text: Cumberland lies at the beginning of the transition from a humid continental climate (Köppen Dfa) to a humid subtropical climate (Cfa), although bearing far more characteristics of the former, with a range of temperatures significantly lower than those in the central and eastern part of Maryland, mostly in the form of depressed nighttime lows. Cumberland is the only major city in Maryland to fall within the humid continental (Dfa) climate. Hagerstown lies in the middle of the transition zone.

text: Cumberland lies at the beginning of the transition from a

entity_name: Humid continental climate

text: humid continental climate

entity_name: Köppen climate classification

text: Köppen

text: Dfa) to a

entity_name: Humid subtropical climate

text: humid subtropical climate

text: (Cfa), although bearing far more characteristics of the former, with a range of temperatures significantly lower than those in the central and eastern part of Maryland, mostly in the form of depressed nighttime lows. Cumberland is the only major city in Maryland to fall within the humid continental (Dfa) climate. Hagerstown lies in the middle of the transition zone.

method: Bert-ConvKNRM

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answers: Köppen Dfa

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answers: Cumberland lies at the beginning of the transition

answers: NDQ_003252

answers: continental drift

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prompt_style: provide a complete and concise answer to the question based on the context.

text: The development of ETRS89 is related to the global ITRS geodetic datum, in which the representation of the continental drift is balanced in such a way that the total apparent angular momentum of continental plates is about 0.  ETRS89 was officially born at the 1990 Florence meeting of EUREF, following its Resolution 1, which recommends that the terrestrial reference system to be adopted by EUREF will be coincident with ITRS at the epoch 1989.0 and fixed to the stable part of the Eurasian Plate. According to the resolution, this system was named European Terrestrial Reference System 89 (ETRS89). Since then ETRS89 and ITRS diverge due to the continental drift at a speed about  2.5 cm per year. By the year 2000 the two coordinate systems differed by about 25 cm.

text: The development of ETRS89 is related to the global

entity_name: International Terrestrial Reference System

text: ITRS

entity_name: Geodetic datum

text: geodetic datum

text: , in which the representation of the continental drift is balanced in such a way that the total apparent

entity_name: Angular momentum

text: angular momentum

text: of

entity_name: Plate tectonics

text: continental plate

text: s is about 0.  ETRS89 was officially born at the 1990

entity_name: Florence

text: Florence

text: meeting of

entity_name: Regional Reference Frame Sub-Commission for Europe

text: EUREF

text: , following its Resolution 1, which recommends that the terrestrial reference system to be adopted by EUREF will be coincident with ITRS at the epoch 1989.0 and fixed to the stable part of the Eurasian Plate. According to the resolution, this system was named European Terrestrial Reference System 89 (ETRS89). Since then ETRS89 and ITRS diverge due to the continental drift at a speed about  2.5 cm per year. By the year 2000 the two coordinate systems differed by about 25 cm.

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answers: NDQ_003228

answers: 0

answers: NDQ_003230

answers: 0

answers: NDQ_003231

answers: 0

answers: NDQ_003233

answers: 0

answers: NDQ_003236

answers: 4

answers: NDQ_003237

answers: 0

answers: NDQ_003239

answers: 0

answers: NDQ_003240

answers: 0

answers: NDQ_003241

answers: 0

answers: NDQ_003242

answers: 0

answers: NDQ_003244

answers: 0

answers: NDQ_003246

answers: 4

answers: NDQ_003247

answers: 0

answers: NDQ_003252

answers: 4

answers: NDQ_003253

answers: 0

answers: NDQ_003254

answers: 0

answers: NDQ_003255

answers: 0

answers: NDQ_003256

answers: 0

answers: NDQ_003257

answers: 0

answers: NDQ_003258

answers: 0

answers: NDQ_003219

answers: continental drift

answers: NDQ_003220

answers: Eurasian

answers: NDQ_003221

answers: 1990

answers: NDQ_003222

answers: ETRS89

answers: NDQ_003223

answers: Eurasian Plate

answers: NDQ_003224

answers: ETRS89

answers: NDQ_003225

answers: ETRS89

answers: NDQ_003226

answers: Eurasian Plate

answers: NDQ_003227

answers: the total apparent angular momentum of continental plates is about 0

answers: NDQ_003228

answers: ETRS89

answers: NDQ_003230

answers: Eurasian

answers: NDQ_003231

answers: angular momentum

answers: NDQ_003233

answers: ETRS89 and ITRS diverge due to the continental drift

answers: NDQ_003236

answers: continental drift

answers: NDQ_003237

answers: total apparent angular momentum of continental plates

answers: NDQ_003239

answers: ETRS89 and ITRS diverge due to the continental drift

answers: NDQ_003240

answers: Eurasian

answers: NDQ_003241

answers: Eurasian Plate

answers: NDQ_003242

answers: angular momentum

answers: NDQ_003244

answers: ETRS89

answers: NDQ_003246

answers: ETRS89 and ITRS diverge

answers: NDQ_003247

answers: ETRS89

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: Eurasian Plate

answers: NDQ_003254

answers: It was widely accepted as soon as it was introduced

answers: NDQ_003255

answers: By the year 2000 the two coordinate systems differed by about 25 cm

answers: NDQ_003256

answers: ETRS89

answers: NDQ_003257

answers: By the year 2000 the two coordinate systems differed by about 25 cm

answers: NDQ_003258

answers: continental drift

text: Forensics uses a variety of different tools and techniques. Fingerprint collection through the use of grey or black magnetic powder. DNA and other bodily fluids are collected and, whether it is hair or fluid, for further examination in a lab. Shoe and tire prints can be collected using dental stone. Electronics are taken for examination by a technical expert to search for further evidence. Documents from the area are also taken for further examination. Ammunition and weapons are taken for matching to wounds and ballistics. Photographs of tool marks are taken because they can be matched to a weapon at a later time. Any other trace evidence is also collected. Trace evidence is anything left behind by a perpetrator or could have been transferred to the perpetrator. Interviews of both witnesses and victims of the crime are taken by law enforcement officials in order to gain knowledge and creating a timeline of events.

text: Forensics uses a variety of different tools and techniques. Fingerprint collection through the use of grey or black magnetic powder. DNA and other bodily fluids are collected and, whether it is hair or fluid, for further examination in a lab. Shoe and tire prints can be collected using dental stone. Electronics are taken for examination by a technical expert to search for further evidence. Documents from the area are also taken for further examination. Ammunition and weapons are taken for matching to wounds and ballistics. Photographs of tool marks are taken because they can be matched to a weapon at a later time. Any other

entity_name: Trace evidence

text: trace evidence

text: is also collected. Trace evidence is anything left behind by a perpetrator or could have been transferred to the perpetrator. Interviews of both witnesses and victims of the crime are taken by law enforcement officials in order to gain knowledge and creating a timeline of events.

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answers: NDQ_003219

answers: 0

answers: NDQ_003220

answers: 0

answers: NDQ_003221

answers: 0

answers: NDQ_003222

answers: 0

answers: NDQ_003223

answers: 0

answers: NDQ_003224

answers: 0

answers: NDQ_003225

answers: 0

answers: NDQ_003226

answers: 0

answers: NDQ_003227

answers: 0

answers: NDQ_003228

answers: 0

answers: NDQ_003230

answers: 0

answers: NDQ_003231

answers: 0

answers: NDQ_003233

answers: 0

answers: NDQ_003236

answers: 0

answers: NDQ_003237

answers: 0

answers: NDQ_003239

answers: 0

answers: NDQ_003240

answers: 0

answers: NDQ_003241

answers: 0

answers: NDQ_003242

answers: 0

answers: NDQ_003244

answers: 0

answers: NDQ_003246

answers: 0

answers: NDQ_003247

answers: 0

answers: NDQ_003252

answers: 3

answers: NDQ_003253

answers: 0

answers: NDQ_003254

answers: 0

answers: NDQ_003255

answers: 0

answers: NDQ_003256

answers: 0

answers: NDQ_003257

answers: 0

answers: NDQ_003258

answers: 0

answers: NDQ_003219

answers: plate tectonics

answers: NDQ_003220

answers: unanswerable

answers: NDQ_003221

answers: 18th century

answers: NDQ_003222

answers: Forensics

answers: NDQ_003223

answers: a volcano

answers: NDQ_003224

answers: shoe and tire prints

answers: NDQ_003225

answers: Forensics

answers: NDQ_003226

answers: Antarctica

answers: NDQ_003227

answers: a timeline of events

answers: NDQ_003228

answers: Forensics

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: Fingerprint

answers: NDQ_003233

answers: Ammunition and weapons are taken for matching to wounds and ballistics

answers: NDQ_003236

answers: is anything left behind

answers: NDQ_003237

answers: Shoe and tire prints

answers: NDQ_003239

answers: Shoe and tire prints can be collected using dental stone

answers: NDQ_003240

answers: a former supercontinent

answers: NDQ_003241

answers: no

answers: NDQ_003242

answers: unanswerable

answers: NDQ_003244

answers: Forensics

answers: NDQ_003246

answers: continents

answers: NDQ_003247

answers: Forensics uses a variety of different tools and techniques

answers: NDQ_003252

answers: plate tectonics

answers: NDQ_003253

answers: no

answers: NDQ_003254

answers: Forensics

answers: NDQ_003255

answers: Forensics uses a variety of different tools

answers: NDQ_003256

answers: Forensics

answers: NDQ_003257

answers: Pangaea

answers: NDQ_003258

answers: The use of grey or black magnetic powder

text: Reconstructions of tectonic plate movement in the past 250 million years (the Cenozoic and Mesozoic eras) can be made reliably using fitting of continental margins, ocean floor magnetic anomalies and paleomagnetic poles. No ocean crust dates back further than that, so earlier reconstructions are more difficult. Paleomagnetic poles are supplemented by geologic evidence such as orogenic belts, which mark the edges of ancient plates, and past distributions of flora and fauna. The further back in time, the scarcer and harder to interpret the data get and the more diverse the reconstructions.

text: Reconstructions of tectonic plate movement in the past 250 million years (the Cenozoic and Mesozoic eras) can be made reliably using fitting of continental margins, ocean floor magnetic anomalies and paleomagnetic poles. No ocean crust dates back further than that, so earlier reconstructions are more difficult. Paleomagnetic poles are supplemented by geologic evidence such as

entity_name: Orogeny

text: orogenic belt

text: s, which mark the edges of ancient plates, and past distributions of flora and fauna. The further back in time, the scarcer and harder to interpret the data get and the more diverse the reconstructions.

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text: As a result of a new emphasis on observing, classifying, and cataloging nature, 16th century natural philosophers in Europe began to establish extensive collections of fossil objects (as well as collections of plant and animal specimens), which were often stored in specially built cabinets to help organize them. Conrad Gesner published a 1565 work on fossils that contained one of the first detailed descriptions of such a cabinet and collection. The collection belonged to a member of the extensive network of correspondents that Gesner drew on for his works. Such informal correspondence networks among natural philosophers and collectors became increasingly important during the course of the 16th century and were direct forerunners of the scientific societies that would begin to form in the 17th century. These cabinet collections and correspondence networks played an important role in the development of natural philosophy.

text: As a result of a new emphasis on observing, classifying, and cataloging nature, 16th century natural philosophers in Europe began to establish extensive

entity_name: Collecting

text: collections

text: of fossil objects (as well as collections of plant and animal specimens), which were often stored in specially built cabinets to help organize them.

entity_name: Conrad Gessner

text: Conrad Gesner

text: published a 1565 work on fossils that contained one of the first detailed descriptions of such a cabinet and collection. The collection belonged to a member of the extensive network of correspondents that Gesner drew on for his works. Such informal correspondence networks among natural philosophers and collectors became increasingly important during the course of the 16th century and were direct forerunners of the scientific societies that would begin to form in the 17th century. These cabinet collections and correspondence networks played an important role in the development of natural philosophy.

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answers: Gesner published a 1565 work

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answers: Europe

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answers: NDQ_003223

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answers: fossil objects (as well as collections of plant and animal specimens)

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answers: It was widely accepted as soon as it was introduced

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answers: Conrad Gesner

text: The Köppen Climate Classification subtype for this climate is "Cwc" (Oceanic Subtropical Highland Climate).

text: The

text: Köppen Climate Classification

text: subtype for this climate is "

entity_name: Oceanic climate

text: Cwc

text: " (Oceanic Subtropical Highland Climate).

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answers: Subtropical Highland Climate

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answers: Highland

answers: NDQ_003221

answers: 18th century

answers: NDQ_003222

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answers: NDQ_003224

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answers: NDQ_003225

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answers: NDQ_003226

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answers: NDQ_003227

answers: continental drift

answers: NDQ_003228

answers: Köppen

answers: NDQ_003230

answers: Oceanic Subtropical Highland Climate

answers: NDQ_003231

answers: subtropical

answers: NDQ_003233

answers: Cwc

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answers: continents move over Earth's surface

answers: NDQ_003237

answers: Wegener

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answers: NDQ_003240

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answers: NDQ_003241

answers: The magnetic north pole and geographic north pole are in the same location.

answers: NDQ_003242

answers: Köppen Climate Classification

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text: Glaciation took place repeatedly during the Quaternary Ice Age – a term coined by Schimper in 1839 that began with the start of the Quaternary about 2.58 Mya and continues to the present-day.

text: Glaciation took place repeatedly during the Quaternary

entity_name: Ice age

text: Ice Age

text: – a term coined by Schimper in 1839 that began with the start of the Quaternary about 2.58 Mya and continues to the present-day.

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answers: 1839

answers: NDQ_003222

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answers: 2.58 Mya

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answers: Quaternary Ice Age

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answers: North America

answers: NDQ_003231

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text: In Ice Age: Continental Drift, she is an understanding wife and a mother. Ellie supports Peaches, when she had an argument with Manny. When the Ice Age: Continental Drift happens she aids the herd to the Land Bridge. In the end she also fights with the Pirates.

text: In

entity_name: Ice Age: Continental Drift

text: Ice Age: Continental Drift

text: , she is an understanding wife and a mother. Ellie supports Peaches, when she had an argument with Manny. When the Ice Age: Continental Drift happens she aids the herd to the Land Bridge. In the end she also fights with the Pirates.

method: UvABottomUpChangeOrder

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answers: Continental Drift

text: This climatic region is typified by large seasonal temperature differences, with warm to hot summers and cold winters.  According to the Köppen Climate Classification system, Essex Junction has a humid continental climate, abbreviated "Dfb" on climate maps.

text: This

entity_name: Climate

text: climatic

text: region is typified by large seasonal temperature differences, with warm to hot summers and cold winters.  According to the

text: Köppen Climate Classification

text: system, Essex Junction has a

text: humid continental climate

text: , abbreviated "Dfb" on climate maps.

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answers: NDQ_003221

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answers: NDQ_003222

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answers: NDQ_003223

answers: Dfb

answers: NDQ_003224

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answers: NDQ_003225

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answers: NDQ_003226

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answers: NDQ_003230

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answers: NDQ_003236

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answers: NDQ_003239

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answers: NDQ_003242

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answers: NDQ_003247

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answers: large seasonal temperature differences

answers: NDQ_003257

answers: According to the Köppen Climate Classification system

answers: NDQ_003258

answers: Köppen Climate Classification system

text: Granite has a felsic composition and is more common in recent geologic time in contrast to Earth's ultramafic ancient igneous history. Felsic rocks are less dense than mafic and ultramafic rocks, and thus they tend to escape subduction, whereas basaltic or gabbroic rocks tend to sink into the mantle beneath the granitic rocks of the continental cratons. Therefore, granitic rocks form the basement of all land continents.

text: Granite has a felsic composition and is more common in recent

entity_name: Geologic time scale

text: geologic time

text: in contrast to Earth's

entity_name: Ultramafic rock

text: ultramafic

text: ancient igneous history. Felsic rocks are less dense than

entity_name: Mafic

text: mafic

text: and ultramafic rocks, and thus they tend to escape

entity_name: Subduction

text: subduction

text: , whereas basaltic or gabbroic rocks tend to sink into the mantle beneath the granitic rocks of the continental

entity_name: Craton

text: cratons

text: . Therefore, granitic rocks form the basement of all land

entity_name: Continent

text: continents

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answers: 4

answers: NDQ_003220

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answers: NDQ_003221

answers: 0

answers: NDQ_003222

answers: 0

answers: NDQ_003223

answers: 0

answers: NDQ_003224

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answers: NDQ_003225

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answers: 4

answers: NDQ_003253

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answers: 4

answers: NDQ_003256

answers: 0

answers: NDQ_003257

answers: 0

answers: NDQ_003258

answers: 0

answers: NDQ_003219

answers: subduction

answers: NDQ_003220

answers: continents

answers: NDQ_003221

answers: geologic time

answers: NDQ_003222

answers: granitic rocks form the basement of all land continents

answers: NDQ_003223

answers: subduction

answers: NDQ_003224

answers: Granite

answers: NDQ_003225

answers: Granite has a felsic composition

answers: NDQ_003226

answers: Earth

answers: NDQ_003227

answers: granitic rocks form the basement of all land continents

answers: NDQ_003228

answers: continental cratons

answers: NDQ_003230

answers: Earth

answers: NDQ_003231

answers: cratons

answers: NDQ_003233

answers: Granite has a felsic composition

answers: NDQ_003236

answers: subduction

answers: NDQ_003237

answers: Granite has a felsic composition

answers: NDQ_003239

answers: Therefore, granitic rocks form the basement of all land continents

answers: NDQ_003240

answers: Earth

answers: NDQ_003241

answers: Earth's

answers: NDQ_003242

answers: subduction

answers: NDQ_003244

answers: granitic rocks

answers: NDQ_003246

answers: The continents have never been together as a single whole continent.

answers: NDQ_003247

answers: Granite has a felsic composition

answers: NDQ_003252

answers: plate tectonics

answers: NDQ_003253

answers: granitic rocks form the basement of all land continents

answers: NDQ_003254

answers: Granite has a felsic composition

answers: NDQ_003255

answers: Therefore, granitic rocks form the basement of all land continents

answers: NDQ_003256

answers: Basaltic or gabbroic rocks

answers: NDQ_003257

answers: Granite has a felsic composition

answers: NDQ_003258

answers: subduction

text: Paleomagnetic study of apparent polar wandering paths also support the theory of a supercontinent. Geologists can determine the movement of continental plates by examining the orientation of magnetic minerals in rocks; when rocks are formed, they take on the magnetic properties of the Earth and indicate in which direction the poles lie relative to the rock. Since the magnetic poles drift about the rotational pole with a period of only a few thousand years, measurements from numerous lavas spanning several thousand years are averaged to give an apparent mean polar position. Samples of sedimentary rock and intrusive igneous rock have magnetic orientations that are typically an average of the "secular variation" in the orientation of magnetic north because their remanent magnetizations are not acquired instantaneously. Magnetic differences between sample groups whose age varies by millions of years is due to a combination of true polar wander and the drifting of continents. The true polar wander component is identical for all samples, and can be removed, leaving geologists with the portion of this motion that shows continental drift and can be used to help reconstruct earlier continental positions.

entity_name: Paleomagnetism

text: Paleomagnetic

text: study of apparent polar wandering paths also support the theory of a supercontinent. Geologists can determine the movement of continental plates by examining the orientation of magnetic minerals in rocks; when rocks are formed, they take on the magnetic properties of the Earth and indicate in which direction the poles lie relative to the rock. Since the magnetic poles

entity_name: Polar drift

text: drift

text: about the rotational pole with a period of only a few thousand years, measurements from numerous lavas spanning several thousand years are averaged to give an apparent mean polar position. Samples of

entity_name: Sedimentary rock

text: sedimentary rock

text: and

entity_name: Intrusive rock

text: intrusive igneous rock

text: have magnetic orientations that are typically an average of the "secular variation" in the orientation of

entity_name: Magnetic declination

text: magnetic north

text: because their

entity_name: Remanence

text: remanent

text: magnetizations are not acquired instantaneously. Magnetic differences between sample groups whose age varies by millions of years is due to a combination of

entity_name: True polar wander

text: true polar wander

text: and the drifting of continents. The true polar wander component is identical for all samples, and can be removed, leaving geologists with the portion of this motion that shows continental drift and can be used to help reconstruct earlier continental positions.

method: UNH-qee

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answers: 4

answers: NDQ_003219

answers: 4

answers: NDQ_003220

answers: 0

answers: NDQ_003221

answers: 0

answers: NDQ_003222

answers: 0

answers: NDQ_003223

answers: 4

answers: NDQ_003224

answers: 4

answers: NDQ_003225

answers: 0

answers: NDQ_003226

answers: 0

answers: NDQ_003227

answers: 0

answers: NDQ_003228

answers: 0

answers: NDQ_003230

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answers: NDQ_003231

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answers: NDQ_003233

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answers: NDQ_003236

answers: 4

answers: NDQ_003237

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answers: NDQ_003239

answers: 4

answers: NDQ_003240

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answers: 4

answers: NDQ_003244

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answers: NDQ_003246

answers: 4

answers: NDQ_003247

answers: 4

answers: NDQ_003252

answers: 4

answers: NDQ_003253

answers: 4

answers: NDQ_003254

answers: 0

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answers: 4

answers: NDQ_003256

answers: 0

answers: NDQ_003257

answers: 0

answers: NDQ_003258

answers: 0

answers: NDQ_003219

answers: a supercontinent

answers: NDQ_003220

answers: continental plates

answers: NDQ_003221

answers: Paleomagnetic

answers: NDQ_003222

answers: a supercontinent

answers: NDQ_003223

answers: a supercontinent

answers: NDQ_003224

answers: magnetic minerals in rocks

answers: NDQ_003225

answers: theory of a supercontinent

answers: NDQ_003226

answers: Europe

answers: NDQ_003227

answers: can be used to help reconstruct earlier continental positions

answers: NDQ_003228

answers: Paleomagnetic study

answers: NDQ_003230

answers: continents

answers: NDQ_003231

answers: magnetic north

answers: NDQ_003233

answers: magnetic minerals in rocks

answers: NDQ_003236

answers: a supercontinent

answers: NDQ_003237

answers: magnetic minerals in rocks

answers: NDQ_003239

answers: The true polar wander component is identical

answers: NDQ_003240

answers: continental drift

answers: NDQ_003241

answers: rotational pole

answers: NDQ_003242

answers: true polar wander

answers: NDQ_003244

answers: Paleomagnetic study

answers: NDQ_003246

answers: continents have never been together

answers: NDQ_003247

answers: Paleomagnetic study

answers: NDQ_003252

answers: theory of a supercontinent

answers: NDQ_003253

answers: supercontinent

answers: NDQ_003254

answers: magnetic poles drift about the rotational pole

answers: NDQ_003255

answers: Paleomagnetic study

answers: NDQ_003256

answers: The true polar wander component is identical

answers: NDQ_003257

answers: The true polar wander component is identical to all samples

answers: NDQ_003258

answers: Paleomagnetic study

text: Some geologists assert that, as the island moved north due to the effects of continental drift, it submerged at various intervals, extinguishing its terrestrial flora and fauna. Botanists counter that some areas must have remained above sea-level, serving as refugia. Many members of the late Cretaceous - early Tertiary Gondwanan flora survived in New Caledonia's equable climate but were eliminated in Australia due to increasingly dry conditions. The isolation of New Caledonia was not absolute, given the rise and fall of sea level caused by the ebb and flow of ice ages. Land bridges or islands formed between New Caledonia and its neighbours, the Solomon Islands, Vanuatu, and Australia. Thus new species came to New Caledonia while Gondwanan species were able to penetrate the Pacific Islands region. Plants have limited seed dispersal mobility away from the parent plant and consequently rely upon a variety of dispersal vectors to transport their propagules, including both abiotic and biotic vectors.

text: Some

entity_name: Geologist

text: geologist

text: s assert that, as the island moved north due to the effects of

entity_name: Continental drift

text: continental drift

text: , it submerged at various intervals, extinguishing its terrestrial flora and fauna.

entity_name: Botany

text: Botanist

text: s counter that some areas must have remained above sea-level, serving as

entity_name: Refugium (population biology)

text: refugia

text: . Many members of the late Cretaceous - early Tertiary Gondwanan flora survived in New Caledonia's equable climate but were eliminated in Australia due to increasingly dry conditions. The isolation of New Caledonia was not absolute, given the rise and fall of

entity_name: Sea level

text: sea level

text: caused by the ebb and flow of

text: ice age

text: s. Land bridges or islands formed between New Caledonia and its neighbours, the

entity_name: Solomon Islands

text: Solomon Islands

entity_name: Vanuatu

text: Vanuatu

text: , and Australia. Thus new species came to New Caledonia while Gondwanan species were able to penetrate the Pacific Islands region. Plants have limited

entity_name: Seed dispersal

text: seed dispersal

text: mobility away from the parent plant and consequently rely upon a variety of

entity_name: Dispersal vector

text: dispersal vector

text: s to transport their propagules, including both

entity_name: Abiotic component

text: abiotic

text: and

entity_name: Biotic component

text: biotic

text: vectors.

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answers: continental drift

answers: NDQ_003220

answers: Solomon Islands

answers: NDQ_003221

answers: Tertiary

answers: NDQ_003222

answers: some areas must have remained above sea-level, serving as refugia

answers: NDQ_003223

answers: the effects of continental drift

answers: NDQ_003224

answers: Cretaceous

answers: NDQ_003225

answers: continental drift

answers: NDQ_003226

answers: New Caledonia

answers: NDQ_003227

answers: the island moved north due to the effects of continental drift

answers: NDQ_003228

answers: geologists

answers: NDQ_003230

answers: Australia

answers: NDQ_003231

answers: magnetic field

answers: NDQ_003233

answers: Land bridges or islands formed between New Caledonia and its neighbours

answers: NDQ_003236

answers: continental drift

answers: NDQ_003237

answers: the island moved north due to the effects of continental drift

answers: NDQ_003239

answers: Land bridges or islands formed between New Caledonia and its neighbours

answers: NDQ_003240

answers: Gondwanan

answers: NDQ_003241

answers: The island moved north

answers: NDQ_003242

answers: continental drift

answers: NDQ_003244

answers: continental drift

answers: NDQ_003246

answers: Land bridges

answers: NDQ_003247

answers: Land bridges or islands formed between New Caledonia and its neighbours

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: Gondwanan

answers: NDQ_003254

answers: Some geologists

answers: NDQ_003255

answers: as the island moved north due to the effects of continental drift

answers: NDQ_003256

answers: continental drift

answers: NDQ_003257

answers: The island moved north due to the effects of continental drift

answers: NDQ_003258

answers: Land bridges or islands

text: Moving on to the 20th century, Alfred Wegener introduced the Theory of Continental Drift in 1912, though it was not widely accepted until the 1960s. This theory was revolutionary because it changed the way that everyone thought about species and their distribution around the globe. The theory explained how continents were formerly joined together in one large landmass, Pangea, and slowly drifted apart due to the movement of the plates below Earth’s surface. The evidence for this theory is in the geological similarities between varying locations around the globe, fossil comparisons from different continents, and the jigsaw puzzle shape of the landmasses on Earth. Though Wegener did not know the mechanism of this concept of Continental Drift, this contribution to the study of biogeography was significant in the way that it shed light on the importance of environmental and geographic similarities or differences as a result of climate and other pressures on the planet.

text: Moving on to the 20th century,

entity_name: Alfred Wegener

text: Alfred Wegener

text: introduced the Theory of

text: Continental Drift

text: in 1912, though it was not widely accepted until the 1960s. This theory was revolutionary because it changed the way that everyone thought about species and their distribution around the globe. The theory explained how continents were formerly joined together in one large landmass,

entity_name: Pangaea

text: Pangea

text: , and slowly drifted apart due to the movement of the plates below Earth’s surface. The evidence for this theory is in the geological similarities between varying locations around the globe, fossil comparisons from different continents, and the jigsaw puzzle shape of the landmasses on Earth. Though Wegener did not know the mechanism of this concept of Continental Drift, this contribution to the study of biogeography was significant in the way that it shed light on the importance of environmental and geographic similarities or differences as a result of climate and other pressures on the planet.

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answers: 4

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answers: 4

answers: NDQ_003239

answers: 4

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answers: 4

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answers: 4

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answers: 0

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answers: 4

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answers: 5

answers: NDQ_003219

answers: plates below Earth’s surface

answers: NDQ_003220

answers: Pangea

answers: NDQ_003221

answers: 20th century

answers: NDQ_003222

answers: Wegener did not know the mechanism

answers: NDQ_003223

answers: Pangea

answers: NDQ_003224

answers: fossil comparisons

answers: NDQ_003225

answers: Theory of Continental Drift

answers: NDQ_003226

answers: Pangea

answers: NDQ_003227

answers: continents were formerly joined together in one large landmass, Pangea, and slowly drifted apart

answers: NDQ_003228

answers: introduced

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: magnetic field

answers: NDQ_003233

answers: geological similarities

answers: NDQ_003236

answers: Theory of Continental Drift

answers: NDQ_003237

answers: geological similarities between varying locations around the globe, fossil comparisons from different continents, and the jigsaw puzzle shape of the landmasses on Earth

answers: NDQ_003239

answers: fossil comparisons from different continents

answers: NDQ_003240

answers: Pangea

answers: NDQ_003241

answers: Earth’s surface

answers: NDQ_003242

answers: Theory of Continental Drift

answers: NDQ_003244

answers: fossil comparisons from different continents

answers: NDQ_003246

answers: Pangea

answers: NDQ_003247

answers: fossil comparisons

answers: NDQ_003252

answers: theory of continental drift

answers: NDQ_003253

answers: Pangea

answers: NDQ_003254

answers: It was not widely accepted

answers: NDQ_003255

answers: geological similarities between varying locations around the globe, fossil comparisons from different continents, and the jigsaw puzzle shape of the landmasses on Earth

answers: NDQ_003256

answers: Geological similarities between varying locations around the globe

answers: NDQ_003257

answers: Theory of Continental Drift

answers: NDQ_003258

answers: the movement of the plates below Earth’s surface

text: In specified intervals, a sample of the ions is let into the drift chamber; the gating mechanism is based on a charged electrode working in a similar way as the control grid in triodes works for electrons. For precise control of the ion pulse width admitted to the drift tube, more complex gating systems such as a Bradbury-Nielsen design are employed.  Once in the drift tube, ions are subjected to a homogeneous electric field ranging from a few volts per centimeter up to many hundreds of volts per centimeter.  This electric field then drives the ions through the drift tube where they interact with the neutral drift molecules contained within the system.

text: In specified intervals, a sample of the ions is let into the drift chamber; the gating mechanism is based on a charged electrode working in a similar way as the

text: control grid

text: in

text: triode

text: s works for electrons. For precise control of the ion pulse width admitted to the drift tube, more complex gating systems such as a

text: Bradbury-Nielsen

text: design are employed.  Once in the drift tube, ions are subjected to a homogeneous electric field ranging from a few volts per centimeter up to many hundreds of volts per centimeter.  This electric field then drives the ions through the drift tube where they interact with the neutral drift molecules contained within the system.

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answers: 3

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answers: NDQ_003257

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answers: NDQ_003258

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answers: NDQ_003219

answers: drift molecules contained within the system

answers: NDQ_003220

answers: are employed

answers: NDQ_003221

answers: 19th century

answers: NDQ_003222

answers: drift molecules contained within the system

answers: NDQ_003223

answers: Volcanic eruptions

answers: NDQ_003224

answers: drift molecules

answers: NDQ_003225

answers: gating mechanism

answers: NDQ_003226

answers: Europe

answers: NDQ_003227

answers: drift molecules contained within the system

answers: NDQ_003228

answers: drift chamber

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: field

answers: NDQ_003233

answers: Bradbury-Nielsen design

answers: NDQ_003236

answers: a Bradbury-Nielsen design

answers: NDQ_003237

answers: drift molecules

answers: NDQ_003239

answers: Fossil records across continents

answers: NDQ_003240

answers: North America

answers: NDQ_003241

answers: no

answers: NDQ_003242

answers: drift

answers: NDQ_003244

answers: drift

answers: NDQ_003246

answers: continents

answers: NDQ_003247

answers: drift molecules

answers: NDQ_003252

answers: plate tectonics

answers: NDQ_003253

answers: unanswerable

answers: NDQ_003254

answers: It was widely accepted as soon as it was introduced

answers: NDQ_003255

answers: Bradbury-Nielsen design

answers: NDQ_003256

answers: The drift chamber

answers: NDQ_003257

answers: Pangaea broke up a short time ago

answers: NDQ_003258

answers: drift molecules contained within the system

text: In Andrews' 1926 book On the Trail of the Ancient Man, Henry Fairfield Osborn noted in the preface that the birthplace of modern humans would be found in Asia and that he had predicted it decades earlier even before the Asiatic expeditions were carried out. Another key proponent of the out of Asia theory of this era was William Diller Matthew who also took part in the Central Asiatic expeditions; Matthew was well known for his deeply influential 1915 article "Climate and evolution". Matthews theory was that climate change was how organisms came to live where we find them today in opposition to the theory of continental drift. His basic premise was that cyclical changes in global climate along with the prevailing tendency for mammals to disperse from north to south account for the odd geographic patterns of living mammals, he believed that humans and many other groups of modern mammals first evolved in the northern areas of the globe, especially central Asia because of the shifting climatic circumstances, Matthew firmly placed hominid origins in central Asia as he claimed that the high plateaux of Tibet was the forcing ground of mammalian evolution.

text: In Andrews' 1926 book On the Trail of the Ancient Man, Henry Fairfield Osborn noted in the preface that the birthplace of modern humans would be found in Asia and that he had predicted it decades earlier even before the Asiatic expeditions were carried out. Another key proponent of the out of Asia theory of this era was

text: William Diller Matthew

text: who also took part in the Central Asiatic expeditions; Matthew was well known for his deeply influential 1915 article "Climate and evolution". Matthews theory was that climate change was how organisms came to live where we find them today in opposition to the theory of

text: continental drift

text: . His basic premise was that cyclical changes in global climate along with the prevailing tendency for mammals to disperse from north to south account for the odd geographic patterns of living mammals, he believed that humans and many other groups of modern mammals first evolved in the northern areas of the globe, especially central Asia because of the shifting climatic circumstances, Matthew firmly placed hominid origins in central Asia as he claimed that the high plateaux of

text: Tibet

text: was the forcing ground of mammalian evolution.

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answers: NDQ_003239

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text: Geological formations near the lake have been studied by scientists researching continental drift.

text: Geological formations near the lake have been studied by scientists researching continental drift.

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answers: It was widely accepted

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answers: Pangaea

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answers: continental drift

text: Climate is characterized by relatively high temperatures and evenly distributed precipitation throughout the year.  The coldest month is usually quite mild, although frosts are not uncommon, and winter precipitation is derived primarily from frontal cyclones along the polar front.  The Köppen Climate Classification subtype for this climate is "Cfa". (Humid Subtropical Climate).

text: Climate is characterized by relatively high temperatures and evenly distributed precipitation throughout the year.  The coldest month is usually quite mild, although frosts are not uncommon, and winter precipitation is derived primarily from frontal cyclones along the polar front.  The

text: Köppen Climate Classification

text: subtype for this climate is "

text: Cfa

text: ". (Humid Subtropical Climate).

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answers: NDQ_003220

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answers: NDQ_003221

answers: 18th century

answers: NDQ_003222

answers: climate classification subtype

answers: NDQ_003223

answers: polar front

answers: NDQ_003224

answers: glaciers

answers: NDQ_003225

answers: climate classification subtype

answers: NDQ_003226

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answers: NDQ_003227

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answers: NDQ_003228

answers: Köppen Climate Classification

answers: NDQ_003230

answers: North America

answers: NDQ_003231

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answers: NDQ_003233

answers: Köppen Climate Classification

answers: NDQ_003236

answers: polar front

answers: NDQ_003237

answers: relatively high temperatures

answers: NDQ_003239

answers: continental drift

answers: NDQ_003240

answers: North America

answers: NDQ_003241

answers: The polar front

answers: NDQ_003242

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answers: NDQ_003244

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answers: NDQ_003246

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answers: NDQ_003247

answers: Köppen Climate Classification

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: Cfa

answers: NDQ_003254

answers: It was widely accepted as soon as it was introduced

answers: NDQ_003255

answers: Cfa

answers: NDQ_003256

answers: The coldest month is usually quite mild

answers: NDQ_003257

answers: Pangaea broke up a short time ago

answers: NDQ_003258

answers: frontal cyclones

text: An early attempt to build a magnetic confinement system was the stellarator, introduced by Lyman Spitzer in 1951. Essentially the stellarator consists of a torus that has been cut in half and then attached back together with straight "crossover" sections to form a figure-8. This has the effect of propagating the nuclei from the inside to outside as it orbits the device, thereby canceling out the drift across the axis, at least if the nuclei orbit fast enough. Newer versions of the stellarator design have replaced the "mechanical" drift cancellation with additional magnets that "wind" the field lines into a helix to cause the same effect.

text: An early attempt to build a magnetic confinement system was the

text: stellarator

text: , introduced by

text: Lyman Spitzer

text: in 1951. Essentially the stellarator consists of a torus that has been cut in half and then attached back together with straight "crossover" sections to form a figure-8. This has the effect of propagating the nuclei from the inside to outside as it orbits the device, thereby canceling out the drift across the axis, at least if the nuclei orbit fast enough. Newer versions of the stellarator design have replaced the "mechanical" drift cancellation with additional magnets that "wind" the field lines into a helix to cause the same effect.

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answers: NDQ_003219

answers: drift across the axis

answers: NDQ_003220

answers: Atlantic Ocean

answers: NDQ_003221

answers: 1951

answers: NDQ_003222

answers: magnetic confinement system

answers: NDQ_003223

answers: Lyman Spitzer

answers: NDQ_003224

answers: torus

answers: NDQ_003225

answers: stellarator

answers: NDQ_003226

answers: Antarctica

answers: NDQ_003227

answers: cancellation with additional magnets that "wind" the field lines into a helix

answers: NDQ_003228

answers: Lyman Spitzer

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: confinement

answers: NDQ_003233

answers: Spitzer

answers: NDQ_003236

answers: drift across the axis

answers: NDQ_003237

answers: a magnetic confinement system was the stellarator

answers: NDQ_003239

answers: drift across the axis

answers: NDQ_003240

answers: torus

answers: NDQ_003241

answers: no

answers: NDQ_003242

answers: drift

answers: NDQ_003244

answers: drift

answers: NDQ_003246

answers: torus that has been cut in half

answers: NDQ_003247

answers: drift across the axis

answers: NDQ_003252

answers: plate tectonics

answers: NDQ_003253

answers: Lyman Spitzer

answers: NDQ_003254

answers: Spitzer

answers: NDQ_003255

answers: Lyman Spitzer

answers: NDQ_003256

answers: Lyman Spitzer

answers: NDQ_003257

answers: Lyman Spitzer

answers: NDQ_003258

answers: drift across the axis

text: All this evidence, both from the ocean floor and from the continental margins, made it clear around 1965 that continental drift was feasible and the theory of plate tectonics, which was defined in a series of papers between 1965 and 1967, was born, with all its extraordinary explanatory and predictive power. The theory revolutionized the Earth sciences, explaining a diverse range of geological phenomena and their implications in other studies such as paleogeography and paleobiology.

text: All this evidence, both from the ocean floor and from the continental margins, made it clear around 1965 that continental drift was feasible and the theory of plate tectonics, which was defined in a series of papers between 1965 and 1967, was born, with all its extraordinary explanatory and predictive power. The theory revolutionized the Earth sciences, explaining a diverse range of geological phenomena and their implications in other studies such as

text: paleogeography

text: and

text: paleobiology

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answers: The theory revolutionized the Earth sciences

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text: As late as 1953 – just five years before Carey introduced the theory of plate tectonics – the theory of continental drift was rejected by the physicist Scheidegger on the following grounds.

text: As late as 1953 – just five years before

text: Carey

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text: – the theory of continental drift was rejected by the physicist Scheidegger on the following grounds.

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answers: As late as 1953

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text: The Omega Anti-Magnetic Seamasterwas announced 17 January 2013.  According to the press release, the OMEGA movement does not rely on a protective container inside the watchcase but on the use of selected non-ferrous materials in the movement itself. The OMEGA prototype was subjected to 1.5 Tesla (15,000 gauss) and continued to perform. Testing showed that the watch was as accurate after its magnetic exposure as it had been before. A live demonstration was then made that offered compelling and conclusive evidence that OMEGA’s new >15,000 gauss movement is a landmark development in watchmaking. OMEGA expects to present the technology at the Baselworld trade fair in April. The new movement, the OMEGA Co-Axial calibre 8508, should be introduced to the market in 2013.

text: The Omega Anti-Magnetic Seamasterwas announced 17 January 2013.  According to the press release, the OMEGA movement does not rely on a protective container inside the watchcase but on the use of selected non-ferrous materials in the movement itself. The OMEGA prototype was subjected to 1.5 Tesla (15,000 gauss) and continued to perform. Testing showed that the watch was as accurate after its magnetic exposure as it had been before. A live demonstration was then made that offered compelling and conclusive evidence that OMEGA’s new >15,000 gauss movement is a landmark development in watchmaking. OMEGA expects to present the technology at the Baselworld trade fair in April. The new movement, the OMEGA Co-Axial calibre 8508, should be introduced to the market in 2013.

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answers: 1.5 Tesla (15,000 gauss)

answers: NDQ_003220

answers: Baselworld trade fair

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answers: 18th century

answers: NDQ_003222

answers: The Omega Anti-Magnetic Seamasterwas announced 17 January 2013

answers: NDQ_003223

answers: 1.5 Tesla (15,000 gauss)

answers: NDQ_003224

answers: Seamasterwas announced 17 January 2013

answers: NDQ_003225

answers: Omega Anti-Magnetic Seamasterwas announced 17 January 2013

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answers: the Himalayas in eastern North America

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answers: The Omega Anti-Magnetic Seamasterwas announced 17 January 2013

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answers: NDQ_003231

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answers: The Omega Anti-Magnetic Seamasterwas announced 17 January 2013

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answers: The Omega Anti-Magnetic Seamasterwas announced

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answers: The Omega Anti-Magnetic Seamasterwas announced 17 January 2013

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answers: The Omega Anti-Magnetic Seamasterwas announced 17 January 2013

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answers: Oceania

answers: NDQ_003241

answers: Magnetic north pole and geographic north pole

answers: NDQ_003242

answers: 1.5 Tesla

answers: NDQ_003244

answers: The Omega Anti-Magnetic Seamasterwas announced 17 January 2013

answers: NDQ_003246

answers: The Omega Anti-Magnetic Seamasterwas announced 17 January 2013

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answers: The Omega Anti-Magnetic Seamasterwas announced 17 January 2013

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answers: The Omega Anti-Magnetic Seamasterwas announced 17 January 2013

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answers: The Omega Anti-Magnetic Seamasterwas announced 17 January 2013

answers: NDQ_003254

answers: The Omega Anti-Magnetic Seamasterwas announced

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answers: The Omega Anti-Magnetic Seamasterwas announced 17 January 2013

answers: NDQ_003256

answers: The Omega Anti-Magnetic Seamasterwas announced 17 January 2013

answers: NDQ_003257

answers: The Omega Anti-Magnetic Seamasterwas announced

answers: NDQ_003258

answers: The Omega Anti-Magnetic Seamasterwas announced 17 January 2013

text: For the purposes of physiographic mapping, landforms are classified according to both their geologic structures and histories. Distinctions based on geologic age also correspond to physiographic distinctions where the forms are so recent as to be in their first erosion cycle, as is generally the case with sheets of glacial drift. Generally, forms which result from similar histories are characterized by certain similar features, and differences in history result in corresponding differences of form, usually resulting in distinctive features which are obvious to the casual observer, but this is not always the case. A maturely dissected plateau may grade without a break from rugged mountains on the one hand to mildly rolling farm lands on the other. So also, forms which are not classified together may be superficially similar; for example, a young coastal plain and a peneplain. In a large number of cases, the boundary lines are also geologic lines, due to differences in the nature or structure of the underlying rocks.

text: For the purposes of physiographic mapping, landforms are classified according to both their geologic structures and histories. Distinctions based on geologic age also correspond to physiographic distinctions where the forms are so recent as to be in their first

text: erosion cycle

text: , as is generally the case with sheets of

text: glacial drift

text: . Generally, forms which result from similar histories are characterized by certain similar features, and differences in history result in corresponding differences of form, usually resulting in distinctive features which are obvious to the casual observer, but this is not always the case. A maturely

text: dissected plateau

text: may grade without a break from rugged mountains on the one hand to mildly rolling farm lands on the other. So also, forms which are not classified together may be superficially similar; for example, a young

text: coastal plain

text: and a

text: peneplain

text: . In a large number of cases, the boundary lines are also geologic lines, due to differences in the nature or structure of the underlying rocks.

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answers: NDQ_003219

answers: 4

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answers: 3

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answers: 4

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answers: 4

answers: NDQ_003256

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answers: 0

answers: NDQ_003258

answers: 0

answers: NDQ_003219

answers: differences in history result in corresponding differences of form

answers: NDQ_003220

answers: coastal plains

answers: NDQ_003221

answers: geologic

answers: NDQ_003222

answers: the boundary lines are also geologic lines

answers: NDQ_003223

answers: geologic age

answers: NDQ_003224

answers: landforms

answers: NDQ_003225

answers: the boundary lines are also geologic lines

answers: NDQ_003226

answers: Antarctica

answers: NDQ_003227

answers: landforms are classified according to both their geologic structures and histories

answers: NDQ_003228

answers: physiographic mapping

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: magnetic field

answers: NDQ_003233

answers: sheets of glacial drift

answers: NDQ_003236

answers: landforms

answers: NDQ_003237

answers: sheets of glacial drift

answers: NDQ_003239

answers: sheets of glacial drift

answers: NDQ_003240

answers: North America

answers: NDQ_003241

answers: In a large number of cases

answers: NDQ_003242

answers: glacial drift

answers: NDQ_003244

answers: sheets of glacial drift

answers: NDQ_003246

answers: continents have never all been together as a single whole continent

answers: NDQ_003247

answers: landforms are classified according to both their geologic structures and histories

answers: NDQ_003252

answers: glacial drift

answers: NDQ_003253

answers: It is not always the case

answers: NDQ_003254

answers: It was widely accepted as soon as it was introduced

answers: NDQ_003255

answers: In a large number of cases

answers: NDQ_003256

answers: landforms are classified according to both their geologic structures and histories

answers: NDQ_003257

answers: Pangaea broke up a short time ago

answers: NDQ_003258

answers: glacial drift

text: The subarctic climate (also called subpolar climate, subalpine climate, or boreal climate) is a climate characterised by long, usually very cold winters, and short, cool to mild summers. It is found on large landmasses, away from the moderating effects of an ocean, generally at latitudes from 50° to 70°N poleward of the humid continental climates. These climates represent Köppen climate classification Dfc, Dwc, Dsc, Dfd, Dwd and  Dsd. In very small areas at high altitudes around the Mediterranean Basin, Iran, Kyrgyzstan, Tajikistan, Turkey, Alaska and other parts of the northwestern United States (Eastern Washington, Eastern Oregon and Idaho) the climate is classified as Dsc with a dry summer climate, such as in Seneca, Oregon.

text: The subarctic climate (also called subpolar climate, subalpine climate, or boreal climate) is a

text: climate

text: characterised by long, usually very cold winters, and short, cool to mild summers. It is found on large landmasses, away from the moderating effects of an ocean, generally at

text: latitude

text: s from 50° to 70°N poleward of the

text: humid continental climate

text: s. These climates represent

text: Köppen climate classification

text: Dfc, Dwc, Dsc, Dfd, Dwd and  Dsd. In very small areas at high altitudes around the Mediterranean Basin,

text: Iran

text: Kyrgyzstan

text: Tajikistan

text: Turkey

text: Alaska

text: and other parts of the

text: northwestern United States

text: Eastern Washington

text: Eastern Oregon

text: and

text: Idaho

text: ) the climate is classified as Dsc with a dry summer climate, such as in

text: Seneca, Oregon

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answers: large landmasses

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answers: subarctic

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answers: Seneca

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answers: subpolar climate

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answers: It is found on large landmasses

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answers: climate classification Dfc, Dwc, Dsc

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answers: It is found on large landmasses

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answers: North America

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answers: It is found on large landmasses

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answers: It is found on large landmasses, away from the moderating effects of an ocean

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answers: continental drift

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answers: It is found on large landmasses

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answers: The subarctic climate

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answers: It is found on large landmasses

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answers: Pangaea

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answers: The subarctic climate

text: North Korea experiences a combination of continental climate and an oceanic climate, but most of the country experiences a humid continental climate within the Köppen climate classification scheme. Winters bring clear weather interspersed with snow storms as a result of northern and northwestern winds that blow from Siberia. Summer tends to be by far the hottest, most humid, and rainiest time of year because of the southern and southeastern monsoon winds that carry moist air from the Pacific Ocean. Approximately 60 percent of all precipitation occurs from June to September. Spring and autumn are transitional seasons between summer and winter. The daily average high and low temperatures for Pyongyang are  in January and  in August.

text: North Korea experiences a combination of

text: continental climate

text: and an

text: oceanic climate

text: , but most of the country experiences a

text: humid continental climate

text: within the

text: Köppen climate classification

text: scheme. Winters bring clear weather interspersed with snow storms as a result of northern and northwestern winds that blow from

text: Siberia

text: . Summer tends to be by far the hottest, most humid, and rainiest time of year because of the southern and southeastern

text: monsoon

text: winds that carry moist air from the

text: Pacific Ocean

text: . Approximately 60 percent of all precipitation occurs from June to September. Spring and autumn are transitional seasons between summer and winter. The daily average high and low temperatures for

text: Pyongyang

text: are  in January and  in August.

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answers: NDQ_003219

answers: continental climate and an oceanic climate

answers: NDQ_003220

answers: Pacific Ocean

answers: NDQ_003221

answers: climate classification scheme

answers: NDQ_003222

answers: climate classification scheme

answers: NDQ_003223

answers: Siberia

answers: NDQ_003224

answers: Siberia

answers: NDQ_003225

answers: climate classification scheme

answers: NDQ_003226

answers: Siberia

answers: NDQ_003227

answers: climate classification scheme

answers: NDQ_003228

answers: climate classification scheme

answers: NDQ_003230

answers: North Korea

answers: NDQ_003231

answers: magnetic field

answers: NDQ_003233

answers: North Korea experiences a combination of continental climate

answers: NDQ_003236

answers: winds that blow from Siberia

answers: NDQ_003237

answers: Köppen climate classification scheme

answers: NDQ_003239

answers: North Korea experiences a combination of continental climate

answers: NDQ_003240

answers: North Korea

answers: NDQ_003241

answers: Siberia

answers: NDQ_003242

answers: continental climate

answers: NDQ_003244

answers: North Korea

answers: NDQ_003246

answers: North Korea

answers: NDQ_003247

answers: The locations of ancient climate zones

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: North Korea

answers: NDQ_003254

answers: It was widely accepted as soon as it was introduced

answers: NDQ_003255

answers: the Köppen climate classification scheme

answers: NDQ_003256

answers: North Korea

answers: NDQ_003257

answers: Pangaea

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answers: northern and northwestern winds that blow from Siberia

text: The Köppen Climate Classification subtype for this climate is Dfc/Dfb (continental subarctic climate), bordering extremely closely on a humid continental climate.

text: The

text: Köppen Climate Classification

text: subtype for this climate is Dfc/Dfb (

text: continental subarctic climate

text: ), bordering extremely closely on a

text: humid continental climate

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answers: NDQ_003222

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answers: NDQ_003219

answers: subarctic climate

answers: NDQ_003220

answers: arctic

answers: NDQ_003221

answers: 18th century

answers: NDQ_003222

answers: continental subarctic climate

answers: NDQ_003223

answers: continental subarctic climate

answers: NDQ_003224

answers: glaciers

answers: NDQ_003225

answers: continental subarctic climate

answers: NDQ_003226

answers: Antarctica

answers: NDQ_003227

answers: continental subarctic climate

answers: NDQ_003228

answers: continental subarctic climate

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: subarctic

answers: NDQ_003233

answers: Dfc/Dfb

answers: NDQ_003236

answers: continental climate

answers: NDQ_003237

answers: Dfc/Dfb

answers: NDQ_003239

answers: continental drift

answers: NDQ_003240

answers: continental

answers: NDQ_003241

answers: The continental subarctic climate

answers: NDQ_003242

answers: Köppen

answers: NDQ_003244

answers: continental subarctic climate

answers: NDQ_003246

answers: continental subarctic climate

answers: NDQ_003247

answers: continental subarctic climate

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: Dfc/Dfb

answers: NDQ_003254

answers: Dfc/Dfb

answers: NDQ_003255

answers: continental subarctic climate

answers: NDQ_003256

answers: continental subarctic climate

answers: NDQ_003257

answers: Dfc/Dfb

answers: NDQ_003258

answers: continental subarctic climate

text: The Köppen climate classification subtype for this climate is "Dfb" (Cool Summer Continental Climate).

text: The

text: Köppen climate classification

text: subtype for this climate is "

text: Dfb

text: " (Cool Summer Continental Climate).

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answers: NDQ_003231

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answers: NDQ_003233

answers: 0

answers: NDQ_003236

answers: 0

answers: NDQ_003237

answers: 0

answers: NDQ_003239

answers: 0

answers: NDQ_003240

answers: 0

answers: NDQ_003241

answers: 0

answers: NDQ_003242

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answers: NDQ_003244

answers: 0

answers: NDQ_003246

answers: 0

answers: NDQ_003247

answers: 0

answers: NDQ_003252

answers: 0

answers: NDQ_003253

answers: 0

answers: NDQ_003254

answers: 0

answers: NDQ_003255

answers: 0

answers: NDQ_003256

answers: 0

answers: NDQ_003257

answers: 0

answers: NDQ_003258

answers: 0

answers: NDQ_003219

answers: Dfb

answers: NDQ_003220

answers: continental

answers: NDQ_003221

answers: 18th century

answers: NDQ_003222

answers: Dfb

answers: NDQ_003223

answers: Dfb

answers: NDQ_003224

answers: Dfb

answers: NDQ_003225

answers: Cool Summer Continental Climate

answers: NDQ_003226

answers: Europe

answers: NDQ_003227

answers: continental drift

answers: NDQ_003228

answers: Köppen

answers: NDQ_003230

answers: Pangaea

answers: NDQ_003231

answers: Dfb

answers: NDQ_003233

answers: "Dfb" (Cool Summer Continental Climate)

answers: NDQ_003236

answers: continental climate

answers: NDQ_003237

answers: Dfb

answers: NDQ_003239

answers: Dfb

answers: NDQ_003240

answers: continental climate

answers: NDQ_003241

answers: The magnetic north pole and geographic north pole are in different locations.

answers: NDQ_003242

answers: Köppen

answers: NDQ_003244

answers: Dfb

answers: NDQ_003246

answers: continental climate

answers: NDQ_003247

answers: Dfb

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: Dfb

answers: NDQ_003254

answers: Dfb

answers: NDQ_003255

answers: Dfb

answers: NDQ_003256

answers: Dfb

answers: NDQ_003257

answers: Dfb

answers: NDQ_003258

answers: Dfb

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.

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answers: 0: The answer is not relevant or complete at all.

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answers: 4: The answer has limited relevance and completeness, with noticeable gaps or inaccuracy.

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answers: 0

answers: NDQ_003219

answers: 4

answers: NDQ_003220

answers: 0

answers: NDQ_003221

answers: 0

answers: NDQ_003222

answers: 0

answers: NDQ_003223

answers: 0

answers: NDQ_003224

answers: 4

answers: NDQ_003225

answers: 0

answers: NDQ_003226

answers: 0

answers: NDQ_003227

answers: 0

answers: NDQ_003228

answers: 0

answers: NDQ_003230

answers: 0

answers: NDQ_003231

answers: 0

answers: NDQ_003233

answers: 0

answers: NDQ_003236

answers: 0

answers: NDQ_003237

answers: 0

answers: NDQ_003239

answers: 0

answers: NDQ_003240

answers: 0

answers: NDQ_003241

answers: 0

answers: NDQ_003242

answers: 0

answers: NDQ_003244

answers: 0

answers: NDQ_003246

answers: 4

answers: NDQ_003247

answers: 4

answers: NDQ_003252

answers: 4

answers: NDQ_003253

answers: 0

answers: NDQ_003254

answers: 0

answers: NDQ_003255

answers: 4

answers: NDQ_003256

answers: 0

answers: NDQ_003257

answers: 0

answers: NDQ_003258

answers: 0

answers: NDQ_003219

answers: the Intermontane Plate

answers: NDQ_003220

answers: Kootenay Fold Belt

answers: NDQ_003221

answers: Triassic period

answers: NDQ_003222

answers: very few twin subduction zones exist on Earth

answers: NDQ_003223

answers: the Slide Mountain Ocean

answers: NDQ_003224

answers: subduction zone

answers: NDQ_003225

answers: twin subduction zone

answers: NDQ_003226

answers: Asia

answers: NDQ_003227

answers: the North American Plate drifted west and the Intermontane Plate drifted east to the ancient continental margin of western North America

answers: NDQ_003228

answers: pre-existing tectonic plate

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: subduction zone

answers: NDQ_003233

answers: The subduction zone eventually jammed and shut down completely about 180 million years ago

answers: NDQ_003236

answers: As the North American Plate drifted west and the Intermontane Plate drifted east

answers: NDQ_003237

answers: This arrangement of two parallel subduction zones is unusual

answers: NDQ_003239

answers: very few twin subduction zones exist on Earth

answers: NDQ_003240

answers: North America

answers: NDQ_003241

answers: North America

answers: NDQ_003242

answers: tectonic plate

answers: NDQ_003244

answers: North America

answers: NDQ_003246

answers: It began forming during the early Jurassic period

answers: NDQ_003247

answers: This arrangement of two parallel subduction zones is unusual because very few twin subduction zones exist on Earth

answers: NDQ_003252

answers: theory of plate tectonics

answers: NDQ_003253

answers: continents were once joined together

answers: NDQ_003254

answers: As the North American Plate drifted west

answers: NDQ_003255

answers: As the North American Plate drifted west

answers: NDQ_003256

answers: This arrangement of two parallel subduction zones is unusual

answers: NDQ_003257

answers: The subduction zone eventually jammed and shut down completely

answers: NDQ_003258

answers: As the North American Plate drifted west

text: In conjunction with a Nuwaubian Nation parade held in Augusta, Georgia in February 2001, the office of Augusta mayor Bob Young (1999–2005) published a proclamation written by the Nuwaubian organization, stating the group's beliefs. Quotes include "the Nuwbuns were the dark, brown-to-black-skin, wooly-hair original Eygyptians." "[T]he Black race's greatness has been accepted in America and many books as people of Timbuktu Africa or the Olmecians from Uganda, Africa, who migrated and walked here to North and South America to set up colonies way before the continental drift."

text: In conjunction with a Nuwaubian Nation parade held in

text: Augusta, Georgia

text: in February 2001, the office of Augusta mayor

text: Bob Young

text: (1999–2005) published a proclamation written by the Nuwaubian organization, stating the group's beliefs. Quotes include "the Nuwbuns were the dark, brown-to-black-skin, wooly-hair original Eygyptians." "[T]he Black race's greatness has been accepted in America and many books as people of Timbuktu Africa or the Olmecians from Uganda, Africa, who migrated and walked here to North and South America to set up colonies way before the continental drift."

