text: Although Littleton had cast a gloved hand in glass in 1979, it was not until 1989 that he and Vogel began to explore glass casting in earnest. The large, work-worn hands of an artist friend inspired one of their early sculptures; initially cast in plaster, the hands and arms, as well as the faces, of family members and friends, children and adults, appeared in subsequent works. Their “Crystal” series includes blocks of colorless crystal glass, faceted to look like large pieces of rock crystal; in the center of the transparent forms frosty white hands (which are actually hand-shaped voids in the glass) hold small rock crystals aloft. The artists left these crystalline forms in favor of cast cubes of crystal that entrap three-dimensional faces and hands. The human forms soon broke free of the cube, appearing in the round with the fine details of skin texture, wrinkles and hair preserved from the original plaster casting. These works appeared in colorless and purple tinted glass. During the 1990s the glass, tinted blue, mimicked "water" from which colorless glass faces and hands seemed to arise. In the brochure for the a twenty-year retrospective of the artists’ work, Joan Byrd wrote of the dichotomy between the continuing series of Bags and the cast sculptures. In the blown pieces

text: Although Littleton had cast a gloved hand in glass in 1979, it was not until 1989 that he and Vogel began to explore glass casting in earnest. The large, work-worn hands of an artist friend inspired one of their early sculptures; initially cast in plaster, the hands and arms, as well as the faces, of family members and friends, children and adults, appeared in subsequent works. Their “Crystal” series includes blocks of colorless

entity_name: Crystal

text: crystal

text: glass, faceted to look like large pieces of rock crystal; in the center of the transparent forms frosty white hands (which are actually hand-shaped voids in the glass) hold small rock crystals aloft. The artists left these crystalline forms in favor of cast cubes of crystal that entrap three-dimensional faces and hands. The human forms soon broke free of the cube, appearing in the round with the fine details of skin texture, wrinkles and hair preserved from the original plaster casting. These works appeared in colorless and purple tinted glass. During the 1990s the glass, tinted blue, mimicked "water" from which colorless glass faces and hands seemed to arise. In the brochure for the a twenty-year retrospective of the artists’ work, Joan Byrd wrote of the dichotomy between the continuing series of Bags and the cast sculptures. In the blown pieces

method: ICT-DRMMTKS

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answers: The artists left these crystalline forms in favor of cast cubes of crystal that entrap three-dimensional faces and hands

answers: NDQ_005762

answers: The artists left these crystalline forms in favor of cast cubes of crystal that entrap three-dimensional faces and hands

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answers: water

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answers: rock crystal

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answers: Cast cubes of crystal that entrap three-dimensional faces and hands

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answers: The artists left these crystalline forms in favor of cast cubes of crystal that entrap three-dimensional faces and hands

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text: Rock can form layers in a variety of ways.  Volcanoes, wind, or water can produce layers.  Layers can be hardened by the action of groundwater.  Martian ground water probably moved hundreds of kilometers, and in the process it dissolved many minerals from the rock it passed through.  When ground water surfaces in low areas containing sediments, water evaporates in the thin atmosphere and leaves behind minerals as deposits and/or cementing agents. Consequently, layers of dust could not later easily erode away since they were cemented together. On Earth, mineral-rich waters often evaporate forming large deposits of various types of salts and other minerals. Sometimes water flows through Earth's aquifers, and then evaporates at the surface just as is hypothesed for Mars.  One location this occurs on Earth is the Great Artesian Basin of Australia.  On Earth the hardness of many sedimentary rocks, like sandstone, is largely due to the cement that was put in place as water passed through.

text: Rock can form layers in a variety of ways.  Volcanoes, wind, or water can produce layers.  Layers can be hardened by the action of groundwater.  Martian ground water probably moved hundreds of kilometers, and in the process it dissolved many minerals from the rock it passed through.  When ground water surfaces in low areas containing sediments, water evaporates in the thin atmosphere and leaves behind minerals as deposits and/or cementing agents. Consequently, layers of dust could not later easily erode away since they were cemented together. On Earth, mineral-rich waters often evaporate forming large deposits of various types of

entity_name: Salt (chemistry)

text: salts

text: and other

entity_name: Mineral

text: mineral

text: s. Sometimes water flows through Earth's aquifers, and then evaporates at the surface just as is hypothesed for Mars.  One location this occurs on Earth is the

entity_name: Great Artesian Basin

text: Great Artesian Basin

text: of

entity_name: Australia

text: Australia

text: .  On Earth the hardness of many

entity_name: Sedimentary rock

text: sedimentary rock

text: s, like

entity_name: Sandstone

text: sandstone

text: , is largely due to the cement that was put in place as water passed through.

method: Bert-ConvKNRM

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answers: It is out of the rock cycle.

answer: Yes

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answer: 1

text: The basement of the core mountains is formed by the Tatric Unit, which is composed of dominantly hercynian metamorphic and igneous rocks and locally also a sedimentary cover of various thickness. In the Paleozoic clastic and volcanoclastic sediments deposited in the area, but later during Hercynian orogeny, sediments were metamorphosed in the greenschist and amphibolite facies (forming large amount of paragneisses and amphibolites, only locally orthogneisses, phyllites and mica schists). Regional and contact metamorphism was induced also by intrusions of granites, which accompanied the Hercynian collision (generally in the Carboniferous). Basement rocks were later exposed due to erosion and at the end of the Paleozoic affected by marine transgression that lasted till the end of Mesozoic. During this period sedimentary rocks, known as Tatric cover units, deposited. They generally consists of clastic and carbonate rocks.

text: The basement of the core mountains is formed by the

text: Tatric

text: Unit, which is composed of dominantly

entity_name: Variscan orogeny

text: hercynian

entity_name: Metamorphic rock

text: metamorphic

text: and

entity_name: Igneous rock

text: igneous rocks

text: and locally also a sedimentary cover of various thickness. In the

entity_name: Paleozoic

text: Paleozoic

text: clastic and volcanoclastic

entity_name: Sediment

text: sediments

text: deposited in the area, but later during

text: Hercynian orogeny

text: , sediments were metamorphosed in the

entity_name: Greenschist

text: greenschist

text: and

entity_name: Amphibolite

entity_section: Amphibolite facies

text: amphibolite facies

text: (forming large amount of

entity_name: Gneiss

text: paragneiss

text: es and

text: amphibolite

text: s, only locally

text: orthogneiss

text: es,

entity_name: Phyllite

text: phyllite

text: s and

entity_name: Schist

text: mica schist

text: s). Regional and contact metamorphism was induced also by

entity_name: Intrusive rock

text: intrusion

text: s of

entity_name: Granite

text: granite

text: s, which accompanied the Hercynian collision (generally in the

entity_name: Carboniferous

text: Carboniferous

text: ). Basement rocks were later exposed due to

entity_name: Erosion

text: erosion

text: and at the end of the Paleozoic affected by marine

entity_name: Marine transgression

text: transgression

text: that lasted till the end of

entity_name: Mesozoic

text: Mesozoic

text: . During this period

text: sedimentary rocks

text: , known as

text: Tatric cover units

text: , deposited. They generally consists of

entity_name: Clastic rock

text: clastic

text: and

entity_name: Carbonate rock

text: carbonate rock

text: s.

method: UNH-ecn

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text: Cyclostratigraphy is the study of astronomically forced climate cycles within sedimentary successions. Astronomical cycles are variations of the Earth's orbit around the sun due to the gravitational interaction with other masses within the solar system. Due to this cyclicity solar irradiation differs through time on different hemispheres and seasonality is affected. These insolation variations have influence on earth's climate and so on the deposition of sedimentary rocks.

text: Cyclostratigraphy is the study of

entity_name: Astronomy

text: astronomically

text: forced

entity_name: Climate oscillation

text: climate cycle

text: s within

text: sedimentary

text: successions. Astronomical cycles are variations of the Earth's orbit around the sun due to the gravitational interaction with other masses within the solar system. Due to this cyclicity solar irradiation differs through time on different hemispheres and seasonality is affected. These insolation variations have influence on earth's climate and so on the deposition of sedimentary rocks.

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text: Soapstone is a metamorphic rock composed predominantly of talc.

entity_name: Soapstone

text: Soapstone

text: is a

text: metamorphic rock

text: composed predominantly of talc.

method: Bert-DRMMTKS

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text: The pile of sediments were later buried and lithified into solid rock. The layers of rock were later uplifted and tilted to their present angle by the mountain building forces that formed the Uintas during the Laramide orogeny . The relentless forces of erosion exposed the layers at the surface to be found by paleontologists.

text: The pile of sediments were later buried and lithified into solid rock. The layers of rock were later uplifted and tilted to their present angle by the mountain building forces that formed the Uintas during the

text: Laramide orogeny

text: . The relentless forces of

text: erosion

text: exposed the layers at the surface to be found by paleontologists.

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answers: faster cooling forms smaller crystals

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answer: No

answer: No

answer: Yes

answer: No

answer: No

answer: 1

text: The advancing and retreating characteristics of the glaciers in the Glacier Bay are explained in simple terms as a steady state of snow getting converted into ice on the hills. Ice, as a lens of water on the base of bedrock, slides by gravity downwards. The good moraine of rock and rubble insulates it from water erosion. As a result, during freezing temperatures that exists all the year, the glacier advances. When the insulation and erosion effect of the hills gets reduced erosion sets in and along with rising temperatures the glaciers start retreating. Another unpredictable phenomenon that is observed in many glaciers in the Glacier Bay is that of calving. Calving is a process in which blocks of ice get detached or break off from the glacier, irrespective of weather conditions, all the year round, and crash into the sea with thundering noise creating a boiling like turbulence.

text: The advancing and retreating characteristics of the glaciers in the Glacier Bay are explained in simple terms as a steady state of snow getting converted into ice on the hills. Ice, as a lens of water on the base of bedrock, slides by gravity downwards. The good moraine of rock and rubble insulates it from water erosion. As a result, during freezing temperatures that exists all the year, the glacier advances. When the insulation and erosion effect of the hills gets reduced erosion sets in and along with rising temperatures the glaciers start retreating. Another unpredictable phenomenon that is observed in many glaciers in the Glacier Bay is that of calving. Calving is a process in which blocks of ice get detached or break off from the glacier, irrespective of weather conditions, all the year round, and crash into the sea with thundering noise creating a boiling like turbulence.

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answers: Yes

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answers: sedimentary

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answers: temperature

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answers: good moraine

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answers: bedrock

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answers: glacier advances

answers: NDQ_005769

answers: calving

answers: NDQ_005770

answers: glaciers start retreating

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The principal rock types are the plagioclase-phyric andesite lavas of the Birker Fell Formation.

text: The principal rock types are the

text: plagioclase

text: -phyric

text: andesite

text: lava

text: s of the Birker Fell Formation.

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answers: Yes

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answers: intrusive

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answers: principal rock types

answers: NDQ_005764

answers: phyric

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answers: andesite

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answers: Plagioclase

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answers: Plagioclase

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answers: It is out of the rock cycle

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Several factors are known to inhibit or mar crystallization. The growing crystals are generally held at a constant temperature and protected from shocks or vibrations that might disturb their crystallization. Impurities in the molecules or in the crystallization solutions are often inimical to crystallization. Conformational flexibility in the molecule also tends to make crystallization less likely, due to entropy. Ironically, molecules that tend to self-assemble into regular helices are often unwilling to assemble into crystals . Crystals can be marred by twinning, which can occur when a unit cell can pack equally favorably in multiple orientations; although recent advances in computational methods may allow solving the structure of some twinned crystals. Having failed to crystallize a target molecule, a crystallographer may try again with a slightly modified version of the molecule; even small changes in molecular properties can lead to large differences in crystallization behavior.

text: Several factors are known to inhibit or mar crystallization. The growing crystals are generally held at a constant temperature and protected from shocks or vibrations that might disturb their crystallization. Impurities in the molecules or in the crystallization solutions are often inimical to crystallization. Conformational flexibility in the molecule also tends to make crystallization less likely, due to entropy. Ironically, molecules that tend to self-assemble into regular helices are often unwilling to assemble into crystals . Crystals can be marred by

text: twinning

text: , which can occur when a unit cell can pack equally favorably in multiple orientations; although recent advances in computational methods may allow solving the structure of some twinned crystals. Having failed to crystallize a target molecule, a crystallographer may try again with a slightly modified version of the molecule; even small changes in molecular properties can lead to large differences in crystallization behavior.

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answers: twinning

answers: NDQ_005769

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answers: Crystals can be marred by twinning

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

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

text: Metamorphic core complexes are exposures of deep

text: crust

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

text: continental crust

text: to the

text: Earth

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

text: metamorphic rock

text: s (

text: eclogite

text: granulite

text: - to

text: amphibolite

text: facies

text: ) are exposed below  low-angle

text: detachment fault

text: s (

text: mylonite

text: shear zones) that show

text: ductile

text: deformation on the lower side  (footwall) with

text: amphibolite

text: - to

text: greenschist

text: -facies  syndeformational

text: metamorphism

text: , and  ductile-brittle to

text: brittle

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

text: tilted

text: geometries.

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answers: Yes

answers: NDQ_005762

answers: sedimentary

answers: NDQ_005763

answers: low-angle detachment faults

answers: NDQ_005764

answers: geometries

answers: NDQ_005765

answers: largely amagmatic extension

answers: NDQ_005766

answers: brittle

answers: NDQ_005768

answers: Faster cooling

answers: NDQ_005769

answers: metamorphism

answers: NDQ_005770

answers: Metamorphic

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Magnetofossils are not only being studied for their paleoenvironmental or paleoclimatic indicators.  As mentioned above, magnetofossils hold a remanent magnetization when they are formed.  That is, the magnetite (or greigite) aligns in the direction of the geomagnetic field.  The magnetite crystals can be thought of as being a simple magnet with a north and south pole, this north-south orientation aligns with the north-south magnetic poles of the Earth.  These fossils are then buried within the rock record.  Researchers can examine these rock samples in a remanent magnetometer where the effects of Earth's current magnetic field is removed, to determine the remanent, or initial, magnetization of the rock sample when it was formed.  In knowing the orientation of the rock in-situ and the remanent magnetization, researchers can determine the Earth's geomagnetic field at the time the rock was formed.  This can be used as an indicator of magnetic field direction, or reversals in the Earth's magnetic field, where the Earth's north and south magnetic poles switch (which happen on average every 450,000 years).

text: Magnetofossils are not only being studied for their paleoenvironmental or paleoclimatic indicators.  As mentioned above, magnetofossils hold a remanent magnetization when they are formed.  That is, the magnetite (or greigite) aligns in the direction of the geomagnetic field.  The magnetite crystals can be thought of as being a simple magnet with a north and south pole, this north-south orientation aligns with the north-south magnetic poles of the Earth.  These fossils are then buried within the rock record.  Researchers can examine these rock samples in a remanent

text: magnetometer

text: where the effects of Earth's current magnetic field is removed, to determine the remanent, or initial, magnetization of the rock sample when it was formed.  In knowing the orientation of the rock in-situ and the remanent magnetization, researchers can determine the Earth's geomagnetic field at the time the rock was formed.  This can be used as an indicator of magnetic field direction, or

text: reversals in the Earth's magnetic field

text: , where the Earth's north and south magnetic poles switch (which happen on average every 450,000 years).

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answers: NDQ_005761

answers: Yes

answers: NDQ_005762

answers: intrusive

answers: NDQ_005763

answers: Earth's geomagnetic field

answers: NDQ_005764

answers: orientation

answers: NDQ_005765

answers: These fossils are then buried within the rock record

answers: NDQ_005766

answers: magnetite

answers: NDQ_005768

answers: magnetite

answers: NDQ_005769

answers: fossilization

answers: NDQ_005770

answers: This north-south orientation aligns with the north-south magnetic poles of the Earth

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Except for a  strip along its eastern edge, the bedrock beneath the ice sheet, which covers Alexander Island, consists of a complex assemblage of metasedimentary and metavolcanic rocks. These rocks, which are locally overlain and intruded by igneous rocks, are known as the "Lemay Group." It consists of turbiditic sandstone (subgraywacke and arkose) interbedded with secondary siltstone, mudstone, tuff, volcaniclastic sedimentary rock, agglomerate, and conglomerate, which have all been metamorphosed to prehnite–pumpellyite to blueschist facies. These metasedimentary rocks contain poorly preserved ammonites, pelecypods, gastropods, radiolarians, and fragmentary plant fossils. The LeMay Group also contains north-south, fault-bound slices of accreted ocean floor, ocean islands and seamounts, which includes pillow basalts, volcaniclastic sedimentary rocks, and chert. The rocks, which comprise the LeMay Group are asymmetrically folded and thrust faulted to the west, contain chaotic zones, and exhibit abundant coeval soft-sediment deformation. Based upon biostratigraphy, the oldest known rocks found within the LeMay Group are Lower Jurassic and range up to late Lower Cretaceous. The oldest rocks within this group may date back to Permo-Carboniferous times (350–260 million years ago). The LeMay Group is interpreted to be an accretionary prism that was built out from the west (fore-arc) side of a long-lived magmatic arc, the roots of which are now exposed on the Antarctic Peninsula, between Early Jurassic and Paleocene times, when subduction ceased.

text: Except for a  strip along its eastern edge, the bedrock beneath the ice sheet, which covers Alexander Island, consists of a complex assemblage of

text: metasediment

text: ary and

text: metavolcanic rock

text: s. These rocks, which are locally overlain and intruded by

text: igneous rock

text: s, are known as the "Lemay Group." It consists of

text: turbiditic

text: sandstone

text: (sub

text: graywacke

text: and

text: arkose

text: ) interbedded with secondary

text: siltstone

text: mudstone

text: tuff

text: , volcaniclastic

text: sedimentary rock

text: agglomerate

text: , and

text: conglomerate

text: , which have all been

text: metamorphosed

text: to

text: prehnite

text: pumpellyite

text: to

text: blueschist

text: facies. These metasedimentary rocks contain poorly preserved

text: ammonite

text: s,

text: pelecypod

text: s,

text: gastropod

text: s,

text: radiolarian

text: s, and fragmentary plant

text: fossil

text: s. The LeMay Group also contains north-south, fault-bound slices of accreted ocean floor, ocean islands and

text: seamount

text: s, which includes

text: pillow basalts

text: , volcaniclastic sedimentary rocks, and

text: chert

text: . The rocks, which comprise the LeMay Group are asymmetrically

text: folded

text: and

text: thrust fault

text: ed to the west, contain chaotic zones, and exhibit abundant coeval soft-sediment deformation. Based upon

text: biostratigraphy

text: , the oldest known rocks found within the LeMay Group are Lower

text: Jurassic

text: and range up to late Lower

text: Cretaceous

text: . The oldest rocks within this group may date back to Permo-

text: Carboniferous

text: times (350–260 million years ago). The LeMay Group is interpreted to be an accretionary prism that was built out from the west (

text: fore-arc

text: ) side of a long-lived magmatic arc, the roots of which are now exposed on the Antarctic Peninsula, between Early Jurassic and

text: Paleocene

text: times, when

text: subduction

text: ceased.

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answers: The LeMay Group also contains north-south, fault-bound slices

answers: NDQ_005762

answers: sedimentary

answers: NDQ_005763

answers: biostratigraphy

answers: NDQ_005764

answers: deformation

answers: NDQ_005765

answers: metamorphosed

answers: NDQ_005766

answers: volcaniclastic sedimentary rock

answers: NDQ_005768

answers: faster cooling forms smaller crystals

answers: NDQ_005769

answers: subduction

answers: NDQ_005770

answers: metamorphosed

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: To date, Firox have only appeared in one set. Firox are sneaky and curious by nature, and fastest of all the rock monsters. Rex hates Firox the most, because they ruin all the machines he made. He enjoys stealing the Power Miners tools, playing tricks and messing up machines. He is one of the four rock monsters created by the Crystal King. Once he eats an orange crystal, he has a surge of super speed. He has two cousins: Firax, which are the Firox heated up badly, and Eruptorr, the larger version of the Firax.

text: To date, Firox have only appeared in one set. Firox are sneaky and curious by nature, and fastest of all the rock monsters. Rex hates Firox the most, because they ruin all the machines he made. He enjoys stealing the Power Miners tools, playing tricks and messing up machines. He is one of the four rock monsters created by the Crystal King. Once he eats an orange crystal, he has a surge of super speed. He has two cousins: Firax, which are the Firox heated up badly, and Eruptorr, the larger version of the Firax.

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answers: Yes

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answers: the Crystal King

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answers: speed

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answers: created by the Crystal King

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answers: faster cooling forms smaller crystals

answers: NDQ_005769

answers: Eruptorr

answers: NDQ_005770

answers: Once he eats an orange crystal

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The Rock then made a grand entrance, which included the Dallas Cowboys Cheerleaders and Rock using a flamethrower to set a big sign bearing his name ablaze. Rock announced that WrestleMania 32 had set the all-time attendance record with 101,763, when he was confronted by The Wyatt Family. After some verbal back-and-forth, Rock (who had his ring gear on underneath his street clothes) challenged them to a match. Wyatt Family member Erick Rowan accepted the challenge and was quickly defeated following a Rock Bottom. WWE recognized the match length as six seconds, though other sources reported seven seconds. This set a new WrestleMania record for the shortest match, besting the previous record (11 seconds) set by Kane and Chavo Guererro's match at WrestleMania XXIV. Enraged by this quick victory, the entire Wyatt Family then surrounded the Rock when surprisingly John Cena emerged and helped Rock clear the ring of the Wyatts. The segment ended with Rock and Cena walking up the ramp and Rock hugging his family before he raised Cena's arm.

text: The Rock

text: then made a grand entrance, which included the

text: Dallas Cowboys Cheerleaders

text: and Rock using a flamethrower to set a big sign bearing his name ablaze. Rock announced that WrestleMania 32 had set the all-time attendance record with 101,763, when he was confronted by

text: The Wyatt Family

text: . After some verbal back-and-forth, Rock (who had his ring gear on underneath his street clothes) challenged them to a match. Wyatt Family member

text: Erick Rowan

text: accepted the challenge and was quickly defeated following a Rock Bottom. WWE recognized the match length as six seconds, though other sources reported seven seconds. This set a new WrestleMania record for the shortest match, besting the previous record (11 seconds) set by

text: Kane

text: and

text: Chavo Guererro

text: 's match at

text: WrestleMania XXIV

text: . Enraged by this quick victory, the entire Wyatt Family then surrounded the Rock when surprisingly

text: John Cena

text: emerged and helped Rock clear the ring of the Wyatts. The segment ended with Rock and Cena walking up the ramp and Rock hugging his family before he raised Cena's arm.

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text: Feldspars crystallize from magma as veins in both intrusive and extrusive igneous rocks and are also present in many types of metamorphic rock. Rock formed almost entirely of calcic plagioclase feldspar (see below) is known as anorthosite. Feldspars are also found in many types of sedimentary rocks.

text: Feldspars

text: crystal

text: lize from

text: magma

text: as

text: veins

text: in both

text: intrusive

text: and

text: extrusive

text: igneous

text: rocks and are also present in many types of

text: metamorphic rock

text: . Rock formed almost entirely of calcic

text: plagioclase

text: feldspar (see below) is known as

text: anorthosite

text: . Feldspars are also found in many types of

text: sedimentary rocks

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text: Burial of rocks due to ongoing sedimentation leads to increased pressure and temperature, which stimulates certain chemical reactions. An example is the reactions by which organic material becomes lignite or coal. When temperature and pressure increase still further, the realm of diagenesis makes way for metamorphism, the process that forms metamorphic rock.

text: Burial of rocks due to ongoing sedimentation leads to increased pressure and temperature, which stimulates certain chemical reactions. An example is the reactions by which

text: organic material

text: becomes

text: lignite

text: or

text: coal

text: . When temperature and pressure increase still further, the realm of diagenesis makes way for

text: metamorphism

text: , the process that forms

text: metamorphic rock

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text: Engineering geologist.(a) Elements of the engineering geologist specialty. The practice of engineering geology involves the interpretation, evaluation, analysis, and application of geological information and data to civil works. Geotechnical soil and rock units are designated, characterized, and classified, using standard engineering soil and rock classification systems. Relationships are interpreted between landform development, current and past geologic processes, ground and surface water, and the strength characteristics of soil and rock. Processes evaluated include both surficial processes (for example, slope, fluvial, and coastal processes), and deep-seated processes (for example, volcanic activity and seismicity). Geotechnical zones or domains are designated based on soil and rocked geological strength characteristics, common landforms, related geologic processes, or other pertinent factors. Proposed developmental modifications are evaluated and, where appropriate, analyzed to predict potential or likely changes in types and rates of surficial geologic processes. Proposed modifications may include such things as vegetation removal, using various types of earth materials in construction, applying loads to shallow or deep foundations, constructing cut or fill slopes and other grading, and modifying ground and surface water flow. The effects of surficial and deep-seated geologic processes are evaluated and analyzed to predict their potential effect on public health, public safety, land use, or proposed development.(b) Typical engineering geologic applications and types of projects. Engineering geology is applied during all project phases, from conception through planning, design, construction, maintenance, and, in some cases, reclamation and closure. Planning-level engineering geologic work is commonly conducted in response to forest practice regulations, critical areas ordinances, and the State Environmental Policy Act. Typical planning-level engineering geologic applications include timber harvest planning, proposed location of residential and commercial developments and other buildings and facilities, and alternative route selection for roads, rail lines, trails, and utilities. Site-specific engineering geologic applications include cuts, fills, and tunnels for roads, trails, railroads, and utility lines; foundations for bridges and other drainage structures, retaining walls and shoring, dams, buildings, water towers, slope, channel and shoreline stabilization facilities, fish ladders and hatcheries, ski lifts and other structures; landings for logging and other work platforms; airport landing strips; rock bolt systems; blasting; and other major earthwork projects such as for aggregate sources and landfills.

