003382

answers: extensional stress to a strike slip fault with lateral stress.

answers: NDQ_003383

answers: lateral stress.

answers: NDQ_003384

answers: curved line.

answers: NDQ_003385

answers: transform faults

answers: NDQ_003386

answers: fracturing

answers: NDQ_003387

answers: extensional stress

answers: NDQ_003388

answers: lateral stress.

answers: NDQ_003389

answers: fracturing along these planes forms transform faults.

answers: NDQ_003390

answers: strike slip fault

answers: NDQ_003391

answers: gabbro

answers: NDQ_003392

answers: strike slip fault

answers: NDQ_003393

answers: strike slip fault with lateral stress.

answers: NDQ_003394

answers: strike slip fault with lateral stress.

answers: NDQ_003395

answers: strike slip fault with lateral stress.

answers: NDQ_003396

answers: strike slip fault

text: The Cascadia subduction zone runs from triple junctions at its north and south ends.  To the north, just below Haida Gwaii, it intersects the Queen Charlotte Fault and the Explorer Ridge.  To the south, just off of Cape Mendocino in California, it intersects the San Andreas Fault and the Mendocino Fracture Zone at the Mendocino Triple Junction.

text: The Cascadia subduction zone runs from

text: triple junction

text: s at its north and south ends.  To the north, just below

text: Haida Gwaii

text: , it intersects the

text: Queen Charlotte Fault

text: and the

text: Explorer Ridge

text: .  To the south, just off of Cape Mendocino in California, it intersects the

text: San Andreas Fault

text: and the

text: Mendocino Fracture Zone

text: at the

text: Mendocino Triple Junction

answers: NDQ_003351

answers: San Andreas Fault

answers: NDQ_003352

answers: fractures

answers: NDQ_003353

answers: Fracture

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: subduction zone

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: San Andreas Fault intersects which fault?

answers: NDQ_003358

answers: ridge

answers: NDQ_003359

answers: intersects the fault

answers: NDQ_003360

answers: San Andreas fault

answers: NDQ_003362

answers: it intersects the Queen Charlotte Fault and the Explorer Ridge

answers: NDQ_003363

answers: Cascadia subduction zone

answers: NDQ_003371

answers: Which of the following is not a fault: the Queen Charlotte Fault, the Explorer Ridge, or the San Andreas Fault?

answers: NDQ_003373

answers: Why would a rock be deeply buried?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: what is the second to last place mentioned?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What type of stress does the Cascadia subduction zone experience?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: What type of fold is the Cascadia subduction zone?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: What is the cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not a normal fault: the San Andreas Fault or the Mendocino Fracture Zone?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip or strike-slip fault?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: San Andreas Fault

answers: NDQ_003391

answers: subduction zone

answers: NDQ_003392

answers: San Andreas Fault

answers: NDQ_003393

answers: Explorer Ridge

answers: NDQ_003394

answers: San Andreas Fault

answers: NDQ_003395

answers: San Andreas Fault

answers: NDQ_003396

answers: San Andreas Fault

answers: NDQ_003351

answers: San Andreas Fault and the Mendocino Fracture Zone

answers: NDQ_003352

answers: Mendocino Fracture Zone

answers: NDQ_003353

answers: Queen Charlotte Fault

answers: NDQ_003354

answers: Haida Gwaii,

answers: NDQ_003355

answers: subduction zone

answers: NDQ_003356

answers: Mendocino Fracture Zone

answers: NDQ_003357

answers: San Andreas Fault

answers: NDQ_003358

answers: Fracture Zone

answers: NDQ_003359

answers: Queen Charlotte Fault

answers: NDQ_003360

answers: The Cascadia subduction zone

answers: NDQ_003362

answers: Queen Charlotte Fault

answers: NDQ_003363

answers: Cascadia subduction zone

answers: NDQ_003371

answers: Queen Charlotte Fault

answers: NDQ_003373

answers: The Cascadia subduction zone

answers: NDQ_003376

answers: The Cascadia subduction zone

answers: NDQ_003378

answers: The Cascadia subduction zone

answers: NDQ_003379

answers: Queen Charlotte Fault

answers: NDQ_003380

answers: Queen Charlotte Fault

answers: NDQ_003381

answers: Queen Charlotte Fault

answers: NDQ_003382

answers: San Andreas Fault

answers: NDQ_003383

answers: triple junctions

answers: NDQ_003384

answers: Queen Charlotte Fault and the Explorer Ridge.

answers: NDQ_003385

answers: Queen Charlotte Fault

answers: NDQ_003386

answers: Queen Charlotte Fault

answers: NDQ_003387

answers: Queen Charlotte Fault

answers: NDQ_003388

answers: Queen Charlotte Fault

answers: NDQ_003389

answers: The Cascadia subduction

answers: NDQ_003390

answers: Queen Charlotte Fault

answers: NDQ_003391

answers: Explorer Ridge.

answers: NDQ_003392

answers: Queen Charlotte Fault

answers: NDQ_003393

answers: Explorer Ridge.

answers: NDQ_003394

answers: Queen Charlotte Fault

answers: NDQ_003395

answers: Queen Charlotte Fault

answers: NDQ_003396

answers: Queen Charlotte Fault

text: The game covers five different locations on Rifts Earth from the RPG sourcebooks:

text: The game covers five different locations on Rifts Earth from the RPG sourcebooks:

answers: NDQ_003351

answers: lateral

answers: NDQ_003352

answers: increases in size.

answers: NDQ_003353

answers: lava to form

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: Rifts Earth is surrounded by a void.

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: falls on it.

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: The San Andreas fault is located in the Pacific Ocean.

answers: NDQ_003363

answers: Rifts

answers: NDQ_003371

answers: a thrust fault may be in between

answers: NDQ_003373

answers: It is more likely to crack than to break apart.

answers: NDQ_003376

answers: compressive forces

answers: NDQ_003378

answers: The amount the ground moves in an earthquake is called slip.

answers: NDQ_003379

answers: The dip of the fault plane is

answers: NDQ_003380

answers: What is the best way to describe a stress?

answers: NDQ_003381

answers: It can be used as a weapon.

answers: NDQ_003382

answers: None of the above choices.

answers: NDQ_003383

answers: What is the best title for this passage?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: Faults are clustered where faults are

answers: NDQ_003386

answers: movement of rock

answers: NDQ_003387

answers: None of the above choices .

answers: NDQ_003388

answers: Strike-slip faults

answers: NDQ_003389

answers: mountain ranges

answers: NDQ_003390

answers: rift

answers: NDQ_003391

answers: rift zone

answers: NDQ_003392

answers: rift

answers: NDQ_003393

answers: A block of rock above a dip-slip fault

answers: NDQ_003394

answers: a fault with a fault plane

answers: NDQ_003395

answers: fault with a horizontal fault plane

answers: NDQ_003396

answers: Fault in which the fault plane is nearly horizontal

answers: NDQ_003351

answers: The game covers five different locations on Rifts Earth

answers: NDQ_003352

answers: five different locations on Rifts Earth

answers: NDQ_003353

answers: Rifts Earth

answers: NDQ_003354

answers: The game covers five different locations on Rifts Earth

answers: NDQ_003355

answers: Rifts Earth

answers: NDQ_003356

answers: Rifts Earth

answers: NDQ_003357

answers: five different locations on Rifts Earth

answers: NDQ_003358

answers: locations on Rifts

answers: NDQ_003359

answers: Rifts Earth

answers: NDQ_003360

answers: Rifts Earth

answers: NDQ_003362

answers: five different locations on Rifts Earth

answers: NDQ_003363

answers: Rifts

answers: NDQ_003371

answers: Rifts Earth

answers: NDQ_003373

answers: The game covers five different locations on Rifts Earth

answers: NDQ_003376

answers: The game covers five different locations on Rifts Earth

answers: NDQ_003378

answers: five different locations on Rifts Earth

answers: NDQ_003379

answers: five different locations on Rifts Earth

answers: NDQ_003380

answers: The game covers five different locations on Rifts Earth

answers: NDQ_003381

answers: five different locations on Rifts Earth

answers: NDQ_003382

answers: The game covers five different locations on Rifts Earth

answers: NDQ_003383

answers: The game covers five different locations on Rifts Earth

answers: NDQ_003384

answers: The game covers five different locations on Rifts Earth

answers: NDQ_003385

answers: Rifts Earth

answers: NDQ_003386

answers: Rifts Earth

answers: NDQ_003387

answers: The game covers five different locations on Rifts Earth

answers: NDQ_003388

answers: RPG sourcebooks:

answers: NDQ_003389

answers: The game covers five different locations on Rifts Earth

answers: NDQ_003390

answers: Rifts Earth

answers: NDQ_003391

answers: Rifts Earth

answers: NDQ_003392

answers: Rifts Earth

answers: NDQ_003393

answers: Rifts Earth

answers: NDQ_003394

answers: Rifts Earth

answers: NDQ_003395

answers: Rifts Earth

answers: NDQ_003396

answers: Rifts Earth

text: Tectonic lithosphere plates consist of lithospheric mantle overlain by either or both of two types of crustal material: oceanic crust (in older texts called sima from silicon and magnesium) and continental crust (sial from silicon and aluminium). Average oceanic lithosphere is typically  thick; its thickness is a function of its age: as time passes, it conductively cools and subjacent cooling mantle is added to its base. Because it is formed at mid-ocean ridges and spreads outwards, its thickness is therefore a function of its distance from the mid-ocean ridge where it was formed. For a typical distance that oceanic lithosphere must travel before being subducted, the thickness varies from about  thick at mid-ocean ridges to greater than  at subduction zones; for shorter or longer distances, the subduction zone (and therefore also the mean) thickness becomes smaller or larger, respectively. Continental lithosphere is typically ~200 km thick, though this varies considerably between basins, mountain ranges, and stable cratonic interiors of continents. The two types of crust also differ in thickness, with continental crust being considerably thicker than oceanic (35 km vs. 6 km).

text: Tectonic lithosphere plates consist of lithospheric mantle overlain by either or both of two types of crustal material:

text: oceanic crust

text: (in older texts called

text: sima

text: from

text: silicon

text: and

text: magnesium

text: ) and

text: continental crust

text: sial

text: from silicon and

text: aluminium

text: ). Average oceanic lithosphere is typically  thick; its thickness is a function of its age: as time passes, it conductively cools and subjacent cooling mantle is added to its base. Because it is formed at mid-ocean ridges and spreads outwards, its thickness is therefore a function of its distance from the mid-ocean ridge where it was formed. For a typical distance that oceanic lithosphere must travel before being subducted, the thickness varies from about  thick at mid-ocean ridges to greater than  at

text: subduction

text: zones; for shorter or longer distances, the subduction zone (and therefore also the mean) thickness becomes smaller or larger, respectively. Continental lithosphere is typically ~200 km thick, though this varies considerably between basins, mountain ranges, and stable

text: craton

text: ic interiors of continents. The two types of crust also differ in thickness, with continental crust being considerably thicker than oceanic (35 km vs. 6 km).

answers: NDQ_003351

answers: subduction

answers: NDQ_003352

answers: increases in thickness

answers: NDQ_003353

answers: subduction zones

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: ridge

answers: NDQ_003356

answers: subduct

answers: NDQ_003357

answers: continental crust is considerably thicker than oceanic

answers: NDQ_003358

answers: unanswerable

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: continental crust

answers: NDQ_003362

answers: continental crust being considerably thicker than oceanic

answers: NDQ_003363

answers: continental lithosphere

answers: NDQ_003371

answers: What is a function of its age?

answers: NDQ_003373

answers: It is formed at mid-ocean ridges

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What is added to its base?

answers: NDQ_003381

answers: What is a function of its thickness?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: movement of rock at faults

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: What type of stress is shear stress?

answers: NDQ_003389

answers: continental crust

answers: NDQ_003390

answers: subduction zone

answers: NDQ_003391

answers: subduction zones

answers: NDQ_003392

answers: subduction zone

answers: NDQ_003393

answers: continental crust

answers: NDQ_003394

answers: subduction zones

answers: NDQ_003395

answers: subduction zones

answers: NDQ_003396

answers: subduction zones

answers: NDQ_003351

answers: subduction zones;

answers: NDQ_003352

answers: it conductively cools

answers: NDQ_003353

answers: it conductively cools

answers: NDQ_003354

answers: continental crust being considerably thicker than oceanic

answers: NDQ_003355

answers: subduction zones;

answers: NDQ_003356

answers: thick;

answers: NDQ_003357

answers: subduction zones;

answers: NDQ_003358

answers: subduction zones;

answers: NDQ_003359

answers: subducted,

answers: NDQ_003360

answers: Continental lithosphere

answers: NDQ_003362

answers: continental crust being considerably thicker than oceanic

answers: NDQ_003363

answers: mid-ocean ridges

answers: NDQ_003371

answers: Tectonic lithosphere plates

answers: NDQ_003373

answers: subjacent cooling mantle

answers: NDQ_003376

answers: mountain ranges,

answers: NDQ_003378

answers: continental

answers: NDQ_003379

answers: thick;

answers: NDQ_003380

answers: age:

answers: NDQ_003381

answers: thick; its thickness is a function of its age:

answers: NDQ_003382

answers: subduction zones;

answers: NDQ_003383

answers: subjacent cooling mantle is added to its base.

answers: NDQ_003384

answers: mid-ocean ridges and spreads outwards,

answers: NDQ_003385

answers: subduction zones;

answers: NDQ_003386

answers: subduction zones;

answers: NDQ_003387

answers: subduction zones;

answers: NDQ_003388

answers: Tectonic lithosphere plates

answers: NDQ_003389

answers: Continental lithosphere

answers: NDQ_003390

answers: subduction zones;

answers: NDQ_003391

answers: subduction zones;

answers: NDQ_003392

answers: subduction zones;

answers: NDQ_003393

answers: subduction zones;

answers: NDQ_003394

answers: subduction zones;

answers: NDQ_003395

answers: subduction zones;

answers: NDQ_003396

answers: subduction zones;

text: The widely accepted explanations for the dynamics and internal evolution of Earth and its neighbors are still based [e.g., for Earth, P. Olson, 2016, Geochemistry, Geophysics, Geosystems, v. 17, p. 22] on speculations from the 1970s and 1980s. These assume slow net separation of continental crust from mantles that are still mostly unfractionated and are vigorously convecting in similar bottom-driven fashions. But they further assume that this common process yields altogether different surface effects on each planet.

text: The widely accepted explanations for the dynamics and internal evolution of Earth and its neighbors are still based [e.g., for Earth, P. Olson, 2016, Geochemistry, Geophysics, Geosystems, v. 17, p. 22] on speculations from the 1970s and 1980s. These assume slow net separation of continental crust from mantles that are still mostly un

text: fractionated

text: and are vigorously convecting in similar bottom-driven fashions. But they further assume that this common process yields altogether different surface effects on each planet.

answers: NDQ_003351

answers: bottom-driven

answers: NDQ_003352

answers: convects

answers: NDQ_003353

answers: convection

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: unfractionated

answers: NDQ_003356

answers: convect

answers: NDQ_003357

answers: crust from mantles that are still mostly unfractionated

answers: NDQ_003358

answers: unfractionated

answers: NDQ_003359

answers: unfractured

answers: NDQ_003360

answers: Earth

answers: NDQ_003362

answers: this common process yields altogether different surface effects on each planet

answers: NDQ_003363

answers: unfractionated

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: What is the reason for this?

answers: NDQ_003376

answers: unfractionated

answers: NDQ_003378

answers: unfractionated

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What process yields altogether different surface effects on each planet

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: bottom-driven fashions

answers: NDQ_003387

answers: None of the above choices.

answers: NDQ_003388

answers: What is a common process yielding altogether different surface effects on each planet?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: fault in which the hanging wall drops down relative to the footwall

answers: NDQ_003391

answers: continental crust

answers: NDQ_003392

answers: unfractionated

answers: NDQ_003393

answers: continental crust

answers: NDQ_003394

answers: unfractionated

answers: NDQ_003395

answers: NDQ_003396

answers: unfractionated

answers: NDQ_003351

answers: bottom-driven fashions.

answers: NDQ_003352

answers: convecting

answers: NDQ_003353

answers: unfractionated

answers: NDQ_003354

answers: 22]

answers: NDQ_003355

answers: unfractionated

answers: NDQ_003356

answers: different surface effects

answers: NDQ_003357

answers: bottom-driven fashions.

answers: NDQ_003358

answers: unfractionated

answers: NDQ_003359

answers: unfractionated

answers: NDQ_003360

answers: vigorously convecting in similar bottom-driven fashions.

answers: NDQ_003362

answers: different surface effects on each planet.

answers: NDQ_003363

answers: slow net separation of continental crust from mantles

answers: NDQ_003371

answers: 22]

answers: NDQ_003373

answers: vigorously convecting in similar bottom-driven fashions.

answers: NDQ_003376

answers: vigorously convecting in similar bottom-driven fashions.

answers: NDQ_003378

answers: 22]

answers: NDQ_003379

answers: 17, p. 22]

answers: NDQ_003380

answers: unfractionated and are vigorously convecting

answers: NDQ_003381

answers: vigorously convecting in similar bottom-driven fashions.