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answers: NDQ_003221

answers: 2001

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answers: Nuwaubian Nation

answers: NDQ_003223

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answers: NDQ_003224

answers: Olmecians

answers: NDQ_003225

answers: The Black race's greatness has been accepted in America

answers: NDQ_003226

answers: Africa

answers: NDQ_003227

answers: migrated and walked here to North and South America to set up colonies way before the continental drift

answers: NDQ_003228

answers: continental drift

answers: NDQ_003230

answers: America

answers: NDQ_003231

answers: magnetic field

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answers: Nuwaubian Nation parade held in Augusta, Georgia

answers: NDQ_003236

answers: continental drift

answers: NDQ_003237

answers: the Nuwaubian Nation parade held in Augusta, Georgia

answers: NDQ_003239

answers: The Nuwaubian Nation parade held in Augusta, Georgia

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answers: Augusta, Georgia

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answers: continental drift

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answers: It was widely accepted as soon as it was introduced

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answers: "the Nuwbuns were the dark, brown-to-black-skin, wooly-hair original Eygyptians

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answers: continental drift

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answers: Pangaea

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answers: continental drift

text: In the 1950s, mapping of the Earth's ocean floors by Bruce Heezen, Maurice Ewing, Marie Tharp and others revealed that the Mid-Atlantic Ridge had a strange bathymetry of valleys and ridges, with its central valley being seismologically active and the epicenter of many earthquakes. Ewing, Heezen and Tharp discovered that the ridge is part of a 40,000-km-long essentially continuous system of mid-ocean ridges on the floors of all the Earth’s oceans. The discovery of this worldwide ridge system led to the theory of seafloor spreading and general acceptance of Wegener's theory of continental drift and expansion in the modified form of plate tectonics. The ridge is central to the breakup of the hypothetical supercontinent of Pangaea that began some 180 million years ago.

text: In the 1950s, mapping of the

text: Earth

text: 's ocean floors by

text: Bruce Heezen

text: Maurice Ewing

text: Marie Tharp

text: and others revealed that the Mid-Atlantic Ridge had a strange

text: bathymetry

text: of valleys and ridges, with its central valley being

text: seismologically

text: active and the

text: epicenter

text: of many

text: earthquake

text: s. Ewing, Heezen and Tharp discovered that the ridge is part of a 40,000-km-long essentially continuous system of

text: mid-ocean ridge

text: s on the floors of all the Earth’s oceans. The discovery of this worldwide ridge system led to the

text: theory

text: of

text: seafloor spreading

text: and general acceptance of

text: Wegener

text: 's theory of

text: continental drift

text: and expansion in the modified form of

text: plate tectonics

text: . The ridge is central to the breakup of the

text: hypothetical

text: supercontinent

text: of

text: Pangaea

text: that began some 180 million years ago.

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answers: NDQ_003220

answers: Mid-Atlantic Ridge

answers: NDQ_003221

answers: 1950s

answers: NDQ_003222

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answers: NDQ_003223

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answers: NDQ_003224

answers: Pangaea

answers: NDQ_003225

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answers: NDQ_003226

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answers: NDQ_003227

answers: the modified form of plate tectonics

answers: NDQ_003228

answers: continental drift and expansion

answers: NDQ_003230

answers: the hypothetical supercontinent

answers: NDQ_003231

answers: epicenter

answers: NDQ_003233

answers: the Mid-Atlantic Ridge

answers: NDQ_003236

answers: Wegener's theory

answers: NDQ_003237

answers: Mid-Atlantic Ridge

answers: NDQ_003239

answers: mid-ocean ridges on the floors of all the Earth’s oceans

answers: NDQ_003240

answers: Pangaea

answers: NDQ_003241

answers: Earth's ocean floors

answers: NDQ_003242

answers: plate tectonics

answers: NDQ_003244

answers: Mid-Atlantic Ridge

answers: NDQ_003246

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answers: NDQ_003247

answers: Mid-Atlantic Ridge

answers: NDQ_003252

answers: plate tectonics

answers: NDQ_003253

answers: hypothetical supercontinent of Pangaea

answers: NDQ_003254

answers: The discovery of this worldwide ridge system led to the theory of seafloor spreading and general acceptance

answers: NDQ_003255

answers: Wegener's theory of continental drift and expansion in the modified form of plate tectonics

answers: NDQ_003256

answers: Mid-Atlantic

answers: NDQ_003257

answers: 180 million years ago

answers: NDQ_003258

answers: plate tectonics

text: With the advent of the Global Positioning System (GPS), it became possible to measure continental drift directly.

text: With the advent of the

text: Global Positioning System

text: (GPS), it became possible to measure continental drift directly.

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answers: continental drift

answers: NDQ_003220

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answers: NDQ_003221

answers: 18th century

answers: NDQ_003222

answers: it became possible to measure continental drift

answers: NDQ_003223

answers: continental drift

answers: NDQ_003224

answers: GPS

answers: NDQ_003225

answers: Continental drift

answers: NDQ_003226

answers: Europe

answers: NDQ_003227

answers: measure continental drift

answers: NDQ_003228

answers: it became possible to measure continental drift directly

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: Magnetic field

answers: NDQ_003233

answers: it became possible to measure continental drift directly

answers: NDQ_003236

answers: continental drift

answers: NDQ_003237

answers: the Global Positioning System (GPS)

answers: NDQ_003239

answers: It became possible to measure continental drift

answers: NDQ_003240

answers: continental drift

answers: NDQ_003241

answers: It became possible to measure continental drift directly

answers: NDQ_003242

answers: continental drift

answers: NDQ_003244

answers: continental drift

answers: NDQ_003246

answers: Continental drift

answers: NDQ_003247

answers: Global Positioning System

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: Wegener

answers: NDQ_003254

answers: It became possible to measure continental drift directly

answers: NDQ_003255

answers: it became possible to measure continental drift directly

answers: NDQ_003256

answers: Continental drift

answers: NDQ_003257

answers: It became possible to measure continental drift directly

answers: NDQ_003258

answers: Wegener

text: Wegener obtained a position as a meteorologist at the German Naval Observatory (Deutsche Seewarte) and moved to Hamburg with his wife and their two daughters. In 1921 he was appointed senior lecturer at the new University of Hamburg. From 1919 to 1923 Wegener did pioneering work on reconstructing the climate of past eras (now known as "paleoclimatology"), closely in collaboration with Milutin Milanković, publishing Die Klimate der geologischen Vorzeit (“The Climates of the Geological Past”) together with his father-in-law, Wladimir Köppen, in 1924. In 1922 the third, fully revised edition of “The Origin of Continents and Oceans” appeared, and discussion began on his theory of continental drift, first in the German language area and later internationally. Withering criticism was the response of most experts.

text: Wegener obtained a position as a meteorologist at the German Naval Observatory (Deutsche Seewarte) and moved to

text: Hamburg

text: with his wife and their two daughters. In 1921 he was appointed senior lecturer at the new

text: University of Hamburg

text: . From 1919 to 1923 Wegener did pioneering work on reconstructing the climate of past eras (now known as "

text: paleoclimatology

text: "), closely in collaboration with

text: Milutin Milanković

text: , publishing Die Klimate der geologischen Vorzeit (“The Climates of the Geological Past”) together with his father-in-law, Wladimir Köppen, in 1924. In 1922 the third, fully revised edition of “The Origin of Continents and Oceans” appeared, and discussion began on his theory of continental drift, first in the German language area and later internationally. Withering criticism was the response of most experts.

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answers: 3

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answers: 2

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answers: 0

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answers: 4

answers: NDQ_003225

answers: 4

answers: NDQ_003226

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answers: NDQ_003227

answers: 4

answers: NDQ_003228

answers: 4

answers: NDQ_003230

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answers: 4

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answers: 4

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answers: 4

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answers: 4

answers: NDQ_003252

answers: 3

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answers: 4

answers: NDQ_003254

answers: 2

answers: NDQ_003255

answers: 4

answers: NDQ_003256

answers: 0

answers: NDQ_003257

answers: 0

answers: NDQ_003258

answers: 4

answers: NDQ_003219

answers: continental drift

answers: NDQ_003220

answers: German Naval Observatory

answers: NDQ_003221

answers: 1922

answers: NDQ_003222

answers: Withering criticism

answers: NDQ_003223

answers: continental drift

answers: NDQ_003224

answers: paleoclimatology

answers: NDQ_003225

answers: continental drift

answers: NDQ_003226

answers: Germany

answers: NDQ_003227

answers: The Origin of Continents and Oceans

answers: NDQ_003228

answers: continental drift

answers: NDQ_003230

answers: Oceans

answers: NDQ_003231

answers: Seewarte

answers: NDQ_003233

answers: discussion began on his theory of continental drift

answers: NDQ_003236

answers: continental drift

answers: NDQ_003237

answers: the climate of past eras

answers: NDQ_003239

answers: Paleoclimatology

answers: NDQ_003240

answers: North America

answers: NDQ_003241

answers: The German Naval Observatory

answers: NDQ_003242

answers: theory of continental drift

answers: NDQ_003244

answers: paleoclimatology

answers: NDQ_003246

answers: continental drift

answers: NDQ_003247

answers: paleoclimatology

answers: NDQ_003252

answers: theory of continental drift

answers: NDQ_003253

answers: theory of continental drift

answers: NDQ_003254

answers: Withering criticism

answers: NDQ_003255

answers: “The Origin of Continents and Oceans” appeared

answers: NDQ_003256

answers: continental drift

answers: NDQ_003257

answers: Pangaea

answers: NDQ_003258

answers: theory of continental drift

text: Microfossil is a descriptive term applied to fossilized plants and animals whose size is just at or below the level at which the fossil can be analyzed by the naked eye. A commonly applied cutoff point between "micro" and "macro" fossils is 1 mm. Microfossils may either be complete (or near-complete) organisms in themselves (such as the marine plankters foraminifera and coccolithophores) or component parts (such as small teeth or spores) of larger animals or plants. Microfossils are of critical importance as a reservoir of paleoclimate information, and are also commonly used by biostratigraphers to assist in the correlation of rock units.

text: Microfossil is a descriptive term applied to fossilized plants and animals whose size is just at or below the level at which the fossil can be analyzed by the naked eye. A commonly applied cutoff point between "micro" and

text: "macro" fossils

text: is 1 mm. Microfossils may either be complete (or near-complete) organisms in themselves (such as the marine plankters

text: foraminifera

text: and

text: coccolithophore

text: s) or component parts (such as small teeth or

text: spores

text: ) of larger animals or plants. Microfossils are of critical importance as a reservoir of

text: paleoclimate

text: information, and are also commonly used by

text: biostratigraphers

text: to assist in the correlation of rock units.

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answers: 0

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answers: 0

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answers: NDQ_003219

answers: microfossils are of critical importance as a reservoir of paleoclimate information

answers: NDQ_003220

answers: Atlantic Ocean

answers: NDQ_003221

answers: paleoclimate

answers: NDQ_003222

answers: microfossils

answers: NDQ_003223

answers: fossilized plants and animals

answers: NDQ_003224

answers: fossilized plants and animals

answers: NDQ_003225

answers: Microfossil

answers: NDQ_003226

answers: Europe

answers: NDQ_003227

answers: paleoclimate information

answers: NDQ_003228

answers: biostratigraphers

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: magnetism

answers: NDQ_003233

answers: Microfossils

answers: NDQ_003236

answers: paleoclimate

answers: NDQ_003237

answers: Microfossils

answers: NDQ_003239

answers: Microfossils

answers: NDQ_003240

answers: North America

answers: NDQ_003241

answers: no

answers: NDQ_003242

answers: paleoclimate

answers: NDQ_003244

answers: Microfossils

answers: NDQ_003246

answers: The continents have never been together

answers: NDQ_003247

answers: Microfossils

answers: NDQ_003252

answers: plate tectonics

answers: NDQ_003253

answers: rock units

answers: NDQ_003254

answers: It was widely accepted

answers: NDQ_003255

answers: Microfossils

answers: NDQ_003256

answers: The Atlantic Ocean

answers: NDQ_003257

answers: Pangaea

answers: NDQ_003258

answers: Microfossils

text: Grabau and Garretson believed in and studied the theory of horizontal displacement, and was considered to be a mobilist. The theory of horizontal displacement was first proposed by Alfred Wegner in 1912 and, due to popular belief at that time, was not widely accepted, especially in North America and Europe. The theory starting gaining traction when the model of plate tectonics and continental drift were first introduced. With these models in place, geologists began searching for fossil evidence that could prove that organisms, that can be found all over the globe now, once existed in the same location. Professor Grabau and Mrs. Garretson were among the scientist who took interest to Wegner's claim, and began looking for fossil evidence in North America. During her tenure at Columbia University, Mrs. Garretson assisted Professor Grabau in his book titled "North American Index Fossils." The goal of this paper was to study the various index fossils found in North America and try to compile evidence that supported the theory that a single, great continent was existed on Earth called Pangaea. The book goes into tremendous detail regarding information on each class of fossils found, and each class having its separate structural descriptions and general description of key characteristics tying it to a family, or, genus. A few examples of evidence from Grabau's book are provided:

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answers: 4

answers: NDQ_003240

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answers: 3

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answers: NDQ_003252

answers: 4

answers: NDQ_003253

answers: 4

answers: NDQ_003254

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answers: NDQ_003255

answers: 4

answers: NDQ_003256

answers: 0

answers: NDQ_003257

answers: 0

answers: NDQ_003258

answers: 4

answers: NDQ_003219

answers: Pangaea

answers: NDQ_003220

answers: North America

answers: NDQ_003221

answers: 1912

answers: NDQ_003222

answers: popular belief at that time

answers: NDQ_003223

answers: Pangaea

answers: NDQ_003224

answers: Pangaea

answers: NDQ_003225

answers: The theory of horizontal displacement

answers: NDQ_003226

answers: Europe

answers: NDQ_003227

answers: a single, great continent was existed on Earth

answers: NDQ_003228

answers: first proposed

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: magnetism

answers: NDQ_003233

answers: North American Index Fossils

answers: NDQ_003236

answers: continental drift

answers: NDQ_003237

answers: North American Index Fossils

answers: NDQ_003239

answers: Pangaea

answers: NDQ_003240

answers: Pangaea

answers: NDQ_003241

answers: Pangaea

answers: NDQ_003242

answers: plate tectonics

answers: NDQ_003244

answers: Pangaea

answers: NDQ_003246

answers: Pangaea

answers: NDQ_003247

answers: fossils found in North America

answers: NDQ_003252

answers: plate tectonics

answers: NDQ_003253

answers: Pangaea

answers: NDQ_003254

answers: The theory starting gaining traction

answers: NDQ_003255

answers: North American Index Fossils

answers: NDQ_003256

answers: Pangaea

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answers: The theory of horizontal displacement was first proposed by Alfred Wegner in 1912

answers: NDQ_003258

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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.

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answers: Earth’s tectonic plates are separating

answers: NDQ_003220

answers: Mid-Ocean

answers: NDQ_003221

answers: late Cretaceous

answers: NDQ_003222

answers: Mid-Ocean ridges

answers: NDQ_003223

answers: Earth’s tectonic plates

answers: NDQ_003224

answers: seafloor spreading

answers: NDQ_003225

answers: seafloor spreading

answers: NDQ_003226

answers: Mid-Ocean ridges

answers: NDQ_003227

answers: This seafloor spreading is the engine of continental drift

answers: NDQ_003228

answers: Mid-Ocean ridges

answers: NDQ_003230

answers: Earth

answers: NDQ_003231

answers: magnetic field

answers: NDQ_003233

answers: Mid-Ocean ridges

answers: NDQ_003236

answers: continental drift

answers: NDQ_003237

answers: Mid-Ocean ridges

answers: NDQ_003239

answers: Mid-Ocean ridges

answers: NDQ_003240

answers: Earth’s

answers: NDQ_003241

answers: Earth’s

answers: NDQ_003242

answers: tectonic plates

answers: NDQ_003244

answers: Mid-Ocean ridges

answers: NDQ_003246

answers: continental drift

answers: NDQ_003247

answers: Mid-Ocean ridges

answers: NDQ_003252

answers: Mid-Ocean ridges

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answers: Mid-Ocean ridges

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answers: Mid-Ocean ridges

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answers: Mid-Ocean ridges

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answers: Mid-Ocean Ridges

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answers: Mid-Ocean ridges

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answers: Mid-Ocean ridges

text: The climate of Bathurst is classified as humid continental (Köppen climate classification Dfb).

text: The

text: climate

text: of Bathurst is classified as

text: humid continental

text: Köppen climate classification

text: Dfb).

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answers: Humid continental

answers: NDQ_003220

answers: Bathurst

answers: NDQ_003221

answers: Köppen

answers: NDQ_003222

answers: climate classification Dfb

answers: NDQ_003223

answers: Dfb

answers: NDQ_003224

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answers: NDQ_003225

answers: Köppen

answers: NDQ_003226

answers: Europe

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answers: NDQ_003228

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answers: NDQ_003230

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answers: NDQ_003231

answers: Köppen

answers: NDQ_003233

answers: Köppen climate classification

answers: NDQ_003236

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answers: Köppen climate classification

answers: NDQ_003239

answers: continental drift

answers: NDQ_003240

answers: continental

answers: NDQ_003241

answers: The magnetic north pole and geographic north pole are in the same location.

answers: NDQ_003242

answers: Köppen

answers: NDQ_003244

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answers: NDQ_003247

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answers: Köppen climate classification Dfb

answers: NDQ_003257

answers: Köppen climate classification Dfb

answers: NDQ_003258

answers: Köppen

text: During reconstruction of the original runway 12/30, the runway was renumbered to the current 13/31 designation.  The Earth's magnetic north pole moves continuously, and when the original runway was constructed the magnetic headings were approximately 120 and 300.  Magnetic north drifted over the life of the runway, such that by the time it was due for reconstruction, the magnetic headings were closer to 130 and 310.

text: During reconstruction of the original runway 12/30, the runway was renumbered to the current 13/31 designation.  The

text: Earth's magnetic north pole

text: moves continuously, and when the original runway was constructed the magnetic headings were approximately 120 and 300.

text: Magnetic north

text: drifted over the life of the runway, such that by the time it was due for reconstruction, the magnetic headings were closer to 130 and 310.

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answers: The Earth's magnetic north pole moves continuously

answers: NDQ_003220

answers: are not mentioned

answers: NDQ_003221

answers: 19th century

answers: NDQ_003222

answers: Magnetic north drifted over the life of the runway

answers: NDQ_003223

answers: Earth

answers: NDQ_003224

answers: magnetic headings

answers: NDQ_003225

answers: Magnetic north drifted

answers: NDQ_003226

answers: the Himalayas

answers: NDQ_003227

answers: The Earth's magnetic north pole moves continuously

answers: NDQ_003228

answers: when the original runway was constructed

answers: NDQ_003230

answers: Earth

answers: NDQ_003231

answers: pole

answers: NDQ_003233

answers: Magnetic north drifted over the life of the runway

answers: NDQ_003236

answers: The Earth's magnetic north pole moves continuously

answers: NDQ_003237

answers: magnetic headings were closer to 130 and 310

answers: NDQ_003239

answers: Magnetic north drifted

answers: NDQ_003240

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answers: NDQ_003241

answers: Earth's

answers: NDQ_003242

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answers: The original runway was constructed

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answers: Magnetic north drifted

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text: Recordings of Richards playing other instruments besides guitar are not unusual. He has played bass guitar on several Rolling Stones' studio recordings, including "Sympathy for the Devil" (1968) and "Happy" (1972). Richards also played bass guitar for the supergroup The Dirty Mac. Richards regards keyboards as a songwriting tool and has played them on several Rolling Stones recordings and played them live for two Ronnie Wood concerts and during The New Barbarians' 1979 tour. Richards has also played percussion on select Rolling Stones tracks, such as the floor tom on "Jumpin' Jack Flash" (1968), tambourine on "Infamy" (2005) and bicycle spokes on "Continental Drift" (1989).

text: Recordings of Richards playing other instruments besides guitar are not unusual. He has played bass guitar on several Rolling Stones' studio recordings, including "

text: Sympathy for the Devil

text: " (1968) and "

text: Happy

text: " (1972). Richards also played bass guitar for the supergroup The Dirty Mac. Richards regards keyboards as a songwriting tool and has played them on several Rolling Stones recordings and played them live for two Ronnie Wood concerts and during

text: The New Barbarians

text: ' 1979 tour. Richards has also played percussion on select Rolling Stones tracks, such as the floor tom on "Jumpin' Jack Flash" (1968), tambourine on "Infamy" (2005) and bicycle spokes on "Continental Drift" (1989).

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text: A useful approach to considering Britain's geological structure is to examine the various

text: terrane

text: s from which it is composed. These are essentially continental fragments whose boundaries are generally defined by faults. Individual terranes typically contain suites of structures, the histories and form of which differ from those of neighbouring terranes.

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text: A 3D short-film entitled The Longest Daycare, focusing on Maggie, was shown in theaters before the 2012 film Ice Age: Continental Drift. It received an Academy Award nomination in the category of best animated short film.

text: A 3D short-film entitled

text: The Longest Daycare

text: , focusing on

text: Maggie

text: , was shown in theaters before the 2012 film

text: Ice Age: Continental Drift

text: . It received an

text: Academy Award

text: nomination in the category of

entity_name: Academy Award for Best Animated Short Film

text: best animated short film

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text: In North America, microthermal climates commence north of Boston along the Atlantic seaboard, this line drifting gradually southward further inland, reaching approximately 38° at the eastern edge of the Rocky Mountains, then curving dramatically northward near the Pacific coast, reaching the Pacific Ocean just south of Juneau, Alaska.  In Asia, the latitude at which these climates begin is several degrees lower due to the pervasive influence of the vast Siberian anticyclone, or high-pressure system, and in continental Europe the line actually runs longitudinally rather than latitudinally, cutting through central Poland after beginning north of the Arctic Circle along the Norwegian coast, thereafter moving diagonally across Scandinavia.

text: In

text: North America

text: , microthermal climates commence north of Boston along the Atlantic seaboard, this line drifting gradually southward further inland, reaching approximately 38° at the eastern edge of the

text: Rocky Mountains

text: , then curving dramatically northward near the

text: Pacific

text: coast, reaching the Pacific Ocean just south of

text: Juneau, Alaska

text: .  In

text: Asia

text: , the latitude at which these climates begin is several degrees lower due to the pervasive influence of the vast Siberian anticyclone, or high-pressure system, and in continental

text: Europe

text: the line actually runs longitudinally rather than latitudinally, cutting through central

text: Poland

text: after beginning north of the

text: Arctic Circle

text: along the Norwegian coast, thereafter moving diagonally across

text: Scandinavia

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answers: climates commence north of Boston along the Atlantic seaboard

answers: NDQ_003220

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answers: NDQ_003221

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answers: NDQ_003222

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answers: NDQ_003223

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answers: NDQ_003227

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answers: NDQ_003228

answers: high-pressure system

answers: NDQ_003230

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answers: NDQ_003231

answers: Arctic Circle

answers: NDQ_003233

answers: this line drifting gradually southward further inland, reaching approximately 38° at the eastern edge of the Rocky Mountains, then curving dramatically northward near the Pacific coast

answers: NDQ_003236

answers: drifting gradually southward further inland

answers: NDQ_003237

answers: this line drifting gradually southward further inland, reaching approximately 38° at the eastern edge of the Rocky Mountains

answers: NDQ_003239

answers: microthermal climates commence north of Boston along the Atlantic seaboard

answers: NDQ_003240

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answers: This line drifting gradually southward further inland, reaching approximately 38° at the eastern edge of the Rocky Mountains, then curving dramatically northward near the Pacific coast, reaching the Pacific Ocean just south of Juneau, Alaska

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answers: Microthermal climates commence north of Boston

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text: Systematic errors which change during an experiment (drift) are easier to detect. Measurements indicate trends with time rather than varying randomly about a mean. Drift is evident if a measurement of a constant quantity is repeated several times and the measurements drift one way during the experiment. If the next measurement is higher than the previous measurement as may occur if an instrument becomes warmer during the experiment then the measured quantity is variable and it is possible to detect a drift by checking the zero reading during the experiment as well as at the start of the experiment (indeed, the zero reading is a measurement of a constant quantity). If the zero reading is consistently above or below zero, a systematic error is present. If this cannot be eliminated, potentially by resetting the instrument immediately before the experiment then it needs to be allowed by subtracting its (possibly time-varying) value from the readings, and by taking it into account while assessing the accuracy of the measurement.

text: Systematic errors which change during an experiment (

text: drift

text: ) are easier to detect. Measurements indicate trends with time rather than varying randomly about a

text: mean

text: . Drift is evident if a measurement of a

text: constant

text: quantity is repeated several times and the measurements drift one way during the experiment. If the next measurement is higher than the previous measurement as may occur if an instrument becomes warmer during the experiment then the measured quantity is variable and it is possible to detect a drift by checking the zero reading during the experiment as well as at the start of the experiment (indeed, the

text: zero reading

text: is a measurement of a constant quantity). If the zero reading is consistently above or below zero, a systematic error is present. If this cannot be eliminated, potentially by resetting the instrument immediately before the experiment then it needs to be allowed by subtracting its (possibly time-varying) value from the readings, and by taking it into account while assessing the accuracy of the measurement.

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answers: are easier to detect

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answers: 18th century

answers: NDQ_003222

answers: Systematic errors which change during an experiment

answers: NDQ_003223

answers: Drift

answers: NDQ_003224

answers: measurement of a constant quantity

answers: NDQ_003225

answers: Drift

answers: NDQ_003226

answers: Antarctica

answers: NDQ_003227

answers: systematic errors which change during an experiment (drift) are easier to detect

answers: NDQ_003228

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answers: NDQ_003230

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answers: NDQ_003231

answers: Drift

answers: NDQ_003233

answers: Systematic errors which change during an experiment (drift) are easier to detect

answers: NDQ_003236

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answers: If the zero reading is consistently above or below zero

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answers: It is possible to detect a drift by checking the zero reading during the experiment as well as at the start of the experiment

answers: NDQ_003240

answers: Drift

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answers: no

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answers: It is possible to detect a drift by checking the zero reading during the experiment as well as at the start of the experiment

answers: NDQ_003246

answers: The continents have never all been together as a single whole continent.

answers: NDQ_003247

answers: If the zero reading is consistently above or below zero

answers: NDQ_003252

answers: plate tectonics

answers: NDQ_003253

answers: The zero reading is a measurement of a constant quantity

answers: NDQ_003254

answers: It was widely accepted as soon as it was introduced

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answers: Systematic errors which change during an experiment (drift) are easier to detect

answers: NDQ_003256

answers: If the zero reading is consistently above or below zero, a systematic error is present

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answers: Pangaea broke up a short time ago

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answers: Systematic errors which change during an experiment

text: In 1578 he laid the basis of a critical treatment of ancient geography by his Synonymia geographica (issued by the Plantin press at Antwerp and republished in expanded form as Thesaurus geographicus in 1587 and again expanded in 1596. In this last edition, Ortelius considers the possibility of continental drift, a hypothesis proved correct only centuries later).

text: In 1578 he laid the basis of a critical treatment of ancient geography by his Synonymia geographica (issued by the

text: Plantin press

text: at Antwerp and republished in expanded form as Thesaurus geographicus in 1587 and again expanded in 1596. In this last edition, Ortelius considers the possibility of

text: continental drift

text: , a hypothesis proved correct only centuries later).

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answers: NDQ_003225

answers: continental drift

answers: NDQ_003226

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answers: NDQ_003227

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answers: NDQ_003228

answers: Ortelius considers the possibility of continental drift

answers: NDQ_003230

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answers: NDQ_003231

answers: Thesaurus geographicus

answers: NDQ_003233

answers: Ortelius

answers: NDQ_003236

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answers: NDQ_003237

answers: Synonymia geographica

answers: NDQ_003239

answers: a hypothesis proved correct only centuries later

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answers: NDQ_003241

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answers: NDQ_003242

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answers: NDQ_003246

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answers: NDQ_003252

answers: Synonymia geographica

answers: NDQ_003253

answers: Synonymia geographica

answers: NDQ_003254

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answers: Ortelius

text: Manfred "Manny", is a woolly mammoth, in all five Ice Age films. His personality is shown to be aloof and stand-offish, but is otherwise loving and courageous. In the first film, while passing through the icy cave, the herd discovers cave paintings of Manny with his wife and child, who were killed by humans; this is a very sentimental moment for Manny, since he failed to protect them. At the end of the film, Manny and Sid return Roshan to the neanderthals with an injured Diego trailing behind them. He finds love with Ellie in Ice Age: The Meltdown. In Ice Age: Dawn of the Dinosaurs, he is anxious when Ellie is pregnant. At the end of the film, he becomes the proud father of a baby daughter named Peaches. In Ice Age: Continental Drift, he gets into an argument with his teenage daughter before being pulled away in by the drift with Diego, Sid and Granny. He and the team later encounter a group of pirates led by Captain Gutt. When the team escaped they destroy the ship and take Shira with them. This enrages the Captain who hunts them down. Later on, he is almost manipulated by sirens.

text: Manfred "Manny", is a

text: woolly mammoth

text: , in all five

text: Ice Age

text: films. His personality is shown to be aloof and stand-offish, but is otherwise loving and courageous. In the first film, while passing through the icy cave, the herd discovers

text: cave painting

text: s of Manny with his wife and child, who were killed by

text: human

text: s; this is a very sentimental moment for Manny, since he failed to protect them. At the end of the film, Manny and Sid return Roshan to the

text: neanderthal

text: s with an injured Diego trailing behind them. He finds love with Ellie in

text: Ice Age: The Meltdown

text: . In

text: Ice Age: Dawn of the Dinosaurs

text: , he is anxious when Ellie is pregnant. At the end of the film, he becomes the proud father of a baby daughter named Peaches. In

text: Ice Age: Continental Drift

text: , he gets into an argument with his teenage daughter before being pulled away in by the drift with Diego, Sid and Granny. He and the team later encounter a group of pirates led by Captain Gutt. When the team escaped they destroy the ship and take Shira with them. This enrages the Captain who hunts them down. Later on, he is almost manipulated by

text: sirens

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answers: NDQ_003219

answers: humans killed by dinosaurs

answers: NDQ_003220

answers: continental

answers: NDQ_003221

answers: Ice Age

answers: NDQ_003222

answers: sirens

answers: NDQ_003223

answers: humans

answers: NDQ_003224

answers: cave paintings

answers: NDQ_003225

answers: manipulated by sirens

answers: NDQ_003226

answers: Ice Age

answers: NDQ_003227

answers: pulled away in by the drift with Diego, Sid and Granny

answers: NDQ_003228

answers: continental drift

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: The Meltdown

answers: NDQ_003233

answers: cave paintings

answers: NDQ_003236

answers: Continental Drift

answers: NDQ_003237

answers: cave paintings

answers: NDQ_003239

answers: In Ice Age: Continental Drift

answers: NDQ_003240

answers: the Neanderthals

answers: NDQ_003241

answers: The geographic north pole

answers: NDQ_003242

answers: continental drift

answers: NDQ_003244

answers: continental drift

answers: NDQ_003246

answers: The continents

answers: NDQ_003247

answers: cave paintings

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: Continental Drift

answers: NDQ_003254

answers: It was widely accepted

answers: NDQ_003255

answers: cave paintings

answers: NDQ_003256

answers: The Atlantic Ocean

answers: NDQ_003257

answers: Pangaea

answers: NDQ_003258

answers: Continental Drift

text: Southwestern Wisconsin and parts of the adjacent states of Illinois, Iowa and Minnesota are known as the driftless zone, because, although bordered by drift sheets and moraines, it is free from glacial deposits. It must therefore have been a sort of oasis, when the ice sheets from the north advanced past it on the east and west and joined around its southern border. The reason for this exemption from glaciation is the converse of that for the southward convexity of the morainic loops. For while they mark the paths of greatest glacial advance along lowland troughs (lake basins), the driftless zone is a district protected from ice invasion by reason of the obstruction which the highlands of northern Wisconsin and Michigan (part of the Superior upland) offered to glacial advance.

text: Southwestern

text: Wisconsin

text: and parts of the adjacent states of

text: Illinois

text: Iowa

text: and

text: Minnesota

text: are known as the

text: driftless zone

text: , because, although bordered by drift sheets and moraines, it is free from glacial deposits. It must therefore have been a sort of oasis, when the ice sheets from the north advanced past it on the east and west and joined around its southern border. The reason for this exemption from glaciation is the converse of that for the southward convexity of the morainic loops. For while they mark the paths of greatest glacial advance along lowland troughs (lake basins), the driftless zone is a district protected from ice invasion by reason of the obstruction which the highlands of northern Wisconsin and Michigan (part of the Superior upland) offered to glacial advance.

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answers: NDQ_003219

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answers: NDQ_003220

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answers: NDQ_003221

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answers: NDQ_003222

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answers: NDQ_003223

answers: 0

answers: NDQ_003224

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answers: NDQ_003225

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answers: NDQ_003226

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answers: NDQ_003227

answers: 0

answers: NDQ_003228

answers: 0

answers: NDQ_003230

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answers: NDQ_003231

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answers: NDQ_003233

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answers: NDQ_003236

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answers: NDQ_003237

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answers: NDQ_003239

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answers: NDQ_003240

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answers: NDQ_003241

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answers: NDQ_003242

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answers: NDQ_003244

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answers: NDQ_003246

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answers: NDQ_003247

answers: 4

answers: NDQ_003252

answers: 4

answers: NDQ_003253

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answers: NDQ_003254

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answers: NDQ_003255

answers: 4

answers: NDQ_003256

answers: 0

answers: NDQ_003257

answers: 0

answers: NDQ_003258

answers: 0

answers: NDQ_003219

answers: drift sheets and moraines

answers: NDQ_003220

answers: Superior upland

answers: NDQ_003221

answers: 18th century

answers: NDQ_003222

answers: it is free from glacial deposits

answers: NDQ_003223

answers: Superior upland

answers: NDQ_003224

answers: glacial deposits

answers: NDQ_003225

answers: the driftless zone

answers: NDQ_003226

answers: Europe

answers: NDQ_003227

answers: ice sheets from the north advanced past it on the east and west and joined around its southern border

answers: NDQ_003228

answers: drift sheets and moraines

answers: NDQ_003230

answers: Wisconsin

answers: NDQ_003231

answers: zone

answers: NDQ_003233

answers: drift sheets and moraines

answers: NDQ_003236

answers: It must therefore have been a sort of oasis

answers: NDQ_003237

answers: drift sheets and moraines

answers: NDQ_003239

answers: drift sheets and moraines

answers: NDQ_003240

answers: North America

answers: NDQ_003241

answers: Wisconsin

answers: NDQ_003242

answers: morainic loops

answers: NDQ_003244

answers: driftless zone

answers: NDQ_003246

answers: It must therefore have been a sort of oasis

answers: NDQ_003247

answers: drift sheets and moraines

answers: NDQ_003252

answers: plate tectonics

answers: NDQ_003253

answers: It must therefore have been a sort of oasis

answers: NDQ_003254

answers: It must therefore have been a sort of oasis

answers: NDQ_003255

answers: Wegener and his supporters provided a lot of evidence for continental drift

answers: NDQ_003256

answers: It must therefore have been a sort of oasis

answers: NDQ_003257

answers: The driftless zone

answers: NDQ_003258

answers: Morainic loops

text: Fossils of organisms' bodies are usually the most informative type of evidence. The most common types are wood, bones, and shells. Fossilisation is a rare event, and most fossils are destroyed by erosion or metamorphism before they can be observed. Hence the fossil record is very incomplete, increasingly so further back in time. Despite this, it is often adequate to illustrate the broader patterns of life's history. There are also biases in the fossil record: different environments are more favorable to the preservation of different types of organism or parts of organisms. Further, only the parts of organisms that were already mineralised are usually preserved, such as the shells of molluscs. Since most animal species are soft-bodied, they decay before they can become fossilised. As a result, although there are 30-plus phyla of living animals, two-thirds have never been found as fossils.

text: Fossils of organisms' bodies are usually the most informative type of evidence. The most common types are wood, bones, and shells. Fossilisation is a rare event, and most fossils are destroyed by

text: erosion

text: or

text: metamorphism

text: before they can be observed. Hence the fossil record is very incomplete, increasingly so further back in time. Despite this, it is often adequate to illustrate the broader patterns of life's history. There are also biases in the fossil record: different environments are more favorable to the preservation of different types of organism or parts of organisms. Further, only the parts of organisms that were already

text: mineralised

text: are usually preserved, such as the shells of molluscs. Since most animal species are soft-bodied, they decay before they can become fossilised. As a result, although there are 30-plus

text: phyla

text: of living animals, two-thirds have never been found as fossils.

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answers: 0

answers: tqa2:L_0076/T_0763/7a7192cbfb0cdb83fb089d3c4f8ea239

answers: 0

answers: NDQ_003219

answers: 0

answers: NDQ_003220

answers: 0

answers: NDQ_003221

answers: 0

answers: NDQ_003222

answers: 0

answers: NDQ_003223

answers: 0

answers: NDQ_003224

answers: 0

answers: NDQ_003225

answers: 4

answers: NDQ_003226

answers: 0

answers: NDQ_003227

answers: 0

answers: NDQ_003228

answers: 0

answers: NDQ_003230

answers: 0

answers: NDQ_003231

answers: 0

answers: NDQ_003233

answers: 0

answers: NDQ_003236

answers: 0

answers: NDQ_003237

answers: 0

answers: NDQ_003239

answers: 0

answers: NDQ_003240

answers: 0

answers: NDQ_003241

answers: 0

answers: NDQ_003242

answers: 0

answers: NDQ_003244

answers: 0

answers: NDQ_003246

answers: 4

answers: NDQ_003247

answers: 0

answers: NDQ_003252

answers: 3

answers: NDQ_003253

answers: 0

answers: NDQ_003254

answers: 0

answers: NDQ_003255

answers: 0

answers: NDQ_003256

answers: 0

answers: NDQ_003257

answers: 0

answers: NDQ_003258

answers: 0

answers: NDQ_003219

answers: Fossilisation is a rare event

answers: NDQ_003220

answers: unanswerable

answers: NDQ_003221

answers: late Cretaceous

answers: NDQ_003222

answers: Fossilisation is a rare event

answers: NDQ_003223

answers: Fossilisation

answers: NDQ_003224

answers: Fossil record is very incomplete

answers: NDQ_003225

answers: the fossil record is very incomplete

answers: NDQ_003226

answers: Europe

answers: NDQ_003227

answers: fossil record is very incomplete, increasingly so further back in time

answers: NDQ_003228

answers: Fossil record

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: magnetic field

answers: NDQ_003233

answers: Fossilisation is a rare event

answers: NDQ_003236

answers: Fossilisation

answers: NDQ_003237

answers: Fossil record is very incomplete

answers: NDQ_003239

answers: Fossil records across continents was evidence for continental drift

answers: NDQ_003240

answers: North America

answers: NDQ_003241

answers: no

answers: NDQ_003242

answers: continental drift

answers: NDQ_003244

answers: Fossilisation is a rare event

answers: NDQ_003246

answers: Fossil record is very incomplete

answers: NDQ_003247

answers: Fossil record is very incomplete

answers: NDQ_003252

answers: Fossilisation

answers: NDQ_003253

answers: Fossil record is very incomplete

answers: NDQ_003254

answers: Fossil records are very incomplete

answers: NDQ_003255

answers: Fossil records are very incomplete

answers: NDQ_003256

answers: Fossilisation is a rare event

answers: NDQ_003257

answers: Fossilisation

answers: NDQ_003258

answers: Fossilisation is a rare event

text: Other proffered explanations are the possible appearance of a displaced iceberg; the fear of running aground while becalmed, and a sudden seaquake. Hydrographical evidence suggests that an iceberg drifting so far south was improbable, and had it done so other ships would have seen it. Begg gives more consideration to a theory that Mary Celeste, while becalmed, began drifting towards the Dollabarat reef off Santa Maria Island. The theory supposes that Briggs, fearing his ship would run aground, launched the yawl in the hope of reaching land. The wind could then have picked up and blown Mary Celeste away from the reef, while the rising seas swamped and sank the yawl. The weakness of this theory is that if the ship had been becalmed, all sails would have been set to catch any available breeze, yet the ship was found with many of its sails furled.

text: Other proffered explanations are the possible appearance of a displaced iceberg; the fear of running aground while becalmed, and a sudden

text: seaquake

text: . Hydrographical evidence suggests that an iceberg drifting so far south was improbable, and had it done so other ships would have seen it. Begg gives more consideration to a theory that Mary Celeste, while becalmed, began drifting towards the

text: Dollabarat reef

text: off Santa Maria Island. The theory supposes that Briggs, fearing his ship would run aground, launched the yawl in the hope of reaching land. The wind could then have picked up and blown Mary Celeste away from the reef, while the rising seas swamped and sank the yawl. The weakness of this theory is that if the ship had been becalmed, all sails would have been set to catch any available breeze, yet the ship was found with many of its sails furled.

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answers: NDQ_003219

answers: 4

answers: NDQ_003220

answers: 0

answers: NDQ_003221

answers: 0

answers: NDQ_003222

answers: 2

answers: NDQ_003223

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answers: NDQ_003219

answers: iceberg drifting so far south was improbable

answers: NDQ_003220

answers: Santa Maria Island

answers: NDQ_003221

answers: early 20th century

answers: NDQ_003222

answers: the ship was found with many of its sails furled

answers: NDQ_003223

answers: Dollabarat reef

answers: NDQ_003224

answers: Mary Celeste

answers: NDQ_003225

answers: the possibility appearance of a displaced iceberg

answers: NDQ_003226

answers: Antarctica

answers: NDQ_003227

answers: an iceberg drifting so far south

answers: NDQ_003228

answers: Begg

answers: NDQ_003230

answers: South America

answers: NDQ_003231

answers: Becalmed

answers: NDQ_003233

answers: an iceberg drifting so far south

answers: NDQ_003236

answers: drifting so far south was improbable

answers: NDQ_003237

answers: an iceberg drifting so far south

answers: NDQ_003239

answers: an iceberg drifting so far south was improbable

answers: NDQ_003240

answers: a former supercontinent

answers: NDQ_003241

answers: The magnetic north pole and geographic north pole

answers: NDQ_003242

answers: Hydrographical

answers: NDQ_003244

answers: Dollabarat

answers: NDQ_003246

answers: continents

answers: NDQ_003247

answers: Dollabarat reef

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: Wegener believed that all the continents were once joined together

answers: NDQ_003254

answers: It was widely accepted as soon as it was introduced

answers: NDQ_003255

answers: Wegener and his supporters provided a lot of evidence for continental drift

answers: NDQ_003256

answers: Dollabarat reef

answers: NDQ_003257

answers: a sudden seaquake

answers: NDQ_003258

answers: displaced iceberg

text: The area experiences a cold, continental climate with extreme temperature differences. According to the Köppen climate classification system, Allakaket has a continental subarctic climate (Dfc). The average high temperature during July is . The average low temperature during January is well below zero and extended periods of  are common. The highest temperature ever recorded was  and the lowest was . Average precipitation is  and annual snowfall is . The Koyukuk River is ice-free from June through October.

text: The area experiences a cold, continental climate with extreme temperature differences. According to the

text: Köppen climate classification

text: system, Allakaket has a continental

text: subarctic climate

text: (Dfc). The average high temperature during July is . The average low temperature during January is well below zero and extended periods of  are common. The highest temperature ever recorded was  and the lowest was . Average

text: precipitation

text: is  and annual snowfall is . The Koyukuk River is ice-free from June through October.

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answers: NDQ_003219

answers: continental subarctic climate

answers: NDQ_003220

answers: Allakaket

answers: NDQ_003221

answers: 18th century

answers: NDQ_003222

answers: climate classification system

answers: NDQ_003223

answers: Allakaket

answers: NDQ_003224

answers: The Koyukuk River

answers: NDQ_003225

answers: climate classification system

answers: NDQ_003226

answers: subarctic

answers: NDQ_003227

answers: climate classification system

answers: NDQ_003228

answers: Köppen climate classification system

answers: NDQ_003230

answers: Allakaket

answers: NDQ_003231

answers: subarctic

answers: NDQ_003233

answers: The Koyukuk River is ice-free from June through October

answers: NDQ_003236

answers: continental climate with extreme temperature differences

answers: NDQ_003237

answers: The highest temperature ever recorded was and the lowest was

answers: NDQ_003239

answers: The highest temperature ever recorded was and the lowest was

answers: NDQ_003240

answers: Allakaket

answers: NDQ_003241

answers: No

answers: NDQ_003242

answers: continental subarctic climate

answers: NDQ_003244

answers: continental subarctic climate

answers: NDQ_003246

answers: The highest temperature ever recorded was and the lowest was

answers: NDQ_003247

answers: Allakaket has a continental subarctic climate

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: Allakaket has a continental subarctic climate

answers: NDQ_003254

answers: It was widely accepted as soon as it was introduced

answers: NDQ_003255

answers: The highest temperature ever recorded was and the lowest was

answers: NDQ_003256

answers: According to the Köppen climate classification system

answers: NDQ_003257

answers: According to the Köppen climate classification system

answers: NDQ_003258

answers: The Koyukuk River is ice-free from June through October

text: One of the most important radiations for land plants occurred in the early Devonian (Pragian), when the first certain rhyniophytes appear in the fossil record, making this rich fossil discovery of major importance to paleobotany. It has been suggested that the poorly preserved Eohostimella, found in deposits of Early Silurian age (Llandovery, around ), may be a rhyniophyte.

text: One of the most important radiations for land plants occurred in the early

text: Devonian

text: (Pragian), when the first certain rhyniophytes appear in the fossil record, making this rich fossil discovery of major importance to

text: paleobotany

text: . It has been suggested that the poorly preserved

text: Eohostimella

text: , found in deposits of

text: Early Silurian

text: age (Llandovery, around ), may be a rhyniophyte.

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answers: Devonian

answers: NDQ_003220

answers: Pragian

answers: NDQ_003221

answers: Devonian

answers: NDQ_003222

answers: poorly preserved Eohostimella

answers: NDQ_003223

answers: Silurian

answers: NDQ_003224

answers: Devonian

answers: NDQ_003225

answers: rhyniophytes

answers: NDQ_003226

answers: Europe

answers: NDQ_003227

answers: Early Silurian age

answers: NDQ_003228

answers: paleobotany

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: magnetic field

answers: NDQ_003233

answers: The poorly preserved Eohostimella

answers: NDQ_003236

answers: Land plants

answers: NDQ_003237

answers: Eohostimella

answers: NDQ_003239

answers: One of the most important radiations

answers: NDQ_003240

answers: Silurian

answers: NDQ_003241

answers: Pragian

answers: NDQ_003242

answers: Silurian

answers: NDQ_003244

answers: Eohostimella

answers: NDQ_003246

answers: The continents have never all been together

answers: NDQ_003247

answers: Late Silurian age

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: Pragian

answers: NDQ_003254

answers: Early Silurian age

answers: NDQ_003255

answers: One of the most important radiations for land plants occurred in the early Devonian

answers: NDQ_003256

answers: Early Silurian age

answers: NDQ_003257

answers: Pangaea

answers: NDQ_003258

answers: Late Silurian

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.

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answers: NDQ_003230

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answers: NDQ_003256

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answers: 0

answers: NDQ_003258

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answers: NDQ_003219

answers: plate tectonics

answers: NDQ_003220

answers: are

answers: NDQ_003221

answers: geologic

answers: NDQ_003222

answers: stereonets

answers: NDQ_003223

answers: fold axes

answers: NDQ_003224

answers: stereonets

answers: NDQ_003225

answers: Stereonets

answers: NDQ_003226

answers: Europe

answers: NDQ_003227

answers: fold axes

answers: NDQ_003228

answers: The analysis of structures

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: sphere

answers: NDQ_003233

answers: fold axes

answers: NDQ_003236

answers: fold axes

answers: NDQ_003237

answers: fold axes

answers: NDQ_003239

answers: relationships between faults

answers: NDQ_003240

answers: a sphere

answers: NDQ_003241

answers: no

answers: NDQ_003242

answers: fold

answers: NDQ_003244

answers: Stereonets

answers: NDQ_003246

answers: Stereonets

answers: NDQ_003247

answers: fold axes

answers: NDQ_003252

answers: plate tectonics

answers: NDQ_003253

answers: Stereonets

answers: NDQ_003254

answers: Stereonets

answers: NDQ_003255

answers: Stereonets

answers: NDQ_003256

answers: Stereonets

answers: NDQ_003257

answers: Pangaea

answers: NDQ_003258

answers: fold axes

text: Canada's tundra runs more or less over all physiographic divisions except the Appalachian Orogen. As these formations are of deep tectonic nature they do not necessarily constitute the structure and material found on the surface, are observable elevated mountain ranges or orogenic belts. Large areas of the Canadian Shield - the ancient geological core of the North American continental plate are buried under sedimentary rocks of the Interior Platform. Repeated glaciations have had a profound impact on shaping land forms and determining drainage patterns.

text: Canada's tundra runs more or less over all physiographic divisions except the

text: Appalachian Orogen

text: . As these formations are of deep

text: tectonic

text: nature they do not necessarily constitute the structure and material found on the surface, are observable elevated mountain ranges or orogenic belts. Large areas of the

text: Canadian Shield

text: - the ancient geological core of the North American continental plate are buried under sedimentary rocks of the

text: Interior Platform

text: . Repeated glaciations have had a profound impact on shaping land forms and determining drainage patterns.

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answers: NDQ_003219

answers: North American continental plate

answers: NDQ_003220

answers: Canadian Shield

answers: NDQ_003221

answers: North American continental plate

answers: NDQ_003222

answers: the Appalachian Orogen

answers: NDQ_003223

answers: the Appalachian Orogen

answers: NDQ_003224

answers: geological core of the North American continental plate

answers: NDQ_003225

answers: deep tectonic nature

answers: NDQ_003226

answers: Canada

answers: NDQ_003227

answers: deep tectonic nature they do not necessarily constitute the structure and material found on the surface

answers: NDQ_003228

answers: geologist

answers: NDQ_003230

answers: North American

answers: NDQ_003231

answers: core

answers: NDQ_003233

answers: Large areas of the Canadian Shield

answers: NDQ_003236

answers: tectonic

answers: NDQ_003237

answers: elevated mountain ranges or orogenic belts

answers: NDQ_003239

answers: North American continental plate are buried under sedimentary rocks of the Interior Platform

answers: NDQ_003240

answers: North American continent

answers: NDQ_003241

answers: North American continental plate

answers: NDQ_003242

answers: tectonic

answers: NDQ_003244

answers: Canadian Shield

answers: NDQ_003246

answers: North American continental plate

answers: NDQ_003247

answers: Canadian Shield - the ancient geological core of the North American continental plate

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: geological core of the North American continental plate

answers: NDQ_003254

answers: North American continental plate are buried under sedimentary rocks of the Interior Platform

answers: NDQ_003255

answers: Large areas of the Canadian Shield are buried under sedimentary rocks of the Interior Platform

answers: NDQ_003256

answers: North American continental plate

answers: NDQ_003257

answers: The Appalachian Orogen

answers: NDQ_003258

answers: North American continental plate

text: Permo-Carboniferous time, about 300 million years ago, was a period of significant glaciation.  The widespread distribution of Permo-Carboniferous glacial sediments in South America, Africa, Madagascar, Arabia, India, Antarctica and Australia was one of the major pieces of evidence for the theory of continental drift, and led ultimately to the concept of a super-continent, Pangaea. Glacial activity spanned virtually the whole of Carboniferous and Early Permian time. Toward the end of the Carboniferous, around 290 million years ago, Gondwana, the southern part of Pangaea, was located near the south pole. Glacial centres expanded across the continents, producing glacial tillites and striations in pre-existing rocks. A complex centre of glaciation migrated across South America, Antarctica and South Africa between about 350 and 240 Ma. Chronological difficulties complicate the task of charting the evolution of the ice sheet over this interval. The Permo-Carboniferous ice sheet was so extensive that it would occupy a circle spanning 50 degrees of latitude centered on the pole.

text: Permo-Carboniferous time, about 300 million years ago, was a period of significant

text: glaciation

text: .  The widespread distribution of Permo-Carboniferous glacial sediments in South America, Africa, Madagascar, Arabia, India, Antarctica and Australia was one of the major pieces of evidence for the theory of

text: continental drift

text: , and led ultimately to the concept of a super-continent,

text: Pangaea

text: . Glacial activity spanned virtually the whole of Carboniferous and Early Permian time. Toward the end of the Carboniferous, around 290 million years ago,

text: Gondwana

text: , the southern part of Pangaea, was located near the south pole. Glacial centres expanded across the continents, producing glacial

text: tillite

text: s and striations in pre-existing rocks. A complex centre of glaciation migrated across South America, Antarctica and South Africa between about 350 and 240 Ma. Chronological difficulties complicate the task of charting the evolution of the ice sheet over this interval. The Permo-Carboniferous ice sheet was so extensive that it would occupy a circle spanning 50 degrees of latitude centered on the pole.

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answers: 0

answers: NDQ_003219

answers: 4

answers: NDQ_003220

answers: 0

answers: NDQ_003221

answers: 4

answers: NDQ_003222

answers: 0

answers: NDQ_003223

answers: 0

answers: NDQ_003224

answers: 4

answers: NDQ_003225

answers: 4

answers: NDQ_003226

answers: 0

answers: NDQ_003227

answers: 0

answers: NDQ_003228

answers: 0

answers: NDQ_003230

answers: 4

answers: NDQ_003231

answers: 0

answers: NDQ_003233

answers: 0

answers: NDQ_003236

answers: 4

answers: NDQ_003237

answers: 4

answers: NDQ_003239

answers: 4

answers: NDQ_003240

answers: 4

answers: NDQ_003241

answers: 0

answers: NDQ_003242

answers: 4

answers: NDQ_003244

answers: 0

answers: NDQ_003246

answers: 4

answers: NDQ_003247

answers: 4

answers: NDQ_003252

answers: 4

answers: NDQ_003253

answers: 4

answers: NDQ_003254

answers: 0

answers: NDQ_003255

answers: 4

answers: NDQ_003256

answers: 0

answers: NDQ_003257

answers: 0

answers: NDQ_003258

answers: 4

answers: NDQ_003219

answers: continental drift

answers: NDQ_003220

answers: Antarctica

answers: NDQ_003221

answers: Permian

answers: NDQ_003222

answers: Chronological difficulties

answers: NDQ_003223

answers: Gondwana

answers: NDQ_003224

answers: glacial sediments

answers: NDQ_003225

answers: continental drift

answers: NDQ_003226

answers: South America

answers: NDQ_003227

answers: a super-continent

answers: NDQ_003228

answers: one of the major pieces of evidence for the theory of continental drift

answers: NDQ_003230

answers: Africa

answers: NDQ_003231

answers: circle

answers: NDQ_003233

answers: The widespread distribution of Permo-Carboniferous glacial sediments

answers: NDQ_003236

answers: continental drift

answers: NDQ_003237

answers: Permo-Carboniferous glacial sediments

answers: NDQ_003239

answers: The widespread distribution of Permo-Carboniferous glacial sediments

answers: NDQ_003240

answers: Pangaea

answers: NDQ_003241

answers: no

answers: NDQ_003242

answers: theory of continental drift

answers: NDQ_003244

answers: Gondwana

answers: NDQ_003246

answers: Pangaea

answers: NDQ_003247

answers: Permo-Carboniferous glacial sediments

answers: NDQ_003252

answers: Permo-Carboniferous

answers: NDQ_003253

answers: Pangaea

answers: NDQ_003254

answers: It was widely accepted as soon as it was introduced

answers: NDQ_003255

answers: widespread distribution of Permo-Carboniferous glacial sediments

answers: NDQ_003256

answers: Permo-Carboniferous

answers: NDQ_003257

answers: Gondwana

answers: NDQ_003258

answers: Permo-Carboniferous

text: The climate is moderately continental, with a Köppen climate classification of Dfb (humid continental climate). The average annual temperature is .

text: The climate is moderately continental, with a

text: Köppen climate classification

text: of Dfb (

text: humid continental climate

text: ). The average annual temperature is .

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answers: The climate is moderately continental

answers: NDQ_003239

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answers: NDQ_003240

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answers: The average annual temperature is

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answers: NDQ_003244

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text: From the Köppen climate classification, Bar has a soft humid continental climate (see the Climate chart). Bar's district is historically known as an apple tree growing region , with the presence of both a soft humid continental climate and appropriate soil.

text: From the

text: Köppen climate classification

text: , Bar has a soft

text: humid continental climate

text: (see the Climate chart). Bar's district is historically known as an apple tree growing region , with the presence of both a soft

text: humid continental climate

text: and appropriate soil.

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answers: The presence of both a soft humid continental climate and appropriate soil

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answers: NDQ_003237

answers: Bar has a soft humid continental climate

answers: NDQ_003239

answers: continental drift

answers: NDQ_003240

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answers: NDQ_003241

answers: The magnetic north pole and geographic north pole are in different locations.

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answers: The Köppen climate classification

answers: NDQ_003255

answers: From the Köppen climate classification

answers: NDQ_003256

answers: Bar has a soft humid continental climate

answers: NDQ_003257

answers: Pangaea

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answers: continental climate

text: Although most fringe science is rejected, the scientific community has come to accept some portions of it. One example of such is plate tectonics, an idea which had its origin in the fringe science of continental drift and was rejected for decades.

text: Although most fringe science is rejected, the scientific community has come to accept some portions of it. One example of such is

text: plate tectonics

text: , an idea which had its origin in the fringe science of

text: continental drift

text: and was rejected for decades.

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answers: continental drift

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.

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answers: continents shifted Earth’s surface

answers: NDQ_003220

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answers: NDQ_003221

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answers: NDQ_003222

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answers: NDQ_003223

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answers: NDQ_003224

answers: plant and animal fossils

answers: NDQ_003225

answers: theory of Continental Drift

answers: NDQ_003226

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answers: NDQ_003227

answers: explained how the continents shifted Earth’s surface

answers: NDQ_003228

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answers: NDQ_003230

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answers: NDQ_003231

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answers: We live in a post Pangaea time period

answers: NDQ_003236

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answers: NDQ_003237

answers: plant fossils from the frigid Arctic of Svalbard

answers: NDQ_003239

answers: Plant and animal fossils

answers: NDQ_003240

answers: Pangaea

answers: NDQ_003241

answers: The magnetic north pole and geographic north pole

answers: NDQ_003242

answers: Continental Drift

answers: NDQ_003244

answers: The theory of Continental Drift

answers: NDQ_003246

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answers: NDQ_003247

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answers: NDQ_003252

answers: Pangaea

answers: NDQ_003253

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answers: NDQ_003254

answers: It was widely accepted

answers: NDQ_003255

answers: The theory of Continental Drift, created by Alfred Wegener

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answers: NDQ_003258

answers: Continental Drift

text: In other regions the glaciations of the last glacial period are given other names: for example that in the Alpine region is called the Würm glaciation, in the British Isles it is the Devensian glaciation and in North America, the Wisconsin glaciation.

text: In other regions the glaciations of the last glacial period are given other names: for example that in the

text: Alpine region

text: is called the

text: Würm glaciation

text: , in the

text: British Isles

text: it is the

text: Devensian glaciation

text: and in North America, the

text: Wisconsin glaciation

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answers: glaciations of the last glacial period

answers: NDQ_003220

answers: British Isles

answers: NDQ_003221

answers: glacial period

answers: NDQ_003222

answers: continental drift

answers: NDQ_003223

answers: glaciation

answers: NDQ_003224

answers: glaciations

answers: NDQ_003225

answers: Devensian glaciation

answers: NDQ_003226

answers: British Isles

answers: NDQ_003227

answers: last glacial period

answers: NDQ_003228

answers: glaciations of the last glacial period

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: Alpine region

answers: NDQ_003233

answers: Würm glaciation

answers: NDQ_003236

answers: glaciation

answers: NDQ_003237

answers: the Wisconsin glaciation

answers: NDQ_003239

answers: continental drift

answers: NDQ_003240

answers: Devensian

answers: NDQ_003241

answers: North America

answers: NDQ_003242

answers: glacial period

answers: NDQ_003244

answers: Wisconsin glaciation

answers: NDQ_003246

answers: In other regions

answers: NDQ_003247

answers: the Wisconsin glaciation

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: North America, the Wisconsin glaciation

answers: NDQ_003254

answers: The glaciations of the last glacial period

answers: NDQ_003255

answers: The glaciations of the last glacial period

answers: NDQ_003256

answers: Devensian glaciation

answers: NDQ_003257

answers: Pangaea

answers: NDQ_003258

answers: The glaciations of the last glacial period

text: Most of Croatia has a moderately warm and rainy continental climate as defined by the Köppen climate classification. Mean monthly temperature ranges between  (in January) and  (in July). The coldest parts of the country are Lika and Gorski Kotar where snowy forested climate is found at elevations above . The warmest areas of Croatia are at the Adriatic coast and especially in its immediate hinterland characterised by the Mediterranean climate, as the temperature highs are moderated by the sea. Consequently, temperature peaks are more pronounced in the continental areas—the lowest temperature of  was recorded on 3 February 1919 in Čakovec, and the highest temperature of  was recorded on 5 July 1950 in Karlovac.

text: Most of Croatia has a moderately warm and rainy

text: continental climate

text: as defined by the

text: Köppen climate classification

text: . Mean monthly temperature ranges between  (in January) and  (in July). The coldest parts of the country are

text: Lika

text: and

text: Gorski Kotar

text: where snowy forested climate is found at elevations above . The warmest areas of Croatia are at the Adriatic coast and especially in its immediate hinterland characterised by the

text: Mediterranean climate

text: , as the temperature highs are moderated by the sea. Consequently, temperature peaks are more pronounced in the continental areas—the lowest temperature of  was recorded on 3 February 1919 in

text: Čakovec

text: , and the highest temperature of  was recorded on 5 July 1950 in

text: Karlovac

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answers: NDQ_003221

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answers: NDQ_003222

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answers: NDQ_003223

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answers: NDQ_003240

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answers: NDQ_003241

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answers: NDQ_003242

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answers: NDQ_003252

answers: 4

answers: NDQ_003253

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answers: NDQ_003256

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answers: NDQ_003257

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answers: NDQ_003258

answers: 0

answers: NDQ_003219

answers: continental climate

answers: NDQ_003220

answers: Adriatic

answers: NDQ_003221

answers: 1950

answers: NDQ_003222

answers: Köppen climate classification

answers: NDQ_003223

answers: the Mediterranean climate

answers: NDQ_003224

answers: Consequently, temperature peaks are more pronounced in the continental areas

answers: NDQ_003225

answers: the Mediterranean climate

answers: NDQ_003226

answers: Croatia

answers: NDQ_003227

answers: temperature peaks are more pronounced in the continental areas

answers: NDQ_003228

answers: climate classification

answers: NDQ_003230

answers: South America

answers: NDQ_003231

answers: hinterland

answers: NDQ_003233

answers: temperature peaks are more pronounced in the continental areas

answers: NDQ_003236

answers: continental climate

answers: NDQ_003237

answers: temperature peaks are more pronounced in the continental areas

answers: NDQ_003239

answers: Consequently, temperature peaks are more pronounced

answers: NDQ_003240

answers: continental

answers: NDQ_003241

answers: The warmest areas of Croatia

answers: NDQ_003242

answers: continental climate

answers: NDQ_003244

answers: continental climate as defined by the Köppen climate classification

answers: NDQ_003246

answers: continental

answers: NDQ_003247

answers: Consequently, temperature peaks are more pronounced in the continental areas

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: continental climate

answers: NDQ_003254

answers: Köppen climate classification

answers: NDQ_003255

answers: Consequently, temperature peaks are more pronounced in the continental areas

answers: NDQ_003256

answers: The warmest areas of Croatia

answers: NDQ_003257

answers: Pangaea broke up a short time ago

answers: NDQ_003258

answers: continental climate

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.