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answers: Engineering geology is applied during all project phases

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answer: No

answer: No

answer: No

answer: No

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text: Between six and nine million years ago, stretching and thinning of the Earth's crust caused movement along the Teton fault. The west block along the fault line rose to form the Teton Range, creating the youngest range of the Rocky Mountains. The fault's east block fell to form the valley called Jackson Hole. The geological processes that led to the current composition of the oldest rocks in the Teton range began about 2.5 billion years ago. At that time, sand and volcanic debris settled into an ancient ocean. Additional sediment was deposited for millions of years and eventually heat and pressure metamorphosed the sediment into gneiss. Subsequently, magma was forced up through the cracks in the gneiss to form granite, anywhere from inches to hundreds of feet thick. Other intrusive igneous rocks are noticeable as the black dikes of diabase, visible on the southwest face of Mount Moran and on the Grand Teton. Starting during the Cambrian period, deep deposits of sedimentary rock were deposited in shallow seas over the metamorphic basement rocks. Erosion and uplift have exposed the metamorphic and intrusive igneous rocks now visible on the east slope of the range and in the Cathedral Group and the paleozoic and cenozoic sedimentary rocks on the west slope. 2.1 million years ago the Huckleberry Ridge Tuff was deposited along the west slope of the north part of the range.

text: Between six and nine million years ago, stretching and thinning of the Earth's crust caused movement along the Teton

text: fault

text: . The west block along the fault line rose to form the Teton Range, creating the youngest range of the Rocky Mountains. The fault's east block fell to form the valley called

text: Jackson Hole

text: . The geological processes that led to the current composition of the oldest rocks in the Teton range began about 2.5 billion years ago. At that time, sand and volcanic debris settled into an ancient ocean. Additional sediment was deposited for millions of years and eventually heat and pressure metamorphosed the sediment into

text: gneiss

text: . Subsequently, magma was forced up through the cracks in the

text: gneiss

text: to form

text: granite

text: , anywhere from inches to hundreds of feet thick. Other intrusive igneous rocks are noticeable as the black dikes of

text: diabase

text: , visible on the southwest face of

text: Mount Moran

text: and on the

text: Grand Teton

text: . Starting during the

text: Cambrian

text: period, deep deposits of sedimentary rock were deposited in shallow seas over the metamorphic basement rocks. Erosion and uplift have exposed the metamorphic and intrusive igneous rocks now visible on the east slope of the range and in the

text: Cathedral Group

text: and the

text: paleozoic

text: and

text: cenozoic

text: sedimentary rocks on the west slope. 2.1 million years ago the

text: Huckleberry Ridge Tuff

text: was deposited along the west slope of the north part of the range.

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answers: Geological processes that led to the current composition of the oldest rocks

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answers: sedimentary

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answers: heat and pressure

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answers: thickness

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answers: Additional sediment was deposited for millions of years and eventually heat and pressure metamorphosed the sediment into gneiss

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answers: granite

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answers: faster cooling forms larger crystals

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answers: metamorphosed

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answers: metamorphosed

answer: No

answer: No

answer: No

answer: No

answer: No

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text: Proteins are biological macromolecules and function in an aqueous environment, so protein crystallization is predominantly carried out in water. Protein crystallization is generally considered challenging due to the restrictions of the aqueous environment, difficulties in obtaining high-quality protein samples, as well as sensitivity of protein samples to temperature, pH, ionic strength, and other factors. Proteins vary greatly in their physicochemical characteristics, and so crystallization of a particular protein is rarely predictable. Determination of appropriate crystallization conditions for a given protein often requires empirical testing of many conditions before a successful crystallization condition is found.

text: Proteins

text: are biological

text: macromolecules

text: and function in an

text: aqueous

text: environment, so protein crystallization is predominantly carried out in water. Protein crystallization is generally considered challenging due to the restrictions of the aqueous environment, difficulties in obtaining high-quality protein samples, as well as sensitivity of protein samples to

text: temperature

text: pH

text: ionic strength

text: , and other factors. Proteins vary greatly in their physicochemical characteristics, and so crystallization of a particular protein is rarely predictable. Determination of appropriate crystallization conditions for a given protein often requires empirical testing of many conditions before a successful crystallization condition is found.

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answers: slower cooling forms smaller crystals

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answers: crystallization

answers: NDQ_005770

answers: Proteins are biological macromolecules

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 0

text: Formation pressure is the pressure of the fluid within the pore spaces of the formation rock. This pressure  can  be  affected  by  the  weight  of  the overburden  (rock  layers)  above  the  formation, which  exerts  pressure  on  both  the  grains  and pore  fluids.  Grains  are  solid  or  rock  material, and  pores  are  spaces  between  grains.  If porefluids  are  free  to  move,  or  escape,  the  grains lose  some  of  their  support  and  move  closer together. This process is called consolidation.Depending on the magnitude of the pore pressure, it can be described as being normal, abnormal or subnormal.Normal pore pressure or formation pressure is equal to the hydrostatic pressure of formation fluid extending from the surface to the surface formation being considered. In other words, if the formation was opened up and allowed to fill a column whose length is equal to the depth of the formation, then the pressure at the bottom of the column will be equal to the formation pressure and the pressure at surface is equal to zero.Normal pore pressure is not a constant. Its magnitude varies with the concentration of dissolved salts, type of fluid, gases present and temperature gradient.

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answers: normal, abnormal or subnormal

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The lyrics to "Crystalline" talk about the process of crystallization in minerals and rocks but taking a more personal point of view, relating the growth of a crystal structure with the growth of relationships in people's hearts. Björk took inspiration for the song from cities and buildings:

text: The lyrics to "Crystalline" talk about the process of

text: crystallization

text: in

text: mineral

text: s and

text: rock

text: s but taking a more personal point of view, relating the growth of a

text: crystal structure

text: with the growth of relationships in people's hearts. Björk took inspiration for the song from cities and buildings:

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answer: No

answer: No

answer: No

answer: No

answer: No

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text: Alignment of tabular minerals in metamorphic rocks, igneous rocks and intrusive rocks may form a foliation. Typical examples of metamorphic rocks include porphyroblastic schists where large, oblate minerals form an alignment either due to growth or rotation in the groundmass.

text: Alignment of tabular minerals in

text: metamorphic rock

text: s,

text: igneous rock

text: s and

text: intrusive rock

text: s may form a foliation. Typical examples of metamorphic rocks include

text: porphyroblast

text: ic schists where large, oblate minerals form an alignment either due to growth or rotation in the groundmass.

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answers: metamorphic

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answers: growth or rotation

answers: NDQ_005764

answers: foliation

answers: NDQ_005765

answers: growth or rotation

answers: NDQ_005766

answers: igneous rocks

answers: NDQ_005768

answers: growth

answers: NDQ_005769

answers: metamorphic

answers: NDQ_005770

answers: metamorphic rocks

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: In some areas, the Prokletije run almost parallel with the Šar Mountains in Macedonia, Albania and Kosovo. This tectonic crash produced the unusual zig-zag shape of Prokletije range, and also their curving from the dominant Dinaric northwestern - southeastern direction toward the northeastern one. In the western and central parts of the range the composition of the mountains is of mainly uniform with Mesozoic limestones and dolomites of the Jurassic and Cretaceous Ages. In the eastern Prokletije in addition to the limestone and dolomite series, there are rocks from the late Palaeozoic and Triassic periods, medium-Triassic volcanic rocks and Jurassic metamorphic rocks.

text: In some areas, the Prokletije run almost parallel with the

text: Šar Mountains

text: in

text: Macedonia

text: , Albania and Kosovo. This tectonic crash produced the unusual zig-zag shape of Prokletije range, and also their curving from the dominant Dinaric northwestern - southeastern direction toward the northeastern one. In the western and central parts of the range the composition of the mountains is of mainly uniform with

text: Mesozoic

text: limestones and dolomites of the Jurassic and

text: Cretaceous

text: Ages. In the eastern Prokletije in addition to the limestone and dolomite series, there are rocks from the late Palaeozoic and Triassic periods, medium-

text: Triassic

text: volcanic rocks and Jurassic metamorphic rocks.

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answers: 0

answers: NDQ_005761

answers: Mesozoic limestones and dolomites

answers: NDQ_005762

answers: sedimentary

answers: NDQ_005763

answers: tectonic crash

answers: NDQ_005764

answers: composition

answers: NDQ_005765

answers: tectonic crash

answers: NDQ_005766

answers: volcanic rocks

answers: NDQ_005768

answers: faster cooling forms smaller crystals

answers: NDQ_005769

answers: limestones

answers: NDQ_005770

answers: metamorphic rocks

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The book includes one of the earliest accounts of the process of magmatic differentiation. While observing a basaltic lava flow in the Galápagos Islands, Darwin observed that "crystals sink from their weight" and that this "throws light on the separation of the high silica versus low silica series of rocks." This was the first proposal of the fractional crystallization hypothesis of magma differentiation that was further developed and demonstrated in the 20th century.

text: The book includes one of the earliest accounts of the process of

text: magmatic differentiation

text: . While observing a

text: basaltic

text: lava flow

text: in the

text: Galápagos Islands

text: , Darwin observed that "crystals sink from their weight" and that this "throws light on the separation of the high silica versus low silica series of rocks." This was the first proposal of the

text: fractional crystallization

text: hypothesis of magma differentiation that was further developed and demonstrated in the 20th century.

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answers: Yes

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answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Erosion represents a subsequent phase of the orogenic cycle. Erosion inevitably removes much of the mountains, exposing the core or mountain roots (metamorphic rocks brought to the surface from a depth of several kilometres). Isostatic movements may help such exhumation by balancing out the buoyancy of the evolving orogen. Scholars debate about the extent to which erosion modifies the patterns of tectonic deformation (see erosion and tectonics). Thus, the final form of the majority of old orogenic belts is a long arcuate strip of crystalline metamorphic rocks sequentially below younger sediments which are thrust atop them and which dip away from the orogenic core.

text: Erosion

text: represents a subsequent phase of the orogenic cycle. Erosion inevitably removes much of the mountains, exposing the core or mountain roots (

text: metamorphic rocks

text: brought to the surface from a depth of several kilometres).

text: Isostatic

text: movements may help such exhumation by balancing out the buoyancy of the evolving orogen. Scholars debate about the extent to which erosion modifies the patterns of tectonic deformation (see

text: erosion and tectonics

text: ). Thus, the final form of the majority of old orogenic belts is a long arcuate strip of crystalline metamorphic rocks sequentially below younger sediments which are thrust atop them and which dip away from the orogenic core.

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answer: No

answer: No

answer: Yes

answer: No

answer: No

answer: 1

text: A sediment basin is a temporary pond built on a construction site to capture eroded or disturbed soil that is washed off during rain storms, and protect the water quality of a nearby stream, river, lake, or bay.  The sediment-laden soil settles in the pond before the runoff is discharged.  Sediment basins are typically used on construction sites of  or more, where there is sufficient room.  They are often used in conjunction with erosion controls and other sediment control practices.  On smaller construction sites, where a basin is not practical, sediment traps may be used.

text: A sediment basin is a temporary pond built on a

text: construction

text: site to capture

text: eroded

text: or disturbed soil that is washed off during rain storms, and protect the

text: water quality

text: of a nearby stream, river, lake, or bay.  The

text: sediment

text: -laden soil settles in the pond before the runoff is discharged.  Sediment basins are typically used on construction sites of  or more, where there is sufficient room.  They are often used in conjunction with

text: erosion control

text: s and other

text: sediment control

text: practices.  On smaller construction sites, where a basin is not practical, sediment traps may be used.

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answers: slower cooling forms smaller crystals

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answer: No

answer: No

answer: No

answer: No

answer: No

answer: 0

text: Herald Island is composed of sedimentary, metamorphic, and igneous rocks. The northeastern tip of this island consists of a -thick sequence of sandstone, phyllite, quartzose sandstone, quartz-chlorite-sericite schist mylonite, and cataclastic quartz syenite. These rocks are of either Proterozoic or Late Paleozoic age. The bulk of this island consists of a Jurassic granite pluton.

text: Herald Island is composed of

text: sedimentary

text: metamorphic

text: , and

text: igneous

text: rocks. The northeastern tip of this island consists of a -thick sequence of

text: sandstone

text: phyllite

text: quartz

text: ose sandstone,

text: quartz

text: chlorite

text: sericite

text: schist

text: mylonite

text: , and

text: cataclastic

text: quartz

text: syenite

text: . These rocks are of either

text: Proterozoic

text: or Late

text: Paleozoic

text: age. The bulk of this island consists of a

text: Jurassic

text: granite

text: pluton

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answers: These rocks are of either Proterozoic or Late Paleozoic age

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answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: There are seven glass vessels in the collection, but a larger number of pieces in transparent rock crystal or quartz, a mineral that might easily be taken for glass. This was always a much more valuable and prestigious material, qualifying as a semi-precious stone.  Needing very patient grinding and drilling, it is much harder to work than glass (though correspondingly less easy to break once finished), and the pieces include mounts or bases in precious metal, which none of the actual glass has; nor are the rock crystal pieces painted.  Read's catalogue groups these and other pieces in semi-precious stone with the objects in gold, as opposed to the "silver plate", which probably reflects how a Renaissance collector would have ranked them.  There are ten pieces in crystal and nine in other stones.

text: There are seven glass vessels in the collection, but a larger number of pieces in transparent rock crystal or

text: quartz

text: , a mineral that might easily be taken for glass. This was always a much more valuable and prestigious material, qualifying as a semi-precious stone.  Needing very patient

text: grinding

text: and

text: drilling

text: , it is much harder to work than glass (though correspondingly less easy to break once finished), and the pieces include mounts or bases in precious metal, which none of the actual glass has; nor are the rock crystal pieces painted.  Read's catalogue groups these and other pieces in semi-precious stone with the objects in gold, as opposed to the "silver plate", which probably reflects how a Renaissance collector would have ranked them.  There are ten pieces in crystal and nine in other stones.

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answers: patient grinding and drilling

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text: Flow in culverts, over dams, and around bridge piers can cause erosion of the bed. This erosion can damage the environment and expose or unsettle the foundations of the structure. Therefore, good knowledge of the mechanics of sediment transport in a built environment are important for civil and hydraulic engineers.

text: Flow in culverts, over dams, and around bridge piers can cause erosion of the bed. This erosion can damage the environment and expose or unsettle the foundations of the structure. Therefore, good knowledge of the mechanics of sediment transport in a built environment are important for civil and hydraulic engineers.

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answer: No

answer: No

answer: No

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text: A bluff will be more susceptible to erosion if the sediment is unconsolidated, and more resistant in crystalline rocks, like granite. Rocks that are heavily fractured are also very likely to suffer from erosion because the water can flow between the cracks to speed up the process. A bluff will retreat towards land as the erosion processes continue.

text: A bluff will be more susceptible to erosion if the sediment is unconsolidated, and more resistant in crystalline rocks, like granite. Rocks that are heavily fractured are also very likely to suffer from erosion because the water can flow between the cracks to speed up the process. A bluff will retreat towards land as the erosion processes continue.

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text: The diverse rock types in the calc-alkaline series include volcanic types such as basalt, andesite, dacite, rhyolite, and also their coarser-grained intrusive equivalents (gabbro, diorite, granodiorite, and granite). They do not include silica-undersaturated, alkalic, or peralkaline rocks.

text: The diverse rock types in the calc-alkaline series include volcanic types such as

text: basalt

text: andesite

text: dacite

text: rhyolite

text: , and also their coarser-grained intrusive equivalents (

text: gabbro

text: diorite

text: granodiorite

text: , and

text: granite

text: ). They do not include

text: silica-undersaturated

text: , alkalic, or

text: peralkaline rock

text: s.

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answers: The diverse rock types in the calc-alkaline series include volcanic types

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The Elephant Rock Ride is primarily sponsored by Subaru and the full event is called the Subaru Elephant Rock Cycling Festival.

text: The Elephant Rock Ride is primarily sponsored by

text: Subaru

text: and the full event is called the Subaru Elephant Rock Cycling Festival.

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answers: slower cooling forms smaller crystals

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answers: The Elephant Rock Ride

answer: No

answer: No

answer: No

answer: No

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text: There are three type of Stones (rocks) indicative of the physical characteristics from its formative process. These three categories are: igneous or volcanic rocks (basalt, granic, etc.), sedimentary or deposit rocks (limestone, sandstone, arenite, etc.), and metamorphic rocks (marble, slate, gypsum, etc.). Igneous rocks are formed by the cooling and/or solidification of magma and the formation of a dense network of crystals—below the Earth's surface as intrusive rock or on the surface as effusive rock. Sedimentary rocks are formed by the deposition of the remains of other rock caused by the action of atmospheric influences. Metamorphic rocks are formed by the transformation of existing rock through the action of temperature and pressure, which cause profound physical and/or chemical changes.

text: There are three type of Stones (rocks) indicative of the physical characteristics from its formative process. These three categories are: igneous or volcanic rocks (basalt, granic, etc.), sedimentary or deposit rocks (limestone, sandstone, arenite, etc.), and metamorphic rocks (marble, slate, gypsum, etc.). Igneous rocks are formed by the cooling and/or solidification of magma and the formation of a dense network of crystals—below the Earth's surface as intrusive rock or on the surface as effusive rock. Sedimentary rocks are formed by the deposition of the remains of other rock caused by the action of atmospheric influences. Metamorphic rocks are formed by the transformation of existing rock through the action of temperature and pressure, which cause profound physical and/or chemical changes.

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answers: Yes

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answers: Igneous

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answers: physical characteristics from its formative process

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answers: Igneous rocks

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answers: solidification

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answers: Metamorphic rocks

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: 1

text: Attrition is a form of coastal or river erosion, when the bed load is eroded by itself and the bed. As rocks are transported downstream along a riverbed, the regular impacts between the grains themselves and between the grains and the bed cause them to be broken up into smaller fragments. This process also makes them rounder and smoother. Attrition can also occur in glaciated regions, where it is caused by the movement of ice with embedded boulders over surface sediments.

text: Attrition is a form of coastal or river

text: erosion

text: , when the

text: bed load

text: is eroded by itself and the bed. As rocks are transported downstream along a riverbed, the regular impacts between the grains themselves and between the grains and the bed cause them to be broken up into smaller fragments. This process also makes them rounder and smoother. Attrition can also occur in glaciated regions, where it is caused by the movement of ice with embedded boulders over surface sediments.

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answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The Paleozoic rocks of the dome consist of a 2.6 km thick section of intensely folded Cambrian through Early Pennsylvanian sediments. The Paleozoic rocks were deformed and thrust into the area from the southeast during the Ouachita orogeny. Following the Permian uplift and erosion during most of the Mesozoic was followed by deposition of Cretaceous carbonate rocks which correlate with the Cretaceous of the Gulf Coast. The area was uplifted by the Laramide orogeny during latest Cretaceous. Following the Eocene intrusive and volcanic events of the Solitario, the area was partially covered by volcanic rocks from the adjacent Bofecillos volcanic center to the west of the area during the Oligocene and early Miocene. Erosion and downcutting following the Pleistocene deepening of the Rio Grande to the southwest and south have produced the current topographic expression of the area.

text: The Paleozoic rocks of the dome consist of a 2.6 km thick section of intensely folded

text: Cambrian

text: through Early

text: Pennsylvanian

text: sediments. The Paleozoic rocks were deformed and

text: thrust

text: into the area from the southeast during the

text: Ouachita orogeny

text: . Following the

text: Permian

text: uplift and erosion during most of the

text: Mesozoic

text: was followed by deposition of

text: Cretaceous

text: carbonate rocks which correlate with the Cretaceous of the Gulf Coast. The area was uplifted by the

text: Laramide orogeny

text: during latest Cretaceous. Following the Eocene intrusive and volcanic events of the Solitario, the area was partially covered by volcanic rocks from the adjacent

text: Bofecillos

text: volcanic center to the west of the area during the

text: Oligocene

text: and early

text: Miocene

text: Erosion

text: and downcutting following the

text: Pleistocene

text: deepening of the

text: Rio Grande

text: to the southwest and south have produced the current topographic expression of the area.

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answers: Yes

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answers: sedimentary

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answers: volcanic events

answers: NDQ_005764

answers: thickness

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answers: orogeny

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answers: volcanic rocks

answers: NDQ_005768

answers: faster cooling forms smaller crystals

answers: NDQ_005769

answers: volcanic

answers: NDQ_005770

answers: Paleozoic rocks

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Corrasional or erosional caves are those that form entirely by erosion by flowing streams carrying rocks and other sediments. These can form in any type of rock, including hard rocks such as granite. Generally there must be some zone of weakness to guide the water, such as a fault or joint. A subtype of the erosional cave is the wind or aeolian cave, carved by wind-born sediments. Many caves formed initially by solutional processes often undergo a subsequent phase of erosional or vadose enlargement where active streams or rivers pass through them.

text: Corrasional or erosional caves are those that form entirely by erosion by flowing streams carrying rocks and other sediments. These can form in any type of rock, including hard rocks such as granite. Generally there must be some zone of weakness to guide the water, such as a fault or joint. A subtype of the erosional cave is the wind or aeolian cave, carved by wind-born sediments. Many caves formed initially by solutional processes often undergo a subsequent phase of erosional or vadose enlargement where active streams or rivers pass through them.

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answers: These can form in any type of rock

answers: NDQ_005762

answers: sedimentary

answers: NDQ_005763

answers: zone of weakness to guide the water

answers: NDQ_005764

answers: hard rocks

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answers: erosion

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answers: hard rocks

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answers: faster cooling forms smaller crystals

answers: NDQ_005769

answers: solutional processes

answers: NDQ_005770

answers: Corrasional or erosional caves

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The water is estimated to come from a container approximately 150 m underground. It owes its excellent quality to the rock formations at Mount Anthemounta which consist of semi-metamorphic, metamorphic and igneous rocks. Water flowing in the substrate is slow-moving and as it passes through the various rocks it is filtered and enriched with beneficial elements giving it its unique mineral composition and distinctive taste. Water in the spring is cold at a steady temperature of around 16 °C. Its special features are a high magnesium content with the ideal calcium to magnesium ratio and a low sodium and nitrate content. It also contains potassium and fluorine as well as valuable trace elements such as iron, copper, manganese, lithium, selenium, chromium and zinc. It has exceptional taste and is very pleasant to drink, assists in the functioning of the digestive and urinary systems and it has several other health benefits. One liter of Souroti water meets 1/4 of the body's daily needs in calcium and magnesium. All this makes it different from soda water, which is ordinary potable water to which sodium bicarbonate has been added so that it acquires approximately the same properties as natural mineral water.

text: The water is estimated to come from a container approximately 150 m underground. It owes its excellent quality to the rock formations at Mount Anthemounta which consist of semi-metamorphic, metamorphic and igneous rocks. Water flowing in the substrate is slow-moving and as it passes through the various rocks it is filtered and enriched with beneficial elements giving it its unique mineral composition and distinctive taste. Water in the spring is cold at a steady temperature of around 16 °C. Its special features are a high

text: magnesium

text: content with the ideal

text: calcium

text: to magnesium ratio and a low

text: sodium

text: and

text: nitrate

text: content. It also contains

text: potassium

text: and

text: fluorine

text: as well as valuable trace elements such as

text: iron

text: copper

text: manganese

text: lithium

text: selenium

text: chromium

text: and

text: zinc

text: . It has exceptional taste and is very pleasant to drink, assists in the functioning of the digestive and urinary systems and it has several other health benefits. One liter of Souroti water meets 1/4 of the body's daily needs in calcium and magnesium. All this makes it different from

text: soda water

text: , which is ordinary potable water to which sodium bicarbonate has been added so that it acquires approximately the same properties as natural mineral water.

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text: Rocks with crystals requiring microscopic or X-ray analysis for identification are termed microcrystalline or cryptocrystalline.

text: Rocks with crystals requiring microscopic or

text: X-ray

text: analysis for identification are termed

text: microcrystalline

text: or

text: cryptocrystalline

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text: Continuing through the Cretaceous period and into the early Tertiary, there was uplifting in the area of the Colorado Plateau, the San Juan Mountains, and the La Plata Mountains, which led to the formation of the Mesa Verde pediment with the help of erosion. Small channels of water ran across this formation depositing gravel. Later in the tertiary, the last period of uplift and rock tilting towards the south caused these streams to cut rapidly into the rock removing loose sediment and forming the vast canyons seen today. This caused the isolation of the Mesa Verde pediment from surrounding rock. Today, since the climate is more arid, these erosional processes are slowed.

text: Continuing through the Cretaceous period and into the early

text: Tertiary

text: , there was uplifting in the area of the Colorado Plateau, the San Juan Mountains, and the

text: La Plata Mountains

text: , which led to the formation of the Mesa Verde pediment with the help of erosion. Small channels of water ran across this formation depositing gravel. Later in the tertiary, the last period of uplift and rock tilting towards the south caused these streams to cut rapidly into the rock removing loose sediment and forming the vast canyons seen today. This caused the isolation of the Mesa Verde pediment from surrounding rock. Today, since the climate is more arid, these erosional processes are slowed.