answers: NDQ_003382

answers: vigorously convecting

answers: NDQ_003383

answers: vigorously convecting

answers: NDQ_003384

answers: 22]

answers: NDQ_003385

answers: 22]

answers: NDQ_003386

answers: vigorously convecting in similar bottom-driven fashions.

answers: NDQ_003387

answers: vigorously convecting

answers: NDQ_003388

answers: vigorously convecting

answers: NDQ_003389

answers: unfractionated

answers: NDQ_003390

answers: 22]

answers: NDQ_003391

answers: mantles

answers: NDQ_003392

answers: 22]

answers: NDQ_003393

answers: continental crust

answers: NDQ_003394

answers: 22]

answers: NDQ_003395

answers: 22]

answers: NDQ_003396

answers: 22]

text: In seismology, geophysicists use ray tracing to aid in earthquake location and tomographic reconstruction of the Earth's interior. Seismic wave velocity varies within and beneath Earth's crust, causing these waves to bend and reflect. Ray tracing may be used to compute paths through a geophysical model, following them back to their source, such as an earthquake, or deducing the properties of the intervening material. In particular, the discovery of the seismic shadow zone (illustrated at right) allowed scientists to deduce the presence of Earth's molten core.

text: In

text: seismology

text: , geophysicists use ray tracing to aid in earthquake location and

text: tomographic

text: reconstruction of the

text: Earth's interior

text: Seismic wave

text: velocity varies within and beneath Earth's

text: crust

text: , causing these waves to bend and reflect. Ray tracing may be used to compute paths through a geophysical model, following them back to their source, such as an earthquake, or deducing the properties of the intervening material. In particular, the discovery of the

text: seismic shadow zone

text: (illustrated at right) allowed scientists to deduce the presence of Earth's molten core.

answers: NDQ_003351

answers: seismic wave velocity

answers: NDQ_003352

answers: bends

answers: NDQ_003353

answers: seismic waves to bend

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: seismic wave

answers: NDQ_003356

answers: bend

answers: NDQ_003357

answers: seismic wave velocity varies within and beneath Earth's crust

answers: NDQ_003358

answers: seismic shadow zone

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: the presence of Earth's molten core

answers: NDQ_003363

answers: molten core

answers: NDQ_003371

answers: What may be used to compute paths through a geophysical model?

answers: NDQ_003373

answers: What type of stresses is a deeply buried rock under?

answers: NDQ_003376

answers: What type of terrain is caused by compressive forces?

answers: NDQ_003378

answers: What is the amount the ground moves in an earthquake?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: What is an example of a stress?

answers: NDQ_003381

answers: What type of stress does ray tracing help scientists with?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is an area where faults are clustered?

answers: NDQ_003386

answers: What is the cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not a type of normal fault?

answers: NDQ_003388

answers: Which of the following is not a type of strike-slip fault?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: seismic shadow zone

answers: NDQ_003391

answers: seismic shadow zone

answers: NDQ_003392

answers: seismic shadow zone

answers: NDQ_003393

answers: seismic shadow zone

answers: NDQ_003394

answers: seismic shadow zone

answers: NDQ_003395

answers: a fault with a vertical fault plane

answers: NDQ_003396

answers: seismic shadow zone

answers: NDQ_003351

answers: Seismic wave velocity

answers: NDQ_003352

answers: bend and reflect.

answers: NDQ_003353

answers: bend and reflect.

answers: NDQ_003354

answers: In seismology,

answers: NDQ_003355

answers: seismic shadow zone

answers: NDQ_003356

answers: bend and reflect.

answers: NDQ_003357

answers: waves to bend and reflect.

answers: NDQ_003358

answers: seismic shadow zone

answers: NDQ_003359

answers: molten core.

answers: NDQ_003360

answers: earthquake,

answers: NDQ_003362

answers: molten core.

answers: NDQ_003363

answers: molten core.

answers: NDQ_003371

answers: seismic shadow zone

answers: NDQ_003373

answers: Seismic wave velocity

answers: NDQ_003376

answers: seismic shadow zone

answers: NDQ_003378

answers: Seismic wave velocity

answers: NDQ_003379

answers: seismic shadow zone

answers: NDQ_003380

answers: earthquake,

answers: NDQ_003381

answers: Seismic wave velocity

answers: NDQ_003382

answers: Seismic wave velocity

answers: NDQ_003383

answers: Seismic wave velocity

answers: NDQ_003384

answers: seismic shadow zone

answers: NDQ_003385

answers: seismic shadow zone

answers: NDQ_003386

answers: Seismic wave velocity

answers: NDQ_003387

answers: Seismic wave velocity

answers: NDQ_003388

answers: Seismic wave velocity

answers: NDQ_003389

answers: Seismic wave velocity

answers: NDQ_003390

answers: seismic shadow zone

answers: NDQ_003391

answers: seismic shadow zone

answers: NDQ_003392

answers: seismic shadow zone

answers: NDQ_003393

answers: seismic shadow zone

answers: NDQ_003394

answers: seismic shadow zone

answers: NDQ_003395

answers: seismic shadow zone

answers: NDQ_003396

answers: seismic shadow zone

text: Stress has been known to cause both physiological and behavioral chronic issues for captive species including, but not limited to, altered reproductive cycling and behavior, reduced immune responses, disrupted hormone and growth levels, reduced body weight, heightened abnormal activities and aggression, and decreased exploratory behavior with increased hiding behaviors. Such stress reactions could be caused by sounds, light conditions, odors, temperature and humidity conditions, material make-up of enclosures, habitat size constraints, lack of proper hiding areas, forced closeness to humans, routine husbandry and feeding conditions, or abnormal social groups to name a few.

text: Stress has been known to cause both physiological and behavioral chronic issues for captive species including, but not limited to, altered reproductive cycling and behavior, reduced immune responses, disrupted hormone and growth levels, reduced body weight, heightened abnormal activities and aggression, and decreased exploratory behavior with increased hiding behaviors. Such stress reactions could be caused by sounds, light conditions, odors, temperature and humidity conditions, material make-up of enclosures, habitat size constraints, lack of proper hiding areas, forced closeness to humans, routine husbandry and feeding conditions, or abnormal social groups to name a few.

answers: NDQ_003351

answers: temperature and humidity conditions

answers: NDQ_003352

answers: decreases in size

answers: NDQ_003353

answers: temperature and humidity conditions

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: decrease in size

answers: NDQ_003357

answers: decreased exploratory behavior with increased hiding behaviors

answers: NDQ_003358

answers: rockfall

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: heightened abnormal activities and aggression

answers: NDQ_003363

answers: the same time

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: Why would a rock be deeply buried?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: Which of the following is not a cause of stress?

answers: NDQ_003381

answers: unanswerable

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What type of fold is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: None of the above choices.

answers: NDQ_003387

answers: Which of the following is not a cause of normal faults?

answers: NDQ_003388

answers: Which of the following is not a cause of strike-slip faults?

answers: NDQ_003389

answers: not enough information

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: dip-slip fault

answers: NDQ_003392

answers: sloping

answers: NDQ_003393

answers: dip-slip fault plane

answers: NDQ_003394

answers: isosceles

answers: NDQ_003395

answers: a vertical fault plane

answers: NDQ_003396

answers: NDQ_003351

answers: abnormal social groups

answers: NDQ_003352

answers: hiding behaviors.

answers: NDQ_003353

answers: disrupted hormone and growth levels,

answers: NDQ_003354

answers: Stress has been known to cause both physiological and behavioral chronic issues for captive species

answers: NDQ_003355

answers: Stress

answers: NDQ_003356

answers: hiding behaviors.

answers: NDQ_003357

answers: routine husbandry and feeding conditions, or abnormal social groups

answers: NDQ_003358

answers: Stress

answers: NDQ_003359

answers: Stress has been known to cause both physiological and behavioral chronic issues for captive species

answers: NDQ_003360

answers: Stress

answers: NDQ_003362

answers: Stress

answers: NDQ_003363

answers: Stress

answers: NDQ_003371

answers: Stress

answers: NDQ_003373

answers: Stress has been known to cause both physiological and behavioral chronic issues for captive species

answers: NDQ_003376

answers: Stress has been known to cause both physiological and behavioral chronic issues for captive species

answers: NDQ_003378

answers: Stress

answers: NDQ_003379

answers: Stress has been known to cause both physiological and behavioral chronic issues for captive species

answers: NDQ_003380

answers: stress reactions could be caused by sounds, light conditions, odors,

answers: NDQ_003381

answers: material make-up of enclosures,

answers: NDQ_003382

answers: reduced body weight,

answers: NDQ_003383

answers: Stress has been known to cause both physiological and behavioral chronic issues for captive species

answers: NDQ_003384

answers: Stress

answers: NDQ_003385

answers: Stress has been known to cause both physiological and behavioral chronic issues for captive species

answers: NDQ_003386

answers: Stress

answers: NDQ_003387

answers: heightened abnormal activities and aggression, and decreased exploratory behavior with increased hiding behaviors.

answers: NDQ_003388

answers: Stress has been known to cause both physiological and behavioral chronic issues for captive species

answers: NDQ_003389

answers: Stress

answers: NDQ_003390

answers: Stress has been known to cause both physiological and behavioral chronic issues for captive species

answers: NDQ_003391

answers: Stress has been known to cause both physiological and behavioral chronic issues for captive species

answers: NDQ_003392

answers: Stress

answers: NDQ_003393

answers: Stress has been known to cause both physiological and behavioral chronic issues for captive species

answers: NDQ_003394

answers: Stress

answers: NDQ_003395

answers: Stress has been known to cause both physiological and behavioral chronic issues for captive species

answers: NDQ_003396

answers: Stress

text: Coastal regions of Peru and Chile lie above the convergent boundary, where the Nazca Plate is being subducted beneath the South American Plate along the line of the Peru–Chile Trench. The rate of convergence across this boundary is measured at about  per year. This boundary has been the site of many great megathrust earthquakes, in addition to events caused by faulting within both the subducting and over-riding plates.

text: Coastal regions of Peru and Chile lie above the

text: convergent boundary

text: , where the

text: Nazca Plate

text: is being

text: subducted

text: beneath the

text: South American Plate

text: along the line of the

text: Peru–Chile Trench

text: . The rate of convergence across this boundary is measured at about  per year. This boundary has been the site of many great

text: megathrust earthquake

text: s, in addition to events caused by faulting within both the subducting and over-riding plates.

answers: NDQ_003351

answers: megathrust

answers: NDQ_003352

answers: more likely to crack

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: plate fold

answers: NDQ_003356

answers: subduct

answers: NDQ_003357

answers: the Nazca Plate is being subducted beneath the South American Plate

answers: NDQ_003358

answers: Trench

answers: NDQ_003359

answers: subducts

answers: NDQ_003360

answers: plates

answers: NDQ_003362

answers: The rate of convergence across this boundary is measured at about per year

answers: NDQ_003363

answers: convergent boundary

answers: NDQ_003371

answers: Which of the following is not a type of fault: subducting or over-riding plates?

answers: NDQ_003373

answers: What is being subducted beneath the South American Plate?

answers: NDQ_003376

answers: Which of the following is not a type of terrain: basin-and-range or faulting?

answers: NDQ_003378

answers: what is the last word in the passage?

answers: NDQ_003379

answers: Which of the following is not a type of strike-slip fault?

answers: NDQ_003380

answers: Which of the following is not a stress?

answers: NDQ_003381

answers: What would happen if the Nazca Plate is subducted?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a type of stress: subducting and over-riding plates?

answers: NDQ_003384

answers: Which of the following is not a type of fold that arches upward?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: yes

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: subducting or over-riding plates?

answers: NDQ_003388

answers: Which plate is being subducted beneath the South American Plate along the line of the Peru–Chile Trench?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: megathrust

answers: NDQ_003391

answers: Nazca Plate

answers: NDQ_003392

answers: megathrust

answers: NDQ_003393

answers: Coastal regions

answers: NDQ_003394

answers: over-riding plates

answers: NDQ_003395

answers: over-riding plates

answers: NDQ_003396

answers: megathrust

answers: NDQ_003351

answers: megathrust earthquakes,

answers: NDQ_003352

answers: megathrust earthquakes,

answers: NDQ_003353

answers: earthquakes,

answers: NDQ_003354

answers: convergent boundary,

answers: NDQ_003355

answers: megathrust

answers: NDQ_003356

answers: megathrust earthquakes,

answers: NDQ_003357

answers: subducting and over-riding plates.

answers: NDQ_003358

answers: megathrust earthquakes,

answers: NDQ_003359

answers: faulting

answers: NDQ_003360

answers: convergent boundary,

answers: NDQ_003362

answers: Coastal regions of Peru and Chile lie above the convergent boundary,

answers: NDQ_003363

answers: the Nazca Plate is being subducted beneath the South American Plate

answers: NDQ_003371

answers: megathrust earthquakes,

answers: NDQ_003373

answers: Peru–Chile Trench.

answers: NDQ_003376

answers: Coastal regions of Peru and Chile lie above the convergent boundary,

answers: NDQ_003378

answers: megathrust

answers: NDQ_003379

answers: Peru–Chile Trench.

answers: NDQ_003380

answers: megathrust earthquakes,

answers: NDQ_003381

answers: faulting

answers: NDQ_003382

answers: faulting within both the subducting and over-riding plates.

answers: NDQ_003383

answers: faulting

answers: NDQ_003384

answers: convergent boundary,

answers: NDQ_003385

answers: convergent boundary,

answers: NDQ_003386

answers: faulting within both the subducting and over-riding plates.

answers: NDQ_003387

answers: faulting within both the subducting and over-riding plates.

answers: NDQ_003388

answers: faulting within both the subducting and over-riding plates.

answers: NDQ_003389

answers: subducted beneath the South American Plate

answers: NDQ_003390

answers: faulting within both the subducting and over-riding plates.

answers: NDQ_003391

answers: South American Plate

answers: NDQ_003392

answers: faulting within both the subducting and over-riding plates.

answers: NDQ_003393

answers: Coastal regions of Peru and Chile lie above the convergent boundary,

answers: NDQ_003394

answers: faulting within both the subducting and over-riding plates.

answers: NDQ_003395

answers: faulting within both the subducting and over-riding plates.

answers: NDQ_003396

answers: over-riding plates.

text: Earthquakes occur as a consequence of gradual stress increases in a region, and once it reaches the maximum stress that the rocks can withstand a rupture generates and the resulting earthquake motion is related to a drop in the shear stress of the system. Earthquakes generate seismic waves when the rupture in the system occurs, the seismic waves consist of different types of waves that are capable of moving through the Earth like ripples over water. The causes that lead to slow earthquakes have only been theoretically investigated, by the formation of longitudinal shear cracks that were analysed using mathematical models. The different distributions of initial stress, sliding frictional stress, and specific fracture energy are all taken into account. If the initial stress minus the sliding frictional stress (with respect to the initial crack) is low, and the specific fracture energy or the strength of the crustal material (relative to the amount of stress) is high then slow earthquakes will occur regularly.In other words, slow earthquakes are caused by a variety of stick-slip and creep processes intermediated between asperity-controlled brittle and ductile fracture.  Asperities are tiny bumps and protrusions along the faces of fractures. They are best documented from intermediate crustal levels of certain subduction zones (especially those that dip shallowly — SW Japan, Cascadia, Chile), but appear to occur on other types of faults as well, notably strike-slip plate boundaries such as the San Andreas fault and "mega-landslide" normal faults on the flanks of volcanos.

text: Earthquakes occur as a consequence of gradual stress increases in a region, and once it reaches the maximum stress that the rocks can withstand a rupture generates and the resulting earthquake motion is related to a drop in the shear stress of the system. Earthquakes generate

text: seismic wave

text: s when the rupture in the system occurs, the seismic waves consist of different types of waves that are capable of moving through the Earth like ripples over water. The causes that lead to slow earthquakes have only been theoretically investigated, by the formation of longitudinal shear cracks that were analysed using mathematical models. The different distributions of

text: initial stress

text: sliding frictional stress

text: , and specific fracture energy are all taken into account. If the initial stress minus the sliding frictional stress (with respect to the initial crack) is low, and the specific fracture energy or the strength of the crustal material (relative to the amount of stress) is high then slow earthquakes will occur regularly.In other words, slow earthquakes are caused by a variety of

text: stick-slip

text: and creep processes intermediated between asperity-controlled

text: brittle and ductile fracture

text: .  Asperities are tiny bumps and protrusions along the faces of fractures. They are best documented from intermediate crustal levels of certain

text: subduction zones

text: (especially those that dip shallowly — SW Japan, Cascadia, Chile), but appear to occur on other types of

text: faults

text: as well, notably

text: strike-slip

text: plate boundaries such as the San Andreas fault and "mega-landslide" normal faults on the flanks of volcanos.