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answers: NDQ_003219

answers: continents of the Earth's crust

answers: NDQ_003220

answers: are extensive

answers: NDQ_003221

answers: 18th century

answers: NDQ_003222

answers: only 8% of the total volume of the crust

answers: NDQ_003223

answers: igneous

answers: NDQ_003224

answers: sedimentary rocks

answers: NDQ_003225

answers: sedimentary rocks are only a thin veneer over a crust consisting mainly of igneous and metamorphic rocks

answers: NDQ_003226

answers: Europe

answers: NDQ_003227

answers: The sedimentary rock cover of the continents of the Earth's crust is extensive

answers: NDQ_003228

answers: The study of sedimentary rocks

answers: NDQ_003230

answers: Earth

answers: NDQ_003231

answers: subsurface

answers: NDQ_003233

answers: 73% of the Earth's current land surface

answers: NDQ_003236

answers: continents of the Earth's crust

answers: NDQ_003237

answers: 73% of the Earth's current land surface

answers: NDQ_003239

answers: The sedimentary rock cover of the continents of the Earth's crust is extensive

answers: NDQ_003240

answers: Earth

answers: NDQ_003241

answers: Earth's crust

answers: NDQ_003242

answers: bedding

answers: NDQ_003244

answers: continents of the Earth's crust

answers: NDQ_003246

answers: continents of the Earth's crust

answers: NDQ_003247

answers: The study of sedimentary rocks and rock strata provides information about the subsurface

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: The sedimentary rock cover of the continents

answers: NDQ_003254

answers: It was widely accepted as soon as it was introduced

answers: NDQ_003255

answers: 73% of the Earth's current land surface

answers: NDQ_003256

answers: Sedimentary rocks are deposited in layers as strata

answers: NDQ_003257

answers: Pangaea broke up

answers: NDQ_003258

answers: Sedimentary rocks are deposited in layers as strata

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

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answers: 0

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answers: 0

answers: tqa2:L_0076/T_0763/3e749bce73370e3289eb5602e4cc94c3

answers: 0

answers: tqa2:L_0076/T_0763/17772420e6087d05eb83b3f0cc3aa451

answers: 0

answers: tqa2:L_0076/T_0763/7a7192cbfb0cdb83fb089d3c4f8ea239

answers: 4

answers: NDQ_003219

answers: 4

answers: NDQ_003220

answers: 0

answers: NDQ_003221

answers: 0

answers: NDQ_003222

answers: 2

answers: NDQ_003223

answers: 4

answers: NDQ_003224

answers: 4

answers: NDQ_003225

answers: 4

answers: NDQ_003226

answers: 0

answers: NDQ_003227

answers: 0

answers: NDQ_003228

answers: 0

answers: NDQ_003230

answers: 0

answers: NDQ_003231

answers: 0

answers: NDQ_003233

answers: 4

answers: NDQ_003236

answers: 5

answers: NDQ_003237

answers: 4

answers: NDQ_003239

answers: 4

answers: NDQ_003240

answers: 0

answers: NDQ_003241

answers: 4

answers: NDQ_003242

answers: 4

answers: NDQ_003244

answers: 0

answers: NDQ_003246

answers: 4

answers: NDQ_003247

answers: 4

answers: NDQ_003252

answers: 4

answers: NDQ_003253

answers: 4

answers: NDQ_003254

answers: 4

answers: NDQ_003255

answers: 4

answers: NDQ_003256

answers: 0

answers: NDQ_003257

answers: 0

answers: NDQ_003258

answers: 4

answers: NDQ_003219

answers: the same forces at work today have been at work in the early Proterozoic

answers: NDQ_003220

answers: island arcs

answers: NDQ_003221

answers: Proterozoic

answers: NDQ_003222

answers: supercontinent cycle

answers: NDQ_003223

answers: plate tectonics

answers: NDQ_003224

answers: Proterozoic and probably earlier

answers: NDQ_003225

answers: supercontinent cycle

answers: NDQ_003226

answers: Wopmay Orogen

answers: NDQ_003227

answers: supercontinent cycle

answers: NDQ_003228

answers: Wopmay Orogen

answers: NDQ_003230

answers: continents

answers: NDQ_003231

answers: magnetic poles

answers: NDQ_003233

answers: Alignments of magnetic particles in rocks

answers: NDQ_003236

answers: Alignments of magnetic particles in rocks demonstrate that continents were drifting

answers: NDQ_003237

answers: the Wopmay Orogen

answers: NDQ_003239

answers: the same forces at work today have been at work in the early Proterozoic and probably earlier

answers: NDQ_003240

answers: Proterozoic

answers: NDQ_003241

answers: Earth

answers: NDQ_003242

answers: plate tectonics

answers: NDQ_003244

answers: continents were drifting

answers: NDQ_003246

answers: supercontinent

answers: NDQ_003247

answers: the same forces at work today

answers: NDQ_003252

answers: plate tectonics

answers: NDQ_003253

answers: supercontinent

answers: NDQ_003254

answers: Alignments of magnetic particles in rocks

answers: NDQ_003255

answers: Wopmay Orogen

answers: NDQ_003256

answers: Wopmay Orogen

answers: NDQ_003257

answers: rifting and subducting, all at least 1.5 billion years ago

answers: NDQ_003258

answers: plate tectonics

text: Earlier theories (e.g. by Alfred Wegener and Alexander du Toit) of continental drift were that continents "ploughed" through the sea. The idea that the seafloor itself moves (and also carries the continents with it) as it expands from a central axis was proposed by Harry Hess from Princeton University in the 1960s. The theory is well accepted now, and the phenomenon is known to be caused by convection currents in the asthenosphere, which is ductile, or  plastic, and the brittle lithosphere.

text: Earlier theories (e.g. by

text: Alfred Wegener

text: and

text: Alexander du Toit

text: ) of continental drift were that

text: continent

text: s "ploughed" through the sea. The idea that the seafloor itself moves (and also carries the continents with it) as it expands from a central axis was proposed by

text: Harry Hess

text: from

text: Princeton University

text: in the 1960s. The theory is well accepted now, and the phenomenon is known to be caused by

text: convection

text: currents in the

text: asthenosphere

text: , which is ductile, or

text: plastic

text: , and the brittle

text: lithosphere

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answers: 0

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answers: 0

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answers: 0

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answers: 0

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answers: 0

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answers: 0

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answers: 0

answers: tqa2:L_0076/T_0763/7a7192cbfb0cdb83fb089d3c4f8ea239

answers: 0

answers: NDQ_003219

answers: 4

answers: NDQ_003220

answers: 0

answers: NDQ_003221

answers: 3

answers: NDQ_003222

answers: 2

answers: NDQ_003223

answers: 0

answers: NDQ_003224

answers: 0

answers: NDQ_003225

answers: 0

answers: NDQ_003226

answers: 0

answers: NDQ_003227

answers: 0

answers: NDQ_003228

answers: 0

answers: NDQ_003230

answers: 0

answers: NDQ_003231

answers: 0

answers: NDQ_003233

answers: 4

answers: NDQ_003236

answers: 4

answers: NDQ_003237

answers: 0

answers: NDQ_003239

answers: 3

answers: NDQ_003240

answers: 0

answers: NDQ_003241

answers: 0

answers: NDQ_003242

answers: 4

answers: NDQ_003244

answers: 0

answers: NDQ_003246

answers: 4

answers: NDQ_003247

answers: 4

answers: NDQ_003252

answers: 4

answers: NDQ_003253

answers: 4

answers: NDQ_003254

answers: 2

answers: NDQ_003255

answers: 4

answers: NDQ_003256

answers: 0

answers: NDQ_003257

answers: 0

answers: NDQ_003258

answers: 3

answers: NDQ_003219

answers: the seafloor itself moves

answers: NDQ_003220

answers: Atlantic Ocean

answers: NDQ_003221

answers: 1960s

answers: NDQ_003222

answers: that continents "ploughed" through the sea

answers: NDQ_003223

answers: convection currents

answers: NDQ_003224

answers: Earlier theories

answers: NDQ_003225

answers: continental drift

answers: NDQ_003226

answers: Europe

answers: NDQ_003227

answers: continents "ploughed" through the sea

answers: NDQ_003228

answers: theories

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: asthenosphere

answers: NDQ_003233

answers: The idea that the seafloor itself moves

answers: NDQ_003236

answers: continental drift

answers: NDQ_003237

answers: continental drift were that continents "ploughed" through the sea

answers: NDQ_003239

answers: continental drift were that continents "ploughed" through the sea

answers: NDQ_003240

answers: Central axis

answers: NDQ_003241

answers: central axis

answers: NDQ_003242

answers: convection currents

answers: NDQ_003244

answers: continental drift

answers: NDQ_003246

answers: continental drift

answers: NDQ_003247

answers: continents "ploughed" through the sea

answers: NDQ_003252

answers: Alfred Wegener and Alexander du Toit

answers: NDQ_003253

answers: Earlier theories

answers: NDQ_003254

answers: The theory is well accepted now

answers: NDQ_003255

answers: Alfred Wegener and Alexander du Toit

answers: NDQ_003256

answers: Wegener and Alexander du Toit

answers: NDQ_003257

answers: Earlier theories

answers: NDQ_003258

answers: Earlier theories

text: The Pit Pony Stables were built in 2013/14, and house the museum's pit ponies. They replace a wooden stable a few metres away in the field opposite the school (the wooden structure remaining). It represents the sort of stables that  were used in drift mines (ponies in deep mines living their whole lives underground), pit ponies having been in use in the north east as late as 1994, in Ellington Colliery. The structure is a recreation of an original building that stood at Rickless Drift Mine, between High Spen and Greenside; it was built using a yellow brick that was common across the Durham coalfield.

text: The Pit Pony Stables were built in 2013/14, and house the museum's

text: pit ponies

text: . They replace a wooden stable a few metres away in the field opposite the school (the wooden structure remaining). It represents the sort of stables that  were used in drift mines (ponies in deep mines living their whole lives underground), pit ponies having been in use in the north east as late as 1994, in

text: Ellington Colliery

text: . The structure is a recreation of an original building that stood at Rickless Drift Mine, between

text: High Spen

text: and

text: Greenside

text: ; it was built using a yellow brick that was common across the Durham coalfield.

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text: The docks received a total renovation in 1992 for NOK 18 million, allowing cruise ships to dock in port. The following year a 60-person café was completed. The Norwegian Mapping Authority completed its continental drift station in 1994, at the same time as a satellite communication link opened on Zeppelinfjellet. By 1996 there were over one hundred research projects in Ny-Ålesund, and the town reaches a capacity for 200 people two years later. On 6 May 1998, Kings Bay Kull. Comp A/S changes its name to Kings Bay AS. The same summer the North Pole Hotel was finished refurbished and opened as the world's northern-most hotel. That year also saw the annual number of researcher-days exceed 15,000. In March 1999 the Norwegian Polar Institute opened its new  Sverdrup Station. The original building on Zeppelinfjellet was demolished and replaced with a new facility.

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text: The patterns of species distribution across geographical areas can usually be explained through a combination of historical factors such as: speciation, extinction, continental drift, and glaciation. Through observing the geographic distribution of species, we can see associated variations in sea level, river routes, habitat, and river capture. Additionally, this science considers the geographic constraints of landmass areas and isolation, as well as the available ecosystem energy supplies.

text: The patterns of species distribution across geographical areas can usually be explained through a combination of historical factors such as:

text: speciation

text: extinction

text: continental drift

text: , and

text: glaciation

text: . Through observing the geographic distribution of species, we can see associated variations in

text: sea level

text: , river routes, habitat, and

text: river capture

text: . Additionally, this science considers the geographic constraints of

text: landmass

text: areas and isolation, as well as the available ecosystem energy supplies.

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answers: NDQ_003220

answers: are isolated

answers: NDQ_003221

answers: 18th century

answers: NDQ_003222

answers: extinction

answers: NDQ_003223

answers: continental drift

answers: NDQ_003224

answers: geographical areas

answers: NDQ_003225

answers: geographic distribution of species

answers: NDQ_003226

answers: Europe

answers: NDQ_003227

answers: can usually be explained through a combination of historical factors

answers: NDQ_003228

answers: continental drift

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: magnetic field

answers: NDQ_003233

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answers: NDQ_003236

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answers: NDQ_003237

answers: patterns of species distribution across geographical areas

answers: NDQ_003239

answers: patterns of species distribution

answers: NDQ_003240

answers: North America

answers: NDQ_003241

answers: no

answers: NDQ_003242

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answers: NDQ_003244

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answers: NDQ_003246

answers: continent drift

answers: NDQ_003247

answers: patterns of species distribution

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: isolation

answers: NDQ_003254

answers: The patterns of species distribution across geographical areas

answers: NDQ_003255

answers: patterns of species distribution across geographical areas

answers: NDQ_003256

answers: continental drift

answers: NDQ_003257

answers: Pangaea

answers: NDQ_003258

answers: continental drift

text: No completely satisfactory theory has been proposed to account for Earth's history of glaciation. The cause of glaciation may be related to several simultaneous factors, such as astronomical cycles, atmospheric composition, plate tectonics, and ocean currents.

text: No completely satisfactory theory has been proposed to account for Earth's history of glaciation. The cause of glaciation may be related to several simultaneous factors, such as

text: astronomical cycles

text: , atmospheric composition,

text: plate tectonics

text: , and

text: ocean current

text: s.

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answers: glaciation may be related to several simultaneous factors

answers: NDQ_003220

answers: Atlantic Ocean

answers: NDQ_003221

answers: astronomical cycles

answers: NDQ_003222

answers: No completely satisfactory theory has been proposed

answers: NDQ_003223

answers: plate tectonics

answers: NDQ_003224

answers: glaciation

answers: NDQ_003225

answers: No completely satisfactory theory

answers: NDQ_003226

answers: Antarctica

answers: NDQ_003227

answers: plate tectonics

answers: NDQ_003228

answers: No completely satisfactory theory has been proposed

answers: NDQ_003230

answers: Earth

answers: NDQ_003231

answers: magnetic field

answers: NDQ_003233

answers: plate tectonics

answers: NDQ_003236

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answers: NDQ_003237

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answers: NDQ_003239

answers: continental drift

answers: NDQ_003240

answers: Earth

answers: NDQ_003241

answers: Earth's

answers: NDQ_003242

answers: plate tectonics

answers: NDQ_003244

answers: continent has drifted

answers: NDQ_003246

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answers: NDQ_003247

answers: continental drift

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

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answers: plate tectonics

answers: NDQ_003255

answers: continental drift

answers: NDQ_003256

answers: ocean currents

answers: NDQ_003257

answers: plate tectonics

answers: NDQ_003258

answers: plate tectonics

text: In reality, the relative polar movement can either be polar wandering or continental drift (or a combination of both).  Data from around the globe are needed in order to isolate or distinguish between the two. Nevertheless, the magnetic poles rarely stray far from the geographic poles of the planet. Therefore, the concept of apparent polar wander is very useful in plate tectonics, since it can retrace the relative motion of continents, as well as the formation and break-up of supercontinents.

text: In reality, the relative polar movement can either be polar wandering or continental drift (or a combination of both).  Data from around the globe are needed in order to isolate or distinguish between the two. Nevertheless, the magnetic poles rarely stray far from the geographic poles of the planet. Therefore, the concept of apparent polar wander is very useful in plate tectonics, since it can retrace the relative motion of continents, as well as the formation and break-up of supercontinents.

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answers: NDQ_003219

answers: the magnetic poles rarely stray far from the geographic poles of the planet

answers: NDQ_003220

answers: geographic poles of the planet

answers: NDQ_003221

answers: plate tectonics

answers: NDQ_003222

answers: data from around the globe

answers: NDQ_003223

answers: the relative motion of continents

answers: NDQ_003224

answers: supercontinents

answers: NDQ_003225

answers: polar wandering

answers: NDQ_003226

answers: Antarctica

answers: NDQ_003227

answers: it can retrace the relative motion of continents

answers: NDQ_003228

answers: Data from around the globe are needed in order to isolate or distinguish between the two

answers: NDQ_003230

answers: continents

answers: NDQ_003231

answers: magnetic poles

answers: NDQ_003233

answers: the relative polar movement can either be polar wandering or continental drift

answers: NDQ_003236

answers: relative motion of continents

answers: NDQ_003237

answers: magnetic poles rarely stray far from the geographic poles

answers: NDQ_003239

answers: Data from around the globe are needed in order to isolate or distinguish between the two

answers: NDQ_003240

answers: break-up

answers: NDQ_003241

answers: the geographic poles of the planet

answers: NDQ_003242

answers: plate tectonics

answers: NDQ_003244

answers: continent drift

answers: NDQ_003246

answers: supercontinents

answers: NDQ_003247

answers: Data from around the globe are needed in order to isolate or distinguish between the two

answers: NDQ_003252

answers: plate tectonics

answers: NDQ_003253

answers: supercontinents

answers: NDQ_003254

answers: The concept of apparent polar wander

answers: NDQ_003255

answers: Data from around the globe

answers: NDQ_003256

answers: It can retrace the relative motion of continents

answers: NDQ_003257

answers: It can retrace the relative motion of continents

answers: NDQ_003258

answers: plate tectonics

text: Michael "Mike" Thurmeier is a Canadian animator and director at Blue Sky Studios. He is most famous for co-directing Ice Age: Dawn of the Dinosaurs and Ice Age: Continental Drift.

text: Michael "Mike" Thurmeier is a Canadian animator and director at

text: Blue Sky Studios

text: . He is most famous for co-directing

text: Ice Age: Dawn of the Dinosaurs

text: and

text: Ice Age: Continental Drift

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answers: Continental Drift

answers: NDQ_003220

answers: Canadian

answers: NDQ_003221

answers: Canadian

answers: NDQ_003222

answers: Dinosaurs

answers: NDQ_003223

answers: Canada

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answers: Dinosaurs

answers: NDQ_003225

answers: Mike

answers: NDQ_003226

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answers: Ice Age: Continental Drift

answers: NDQ_003228

answers: co-director

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answers: Ice Age

answers: NDQ_003233

answers: Ice Age: Continental Drift

answers: NDQ_003236

answers: Continental Drift

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answers: Ice Age: Continental Drift

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answers: Ice Age: Continental Drift

answers: NDQ_003240

answers: Ice Age

answers: NDQ_003241

answers: Canada

answers: NDQ_003242

answers: Continental Drift

answers: NDQ_003244

answers: Continental Drift

answers: NDQ_003246

answers: Continental Drift

answers: NDQ_003247

answers: Continental Drift

answers: NDQ_003252

answers: Continental Drift

answers: NDQ_003253

answers: Continental Drift

answers: NDQ_003254

answers: It was widely accepted

answers: NDQ_003255

answers: Ice Age: Continental Drift

answers: NDQ_003256

answers: Continental Drift

answers: NDQ_003257

answers: Pangaea

answers: NDQ_003258

answers: Continental Drift

text: In the important limit of stationary magnetic field and weak electric field, the inertial drift is dominated by the curvature drift term.

text: In the important limit of stationary magnetic field and weak electric field, the inertial drift is dominated by the curvature drift term.

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answers: 3

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answers: NDQ_003256

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answers: 0

answers: NDQ_003258

answers: 0

answers: NDQ_003219

answers: magnetic field and weak electric field

answers: NDQ_003220

answers: Atlantic Ocean

answers: NDQ_003221

answers: 18th century

answers: NDQ_003222

answers: curvature drift term

answers: NDQ_003223

answers: weak electric field

answers: NDQ_003224

answers: magnetic field

answers: NDQ_003225

answers: curvature drift term

answers: NDQ_003226

answers: the Himalayas

answers: NDQ_003227

answers: stationary magnetic field and weak electric field

answers: NDQ_003228

answers: inertial drift

answers: NDQ_003230

answers: Pangaea

answers: NDQ_003231

answers: stationary magnetic field

answers: NDQ_003233

answers: Curvature drift term

answers: NDQ_003236

answers: inertial drift

answers: NDQ_003237

answers: inertial drift

answers: NDQ_003239

answers: continental drift

answers: NDQ_003240

answers: Curvature

answers: NDQ_003241

answers: no

answers: NDQ_003242

answers: curvature drift

answers: NDQ_003244

answers: continent

answers: NDQ_003246

answers: continents have never been together as a single whole continent

answers: NDQ_003247

answers: Curvature drift

answers: NDQ_003252

answers: plate tectonics

answers: NDQ_003253

answers: Wegener believed that all the continents were once joined together

answers: NDQ_003254

answers: Wegener hypothesis

answers: NDQ_003255

answers: Wegener

answers: NDQ_003256

answers: Curvature drift term

answers: NDQ_003257

answers: Pangaea broke up a short time ago

answers: NDQ_003258

answers: inertial drift

text: The rising temperatures, and increased oceanic surface area - due to reduced ice cover and rising sea levels - at the end of a glaciation increase the rate of precipitation.

text: The rising temperatures, and increased oceanic surface area - due to reduced ice cover and rising sea levels - at the end of a glaciation increase the rate of

text: precipitation

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answers: 2: The answer has limited relevance and completeness, with significant gaps or inaccuracies.

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answers: NDQ_003256

answers: 0

answers: NDQ_003257

answers: 0

answers: NDQ_003258

answers: 0

answers: NDQ_003219

answers: glaciation

answers: NDQ_003220

answers: glaciation

answers: NDQ_003221

answers: 19th century

answers: NDQ_003222

answers: increased oceanic surface area

answers: NDQ_003223

answers: glaciation

answers: NDQ_003224

answers: glaciation

answers: NDQ_003225

answers: glaciation

answers: NDQ_003226

answers: Antarctica

answers: NDQ_003227

answers: reduced ice cover and rising sea levels

answers: NDQ_003228

answers: increased oceanic surface area

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: magnetic field

answers: NDQ_003233

answers: reduced ice cover and rising sea levels

answers: NDQ_003236

answers: glaciation

answers: NDQ_003237

answers: reduced ice cover and rising sea levels

answers: NDQ_003239

answers: continental drift

answers: NDQ_003240

answers: North America

answers: NDQ_003241

answers: The rising temperatures, and increased oceanic surface area

answers: NDQ_003242

answers: glaciation

answers: NDQ_003244

answers: continent

answers: NDQ_003246

answers: glaciation

answers: NDQ_003247

answers: Continental drift

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: The rising temperatures, and increased oceanic surface area

answers: NDQ_003254

answers: Wegener hypothesis of continental drift

answers: NDQ_003255

answers: reduced ice cover and rising sea levels

answers: NDQ_003256

answers: reduced ice cover and rising sea levels

answers: NDQ_003257

answers: Pangaea broke up a short time ago

answers: NDQ_003258

answers: glaciation

text: The granite outcrops of the Seychelles Islands in the central Indian Ocean were amongst the earliest examples cited by Alfred Wegener as evidence for his continental drift theory. Ridge–plume interactions have been responsible for separating a thinned continental sliver from a large continent (i.e. India).

text: The granite outcrops of the

text: Seychelles Islands

text: in the central Indian Ocean were amongst the earliest examples cited by

text: Alfred Wegener

text: as evidence for his

text: continental drift

text: theory. Ridge–plume interactions have been responsible for separating a thinned continental sliver from a large continent (i.e. India).

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answers: NDQ_003219

answers: continental drift

answers: NDQ_003220

answers: Indian Ocean

answers: NDQ_003221

answers: Alfred Wegener

answers: NDQ_003222

answers: separating a thinned continental sliver from a large continent

answers: NDQ_003223

answers: continental drift

answers: NDQ_003224

answers: Seychelles Islands

answers: NDQ_003225

answers: continental drift theory

answers: NDQ_003226

answers: India

answers: NDQ_003227

answers: Ridge–plume interactions

answers: NDQ_003228

answers: earliest examples cited

answers: NDQ_003230

answers: India

answers: NDQ_003231

answers: Ridge

answers: NDQ_003233

answers: Ridge–plume interactions

answers: NDQ_003236

answers: continental drift theory

answers: NDQ_003237

answers: the Seychelles Islands in the central Indian Ocean

answers: NDQ_003239

answers: Ridge–plume interactions

answers: NDQ_003240

answers: India

answers: NDQ_003241

answers: Indian Ocean

answers: NDQ_003242

answers: continental drift theory

answers: NDQ_003244

answers: Seychelles Islands

answers: NDQ_003246

answers: Ridge–plume interactions

answers: NDQ_003247

answers: Ridge–plume interactions

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: continent drift theory

answers: NDQ_003254

answers: Ridge–plume interactions

answers: NDQ_003255

answers: Ridge–plume interactions

answers: NDQ_003256

answers: Indian Ocean

answers: NDQ_003257

answers: Ridge–plume interactions

answers: NDQ_003258

answers: continental drift theory

text: The Birbal Sahni Institute of Palaeobotany, Lucknow, has done some work on the plant fossils of Mandla, though the study is yet in a preliminary stage. In Ghuguwa and Umaria the standing, petrified trunks of trees have been identified as Gymnosperms and Angiosperms- Monocotyledons and palms. There are certain Bryophytes also. There is some question about whether the fossils are from the late Jurassic or the early and mid Cretaceous age. This is because when the breakup of the single land mass, Pangaea occurred, it was split by the continental drift into Laurasia and Gondwana somewhere between the Jurassic and Cretaceous ages. India formed a part of Gondwana. Depending on the age in which the split occurred, the fossils are either Jurassic or Cretaceous.

text: The

text: Birbal Sahni Institute of Palaeobotany

text: Lucknow

text: , has done some work on the plant fossils of Mandla, though the study is yet in a preliminary stage. In Ghuguwa and Umaria the standing, petrified trunks of

text: trees

text: have been identified as

text: Gymnosperms

text: and

text: Angiosperms

text: Monocotyledons

text: and

text: palms

text: . There are certain

text: Bryophytes

text: also. There is some question about whether the fossils are from the late

text: Jurassic

text: or the early and mid

text: Cretaceous

text: age. This is because when the breakup of the single land mass,

text: Pangaea

text: occurred, it was split by the continental drift into

text: Laurasia

text: and

text: Gondwana

text: somewhere between the Jurassic and Cretaceous ages. India formed a part of Gondwana. Depending on the age in which the split occurred, the fossils are either Jurassic or Cretaceous.

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answers: NDQ_003219

answers: 4

answers: NDQ_003220

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answers: NDQ_003221

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answers: NDQ_003222

answers: 0

answers: NDQ_003223

answers: 0

answers: NDQ_003224

answers: 4

answers: NDQ_003225

answers: 0

answers: NDQ_003226

answers: 0

answers: NDQ_003227

answers: 0

answers: NDQ_003228

answers: 0

answers: NDQ_003230

answers: 0

answers: NDQ_003231

answers: 0

answers: NDQ_003233

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answers: NDQ_003236

answers: 4

answers: NDQ_003237

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answers: NDQ_003239

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answers: NDQ_003240

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answers: NDQ_003244

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answers: NDQ_003246

answers: 4

answers: NDQ_003247

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answers: NDQ_003256

answers: 0

answers: NDQ_003257

answers: 0

answers: NDQ_003258

answers: 0

answers: NDQ_003219

answers: Pangaea was split by the continental drift

answers: NDQ_003220

answers: Gondwana

answers: NDQ_003221

answers: Cretaceous

answers: NDQ_003222

answers: there is some question about whether the fossils are from the late Jurassic or the early and mid Cretaceous age

answers: NDQ_003223

answers: Cretaceous

answers: NDQ_003224

answers: Pangaea

answers: NDQ_003225

answers: Jurassic or Cretaceous

answers: NDQ_003226

answers: Africa

answers: NDQ_003227

answers: split by the continental drift into Laurasia and Gondwana somewhere between the Jurassic and Cretaceous ages

answers: NDQ_003228

answers: Palaeobotany

answers: NDQ_003230

answers: Laurasia

answers: NDQ_003231

answers: magnetism

answers: NDQ_003233

answers: Pangaea

answers: NDQ_003236

answers: continental drift

answers: NDQ_003237

answers: Pangaea

answers: NDQ_003239

answers: Depending on the age in which the split occurred, the fossils are either Jurassic or Cretaceous

answers: NDQ_003240

answers: Pangaea

answers: NDQ_003241

answers: Gondwana

answers: NDQ_003242

answers: continental drift

answers: NDQ_003244

answers: Gondwana

answers: NDQ_003246

answers: Pangaea

answers: NDQ_003247

answers: between the Jurassic and Cretaceous ages

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: Pangaea

answers: NDQ_003254

answers: It was split by the continental drift

answers: NDQ_003255

answers: The Birbal Sahni Institute of Palaeobotany

answers: NDQ_003256

answers: Cretaceous

answers: NDQ_003257

answers: between the Jurassic and Cretaceous ages

answers: NDQ_003258

answers: continental drift

text: The Sallandse heuvelrug is a moraine, created in the one but last glaciation, Saalien, 150.000 years ago. During the Holocene forests started to develop, but after the growth of the human population, these forests had been cut. From the Middle Ages onwards the area was used for grazing by sheep and goat, and the upper layer of the soil was removed to use it as fertilizer for the crop fields. In this period, the area became a heathland because of sand-drifting. In the beginning of the 20th century the state started forestry programms, to prevent this erosion and to produce pine wood.The area is well known for its scenery because of its relatively large heathlands.

text: The Sallandse heuvelrug is a

text: moraine

text: , created in the one but last

text: glaciation

text: Saalien

text: , 150.000 years ago. During the

text: Holocene

text: forests started to develop, but after the growth of the human population, these forests had been cut. From the Middle Ages onwards the area was used for grazing by sheep and goat, and the upper layer of the soil was removed to use it as fertilizer for the crop fields. In this period, the area became a heathland because of sand-drifting. In the beginning of the 20th century the state started forestry programms, to prevent this erosion and to produce pine wood.The area is well known for its scenery because of its relatively large heathlands.

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answers: NDQ_003219

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answers: NDQ_003220

answers: 0

answers: NDQ_003221

answers: 0

answers: NDQ_003222

answers: 2

answers: NDQ_003223

answers: 0

answers: NDQ_003224

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answers: NDQ_003225

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answers: NDQ_003226

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answers: NDQ_003228

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answers: NDQ_003230

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answers: NDQ_003231

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answers: NDQ_003233

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answers: NDQ_003236

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answers: NDQ_003237

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answers: NDQ_003239

answers: 0

answers: NDQ_003240

answers: 0

answers: NDQ_003241

answers: 0

answers: NDQ_003242

answers: 0

answers: NDQ_003244

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answers: NDQ_003247

answers: 4

answers: NDQ_003252

answers: 4

answers: NDQ_003253

answers: 0

answers: NDQ_003254

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answers: 4

answers: NDQ_003256

answers: 0

answers: NDQ_003257

answers: 0

answers: NDQ_003258

answers: 0

answers: NDQ_003219

answers: glaciation

answers: NDQ_003220

answers: Saalien

answers: NDQ_003221

answers: 20th century

answers: NDQ_003222

answers: sand-drifting

answers: NDQ_003223

answers: Saalien

answers: NDQ_003224

answers: moraine

answers: NDQ_003225

answers: Sallandse heuvelrug

answers: NDQ_003226

answers: Saalien

answers: NDQ_003227

answers: the area became a heathland because of sand-drifting

answers: NDQ_003228

answers: The Sallandse heuvelrug

answers: NDQ_003230

answers: South America

answers: NDQ_003231

answers: Heuvelrug

answers: NDQ_003233

answers: the area became a heathland because of sand-drifting

answers: NDQ_003236

answers: sand-drifting

answers: NDQ_003237

answers: sand-drifting

answers: NDQ_003239

answers: sand-drifting

answers: NDQ_003240

answers: Saalien

answers: NDQ_003241

answers: no

answers: NDQ_003242

answers: glaciation

answers: NDQ_003244

answers: Saalien

answers: NDQ_003246

answers: The Sallandse heuvelrug

answers: NDQ_003247

answers: The Sallandse heuvelrug

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: Saalien

answers: NDQ_003254

answers: sand-drifting

answers: NDQ_003255

answers: sand-drifting

answers: NDQ_003256

answers: Saalien

answers: NDQ_003257

answers: 150.000 years ago

answers: NDQ_003258

answers: sand-drifting

text: See drift–diffusion equation for the way that the drift current, diffusion current, and carrier generation and recombination are combined into a single equation.

text: See

text: drift–diffusion equation

text: for the way that the drift current,

text: diffusion current

text: , and

text: carrier generation and recombination

text: are combined into a single equation.

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text: The development of plate tectonics provided a physical basis for many observations of the solid Earth. Long linear regions of geologic features could be explained as plate boundaries. Mid-ocean ridges, high regions on the seafloor where hydrothermal vents and volcanoes exist, were explained as divergent boundaries, where two plates move apart. Arcs of volcanoes and earthquakes were explained as convergent boundaries, where one plate subducts under another. Transform boundaries, such as the San Andreas Fault system, resulted in widespread powerful earthquakes. Plate tectonics also provided a mechanism for Alfred Wegener's theory of continental drift, in which the continents move across the surface of the Earth over geologic time. They also provided a driving force for crustal deformation, and a new setting for the observations of structural geology. The power of the theory of plate tectonics lies in its ability to combine all of these observations into a single theory of how the lithosphere moves over the convecting mantle.

text: The development of plate tectonics provided a physical basis for many observations of the solid Earth. Long linear regions of geologic features could be explained as plate boundaries.

text: Mid-ocean ridge

text: s, high regions on the seafloor where

text: hydrothermal vent

text: s and volcanoes exist, were explained as

text: divergent boundaries

text: , where two plates move apart. Arcs of volcanoes and earthquakes were explained as

text: convergent boundaries

text: , where one plate

text: subducts

text: under another.

text: Transform boundaries

text: , such as the

text: San Andreas Fault

text: system, resulted in widespread powerful earthquakes. Plate tectonics also provided a mechanism for

text: Alfred Wegener

text: 's theory of

text: continental drift

text: , in which the

text: continents

text: move across the surface of the Earth over geologic time. They also provided a driving force for crustal deformation, and a new setting for the observations of structural geology. The power of the theory of plate tectonics lies in its ability to combine all of these observations into a single theory of how the lithosphere moves over the convecting mantle.

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text: After publishing Continental Drift, Banks won the Dos Passos Prize for Literature.

text: After publishing Continental Drift, Banks won the

text: Dos Passos Prize for Literature

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answers: Continental Drift

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answers: Continental Drift

text: The oldest rocks in the group are in the north west of Scotland, Ireland and North Wales and are 2,700 million years old. During the Silurian period the north-western regions collided with the south-east, which had been part of a separate continental landmass. The topography of the islands is modest in scale by global standards. Ben Nevis rises to an elevation of only , and Lough Neagh, which is notably larger than other lakes on the isles, covers . The climate is temperate marine, with mild winters and warm summers. The North Atlantic Drift brings significant moisture and raises temperatures 11 °C (20 °F) above the global average for the latitude. This led to a landscape which was long dominated by temperate rainforest, although human activity has since cleared the vast majority of forest cover. The region was re-inhabited after the last glacial period of Quaternary glaciation, by 12,000 BC when Great Britain was still a peninsula of the European continent.  Ireland, which became an island by 12,000 BC, was not inhabited until after 8000 BC. Great Britain became an island by 5600 BC.

text: The oldest rocks in the group are in the north west of

text: Scotland

text: , Ireland and North Wales and are 2,700

text: million years old

text: . During the

text: Silurian

text: period the north-western regions

text: collided

text: with the south-east, which had been part of a separate continental landmass. The topography of the islands is modest in scale by global standards.

text: Ben Nevis

text: rises to an

text: elevation

text: of only , and

text: Lough Neagh

text: , which is notably larger than other lakes on the isles, covers . The climate is

text: temperate

text: marine

text: , with mild winters and warm summers. The

text: North Atlantic Drift

text: brings significant moisture and raises temperatures 11 °C (20 °F) above the global average for the latitude. This led to a landscape which was long dominated by

text: temperate rainforest

text: , although human activity has since cleared the vast majority of forest cover. The region was re-inhabited after the

text: last glacial period

text: of

text: Quaternary glaciation

text: , by 12,000 BC when Great Britain was still a

text: peninsula of the European continent

text: .  Ireland, which became an island by 12,000 BC, was not inhabited until after 8000 BC. Great Britain became an island by 5600 BC.

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answers: continental landmass collided with the south-east

answers: NDQ_003220

answers: The North Atlantic Drift

answers: NDQ_003221

answers: Silurian period

answers: NDQ_003222

answers: Great Britain was still a peninsula of the European continent

answers: NDQ_003223

answers: the Silurian period

answers: NDQ_003224

answers: rocks

answers: NDQ_003225

answers: During the Silurian period

answers: NDQ_003226

answers: Great Britain

answers: NDQ_003227

answers: separate continental landmass

answers: NDQ_003228

answers: The North Atlantic Drift

answers: NDQ_003230

answers: Europe

answers: NDQ_003231

answers: magnetic field

answers: NDQ_003233

answers: During the Silurian period

answers: NDQ_003236

answers: The North Atlantic Drift

answers: NDQ_003237

answers: The North Atlantic Drift

answers: NDQ_003239

answers: The North Atlantic Drift

answers: NDQ_003240

answers: European continent

answers: NDQ_003241

answers: The North Atlantic

answers: NDQ_003242

answers: The North Atlantic Drift

answers: NDQ_003244

answers: North Atlantic Drift

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answers: During the Silurian period the north-western regions collided with the south-east

answers: NDQ_003247

answers: The north-western regions collided with the south-east, which had been part of a separate continental landmass

answers: NDQ_003252

answers: The North Atlantic Drift

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answers: The oldest rocks in the group are in the north west of Scotland, Ireland and North Wales

answers: NDQ_003254

answers: The North Atlantic Drift

answers: NDQ_003255

answers: The North Atlantic Drift

answers: NDQ_003256

answers: The North Atlantic Drift

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answers: During the Silurian period

answers: NDQ_003258

answers: The North Atlantic Drift

text: Subtropical highland variety of the oceanic climate exists in elevated portions of the world that are within either the tropics or subtropics, though it is typically found in mountainous locations in some tropical countries.  The Köppen Climate Classification subtype for this climate is "Cwb" (Oceanic Subtropical Highland Climate).

text: Subtropical highland variety of the oceanic climate exists in elevated portions of the world that are within either the tropics or subtropics, though it is typically found in mountainous locations in some tropical countries.  The

text: Köppen Climate Classification

text: subtype for this climate is "

text: Cwb

text: " (Oceanic Subtropical Highland Climate).

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answers: NDQ_003219

answers: oceanic climate exists in elevated portions of the world that are within either the tropics or subtropics

answers: NDQ_003220

answers: mountainous

answers: NDQ_003221

answers: 18th century

answers: NDQ_003222

answers: mountainous locations

answers: NDQ_003223

answers: mountainous locations

answers: NDQ_003224

answers: mountainous locations

answers: NDQ_003225

answers: Subtropical highland

answers: NDQ_003226

answers: tropical countries

answers: NDQ_003227

answers: elevated portions of the world

answers: NDQ_003228

answers: Köppen Climate Classification

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: subtropics

answers: NDQ_003233

answers: mountainous locations in some tropical countries

answers: NDQ_003236

answers: mountainous locations

answers: NDQ_003237

answers: mountainous locations

answers: NDQ_003239

answers: continental drift

answers: NDQ_003240

answers: Oceanic

answers: NDQ_003241

answers: It is typically found in mountainous locations in some tropical countries

answers: NDQ_003242

answers: oceanic

answers: NDQ_003244

answers: Arctic Subtropical Highland Climate

answers: NDQ_003246

answers: continents

answers: NDQ_003247

answers: mountainous locations in some tropical countries

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: Subtropical highland

answers: NDQ_003254

answers: It was widely accepted as soon as it was introduced

answers: NDQ_003255

answers: Wegener and his supporters

answers: NDQ_003256

answers: Cwb

answers: NDQ_003257

answers: Pangaea

answers: NDQ_003258

answers: Subtropical highland

text: There is little documentary evidence about the nature of trade in Æthelberht's Kent. It is known that the kings of Kent had established royal control of trade by the late seventh century, but it is not known how early this control began. There is archaeological evidence suggesting that the royal influence predates any of the written sources. It has been suggested that one of Æthelberht's achievements was to take control of trade away from the aristocracy and to make it a royal monopoly. The continental trade provided Kent access to luxury goods which gave it an advantage in trading with the other Anglo-Saxon nations, and the revenue from trade was important in itself.

text: There is little documentary evidence about the nature of trade in Æthelberht's Kent. It is known that the kings of Kent had established royal control of trade by the late seventh century, but it is not known how early this control began. There is archaeological evidence suggesting that the royal influence predates any of the written sources. It has been suggested that one of Æthelberht's achievements was to take control of trade away from the aristocracy and to make it a royal monopoly. The continental trade provided Kent access to luxury goods which gave it an advantage in trading with the other Anglo-Saxon nations, and the revenue from trade was important in itself.

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answers: 0

answers: NDQ_003257

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answers: NDQ_003258

answers: 0

answers: NDQ_003219

answers: continental trade provided Kent access to luxury goods

answers: NDQ_003220

answers: continental

answers: NDQ_003221

answers: Anglo-Saxon

answers: NDQ_003222

answers: archaeological evidence suggesting that the royal influence predates any of the written sources

answers: NDQ_003223

answers: royal influence

answers: NDQ_003224

answers: archaeological evidence

answers: NDQ_003225

answers: royal monopoly

answers: NDQ_003226

answers: Anglo-Saxon

answers: NDQ_003227

answers: The continental trade provided Kent access to luxury goods which gave it an advantage in trading with the other Anglo-Saxon nations

answers: NDQ_003228

answers: The continental trade provided Kent access to luxury goods which gave it an advantage in trading with the other Anglo-Saxon nations

answers: NDQ_003230

answers: Anglo-Saxon

answers: NDQ_003231

answers: Thelberht

answers: NDQ_003233

answers: archaeological evidence suggesting that the royal influence predates any of the written sources

answers: NDQ_003236

answers: continental trade provided Kent access to luxury goods

answers: NDQ_003237

answers: archaeological evidence suggesting that the royal influence predates any of the written sources

answers: NDQ_003239

answers: It is known that the kings of Kent had established royal control of trade by the late seventh century

answers: NDQ_003240

answers: thelberht

answers: NDQ_003241

answers: no

answers: NDQ_003242

answers: continental trade

answers: NDQ_003244

answers: continental

answers: NDQ_003246

answers: The continents have never all been together as a single whole continent

answers: NDQ_003247

answers: The continental trade provided Kent access to luxury goods

answers: NDQ_003252

answers: royal influence predates any of the written sources

answers: NDQ_003253

answers: The continental trade

answers: NDQ_003254

answers: It is known that the kings of Kent had established royal control of trade by the late seventh century, but it is not known how early this control began

answers: NDQ_003255

answers: There is little documentary evidence about the nature of trade in  thelberht's Kent

answers: NDQ_003256

answers: There is archaeological evidence suggesting that the royal influence predates any of the written sources

answers: NDQ_003257

answers: Pangaea broke up a short time ago

answers: NDQ_003258

answers: The continental trade provided Kent access to luxury goods

text: Glaciation has been a rare event in Earth's history, but there is evidence of widespread glaciation during the late Paleozoic Era (200 to 300 Ma) and during late Precambrian (i.e. in the Neoproterozoic Era, 600 to 800 Ma). Before the current ice age, which began 2 to 3 Ma, Earth's climate was typically mild and uniform for long periods of time. This climatic history is implied by the types of fossil plants and animals and by the characteristics of sediments preserved in the stratigraphic record. There are, however, widespread glacial deposits, recording several major periods of ancient glaciation in various parts of the geologic record. Such evidence suggests major periods of glaciation prior to the current Quaternary glaciation.

text: Glaciation has been a rare event in Earth's history, but there is evidence of widespread glaciation during the late

text: Paleozoic

text: Era (200 to 300 Ma) and during late Precambrian (i.e. in the

text: Neoproterozoic

text: Era, 600 to 800 Ma). Before the current

text: ice age

text: , which began 2 to 3 Ma, Earth's climate was typically mild and uniform for long periods of time. This climatic history is implied by the types of

text: fossil

text: plants and animals and by the characteristics of sediments preserved in the

text: stratigraphic

text: record. There are, however, widespread glacial deposits, recording several major periods of ancient glaciation in various parts of the geologic record. Such evidence suggests major periods of glaciation prior to the current Quaternary glaciation.

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answers: Earth's climate was typically mild for long periods of time

answers: NDQ_003220

answers: Atlantic Ocean

answers: NDQ_003221

answers: Neoproterozoic Era

answers: NDQ_003222

answers: glaciation has been a rare event

answers: NDQ_003223

answers: major periods of glaciation

answers: NDQ_003224

answers: glacial deposits

answers: NDQ_003225

answers: Quaternary glaciation

answers: NDQ_003226

answers: Earth's history

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answers: glaciation prior to the current Quaternary glaciation

answers: NDQ_003228

answers: climatic history

answers: NDQ_003230

answers: Earth

answers: NDQ_003231

answers: magnetic field

answers: NDQ_003233

answers: Such evidence suggests major periods of glaciation prior to the current Quaternary glaciation

answers: NDQ_003236

answers: This climatic history is implied

answers: NDQ_003237

answers: widespread glacial deposits

answers: NDQ_003239

answers: Such evidence suggests major periods of glaciation prior to the current Quaternary glaciation

answers: NDQ_003240

answers: Earth

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answers: Earth's

answers: NDQ_003242

answers: Quaternary

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answers: glacial deposits

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answers: Earth's history

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answers: various parts of the geologic record

answers: NDQ_003252

answers: plate tectonics

answers: NDQ_003253

answers: Earth's climate was typically mild and uniform

answers: NDQ_003254

answers: It was widely accepted as soon as it was introduced

answers: NDQ_003255

answers: There are, however, widespread glacial deposits

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answers: It has been a rare event in Earth's history

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answers: The current ice age, which began 2 to 3 Ma

answers: NDQ_003258

answers: Quaternary glaciation

text: An important difference between the paleopedological record and the fossil record of plants and animals is that very few of the soils found are extinct types. Despite the difficulties of identification mentioned earlier, this makes paleopedology (the study of fossil soils) potentially very useful to understanding the ecological relationships in past ecosystems.

text: An important difference between the paleopedological record and the fossil record of

text: plant

text: s and

text: animal

text: s is that very few of the soils found are extinct types. Despite the difficulties of identification mentioned earlier, this makes

text: paleopedology

text: (the study of fossil soils) potentially very useful to understanding the ecological relationships in past ecosystems.

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answers: extinct types

answers: NDQ_003220

answers: are extinct

answers: NDQ_003221

answers: paleopedological

answers: NDQ_003222

answers: difficulties of identification

answers: NDQ_003223

answers: extinct types

answers: NDQ_003224

answers: paleopedology

answers: NDQ_003225

answers: paleopedology

answers: NDQ_003226

answers: Europe

answers: NDQ_003227

answers: very few of the soils found are extinct types

answers: NDQ_003228

answers: the study of fossil soils

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: magnetic field

answers: NDQ_003233

answers: paleopedology

answers: NDQ_003236

answers: paleopedology (the study of fossil soils)

answers: NDQ_003237

answers: paleopedology

answers: NDQ_003239

answers: The study of fossil soils

answers: NDQ_003240

answers: extinct types

answers: NDQ_003241

answers: no

answers: NDQ_003242

answers: paleopedology

answers: NDQ_003244

answers: paleopedology

answers: NDQ_003246

answers: continents

answers: NDQ_003247

answers: paleopedology

answers: NDQ_003252

answers: plate tectonics

answers: NDQ_003253

answers: paleopedology

answers: NDQ_003254

answers: The study of fossil soils

answers: NDQ_003255

answers: paleopedology

answers: NDQ_003256

answers: paleopedology

answers: NDQ_003257

answers: Pangaea

answers: NDQ_003258

answers: paleopedology

text: Neil D. Opdyke is Distinguished Professor Emeritus in the Department of Geological Sciences at the University of Florida in Gainesville, Florida, USA.  He was previously with Lamont-Doherty Geological Observatory of Columbia University, including a stint as Director.  He is well known for his groundbreaking research in the 1950s on paleoclimate and continental drift, with Keith Runcorn, and later in Africa and Australia with Mike McElhinny and others.  Back the US in the mid-1960s he worked on the documentation of magnetic reversals in deep-sea sediments, which led to proof of the Vine–Matthews–Morley hypothesis the governing paradigm for marine magnetic anomalies.

text: Neil D. Opdyke is Distinguished Professor Emeritus in the Department of Geological Sciences at the University of Florida in Gainesville, Florida, USA.  He was previously with

text: Lamont-Doherty Geological Observatory

text: of Columbia University, including a stint as Director.  He is well known for his groundbreaking research in the 1950s on paleoclimate and continental drift, with

text: Keith Runcorn

text: , and later in Africa and Australia with

text: Mike McElhinny

text: and others.  Back the US in the mid-1960s he worked on the documentation of

text: magnetic reversals

text: in deep-sea sediments, which led to proof of the

text: Vine–Matthews–Morley hypothesis

text: the governing paradigm for marine magnetic anomalies.

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text: These animals are commonly found in Wyoming fossil beds primarily as fossilized teeth. From all of the species of this animal, it is concluded that P. major was the largest, reaching the size of a tapir. Its describer, Joseph Leidy, erroneously thought that Palaeosyops consumed both plants and animals after examining the fang-like canines.  However, it is now known that all brontotheres were strict herbivores, and that many, if not most genera of hornless brontotheres had fang-like canines, possibly for both defense from predators, and intraspecific competition.

text: These animals are commonly found in

text: Wyoming

text: fossil beds primarily as fossilized teeth. From all of the species of this animal, it is concluded that P. major was the largest, reaching the size of a tapir. Its describer,

text: Joseph Leidy

text: , erroneously thought that Palaeosyops consumed both plants and animals after examining the fang-like canines.  However, it is now known that all brontotheres were strict herbivores, and that many, if not most genera of hornless brontotheres had fang-like canines, possibly for both defense from predators, and intraspecific competition.

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answers: NDQ_003223

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answers: NDQ_003224

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answers: NDQ_003225

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answers: NDQ_003228

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answers: NDQ_003233

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answers: NDQ_003239

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answers: NDQ_003240

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answers: NDQ_003252

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answers: NDQ_003253

answers: Palaeosyops

answers: NDQ_003254

answers: Joseph Leidy

answers: NDQ_003255

answers: fossilized teeth

answers: NDQ_003256

answers: fossilized teeth

answers: NDQ_003257

answers: Pangaea

answers: NDQ_003258

answers: Palaeosyops

text: In 1889 and 1909 Roberto Mantovani published a hypothesis of Earth expansion and continental drift. He assumed that a closed continent covered the entire surface of a smaller Earth. Thermal expansion led to volcanic activity, which broke the land mass into smaller continents. These continents drifted away from each other because of further expansion at the rip-zones, where oceans currently lie. Although Alfred Wegener noticed some similarities to his own hypothesis of continental drift, he did not mention Earth expansion as the cause of drift in Mantovani's hypothesis.

text: In 1889 and 1909

text: Roberto Mantovani

text: published a hypothesis of Earth expansion and continental drift. He assumed that a closed continent covered the entire surface of a smaller Earth.

text: Thermal expansion

text: led to

text: volcanic

text: activity, which broke the land mass into smaller continents. These continents drifted away from each other because of further expansion at the rip-zones, where oceans currently lie. Although

text: Alfred Wegener

text: noticed some similarities to his own hypothesis of

text: continental drift

text: , he did not mention Earth expansion as the cause of drift in Mantovani's hypothesis.

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answers: NDQ_003219

answers: Earth expansion

answers: NDQ_003220

answers: are not mentioned

answers: NDQ_003221

answers: 1889

answers: NDQ_003222

answers: Mantovani's hypothesis

answers: NDQ_003223

answers: Earth expansion

answers: NDQ_003224

answers: Earth expansion

answers: NDQ_003225

answers: continental drift

answers: NDQ_003226

answers: the Himalayas

answers: NDQ_003227

answers: he did not mention Earth expansion as the cause of drift

answers: NDQ_003228

answers: his own hypothesis of continental drift

answers: NDQ_003230

answers: Earth

answers: NDQ_003231

answers: rip-zones

answers: NDQ_003233

answers: Roberto Mantovani

answers: NDQ_003236

answers: drift

answers: NDQ_003237

answers: similarities to his own hypothesis

answers: NDQ_003239

answers: Mantovani's hypothesis

answers: NDQ_003240

answers: Earth

answers: NDQ_003241

answers: Earth

answers: NDQ_003242

answers: Thermal expansion

answers: NDQ_003244

answers: drifted away

answers: NDQ_003246

answers: These continents drifted away from each other

answers: NDQ_003247

answers: oceans

answers: NDQ_003252

answers: Earth expansion

answers: NDQ_003253

answers: continent covered the entire surface of a smaller Earth

answers: NDQ_003254

answers: It was widely accepted as soon as it was introduced

answers: NDQ_003255

answers: Roberto Mantovani

answers: NDQ_003256

answers: The Atlantic Ocean

answers: NDQ_003257

answers: Pangaea broke up a short time ago

answers: NDQ_003258

answers: Earth expansion

text: Buck and Rudy made a brief cameo in the following film Ice Age: Continental Drift.

text: Buck and Rudy made a brief cameo in the following film

text: Ice Age: Continental Drift

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answers: NDQ_003219

answers: Continental Drift

answers: NDQ_003220

answers: Continental

answers: NDQ_003221

answers: Ice Age

answers: NDQ_003222

answers: Ice Age: Continental Drift

answers: NDQ_003223

answers: Ice Age

answers: NDQ_003224

answers: Ice Age

answers: NDQ_003225

answers: cameo

answers: NDQ_003226

answers: Ice Age

answers: NDQ_003227

answers: Ice Age

answers: NDQ_003228

answers: Continental Drift

answers: NDQ_003230

answers: Ice Age

answers: NDQ_003231

answers: Ice Age

answers: NDQ_003233

answers: Ice Age

answers: NDQ_003236

answers: Continental Drift

answers: NDQ_003237

answers: Ice Age: Continental Drift

answers: NDQ_003239

answers: Continental Drift

answers: NDQ_003240

answers: Ice Age

answers: NDQ_003241

answers: Continental Drift

answers: NDQ_003242

answers: Ice Age

answers: NDQ_003244

answers: Continental Drift

answers: NDQ_003246

answers: Continental Drift

answers: NDQ_003247

answers: Ice Age: Continental Drift

answers: NDQ_003252

answers: Continental Drift

answers: NDQ_003253

answers: Continental Drift

answers: NDQ_003254

answers: It was widely accepted

answers: NDQ_003255

answers: Wegener and his supporters

answers: NDQ_003256

answers: Continental Drift

answers: NDQ_003257

answers: Buck and Rudy

answers: NDQ_003258

answers: Continental Drift

text: The bedrock consists of many layers formed over vast periods of time. These were laid down in various climates as the global climate changed, the landmasses moved due to continental drift, and the land and sea levels rose or fell. From time to time horizontal forces caused the rock to undergo considerable deformation, folding the layers of rock to form mountains which have since been eroded and overlain with other layers. To further complicate the geology, the land has also been subject to periods of earthquakes and volcanic activity.

text: The

text: bedrock

text: consists of many layers formed over vast periods of time. These were laid down in various

text: climate

text: s as the global climate changed, the landmasses moved due to

text: continental drift

text: , and the land and sea levels rose or fell. From time to time horizontal forces caused the rock to undergo considerable

text: deformation

text: , folding the layers of rock to form mountains which have since been

text: eroded

text: and overlain with other layers. To further complicate the geology, the land has also been subject to periods of

text: earthquake

text: s and

text: volcanic

text: activity.