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answers: Tertiary

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answers: Mesa Verde

answers: NDQ_005768

answers: erosional processes are slowed

answers: NDQ_005769

answers: erosion

answers: NDQ_005770

answers: Mesa Verde pediment

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Rock samples collected from the northern slopes of the mountain and streams rising from the mountain have revealed traces of tin. The mountain has an established belt of Cretaceous tin "granites". It was noted that this tin content matched well with the degree of "greisen alteration". Analyses of samples of unaltered granites pointed to a tin content of less than 80 ppm, as against the disturbed granites which showed a tin content of 950 ppm. It was also reported that the tin concentrations in "unaltered granitic rocks increase progressively from porphyritic to seriate to some equigranular rocks, indicating a progressive concentration of tin with fractional crystallization." Cassiterite is found in large quantities in placers enveloping the pluton. At the beginning of the 20th century, there were plans to lay a railroad up to Port Clarence for the purpose of tin mining.

text: Rock samples collected from the northern slopes of the mountain and streams rising from the mountain have revealed traces of tin. The mountain has an established belt of Cretaceous tin "granites". It was noted that this tin content matched well with the degree of "greisen alteration". Analyses of samples of unaltered granites pointed to a tin content of less than 80 ppm, as against the disturbed granites which showed a tin content of 950 ppm. It was also reported that the tin concentrations in "unaltered granitic rocks increase progressively from

text: porphyritic

text: to

text: seriate

text: to some equigranular rocks, indicating a progressive concentration of tin with fractional crystallization."

text: Cassiterite

text: is found in large quantities in placers enveloping the

text: pluton

text: . At the beginning of the 20th century, there were plans to lay a railroad up to

text: Port Clarence

text: for the purpose of tin mining.

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answers: fractional crystallization

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answers: unaltered granitic rocks

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Sediment is a naturally occurring material that is broken down by processes of weathering and erosion, and is subsequently transported by the action of wind, water, or ice, and/or by the force of gravity acting on the particles. For example, sand and silt can be carried in suspension in river water and on reaching the sea be deposited by sedimentation and if buried this may eventually become sandstone and siltstone, ( sedimentary rocks).

text: Sediment is a naturally occurring material that is broken down by processes of

text: weathering

text: and

text: erosion

text: , and is subsequently

text: transported

text: by the action of wind, water, or ice, and/or by the force of

text: gravity

text: acting on the particles. For example,

text: sand

text: and

text: silt

text: can be carried in

text: suspension

text: in river water and on reaching the sea be deposited by

text: sedimentation

text: and if buried this may eventually become

text: sandstone

text: and

text: siltstone

text: sedimentary rock

text: s).

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answers: Sediment

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Truttman Sink is associated with the Franciscan Formation (or Complex/Assemblage), which is made up of rock types such as: sedimentary sandstone and shale, oceanic basalt, greenstone, chert, serpentinite, limestone, and several metamorphic rock types (blueschist, amphibolite, and eclogite). Franciscan rock is considered a part of a Mesozoic subduction complex and ranges all along the Californian coast.

text: Truttman Sink is associated with the

text: Franciscan Formation

text: (or Complex/Assemblage), which is made up of rock types such as: sedimentary

text: sandstone

text: and

text: shale

text: , oceanic

text: basalt

text: , greenstone,

text: chert

text: serpentinite

text: limestone

text: , and several metamorphic rock types (

text: blueschist

text: amphibolite

text: , and

text: eclogite

text: ). Franciscan rock is considered a part of a

text: Mesozoic

text: subduction

text: complex and ranges all along the Californian coast.

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answers: Yes

answers: NDQ_005762

answers: Franciscan Formation

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answers: subduction complex

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answers: sedimentary

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answers: subduction

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answers: oceanic basalt

answers: NDQ_005768

answers: serpentinite

answers: NDQ_005769

answers: Sink

answers: NDQ_005770

answers: Metamorphic

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Under extreme compressive stresses and pressure, marine sedimentary rocks were uplifted, creating characteristic recumbent folds, or nappes, and thrust faults.  As the rising peaks underwent erosion, a layer of marine flysch sediments was deposited in the foreland basin, and the sediments became involved in younger nappes (folds) as the orogeny progressed. Coarse sediments from the continual uplift and erosion were later deposited in foreland areas as molasse. The molasse regions in Switzerland and Bavaria were well-developed and saw further upthrusting of flysch.

text: Under extreme

text: compressive stress

text: es and pressure, marine

text: sedimentary rock

text: s were uplifted, creating characteristic recumbent

text: folds

text: , or

text: nappe

text: s, and

text: thrust fault

text: s.  As the rising peaks underwent erosion, a layer of marine

text: flysch

text: sediments was deposited in the

text: foreland basin

text: , and the sediments became involved in younger nappes (folds) as the orogeny progressed. Coarse sediments from the continual uplift and erosion were later deposited in foreland areas as

text: molasse

text: . The molasse regions in Switzerland and Bavaria were well-developed and saw further upthrusting of flysch.

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answers: Yes

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answers: sedimentary

answers: NDQ_005763

answers: compressive stresses and pressure

answers: NDQ_005764

answers: folds

answers: NDQ_005765

answers: orogeny

answers: NDQ_005766

answers: flysch

answers: NDQ_005768

answers: faster cooling forms smaller crystals

answers: NDQ_005769

answers: molasse

answers: NDQ_005770

answers: molasse

answer: No

answer: No

answer: Yes

answer: No

answer: No

answer: 1

text: The lavas of Taftan are porphyritic. Mineral components include biotite, clinopyroxene, hornblende, orthopyroxene, plagioclase and quartz. Other components are chalcopyrite, haematite, ilmenite, magnetite and pyrite. Complex phenocryst assemblages found in a sample indicate that the magma formation is a complex process. Taftan rocks overall are -rich calc-alkaline, of sub–alkaline affinity. The magma that formed these rocks was influenced by crystal fractionation and mixing processes. Its composition has characteristics of volcanic arc magmas. Crustal materials were involved in the formation of the magma, with  isotope data indicating crustal assimilation.

text: The lavas of Taftan are porphyritic. Mineral components include biotite,

text: clinopyroxene

text: hornblende

text: orthopyroxene

text: plagioclase

text: and

text: quartz

text: . Other components are

text: chalcopyrite

text: , haematite,

text: ilmenite

text: magnetite

text: and

text: pyrite

text: . Complex

text: phenocryst

text: assemblages found in a sample indicate that the magma formation is a complex process. Taftan rocks overall are -rich

text: calc-alkaline

text: , of sub–alkaline affinity. The magma that formed these rocks was influenced by

text: crystal fractionation

text: and mixing processes. Its composition has characteristics of volcanic arc magmas. Crustal materials were involved in the formation of the magma, with  isotope data indicating crustal assimilation.

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answers: Yes

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answers: intrusive

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answers: crystal fractionation and mixing processes

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answers: crustal assimilation

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answers: porphyritic

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answers: crystal fractionation and mixing processes

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answers: fractionation

answers: NDQ_005770

answers: rock cycle

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Metamorphic rocks composed dominantly of amphiboles are referred to as amphibolites.

text: Metamorphic rock

text: s composed dominantly of amphiboles are referred to as

text: amphibolite

text: s.

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answers: Metamorphic rocks

answer: No

answer: No

answer: No

answer: No

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text: Rocks on Mars have been found to frequently occur as layers, called strata, in many different places. Columbus Crater is one of many craters that contain layers. Rock can form layers in a variety of ways. Volcanoes, wind, or water can produce layers.  Many places on Mars show rocks arranged in layers. Scientists are happy about finding layers on Mars since layers may have formed under large bodies of water.  Layers may be formed by groundwater rising up depositing minerals and cementing sediments.  The hardned layers are consequently more protected from erosion.  This process may occur instead of layers forming under lakes.

text: Rocks on Mars have been found to frequently occur as layers, called strata, in many different places.

text: Columbus Crater

text: is one of many craters that contain layers. Rock can form layers in a variety of ways. Volcanoes, wind, or water can produce layers.  Many places on Mars show rocks arranged in layers. Scientists are happy about finding layers on Mars since layers may have formed under large bodies of water.  Layers may be formed by groundwater rising up depositing minerals and cementing sediments.  The hardned layers are consequently more protected from erosion.  This process may occur instead of layers forming under lakes.

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answer: No

answer: No

answer: Yes

answer: No

answer: No

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text: It is estimated that the whirlpool formed approximately 4,200 years ago by the upstream erosion of the Niagara Escarpment by the Niagara River.  Niagara Falls is located along the boundary of the Niagara Escarpment and has been "retreating" upstream since its formation. During this normally slow process, the retreating falls intersected with an ancient pre-glacial river bed inside Saint David's Buried Gorge.  During the retreat of ice from the Wisconsinan glaciation of the last glacial period, the gorge was filled with loose sediment and rock.  When the falls intersected with this buried gorge, the river quickly washed away the filled-in silt and rocks. The ancient buried gorge was nearly perpendicular to the Niagara River.  This sharp and sudden change in direction of water flow, coupled with the rapid flow of water exiting the Niagara Gorge (speeds as high as 30 feet per second [9 m•s]), resulted in turbulent swirling of the river.  Further erosion of the harder rock has resulted in a rounded basin that extends just to the side of the actual river's course.

text: It is estimated that the whirlpool formed approximately 4,200 years ago by the upstream erosion of the

text: Niagara Escarpment

text: by the Niagara River.  Niagara Falls is located along the boundary of the Niagara Escarpment and has been "

text: retreating

text: " upstream since its formation. During this normally slow process, the retreating falls intersected with an ancient pre-glacial river bed inside

text: Saint David's Buried Gorge

text: .  During the retreat of ice from the

text: Wisconsinan glaciation

text: of the

text: last glacial period

text: , the gorge was filled with loose sediment and rock.  When the falls intersected with this buried gorge, the river quickly washed away the filled-in silt and rocks. The ancient buried gorge was nearly perpendicular to the Niagara River.  This sharp and sudden change in direction of water flow, coupled with the rapid flow of water exiting the Niagara Gorge (speeds as high as 30 feet per second [9 m•s]), resulted in turbulent swirling of the river.  Further erosion of the harder rock has resulted in a rounded basin that extends just to the side of the actual river's course.

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answers: When the falls intersected with this buried gorge, the river quickly washed away the filled-in silt and rocks

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The chemical name of a felsic rock is given according to the TAS classification of Le Maitre (1975). However, this only applies to volcanic rocks. If the rock is analyzed and found to be felsic but is metamorphic and has no definite volcanic protolith, it may be sufficient to simply call it a 'felsic schist'. There are examples known of highly sheared granites which can be mistaken for rhyolites.

text: The chemical name of a felsic rock is given according to the

text: TAS classification

text: of Le Maitre (1975). However, this only applies to volcanic rocks. If the rock is analyzed and found to be felsic but is

text: metamorphic

text: and has no definite volcanic

text: protolith

text: , it may be sufficient to simply call it a 'felsic schist'. There are examples known of highly

text: sheared

text: granites which can be mistaken for rhyolites.

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answers: This only applies to volcanic rocks

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answer: No

answer: No

answer: No

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text: Erosion can be the result of material movement by the wind. There are two main effects. First, wind causes small particles to be lifted and therefore moved to another region. This is called deflation. Second, these suspended particles may impact on solid objects causing erosion by abrasion (ecological succession). Wind erosion generally occurs in areas with little or no vegetation, often in areas where there is insufficient rainfall to support vegetation. An example is the formation of sand dunes, on a beach or in a desert. Loess is a homogeneous, typically nonstratified, porous, friable, slightly coherent, often calcareous, fine-grained, silty, pale yellow or buff, windblown (Aeolian) sediment. It generally occurs as a widespread blanket deposit that covers areas of hundreds of square kilometers and tens of meters thick. Loess often stands in either steep or vertical faces. Loess tends to develop into highly rich soils. Under appropriate climatic conditions, areas with loess are among the most agriculturally productive in the world. Loess deposits are geologically unstable by nature, and will erode very readily. Therefore, windbreaks (such as big trees and bushes) are often planted by farmers to reduce the wind erosion of loess.

text: Erosion can be the result of material movement by the wind. There are two main effects. First, wind causes small particles to be lifted and therefore moved to another region. This is called deflation. Second, these suspended particles may impact on solid objects causing erosion by abrasion (ecological succession). Wind erosion generally occurs in areas with little or no vegetation, often in areas where there is insufficient rainfall to support vegetation. An example is the formation of sand

text: dunes

text: , on a beach or in a desert. Loess is a homogeneous, typically nonstratified, porous,

text: friable

text: , slightly coherent, often calcareous, fine-grained,

text: silt

text: y, pale yellow or buff, windblown (Aeolian)

text: sediment

text: . It generally occurs as a widespread blanket deposit that covers areas of hundreds of square kilometers and tens of meters thick. Loess often stands in either steep or vertical faces. Loess tends to develop into highly rich soils. Under appropriate climatic conditions, areas with loess are among the most agriculturally productive in the world. Loess deposits are geologically unstable by nature, and will erode very readily. Therefore, windbreaks (such as big trees and bushes) are often planted by farmers to reduce the wind erosion of loess.

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answers: Yes

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answers: sedimentary

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answers: climatic conditions

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answers: Erosion

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answers: Loess

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answers: This is called deflation

answers: NDQ_005769

answers: deflation

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answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Retrograde metamorphism involves the reconstitution of a rock via revolatisation under decreasing temperatures (and usually pressures), allowing the mineral assemblages formed in prograde metamorphism to revert to those more stable at less extreme conditions. This is a relatively uncommon process, because volatiles must be present.

text: Retrograde metamorphism involves the reconstitution of a rock via revolatisation under decreasing temperatures (and usually pressures), allowing the mineral assemblages formed in prograde metamorphism to revert to those more stable at less extreme conditions. This is a relatively uncommon process, because volatiles must be present.

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answers: volatiles must be present

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answers: Retrograde metamorphism

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answers: Retrograde metamorphism

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answer: No

answer: No

answer: No

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answer: 1

text: In the 1950s, the Pagoda Gift Shop was a post-office and the Crystal Rock Castle was turned into a maintenance shop in the late-1950s. In 1959, the hotels were repainted, new admission gates were installed, and over $1,200,000 was spent to refresh Cedar Point. The park's first roller coaster since the Cyclone, the Wild Mouse, was built. The resort also got a new kind of ride, a monorail that was the most popular ride in 1959. Breakers Hotel was restored, and the neglected cottages were demolished. The Coliseum and Grand Pavilion were both painted and remodeled. The Crystal Rock Castle Maintenance Shop, bathhouses, and the old powerhouse were demolished, and a new $50,000 bathhouse, boiler house, and maintenance shop were built in their place.

text: In the 1950s, the Pagoda Gift Shop was a post-office and the Crystal Rock Castle was turned into a maintenance shop in the late-1950s. In 1959, the hotels were repainted, new admission gates were installed, and over $1,200,000 was spent to refresh Cedar Point. The park's first roller coaster since the Cyclone, the Wild Mouse, was built. The resort also got a new kind of ride, a

text: monorail

text: that was the most popular ride in 1959. Breakers Hotel was restored, and the neglected cottages were demolished. The Coliseum and Grand Pavilion were both painted and remodeled. The Crystal Rock Castle Maintenance Shop, bathhouses, and the old powerhouse were demolished, and a new $50,000 bathhouse, boiler house, and maintenance shop were built in their place.

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answers: Yes

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answers: temperature

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answers: demolished

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answers: a maintenance shop

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answers: slower cooling forms smaller crystals

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answers: Cyclone

answers: NDQ_005770

answers: Crystal Rock Castle was turned into a maintenance shop

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 0

text: A rock structure can be created in any rock type or combination:

text: A rock structure can be created in any rock type or combination:

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answers: NDQ_005761

answers: Rocks are part of the rock cycle.

answers: NDQ_005762

answers: sedimentary

answers: NDQ_005763

answers: magma

answers: NDQ_005764

answers: structure

answers: NDQ_005765

answers: rock formation

answers: NDQ_005766

answers: A rock structure

answers: NDQ_005768

answers: slower cooling forms smaller crystals.

answers: NDQ_005769

answers: rock formation

answers: NDQ_005770

answers: A rock structure can be created in any rock type

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The C horizon (parent material) is below the B Horizon. This layer is barely affected by soil-forming processes and they thus have a lack of pedological development. In other words, the C horizon is the unconsolidated material underlying the solum (A and B horizons). It may or may not be the same as the parent material from which the solum formed. The C horizon forms as the R horizon weathers and rocks break up into smaller particles. The C horizon is below the zones of greatest biological activity and it has not been sufficiently altered by soil genesis to qualify as a B horizon. In dry regions, carbonates and gypsum may be concentrated in the C horizon. While loose enough to be dug with a shovel, C horizon material often retains some of the structural features of the parent rock or geologic deposits from which it formed. The A and B layers usually originated from the C horizon. The upper layers of the C horizon may in time become a part of the solum as weathering and erosion continue. The C Horizon may contain lumps or more likely large shelves of unweathered rock, rather than being made up solely of small fragments as in the solum. It contains rocks with cracks and crevices.

text: rocks

text: with cracks and crevices.

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answers: Rocks with cracks and crevices

answers: NDQ_005762

answers: intrusive

answers: NDQ_005763

answers: The C horizon

answers: NDQ_005764

answers: structural

answers: NDQ_005765

answers: rocks break up into smaller particles

answers: NDQ_005766

answers: unweathered rock

answers: NDQ_005768

answers: faster cooling forms smaller crystals

answers: NDQ_005769

answers: R horizon weathers

answers: NDQ_005770

answers: The C horizon forms as the R horizon weathers

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Petrologically the volcanic Kaiserstuhl is an alkali-carbonate rock formation. The volcanic rocks making up a large part of the central and western Kaiserstuhl were the result of numerous volcanic eruptions during the Miocene, about 19 to 16 million years ago. They cover parts of the sedimentary base of the eastern Kaiserstuhl, which is why in some places changes in the base’s mineralogical composition occurred. The driving force behind this process of contact metamorphism was an increase in temperature. Due to the alternate eruption of tephra and lava flows from several vents a complex stratovolcano came into existence. Some of the rising magma solidified as volcanic intrusions below the surface – and today forms the central part of the Kaiserstuhl. Laterally rising phonolite magma also intruded into the sedimentary base of the Eastern Kaiserstuhl. Several hundred metres of the original volcano have been eroded.

text: Petrologically the volcanic Kaiserstuhl is an alkali-carbonate rock formation. The volcanic rocks making up a large part of the central and western Kaiserstuhl were the result of numerous volcanic eruptions during the

text: Miocene

text: , about 19 to 16 million years ago. They cover parts of the sedimentary base of the eastern Kaiserstuhl, which is why in some places changes in the base’s mineralogical composition occurred. The driving force behind this process of

text: contact metamorphism

text: was an increase in temperature. Due to the alternate eruption of

text: tephra

text: and

text: lava flow

text: s from several vents a complex

text: stratovolcano

text: came into existence. Some of the rising

text: magma

text: solidified as volcanic intrusions below the surface – and today forms the central part of the Kaiserstuhl. Laterally rising

text: phonolite

text: magma also intruded into the sedimentary base of the Eastern Kaiserstuhl. Several hundred metres of the original volcano have been eroded.

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answers: faster cooling forms larger crystals

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answer: No

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text: If a material that selectively rejects the daughter nuclide is heated, any daughter nuclides that have been accumulated over time will be lost through diffusion, setting the isotopic "clock" to zero. The temperature at which this happens is known as the closure temperature or blocking temperature and is specific to a particular material and isotopic system. These temperatures are experimentally determined in the lab by artificially resetting sample minerals using a high-temperature furnace. As the mineral cools, the crystal structure begins to form and diffusion of isotopes is less easy. At a certain temperature, the crystal structure has formed sufficiently to prevent diffusion of isotopes. This temperature is what is known as closure temperature and represents the temperature below which the mineral is a closed system to isotopes. Thus an igneous or metamorphic rock or melt, which is slowly cooling, does not begin to exhibit measurable radioactive decay until it cools below the closure temperature. The age that can be calculated by radiometric dating is thus the time at which the rock or mineral cooled to closure temperature. Dating of different minerals and/or isotope systems (with differing closure temperatures) within the same rock can therefore enable the tracking of the thermal history of the rock in question with time, and thus the history of metamorphic events may become known in detail. This field is known as thermochronology or thermochronometry.

text: If a material that selectively rejects the daughter nuclide is heated, any daughter nuclides that have been accumulated over time will be lost through

text: diffusion

text: , setting the isotopic "clock" to zero. The temperature at which this happens is known as the

text: closure temperature

text: or blocking temperature and is specific to a particular material and isotopic system. These temperatures are experimentally determined in the lab by

text: artificially resetting sample minerals

text: using a high-temperature furnace. As the mineral cools, the crystal structure begins to form and diffusion of isotopes is less easy. At a certain temperature, the crystal structure has formed sufficiently to prevent diffusion of isotopes. This temperature is what is known as closure temperature and represents the temperature below which the mineral is a closed system to isotopes. Thus an igneous or metamorphic rock or melt, which is slowly cooling, does not begin to exhibit measurable radioactive decay until it cools below the closure temperature. The age that can be calculated by radiometric dating is thus the time at which the rock or mineral cooled to closure temperature. Dating of different minerals and/or isotope systems (with differing closure temperatures) within the same rock can therefore enable the tracking of the thermal history of the rock in question with time, and thus the history of metamorphic events may become known in detail. This field is known as

text: thermochronology

text: or thermochronometry.

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answers: Rocks are part of the rock cycle.

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answers: As the mineral cools, the crystal structure begins to form

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text: In 1967, J. Tuzo Wilson published an article in Nature describing the repeated opening and closing of ocean basins, in particular focusing on the current Atlantic Ocean area. This concept, a part of the plate tectonics revolution, became known as the Wilson cycle. The Wilson cycle has had profound effects on the modern interpretation of the rock cycle as plate tectonics became recognized as the driving force for the rock cycle.

text: In 1967, J. Tuzo Wilson published an article in Nature describing the repeated opening and closing of ocean basins, in particular focusing on the current

text: Atlantic Ocean

text: area. This concept, a part of the plate tectonics revolution, became known as the Wilson cycle. The Wilson cycle has had profound effects on the modern interpretation of the rock cycle as plate tectonics became recognized as the driving force for the rock cycle.

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answers: Wilson cycle

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answers: The Wilson cycle

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Phaneritic (phaner = visible) textures are typical of intrusive igneous rocks, these rocks crystallized slowly below Earth's surface. As magma cools slowly the minerals have time to grow and form large crystals. The minerals in a phaneritic igneous rock are sufficiently large to see each individual crystal with the naked eye. Examples of phaneritic igneous rocks are gabbro, diorite and granite.

text: Phaneritic

text: (phaner = visible) textures are typical of intrusive igneous rocks, these rocks crystallized slowly below Earth's surface. As

text: magma

text: cools slowly the

text: mineral

text: s have time to grow and form large crystals. The minerals in a phaneritic igneous rock are sufficiently large to see each individual

text: crystal

text: with the

text: naked eye

text: . Examples of phaneritic igneous rocks are

text: gabbro

text: diorite

text: and

text: granite

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answers: intrusive

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answers: magma cools slowly

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answers: faster cooling forms larger crystals

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answers: crystallized

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answers: rock crystallized slowly below Earth's surface

answer: No

answer: No

answer: No

answer: No

answer: No

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text: The origin of the increased sediment transport into an area may be erosion on land, or activities in the water.

text: The origin of the increased sediment transport into an area may be erosion on land, or activities in the water.

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answers: slower cooling forms smaller crystals

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answer: No

answer: No

answer: No

answer: No

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answer: 1

text: Hydraulic joints are joints thought to have formed when pore fluid pressure became elevated as a result of vertical gravitational loading. In simple terms, the accumulation of either sediments, volcanic, or other material causes an increase in the pore pressure of groundwater and other fluids in the underlying rock when they cannot move either laterally of vertically in response to this pressure. This also causes an increase in pore pressure in  preexisting cracks that increases the tensile stress on them perpendicular to the minimum principal stress (the direction in which the rock is being stretched). If the tensile stress exceeds the magnitude of the least principal compressive stress the rock will fail in a brittle manner and these cracks propagate in a process called hydraulic fracturing. Hydraulic joints occur as both nonsystematic and systematic joints, including orthogonal and conjugate joint sets. In some cases, joint sets can be a tectonic - hydraulic hybrid.

text: Hydraulic joints are joints thought to have formed when pore fluid pressure became elevated as a result of vertical gravitational loading. In simple terms, the accumulation of either sediments, volcanic, or other material causes an increase in the pore pressure of groundwater and other fluids in the underlying rock when they cannot move either laterally of vertically in response to this pressure. This also causes an increase in pore pressure in  preexisting cracks that increases the tensile stress on them perpendicular to the minimum principal stress (the direction in which the rock is being stretched). If the tensile stress exceeds the magnitude of the least principal compressive stress the rock will fail in a brittle manner and these cracks propagate in a process called

text: hydraulic fracturing

text: . Hydraulic joints occur as both nonsystematic and systematic joints, including orthogonal and conjugate joint sets. In some cases, joint sets can be a tectonic - hydraulic hybrid.

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answer: No

answer: No

answer: No

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text: In Bruges, the Procession of the Holy Blood (Heilig Bloedprocessie) is held on Ascension Day each year, during which a relic - a rock-crystal vial allegedly found during in 1148 during the Second Crusade by Derick of Alsace (the Count of Flanders) which is believed to contain the blood of Christ - is paraded round the city. The procession itself is said to date to the 13th Century. Each year, the procession attracts some 50,000 visitors and pilgrims.

text: In

text: Bruges

text: , the

text: Procession of the Holy Blood

text: (Heilig Bloedprocessie) is held on

text: Ascension Day

text: each year, during which a

text: relic

text: - a rock-crystal vial allegedly found during in 1148 during the

text: Second Crusade

text: by

text: Derick of Alsace

text: (the

text: Count of Flanders

text: ) which is believed to contain the blood of Christ - is paraded round the city. The procession itself is said to date to the 13th Century. Each year, the procession attracts some 50,000 visitors and pilgrims.

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text: Contact metamorphism occurs typically around intrusive igneous rocks as a result of the temperature increase caused by the intrusion of magma into cooler country rock. The area surrounding the intrusion where the contact metamorphism effects are present is called the metamorphic aureole. Contact metamorphic rocks are usually known as hornfels. Rocks formed by contact metamorphism may not present signs of strong deformation and are often fine-grained.

text: Contact metamorphism occurs typically around

text: intrusive

text: igneous rock

text: s as a result of the temperature increase caused by the intrusion of

text: magma

text: into cooler

text: country rock

text: . The area surrounding the intrusion where the contact metamorphism effects are present is called the metamorphic aureole. Contact metamorphic rocks are usually known as

text: hornfels

text: . Rocks formed by contact metamorphism may not present signs of strong deformation and are often fine-grained.