answers: NDQ_003351

answers: sliding frictional stress

answers: NDQ_003352

answers: can withstand more

answers: NDQ_003353

answers: shear cracks

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: subduction zone

answers: NDQ_003356

answers: stick-slip

answers: NDQ_003357

answers: Asperities are tiny bumps

answers: NDQ_003358

answers: slow earthquakes

answers: NDQ_003359

answers: it reaches the maximum stress

answers: NDQ_003360

answers: subduction zones

answers: NDQ_003362

answers: the San Andreas fault is on the flanks of volcanos

answers: NDQ_003363

answers: subduction zones

answers: NDQ_003371

answers: What is a consequence of gradual stress increases in a region?

answers: NDQ_003373

answers: What is the maximum stress that the rocks can withstand?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: no

answers: NDQ_003380

answers: What is the maximum stress that the rocks can withstand

answers: NDQ_003381

answers: unanswerable

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: unanswerable

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: yes

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: subduction zones

answers: NDQ_003391

answers: subduction zone

answers: NDQ_003392

answers: San Andreas fault

answers: NDQ_003393

answers: subduction zone

answers: NDQ_003394

answers: strike-slip

answers: NDQ_003395

answers: strike-slip plate boundaries

answers: NDQ_003396

answers: strike-slip plate boundaries

answers: NDQ_003351

answers: strike-slip

answers: NDQ_003352

answers: maximum stress that the rocks can withstand

answers: NDQ_003353

answers: longitudinal shear cracks

answers: NDQ_003354

answers: Earthquakes

answers: NDQ_003355

answers: subduction zones

answers: NDQ_003356

answers: slow earthquakes

answers: NDQ_003357

answers: Asperities

answers: NDQ_003358

answers: slow earthquakes

answers: NDQ_003359

answers: maximum stress that the rocks can withstand

answers: NDQ_003360

answers: faults

answers: NDQ_003362

answers: strike-slip plate boundaries

answers: NDQ_003363

answers: subduction zones

answers: NDQ_003371

answers: San Andreas fault

answers: NDQ_003373

answers: Earthquakes

answers: NDQ_003376

answers: asperity-controlled brittle and ductile fracture.

answers: NDQ_003378

answers: stick-slip

answers: NDQ_003379

answers: San Andreas fault

answers: NDQ_003380

answers: stress increases in a region, and once it reaches the maximum stress

answers: NDQ_003381

answers: maximum stress that the rocks can withstand

answers: NDQ_003382

answers: strike-slip plate boundaries

answers: NDQ_003383

answers: Asperities

answers: NDQ_003384

answers: Asperities

answers: NDQ_003385

answers: Earthquakes

answers: NDQ_003386

answers: gradual stress increases in a region,

answers: NDQ_003387

answers: "mega-landslide"

answers: NDQ_003388

answers: strike-slip plate boundaries

answers: NDQ_003389

answers: Earthquakes

answers: NDQ_003390

answers: San Andreas fault

answers: NDQ_003391

answers: subduction zones

answers: NDQ_003392

answers: strike-slip plate boundaries such as the San Andreas fault

answers: NDQ_003393

answers: strike-slip plate boundaries

answers: NDQ_003394

answers: strike-slip plate boundaries such as the San Andreas fault

answers: NDQ_003395

answers: strike-slip plate boundaries such as the San Andreas fault

answers: NDQ_003396

answers: strike-slip plate boundaries such as the San Andreas fault

text: Structural geologists study the results of deformation, using observations of rock, especially the mode and geometry of deformation to reconstruct the stress field that affected the rock over time. Structural geology is an important complement to geodynamics because it provides the most direct source of data about the movements of the Earth. Different modes of deformation result in distinct geological structures. Figures 3 shows the appearance of brittle fracture in rocks while figure 4 shows the appearance of ductile folding.

text: Structural geologists study the results of deformation, using observations of rock, especially the mode and geometry of deformation to reconstruct the stress field that affected the rock over time.

text: Structural geology

text: is an important complement to geodynamics because it provides the most direct source of data about the movements of the Earth. Different modes of deformation result in distinct geological structures. Figures 3 shows the appearance of brittle fracture in rocks while figure 4 shows the appearance of ductile folding.

answers: NDQ_003351

answers: ductile folding

answers: NDQ_003352

answers: brittle fracture

answers: NDQ_003353

answers: deformation

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: ductile folding

answers: NDQ_003356

answers: fold

answers: NDQ_003357

answers: ductile folding is a type of

answers: NDQ_003358

answers: brittle

answers: NDQ_003359

answers: deforms

answers: NDQ_003360

answers: Earth's surface

answers: NDQ_003362

answers: brittle fracture in rocks

answers: NDQ_003363

answers: ductile folding

answers: NDQ_003371

answers: Which of the following is not a mode of deformation?

answers: NDQ_003373

answers: Which of the following is not a mode of deformation?

answers: NDQ_003376

answers: what is the most direct source of data about the movements of the Earth

answers: NDQ_003378

answers: What is the most direct source of data about the movements of the Earth?

answers: NDQ_003379

answers: Which of the following is not a mode of deformation?

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: Which of the following is not a type of deformation: brittle fracture, ductile folding, or stress field?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rocks?

answers: NDQ_003384

answers: Which of the following is not a type of fold: syncline, brittle fracture, or ductile folding?

answers: NDQ_003385

answers: What is the term for an area where faults are clustered?

answers: NDQ_003386

answers: Which of the following is not a cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not a mode of deformation?

answers: NDQ_003388

answers: How do structural geologists study the results of deformation?

answers: NDQ_003389

answers: Which of the following is not a type of folding?

answers: NDQ_003390

answers: ductile folding

answers: NDQ_003391

answers: ductile folding

answers: NDQ_003392

answers: ductile

answers: NDQ_003393

answers: ductile folding

answers: NDQ_003394

answers: lateral

answers: NDQ_003395

answers: ductile folding

answers: NDQ_003396

answers: ductile

answers: NDQ_003351

answers: brittle fracture

answers: NDQ_003352

answers: brittle fracture

answers: NDQ_003353

answers: brittle fracture

answers: NDQ_003354

answers: Structural geologists

answers: NDQ_003355

answers: ductile

answers: NDQ_003356

answers: ductile folding.

answers: NDQ_003357

answers: brittle fracture

answers: NDQ_003358

answers: brittle fracture

answers: NDQ_003359

answers: brittle fracture

answers: NDQ_003360

answers: deformation,

answers: NDQ_003362

answers: brittle fracture

answers: NDQ_003363

answers: deformation,

answers: NDQ_003371

answers: Structural geologists

answers: NDQ_003373

answers: brittle fracture in rocks

answers: NDQ_003376

answers: ductile folding.

answers: NDQ_003378

answers: deformation,

answers: NDQ_003379

answers: brittle fracture in rocks while figure 4

answers: NDQ_003380

answers: deformation,

answers: NDQ_003381

answers: ductile folding.

answers: NDQ_003382

answers: ductile folding.

answers: NDQ_003383

answers: brittle fracture

answers: NDQ_003384

answers: ductile

answers: NDQ_003385

answers: Structural geologists study the results of deformation,

answers: NDQ_003386

answers: deformation,

answers: NDQ_003387

answers: ductile folding.

answers: NDQ_003388

answers: ductile folding.

answers: NDQ_003389

answers: ductile folding.

answers: NDQ_003390

answers: ductile folding.

answers: NDQ_003391

answers: brittle fracture

answers: NDQ_003392

answers: ductile folding.

answers: NDQ_003393

answers: brittle fracture

answers: NDQ_003394

answers: ductile folding.

answers: NDQ_003395

answers: ductile folding.

answers: NDQ_003396

answers: ductile folding.

text: Everything on the Pacific plate that enters the IBM trench is subducted.  The next section discusses some modifications of the lithosphere just prior to its descent and the age and composition of oceanic crust and sediments on the Pacific plate adjacent to the trench.  In addition to subducted sediments and crust of the Pacific plate, there is also a very substantial volume of material from the overriding IBM forearc that is lost to the subduction zone by tectonic erosion .

text: Everything on the Pacific plate that enters the IBM trench is subducted.  The next section discusses some modifications of the lithosphere just prior to its descent and the age and composition of oceanic crust and sediments on the Pacific plate adjacent to the trench.  In addition to subducted sediments and crust of the Pacific plate, there is also a very substantial volume of material from the overriding IBM forearc that is lost to the subduction zone by

text: tectonic erosion

answers: NDQ_003351

answers: subduction zone

answers: NDQ_003352

answers: subducts

answers: NDQ_003353

answers: subduction

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: trench

answers: NDQ_003356

answers: subduct

answers: NDQ_003357

answers: sediments and crust of the Pacific plate are subducted

answers: NDQ_003358

answers: Forearc

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Pacific plate

answers: NDQ_003362

answers: Everything on the Pacific plate that enters the IBM trench is subducted

answers: NDQ_003363

answers: IBM trench

answers: NDQ_003371

answers: Which of the following is not an example of a thrust fault?

answers: NDQ_003373

answers: Which of the following is not a type of stress?

answers: NDQ_003376

answers: What type of terrain is caused by compressive forces?

answers: NDQ_003378

answers: What is the amount the ground moves in an earthquake?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: Which of the following is not a stress?

answers: NDQ_003381

answers: What happens to rock when confining stress occurs?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not the cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is the area where faults are clustered called?

answers: NDQ_003386

answers: What is the cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not a cause of normal faults?

answers: NDQ_003388

answers: Which of the following is not a type of strike-slip fault?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: subduction zone

answers: NDQ_003391

answers: subduction zone

answers: NDQ_003392

answers: subduction zone

answers: NDQ_003393

answers: lithosphere

answers: NDQ_003394

answers: subduction zone

answers: NDQ_003395

answers: tectonic

answers: NDQ_003396

answers: subduction zone

answers: NDQ_003351

answers: tectonic erosion.

answers: NDQ_003352

answers: subducted.

answers: NDQ_003353

answers: tectonic erosion.

answers: NDQ_003354

answers: Everything on the Pacific plate that enters the IBM trench is subducted.

answers: NDQ_003355

answers: forearc

answers: NDQ_003356

answers: tectonic erosion.

answers: NDQ_003357

answers: subducted.

answers: NDQ_003358

answers: subduction zone

answers: NDQ_003359

answers: tectonic erosion.

answers: NDQ_003360

answers: tectonic erosion.

answers: NDQ_003362

answers: Everything on the Pacific plate that enters the IBM trench is subducted.

answers: NDQ_003363

answers: IBM trench

answers: NDQ_003371

answers: Everything on the Pacific plate that enters the IBM trench is subducted.

answers: NDQ_003373

answers: Everything on the Pacific plate that enters the IBM trench is subducted.

answers: NDQ_003376

answers: tectonic erosion.

answers: NDQ_003378

answers: subducted.

answers: NDQ_003379

answers: Everything on the Pacific plate that enters the IBM trench is subducted.

answers: NDQ_003380

answers: tectonic erosion.

answers: NDQ_003381

answers: tectonic erosion.

answers: NDQ_003382

answers: tectonic erosion.

answers: NDQ_003383

answers: tectonic erosion.

answers: NDQ_003384

answers: IBM forearc

answers: NDQ_003385

answers: subduction zone

answers: NDQ_003386

answers: tectonic erosion.

answers: NDQ_003387

answers: tectonic erosion.

answers: NDQ_003388

answers: tectonic erosion.

answers: NDQ_003389

answers: tectonic erosion.

answers: NDQ_003390

answers: IBM trench

answers: NDQ_003391

answers: subducted.

answers: NDQ_003392

answers: IBM trench

answers: NDQ_003393

answers: IBM forearc

answers: NDQ_003394

answers: IBM trench

answers: NDQ_003395

answers: IBM trench

answers: NDQ_003396

answers: IBM trench

text: Metamorphic rocks make up a large part of the Earth's crust and form 12% of the Earth's current land surface. They are classified by texture and by chemical and mineral assemblage (metamorphic facies). They may be formed simply by being deep beneath the Earth's surface, subjected to high temperatures and the great pressure of the rock layers above it. They can form from tectonic processes such as continental collisions, which cause horizontal pressure, friction and distortion. They are also formed when rock is heated up by the intrusion of hot molten rock called magma from the Earth's interior. The study of metamorphic rocks (now exposed at the Earth's surface following erosion and uplift) provides information about the temperatures and pressures that occur at great depths within the Earth's crust.Some examples of metamorphic rocks are gneiss, slate, marble, schist, and quartzite.

text: Metamorphic rocks make up a large part of the

text: Earth

text: 's

text: crust

text: and form 12% of the Earth's current land surface. They are classified by

text: texture

text: and by

text: chemical

text: and

text: mineral

text: assemblage (

text: metamorphic facies

text: ). They may be formed simply by being deep beneath the Earth's surface, subjected to high temperatures and the great pressure of the rock layers above it. They can form from

text: tectonic

text: processes such as continental collisions, which cause horizontal pressure, friction and distortion. They are also formed when rock is heated up by the

text: intrusion

text: of hot molten rock called

text: magma

text: from the Earth's interior. The study of metamorphic rocks (now exposed at the Earth's surface following erosion and uplift) provides information about the temperatures and pressures that occur at great depths within the Earth's crust.Some examples of metamorphic rocks are

text: gneiss

text: slate

text: marble

text: schist

text: , and

text: quartzite

answers: NDQ_003351

answers: horizontal pressure

answers: NDQ_003352

answers: is more likely to form

answers: NDQ_003353

answers: horizontal pressure

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: horizontal

answers: NDQ_003356

answers: heat up

answers: NDQ_003357

answers: horizontal pressure, friction and distortion are caused

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: is heated up

answers: NDQ_003360

answers: tectonic processes

answers: NDQ_003362

answers: they may be formed simply by being deep beneath the Earth's surface

answers: NDQ_003363

answers: tectonic processes

answers: NDQ_003371

answers: What can form from tectonic processes such as continental collisions

answers: NDQ_003373

answers: high temperatures and the great pressure

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a type of stress: horizontal pressure, friction and distortion

answers: NDQ_003381

answers: What can form from continental collisions?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not a type of fold that arches upward?

answers: NDQ_003385

answers: What type of rocks are gneiss, slate, marble, schist, and quartzite?

answers: NDQ_003386

answers: Which of the following is not the cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: horizontal pressure, friction and distortion

answers: NDQ_003388

answers: What can form from tectonic processes such as continental collisions, which cause horizontal pressure, friction and distortion?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: continental collisions

answers: NDQ_003391

answers: metamorphic rocks

answers: NDQ_003392

answers: uplift

answers: NDQ_003393

answers: metamorphic rocks

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: continental collisions

answers: NDQ_003396

answers: continental collisions

answers: NDQ_003351

answers: horizontal pressure,

answers: NDQ_003352

answers: distortion.

answers: NDQ_003353

answers: distortion.

answers: NDQ_003354

answers: Metamorphic rocks

answers: NDQ_003355

answers: Metamorphic rocks

answers: NDQ_003356

answers: distortion.

answers: NDQ_003357

answers: horizontal pressure, friction and distortion.

answers: NDQ_003358

answers: Metamorphic rocks

answers: NDQ_003359

answers: heated up

answers: NDQ_003360

answers: tectonic processes such as continental collisions,

answers: NDQ_003362

answers: Metamorphic rocks

answers: NDQ_003363

answers: deep beneath the Earth's surface,

answers: NDQ_003371

answers: Metamorphic rocks

answers: NDQ_003373

answers: high temperatures and the great pressure of the rock layers above it.

answers: NDQ_003376

answers: tectonic processes such as continental collisions,

answers: NDQ_003378

answers: Metamorphic rocks

answers: NDQ_003379

answers: horizontal

answers: NDQ_003380

answers: pressure, friction and distortion.

answers: NDQ_003381

answers: distortion.

answers: NDQ_003382

answers: horizontal pressure,

answers: NDQ_003383

answers: tectonic processes such as continental collisions,

answers: NDQ_003384

answers: Metamorphic rocks

answers: NDQ_003385

answers: Metamorphic rocks

answers: NDQ_003386

answers: tectonic processes such as continental collisions,

answers: NDQ_003387

answers: tectonic processes such as continental collisions,

answers: NDQ_003388

answers: tectonic processes such as continental collisions,

answers: NDQ_003389

answers: tectonic processes such as continental collisions,

answers: NDQ_003390

answers: tectonic processes such as continental collisions,

answers: NDQ_003391

answers: Metamorphic rocks

answers: NDQ_003392

answers: Metamorphic rocks

answers: NDQ_003393

answers: Metamorphic rocks

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: continental collisions,

answers: NDQ_003396

answers: continental collisions,

text: Metallic or native iron is rarely found on the surface of the Earth because it tends to oxidize, but its oxides are pervasive and represent the primary ores. While it makes up about 5% of the Earth's crust, both the Earth's inner and outer core are believed to consist largely of an iron-nickel alloy constituting 35% of the mass of the Earth as a whole. Iron is consequently the most abundant element on Earth, but only the fourth most abundant element in the Earth's crust, after oxygen, silicon, and aluminium. Most of the iron in the crust is found combined with oxygen as iron oxide minerals such as hematite (FeO), magnetite (FeO), and siderite (FeCO). Many igneous rocks also contain the sulfide minerals pyrrhotite and pentlandite.