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answers: 0

answers: NDQ_003219

answers: 4

answers: NDQ_003220

answers: 0

answers: NDQ_003221

answers: 0

answers: NDQ_003222

answers: 2

answers: NDQ_003223

answers: 0

answers: NDQ_003224

answers: 0

answers: NDQ_003225

answers: 4

answers: NDQ_003226

answers: 0

answers: NDQ_003227

answers: 0

answers: NDQ_003228

answers: 0

answers: NDQ_003230

answers: 0

answers: NDQ_003231

answers: 0

answers: NDQ_003233

answers: 0

answers: NDQ_003236

answers: 5

answers: NDQ_003237

answers: 4

answers: NDQ_003239

answers: 4

answers: NDQ_003240

answers: 0

answers: NDQ_003241

answers: 0

answers: NDQ_003242

answers: 4

answers: NDQ_003244

answers: 0

answers: NDQ_003246

answers: 4

answers: NDQ_003247

answers: 4

answers: NDQ_003252

answers: 4

answers: NDQ_003253

answers: 4

answers: NDQ_003254

answers: 4

answers: NDQ_003255

answers: 4

answers: NDQ_003256

answers: 0

answers: NDQ_003257

answers: 0

answers: NDQ_003258

answers: 4

answers: NDQ_003219

answers: land masses moved due to continental drift

answers: NDQ_003220

answers: continental drift

answers: NDQ_003221

answers: geology

answers: NDQ_003222

answers: the global climate changed

answers: NDQ_003223

answers: volcanic activity

answers: NDQ_003224

answers: mountains

answers: NDQ_003225

answers: continental drift

answers: NDQ_003226

answers: Europe

answers: NDQ_003227

answers: the landmasses moved due to continental drift

answers: NDQ_003228

answers: continental drift

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: magnetic field

answers: NDQ_003233

answers: landmasses moved due to continental drift

answers: NDQ_003236

answers: continental drift

answers: NDQ_003237

answers: landmasses moved

answers: NDQ_003239

answers: landmasses moved due to continental drift

answers: NDQ_003240

answers: North America

answers: NDQ_003241

answers: no

answers: NDQ_003242

answers: continental drift

answers: NDQ_003244

answers: continental drift

answers: NDQ_003246

answers: continental drift

answers: NDQ_003247

answers: landmasses moved

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: continental drift

answers: NDQ_003254

answers: landmasses moved due to continental drift

answers: NDQ_003255

answers: landmasses moved

answers: NDQ_003256

answers: continental drift

answers: NDQ_003257

answers: Pangaea broke up

answers: NDQ_003258

answers: continental drift

text: In 1904 he was hired by the Brazilian government as head of the "Comissão de Estudos das Minas de Carvão de Pedra do Brasil" (Commission for Studies on Brazilian Coal Mines), whose aim was to identify the potential of Brazilian coal, and whose report, published in 1908, was a milestone for understanding the geology of the Paraná Basin in Southern Brazil. One of the main results of these studies, besides the reconnaissance for coal, was the discovery of Mesosaurus fossils within Permian black shales (Irati Formation), and the Glossopteris flora within the Permian coals. White was one of the first to propose the  equivalence between the South American Permian strata and similar rocks of the Karoo Basin in South Africa. This report had an important contribution to the development of Continental Drift Theory, published by Alfred Wegener in 1912.

text: In 1904 he was hired by the

text: Brazil

text: ian government as head of the "Comissão de Estudos das Minas de Carvão de Pedra do Brasil" (Commission for Studies on Brazilian Coal Mines), whose aim was to identify the potential of Brazilian coal, and whose report, published in 1908, was a milestone for understanding the geology of the

text: Paraná Basin

text: in

text: Southern Brazil

text: . One of the main results of these studies, besides the reconnaissance for coal, was the discovery of

text: Mesosaurus

text: fossil

text: s within

text: Permian

text: black

text: shale

text: s (

text: Irati Formation

text: ), and the

text: Glossopteris

text: flora

text: within the Permian coals. White was one of the first to propose the  equivalence between the

text: South American

text: Permian strata and similar rocks of the

text: Karoo Basin

text: in

text: South Africa

text: . This report had an important contribution to the development of

text: Continental Drift Theory

text: , published by

text: Alfred Wegener

text: in 1912.

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answers: 2 The answer has limited relevance and completeness, with significant gaps or inaccuracies.

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answers: 5: The answer is highly relevant, complete, and accurate.

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answers: 4

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answers: NDQ_003257

answers: 0

answers: NDQ_003258

answers: 5

answers: NDQ_003219

answers: Continental Drift Theory

answers: NDQ_003220

answers: South American

answers: NDQ_003221

answers: 1912

answers: NDQ_003222

answers: Alfred Wegener in 1912

answers: NDQ_003223

answers: Permian

answers: NDQ_003224

answers: Mesosaurus fossils

answers: NDQ_003225

answers: Continental Drift Theory

answers: NDQ_003226

answers: South Africa

answers: NDQ_003227

answers: Theorem

answers: NDQ_003228

answers: first to propose the equivalence between the South American Permian strata and similar rocks of the Karoo Basin

answers: NDQ_003230

answers: Brazil

answers: NDQ_003231

answers: Drift Theory

answers: NDQ_003233

answers: Mesosaurus fossils within Permian black shales

answers: NDQ_003236

answers: Continental Drift Theory

answers: NDQ_003237

answers: Mesosaurus fossils

answers: NDQ_003239

answers: The discovery of Mesosaurus fossils within Permian black shales

answers: NDQ_003240

answers: continental drift theory

answers: NDQ_003241

answers: South American

answers: NDQ_003242

answers: Drift Theory

answers: NDQ_003244

answers: Mesosaurus fossils

answers: NDQ_003246

answers: Continental Drift Theory

answers: NDQ_003247

answers: the Karoo Basin in South Africa

answers: NDQ_003252

answers: Continental Drift Theory

answers: NDQ_003253

answers: Drift Theory

answers: NDQ_003254

answers: It was widely accepted as soon as it was introduced

answers: NDQ_003255

answers: The discovery of Mesosaurus fossils

answers: NDQ_003256

answers: The Karoo Basin

answers: NDQ_003257

answers: Continental Drift Theory

answers: NDQ_003258

answers: Continental Drift Theory

text: In 1920 Epstein calculated the effect of Polflucht as a possible causing force of Wegener's continental drift. His value was about 10^-6 of the gravitational force. Some years later other geophysicists could show that the Polflucht force is far too weak to cause plate tectonics. The toughness of the sublayers of the Earth's crust is much more stronger than assumed by Epstein.

text: In 1920 Epstein calculated the effect of

text: Polflucht

text: as a possible causing force of

text: Wegener

text: 's

text: continental drift

text: . His value was about 10^-6 of the gravitational force. Some years later other geophysicists could show that the Polflucht force is far too weak to cause

text: plate tectonics

text: . The toughness of the sublayers of the

text: Earth's crust

text: is much more stronger than assumed by Epstein.

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answers: 4

answers: NDQ_003222

answers: 2

answers: NDQ_003223

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answers: 4

answers: NDQ_003226

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answers: 2

answers: NDQ_003237

answers: 1

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answers: 4

answers: NDQ_003247

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answers: 3

answers: NDQ_003253

answers: 4

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answers: NDQ_003255

answers: 3

answers: NDQ_003256

answers: 0

answers: NDQ_003257

answers: 0

answers: NDQ_003258

answers: 4

answers: NDQ_003219

answers: Polflucht

answers: NDQ_003220

answers: Polflucht

answers: NDQ_003221

answers: Wegener

answers: NDQ_003222

answers: Polflucht force is far too weak

answers: NDQ_003223

answers: Polflucht

answers: NDQ_003224

answers: Polflucht

answers: NDQ_003225

answers: continental drift

answers: NDQ_003226

answers: Europe

answers: NDQ_003227

answers: plate tectonics

answers: NDQ_003228

answers: continental drift

answers: NDQ_003230

answers: Earth

answers: NDQ_003231

answers: Polflucht

answers: NDQ_003233

answers: The toughness of the sublayers of the Earth's crust

answers: NDQ_003236

answers: Wegener's continental drift

answers: NDQ_003237

answers: Polflucht

answers: NDQ_003239

answers: Polflucht

answers: NDQ_003240

answers: Earth

answers: NDQ_003241

answers: Earth's crust

answers: NDQ_003242

answers: plate tectonics

answers: NDQ_003244

answers: continent drift

answers: NDQ_003246

answers: continental drift

answers: NDQ_003247

answers: Polflucht

answers: NDQ_003252

answers: plate tectonics

answers: NDQ_003253

answers: Polflucht

answers: NDQ_003254

answers: Some years later

answers: NDQ_003255

answers: Polflucht

answers: NDQ_003256

answers: Polflucht

answers: NDQ_003257

answers: Polflucht

answers: NDQ_003258

answers: Polflucht

text: The Park both below and above the Great Escarpment is situated on the Beaufort group of rocks, which form part of the Karoo geological system of deposits. The Beaufort sediments were laid down on a vast alluvial plain covering much of what was to become Southern Africa, when it was still part of Gondwana, beginning about 280 million years ago, and ending about 240 million years ago. These 6 km thick sediments were deposited by rivers similar in size and number to the Ganges, Brahmaputra, and Indus rivers which drain the Himalaya mountains on the Indian subcontinent today. In Gondwana, when the Beaufort sediments were being laid down, the Himalaya-sized mountains were to the south of the present South African coastline, on what is geologically known as the “Falklands Plateau”, now separated from South Africa by continental drift, and lying as severely eroded islands in the south western Atlantic Ocean. A large variety of amphibians and reptiles lived on the lush vegetation of  these well-watered plains, the most interesting of which were the mammal-like reptiles, which have made the Karoo paleontologically famous. Their fossils have been found all over the Karoo. Some of these fossils are on display in the Park, though none of them have been found there.

text: The Park both below and above the Great Escarpment is situated on the

text: Beaufort group

text: of rocks, which form part of the

text: Karoo geological system of deposits

text: . The Beaufort sediments were laid down on a vast alluvial plain covering much of what was to become Southern Africa, when it was still part of

text: Gondwana

text: , beginning about 280 million years ago, and ending about 240 million years ago. These 6 km thick sediments were deposited by rivers similar in size and number to the

text: Ganges

text: Brahmaputra

text: , and

text: Indus

text: rivers which drain the

text: Himalaya

text: mountains on the Indian subcontinent today. In Gondwana, when the Beaufort sediments were being laid down, the Himalaya-sized mountains were to the south of the present South African coastline, on what is geologically known as the “Falklands Plateau”, now separated from South Africa by

text: continental drift

text: , and lying as severely eroded islands in the south western Atlantic Ocean. A large variety of amphibians and reptiles lived on the lush vegetation of  these well-watered plains, the most interesting of which were the

text: mammal-like reptiles

text: , which have made the Karoo paleontologically famous. Their fossils have been found all over the Karoo. Some of these fossils are on display in the Park, though none of them have been found there.

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answers: It was widely accepted as soon as it was introduced

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answers: the “Falklands Plateau”

text: In the early 1940s, he took a position at the University of Alberta. While there he hypothesized that coral reefs had once lived in what is now the Arctic. He further hypothesized that this would mean there would be oil there now. There has been speculation that his hypothesis was not a stretch given the fact that the Norman Wells had been discovered in the early 1920s and oil seeps had been reported along the river for centuries. The explanation was not yet clear, however, since the theory of continental drift had yet to be proposed.

text: In the early 1940s, he took a position at the University of Alberta. While there he hypothesized that

text: coral reef

text: s had once lived in what is now the

text: Arctic

text: . He further hypothesized that this would mean there would be oil there now. There has been speculation that his hypothesis was not a stretch given the fact that the Norman Wells had been discovered in the early 1920s and oil seeps had been reported along the river for centuries. The explanation was not yet clear, however, since the theory of

text: continental drift

text: had yet to be proposed.

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answers: oil seeps had been reported along the river for centuries

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text: Old and Young Drift are geographic names given to the morainic landscapes that were formed in Central Europe; the Old Drift during the older ice ages and the Young Drift during the latest glaciations – the Weichselian in North Germany and the Würm in the Alps. Their landforms are quite different. Areas of Old Drift have been heavily flattened and transformed as a result of geomorphic processes such as denudation and erosion, whilst areas of Young Drift have largely retained their original shape. Whilst the majority of Old Drift moraines were formed during the Saale glaciation about 130,000 to 140,000 years ago, the Young Drift moraines in Central Europe are only about 15,000 to 20,000 years old. The terms Old and Young Drift are used for all elements of the glacial series even though the meltwater deposits and landforms are not strictly moraines.

text: Old and Young Drift are geographic names given to the

text: morainic

text: landscapes that were formed in Central Europe; the Old Drift during the older

text: ice age

text: s and the Young Drift during the latest

text: glaciation

text: s – the

text: Weichselian

text: in North Germany and the

text: Würm

text: in the

text: Alps

text: . Their

text: landform

text: s are quite different. Areas of Old Drift have been heavily flattened and transformed as a result of geomorphic processes such as

text: denudation

text: and

text: erosion

text: , whilst areas of Young Drift have largely retained their original shape. Whilst the majority of Old Drift moraines were formed during the

text: Saale glaciation

text: about 130,000 to 140,000 years ago, the Young Drift moraines in Central Europe are only about 15,000 to 20,000 years old. The terms Old and Young Drift are used for all elements of the

text: glacial series

text: even though the meltwater deposits and landforms are not strictly moraines.

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answers: NDQ_003219

answers: ice ages

answers: NDQ_003220

answers: Alps

answers: NDQ_003221

answers: glacial series

answers: NDQ_003222

answers: Old Drift have been heavily flattened and transformed

answers: NDQ_003223

answers: the Saale glaciation

answers: NDQ_003224

answers: Old and Young Drift

answers: NDQ_003225

answers: Old Drift

answers: NDQ_003226

answers: Central Europe

answers: NDQ_003227

answers: The terms Old and Young Drift are used for all elements of the glacial series

answers: NDQ_003228

answers: geomorphic processes

answers: NDQ_003230

answers: Central Europe

answers: NDQ_003231

answers: moraines

answers: NDQ_003233

answers: Old Drift have been heavily flattened and transformed as a result of geomorphic processes

answers: NDQ_003236

answers: Drift are geographic names given to the morainic landscapes that were formed in Central Europe

answers: NDQ_003237

answers: Old Drift have been heavily flattened and transformed as a result of geomorphic processes

answers: NDQ_003239

answers: Old and Young Drift

answers: NDQ_003240

answers: Old Drift

answers: NDQ_003241

answers: No

answers: NDQ_003242

answers: glacial series

answers: NDQ_003244

answers: Central Europe

answers: NDQ_003246

answers: They have never all been together as a single whole continent

answers: NDQ_003247

answers: Old Drift have been heavily flattened and transformed as a result of geomorphic processes

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: Central Europe

answers: NDQ_003254

answers: Würm in the Alps

answers: NDQ_003255

answers: Wegener and his supporters provided a lot of evidence for continental drift

answers: NDQ_003256

answers: Old and Young Drift

answers: NDQ_003257

answers: Young Drift

answers: NDQ_003258

answers: Wegener developed a theory to explain how continents can drift

text: Although this was long before general acceptance of 'continental-drift', plate tectonics and sea-floor spreading, some saw the Antarctic fossil plants as compelling evidence for the existence of the former 'super-continent', Gondwana. Some five years after the palaeobotanical evidence was announced to the world, James Kitching added the evidence of vertebrate fossils to this debate when he joined the United States Antarctic Research Group on a visit in 1970, and collected vertebrate fossils identical to those he was accustomed to finding in the Karoo.

text: Although this was long before general acceptance of 'continental-drift',

text: plate tectonics

text: and

text: sea-floor spreading

text: , some saw the Antarctic fossil plants as compelling evidence for the existence of the former 'super-continent',

text: Gondwana

text: . Some five years after the palaeobotanical evidence was announced to the world,

text: James Kitching

text: added the evidence of vertebrate fossils to this debate when he joined the

text: United States Antarctic Research Group

text: on a visit in 1970, and collected vertebrate fossils identical to those he was accustomed to finding in the

text: Karoo

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answers: NDQ_003258

answers: 4

answers: NDQ_003219

answers: continental-drift

answers: NDQ_003220

answers: Antarctic

answers: NDQ_003221

answers: 1970

answers: NDQ_003222

answers: long before general acceptance

answers: NDQ_003223

answers: Gondwana

answers: NDQ_003224

answers: Antarctic fossil plants

answers: NDQ_003225

answers: continental-drift

answers: NDQ_003226

answers: Antarctic

answers: NDQ_003227

answers: the former'super-continent', Gondwana

answers: NDQ_003228

answers: palaeobotanical evidence

answers: NDQ_003230

answers: Antarctica

answers: NDQ_003231

answers: magnetism

answers: NDQ_003233

answers: Some five years after the palaeobotanical evidence was announced to the world

answers: NDQ_003236

answers: continental-drift

answers: NDQ_003237

answers: Antarctic fossil plants

answers: NDQ_003239

answers: Gondwana

answers: NDQ_003240

answers: Gondwana

answers: NDQ_003241

answers: Antarctic

answers: NDQ_003242

answers: plate tectonics

answers: NDQ_003244

answers: Gondwana

answers: NDQ_003246

answers: Gondwana

answers: NDQ_003247

answers: Antarctic

answers: NDQ_003252

answers: continental-drift

answers: NDQ_003253

answers: super-continent

answers: NDQ_003254

answers: Some five years after the palaeobotanical evidence was announced to the world

answers: NDQ_003255

answers: palaeobotanical evidence

answers: NDQ_003256

answers: Gondwana

answers: NDQ_003257

answers: Gondwana

answers: NDQ_003258

answers: plate tectonics

text: As early as the 18th century, it was noticed that compass needles deviated near strongly magnetized outcrops. In 1797, Von Humboldt attributed this magnetization to lightning strikes (and lightning strikes do often magnetize surface rocks).  In the 19th century studies of the direction of magnetization in rocks showed that some recent lavas were magnetized parallel to the Earth's magnetic field. Early in the 20th century, work by David, Brunhes and Mercanton showed that many rocks were magnetized antiparallel to the field. Japanese geophysicist Motonori Matuyama showed that the Earth's magnetic field reversed in the  mid-Quaternary, a reversal now known as the Brunhes-Matuyama reversal.

text: As early as the 18th century, it was noticed that compass needles deviated near strongly magnetized outcrops. In 1797, Von Humboldt attributed this magnetization to lightning strikes (and lightning strikes do often magnetize surface rocks).  In the 19th century studies of the direction of magnetization in rocks showed that some recent lavas were magnetized parallel to the Earth's magnetic field. Early in the 20th century, work by David, Brunhes and Mercanton showed that many rocks were magnetized antiparallel to the field. Japanese geophysicist

text: Motonori Matuyama

text: showed that the Earth's magnetic field reversed in the  mid-

text: Quaternary

text: , a reversal now known as the

text: Brunhes-Matuyama reversal

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answers: NDQ_003219

answers: lightning strikes do often magnetize surface rocks

answers: NDQ_003220

answers: Antiparallel to the field

answers: NDQ_003221

answers: 18th century

answers: NDQ_003222

answers: antiparallel to the field

answers: NDQ_003223

answers: Earth's magnetic field

answers: NDQ_003224

answers: magnetic outcrops

answers: NDQ_003225

answers: attributed this magnetization to lightning strikes

answers: NDQ_003226

answers: the Earth's magnetic field

answers: NDQ_003227

answers: many rocks were magnetized antiparallel to the field

answers: NDQ_003228

answers: Japanese geophysicist

answers: NDQ_003230

answers: Earth

answers: NDQ_003231

answers: field

answers: NDQ_003233

answers: Brunhes-Matuyama reversal

answers: NDQ_003236

answers: Brunhes-Matuyama reversal

answers: NDQ_003237

answers: strongly magnetized outcrops

answers: NDQ_003239

answers: Many rocks were magnetized antiparallel to the field

answers: NDQ_003240

answers: Earth

answers: NDQ_003241

answers: Earth

answers: NDQ_003242

answers: Earth's magnetic field

answers: NDQ_003244

answers: antiparallel to the field

answers: NDQ_003246

answers: Many rocks were magnetized antiparallel to the field

answers: NDQ_003247

answers: magnetized antiparallel to the field

answers: NDQ_003252

answers: plate tectonics

answers: NDQ_003253

answers: The Brunhes-Matuyama reversal

answers: NDQ_003254

answers: It was noticed that compass needles deviated near strongly magnetized outcrops

answers: NDQ_003255

answers: many rocks were magnetized antiparallel to the field

answers: NDQ_003256

answers: rocks were magnetized antiparallel to the field

answers: NDQ_003257

answers: The Brunhes-Matuyama reversal

answers: NDQ_003258

answers: the Brunhes-Matuyama reversal

text: Identification of the 'Atlantic' and 'Pacific' trilobite faunas in North America and Europe implied the closure of the Iapetus Ocean (producing the Iapetus suture), thus providing important supporting evidence for the theory of continental drift.

text: Identification of the 'Atlantic' and 'Pacific' trilobite faunas in North America and Europe implied the closure of the

text: Iapetus Ocean

text: (producing the

text: Iapetus suture

text: ), thus providing important supporting evidence for the theory of

text: continental drift

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answers: 4

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answers: 4

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answers: NDQ_003223

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answers: 4

answers: NDQ_003225

answers: 4

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answers: 4

answers: NDQ_003252

answers: 4

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answers: 4

answers: NDQ_003255

answers: 4

answers: NDQ_003256

answers: 0

answers: NDQ_003257

answers: 0

answers: NDQ_003258

answers: 4

answers: NDQ_003219

answers: continental drift

answers: NDQ_003220

answers: North America

answers: NDQ_003221

answers: continental drift

answers: NDQ_003222

answers: closed of the Iapetus Ocean

answers: NDQ_003223

answers: Iapetus suture

answers: NDQ_003224

answers: trilobite

answers: NDQ_003225

answers: continental drift

answers: NDQ_003226

answers: Europe

answers: NDQ_003227

answers: the closure of the Iapetus Ocean

answers: NDQ_003228

answers: important supporting evidence for the theory of continental drift

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: suture

answers: NDQ_003233

answers: the closure of the Iapetus Ocean

answers: NDQ_003236

answers: continental drift

answers: NDQ_003237

answers: trilobite faunas

answers: NDQ_003239

answers: Iapetus suture

answers: NDQ_003240

answers: Iapetus

answers: NDQ_003241

answers: North America

answers: NDQ_003242

answers: theory of continental drift

answers: NDQ_003244

answers: trilobite faunas

answers: NDQ_003246

answers: continental drift

answers: NDQ_003247

answers: Iapetus suture

answers: NDQ_003252

answers: plate tectonics

answers: NDQ_003253

answers: Iapetus suture

answers: NDQ_003254

answers: The theory of continental drift

answers: NDQ_003255

answers: Iapetus suture

answers: NDQ_003256

answers: Iapetus suture

answers: NDQ_003257

answers: Iapetus suture

answers: NDQ_003258

answers: Iapetus suture

text: In the Himalaya, the Indian continental plate is crashing into the Eurasian continental plate with nearly north-south motion. Therefore, the compression of the rocks in the Himalaya is in the north-south direction.  So, folding should occur trending east-west, as is observed. However, it has also been noted that folding occurs in the north-south direction.  It was noted that these folds follow the traces of the major rivers, such as the Arun and the Indus. Originally these folds were explained by assuming that the rivers did not form these anticlines, instead the river's course was by coincidence on top of these geologic features, forming by differential erosion. The idea of isostatic rebound was suggested as the best fit mechanism for these north-south trending folds and is now widely accepted.

text: In the Himalaya, the

text: Indian continental plate

text: is crashing into the

text: Eurasian continental plate

text: with nearly north-south motion. Therefore, the compression of the rocks in the Himalaya is in the north-south direction.  So, folding should occur trending east-west, as is observed. However, it has also been noted that folding occurs in the north-south direction.  It was noted that these folds follow the traces of the major rivers, such as the Arun and the Indus. Originally these folds were explained by assuming that the rivers did not form these anticlines, instead the river's course was by coincidence on top of these geologic features, forming by differential erosion. The idea of

text: isostatic rebound

text: was suggested as the best fit mechanism for these north-south trending folds and is now widely accepted.

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answers: 5: The answer is highly relevant, complete, and accurate.

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answers: NDQ_003219

answers: 4

answers: NDQ_003220

answers: 0

answers: NDQ_003221

answers: 2

answers: NDQ_003222

answers: 2

answers: NDQ_003223

answers: 0

answers: NDQ_003224

answers: 0

answers: NDQ_003225

answers: 4

answers: NDQ_003226

answers: 0

answers: NDQ_003227

answers: 0

answers: NDQ_003228

answers: 0

answers: NDQ_003230

answers: 0

answers: NDQ_003231

answers: 0

answers: NDQ_003233

answers: 0

answers: NDQ_003236

answers: 4

answers: NDQ_003237

answers: 0

answers: NDQ_003239

answers: 0

answers: NDQ_003240

answers: 0

answers: NDQ_003241

answers: 0

answers: NDQ_003242

answers: 0

answers: NDQ_003244

answers: 0

answers: NDQ_003246

answers: 4

answers: NDQ_003247

answers: 0

answers: NDQ_003252

answers: 4

answers: NDQ_003253

answers: 0

answers: NDQ_003254

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answers: NDQ_003255

answers: 4

answers: NDQ_003256

answers: 0

answers: NDQ_003257

answers: 0

answers: NDQ_003258

answers: 0

answers: NDQ_003219

answers: rivers did not form these anticlines

answers: NDQ_003220

answers: Himalaya

answers: NDQ_003221

answers: late 19th century

answers: NDQ_003222

answers: rivers did not form these anticlines

answers: NDQ_003223

answers: isostatic rebound

answers: NDQ_003224

answers: rivers

answers: NDQ_003225

answers: isostatic rebound

answers: NDQ_003226

answers: Himalaya

answers: NDQ_003227

answers: the rivers did not form these anticlines

answers: NDQ_003228

answers: the Indian continental plate is crashing into the Eurasian continental plate with nearly north-south motion

answers: NDQ_003230

answers: Eurasian

answers: NDQ_003231

answers: magnetism

answers: NDQ_003233

answers: the Indian continental plate is crashing into the Eurasian continental plate with nearly north-south motion

answers: NDQ_003236

answers: north-south motion

answers: NDQ_003237

answers: folds follow the traces of the major rivers

answers: NDQ_003239

answers: It was noted that these folds follow the traces of the major rivers

answers: NDQ_003240

answers: Eurasian

answers: NDQ_003241

answers: Eurasian

answers: NDQ_003242

answers: isostatic rebound

answers: NDQ_003244

answers: Indian continental plate is crashing into the Eurasian continental plate

answers: NDQ_003246

answers: Indian continental plate is crashing into the Eurasian continental plate

answers: NDQ_003247

answers: rivers, such as the Arun and the Indus

answers: NDQ_003252

answers: plate tectonics

answers: NDQ_003253

answers: Indian continental plate is crashing into the Eurasian continental plate

answers: NDQ_003254

answers: The idea of isostatic rebound

answers: NDQ_003255

answers: The idea of isostatic rebound was suggested as the best fit mechanism

answers: NDQ_003256

answers: The idea of isostatic rebound

answers: NDQ_003257

answers: The idea of isostatic rebound

answers: NDQ_003258

answers: isostatic rebound

text: The village of Rhynie in Aberdeenshire is the site of an important sedimentary deposit - Rhynie chert. The bulk of this fossil bed consists of primitive plants that had water-conducting cells and sporangia but no leaves, along with arthropods: Collembola, Opiliones (harvestmen), pseudoscorpions and the extinct, spider-like Trigonotarbids. This fossil bed is remarkable for two reasons. Firstly, the age of the find (early Devonian circa 410 Ma) makes this one of the earliest sites anywhere containing terrestrial fossils, coinciding with the first stages of the colonisation of land by plants and animals. Secondly, these cherts are famous for their exceptional state of ultrastructural preservation, with individual cell walls easily visible in polished specimens. For example, stomata have been counted and lignin remnants detected in the plant material.

text: The village of

text: Rhynie

text: in

text: Aberdeenshire

text: is the site of an important sedimentary deposit -

text: Rhynie chert

text: . The bulk of this fossil bed consists of primitive

text: plant

text: s that had

text: water-conducting cells

text: and

text: sporangia

text: but no

text: leaves

text: , along with

text: arthropod

text: s:

text: Collembola

text: Opiliones

text: harvestmen

text: pseudoscorpion

text: s and the extinct, spider-like

text: Trigonotarbid

text: s. This fossil bed is remarkable for two reasons. Firstly, the age of the find (

text: early Devonian

text: circa 410 Ma) makes this one of the earliest sites anywhere containing terrestrial fossils, coinciding with the first stages of the colonisation of land by plants and

text: animal

text: s. Secondly, these

text: chert

text: s are famous for their exceptional state of

text: ultrastructural

text: preservation, with individual cell walls easily visible in polished specimens. For example,

text: stomata

text: have been counted and

text: lignin

text: remnants detected in the plant material.

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text: Historical evidence of shallow coal drift-mining of the Ringinglow seam which lies on top of the Chatsworth Grit has been found in the Barber Fields area. The workings extended beneath the watercourse. Stratigraphically this was the lowest coal seams ever worked in the Sheffield area. The mine was served by a short railway which, along with the mine is no more. All that remains is a spoil-heap on the North bank of the brook. The mine is one of the few known examples of a shallow drift to have been worked by a small number of men in the Sheffield area.

text: Historical evidence of shallow coal drift-mining of the Ringinglow seam which lies on top of the Chatsworth Grit has been found in the Barber Fields area. The workings extended beneath the watercourse. Stratigraphically this was the lowest coal seams ever worked in the Sheffield area. The mine was served by a short railway which, along with the mine is no more. All that remains is a spoil-heap on the North bank of the brook. The mine is one of the few known examples of a shallow drift to have been worked by a small number of men in the Sheffield area.

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answers: The magnetic north pole

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answers: Stratigraphically this was the lowest coal seams ever worked in the Sheffield area

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text: In 2002, Romano voiced Manfred aka Manny, a woolly mammoth in the first film Ice Age, then in 2006, Romano returned to voice Manny in the second film Ice Age: The Meltdown, next in 2009, Romano voiced the role of Manny in the third film Ice Age: Dawn of the Dinosaurs then in 2012, Romano voiced Manny in the fourth film Ice Age: Continental Drift, then in 2016, Romano voiced Manny in the fifth film Ice Age: Collision Course from the Blue Sky Studios' Ice Age film series.

text: In 2002, Romano voiced Manfred aka Manny, a woolly mammoth in the first film

text: Ice Age

text: , then in 2006, Romano returned to voice Manny in the second film

text: Ice Age: The Meltdown

text: , next in 2009, Romano voiced the role of Manny in the third film

text: Ice Age: Dawn of the Dinosaurs

text: then in 2012, Romano voiced Manny in the fourth film

text: Ice Age: Continental Drift

text: , then in 2016, Romano voiced Manny in the fifth film

text: Ice Age: Collision Course

text: from the Blue Sky Studios' Ice Age film series.

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answers: Continental Drift

text: Shira appears in Ice Age: Continental Drift as part of Gutt's crew, and is Captain Gutt's pawn. She is a dazzlingly beautiful, female saber-toothed cat and Diego's lover resembling a snow leopard. She makes her first appearance in Scrat's Continental Crack-up: Part 2 standing next to Captain Gutt, who is holding Scrat.

text: Shira appears in

text: Ice Age: Continental Drift

text: as part of Gutt's crew, and is Captain Gutt's pawn. She is a dazzlingly beautiful, female saber-toothed cat and Diego's lover resembling a

text: snow leopard

text: . She makes her first appearance in

text: Scrat's Continental Crack-up: Part 2

text: standing next to Captain Gutt, who is holding Scrat.

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answers: Continental Drift

text: In 1957 Blackett gave the presidential address (Technology and World Advancement) to the British Association meeting in Dublin. In 1965 he was invited to deliver the MacMillan Memorial Lecture to the Institution of Engineers and Shipbuilders in Scotland. He chose the subject "Continental Drift".

text: In 1957 Blackett gave the presidential address (Technology and World Advancement) to the

text: British Association

text: meeting in Dublin. In 1965 he was invited to deliver the MacMillan Memorial Lecture to the

entity_name: Institution of Engineers and Shipbuilders in Scotland

text: Institution of Engineers and Shipbuilders in Scotland

text: . He chose the subject "Continental Drift".

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answers: NDQ_003220

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answers: NDQ_003221

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answers: NDQ_003222

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answers: NDQ_003223

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answers: NDQ_003224

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answers: NDQ_003225

answers: Continental Drift

answers: NDQ_003226

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answers: NDQ_003227

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answers: NDQ_003228

answers: MacMillan Memorial Lecture

answers: NDQ_003230

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answers: NDQ_003231

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answers: NDQ_003233

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answers: NDQ_003236

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answers: NDQ_003237

answers: He chose the subject "Continental Drift"

answers: NDQ_003239

answers: Fossil records

answers: NDQ_003240

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answers: NDQ_003241

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answers: NDQ_003242

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answers: NDQ_003244

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answers: NDQ_003246

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answers: NDQ_003247

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answers: NDQ_003252

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answers: NDQ_003253

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answers: NDQ_003254

answers: It was widely accepted as soon as it was introduced

answers: NDQ_003255

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answers: NDQ_003256

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text: Alfred Wegener first thought of this idea by noticing that the different large landmasses of the Earth almost fit together like a jigsaw puzzle. The Continental shelf of the Americas fit closely to Africa and Europe, and Antarctica, Australia, India and Madagascar fitted next to the tip of Southern Africa. But Wegener only took action after reading a paper in 1911 and seeing that a flooded land-bridge contradicts isostasy. Wegener's main interest was meteorology, and he wanted to join the Denmark-Greenland expedition scheduled for mid-1912. He presented his Continental Drift hypothesis on 6 January 1912. He analyzed both sides of the Atlantic Ocean for rock type, geological structures and fossils. He noticed that there was a significant similarity between matching sides of the continents, especially in fossil plants.

text: Alfred Wegener first thought of this idea by noticing that the different large landmasses of the Earth almost fit together like a jigsaw puzzle. The

text: Continental shelf

text: of the Americas fit closely to Africa and Europe, and Antarctica, Australia, India and Madagascar fitted next to the tip of Southern Africa. But Wegener only took action after reading a paper in 1911 and seeing that a flooded land-bridge contradicts

text: isostasy

text: . Wegener's main interest was meteorology, and he wanted to join the Denmark-Greenland expedition scheduled for mid-1912. He presented his Continental Drift hypothesis on 6 January 1912. He analyzed both sides of the Atlantic Ocean for rock type, geological structures and fossils. He noticed that there was a significant similarity between matching sides of the continents, especially in

text: fossil plants

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answers: NDQ_003223

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answers: NDQ_003224

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answers: NDQ_003225

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answers: NDQ_003226

answers: Africa and Europe

answers: NDQ_003227

answers: there was a significant similarity between matching sides of the continents, especially in fossil plants

answers: NDQ_003228

answers: He analyzed both sides of the Atlantic Ocean for rock type, geological structures and fossils

answers: NDQ_003230

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answers: NDQ_003231

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answers: NDQ_003233

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answers: NDQ_003236

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answers: NDQ_003237

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answers: NDQ_003239

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answers: NDQ_003242

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answers: NDQ_003246

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answers: NDQ_003247

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answers: NDQ_003252

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answers: NDQ_003254

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text: The company was created in 2003 when the construction division of Statens Vegvesen was demerged to become a separate limited company that has to compete for each contract. During the summer of 2008 the company experienced a restructuring of the entire organizational structure. The company now consists of eight fully owned subsidiaries: Geo Survey, Eiendom (Property), Entreprenør (Entrepreneur), Asfalt (Asphalt), Stein (Rock), Elektro (Electro), Drift (Operation), and Verksted (Maintenance). The corporate HQ is positioned in Oslo. The subsidiaries are structured as own entities and  are limited companies.

text: The company was created in 2003 when the construction division of

text: Statens Vegvesen

text: was

text: demerged

text: to become a separate

text: limited company

text: that has to compete for each contract. During the summer of 2008 the company experienced a restructuring of the entire organizational structure. The company now consists of eight fully owned subsidiaries: Geo Survey, Eiendom (Property), Entreprenør (Entrepreneur), Asfalt (Asphalt), Stein (Rock), Elektro (Electro), Drift (Operation), and Verksted (Maintenance). The corporate HQ is positioned in Oslo. The subsidiaries are structured as own entities and  are limited companies.

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text: Many aspects of Gaga's career are referenced in the episode. "You're All My Little Monsters", a musical number specifically created for the episode, is a parody of Gaga's relationship with her devout "Little Monsters"—a phrase Gaga uses to refer to her fans. To Spin columnist Devon Maloney, the song was ultimately an overtly cartoonized version of her single "Born This Way" (2011) that embraces the "freakiness" of Springfield. Several of Gaga's outfits and looks emulate several iconic costumes the singer had previously worn, such as the "Living Dress" and pyrotechnic leotard she wore during her endeavors on The Monster Ball Tour, as well as her wardrobe at the 53rd Grammy Awards. One in particular, a dress consisting of pork chops, is a parody of the singer's meat dress, which she wore at the 2010 MTV Video Music Awards. During the credits of "Lisa Goes Gaga", main character Homer Simpson performs a rendition of "Poker Face" (2009). At the end of the episode, a title card promotes the Maggie-starring short film The Longest Daycare, which showed before the animated film Ice Age: Continental Drift (2012).

text: Many aspects of Gaga's career are referenced in the episode. "You're All My Little Monsters", a musical number specifically created for the episode, is a parody of Gaga's relationship with her devout "Little Monsters"—a phrase Gaga uses to refer to her fans. To

text: Spin

text: columnist Devon Maloney, the song was ultimately an overtly cartoonized version of her single "

text: Born This Way

text: " (2011) that embraces the "freakiness" of Springfield. Several of Gaga's outfits and looks emulate several iconic costumes the singer had previously worn, such as the "Living Dress" and pyrotechnic leotard she wore during her endeavors on

text: The Monster Ball Tour

text: , as well as her wardrobe at the

text: 53rd Grammy Awards

text: . One in particular, a dress consisting of

text: pork chops

text: , is a parody of the singer's meat dress, which she wore at the

text: 2010 MTV Video Music Awards

text: . During the credits of "Lisa Goes Gaga", main character

text: Homer Simpson

text: performs a rendition of "

text: Poker Face

text: " (2009). At the end of the episode, a title card promotes the

text: Maggie

text: -starring short film

text: The Longest Daycare

text: , which showed before the animated film

text: Ice Age: Continental Drift

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text: In October 2012, it was announced that a 3D computer-animated feature film titled The Peanuts Movie was released on November 6, 2015, coinciding with the 65th anniversary of the debut of the comic strip and the 50th anniversary of the television special, A Charlie Brown Christmas. Written by Charles Schulz's son, Craig, his grandson, Bryan, and Cornelius Uliano—who are also producing the film alongside Paul Feig—it was animated by 20th Century Fox's Blue Sky Studios, and directed by Steve Martino, the director of Horton Hears a Who! and Ice Age: Continental Drift. A trailer for the film was released on March 18, 2014. The same day, it was also announced that archive recordings of Bill Melendez would be used to make up Snoopy and Woodstock's dialogue.

text: In October 2012, it was announced that a 3D computer-animated feature film titled

text: The Peanuts Movie

text: was released on November 6, 2015, coinciding with the 65th anniversary of the debut of the comic strip and the 50th anniversary of the television special,

text: A Charlie Brown Christmas

text: . Written by Charles Schulz's son, Craig, his grandson, Bryan, and Cornelius Uliano—who are also producing the film alongside

text: Paul Feig

text: —it was animated by

text: 20th Century Fox

text: 's

text: Blue Sky Studios

text: , and directed by

text: Steve Martino

text: , the director of

text: Horton Hears a Who!

text: and

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text: In 2004, an exhibition of Central European Mesosoic reptiles—DinoPark—was opened in the central area of the zoo, becoming a major attraction for ZOO Bratislava. At the area of almost  DinoPark features life-sized sculptures of dinosaurs that are animated during the summer season. It also features a 3D cinema,

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answers: paleontological

answers: NDQ_003230

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answers: NDQ_003231

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answers: NDQ_003237

answers: fake fossils

answers: NDQ_003239

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answers: NDQ_003240

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answers: It also features a 3D cinema

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answers: fake fossils

answers: NDQ_003256

answers: Mesosoic

answers: NDQ_003257

answers: Pangaea

answers: NDQ_003258

answers: Mesosoic

text: The course of the upper Mississippi River is largely consequent upon glacial deposits. Its sources are in the morainic lakes in northern Minnesota. The drift deposits thereabouts are so heavy that the present divides between the drainage basins of Hudson Bay, Lake Superior and the Gulf of Mexico evidently stand in no very definite relation to the preglacial divides. The course of the Mississippi through Minnesota is largely guided by the form of the drift cover. Several rapids and the Saint Anthony Falls (determining the site of Minneapolis) are signs of immaturity, resulting from superposition through the drift on the under rock. Farther south, as far as the entrance of the Ohio River, the Mississippi follows a rock-walled valley 300 to 400 ft (90 to 120 m) deep, with a flood-plain 2 to 4 mi (3 to 7 km) wide. This valley seems to represent the path of an enlarged early-glacial Mississippi, when much precipitation that is today discharged to Hudson Bay and the Gulf of St Lawrence was delivered to the Gulf of Mexico, for the curves of the present river are of distinctly smaller radii than the curves of the valley. Lake Pepin (30 mi [50 km] below St. Paul), a picturesque expansion of the river across its flood-plain, is due to the aggradation of the valley floor where the Chippewa River, coming from the northeast, brought an overload of fluvio-glacial drift. Hence even the father of waters, like so many other rivers in the Northern states, owes many of its features more or less directly to glacial action.

text: The course of the upper

text: Mississippi River

text: is largely consequent upon glacial deposits. Its sources are in the morainic lakes in northern

text: Minnesota

text: . The drift deposits thereabouts are so heavy that the present divides between the drainage basins of

text: Hudson Bay

text: Lake Superior

text: and the

text: Gulf of Mexico

text: evidently stand in no very definite relation to the preglacial divides. The course of the Mississippi through Minnesota is largely guided by the form of the drift cover. Several rapids and the

text: Saint Anthony Falls

text: (determining the site of

text: Minneapolis

text: ) are signs of immaturity, resulting from superposition through the drift on the under rock. Farther south, as far as the entrance of the

text: Ohio River

text: , the Mississippi follows a rock-walled valley 300 to 400 ft (90 to 120 m) deep, with a flood-plain 2 to 4 mi (3 to 7 km) wide. This valley seems to represent the path of an enlarged early-glacial Mississippi, when much precipitation that is today discharged to Hudson Bay and the Gulf of St Lawrence was delivered to the Gulf of Mexico, for the curves of the present river are of distinctly smaller

text: radii

text: than the curves of the valley.

text: Lake Pepin

text: (30 mi [50 km] below

text: St. Paul

text: ), a picturesque expansion of the river across its flood-plain, is due to the aggradation of the valley floor where the

text: Chippewa River

text: , coming from the northeast, brought an overload of fluvio-glacial drift. Hence even the father of waters, like so many other rivers in the Northern states, owes many of its features more or less directly to glacial action.

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answers: NDQ_003222

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answers: NDQ_003223

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answers: NDQ_003224

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answers: 4

answers: NDQ_003226

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answers: NDQ_003227

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answers: NDQ_003256

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answers: NDQ_003219

answers: glacial action

answers: NDQ_003220

answers: Gulf of St Lawrence

answers: NDQ_003221

answers: 18th century

answers: NDQ_003222

answers: the present divides between the drainage basins of Hudson Bay, Lake Superior and the Gulf of Mexico evidently stand in no very definite relation to the preglacial divides

answers: NDQ_003223

answers: preglacial

answers: NDQ_003224

answers: preglacial divides

answers: NDQ_003225

answers: glacial action

answers: NDQ_003226

answers: the Northern states

answers: NDQ_003227

answers: The course of the upper Mississippi River is largely consequent upon glacial deposits

answers: NDQ_003228

answers: course of the upper Mississippi River

answers: NDQ_003230

answers: Mexico

answers: NDQ_003231

answers: magnetic field

answers: NDQ_003233

answers: The present divides between the drainage basins of Hudson Bay, Lake Superior and the Gulf of Mexico evidently stand in no very definite relation to the preglacial divides

answers: NDQ_003236

answers: glacial deposits

answers: NDQ_003237

answers: The course of the upper Mississippi River is largely consequent upon glacial deposits

answers: NDQ_003239

answers: Lake Pepin

answers: NDQ_003240

answers: North America

answers: NDQ_003241

answers: Minnesota

answers: NDQ_003242

answers: preglacial

answers: NDQ_003244

answers: Lake Pepin

answers: NDQ_003246

answers: The course of the upper Mississippi River

answers: NDQ_003247

answers: The course of the upper Mississippi River is largely consequent upon glacial deposits

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: The course of the upper Mississippi River is largely consequent upon glacial deposits

answers: NDQ_003254

answers: Its sources are in the morainic lakes in northern Minnesota

answers: NDQ_003255

answers: The course of the upper Mississippi River is largely consequent upon glacial deposits

answers: NDQ_003256

answers: The course of the upper Mississippi River

answers: NDQ_003257

answers: Pangaea

answers: NDQ_003258

answers: Fluvio-glacial

text: Wine regions with continental climates are characterised by the very marked seasonal changes that occur throughout the growing season, with hot temperatures during the summer season and winters cold enough for periodic ice and snow. This is generally described as having a high degree of continentality. Regions with this type of climate are often found inland on continents without a significant body of water, such as an inland sea, that can moderate their temperatures. Often during the growing season, continental climates will have wide diurnal temperature variations with very warm temperatures during the day that drop drastically at night. During the winter and early spring months, frost and hail can be viticultural hazards. Depending on the particular macroclimate of the region, irrigation may be needed to supplement seasonal rainfall. These many climatic influences contribute to the wide vintage variation that is often typical of continental climates such as Burgundy.

text: Wine regions with

text: continental climate

text: s are characterised by the very marked seasonal changes that occur throughout the growing season, with hot temperatures during the summer season and winters cold enough for periodic ice and snow. This is generally described as having a high degree of

text: continentality

text: . Regions with this type of climate are often found inland on

text: continents

text: without a significant body of water, such as an

text: inland sea

text: , that can moderate their temperatures. Often during the growing season, continental climates will have wide

text: diurnal temperature variations

text: with very warm temperatures during the day that drop drastically at night. During the winter and early spring months,

text: frost

text: and

text: hail

text: can be viticultural hazards. Depending on the particular macroclimate of the region, irrigation may be needed to supplement seasonal rainfall. These many climatic influences contribute to the wide

text: vintage

text: variation that is often typical of continental climates such as

text: Burgundy

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answers: NDQ_003219

answers: 0

answers: NDQ_003220

answers: 0

answers: NDQ_003221

answers: 0

answers: NDQ_003222

answers: 0

answers: NDQ_003223

answers: 0

answers: NDQ_003224

answers: 0

answers: NDQ_003225

answers: 0

answers: NDQ_003226

answers: 0

answers: NDQ_003227

answers: 0

answers: NDQ_003228

answers: 0

answers: NDQ_003230

answers: 0

answers: NDQ_003231

answers: 0

answers: NDQ_003233

answers: 0

answers: NDQ_003236

answers: 0

answers: NDQ_003237

answers: 0

answers: NDQ_003239

answers: 0

answers: NDQ_003240

answers: 0

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answers: 0

answers: NDQ_003242

answers: 0

answers: NDQ_003244

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answers: NDQ_003252

answers: 4

answers: NDQ_003253

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answers: NDQ_003256

answers: 0

answers: NDQ_003257

answers: 0

answers: NDQ_003258

answers: 0

answers: NDQ_003219

answers: continental climates

answers: NDQ_003220

answers: unanswerable

answers: NDQ_003221

answers: 18th century

answers: NDQ_003222

answers: continents without a significant body of water

answers: NDQ_003223

answers: continental climates

answers: NDQ_003224

answers: Burgundy

answers: NDQ_003225

answers: continentality

answers: NDQ_003226

answers: Burgundy

answers: NDQ_003227

answers: inland sea, that can moderate their temperatures

answers: NDQ_003228

answers: continental climates

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: macroclimate

answers: NDQ_003233

answers: Burgundy

answers: NDQ_003236

answers: continents

answers: NDQ_003237

answers: inland sea, that can moderate their temperatures

answers: NDQ_003239

answers: regions with this type of climate are often found inland

answers: NDQ_003240

answers: continentality

answers: NDQ_003241

answers: continents

answers: NDQ_003242

answers: continentality

answers: NDQ_003244

answers: continents without a significant body of water

answers: NDQ_003246

answers: continents

answers: NDQ_003247

answers: inland on continents without a significant body of water, such as an inland sea

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: inland sea

answers: NDQ_003254

answers: It was widely accepted as soon as it was introduced

answers: NDQ_003255

answers: inland sea

answers: NDQ_003256

answers: unanswerable

answers: NDQ_003257

answers: Pangaea

answers: NDQ_003258

answers: without a significant body of water

text: The input offset voltage of amplifiers becomes important when trying to amplify small signals with very high gain. Because this technique creates a very low input offset voltage amplifier, and because this input offset voltage does not change much with time and temperature, these techniques are also called "zero-drift" amplifiers (because there is no drift in input offset voltage with time and temperature). Related techniques that also give these zero-drift advantages are auto-zero and chopper-stabilized amplifiers.

text: The

text: input offset voltage

text: of amplifiers becomes important when trying to amplify small signals with very high gain. Because this technique creates a very low input offset voltage amplifier, and because this input offset voltage does not change much with time and temperature, these techniques are also called "zero-drift" amplifiers (because there is no drift in input offset voltage with time and temperature). Related techniques that also give these zero-drift advantages are auto-zero and chopper-stabilized amplifiers.

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answers: 0

answers: NDQ_003219

answers: zero-drift

answers: NDQ_003220

answers: unanswerable

answers: NDQ_003221

answers: late 19th century

answers: NDQ_003222

answers: zero-drift

answers: NDQ_003223

answers: zero-drift

answers: NDQ_003224

answers: zero-drift

answers: NDQ_003225

answers: zero-drift

answers: NDQ_003226

answers: Antarctica

answers: NDQ_003227

answers: zero-drift

answers: NDQ_003228

answers: zero-drift

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: zero-drift

answers: NDQ_003233

answers: zero-drift

answers: NDQ_003236

answers: zero-drift

answers: NDQ_003237

answers: zero-drift

answers: NDQ_003239

answers: zero-drift

answers: NDQ_003240

answers: zero-drift

answers: NDQ_003241

answers: no

answers: NDQ_003242

answers: zero-drift

answers: NDQ_003244

answers: zero-drift

answers: NDQ_003246

answers: zero-drift

answers: NDQ_003247

answers: zero-drift

answers: NDQ_003252

answers: zero-drift

answers: NDQ_003253

answers: zero-drift

answers: NDQ_003254

answers: zero-drift

answers: NDQ_003255

answers: zero-drift

answers: NDQ_003256

answers: zero-drift

answers: NDQ_003257

answers: zero-drift

answers: NDQ_003258

answers: zero-drift

text: Geological occurrence, structure, mineralogical constitution—the hitherto accepted criteria for the discrimination of rock species—were relegated to the background. The completed rock analysis is first to be interpreted in terms of the rock-forming minerals which might be expected to be formed when the magma crystallizes, e.g., quartz feldspars, olivine, akermannite, Feldspathoids, magnetite, corundum, and so on, and the rocks are divided into groups strictly according to the relative proportion of these minerals to one another.

text: Geological occurrence, structure, mineralogical constitution—the hitherto accepted criteria for the discrimination of rock species—were relegated to the background. The completed rock analysis is first to be interpreted in terms of the rock-forming minerals which might be expected to be formed when the magma crystallizes, e.g., quartz feldspars,

text: olivine

text: , akermannite,

text: Feldspathoid

text: s,

text: magnetite

text: corundum

text: , and so on, and the rocks are divided into groups strictly according to the relative proportion of these minerals to one another.

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answers: geological occurrence, structure, mineralogical constitution

text: The Continental Can Company, founded in 1904, was taking bids for a new addition on their factory in 1913. The new structure was two-stories and measured  by . In 1976, CCC changed its name to the Continental Group, a conglomerate with operations in many countries, but kept Continental Can as its packaging unit within Continental Group. In 1987, the remnants of Continental Can Company became part of the United States Can Company, a subsidiary of Inter-American Packaging. Continental Group was dismantled in 1991.

text: The

text: Continental Can Company

text: , founded in 1904, was taking bids for a new addition on their factory in 1913. The new structure was two-stories and measured  by . In 1976, CCC changed its name to the Continental Group, a conglomerate with operations in many countries, but kept Continental Can as its packaging unit within Continental Group. In 1987, the remnants of Continental Can Company became part of the United States Can Company, a subsidiary of Inter-American Packaging. Continental Group was dismantled in 1991.

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answers: The Continental Group

text: Climate: Tianjin Port is at the northern limit of the continental monsoon climate area. Specifically, it belongs to the temperate semi-humid continental climate type (Köppen Dwa), with a short rainy season in the summer, large seasonal differences in temperature, and large variation in weather year to year. Annual average temperature is . The hottest months are July and August (maximum temperature recorded was  on 24 July 1955), and the coldest is January (minimum temperature recorded was  on 17 January 1953). The average relative humidity is 65%, with a maximum of 100% recorded in summer, and a minimum of 3% recorded in winter.

text: Climate: Tianjin Port is at the northern limit of the continental monsoon climate area. Specifically, it belongs to the

text: temperate semi-humid continental

text: climate type (

text: Köppen

text: Dwa), with a short rainy season in the summer, large seasonal differences in temperature, and large variation in weather year to year. Annual average temperature is . The hottest months are July and August (maximum temperature recorded was  on 24 July 1955), and the coldest is January (minimum temperature recorded was  on 17 January 1953). The average relative humidity is 65%, with a maximum of 100% recorded in summer, and a minimum of 3% recorded in winter.

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answers: Atlantic Ocean

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answers: 1950s

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answers: Tianjin Port

answers: NDQ_003223

answers: Tianjin

answers: NDQ_003224

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answers: NDQ_003225

answers: Köppen Dwa

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answers: climate type

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answers: Köppen Dwa

answers: NDQ_003230

answers: Tianjin

answers: NDQ_003231

answers: conduction

answers: NDQ_003233

answers: The average relative humidity is 65%

answers: NDQ_003236

answers: continental monsoon climate

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answers: Koppen Dwa

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text: The Köppen Climate Classification subtype for this climate is "Dfb"  (Warm Summer Continental Climate).

text: The

text: Köppen Climate Classification

text: subtype for this climate is "

text: Dfb

text: "  (Warm Summer Continental Climate).

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answers: Dfb

answers: NDQ_003220

answers: continental climate

answers: NDQ_003221

answers: 18th century

answers: NDQ_003222

answers: Köppen Climate Classification

answers: NDQ_003223

answers: Dfb

answers: NDQ_003224

answers: Dfb

answers: NDQ_003225

answers: Dfb

answers: NDQ_003226

answers: Europe

answers: NDQ_003227

answers: Warm Summer Continental Climate

answers: NDQ_003228

answers: Köppen

answers: NDQ_003230

answers: South America was attached to present-day

answers: NDQ_003231

answers: Dfb

answers: NDQ_003233

answers: Dfb (Warm Summer Continental Climate)

answers: NDQ_003236

answers: continental climate

answers: NDQ_003237

answers: Dfb

answers: NDQ_003239

answers: Dfb

answers: NDQ_003240

answers: continental climate

answers: NDQ_003241

answers: The magnetic north pole and geographic north pole are in different locations.

answers: NDQ_003242

answers: Köppen

answers: NDQ_003244

answers: Dfb

answers: NDQ_003246

answers: continental climate

answers: NDQ_003247

answers: Dfb

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: Dfb

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answers: Dfb

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answers: Dfb

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answers: Dfb

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answers: Dfb

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answers: Dfb

text: Mawson's ideas of global glaciation, however, were based on the mistaken assumption that the geographic position of Australia, and that of other continents where low-latitude glacial deposits are found, has remained constant through time. With the advancement of the continental drift hypothesis, and eventually plate tectonic theory, came an easier explanation for the glaciogenic sediments — they were deposited at a point in time when the continents were at higher latitudes.

text: Mawson's ideas of global glaciation, however, were based on the mistaken assumption that the geographic position of Australia, and that of other continents where low-latitude glacial deposits are found, has remained constant through time. With the advancement of the

text: continental drift

text: hypothesis, and eventually

text: plate tectonic

text: theory, came an easier explanation for the glaciogenic sediments — they were deposited at a point in time when the continents were at higher latitudes.

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answers: 4

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answers: 2

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answers: NDQ_003219

answers: continental drift hypothesis

answers: NDQ_003220

answers: are found

answers: NDQ_003221

answers: continental drift hypothesis

answers: NDQ_003222

answers: the geographic position of Australia

answers: NDQ_003223

answers: higher latitudes

answers: NDQ_003224

answers: glaciogenic sediments

answers: NDQ_003225

answers: continental drift hypothesis

answers: NDQ_003226

answers: Australia

answers: NDQ_003227

answers: an easier explanation for the glaciogenic sediments

answers: NDQ_003228

answers: an easier explanation for the glaciogenic sediments

answers: NDQ_003230

answers: Australia

answers: NDQ_003231

answers: latitude

answers: NDQ_003233

answers: plate tectonic theory

answers: NDQ_003236

answers: continental drift

answers: NDQ_003237

answers: low-latitude glacial deposits

answers: NDQ_003239

answers: low-latitude glacial deposits

answers: NDQ_003240

answers: Mawson

answers: NDQ_003241

answers: no

answers: NDQ_003242

answers: continental drift hypothesis

answers: NDQ_003244

answers: continents

answers: NDQ_003246

answers: continents at higher latitudes

answers: NDQ_003247

answers: low-latitude

answers: NDQ_003252

answers: continental drift hypothesis

answers: NDQ_003253

answers: continents were at higher latitudes

answers: NDQ_003254

answers: It was widely accepted as soon as it was introduced

answers: NDQ_003255

answers: plate tectonic theory

answers: NDQ_003256

answers: The advancement of the continental drift hypothesis

answers: NDQ_003257

answers: continents were at higher latitudes

answers: NDQ_003258

answers: continental drift hypothesis

text: Humid continental climates tend to be found between latitudes 37° N and 60° N, within the central and northeastern portions of North America, Europe, and Asia. They are much less commonly found in the Southern Hemisphere due to the larger ocean area at that latitude and the consequent greater maritime moderation. In the Northern Hemisphere some of the humid continental climates, typically in Scandinavia, Nova Scotia, and Newfoundland are heavily maritime-influenced, with relatively cool summers and winters being just below the freezing mark. More extreme humid continental climates found in southern Siberia and the American Midwest combine hotter summer maxima and colder winters than the marine-based variety. In some areas there are both strong subtropical and subarctic air mass influences depending on season, like the humid and hot summers and the frigid winters of Milwaukee, Wisconsin in the Upper Midwest of the United States.

text: Humid continental climates tend to be found between latitudes 37° N and 60° N, within the central and northeastern portions of

text: North America

text: Europe

text: , and

text: Asia

text: . They are much less commonly found in the

text: Southern Hemisphere

text: due to the larger ocean area at that latitude and the consequent greater maritime moderation. In the Northern Hemisphere some of the humid continental climates, typically in

text: Scandinavia

text: Nova Scotia

text: , and

text: Newfoundland

text: are heavily maritime-influenced, with relatively cool summers and winters being just below the freezing mark. More extreme humid continental climates found in southern

text: Siberia

text: and the

text: American Midwest

text: combine hotter summer maxima and colder winters than the marine-based variety. In some areas there are both strong subtropical and subarctic air mass influences depending on season, like the humid and hot summers and the frigid winters of

text: Milwaukee

text: Wisconsin

text: in the Upper Midwest of the United States.