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text: The Lego Power Miners and Lego Rock Raiders theme both have settings that take place underground and both themes have each team search for crystals, whilst trying to prevent the Rock/Lava Monsters from eating them. However the difference is while the crystals in Lego Rock Raiders were Energy Crystals with massive power in them, the Lego Power Miners crystals seem to be kinetic energy based instead. While Lego Power Miners collect their crystals for research purposes, the Rock Raiders collect them as fuel for their ship. Another difference between the themes is that the Crystals eaten by Rock Monsters in Power Miners make them release the kinetic energy, causing massive rumbles when underneath the surface.

text: The Lego Power Miners and Lego Rock Raiders theme both have settings that take place underground and both themes have each team search for crystals, whilst trying to prevent the Rock/Lava Monsters from eating them. However the difference is while the crystals in Lego Rock Raiders were Energy Crystals with massive power in them, the Lego Power Miners crystals seem to be kinetic energy based instead. While Lego Power Miners collect their crystals for research purposes, the Rock Raiders collect them as fuel for their ship. Another difference between the themes is that the Crystals eaten by Rock Monsters in Power Miners make them release the kinetic energy, causing massive rumbles when underneath the surface.

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answers: Yes

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answers: Crystals eaten by Rock Monsters

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answers: faster cooling forms smaller crystals

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answers: Lava

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answers: The Lego Power Miners

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: While volcanic activity is reported as formation of a group of small islands, erosion has created the depressions which have a permeable base of "light grey, broken lava rocks, with harder rocks and grey or dark grey lavas overlying". Sandy soils resulting from sedimentation dominates the reserve with formation of parallel bars in the coastal area. The depressions are subject to filling by ephemeral floods; estuary lakes, grass marshes and wooded swamps caused by very heavy rainfall. Small tides of about  height have also affected the coastal zone. The small rivers and streams that originate in the hills and flow through the park generally have water  deep. The lakes in the northern part of the reserve are fed by the Colorado River. The very humid tropical forest is influenced by excessive humidity, rapid drainage and thin soils, with over 330 days of cloud cover per year. Moisture-laden winds come from the Caribbean.

text: While volcanic activity is reported as formation of a group of small islands, erosion has created the depressions which have a permeable base of "light grey, broken lava rocks, with harder rocks and grey or dark grey

text: lava

text: s overlying". Sandy soils resulting from sedimentation dominates the reserve with formation of parallel bars in the coastal area. The depressions are subject to filling by ephemeral floods; estuary lakes, grass marshes and wooded swamps caused by very heavy rainfall. Small tides of about  height have also affected the coastal zone. The small rivers and streams that originate in the hills and flow through the park generally have water  deep. The lakes in the northern part of the reserve are fed by the

text: Colorado River

text: . The very humid tropical forest is influenced by excessive humidity, rapid drainage and thin soils, with over 330 days of cloud cover per year. Moisture-laden winds come from the Caribbean.

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answers: light grey, broken lava rocks

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answers: Small tides

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answers: sedimentation

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The typical metamorphic assemblage reactions for low-magnesian (<25% MgO) and high-magnesian (>25% MgO) ultramafic rocks are;

text: The typical metamorphic assemblage reactions for low-magnesian (<25% MgO) and high-magnesian (>25% MgO) ultramafic rocks are;

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answers: Yes

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text: Rock engraving depends on the type of rock being used. Many different methods are used to create rock engravings. There are several different types of Rock art across Australia, the most famous of which is Murujuga in Western Australia, the Sydney rock engravings around Plymouth in New South Wales, and the Panaramitee rock art in Central Australia. The Sydney engravings, depicting carved animals and humans, have their own peculiar style not found elsewhere in Australia.

text: Rock engraving depends on the type of rock being used. Many different methods are used to create rock engravings. There are several different types of

text: Rock art

text: across Australia, the most famous of which is

text: Murujuga

text: in

text: Western Australia

text: , the

text: Sydney rock engravings

text: around

text: Plymouth

text: in

text: New South Wales

text: , and the

text: Panaramitee

text: rock art in

text: Central Australia

text: . The Sydney engravings, depicting carved animals and humans, have their own peculiar style not found elsewhere in Australia.

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text: Robert Arbuckle Berner  (November 25, 1935 – January 10, 2015) was an American scientist known for his contributions to the modeling of the carbon cycle. He taught Geology and Geophysics from 1965 to 2007 at Yale University, where he latterly served as Professor Emeritus until his death. His work on sedimentary rocks led to the co-founding of the BLAG model of atmospheric carbon dioxide, which takes into account both geochemical and biological contributions to the carbon cycle.

text: Robert Arbuckle Berner  (November 25, 1935 – January 10, 2015) was an American scientist known for his contributions to the modeling of the

text: carbon cycle

text: . He taught Geology and Geophysics from 1965 to 2007 at

text: Yale University

text: , where he latterly served as

text: Professor Emeritus

text: until his death. His work on

text: sedimentary rocks

text: led to the co-founding of the BLAG model of atmospheric

text: carbon dioxide

text: , which takes into account both geochemical and biological contributions to the carbon cycle.

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text: Many areas of high erosion are due to human activities. Reasons can include:  seawalls locking up sand dunes, coastal structures like ports and harbors that prevent longshore transport, dams and other river management structures. These activities interfere with the natural sediment flows either through dam construction (thereby reducing riverine sediment sources) or construction of littoral barriers such as jetties, or by deepening of inlets; thus preventing longshore transport of sediment across these channels.

text: Many areas of high erosion are due to human activities. Reasons can include:

text: seawall

text: s locking up

text: sand dunes

text: , coastal structures like ports and harbors that prevent

text: longshore transport

text: dam

text: s and other river management structures. These activities interfere with the natural sediment flows either through

text: dam

text: construction (thereby reducing riverine sediment sources) or construction of littoral barriers such as

text: jetties

text: , or by deepening of inlets; thus preventing longshore transport of sediment across these channels.

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text: The diversity of the landscapes of the United States can be easily seen on the shaded relief image to the right. The stark contrast between the ‘rough' texture of the western US and the ‘smooth' central and eastern regions is immediately apparent. Differences in roughness (topographic relief) result from a variety of processes acting on the underlying rock. The plate tectonic history of a region strongly influences the rock type and structure exposed at the surface, but differing rates of erosion that accompany changing climates can also have profound impacts on the land.

text: The diversity of the landscapes of the United States can be easily seen on the shaded relief image to the right. The stark contrast between the ‘rough' texture of the

text: western US

text: and the ‘smooth'

text: central

text: and

text: eastern

text: regions is immediately apparent. Differences in roughness (topographic relief) result from a variety of processes acting on the underlying rock. The plate tectonic history of a region strongly influences the rock type and structure exposed at the surface, but differing rates of erosion that accompany changing climates can also have profound impacts on the land.

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answers: Faster cooling forms larger crystals.

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answers: Different rates of erosion that accompany changing climates can also have profound impacts on the land

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The separation of mineral from gangue is known as mineral processing, mineral dressing or ore dressing and it is a necessary and often significant aspect of mining. It can be a complicated process, depending on the nature of the minerals involved. For example, galena, an ore of lead, is usually found in large pieces within its gangue, so it does not normally need extensive processing to remove it; but cassiterite, the chief ore of tin, is usually disseminated as very small crystals throughout its gangue, so when it is mined from hard rock, the ore-bearing rock first needs to be crushed very finely, and then has to be subjected to sophisticated processes to separate the ore.

text: The separation of mineral from gangue is known as

text: mineral processing

text: , mineral dressing or ore dressing and it is a necessary and often significant aspect of

text: mining

text: . It can be a complicated process, depending on the nature of the minerals involved. For example,

text: galena

text: , an ore of lead, is usually found in large pieces within its gangue, so it does not normally need extensive processing to remove it; but

text: cassiterite

text: , the chief ore of

text: tin

text: , is usually disseminated as very small crystals throughout its gangue, so when it is

text: mined from hard rock

text: , the ore-bearing rock first needs to be crushed very finely, and then has to be subjected to sophisticated processes to separate the ore.

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answers: cassiterite

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answers: Separation

answer: No

answer: No

answer: No

answer: No

answer: No

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text: In the 1960s, there were two main types of psychedelic rock: the whimsical British variant, and the harder American West Coast acid rock. The terms "psychedelic rock" and "acid rock" are often deployed interchangeably, but "acid rock" sometimes refers to the more extreme ends of the genre. Psychedelic rock influenced the creation of psychedelic soul and bridged the transition from early blues- and folk music-based rock to progressive rock, glam rock, hard rock and as a result influenced the development of subgenres such as heavy metal. Since the late 1970s it has been revived in various forms of neo-psychedelia.

text: In the 1960s, there were two main types of psychedelic rock: the whimsical British variant, and the harder American West Coast

text: acid rock

text: . The terms "psychedelic rock" and "acid rock" are often deployed interchangeably, but "acid rock" sometimes refers to the more extreme ends of the genre. Psychedelic rock influenced the creation of

text: psychedelic soul

text: and bridged the transition from early

text: blues

text: - and

text: folk music

text: -based rock to

text: progressive rock

text: glam rock

text: hard rock

text: and as a result influenced the development of subgenres such as

text: heavy metal

text: . Since the late 1970s it has been revived in various forms of

text: neo-psychedelia

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answers: Psychedelic rock

answer: No

answer: No

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text: The textures of dynamic metamorphic zones are dependent on the depth at which they were formed, as the temperature and confining pressure determine the deformation mechanisms which predominate. Within depths less than 5 km, dynamic metamorphism is not often produced because the confining pressure is too low to produce frictional heat. Instead, a zone of breccia or cataclasite is formed, with the rock milled and broken into random fragments. This generally forms a mélange. At depth, the angular breccias transit into a ductile shear texture and into mylonite zones.

text: The textures of dynamic metamorphic zones are dependent on the depth at which they were formed, as the temperature and confining pressure determine the

text: deformation mechanism

text: s which predominate. Within depths less than 5 km, dynamic metamorphism is not often produced because the confining pressure is too low to produce frictional heat. Instead, a zone of

text: breccia

text: or

text: cataclasite

text: is formed, with the rock milled and broken into random fragments. This generally forms a

text: mélange

text: . At depth, the angular breccias transit into a ductile shear texture and into mylonite zones.

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text: {| class="wikitable"|-! Band || Active || Notes|-| 10 Years ||Yes|| Also classed as post-grunge and progressive metal.|-| 12 Stones ||Yes|| Also classed as post-grunge, alternative rock, hard rock and christian rock.|-| 36 Crazyfists ||Yes|| Also classed as metalcore, post-hardcore and nu metal.|-| 311 ||Yes|| Also classed as reggae rock, alternative rock, rap metal, funk rock, rap rock and funk metal.|-| Alice in Chains || Yes || Also classed as grunge, heavy metal, doom metal, sludge metal, dark metal and alternative rock.|-| Alien Ant Farm ||Yes|| Also classed as alternative rock, nu metal, pop punk and post-grunge.|-| Alter Bridge ||Yes|| Also classed as hard rock and heavy metal.|-| Anthrax ||Yes|| Also classed as thrash metal, heavy metal, groove metal, speed metal, rap metal and grunge.

text: {| class="wikitable"|-! Band || Active || Notes|-|

text: 10 Years

text: ||Yes|| Also classed as

text: post-grunge

text: and

text: progressive metal

text: 12 Stones

text: ||Yes|| Also classed as

text: post-grunge

text: alternative rock

text: hard rock

text: and

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text: 36 Crazyfists

text: ||Yes|| Also classed as

text: metalcore

text: post-hardcore

text: and

text: nu metal

text: ||Yes|| Also classed as

text: reggae rock

text: alternative rock

text: rap metal

text: funk rock

text: rap rock

text: and

text: funk metal

text: Alice in Chains

text: || Yes || Also classed as

text: grunge

text: heavy metal

text: doom metal

text: sludge metal

text: dark metal

text: and

text: alternative rock

text: Alien Ant Farm

text: ||Yes|| Also classed as

text: alternative rock

text: nu metal

text: pop punk

text: and

text: post-grunge

text: Alter Bridge

text: ||Yes|| Also classed as

text: hard rock

text: and

text: heavy metal

text: Anthrax

text: ||Yes|| Also classed as

text: thrash metal

text: heavy metal

text: groove metal

text: speed metal

text: rap metal

text: and

text: grunge

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answers: Slower cooling forms smaller crystals.

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answers: It is out of the rock cycle.

answer: No

answer: No

answer: No

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text: This type of rock formation and weathering process has happened in many other places locally and throughout the world, but what makes Meteora's appearance special is firstly the uniformity of the sedimentary rock constituents deposited over millions of years leaving few signs of vertical layering, and secondly the localised abrupt vertical weathering.

text: This type of rock formation and weathering process has happened in many other places locally and throughout the world, but what makes Meteora's appearance special is firstly the uniformity of the sedimentary rock constituents deposited over millions of years leaving few signs of vertical layering, and secondly the localised abrupt vertical weathering.

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answers: localised abrupt vertical weathering

answers: NDQ_005764

answers: uniformity

answers: NDQ_005765

answers: weathering

answers: NDQ_005766

answers: meteorite

answers: NDQ_005768

answers: faster cooling forms smaller crystals

answers: NDQ_005769

answers: weathering

answers: NDQ_005770

answers: Meteora

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The overall balance between sediment in transport and sediment being deposited on the bed is given by the Exner equation. This expression states that the rate of increase in bed elevation due to deposition is proportional to the amount of sediment that falls out of the flow. This equation is important in that changes in the power of the flow changes the ability of the flow to carry sediment, and this is reflected in patterns of erosion and deposition observed throughout a stream. This can be localized, and simply due to small obstacles: examples are scour holes behind boulders, where flow accelerates, and deposition on the inside of meander bends. Erosion and deposition can also be regional: erosion can occur due to dam removal and base level fall. Deposition can occur due to dam emplacement that causes the river to pool, and deposit its entire load or due to base level rise.

text: The overall balance between sediment in transport and sediment being deposited on the bed is given by the

text: Exner equation

text: . This expression states that the rate of increase in bed elevation due to deposition is proportional to the amount of sediment that falls out of the flow. This equation is important in that changes in the power of the flow changes the ability of the flow to carry sediment, and this is reflected in patterns of erosion and deposition observed throughout a stream. This can be localized, and simply due to small obstacles: examples are scour holes behind boulders, where flow accelerates, and deposition on the inside of

text: meander

text: bends. Erosion and deposition can also be regional: erosion can occur due to

text: dam removal

text: and

text: base level

text: fall. Deposition can occur due to dam emplacement that causes the river to pool, and deposit its entire load or due to base level rise.

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answers: This can be localized, and simply due to small obstacles

answers: NDQ_005762

answers: sedimentary

answers: NDQ_005763

answers: changes in the power of the flow

answers: NDQ_005764

answers: bed elevation

answers: NDQ_005765

answers: deposition

answers: NDQ_005766

answers: boulders

answers: NDQ_005768

answers: rate of increase in bed elevation due to deposition

answers: NDQ_005769

answers: deposition

answers: NDQ_005770

answers: Deposition

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The evolving melt will remain here until it fractionates enough (through MASH processes) that the remaining melt is less dense than the surrounding rock; the melt will then continue up into the crust, leaving behind the heavier mafic minerals which were crystallized during fractional crystallization. The assemblage of minerals remaining behind are typically mafic or ultramafic, and are responsible for the observed seismic anomaly which indicates underplated material.

text: The evolving melt will remain here until it fractionates enough (through MASH processes) that the remaining melt is less dense than the surrounding rock; the melt will then continue up into the crust, leaving behind the heavier

text: mafic

text: minerals which were crystallized during

text: fractional crystallization

text: . The assemblage of minerals remaining behind are typically mafic or

text: ultramafic

text: , and are responsible for the observed

text: seismic anomaly

text: which indicates underplated material.

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answers: Yes

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answers: sedimentary

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answers: fractional crystallization

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answers: density

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answers: fractionates enough

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answers: mafic

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answers: fractional crystallization

answers: NDQ_005769

answers: fractionates

answers: NDQ_005770

answers: fractionates

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The Ordovician turbidites, consisting of greywacke, feldspathic sandstone, micaceous siltstone, micaceous shale, chert, and phyllite, are very similar in all parts of the Tasman Orogen, including New Zealand and the Transantarctic Mountains. Detrital zircons from the turbidites have been isotopically dated with age ranges of 0.46 and 0.60 Gya, 1.0 and 1.2 Gya, and at ~1.8 Gya, ~2.2 Gya and ~2.7 Gya. These do not match the age of zircons from the interior of the Australian Shield, so the source of the sediments is from another continent. The other evidence from the Ordovician sediments are chemical composition indicates granitic source, with the absence of feldspar. Secondly the fine grained nature shows the sediments have been transported a long way from their ultimate, source, and could have been second cycle, derived from sedimentary rocks.

text: The Ordovician

text: turbidite

text: s, consisting of

text: greywacke

text: , feldspathic sandstone, micaceous siltstone, micaceous shale, chert, and

text: phyllite

text: , are very similar in all parts of the Tasman Orogen, including New Zealand and the

text: Transantarctic Mountains

text: . Detrital

text: zircon

text: s from the turbidites have been

text: isotopically dated

text: with age ranges of 0.46 and 0.60 Gya, 1.0 and 1.2 Gya, and at ~1.8 Gya, ~2.2 Gya and ~2.7 Gya. These do not match the age of zircons from the interior of the

text: Australian Shield

text: , so the source of the sediments is from another continent. The other evidence from the Ordovician sediments are chemical composition indicates granitic source, with the absence of feldspar. Secondly the fine grained nature shows the sediments have been transported a long way from their ultimate, source, and could have been second cycle, derived from sedimentary rocks.

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answers: Yes

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answers: sedimentary

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answers: Tasman Orogen

answers: NDQ_005764

answers: age

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answers: second cycle, derived from sedimentary rocks

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answers: granitic

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answers: Detrital zircons

answers: NDQ_005769

answers: turbidites

answers: NDQ_005770

answers: derived from sedimentary rocks

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The type of dominating deformation process also has a great impact on the types of rocks and structures found at certain depths within the Earth's crust. As evident from Fig. 1.1, different geological formations and rocks are found in accordance to the dominant deformation process. Gouge and Breccia form in the uppermost, brittle regime while Cataclasite and Pseudotachylite form in the lower parts of the brittle regime, edging upon the transition zone. Mylonite forms in the more ductile regime at greater depths while Blastomylonite forms well past the transition zone and well into the ductile regime, even deeper into the crust.

text: The type of dominating deformation process also has a great impact on the types of rocks and structures found at certain depths within the Earth's crust. As evident from Fig. 1.1, different geological formations and rocks are found in accordance to the dominant deformation process. Gouge and

text: Breccia

text: form in the uppermost, brittle regime while

text: Cataclasite

text: and

text: Pseudotachylite

text: form in the lower parts of the brittle regime, edging upon the transition zone.

text: Mylonite

text: forms in the more ductile regime at greater depths while Blastomylonite forms well past the transition zone and well into the ductile regime, even deeper into the crust.

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answers: different geological formations

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answers: extrusive

answers: NDQ_005763

answers: dominant deformation process

answers: NDQ_005764

answers: ductile

answers: NDQ_005765

answers: dominant deformation

answers: NDQ_005766

answers: Blastomylonite

answers: NDQ_005768

answers: Cataclasite

answers: NDQ_005769

answers: Cataclasite

answers: NDQ_005770

answers: past the transition zone

answer: No

answer: No

answer: Yes

answer: No

answer: No

answer: 1

text: The addition of new rock units, both depositionally and intrusively, often occurs during deformation. Faulting and other deformational processes result in the creation of topographic gradients, causing material on the rock unit that is increasing in elevation to be eroded by hillslopes and channels. These sediments are deposited on the rock unit that is going down. Continual motion along the fault maintains the topographic gradient in spite of the movement of sediment, and continues to create accommodation space for the material to deposit. Deformational events are often also associated with volcanism and igneous activity. Volcanic ashes and lavas accumulate on the surface, and igneous intrusions enter from below. Dikes, long, planar igneous intrusions, enter along cracks, and therefore often form in large numbers in areas that are being actively deformed. This can result in the emplacement of dike swarms, such as those that are observable across the Canadian shield, or rings of dikes around the lava tube of a volcano.

text: The addition of new rock units, both depositionally and intrusively, often occurs during deformation. Faulting and other deformational processes result in the creation of topographic gradients, causing material on the rock unit that is increasing in elevation to be eroded by hillslopes and channels. These sediments are deposited on the rock unit that is going down. Continual motion along the fault maintains the topographic gradient in spite of the movement of sediment, and continues to create

text: accommodation space

text: for the material to deposit. Deformational events are often also associated with volcanism and igneous activity. Volcanic ashes and lavas accumulate on the surface, and igneous intrusions enter from below.

text: Dikes

text: , long, planar igneous intrusions, enter along cracks, and therefore often form in large numbers in areas that are being actively deformed. This can result in the emplacement of

text: dike swarm

text: s, such as those that are observable across the Canadian shield, or rings of dikes around the

text: lava tube

text: of a volcano.

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answers: Yes

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answers: sedimentary

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answers: volcanoes

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answers: elevation

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answers: The addition of new rock units

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answers: igneous

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answers: faster cooling forms smaller crystals

answers: NDQ_005769

answers: deposition

answers: NDQ_005770

answers: The addition of new rock units

answer: No

answer: No

answer: Yes

answer: No

answer: No

answer: 1

text: Regional metamorphism, also known as dynamic metamorphism, is the name given to changes in great masses of rock over a wide area. Rocks can be metamorphosed simply by being at great depths below the Earth's surface, subjected to high temperatures and the great pressure caused by the immense weight of the rock layers above. Much of the lower continental crust is metamorphic, except for recent igneous intrusions. Horizontal tectonic movements such as the collision of continents create orogenic belts, and cause high temperatures, pressures and deformation in the rocks along these belts. If the metamorphosed rocks are later uplifted and exposed by erosion, they may occur in long belts or other large areas at the surface. The process of metamorphism may have destroyed the original features that could have revealed the rock's previous history. Recrystallization of the rock will destroy the textures and fossils present in sedimentary rocks. Metasomatism will change the original composition.

text: Regional metamorphism, also known as dynamic metamorphism, is the name given to changes in great masses of rock over a wide area. Rocks can be metamorphosed simply by being at great depths below the Earth's surface, subjected to high temperatures and the great pressure caused by the immense weight of the rock layers above. Much of the lower continental crust is metamorphic, except for recent igneous intrusions. Horizontal tectonic movements such as the collision of continents create

text: orogenic belts

text: , and cause high temperatures, pressures and deformation in the rocks along these belts. If the metamorphosed rocks are later uplifted and exposed by

text: erosion

text: , they may occur in long belts or other large areas at the surface. The process of metamorphism may have destroyed the original features that could have revealed the rock's previous history.

text: Recrystallization

text: of the rock will destroy the textures and

text: fossil

text: s present in sedimentary rocks. Metasomatism will change the original composition.

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answers: Much of the lower continental crust

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answer: Yes

answer: No

answer: Yes

answer: No

answer: No

answer: 1

text: The main event at Backlash was the encounter of Goldberg and The Rock; the main feud from the Raw brand heading into the event. The feud began on the March 31, 2003 episode of Raw, where The Rock held a segment entitled The Rock Appreciation Night, a segment intended to promote his win against Steve Austin at WrestleMania XIX. During the segment, The Rock discussed the list of people he has beaten in his career including Steve Austin, wondering who would challenge him next into a match. Goldberg then made his WWE debut, as he came down to the ring and stated that he would be The Rock's next challenge. After the confrontation, Goldberg speared The Rock. The following week on Raw, Goldberg and The Rock had another confrontation, where Goldberg provoked The Rock into answering his challenge, but The Rock refused. The Rock finally accepted Goldberg's challenge on the April 14, 2003 episode of Raw via satellite. The week before Backlash, the feud intensified as The Rock held another segment entitled The Rock Concert, where he mocked Goldberg with Gillberg, a wrestler whose gimmick was to parody Goldberg. Later into the segment, Goldberg appeared from the audience and entered the ring, only to have The Rock execute a Rock Bottom on him.

text: The

text: main event

text: at Backlash was the encounter of

text: Goldberg

text: and

text: The Rock

text: ; the main

text: feud

text: from the

text: Raw

text: brand

text: heading into the event. The feud began on the March 31, 2003 episode of Raw, where The Rock held a segment entitled The Rock Appreciation Night, a segment intended to promote his win against

text: Steve Austin

text: at

text: WrestleMania XIX

text: . During the segment, The Rock discussed the list of people he has beaten in his career including Steve Austin, wondering who would challenge him next into a match. Goldberg then made his WWE debut, as he came down to the ring and stated that he would be The Rock's next challenge. After the confrontation, Goldberg

text: speared

text: The Rock. The following week on Raw, Goldberg and The Rock had another confrontation, where Goldberg provoked The Rock into answering his challenge, but The Rock refused. The Rock finally accepted Goldberg's challenge on the April 14, 2003 episode of Raw via satellite. The week before Backlash, the feud intensified as The Rock held another segment entitled The Rock Concert, where he mocked Goldberg with

text: Gillberg

text: , a wrestler whose

entity_name: Glossary of professional wrestling terms

text: gimmick

text: was to parody Goldberg. Later into the segment, Goldberg appeared from the audience and entered the ring, only to have The Rock execute a

text: Rock Bottom

text: on him.