text: Metallic or

text: native iron

text: is rarely found on the surface of the Earth because it tends to oxidize, but its oxides are pervasive and represent the primary ores. While it makes up about 5% of the

text: Earth's crust

text: , both the Earth's

text: inner

text: and

text: outer core

text: are believed to consist largely of an iron-

text: nickel

text: alloy constituting 35% of the mass of the Earth as a whole. Iron is consequently the most abundant element on Earth, but only the fourth most abundant element in the Earth's crust, after

text: oxygen

text: silicon

text: , and

text: aluminium

text: . Most of the iron in the crust is found combined with oxygen as

text: iron oxide

text: minerals such as

text: hematite

text: (FeO),

text: magnetite

text: (FeO), and

text: siderite

text: (FeCO). Many

text: igneous rock

text: s also contain the sulfide minerals

text: pyrrhotite

text: and

text: pentlandite

answers: NDQ_003351

answers: iron

answers: NDQ_003352

answers: oxidizes

answers: NDQ_003353

answers: iron oxide minerals

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: siderite

answers: NDQ_003356

answers: metalize

answers: NDQ_003357

answers: iron oxide minerals such as hematite (FeO), magnetite (FeO), and siderite (FeCO)

answers: NDQ_003358

answers: igneous

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: metallic or native iron is rarely found on the surface of the Earth

answers: NDQ_003363

answers: igneous rocks

answers: NDQ_003371

answers: What is the most abundant element in the Earth's crust?

answers: NDQ_003373

answers: What is the most abundant element on Earth?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What is the third most abundant element in the Earth's crust?

answers: NDQ_003381

answers: What is the most abundant element on Earth?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: What is the third most abundant element in the Earth's crust?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: movement of rock at faults

answers: NDQ_003387

answers: Which of the following is not a mineral: pyrrhotite or pentlandite?

answers: NDQ_003388

answers: How many percent of the Earth's crust does iron make up?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: igneous rocks

answers: NDQ_003391

answers: igneous rocks

answers: NDQ_003392

answers: The hanging wall pushes up relative to the footwall

answers: NDQ_003393

answers: igneous rocks

answers: NDQ_003394

answers: igneous rocks

answers: NDQ_003395

answers: igneous rocks

answers: NDQ_003396

answers: pyrrhotite

answers: NDQ_003351

answers: oxygen,

answers: NDQ_003352

answers: oxidize,

answers: NDQ_003353

answers: oxidize,

answers: NDQ_003354

answers: Metallic or native iron is rarely found on the surface of the Earth

answers: NDQ_003355

answers: igneous rocks

answers: NDQ_003356

answers: oxidize,

answers: NDQ_003357

answers: oxygen

answers: NDQ_003358

answers: igneous rocks

answers: NDQ_003359

answers: igneous rocks

answers: NDQ_003360

answers: iron

answers: NDQ_003362

answers: Metallic or native iron

answers: NDQ_003363

answers: igneous rocks

answers: NDQ_003371

answers: Metallic or native iron is rarely found on the surface of the Earth

answers: NDQ_003373

answers: igneous rocks

answers: NDQ_003376

answers: Metallic or native iron is rarely found on the surface of the Earth

answers: NDQ_003378

answers: Metallic or native iron is rarely found on the surface of the Earth

answers: NDQ_003379

answers: oxygen

answers: NDQ_003380

answers: iron

answers: NDQ_003381

answers: Metallic or native iron

answers: NDQ_003382

answers: oxygen, silicon, and aluminium.

answers: NDQ_003383

answers: Metallic or native iron

answers: NDQ_003384

answers: Metallic or native iron is rarely found on the surface of the Earth

answers: NDQ_003385

answers: Metallic or native iron is rarely found on the surface of the Earth

answers: NDQ_003386

answers: Metallic or native iron

answers: NDQ_003387

answers: Metallic or native iron is rarely found on the surface of the Earth

answers: NDQ_003388

answers: Metallic or native iron

answers: NDQ_003389

answers: igneous rocks

answers: NDQ_003390

answers: Metallic or native iron is rarely found on the surface of the Earth

answers: NDQ_003391

answers: igneous rocks

answers: NDQ_003392

answers: Metallic or native iron is rarely found on the surface of the Earth

answers: NDQ_003393

answers: igneous rocks

answers: NDQ_003394

answers: Metallic or native iron is rarely found on the surface of the Earth

answers: NDQ_003395

answers: Metallic or native iron is rarely found on the surface of the Earth

answers: NDQ_003396

answers: Metallic or native iron is rarely found on the surface of the Earth

text: Subduction is the density-driven process by which one tectonic plate moves under another and sinks into the mantle at a convergent boundary. Gravitational pull from dense slabs provides approximately 90% of the driving force for plate tectonics, and consequently subduction is crucial in changing the Earth's layout, guiding its thermal evolution and building its compositional structure. In particular, subduction zones are the primary sites of present-day continental crust formation, another process of modern Earth that has a mysterious past. Furthermore, subduction is the main mechanism by which surface materials enter the deep Earth and is also largely responsible for the formation of ores. Considering the importance of subduction in many geological processes, it is clear that studying its past and present nature is essential to developing our understanding of the Earth as a dynamic system.

text: Subduction is the density-driven process by which one tectonic plate moves under another and sinks into the

text: mantle

text: at a

text: convergent boundary

text: . Gravitational pull from dense slabs provides approximately 90% of the driving force for

text: plate tectonics

text: , and consequently subduction is crucial in changing the Earth's layout, guiding its

text: thermal evolution

text: and building its compositional structure. In particular, subduction zones are the primary sites of present-day

text: continental crust

text: formation, another process of modern Earth that has a mysterious past. Furthermore, subduction is the main mechanism by which surface materials enter the deep

text: Earth

text: and is also largely responsible for the formation of

text: ores

text: . Considering the importance of subduction in many

text: geological

text: processes, it is clear that studying its past and present nature is essential to developing our understanding of the Earth as a dynamic system.

answers: NDQ_003351

answers: Gravitational pull

answers: NDQ_003352

answers: sinks

answers: NDQ_003353

answers: subduction

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: subduction zone

answers: NDQ_003356

answers: sink

answers: NDQ_003357

answers: one tectonic plate moves under another and sinks into the mantle

answers: NDQ_003358

answers: unanswerable

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: subduction

answers: NDQ_003362

answers: the San Andreas fault is the primary site of present-day continental crust formation

answers: NDQ_003363

answers: subduction zones

answers: NDQ_003371

answers: What is the primary site of present-day continental crust formation

answers: NDQ_003373

answers: Why is studying its past and present nature essential to developing our understanding of the Earth as a dynamic system?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: vertical

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What is the primary site of present-day continental crust formation?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is the primary site of present-day continental crust formation?

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: What is the main mechanism by which surface materials enter the deep Earth?

answers: NDQ_003388

answers: What is the primary site of present-day continental crust formation

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: subduction zone

answers: NDQ_003391

answers: subduction zone

answers: NDQ_003392

answers: subduction zone

answers: NDQ_003393

answers: continental crust

answers: NDQ_003394

answers: subduction zone

answers: NDQ_003395

answers: subduction zone

answers: NDQ_003396

answers: Subduction

answers: NDQ_003351

answers: Gravitational pull from dense slabs

answers: NDQ_003352

answers: sinks into the mantle

answers: NDQ_003353

answers: Subduction

answers: NDQ_003354

answers: Subduction

answers: NDQ_003355

answers: Subduction

answers: NDQ_003356

answers: ores.

answers: NDQ_003357

answers: convergent boundary.

answers: NDQ_003358

answers: subduction zones

answers: NDQ_003359

answers: convergent boundary.

answers: NDQ_003360

answers: Subduction

answers: NDQ_003362

answers: Subduction

answers: NDQ_003363

answers: subduction zones

answers: NDQ_003371

answers: Subduction

answers: NDQ_003373

answers: Subduction

answers: NDQ_003376

answers: Subduction

answers: NDQ_003378

answers: Subduction

answers: NDQ_003379

answers: Subduction

answers: NDQ_003380

answers: Gravitational pull from dense slabs provides approximately 90% of the driving force

answers: NDQ_003381

answers: Subduction

answers: NDQ_003382

answers: Subduction

answers: NDQ_003383

answers: Subduction

answers: NDQ_003384

answers: Subduction

answers: NDQ_003385

answers: subduction zones

answers: NDQ_003386

answers: Subduction

answers: NDQ_003387

answers: Subduction

answers: NDQ_003388

answers: Subduction

answers: NDQ_003389

answers: Subduction

answers: NDQ_003390

answers: Subduction

answers: NDQ_003391

answers: Subduction

answers: NDQ_003392

answers: Subduction

answers: NDQ_003393

answers: continental crust

answers: NDQ_003394

answers: Subduction

answers: NDQ_003395

answers: Subduction

answers: NDQ_003396

answers: Subduction

text: The Northern Harz Boundary Fault (, Nordharzrandverwerfung or Harznordrandstörung) is a geological fault where the Harz Block, which consists of rocks formed during the Palaeozoic Era and folded in the course of Hercynian mountain building, borders on the Subhercynian Basin or Harz Foreland. The fault is also known in English as the Harz North Rim Fault or Harznordrand Thrust (Fault).

text: The Northern Harz Boundary Fault (, Nordharzrandverwerfung or Harznordrandstörung) is a

text: geological fault

text: where the

text: Harz Block

text: , which consists of rocks formed during the

text: Palaeozoic

text: Era and folded in the course of

text: Hercynian mountain building

text: , borders on the

text: Subhercynian Basin

text: or

text: Harz Foreland

text: . The fault is also known in English as the Harz North Rim Fault or Harznordrand Thrust (Fault).

answers: NDQ_003351

answers: subhercynian

answers: NDQ_003352

answers: folds

answers: NDQ_003353

answers: faults

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fault

answers: NDQ_003356

answers: fold

answers: NDQ_003357

answers: Harz Block consists of rocks formed during what time period?

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: folded

answers: NDQ_003360

answers: faults

answers: NDQ_003362

answers: The Northern Harz Boundary Fault is a geological fault

answers: NDQ_003363

answers: Hercynian

answers: NDQ_003371

answers: What is a thrust fault?

answers: NDQ_003373

answers: How would you describe a rock that is deeply buried?

answers: NDQ_003376

answers: What is the cause of the terrain known as basin-and-range?

answers: NDQ_003378

answers: What is the amount of the ground moving in an earthquake?

answers: NDQ_003379

answers: What type of fault is the Northern Harz Boundary Fault?

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What type of stress is the Northern Harz Boundary Fault?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: What is the cause of earthquakes?

answers: NDQ_003387

answers: What are normal faults caused by?

answers: NDQ_003388

answers: What type of stress does the Northern Harz Boundary Fault result from?

answers: NDQ_003389

answers: Yes

answers: NDQ_003390

answers: Northern Harz Boundary Fault

answers: NDQ_003391

answers: Harz Block

answers: NDQ_003392

answers: Northern Harz Boundary Fault

answers: NDQ_003393

answers: Harz Block

answers: NDQ_003394

answers: Northern Harz Boundary Fault

answers: NDQ_003395

answers: Northern Harz Boundary Fault

answers: NDQ_003396

answers: Nordharzrandverwerfung

answers: NDQ_003351

answers: The Northern Harz Boundary Fault

answers: NDQ_003352

answers: folded

answers: NDQ_003353

answers: folded

answers: NDQ_003354

answers: The Northern Harz Boundary Fault

answers: NDQ_003355

answers: fault

answers: NDQ_003356

answers: folded in the course of Hercynian mountain building,

answers: NDQ_003357

answers: borders on the Subhercynian Basin

answers: NDQ_003358

answers: geological fault

answers: NDQ_003359

answers: folded

answers: NDQ_003360

answers: Northern Harz Boundary Fault

answers: NDQ_003362

answers: The Northern Harz Boundary Fault

answers: NDQ_003363

answers: Hercynian

answers: NDQ_003371

answers: Harznordrand Thrust

answers: NDQ_003373

answers: The Northern Harz Boundary Fault

answers: NDQ_003376

answers: Hercynian mountain building,

answers: NDQ_003378

answers: The Northern Harz Boundary Fault

answers: NDQ_003379

answers: The Northern Harz Boundary Fault

answers: NDQ_003380

answers: folded in the course of Hercynian mountain building,

answers: NDQ_003381

answers: folded in the course of Hercynian mountain building,

answers: NDQ_003382

answers: The Northern Harz Boundary Fault

answers: NDQ_003383

answers: folded in the course of Hercynian mountain building,

answers: NDQ_003384

answers: The Northern Harz Boundary Fault

answers: NDQ_003385

answers: The Northern Harz Boundary Fault

answers: NDQ_003386

answers: folded in the course of Hercynian mountain building,

answers: NDQ_003387

answers: The Northern Harz Boundary Fault

answers: NDQ_003388

answers: The Northern Harz Boundary Fault

answers: NDQ_003389

answers: Hercynian mountain building,

answers: NDQ_003390

answers: Northern Harz Boundary Fault

answers: NDQ_003391

answers: Harz Block,

answers: NDQ_003392

answers: Northern Harz Boundary Fault

answers: NDQ_003393

answers: Harz Block,

answers: NDQ_003394

answers: The Northern Harz Boundary Fault

answers: NDQ_003395

answers: The Northern Harz Boundary Fault

answers: NDQ_003396

answers: Northern Harz Boundary Fault

text: Skin folds or skinfolds are areas of skin where it folds. Many skin folds are distinct, heritable anatomical features, and may be used for identification of animal species, while others are non-specific and may be produced either by individual development of an organism or by arbitrary application of force to skin, either by the actions of the muscles of the body or by external force, e.g., gravity. Anatomical folds can also be found in other structures and tissues besides the skin, such as the ileocecal fold beneath the terminal ileum of the cecum.

text: Skin folds or skinfolds are areas of

text: skin

text: where it folds. Many skin folds are distinct, heritable anatomical features, and may be used for identification of animal

text: species

text: , while others are non-specific and may be produced either by individual development of an organism or by arbitrary application of force to skin, either by the actions of the

text: muscle

text: s of the body or by external force, e.g.,

text: gravity

text: . Anatomical folds can also be found in other structures and tissues besides the skin, such as the

text: ileocecal fold

text: beneath the terminal ileum of the cecum.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: skin folds

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: fold that bends downward

answers: NDQ_003356

answers: fold

answers: NDQ_003357

answers: skin folds can also be found in other structures and tissues besides the skin

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: gravity

answers: NDQ_003362

answers: arbitrary application of force to skin

answers: NDQ_003363

answers: the same time

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: How would you describe compressive stresses?

answers: NDQ_003376

answers: compressive forces

answers: NDQ_003378

answers: What is the amount the ground moves in an earthquake?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: Which of the following is not a type of force: gravity, muscle action, or skin folds?

answers: NDQ_003381

answers: What happens to rock when confining stress occurs?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: Fault zone

answers: NDQ_003386

answers: movement of rock at faults

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: normal faults or gravity?

answers: NDQ_003388

answers: Which of the following is not a cause of strike-slip faults?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: ileocecal fold

answers: NDQ_003391

answers: dip-slip fault plane

answers: NDQ_003392

answers: The hanging wall pushes up relative to the footwall

answers: NDQ_003393

answers: dip-slip fault plane

answers: NDQ_003394

answers: lateral

answers: NDQ_003395

answers: Fault with a vertical fault plane

answers: NDQ_003396

answers: Fault plane

answers: NDQ_003351

answers: gravity.

answers: NDQ_003352

answers: gravity.

answers: NDQ_003353

answers: gravity.

answers: NDQ_003354

answers: Skin folds

answers: NDQ_003355

answers: ileocecal fold

answers: NDQ_003356

answers: gravity.

answers: NDQ_003357

answers: gravity.

answers: NDQ_003358

answers: Skin folds

answers: NDQ_003359

answers: external force,

answers: NDQ_003360

answers: gravity.

answers: NDQ_003362

answers: Skin folds

answers: NDQ_003363

answers: gravity.

answers: NDQ_003371

answers: Skin folds

answers: NDQ_003373

answers: gravity.

answers: NDQ_003376

answers: gravity.

answers: NDQ_003378

answers: gravity.

answers: NDQ_003379

answers: gravity.

answers: NDQ_003380

answers: gravity.

answers: NDQ_003381

answers: gravity.

answers: NDQ_003382

answers: gravity.

answers: NDQ_003383

answers: gravity.

answers: NDQ_003384

answers: gravity.

answers: NDQ_003385

answers: ileocecal fold

answers: NDQ_003386

answers: Skin folds

answers: NDQ_003387

answers: gravity.

answers: NDQ_003388

answers: arbitrary application of force

answers: NDQ_003389

answers: Skin folds

answers: NDQ_003390

answers: gravity.

answers: NDQ_003391

answers: ileocecal fold

answers: NDQ_003392

answers: gravity.

answers: NDQ_003393

answers: ileocecal fold

answers: NDQ_003394

answers: gravity.

answers: NDQ_003395

answers: gravity.