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answers: NDQ_003219

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answers: NDQ_003221

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answers: NDQ_003222

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answers: NDQ_003223

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answers: NDQ_003224

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answers: NDQ_003225

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answers: NDQ_003226

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answers: NDQ_003227

answers: 0

answers: NDQ_003228

answers: 0

answers: NDQ_003230

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answers: NDQ_003231

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answers: NDQ_003233

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answers: NDQ_003236

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answers: NDQ_003237

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answers: NDQ_003239

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answers: NDQ_003240

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answers: NDQ_003241

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answers: NDQ_003242

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answers: NDQ_003244

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answers: NDQ_003246

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answers: NDQ_003247

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answers: NDQ_003252

answers: 4

answers: NDQ_003253

answers: 0

answers: NDQ_003254

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answers: NDQ_003255

answers: 4

answers: NDQ_003256

answers: 0

answers: NDQ_003257

answers: 0

answers: NDQ_003258

answers: 0

answers: NDQ_003219

answers: latitudes 37° N and 60° N

answers: NDQ_003220

answers: Nova Scotia

answers: NDQ_003221

answers: 18th century

answers: NDQ_003222

answers: Humid continental climates

answers: NDQ_003223

answers: Siberia

answers: NDQ_003224

answers: Siberia

answers: NDQ_003225

answers: humid continental climates

answers: NDQ_003226

answers: Europe

answers: NDQ_003227

answers: They are much less commonly found in the Southern Hemisphere

answers: NDQ_003228

answers: Humid continental climates

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: subarctic

answers: NDQ_003233

answers: Humid continental climates

answers: NDQ_003236

answers: The Southern Hemisphere

answers: NDQ_003237

answers: Humid continental climates

answers: NDQ_003239

answers: Humid continental climates

answers: NDQ_003240

answers: Asia

answers: NDQ_003241

answers: North America

answers: NDQ_003242

answers: continental drift

answers: NDQ_003244

answers: subarctic

answers: NDQ_003246

answers: Asia

answers: NDQ_003247

answers: between latitudes 37° N and 60° N

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: Europe, and Asia

answers: NDQ_003254

answers: Humid continental climates

answers: NDQ_003255

answers: Humid continental climates

answers: NDQ_003256

answers: North America, Europe, and Asia

answers: NDQ_003257

answers: Pangaea

answers: NDQ_003258

answers: continental climates

text: The Mark I Ford Escort was introduced in the United Kingdom at the end of 1967, making its show debut at Brussels Motor Show in January 1968. It replaced the successful, long-running Anglia. The car was presented in continental Europe as a product of Ford's European operation. Escort production commenced at the Halewood plant in England during the closing months of 1967, and for left hand drive markets during September 1968 at the Ford plant in Genk. Initially the continental Escorts differed slightly from the UK built ones under the skin. The front suspension and steering gear were differently configured and the brakes were fitted with dual hydraulic circuits; also the wheels fitted on the Genk-built Escorts had wider rims. At the beginning of 1970, continental European production transferred to a new plant on the edge of Saarlouis, West Germany.

text: The Mark I Ford Escort was introduced in the United Kingdom at the end of 1967, making its show debut at

text: Brussels Motor Show

text: in January 1968. It replaced the successful, long-running

text: Anglia

text: . The car was presented in continental Europe as a product of Ford's European operation. Escort production commenced at the

text: Halewood plant

text: in England during the closing months of 1967, and for left hand drive markets during September 1968 at the Ford plant in

text: Genk

text: . Initially the continental Escorts differed slightly from the UK built ones under the skin. The front suspension and steering gear were differently configured and the brakes were fitted with dual hydraulic circuits; also the wheels fitted on the Genk-built Escorts had wider rims. At the beginning of 1970, continental European production transferred to a

text: new plant

text: on the edge of

text: Saarlouis

text: , West Germany.

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text: Later, in 1940, the South Dakota School of Mines and Technology collaborated with National Geographic on an expedition into the badlands. They uncovered tons of fossils from at least 175 different species of Oligocene life. The fossils were taken to the South Dakota School of Mines in Rapid City. Among the mammal discoveries were the remains of rhinoceroses, tapirs, three-toed horses, pig-like animals, and rodents. The team also uncovered some bird fossils, which are very rare. One of these was a fossil egg, which author Marian Murray has called "[t]he best find" of the entire expedition. Only a few plant specimens were discovered, but these included fossil hackberry seeds and petrified wood. Some of the fossils were so precariously located that the excavators had to use block and tackle to lower the fossils down from the tops of "slender pinnacles". The fossils were preserved in channel sandstones that had received little scientific attention prior to the expedition. In June 1947 the South Dakota School of mines sent another expedition into the Badlands. They uncovered a wide variety of fossils preserved in the Oligocene White River Formation. Among the creatures discovered were rhinoceroses, saber teeth, giant pig-like animals, Protoceros, tapirs, horses and more. In 1990, Sue Hendrickson discovered a new specimen of Tyrannosaurus rex that would later be nicknamed in her honor. The specimen made headlines when a dispute over ownership rights raged for more than five years. "Sue" was determined to rightfully belong to the owner of the property it was found on. The rancher put the specimen up for auction and was purchased by the Chicago Field Museum for 8.36 million dollars.

text: Later, in 1940, the South Dakota School of Mines and Technology collaborated with

text: National Geographic

text: on an expedition into the badlands. They uncovered tons of fossils from at least 175 different species of Oligocene life. The fossils were taken to the South Dakota School of Mines in

text: Rapid City

text: . Among the mammal discoveries were the remains of

text: rhinoceroses

text: tapirs

text: , three-toed

text: horses

text: , pig-like animals, and

text: rodents

text: . The team also uncovered some

text: bird

text: fossils, which are very rare. One of these was a

text: fossil egg

text: , which author Marian Murray has called "[t]he best find" of the entire expedition. Only a few plant specimens were discovered, but these included fossil

text: hackberry

text: seeds and

text: petrified wood

text: . Some of the fossils were so precariously located that the excavators had to use block and tackle to lower the fossils down from the tops of "slender pinnacles". The fossils were preserved in channel sandstones that had received little scientific attention prior to the expedition. In June 1947 the South Dakota School of mines sent another expedition into the Badlands. They uncovered a wide variety of fossils preserved in the Oligocene White River Formation. Among the creatures discovered were rhinoceroses,

text: saber teeth

text: , giant pig-like animals,

text: Protoceros

text: , tapirs, horses and more. In 1990, Sue Hendrickson discovered a new specimen of Tyrannosaurus rex that would later be nicknamed in her honor. The specimen made headlines when a dispute over ownership rights raged for more than five years. "Sue" was determined to rightfully belong to the owner of the property it was found on. The rancher put the specimen up for auction and was purchased by the Chicago Field Museum for 8.36 million dollars.

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answers: Oligocene life

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answers: Badlands

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answers: 1940

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answers: fossils were preserved in channel sandstones

answers: NDQ_003223

answers: Oligocene

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answers: Oligocene

answers: NDQ_003225

answers: "slender pinnacles"

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answers: the Badlands

answers: NDQ_003227

answers: fossils were preserved in channel sandstones that had received little scientific attention prior to the expedition

answers: NDQ_003228

answers: South Dakota School of Mines

answers: NDQ_003230

answers: North America

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answers: pinnacles

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answers: The fossils were preserved in channel sandstones that had received little scientific attention prior to the expedition

answers: NDQ_003236

answers: slender pinnacles

answers: NDQ_003237

answers: fossil egg

answers: NDQ_003239

answers: fossils from at least 175 different species of Oligocene life

answers: NDQ_003240

answers: South Dakota

answers: NDQ_003241

answers: The Chicago Field Museum

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answers: continental drift

answers: NDQ_003244

answers: unanswerable

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answers: South Dakota

answers: NDQ_003247

answers: fossils from at least 175 different species of Oligocene life

answers: NDQ_003252

answers: plate tectonics

answers: NDQ_003253

answers: South Dakota School of Mines

answers: NDQ_003254

answers: It was widely accepted as soon as it was introduced

answers: NDQ_003255

answers: The fossils were preserved in channel sandstones

answers: NDQ_003256

answers: Oligocene

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answers: Pangaea

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answers: The fossils were preserved in channel sandstones that had received little scientific attention prior to the expedition

text: Under recent renovation, the Conservatory currently houses an exhibit on Living Fossils showing many types of prehistoric plant life, fossilized foliage, mosses, and ferns. Known mostly for its remarkable glass dome, the conservatory also boasts a tropical rainforest supported by a climate control system and a waterfall and cave system that house some animals indigenous to more tropical areas of the world. The Botanical Garden is currently securing funding to expand the Conservatory and ad d additional exhibits and planting space such as a desert exhibit, a mountain exhibit, and a section to showcase the garden’s orchids.

text: Under recent renovation, the Conservatory currently houses an exhibit on Living Fossils showing many types of prehistoric plant life, fossilized foliage, mosses, and ferns. Known mostly for its remarkable glass dome, the conservatory also boasts a tropical rainforest supported by a climate control system and a waterfall and cave system that house some animals indigenous to more tropical areas of the world. The Botanical Garden is currently securing funding to expand the Conservatory and ad d additional exhibits and planting space such as a desert exhibit, a mountain exhibit, and a section to showcase the garden’s orchids.

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answers: Living Fossils

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answers: Living Fossils

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text: Bauschinger was dissertation advisor for Alfred Wegener's 1905 doctral thesis in astronomy. Wegener, in 1910, proposed a system of continental drift which was eventually modified and generally accepted as plate tectonics.

text: Bauschinger was dissertation advisor for

text: Alfred Wegener's

text: 1905 doctral thesis in astronomy. Wegener, in 1910, proposed a system of

text: continental drift

text: which was eventually modified and generally accepted as

text: plate tectonics

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answers: was eventually modified and generally accepted

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answers: Wegener, in 1910, proposed a system of continental drift

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text: Ice Age: Continental Drift was released on DVD, Blu-ray, and Blu-ray 3D on December 11, 2012.

text: Ice Age: Continental Drift was released on DVD, Blu-ray, and Blu-ray 3D on December 11, 2012.

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answers: Ice Age: Continental Drift

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answers: Ice Age: Continental Drift was released on DVD, Blu-ray 3D on December 11, 2012.

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answers: Fossil records across continents was evidence for continental drift.

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answers: Ice Age: Continental Drift

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answers: The theory of plate tectonics was developed before the idea of continental drift

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answers: It was widely accepted as soon as it was introduced.

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answers: Wegener and his supporters provided a lot of evidence

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answers: Wegener developed a theory to explain how continents can drift.

text: The features that became Niagara Falls were created by the Wisconsin glaciation about 10,000 years ago. The same forces also created the North American Great Lakes and the Niagara River. All were dug by a continental ice sheet that drove through the area, deepening some river channels to form lakes, and damming others with debris. Scientists argue there is an old valley, buried by glacial drift, at the approximate location of the present Welland Canal.

text: The features that became Niagara Falls were created by the

text: Wisconsin glaciation

text: about 10,000 years ago. The same forces also created the North American

text: Great Lakes

text: and the Niagara River. All were dug by a continental

text: ice sheet

text: that drove through the area, deepening some river channels to form lakes, and damming others with debris. Scientists argue there is an old valley, buried by

text: glacial drift

text: , at the approximate location of the present

text: Welland Canal

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answers: It was widely accepted as soon as it was introduced

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answers: Wegener and his supporters provided a lot of evidence

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answers: North American Great Lakes

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text: Gordon James Fraser MacDonald (July 30, 1929 – May 14, 2002) was an American geophysicist and environmental scientist, best known for his principled skepticism regarding continental drift (now called plate tectonics), involvement in the development of the McNamara Line electronic defense barrier during the Vietnam War, and early research and advocacy on manmade global climate change.  MacDonald was admired for his creative mind, and his ability to connect scientific issues and matters of public policy.

text: Gordon James Fraser MacDonald (July 30, 1929 – May 14, 2002) was an American geophysicist and environmental scientist, best known for his principled skepticism regarding

text: continental drift

text: (now called

text: plate tectonics

text: ), involvement in the development of the

text: McNamara Line

text: electronic defense barrier during the

text: Vietnam War

text: , and early research and advocacy on manmade

text: global climate change

text: .  MacDonald was admired for his creative mind, and his ability to connect scientific issues and matters of public policy.

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text: La Siberia lies between two climate zones - a continental climate to the north and a Mediterranean climate to the south - making this area a transition zone. Most of the area lies in the Mediterranean zone, but the far north has a continental climate. Summers are long and hot while winters are short and moderately cold.

text: La Siberia lies between two climate zones - a

text: continental climate

text: to the north and a

text: Mediterranean climate

text: to the south - making this area a transition zone. Most of the area lies in the Mediterranean zone, but the far north has a continental climate. Summers are long and hot while winters are short and moderately cold.

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answers: NDQ_003219

answers: continental climate

answers: NDQ_003220

answers: Mediterranean

answers: NDQ_003221

answers: late 19th century

answers: NDQ_003222

answers: continental climate

answers: NDQ_003223

answers: La Siberia

answers: NDQ_003224

answers: Siberia

answers: NDQ_003225

answers: a transition zone

answers: NDQ_003226

answers: Mediterranean

answers: NDQ_003227

answers: continental climate

answers: NDQ_003228

answers: continental climate

answers: NDQ_003230

answers: Europe

answers: NDQ_003231

answers: zone

answers: NDQ_003233

answers: La Siberia lies between two climate zones

answers: NDQ_003236

answers: continents move over Earths surface

answers: NDQ_003237

answers: La Siberia lies between two climate zones

answers: NDQ_003239

answers: continental drift

answers: NDQ_003240

answers: North America

answers: NDQ_003241

answers: La Siberia

answers: NDQ_003242

answers: transition zone

answers: NDQ_003244

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answers: NDQ_003246

answers: La Siberia

answers: NDQ_003247

answers: La Siberia

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: La Siberia lies between two climate zones

answers: NDQ_003254

answers: It was widely accepted as soon as it was introduced

answers: NDQ_003255

answers: Wegener and his supporters

answers: NDQ_003256

answers: Mediterranean zone

answers: NDQ_003257

answers: Pangaea

answers: NDQ_003258

answers: continental climate

text: Sea level can also change (primarily due to the formation or melting of continental ice sheets), and raise or lower the final base level for coastal rivers. Along the east coast of North America, river valleys extend out onto the continental shelf, indicating a time when erosion was possible due to the lower base level of a lower sea level in the past. Today many of these same rivers end in bays, indicating that sea level has risen in recent geologic time. This is referred to as a drowned coastline.

text: Sea level can also change (primarily due to the formation or melting of continental ice sheets), and raise or lower the final base level for coastal rivers. Along the east coast of

text: North America

text: , river valleys extend out onto the

text: continental shelf

text: , indicating a time when erosion was possible due to the lower base level of a lower sea level in the past. Today many of these same rivers end in

text: bay

text: s, indicating that sea level has risen in recent geologic time. This is referred to as a

text: drowned coastline

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answers: NDQ_003219

answers: sea level can change

answers: NDQ_003220

answers: coast of North America

answers: NDQ_003221

answers: geologic time

answers: NDQ_003222

answers: a drowned coastline

answers: NDQ_003223

answers: a lower sea level

answers: NDQ_003224

answers: river valleys

answers: NDQ_003225

answers: drowned coastline

answers: NDQ_003226

answers: continental ice sheets

answers: NDQ_003227

answers: sea level has risen in recent geologic time

answers: NDQ_003228

answers: Sea level can also change

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: base

answers: NDQ_003233

answers: river valleys extend out onto the continental shelf

answers: NDQ_003236

answers: Sea level can also change

answers: NDQ_003237

answers: river valleys extend out onto the continental shelf

answers: NDQ_003239

answers: river valleys extend out onto the continental shelf

answers: NDQ_003240

answers: North America

answers: NDQ_003241

answers: The east coast of North America

answers: NDQ_003242

answers: continental shelf

answers: NDQ_003244

answers: Along the east coast of North America

answers: NDQ_003246

answers: North America

answers: NDQ_003247

answers: river valleys extend out onto the continental shelf

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: The east coast of North America

answers: NDQ_003254

answers: It was widely accepted

answers: NDQ_003255

answers: sea level has risen in recent geologic time

answers: NDQ_003256

answers: Along the east coast of North America

answers: NDQ_003257

answers: Sea level has risen in recent geologic time

answers: NDQ_003258

answers: Sea level can also change

text: Many drift drivers will utilise the feint or weight transfer drift on track, in order to send the rear of their car into a more accentuated drift where the track width allows them. In most situations, this is preferable to drivers of lower powered cars, who cannot induce a drift with engine power alone, but it is also useful to drivers of turbo charged cars, when they find that their car is not "on boost". Many Japanese based vehicles use smaller capacity engines with larger turbos, so can "fall" off the power band created by the forced induction. The alternative methods to create power pre-corner include the feint drift incorporated with a "clutch kick", which starts the weight transfer, but allow the engine to free-rev and create boost pressure in the turbo to create more power to break the traction of the rear wheels when the clutch re-engages on the drivetrain with the car unsettled.

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answers: 0

answers: tqa2:L_0076/T_0763/7a7192cbfb0cdb83fb089d3c4f8ea239

answers: 0

answers: NDQ_003219

answers: 0

answers: NDQ_003220

answers: 0

answers: NDQ_003221

answers: 0

answers: NDQ_003222

answers: 0

answers: NDQ_003223

answers: 0

answers: NDQ_003224

answers: 0

answers: NDQ_003225

answers: 0

answers: NDQ_003226

answers: 0

answers: NDQ_003227

answers: 0

answers: NDQ_003228

answers: 0

answers: NDQ_003230

answers: 0

answers: NDQ_003231

answers: 0

answers: NDQ_003233

answers: 0

answers: NDQ_003236

answers: 0

answers: NDQ_003237

answers: 0

answers: NDQ_003239

answers: 0

answers: NDQ_003240

answers: 0

answers: NDQ_003241

answers: 0

answers: NDQ_003242

answers: 0

answers: NDQ_003244

answers: 0

answers: NDQ_003246

answers: 0

answers: NDQ_003247

answers: 0

answers: NDQ_003252

answers: 0

answers: NDQ_003253

answers: 0

answers: NDQ_003254

answers: 0

answers: NDQ_003255

answers: 0

answers: NDQ_003256

answers: 0

answers: NDQ_003257

answers: 0

answers: NDQ_003258

answers: 0

answers: NDQ_003219

answers: weight transfer

answers: NDQ_003220

answers: unanswerable

answers: NDQ_003221

answers: Japanese

answers: NDQ_003222

answers: weight transfer

answers: NDQ_003223

answers: Japan

answers: NDQ_003224

answers: Ancient

answers: NDQ_003225

answers: the feint

answers: NDQ_003226

answers: Japan

answers: NDQ_003227

answers: the feint or weight transfer drift

answers: NDQ_003228

answers: drift drivers

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: pressure

answers: NDQ_003233

answers: Many drift drivers will utilise the feint or weight transfer drift on track

answers: NDQ_003236

answers: continents move over Earths surface

answers: NDQ_003237

answers: weight transfer

answers: NDQ_003239

answers: Fossil records across continents was evidence for continental drift

answers: NDQ_003240

answers: North America

answers: NDQ_003241

answers: no

answers: NDQ_003242

answers: weight transfer

answers: NDQ_003244

answers: Japan

answers: NDQ_003246

answers: Japanese

answers: NDQ_003247

answers: Many Japanese based vehicles

answers: NDQ_003252

answers: plate tectonics

answers: NDQ_003253

answers: unanswerable

answers: NDQ_003254

answers: It is not possible to tell

answers: NDQ_003255

answers: Many drift drivers

answers: NDQ_003256

answers: Wegener

answers: NDQ_003257

answers: Pangaea

answers: NDQ_003258

answers: unanswerable

text: The genus was present until at least about 50,000 years ago before going extinct, although there is some evidence they may have survived to as recently as 18,000 years ago. Its extinction may have been due to climate shifts during the Pleistocene, or to human hunting. Those who support the hypothesis of a human-mediated extinction process cite the fact that the arrival of humans to continental Australia occurred at approximately the same time as the disappearance of this species. More evidence that this extinction was facilitated by human interaction is present in the fact that the time period in which the extinction occurred was characterised by a relatively stable climate. However, there is no evidence of predation on or consumption of P. goliah by humans in the fossil record.

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answers: 4

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answers: 0

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answers: 0

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answers: 0

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answers: 0

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answers: 0

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answers: 0

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answers: 0

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answers: 0

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answers: 0

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answers: 0

answers: tqa2:L_0076/T_0763/7a7192cbfb0cdb83fb089d3c4f8ea239

answers: 0

answers: NDQ_003219

answers: 0

answers: NDQ_003220

answers: 0

answers: NDQ_003221

answers: 0

answers: NDQ_003222

answers: 2

answers: NDQ_003223

answers: 0

answers: NDQ_003224

answers: 0

answers: NDQ_003225

answers: 0

answers: NDQ_003226

answers: 0

answers: NDQ_003227

answers: 0

answers: NDQ_003228

answers: 0

answers: NDQ_003230

answers: 0

answers: NDQ_003231

answers: 0

answers: NDQ_003233

answers: 0

answers: NDQ_003236

answers: 0

answers: NDQ_003237

answers: 0

answers: NDQ_003239

answers: 0

answers: NDQ_003240

answers: 0

answers: NDQ_003241

answers: 0

answers: NDQ_003242

answers: 0

answers: NDQ_003244

answers: 0

answers: NDQ_003246

answers: 4

answers: NDQ_003247

answers: 4

answers: NDQ_003252

answers: 4

answers: NDQ_003253

answers: 0

answers: NDQ_003254

answers: 0

answers: NDQ_003255

answers: 4

answers: NDQ_003256

answers: 0

answers: NDQ_003257

answers: 0

answers: NDQ_003258

answers: 0

answers: NDQ_003219

answers: climate changes during the Pleistocene

answers: NDQ_003220

answers: Australia

answers: NDQ_003221

answers: Pleistocene

answers: NDQ_003222

answers: climate shifts during the Pleistocene, or to human hunting

answers: NDQ_003223

answers: humans

answers: NDQ_003224

answers: fossil record

answers: NDQ_003225

answers: human-mediated extinction process

answers: NDQ_003226

answers: Australia

answers: NDQ_003227

answers: arrival of humans to continental Australia

answers: NDQ_003228

answers: climate shifts during the Pleistocene

answers: NDQ_003230

answers: Australia

answers: NDQ_003231

answers: magnetic field

answers: NDQ_003233

answers: The arrival of humans to continental Australia occurred at approximately the same time as the disappearance of this species

answers: NDQ_003236

answers: climate shifts

answers: NDQ_003237

answers: the time period in which the extinction occurred was characterised by a relatively stable climate

answers: NDQ_003239

answers: There is no evidence of predation on or consumption of P. goliah by humans

answers: NDQ_003240

answers: Australia

answers: NDQ_003241

answers: no

answers: NDQ_003242

answers: climate shifts

answers: NDQ_003244

answers: Australia

answers: NDQ_003246

answers: Australia

answers: NDQ_003247

answers: the time period in which the extinction occurred was characterised by a relatively stable climate

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: continental Australia

answers: NDQ_003254

answers: Its extinction may have been due to climate shifts

answers: NDQ_003255

answers: The arrival of humans to continental Australia occurred at approximately the same time as the disappearance of this species

answers: NDQ_003256

answers: no evidence of predation on or consumption of P. goliah

answers: NDQ_003257

answers: There is some evidence they may have survived to as recently as 18,000 years ago

answers: NDQ_003258

answers: The arrival of humans to continental Australia

text: The geologic history of the Australian continental mass is extremely prolonged and involved, continuing from the Archaean to the recent. In a gross pattern, continental Australia grew from west to east, with Archean rocks mostly in the west, Proterozoic rocks in the centre, and Phanerozoic rocks in the east. Recent geologic events are confined to intraplate earthquakes, as the continent of Australia sits distant from the plate boundary.

text: The geologic history of the Australian continental mass is extremely prolonged and involved, continuing from the

text: Archaean

text: to the recent. In a gross pattern, continental Australia grew from west to east, with Archean rocks mostly in the west, Proterozoic rocks in the centre, and Phanerozoic rocks in the east. Recent geologic events are confined to intraplate earthquakes, as the continent of Australia sits distant from the plate boundary.

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answers: 0

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answers: 4

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answers: 0

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answers: 0

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answers: 0

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text: In line with other previous and contemporaneous proposals, in 1912 the meteorologist Alfred Wegener amply described what he called continental drift, expanded in his 1915 book The Origin of Continents and Oceans and the scientific debate started that would end up fifty years later in the theory of plate tectonics. Starting from the idea (also expressed by his forerunners) that the present continents once formed a single land mass (which was called Pangea later on) that drifted apart, thus releasing the continents from the Earth's mantle and likening them to "icebergs" of low density granite floating on a sea of denser basalt. Supporting evidence for the idea came from the dove-tailing outlines of South America's east coast and Africa's west coast, and from the matching of the rock formations along these edges. Confirmation of their previous contiguous nature also came from the fossil plants Glossopteris and Gangamopteris, and the therapsid or mammal-like reptile Lystrosaurus, all widely distributed over South America, Africa, Antarctica, India and Australia. The evidence for such an erstwhile joining of these continents was patent to field geologists working in the southern hemisphere. The South African Alex du Toit put together a mass of such information in his 1937 publication Our Wandering Continents, and went further than Wegener in recognising the strong links between the Gondwana fragments.

text: In line with other previous and contemporaneous proposals, in 1912 the meteorologist

text: Alfred Wegener

text: amply described what he called continental drift, expanded in his 1915 book The Origin of Continents and Oceans and the scientific debate started that would end up fifty years later in the theory of plate tectonics. Starting from the idea (also expressed by his forerunners) that the present continents once formed a single land mass (which was called

text: Pangea

text: later on) that drifted apart, thus releasing the continents from the Earth's mantle and likening them to "icebergs" of low density

text: granite

text: floating on a sea of denser

text: basalt

text: . Supporting evidence for the idea came from the dove-tailing outlines of South America's east coast and Africa's west coast, and from the matching of the rock formations along these edges. Confirmation of their previous contiguous nature also came from the fossil plants

text: Glossopteris

text: and

text: Gangamopteris

text: , and the

text: therapsid

text: or

text: mammal-like reptile

text: Lystrosaurus

text: , all widely distributed over South America, Africa, Antarctica, India and Australia. The evidence for such an erstwhile joining of these continents was patent to field geologists working in the southern hemisphere. The South African

text: Alex du Toit

text: put together a mass of such information in his 1937 publication Our Wandering Continents, and went further than Wegener in recognising the strong links between the

text: Gondwana

text: fragments.

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answers: NDQ_003230

answers: Africa

answers: NDQ_003231

answers: magnetic field

answers: NDQ_003233

answers: Alex du Toit

answers: NDQ_003236

answers: continental drift

answers: NDQ_003237

answers: the dove-tailing outlines of South America's east coast and Africa's west coast

answers: NDQ_003239

answers: fossil plants Glossopteris and Gangamopteris

answers: NDQ_003240

answers: Pangea

answers: NDQ_003241

answers: Antarctica

answers: NDQ_003242

answers: plate tectonics

answers: NDQ_003244

answers: Antarctica

answers: NDQ_003246

answers: Pangea

answers: NDQ_003247

answers: the dove-tailing outlines of South America's east coast and Africa's west coast

answers: NDQ_003252

answers: theory of plate tectonics

answers: NDQ_003253

answers: Pangea

answers: NDQ_003254

answers: It was patent to field geologists working in the southern hemisphere

answers: NDQ_003255

answers: the fossil plants Glossopteris and Gangamopteris, and the therapsid or mammal-like reptile Lystrosaurus

answers: NDQ_003256

answers: The South African Alex du Toit

answers: NDQ_003257

answers: continents once formed a single land mass

answers: NDQ_003258

answers: the present continents once formed a single land mass

text: Alternative names include: Weichsel glaciation or Vistulian glaciation (referring to the Polish river Vistula or its German name Weichsel). Evidence suggests that the ice sheets were at their maximum size for only a short period, between 25,000 and 13,000 BP. Eight interstadials have been recognized in the Weichselian, including: the Oerel, Glinde, Moershoofd, Hengelo and Denekamp; however correlation with isotope stages is still in process. During the glacial maximum in Scandinavia, only the western parts of Jutland were ice-free, and a large part of what is today the North Sea was dry land connecting Jutland with Britain (see Doggerland). It is also in Denmark that the only Scandinavian ice-age animals older than 13,000 BC are found.

text: Alternative names include: Weichsel glaciation or Vistulian glaciation (referring to the Polish river

text: Vistula

text: or its German name Weichsel). Evidence suggests that the ice sheets were at their

text: maximum size

text: for only a short period, between 25,000 and 13,000

text: BP

text: . Eight

text: interstadial

text: s have been recognized in the Weichselian, including: the Oerel, Glinde, Moershoofd, Hengelo and Denekamp; however correlation with

text: isotope stages

text: is still in process. During the

text: glacial maximum

text: in Scandinavia, only the western parts of

text: Jutland

text: were ice-free, and a large part of what is today the

text: North Sea

text: was dry land connecting Jutland with Britain (see

text: Doggerland

text: ). It is also in Denmark that the only Scandinavian ice-age animals older than 13,000 BC are found.

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answers: 0

answers: NDQ_003219

answers: 4

answers: NDQ_003220

answers: 0

answers: NDQ_003221

answers: 0

answers: NDQ_003222

answers: 2

answers: NDQ_003223

answers: 0

answers: NDQ_003224

answers: 0

answers: NDQ_003225

answers: 0

answers: NDQ_003226

answers: 0

answers: NDQ_003227

answers: 0

answers: NDQ_003228

answers: 0

answers: NDQ_003230

answers: 0

answers: NDQ_003231

answers: 0

answers: NDQ_003233

answers: 0

answers: NDQ_003236

answers: 0

answers: NDQ_003237

answers: 0

answers: NDQ_003239

answers: 0

answers: NDQ_003240

answers: 0

answers: NDQ_003241

answers: 0

answers: NDQ_003242

answers: 0

answers: NDQ_003244

answers: 0

answers: NDQ_003246

answers: 4

answers: NDQ_003247

answers: 4

answers: NDQ_003252

answers: 4

answers: NDQ_003253

answers: 0

answers: NDQ_003254

answers: 0

answers: NDQ_003255

answers: 4

answers: NDQ_003256

answers: 0

answers: NDQ_003257

answers: 0

answers: NDQ_003258

answers: 0

answers: NDQ_003219

answers: ice sheets were at their maximum size

answers: NDQ_003220

answers: Scandinavia

answers: NDQ_003221

answers: BP

answers: NDQ_003222

answers: the ice sheets were at their maximum size for only a short period

answers: NDQ_003223

answers: 25,000 and 13,000 BP

answers: NDQ_003224

answers: ice-age animals

answers: NDQ_003225

answers: Weichsel glaciation

answers: NDQ_003226

answers: Scandinavia

answers: NDQ_003227

answers: ice sheets were at their maximum size for only a short period

answers: NDQ_003228

answers: Eight interstadials have been recognized in the Weichselian

answers: NDQ_003230

answers: Britain

answers: NDQ_003231

answers: magnetism

answers: NDQ_003233

answers: Eight interstadials have been recognized in the Weichselian

answers: NDQ_003236

answers: ice sheets were at their maximum size for only a short period, between 25,000 and 13,000 BP

answers: NDQ_003237

answers: Eight interstadials have been recognized in the Weichselian

answers: NDQ_003239

answers: ice sheets were at their maximum size for only a short period, between 25,000 and 13,000 BP

answers: NDQ_003240

answers: North Sea

answers: NDQ_003241

answers: no

answers: NDQ_003242

answers: interstadials

answers: NDQ_003244

answers: Denmark

answers: NDQ_003246

answers: Scandinavia

answers: NDQ_003247

answers: Denmark

answers: NDQ_003252

answers: plate tectonics

answers: NDQ_003253

answers: North Sea was dry land connecting Jutland with Britain

answers: NDQ_003254

answers: ice sheets were at their maximum size for only a short period

answers: NDQ_003255

answers: Evidence suggests that the ice sheets were at their maximum size for only a short period, between 25,000 and 13,000 BP

answers: NDQ_003256

answers: During the glacial maximum in Scandinavia

answers: NDQ_003257

answers: between 25,000 and 13,000 BP

answers: NDQ_003258

answers: 25,000 and 13,000 BP

text: During the Permian, all the Earth's major landmasses were collected into a single supercontinent known as Pangaea. Pangaea straddled the equator and extended toward the poles, with a corresponding effect on ocean currents in the single great ocean ("Panthalassa", the "universal sea"), and the Paleo-Tethys Ocean, a large ocean that was between Asia and Gondwana. The Cimmeria continent rifted away from Gondwana and drifted north to Laurasia, causing the Paleo-Tethys ocean to shrink. A new ocean was growing on its southern end, the Tethys Ocean, an ocean that would dominate much of the Mesozoic Era. Large continental landmass interiors experience climates with extreme variations of heat and cold ("continental climate") and monsoon conditions with highly seasonal rainfall patterns. Deserts seem to have been widespread on Pangaea. Such dry conditions favored gymnosperms, plants with seeds enclosed in a protective cover, over plants such as ferns that disperse spores in a wetter environment. The first modern trees (conifers, ginkgos and cycads) appeared in the Permian.

text: During the Permian, all the

text: Earth

text: 's major landmasses were collected into a single supercontinent known as

text: Pangaea

text: . Pangaea straddled the

text: equator

text: and extended toward the poles, with a corresponding effect on ocean currents in the single great ocean ("

text: Panthalassa

text: ", the "universal sea"), and the Paleo-Tethys Ocean, a large ocean that was between Asia and Gondwana. The

text: Cimmeria

text: continent

text: rift

text: ed away from

text: Gondwana

text: and drifted north to

text: Laurasia

text: , causing the

text: Paleo-Tethys

text: ocean to shrink. A new ocean was growing on its southern end, the

text: Tethys Ocean

text: , an ocean that would dominate much of the

text: Mesozoic

text: Era. Large continental landmass interiors experience climates with extreme variations of heat and cold ("

text: continental climate

text: ") and

text: monsoon

text: conditions with highly seasonal rainfall patterns.

text: Desert

text: s seem to have been widespread on Pangaea. Such dry conditions favored

text: gymnosperm

text: s, plants with seeds enclosed in a protective cover, over plants such as

text: fern

text: s that disperse

text: spore

text: s in a wetter environment. The first modern trees (

text: conifers

text: ginkgo

text: s and

text: cycad

text: s) appeared in the Permian.

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text: The film earned an estimated $4.5 million on its opening day. During its opening weekend it earned $12.7 million from 3,168 theaters – an average of $4,025 per theater – ranking third behind Ice Age: Continental Drift ($13.3 million) and The Dark Knight Rises ($62.1 million). The largest segments of the opening-weekend audience were over age 25 (59%) and male (60%). The film left theaters on October 18, 2012 (after 12 weeks) with a total gross of $35.3 million.

text: The film earned an estimated $4.5 million on its opening day. During its opening weekend it earned $12.7 million from 3,168 theaters – an average of $4,025 per theater – ranking third behind

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text: ($13.3 million) and

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text: ($62.1 million). The largest segments of the opening-weekend audience were over age 25 (59%) and male (60%). The film left theaters on October 18, 2012 (after 12 weeks) with a total gross of $35.3 million.

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answers: 4: The answer has limited relevance and completeness, with noticeable gaps or inaccuracy.

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answers: NDQ_003219

answers: glaciation is caused by plate movement

answers: NDQ_003220

answers: Glaciers

answers: NDQ_003221

answers: 19th century

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answers: glaciation is a natural process

answers: NDQ_003223

answers: glaciation

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answers: glaciation

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answers: NDQ_003226

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answers: major periods of glaciation

answers: NDQ_003230

answers: South America was attached to present-day

answers: NDQ_003231

answers: magnetism

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answers: At least two major periods of glaciation

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answers: major periods of glaciation

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answers: continental drift

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answers: Eocene

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answers: The magnetic north pole and geographic north pole are in the same location.

answers: NDQ_003242

answers: glaciation

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answers: Antarctica has drifted

answers: NDQ_003246

answers: The continents have never been together as a single whole continent

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answers: At least two major periods of glaciation

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answers: continental drift was developed before plate tectonics.

answers: NDQ_003253

answers: Wegener believed that all the continents were once joined together

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answers: Wegener's hypothesis of continental drift

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answers: At least two major periods of glaciation have been discovered

answers: NDQ_003256

answers: rocks of the same type and age

answers: NDQ_003257

answers: At least two major periods of glaciation have been discovered

answers: NDQ_003258

answers: Wegener

text: The British geologist Arthur Holmes championed the theory of continental drift at a time when it was deeply unfashionable. He proposed in 1931 that the Earth's mantle contained convection cells that dissipated radioactive heat and moved the crust at the surface. His Principles of Physical Geology, ending with a chapter on continental drift, was published in 1944.

text: The British geologist

text: Arthur Holmes

text: championed the theory of continental drift at a time when it was deeply unfashionable. He proposed in 1931 that the Earth's mantle contained convection cells that dissipated radioactive heat and moved the crust at the surface. His Principles of Physical Geology, ending with a chapter on continental drift, was published in 1944.

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answers: NDQ_003219

answers: convection cells

answers: NDQ_003220

answers: British

answers: NDQ_003221

answers: 1931

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answers: unfashionable

answers: NDQ_003223

answers: continental drift

answers: NDQ_003224

answers: radioactive heat

answers: NDQ_003225

answers: continental drift

answers: NDQ_003226

answers: Europe

answers: NDQ_003227

answers: that the Earth's mantle contained convection cells that dissipated radioactive heat

answers: NDQ_003228

answers: geologist

answers: NDQ_003230

answers: Earth

answers: NDQ_003231

answers: convection

answers: NDQ_003233

answers: His Principles of Physical Geology

answers: NDQ_003236

answers: continental drift

answers: NDQ_003237

answers: the Earth's mantle contained convection cells

answers: NDQ_003239

answers: continental drift

answers: NDQ_003240

answers: Earth

answers: NDQ_003241

answers: Earth's

answers: NDQ_003242

answers: convection cells

answers: NDQ_003244

answers: continental drift

answers: NDQ_003246

answers: continental drift

answers: NDQ_003247

answers: continental drift

answers: NDQ_003252

answers: plate tectonics

answers: NDQ_003253

answers: continental drift

answers: NDQ_003254

answers: unfashionable

answers: NDQ_003255

answers: Holmes championed the theory

answers: NDQ_003256

answers: continental drift

answers: NDQ_003257

answers: Pangaea

answers: NDQ_003258

answers: the Earth's mantle contained convection cells

text: The climatic conditions that cause glaciation had an indirect effect on arid and semiarid regions far removed from the large ice sheets. The increased precipitation that fed the glaciers also increased the runoff of major rivers and intermittent streams, resulting in the growth and development of large pluvial lakes. Most pluvial lakes developed in relatively arid regions where there typically was insufficient rain to establish a drainage system to the sea. Instead, stream runoff in those areas flowed into closed basins and formed playa lakes. With increased rainfall, the playa lakes enlarged and overflowed. Pluvial lakes were most extensive during glacial periods. During interglacial stages, when less precipitation fell, the pluvial lakes shrank to form small salt flats.

text: The climatic conditions that cause glaciation had an indirect effect on arid and semiarid regions far removed from the large

text: ice sheet

text: s. The increased precipitation that fed the

text: glacier

text: s also increased the runoff of major rivers and intermittent streams, resulting in the growth and development of large pluvial lakes. Most pluvial lakes developed in relatively arid regions where there typically was insufficient rain to establish a drainage system to the sea. Instead, stream runoff in those areas flowed into closed basins and formed

text: playa lake

text: s. With increased rainfall, the playa lakes enlarged and overflowed. Pluvial lakes were most extensive during glacial periods. During interglacial stages, when less precipitation fell, the pluvial lakes shrank to form small salt flats.

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answers: NDQ_003256

answers: 0

answers: NDQ_003257

answers: 0

answers: NDQ_003258

answers: 0

answers: NDQ_003219

answers: glaciation had an indirect effect

answers: NDQ_003220

answers: are not mentioned

answers: NDQ_003221

answers: 19th century

answers: NDQ_003222

answers: glacial periods

answers: NDQ_003223

answers: glacial periods

answers: NDQ_003224

answers: glacial periods

answers: NDQ_003225

answers: glaciation

answers: NDQ_003226

answers: ice sheets

answers: NDQ_003227

answers: glaciation had an indirect effect

answers: NDQ_003228

answers: major rivers and intermittent streams

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: magnetic field

answers: NDQ_003233

answers: arid and semiarid regions

answers: NDQ_003236

answers: glaciation

answers: NDQ_003237

answers: large ice sheets

answers: NDQ_003239

answers: continental drift

answers: NDQ_003240

answers: North America

answers: NDQ_003241

answers: no

answers: NDQ_003242

answers: interglacial

answers: NDQ_003244

answers: It is on a continent

answers: NDQ_003246

answers: continents

answers: NDQ_003247

answers: Most pluvial lakes developed in relatively arid regions

answers: NDQ_003252

answers: plate tectonics

answers: NDQ_003253

answers: The climatic conditions

answers: NDQ_003254

answers: The climatic conditions that cause glaciation

answers: NDQ_003255

answers: Wegener and his supporters provided a lot of evidence for continental drift

answers: NDQ_003256

answers: arid and semiarid regions

answers: NDQ_003257

answers: Pangaea

answers: NDQ_003258

answers: continents can drift

text: New Caledonia and New Zealand ecoregions became separated  from Australia by continental drift 85 million years ago. The islands still retain plants that originated in Gondwana and spread to the Southern Hemisphere continents later. However, strong evidence exists of glaciation during the Carboniferous to Permian time, especially in South Africa.

text: New Caledonia and New Zealand ecoregions became separated  from Australia by

text: continental drift

text: 85 million years ago. The islands still retain plants that originated in Gondwana and spread to the Southern Hemisphere continents later. However, strong evidence exists of

text: glaciation

text: during the

text: Carboniferous

text: to

text: Permian

text: time, especially in South Africa.

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answers: 4

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answers: 0

answers: NDQ_003221

answers: 0

answers: NDQ_003222

answers: 2

answers: NDQ_003223

answers: 0

answers: NDQ_003224

answers: 4

answers: NDQ_003225

answers: 0

answers: NDQ_003226

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answers: NDQ_003227

answers: 0

answers: NDQ_003228

answers: 0

answers: NDQ_003230

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answers: NDQ_003231

answers: 0

answers: NDQ_003233

answers: 4

answers: NDQ_003236

answers: 5

answers: NDQ_003237

answers: 0

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answers: 4

answers: NDQ_003240

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answers: NDQ_003242

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answers: NDQ_003246

answers: 4

answers: NDQ_003247

answers: 4

answers: NDQ_003252

answers: 4

answers: NDQ_003253

answers: 0

answers: NDQ_003254

answers: 4

answers: NDQ_003255

answers: 4

answers: NDQ_003256

answers: 0

answers: NDQ_003257

answers: 0

answers: NDQ_003258

answers: 4

answers: NDQ_003219

answers: continental drift

answers: NDQ_003220

answers: New Caledonia

answers: NDQ_003221

answers: late Carboniferous

answers: NDQ_003222

answers: strong evidence exists of glaciation

answers: NDQ_003223

answers: Gondwana

answers: NDQ_003224

answers: glaciation

answers: NDQ_003225

answers: continental drift

answers: NDQ_003226

answers: New Caledonia

answers: NDQ_003227

answers: separated from Australia

answers: NDQ_003228

answers: continental drift

answers: NDQ_003230

answers: Gondwana

answers: NDQ_003231

answers: Hemisphere

answers: NDQ_003233

answers: strong evidence exists of glaciation

answers: NDQ_003236

answers: continental drift

answers: NDQ_003237

answers: strong evidence exists of glaciation

answers: NDQ_003239

answers: Gondwana and spread to the Southern Hemisphere continents later

answers: NDQ_003240

answers: Gondwana

answers: NDQ_003241

answers: The Southern Hemisphere

answers: NDQ_003242

answers: continental drift

answers: NDQ_003244

answers: Australia

answers: NDQ_003246

answers: Gondwana

answers: NDQ_003247

answers: Strong evidence exists of glaciation during the Carboniferous to Permian time

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: Gondwana

answers: NDQ_003254

answers: It was widely accepted

answers: NDQ_003255

answers: New Caledonia and New Zealand ecoregions became separated from Australia

answers: NDQ_003256

answers: Gondwana

answers: NDQ_003257

answers: Gondwana

answers: NDQ_003258

answers: Gondwana

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.

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answers: North America

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answers: Paleozoic era

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answers: very few twin subduction zones exist on Earth

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answers: the Insular Plate

answers: NDQ_003224

answers: subduction zone

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answers: twin subduction zone

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answers: Asia

answers: NDQ_003227

answers: As the North American Plate drifted west and the Insular Plate drifted east

answers: NDQ_003228

answers: geoscientist

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answers: North America

answers: NDQ_003231

answers: magnetic field

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answers: This large mass of igneous rock is the largest granite outcropping in North America

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answers: continents move over Earths surface

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answers: This arrangement of two parallel subduction zones is unusual

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answers: This arrangement of two parallel subduction zones

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answers: Farallon Plate

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answers: North America

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answers: subduction

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answers: NDQ_003247

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answers: plate tectonics

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answers: The largest granite outcropping in North America

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answers: Pangaea

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answers: As the North American Plate drifted west

text: In February 2008, UAL Corporation and Continental Airlines began the advanced stages of merger talks and were expected to announce their decision in the immediate aftermath of a definitive merger agreement between rival Delta Air Lines and Northwest Airlines. The timing of the events was notable because Northwest's golden shares in Continental (that gave Northwest veto authority against any merger involving Continental) could be redeemed, freeing Continental to pursue a marriage with United. On April 27, 2008, Continental broke off merger negotiations with United and stated it was going to stand alone. Despite ending merger talks, Continental announced that it will join United in the Star Alliance.

text: In February 2008,

text: UAL Corporation

text: and Continental Airlines began the advanced stages of merger talks and were expected to announce their decision in the immediate aftermath of a definitive merger agreement between rival

text: Delta Air Lines

text: and

text: Northwest Airlines

text: . The timing of the events was notable because Northwest's golden shares in Continental (that gave Northwest veto authority against any merger involving Continental) could be redeemed, freeing Continental to pursue a marriage with United. On April 27, 2008, Continental broke off merger negotiations with United and stated it was going to stand alone. Despite ending merger talks, Continental announced that it will join United in the Star Alliance.

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answers: continental plates collide

answers: NDQ_003220

answers: Northwest

answers: NDQ_003221

answers: February 2008

answers: NDQ_003222

answers: Continental broke off merger negotiations

answers: NDQ_003223

answers: UAL Corporation

answers: NDQ_003224

answers: ancient

answers: NDQ_003225

answers: Northwest's golden shares in Continental

answers: NDQ_003226

answers: Europe

answers: NDQ_003227

answers: freeing Continental to pursue a marriage with United

answers: NDQ_003228

answers: veto authority

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: magnetic field

answers: NDQ_003233

answers: Northwest's golden shares in Continental

answers: NDQ_003236

answers: is not applicable

answers: NDQ_003237

answers: a definitive merger agreement between rival Delta Air Lines and Northwest Airlines

answers: NDQ_003239

answers: Continental broke off merger negotiations

answers: NDQ_003240

answers: North America

answers: NDQ_003241

answers: Northwest's golden shares in Continental

answers: NDQ_003242

answers: Golden shares

answers: NDQ_003244

answers: continent

answers: NDQ_003246

answers: Northwest's golden shares in Continental

answers: NDQ_003247

answers: continental drift

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: It will join United in the Star Alliance

answers: NDQ_003254

answers: It was widely accepted as soon as it was introduced

answers: NDQ_003255

answers: Wegener and his supporters provided a lot of evidence

answers: NDQ_003256

answers: Continental broke off merger negotiations with United

answers: NDQ_003257

answers: Continental broke off merger negotiations

answers: NDQ_003258

answers: On April 27, 2008, Continental broke off merger negotiations with United

text: If the sample is cooled below T in the absence of an external magnetic field and a magnetic field is applied after the transition to the spin glass phase, there is a rapid initial increase to a value called the zero-field-cooled magnetization. A slow upward drift then occurs toward the field-cooled magnetization.

text: If the sample is cooled below T in the absence of an external magnetic field and a magnetic field is applied after the transition to the spin glass phase, there is a rapid initial increase to a value called the zero-field-cooled magnetization. A slow upward drift then occurs toward the field-cooled magnetization.

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answers: 0

answers: NDQ_003219

answers: 0

answers: NDQ_003220

answers: 0

answers: NDQ_003221

answers: 0

answers: NDQ_003222

answers: 0

answers: NDQ_003223

answers: 0

answers: NDQ_003224

answers: 0

answers: NDQ_003225

answers: 0

answers: NDQ_003226

answers: 0

answers: NDQ_003227

answers: 0

answers: NDQ_003228

answers: 0

answers: NDQ_003230

answers: 0

answers: NDQ_003231

answers: 0

answers: NDQ_003233

answers: 0

answers: NDQ_003236

answers: 0

answers: NDQ_003237

answers: 0

answers: NDQ_003239

answers: 0

answers: NDQ_003240

answers: 0

answers: NDQ_003241

answers: 0

answers: NDQ_003242

answers: 0

answers: NDQ_003244

answers: 0

answers: NDQ_003246

answers: 0

answers: NDQ_003247

answers: 0

answers: NDQ_003252

answers: 3

answers: NDQ_003253

answers: 0

answers: NDQ_003254

answers: 0

answers: NDQ_003255

answers: 0

answers: NDQ_003256

answers: 0

answers: NDQ_003257

answers: 0

answers: NDQ_003258

answers: 0

answers: NDQ_003219

answers: an external magnetic field is applied

answers: NDQ_003220

answers: unanswerable

answers: NDQ_003221

answers: 19th century

answers: NDQ_003222

answers: zero-field-cooled magnetization

answers: NDQ_003223

answers: a magnetic field

answers: NDQ_003224

answers: magnetic field

answers: NDQ_003225

answers: zero-field-cooled magnetization

answers: NDQ_003226

answers: Antarctica

answers: NDQ_003227

answers: drift then occurs toward the field-cooled magnetization

answers: NDQ_003228

answers: magnetic field

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: external magnetic field

answers: NDQ_003233

answers: A slow upward drift then occurs toward the field-cooled magnetization

answers: NDQ_003236

answers: A slow upward drift

answers: NDQ_003237

answers: a slow upward drift

answers: NDQ_003239

answers: fossil records across continents

answers: NDQ_003240

answers: unanswerable

answers: NDQ_003241

answers: no

answers: NDQ_003242

answers: A slow upward drift

answers: NDQ_003244

answers: drift

answers: NDQ_003246

answers: None of the above choices.

answers: NDQ_003247

answers: A slow upward drift

answers: NDQ_003252

answers: plate tectonics

answers: NDQ_003253

answers: unanswerable

answers: NDQ_003254

answers: The zero-field-cooled magnetization

answers: NDQ_003255

answers: Wegener and his supporters provided a lot of evidence for continental drift

answers: NDQ_003256

answers: The Atlantic Ocean

answers: NDQ_003257

answers: Pangaea

answers: NDQ_003258

answers: A slow upward drift then occurs toward the field-cooled magnetization

text: The Canadian portion of the Pacific Northwest began forming during the early Jurassic period when a group of active volcanic islands collided against a pre-existing continental margin and coastline of Western Canada. These volcanic islands, known as the Intermontane Islands by geoscientists, were formed on a pre-existing tectonic plate called the Intermontane Plate about 245 million years ago by subduction of the former Insular Plate to its west 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 Western Canada called the Slide Mountain 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 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 Canada, supporting a volcanic arc on the former continental margin of Western Canada. As the North American Plate drifted west and the Intermontane Plate continued to drift east to the ancient continental margin of Western Canada, the Slide Mountain Ocean began to close by ongoing subduction under the Slide Mountain Ocean. This subduction zone eventually jammed and shut down completely about 180 million years ago, ending the arc volcanism on the ancient continental margin of Western Canada and the Intermontane Islands collided, forming a long chain of deformed volcanic and sedimentary rock called the Intermontane Belt, which consists of deeply cut valleys, high plateaus, and rolling uplands. This collision also crushed and folded sedimentary and igneous rocks, creating a mountain range called the Kootenay Fold Belt which existed in far eastern British Columbia.

text: The Canadian portion of the

text: Pacific Northwest

text: began forming during the early

text: Jurassic

text: period when a group of active volcanic islands collided against a pre-existing

text: continental margin

text: and coastline of Western Canada. These volcanic islands, known as the

text: Intermontane Islands

text: by geoscientists, were 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: to its west 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 Western Canada called the

text: Slide Mountain 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 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 Canada, supporting a volcanic arc on the former continental margin of Western Canada. As the

text: North American Plate

text: drifted west and the Intermontane Plate continued to drift east to the ancient continental margin of Western Canada, the Slide Mountain Ocean began to close by ongoing subduction under the Slide Mountain Ocean. This subduction zone eventually jammed and shut down completely about 180 million years ago, ending the arc volcanism on the ancient continental margin of Western Canada and the Intermontane Islands collided, forming a long chain of deformed volcanic and sedimentary rock called the

text: Intermontane Belt

text: , which consists of deeply cut valleys, high plateaus, and rolling uplands. This collision also crushed and

text: fold

text: ed

text: sedimentary

text: and

text: igneous rock

text: s, creating a

text: mountain range

text: called the Kootenay Fold Belt which existed in far eastern British Columbia.

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answers: 3: The answer has limited relevance and completeness, with noticeable gaps or inaccuracy.

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answers: two parallel subduction zones exist on Earth

answers: NDQ_003220

answers: Kootenay Fold

answers: NDQ_003221

answers: Triassic period

answers: NDQ_003222

answers: very few twin subduction zones exist on Earth

answers: NDQ_003223

answers: the Slide Mountain Ocean

answers: NDQ_003224

answers: subduction zone

answers: NDQ_003225

answers: twin subduction zone

answers: NDQ_003226

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answers: NDQ_003227

answers: As the North American Plate drifted west and the Intermontane Plate continued to drift east to the ancient continental margin of Western Canada

answers: NDQ_003228

answers: geoscientists

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answers: North America

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answers: As the North American Plate drifted west

answers: NDQ_003236

answers: tectonic plate

answers: NDQ_003237

answers: This arrangement of two parallel subduction zones is unusual

answers: NDQ_003239

answers: very few twin subduction zones exist on Earth

answers: NDQ_003240

answers: Insular Plate

answers: NDQ_003241

answers: North American Plate

answers: NDQ_003242

answers: subduction

answers: NDQ_003244

answers: The North American Plate drifted west

answers: NDQ_003246

answers: As the North American Plate drifted west

answers: NDQ_003247

answers: As the North American Plate drifted west and the Intermontane Plate continued to drift east to the ancient continental margin of Western Canada

answers: NDQ_003252

answers: plate tectonics

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answers: The Canadian portion of the Pacific Northwest

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answers: As the North American Plate drifted west

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answers: The Canadian portion of the Pacific Northwest began forming during the early Jurassic period

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answers: This arrangement of two parallel subduction zones

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answers: Pangaea

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answers: As the North American Plate drifted west

text: As a promotion for Ice Age: Continental Drift, Fox released two 3-minute short segments from the film, titled Scrat's Continental Crack-up and Scrat's Continental Crack-up: Part 2. The first part premiered as a theatrical release attached to Gulliver's Travels in 2010, and it was released on-line on January 6, 2011, on iTunes Movie Trailers. The second part was released on November 16, 2011, on iTunes, and debuted in theatres with Alvin and the Chipmunks: Chipwrecked. The first part shows how the Scrat's actions lead to split of the continents, while in the second part, Scrat's underwater pursuit of acorns leads him to a pirate ship.

text: As a promotion for Ice Age: Continental Drift, Fox released two 3-minute short segments from the film, titled Scrat's Continental Crack-up and Scrat's Continental Crack-up: Part 2. The first part premiered as a theatrical release attached to

text: Gulliver's Travels

text: in 2010, and it was released on-line on January 6, 2011, on

text: iTunes Movie Trailers

text: . The second part was released on November 16, 2011, on iTunes, and debuted in theatres with

text: Alvin and the Chipmunks: Chipwrecked

text: . The first part shows how the Scrat's actions lead to split of the continents, while in the second part, Scrat's underwater pursuit of acorns leads him to a pirate ship.

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answers: split of the continents

answers: NDQ_003220

answers: are split

answers: NDQ_003221

answers: Ice Age

answers: NDQ_003222

answers: Scrat's Continental Crack-up

answers: NDQ_003223

answers: split of the continents

answers: NDQ_003224

answers: Gulliver

answers: NDQ_003225

answers: Split of the continents

answers: NDQ_003226

answers: Ice Age

answers: NDQ_003227

answers: split of the continents

answers: NDQ_003228

answers: continental crack-up

answers: NDQ_003230

answers: Ice Age

answers: NDQ_003231

answers: Chipwreck

answers: NDQ_003233

answers: Scrat's Continental Crack-up

answers: NDQ_003236

answers: The first part shows how the Scrat's actions lead to split of the continents

answers: NDQ_003237

answers: Scrat's Continental Crack-up

answers: NDQ_003239

answers: Scrat's Continental Crack-up: Part 2

answers: NDQ_003240

answers: Ice Age

answers: NDQ_003241

answers: no

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answers: Continental Drift

answers: NDQ_003244

answers: Continental Drift

answers: NDQ_003246

answers: Split of the continents

answers: NDQ_003247

answers: Scrat's Continental Crack-up

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

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answers: NDQ_003254

answers: It was widely accepted as soon as it was introduced

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answers: Scrat's Continental Crack-up: Part 2

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answers: Scrat's Continental Crack-up

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answers: Scrat's Continental Crack-up: Part 2

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answers: Scrat's Continental Crack-up

text: A team from the Centre for Remote Sensing (CRS) of Bharathidasan University, Tiruchi led by Professor S.M. Ramasamy in 2003 said "the land/beaches were formed between Ramanathapuram and Pamban because of the long shore drifting currents which moved in an anti-clockwise direction in the north and clockwise direction in the south of Rameswaram and Talaimannar about 3,500 years ago," and, "as the carbon dating of the beaches roughly matches the dates of Ramayana, its link to the epic needs to be explored". A former director of the Geological Survey of India, S. Badrinarayanan, claims that such a natural formation would be impossible. He justifies the same by the presence of a loose sand layer under corals for the entire stretch. Corals normally form above rocks. He feels that a thorough analysis was not conducted by the Geological Survey of India before undertaking the SSCP project. The Government of India, in an affidavit in the Supreme Court of India, said that there is no historical proof of the bridge being built by Rama. In connection with the canal project, the Madras High Court in its verdict stated that the Rama Sethu is a man-made structure.

text: A team from the Centre for Remote Sensing (CRS) of

text: Bharathidasan University

text: , Tiruchi led by Professor S.M. Ramasamy in 2003 said "the land/beaches were formed between Ramanathapuram and Pamban because of the long shore drifting currents which moved in an anti-clockwise direction in the north and clockwise direction in the south of Rameswaram and Talaimannar about 3,500 years ago," and, "as the

text: carbon dating

text: of the beaches roughly matches the dates of Ramayana, its link to the epic needs to be explored". A former director of the

text: Geological Survey of India

text: , S. Badrinarayanan, claims that such a natural formation would be impossible. He justifies the same by the presence of a loose sand layer under corals for the entire stretch. Corals normally form above rocks. He feels that a thorough analysis was not conducted by the Geological Survey of India before undertaking the SSCP project. The Government of India, in an affidavit in the

text: Supreme Court of India

text: , said that there is no historical proof of the bridge being built by Rama. In connection with the canal project, the

text: Madras High Court

text: in its verdict stated that the Rama Sethu is a man-made structure.