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answers: slower cooling forms smaller crystals

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answer: No

answer: No

answer: No

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text: The rocks in question are part of a metamorphosed supracrustal sequence located at the south-western tip of the island. The sequence has been dated as no younger than 3.85 billion years old - that is,  in the Hadean eon - based on the age of an igneous band that cuts the rock.  The supracrustal sequence contains layers rich in iron and silica, which are variously interpreted as banded iron formation, chemical sediments from submarine hot springs, or hydrothermal vein deposits. Carbon in the rock, present as graphite, shows low levels of carbon-13, which may suggest an origin as isotopically light organic matter derived from living organisms.  However, this interpretation is complicated because of high-grade metamorphism that  affected the Akilia rocks after their formation. The sedimentary origin, age and the carbon content of the rocks have been questioned.

text: The rocks in question are part of a

text: metamorphosed

text: supracrustal

text: sequence located at the south-western tip of the island. The sequence has been dated as no younger than 3.85 billion years old - that is,  in the

text: Hadean

text: eon - based on the age of an

text: igneous

text: band that cuts the rock.  The supracrustal sequence contains layers rich in

text: iron

text: and

text: silica

text: , which are variously interpreted as

text: banded iron formation

text: , chemical sediments from

text: submarine hot springs

text: , or

text: hydrothermal

text: vein deposits.

text: Carbon

text: in the rock, present as

text: graphite

text: , shows low levels of

text: , which may suggest an origin as

text: isotopically

text: light organic matter derived from living organisms.  However, this interpretation is complicated because of high-grade

text: metamorphism

text: that  affected the Akilia rocks after their formation. The sedimentary origin, age and the carbon content of the rocks have been questioned.

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answers: Yes

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answers: metamorphism that affected the Akilia rocks after their formation

answers: NDQ_005769

answers: hydrothermal

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answers: metamorphism

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Igneous rock (derived from the Latin word ignis meaning fire), or magmatic rock, is one of the three main rock types, the others being sedimentary and metamorphic. Igneous rock is formed through the cooling and solidification of magma or lava. The magma can be derived from partial melts of existing rocks in either a planet's mantle or crust. Typically, the melting is caused by one or more of three processes: an increase in temperature, a decrease in pressure, or a change in composition. Solidification into rock occurs either below the surface as intrusive rocks or on the surface as extrusive rocks. Igneous rock may form with crystallization to form granular, crystalline rocks,  or without crystallization to form natural glasses.

text: Igneous rock (derived from the

text: Latin

text: word ignis meaning fire), or magmatic rock, is one of the three main

text: rock types

text: , the others being

text: sedimentary

text: and

text: metamorphic

text: . Igneous rock is formed through the cooling and solidification of

text: magma

text: or

text: lava

text: . The magma can be derived from

text: partial melts

text: of existing rocks in either a

text: planet

text: 's

text: mantle

text: or

text: crust

text: . Typically, the melting is caused by one or more of three processes: an increase in

text: temperature

text: , a decrease in

text: pressure

text: , or a change in composition. Solidification into rock occurs either below the surface as

text: intrusive

text: rocks or on the surface as

text: extrusive

text: rocks. Igneous rock may form with

text: crystallization

text: to form granular, crystalline rocks,  or without crystallization to form

text: natural glass

text: es.

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answers: Igneous rock is one of the three main rock types

answers: NDQ_005762

answers: Igneous rock

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answers: an increase in temperature, a decrease in pressure, or a change in composition

answers: NDQ_005764

answers: solidification

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answers: solidification of magma or lava

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answers: Igneous

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answers: crystallization

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answers: solidification of magma or lava

answer: Yes

answer: No

answer: No

answer: No

answer: No

answer: 1

text: A river flowing in its channel is a source of energy which acts on the river channel to change its shape and form. In 1757, the German hydrologist Albert Brahms empirically observed that the submerged weight of objects that may be carried away by a river is proportional to the sixth power of the river flow speed. This formulation is also sometimes called Airy's law. Thus, if the speed of flow is doubled, the flow would dislodge objects with 64 times as much submerged weight. In mountainous torrential zones this can be seen as erosion channels through hard rocks and the creation of sands and gravels from the destruction of larger rocks. In U-shaped glaciated valleys, the subsequent river valley can often easily be identified by the V-shaped channel that it has carved. In the middle reaches where a river flows over flatter land, meanders may form through erosion of the river banks and deposition on the inside of bends. Sometimes the river will cut off a loop, shortening the channel and forming an oxbow lake or billabong. Rivers that carry large amounts of sediment may develop conspicuous deltas at their mouths. Rivers whose mouths are in saline tidal waters may form estuaries.

text: A river flowing in its channel is a source of energy which acts on the river channel to change its shape and form. In 1757, the German hydrologist

text: Albert Brahms

text: empirically observed that the submerged weight of objects that may be carried away by a river is proportional to the sixth power of the river flow speed. This formulation is also sometimes called Airy's law. Thus, if the speed of flow is doubled, the flow would dislodge objects with 64 times as much submerged weight. In mountainous torrential zones this can be seen as erosion channels through hard rocks and the creation of sands and gravels from the destruction of larger rocks. In U-shaped

text: glaciated

text: valleys, the subsequent river valley can often easily be identified by the V-shaped channel that it has carved. In the middle reaches where a river flows over flatter land,

text: meander

text: s may form through erosion of the river banks and deposition on the inside of bends. Sometimes the river will cut off a loop, shortening the channel and forming an

text: oxbow lake

text: or

text: billabong

text: . Rivers that carry large amounts of

text: sediment

text: may develop conspicuous

text: deltas

text: at their mouths. Rivers whose mouths are in saline

text: tidal

text: waters may form

text: estuaries

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answers: The destruction of larger rocks

answers: NDQ_005762

answers: sedimentary

answers: NDQ_005763

answers: speed of flow

answers: NDQ_005764

answers: shape

answers: NDQ_005765

answers: destruction of larger rocks

answers: NDQ_005766

answers: glaciated

answers: NDQ_005768

answers: Submerged weight of objects that may be carried away by a river is proportional to the sixth power of the river flow speed

answers: NDQ_005769

answers: estuaries

answers: NDQ_005770

answers: Rivers that carry large amounts of sediment may develop conspicuous deltas at their mouths

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: There are four primary types of sedimentary rocks: clastics, carbonates, evaporites, and chemical.

text: There are four primary types of

text: sedimentary rocks

text: : clastics, carbonates, evaporites, and chemical.

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answers: clastics

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answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The term porphyry is also used for a mineral deposit called a "copper porphyry".  The different stages of cooling that create porphyritic textures in intrusive and hypabyssal porphyritic rocks also lead to a separation of dissolved metals into distinct zones. This process, which occurs primarily when fluids are driven off the cooling magma, is one of the main reasons for the existence in the world of rich, localized metal ore deposits such as those of gold, copper, molybdenum, lead, tin, zinc, rhenium and tungsten. This enrichment occurs in the porphyry itself, or in other related igneous rocks or surrounding country rocks, especially carbonate rock (in a process similar to skarns). Collectively, these type of deposits are known as "porphyry copper deposits".

text: The term porphyry is also used for a mineral deposit called a "copper porphyry".  The different stages of cooling that create porphyritic textures in intrusive and

text: hypabyssal

text: porphyritic rocks also lead to a separation of dissolved metals into distinct zones. This process, which occurs primarily when fluids are driven off the cooling magma, is one of the main reasons for the existence in the world of rich, localized metal ore deposits such as those of

text: gold

text: copper

text: molybdenum

text: lead

text: tin

text: zinc

text: rhenium

text: and

text: tungsten

text: . This enrichment occurs in the porphyry itself, or in other related igneous rocks or surrounding country rocks, especially

text: carbonate rock

text: (in a process similar to

text: skarn

text: s). Collectively, these type of deposits are known as "porphyry copper deposits".

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answers: The term porphyry is also used for a mineral deposit called a "copper porphyry"

answers: NDQ_005762

answers: intrusive

answers: NDQ_005763

answers: different stages of cooling

answers: NDQ_005764

answers: porphyritic

answers: NDQ_005765

answers: skarns

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answers: magma

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answers: The different stages of cooling

answers: NDQ_005769

answers: separation

answers: NDQ_005770

answers: porphyry

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The characteristic rocks of obducted oceanic lithosphere are the ophiolites. Ophiolites are an assemblage of oceanic lithosphere rocks that have been emplaced onto a continent. This assemblage consists of deep-marine sedimentary rock (chert, limestone, clastic sediments), volcanic rocks (pillow lavas, glass, ash, sheeted dykes and gabbros) and peridotite (mantle rock).

text: The characteristic rocks of obducted oceanic lithosphere are the

text: ophiolites

text: . Ophiolites are an assemblage of oceanic lithosphere rocks that have been emplaced onto a continent. This assemblage consists of deep-marine sedimentary rock (chert, limestone, clastic sediments), volcanic rocks (

text: pillow lava

text: s, glass, ash,

text: sheeted dykes

text: and

text: gabbro

text: s) and

text: peridotite

text: (mantle rock).

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answers: Yes

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answers: deep-marine sedimentary rock

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answers: mantle

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answers: peridotite

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answer: No

answer: No

answer: No

answer: No

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text: Geologically the Ivrea zone is considered a part of the Southern Alps. Most rocks in the zone are sedimentary, for example limestones that have been turned into marble by metamorphism. Most of the zone has been through granulite facies metamorphism and was intruded by mafic plutons. This is the type of rock common in the lower regions of the crust. When the terrane was uplifted during the formation of the Alps, the upper crust was eroded off so that these rocks are now at the surface.

text: Geologically the Ivrea zone is considered a part of the

text: Southern Alps

text: . Most rocks in the zone are

text: sedimentary

text: , for example

text: limestone

text: s that have been turned into

text: marble

text: by

text: metamorphism

text: . Most of the zone has been through

text: granulite facies

text: metamorphism and was intruded by

text: mafic

text: pluton

text: s. This is the type of rock common in the lower regions of the crust. When the terrane was

text: uplifted

text: during the formation of the Alps, the upper crust was eroded off so that these rocks are now at the surface.

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text: Rocks exposed to high temperatures and pressures can be changed physically or chemically to form a different rock, called metamorphic. Regional metamorphism refers to the effects on large masses of rocks over a wide area, typically associated with mountain building events within orogenic belts. These rocks commonly exhibit distinct bands of differing mineralogy and colors, called foliation. Another main type of metamorphism is caused when a body of rock comes into contact with an igneous intrusion that heats up this surrounding country rock. This contact metamorphism results in a rock that is altered and re-crystallized by the extreme heat of the magma and/or by the addition of fluids from the magma that add chemicals to the surrounding rock (metasomatism). Any pre-existing type of rock can be modified by the processes of metamorphism.

text: Rocks exposed to high temperatures and pressures can be changed physically or chemically to form a different rock, called metamorphic. Regional metamorphism refers to the effects on large masses of rocks over a wide area, typically associated with mountain building events within

text: orogenic belts

text: . These rocks commonly exhibit distinct bands of differing mineralogy and colors, called

text: foliation

text: . Another main type of metamorphism is caused when a body of rock comes into contact with an igneous intrusion that heats up this surrounding country rock. This contact metamorphism results in a rock that is altered and re-crystallized by the extreme heat of the magma and/or by the addition of fluids from the magma that add chemicals to the surrounding rock (

text: metasomatism

text: ). Any pre-existing type of rock can be modified by the processes of metamorphism.

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answers: Any pre-existing type of rock

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text: The fifth match was between The Rock and The Undertaker. After Rock kicked out of a Chokeslam, Undertaker threw the referee into the steel steps and retrieved a lead pipe from his motorbike. Ric Flair interfered, attacking Undertaker but Undertaker performed a Big Boot on Flair. Undertaker attempted to hit Rock with the pipe but Rock applied the Sharpshooter on Undertaker. Vince McMahon interfered, distracting the referee. Rock attacked Vince, which distracted the referee. Undertaker attempted a Tombstone Piledriver on Rock but Flair hit Undertaker with the pipe and Rock pinned Undertaker after a Rock Bottom to win the match.

text: The fifth match was between

text: The Rock

text: and

text: The Undertaker

text: . After Rock kicked out of a Chokeslam, Undertaker threw the referee into the steel steps and retrieved a lead pipe from his motorbike.

text: Ric Flair

text: interfered, attacking Undertaker but Undertaker performed a Big Boot on Flair. Undertaker attempted to hit Rock with the pipe but Rock applied the Sharpshooter on Undertaker. Vince McMahon interfered, distracting the referee. Rock attacked Vince, which distracted the referee. Undertaker attempted a Tombstone Piledriver on Rock but Flair hit Undertaker with the pipe and Rock pinned Undertaker after a Rock Bottom to win the match.

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text: Fractional crystallization and accumulation of crystals formed during the differentiation process of a magmatic event are known as cumulate rocks, and those parts are the first which crystallize out of the magma. Identifying whether a rock is a cumulate or not is crucial for understanding if it can be modelled back to a primary melt or a primitive melt, and identifying whether the magma has dropped out cumulate minerals is equally important even for rocks which carry no phenocrysts.

text: Fractional crystallization and accumulation of crystals formed during the differentiation process of a magmatic event are known as cumulate rocks, and those parts are the first which crystallize out of the magma. Identifying whether a rock is a cumulate or not is crucial for understanding if it can be modelled back to a primary melt or a primitive melt, and identifying whether the magma has dropped out cumulate minerals is equally important even for rocks which carry no

text: phenocryst

text: s.

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answer: No

answer: No

answer: No

answer: No

answer: No

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text: This forms disseminated needle like millerite crystals dispersed throughout the rock mass.

text: This forms disseminated needle like millerite crystals dispersed throughout the rock mass.

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answer: No

answer: No

answer: No

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text: They are the oldest igneous rocks, with crystallization ages of around 4.55 billion years.

text: They are the oldest

text: igneous rocks

text: , with

text: crystallization

text: ages of around 4.55 billion years.

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answer: No

answer: No

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answer: 1

text: South of the Pieniny Klippen Belt, the zone of core mountains is present. The core is formed by the Tatric unit composed predominantly by Paleozoic metamorphic rock, younger plutonic rock, and Carboniferous to Mesozoic sedimentary cover. Basement rock was formed during the Hercynian orogeny when a strong regional metamorphism affected the area. Paragneisses and amphibolites are most abundant, but low grade metamorphic rock is also present. Later, at the end of Hercynian orogeny in the Carboniferous and Permian, the area was intruded by granitic rock and strongly affected by erosion, which affected even the deeply situated granites. The autochthonous Carboniferous, Permian and most commonly Mesozoic sediments are onlaping the crystalline basement. They are represented by greywackes, quartz sandstones, shales, limestones, and marls. Sedimentary cover of the Tatric unit is overridden by Mesozoic nappes. Nappes are large slabs of the Mesozoic carbonate rock with similar sedimentary sequence as present in the Tatric cover. There are two so-called Subtatric nappes: the lower called the Kížna nappe (or the Fatric) and the upper called Choč nappe (or the Hronic). The Fatric is characterised by the occurrence of thicker formations of the Carpathian Keuper. The Hronic is typical with the occurrence of Permian andesitic-basalts (so called Ipoltica Group) and a larger thickness of variable Triassic carbonate rock. Thrusting of the nappes took place in the Upper Cretaceous, probably during the Turonian. The whole area was not so rangy as it is today. Uplift of the mountains took place at the end of the Oligocene and in the Miocene. It caused the uplift of the horsts, usually asymmetric, on the South flank, steeply bounded by normal faults and slightly declining to the North flank. The crystalline basement is usually uncovered on the South flank of the horsts. The horsts form two rows of mountains. The northern (outer) row consists of the Malé Karpaty Mts. (Pezinok part and Hainburg Mts.), Považský Inovec Mts., Strážovské vrchy Mts., Malá Fatra Mts., and Tatra Mts. The Southern row of core mountains includes the Tríbeč Mts., Žiar Mts., Veľká Fatra Mts., Chočské vrchy Mts., The Eastern part of Nízke Tatry Mts. (so called Ďumbierske Tatry) and Branisko Mts..

text: South of the Pieniny Klippen Belt, the zone of core mountains is present. The core is formed by the

text: Tatric

text: unit composed predominantly by

text: Paleozoic

text: metamorphic rock, younger plutonic rock, and

text: Carboniferous

text: to

text: Mesozoic

text: sedimentary cover. Basement rock was formed during the

text: Hercynian orogeny

text: when a strong regional

text: metamorphism

text: affected the area.

text: Paragneiss

text: es and

text: amphibolite

text: s are most abundant, but low grade metamorphic rock is also present. Later, at the end of Hercynian orogeny in the Carboniferous and

text: Permian

text: , the area was intruded by

text: granitic rock

text: and strongly affected by

text: erosion

text: , which affected even the deeply situated granites. The

text: autochthon

text: ous Carboniferous, Permian and most commonly

text: Mesozoic

text: sediments are

text: onlap

text: ing the crystalline basement. They are represented by

text: greywacke

text: s, quartz

text: sandstone

text: s,

text: shale

text: s,

text: limestone

text: s, and

text: marl

text: s. Sedimentary cover of the Tatric unit is overridden by Mesozoic nappes. Nappes are large slabs of the Mesozoic carbonate rock with similar sedimentary sequence as present in the Tatric cover. There are two so-called

text: Subtatric nappes

text: : the lower called the

text: Kížna nappe

text: (or the

text: Fatric

text: ) and the upper called

text: Choč nappe

text: (or the

text: Hronic

text: ). The Fatric is characterised by the occurrence of thicker formations of the

text: Carpathian Keuper

text: . The Hronic is typical with the occurrence of Permian

text: andesitic

text: basalt

text: s (so called

text: Ipoltica Group

text: ) and a larger thickness of variable

text: Triassic

text: carbonate rock. Thrusting of the nappes took place in the

text: Upper Cretaceous

text: , probably during the

text: Turonian

text: . The whole area was not so rangy as it is today. Uplift of the mountains took place at the end of the

text: Oligocene

text: and in the

text: Miocene

text: . It caused the uplift of the

text: horsts

text: , usually asymmetric, on the South flank, steeply bounded by

text: normal fault

text: s and slightly declining to the North flank. The crystalline basement is usually uncovered on the South flank of the horsts. The horsts form two rows of mountains. The northern (outer) row consists of the

text: Malé Karpaty Mts.

text: Pezinok

text: part and

text: Hainburg Mts.

text: Považský Inovec Mts.

text: Strážovské vrchy Mts.

text: Malá Fatra Mts.

text: , and

text: Tatra Mts

text: . The Southern row of core mountains includes the

text: Tríbeč Mts.

text: Žiar Mts.

text: Veľká Fatra Mts.

text: Chočské vrchy Mts.

text: , The Eastern part of

text: Nízke Tatry Mts.

text: (so called Ďumbierske Tatry) and

text: Branisko Mts.

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answers: faster cooling forms smaller crystals

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answers: Metamorphic rock

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Layered gabbro and dolerite of Silurian age occur at Kapp Laura in easternmost Nordaustlandet, on the island of Storøya, and in the eastern part of the island of Kvitøya. On Andréeneset, in the southern part of Kvitøya, gneisses and granites are the most common rock types. Four generations of rocks: gneiss, amphibolite, and grey and pink granite are present on Isispynten, a headland east of Austfonna. South of Wahlenbergfjorden there is a large area with sedimentary rocks – mostly limestone and dolomite – from the Carboniferous and Permian. The youngest rocks in Nordaustlandet are Jurassic–Cretaceous dolerite dikes, which intrude the basement rocks on the island of Lågøya and in the outlet of Brennevinsfjorden.

text: Layered

text: gabbro

text: and

text: dolerite

text: of Silurian age occur at

text: Kapp Laura

text: in easternmost Nordaustlandet, on the island of

text: Storøya

text: , and in the eastern part of the island of

text: Kvitøya

text: . On

text: Andréeneset

text: , in the southern part of Kvitøya, gneisses and granites are the most common rock types. Four generations of rocks: gneiss,

text: amphibolite

text: , and grey and pink granite are present on

text: Isispynten

text: , a headland east of Austfonna. South of

text: Wahlenbergfjorden

text: there is a large area with

text: sedimentary rock

text: s – mostly

text: limestone

text: and

text: dolomite

text: – from the Carboniferous and Permian. The youngest rocks in Nordaustlandet are Jurassic–Cretaceous dolerite dikes, which intrude the basement rocks on the island of

text: Lågøya

text: and in the outlet of

text: Brennevinsfjorden

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answers: Four generations

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answers: dolerite dikes

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answers: Silurian

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answers: Silurian

answer: No

answer: No

answer: No

answer: No

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answer: 1

text: Rocks in the anchorage include Saavedra Rock and Romero Rock.

text: Rocks in the anchorage include

text: Saavedra Rock

text: and

text: Romero Rock

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text: An alternative metaphor is the “crystallized self,” a notion that pulls from Laurel Richardson’s (2001) epistemological notion of "crystallization". The “crystallized self” is considered a positive term that helps people to experience and talk about the self in more appropriately politicized and layered ways. Tracy and Tretheway say:“The crystallized self is neither real nor fake…. The crystallized self is multidimensional; the more facets, the more beautiful and complex. Certainly crystals may feel solid, stable, and fixed. But just as crystals have differing forms, depending upon whether they grow rapidly or slowly, under constant or fluctuating conditions, or from highly variable or remarkably uniform fluids or gasses, crystallized selves have different shapes depending on the various discourses through which they are constructed and constrained” (Tracy & Trethewey, 2005, p. 186).Viewing the self as crystallized moves away from ideas of which parts of the self are more “authentic” and rather suggests that the self is constructed through context and communication. Multiple facets can be “real” and competing simultaneously.

text: An alternative metaphor is the “crystallized self,” a notion that pulls from Laurel Richardson’s (2001)

text: epistemological

text: notion of "crystallization". The “crystallized self” is considered a positive term that helps people to experience and talk about the self in more appropriately politicized and layered ways. Tracy and Tretheway say:“The crystallized self is neither real nor fake…. The crystallized self is multidimensional; the more facets, the more beautiful and complex. Certainly crystals may feel solid, stable, and fixed. But just as crystals have differing forms, depending upon whether they grow rapidly or slowly, under constant or fluctuating conditions, or from highly variable or remarkably uniform fluids or gasses, crystallized selves have different shapes depending on the various discourses through which they are constructed and constrained” (Tracy & Trethewey, 2005, p. 186).Viewing the self as crystallized moves away from ideas of which parts of the self are more “authentic” and rather suggests that the self is constructed through context and communication. Multiple facets can be “real” and competing simultaneously.

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text: The high mountain ranges produced by continental collisions are immediately subjected to the forces of erosion. Erosion wears down the mountains and massive piles of sediment are developed in adjacent ocean margins, shallow seas, and as continental deposits. As these sediment piles are buried deeper they become lithified into sedimentary rock. The metamorphic, igneous, and sedimentary rocks of the mountains become the new piles of sediments in the adjoining basins and eventually become sedimentary rock.

text: The high mountain ranges produced by continental collisions are immediately subjected to the forces of erosion. Erosion wears down the mountains and massive piles of sediment are developed in adjacent ocean margins, shallow seas, and as continental deposits. As these sediment piles are buried deeper they become lithified into sedimentary rock. The metamorphic, igneous, and sedimentary rocks of the mountains become the new piles of sediments in the adjoining basins and eventually become sedimentary rock.

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text: A solo show named Swimming Rocks which was on exhibit on June 27, 2014 at the Art Gallery of Kırmızı Ardıç Kuşu, Gallery Metazori in Çeşme, Alaçatı where Gülan spent most of his childhood is not only the name of the exhibition, but also one of the significant artworks in the exhibition, the Swimming Rocks are pumice typed rocks that can float on the sea and be found in Aegean Sea, especially in Çeşme and Alaçatı inspiring the artist in this process. Gülan made a sculpture, named Swimming Rocks from these and other stones; therefore this and some other sculptural pieces float on the sea and in the gallery. He made floating figurative, human-sized sculptures covered with stone. The artworks of Genco Gülan's mother, Tezer Gülan and his grandmother, Saime İzmiroğlu where also exhibited in the show. Genco Gülan had also a series called as “New Landscape” in this exhibition. This series being a conceptual/electronic interpretation of landscapes as barcodes dealing with questions, such as how the landscape pictures change in time, how different our landscapes became now and how the landscapes in the future will become. Gülan juxtaposed classical landscape paintings, barcodes and produced new pieces. Gülan also exhibited his new series; Digital Ghost in the show. The artist painted on large canvases; the non-existing images that appeared in his formatted laptop.

text: A solo show named Swimming Rocks which was on exhibit on June 27, 2014 at the Art Gallery of Kırmızı Ardıç Kuşu, Gallery Metazori in Çeşme, Alaçatı where Gülan spent most of his childhood is not only the name of the exhibition, but also one of the significant artworks in the exhibition, the Swimming Rocks are

text: pumice

text: typed rocks that can float on the sea and be found in

text: Aegean Sea

text: , especially in

text: Çeşme

text: and

text: Alaçatı

text: inspiring the artist in this process. Gülan made a sculpture, named Swimming Rocks from these and other stones; therefore this and some other sculptural pieces float on the sea and in the gallery. He made floating figurative, human-sized sculptures covered with stone. The artworks of Genco Gülan's mother, Tezer Gülan and his grandmother, Saime İzmiroğlu where also exhibited in the show. Genco Gülan had also a series called as “New Landscape” in this exhibition. This series being a conceptual/electronic interpretation of landscapes as barcodes dealing with questions, such as how the landscape pictures change in time, how different our landscapes became now and how the landscapes in the future will become. Gülan juxtaposed classical landscape paintings, barcodes and produced new pieces. Gülan also exhibited his new series; Digital Ghost in the show. The artist painted on large canvases; the non-existing images that appeared in his formatted laptop.