answers: NDQ_003396

answers: gravity.

text: For a given g-force the stresses are the same, regardless of whether this g-force is caused by mechanical resistance to gravity, or by a coordinate-acceleration (change in velocity) caused by a mechanical force, or by a combination of these. Hence, for people all mechanical forces feels exactly the same whether they cause coordinate acceleration or not. For objects likewise, the question of whether they can withstand the mechanical g-force without damage is the same for any type of g-force. For example, upward acceleration (e.g., increase of speed when going up or decrease of speed when going down) on Earth feels the same as being stationary on a celestial body with a higher surface gravity. Again, one should note that gravitation acting alone does not produce any g-force; g-force is only produced from mechanical pushes and pulls. For a free body (one that is free to move in space) such g-forces only arise as the "inertial" path that is the natural effect of gravitation, or the natural effect of the inertia of mass, is modified. Such modification may only arise from influences other than gravitation.

text: For a given g-force the stresses are the same, regardless of whether this g-force is caused by mechanical resistance to gravity, or by a coordinate-acceleration (change in velocity) caused by a mechanical force, or by a combination of these. Hence, for people all mechanical forces feels exactly the same whether they cause coordinate acceleration or not. For objects likewise, the question of whether they can withstand the mechanical g-force without damage is the same for any type of g-force. For example, upward acceleration (e.g., increase of speed when going up or decrease of speed when going down) on Earth feels the same as being stationary on a celestial body with a higher

text: surface gravity

text: . Again, one should note that gravitation acting alone does not produce any g-force; g-force is only produced from mechanical pushes and pulls. For a free body (one that is free to move in space) such g-forces only arise as the "inertial" path that is the natural effect of gravitation, or the natural effect of the inertia of mass, is modified. Such modification may only arise from influences other than gravitation.

answers: NDQ_003351

answers: g-force

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: damage

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: downward

answers: NDQ_003356

answers: break apart

answers: NDQ_003357

answers: gravitation acting alone does not produce any g-force

answers: NDQ_003358

answers: stationary

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth

answers: NDQ_003362

answers: gravity acting alone does not produce any g-force

answers: NDQ_003363

answers: a higher surface gravity

answers: NDQ_003371

answers: how old rocks are above much younger rocks

answers: NDQ_003373

answers: g-force

answers: NDQ_003376

answers: for people all mechanical forces feels exactly the same whether they cause coordinate acceleration or not

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: vertical

answers: NDQ_003380

answers: For a given G-force the stresses are the same

answers: NDQ_003381

answers: the same for any type of g-force

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: syncline

answers: NDQ_003385

answers: fault zone

answers: NDQ_003386

answers: movement of rock at faults is the cause of earthquakes

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: shear stress

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: unanswerable

answers: NDQ_003391

answers: is a free body

answers: NDQ_003392

answers: upward acceleration

answers: NDQ_003393

answers: a dip-slip fault

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: a vertical fault plane

answers: NDQ_003396

answers: horizontal

answers: NDQ_003351

answers: mechanical resistance to gravity,

answers: NDQ_003352

answers: damage

answers: NDQ_003353

answers: damage

answers: NDQ_003354

answers: gravitation acting alone does not produce any g-force;

answers: NDQ_003355

answers: upward acceleration

answers: NDQ_003356

answers: damage

answers: NDQ_003357

answers: g-force is only produced from mechanical pushes and pulls.

answers: NDQ_003358

answers: stationary

answers: NDQ_003359

answers: gravitation acting alone does not produce any g-force;

answers: NDQ_003360

answers: gravity,

answers: NDQ_003362

answers: gravitation acting alone does not produce any g-force;

answers: NDQ_003363

answers: Earth

answers: NDQ_003371

answers: For a given g-force

answers: NDQ_003373

answers: For a given g-force

answers: NDQ_003376

answers: gravitation acting alone does not produce any g-force;

answers: NDQ_003378

answers: gravitation acting alone does not produce any g-force;

answers: NDQ_003379

answers: gravitation acting alone does not produce any g-force;

answers: NDQ_003380

answers: the question of whether they can withstand the mechanical g-force

answers: NDQ_003381

answers: the question of whether they can withstand the mechanical g-force

answers: NDQ_003382

answers: mechanical resistance to gravity,

answers: NDQ_003383

answers: mechanical resistance to gravity,

answers: NDQ_003384

answers: upward acceleration

answers: NDQ_003385

answers: For a given g-force

answers: NDQ_003386

answers: gravitation acting alone does not produce any g-force;

answers: NDQ_003387

answers: gravitation acting alone does not produce any g-force;

answers: NDQ_003388

answers: gravitation acting alone does not produce any g-force;

answers: NDQ_003389

answers: gravitation acting alone does not produce any g-force;

answers: NDQ_003390

answers: mechanical resistance to gravity,

answers: NDQ_003391

answers: mechanical g-force

answers: NDQ_003392

answers: upward acceleration

answers: NDQ_003393

answers: gravitation acting alone does not produce any g-force;

answers: NDQ_003394

answers: For a given g-force

answers: NDQ_003395

answers: For a given g-force

answers: NDQ_003396

answers: For a given g-force

text: Evidence exists in rats that the stress levels of the mother can also have an effect on fetal development. As Ellis & Cole-Harding (2001) outline, the chain of events in prenatal stress affecting brain sex differentiation appears to be that stress causes the mother's adrenal glands to release high levels of stress hormones into the blood system, substantial proportions of which cross the placental barrier and interfere with the fetus' production of sex hormones temporarily, most notably testosterone. These results have been applied to human sexual orientation, although studies of maternal stress often lack generalizability due to small sample sizes and the inherent difficulty of accurately measuring stress levels in pregnancy. Criticisms of this study outline that subprimate mammals are invalid measures of human sexual differentiation, as sex hormones follow a more "on-off" role in sex-typed behavior than is found in primates.

text: Evidence exists in rats that the stress levels of the mother can also have an effect on fetal development. As Ellis & Cole-Harding (2001) outline, the chain of events in prenatal stress affecting brain sex differentiation appears to be that stress causes the mother's adrenal glands to release high levels of stress hormones into the blood system, substantial proportions of which cross the placental barrier and interfere with the fetus' production of sex hormones temporarily, most notably testosterone. These results have been applied to human sexual orientation, although studies of maternal stress often lack generalizability due to small sample sizes and the inherent difficulty of accurately measuring stress levels in pregnancy. Criticisms of this study outline that subprimate mammals are invalid measures of human sexual differentiation, as sex hormones follow a more "on-off" role in sex-typed behavior than is found in primates.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: is more likely to crack

answers: NDQ_003353

answers: high levels of stress hormones

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: swell

answers: NDQ_003357

answers: sex hormones follow a more "on-off" role

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: subprimate mammals are invalid measures of human sexual differentiation

answers: NDQ_003363

answers: prenatal stress

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: How would you describe the stress?

answers: NDQ_003376

answers: basin-and-range

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What is a stress?

answers: NDQ_003381

answers: what is the last word in the passage?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: movement of rock at faults

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: normal faults or stress hormones?

answers: NDQ_003388

answers: Which of the following is not a result of shear stress?

answers: NDQ_003389

answers: mountains

answers: NDQ_003390

answers: subprimate

answers: NDQ_003391

answers: subprimate

answers: NDQ_003392

answers: subprimate mammals

answers: NDQ_003393

answers: subprimate

answers: NDQ_003394

answers: subprimate

answers: NDQ_003395

answers: NDQ_003396

answers: subprimate

answers: NDQ_003351

answers: testosterone.

answers: NDQ_003352

answers: high levels of stress hormones

answers: NDQ_003353

answers: mother's adrenal glands to release high levels of stress hormones

answers: NDQ_003354

answers: stress levels of the mother can also have an effect on fetal development.

answers: NDQ_003355

answers: fetal development.

answers: NDQ_003356

answers: fetal development.

answers: NDQ_003357

answers: interfere with the fetus'

answers: NDQ_003358

answers: Evidence exists in rats

answers: NDQ_003359

answers: stress levels of the mother can also have an effect on fetal development.

answers: NDQ_003360

answers: stress levels of the mother

answers: NDQ_003362

answers: high levels of stress hormones

answers: NDQ_003363

answers: stress levels of the mother can also have an effect on fetal development.

answers: NDQ_003371

answers: stress levels of the mother can also have an effect on fetal development.

answers: NDQ_003373

answers: Evidence exists in rats

answers: NDQ_003376

answers: stress levels of the mother can also have an effect on fetal development.

answers: NDQ_003378

answers: stress levels of the mother can also have an effect on fetal development.

answers: NDQ_003379

answers: stress levels of the mother can also have an effect on fetal development.

answers: NDQ_003380

answers: stress levels of the mother can also have an effect on fetal development.

answers: NDQ_003381

answers: cross the placental barrier

answers: NDQ_003382

answers: stress levels of the mother can also have an effect on fetal development.

answers: NDQ_003383

answers: stress causes the mother's adrenal glands

answers: NDQ_003384

answers: fetal development.

answers: NDQ_003385

answers: stress levels of the mother can also have an effect on fetal development.

answers: NDQ_003386

answers: stress levels of the mother can also have an effect on fetal development.

answers: NDQ_003387

answers: high levels of stress hormones

answers: NDQ_003388

answers: stress levels of the mother can also have an effect on fetal development.

answers: NDQ_003389

answers: stress levels of the mother can also have an effect on fetal development.

answers: NDQ_003390

answers: stress levels of the mother can also have an effect on fetal development.

answers: NDQ_003391

answers: placental barrier

answers: NDQ_003392

answers: stress levels of the mother can also have an effect on fetal development.

answers: NDQ_003393

answers: fetal development.

answers: NDQ_003394

answers: Evidence exists in rats

answers: NDQ_003395

answers: stress levels of the mother can also have an effect on fetal development.

answers: NDQ_003396

answers: stress levels of the mother can also have an effect on fetal development.

text: Although mutations that cause changes in protein sequences can be harmful to an organism, on occasions the effect may be positive in a given environment. In this case, the mutation may enable the mutant organism to withstand particular environmental stresses better than wild-type organisms, or reproduce more quickly. In these cases a mutation will tend to become more common in a population through natural selection.

text: Although mutations that cause changes in protein sequences can be harmful to an organism, on occasions the effect may be positive in a given environment. In this case, the mutation may enable the mutant organism to withstand particular environmental stresses better than wild-type organisms, or reproduce more quickly. In these cases a mutation will tend to become more common in a population through natural selection.

answers: NDQ_003351

answers: mutation

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: mutations

answers: NDQ_003354

answers: Toroweap Formation is above the Kaibab Limestone

answers: NDQ_003355

answers: fold

answers: NDQ_003356

answers: withstand particular environmental stresses

answers: NDQ_003357

answers: mutations that cause changes in protein sequences can be harmful

answers: NDQ_003358

answers: rockfall

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: natural causes

answers: NDQ_003362

answers: wild-type organisms, or reproduce more quickly.

answers: NDQ_003363

answers: the same time

answers: NDQ_003371

answers: What is the best way to describe a thrust fault?

answers: NDQ_003373

answers: a mutation may enable the mutant organism to withstand

answers: NDQ_003376

answers: basin-and-range

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: vertical

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: mutations that cause changes in protein sequences

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: mutations

answers: NDQ_003384

answers: What type of fold is a syncline?

answers: NDQ_003385

answers: Fault zone

answers: NDQ_003386

answers: faults

answers: NDQ_003387

answers: None of the above choices.

answers: NDQ_003388

answers: What is shear stress?

answers: NDQ_003389

answers: mutations

answers: NDQ_003390

answers: A fault in which the hanging wall drops down relative to the footwall

answers: NDQ_003391

answers: dip-slip fault

answers: NDQ_003392

answers: the hanging wall

answers: NDQ_003393

answers: dip-slip fault

answers: NDQ_003394

answers: isosceles

answers: NDQ_003395

answers: is called a vertical fault

answers: NDQ_003396

answers: is a type of fault

answers: NDQ_003351

answers: mutations that cause changes in protein sequences

answers: NDQ_003352

answers: withstand particular environmental stresses better than wild-type organisms,

answers: NDQ_003353

answers: mutations that cause changes in protein sequences

answers: NDQ_003354

answers: positive in a given environment.

answers: NDQ_003355

answers: mutations that cause changes in protein sequences

answers: NDQ_003356

answers: withstand particular environmental stresses

answers: NDQ_003357

answers: withstand particular environmental stresses better than wild-type organisms,

answers: NDQ_003358

answers: mutations that cause changes in protein sequences

answers: NDQ_003359

answers: stresses

answers: NDQ_003360

answers: mutations

answers: NDQ_003362

answers: mutant organism to withstand particular environmental stresses better than wild-type organisms,

answers: NDQ_003363

answers: mutations

answers: NDQ_003371

answers: mutations that cause changes in protein sequences

answers: NDQ_003373

answers: withstand particular environmental stresses

answers: NDQ_003376

answers: the mutation may enable the mutant organism to withstand particular environmental stresses

answers: NDQ_003378

answers: mutations that cause changes in protein sequences

answers: NDQ_003379

answers: the mutation may enable the mutant organism to withstand particular environmental stresses

answers: NDQ_003380

answers: stresses

answers: NDQ_003381

answers: the mutation may enable the mutant organism to withstand particular environmental stresses

answers: NDQ_003382

answers: the mutation may enable the mutant organism to withstand particular environmental stresses

answers: NDQ_003383

answers: stresses

answers: NDQ_003384

answers: mutations that cause changes in protein sequences

answers: NDQ_003385

answers: mutations that cause changes in protein sequences

answers: NDQ_003386

answers: mutations that cause changes in protein sequences

answers: NDQ_003387

answers: the mutation may enable the mutant organism to withstand particular environmental stresses

answers: NDQ_003388

answers: the mutation may enable the mutant organism to withstand particular environmental stresses

answers: NDQ_003389

answers: mutations that cause changes in protein sequences

answers: NDQ_003390

answers: mutations that cause changes in protein sequences

answers: NDQ_003391

answers: mutations that cause changes in protein sequences

answers: NDQ_003392

answers: mutations that cause changes in protein sequences

answers: NDQ_003393

answers: mutations that cause changes in protein sequences

answers: NDQ_003394

answers: mutations that cause changes in protein sequences

answers: NDQ_003395

answers: mutations that cause changes in protein sequences

answers: NDQ_003396

answers: mutations that cause changes in protein sequences

text: The geological structure of Great Britain is complex, resulting as it does from a long and varied geological history spanning more than two billion years. This piece of the Earth's crust has experienced several episodes of mountain building or 'orogenies', each of which has added further complexity to the picture.

text: The geological structure of

text: Great Britain

text: is complex, resulting as it does from a long and varied

text: geological history

text: spanning more than two billion years. This piece of the Earth's

text: crust

text: has experienced several episodes of mountain building or '

text: orogenies

text: ', each of which has added further complexity to the picture.

answers: NDQ_003351

answers: unanswerable

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: orogeny

answers: NDQ_003356

answers: build mountains

answers: NDQ_003357

answers: mountains are formed by the movement of

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: the San Andreas fault is the only fault in the world

answers: NDQ_003363

answers: two billion years ago

answers: NDQ_003371

answers: Which of the following is not a type of mountain building?

answers: NDQ_003373

answers: What is the best title for this passage?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: what is the first type of stress mentioned?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: what is the first word in the first paragraph?

answers: NDQ_003386

answers: Which of the following is not a cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not a type of mountain building?

answers: NDQ_003388

answers: Which of the following is not a result of shear stress: strike-slip faults, orogenies

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: orogeny

answers: NDQ_003391

answers: unanswerable

answers: NDQ_003392

answers: orogeny

answers: NDQ_003393

answers: mountain

answers: NDQ_003394

answers: horizontal

answers: NDQ_003395

answers: unanswerable

answers: NDQ_003396

answers: NDQ_003351

answers: mountain building

answers: NDQ_003352

answers: mountain building

answers: NDQ_003353

answers: mountain building

answers: NDQ_003354

answers: The geological structure of Great Britain

answers: NDQ_003355

answers: 'orogenies',

answers: NDQ_003356

answers: mountain building

answers: NDQ_003357

answers: mountain building

answers: NDQ_003358

answers: 'orogenies',

answers: NDQ_003359

answers: mountain building

answers: NDQ_003360

answers: 'orogenies',

answers: NDQ_003362

answers: The geological structure of Great Britain

answers: NDQ_003363

answers: 'orogenies',

answers: NDQ_003371

answers: two billion years.

answers: NDQ_003373

answers: two billion years.

answers: NDQ_003376

answers: mountain building

answers: NDQ_003378

answers: mountain building

answers: NDQ_003379

answers: two billion years.

answers: NDQ_003380

answers: mountain building

answers: NDQ_003381

answers: mountain building

answers: NDQ_003382

answers: two billion years.

answers: NDQ_003383

answers: mountain building

answers: NDQ_003384

answers: mountain building or 'orogenies',

answers: NDQ_003385

answers: a long and varied geological history spanning more than two billion years.