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answers: NDQ_003220

answers: 0

answers: NDQ_003221

answers: 0

answers: NDQ_003222

answers: 2

answers: NDQ_003223

answers: 0

answers: NDQ_003224

answers: 0

answers: NDQ_003225

answers: 0

answers: NDQ_003226

answers: 0

answers: NDQ_003227

answers: 0

answers: NDQ_003228

answers: 0

answers: NDQ_003230

answers: 0

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answers: 0

answers: NDQ_003233

answers: 0

answers: NDQ_003236

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answers: 0

answers: NDQ_003240

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answers: NDQ_003244

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answers: 4

answers: NDQ_003252

answers: 4

answers: NDQ_003253

answers: 0

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answers: NDQ_003256

answers: 0

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answers: 0

answers: NDQ_003258

answers: 0

answers: NDQ_003219

answers: long shore drifting currents which moved in an anti-clockwise direction

answers: NDQ_003220

answers: Madras High Court

answers: NDQ_003221

answers: Bharathidasan University

answers: NDQ_003222

answers: such a natural formation would be impossible

answers: NDQ_003223

answers: man-made

answers: NDQ_003224

answers: Ramayana

answers: NDQ_003225

answers: the Rama Sethu is a man-made structure

answers: NDQ_003226

answers: India

answers: NDQ_003227

answers: long shore drifting currents which moved in an anti-clockwise direction in the north and clockwise direction in the south

answers: NDQ_003228

answers: Geological Survey of India

answers: NDQ_003230

answers: India

answers: NDQ_003231

answers: clockwise direction

answers: NDQ_003233

answers: carbon dating of the beaches roughly matches the dates of Ramayana

answers: NDQ_003236

answers: long shore drifting currents

answers: NDQ_003237

answers: carbon dating of the beaches roughly matches the dates of Ramayana

answers: NDQ_003239

answers: carbon dating of the beaches roughly matches the dates of Ramayana

answers: NDQ_003240

answers: SSCP

answers: NDQ_003241

answers: Anti-clockwise direction

answers: NDQ_003242

answers: long shore drifting currents

answers: NDQ_003244

answers: India

answers: NDQ_003246

answers: continents

answers: NDQ_003247

answers: anti-clockwise direction in the north and clockwise direction in the south

answers: NDQ_003252

answers: long shore drifting currents

answers: NDQ_003253

answers: Geological Survey of India

answers: NDQ_003254

answers: long shore drifting currents

answers: NDQ_003255

answers: long shore drifting currents

answers: NDQ_003256

answers: Corals normally form above rocks

answers: NDQ_003257

answers: about 3,500 years ago

answers: NDQ_003258

answers: long shore drifting currents

text: The intertidal zone and the photic zone in the oceans are relatively familiar habitats. However the vast bulk of the ocean is unhospitable to air-breathing humans, with scuba divers limited to the upper  or so. The lower limit for photosynthesis is  and below that depth the prevailing conditions include total darkness, high pressure, little oxygen (in some places), scarce food resources and extreme cold. This habitat is very challenging to research, and as well as being little studied, it is vast, with 79% of the Earth's biosphere being at depths greater than . With no plant life, the animals in this zone are either detritivores, reliant on food drifting down from surface layers, or they are predators, feeding on each other. Some organisms are pelagic, swimming or drifting in mid-ocean, while others are benthic, living on or near the seabed. Their growth rates and metabolisms tend to be slow, their eyes may be very large to detect what little illumination there is, or they may be blind and rely on other sensory inputs. A number of deep sea creatures are bioluminescent; this serves a variety of functions including predation, protection and social recognition. In general, the bodies of animals living at great depths are adapted to high pressure environments by having pressure-resistant biomolecules and small organic molecules present in their cells know as piezolytes, which give the proteins the flexibility they need. There are also unsaturated fats in their membranes which prevent them from solidifying at low temperatures.

text: The

text: intertidal zone

text: and the

text: photic zone

text: in the oceans are relatively familiar habitats. However the vast bulk of the ocean is unhospitable to air-breathing humans, with

text: scuba divers

text: limited to the upper  or so. The lower limit for photosynthesis is  and below that depth the prevailing conditions include total darkness, high pressure, little oxygen (in some places), scarce food resources and extreme cold. This habitat is very challenging to research, and as well as being little studied, it is vast, with 79% of the Earth's

text: biosphere

text: being at depths greater than . With no plant life, the animals in this zone are either

text: detritivore

text: s, reliant on food drifting down from surface layers, or they are

text: predators

text: , feeding on each other. Some organisms are

text: pelagic

text: , swimming or drifting in mid-ocean, while others are benthic, living on or near the seabed. Their growth rates and metabolisms tend to be slow, their eyes may be very large to detect what little illumination there is, or they may be blind and rely on other sensory inputs. A number of deep sea creatures are

text: bioluminescent

text: ; this serves a variety of functions including predation, protection and social recognition. In general, the bodies of animals living at great depths are adapted to high pressure environments by having pressure-resistant biomolecules and small organic molecules present in their cells know as

text: piezolyte

text: s, which give the proteins the flexibility they need. There are also unsaturated fats in their membranes which prevent them from solidifying at low temperatures.

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answers: 0

answers: NDQ_003219

answers: 0

answers: NDQ_003220

answers: 0

answers: NDQ_003221

answers: 0

answers: NDQ_003222

answers: 0

answers: NDQ_003223

answers: 0

answers: NDQ_003224

answers: 0

answers: NDQ_003225

answers: 0

answers: NDQ_003226

answers: 0

answers: NDQ_003227

answers: 0

answers: NDQ_003228

answers: 0

answers: NDQ_003230

answers: 0

answers: NDQ_003231

answers: 0

answers: NDQ_003233

answers: 0

answers: NDQ_003236

answers: 0

answers: NDQ_003237

answers: 0

answers: NDQ_003239

answers: 0

answers: NDQ_003240

answers: 0

answers: NDQ_003241

answers: 0

answers: NDQ_003242

answers: 0

answers: NDQ_003244

answers: 0

answers: NDQ_003246

answers: 0

answers: NDQ_003247

answers: 0

answers: NDQ_003252

answers: 4

answers: NDQ_003253

answers: 0

answers: NDQ_003254

answers: 0

answers: NDQ_003255

answers: 4

answers: NDQ_003256

answers: 0

answers: NDQ_003257

answers: 0

answers: NDQ_003258

answers: 0

answers: NDQ_003219

answers: Earth's biosphere being at depths greater than

answers: NDQ_003220

answers: are

answers: NDQ_003221

answers: late 19th century

answers: NDQ_003222

answers: The vast bulk of the ocean is unhospitable to air-breathing humans

answers: NDQ_003223

answers: depths greater than

answers: NDQ_003224

answers: scuba divers

answers: NDQ_003225

answers: The vast bulk of the ocean is unhospitable

answers: NDQ_003226

answers: the oceans

answers: NDQ_003227

answers: 79% of the Earth's biosphere being at depths greater

answers: NDQ_003228

answers: scuba divers

answers: NDQ_003230

answers: Earth

answers: NDQ_003231

answers: high pressure

answers: NDQ_003233

answers: 79% of the Earth's biosphere

answers: NDQ_003236

answers: The vast bulk of the ocean

answers: NDQ_003237

answers: 79% of the Earth's biosphere

answers: NDQ_003239

answers: 79% of the Earth's biosphere

answers: NDQ_003240

answers: Earth

answers: NDQ_003241

answers: Earth's biosphere

answers: NDQ_003242

answers: continental drift

answers: NDQ_003244

answers: It is on a continent that has drifted

answers: NDQ_003246

answers: The vast bulk of the ocean

answers: NDQ_003247

answers: 79% of the Earth's biosphere

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: Wegener

answers: NDQ_003254

answers: 79% of the Earth's biosphere

answers: NDQ_003255

answers: 79% of the Earth's biosphere being at depths greater than

answers: NDQ_003256

answers: The vast bulk of the ocean

answers: NDQ_003257

answers: Pangaea

answers: NDQ_003258

answers: The vast bulk of the ocean

text: Fossil plants, and in particular their leaves, have been the most useful sources of information of paleoclimate during the time of deposition of the Florissant Formation. Plants have a smaller tolerance on average to climatic changes, whereas many animals can be mobile and respond to rapid seasonal or daily changes.

text: Fossil plants, and in particular their leaves, have been the most useful sources of information of paleoclimate during the time of deposition of the Florissant Formation. Plants have a smaller tolerance on average to climatic changes, whereas many animals can be mobile and respond to rapid seasonal or daily changes.

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answers: NDQ_003222

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answers: NDQ_003223

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answers: NDQ_003225

answers: 4

answers: NDQ_003226

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answers: NDQ_003227

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answers: NDQ_003230

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answers: 0

answers: NDQ_003258

answers: 0

answers: NDQ_003219

answers: Fossil plants

answers: NDQ_003220

answers: Florissant Formation

answers: NDQ_003221

answers: paleoclimate

answers: NDQ_003222

answers: many animals can be mobile and respond to rapid seasonal or daily changes

answers: NDQ_003223

answers: paleoclimate

answers: NDQ_003224

answers: Florissant Formation

answers: NDQ_003225

answers: Paleoclimate

answers: NDQ_003226

answers: Europe

answers: NDQ_003227

answers: Plants have a smaller tolerance on average to climatic changes

answers: NDQ_003228

answers: paleoclimate

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: magnet

answers: NDQ_003233

answers: Fossil plants

answers: NDQ_003236

answers: mobile

answers: NDQ_003237

answers: Fossil plants

answers: NDQ_003239

answers: Fossil plants

answers: NDQ_003240

answers: North America

answers: NDQ_003241

answers: The magnetic north pole and geographic north pole

answers: NDQ_003242

answers: paleoclimate

answers: NDQ_003244

answers: Florissant Formation

answers: NDQ_003246

answers: Paleoclimate

answers: NDQ_003247

answers: Paleoclimate

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: Fossil plants

answers: NDQ_003254

answers: Fossil plants

answers: NDQ_003255

answers: Fossil plants

answers: NDQ_003256

answers: Florissant Formation

answers: NDQ_003257

answers: Pangaea

answers: NDQ_003258

answers: Fossil plants, and in particular their leaves

text: IOTs have been described as a cross between a klystron and a triode, hence Eimac's trade name for them, Klystrode.  They have an electron gun like a klystron, but with a control grid in front of it like a triode, with a very close spacing of around 0.1 mm. The high frequency RF voltage on the grid allows the electrons through in bunches.    High voltage DC on a cylindrical anode accelerates the modulated electron beam through a small drift tube like a klystron. This drift tube prevents backflow of electromagnetic radiation. The bunched electron beam passes through the hollow anode into a resonant cavity, similar to the output cavity of a klystron, and strikes a collector electrode.  As in a klystron, each bunch passes into the cavity at a time when the electric field decelerates it, transforming the kinetic energy of the beam into potential energy of the RF field, amplifying the signal.  The oscillating electromagnetic energy in the cavity is extracted by a coaxial transmission line.  An axial magnetic field prevents space charge spreading of the beam.  The collector electrode is at a lower potential than the anode (depressed collector) which recovers some of the energy from the beam, increasing efficiency.

text: IOTs have been described as a cross between a klystron and a

text: triode

text: , hence

text: Eimac

text: 's trade name for them, Klystrode.  They have an

text: electron gun

text: like a klystron, but with a

text: control grid

text: in front of it like a triode, with a very close spacing of around 0.1 mm. The high frequency RF voltage on the grid allows the electrons through in bunches.    High voltage

text: DC

text: on a cylindrical anode accelerates the modulated electron beam through a small drift tube like a klystron. This drift tube prevents backflow of electromagnetic radiation. The bunched electron beam passes through the hollow anode into a resonant cavity, similar to the output cavity of a klystron, and strikes a collector electrode.  As in a klystron, each bunch passes into the cavity at a time when the electric field decelerates it, transforming the kinetic energy of the beam into potential energy of the RF field, amplifying the signal.  The oscillating electromagnetic energy in the cavity is extracted by a coaxial transmission line.  An axial

text: magnetic field

text: prevents space charge spreading of the beam.  The collector electrode is at a lower potential than the anode (depressed collector) which recovers some of the energy from the beam, increasing efficiency.

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answers: 0

answers: NDQ_003219

answers: 0

answers: NDQ_003220

answers: 0

answers: NDQ_003221

answers: 0

answers: NDQ_003222

answers: 0

answers: NDQ_003223

answers: 0

answers: NDQ_003224

answers: 0

answers: NDQ_003225

answers: 0

answers: NDQ_003226

answers: 0

answers: NDQ_003227

answers: 0

answers: NDQ_003228

answers: 0

answers: NDQ_003230

answers: 0

answers: NDQ_003231

answers: 0

answers: NDQ_003233

answers: 0

answers: NDQ_003236

answers: 0

answers: NDQ_003237

answers: 0

answers: NDQ_003239

answers: 0

answers: NDQ_003240

answers: 0

answers: NDQ_003241

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answers: NDQ_003242

answers: 0

answers: NDQ_003244

answers: 0

answers: NDQ_003246

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answers: NDQ_003247

answers: 0

answers: NDQ_003252

answers: 3

answers: NDQ_003253

answers: 0

answers: NDQ_003254

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answers: NDQ_003255

answers: 0

answers: NDQ_003256

answers: 0

answers: NDQ_003257

answers: 0

answers: NDQ_003258

answers: 0

answers: NDQ_003219

answers: plate tectonics

answers: NDQ_003220

answers: unanswerable

answers: NDQ_003221

answers: IOTs

answers: NDQ_003222

answers: An axial magnetic field prevents space charge spreading of the beam

answers: NDQ_003223

answers: IOTs

answers: NDQ_003224

answers: IOTs

answers: NDQ_003225

answers: IOTs

answers: NDQ_003226

answers: Europe

answers: NDQ_003227

answers: a cross between a klystron and a triode

answers: NDQ_003228

answers: Eimac

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: axial magnetic field

answers: NDQ_003233

answers: Eimac's trade name for them, Klystrode

answers: NDQ_003236

answers: continents move over Earths surface

answers: NDQ_003237

answers: a cross between a klystron and a triode

answers: NDQ_003239

answers: drift tube like a klystron

answers: NDQ_003240

answers: Klystron

answers: NDQ_003241

answers: An axial magnetic field

answers: NDQ_003242

answers: drift tube

answers: NDQ_003244

answers: continent

answers: NDQ_003246

answers: continents

answers: NDQ_003247

answers: drift tube

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: unanswerable

answers: NDQ_003254

answers: IOTs

answers: NDQ_003255

answers: high frequency RF voltage on the grid allows the electrons through in bunches

answers: NDQ_003256

answers: The bunched electron beam passes through the hollow anode

answers: NDQ_003257

answers: Pangaea

answers: NDQ_003258

answers: unanswerable

text: The reasons for voyaging vary from recreation to one way trips for colonization.  Some of these were accidental and achieved by drifting rather than sailing. Many canoes which storm-drifted to the Philippines from the Yap region made successful returns home. But because of prevailing winds, westerly drifts are far more common than easterly. Tahiti to Hawaii, 2000 miles across the prevailing winds is impossible to drift but fine for sailing. Arriving at Easter Island must have been fortuitous. Raiding and conquest were a traditional motive.

text: The reasons for voyaging vary from recreation to one way trips for colonization.  Some of these were accidental and achieved by drifting rather than sailing. Many canoes which storm-drifted to the

text: Philippines

text: from the

text: Yap

text: region made successful returns home. But because of prevailing winds, westerly drifts are far more common than easterly.

text: Tahiti

text: to

text: Hawaii

text: , 2000 miles across the prevailing winds is impossible to drift but fine for sailing. Arriving at

text: Easter Island

text: must have been fortuitous. Raiding and conquest were a traditional motive.

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answers: 0

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answers: 0

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answers: 0

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answers: 4

answers: tqa2:L_0076/T_0762/f796d969186fb510d04d66dce1ae35e7

answers: 0

answers: tqa2:L_0076/T_0763/896ff43d2f7e77ad28826b49bac52744

answers: 0

answers: tqa2:L_0076/T_0763/fd681b49e2c03d0739c38fe5359da5f9

answers: 0

answers: tqa2:L_0076/T_0763/bedb1a7ca86f62fc769ad0962c5e194e

answers: 0

answers: tqa2:L_0076/T_0763/0c8f00338a2b79498081fa1418fb4dc8

answers: 0

answers: tqa2:L_0076/T_0763/1a8478e827d477fb60df2e5d5db61c15

answers: 0

answers: tqa2:L_0076/T_0763/e9a7f23543f06d61ea25a4487734c47c

answers: 0

answers: tqa2:L_0076/T_0763/76c6b32f924d16e4968b987ee335032b

answers: 0

answers: tqa2:L_0076/T_0763/3e749bce73370e3289eb5602e4cc94c3

answers: 0

answers: tqa2:L_0076/T_0763/17772420e6087d05eb83b3f0cc3aa451

answers: 0

answers: tqa2:L_0076/T_0763/7a7192cbfb0cdb83fb089d3c4f8ea239

answers: 0

answers: NDQ_003219

answers: 0

answers: NDQ_003220

answers: 0

answers: NDQ_003221

answers: 0

answers: NDQ_003222

answers: 2

answers: NDQ_003223

answers: 0

answers: NDQ_003224

answers: 0

answers: NDQ_003225

answers: 0

answers: NDQ_003226

answers: 0

answers: NDQ_003227

answers: 0

answers: NDQ_003228

answers: 0

answers: NDQ_003230

answers: 0

answers: NDQ_003231

answers: 0

answers: NDQ_003233

answers: 0

answers: NDQ_003236

answers: 0

answers: NDQ_003237

answers: 0

answers: NDQ_003239

answers: 4

answers: NDQ_003240

answers: 0

answers: NDQ_003241

answers: 0

answers: NDQ_003242

answers: 0

answers: NDQ_003244

answers: 0

answers: NDQ_003246

answers: 4

answers: NDQ_003247

answers: 4

answers: NDQ_003252

answers: 4

answers: NDQ_003253

answers: 0

answers: NDQ_003254

answers: 0

answers: NDQ_003255

answers: 4

answers: NDQ_003256

answers: 0

answers: NDQ_003257

answers: 0

answers: NDQ_003258

answers: 0

answers: NDQ_003219

answers: drifting

answers: NDQ_003220

answers: Tahiti

answers: NDQ_003221

answers: colonization

answers: NDQ_003222

answers: Tahiti to Hawaii

answers: NDQ_003223

answers: Easter Island

answers: NDQ_003224

answers: Easter Island

answers: NDQ_003225

answers: drifting

answers: NDQ_003226

answers: Tahiti

answers: NDQ_003227

answers: colonization

answers: NDQ_003228

answers: colonization

answers: NDQ_003230

answers: Philippines

answers: NDQ_003231

answers: region

answers: NDQ_003233

answers: Tahiti to Hawaii

answers: NDQ_003236

answers: Drifting

answers: NDQ_003237

answers: Tahiti to Hawaii

answers: NDQ_003239

answers: Tahiti to Hawaii

answers: NDQ_003240

answers: Yap

answers: NDQ_003241

answers: no

answers: NDQ_003242

answers: prevailing winds

answers: NDQ_003244

answers: Tahiti

answers: NDQ_003246

answers: continents have never been together as a single whole continent

answers: NDQ_003247

answers: Tahiti to Hawaii

answers: NDQ_003252

answers: plate tectonics

answers: NDQ_003253

answers: Tahiti to Hawaii

answers: NDQ_003254

answers: It was widely accepted

answers: NDQ_003255

answers: Some of these were accidental and achieved by drifting

answers: NDQ_003256

answers: Easter Island

answers: NDQ_003257

answers: Pangaea

answers: NDQ_003258

answers: because of prevailing winds

text: Designated as having a humid continental climate, this region typically has a large seasonal temperature differences, with warm to hot (and often humid) summers and cold (sometimes severely cold) winters. Precipitation is relatively well distributed year-round in many areas with this climate.  The Köppen Climate Classification subtype for this climate is "Dfa". (Hot Summer Continental Climate).

text: Designated as having a humid continental climate, this region typically has a large seasonal temperature differences, with warm to hot (and often humid) summers and cold (sometimes severely cold) winters. Precipitation is relatively well distributed year-round in many areas with this climate.  The

text: Köppen Climate Classification

text: subtype for this climate is "

text: Dfa

text: ". (Hot Summer Continental Climate).

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text: The perspective returns to Earth and the film continuity, where Bumblebee and Drift work their way through canyons which lead to Lockdown's stronghold. Drift is captured, and Bumblebee is left to rescue him. The two battle insurmountable forces, and at their most desperate moment Grimlock bursts into the stronghold and comes to their rescue. Lockdown escapes, fleeing to a second site where he intends to open a time bridge and begin the Autobot and Decepticon war anew. Grimlock, Bumblebee, Drift and Optimus work their way through the city to the entrance of Lockdown's base. Optimus bests Lockdown in combat, and the final shard of the Dark Spark is ejected from Lockdown's body by Drift's sword. Optimus uses a beam from the Matrix of Leadership stored within his chest to destroy the Dark Spark shard.

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text: The geology of the UK is complex and diverse, a result of it being subject to a variety of plate tectonic processes over a very extended period of time. Changing latitude and sea levels have been important factors in the nature of sedimentary sequences, whilst successive continental collisions have affected its geological structure with major faulting and folding being a legacy of each orogeny (mountain-building period), often associated with volcanic activity and the metamorphism of existing rock sequences. As a result of this eventful geological history, the UK shows a rich variety of landscapes.

text: The geology of the UK is complex and diverse, a result of it being subject to a variety of

text: plate tectonic

text: processes over a very extended period of time. Changing latitude and sea levels have been important factors in the nature of sedimentary sequences, whilst successive continental collisions have affected its

text: geological structure

text: with major faulting and folding being a legacy of each

text: orogeny

text: (mountain-building period), often associated with

text: volcanic

text: activity and the metamorphism of existing rock sequences. As a result of this eventful geological history, the UK shows a rich variety of

text: landscape

text: s.

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answers: the UK shows a rich variety of landscapes

answers: NDQ_003223

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answers: NDQ_003225

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answers: plate tectonic

text: The glacial history of Minnesota is most defined since the onset of the last glacial period, which ended some 10,000 years ago. Within the last million years, most of the Midwestern United States and much of Canada were covered at one time or another with an ice sheet. This continental glacier had a profound effect on the surface features of the area over which it moved. Vast quantities of rock and soil were scraped from the glacial centers to its margins by slowly moving ice and redeposited as drift or till. Much of this drift was dumped into old preglacial river valleys, while some of it was heaped into belts of hills (terminal moraines) at the margin of the glacier. The chief result of glaciation has been the modification of the preglacial topography by the deposition of drift over the countryside. However, continental glaciers possess great power of erosion and may actually modify the preglacial land surface by scouring and abrading rather than by the deposition of the drift.

text: The glacial history of

text: Minnesota

text: is most defined since the onset of the

text: last glacial period

text: , which ended some 10,000 years ago. Within the last million years, most of the

text: Midwestern United States

text: and much of

text: Canada

text: were covered at one time or another with an

text: ice sheet

text: . This continental

text: glacier

text: had a profound effect on the surface features of the area over which it moved. Vast quantities of rock and soil were scraped from the glacial centers to its margins by slowly moving ice and redeposited as

text: drift

text: or

text: till

text: . Much of this drift was dumped into old preglacial river valleys, while some of it was heaped into belts of hills (

text: terminal moraine

text: s) at the margin of the glacier. The chief result of glaciation has been the modification of the preglacial

text: topography

text: by the deposition of drift over the countryside. However, continental glaciers possess great power of erosion and may actually modify the preglacial land surface by scouring and abrading rather than by the deposition of the drift.

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answers: NDQ_003219

answers: glaciers possess great power of erosion

answers: NDQ_003220

answers: Canada

answers: NDQ_003221

answers: glacial period

answers: NDQ_003222

answers: may actually modify the preglacial land surface by scouring and abrading

answers: NDQ_003223

answers: 10,000 years ago

answers: NDQ_003224

answers: river valleys

answers: NDQ_003225

answers: The chief result of glaciation

answers: NDQ_003226

answers: Canada

answers: NDQ_003227

answers: scouring and abrading rather than by the deposition of the drift

answers: NDQ_003228

answers: glacial history of Minnesota

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: magnetic field

answers: NDQ_003233

answers: Vast quantities of rock and soil were scraped from the glacial centers to its margins by slowly moving ice

answers: NDQ_003236

answers: Vast quantities of rock and soil were scraped from the glacial centers to its margins by slowly moving ice

answers: NDQ_003237

answers: Vast quantities of rock and soil were scraped from the glacial centers to its margins by slowly moving ice

answers: NDQ_003239

answers: Vast quantities of rock and soil were scraped from the glacial centers to its margins

answers: NDQ_003240

answers: North America

answers: NDQ_003241

answers: The glacial history of Minnesota

answers: NDQ_003242

answers: glaciation

answers: NDQ_003244

answers: drift

answers: NDQ_003246

answers: United States and much of Canada

answers: NDQ_003247

answers: Much of this drift was dumped into old preglacial river valleys

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: continents

answers: NDQ_003254

answers: It was widely accepted as soon as it was introduced

answers: NDQ_003255

answers: Vast quantities of rock and soil were scraped from the glacial centers to its margins

answers: NDQ_003256

answers: The chief result of glaciation

answers: NDQ_003257

answers: Pangaea

answers: NDQ_003258

answers: slowly moving ice and redeposited as drift or till

text: Also called range fragmentation, disjunct distributions may be caused by changes in the environment, such as mountain building and continental drift or rising sea levels; it may also be due to an organism expanding its range into new areas, by such means as rafting, or other animals transporting an organism to a new location (plant seeds consumed by birds and animals, can be moved to new locations during bird or animals migrations, and those seeds can be deposited in new locations in fecal matter). Other conditions that can produce disjunct distributions include: flooding, or changes in wind, stream, and current flows, plus others such as anthropogenic introduction of alien introduced species either accidentally or deliberately (agriculture and horticulture).

text: Also called range fragmentation, disjunct distributions may be caused by changes in the environment, such as

text: mountain building

text: and

text: continental drift

text: or rising

text: sea level

text: s; it may also be due to an

text: organism

text: expanding its range into new areas, by such means as

text: rafting

text: , or other animals transporting an organism to a new location (plant seeds consumed by birds and animals, can be moved to new locations during bird or animals migrations, and those seeds can be deposited in new locations in fecal matter). Other conditions that can produce disjunct distributions include: flooding, or changes in wind, stream, and current flows, plus others such as anthropogenic introduction of alien

text: introduced species

text: either accidentally or deliberately (agriculture and horticulture).

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answers: NDQ_003223

answers: rising sea levels

answers: NDQ_003224

answers: mountain building

answers: NDQ_003225

answers: range fragmentation

answers: NDQ_003226

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answers: NDQ_003227

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answers: NDQ_003230

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text: Magnet therapy has been promoted as a treatment for cancer and other diseases; the American Cancer Society states that "available scientific evidence does not support these claims". According to the National Center for Complementary and Integrative Health, studies of magnetic jewelry haven’t shown demonstrable effects on pain, nerve function, cell growth or blood flow.

text: Magnet therapy has been promoted as a treatment for cancer and other diseases; the

text: American Cancer Society

text: states that "available scientific evidence does not support these claims". According to the

entity_name: National Center for Complementary and Integrative Health

text: National Center for Complementary and Integrative Health

text: , studies of magnetic jewelry haven’t shown demonstrable effects on pain, nerve function, cell growth or blood flow.

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answers: available scientific evidence does not support these claims

answers: NDQ_003220

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answers: American Cancer Society

answers: NDQ_003222

answers: available scientific evidence does not support these claims

answers: NDQ_003223

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answers: NDQ_003224

answers: Magnet therapy

answers: NDQ_003225

answers: Magnet therapy

answers: NDQ_003226

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answers: Magnet therapy has been promoted as a treatment for cancer and other diseases

answers: NDQ_003228

answers: magnetic

answers: NDQ_003230

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answers: NDQ_003231

answers: magnet

answers: NDQ_003233

answers: available scientific evidence does not support these claims

answers: NDQ_003236

answers: The American Cancer Society

answers: NDQ_003237

answers: available scientific evidence

answers: NDQ_003239

answers: similar fossil records across continents

answers: NDQ_003240

answers: North America

answers: NDQ_003241

answers: Magnetic north pole

answers: NDQ_003242

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answers: NDQ_003244

answers: The American Cancer Society

answers: NDQ_003246

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answers: NDQ_003247

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answers: NDQ_003252

answers: Magnet therapy

answers: NDQ_003253

answers: Magnet therapy has been promoted as a treatment for cancer

answers: NDQ_003254

answers: The American Cancer Society

answers: NDQ_003255

answers: available scientific evidence does not support these claims

answers: NDQ_003256

answers: Magnet therapy

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answers: Magnet therapy

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.

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answers: the evidence was equally in support of continental drift

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answers: other work would soon show that the evidence was equally in support of continental drift

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answers: the evidence was equally in support of continental drift

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answers: This was immediately followed by a symposium in Tasmania in March 1956

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answers: evidence was used in the theory of an expansion of the global crust

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answers: This was immediately followed by a symposium in Tasmania in March 1956

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answers: theory of an expansion of the global crust

text: Granitic rocks represent the roots of ancient continental-margin volcanic systems. Most of the granitic rock in the Mojave Desert is late Mesozoic in age (80 to 180 million years old). The granites formed at depth within a volcanically active mountain range comparable in geologic setting to the Andes chain in South America.

text: Granitic rocks represent the roots of ancient

text: continental-margin

text: volcanic systems. Most of the granitic rock in the Mojave Desert is late

text: Mesozoic

text: in age (80 to 180 million years old). The granites formed at depth within a volcanically active mountain range comparable in geologic setting to the

text: Andes

text: chain in

text: South America

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answers: continental-margin volcanic systems

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answers: Andes chain

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answers: Mesozoic

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answers: the Andes chain

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answers: late Mesozoic

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answers: Late Mesozoic

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answers: the roots of ancient continental-margin volcanic systems

answers: NDQ_003226

answers: South America

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answers: ancient continental-margin volcanic systems

answers: NDQ_003228

answers: geologic setting

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answers: Europe

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answers: margin

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answers: Granitic rocks represent the roots of ancient continental-margin volcanic systems

answers: NDQ_003236

answers: continental-margin volcanic systems

answers: NDQ_003237

answers: Granitic rocks

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answers: The Andes chain

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answers: Mesozoic

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answers: The Andes chain

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answers: Mesozoic

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answers: continental-margin volcanic systems

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answers: Andes chain

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answers: The Andes chain in South America

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: Andes chain

answers: NDQ_003254

answers: Wegener hypothesis of continental drift

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answers: The Andes chain in South America

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answers: The Andes chain

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answers: Pangaea

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answers: The Andes chain

text: The Dutch version of the DVD produced by Evangelische Omroep removed all references to (amongst others) evolution, fossils, and continental drift. The narration by David Attenborough has been replaced by a not always accurate Dutch translation, and cuts were made to the episodes. The tenth episode was not broadcast at all on Evangelische Omroep, and is not included on the EO DVD of the series. The Dutch version of the book includes the full text of the original book, as did the Dutch language version of the programme broadcast on the Belgian broadcaster Canvas.

text: The Dutch version of the DVD produced by

text: Evangelische Omroep

text: removed all references to (amongst others) evolution, fossils, and continental drift. The narration by David Attenborough has been replaced by a not always accurate Dutch translation, and cuts were made to the episodes. The tenth episode was not broadcast at all on

text: Evangelische Omroep

text: , and is not included on the EO DVD of the series. The Dutch version of the book includes the full text of the original book, as did the

text: Dutch language

text: version of the programme broadcast on the Belgian broadcaster

text: Canvas

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answers: NDQ_003219

answers: continental drift

answers: NDQ_003220

answers: continental drift

answers: NDQ_003221

answers: late 19th century

answers: NDQ_003222

answers: not always accurate Dutch translation

answers: NDQ_003223

answers: continental drift

answers: NDQ_003224

answers: fossils

answers: NDQ_003225

answers: evolution

answers: NDQ_003226

answers: Europe

answers: NDQ_003227

answers: evolution

answers: NDQ_003228

answers: continental drift

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: magnetic field

answers: NDQ_003233

answers: fossils

answers: NDQ_003236

answers: continental drift

answers: NDQ_003237

answers: fossils

answers: NDQ_003239

answers: fossil records

answers: NDQ_003240

answers: continental drift

answers: NDQ_003241

answers: no

answers: NDQ_003242

answers: continental drift

answers: NDQ_003244

answers: continental drift

answers: NDQ_003246

answers: continental drift

answers: NDQ_003247

answers: fossils

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: continental drift

answers: NDQ_003254

answers: The Dutch version

answers: NDQ_003255

answers: fossils

answers: NDQ_003256

answers: continental drift

answers: NDQ_003257

answers: The Evangelische Omroep

answers: NDQ_003258

answers: continental drift

text: Tropical savanna climates have monthly mean temperature above 18 °C (64 °F) in every month of the year and typically a pronounced dry season, with the driest month having precipitation less than 60mm (2.36 in) of precipitation. In essence, a tropical savanna climate tends to either see less rainfall than a tropical monsoon climate or have more pronounced dry seasons than a tropical monsoon climate.  The Köppen Climate Classification subtype for this climate is "As". (Tropical Savanna Climate).

text: Tropical savanna climates have monthly mean temperature above 18 °C (64 °F) in every month of the year and typically a pronounced dry season, with the driest month having precipitation less than 60mm (2.36 in) of precipitation. In essence, a tropical savanna climate tends to either see less rainfall than a tropical monsoon climate or have more pronounced dry seasons than a tropical monsoon climate.  The

text: Köppen Climate Classification

text: subtype for this climate is "

text: As

text: ". (Tropical Savanna Climate).

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answers: NDQ_003224

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answers: NDQ_003226

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answers: NDQ_003227

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answers: NDQ_003239

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answers: NDQ_003252

answers: 4

answers: NDQ_003253

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answers: NDQ_003255

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answers: NDQ_003256

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answers: NDQ_003257

answers: 0

answers: NDQ_003258

answers: 0

answers: NDQ_003219

answers: climates have monthly mean temperature above 18 °C

answers: NDQ_003220

answers: Atlantic Ocean

answers: NDQ_003221

answers: late 19th century

answers: NDQ_003222

answers: tropical savanna climate

answers: NDQ_003223

answers: Tropical Savanna Climate

answers: NDQ_003224

answers: tropical savanna climate

answers: NDQ_003225

answers: Tropical Savanna Climate

answers: NDQ_003226

answers: Tropical Savanna climate

answers: NDQ_003227

answers: continental drift

answers: NDQ_003228

answers: pronounced dry season

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: magnetic field

answers: NDQ_003233

answers: Tropical Savanna Climate

answers: NDQ_003236

answers: continents move

answers: NDQ_003237

answers: The Köppen Climate Classification subtype for this climate is "As". (Tropical Savanna Climate)

answers: NDQ_003239

answers: continental drift

answers: NDQ_003240

answers: North America

answers: NDQ_003241

answers: The magnetic north pole and geographic north pole

answers: NDQ_003242

answers: continental drift

answers: NDQ_003244

answers: Tropical Savanna Climate

answers: NDQ_003246

answers: The continents have never been together

answers: NDQ_003247

answers: Tropical Savanna Climate

answers: NDQ_003252

answers: plate tectonics

answers: NDQ_003253

answers: Tropical Savanna Climate

answers: NDQ_003254

answers: Tropical savanna climates

answers: NDQ_003255

answers: Wegener and his supporters provided a lot of evidence for continental drift

answers: NDQ_003256

answers: Tropical Savanna Climate

answers: NDQ_003257

answers: Pangaea

answers: NDQ_003258

answers: The Köppen Climate Classification

text: Peaches is the daughter of Manny and Ellie, born in the Dinosaurs' world whilst they were under attack by a pack of Guanlong. She appeared close to end of Ice Age: Dawn of the Dinosaurs and was named after the code-word that was thought up to say that Ellie was going into labour. Manny also claims that peaches are sweet, round and fuzzy, just like Peaches and Ellie. She looks exactly like her mother, Ellie (which Sid thinks is very lucky). At the end of the film, she returned to the surface with her parents and the rest of the group. She is voiced by Ciara Bravo in Ice Age: A Mammoth Christmas and Keke Palmer in Ice Age: Continental Drift.

text: Peaches is the daughter of

text: Manny

text: and

text: Ellie

text: , born in the Dinosaurs' world whilst they were under attack by a pack of Guanlong. She appeared close to end of Ice Age: Dawn of the Dinosaurs and was named after the code-word that was thought up to say that Ellie was going into labour. Manny also claims that

text: peach

text: es are sweet, round and fuzzy, just like Peaches and Ellie. She looks exactly like her mother, Ellie (which Sid thinks is very lucky). At the end of the film, she returned to the surface with her parents and the rest of the group. She is voiced by

text: Ciara Bravo

text: in

text: Ice Age: A Mammoth Christmas

text: and

text: Keke Palmer

text: in

text: Ice Age: Continental Drift

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answers: NDQ_003220

answers: Continental

answers: NDQ_003221

answers: Dinosaurs

answers: NDQ_003222

answers: Dinosaurs

answers: NDQ_003223

answers: Guanlong

answers: NDQ_003224

answers: Dinosaurs

answers: NDQ_003225

answers: code-word

answers: NDQ_003226

answers: Antarctica

answers: NDQ_003227

answers: Ice Age: Continental Drift

answers: NDQ_003228

answers: continental drift

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: surface

answers: NDQ_003233

answers: Ice Age: Continental Drift

answers: NDQ_003236

answers: Ice Age: Continental Drift

answers: NDQ_003237

answers: Ice Age: Continental Drift

answers: NDQ_003239

answers: Ice Age: Continental Drift

answers: NDQ_003240

answers: dinosaurs' world

answers: NDQ_003241

answers: The magnetic north pole

answers: NDQ_003242

answers: continental drift

answers: NDQ_003244

answers: continental drift

answers: NDQ_003246

answers: Ice Age: Continental Drift

answers: NDQ_003247

answers: Peaches are sweet, round and fuzzy

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: continents were once joined together

answers: NDQ_003254

answers: It was widely accepted

answers: NDQ_003255

answers: Peaches

answers: NDQ_003256

answers: Continental Drift

answers: NDQ_003257

answers: Pangaea

answers: NDQ_003258

answers: Continental Drift

text: Jack Wills’s researches started with the plant and animal fossils of the Keuper sediments exposed in quarries around Bromsgrove, and he retained a lifelong interest in the continental deposits and fossils of the Upper Paleozoic and Triassic.

text: Jack Wills’s researches started with the plant and animal fossils of the

text: Keuper sediment

text: s exposed in quarries around

text: Bromsgrove

text: , and he retained a lifelong interest in the continental deposits and fossils of the

text: Upper Paleozoic

text: and

text: Triassic

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answers: NDQ_003253

answers: 0

answers: NDQ_003254

answers: 0

answers: NDQ_003255

answers: 4

answers: NDQ_003256

answers: 0

answers: NDQ_003257

answers: 0

answers: NDQ_003258

answers: 0

answers: NDQ_003219

answers: continental deposits and fossils

answers: NDQ_003220

answers: Keuper

answers: NDQ_003221

answers: Paleozoic

answers: NDQ_003222

answers: fossils of the Upper Paleozoic and Triassic

answers: NDQ_003223

answers: Triassic

answers: NDQ_003224

answers: fossils

answers: NDQ_003225

answers: Keuper sediments

answers: NDQ_003226

answers: Europe

answers: NDQ_003227

answers: fossils

answers: NDQ_003228

answers: Jack Wills’s researches

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: Keuper

answers: NDQ_003233

answers: Jack Wills

answers: NDQ_003236

answers: continental deposits

answers: NDQ_003237

answers: Keuper sediments

answers: NDQ_003239

answers: Keuper sediments

answers: NDQ_003240

answers: Keuper

answers: NDQ_003241

answers: Bromsgrove

answers: NDQ_003242

answers: Paleozoic

answers: NDQ_003244

answers: Keuper

answers: NDQ_003246

answers: The continents have never been together as a single whole continent

answers: NDQ_003247

answers: Keuper sediments

answers: NDQ_003252

answers: continental deposits and fossils

answers: NDQ_003253

answers: Keuper sediments

answers: NDQ_003254

answers: Keuper sediments

answers: NDQ_003255

answers: Keuper sediments

answers: NDQ_003256

answers: Wegener

answers: NDQ_003257

answers: Pangaea

answers: NDQ_003258

answers: Wegener

text: Fossils of plant leaves, shoots, seeds, flowers and cones are abundant and well preserved, and include up to 76 genera of plants. Fossil plants described from the fossil beds include rare flowers such as Dipteronia, a genus of trees related to maples (Acer. spp.) that today grows in eastern Asia, extinct members of the birch family (Betulaceae) such as Palaeocarpinus, maple seeds (Acer rousei), and fruits and leaves of a beech (''Fagus langevinii'') and an elm (''Ulmus okanaganensis'').

text: Fossils of plant leaves, shoots, seeds, flowers and cones are abundant and well preserved, and include up to 76

text: genera

text: of plants. Fossil plants described from the fossil beds include rare flowers such as

text: Dipteronia

text: , a genus of trees related to maples (

text: Acer

text: . spp.) that today grows in eastern Asia, extinct members of the birch family (

text: Betulaceae

text: ) such as Palaeocarpinus, maple seeds (

text: Acer rousei

text: ), and fruits and leaves of a

text: beech

text: (''Fagus langevinii'') and an elm (''Ulmus okanaganensis'').

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answers: 0

answers: NDQ_003219

answers: 0

answers: NDQ_003220

answers: 0

answers: NDQ_003221

answers: 0

answers: NDQ_003222

answers: 0

answers: NDQ_003223

answers: 0

answers: NDQ_003224

answers: 0

answers: NDQ_003225

answers: 0

answers: NDQ_003226

answers: 0

answers: NDQ_003227

answers: 0

answers: NDQ_003228

answers: 0

answers: NDQ_003230

answers: 0

answers: NDQ_003231

answers: 0

answers: NDQ_003233

answers: 0

answers: NDQ_003236

answers: 0

answers: NDQ_003237

answers: 0

answers: NDQ_003239

answers: 0

answers: NDQ_003240

answers: 0

answers: NDQ_003241

answers: 0

answers: NDQ_003242

answers: 0

answers: NDQ_003244

answers: 0

answers: NDQ_003246

answers: 0

answers: NDQ_003247

answers: 0

answers: NDQ_003252

answers: 4

answers: NDQ_003253

answers: 0

answers: NDQ_003254

answers: 0

answers: NDQ_003255

answers: 4

answers: NDQ_003256

answers: 0

answers: NDQ_003257

answers: 0

answers: NDQ_003258

answers: 0

answers: NDQ_003219

answers: extinct members of the birch family

answers: NDQ_003220

answers: Kanagan

answers: NDQ_003221

answers: late Cretaceous

answers: NDQ_003222

answers: fossils are abundant and well preserved

answers: NDQ_003223

answers: fossil beds

answers: NDQ_003224

answers: fossil beds

answers: NDQ_003225

answers: Fossil plants

answers: NDQ_003226

answers: Asia

answers: NDQ_003227

answers: fossil plants described from the fossil beds

answers: NDQ_003228

answers: fossil beds

answers: NDQ_003230

answers: Asia

answers: NDQ_003231

answers: magnetic field

answers: NDQ_003233

answers: Palaeocarpinus

answers: NDQ_003236

answers: Fossil beds

answers: NDQ_003237

answers: Fossils

answers: NDQ_003239

answers: abundant and well preserved

answers: NDQ_003240

answers: North America

answers: NDQ_003241

answers: Asia

answers: NDQ_003242

answers: Palaeocarpinus

answers: NDQ_003244

answers: Fossil beds

answers: NDQ_003246

answers: The continents have never been together as a single whole continent

answers: NDQ_003247

answers: Fossil beds

answers: NDQ_003252

answers: plate tectonics

answers: NDQ_003253

answers: Asia

answers: NDQ_003254

answers: Fossils of plant leaves

answers: NDQ_003255

answers: Fossils

answers: NDQ_003256

answers: Fossils

answers: NDQ_003257

answers: Pangaea

answers: NDQ_003258

answers: Fossils of plant leaves

text: The second piece of evidence in support of continental drift came during the late 1950s and early 60s from data on the bathymetry of the deep ocean floors and the nature of the oceanic crust such as magnetic properties and, more generally, with the development of marine geology which gave evidence for the association of seafloor spreading along the mid-oceanic ridges and magnetic field reversals, published between 1959 and 1963 by Heezen, Dietz, Hess, Mason, Vine & Matthews, and Morley.

text: The second piece of evidence in support of continental drift came during the late 1950s and early 60s from data on the bathymetry of the deep

text: ocean floor

text: s and the nature of the oceanic crust such as magnetic properties and, more generally, with the development of

text: marine geology

text: which gave evidence for the association of seafloor spreading along the

text: mid-oceanic ridge

text: s and

text: magnetic field reversals

text: , published between 1959 and 1963 by Heezen, Dietz, Hess, Mason, Vine & Matthews, and Morley.

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answers: continental drift

answers: NDQ_003220

answers: Mid-oceanic

answers: NDQ_003221

answers: 1960s

answers: NDQ_003222

answers: the nature of the oceanic crust such as magnetic properties

answers: NDQ_003223

answers: continental drift

answers: NDQ_003224

answers: seafloor spreading

answers: NDQ_003225

answers: continental drift

answers: NDQ_003226

answers: oceanic crust

answers: NDQ_003227

answers: association of seafloor spreading along the mid-oceanic ridges

answers: NDQ_003228

answers: published between 1959 and 1963

answers: NDQ_003230

answers: South America

answers: NDQ_003231

answers: magnetic field

answers: NDQ_003233

answers: Heezen, Dietz, Hess, Mason, Vine & Matthews

answers: NDQ_003236

answers: continental drift

answers: NDQ_003237

answers: magnetic properties and, more generally, with the development of marine geology

answers: NDQ_003239

answers: The second piece of evidence in support of continental drift

answers: NDQ_003240

answers: continental drift

answers: NDQ_003241

answers: no

answers: NDQ_003242

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answers: NDQ_003244

answers: mid-oceanic ridges

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answers: NDQ_003247

answers: mid-oceanic ridges

answers: NDQ_003252

answers: plate tectonics

answers: NDQ_003253

answers: continental drift

answers: NDQ_003254

answers: It was widely accepted

answers: NDQ_003255

answers: Heezen, Dietz, Hess, Mason, Vine & Matthews, and Morley

answers: NDQ_003256

answers: Mid-oceanic ridges and magnetic field reversals

answers: NDQ_003257

answers: The second piece of evidence in support of continental drift

answers: NDQ_003258

answers: continental drift

text: The speculation that continents might have 'drifted' was first put forward by Abraham Ortelius in 1596. The concept was independently and more fully developed by Alfred Wegener in 1912. Because Wegener's publications were widely available in German and English and because he adduced geological support for the idea, he is credited by most geologists as the first to recognize the possibility of continental drift. During the 1960s geophysical and geological evidence for seafloor spreading at mid-oceanic ridges established continental drift as the standard theory or continental origin and an ongoing global mechanism.

text: The speculation that

text: continent

text: s might have 'drifted' was first put forward by

text: Abraham Ortelius

text: in 1596. The concept was independently and more fully developed by

text: Alfred Wegener

text: in 1912. Because Wegener's publications were widely available in German and English and because he adduced geological support for the idea, he is credited by most geologists as the first to recognize the possibility of

text: continental drift

text: . During the 1960s geophysical and geological evidence for seafloor spreading at mid-oceanic ridges established continental drift as the standard theory or continental origin and an ongoing global mechanism.

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answers: 5

answers: NDQ_003219

answers: continental drift

answers: NDQ_003220

answers: mid-oceanic ridges

answers: NDQ_003221

answers: 1596

answers: NDQ_003222

answers: Abraham Ortelius

answers: NDQ_003223

answers: continental drift

answers: NDQ_003224

answers: seafloor spreading

answers: NDQ_003225

answers: continental drift

answers: NDQ_003226

answers: German

answers: NDQ_003227

answers: the possibility of continental drift

answers: NDQ_003228

answers: first to recognize the possibility of continental drift

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: mid-oceanic

answers: NDQ_003233

answers: 1960s

answers: NDQ_003236

answers: continental drift

answers: NDQ_003237

answers: During the 1960s

answers: NDQ_003239

answers: seafloor spreading at mid-oceanic ridges

answers: NDQ_003240

answers: North America

answers: NDQ_003241

answers: no

answers: NDQ_003242

answers: continental drift

answers: NDQ_003244

answers: mid-oceanic ridges

answers: NDQ_003246

answers: continents might have drifted

answers: NDQ_003247

answers: mid-oceanic ridges

answers: NDQ_003252

answers: Alfred Wegener

answers: NDQ_003253

answers: continents might have 'drifted'

answers: NDQ_003254

answers: During the 1960s

answers: NDQ_003255

answers: During the 1960s

answers: NDQ_003256

answers: It is not possible to tell

answers: NDQ_003257

answers: continents might have 'drifted'

answers: NDQ_003258

answers: The concept was independently and more fully developed

text: Ari Brynjolfsson was born in Akureyri, Iceland, one of the seven children of Brynjólf Sigtryggsson and Guðrún Rósinkarsdóttir from Hörgárdalur. He lived in  Krossanes, Eyjafjörður and graduated from Menntaskólinn á Akureyri in 1948, then studied nuclear physics at the Niels Bohr Institute, University of Copenhagen, Denmark, from 1948 to 1954, gaining his PhD, with a thesis which dealt with a device he had constructed for accurately measuring magnetism in rocks. Following this he became a special research fellow of the University of Iceland from 1954 to 1955, then an Alexander von Humboldt fellow of the University of Göttingen, Germany, from 1955 to 1957. While at Göttingen he contributed important work in magnetic moments, using a self-devised instrument with which he and others provided the strongest evidence to that date for magnetic field reversals.

text: Ari Brynjolfsson was born in

text: Akureyri, Iceland

text: , one of the seven children of Brynjólf Sigtryggsson and Guðrún Rósinkarsdóttir from Hörgárdalur. He lived in  Krossanes,

text: Eyjafjörður

text: and graduated from

text: Menntaskólinn á Akureyri

text: in 1948, then studied

text: nuclear physics

text: at the

text: Niels Bohr Institute

text: University of Copenhagen

text: , Denmark, from 1948 to 1954, gaining his PhD, with a thesis which dealt with a device he had constructed for accurately measuring magnetism in rocks. Following this he became a special research fellow of the

text: University of Iceland

text: from 1954 to 1955, then an

text: Alexander von Humboldt

text: fellow of the

text: University of Göttingen

text: , Germany, from 1955 to 1957. While at Göttingen he contributed important work in

text: magnetic moment

text: s, using a self-devised instrument with which he and others provided the strongest evidence to that date for

text: magnetic field reversal

text: s.

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answers: magnetic field reversals

answers: NDQ_003220

answers: Hörgárdalur

answers: NDQ_003221

answers: Göttingen

answers: NDQ_003222

answers: magnetic field reversals

answers: NDQ_003223

answers: Iceland

answers: NDQ_003224

answers: rocks

answers: NDQ_003225

answers: magnetic moments

answers: NDQ_003226

answers: Germany

answers: NDQ_003227

answers: magnetic field reversals

answers: NDQ_003228

answers: While at Göttingen he contributed important work in magnetic moments

answers: NDQ_003230

answers: Europe

answers: NDQ_003231

answers: magnetic field

answers: NDQ_003233

answers: he and others provided the strongest evidence to that date for magnetic field reversals

answers: NDQ_003236

answers: magnetic field reversals

answers: NDQ_003237

answers: magnetic field reversals

answers: NDQ_003239

answers: magnetic field reversals

answers: NDQ_003240

answers: Eritrea

answers: NDQ_003241

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answers: NDQ_003242

answers: field reversals

answers: NDQ_003244

answers: Iceland

answers: NDQ_003246

answers: Iceland

answers: NDQ_003247

answers: rocks

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: magnetic field reversals

answers: NDQ_003254

answers: While at Göttingen he contributed important work in magnetic moments

answers: NDQ_003255

answers: while at Göttingen

answers: NDQ_003256

answers: Göttingen

answers: NDQ_003257

answers: While at Göttingen he contributed important work in magnetic moments

answers: NDQ_003258

answers: magnetic field reversals

text: The Tienen Formation consists of clay with thin lignite layers and lithified wood, sand (sometimes with shells) and marl. It has a continental to lagoonal sedimentary facies. The formation is a lagerstätte for fossils of vertebrate animals.

text: The Tienen Formation consists of

text: clay

text: with thin

text: lignite

text: layers and

text: lithified

text: wood,

text: sand

text: (sometimes with shells) and

text: marl

text: . It has a

text: continental

text: to

text: lagoon

text: al

text: sedimentary facies

text: . The formation is a

text: lagerstätte

text: for

text: fossil

text: s of

text: vertebrate

text: animals.

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answers: NDQ_003219

answers: continental to lagoonal

answers: NDQ_003220

answers: continental

answers: NDQ_003221

answers: geological time

answers: NDQ_003222

answers: fossils of vertebrate animals

answers: NDQ_003223

answers: Tienen Formation

answers: NDQ_003224

answers: fossils

answers: NDQ_003225

answers: Tienen Formation

answers: NDQ_003226

answers: Lagoon

answers: NDQ_003227

answers: continental to lagoonal

answers: NDQ_003228

answers: fossils of vertebrate animals

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: lagerstätte

answers: NDQ_003233

answers: It has a continental to lagoonal sedimentary facies

answers: NDQ_003236

answers: continental to lagoonal

answers: NDQ_003237

answers: fossils of vertebrate animals

answers: NDQ_003239

answers: The Tienen Formation

answers: NDQ_003240

answers: Tienen

answers: NDQ_003241

answers: The Tienen Formation

answers: NDQ_003242

answers: lagoonal

answers: NDQ_003244

answers: Tienen Formation

answers: NDQ_003246

answers: continental

answers: NDQ_003247

answers: continental to lagoonal

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: continental to lagoonal

answers: NDQ_003254

answers: continental to lagoonal sedimentary facies

answers: NDQ_003255

answers: fossils of vertebrate animals

answers: NDQ_003256

answers: continental to lagoonal

answers: NDQ_003257

answers: Pangaea

answers: NDQ_003258

answers: continental to lagoonal

text: The Ouachita Mountains are fold mountains like the Appalachian Mountains to the east, and were originally part of that range. During the Pennsylvanian period, roughly 300 million years ago, the coastline of the Gulf of Mexico ran through the central parts of Arkansas. The South American Plate drifted northward, riding up over the denser North American continental crust. Geologists call this collision the Ouachita orogeny. The collision buckled the overriding plate, producing the fold mountains we call the Ouachitas. At one time the Ouachita Mountains were very similar in height to the current elevations of the Rocky Mountains. Because of the Ouachitas' age, the craggy tops have eroded away, leaving the low formations that used to be the heart of the mountains.

text: The Ouachita Mountains are

text: fold mountain

text: s like the Appalachian Mountains to the east, and were originally part of that range. During the

text: Pennsylvanian

text: period, roughly 300 million years ago, the coastline of the

text: Gulf of Mexico

text: ran through the central parts of Arkansas. The

text: South American Plate

text: drifted northward, riding up over the denser North American

text: continental crust

text: . Geologists call this collision the

text: Ouachita orogeny

text: . The collision buckled the overriding plate, producing the fold mountains we call the Ouachitas. At one time the Ouachita Mountains were very similar in height to the current elevations of the Rocky Mountains. Because of the Ouachitas' age, the craggy tops have eroded away, leaving the low formations that used to be the heart of the mountains.

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answers: NDQ_003219

answers: South American Plate drifted northward, riding up over the denser North American continental crust

answers: NDQ_003220

answers: Appalachian Mountains

answers: NDQ_003221

answers: Pennsylvanian period

answers: NDQ_003222

answers: the collision buckled the overriding plate

answers: NDQ_003223

answers: South American Plate drifted northward

answers: NDQ_003224

answers: the Ouachita Mountains

answers: NDQ_003225

answers: Ouachita orogeny

answers: NDQ_003226

answers: the Rocky Mountains

answers: NDQ_003227

answers: South American Plate drifted northward, riding up over the denser North American continental crust

answers: NDQ_003228

answers: Geologists

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: heart

answers: NDQ_003233

answers: The collision buckled the overriding plate

answers: NDQ_003236

answers: Plate drifted northward

answers: NDQ_003237

answers: The collision buckled the overriding plate

answers: NDQ_003239

answers: During the Pennsylvanian period

answers: NDQ_003240

answers: South American Plate

answers: NDQ_003241

answers: North American continental crust

answers: NDQ_003242

answers: Ouachita orogeny

answers: NDQ_003244

answers: South American Plate drifted

answers: NDQ_003246

answers: The continents have never all been together as a single whole continent

answers: NDQ_003247

answers: the coastline of the Gulf of Mexico ran through the central parts of Arkansas

answers: NDQ_003252

answers: plate tectonics

answers: NDQ_003253

answers: The South American Plate drifted northward

answers: NDQ_003254

answers: The South American Plate drifted northward

answers: NDQ_003255

answers: The collision buckled the overriding plate

answers: NDQ_003256

answers: The collision buckled the overriding plate

answers: NDQ_003257

answers: The collision buckled the overriding plate

answers: NDQ_003258

answers: South American Plate

text: Fossils can be both the direct remains or imprints of organisms and their skeletons. Most commonly preserved are the harder parts of organisms such as bones, shells, and the woody tissue of plants. Soft tissue has a much smaller chance of being fossilized, and the preservation of soft tissue of animals older than 40 million years is very rare. Imprints of organisms made while they were still alive are called trace fossils, examples of which are burrows, footprints, etc.

text: Fossils can be both the direct remains or imprints of organisms and their skeletons. Most commonly preserved are the harder parts of organisms such as bones, shells, and the woody

text: tissue

text: of plants. Soft tissue has a much smaller chance of being fossilized, and the preservation of soft tissue of animals older than 40 million years is very rare. Imprints of organisms made while they were still alive are called

text: trace fossil

text: s, examples of which are

text: burrow

text: s,

text: footprint

text: s, etc.

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answers: 3

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answers: NDQ_003219

answers: fossils can be both the direct remains

answers: NDQ_003220

answers: can be fossilized

answers: NDQ_003221

answers: 19th century

answers: NDQ_003222

answers: preservation of soft tissue of animals older than 40 million years is very rare

answers: NDQ_003223

answers: Fossils

answers: NDQ_003224

answers: Fossils

answers: NDQ_003225

answers: Fossils

answers: NDQ_003226

answers: Europe

answers: NDQ_003227

answers: the preservation of soft tissue of animals older than 40 million years is very rare

answers: NDQ_003228

answers: fossils

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: skeleton

answers: NDQ_003233

answers: Fossils

answers: NDQ_003236

answers: Fossils

answers: NDQ_003237

answers: fossils

answers: NDQ_003239

answers: Fossil records across continents was evidence for continental drift

answers: NDQ_003240

answers: North America

answers: NDQ_003241

answers: no

answers: NDQ_003242

answers: continental drift

answers: NDQ_003244

answers: Fossils

answers: NDQ_003246

answers: Fossils

answers: NDQ_003247

answers: Fossils

answers: NDQ_003252

answers: plate tectonics

answers: NDQ_003253

answers: Fossils

answers: NDQ_003254

answers: It was widely accepted as soon as it was introduced

answers: NDQ_003255

answers: Fossils

answers: NDQ_003256

answers: Fossils

answers: NDQ_003257

answers: Pangaea

answers: NDQ_003258

answers: Fossils

text: The Museum am Löwentor exhibition focuses mainly on fossils from its home state of Baden-Württemberg in southwestern Germany, and other localities in Germany. The state is rich in fossils, including several famous classical localities. Especially well exposed are terrestrial and marine Triassic, marine Jurassic and terrestrial Cenozoic sediments. Therefore, the museum exhibits the early prosauropod dinosaur Plateosaurus and other terrestrial animals from the Lower and Upper Triassic (Buntsandstein and Keuper, respectively), a wide range of marine fossils, mainly invertebrates, from the Muschelkalk, and a plethora of ichthyosaurs, pliosaurs and plesiosaurs, as well as sharks from the Posidonia Shale and other Lower Jurassic formations. Furthermore, exquisite Jurassic ammonites and other invertebrates are shown in large numbers.The Cenozoic is represented by invertebrates and mainly vertebrates from various German localities, including a pleistocene elephant and a copy of a mammuth mummy. Also on exhibit is the skull of the prehistoric man of Steinheim (Homo steinheimensis).The museum also houses a spectacular collection of plant and animal fossils in amber.

text: The Museum am Löwentor exhibition focuses mainly on fossils from its home state of

text: Baden-Württemberg

text: in southwestern Germany, and other localities in Germany. The state is rich in fossils, including several famous classical localities. Especially well exposed are terrestrial and marine

text: Triassic

text: , marine

text: Jurassic

text: and terrestrial

text: Cenozoic

text: sediments. Therefore, the museum exhibits the early

text: prosauropod

text: dinosaur

text: Plateosaurus

text: and other terrestrial animals from the Lower and Upper Triassic (

text: Buntsandstein

text: and

text: Keuper

text: , respectively), a wide range of marine fossils, mainly invertebrates, from the

text: Muschelkalk

text: , and a plethora of

text: ichthyosaur

text: s,

text: pliosaur

text: s and

text: plesiosaur

text: s, as well as

text: shark

text: s from the

text: Posidonia Shale

text: and other

text: Lower Jurassic

text: formations. Furthermore, exquisite Jurassic ammonites and other invertebrates are shown in large numbers.The Cenozoic is represented by invertebrates and mainly vertebrates from various German localities, including a pleistocene elephant and a copy of a mammuth mummy. Also on exhibit is the skull of the prehistoric man of Steinheim (

text: Homo steinheimensis

text: ).The museum also houses a spectacular collection of plant and animal fossils in amber.