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answers: Gülan juxtaposed classical landscape paintings, barcodes and produced new pieces

answer: No

answer: No

answer: No

answer: No

answer: No

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text: Modern geology acknowledges many different forms of rock formation, and explains the formation of sedimentary rock through processes very similar to those described by neptunism.

text: Modern geology acknowledges many different forms of rock formation, and explains the formation of

text: sedimentary rock

text: through processes very similar to those described by neptunism.

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answers: Many different forms of rock formation

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text: A long thin sand and gravel spit named "Elephant Spit" extends for about  to the Southern Ocean from the eastern end of the island. From Big Ben, rock buttresses of exposed rock descending in a radial pattern have been created due to erosion of the volcanic formations. Glaciers have carried the eroded sediment to the downstream end of the island and formed the low land of the Nullarbor (gravel isthmus) between the two volcanoes, and further to the east in the Elephant Spit. The end of this spit is called "Spit Point", and the bay to the north is named "Spit Bay". To the southwest of this spit on the southeast coast of the island is the Winston Lagoon. Cape Gazert, on the northwestern coast of the island, is just to the south of South West Bay, a bay which lies between Cape Gazert and the peninsula on the northwestern tip of Heard Island, the Laurens Peninsula. This peninsula contains the Anzac peak at , with Red Island on the very northern tip of the island and peninsula. Immediately to the east of the peninsula along the northern coast is Atlas Cove, a small peninsula in turn separates it from Corinthian Bay, further to the east.

text: A long thin sand and gravel

text: spit

text: named "

text: Elephant Spit

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answers: Elephant Spit

answer: No

answer: No

answer: No

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answer: 1

text: The Belomorian Belt is a tectonic pile of metasedimentary, metavolcanic and metaplutonic rocks which has been folded and metamorphosed several times. According to a study by Bibikova et al. (1999), the earliest metamorphic event took place ca. 2.8 Ga. "Sm-Nd isotope studies of whole rock metasediment samples have constrained their mean protolith ages to between 3.00 and 2.86 Ga, indicating a short prehistory....Zircons were separated from different localities and at various levels of the Belomorian tectonostratigraphical column. We have recognized three age groups of ancient cores at 3.2–3.1 Ga, 3.00–2.97 Ga and 2.93–2.90 Ga. The plus 3.1 Ga cores were obtained solely from localities in the northern part of the Belt. It has also been possible to distinguish three groups of metamorphic grains and overgrowths which are 2.84–2.80 Ga, 2.72–2.68 Ga and ca. 2.61 Ga old. The data presented confirm the absence of detrital material older than 3.2 Ga in the Belomorian metasediments. This differs from the adjacent Karelian craton where crustal rocks of about 3.4 Ga have been recorded. If these ages are representative of the rocks discussed, our data suggest that the Belomorian Belt represents a Neoarchaean accretionary environment in the vicinity of the Karelian craton." (Bibikova et al., 1999).

text: The Belomorian Belt is a tectonic pile of meta

text: sedimentary

text: , metavolcanic and meta

text: plutonic

text: rocks which has been folded and metamorphosed several times. According to a study by Bibikova et al. (1999), the earliest metamorphic event took place ca. 2.8 Ga. "

text: Sm-Nd

text: isotope

text: studies of whole rock metasediment samples have constrained their mean

text: protolith

text: ages to between 3.00 and 2.86 Ga, indicating a short prehistory....

text: Zircons

text: were separated from different localities and at various levels of the Belomorian

text: tectonostratigraphical

text: column. We have recognized three age groups of ancient cores at 3.2–3.1 Ga, 3.00–2.97 Ga and 2.93–2.90 Ga. The plus 3.1 Ga cores were obtained solely from localities in the northern part of the Belt. It has also been possible to distinguish three groups of

text: metamorphic

text: grains and overgrowths which are 2.84–2.80 Ga, 2.72–2.68 Ga and ca. 2.61 Ga old. The data presented confirm the absence of detrital material older than 3.2 Ga in the Belomorian metasediments. This differs from the adjacent

text: Karelian craton

text: where crustal rocks of about 3.4 Ga have been recorded. If these ages are representative of the rocks discussed, our data suggest that the Belomorian Belt represents a Neoarchaean

text: accretionary

text: environment in the vicinity of the Karelian craton." (Bibikova et al., 1999).

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text: The definition of LIP has been expanded and refined, and is still a work in progress. LIP is now frequently also used to describe voluminous areas of, not just mafic, but all types of igneous rocks. Sub-categorization of LIPs into large volcanic provinces (LVP) and large plutonic provinces (LPP), and including rocks produced by normal plate tectonic processes, has been proposed.

text: The definition of LIP has been expanded and refined, and is still a work in progress. LIP is now frequently also used to describe voluminous areas of, not just mafic, but all types of igneous rocks. Sub-categorization of LIPs into large volcanic provinces (LVP) and large plutonic provinces (LPP), and including rocks produced by normal plate tectonic processes, has been proposed.

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answers: all types of igneous rocks

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answers: large volcanic provinces (LVP) and large plutonic provinces (LPP)

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answers: plate tectonic processes

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answers: Sub-categorization

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text: Ultra high-pressure metamorphism refers to metamorphic processes at pressures high enough to stabilize coesite, the high-pressure polymorph of SiO. It is important because the processes that form and exhume ultra high-pressure (UHP) metamorphic rocks may strongly affect plate tectonics, the composition and evolution of Earth's crust. The discovery of UHP metamorphic rocks in 1984 revolutionized our understanding of plate tectonics. Prior to 1984 there was little suspicion that continental rocks could reach such high pressures.

text: Ultra high-pressure metamorphism refers to

text: metamorphic

text: processes at pressures high enough to stabilize

text: coesite

text: , the high-pressure

text: polymorph

text: of SiO. It is important because the processes that form and exhume ultra high-pressure (UHP) metamorphic rocks may strongly affect

text: plate tectonics

text: , the composition and evolution of Earth's crust. The discovery of UHP metamorphic rocks in 1984 revolutionized our understanding of plate tectonics. Prior to 1984 there was little suspicion that continental rocks could reach such high pressures.

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answer: No

answer: No

answer: No

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text: Sedimentology encompasses the study of modern sediments such as sand, silt, and clay, and the processes that result in their formation (erosion and weathering), transport,  deposition and diagenesis. Sedimentologists apply their understanding of modern processes to interpret geologic history through observations of sedimentary rocks and sedimentary structures.

text: Sedimentology encompasses the study of modern

text: sediment

text: s such as

text: sand

text: silt

text: , and

text: clay

text: , and the processes that result in their formation (

text: erosion

text: and

text: weathering

text: transport

text: deposition

text: and

text: diagenesis

text: . Sedimentologists apply their understanding of modern processes to interpret geologic history through observations of

text: sedimentary rocks

text: and

text: sedimentary structures

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answer: Yes

answer: Yes

answer: No

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answer: 1

text: THEMIS found a wide range of igneous rocks and minerals.  Some of the rocks were low-silica basalts, high silica dacite, olivine basalts ultramafic (picratic) basalts, and quartz-bearning granitoid rocks.   The olivine basalts were present in a variety of locations, such as on crater floors and in some canyon wall layers.  The mineral olivine is important because it is common in more primitive magmas from the mantle and it weathers quickly when mositure is present.  So if olivine is present, the climate must have been dry since the time that olivine was exposed.  Quartz-bearing rocks were found in the central uplifts in craters.  Rocks in the central uplifts were probably once buried several kilometers beneath the surface, but raised by the impact process.  Rocks of dacite composition show that within magma chambers frational crystallization occurred.   In this process, some minerals form crystals, then settle to the bottom of the chamber.  Having a variety of rocks increases the chances that some useful/valuable minerals may be found on Mars.

text: THEMIS found a wide range of igneous rocks and minerals.  Some of the rocks were low-silica

text: basalts

text: , high silica

text: dacite

text: olivine

text: basalts ultramafic (picratic) basalts, and quartz-bearning granitoid rocks.   The olivine basalts were present in a variety of locations, such as on crater floors and in some canyon wall layers.  The mineral olivine is important because it is common in more primitive

text: magma

text: s from the

text: mantle

text: and it weathers quickly when mositure is present.  So if olivine is present, the climate must have been dry since the time that olivine was exposed.

text: Quartz

text: -bearing rocks were found in the central uplifts in craters.  Rocks in the central uplifts were probably once buried several kilometers beneath the surface, but raised by the impact process.  Rocks of dacite composition show that within magma chambers frational crystallization occurred.   In this process, some minerals form crystals, then settle to the bottom of the chamber.  Having a variety of rocks increases the chances that some useful/valuable minerals may be found on Mars.

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answers: Rocks of dacite composition

answers: NDQ_005762

answers: intrusive

answers: NDQ_005763

answers: climate

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answers: composition

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answers: NDQ_005768

answers: frational crystallization

answers: NDQ_005769

answers: crystallization

answers: NDQ_005770

answers: frational crystallization

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Its geology features intrusive igneous rock formations, such as gabbro, combined with metamorphic minerals such as serpentine.

text: Its

text: geology

text: features intrusive

text: igneous rock

text: formations, such as

text: gabbro

text: , combined with

text: metamorphic

text: mineral

text: s such as

text: serpentine

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answers: Yes

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answers: slower cooling forms smaller crystals

answers: NDQ_005769

answers: metamorphic

answers: NDQ_005770

answers: metamorphic minerals

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The rock types Collins worked on are mainly granitoids, gneisses, augen gneisses, mylonites and metasedimentary rocks.

text: The rock types Collins worked on are mainly

text: granitoid

text: s,

text: gneiss

text: es,

text: augen gneiss

text: es,

text: mylonite

text: s and

text: metasedimentary rocks

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answer: No

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text: In a simplified classification, igneous rock types are separated on the basis of the type of feldspar present, the presence or absence of quartz, and in rocks with no feldspar or quartz, the type of iron or magnesium minerals present. Rocks containing quartz (silica in composition) are silica-oversaturated. Rocks with feldspathoids are silica-undersaturated, because feldspathoids cannot coexist in a stable association with quartz.

text: In a simplified classification, igneous rock types are separated on the basis of the type of feldspar present, the presence or absence of

text: quartz

text: , and in rocks with no feldspar or quartz, the type of iron or magnesium minerals present. Rocks containing quartz (silica in composition) are silica-oversaturated. Rocks with

text: feldspathoid

text: s are silica-undersaturated, because feldspathoids cannot coexist in a stable association with quartz.

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answers: igneous rock types

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answers: Rocks with feldspathoids are silica-undersaturated

answer: No

answer: No

answer: No

answer: No

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answer: 1

text: The change in the particle size of the rock during the process of metamorphism is called recrystallization. For instance, the small calcite crystals in the sedimentary rock limestone and chalk change into larger crystals in the metamorphic rock marble, or in metamorphosed sandstone, recrystallization of the original quartz sand grains results in very compact quartzite, also known as metaquartzite, in which the often larger quartz crystals are interlocked. Both high temperatures and pressures contribute to recrystallization. High temperatures allow the atoms and ions in solid crystals to migrate, thus reorganizing the crystals, while high pressures cause solution of the crystals within the rock at their point of contact.

text: The change in the particle size of the rock during the process of metamorphism is called

text: recrystallization

text: . For instance, the small

text: calcite

text: crystals in the sedimentary rock

text: limestone

text: and

text: chalk

text: change into larger crystals in the metamorphic rock

text: marble

text: , or in metamorphosed sandstone, recrystallization of the original quartz sand grains results in very compact quartzite, also known as metaquartzite, in which the often larger quartz crystals are interlocked. Both high temperatures and pressures contribute to recrystallization. High temperatures allow the

text: atom

text: s and

text: ion

text: s in solid crystals to migrate, thus reorganizing the crystals, while high pressures cause solution of the crystals within the rock at their point of contact.

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answers: Yes

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answers: sedimentary

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answers: Both high temperatures and pressures

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answers: particle size

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answers: calcite crystals

answers: NDQ_005769

answers: recrystallization

answers: NDQ_005770

answers: metamorphism

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: There are no rocks on Mt. Everts from 65 to 2.1 million years ago. The absence of rocks is called an unconformity. During this period few or no rocks were deposited, and erosion carried away any sediments that were deposited.

text: There are no rocks on Mt. Everts from 65 to 2.1 million years ago. The absence of rocks is called an unconformity. During this period few or no rocks were deposited, and erosion carried away any sediments that were deposited.

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answers: Yes

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answers: faster cooling forms smaller crystals

answers: NDQ_005769

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answers: unconformity

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: In a lab, this is often done by placing the material in a freeze-drying flask and rotating the flask in a bath, called a shell freezer, which is cooled by mechanical refrigeration, dry ice in aqueous methanol, or liquid nitrogen. On a larger scale, freezing is usually done using a freeze-drying machine. In this step, it is important to cool the material below its triple point, the lowest temperature at which the solid and liquid phases of the material can coexist. This ensures that sublimation rather than melting will occur in the following steps. Larger crystals are easier to freeze-dry. To produce larger crystals, the product should be frozen slowly or can be cycled up and down in temperature. This cycling process is called annealing. However, in the case of food, or objects with formerly-living cells, large ice crystals will break the cell walls (a problem discovered, and solved, by Clarence Birdseye), resulting in the destruction of more cells, which can result in increasingly poor texture and nutritive content. In this case, the freezing is done rapidly, in order to lower the material to below its eutectic point quickly, thus avoiding the formation of ice crystals. Usually, the freezing temperatures are between −50 °C and −80 °C (-58 °F and -112 °F) . The freezing phase is the most critical in the whole freeze-drying process, because the product can be spoiled if improperly done.

text: In a lab, this is often done by placing the material in a freeze-drying flask and rotating the flask in a bath, called a shell freezer, which is cooled by mechanical refrigeration,

text: dry ice

text: in aqueous

text: methanol

text: , or

text: liquid nitrogen

text: . On a larger scale, freezing is usually done using a freeze-drying machine. In this step, it is important to cool the material below its

text: triple point

text: , the lowest temperature at which the solid and liquid phases of the material can coexist. This ensures that sublimation rather than melting will occur in the following steps. Larger crystals are easier to freeze-dry. To produce larger crystals, the product should be frozen slowly or can be cycled up and down in temperature. This cycling process is called

text: annealing

text: . However, in the case of food, or objects with formerly-living cells, large ice crystals will break the cell walls (a problem discovered, and solved, by

text: Clarence Birdseye

text: ), resulting in the destruction of more cells, which can result in increasingly poor texture and nutritive content. In this case, the freezing is done rapidly, in order to lower the material to below its

text: eutectic point

text: quickly, thus avoiding the formation of ice crystals. Usually, the freezing temperatures are between −50 °C and −80 °C (-58 °F and -112 °F) . The freezing phase is the most critical in the whole freeze-drying process, because the product can be spoiled if improperly done.

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answers: This ensures that sublimation rather than melting will occur in the following steps

answers: NDQ_005762

answers: In this step, it is important to cool the material below its triple point

answers: NDQ_005763

answers: Larger crystals

answers: NDQ_005764

answers: texture

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answers: annealing

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answers: larger crystals are easier to freeze-dry

answers: NDQ_005769

answers: sublimation

answers: NDQ_005770

answers: This ensures that sublimation rather than melting will occur in the following steps

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: 23. Metamorphic Rock ()

text: 23. Metamorphic Rock ()

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answers: All rocks are part of the rock cycle.

answers: NDQ_005762

answers: metamorphic

answers: NDQ_005763

answers: magma

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answers: metamorphic

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answers: Metamorphic

answers: NDQ_005768

answers: slower cooling forms smaller crystals

answers: NDQ_005769

answers: metamorphic rock

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answers: Metamorphic Rock

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: <br>The T age of a rock, can yield a formation age for the crust as a whole if the sample has not suffered disturbance after its formation. Since Sm/Nd are rare-earth elements (REE), their characterisity enables theitic immobilr ratios to resist partitioning during metamorphism and melting of silicate rocks. This therefore allows for crustal formation ages to be calculated, despite any metamorphism the sample has undergone.

text: <br>The T age of a rock, can yield a formation age for the crust as a whole if the sample has not suffered disturbance after its formation. Since Sm/Nd are rare-earth elements (REE), their characterisity enables theitic immobilr ratios to resist partitioning during metamorphism and melting of silicate rocks. This therefore allows for crustal formation ages to be calculated, despite any metamorphism the sample has undergone.

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answers: Yes

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answers: rare-earth elements

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answers: formation age

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answers: Sm/Nd

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answers: metamorphism

answer: No

answer: No

answer: No

answer: No

answer: No

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text: The geology of Angola includes large areas of Precambrian age rocks. The west of the country is characterized by meta-sedimentary rocks of Proterozoic age including tillites assigned to the Bembe System. Overlying these are a thick pile of limestones and other marine sediments laid down during the Mesozoic and Cenozoic eras.  Amidst the Proterozoic sequence are areas of crystalline basement dating from the Archaean. More Archaean basement rocks form the Kasai Craton in northeastern Angola. In the north, within the Cassanje Graben are clastic sediments and volcanic rocks of the Karoo Supergroup. Kimberlites and carbonatites resulting from magmatic activity during the Karoo period are found along a northeast-southwest line through the country. Continental sediments of the Kalahari Group are widespread in eastern Angola.

text: The geology of Angola includes large areas of

text: Precambrian

text: age rocks. The west of the country is characterized by meta-sedimentary rocks of

text: Proterozoic

text: age including

text: tillite

text: s assigned to the Bembe System. Overlying these are a thick pile of

text: limestone

text: s and other marine sediments laid down during the

text: Mesozoic

text: and

text: Cenozoic

text: eras.  Amidst the Proterozoic sequence are areas of crystalline

text: basement

text: dating from the

text: Archaean

text: . More Archaean basement rocks form the

text: Kasai Craton

text: in northeastern

text: Angola

text: . In the north, within the Cassanje Graben are

text: clastic

text: sediments and

text: volcanic rock

text: s of the

text: Karoo Supergroup

text: Kimberlite

text: s and

text: carbonatite

text: s resulting from

text: magmatic activity

text: during the Karoo period are found along a northeast-southwest line through the country. Continental sediments of the

text: Kalahari Group

text: are widespread in eastern Angola.

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answers: Precambrian age rocks

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answers: sedimentary

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answers: Karoo period

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answers: age

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answers: magmatic activity

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answers: volcanic

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answers: faster cooling forms smaller crystals

answers: NDQ_005769

answers: tillites

answers: NDQ_005770

answers: Precambrian age rocks

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Sedimentary rocks contain important information about the history of the Earth. They contain fossils, the preserved remains of ancient plants and animals. Coal is considered a type of sedimentary rock. The composition of sediments provides us with clues as to the original rock. Differences between successive layers indicate changes to the environment over time. Sedimentary rocks can contain fossils because, unlike most igneous and metamorphic rocks, they form at temperatures and pressures that do not destroy fossil remains.

text: Sedimentary rocks contain important information about the

text: history of the Earth

text: . They contain

text: fossil

text: s, the preserved remains of ancient

text: plant

text: s and

text: animal

text: s. Coal is considered a type of sedimentary rock. The composition of sediments provides us with clues as to the original rock. Differences between successive layers indicate changes to the environment over time. Sedimentary rocks can contain fossils because, unlike most igneous and metamorphic rocks, they form at temperatures and pressures that do not destroy fossil remains.

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answers: composition

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answers: Sedimentary rocks can contain fossils

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answers: fossils

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answers: Metamorphic rocks

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Hydraulic action is erosion that occurs when the motion of water against a rock surface produces mechanical weathering. Most generally, it is the ability of moving water (flowing or waves) to dislodge and transport rock particles.  Within this rubric are a number of specific erosional processes, including abrasion, attrition, corrasion, saltation, and scouring (downcutting).  Hydraulic action is distinguished from other types of water facilitated erosion, such as static erosion where water leaches salts and floats off organic material from unconsolidated sediments, and from chemical erosion more often called chemical weathering.It is a mechanical process, in which the moving water current flows against the banks and bed of a river, thereby removing rock particles.

text: Hydraulic action is erosion that occurs when the motion of water against a rock surface produces mechanical weathering. Most generally, it is the ability of moving water (flowing or waves) to dislodge and transport rock particles.  Within this

text: rubric

text: are a number of specific erosional processes, including

text: abrasion

text: , attrition,

text: corrasion

text: , saltation, and scouring (

text: downcutting

text: ).  Hydraulic action is distinguished from other types of water facilitated erosion, such as static erosion where water leaches salts and floats off organic material from unconsolidated sediments, and from chemical erosion more often called

text: chemical weathering

text: .It is a mechanical process, in which the moving water current flows against the banks and bed of a river, thereby removing rock particles.

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answers: Saltation

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answers: saltation

answers: NDQ_005770

answers: Hydraulic action

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Titanium in zircon geothermometry can be used in zircons found in metamorphic rocks to estimate the pressure and temperatures conditions during metamorphism. This helps identify the metamorphic facies and thus the geologic setting of a rock formation. It can also be used in sedimentary rocks to help determine the source of detrital minerals. However, these crystals may sometimes be contaminated by external titanium seeping into fractures.

text: Titanium in zircon geothermometry can be used in zircons found in

text: metamorphic rock

text: s to estimate the pressure and temperatures conditions during metamorphism. This helps identify the

text: metamorphic facies

text: and thus the geologic setting of a rock formation. It can also be used in

text: sedimentary rock

text: s to help determine the source of detrital minerals. However, these crystals may sometimes be contaminated by external titanium seeping into fractures.

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answer: No

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text: Easily identified by its red-green color (sometimes dark blue) and furrowed, twisted appearance, the assemblage is usually characterized as being primarily metamorphic in nature, its most well-known rocks being serpentine schists. However, the assemblage contains a wide range of different rocks in different stages of the rock cycle. A single outcrop may contain basalt, chert, and other rocks in addition to schist.

text: Easily identified by its red-green color (sometimes dark blue) and furrowed, twisted appearance, the assemblage is usually characterized as being primarily metamorphic in nature, its most well-known rocks being

text: serpentine

text: schist

text: s. However, the assemblage contains a wide range of different rocks in different stages of the rock cycle. A single outcrop may contain basalt, chert, and other rocks in addition to schist.

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answers: stages of the rock cycle

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answers: metamorphic

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answers: faster cooling forms smaller crystals

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answers: stage of the rock cycle

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: 1

text: Three conditions must be present for oil reservoirs to form: a source rock rich in hydrocarbon material buried deep enough for subterranean heat to cook it into oil, a porous and permeable reservoir rock for it to accumulate in, and a cap rock (seal) or other mechanism that prevents it from escaping to the surface. Within these reservoirs, fluids will typically organize themselves like a three-layer cake with a layer of water below the oil layer and a layer of gas above it, although the different layers vary in size between reservoirs. Because most hydrocarbons are less dense than rock or water, they often migrate upward through adjacent rock layers until either reaching the surface or becoming trapped within porous rocks (known as reservoirs) by impermeable rocks above. However, the process is influenced by underground water flows, causing oil to migrate hundreds of kilometres horizontally or even short distances downward before becoming trapped in a reservoir. When hydrocarbons are concentrated in a trap, an oil field forms, from which the liquid can be extracted by drilling and pumping.

text: Three conditions must be present for oil reservoirs to form: a

text: source rock

text: rich in hydrocarbon material buried deep enough for subterranean heat to cook it into oil, a

text: porous

text: and

text: permeable

text: reservoir rock for it to accumulate in, and a cap rock (seal) or other mechanism that prevents it from escaping to the surface. Within these reservoirs, fluids will typically organize themselves like a three-layer cake with a layer of water below the oil layer and a layer of gas above it, although the different layers vary in size between reservoirs. Because most hydrocarbons are less dense than rock or water, they often migrate upward through adjacent rock layers until either reaching the surface or becoming trapped within porous rocks (known as

text: reservoirs

text: ) by impermeable rocks above. However, the process is influenced by underground water flows, causing oil to migrate hundreds of kilometres horizontally or even short distances downward before becoming trapped in a reservoir. When hydrocarbons are concentrated in a trap, an

text: oil field

text: forms, from which the liquid can be extracted by

text: drill

text: ing and

text: pump

text: ing.

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answers: Yes

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answers: sedimentary

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answers: source rock rich in hydrocarbon

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answers: hydrocarbons are less dense than rock or water, they often migrate upward through adjacent rock layers

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answers: oil

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answers: slower cooling forms smaller crystals

answers: NDQ_005769

answers: escaping

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answers: An oil field

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Sediment is transported along the coast in the direction of the prevailing current (longshore drift). When the upcurrent amount of sediment is less than the amount being carried away, erosion occurs. When the upcurrent amount of sediment is greater, sand or gravel banks will tend to form as a result of deposition. These banks may slowly migrate along the coast in the direction of the longshore drift, alternately protecting and exposing parts of the coastline. Where there is a bend in the coastline, quite often a buildup of eroded material occurs forming a long narrow bank (a spit). Armoured beaches and submerged offshore sandbanks may also protect parts of a coastline from erosion. Over the years, as the shoals gradually shift, the erosion may be redirected to attack different parts of the shore.

text: Sediment

text: is transported along the coast in the direction of the prevailing current (

text: longshore drift

text: ). When the upcurrent amount of sediment is less than the amount being carried away, erosion occurs. When the upcurrent amount of sediment is greater, sand or gravel banks will tend to form as a result of

text: deposition

text: . These banks may slowly migrate along the coast in the direction of the longshore drift, alternately protecting and exposing parts of the coastline. Where there is a bend in the coastline, quite often a buildup of eroded material occurs forming a long narrow bank (a

text: spit

text: Armoured

text: beaches and submerged offshore

text: sandbanks

text: may also protect parts of a coastline from erosion. Over the years, as the shoals gradually shift, the erosion may be redirected to attack different parts of the shore.