answers: NDQ_003386

answers: mountain building

answers: NDQ_003387

answers: two billion years.

answers: NDQ_003388

answers: two billion years.

answers: NDQ_003389

answers: 'orogenies',

answers: NDQ_003390

answers: mountain building or 'orogenies',

answers: NDQ_003391

answers: mountain building or 'orogenies',

answers: NDQ_003392

answers: 'orogenies',

answers: NDQ_003393

answers: mountain

answers: NDQ_003394

answers: mountain building or 'orogenies',

answers: NDQ_003395

answers: The geological structure of Great Britain

answers: NDQ_003396

answers: mountain building or 'orogenies',

text: The Trans-Hudson orogeny was the culminating event of the Paleoproterozoic Laurentian assembly, which occurred after the Wopmay orogeny (West of Hudson Bay, ca. 2.1-1.9 Ga.).  The Trans-Hudson orogeny resulted from the collision of the Superior Craton of eastern Canada with the Hearne Craton in northern Saskatchewan and the Wyoming Craton of the western United States, with the Archean microcontinent Sask Craton trapped in the THO western interior. Similar to the Himalayas, the Trans-Hudson orogeny was also the result of continent-continent collision along a suture zone.  Only the roots of this mountain chain remain, but these can be seen in northeastern Saskatchewan and in the Black Hills of South Dakota.  The Trans-Hudson orogeny and the consequent upheaval of the continental crust in the middle Proterozoic eon caused the area around the Great Lakes to become a flattened plain, which in turn led to the creation of the intercontinental basin and the interior and central plains of the United States (the Great Plains are the westernmost portion of North America's Interior Plains, which extend east to the Appalachian Plateau).

text: The Trans-Hudson orogeny was the culminating event of the Paleoproterozoic Laurentian assembly, which occurred after the

text: Wopmay orogen

text: y (West of

text: Hudson Bay

text: , ca. 2.1-1.9 Ga.).  The Trans-Hudson orogeny resulted from the collision of the Superior Craton of eastern

text: Canada

text: with the Hearne Craton in northern

text: Saskatchewan

text: and the Wyoming Craton of the western

text: United States

text: , with the

text: Archean

text: microcontinent

text: Sask Craton

text: trapped in the THO western interior. Similar to the Himalayas, the Trans-Hudson orogeny was also the result of continent-continent collision along a suture zone.  Only the roots of this mountain chain remain, but these can be seen in northeastern Saskatchewan and in the Black Hills of South Dakota.  The Trans-Hudson orogeny and the consequent upheaval of the continental crust in the middle Proterozoic eon caused the area around the

text: Great Lakes

text: to become a flattened plain, which in turn led to the creation of the intercontinental basin and the interior and central plains of the

text: United States

text: (the

text: Great Plains

text: are the westernmost portion of North America's

text: Interior Plains

text: , which extend east to the

text: Appalachian Plateau

answers: NDQ_003351

answers: suture zone

answers: NDQ_003352

answers: flattens

answers: NDQ_003353

answers: upheaval

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: suture zone

answers: NDQ_003356

answers: flatten

answers: NDQ_003357

answers: continent-continent collision along a suture zone

answers: NDQ_003358

answers: suture zone

answers: NDQ_003359

answers: collision

answers: NDQ_003360

answers: continent-continent collision

answers: NDQ_003362

answers: only the roots of this mountain chain remain, but these can be seen in northeastern Saskatchewan and in the Black Hills of South Dakota

answers: NDQ_003363

answers: Trans-Hudson orogeny

answers: NDQ_003371

answers: What was the result of continent-continent collision?

answers: NDQ_003373

answers: What is the result of continent-continent collision along a suture zone?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: What was the result of continent-continent collision along a suture zone

answers: NDQ_003380

answers: What was the result of continent-continent collision along a suture zone?

answers: NDQ_003381

answers: What caused the area around the Great Lakes to become a flattened plain?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What was the result of continent-continent collision along a suture zone?

answers: NDQ_003385

answers: what is the trans-Hudson orogeny

answers: NDQ_003386

answers: upheaval of the continental crust

answers: NDQ_003387

answers: What was the result of continent-continent collision along a suture zone?

answers: NDQ_003388

answers: What was the result of continent-continent collision along a suture zone?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: a suture zone

answers: NDQ_003391

answers: Superior Craton

answers: NDQ_003392

answers: a suture zone

answers: NDQ_003393

answers: Superior Craton

answers: NDQ_003394

answers: trans-Hudson orogeny

answers: NDQ_003395

answers: Trans-Hudson orogeny

answers: NDQ_003396

answers: a suture zone

answers: NDQ_003351

answers: continent-continent collision along a suture zone.

answers: NDQ_003352

answers: flattened

answers: NDQ_003353

answers: upheaval

answers: NDQ_003354

answers: Black Hills of South Dakota.

answers: NDQ_003355

answers: suture zone.

answers: NDQ_003356

answers: flattened

answers: NDQ_003357

answers: suture zone.

answers: NDQ_003358

answers: suture zone.

answers: NDQ_003359

answers: continent-continent collision along a suture zone.

answers: NDQ_003360

answers: continent-continent collision along a suture zone.

answers: NDQ_003362

answers: The Trans-Hudson orogeny

answers: NDQ_003363

answers: continent-continent collision along a suture zone.

answers: NDQ_003371

answers: suture zone.

answers: NDQ_003373

answers: Hearne Craton

answers: NDQ_003376

answers: intercontinental basin

answers: NDQ_003378

answers: upheaval

answers: NDQ_003379

answers: Hearne Craton

answers: NDQ_003380

answers: upheaval

answers: NDQ_003381

answers: upheaval

answers: NDQ_003382

answers: continent-continent collision along a suture zone.

answers: NDQ_003383

answers: continent-continent collision along a suture zone.

answers: NDQ_003384

answers: suture zone.

answers: NDQ_003385

answers: suture zone.

answers: NDQ_003386

answers: upheaval

answers: NDQ_003387

answers: continent-continent collision along a suture zone.

answers: NDQ_003388

answers: continent-continent collision along a suture zone.

answers: NDQ_003389

answers: continent-continent collision along a suture zone.

answers: NDQ_003390

answers: suture zone.

answers: NDQ_003391

answers: suture zone.

answers: NDQ_003392

answers: suture zone.

answers: NDQ_003393

answers: suture zone.

answers: NDQ_003394

answers: continent-continent collision along a suture zone.

answers: NDQ_003395

answers: continent-continent collision along a suture zone.

answers: NDQ_003396

answers: suture zone.

text: Plates include both oceanic crust and continental crust. Stable subduction zones involve the oceanic lithosphere of one plate sliding beneath the continental or oceanic lithosphere of another plate due to the higher density of the oceanic lithosphere. That is, the subducted lithosphere is always oceanic while the overriding lithosphere may or may not be oceanic. Subduction zones are sites that have a high rate of volcanism, earthquakes, and mountain building.

text: Plates include both

text: oceanic crust

text: and

text: continental crust

text: . Stable subduction zones involve the oceanic

text: lithosphere

text: of one plate sliding beneath the continental or oceanic lithosphere of another plate due to the higher density of the oceanic lithosphere. That is, the subducted lithosphere is always oceanic while the overriding lithosphere may or may not be oceanic. Subduction zones are sites that have a high rate of

text: volcanism

text: earthquake

text: s, and

text: mountain building

answers: NDQ_003351

answers: subduction

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: earthquakes

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: continental fold

answers: NDQ_003356

answers: subduct

answers: NDQ_003357

answers: the overriding lithosphere may or may not be oceanic

answers: NDQ_003358

answers: unanswerable

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: Subduction zones

answers: NDQ_003362

answers: the subducted lithosphere is always oceanic

answers: NDQ_003363

answers: Subduction zones

answers: NDQ_003371

answers: Which of the following is not a type of crust: oceanic crust or continental crust?

answers: NDQ_003373

answers: what is the last word in the passage?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: Which of the following is not a type of stress?

answers: NDQ_003381

answers: What type of rock deforms?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is the name of the area where faults are clustered?

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: Which of the following is not caused by compression stress: normal faults, earthquakes, or mountain building?

answers: NDQ_003388

answers: Which of the following is not a type of fault: Stable subduction zones or strike-slip faults?

answers: NDQ_003389

answers: Subduction zones

answers: NDQ_003390

answers: subduction zone

answers: NDQ_003391

answers: continental crust

answers: NDQ_003392

answers: subduction zone

answers: NDQ_003393

answers: continental crust

answers: NDQ_003394

answers: subduction zone

answers: NDQ_003395

answers: unanswerable

answers: NDQ_003396

answers: subduction zone

answers: NDQ_003351

answers: volcanism,

answers: NDQ_003352

answers: mountain building.

answers: NDQ_003353

answers: earthquakes,

answers: NDQ_003354

answers: Subduction zones

answers: NDQ_003355

answers: subduction zones

answers: NDQ_003356

answers: earthquakes, and mountain building.

answers: NDQ_003357

answers: higher density of the oceanic lithosphere.

answers: NDQ_003358

answers: Subduction zones are sites that have a high rate of volcanism,

answers: NDQ_003359

answers: higher density of the oceanic lithosphere.

answers: NDQ_003360

answers: subduction zones

answers: NDQ_003362

answers: the subducted lithosphere is always oceanic

answers: NDQ_003363

answers: Subduction zones

answers: NDQ_003371

answers: Stable subduction zones

answers: NDQ_003373

answers: Subduction zones

answers: NDQ_003376

answers: Stable subduction zones

answers: NDQ_003378

answers: Subduction zones

answers: NDQ_003379

answers: Stable subduction zones

answers: NDQ_003380

answers: earthquakes, and mountain building.

answers: NDQ_003381

answers: Subduction zones

answers: NDQ_003382

answers: subduction zones

answers: NDQ_003383

answers: Stable subduction zones

answers: NDQ_003384

answers: Stable subduction zones

answers: NDQ_003385

answers: Subduction zones

answers: NDQ_003386

answers: Subduction zones

answers: NDQ_003387

answers: Stable subduction zones

answers: NDQ_003388

answers: Stable subduction zones

answers: NDQ_003389

answers: Subduction zones

answers: NDQ_003390

answers: subduction zones

answers: NDQ_003391

answers: subduction zones

answers: NDQ_003392

answers: subduction zones

answers: NDQ_003393

answers: mountain building.

answers: NDQ_003394

answers: Stable subduction zones

answers: NDQ_003395

answers: subduction zones

answers: NDQ_003396

answers: Stable subduction zones

text: The Mount Edziza volcanic complex began forming about 7.5 million years ago and has grown steadily since then. Like other volcanoes in northwestern British Columbia, the Mount Edziza volcanic complex has its origins in continental rifting—a long divergent plate boundary where the lithosphere is being pulled apart. Here, the continental crust of the North American Plate is being stretched at a rate of about  per year. This incipient rifting has formed as a result of the Pacific Plate sliding northward along the Queen Charlotte Fault, on its way to the Aleutian Trench, which extends along the southern coastline of Alaska and the adjacent waters of northeastern Siberia off the coast of Kamchatka Peninsula. As the continental crust stretches, the  near-surface rocks fracture along steeply dipping cracks parallel to the rift known as faults. Hot basaltic magma rises along these fractures to create passive lava eruptions, known as effusive eruptions.

text: The Mount Edziza volcanic complex began forming about 7.5 million years ago and has grown steadily since then. Like other volcanoes in northwestern British Columbia, the Mount Edziza volcanic complex has its origins in

text: continent

text: al

text: rift

text: ing—a long

text: divergent plate boundary

text: where the

text: lithosphere

text: is being pulled apart. Here, the

text: continental crust

text: of the

text: North American Plate

text: is being stretched at a rate of about  per year. This incipient rifting has formed as a result of the

text: Pacific Plate

text: sliding northward along the

text: Queen Charlotte Fault

text: , on its way to the

text: Aleutian Trench

text: , which extends along the southern coastline of

text: Alaska

text: and the adjacent waters of northeastern

text: Siberia

text: off the coast of

text: Kamchatka Peninsula

text: . As the continental crust stretches, the  near-surface rocks fracture along steeply dipping cracks parallel to the rift known as

text: faults

text: . Hot

text: basalt

text: ic

text: magma

text: rises along these fractures to create passive lava eruptions, known as

text: effusive eruption

text: s.

answers: NDQ_003351

answers: Faults

answers: NDQ_003352

answers: fractures

answers: NDQ_003353

answers: fractures

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: Fault

answers: NDQ_003356

answers: crack

answers: NDQ_003357

answers: steeply dipping cracks parallel to the rift

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: as the continental crust stretches

answers: NDQ_003360

answers: continental faults

answers: NDQ_003362

answers: unanswerable

answers: NDQ_003363

answers: continental rifting

answers: NDQ_003371

answers: Which of the following is not a rift fault: Queen Charlotte Fault, Aleutian Trench or Kamchatka Peninsula?

answers: NDQ_003373

answers: What is the cause of the Aleutian Trench?

answers: NDQ_003376

answers: Which of the following is not caused by compressive forces: basin-and-range?

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: no

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What is the opposite of rifting?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not a type of fold?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: Which of the following is not a normal fault: compression stress, rifting or lava eruptions?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip faults or effusive eruptions?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: Queen Charlotte Fault

answers: NDQ_003391

answers: lithosphere

answers: NDQ_003392

answers: Queen Charlotte Fault

answers: NDQ_003393

answers: surface rocks

answers: NDQ_003394

answers: steeply dipping cracks

answers: NDQ_003395

answers: Queen Charlotte Fault

answers: NDQ_003396

answers: Queen Charlotte Fault

answers: NDQ_003351

answers: faults.

answers: NDQ_003352

answers: fracture

answers: NDQ_003353

answers: fracture along steeply dipping cracks

answers: NDQ_003354

answers: faults.

answers: NDQ_003355

answers: faults.

answers: NDQ_003356

answers: fracture along steeply dipping cracks

answers: NDQ_003357

answers: steeply dipping cracks

answers: NDQ_003358

answers: faults.

answers: NDQ_003359

answers: As the continental crust stretches,

answers: NDQ_003360

answers: continental rifting—a

answers: NDQ_003362

answers: Queen Charlotte Fault,

answers: NDQ_003363

answers: continental rifting—a

answers: NDQ_003371

answers: faults.

answers: NDQ_003373

answers: faults.

answers: NDQ_003376

answers: faults.

answers: NDQ_003378

answers: faults.

answers: NDQ_003379

answers: steeply dipping

answers: NDQ_003380

answers: faults.

answers: NDQ_003381

answers: faults.

answers: NDQ_003382

answers: faults.

answers: NDQ_003383

answers: faults.

answers: NDQ_003384

answers: faults.

answers: NDQ_003385

answers: steeply dipping cracks parallel to the rift

answers: NDQ_003386

answers: fracture along steeply dipping cracks

answers: NDQ_003387

answers: steeply dipping cracks

answers: NDQ_003388

answers: steeply dipping cracks

answers: NDQ_003389

answers: continental rifting—a

answers: NDQ_003390

answers: Queen Charlotte Fault,

answers: NDQ_003391

answers: near-surface rocks

answers: NDQ_003392

answers: Queen Charlotte Fault,

answers: NDQ_003393

answers: near-surface

answers: NDQ_003394

answers: steeply dipping cracks

answers: NDQ_003395

answers: steeply dipping cracks parallel to the rift

answers: NDQ_003396

answers: Queen Charlotte Fault,

text: The Farallon Basin has a spreading axis at its center, so the seafloor here is oceanic crust, transitioning into thin, rifted continental crust at the basin's edges. Spreading centers in the Gulf, like this one in Farallon, are different from more well known spreading axes like the Mid-Atlantic Ridge and East Pacific Rise, since they form as deep rift valleys rather than bathymetric highs.

text: The Farallon Basin has a spreading axis at its center, so the seafloor here is

text: oceanic crust

text: , transitioning into thin, rifted continental crust at the basin's edges. Spreading centers in the Gulf, like this one in Farallon, are different from more well known spreading axes like the

text: Mid-Atlantic Ridge

text: and

text: East Pacific Rise

text: , since they form as deep rift valleys rather than bathymetric highs.

answers: NDQ_003351

answers: continental crust

answers: NDQ_003352

answers: cracks

answers: NDQ_003353

answers: rifts

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: rift valley

answers: NDQ_003356

answers: change shape

answers: NDQ_003357

answers: oceanic crust transitions into thin, rifted continental crust at the basin's edges

answers: NDQ_003358

answers: rift valley

answers: NDQ_003359

answers: fractures

answers: NDQ_003360

answers: continental crust

answers: NDQ_003362

answers: bathymetric highs

answers: NDQ_003363

answers: Farallon

answers: NDQ_003371

answers: Which of the following is not a type of spreading axis?

answers: NDQ_003373

answers: Why is the Farallon Basin different from other spreading axes?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: what is the last word in the passage?

answers: NDQ_003379

answers: Which of the following is not a type of strike-slip fault?

answers: NDQ_003380

answers: Which of the following is not a stress?