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answers: The state is rich in fossils

answers: NDQ_003226

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answers: NDQ_003236

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answers: NDQ_003241

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answers: Pangaea

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answers: The Cenozoic

text: Vértes is a mountain range in north-western Hungary, in the Central Transdanubian region, between the ranges Bakony and Gerecse. The Vértes Mountains are part of the Transdanubian Mountains. Area of the Vértes occupies 314 km. It is about 30 km long and 11c12 km wide. The average altitude is above sea level is 350 meters, in highest points are 487 m (Nagy-Csákány), 480 m (Körtvélyes) and 479 m (Csóka-hegy). Geologically the Vértes constitute a fairlyuniform structure. On the surface of the eptire mountain there are no older rocks than those of the mid-Triassic. The main rock is dolomite—CaMg(CO)—from the upper Triassic. All the layers are ancient marine deposits.

text: Vértes is a

text: mountain range

text: in north-western

text: Hungary

text: , in the Central Transdanubian region, between the ranges

text: Bakony

text: and

text: Gerecse

text: . The Vértes Mountains are part of the

text: Transdanubian Mountains

text: . Area of the Vértes occupies 314 km. It is about 30 km long and 11c12 km wide. The average altitude is above sea level is 350 meters, in highest points are 487 m (Nagy-Csákány), 480 m (Körtvélyes) and 479 m (Csóka-hegy). Geologically the Vértes constitute a fairlyuniform structure. On the surface of the eptire mountain there are no older rocks than those of the mid-Triassic. The main rock is dolomite—CaMg(CO)—from the upper Triassic. All the layers are ancient marine deposits.

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answers: NDQ_003219

answers: the Vértes constitute a fairlyuniform structure

answers: NDQ_003220

answers: Transdanubian Mountains

answers: NDQ_003221

answers: mid-Triassic

answers: NDQ_003222

answers: Vértes constitute a fairlyuniform structure

answers: NDQ_003223

answers: the upper Triassic

answers: NDQ_003224

answers: marine deposits

answers: NDQ_003225

answers: Vértes constitute a fairlyuniform structure

answers: NDQ_003226

answers: Hungary

answers: NDQ_003227

answers: The Vértes constitute a fairlyuniform structure

answers: NDQ_003228

answers: geologist

answers: NDQ_003230

answers: Transdanubian

answers: NDQ_003231

answers: region

answers: NDQ_003233

answers: Geologically the Vértes constitute a fairlyuniform structure

answers: NDQ_003236

answers: The Vértes Mountains are part of the Transdanubian Mountains

answers: NDQ_003237

answers: Vértes constitute a fairlyuniform structure

answers: NDQ_003239

answers: Geologically the Vértes constitute a fairlyuniform structure

answers: NDQ_003240

answers: Transdanubian

answers: NDQ_003241

answers: The Transdanubian Mountains

answers: NDQ_003242

answers: Triassic

answers: NDQ_003244

answers: ancient marine deposits

answers: NDQ_003246

answers: Transdanubian

answers: NDQ_003247

answers: Vértes Mountains are part of the Transdanubian Mountains

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: Transdanubian

answers: NDQ_003254

answers: It is about 30 km long and 11c12 km wide

answers: NDQ_003255

answers: Geologically the Vértes constitute a fairlyuniform structure

answers: NDQ_003256

answers: The Vértes constitute a fairlyuniform structure

answers: NDQ_003257

answers: The Vértes constitute a fairlyuniform structure

answers: NDQ_003258

answers: The Vértes Mountains are part of the Transdanubian Mountains

text: Much of the national park is covered by tropical forest.  The Greater Daintree Rainforest has existed continuously for more than 110 million years, making it possibly the oldest existing tropical forest. The persistence of this forest is believed to be a product of a fortuitous continental drift; after the breakup of its parent supercontinent a portion drifted toward the pole to become Antarctica, disturbing ocean currents and becoming quite chilly, while other portions were moved to hotter and drier locations. The rainforests of the parent continent preserved its climate, and so also its original trees. Tree species, once thought to be long extinct, have only relatively recently been discovered here.

text: Much of the national park is covered by

entity_name: Tropical and subtropical moist broadleaf forests

text: tropical forest

text: .  The

text: Greater Daintree Rainforest

text: has existed continuously for more than 110 million years, making it possibly the oldest existing tropical forest. The persistence of this forest is believed to be a product of a fortuitous

text: continental drift

text: ; after the breakup of its parent supercontinent a portion drifted toward the pole to become

text: Antarctica

text: , disturbing ocean currents and becoming quite chilly, while other portions were moved to hotter and drier locations. The rainforests of the parent continent preserved its climate, and so also its original trees. Tree species, once thought to be long extinct, have only relatively recently been discovered here.

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answers: 4

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answers: 0

answers: NDQ_003219

answers: 4

answers: NDQ_003220

answers: 0

answers: NDQ_003221

answers: 0

answers: NDQ_003222

answers: 0

answers: NDQ_003223

answers: 0

answers: NDQ_003224

answers: 5

answers: NDQ_003225

answers: 0

answers: NDQ_003226

answers: 0

answers: NDQ_003227

answers: 0

answers: NDQ_003228

answers: 0

answers: NDQ_003230

answers: 4

answers: NDQ_003231

answers: 0

answers: NDQ_003233

answers: 0

answers: NDQ_003236

answers: 4

answers: NDQ_003237

answers: 4

answers: NDQ_003239

answers: 0

answers: NDQ_003240

answers: 4

answers: NDQ_003241

answers: 0

answers: NDQ_003242

answers: 4

answers: NDQ_003244

answers: 0

answers: NDQ_003246

answers: 4

answers: NDQ_003247

answers: 4

answers: NDQ_003252

answers: 4

answers: NDQ_003253

answers: 4

answers: NDQ_003254

answers: 4

answers: NDQ_003255

answers: 4

answers: NDQ_003256

answers: 0

answers: NDQ_003257

answers: 0

answers: NDQ_003258

answers: 0

answers: NDQ_003219

answers: continental drift

answers: NDQ_003220

answers: Antarctica

answers: NDQ_003221

answers: late 19th century

answers: NDQ_003222

answers: the breakup of its parent supercontinent

answers: NDQ_003223

answers: parent supercontinent

answers: NDQ_003224

answers: rainforests

answers: NDQ_003225

answers: fortuitous continental drift

answers: NDQ_003226

answers: Antarctica

answers: NDQ_003227

answers: after the breakup of its parent supercontinent a portion drifted toward the pole

answers: NDQ_003228

answers: continental drift

answers: NDQ_003230

answers: Antarctica

answers: NDQ_003231

answers: pole

answers: NDQ_003233

answers: Tree species, once thought to be long extinct, have only relatively recently been discovered

answers: NDQ_003236

answers: continental drift

answers: NDQ_003237

answers: The persistence of this forest is believed to be a product of a fortuitous continental drift

answers: NDQ_003239

answers: The persistence of this forest is believed to be a product of a fortuitous continental drift

answers: NDQ_003240

answers: parent continent

answers: NDQ_003241

answers: Antarctica

answers: NDQ_003242

answers: fortuitous continental drift

answers: NDQ_003244

answers: Antarctica

answers: NDQ_003246

answers: parent supercontinent

answers: NDQ_003247

answers: The Greater Daintree Rainforest has existed continuously for more than 110 million years

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: supercontinent

answers: NDQ_003254

answers: It was widely accepted as soon as it was introduced

answers: NDQ_003255

answers: The persistence of this forest is believed to be a product of a fortuitous continental drift

answers: NDQ_003256

answers: The Greater Daintree Rainforest

answers: NDQ_003257

answers: It is believed to be a product of a fortuitous continental drift

answers: NDQ_003258

answers: after the breakup of its parent supercontinent

text: Alfred Wegener, being a meteorologist, had proposed tidal forces and pole flight force as the main driving mechanisms behind continental drift; however, these forces were considered far too small to cause continental motion as the concept then was of continents plowing through oceanic crust. Therefore, Wegener later changed his position and asserted that convection currents are the main driving force of plate tectonics in the last edition of his book in 1929.

text: Alfred Wegener

text: , being a

text: meteorologist

text: , had proposed

text: tidal force

text: s and pole flight force as the main driving mechanisms behind

text: continental drift

text: ; however, these forces were considered far too small to cause continental motion as the concept then was of continents plowing through oceanic crust. Therefore, Wegener later changed his position and asserted that convection currents are the main driving force of plate tectonics in the last edition of his book in 1929.

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answers: 4

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answers: 4

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answers: meteorologist

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answers: 4

answers: NDQ_003219

answers: continents plowing through oceanic crust

answers: NDQ_003220

answers: pole

answers: NDQ_003221

answers: 19th century

answers: NDQ_003222

answers: continents plowing through oceanic crust

answers: NDQ_003223

answers: continental drift

answers: NDQ_003224

answers: continental motion

answers: NDQ_003225

answers: continental drift

answers: NDQ_003226

answers: continental drift

answers: NDQ_003227

answers: continents plowing through oceanic crust

answers: NDQ_003228

answers: meteorologist

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: pole

answers: NDQ_003233

answers: the concept then was of continents plowing through oceanic crust

answers: NDQ_003236

answers: continental drift

answers: NDQ_003237

answers: continents plowing through oceanic crust

answers: NDQ_003239

answers: plate tectonics

answers: NDQ_003240

answers: continental drift

answers: NDQ_003241

answers: no

answers: NDQ_003242

answers: plate tectonics

answers: NDQ_003244

answers: continental drift

answers: NDQ_003246

answers: continents

answers: NDQ_003247

answers: continental drift

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: continents plowing through oceanic crust

answers: NDQ_003254

answers: The concept then was of continents plowing through oceanic crust

answers: NDQ_003255

answers: continents plowing through oceanic crust

answers: NDQ_003256

answers: continents plowing through oceanic crust

answers: NDQ_003257

answers: continents plowing through oceanic crust

answers: NDQ_003258

answers: plate tectonics

text: Glaciation following the Namurian phase facilitated greater denudation. The result is that Inisheer is one of the finest examples of a Glacio-Karst landscape in the world. The effects of the last glacial period (the Midlandian) are most in evidence, with the island overrun by ice during this glaciation. The impact of earlier Karstification (solutional erosion) has been eliminated by the last glacial period, so any Karstification now seen dates from approximately 10,000 years ago and the island Karst is thus recent.

text: Glaciation following the

text: Namurian

text: phase facilitated greater denudation. The result is that Inisheer is one of the finest examples of a Glacio-

text: Karst

text: landscape in the world. The effects of the

text: last glacial period

text: (the Midlandian) are most in evidence, with the island overrun by ice during this glaciation. The impact of earlier

text: Karstification

text: (solutional erosion) has been eliminated by the

text: last glacial period

text: , so any Karstification now seen dates from approximately 10,000 years ago and the island Karst is thus recent.

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answers: NDQ_003219

answers: Glaciation

answers: NDQ_003220

answers: Inisheer

answers: NDQ_003221

answers: Namurian

answers: NDQ_003222

answers: Glaciation

answers: NDQ_003223

answers: Glaciation

answers: NDQ_003224

answers: Inisheer

answers: NDQ_003225

answers: Glaciation

answers: NDQ_003226

answers: the world

answers: NDQ_003227

answers: Glaciation

answers: NDQ_003228

answers: Glaciation

answers: NDQ_003230

answers: Namurian

answers: NDQ_003231

answers: Karst

answers: NDQ_003233

answers: Glaciation following the Namurian phase

answers: NDQ_003236

answers: Glaciation

answers: NDQ_003237

answers: Inisheer

answers: NDQ_003239

answers: Glaciation

answers: NDQ_003240

answers: Namurian

answers: NDQ_003241

answers: no

answers: NDQ_003242

answers: Glaciation

answers: NDQ_003244

answers: Glaciation

answers: NDQ_003246

answers: Glaciation

answers: NDQ_003247

answers: Glaciation following the Namurian phase facilitated greater denudation

answers: NDQ_003252

answers: Glaciation

answers: NDQ_003253

answers: Namurian

answers: NDQ_003254

answers: It was widely accepted as soon as it was introduced

answers: NDQ_003255

answers: Glaciation following the Namurian phase facilitated greater denudation

answers: NDQ_003256

answers: Glaciation following the Namurian phase facilitated greater denudation

answers: NDQ_003257

answers: Pangaea broke up a short time ago

answers: NDQ_003258

answers: Glaciation

text: For the most part Europe lies in the northern temperate climate zone. Much of far western Europe is classified as a Temperate Oceanic climate, while far southern Europe is a Mediterranean climate in the south.  The climate is strongly conditioned by the Gulf Stream, which keeps mild air (for the latitude) over Northwestern Europe in the winter months, especially in Ireland, the UK and coastal Norway.  While Western Europe has an oceanic climate, Eastern Europe has a drier, continental climate. Parts of the Central European plains have a hybrid oceanic/continental climate. Four seasons occur in Eastern Europe, while southern Europe experiences distinct wet season and dry seasons, with prevailing hot and dry conditions during the summer months.  The heaviest precipitation occurs downwind of water bodies due to the prevailing westerlies, with higher amounts also seen in the Alps. Tornadoes occur within Europe, with most but not all occurrences being weak.

text: For the most part

text: Europe

text: lies in the northern

text: temperate

text: climate zone. Much of far western Europe is classified as a Temperate Oceanic climate, while far southern Europe is a

text: Mediterranean climate

text: in the south.  The climate is strongly conditioned by the

text: Gulf Stream

text: , which keeps mild air (for the latitude) over Northwestern Europe in the winter months, especially in Ireland, the UK and coastal Norway.  While Western Europe has an oceanic climate, Eastern Europe has a drier, continental climate. Parts of the Central European plains have a hybrid oceanic/continental climate. Four seasons occur in Eastern Europe, while southern Europe experiences distinct

text: wet season

text: and

text: dry season

text: s, with prevailing hot and dry conditions during the summer months.  The heaviest precipitation occurs downwind of water bodies due to the prevailing

text: westerlies

text: , with higher amounts also seen in the

text: Alps

text: Tornado

text: es occur within Europe, with most but not all occurrences being weak.

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answers: NDQ_003258

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answers: NDQ_003219

answers: Europe lies in the northern temperate climate zone

answers: NDQ_003220

answers: The Alps

answers: NDQ_003221

answers: late 19th century

answers: NDQ_003222

answers: Europe lies in the northern temperate climate zone

answers: NDQ_003223

answers: the Alps

answers: NDQ_003224

answers: Europe

answers: NDQ_003225

answers: The heaviest precipitation occurs downwind

answers: NDQ_003226

answers: Europe

answers: NDQ_003227

answers: continental drift

answers: NDQ_003228

answers: continental climate

answers: NDQ_003230

answers: Europe

answers: NDQ_003231

answers: magnetic field

answers: NDQ_003233

answers: Parts of the Central European plains have a hybrid oceanic/continental climate

answers: NDQ_003236

answers: continents move over Earths surface

answers: NDQ_003237

answers: Western Europe has an oceanic climate, Eastern Europe has a drier, continental climate

answers: NDQ_003239

answers: Europe lies in the northern temperate climate zone

answers: NDQ_003240

answers: Oceanic

answers: NDQ_003241

answers: The Alps

answers: NDQ_003242

answers: continental drift

answers: NDQ_003244

answers: Europe lies in the northern temperate climate zone

answers: NDQ_003246

answers: Europe

answers: NDQ_003247

answers: Parts of the Central European plains

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: Europe

answers: NDQ_003254

answers: It was widely accepted as soon as it was introduced

answers: NDQ_003255

answers: Western Europe has an oceanic climate, Eastern Europe has a drier, continental climate

answers: NDQ_003256

answers: Europe lies in the northern temperate climate zone

answers: NDQ_003257

answers: Europe lies in the northern temperate climate zone

answers: NDQ_003258

answers: Europe

text: Mesosaurus was significant in providing evidence for the theory of continental drift, because its remains were found in southern Africa and eastern South America, two widely separated regions. As Mesosaurus was a coastal animal, and therefore could not have crossed the Atlantic Ocean, this distribution indicated that the two continents used to be joined together.

text: Mesosaurus was significant in providing evidence for the

text: theory

text: of

text: continental drift

text: , because its remains were found in southern Africa and eastern South America, two widely separated regions. As Mesosaurus was a coastal animal, and therefore could not have crossed the

text: Atlantic Ocean

text: , this distribution indicated that the two continents used to be joined together.

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answers: NDQ_003219

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answers: NDQ_003225

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answers: NDQ_003231

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answers: NDQ_003233

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answers: 4

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answers: NDQ_003240

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answers: NDQ_003258

answers: 4

answers: NDQ_003219

answers: continents used to be joined together

answers: NDQ_003220

answers: widely separated regions

answers: NDQ_003221

answers: continental drift

answers: NDQ_003222

answers: Mesosaurus was a coastal animal

answers: NDQ_003223

answers: Mesosaurus

answers: NDQ_003224

answers: fossils

answers: NDQ_003225

answers: continental drift

answers: NDQ_003226

answers: South America

answers: NDQ_003227

answers: that the two continents used to be joined together

answers: NDQ_003228

answers: Mesosaurus

answers: NDQ_003230

answers: Africa

answers: NDQ_003231

answers: region

answers: NDQ_003233

answers: Mesosaurus

answers: NDQ_003236

answers: theory of continental drift

answers: NDQ_003237

answers: Mesosaurus

answers: NDQ_003239

answers: Mesosaurus was a coastal animal

answers: NDQ_003240

answers: Mesosaurus

answers: NDQ_003241

answers: no

answers: NDQ_003242

answers: theory of continental drift

answers: NDQ_003244

answers: Mesosaurus

answers: NDQ_003246

answers: Mesosaurus was a coastal animal

answers: NDQ_003247

answers: Mesosaurus

answers: NDQ_003252

answers: plate tectonics

answers: NDQ_003253

answers: Mesosaurus

answers: NDQ_003254

answers: It was widely accepted as soon as it was introduced

answers: NDQ_003255

answers: Mesosaurus

answers: NDQ_003256

answers: Mesosaurus

answers: NDQ_003257

answers: Mesosaurus

answers: NDQ_003258

answers: Mesosaurus

text: Before the theory of continental drift, glacial deposits in Carboniferous strata in tropical continents areas such as India and South America led to speculation that the Karoo Ice Age glaciation reached into the tropics. However, a continental reconstruction shows that ice was in fact constrained to the polar parts of the supercontinent Gondwana.

text: Before the theory of continental drift, glacial deposits in

text: Carboniferous

text: strata in tropical continents areas such as India and South America led to speculation that the

text: Karoo Ice Age

text: glaciation reached into the tropics. However, a continental reconstruction shows that ice was in fact constrained to the polar parts of the

text: supercontinent

text: Gondwana

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answers: led to speculation

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answers: ice was in fact constrained to the polar parts

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answers: Gondwana

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answers: Carboniferous strata

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answers: South America

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answers: the Karoo Ice Age glaciation reached into the tropics

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answers: supercontinent

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answers: supercontinent

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answers: It was widely accepted

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answers: glacial deposits

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answers: continental drift

text: But without detailed evidence and a force sufficient to drive the movement, the theory was not generally accepted: the Earth might have a solid crust and mantle and a liquid core, but there seemed to be no way that portions of the crust could move around. Distinguished scientists, such as Harold Jeffreys and Charles Schuchert, were outspoken critics of continental drift.

text: But without detailed evidence and a force sufficient to drive the movement, the theory was not generally accepted: the Earth might have a solid crust and mantle and a liquid core, but there seemed to be no way that portions of the crust could move around. Distinguished scientists, such as

text: Harold Jeffreys

text: and

text: Charles Schuchert

text: , were outspoken critics of continental drift.

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answers: crust could move around

answers: NDQ_003220

answers: continental drift

answers: NDQ_003221

answers: Distinguished scientists

answers: NDQ_003222

answers: detailed evidence and a force sufficient to drive the movement

answers: NDQ_003223

answers: continental drift

answers: NDQ_003224

answers: Distinguished scientists

answers: NDQ_003225

answers: continental drift

answers: NDQ_003226

answers: Europe

answers: NDQ_003227

answers: there seemed to be no way that portions of the crust could move around

answers: NDQ_003228

answers: Distinguished scientists

answers: NDQ_003230

answers: Earth

answers: NDQ_003231

answers: core

answers: NDQ_003233

answers: Harold Jeffreys and Charles Schuchert

answers: NDQ_003236

answers: continental drift

answers: NDQ_003237

answers: detailed evidence and a force sufficient to drive the movement

answers: NDQ_003239

answers: continental drift

answers: NDQ_003240

answers: Earth

answers: NDQ_003241

answers: Earth

answers: NDQ_003242

answers: continental drift

answers: NDQ_003244

answers: continental drift

answers: NDQ_003246

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answers: NDQ_003247

answers: detailed evidence

answers: NDQ_003252

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answers: NDQ_003253

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answers: NDQ_003255

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answers: NDQ_003256

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answers: continental drift

text: The first evidence that a capacitor and inductor could produce electrical oscillations was discovered in 1826 by French scientist Felix Savary. He found that when a Leyden jar was discharged through a wire wound around an iron needle, sometimes the needle was left magnetized in one direction and sometimes in the opposite direction. He correctly deduced that this was caused by a damped oscillating discharge current in the wire, which reversed the magnetization of the needle back and forth until it was too small to have an effect, leaving the needle magnetized in a random direction. American physicist Joseph Henry repeated Savary's experiment in 1842 and came to the same conclusion, apparently independently. British scientist William Thomson (Lord Kelvin) in 1853 showed mathematically that the discharge of a Leyden jar through an inductance should be oscillatory, and derived its resonant frequency. British radio researcher Oliver Lodge, by discharging a large battery of Leyden jars through a long wire, created a tuned circuit with its resonant frequency in the audio range, which produced a musical tone from the spark when it was discharged. In 1857, German physicist Berend Wilhelm Feddersen photographed the spark produced by a resonant Leyden jar circuit in a rotating mirror, providing visible evidence of the oscillations. In 1868, Scottish physicist James Clerk Maxwell calculated the effect of applying an alternating current to a circuit with inductance and capacitance, showing that the response is maximum at the resonant frequency. The first example of an electrical resonance curve was published in 1887 by German physicist Heinrich Hertz in his pioneering paper on the discovery of radio waves, showing the length of spark obtainable from his spark-gap LC resonator detectors as a function of frequency.

text: The first evidence that a capacitor and inductor could produce electrical oscillations was discovered in 1826 by French scientist

text: Felix Savary

text: . He found that when a

text: Leyden jar

text: was discharged through a wire wound around an iron needle, sometimes the needle was left magnetized in one direction and sometimes in the opposite direction. He correctly deduced that this was caused by a damped oscillating discharge current in the wire, which reversed the magnetization of the needle back and forth until it was too small to have an effect, leaving the needle magnetized in a random direction. American physicist

text: Joseph Henry

text: repeated Savary's experiment in 1842 and came to the same conclusion, apparently independently. British scientist

text: William Thomson

text: (Lord Kelvin) in 1853 showed mathematically that the discharge of a Leyden jar through an inductance should be oscillatory, and derived its resonant frequency. British radio researcher

text: Oliver Lodge

text: , by discharging a large battery of Leyden jars through a long wire, created a tuned circuit with its resonant frequency in the audio range, which produced a musical tone from the spark when it was discharged. In 1857, German physicist

text: Berend Wilhelm Feddersen

text: photographed the spark produced by a resonant Leyden jar circuit in a rotating mirror, providing visible evidence of the oscillations. In 1868, Scottish physicist

text: James Clerk Maxwell

text: calculated the effect of applying an alternating current to a circuit with inductance and capacitance, showing that the response is maximum at the resonant frequency. The first example of an electrical

text: resonance

text: curve was published in 1887 by German physicist

text: Heinrich Hertz

text: in his pioneering paper on the discovery of radio waves, showing the length of spark obtainable from his spark-gap LC resonator detectors as a function of frequency.

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answers: a capacitor and inductor could produce electrical oscillations

answers: NDQ_003220

answers: Scottish

answers: NDQ_003221

answers: 1840s

answers: NDQ_003222

answers: it was too small to have an effect, leaving the needle magnetized in a random direction

answers: NDQ_003223

answers: Leyden jars

answers: NDQ_003224

answers: Leyden

answers: NDQ_003225

answers: a damped oscillating discharge current

answers: NDQ_003226

answers: British

answers: NDQ_003227

answers: discovered that a capacitor and inductor could produce electrical oscillations

answers: NDQ_003228

answers: British radio researcher

answers: NDQ_003230

answers: America

answers: NDQ_003231

answers: magnetization

answers: NDQ_003233

answers: Heinrich Hertz in his pioneering paper on the discovery of radio waves

answers: NDQ_003236

answers: continents move over Earths surface

answers: NDQ_003237

answers: LC resonator detectors as a function of frequency

answers: NDQ_003239

answers: Fossil records across continents was evidence for continental drift.

answers: NDQ_003240

answers: North America

answers: NDQ_003241

answers: no

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answers: a random direction

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answers: NDQ_003256

answers: Leyden jar circuit

answers: NDQ_003257

answers: Pangaea

answers: NDQ_003258

answers: unanswerable

text: Drifting station North Pole-38 was established in October 2010. In July 2011 the icebreaker Rossiya and the research ship Akademik Fyodorov began conducting seismic studies north of Franz Josef Land to find evidence to back up Russia's territorial claims in the Arctic. The Akademik Fyodorov and the icebreaker Yamal went on a similar mission the year before. The Lena-2011 expedition, a joint Russian-German project headed by Jörn Thiede, left for the Laptev Sea and the Lena River in the summer of 2011. It was to study Siberian climate and climate change, as well as gather information about the Russian continental shelf. The head of the expedition, who is also the chairman of the European Arctic Commission, expressed confidence that Russia will gather the evidence needed to confirm its claim to additional parts of the Arctic shelf.

text: Drifting station

text: North Pole-38

text: was established in October 2010. In July 2011 the icebreaker Rossiya and the research ship

text: Akademik Fyodorov

text: began conducting seismic studies north of

text: Franz Josef Land

text: to find evidence to back up Russia's territorial claims in the Arctic. The Akademik Fyodorov and the icebreaker

text: Yamal

text: went on a similar mission the year before. The Lena-2011 expedition, a joint Russian-German project headed by

text: Jörn Thiede

text: , left for the

text: Laptev Sea

text: and the

text: Lena River

text: in the summer of 2011. It was to study Siberian climate and climate change, as well as gather information about the Russian continental shelf. The head of the expedition, who is also the chairman of the

text: European Arctic Commission

text: , expressed confidence that Russia will gather the evidence needed to confirm its claim to additional parts of the Arctic shelf.

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answers: NDQ_003257

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answers: NDQ_003258

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answers: NDQ_003219

answers: continental shelf

answers: NDQ_003220

answers: Siberian

answers: NDQ_003221

answers: Russian

answers: NDQ_003222

answers: the Arctic shelf

answers: NDQ_003223

answers: Russian continental shelf

answers: NDQ_003224

answers: Siberian

answers: NDQ_003225

answers: Drifting station

answers: NDQ_003226

answers: Siberia

answers: NDQ_003227

answers: to back up Russia's territorial claims in the Arctic

answers: NDQ_003228

answers: Drifting

answers: NDQ_003230

answers: Antarctica

answers: NDQ_003231

answers: Pole

answers: NDQ_003233

answers: Drifting station North Pole-38 was established in October 2010

answers: NDQ_003236

answers: Drifting

answers: NDQ_003237

answers: Franz Josef Land

answers: NDQ_003239

answers: Drifting station North Pole-38

answers: NDQ_003240

answers: North America

answers: NDQ_003241

answers: The Arctic

answers: NDQ_003242

answers: Drifting

answers: NDQ_003244

answers: Franz Josef Land

answers: NDQ_003246

answers: Siberian

answers: NDQ_003247

answers: Franz Josef Land

answers: NDQ_003252

answers: Drifting

answers: NDQ_003253

answers: Franz Josef Land

answers: NDQ_003254

answers: Drifting station North Pole-38

answers: NDQ_003255

answers: Drifting station North Pole-38

answers: NDQ_003256

answers: The Akademik Fyodorov

answers: NDQ_003257

answers: Pangaea

answers: NDQ_003258

answers: Drifting

text: This region has also seen its landscape altered by glaciation and the fluvial processes of the Susquehanna River. Most of the ridges in this region are parallel to the streams that drain the area. The Susquehanna also cuts through many of the mountain ridges leading some to believe that the Susquehanna is an ancient river system that existed even before the recent continental glaciation. (Some speculate as far back as the Jurassic Period) None of the mountains in this section rise above  and the river valley is as low as .

text: This region has also seen its landscape altered by glaciation and the

text: fluvial

text: processes of the Susquehanna River. Most of the ridges in this region are parallel to the streams that drain the area. The Susquehanna also cuts through many of the mountain ridges leading some to believe that the Susquehanna is an ancient river system that existed even before the recent continental glaciation. (Some speculate as far back as the

text: Jurassic

text: Period) None of the mountains in this section rise above  and the river valley is as low as .

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answers: NDQ_003219

answers: glaciation

answers: NDQ_003220

answers: Susquehanna

answers: NDQ_003221

answers: Jurassic Period

answers: NDQ_003222

answers: Jurassic Period

answers: NDQ_003223

answers: Jurassic Period

answers: NDQ_003224

answers: Jurassic Period

answers: NDQ_003225

answers: the Susquehanna is an ancient river system

answers: NDQ_003226

answers: Jurassic

answers: NDQ_003227

answers: existed even before the recent continental glaciation

answers: NDQ_003228

answers: continental glaciation

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: region

answers: NDQ_003233

answers: the Jurassic Period

answers: NDQ_003236

answers: glaciation

answers: NDQ_003237

answers: the Jurassic Period

answers: NDQ_003239

answers: The Susquehanna

answers: NDQ_003240

answers: Jurassic

answers: NDQ_003241

answers: The Susquehanna

answers: NDQ_003242

answers: glaciation

answers: NDQ_003244

answers: the Jurassic Period

answers: NDQ_003246

answers: The Susquehanna

answers: NDQ_003247

answers: Some speculate as far back as the Jurassic Period

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: Jurassic Period

answers: NDQ_003254

answers: Jurassic Period

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answers: The Susquehanna

answers: NDQ_003256

answers: Jurassic Period

answers: NDQ_003257

answers: Some speculate as far back as the Jurassic Period

answers: NDQ_003258

answers: the Jurassic Period

text: The publication of Alfred Wegener's (1880–1930) theory of continental drift 1912 gave additional impetus to comparative physiology and the study of biogeography while ecology in the 1930s contributed the important ideas of plant community, succession, community change, and energy flows. From 1940 to 1950 ecology matured to become an independent discipline as Eugene Odum (1913–2002) formulated many of the concepts of ecosystem ecology, emphasising relationships between groups of organisms (especially material and energy relationships) as key factors in the field. Building on the extensive earlier work of Alphonse de Candolle, Nikolai Vavilov (1887–1943) from 1914 to 1940 produced accounts of the geography, centres of origin, and evolutionary history of economic plants.

text: The publication of

text: Alfred Wegener

text: 's (1880–1930) theory of

text: continental drift

text: 1912 gave additional impetus to comparative physiology and the study of

text: biogeography

text: while ecology in the 1930s contributed the important ideas of plant community,

text: succession

text: , community change, and energy flows. From 1940 to 1950 ecology matured to become an independent discipline as

text: Eugene Odum

text: (1913–2002) formulated many of the concepts of

text: ecosystem ecology

text: , emphasising relationships between groups of organisms (especially material and energy relationships) as key factors in the field. Building on the extensive earlier work of Alphonse de Candolle,

text: Nikolai Vavilov

text: (1887–1943) from 1914 to 1940 produced accounts of the geography, centres of origin, and evolutionary history of economic plants.

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answers: NDQ_003220

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answers: NDQ_003221

answers: 1912

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answers: NDQ_003223

answers: centres of origin

answers: NDQ_003224

answers: Alfred Wegener

answers: NDQ_003225

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answers: NDQ_003226

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answers: NDQ_003227

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answers: NDQ_003228

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answers: NDQ_003230

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answers: NDQ_003231

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answers: NDQ_003233

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answers: NDQ_003236

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answers: NDQ_003239

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answers: NDQ_003240

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answers: NDQ_003241

answers: no

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answers: theory of continental drift

text: At perhaps the most fundamental level, distinction can be made between mineral soil horizons and organic soil horizons. The primary difference between the two classes of horizon is in the nature of their soil material: perhaps obviously, mineral soil horizons are dominated by mineral soil material whereas organic soil horizons are dominated by organic soil material. Mineral soil material is a product of the weathering of parent material such as bedrock or glacial drift whereas organic soil material is the product of decomposition of organic matter such as plants and animals.

text: At perhaps the most fundamental level, distinction can be made between mineral soil horizons and organic soil horizons. The primary difference between the two classes of horizon is in the nature of their soil material: perhaps obviously, mineral soil horizons are dominated by mineral soil material whereas organic soil horizons are dominated by organic soil material. Mineral soil material is a product of the

text: weathering

text: of

text: parent material

text: such as bedrock or glacial drift whereas organic soil material is the product of

text: decomposition

text: of organic matter such as plants and animals.

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answers: NDQ_003220

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answers: NDQ_003221

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answers: NDQ_003222

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answers: NDQ_003223

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answers: NDQ_003224

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answers: NDQ_003225

answers: the most fundamental level

answers: NDQ_003226

answers: Europe

answers: NDQ_003227

answers: Mineral soil material is a product of the weathering of parent material

answers: NDQ_003228

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answers: NDQ_003230

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answers: NDQ_003231

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answers: NDQ_003233

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answers: NDQ_003236

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answers: NDQ_003239

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answers: NDQ_003240

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answers: NDQ_003254

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answers: Pangaea

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answers: glacial drift

text: The Newcomen family, from nearby Kirkleatham, opened an ironstone mine in Dunsdale, in 1872. It exploited two pockets of ironstone left by glaciation. The two rows of cottages forming the village of Dunsdale were part of the mine property and form the major part of the village as it is today. Traces of the drift and buildings remain with parts of the railbed in the Dunsdale area leading to the top of the incline. Unfortunately, the mine was not a particular success and was abandoned on 31 December 1886, but the village still remains.

text: The Newcomen family, from nearby

text: Kirkleatham

text: , opened an ironstone mine in Dunsdale, in 1872. It exploited two pockets of ironstone left by glaciation. The two rows of cottages forming the village of Dunsdale were part of the mine property and form the major part of the village as it is today. Traces of the drift and buildings remain with parts of the railbed in the Dunsdale area leading to the top of the incline. Unfortunately, the mine was not a particular success and was abandoned on 31 December 1886, but the village still remains.

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text: The climate of Lazovski is Humid continental climate, cool summer (Köppen climate classification (Dwb)). This climate is characterized by high variation in temperature, both daily and seasonally; with dry winters and cool summers.  The Zapovedny Ridge runs across the middle; the northern extent of the reserve has a more continental climate, the southern extent more maritime.

text: The climate of Lazovski is

text: Humid continental climate, cool summer

text: Köppen climate classification

text: (Dwb)

text: ). This climate is characterized by high variation in temperature, both daily and seasonally; with dry winters and cool summers.  The Zapovedny Ridge runs across the middle; the northern extent of the reserve has a more continental climate, the southern extent more maritime.

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answers: NDQ_003223

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answers: NDQ_003228

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answers: NDQ_003233

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answers: NDQ_003236

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answers: NDQ_003237

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answers: NDQ_003239

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answers: NDQ_003241

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answers: NDQ_003242

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answers: NDQ_003252

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answers: NDQ_003253

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answers: NDQ_003254

answers: It was widely accepted as soon as it was introduced

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answers: The Zapovedny Ridge

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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.

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text: This climatic region is typified by large seasonal temperature differences, with hot and humid summers and cold and dry winters.  According to the Köppen Climate Classification system, Belfast has a humid continental climate, abbreviated "Dfb" on climate maps.

text: This

text: climatic

text: region is typified by large seasonal temperature differences, with hot and humid summers and cold and dry winters.  According to the

text: Köppen Climate Classification

text: system, Belfast has a

text: humid continental climate

text: , abbreviated "Dfb" on climate maps.

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text: Due to the chaotic nature of trace fossil classification, several ichnogenera hold names normally affiliated with animal body fossils or plant fossils. For example, many ichnogenera are named with the suffix -phycus due to misidentification as algae.

text: Due to the chaotic nature of trace fossil classification, several ichnogenera hold names normally affiliated with animal body fossils or plant fossils. For example, many ichnogenera are named with the suffix -phycus due to misidentification as algae.

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answers: NDQ_003223

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answers: NDQ_003224

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answers: NDQ_003240

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answers: NDQ_003246

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answers: NDQ_003252

answers: 3

answers: NDQ_003253

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answers: NDQ_003254

answers: 0

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answers: 0

answers: NDQ_003256

answers: 0

answers: NDQ_003257

answers: 0

answers: NDQ_003258

answers: 0

answers: NDQ_003219

answers: the chaotic nature of trace fossil classification

answers: NDQ_003220

answers: Atlantic Ocean

answers: NDQ_003221

answers: paleoenvironments

answers: NDQ_003222

answers: chaotic nature of trace fossil classification

answers: NDQ_003223

answers: animal body fossils

answers: NDQ_003224

answers: trace fossils

answers: NDQ_003225

answers: misidentification

answers: NDQ_003226

answers: Europe

answers: NDQ_003227

answers: chaotic nature of trace fossil classification

answers: NDQ_003228

answers: trace fossil classification

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: phycus

answers: NDQ_003233

answers: ichnogenera

answers: NDQ_003236

answers: chaotic nature

answers: NDQ_003237

answers: trace fossil classification

answers: NDQ_003239

answers: Due to the chaotic nature of trace fossil classification

answers: NDQ_003240

answers: Phycus

answers: NDQ_003241

answers: no

answers: NDQ_003242

answers: chaotic nature

answers: NDQ_003244

answers: ichnogenera

answers: NDQ_003246

answers: chaotic

answers: NDQ_003247

answers: trace fossil classification

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: The chaotic nature of trace fossil classification

answers: NDQ_003254

answers: due to misidentification as algae

answers: NDQ_003255

answers: trace fossil classification

answers: NDQ_003256

answers: Due to the chaotic nature of trace fossil classification

answers: NDQ_003257

answers: Due to the chaotic nature of trace fossil classification

answers: NDQ_003258

answers: Due to the chaotic nature of trace fossil classification

text: The flora of Australia comprises a vast assemblage of plant species estimated to over 20,000 vascular and 14,000 non-vascular plants, 250,000 species of fungi and over 3,000 lichens. The flora has strong affinities with the flora of Gondwana, and below the family level has a highly endemic angiosperm flora whose diversity was shaped by the effects of continental drift and climate change since the Cretaceous. Prominent features of the Australian flora are adaptations to aridity and fire which include scleromorphy and serotiny. These adaptations are common in species from the large and well-known families Proteaceae (Banksia), Myrtaceae (Eucalyptus - gum trees), and Fabaceae (Acacia - wattle).

text: The flora of

text: Australia

text: comprises a vast assemblage of plant species estimated to over 20,000

text: vascular

text: and 14,000

text: non-vascular plant

text: s, 250,000 species of

text: fungi

text: and over 3,000

text: lichen

text: s. The flora has strong affinities with the flora of

text: Gondwana

text: , and below the

text: family

text: level has a highly

text: endemic

text: angiosperm flora whose diversity was shaped by the effects of

text: continental drift

text: and climate change since the

text: Cretaceous

text: . Prominent features of the Australian flora are adaptations to

text: aridity

text: and fire which include

text: scleromorphy

text: and

text: serotiny

text: . These adaptations are common in species from the large and well-known families

text: Proteaceae

text: Banksia

text: Myrtaceae

text: Eucalyptus

text: - gum trees), and

text: Fabaceae

text: Acacia

text: - wattle).

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answers: 0

answers: NDQ_003219

answers: 0

answers: NDQ_003220

answers: 0

answers: NDQ_003221

answers: 0

answers: NDQ_003222

answers: 0

answers: NDQ_003223

answers: 0

answers: NDQ_003224

answers: 4

answers: NDQ_003225

answers: 0

answers: NDQ_003226

answers: 0

answers: NDQ_003227

answers: 0

answers: NDQ_003228

answers: 0

answers: NDQ_003230

answers: 0

answers: NDQ_003231

answers: 0

answers: NDQ_003233

answers: 0

answers: NDQ_003236

answers: 4

answers: NDQ_003237

answers: 0

answers: NDQ_003239

answers: 0

answers: NDQ_003240

answers: 0

answers: NDQ_003241

answers: 0

answers: NDQ_003242

answers: 0

answers: NDQ_003244

answers: 0

answers: NDQ_003246

answers: 4

answers: NDQ_003247

answers: 4

answers: NDQ_003252

answers: 4

answers: NDQ_003253

answers: 0

answers: NDQ_003254

answers: 0

answers: NDQ_003255

answers: 4

answers: NDQ_003256

answers: 0

answers: NDQ_003257

answers: 0

answers: NDQ_003258

answers: 0

answers: NDQ_003219

answers: continental drift and climate change

answers: NDQ_003220

answers: Gondwana

answers: NDQ_003221

answers: Cretaceous

answers: NDQ_003222

answers: highly endemic angiosperm flora

answers: NDQ_003223

answers: the Cretaceous

answers: NDQ_003224

answers: Cretaceous

answers: NDQ_003225

answers: the effects of continental drift and climate change

answers: NDQ_003226

answers: Gondwana

answers: NDQ_003227

answers: highly endemic angiosperm flora

answers: NDQ_003228

answers: continental drift and climate change

answers: NDQ_003230

answers: Australia

answers: NDQ_003231

answers: magnetism

answers: NDQ_003233

answers: highly endemic angiosperm flora whose diversity was shaped by the effects of continental drift and climate change since the Cretaceous

answers: NDQ_003236

answers: continental drift

answers: NDQ_003237

answers: highly endemic angiosperm flora

answers: NDQ_003239

answers: highly endemic angiosperm flora

answers: NDQ_003240

answers: Gondwana

answers: NDQ_003241

answers: Australia

answers: NDQ_003242

answers: continental drift

answers: NDQ_003244

answers: Australia

answers: NDQ_003246

answers: continental drift

answers: NDQ_003247

answers: highly endemic angiosperm flora

answers: NDQ_003252

answers: Cretaceous

answers: NDQ_003253

answers: Gondwana

answers: NDQ_003254

answers: It was widely accepted as soon as it was introduced

answers: NDQ_003255

answers: highly endemic angiosperm flora

answers: NDQ_003256

answers: Gondwana

answers: NDQ_003257

answers: Gondwana

answers: NDQ_003258

answers: continental drift and climate change

text: Ortelius was the first to underline the geometrical similarity between the coasts of America and Europe-Africa, and to propose continental drift as an explanation. Kious described Ortelius' thoughts in this way:Ortelius's observations of continental juxtaposition and his proposal of rupture and separation were repeated by Alfred Wegener who published his hypothesis of continental drift in 1912 and in following years.  Because his publications were widely available in German and English, and because he adduced geological support for the idea, Wegener is credited by most geologists as the first to recognize the possibility of continental drift. During the 1960s geophysical and geological evidence for seafloor spreading at mid-oceanic ridges became increasingly compelling to geologists (e.g. Hess, 1960,) and finally established continental drift as an ongoing global mechanism. After more than three centuries, Ortelius's supposition of continental drift was proven correct.

text: Ortelius was the first to underline the geometrical similarity between the coasts of America and Europe-Africa, and to propose

text: continental drift

text: as an explanation. Kious described Ortelius' thoughts in this way:Ortelius's observations of continental juxtaposition and his proposal of rupture and separation were repeated by

text: Alfred Wegener

text: who published his hypothesis of continental drift in 1912 and in following years.  Because his publications were widely available in German and English, and because he adduced geological support for the idea, Wegener is credited by most geologists as the first to recognize the possibility of continental drift. During the 1960s geophysical and geological evidence for

text: seafloor spreading

text: at

text: mid-oceanic ridge

text: s became increasingly compelling to geologists (e.g. Hess, 1960,) and finally established continental drift as an ongoing global mechanism. After more than three centuries, Ortelius's supposition of continental drift was proven correct.

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answers: 4

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answers: 0

answers: NDQ_003221

answers: 3

answers: NDQ_003222

answers: 0

answers: NDQ_003223

answers: 0

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answers: 0

answers: NDQ_003225

answers: 5

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answers: 4

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answers: 4

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answers: 4

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answers: 4

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answers: 0

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answers: 4

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answers: 4

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answers: 0

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answers: 0

answers: NDQ_003258

answers: 5

answers: NDQ_003219

answers: continental drift as an ongoing global mechanism

answers: NDQ_003220

answers: Europe-Africa

answers: NDQ_003221

answers: Ortelius

answers: NDQ_003222

answers: Ortelius's observations of continental juxtaposition

answers: NDQ_003223

answers: continental drift

answers: NDQ_003224

answers: Ortelius

answers: NDQ_003225

answers: hypothesis of continental drift

answers: NDQ_003226

answers: Europe-Africa

answers: NDQ_003227

answers: hypothesis

answers: NDQ_003228

answers: published his hypothesis of continental drift

answers: NDQ_003230

answers: Europe-Africa

answers: NDQ_003231

answers: mid-oceanic

answers: NDQ_003233

answers: Hess

answers: NDQ_003236

answers: continental drift

answers: NDQ_003237

answers: seafloor spreading at mid-oceanic ridges

answers: NDQ_003239

answers: seafloor spreading at mid-oceanic ridges

answers: NDQ_003240

answers: North America

answers: NDQ_003241

answers: America

answers: NDQ_003242

answers: rupture and separation

answers: NDQ_003244

answers: continental drift

answers: NDQ_003246

answers: Europe-Africa

answers: NDQ_003247

answers: mid-oceanic ridges

answers: NDQ_003252

answers: plate tectonics

answers: NDQ_003253

answers: continents were once joined together

answers: NDQ_003254

answers: Most geologists

answers: NDQ_003255

answers: geological support for the idea

answers: NDQ_003256

answers: Hess

answers: NDQ_003257

answers: Ortelius's observations of continental juxtaposition and his proposal of rupture and separation

answers: NDQ_003258

answers: Alfred Wegener

text: As the continent drifted north from Antarctica, a unique fauna, flora and mycobiota developed. Marsupials and monotremes also existed on other continents, but only in Australia–New Guinea did they out-compete the placental mammals and come to dominate. Bird life also flourished — in particular, the songbirds (order Passeriformes, suborder Passeri) are thought to have evolved 50 million years ago in the part of Gondwana that later became Australia, New Zealand, New Guinea, and Antarctica, before radiating into a great number of different forms and then spreading around the globe.  Among the fungi, the remarkable association between Cyttaria gunnii (one of the "golf-ball" fungi) and its associated trees in the genus Nothofagus is evidence of that drift: the only other places where this association is known are New Zealand and southern Argentina and Chile.

text: As the continent drifted north from Antarctica, a unique

text: fauna

text: flora

text: and

text: mycobiota

text: developed.

text: Marsupial

text: s and

text: monotreme

text: s also existed on other continents, but only in Australia–New Guinea did they out-compete the

text: placental

text: mammals

text: and come to dominate.

text: Bird

text: life also flourished — in particular, the

text: songbird

text: s (order

text: Passeriformes

text: , suborder Passeri) are thought to have evolved 50 million years ago in the part of

text: Gondwana

text: that later became

text: Australia

text: , New Zealand,

text: New Guinea

text: , and

text: Antarctica

text: , before radiating into a great number of different forms and then spreading around the globe.  Among the fungi, the remarkable association between

text: Cyttaria

text: gunnii (one of the "golf-ball" fungi) and its associated trees in the genus

text: Nothofagus

text: is evidence of that drift: the only other places where this association is known are

text: New Zealand

text: and southern

text: Argentina

text: and

text: Chile

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answers: 0

answers: NDQ_003219

answers: 4

answers: NDQ_003220

answers: 0

answers: NDQ_003221

answers: 0

answers: NDQ_003222

answers: 0

answers: NDQ_003223

answers: 0

answers: NDQ_003224

answers: 0

answers: NDQ_003225

answers: 0

answers: NDQ_003226

answers: 0

answers: NDQ_003227

answers: 0

answers: NDQ_003228

answers: 0

answers: NDQ_003230

answers: 0

answers: NDQ_003231

answers: 0

answers: NDQ_003233

answers: 4

answers: NDQ_003236

answers: 4

answers: NDQ_003237

answers: 4

answers: NDQ_003239

answers: 0

answers: NDQ_003240

answers: 0

answers: NDQ_003241

answers: 0

answers: NDQ_003242

answers: 0

answers: NDQ_003244

answers: 0

answers: NDQ_003246

answers: 4

answers: NDQ_003247

answers: 4

answers: NDQ_003252

answers: 4

answers: NDQ_003253

answers: 4

answers: NDQ_003254

answers: 0

answers: NDQ_003255

answers: 4

answers: NDQ_003256

answers: 0

answers: NDQ_003257

answers: 0

answers: NDQ_003258

answers: 4

answers: NDQ_003219

answers: continent drifted north

answers: NDQ_003220

answers: Antarctica

answers: NDQ_003221

answers: Gondwana

answers: NDQ_003222

answers: the only other places where this association is known are New Zealand and southern Argentina and Chile

answers: NDQ_003223

answers: Gondwana

answers: NDQ_003224

answers: Gondwana

answers: NDQ_003225

answers: drift

answers: NDQ_003226

answers: Antarctica

answers: NDQ_003227

answers: the continent drifted north from Antarctica, a unique fauna, flora and mycobiota developed

answers: NDQ_003228

answers: physicist

answers: NDQ_003230

answers: Antarctica

answers: NDQ_003231

answers: Antarctica

answers: NDQ_003233

answers: the only other places where this association is known are New Zealand and southern Argentina and Chile

answers: NDQ_003236

answers: drift

answers: NDQ_003237

answers: Cyttaria gunnii (one of the "golf-ball" fungi) and its associated trees

answers: NDQ_003239

answers: The only other places where this association is known are New Zealand and southern Argentina and Chile

answers: NDQ_003240

answers: Gondwana

answers: NDQ_003241

answers: Antarctica

answers: NDQ_003242

answers: Gondwana

answers: NDQ_003244

answers: Antarctica

answers: NDQ_003246

answers: Gondwana

answers: NDQ_003247

answers: Australia, New Zealand, New Guinea, and Antarctica

answers: NDQ_003252

answers: plate tectonics

answers: NDQ_003253

answers: Gondwana

answers: NDQ_003254

answers: It was widely accepted as soon as it was introduced

answers: NDQ_003255

answers: "golf-ball" fungi and its associated trees in the genus Nothofagus

answers: NDQ_003256

answers: As the continent drifted north from Antarctica

answers: NDQ_003257

answers: Gondwana

answers: NDQ_003258

answers: As the continent drifted north from Antarctica

text: Detailed studies of the paleontology, sedimentology, and stratigraphy of glacial and nonglacial deposits within the Antarctic Peninsula and adjacent parts of the Weddell Sea and its Pacific continental shelf have found that it has become progressively glaciated as the climate of Antarctica dramatically and progressively cooled during the last 37 million years. This progressive cooling was contemporaneous with a reduction in atmospheric CO2 concentrations. During this climatic cooling, the Antarctic Peninsula was probably the last region of Antarctica to have been fully glaciated. Within the Antarctic Peninsula, mountain glaciation was initiated during the latest Eocene, about 37–34 Ma. The transition from temperate, alpine glaciation to a dynamic ice sheet occurred about 12.8 Ma. At this time, the Antarctic Peninsula formed as the bedrock islands underlying it were overridden and joined together by an ice sheet in the early Pliocene about 5.3–3.6 Ma. During the Quaternary Period, the size of the West Antarctic Ice Sheet has fluctuated in response to glacial - interglacial cycles. During glacial epochs, this ice sheet was significantly thicker than it is currently is and extended to the edge of the continental shelves. During interglacial epochs, the West Antarctica Ice Sheet was thinner than during glacial epochs and its margins lay significantly inland of the continental margins.

text: Pliocene

text: about 5.3–3.6 Ma. During the

text: Quaternary

text: Period, the size of the West Antarctic Ice Sheet has fluctuated in response to glacial - interglacial cycles. During glacial epochs, this ice sheet was significantly thicker than it is currently is and extended to the edge of the continental shelves. During interglacial epochs, the West Antarctica Ice Sheet was thinner than during glacial epochs and its margins lay significantly inland of the continental margins.

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answers: NDQ_003233

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answers: NDQ_003236

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answers: NDQ_003237

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answers: NDQ_003239

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answers: NDQ_003240

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answers: NDQ_003252

answers: 4

answers: NDQ_003253

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answers: NDQ_003254

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answers: NDQ_003256

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answers: NDQ_003258

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answers: NDQ_003219

answers: glaciation was initiated during the latest Eocene

answers: NDQ_003220

answers: Pacific

answers: NDQ_003221

answers: Pliocene

answers: NDQ_003222

answers: Detailed studies of the paleontology, sedimentology, and stratigraphy

answers: NDQ_003223

answers: Antarctica

answers: NDQ_003224

answers: Paleontology

answers: NDQ_003225

answers: glacial epochs

answers: NDQ_003226

answers: Antarctica

answers: NDQ_003227

answers: the Antarctic Peninsula was probably the last region of Antarctica to have been fully glaciated

answers: NDQ_003228

answers: paleontology, sedimentology, and stratigraphy

answers: NDQ_003230

answers: Pacific

answers: NDQ_003231

answers: peninsula

answers: NDQ_003233

answers: The Antarctic Peninsula was probably the last region of Antarctica to have been fully glaciated

answers: NDQ_003236

answers: continental shelf

answers: NDQ_003237

answers: the Antarctic Peninsula was probably the last region of Antarctica to have been fully glaciated

answers: NDQ_003239

answers: The Antarctic Peninsula was probably the last region of Antarctica to have been fully glaciated

answers: NDQ_003240

answers: Pacific

answers: NDQ_003241

answers: Pacific

answers: NDQ_003242

answers: interglacial

answers: NDQ_003244

answers: Antarctic Peninsula

answers: NDQ_003246

answers: Antarctic Peninsula and adjacent parts of the Weddell Sea and its Pacific continental shelf

answers: NDQ_003247

answers: its margins lay significantly inland of the continental margins

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: Antarctic Peninsula formed as the bedrock islands underlying it were overridden and joined together by an ice sheet

answers: NDQ_003254

answers: It has become progressively glaciated

answers: NDQ_003255

answers: Detailed studies of the paleontology, sedimentology, and stratigraphy

answers: NDQ_003256

answers: Weddell Sea

answers: NDQ_003257

answers: Pangaea

answers: NDQ_003258

answers: Bedrock islands underlying it were overridden and joined together by an ice sheet

text: The Silurian Lagerstätte preserved in the limestone Wenlock Series of Herefordshire, England, offers paleontologists a rare snapshot of a moment in time, about 420 Mya. In the formation, layers of fine-grained volcanic ash punctuate a sequence of carbonate muds that were accumulating in a marine environment on the outer continental shelf. In this fine-grained matrix, soft-bodied animals and delicate, lightly sclerotized chitinous shells are often preserved in three dimensions, as calcitic fossilizations within calcareous nodules. Calcitic fossilization is an unusual feature.

text: The

text: Silurian

text: Lagerstätte

text: preserved in the

text: limestone

text: Wenlock Series of

text: Herefordshire

text: England

text: , offers paleontologists a rare snapshot of a moment in time, about 420 Mya. In the formation, layers of fine-grained volcanic ash punctuate a sequence of carbonate muds that were accumulating in a marine environment on the outer

text: continental shelf

text: . In this fine-grained matrix,

text: soft-bodied animals

text: and delicate, lightly sclerotized

text: chitin

text: ous shells are often preserved in three dimensions, as calcitic fossilizations within calcareous nodules. Calcitic fossilization is an unusual feature.

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answers: NDQ_003219

answers: continental shelf

answers: NDQ_003220

answers: England

answers: NDQ_003221

answers: Silurian

answers: NDQ_003222

answers: Silurian Lagerstätte

answers: NDQ_003223

answers: a marine environment

answers: NDQ_003224

answers: Silurian

answers: NDQ_003225

answers: Silurian Lagerstätte

answers: NDQ_003226

answers: England

answers: NDQ_003227

answers: the outer continental shelf

answers: NDQ_003228

answers: paleontologists

answers: NDQ_003230

answers: England

answers: NDQ_003231

answers: nodules

answers: NDQ_003233

answers: Silurian Lagerstätte

answers: NDQ_003236

answers: continental shelf

answers: NDQ_003237

answers: Silurian Lagerstätte

answers: NDQ_003239

answers: Silurian Lagerstätte

answers: NDQ_003240

answers: Silurian

answers: NDQ_003241

answers: England

answers: NDQ_003242

answers: a marine environment

answers: NDQ_003244

answers: It is on a drifting continent

answers: NDQ_003246

answers: continental shelf

answers: NDQ_003247

answers: Silurian Lagerstätte

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: continental shelf

answers: NDQ_003254

answers: The Silurian Lagerstätte

answers: NDQ_003255

answers: Silurian Lagerstätte

answers: NDQ_003256

answers: Wenlock Series

answers: NDQ_003257

answers: 420 Mya

answers: NDQ_003258

answers: continental shelf

text: Another effect of glaciation can be seen on East Falkland in the basins called glacial cirques that were created on Mount Usborne.  On West Falkland there are glacial cirques on Mount Adam and on the Hornby mountains.  Several of these hold tarns, or small cirque ponds.

text: Another effect of glaciation can be seen on East Falkland in the basins called glacial

text: cirques

text: that were created on

text: Mount Usborne

text: .  On West Falkland there are glacial cirques on

text: Mount Adam

text: and on the Hornby mountains.  Several of these hold

text: tarns

text: , or small cirque ponds.

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answers: NDQ_003222

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answers: NDQ_003223

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answers: NDQ_003224

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answers: NDQ_003228

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answers: NDQ_003230

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answers: NDQ_003231

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answers: NDQ_003233

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answers: NDQ_003236

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answers: NDQ_003237

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answers: NDQ_003244

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answers: NDQ_003246

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answers: NDQ_003252

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answers: NDQ_003253

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answers: NDQ_003254

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answers: NDQ_003255

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answers: NDQ_003256

answers: 0

answers: NDQ_003257

answers: 0

answers: NDQ_003258

answers: 0

answers: NDQ_003219

answers: glaciation

answers: NDQ_003220

answers: West Falkland

answers: NDQ_003221

answers: 19th century

answers: NDQ_003222

answers: glaciation

answers: NDQ_003223

answers: glaciation

answers: NDQ_003224

answers: glacial cirques

answers: NDQ_003225

answers: glacial cirques

answers: NDQ_003226

answers: Falkland

answers: NDQ_003227

answers: glaciation

answers: NDQ_003228

answers: glacial cirques

answers: NDQ_003230

answers: Falkland

answers: NDQ_003231

answers: cirques

answers: NDQ_003233

answers: glacial cirques

answers: NDQ_003236

answers: glaciation

answers: NDQ_003237

answers: glacial cirques

answers: NDQ_003239

answers: glacial cirques

answers: NDQ_003240

answers: Falkland

answers: NDQ_003241

answers: Falkland

answers: NDQ_003242

answers: glaciation

answers: NDQ_003244

answers: Falkland

answers: NDQ_003246

answers: Falkland

answers: NDQ_003247

answers: glacial cirques

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: Falkland

answers: NDQ_003254

answers: glacial cirques

answers: NDQ_003255

answers: glacial cirques that were created on Mount Usborne

answers: NDQ_003256

answers: West Falkland

answers: NDQ_003257

answers: The Hornby mountains

answers: NDQ_003258

answers: glacial cirques

text: Factors in mass extinctions include continental drift, changes in atmospheric and marine chemistry, volcanism and other aspects of mountain formation, changes in glaciation, changes in sea level, and impact events.

text: Factors in mass extinctions include

text: continental drift

text: , changes in atmospheric and marine

text: chemistry

text: volcanism

text: and other aspects of

text: mountain formation

text: , changes in

text: glaciation

text: , changes in

text: sea level

text: , and

text: impact event

text: s.