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answers: Yes

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answers: sedimentary

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answers: upcurrent amount of sediment

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answers: igneous

answers: NDQ_005765

answers: erosion

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answers: sand

answers: NDQ_005768

answers: faster cooling forms smaller crystals

answers: NDQ_005769

answers: erosion

answers: NDQ_005770

answers: Sediment is transported along the coast in the direction of the prevailing current

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: This zone extends from Bandar Abbas in the south to Kermanshah in the northwest and continues through to Iraq. Zagros is in fact the northeastern edge of the Arabian plate. Some important features of Zagros include: Absence of magmatic and metamorphic events after Triassic, and low abundance of the outcrops of Paleozoic rocks. Structurally, it consists of large anticlines and small synclines and continuous marine sedimentation from the Carboniferous to the Miocene. On the whole, a sequence of Precambrian to Pliocene rocks about 8-10 kilometres in thickness has undergone folding from the Miocene to the Recent time in the Zagros Mountains. The Zagros fold and thrust belt was formed by the collision of two tectonic plates — the Iranian Plate and the Arabian Plate. This collision primarily happened during the Miocene and folded the entire rocks that had been deposited from the Carboniferous to the Miocene in the geosyncline in front of the Iranian Plate. The process of collision continues to the present and as the Arabian Plate is being pushed against the Iranian Plate, the Zagros Mountains and the Iranian Plateau are getting higher and higher. The Zagros mountain range, itself, has a totally sedimentary origin and is made primarily of limestone. In the Elevated Zagros or the Higher Zagros, the Paleozoic rocks could be found mainly in the upper and higher sections of the peaks of the Zagros Mountains along the Zagros main fault. On the both sides of this fault, there are Mesozoic rocks, a combination of Triassic and Jurassic rocks that are surrounded by Cretaceous rocks on the both sides. The Folded Zagros (the mountains south of the Elevated Zagros and almost parallel to the main Zagros fault) is formed mainly of Tertiary rocks, with the Paleogene rocks south of the Cretaceous rocks and then the Neogene rocks south of the Paleogene rocks.

text: This zone extends from

text: Bandar Abbas

text: in the south to

text: Kermanshah

text: in the northwest and continues through to

text: Iraq

text: . Zagros is in fact the northeastern edge of the Arabian plate. Some important features of Zagros include: Absence of magmatic and metamorphic events after Triassic, and low abundance of the outcrops of

text: Paleozoic

text: rocks. Structurally, it consists of large

text: anticline

text: s and small

text: syncline

text: s and continuous marine sedimentation from the

text: Carboniferous

text: to the

text: Miocene

text: . On the whole, a sequence of

text: Precambrian

text: to

text: Pliocene

text: rocks about 8-10 kilometres in thickness has undergone folding from the Miocene to the

text: Recent

text: time in the

text: Zagros Mountains

text: . The Zagros fold and thrust belt was formed by the collision of two tectonic plates — the

text: Iranian Plate

text: and the

text: Arabian Plate

text: . This collision primarily happened during the Miocene and folded the entire rocks that had been deposited from the Carboniferous to the Miocene in the

text: geosyncline

text: in front of the Iranian Plate. The process of collision continues to the present and as the Arabian Plate is being pushed against the Iranian Plate, the Zagros Mountains and the

text: Iranian Plateau

text: are getting higher and higher. The Zagros mountain range, itself, has a totally sedimentary origin and is made primarily of

text: limestone

text: . In the Elevated Zagros or the Higher Zagros, the Paleozoic rocks could be found mainly in the upper and higher sections of the peaks of the Zagros Mountains along the Zagros main fault. On the both sides of this fault, there are

text: Mesozoic

text: rocks, a combination of

text: Triassic

text: and

text: Jurassic

text: rocks that are surrounded by

text: Cretaceous

text: rocks on the both sides. The Folded Zagros (the mountains south of the Elevated Zagros and almost parallel to the main Zagros fault) is formed mainly of

text: Tertiary

text: rocks, with the

text: Paleogene

text: rocks south of the Cretaceous rocks and then the

text: Neogene

text: rocks south of the Paleogene rocks.

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answers: Tertiary rocks

answers: NDQ_005762

answers: Paleogene rocks

answers: NDQ_005763

answers: lack of magmatic and metamorphic events after Triassic

answers: NDQ_005764

answers: Abundance

answers: NDQ_005765

answers: metamorphic

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answers: Tertiary

answers: NDQ_005768

answers: Cretaceous rocks

answers: NDQ_005769

answers: metamorphic

answers: NDQ_005770

answers: Paleozoic rocks

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Detrital zircons usually retain similar properties as their parent igneous rocks, such as age, rough size and mineral chemistry. However, the composition of detrital zircons is not entirely controlled by the crystallization of the zircon mineral. In fact, many of them are modified by later processes in the sedimentary cycle. Depending on the degree of physical sorting, mechanical abrasion and dissolution, a detrital zircon grain may lose some of its inherent features and gain some over-printed properties like rounded shape and smaller size.  On a larger scale, two or more tribes of detrital zircons from different origins may deposit within the same sedimentary basin. This give rise to a natural complexity of associating detrital zircon populations and their sources.

text: Detrital zircons usually retain similar properties as their parent

text: igneous rock

text: s, such as age, rough size and mineral chemistry. However, the composition of detrital zircons is not entirely controlled by the crystallization of the zircon mineral. In fact, many of them are modified by later processes in the sedimentary cycle. Depending on the degree of physical

text: sorting

text: , mechanical

text: abrasion

text: and dissolution, a detrital zircon grain may lose some of its inherent features and gain some over-printed properties like

text: rounded shape

text: and smaller size.  On a larger scale, two or more tribes of detrital zircons from different origins may deposit within the same

text: sedimentary basin

text: . This give rise to a natural complexity of associating detrital zircon populations and their sources.

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answers: Yes

answers: NDQ_005762

answers: sedimentary

answers: NDQ_005763

answers: age, rough size and mineral chemistry

answers: NDQ_005764

answers: age

answers: NDQ_005765

answers: crystallization

answers: NDQ_005766

answers: igneous

answers: NDQ_005768

answers: a detrital zircon grain

answers: NDQ_005769

answers: dissolution

answers: NDQ_005770

answers: Detrital zircons

answer: No

answer: No

answer: Yes

answer: No

answer: No

answer: 1

text: Volcanic rock (often shortened to volcanics in scientific contexts) is a rock formed from magma erupted from a volcano. In other words, it differs from other igneous rock by being of volcanic origin. Like all rock types, the concept of volcanic rock is artificial, and in nature volcanic rocks grade into hypabyssal and metamorphic rocks and constitute an important element of some sediments and sedimentary rocks. For these reasons, in geology, volcanics and shallow hypabyssal rocks are not always treated as distinct. In the context of Precambrian shield geology, the term "volcanic" is often applied to what are strictly metavolcanic rocks.

text: Volcanic rock (often shortened to volcanics in scientific contexts) is a rock formed from

text: magma

text: erupted from a

text: volcano

text: . In other words, it differs from other

text: igneous rock

text: by being of

text: volcanic

text: origin. Like all rock types, the concept of volcanic rock is artificial, and in nature volcanic rocks grade into

text: hypabyssal

text: and

text: metamorphic rock

text: s and constitute an important element of some

text: sediment

text: s and

text: sedimentary rock

text: s. For these reasons, in geology, volcanics and shallow hypabyssal rocks are not always treated as distinct. In the context of

text: Precambrian

text: shield

text: geology, the term "volcanic" is often applied to what are strictly

text: metavolcanic rock

text: s.

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answers: Like all rock types

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answers: faster cooling forms smaller crystals

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answers: metamorphic

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answers: In the context of Precambrian shield geology

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The 250-meter track is made of concrete with a 42.5 degree embankment in the corners and a 17 degree embankment on the front and back straights.The velodrome is part of the Rock Hill Outdoor Center. U.S. national track cycling championships will be held there in 2012 and 2013. The velodrome was designed by Ralph Schürmann, a cycling track architect from Münster, Germany.

text: The 250-meter track is made of concrete with a 42.5 degree embankment in the corners and a 17 degree embankment on the front and back straights.The

text: velodrome

text: is part of the Rock Hill Outdoor Center. U.S. national track cycling championships will be held there in 2012 and 2013. The velodrome was designed by Ralph Schürmann, a cycling track architect from

text: Münster

text: Germany

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answers: Yes

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text: In geology, a complex is a unit of rocks composed of rocks of two or three of the following rock types: metamorphic, igneous or sedimentary. Complexes are lithodemic units usually of regional extent.

text: In

text: geology

text: , a complex is a unit of rocks composed of rocks of two or three of the following rock types:

text: metamorphic

text: igneous

text: or

text: sedimentary

text: . Complexes are

text: lithodemic

text: units usually of regional extent.

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text: Crystallization is the (natural or artificial) process where a solid forms where the atoms or molecules are highly organized in a structure known as a crystal. Some of the ways which crystals form are through  precipitating from a solution, melting or more rarely deposition directly from a gas. Crystallization is also a chemical solid–liquid separation technique, in which mass transfer of a solute from the liquid solution to a pure solid crystalline phase occurs. In chemical engineering crystallization occurs in a crystallizer. Crystallization is therefore related to precipitation, although the result is not amorphous or disordered, but a crystal.

text: Crystallization is the (natural or artificial) process where a solid forms where the atoms or molecules are highly organized in a structure known as a

text: crystal

text: . Some of the ways which crystals form are through

text: precipitating

text: from a

text: solution

text: melting

text: or more rarely

text: deposition

text: directly from a

text: gas

text: . Crystallization is also a chemical solid–liquid separation technique, in which mass transfer of a solute from the liquid solution to a pure solid crystalline phase occurs. In

text: chemical engineering

text: crystallization occurs in a crystallizer. Crystallization is therefore related to precipitation, although the result is not amorphous or disordered, but a crystal.

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answer: No

answer: No

answer: No

answer: No

answer: No

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text: Sediments are moved by moving water and wind according to their particle size and state of compaction. Particles tend to settle and compact in still water.  Once compacted, they are more resistant to erosion.  Established vegetation (especially species with complex network root systems) will resist erosion by slowing the fluid flow at the surface layer.

text: Sediments are moved by moving water and wind according to their particle size and state of compaction. Particles tend to settle and compact in still water.  Once compacted, they are more resistant to erosion.  Established vegetation (especially species with complex network root systems) will resist erosion by slowing the fluid flow at the surface layer.

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answer: No

answer: No

answer: No

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text: In the Cenozoic (66 to 1.8 mya), the processes that raised the Peñalara massif and divided it into the blocks we find today began to work again. Erosion of the rocky massif filled the basins with sediment. Glacial action in the Quaternary (1.8 mya to present) finished shaping the Peñalara cirque and the walls of the mountainous axis. The cirques were covered by a mantle of ice up to 300 m thick. Later, the confluence of the rivers gave the final touch to the landscape. The dominant rock in the park is granite, which is very hard and erosion-resistant.

text: In the

text: Cenozoic

text: (66 to 1.8 mya), the processes that raised the Peñalara massif and divided it into the blocks we find today began to work again. Erosion of the rocky massif filled the basins with sediment. Glacial action in the

text: Quaternary

text: (1.8 mya to present) finished shaping the Peñalara cirque and the walls of the mountainous axis. The cirques were covered by a mantle of ice up to 300 m thick. Later, the confluence of the rivers gave the final touch to the landscape. The dominant rock in the park is

text: granite

text: , which is very hard and erosion-resistant.

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answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Not all solids are crystals. For example, when liquid water starts freezing, the phase change begins with small ice crystals that grow until they fuse, forming a polycrystalline structure. In the final block of ice, each of the small crystals (called "crystallites" or "grains") is a true crystal with a periodic arrangement of atoms, but the whole polycrystal does not have a periodic arrangement of atoms, because the periodic pattern is broken at the grain boundaries. Most macroscopic inorganic solids are polycrystalline, including almost all metals, ceramics, ice, rocks, etc. Solids that are neither crystalline nor polycrystalline, such as glass, are called amorphous solids, also called glassy, vitreous, or noncrystalline. These have no periodic order, even microscopically. There are distinct differences between crystalline solids and amorphous solids: most notably, the process of forming a glass does not release the latent heat of fusion, but forming a crystal does.

text: Not all solids are crystals. For example, when liquid water starts freezing, the phase change begins with small ice crystals that grow until they fuse, forming a

text: polycrystalline

text: structure. In the final block of ice, each of the small crystals (called "

text: crystallite

text: s" or "grains") is a true crystal with a periodic arrangement of atoms, but the whole polycrystal does not have a periodic arrangement of atoms, because the periodic pattern is broken at the

text: grain boundaries

text: . Most macroscopic

text: inorganic

text: solids are polycrystalline, including almost all

text: metal

text: s,

text: ceramic

text: s,

text: ice

text: rocks

text: , etc. Solids that are neither crystalline nor polycrystalline, such as

text: glass

text: , are called

text: amorphous solid

text: s, also called

text: glass

text: y, vitreous, or noncrystalline. These have no periodic order, even microscopically. There are distinct differences between crystalline solids and amorphous solids: most notably, the process of forming a glass does not release the

text: latent heat of fusion

text: , but forming a crystal does.

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answers: Yes

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answers: intrusive

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answers: crystalline structure

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answers: Most macroscopic inorganic solids

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answers: crystalline

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answers: When liquid water starts freezing

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answers: phase change

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answers: solids that are neither crystalline nor polycrystalline

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Volcanic pyroclastic rocks are formed by explosive eruption of lava and any rocks which are entrained within the eruptive column. This may include rocks plucked off the wall of the magma conduit, or physically picked up by the ensuing pyroclastic surge. Lavas, especially rhyolite and dacite flows, tend to form clastic volcanic rocks by a process known as autobrecciation. This occurs when the thick, nearly solid lava breaks up into blocks and these blocks are then reincorporated into the lava flow again and mixed in with the remaining liquid magma. The resulting breccia is uniform in rock type and chemical composition.

text: Volcanic

text: pyroclastic

text: rocks are formed by explosive eruption of

text: lava

text: and any rocks which are entrained within the eruptive column. This may include rocks plucked off the wall of the

text: magma

text: conduit, or physically picked up by the ensuing

text: pyroclastic surge

text: Lava

text: s, especially

text: rhyolite

text: and

text: dacite

text: flows, tend to form clastic volcanic rocks by a process known as autobrecciation. This occurs when the thick, nearly solid lava breaks up into blocks and these blocks are then reincorporated into the lava flow again and mixed in with the remaining liquid magma. The resulting breccia is uniform in rock type and chemical composition.

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answers: Rock type and chemical composition

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answers: extrusive

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answers: chemical composition

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answers: rock type

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answers: autobrecciation

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answers: pyroclastic

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answers: slower cooling forms smaller crystals

answers: NDQ_005769

answers: autobrecciation

answers: NDQ_005770

answers: Autobrecciation

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The Cadaqués migmatites formed under extreme pressure and temperatures: a partial melt. They are halfway between an igneous and metamorphic rock. The area also contains a lot of schist: a medium grade metamorphic rock that has been flattened into sheets. White blocks of pegmatite mark where molten rock was squeezed through the older metamorphics at the end of the orogeny or mountain building.

text: The Cadaqués migmatites formed under extreme pressure and temperatures: a partial melt. They are halfway between an igneous and metamorphic rock. The area also contains a lot of schist: a medium grade metamorphic rock that has been flattened into sheets. White blocks of pegmatite mark where molten rock was squeezed through the older metamorphics at the end of the orogeny or mountain building.

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answers: Yes

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answers: metamorphic

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answers: grade

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answers: pegmatite

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answer: No

answer: No

answer: No

answer: No

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text: Protoliths are non-metamorphic rocks and thus have no protoliths themselves. The non-metamorphic rocks fall into two classes: sedimentary rocks, formed from sediment, and igneous rocks, formed from magma. The source of the sediment of a sedimentary rock is termed its provenance.

text: Protoliths are non-metamorphic rocks and thus have no protoliths themselves. The non-metamorphic rocks fall into two classes:

text: sedimentary rock

text: s, formed from sediment, and

text: igneous rock

text: s, formed from

text: magma

text: . The source of the sediment of a sedimentary rock is termed its

text: provenance

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answers: formed from sediment

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text: The Puerto Edén Igneous and Metamorphic Complex is a large coherent but varied group of metamorphic and igneous rocks –in other words a geologic complex– that crops out in the Patagonian channels of Magallanes Region. At present the rocks of the complex include migmatites, plutonic rocks and high-grade metamorphic rocks. To the west the Puerto Edén Igneous and Metamorphic Complex bounds the South Patagonian Batholith.

text: The Puerto Edén Igneous and Metamorphic Complex is a large coherent but varied group of

text: metamorphic

text: and

text: igneous rock

text: s –in other words a

text: geologic complex

text: – that

text: crops out

text: in the

text: Patagonian channels

text: of

text: Magallanes Region

text: . At present the rocks of the complex include

text: migmatite

text: s,

text: plutonic rock

text: s and

text: high-grade

text: metamorphic rocks

text: . To the west the Puerto Edén Igneous and Metamorphic Complex bounds the

text: South Patagonian Batholith

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answer: No

answer: No

answer: No

answer: No

answer: No

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text: The most striking feature about Bilger's Rocks are the various openings, crawlspaces, passageways, and arches found throughout the outcrop. These minute fissures and larger gaps are primarily caused by jointing within the rocks. Joints are caused by tectonic, or mountain-building forces that move and stress rocks, causing them to fracture. The resulting cracks provide an inlet for water, which slowly dissolves the rocks and allows space for ice crystals to freeze and thaw during the seasonal cycles, further pushing the rocks apart. Eventually, plants and trees also grow up through crevasses in the rocks and can exert considerable pressure as they grow, forcing even larger gaps to form. Gravity and erosion work together to slowly level the landscape by breaking the rock into ever smaller pieces and transporting it away. The steady continental movement combined with relentless erosion and weathering over hundreds of millions of years has left the continually evolving "Rock City" that we can observe today.

text: The most striking feature about Bilger's Rocks are the various openings, crawlspaces, passageways, and arches found throughout the outcrop. These minute fissures and larger gaps are primarily caused by jointing within the rocks. Joints are caused by tectonic, or mountain-building forces that move and stress rocks, causing them to fracture. The resulting cracks provide an inlet for water, which slowly dissolves the rocks and allows space for

text: ice crystal

text: s to freeze and thaw during the seasonal cycles, further pushing the rocks apart. Eventually, plants and trees also grow up through crevasses in the rocks and can exert considerable pressure as they grow, forcing even larger gaps to form.

text: Gravity

text: and

text: erosion

text: work together to slowly level the landscape by breaking the rock into ever smaller pieces and transporting it away. The steady continental movement combined with relentless erosion and weathering over hundreds of millions of years has left the continually evolving "Rock City" that we can observe today.

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answer: Yes

answer: Yes

answer: No

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text: There is general agreement that most well-exposed and well-studied UHP terrains formed by the burial of crustal rocks during subduction. Continental margin subduction is well documented in the Dabie Shan where Sino–Korean craton passive-margin sedimentary and volcanic sequences are preserved, in the Arabian continental margin beneath the Samail ophiolite (in the Al Hajar Mountains, Oman), and in the Australian margin presently subducting beneath the Banda Arc. Sediment subduction occurs beneath volcanoplutonic arcs around the world and is recognized in the compositions of arc lavas. Intracontinental subduction may be underway beneath the Pamir and may have produced UHP rocks in Greenland. Subduction erosion also occurs beneath volcanoplutonic arcs around the world, carrying continental rocks to mantle depths at least locally. Both subducted sediment and crystalline rocks may rise through the mantle diapirically to form UHP terranes. Foundering of the gravitationally unstable portions of continental lithosphere locally carries quartzofeldspathic rocks into the mantle and may be ongoing beneath the Pamir. The specific processes by which UHP terrains were exhumed to Earth's surface appear to have been different in different locations.

text: There is general agreement that most well-exposed and well-studied UHP terrains formed by the burial of crustal rocks during

text: subduction

text: . Continental margin subduction is well documented in the

text: Dabie Shan

text: where

text: Sino–Korean craton

text: passive-margin sedimentary and volcanic sequences are preserved, in the Arabian continental margin beneath the Samail ophiolite (in the

text: Al Hajar Mountains

text: , Oman), and in the Australian margin presently subducting beneath the

text: Banda Arc

text: . Sediment subduction occurs beneath

text: volcanoplutonic arcs

text: around the world and is recognized in the compositions of arc lavas. Intracontinental subduction may be underway beneath the

text: Pamir

text: and may have produced UHP rocks in Greenland. Subduction erosion also occurs beneath volcanoplutonic arcs around the world, carrying continental rocks to mantle depths at least locally. Both subducted sediment and crystalline rocks may rise through the mantle

text: diapir

text: ically to form UHP terranes. Foundering of the gravitationally unstable portions of continental lithosphere locally carries

text: quartzofeldspathic

text: rocks into the mantle and may be ongoing beneath the Pamir. The specific processes by which UHP terrains were exhumed to Earth's surface appear to have been different in different locations.

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answers: Earth's surface appear to have been different in different locations

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answers: Subduction erosion

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answers: subducted sediment and crystalline rocks may rise through the mantle diapirically

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answers: Subduction

answer: No

answer: No

answer: No

answer: No

answer: No

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text: Once the blade had been heat treated, a sword would be ground with progressively finer abrasives, typically different types of rock. Some grinding rocks can range in the thousands of dollars today. They would polish and sharpen the sword until the desired finish was achieved. This process is long and tedious, but a good polisher was of great value to the swordsmith and was often paid well. After the sword was polished, the fine tip could be sharpened. The sharpness of a sword, and ability to keep that edge, is based on the angle of the edge and the width of the body of the sword. How long it can hold the edge is also dependent on the material used.

text: Once the blade had been heat treated, a sword would be ground with progressively finer abrasives, typically different types of rock. Some grinding rocks can range in the thousands of dollars today. They would polish and sharpen the sword until the desired finish was achieved. This process is long and tedious, but a good polisher was of great value to the swordsmith and was often paid well. After the sword was polished, the fine tip could be sharpened. The sharpness of a sword, and ability to keep that edge, is based on the angle of the edge and the width of the body of the sword. How long it can hold the edge is also dependent on the material used.

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answers: slower cooling forms smaller crystals

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answers: heat treatment

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answers: After the sword was polished, the fine tip could be sharpened

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Two types or habits of anatase crystals may be distinguished. The more common occurs as simple acute double pyramids with an indigo-blue to black color and steely luster.  Crystals of this kind are abundant at Le Bourg-d'Oisans in Dauphiné, where they are associated with rock-crystal, feldspar, and axinite in crevices in granite and mica-schist.  Similar crystals, but of microscopic size, are widely distributed in sedimentary rocks, such as sandstones, clays, and slates, from which they may be separated by washing away the lighter constituents of the powdered rock.

text: Two types or

text: habits

text: of anatase crystals may be distinguished. The more common occurs as simple acute double pyramids with an indigo-blue to black color and steely luster.  Crystals of this kind are abundant at

text: Le Bourg-d'Oisans

text: in

text: Dauphiné

text: , where they are associated with rock-crystal,

text: feldspar

text: , and

text: axinite

text: in crevices in

text: granite

text: and

text: mica

text: schist

text: .  Similar crystals, but of microscopic size, are widely distributed in

text: sedimentary rock

text: s, such as

text: sandstone

text: s,

text: clay

text: s, and

text: slate

text: s, from which they may be separated by washing away the lighter constituents of the powdered rock.

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answers: Yes

answers: NDQ_005762

answers: sedimentary

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answers: habits

answers: NDQ_005764

answers: color

answers: NDQ_005765

answers: washing away the lighter constituents

answers: NDQ_005766

answers: granite

answers: NDQ_005768

answers: microscopic size

answers: NDQ_005769

answers: Separation

answers: NDQ_005770

answers: It is out of the rock cycle

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Chrysoberyl forms as a result of pegmatitic processes. Melting in the Earth's crust produces relatively low-density molten magma which can rise upwards towards the surface. As the main magma body cools, water originally present in low concentrations became more concentrated in the molten rock because it could not be incorporated into the crystallization of solid minerals. The remnant magma thus becomes richer in water, and also in rare elements that similarly do not fit in the crystal structures of major rock-forming minerals. The water extends the temperature range downwards before the magma becomes completely solid, allowing concentration of rare elements to proceed so far that they produce their own distinctive minerals. The resulting rock is igneous in appearance but formed at a low temperature from a water-rich melt, with large crystals of the common minerals such as quartz and feldspar, but also with elevated concentrations of rare elements such as beryllium, lithium, or niobium, often forming their own minerals; this is called a pegmatite. The high water content of the magma made it possible for the crystals to grow quickly, so pegmatite crystals are often quite large, which increases the likelihood of gem specimens forming.

text: Chrysoberyl forms as a result of

text: pegmatitic

text: processes. Melting in the

text: Earth's crust

text: produces relatively low-density molten

text: magma

text: which can rise upwards towards the surface. As the main magma body cools, water originally present in low concentrations became more concentrated in the molten rock because it could not be incorporated into the

text: crystallization

text: of solid minerals. The remnant magma thus becomes richer in water, and also in rare elements that similarly do not fit in the crystal structures of major rock-forming minerals. The water extends the temperature range downwards before the magma becomes completely solid, allowing concentration of rare elements to proceed so far that they produce their own distinctive minerals. The resulting rock is igneous in appearance but formed at a low temperature from a water-rich melt, with large crystals of the common minerals such as

text: quartz

text: and

text: feldspar

text: , but also with elevated concentrations of rare elements such as beryllium,

text: lithium

text: , or

text: niobium

text: , often forming their own minerals; this is called a

text: pegmatite

text: . The high water content of the magma made it possible for the crystals to grow quickly, so pegmatite crystals are often quite large, which increases the likelihood of gem specimens forming.