answers: NDQ_003381

answers: What type of stress does the Farallon Basin experience?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not a type of fold: Mid-Atlantic Ridge or East Pacific Rise?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: Which of the following is not a cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not a type of normal fault?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip, Mid-Atlantic Ridge or East Pacific Rise?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: rift valleys

answers: NDQ_003391

answers: seafloor

answers: NDQ_003392

answers: rift valley

answers: NDQ_003393

answers: oceanic crust

answers: NDQ_003394

answers: rift valley

answers: NDQ_003395

answers: a spreading axis

answers: NDQ_003396

answers: unanswerable

answers: NDQ_003351

answers: bathymetric highs.

answers: NDQ_003352

answers: deep rift valleys rather than bathymetric highs.

answers: NDQ_003353

answers: rifted

answers: NDQ_003354

answers: The Farallon Basin has a spreading axis

answers: NDQ_003355

answers: spreading axis

answers: NDQ_003356

answers: deep rift valleys rather than bathymetric highs.

answers: NDQ_003357

answers: bathymetric highs.

answers: NDQ_003358

answers: bathymetric highs.

answers: NDQ_003359

answers: rifted continental crust

answers: NDQ_003360

answers: spreading axis

answers: NDQ_003362

answers: bathymetric highs.

answers: NDQ_003363

answers: bathymetric highs.

answers: NDQ_003371

answers: The Farallon Basin has a spreading axis

answers: NDQ_003373

answers: deep rift valleys rather than bathymetric highs.

answers: NDQ_003376

answers: deep rift valleys rather than bathymetric highs.

answers: NDQ_003378

answers: The Farallon Basin has a spreading axis

answers: NDQ_003379

answers: Mid-Atlantic Ridge and East Pacific Rise,

answers: NDQ_003380

answers: oceanic crust,

answers: NDQ_003381

answers: spreading axis

answers: NDQ_003382

answers: spreading axis

answers: NDQ_003383

answers: rifted continental crust

answers: NDQ_003384

answers: spreading axis

answers: NDQ_003385

answers: Spreading centers

answers: NDQ_003386

answers: rifted continental crust

answers: NDQ_003387

answers: Mid-Atlantic Ridge and East Pacific Rise,

answers: NDQ_003388

answers: Mid-Atlantic Ridge

answers: NDQ_003389

answers: rift valleys rather than bathymetric highs.

answers: NDQ_003390

answers: The Farallon Basin has a spreading axis

answers: NDQ_003391

answers: oceanic crust,

answers: NDQ_003392

answers: The Farallon Basin has a spreading axis

answers: NDQ_003393

answers: bathymetric highs.

answers: NDQ_003394

answers: Mid-Atlantic Ridge and East Pacific Rise,

answers: NDQ_003395

answers: Mid-Atlantic Ridge and East Pacific Rise,

answers: NDQ_003396

answers: Mid-Atlantic Ridge and East Pacific Rise,

text: Many volcanoes produce deformational structures as they grow. The flanks of volcanoes commonly exhibit shallow gravity slumps, faults and associated folds. Large volcanoes grow not only by adding erupted material to their flanks, but also by spreading laterally at their bases, particularly if they rest on weak or ductile materials. As a volcano grows in size and weight, the stress field underneath the volcano changes from compressional to extensional. A subterranean rift may develop at the base of the volcano where the crust is wrenched apart. This volcanic spreading may initiate further structural deformation in the form of thrust faults along the volcano's distal flanks, pervasive grabens and normal faults across the edifice, and catastrophic flank failure (sector collapse). Mathematical analysis shows that volcanic spreading operates on volcanoes at a wide range of scales and is theoretically similar to the larger-scale rifting that occurs at mid-ocean ridges (divergent plate boundaries). Thus, in this view, the distinction between tectonic plate, spreading volcano, and rift is nebulous, all being part of the same geodynamic system.

text: Many volcanoes produce deformational

text: structures

text: as they grow. The flanks of volcanoes commonly exhibit shallow gravity slumps,

text: fault

text: s and associated

text: folds

text: . Large volcanoes grow not only by adding erupted material to their flanks, but also by spreading laterally at their bases, particularly if they rest on weak or

text: ductile

text: materials. As a volcano grows in size and weight, the

text: stress

text: field underneath the volcano changes from compressional to extensional. A subterranean rift may develop at the base of the volcano where the crust is wrenched apart. This volcanic spreading may initiate further structural deformation in the form of

text: thrust fault

text: s along the volcano's

text: distal

text: flanks, pervasive

text: graben

text: s and normal faults across the edifice, and catastrophic flank failure (sector collapse). Mathematical analysis shows that volcanic spreading operates on volcanoes at a wide range of scales and is theoretically similar to the larger-scale rifting that occurs at

text: mid-ocean ridge

text: s (

text: divergent plate boundaries

text: ). Thus, in this view, the distinction between

text: tectonic plate

text: , spreading volcano, and rift is nebulous, all being part of the same geodynamic system.

answers: NDQ_003351

answers: compressional

answers: NDQ_003352

answers: compresses

answers: NDQ_003353

answers: deformation

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: grabens

answers: NDQ_003356

answers: collapse

answers: NDQ_003357

answers: the stress field underneath the volcano changes from compressional to extensional

answers: NDQ_003358

answers: rift

answers: NDQ_003359

answers: weakens

answers: NDQ_003360

answers: plate boundaries

answers: NDQ_003362

answers: the distinction between tectonic plate, spreading volcano, and rift is nebulous

answers: NDQ_003363

answers: tectonic plate boundaries

answers: NDQ_003371

answers: Which of the following is not a type of structural deformation: thrust faults, pervasive grabens, or normal faults?

answers: NDQ_003373

answers: unanswerable

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What happens when a volcano grows in size and weight

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: unanswerable

answers: NDQ_003387

answers: unanswerable

answers: NDQ_003388

answers: Which of the following is not a result of shear stress: thrust faults, pervasive grabens, or normal faults?

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: thrust faults

answers: NDQ_003391

answers: unanswerable

answers: NDQ_003392

answers: thrust faults

answers: NDQ_003393

answers: grabens

answers: NDQ_003394

answers: laterally

answers: NDQ_003395

answers: thrust faults

answers: NDQ_003396

answers: thrust faults

answers: NDQ_003351

answers: rifting

answers: NDQ_003352

answers: compressional to extensional.

answers: NDQ_003353

answers: compressional to extensional.

answers: NDQ_003354

answers: Many volcanoes

answers: NDQ_003355

answers: folds.

answers: NDQ_003356

answers: thrust faults

answers: NDQ_003357

answers: across the edifice,

answers: NDQ_003358

answers: subterranean rift

answers: NDQ_003359

answers: weak or ductile materials.

answers: NDQ_003360

answers: weak or ductile materials.

answers: NDQ_003362

answers: rift

answers: NDQ_003363

answers: weak or ductile materials.

answers: NDQ_003371

answers: thrust faults

answers: NDQ_003373

answers: compressional to extensional.

answers: NDQ_003376

answers: compressional to extensional.

answers: NDQ_003378

answers: rift

answers: NDQ_003379

answers: subterranean rift

answers: NDQ_003380

answers: stress field underneath the volcano changes from compressional to extensional.

answers: NDQ_003381

answers: compressional to extensional.

answers: NDQ_003382

answers: compressional to extensional.

answers: NDQ_003383

answers: faults and associated folds.

answers: NDQ_003384

answers: folds.

answers: NDQ_003385

answers: faults and associated folds.

answers: NDQ_003386

answers: thrust faults

answers: NDQ_003387

answers: compressional to extensional.

answers: NDQ_003388

answers: thrust faults

answers: NDQ_003389

answers: Large volcanoes

answers: NDQ_003390

answers: thrust faults

answers: NDQ_003391

answers: subterranean rift

answers: NDQ_003392

answers: thrust faults

answers: NDQ_003393

answers: subterranean rift

answers: NDQ_003394

answers: thrust faults

answers: NDQ_003395

answers: thrust faults

answers: NDQ_003396

answers: thrust faults

text: Morton's 1959 paper touched on one of the most intriguing aspects of the geology of Oman: how oceanic crust, known as the Semail Ophiolite, came to occur all around the Hajar mountains and Jebel Akhdar, the "Green Mountain". The theory supported by Morton and others – Tschopp (1967) and Wilson (1969)) – was that these igneous rocks had essentially flowed into position. Lees (1928) had earlier proposed a huge thrust sheet, the Semail Nappe, based on his observations in the Oman Mountains, and on his knowledge of the Alps and of the Zagros. As evidence of plate tectonics grew, a development of Lees' theory (Glennie (1974)) emerged.  This postulated that, as the continents moved together, a slab of ocean crust from the ancient Tethys Ocean had been pushed over the continental margin for hundreds of kilometres about 87-76 million years ago. However, a leading proponent of the ‘in-situ’ theory, Hugh Wilson, observed that the major displacement surfaces were not prominent in the field and that he had seen more evidence of extension than compression in the Oman Mountains. Glennie (2001) remains a spirited critique of most of Wilson’s arguments. Almost all later authors interpret the Semail ophiolite as thrust, or obducted, probably due to a short period of subduction close to the margin of the Arabian plate.

text: Morton's 1959 paper touched on one of the most intriguing aspects of the geology of Oman: how oceanic crust, known as the

text: Semail Ophiolite

text: , came to occur all around the Hajar mountains and Jebel Akhdar, the "Green Mountain". The theory supported by Morton and others – Tschopp (1967) and Wilson (1969)) – was that these igneous rocks had essentially flowed into position. Lees (1928) had earlier proposed a huge thrust sheet, the Semail Nappe, based on his observations in the Oman Mountains, and on his knowledge of the Alps and of the Zagros. As evidence of plate tectonics grew, a development of Lees' theory (Glennie (1974)) emerged.  This postulated that, as the continents moved together, a slab of ocean crust from the ancient Tethys Ocean had been pushed over the continental margin for hundreds of kilometres about 87-76 million years ago. However, a leading proponent of the ‘in-situ’ theory, Hugh Wilson, observed that the major displacement surfaces were not prominent in the field and that he had seen more evidence of extension than compression in the Oman Mountains. Glennie (2001) remains a spirited critique of most of Wilson’s arguments. Almost all later authors interpret the Semail ophiolite as thrust, or obducted, probably due to a short period of subduction close to the margin of the Arabian plate.

answers: NDQ_003351

answers: extension

answers: NDQ_003352

answers: compresses

answers: NDQ_003353

answers: compression

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: Nappe

answers: NDQ_003356

answers: flow

answers: NDQ_003357

answers: igneous rocks had essentially flowed into position

answers: NDQ_003358

answers: unanswerable

answers: NDQ_003359

answers: subducts

answers: NDQ_003360

answers: continents moving together

answers: NDQ_003362

answers: a short period of subduction close to the margin of the Arabian plate

answers: NDQ_003363

answers: Tethys Ocean

answers: NDQ_003371

answers: What is the Semail ophiolite?

answers: NDQ_003373

answers: unanswerable

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What did Hugh Wilson observe in the Oman Mountains?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What is the cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: Semail Nappe

answers: NDQ_003386

answers: plate tectonics

answers: NDQ_003387

answers: What did Hugh Wilson observe in the Oman Mountains?

answers: NDQ_003388

answers: What type of faults result from shear stress?

answers: NDQ_003389

answers: The theory supported by Morton and others

answers: NDQ_003390

answers: Semail Nappe

answers: NDQ_003391

answers: ophiolite

answers: NDQ_003392

answers: Semail Nappe

answers: NDQ_003393

answers: ophiolite

answers: NDQ_003394

answers: Semail Nappe

answers: NDQ_003395

answers: Semail Nappe

answers: NDQ_003396

answers: Semail Nappe

answers: NDQ_003351

answers: extension than compression

answers: NDQ_003352

answers: extension than compression

answers: NDQ_003353

answers: extension than compression

answers: NDQ_003354

answers: Semail Ophiolite,

answers: NDQ_003355

answers: thrust sheet,

answers: NDQ_003356

answers: flowed into position.

answers: NDQ_003357

answers: subduction

answers: NDQ_003358

answers: thrust sheet, the Semail Nappe,

answers: NDQ_003359

answers: flowed into position.

answers: NDQ_003360

answers: plate tectonics

answers: NDQ_003362

answers: ‘in-situ’ theory,

answers: NDQ_003363

answers: plate tectonics

answers: NDQ_003371

answers: thrust sheet, the Semail Nappe,

answers: NDQ_003373

answers: extension than compression

answers: NDQ_003376

answers: thrust sheet,

answers: NDQ_003378

answers: thrust

answers: NDQ_003379

answers: thrust sheet, the Semail Nappe,

answers: NDQ_003380

answers: thrust

answers: NDQ_003381

answers: thrust sheet,

answers: NDQ_003382

answers: extension than compression

answers: NDQ_003383

answers: thrust sheet,

answers: NDQ_003384

answers: thrust sheet,

answers: NDQ_003385

answers: thrust sheet,

answers: NDQ_003386

answers: plate tectonics

answers: NDQ_003387

answers: thrust sheet,

answers: NDQ_003388

answers: thrust sheet,

answers: NDQ_003389

answers: flowed into position.

answers: NDQ_003390

answers: Semail Nappe,

answers: NDQ_003391

answers: thrust sheet, the Semail Nappe,

answers: NDQ_003392

answers: thrust sheet, the Semail Nappe,

answers: NDQ_003393

answers: thrust sheet, the Semail Nappe,

answers: NDQ_003394

answers: thrust sheet, the Semail Nappe,

answers: NDQ_003395

answers: Semail Nappe,

answers: NDQ_003396

answers: thrust sheet, the Semail Nappe,

text: Subduction orogeny has been occurring in what is now western South America since the break-up of the supercontinent Rodinia in the Neoproterozoic. The Paleozoic Pampean, Famatinian and Gondwanan orogenies are the immediate precursors to the later Andean orogeny. The first phases of Andean orogeny in the Jurassic and Early Cretaceous were characterized by extensional tectonics, rifting, the development of back-arc basins and the emplacement of large batholiths. This development is presumed to have been linked to the subduction of cold oceanic lithosphere. During the mid to Late Cretaceous (ca. 90 million years ago) the Andean orogeny changed significantly in character. Warmer and younger oceanic lithosphere is believed to have started to be subducted beneath South America around this time. Such kind of subduction is held responsible not only for the intense contractional deformation that different lithologies were subject to, but also the uplift and erosion known to have occurred from the Late Cretaceous onward. Plate tectonic reorganization since the mid-Cretaceous might also have been linked to the opening of the South Atlantic Ocean. Another change related to mid-Cretaceous plate tectonic changes was the change of subduction direction of the oceanic lithosphere that went from having south-east motion to having a north-east motion at about 90 million years ago. While subduction direction changed it remained oblique (and not perpendicular) to the coast of South America, and the direction change affected several subduction zone-parallel faults including Atacama, Domeyko and Liquiñe-Ofqui.

text: Subduction orogeny has been occurring in what is now western South America since the break-up of the

text: supercontinent

text: Rodinia

text: in the

text: Neoproterozoic

text: . The

text: Paleozoic

text: Pampean

text: Famatinian

text: and

text: Gondwanan

text: orogenies are the immediate precursors to the later Andean orogeny. The first phases of Andean orogeny in the

text: Jurassic

text: and

text: Early Cretaceous

text: were characterized by

text: extensional tectonics

text: rift

text: ing, the development of

text: back-arc basin

text: s and the emplacement of large

text: batholith

text: s. This development is presumed to have been linked to the subduction of cold

text: oceanic

text: lithosphere

text: . During the mid to

text: Late Cretaceous

text: (ca. 90 million years ago) the Andean orogeny changed significantly in character. Warmer and younger oceanic lithosphere is believed to have started to be subducted beneath South America around this time. Such kind of subduction is held responsible not only for the intense contractional

text: deformation

text: that different lithologies were subject to, but also the

text: uplift

text: and

text: erosion

text: known to have occurred from the Late Cretaceous onward.

text: Plate tectonic

text: reorganization since the mid-Cretaceous might also have been linked to the

text: opening

text: of the

text: South Atlantic Ocean

text: . Another change related to mid-Cretaceous plate tectonic changes was the change of subduction direction of the oceanic lithosphere that went from having south-east motion to having a north-east motion at about 90 million years ago. While subduction direction changed it remained oblique (and not perpendicular) to the coast of South America, and the direction change affected several

text: subduction zone

text: -parallel faults including

text: Atacama

text: Domeyko

text: and

text: Liquiñe-Ofqui

answers: NDQ_003351

answers: contractional

answers: NDQ_003352

answers: contractional deformation

answers: NDQ_003353

answers: deformation

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: back-arc basin

answers: NDQ_003356

answers: uplift

answers: NDQ_003357

answers: subduction direction of the oceanic lithosphere

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: subducts

answers: NDQ_003360

answers: Subduction orogeny

answers: NDQ_003362

answers: perpendicular to the coast of South America

answers: NDQ_003363

answers: Subduction orogeny

answers: NDQ_003371

answers: What kind of subduction is held responsible for the intense contractional deformation that different lithologies were subject to

answers: NDQ_003373

answers: What kind of subduction is held responsible not only for the intense contractional deformation that different lithologies were subject to?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: what is the first phase of Andean orogeny in the Jurassic and Early Cretaceous

answers: NDQ_003379

answers: unanswerable

answers: NDQ_003380

answers: What kind of subduction is held responsible not only for the intense contractional deformation

answers: NDQ_003381

answers: What kind of subduction is held responsible not only for the intense contractional deformation that different lithologies were subject to?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: What kind of subduction is held responsible not only for the intense contractional deformation

answers: NDQ_003384

answers: What kind of subduction is held responsible for the intense contractional deformation that different lithologies were subject to?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: subduction zone-parallel faults

answers: NDQ_003387

answers: What kind of subduction is held responsible not only for the intense contractional deformation

answers: NDQ_003388

answers: What kind of subduction is held responsible not only for the intense contractional deformation