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text: The villa has been designated by UNESCO as part of the World Heritage Site "City of Vicenza and the Palladian Villas of the Veneto".The villa and extensive gardens are open to the public in the afternoon, year round. The building also houses a museum of archeology in the basement, with hundreds of fossils of plant and animal life in the region. Its large park was laid out in the 19th century and was used as a film location for Senso.

text: The villa has been designated by

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text: To gain better research and knowledge about these climate changes, buoys are cast out to sea where they are located by satellite.  The satellite pics up these frequencies sent out by the buoys drifting in the ocean off the continental coast, producing much needed data to increase predictability. Original technology of the buoy can date back thirty years, but with advancements in technology, the data collected nowadays do not just focus on the oceanic currents.  Information gathered can reflect the wind patterns, temperatures, and certain densities of the ocean in specific areas, as all these factors are constantly fluctuating.  These buoys are located all over the world, oceans and great lakes.  The data collected goes to the National Data Buoy Center, where experts record and analyze the feedback.  With relation to wave currents, the buoys use accelerometers that can identify the directional vector of the waves.  They also record the special distance between the trough and crest of each wave.  This information that is constantly used by sailors, can be life saving and result in a more efficient trip across the sea.

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answers: 0

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answers: 0

answers: NDQ_003219

answers: 0

answers: NDQ_003220

answers: 0

answers: NDQ_003221

answers: 0

answers: NDQ_003222

answers: 0

answers: NDQ_003223

answers: 0

answers: NDQ_003224

answers: 0

answers: NDQ_003225

answers: 0

answers: NDQ_003226

answers: 0

answers: NDQ_003227

answers: 0

answers: NDQ_003228

answers: 0

answers: NDQ_003230

answers: 0

answers: NDQ_003231

answers: 0

answers: NDQ_003233

answers: 0

answers: NDQ_003236

answers: 0

answers: NDQ_003237

answers: 0

answers: NDQ_003239

answers: 0

answers: NDQ_003240

answers: 0

answers: NDQ_003241

answers: 0

answers: NDQ_003242

answers: 0

answers: NDQ_003244

answers: 0

answers: NDQ_003246

answers: 0

answers: NDQ_003247

answers: 0

answers: NDQ_003252

answers: 3

answers: NDQ_003253

answers: 0

answers: NDQ_003254

answers: 0

answers: NDQ_003255

answers: 0

answers: NDQ_003256

answers: 0

answers: NDQ_003257

answers: 0

answers: NDQ_003258

answers: 0

answers: NDQ_003219

answers: oceanic currents

answers: NDQ_003220

answers: continental coast

answers: NDQ_003221

answers: 20th century

answers: NDQ_003222

answers: buoys are cast out to sea where they are located by satellite

answers: NDQ_003223

answers: climate changes

answers: NDQ_003224

answers: Buoys

answers: NDQ_003225

answers: buoys are cast out to sea

answers: NDQ_003226

answers: Great Lakes

answers: NDQ_003227

answers: to increase predictability

answers: NDQ_003228

answers: knowledge about these climate changes

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: trough

answers: NDQ_003233

answers: buoys are cast out to sea

answers: NDQ_003236

answers: coast

answers: NDQ_003237

answers: buoys drifting in the ocean off the continental coast

answers: NDQ_003239

answers: buoys are cast out to sea where they are located by satellite

answers: NDQ_003240

answers: continental

answers: NDQ_003241

answers: no

answers: NDQ_003242

answers: oceanic currents

answers: NDQ_003244

answers: buoys are cast out to sea

answers: NDQ_003246

answers: These buoys are located all over the world

answers: NDQ_003247

answers: buoys are cast out to sea

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: It does not say

answers: NDQ_003254

answers: It was widely accepted

answers: NDQ_003255

answers: buoys are cast out to sea where they are located by satellite

answers: NDQ_003256

answers: Buoys are cast out to sea where they are located by satellite

answers: NDQ_003257

answers: Pangaea

answers: NDQ_003258

answers: The satellite pics up these frequencies sent out by the buoys

text: Early plants were small, unicellular or filamentous, composed mostly of soft body tissues, with simple branching.  The identification of plant tissues in Cambrian strata is an uncertain area in the evolutionary history of plants because of the small and soft-bodied nature of these plants.  It is also difficult in a fossil of this age to distinguish among various similar appearing groups with simple branching patterns, and not all of these groups are plants.  One exception to the uncertainty of fossils from this age is the group of calcareous green algae, Dasycladales found in the fossil record since the middle Cambrian.  These algae do not belong to the lineage that is ancestral to the land plants.  Other major groups of green algae had been established by this time, but there were no land plants with vascular tissues until the mid-Silurian.

text: Early plants were small, unicellular or filamentous, composed mostly of soft body tissues, with simple branching.  The identification of plant tissues in Cambrian strata is an uncertain area in the evolutionary history of plants because of the small and soft-bodied nature of these plants.  It is also difficult in a fossil of this age to distinguish among various similar appearing groups with simple branching patterns, and not all of these groups are plants.  One exception to the uncertainty of fossils from this age is the group of calcareous green algae,

text: Dasycladales

text: found in the fossil record since the middle Cambrian.  These algae do not belong to the lineage that is ancestral to the land plants.  Other major groups of green algae had been established by this time, but there were no

text: land plants

text: with vascular tissues until the mid-

text: Silurian

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answers: 0

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answers: 0

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answers: 0

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answers: 0

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answers: 0

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answers: 0

answers: NDQ_003219

answers: 0

answers: NDQ_003220

answers: 0

answers: NDQ_003221

answers: 0

answers: NDQ_003222

answers: 0

answers: NDQ_003223

answers: 0

answers: NDQ_003224

answers: 0

answers: NDQ_003225

answers: 0

answers: NDQ_003226

answers: 0

answers: NDQ_003227

answers: 0

answers: NDQ_003228

answers: 0

answers: NDQ_003230

answers: 0

answers: NDQ_003231

answers: 0

answers: NDQ_003233

answers: 0

answers: NDQ_003236

answers: 0

answers: NDQ_003237

answers: 0

answers: NDQ_003239

answers: 0

answers: NDQ_003240

answers: 0

answers: NDQ_003241

answers: 0

answers: NDQ_003242

answers: 0

answers: NDQ_003244

answers: 0

answers: NDQ_003246

answers: 4

answers: NDQ_003247

answers: 0

answers: NDQ_003252

answers: 0

answers: NDQ_003253

answers: 0

answers: NDQ_003254

answers: 0

answers: NDQ_003255

answers: 0

answers: NDQ_003256

answers: 0

answers: NDQ_003257

answers: 0

answers: NDQ_003258

answers: 0

answers: NDQ_003219

answers: land plants with vascular tissues

answers: NDQ_003220

answers: Cambrian

answers: NDQ_003221

answers: Cambrian

answers: NDQ_003222

answers: Early plants were small, unicellular or filamentous, composed mostly of soft body tissues

answers: NDQ_003223

answers: Cambrian

answers: NDQ_003224

answers: Cambrian

answers: NDQ_003225

answers: Early plants were small, unicellular or filamentous

answers: NDQ_003226

answers: Cambrian

answers: NDQ_003227

answers: land plants with vascular tissues until the mid-Silurian

answers: NDQ_003228

answers: calcareous green algae

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: Silurian

answers: NDQ_003233

answers: Dasycladales

answers: NDQ_003236

answers: These algae do not belong to the lineage that is ancestral to the land plants

answers: NDQ_003237

answers: Dasycladales

answers: NDQ_003239

answers: The identification of plant tissues in Cambrian strata is an uncertain area

answers: NDQ_003240

answers: Silurian

answers: NDQ_003241

answers: The identification of plant tissues in Cambrian strata

answers: NDQ_003242

answers: Cambrian

answers: NDQ_003244

answers: Dasycladales

answers: NDQ_003246

answers: continents have never been together as a single whole continent

answers: NDQ_003247

answers: Cambrian

answers: NDQ_003252

answers: plate tectonics

answers: NDQ_003253

answers: Dasycladales

answers: NDQ_003254

answers: no land plants with vascular tissues until the mid-Silurian

answers: NDQ_003255

answers: There were no land plants with vascular tissues until the mid-Silurian

answers: NDQ_003256

answers: Dasycladales

answers: NDQ_003257

answers: Pangaea

answers: NDQ_003258

answers: Dasycladales

text: The hypothesis that continents might have 'drifted' was first put forward by Flemish cartographer and geographer Abraham Ortelius in 1596.

text: The

text: hypothesis

text: that

text: continents might have 'drifted'

text: was first put forward by Flemish cartographer and geographer

text: Abraham Ortelius

text: in 1596.

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answers: 4: The answer has limited relevance and completeness, with noticeable gaps or inaccuracy.

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answers: NDQ_003219

answers: continents might have 'drifted

answers: NDQ_003220

answers: continents

answers: NDQ_003221

answers: 1596

answers: NDQ_003222

answers: Abraham Ortelius

answers: NDQ_003223

answers: continental drift

answers: NDQ_003224

answers: cartographer and geographer

answers: NDQ_003225

answers: The hypothesis

answers: NDQ_003226

answers: Flemish

answers: NDQ_003227

answers: continents might have 'drifted'

answers: NDQ_003228

answers: cartographer and geographer

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: magnet

answers: NDQ_003233

answers: Ortelius

answers: NDQ_003236

answers: drifted

answers: NDQ_003237

answers: Abraham Ortelius

answers: NDQ_003239

answers: fossil records across continents

answers: NDQ_003240

answers: drifted

answers: NDQ_003241

answers: no

answers: NDQ_003242

answers: The hypothesis

answers: NDQ_003244

answers: continents might have drifted

answers: NDQ_003246

answers: continents might have drifted

answers: NDQ_003247

answers: continental drift

answers: NDQ_003252

answers: continents might have 'drifted'

answers: NDQ_003253

answers: Abraham Ortelius

answers: NDQ_003254

answers: Ortelius

answers: NDQ_003255

answers: Wegener

answers: NDQ_003256

answers: Wegener

answers: NDQ_003257

answers: Abraham Ortelius

answers: NDQ_003258

answers: Abraham Ortelius

text: As with the Oregon Coast Range as a whole, the Southern Oregon Coast Range likely began as an ocean island chain that collided with the continental tectonic plate of North America more than 60 million years ago. In the Southern Range the 64‑million-year-old Roseburg volcanics that formed this section are the oldest portions of the entire range. The range is part of a forearc basin that has slowly rotated about 51 degrees since the Eocene period. Much of the mountain structures are pillow basalt formations created during the volcanic period and then uplifted with the collision into the continental plate. Other geologic features are mainly the result of erosion and weather forces carving steam beds and valleys out of the rock formations.

text: As with the Oregon Coast Range as a whole, the Southern Oregon Coast Range likely began as an ocean island chain that collided with the continental

text: tectonic plate

text: of

text: North America

text: more than 60 million years ago. In the Southern Range the 64‑million-year-old

text: Roseburg volcanics

text: that formed this section are the oldest portions of the entire range. The range is part of a forearc basin that has slowly rotated about 51 degrees since the Eocene period. Much of the mountain structures are

text: pillow basalt

text: formations created during the volcanic period and then uplifted with the collision into the continental plate. Other geologic features are mainly the result of

text: erosion

text: and weather forces carving steam beds and valleys out of the rock formations.

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answers: NDQ_003252

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answers: NDQ_003258

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answers: NDQ_003219

answers: continental tectonic plate

answers: NDQ_003220

answers: Oregon Coast Range

answers: NDQ_003221

answers: Eocene

answers: NDQ_003222

answers: collided with the continental tectonic plate

answers: NDQ_003223

answers: the collision into the continental plate

answers: NDQ_003224

answers: roseburg volcanics

answers: NDQ_003225

answers: an ocean island chain

answers: NDQ_003226

answers: Oregon Coast Range

answers: NDQ_003227

answers: began as an ocean island chain that collided with the continental tectonic plate

answers: NDQ_003228

answers: continental tectonic plate

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: forearc

answers: NDQ_003233

answers: The range is part of a forearc basin that has slowly rotated about 51 degrees since the Eocene period

answers: NDQ_003236

answers: continental tectonic plate

answers: NDQ_003237

answers: mountain structures are pillow basalt formations created during the volcanic period

answers: NDQ_003239

answers: collided with the continental tectonic plate

answers: NDQ_003240

answers: North America

answers: NDQ_003241

answers: North America

answers: NDQ_003242

answers: continental tectonic plate

answers: NDQ_003244

answers: ocean island chain

answers: NDQ_003246

answers: continental tectonic plate

answers: NDQ_003247

answers: roseburg volcanics that formed this section are the oldest portions of the entire range

answers: NDQ_003252

answers: continental tectonic plate

answers: NDQ_003253

answers: continental tectonic plate

answers: NDQ_003254

answers: It was widely accepted as soon as it was introduced

answers: NDQ_003255

answers: roseburg volcanics that formed this section are the oldest portions of the entire range

answers: NDQ_003256

answers: ocean island chain that collided with the continental tectonic plate

answers: NDQ_003257

answers: The Southern Oregon Coast Range likely began as an ocean island chain

answers: NDQ_003258

answers: collided with the continental tectonic plate

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.

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answers: oil and gas fields may reflect influences from multiple geological periods and events

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answers: geological structures

answers: NDQ_003225

answers: dominant geological event

answers: NDQ_003226

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answers: NDQ_003227

answers: classify the subsurface characteristics, or tectonic setting

answers: NDQ_003228

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answers: NDQ_003230

answers: North America

answers: NDQ_003231

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answers: NDQ_003236

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answers: NDQ_003239

answers: Any one oil and gas field may reflect influences from multiple geological periods

answers: NDQ_003240

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answers: no

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answers: Any one oil and gas field may reflect influences from multiple geological periods

answers: NDQ_003252

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answers: Any one oil and gas field

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answers: Pangaea broke up a short time ago

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answers: geological event

text: Factors that can shape climate are called climate forcings or "forcing mechanisms". These include processes such as variations in solar radiation, variations in the Earth's orbit, variations in the albedo or reflectivity of the continents and oceans, mountain-building and continental drift and changes in greenhouse gas concentrations. There are a variety of climate change feedbacks that can either amplify or diminish the initial forcing. Some parts of the climate system, such as the oceans and ice caps, respond more slowly in reaction to climate forcings, while others respond more quickly.  There are also key threshold factors which when exceeded can produce rapid change.

text: Factors that can shape climate are called

text: climate forcing

text: s or "forcing mechanisms". These include processes such as variations in

text: solar radiation

text: , variations in the Earth's orbit, variations in the

text: albedo

text: or reflectivity of the continents and oceans,

text: mountain-building

text: and

text: continental drift

text: and changes in

text: greenhouse gas

text: concentrations. There are a variety of

text: climate change feedbacks

text: that can either amplify or diminish the initial forcing. Some parts of the climate system, such as the oceans and ice caps, respond more slowly in reaction to climate forcings, while others respond more quickly.  There are also key

text: threshold factors

text: which when exceeded can produce rapid change.

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answers: the Earth's orbit

answers: NDQ_003220

answers: can shape climate

answers: NDQ_003221

answers: 19th century

answers: NDQ_003222

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answers: NDQ_003223

answers: Earth's orbit

answers: NDQ_003224

answers: mountain-building

answers: NDQ_003225

answers: climate forcings

answers: NDQ_003226

answers: Earth's orbit

answers: NDQ_003227

answers: mountain-building and continental drift

answers: NDQ_003228

answers: mountain-building and continental drift

answers: NDQ_003230

answers: Earth

answers: NDQ_003231

answers: Earth's orbit

answers: NDQ_003233

answers: mountain-building

answers: NDQ_003236

answers: continental drift

answers: NDQ_003237

answers: mountain-building

answers: NDQ_003239

answers: mountain-building

answers: NDQ_003240

answers: Earth

answers: NDQ_003241

answers: Earth's orbit

answers: NDQ_003242

answers: climate forcings

answers: NDQ_003244

answers: continent drift

answers: NDQ_003246

answers: continent drift

answers: NDQ_003247

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answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: continental drift

answers: NDQ_003254

answers: It was widely accepted

answers: NDQ_003255

answers: mountain-building and continental drift

answers: NDQ_003256

answers: climate forcings or "forcing mechanisms

answers: NDQ_003257

answers: Pangaea

answers: NDQ_003258

answers: continental drift

text: According to the Köppen climate classification, Västerås experiences a humid continental climate with cold winters and warm summers.

text: According to the

text: Köppen climate classification

text: , Västerås experiences a

text: humid continental climate

text: with cold winters and warm summers.

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answers: NDQ_003221

answers: Köppen

answers: NDQ_003222

answers: continental drift

answers: NDQ_003223

answers: Köppen

answers: NDQ_003224

answers: continental climate

answers: NDQ_003225

answers: Köppen

answers: NDQ_003226

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answers: NDQ_003228

answers: Köppen

answers: NDQ_003230

answers: Västers

answers: NDQ_003231

answers: magnetism

answers: NDQ_003233

answers: Köppen climate classification

answers: NDQ_003236

answers: continental climate

answers: NDQ_003237

answers: Köppen climate classification

answers: NDQ_003239

answers: continental drift

answers: NDQ_003240

answers: continental

answers: NDQ_003241

answers: The magnetic north pole and geographic north pole are in the same location

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answers: Köppen

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answers: NDQ_003253

answers: Köppen climate classification

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answers: Wegener and his supporters

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answers: Köppen climate classification

answers: NDQ_003257

answers: The Köppen climate classification

answers: NDQ_003258

answers: Köppen climate classification

text: One famous example is the coelacanth, which was thought to have become extinct in the very late Cretaceous – until a live specimen was caught in 1938.  The animals known as "Burgess Shale type fauna" are best known from rocks of the Early and Middle Cambrian periods. Since 2006, though, a few fossils of similar animals have been found in rocks from the Ordovician, Silurian, and Early Devonian periods, in other words up to 100 million years after the Burgess Shale. The particular way in which such animals have been fossilized may depend on types of ocean chemistry that were present for limited periods of time.

text: One famous example is the

text: coelacanth

text: , which was thought to have become extinct in the very late

text: Cretaceous

text: – until a live specimen was caught in 1938.  The animals known as "

text: Burgess Shale type fauna

text: " are best known from rocks of the Early and Middle

text: Cambrian

text: periods. Since 2006, though, a few fossils of similar animals have been found in rocks from the

text: Ordovician

text: Silurian

text: , and Early

text: Devonian

text: periods, in other words up to 100 million years after the Burgess Shale. The

text: particular way

text: in which such animals have been fossilized may depend on types of ocean chemistry that were present for limited periods of time.

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answers: NDQ_003219

answers: ocean chemistry

answers: NDQ_003220

answers: Devonian

answers: NDQ_003221

answers: Cretaceous

answers: NDQ_003222

answers: fossils of similar animals have been found in rocks

answers: NDQ_003223

answers: the Burgess Shale

answers: NDQ_003224

answers: Cretaceous

answers: NDQ_003225

answers: "Burgess Shale type fauna"

answers: NDQ_003226

answers: Cambrian

answers: NDQ_003227

answers: 100 million years after the Burgess Shale

answers: NDQ_003228

answers: coelacanth

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: magnetic field

answers: NDQ_003233

answers: Since 2006, though, a few fossils of similar animals have been found in rocks from the Ordovician, Silurian, and Early Devonian periods

answers: NDQ_003236

answers: Cretaceous

answers: NDQ_003237

answers: coelacanth

answers: NDQ_003239

answers: fossil records across continents was evidence for continental drift

answers: NDQ_003240

answers: North America

answers: NDQ_003241

answers: The particular way in which such animals have been fossilized

answers: NDQ_003242

answers: ocean chemistry

answers: NDQ_003244

answers: It is on a continent

answers: NDQ_003246

answers: continents have never been together as a single whole continent

answers: NDQ_003247

answers: The particular way in which such animals have been fossilized may depend on types of ocean chemistry that were present for limited periods of time

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: ocean chemistry

answers: NDQ_003254

answers: It was thought to have become extinct

answers: NDQ_003255

answers: the coelacanth

answers: NDQ_003256

answers: The animals known as "Burgess Shale type fauna

answers: NDQ_003257

answers: Pangaea

answers: NDQ_003258

answers: ocean chemistry that were present for limited periods of time

text: According to satellite measurements, the total area of the glaciation in the Tavan Bogd massif area amounted to 204 km in 2009. The glaciates area was 213 km in 1989; in other words, the glaciers lost 4.2% of their area over the 20 years.

text: According to satellite measurements, the total area of the glaciation in the Tavan Bogd massif area amounted to 204 km in 2009. The glaciates area was 213 km in 1989; in other words, the glaciers lost 4.2% of their area over the 20 years.

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answers: NDQ_003219

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answers: NDQ_003220

answers: 0

answers: NDQ_003221

answers: 0

answers: NDQ_003222

answers: 2

answers: NDQ_003223

answers: 0

answers: NDQ_003224

answers: 0

answers: NDQ_003225

answers: 0

answers: NDQ_003226

answers: 0

answers: NDQ_003227

answers: 0

answers: NDQ_003228

answers: 0

answers: NDQ_003230

answers: 0

answers: NDQ_003231

answers: 0

answers: NDQ_003233

answers: 0

answers: NDQ_003236

answers: 0

answers: NDQ_003237

answers: 0

answers: NDQ_003239

answers: 0

answers: NDQ_003240

answers: 0

answers: NDQ_003241

answers: 0

answers: NDQ_003242

answers: 0

answers: NDQ_003244

answers: 0

answers: NDQ_003246

answers: 0

answers: NDQ_003247

answers: 0

answers: NDQ_003252

answers: 4

answers: NDQ_003253

answers: 0

answers: NDQ_003254

answers: 0

answers: NDQ_003255

answers: 4

answers: NDQ_003256

answers: 0

answers: NDQ_003257

answers: 0

answers: NDQ_003258

answers: 0

answers: NDQ_003219

answers: glaciers lost 4.2% of their area

answers: NDQ_003220

answers: Tavan Bogd

answers: NDQ_003221

answers: late 19th century

answers: NDQ_003222

answers: glaciers lost 4.2% of their area

answers: NDQ_003223

answers: Tavan Bogd

answers: NDQ_003224

answers: glaciation

answers: NDQ_003225

answers: glaciers lost 4.2% of their area

answers: NDQ_003226

answers: Europe

answers: NDQ_003227

answers: lost 4.2% of their area over the 20 years

answers: NDQ_003228

answers: satellite measurements

answers: NDQ_003230

answers: South America

answers: NDQ_003231

answers: massif

answers: NDQ_003233

answers: The glaciers lost 4.2% of their area over the 20 years

answers: NDQ_003236

answers: glaciers lost 4.2% of their area over the 20 years

answers: NDQ_003237

answers: the glaciation in the Tavan Bogd massif area

answers: NDQ_003239

answers: The glaciates area was 213 km in 1989

answers: NDQ_003240

answers: Tavan Bogd

answers: NDQ_003241

answers: The magnetic north pole and geographic north pole are in the same location

answers: NDQ_003242

answers: glaciation

answers: NDQ_003244

answers: Antarctic

answers: NDQ_003246

answers: The continents

answers: NDQ_003247

answers: Tavan Bogd massif

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: Tavan Bogd massif

answers: NDQ_003254

answers: Wegener hypothesis of continental drift

answers: NDQ_003255

answers: The glaciers lost 4.2% of their area over the 20 years

answers: NDQ_003256

answers: Tavan Bogd massif

answers: NDQ_003257

answers: Pangaea broke up a short time ago

answers: NDQ_003258

answers: The glaciers lost 4.2% of their area over the 20 years

text: The site of the Princeton Chert (Ashnola in older sources) and its fossils have been known since the 1950s, but have recently attracted increased attention. This may be due to the rare type of silica permineralized fossil Lagerstätten found, which has preserved plants and animals in minute 3D detail, with exceptional internal cellular detail. This has meant anatomical descriptions and reconstruction of whole plants from isolated parts has been possible in many species. Few plant fossils elsewhere in the world exhibit such excellence in both preservation and diversity. Similar aged fossil beds in Eocene lake sediments are found elsewhere in British Columbia, including in Driftwood Canyon Provincial Park near Smithers in northern British Columbia, and the McAbee Fossil Beds west of Kamloops, about  NNW of the Princeton Chert beds.

text: The site of the Princeton Chert (Ashnola in older sources) and its fossils have been known since the 1950s, but have recently attracted increased attention. This may be due to the rare type of silica permineralized fossil

text: Lagerstätten

text: found, which has preserved plants and animals in minute 3D detail, with exceptional internal cellular detail. This has meant anatomical descriptions and reconstruction of whole plants from isolated parts has been possible in many species. Few plant fossils elsewhere in the world exhibit such excellence in both preservation and diversity. Similar aged fossil beds in

text: Eocene

text: lake sediments are found elsewhere in

text: British Columbia

text: , including in

text: Driftwood Canyon Provincial Park

text: near

text: Smithers

text: in northern British Columbia, and the

text: McAbee Fossil Beds

text: west of

text: Kamloops

text: , about  NNW of the Princeton Chert beds.

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answers: NDQ_003219

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answers: NDQ_003220

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answers: NDQ_003221

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answers: NDQ_003222

answers: 0

answers: NDQ_003223

answers: 0

answers: NDQ_003224

answers: 0

answers: NDQ_003225

answers: 0

answers: NDQ_003226

answers: 0

answers: NDQ_003227

answers: 0

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answers: 0

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answers: 4

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answers: 4

answers: NDQ_003253

answers: 0

answers: NDQ_003254

answers: 0

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answers: 4

answers: NDQ_003256

answers: 0

answers: NDQ_003257

answers: 0

answers: NDQ_003258

answers: 0

answers: NDQ_003219

answers: Eocene

answers: NDQ_003220

answers: British Columbia

answers: NDQ_003221

answers: 1950s

answers: NDQ_003222

answers: The site of the Princeton Chert

answers: NDQ_003223

answers: Eocene

answers: NDQ_003224

answers: fossils

answers: NDQ_003225

answers: The site of the Princeton Chert

answers: NDQ_003226

answers: British Columbia

answers: NDQ_003227

answers: Eocene lake sediments

answers: NDQ_003228

answers: anatomical descriptions

answers: NDQ_003230

answers: British Columbia

answers: NDQ_003231

answers: permineralized

answers: NDQ_003233

answers: Driftwood Canyon Provincial Park near Smithers in northern British Columbia

answers: NDQ_003236

answers: This may be due to the rare type of silica permineralized fossil Lagerstätten found

answers: NDQ_003237

answers: The site of the Princeton Chert

answers: NDQ_003239

answers: Few plant fossils elsewhere in the world

answers: NDQ_003240

answers: North America

answers: NDQ_003241

answers: British Columbia

answers: NDQ_003242

answers: sedimentary

answers: NDQ_003244

answers: British Columbia

answers: NDQ_003246

answers: British Columbia

answers: NDQ_003247

answers: fossil beds in Eocene lake sediments

answers: NDQ_003252

answers: plate tectonics

answers: NDQ_003253

answers: The Princeton Chert (Ashnola in older sources)

answers: NDQ_003254

answers: It has meant anatomical descriptions and reconstruction of whole plants from isolated parts

answers: NDQ_003255

answers: The site of the Princeton Chert

answers: NDQ_003256

answers: similar aged fossil beds in Eocene lake sediments

answers: NDQ_003257

answers: Pangaea broke up a short time ago

answers: NDQ_003258

answers: The Princeton Chert

text: A plant fossil is any preserved part of a plant that has long since died. Such fossils may be prehistoric impressions that are many millions of years old, or bits of charcoal that are only a few hundred years old. Prehistoric plants are various groups of plants that lived before recorded history (before about 3500 BC).

text: A

text: plant

text: fossil

text: is any preserved part of a

text: plant

text: that has long since died. Such fossils may be prehistoric impressions that are many millions of years old, or bits of

text: charcoal

text: that are only a few hundred years old. Prehistoric plants are various groups of plants that lived before recorded

text: history

text: (before about

text: 3500 BC

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answers: NDQ_003231

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answers: 3

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answers: 3

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answers: 0

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answers: 0

answers: NDQ_003255

answers: 0

answers: NDQ_003256

answers: 0

answers: NDQ_003257

answers: 0

answers: NDQ_003258

answers: 0

answers: NDQ_003219

answers: plants that lived before recorded history

answers: NDQ_003220

answers: Atlantic Ocean

answers: NDQ_003221

answers: 3500 BC

answers: NDQ_003222

answers: fossils

answers: NDQ_003223

answers: 3500 BC

answers: NDQ_003224

answers: fossils

answers: NDQ_003225

answers: A plant fossil

answers: NDQ_003226

answers: Europe

answers: NDQ_003227

answers: Many millions of years old

answers: NDQ_003228

answers: fossils

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: magnetic field

answers: NDQ_003233

answers: fossils

answers: NDQ_003236

answers: Many millions of years old

answers: NDQ_003237

answers: fossils

answers: NDQ_003239

answers: Similar fossil records across continents was evidence for continental drift

answers: NDQ_003240

answers: North America

answers: NDQ_003241

answers: no

answers: NDQ_003242

answers: fossils

answers: NDQ_003244

answers: The continent it is on has drifted

answers: NDQ_003246

answers: continents have never been together as a single whole continent

answers: NDQ_003247

answers: The locations of ancient climate zones provide evidence for continental drift

answers: NDQ_003252

answers: plate tectonics

answers: NDQ_003253

answers: prehistoric impressions

answers: NDQ_003254

answers: Wegener's hypothesis of continental drift

answers: NDQ_003255

answers: fossils

answers: NDQ_003256

answers: fossils

answers: NDQ_003257

answers: 3500 BC

answers: NDQ_003258

answers: continents can drift

text: The group's performance was used on the Rolling Stones' song "Continental Drift" on their 1989 Steel Wheels album, whose recording was documented in author Paul Bowles' Tangier journal, Days and in journalist Stephen Davis's history of the Rolling Stones, Old Gods Almost Dead. An online African Music Encyclopedia quoted Mick Jagger as calling the group "one of the most musically inspiring groups still left on the planet". Also in 1989, they toured a couple of dates with Ornette Coleman. In 1992, Axiom released the album Apocalypse Across the Sky, recorded in 1991 and produced by Bill Laswell. A track from the 1991 sessions also was featured on the 1994 Bill Laswell-produced Lost in the Translation: Axiom Ambient various artists compilation.

text: The group's performance was used on the Rolling Stones' song "Continental Drift" on their 1989 Steel Wheels album, whose recording was documented in author

text: Paul Bowles

text: ' Tangier journal, Days and in journalist

text: Stephen Davis

text: 's history of the Rolling Stones, Old Gods Almost Dead. An online African Music Encyclopedia quoted

text: Mick Jagger

text: as calling the group "one of the most musically inspiring groups still left on the planet". Also in 1989, they toured a couple of dates with Ornette Coleman. In 1992,

text: Axiom

text: released the album Apocalypse Across the Sky, recorded in 1991 and produced by

text: Bill Laswell

text: . A track from the 1991 sessions also was featured on the 1994 Bill Laswell-produced Lost in the Translation: Axiom Ambient various artists compilation.

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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.

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text: Chinese pottery can also classified as being either northern or southern.  China comprises two separate and geologically different land masses, brought together by the action of continental drift and forming a junction that lies between the Yellow and Yangtze rivers, sometimes known as the Nanshan-Qinling divide. The contrasting geology of the north and south led to differences in the raw materials available for making ceramics; in particular the north lacks petunse or "porcelain stone", needed for porcelain on the strict definition.  Ware-types can be from very widespread kiln-sites in either north or south China, but the two can nearly always be distinguished, and influences across this divide may affect shape and decoration, but will be based on very different clay bodies, with fundamental effects.  The kiln types were also different. Southern materials have high silica, low alumina and high potassium oxide, the reverse of northern materials in each case.  The northern materials are often very suitable for stoneware, while in the south there are also areas highly suitable for porcelain.

text: Chinese pottery can also classified as being either northern or southern.  China comprises two separate and geologically different land masses, brought together by the action of

text: continental drift

text: and forming a junction that lies between the

text: Yellow

text: and

text: Yangtze

text: rivers, sometimes known as the Nanshan-Qinling divide. The contrasting geology of the north and south led to differences in the raw materials available for making ceramics; in particular the north lacks

text: petunse

text: or "porcelain stone", needed for porcelain on the strict definition.  Ware-types can be from very widespread kiln-sites in either north or south China, but the two can nearly always be distinguished, and influences across this divide may affect shape and decoration, but will be based on very different clay bodies, with fundamental effects.  The kiln types were also different. Southern materials have high

text: silica

text: , low

text: alumina

text: and high

text: potassium oxide

text: , the reverse of northern materials in each case.  The northern materials are often very suitable for stoneware, while in the south there are also areas highly suitable for porcelain.

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text: Continental Drifts, 16 July, at Rough Trade East, Tower Hamlets

text: Continental Drifts, 16 July, at

text: Rough Trade East

text: Tower Hamlets

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answers: 4: The answer has limited relevance and completeness, with noticeable gaps or inaccuracies.

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answers: 4

answers: NDQ_003219

answers: continental drifts

answers: NDQ_003220

answers: The Rocky Mountains

answers: NDQ_003221

answers: 18th century

answers: NDQ_003222

answers: Continental drifts, 16 July

answers: NDQ_003223

answers: volcanoes

answers: NDQ_003224

answers: Evidence for continental drift comes from ancient

answers: NDQ_003225

answers: Continental drifts

answers: NDQ_003226

answers: Europe

answers: NDQ_003227

answers: Continental Drifts

answers: NDQ_003228

answers: Continental Drifts

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: magnetic field

answers: NDQ_003233

answers: Rough Trade East, Tower Hamlets

answers: NDQ_003236

answers: Drifts is a term used to describe the movement of continents.

answers: NDQ_003237

answers: Continental Drifts, 16 July

answers: NDQ_003239

answers: fossil records across continents was evidence for continental drift

answers: NDQ_003240

answers: continental drifts

answers: NDQ_003241

answers: The magnetic north pole and geographic north pole are the same location.

answers: NDQ_003242

answers: continental drifts

answers: NDQ_003244

answers: continental drifts

answers: NDQ_003246

answers: The continents have never all been together

answers: NDQ_003247

answers: Rough Trade East, Tower Hamlets

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: The continents were once joined together.

answers: NDQ_003254

answers: It was widely accepted as soon as it was introduced.

answers: NDQ_003255

answers: Wegener and his supporters

answers: NDQ_003256

answers: The Atlantic Ocean

answers: NDQ_003257

answers: Pangaea broke up a short time ago

answers: NDQ_003258

answers: Wegener

text: The area is characterized by humid continental climate which typically has a large seasonal temperature difference, with warm to hot (and often humid) summers and cold (sometimes severely cold) winters. Precipitation is relatively well distributed year-round in many areas with this climate, while others may see a marked reduction in wintry precipitation and even a wintertime drought.  The Köppen Climate Classification subtype for this climate is "Dfa" (Hot Summer Continental Climate).

text: The area is characterized by humid continental climate which typically has a large seasonal temperature difference, with warm to hot (and often humid) summers and cold (sometimes severely cold) winters. Precipitation is relatively well distributed year-round in many areas with this climate, while others may see a marked reduction in wintry precipitation and even a wintertime drought.  The

text: Köppen Climate Classification

text: subtype for this climate is "

text: Dfa

text: " (Hot Summer Continental Climate).

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answers: NDQ_003252

answers: 4

answers: NDQ_003253

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answers: NDQ_003254

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answers: NDQ_003255

answers: 4

answers: NDQ_003256

answers: 0

answers: NDQ_003257

answers: 0

answers: NDQ_003258

answers: 0

answers: NDQ_003219

answers: continental climate

answers: NDQ_003220

answers: are characterized by humid continental climate

answers: NDQ_003221

answers: 18th century

answers: NDQ_003222

answers: large seasonal temperature difference

answers: NDQ_003223

answers: Dfa

answers: NDQ_003224

answers: Köppen Climate Classification subtype

answers: NDQ_003225

answers: Hot Summer Continental Climate

answers: NDQ_003226

answers: continental climate

answers: NDQ_003227

answers: large seasonal temperature difference

answers: NDQ_003228

answers: Köppen Climate Classification

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: magnetic field

answers: NDQ_003233

answers: Köppen Climate Classification subtype for this climate

answers: NDQ_003236

answers: continental climate

answers: NDQ_003237

answers: large seasonal temperature difference

answers: NDQ_003239

answers: The area is characterized by humid continental climate

answers: NDQ_003240

answers: North America

answers: NDQ_003241

answers: no

answers: NDQ_003242

answers: continental climate

answers: NDQ_003244

answers: Dfa

answers: NDQ_003246

answers: continents

answers: NDQ_003247

answers: Köppen Climate Classification subtype

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: It is characterized by humid continental climate

answers: NDQ_003254

answers: It was widely accepted

answers: NDQ_003255

answers: The area is characterized by humid continental climate

answers: NDQ_003256

answers: Dfa

answers: NDQ_003257

answers: The area is characterized by humid continental climate

answers: NDQ_003258

answers: The area is characterized by humid continental climate

text: In 1906 he became professor at Delft University and this time he got enough resources and students to make his work successful. The same year he became member of the Royal Netherlands Academy of Arts and Sciences. In 1910-1911 he led a geological expedition to Timor. His research at Delft was mainly on the material collected during that expedition, and (together with W.A.J.M. van Waterschoot van der Gracht) on the geology of the Netherlands. In 1927 he was a guide of the Shaler Memorial Expedition to South Africa, organized by Harvard University. On the expedition he met Alexander Du Toit, both geologists were among the (at that time rare) supporters of Alfred Wegeners' continental drift theory.

text: In 1906 he became professor at

text: Delft University

text: and this time he got enough resources and students to make his work successful. The same year he became member of the

entity_name: Royal Netherlands Academy of Arts and Sciences

text: Royal Netherlands Academy of Arts and Sciences

text: . In 1910-1911 he led a geological expedition to

text: Timor

text: . His research at

text: Delft

text: was mainly on the material collected during that expedition, and (together with

text: W.A.J.M. van Waterschoot van der Gracht

text: ) on the geology of the Netherlands. In 1927 he was a guide of the

text: Shaler Memorial Expedition

text: to South Africa, organized by

text: Harvard University

text: . On the expedition he met

text: Alexander Du Toit

text: , both geologists were among the (at that time rare) supporters of

text: Alfred Wegener

text: s'

text: continental drift

text: theory.

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answers: NDQ_003220

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answers: NDQ_003221

answers: 1927

answers: NDQ_003222

answers: rare

answers: NDQ_003223

answers: continental drift

answers: NDQ_003224

answers: Timor

answers: NDQ_003225

answers: continental drift theory

answers: NDQ_003226

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answers: NDQ_003230

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answers: NDQ_003231

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answers: Alexander Du Toit

answers: NDQ_003236

answers: continental drift theory

answers: NDQ_003237

answers: On the expedition he met Alexander Du Toit

answers: NDQ_003239

answers: on the geology of the Netherlands

answers: NDQ_003240

answers: Timor

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answers: Alexander Du Toit

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answers: On the expedition he met Alexander Du Toit

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answers: continental drift theory

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answers: continental drift theory

text: Fossils are the preserved remains or traces of animals, plants, and other organisms from the remote past. The totality of fossils, both discovered and undiscovered, and their placement in fossil-containing rock formations and sedimentary layers (strata) is known as the fossil record. A preserved specimen is called a fossil if it is older than the arbitrary date of 10,000 years ago. Hence, fossils range in age from the youngest at the start of the Holocene Epoch to the oldest from the Archaean Eon, up to 3.4 billion years old.

text: Fossils are the preserved remains or

text: traces

text: of animals, plants, and other organisms from the remote past. The totality of fossils, both discovered and undiscovered, and their placement in fossil-containing

text: rock

text: formations and

text: sedimentary

text: layers (

text: strata

text: ) is known as the fossil record. A preserved specimen is called a fossil if it is older than the arbitrary date of 10,000 years ago. Hence, fossils range in age from the youngest at the start of the

text: Holocene

text: Epoch to the oldest from the

text: Archaean

text: Eon, up to 3.4

text: billion

text: years old.

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answers: fossils range in age

answers: NDQ_003220

answers: Atlantic Ocean

answers: NDQ_003221

answers: Archaean

answers: NDQ_003222

answers: Fossils

answers: NDQ_003223

answers: Archaean

answers: NDQ_003224

answers: Archaean Eon

answers: NDQ_003225

answers: fossil record

answers: NDQ_003226

answers: Europe

answers: NDQ_003227

answers: 3.4 billion years old

answers: NDQ_003228

answers: 3.4 billion years old

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: Strato

answers: NDQ_003233

answers: Fossils

answers: NDQ_003236

answers: strata

answers: NDQ_003237

answers: Fossils

answers: NDQ_003239

answers: Fossils

answers: NDQ_003240

answers: Archaean Eon

answers: NDQ_003241

answers: no

answers: NDQ_003242

answers: Holocene Epoch

answers: NDQ_003244

answers: Fossils

answers: NDQ_003246

answers: Fossils

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answers: Fossils

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answers: Fossils

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answers: Fossils

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answers: Fossils

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answers: Pangaea

answers: NDQ_003258

answers: Fossils

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.

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text: Generally, products made from fossilized or decomposed animals, such as petroleum formed from the ancient remains of marine animals, are not considered animal products. Crops grown in soil fertilized with animal remains are rarely characterized as animal products.

text: Generally, products made from fossilized or decomposed animals, such as

text: petroleum

text: formed

text: from the ancient remains of marine animals, are not considered animal products. Crops grown in soil

text: fertilized

text: with animal remains are rarely characterized as animal products.

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answers: NDQ_003231

answers: magnetic field

answers: NDQ_003233

answers: petroleum formed from the ancient remains of marine animals

answers: NDQ_003236

answers: is not considered animal products

answers: NDQ_003237

answers: fossilized or decomposed animals

answers: NDQ_003239

answers: similar fossil records across continents

answers: NDQ_003240

answers: Oceania

answers: NDQ_003241

answers: no

answers: NDQ_003242

answers: marine

answers: NDQ_003244

answers: drifted

answers: NDQ_003246

answers: continents

answers: NDQ_003247

answers: fossilized or decomposed animals

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: marine

answers: NDQ_003254

answers: products made from fossilized or decomposed animals

answers: NDQ_003255

answers: products made from fossilized or decomposed animals

answers: NDQ_003256

answers: fossilized or decomposed animals

answers: NDQ_003257

answers: Pangaea

answers: NDQ_003258

answers: fossilized or decomposed

text: Fossil plants from the same area as the McAbee fossil beds (Cache Creek and Kamloops B.C.) were first reported by G.M. Dawson. Palaeontological and geological studies of the McAbee Fossil Beds are more recent, however, going back at least to research in the 1960s and early 1970s by Dr. Len Hills of the University of Calgary and his students on the fossil spores and pollen (palynology) and the leaf fossils, and research on the fossil fish from the fossil beds by Dr. Mark Wilson of the University of Alberta. Thomas Ewing provided a detailed analysis of the geology of the Kamloops Group, including the McAbee beds.  Significant research on the fossil plants and insects has only occurred since the late 1980s.<ref name="Greenwood1995">{{cite journal |last1=Greenwood |first1=D.R. |last2=Wing |first2=S.L. |year=1995 |title=Eocene continental climates and latitudinal temperature gradients |journal=Geology |volume=23 |issue=11 |pages=1044–1048 |doi=10.1130/0091-7613(1995)023

text: Fossil plants from the same area as the McAbee fossil beds (

text: Cache Creek

text: and

text: Kamloops

text: B.C.) were first reported by G.M.

text: Dawson

text: . Palaeontological and geological studies of the McAbee Fossil Beds are more recent, however, going back at least to research in the 1960s and early 1970s by Dr. Len Hills of the

text: University of Calgary

text: and his students on the fossil spores and pollen (

text: palynology

text: ) and the leaf fossils, and research on the

text: fossil fish

text: from the fossil beds by Dr. Mark Wilson of the

text: University of Alberta

text: . Thomas Ewing provided a detailed analysis of the geology of the Kamloops Group, including the McAbee beds.  Significant research on the fossil plants and insects has only occurred since the late 1980s.<ref name="Greenwood1995">{{cite journal |last1=Greenwood |first1=D.R. |last2=Wing |first2=S.L. |year=1995 |title=Eocene continental climates and latitudinal temperature gradients |journal=Geology |volume=23 |issue=11 |pages=1044–1048 |doi=10.1130/0091-7613(1995)023

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answers: 0

answers: NDQ_003222

answers: 0

answers: NDQ_003223

answers: 0

answers: NDQ_003224

answers: 4

answers: NDQ_003225

answers: 0

answers: NDQ_003226

answers: 0

answers: NDQ_003227

answers: 0

answers: NDQ_003228

answers: 0

answers: NDQ_003230

answers: 0

answers: NDQ_003231

answers: 0

answers: NDQ_003233

answers: 0

answers: NDQ_003236

answers: 0

answers: NDQ_003237

answers: 0

answers: NDQ_003239

answers: 0

answers: NDQ_003240

answers: 0

answers: NDQ_003241

answers: 0

answers: NDQ_003242

answers: 0

answers: NDQ_003244

answers: 0

answers: NDQ_003246

answers: 3

answers: NDQ_003247

answers: 4

answers: NDQ_003252

answers: 4

answers: NDQ_003253

answers: 0

answers: NDQ_003254

answers: 0

answers: NDQ_003255

answers: 0

answers: NDQ_003256

answers: 0

answers: NDQ_003257

answers: 0

answers: NDQ_003258

answers: 0

answers: NDQ_003219

answers: Eocene continental climates and latitudinal temperature gradients

answers: NDQ_003220

answers: Kamloops Group

answers: NDQ_003221

answers: 1980s

answers: NDQ_003222

answers: significant research on the fossil plants and insects has only occurred since the late 1980s

answers: NDQ_003223

answers: Eocene

answers: NDQ_003224

answers: Eocene

answers: NDQ_003225

answers: McAbee fossil beds

answers: NDQ_003226

answers: Canada

answers: NDQ_003227

answers: Latitudinal temperature gradients

answers: NDQ_003228

answers: first reported by G.M. Dawson

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: magnetism

answers: NDQ_003233

answers: significant research on the fossil plants

answers: NDQ_003236

answers: Latitudinal temperature gradients

answers: NDQ_003237

answers: the Kamloops Group

answers: NDQ_003239

answers: Fossil records across continents was evidence for continental drift.

answers: NDQ_003240

answers: Eocene

answers: NDQ_003241

answers: The magnetic north pole and geographic north pole are in the same location

answers: NDQ_003242

answers: Eocene continental climates

answers: NDQ_003244

answers: Fossil fish from the fossil beds

answers: NDQ_003246

answers: The continents have never been together as a single whole continent.

answers: NDQ_003247

answers: The locations of ancient climate zones provide evidence for continental drift.

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: Wegener

answers: NDQ_003254

answers: Greenwood 1995

answers: NDQ_003255

answers: Wegener and his supporters provided a lot of evidence for continental drift.

answers: NDQ_003256

answers: Wegener found rocks of the same type and age on both sides of the Atlantic Ocean

answers: NDQ_003257

answers: The Kamloops Group

answers: NDQ_003258

answers: The McAbee Fossil Beds

text: When Irving started his graduate studies, the history of the Earth's magnetic field was known for the few centuries since the first magnetic observatories had been established. With fellow students Ken Creer and Jan Hospers, he looked to extend this record back in time. Irving used a magnetometer, recently designed by Patrick Blackett, to analyze the magnetic directions imparted to rocks by their iron minerals. He found large discrepancies between the directions of the present magnetic field direction and those recorded in Precambrian rock in the highlands of Scotland. He surmised the only explanation could be that Scotland had shifted relative to the geomagnetic pole. Irving also determined that India had moved northward by 6000 km and rotated by more than . These results confirmed the predictions Alfred Wegener had put forth in his theory of continental drift in 1912.

text: When Irving started his graduate studies, the history of the

text: Earth's magnetic field

text: was known for the few centuries since the first magnetic observatories had been established. With fellow students Ken Creer and Jan Hospers, he looked to extend this record back in time. Irving used a

text: magnetometer

text: , recently designed by

text: Patrick Blackett

text: , to analyze the magnetic directions imparted to rocks by their

text: iron

text: minerals. He found large discrepancies between the directions of the present magnetic field direction and those recorded in

text: Precambrian

text: rock in the highlands of

text: Scotland

text: . He surmised the only explanation could be that Scotland had shifted relative to the

text: geomagnetic pole

text: . Irving also determined that

text: India

text: had moved northward by 6000 km and rotated by more than . These results confirmed the predictions

text: Alfred Wegener

text: had put forth in his theory of

text: continental drift

text: in 1912.

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answers: 4: The answer has limited relevance and completeness, with noticeable gaps or inaccuracy.

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answers: 0

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answers: 4

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answers: 4

answers: NDQ_003219

answers: 4

answers: NDQ_003220

answers: 0

answers: NDQ_003221

answers: 4

answers: NDQ_003222

answers: 0

answers: NDQ_003223

answers: 0

answers: NDQ_003224

answers: 4

answers: NDQ_003225

answers: 4

answers: NDQ_003226

answers: 0

answers: NDQ_003227

answers: 4

answers: NDQ_003228

answers: 0

answers: NDQ_003230

answers: 0

answers: NDQ_003231

answers: 0

answers: NDQ_003233

answers: 4

answers: NDQ_003236

answers: 4

answers: NDQ_003237

answers: 4

answers: NDQ_003239

answers: 4

answers: NDQ_003240

answers: 0

answers: NDQ_003241

answers: 4

answers: NDQ_003242

answers: 4

answers: NDQ_003244

answers: 0

answers: NDQ_003246

answers: 4

answers: NDQ_003247

answers: 4

answers: NDQ_003252

answers: 4

answers: NDQ_003253

answers: 4

answers: NDQ_003254

answers: 0

answers: NDQ_003255

answers: 4

answers: NDQ_003256

answers: 0

answers: NDQ_003257

answers: 0

answers: NDQ_003258

answers: 4

answers: NDQ_003219

answers: continental drift

answers: NDQ_003220

answers: highlands

answers: NDQ_003221

answers: 1912

answers: NDQ_003222

answers: the history of the Earth's magnetic field

answers: NDQ_003223

answers: Scotland had shifted relative to the geomagnetic pole

answers: NDQ_003224

answers: Precambrian rock

answers: NDQ_003225

answers: theory of continental drift

answers: NDQ_003226

answers: Scotland

answers: NDQ_003227

answers: theory of continental drift

answers: NDQ_003228

answers: continental drift

answers: NDQ_003230

answers: North America

answers: NDQ_003231

answers: magnetic field

answers: NDQ_003233

answers: India had moved northward by 6000 km and rotated by more than

answers: NDQ_003236

answers: continental drift

answers: NDQ_003237

answers: These results confirmed the predictions Alfred Wegener had put forth in his theory of continental drift in 1912

answers: NDQ_003239

answers: These results confirmed the predictions Alfred Wegener had put forth in his theory of continental drift in 1912.

answers: NDQ_003240

answers: Earth

answers: NDQ_003241

answers: Earth's magnetic field

answers: NDQ_003242

answers: theory of continental drift

answers: NDQ_003244

answers: Scotland

answers: NDQ_003246

answers: Scotland had shifted relative to the geomagnetic pole

answers: NDQ_003247

answers: Scotland had shifted relative to the geomagnetic pole

answers: NDQ_003252

answers: plate tectonics

answers: NDQ_003253

answers: theory of continental drift

answers: NDQ_003254

answers: It was widely accepted

answers: NDQ_003255

answers: Irving also determined that India had moved northward by 6000 km

answers: NDQ_003256

answers: He found large discrepancies

answers: NDQ_003257

answers: Pangaea broke up a short time ago

answers: NDQ_003258

answers: Alfred Wegener

text: Distinct island flora and fauna have evolved over thousands of years.  Species here often differ from those found on the mainland.  Many common continental species are not found on the islands, or have evolved into unique subspecies such as the black bear which is larger than its mainland cousin.  Other species have been introduced relatively recently, such as the Sitka deer, ermine, raccoon, squirrel and beaver. Introduced species now exist in large numbers, much to the detriment of native plants and animals.

text: Distinct island flora and fauna have evolved over thousands of years.  Species here often differ from those found on the mainland.  Many common continental species are not found on the islands, or have evolved into unique subspecies such as the

text: black bear

text: which is larger than its mainland cousin.  Other species have been introduced relatively recently, such as the

text: Sitka deer

text: ermine

text: raccoon

text: squirrel

text: and

text: beaver

text: . Introduced species now exist in large numbers, much to the detriment of native plants and animals.

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answers: 0

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answers: 0

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answers: 0

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answers: 0

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answers: 0

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answers: 0

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answers: 0

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answers: 0

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answers: 0

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answers: 0

answers: tqa2:L_0076/T_0763/7a7192cbfb0cdb83fb089d3c4f8ea239

answers: 0

answers: NDQ_003219

answers: 0

answers: NDQ_003220

answers: 0

answers: NDQ_003221

answers: 0

answers: NDQ_003222

answers: 2

answers: NDQ_003223

answers: 0

answers: NDQ_003224

answers: 0

answers: NDQ_003225

answers: 0

answers: NDQ_003226

answers: 0

answers: NDQ_003227

answers: 0

answers: NDQ_003228

answers: 0

answers: NDQ_003230

answers: 0

answers: NDQ_003231

answers: 0

answers: NDQ_003233

answers: 0

answers: NDQ_003236

answers: 0

answers: NDQ_003237

answers: 0

answers: NDQ_003239

answers: 0

answers: NDQ_003240

answers: 0

answers: NDQ_003241

answers: 0

answers: NDQ_003242

answers: 0

answers: NDQ_003244

answers: 0

answers: NDQ_003246

answers: 4

answers: NDQ_003247

answers: 0

answers: NDQ_003252

answers: 4

answers: NDQ_003253

answers: 0

answers: NDQ_003254

answers: 0

answers: NDQ_003255

answers: 4

answers: NDQ_003256

answers: 0

answers: NDQ_003257

answers: 0

answers: NDQ_003258

answers: 0

answers: NDQ_003219

answers: continental species are not found

answers: NDQ_003220

answers: mainland

answers: NDQ_003221

answers: late 19th century

answers: NDQ_003222

answers: introduced species now exist in large numbers

answers: NDQ_003223

answers: islands

answers: NDQ_003224

answers: islands

answers: NDQ_003225

answers: the detriment of native plants and animals

answers: NDQ_003226

answers: mainland

answers: NDQ_003227

answers: Introduced species now exist in large numbers

answers: NDQ_003228

answers: physicist

answers: NDQ_003230

answers: mainland

answers: NDQ_003231

answers: subspecies

answers: NDQ_003233

answers: Many common continental species are not found on the islands

answers: NDQ_003236

answers: mainland

answers: NDQ_003237

answers: Many common continental species are not found on the islands

answers: NDQ_003239

answers: Introduced species now exist in large numbers

answers: NDQ_003240

answers: mainland

answers: NDQ_003241

answers: no

answers: NDQ_003242

answers: continental drift

answers: NDQ_003244

answers: mainland

answers: NDQ_003246

answers: Many common continental species are not found on the islands

answers: NDQ_003247

answers: Distinct island flora and fauna

answers: NDQ_003252

answers: continental drift

answers: NDQ_003253

answers: mainland

answers: NDQ_003254

answers: Introduced species now exist in large numbers

answers: NDQ_003255

answers: Many common continental species are not found on the islands

answers: NDQ_003256

answers: The Atlantic Ocean

answers: NDQ_003257

answers: Pangaea

answers: NDQ_003258

answers: Introduced species now exist in large numbers

text: The Acadian orogeny is a long-lasting mountain building event which began in the Middle Devonian, reaching a climax in the early Late Devonian.  It was active for approximately 50 million years, beginning roughly around 375 million years ago, with deformational, plutonic, and metamorphic events extending into the Early Mississippian.  The Acadian orogeny is the third of the four orogenies that created the Appalachian orogen and subsequent basin.  The preceding orogenies consisted of the Potomac and Taconic orogeny, which followed a rift/drift stage in the Late Neoproterozoic.  The Acadian orogeny involved the collision of a series of Avalonian continental fragments with the Laurasian continent.  Geographically, the Acadian orogen extended from the Canadian Maritime provinces migrating in a southwesterly direction toward Alabama.  However, the Northern Appalachian region, from New England northeastern ward into Gaspé region of Canada, was the most greatly affected region by the collision.

text: The Acadian orogeny is a long-lasting

text: mountain

text: building event which began in the Middle

text: Devonian

text: , reaching a climax in the early Late

text: Devonian

text: .  It was active for approximately 50 million years, beginning roughly around 375 million years ago, with deformational,

text: plutonic

text: , and

text: metamorphic

text: events extending into the Early

text: Mississippian

text: .  The Acadian orogeny is the third of the four orogenies that created the

text: Appalachian

text: orogen

text: and subsequent basin.  The preceding orogenies consisted of the Potomac and

text: Taconic orogeny

text: , which followed a rift/drift stage in the Late

text: Neoproterozoic

text: .  The Acadian orogeny involved the collision of a series of

text: Avalonia

text: n continental fragments with the

text: Laurasia

text: n continent.  Geographically, the Acadian orogen extended from the Canadian Maritime provinces migrating in a southwesterly direction toward Alabama.  However, the Northern Appalachian region, from New England northeastern ward into

text: Gaspé

text: region of Canada, was the most greatly affected region by the collision.

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answers: NDQ_003219

answers: continental fragments with the Laurasian continent

answers: NDQ_003220

answers: Canadian Maritime provinces

answers: NDQ_003221

answers: Late Neoproterozoic

answers: NDQ_003222

answers: Acadian orogeny

answers: NDQ_003223

answers: the Late Neoproterozoic

answers: NDQ_003224

answers: Late Neoproterozoic

answers: NDQ_003225

answers: The Acadian orogeny

answers: NDQ_003226

answers: Canada

answers: NDQ_003227

answers: collision of a series of Avalonian continental fragments with the Laurasian continent

answers: NDQ_003228

answers: collision of a series of Avalonian continental fragments with the Laurasian continent

answers: NDQ_003230

answers: Laurasian

answers: NDQ_003231

answers: orogen

answers: NDQ_003233

answers: The Acadian orogeny

answers: NDQ_003236

answers: continental fragments with the Laurasian continent

answers: NDQ_003237

answers: collision of a series of Avalonian continental fragments with the Laurasian continent

answers: NDQ_003239

answers: The Acadian orogeny

answers: NDQ_003240

answers: Avalonian

answers: NDQ_003241

answers: Canadian Maritime provinces

answers: NDQ_003242

answers: rift

answers: NDQ_003244

answers: Acadian orogeny

answers: NDQ_003246

answers: Avalonian continental fragments with the Laurasian continent

answers: NDQ_003247

answers: the Northern Appalachian region, from New England northeastern ward into Gaspé region of Canada

answers: NDQ_003252

answers: The theory of plate tectonics

answers: NDQ_003253

answers: The Acadian orogeny

answers: NDQ_003254

answers: It was active for approximately 50 million years, beginning roughly around 375 million years ago

answers: NDQ_003255

answers: The Acadian orogeny

answers: NDQ_003256

answers: Acadian orogeny

answers: NDQ_003257

answers: The Acadian orogeny

answers: NDQ_003258

answers: The Acadian orogeny

text: Nothing compels citizens to experience time at such a high rate; they can equally choose to "rush", meaning to experience consciousness at a speed slower than the maximum the polis hardware can maintain. Hence citizens could experience consciousness at the same speed as a human flesher would, or slower, or even freeze their conscious state for a set time or until a previously determined event occurs. Citizens in Lokhande Polis have opted to experience consciousness so slowly that they can witness continental drift and geological erosion.

text: Nothing compels citizens to experience time at such a high rate; they can equally choose to "rush", meaning to experience consciousness at a speed slower than the maximum the polis hardware can maintain. Hence citizens could experience consciousness at the same speed as a human flesher would, or slower, or even freeze their conscious state for a set time or until a previously determined event occurs. Citizens in Lokhande Polis have opted to experience consciousness so slowly that they can witness

text: continental drift

text: and geological

text: erosion

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