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: parallel faults

answers: NDQ_003391

answers: subduction zone

answers: NDQ_003392

answers: parallel faults

answers: NDQ_003393

answers: batholiths

answers: NDQ_003394

answers: parallel faults

answers: NDQ_003395

answers: parallel faults

answers: NDQ_003396

answers: parallel faults

answers: NDQ_003351

answers: contractional deformation

answers: NDQ_003352

answers: contractional deformation

answers: NDQ_003353

answers: contractional deformation

answers: NDQ_003354

answers: uplift and erosion

answers: NDQ_003355

answers: back-arc

answers: NDQ_003356

answers: contractional deformation

answers: NDQ_003357

answers: oblique

answers: NDQ_003358

answers: subduction zone-parallel faults

answers: NDQ_003359

answers: subduction zone-parallel faults

answers: NDQ_003360

answers: Plate tectonic

answers: NDQ_003362

answers: perpendicular) to the coast of South America,

answers: NDQ_003363

answers: Late Cretaceous

answers: NDQ_003371

answers: Late Cretaceous

answers: NDQ_003373

answers: contractional deformation

answers: NDQ_003376

answers: uplift and erosion

answers: NDQ_003378

answers: erosion

answers: NDQ_003379

answers: Plate tectonic reorganization

answers: NDQ_003380

answers: contractional deformation

answers: NDQ_003381

answers: contractional deformation

answers: NDQ_003382

answers: erosion

answers: NDQ_003383

answers: Plate tectonic reorganization

answers: NDQ_003384

answers: erosion known to have occurred from the Late Cretaceous

answers: NDQ_003385

answers: subduction zone-parallel faults

answers: NDQ_003386

answers: Subduction orogeny

answers: NDQ_003387

answers: Plate tectonic reorganization

answers: NDQ_003388

answers: Subduction orogeny has been occurring in what is now western South America

answers: NDQ_003389

answers: Plate tectonic

answers: NDQ_003390

answers: subduction zone-parallel faults

answers: NDQ_003391

answers: subduction zone-parallel

answers: NDQ_003392

answers: subduction zone-parallel faults

answers: NDQ_003393

answers: subduction zone-parallel

answers: NDQ_003394

answers: oblique

answers: NDQ_003395

answers: oblique

answers: NDQ_003396

answers: subduction zone-parallel faults

text: Once the corbelled dome is complete, it can be covered in several different kinds of exterior treatments, usually plaster. Khalili developed a system that used 85% earth and 15% cement plaster and which is then covered by “reptile”, a veneer of grapefruit sized balls of cement and earth.  Reptile is easy to install and because the balls create easy paths for stress, it doesn't crack with time. There are many different possibilities.  Some Superadobe buildings have even been covered by living grass, a kind of green roof but covering the entire structure. Any exterior treatment and building details would need to be adapted to a region’s specific climatic needs.

text: Once the corbelled dome is complete, it can be covered in several different kinds of exterior treatments, usually plaster. Khalili developed a system that used 85% earth and 15% cement plaster and which is then covered by “reptile”, a veneer of grapefruit sized balls of cement and earth.  Reptile is easy to install and because the balls create easy paths for stress, it doesn't crack with time. There are many different possibilities.  Some Superadobe buildings have even been covered by living grass, a kind of

text: green roof

text: but covering the entire structure. Any exterior treatment and building details would need to be adapted to a region’s specific climatic needs.

answers: NDQ_003351

answers: reptile

answers: NDQ_003352

answers: cracks

answers: NDQ_003353

answers: cracks

answers: NDQ_003354

answers: Kaibab Limestone is above the Toroweap Formation

answers: NDQ_003355

answers: corbel

answers: NDQ_003356

answers: crack

answers: NDQ_003357

answers: reptile creates easy paths for stress

answers: NDQ_003358

answers: crater

answers: NDQ_003359

answers: cracks

answers: NDQ_003360

answers: Earth's crust

answers: NDQ_003362

answers: living grass, a kind of green roof but covering the entire structure

answers: NDQ_003363

answers: the same time

answers: NDQ_003371

answers: What may be a thrust fault in between?

answers: NDQ_003373

answers: How would you describe Khalili?

answers: NDQ_003376

answers: what kind of terrain is caused by compressive forces?

answers: NDQ_003378

answers: what is the last word in the passage?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: Which of the following is not a kind of green roof but covering the entire structure?

answers: NDQ_003381

answers: Which of the following is not an example of confining stress?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: What is a syncline?

answers: NDQ_003385

answers: What is a fault zone?

answers: NDQ_003386

answers: Which of the following is not a cause of earthquakes?

answers: NDQ_003387

answers: Which of the following is not a kind of green roof but covering the entire structure?

answers: NDQ_003388

answers: Which of the following is not a kind of green roof but covering the entire structure?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: superadobe

answers: NDQ_003391

answers: superadobe

answers: NDQ_003392

answers: corbelled dome

answers: NDQ_003393

answers: superadobe

answers: NDQ_003394

answers: vertical fault

answers: NDQ_003395

answers: fault with a vertical fault plane

answers: NDQ_003396

answers: NDQ_003351

answers: “reptile”,

answers: NDQ_003352

answers: crack with time.

answers: NDQ_003353

answers: crack

answers: NDQ_003354

answers: Superadobe buildings have even been covered by living grass,

answers: NDQ_003355

answers: corbelled

answers: NDQ_003356

answers: crack with time.

answers: NDQ_003357

answers: crack with time.

answers: NDQ_003358

answers: “reptile”,

answers: NDQ_003359

answers: stress,

answers: NDQ_003360

answers: climatic needs.

answers: NDQ_003362

answers: “reptile”,

answers: NDQ_003363

answers: 85% earth

answers: NDQ_003371

answers: Some Superadobe buildings have even been covered by living grass,

answers: NDQ_003373

answers: crack with time.

answers: NDQ_003376

answers: “reptile”,

answers: NDQ_003378

answers: “reptile”,

answers: NDQ_003379

answers: “reptile”,

answers: NDQ_003380

answers: stress,

answers: NDQ_003381

answers: crack with time.

answers: NDQ_003382

answers: “reptile”,

answers: NDQ_003383

answers: stress,

answers: NDQ_003384

answers: “reptile”,

answers: NDQ_003385

answers: “reptile”,

answers: NDQ_003386

answers: “reptile”,

answers: NDQ_003387

answers: “reptile”,

answers: NDQ_003388

answers: “reptile”,

answers: NDQ_003389

answers: “reptile”,

answers: NDQ_003390

answers: corbelled dome

answers: NDQ_003391

answers: earth

answers: NDQ_003392

answers: corbelled dome

answers: NDQ_003393

answers: Superadobe buildings have even been covered by living grass,

answers: NDQ_003394

answers: Superadobe buildings have even been covered by living grass,

answers: NDQ_003395

answers: “reptile”,

answers: NDQ_003396

answers: Superadobe buildings have even been covered by living grass,

text: Ruptures along the nearby San Andreas fault caused severe earth movement in the San Francisco Bay Area in 1906 and 1989. San Andreas quakes induces creep (movement occurring on earthquake faults) in the Hayward fault, which runs directly through Oakland, Berkeley, San Jose and other Bay Area cities.

text: Ruptures along the nearby

text: San Andreas fault

text: caused severe earth movement in the San Francisco Bay Area in 1906 and 1989. San Andreas quakes induces creep (movement occurring on earthquake faults) in the Hayward fault, which runs directly through Oakland, Berkeley, San Jose and other Bay Area cities.

answers: NDQ_003351

answers: Creep

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: Creep

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: Creep

answers: NDQ_003356

answers: Creep

answers: NDQ_003357

answers: San Andreas quakes induces movement on earthquake faults

answers: NDQ_003358

answers: fault

answers: NDQ_003359

answers: cracks

answers: NDQ_003360

answers: faults

answers: NDQ_003362

answers: the Hayward fault runs directly through Oakland, Berkeley, San Jose and other Bay Area cities

answers: NDQ_003363

answers: San Andreas fault

answers: NDQ_003371

answers: Which of the following is not a type of fault: San Andreas fault, Hayward fault, or San Jose fault?

answers: NDQ_003373

answers: what is the last word in the passage?

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: what is the second to last word?

answers: NDQ_003379

answers: What is the dip of the fault plane?

answers: NDQ_003380

answers: Which of the following is not a type of force applied to rock?

answers: NDQ_003381

answers: Which of the following is not an example of confining stress: San Andreas fault, Hayward fault, or Oakland?

answers: NDQ_003382

answers: What is the most common stress at convergent plates?

answers: NDQ_003383

answers: Which of the following is not a cause of joints in rock?

answers: NDQ_003384

answers: Which of the following is not an example of a fold that arches upward?

answers: NDQ_003385

answers: What is the San Andreas fault?

answers: NDQ_003386

answers: yes

answers: NDQ_003387

answers: Which of the following is not a normal fault: San Andreas fault, Hayward fault or San Jose fault?

answers: NDQ_003388

answers: Which of the following is not a type of fault: strike-slip faults, earthquake faults, or creep faults?

answers: NDQ_003389

answers: unanswerable

answers: NDQ_003390

answers: Hayward fault

answers: NDQ_003391

answers: quake

answers: NDQ_003392

answers: Hayward fault

answers: NDQ_003393

answers: San Andreas fault

answers: NDQ_003394

answers: Hayward fault

answers: NDQ_003395

answers: Hayward fault

answers: NDQ_003396

answers: Hayward fault

answers: NDQ_003351

answers: creep

answers: NDQ_003352

answers: movement

answers: NDQ_003353

answers: earth movement

answers: NDQ_003354

answers: Ruptures along the nearby San Andreas fault

answers: NDQ_003355

answers: creep

answers: NDQ_003356

answers: earth movement

answers: NDQ_003357

answers: (movement occurring on earthquake faults)

answers: NDQ_003358

answers: earthquake faults)

answers: NDQ_003359

answers: Ruptures

answers: NDQ_003360

answers: earthquake faults)

answers: NDQ_003362

answers: 1989.

answers: NDQ_003363

answers: San Andreas fault

answers: NDQ_003371

answers: San Andreas fault

answers: NDQ_003373

answers: Ruptures along the nearby San Andreas fault caused severe earth movement

answers: NDQ_003376

answers: San Andreas fault caused severe earth movement

answers: NDQ_003378

answers: creep

answers: NDQ_003379

answers: 1989.

answers: NDQ_003380

answers: earth movement

answers: NDQ_003381

answers: San Andreas fault caused severe earth movement

answers: NDQ_003382

answers: San Andreas fault

answers: NDQ_003383

answers: Ruptures along the nearby San Andreas fault caused severe earth movement

answers: NDQ_003384

answers: San Andreas fault

answers: NDQ_003385

answers: San Andreas fault caused severe earth movement in the San Francisco Bay Area

answers: NDQ_003386

answers: (movement occurring on earthquake faults)

answers: NDQ_003387

answers: Ruptures

answers: NDQ_003388

answers: earthquake faults)

answers: NDQ_003389

answers: earth movement

answers: NDQ_003390

answers: Hayward fault,

answers: NDQ_003391

answers: San Andreas fault

answers: NDQ_003392

answers: Hayward fault,

answers: NDQ_003393

answers: San Andreas fault

answers: NDQ_003394

answers: Hayward fault,

answers: NDQ_003395

answers: Hayward fault,

answers: NDQ_003396

answers: Hayward fault,

text: Mauna Loa has complex interactions with its neighbors, Hualālai to the west, Mauna Kea to the north, and particularly Kīlauea to the east. Lavas from Mauna Kea intersect with Mauna Loa's basal flows as a consequence of Kea's older age, and Mauna Kea's original rift zones were buried beneath post-shield volcanic rocks of Mauna Loa; additionally, Mauna Kea shares Mauna Loa's gravity well, depressing the ocean crust beneath it by .  There are also a series of normal faults on Mauna Loa's northern and western slopes, between its two major rift zones, that are believed to be the result of combined circumferential tension from the two rift zones and from added pressure due to the westward growth of neighboring Kīlauea.

text: Mauna Loa has complex interactions with its neighbors,

text: Hualālai

text: to the west,

text: Mauna Kea

text: to the north, and particularly

text: Kīlauea

text: to the east. Lavas from Mauna Kea intersect with Mauna Loa's basal flows as a consequence of Kea's older age, and Mauna Kea's original

text: rift zone

text: s were buried beneath post-shield volcanic rocks of Mauna Loa; additionally, Mauna Kea shares Mauna Loa's gravity well, depressing the

text: ocean crust

text: beneath it by .  There are also a series of

text: normal fault

text: s on Mauna Loa's northern and western slopes, between its two major rift zones, that are believed to be the result of combined circumferential tension from the two rift zones and from added pressure due to the westward growth of neighboring Kīlauea.

answers: NDQ_003351

answers: circumferential

answers: NDQ_003352

answers: increases in size

answers: NDQ_003353

answers: normal faults

answers: NDQ_003354

answers: Toroweap Formation

answers: NDQ_003355

answers: fault

answers: NDQ_003356

answers: depress the ocean crust

answers: NDQ_003357

answers: circumferential tension from the two rift zones

answers: NDQ_003358

answers: normal faults

answers: NDQ_003359

answers: added pressure

answers: NDQ_003360

answers: gravity well

answers: NDQ_003362

answers: Mauna Kea shares Mauna Loa's gravity well

answers: NDQ_003363

answers: Mauna Kea

answers: NDQ_003371

answers: normal faults on Mauna Loa's northern and western slopes

answers: NDQ_003373

answers: yes

answers: NDQ_003376

answers: unanswerable

answers: NDQ_003378

answers: unanswerable

answers: NDQ_003379

answers: no

answers: NDQ_003380

answers: What type of force is applied to rock?

answers: NDQ_003381

answers: What is a consequence of Kea's older age?

answers: NDQ_003382

answers: unanswerable

answers: NDQ_003383

answers: unanswerable

answers: NDQ_003384

answers: What type of fold is Mauna Loa?

answers: NDQ_003385

answers: fault zone

answers: NDQ_003386

answers: no

answers: NDQ_003387

answers: no

answers: NDQ_003388

answers: unanswerable

answers: NDQ_003389

answers: no

answers: NDQ_003390

answers: normal faults

answers: NDQ_003391

answers: Mauna Kea

answers: NDQ_003392

answers: normal faults

answers: NDQ_003393

answers: Mauna Loa

answers: NDQ_003394

answers: normal faults

answers: NDQ_003395

answers: Mauna Loa

answers: NDQ_003396

answers: normal faults

answers: NDQ_003351

answers: circumferential tension

answers: NDQ_003352

answers: faults

answers: NDQ_003353

answers: faults

answers: NDQ_003354

answers: Mauna Kea's original rift zones

answers: NDQ_003355

answers: normal faults

answers: NDQ_003356

answers: normal faults

answers: NDQ_003357

answers: combined circumferential tension

answers: NDQ_003358

answers: normal faults

answers: NDQ_003359

answers: added pressure

answers: NDQ_003360

answers: westward growth

answers: NDQ_003362

answers: Kea's older age,

answers: NDQ_003363

answers: Mauna Loa

answers: NDQ_003371

answers: normal faults

answers: NDQ_003373

answers: Mauna Kea's original rift zones

answers: NDQ_003376

answers: basal flows

answers: NDQ_003378

answers: normal faults

answers: NDQ_003379

answers: normal faults

answers: NDQ_003380

answers: pressure

answers: NDQ_003381

answers: normal faults

answers: NDQ_003382

answers: pressure

answers: NDQ_003383

answers: faults

answers: NDQ_003384

answers: normal faults

answers: NDQ_003385

answers: rift zones,

answers: NDQ_003386

answers: circumferential tension

answers: NDQ_003387

answers: combined circumferential tension

answers: NDQ_003388

answers: normal faults

answers: NDQ_003389

answers: normal faults

answers: NDQ_003390

answers: normal faults

answers: NDQ_003391

answers: post-shield volcanic rocks

answers: NDQ_003392

answers: normal faults

answers: NDQ_003393

answers: post-shield volcanic rocks

answers: NDQ_003394

answers: normal faults

answers: NDQ_003395

answers: normal faults

answers: NDQ_003396

answers: normal faults