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answers: 4

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answers: Yes

answers: NDQ_005762

answers: intrusive

answers: NDQ_005763

answers: high water content

answers: NDQ_005764

answers: appearance

answers: NDQ_005765

answers: Chrysoberyl forms as a result of pegmatitic processes

answers: NDQ_005766

answers: igneous

answers: NDQ_005768

answers: crystals to grow quickly

answers: NDQ_005769

answers: crystallization

answers: NDQ_005770

answers: pegmatite

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The different metamorphic facies are defined by the mineralogical composition of a rock. When the temperature or pressure in a rock body change, the rock can cross into a different facies and some minerals become stable while others become unstable or metastable. Whether minerals really react depends on the reaction kinetics, the activation energy of the reaction and how much fluid is present in the rock.

text: The different metamorphic facies are defined by the mineralogical composition of a rock. When the temperature or pressure in a rock body change, the rock can cross into a different facies and some minerals become

text: stable

text: while others become unstable or

text: metastable

text: . Whether minerals really react depends on the

text: reaction kinetics

text: , the

text: activation energy

text: of the reaction and how much

text: fluid

text: is present in the rock.

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answers: unstable

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answers: slower cooling forms smaller crystals

answers: NDQ_005769

answers: metamorphic

answers: NDQ_005770

answers: Metamorphic

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The rock of the Santa Lucias is dominated by granitic basement of the Salinian Block, between the San Andreas Fault and Sur-Nacimiento Fault.  The core of the Salinian block formed as part of the same batholith which forms the core of the Sierra Nevada Mountains and the Peninsular Ranges of Baja California.  It was separated from the North American Plate and transported north by the action of the San Andreas Fault from an original position.  It is predominantly Mesozoic granitic and pre-Cretaceous metamorphic rocks.  There is some Cretaceous sedimentary rock of the Great Valley Sequence, considerable Miocene marine sediments, and some other Cenozoic sediments.  Units west of the Sur-Nacimiento Fault are dominated by rocks of the Franciscan Assemblage.

text: The rock of the Santa Lucias is dominated by

text: granitic

text: basement of the

text: Salinian Block

text: , between the

text: San Andreas Fault

text: and

text: Sur-Nacimiento Fault

text: .  The core of the Salinian block formed as part of the same

text: batholith

text: which forms the core of the

text: Sierra Nevada Mountains

text: and the

text: Peninsular Ranges

text: of

text: Baja California

text: .  It was separated from the

text: North American Plate

text: and transported north by the action of the

text: San Andreas Fault

text: from an original position.  It is predominantly

text: Mesozoic

text: granitic and pre-

text: Cretaceous

text: metamorphic rock

text: s.  There is some Cretaceous

text: sedimentary rock

text: of the Great Valley Sequence, considerable

text: Miocene

text: marine sediments, and some other

text: Cenozoic

text: sediments.  Units west of the Sur-Nacimiento Fault are dominated by rocks of the

text: Franciscan Assemblage

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answers: The rock of the Santa Lucias

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answers: sedimentary

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answers: San Andreas Fault

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answers: basement

answers: NDQ_005765

answers: It was separated from the North American Plate

answers: NDQ_005766

answers: granitic

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answers: Faster cooling forms larger crystals

answers: NDQ_005769

answers: granitic

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answers: Metamorphic rocks

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: This process occurs either after deformation or in the absence of dynamic deformation. Depending on the intensity of heat during recrystallization, the foliation will either be strengthened or weakened. If the heat is too intense, foliation will be weakened due to the nucleation and growth of new randomly oriented crystals and the rock will become a hornfels. If minimal heat is applied to a rock with a preexisting foliation and without a change in mineral assemblage, the cleavage will be strengthened by growth of micas parallel to foliation.

text: This process occurs either after deformation or in the absence of dynamic deformation. Depending on the intensity of heat during recrystallization, the foliation will either be strengthened or weakened. If the heat is too intense, foliation will be weakened due to the nucleation and growth of new randomly oriented crystals and the rock will become a

text: hornfels

text: . If minimal heat is applied to a rock with a preexisting foliation and without a change in mineral assemblage, the cleavage will be strengthened by growth of micas parallel to foliation.

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answers: Yes

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answers: sedimentary

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answers: intensity of heat

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answers: foliation

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answers: recrystallization

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answers: hornfels

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answers: If the heat is too intense, foliation will be weakened

answers: NDQ_005769

answers: recrystallization

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answers: The rock will become a hornfels

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Sedimentary breccia is a type of clastic sedimentary rock which is made of angular to subangular, randomly oriented clasts of other sedimentary rocks. A conglomerate, by contrast, is a sedimentary rock composed of rounded fragments or clasts of pre-existing rocks. Both breccia and conglomerate are composed of fragments averaging greater than  in size. The angular shape of the fragments indicates that the material has not been transported far from its source.

text: Sedimentary breccia is a type of

text: clastic

text: sedimentary rock

text: which is made of angular to subangular, randomly oriented

text: clasts

text: of other sedimentary rocks. A

text: conglomerate

text: , by contrast, is a sedimentary rock composed of rounded fragments or clasts of pre-existing rocks. Both breccia and conglomerate are composed of fragments averaging greater than  in size. The angular shape of the fragments indicates that the material has not been transported far from its source.

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answers: Yes

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answers: angular shape

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answers: angular to subangular

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answers: transported

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answers: subangular

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answers: breccia

answers: NDQ_005770

answers: It is out of the rock cycle

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Certain rock types, such as granite and limestone, are more resistant to erosion due to their relatively high mechanical strength.

text: Certain rock types, such as

text: granite

text: and

text: limestone

text: , are more resistant to erosion due to their relatively high mechanical strength.

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text: At the mid-ocean divergent boundaries new magma is produced by mantle upwelling and a shallow melting zone. This juvenile basaltic magma is an early phase of the igneous portion of the cycle. As the tectonic plates on either side of the ridge move apart the new rock is carried away from the ridge, the interaction of heated circulating seawater through fractures starts the retrograde metamorphism of the new rock.

text: At the

text: mid-ocean divergent boundaries

text: new

text: magma

text: is produced by

text: mantle

text: upwelling and a shallow melting zone. This juvenile

text: basalt

text: ic magma is an early phase of the igneous portion of the cycle. As the

text: tectonic plates

text: on either side of the ridge move apart the new rock is carried away from the ridge, the interaction of heated circulating

text: seawater

text: through

text: fractures

text: starts the

text: retrograde metamorphism

text: of the new rock.

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text: The park's landscape has been shaped by plate tectonics, with the Pacific Plate subducting beneath the North American Plate. The process has lowered the elevation of the Kenai Mountains, gradually pulling glacial features down into the sea, which is at the same time rising. The floors of the fjords can be from  below the present sea level.  The motion of the North Pacific Plate has accreted a variety of terranes against  the shoreline, so that the coastal region is a mixture of rocks that originated elsewhere, together with local igneous rock. Predominant rock types include shale and graywacke, with greenstone, tuff and chert.  The erosive power of the glaciers produces sediment as rock flour coloring the waters around the toes of glaciers, carrying minerals into the ecosystem that support phytoplankton, which in turn sustain larger animals.

text: The park's landscape has been shaped by

text: plate tectonics

text: , with the

text: Pacific Plate

text: subducting

text: beneath the

text: North American Plate

text: . The process has lowered the elevation of the Kenai Mountains, gradually pulling glacial features down into the sea, which is at the same time rising. The floors of the fjords can be from  below the present sea level.  The motion of the North Pacific Plate has accreted a variety of

text: terrane

text: s against  the shoreline, so that the coastal region is a mixture of rocks that originated elsewhere, together with local

text: igneous rock

text: . Predominant rock types include shale and

text: graywacke

text: , with

text: greenstone

text: tuff

text: and

text: chert

text: .  The erosive power of the glaciers produces sediment as

text: rock flour

text: coloring the waters around the toes of glaciers, carrying minerals into the ecosystem that support

text: phytoplankton

text: , which in turn sustain larger animals.

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text: Many places on Mars show rocks arranged in layers. Rock can form layers in a variety of ways.  Volcanoes, wind, or water can produce layers.  Layers may be formed by groundwater rising up depositing minerals and cementing sediments.  The hardned layers are consequently more protected from erosion.  This process may occur instead of layers forming under lakes.

text: Many places on Mars show rocks arranged in layers. Rock can form layers in a variety of ways.  Volcanoes, wind, or water can produce layers.  Layers may be formed by groundwater rising up depositing minerals and cementing sediments.  The hardned layers are consequently more protected from erosion.  This process may occur instead of layers forming under lakes.

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answers: Yes

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answers: faster cooling forms smaller crystals

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answers: It is out of the rock cycle

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: No

answer: 1

text: Tuff (from the Italian tufo) is a type of rock made of volcanic ash ejected from a vent during a volcanic eruption. Following ejection and deposition, the ash is compacted into a solid rock in a process called consolidation.  Tuff is sometimes called tufa, particularly when used as construction material, although tufa also refers to a quite different rock.  Rock that contains greater than 50% tuff is considered tuffaceous.

text: Tuff (from the

text: Italian

text: tufo) is a type of

text: rock

text: made of

text: volcanic ash

text: ejected from a

text: vent

text: during a

text: volcanic eruption

text: . Following ejection and deposition, the ash is compacted into a solid rock in a process called

text: consolidation

text: .  Tuff is sometimes called tufa, particularly when used as construction material, although

text: tufa

text: also refers to a quite different rock.  Rock that contains greater than 50% tuff is considered tuffaceous.

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answers: Tuff

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answers: NDQ_005770

answers: Tuff

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The Arc has two sections: the Internal and External Zones. The Internal Zone, which is located on the inner side of the arc, adjacent to the Alboran Sea, mostly consists of high-pressure, low-temperature metamorphic rocks. The External Zone, located on the outer side of the arc, is mostly made of sediments deposited on the passive margins of Africa and Iberia. These rocks became highly deformed during the westward emplacement of the hinterland of the subduction system, with some units in the External Rif having undergone medium-pressure, low-temperature metamorphism during the Oligocene. Flysch units from the Cretaceous to Early Miocene are located between the External and Internal Zones. These were folded and thrusted during the westward migration of the Internal Zones and can be interpreted as the palaeo-accretionary wedge of the subduction system that was active during the Lower and Middle Miocene.

text: The Arc has two sections: the Internal and External Zones. The Internal Zone, which is located on the inner side of the arc, adjacent to the Alboran Sea, mostly consists of high-pressure, low-temperature

text: metamorphic rocks

text: . The External Zone, located on the outer side of the arc, is mostly made of sediments deposited on the

text: passive margin

text: s of Africa and Iberia. These rocks became highly deformed during the westward emplacement of the hinterland of the subduction system, with some units in the External Rif having undergone medium-pressure, low-temperature metamorphism during the Oligocene.

text: Flysch

text: units from the

text: Cretaceous

text: to Early Miocene are located between the External and Internal Zones. These were

text: folded

text: and

text: thrusted

text: during the westward migration of the Internal Zones and can be interpreted as the palaeo-

text: accretionary wedge

text: of the subduction system that was active during the Lower and Middle Miocene.

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answers: Yes

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answers: low-temperature

answers: NDQ_005769

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answers: metamorphism

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Storm induced large erosion events are a part of the natural evolutionary process of fine sediment, gently sloping beaches. Increased wave energy in storms leads to the removal of foreshore, berm and dune sediments. These displaced sediments are then deposited as near shore sand bars and act to dampen the wave energy lessoning the amount of sediment that is being eroded from the coast. When wave energies decrease post storm events, the sediments from these newly deposited near shore bars are returned to the upper beach, rebuilding the berm. This self-correcting cycle is an active balance between wave energies and fine sediment deposition. This store of sediment being available for erosion in storms and re-depositing when the event has subsided is an important natural buffer mechanism against protecting the mainland from erosion and minimising coastal retreat.

text: Storm induced large erosion events are a part of the natural

text: evolutionary

text: process of fine

text: sediment

text: , gently sloping

text: beaches

text: . Increased

text: wave energy

text: in storms leads to the removal of

text: foreshore

text: berm

text: and

text: dune

text: sediments. These displaced sediments are then deposited as near

text: shore

text: sand bars and act to dampen the wave energy lessoning the amount of sediment that is being eroded from the coast. When wave energies decrease post storm events, the sediments from these newly deposited near shore bars are returned to the upper beach, rebuilding the berm. This self-correcting cycle is an active balance between wave energies and fine sediment

text: deposition

text: . This store of sediment being available for erosion in storms and re-depositing when the event has subsided is an important natural buffer mechanism against protecting the

text: mainland

text: from erosion and minimising coastal retreat.

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answer: No

answer: No

answer: No

answer: No

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text: A cratonic sequence is a very large-scale lithostratographic sequence that covers a complete marine transgressive-regressive cycle across a craton.  They are also known as "megasequences", "stratigraphic sequences", "sloss sequence" "supersequence" or simply "sequences."  In plain English, it is the geological evidence of the sea level rising and then falling, thereby depositing layers of sediment onto an area of ancient rock called a craton.

text: A cratonic sequence is a very large-scale

text: lithostratographic

text: sequence that covers a complete

text: marine transgressive-regressive

text: cycle across a

text: craton

text: .  They are also known as "megasequences", "stratigraphic sequences", "sloss sequence" "supersequence" or simply "sequences."  In plain English, it is the geological evidence of the sea level rising and then falling, thereby depositing layers of sediment onto an area of ancient rock called a craton.

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answer: No

answer: No

answer: No

answer: No

answer: No

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text: The term was originally defined by Stern et al. (1989) to refer to plutonic rocks containing between 55 and 60 weight percent SiO, with Mg# >0.6, Ni >100 ppm, Cr >200 ppm, KO >1 weight percent, Rb/Sr <0.1, Ba >500 ppm, Sr >500 ppm, enrichment in LREEs, and no or minor Eu anomalies. The term "sanukitoid suite" includes more evolved rocks derived from sanukitoid through fractional crystallization. Sanukitoids are similar in major and trace element composition to "adakites" (named for occurrences on the Adak Island in the Aleutian island arc). Both suites are thought to form by melting of a mafic igneous rock protolith that has been metamorphosed to garnet-pyroxene (eclogite) or garnet-amphibole assemblages (Rapp et al. 1991; Thorkelson & Breitsprecher 2005).

text: The term was originally defined by Stern et al. (1989) to refer to plutonic rocks containing between 55 and 60 weight percent SiO, with Mg# >0.6, Ni >100 ppm, Cr >200 ppm, KO >1 weight percent, Rb/Sr <0.1, Ba >500 ppm, Sr >500 ppm, enrichment in L

text: REE

text: s, and no or minor

text: Eu anomalies

text: . The term "sanukitoid suite" includes more evolved rocks derived from sanukitoid through fractional

text: crystallization

text: . Sanukitoids are similar in major and trace element composition to "

text: adakite

text: s" (named for occurrences on the Adak Island in the Aleutian island arc). Both suites are thought to form by melting of a mafic igneous rock protolith that has been metamorphosed to garnet-pyroxene (eclogite) or garnet-amphibole assemblages (Rapp et al. 1991; Thorkelson & Breitsprecher 2005).

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answers: intrusive

answers: NDQ_005763

answers: containing between 55 and 60 weight percent SiO

answers: NDQ_005764

answers: major and trace element composition

answers: NDQ_005765

answers: metamorphosed

answers: NDQ_005766

answers: garnet

answers: NDQ_005768

answers: fractional crystallization

answers: NDQ_005769

answers: crystallization

answers: NDQ_005770

answers: metamorphosed

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The Adamsfield Jubilee element is east of the Tyennan Block. It has a strip exposed on the surface that includes the Florentine Synclinorium, The Adamsfield District, the Jubilee Region, and down to the South Coast at Precipitous Bluff and Surprise Bay. It also underlies the Tasmania Basin across southeastern Tasmania, but not including the east coast. The subsurface structure has been studied from a few outliers, boreholes, xenoliths, and gravity and magnetic surveys. The basement at 5 km deep is the same as the Tyennan metamorphic rocks (Scotchfire Metamorphic Complex). Its oldest exposed rocks are from the Clark Group, of pelitic rocks, some with stromatolites, and evaporites, and overlaid with orthoquartzite. The Weld River Group lies above, starting with 0.5 km thickness of conglomerate and sandstone, then up to 3 km of dolostone, interbedded with sandstone, mudstone and diamictite. Glacial dropstones are found in the interbedding, suggesting Cryogenian age, however carbon isotope results suggest Ediacaran age instead. Gravity and magnetic studies indicate that this sort of dolomite (dense and non-magnetic) underlies Hobart and Bruny Island in a north–south strip, and also in a region west of Hobart.

text: The Adamsfield Jubilee element is east of the Tyennan Block. It has a strip exposed on the surface that includes the Florentine Synclinorium, The Adamsfield District, the Jubilee Region, and down to the South Coast at

text: Precipitous Bluff

text: and Surprise Bay. It also underlies the Tasmania Basin across southeastern Tasmania, but not including the east coast. The subsurface structure has been studied from a few outliers, boreholes,

text: xenolith

text: s, and gravity and magnetic surveys. The basement at 5 km deep is the same as the Tyennan metamorphic rocks (Scotchfire Metamorphic Complex). Its oldest exposed rocks are from the Clark Group, of pelitic rocks, some with

text: stromatolite

text: s, and

text: evaporite

text: s, and overlaid with orthoquartzite. The Weld River Group lies above, starting with 0.5 km thickness of conglomerate and sandstone, then up to 3 km of

text: dolostone

text: , interbedded with sandstone, mudstone and diamictite. Glacial dropstones are found in the interbedding, suggesting Cryogenian age, however

text: carbon isotope

text: results suggest Ediacaran age instead. Gravity and magnetic studies indicate that this sort of dolomite (dense and non-magnetic) underlies Hobart and Bruny Island in a north–south strip, and also in a region west of Hobart.

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answers: 5

answers: NDQ_005762

answers: 4

answers: NDQ_005763

answers: 0

answers: NDQ_005764

answers: 0

answers: NDQ_005765

answers: 0

answers: NDQ_005766

answers: 0

answers: NDQ_005768

answers: 0

answers: NDQ_005769

answers: 0

answers: NDQ_005770

answers: 0

answers: NDQ_005761

answers: The subsurface structure has been studied from a few outliers, boreholes, xenoliths, and gravity and magnetic surveys

answers: NDQ_005762

answers: sedimentary

answers: NDQ_005763

answers: carbon isotope

answers: NDQ_005764

answers: density

answers: NDQ_005765

answers: Cryogenian

answers: NDQ_005766

answers: dolomite

answers: NDQ_005768

answers: glacial dropstones

answers: NDQ_005769

answers: evaporites

answers: NDQ_005770

answers: Metamorphic rocks

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: In the Tyennan block, the Precambrian basement that forms the central core of Tasmania there are two formations. First, the Oonah Formation contains turbidite with quartz sandstone interbedded with siltstone deposited by gravity flows. This has been deformed with tight folds that have been overturned, and exhibits crenulation cleavage and brittle faulting.  Zircons in the quartzite have peak numbers aged  and . Secondly, the Scotchfire Metamorphic Complex contains quartzite deposited in the sea from windblown desert sands, schist and phyllite possibly from a delta. Small quantities of dolomite and boulder conglomerate are also included. The complex includes boudinage structure and en echelon veins. Phyllitenear Strathgordon has been dated at . Metamorphism to greenschist facies occurred at around 400 °C and 300 MPa. The Franklin Metamorphic Complex is near Mount Franklin. At Raglan Range the rocks are a mixture of quartzite and knotted schist. Metamorphism in this area was higher grade with almandine garnet forming. The Collingwood area experienced the highest grade of metamorphism with garnet-mica schist, mica schist and garnet-mica-kyanite gneiss present, and enough heat to form veins of migmatite.  Eclogite and garnet amphibolite are believed to be the remains of basalt. The eclogite has been heated to 700° at 1520 MPa, a burial depth of perhaps 50 km. Metamorphism happened  at the same time as the Cambrian ultramafic complexes were introduced.

text: In the Tyennan block, the Precambrian basement that forms the central core of Tasmania there are two formations. First, the Oonah Formation contains

text: turbidite

text: with quartz

text: sandstone

text: interbedded with siltstone deposited by gravity flows. This has been deformed with tight folds that have been overturned, and exhibits crenulation

text: cleavage

text: and brittle faulting.  Zircons in the quartzite have peak numbers aged  and . Secondly, the Scotchfire Metamorphic Complex contains quartzite deposited in the sea from

text: windblown

text: desert sands,

text: schist

text: and

text: phyllite

text: possibly from a delta. Small quantities of dolomite and boulder

text: conglomerate

text: are also included. The complex includes

text: boudinage structure

text: and en echelon

text: veins

text: . Phyllitenear

text: Strathgordon

text: has been dated at . Metamorphism to

text: greenschist facies

text: occurred at around 400 °C and 300 MPa. The Franklin Metamorphic Complex is near Mount Franklin. At Raglan Range the rocks are a mixture of quartzite and knotted

text: schist

text: . Metamorphism in this area was higher grade with

text: almandine

text: garnet

text: forming. The Collingwood area experienced the highest grade of metamorphism with garnet-mica schist, mica schist and garnet-mica-

text: kyanite

text: gneiss

text: present, and enough heat to form veins of

text: migmatite

text: Eclogite

text: and garnet amphibolite are believed to be the remains of basalt. The eclogite has been heated to 700° at 1520 MPa, a burial depth of perhaps 50 km. Metamorphism happened  at the same time as the Cambrian

text: ultramafic

text: complexes were introduced.

answers: tqa2:L_0289/T_1626/417decf02ed5c65ff7697111ab04772a

answers: 0

answers: tqa2:L_0289/T_1626/2e5cf706719179f148aade7c740bc774

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

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

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

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

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answers: 5

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answers: 4

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answers: NDQ_005770

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answers: NDQ_005761

answers: Metamorphism to greenschist facies

answers: NDQ_005762

answers: sedimentary

answers: NDQ_005763

answers: heat

answers: NDQ_005764

answers: age

answers: NDQ_005765

answers: metamorphism

answers: NDQ_005766

answers: basalt

answers: NDQ_005768

answers: Metamorphism

answers: NDQ_005769

answers: metamorphism

answers: NDQ_005770

answers: Metamorphism

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The original concept of the rock cycle is usually attributed to James Hutton, from the eighteenth century Father of Geology. The rock cycle was a part of Hutton's uniformitarianism  and his famous quote: no vestige of a beginning, and no prospect of an end, applied in particular to the rock cycle and the envisioned cyclical nature of geologic processes. This concept of a repetitive non-evolutionary rock cycle remained dominant until the plate tectonics revolution of the 1960s. With the developing understanding of the driving engine of plate tectonics, the rock cycle changed from endlessly repetitive to a gradually evolving process. The Wilson cycle (a plate tectonics based rock cycle) was developed by J. Tuzo Wilson during the 1950s and 1960s. The world is made out of rocks.

text: The original concept of the rock cycle is usually attributed to

text: James Hutton

text: , from the eighteenth century Father of Geology. The rock cycle was a part of Hutton's

text: uniformitarianism

text: and his famous quote: no vestige of a beginning, and no prospect of an end, applied in particular to the rock cycle and the envisioned cyclical nature of geologic processes. This concept of a repetitive non-evolutionary rock cycle remained dominant until the plate tectonics revolution of the 1960s. With the developing understanding of the driving engine of

text: plate tectonics

text: , the rock cycle changed from endlessly repetitive to a gradually evolving process. The

text: Wilson cycle

text: (a plate tectonics based rock cycle) was developed by

text: J. Tuzo Wilson

text: during the 1950s and 1960s. The world is made out of rocks.

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answer: Yes

answer: No

answer: Yes

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text: Some proteins present unique challenges for crystallization. Membrane proteins frequently require the addition of a detergent for isolation and crystallization, and tend to form "very small, weakly (x-ray) diffracting, radiation-sensitive crystals".  Proteins that form fibres need to be stabilized in a monomeric form.  Small proteins can have  poor solubility in water and require specialized crystallization techniques.

text: Some proteins present unique challenges for crystallization. Membrane proteins frequently require the addition of a

text: detergent

text: for isolation and crystallization, and tend to form "very small, weakly (x-ray) diffracting, radiation-sensitive crystals".  Proteins that form fibres need to be stabilized in a

text: monomeric

text: form.  Small proteins can have  poor

text: solubility

text: in water and require specialized crystallization techniques.

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answer: No

answer: No

answer: No

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text: About 60% crystallization is the upper limit for commercial products, with the exception of polyester fibers. Clear products can be produced by rapidly cooling molten polymer below T glass transition temperature to form an amorphous solid. Like glass, amorphous PET forms when its molecules are not given enough time to arrange themselves in an orderly, crystalline fashion as the melt is cooled. At room temperature the molecules are frozen in place, but, if enough heat energy is put back into them by heating above T, they begin to move again, allowing crystals to nucleate and grow. This procedure is known as solid-state crystallization.

text: About 60% crystallization is the upper limit for commercial products, with the exception of polyester fibers. Clear products can be produced by rapidly cooling molten polymer below T

text: glass transition temperature

text: to form an

text: amorphous solid

text: . Like

text: glass

text: , amorphous PET forms when its molecules are not given enough time to arrange themselves in an orderly, crystalline fashion as the melt is cooled. At room temperature the molecules are frozen in place, but, if enough heat energy is put back into them by heating above T, they begin to move again, allowing crystals to

text: nucleate

text: and grow. This procedure is known as solid-state

text: crystallization

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answers: At room temperature

answers: NDQ_005769

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answer: No

answer: No

answer: No

answer: No

answer: No

answer: 0

text: Peninsular Gneiss is a term coined to highlight the older gneissic complex of the metamorphics found all over the Indian Peninsula. This term was first fashioned by W.F.Smeeth of the Mysore Geological Department in 1916 based on the first scientific study of this rock exposure. The Geological Survey of India identified one of the best exposures of this rock mass, protruding high above the ground as a hillock (pictured), dated 2.5 to 3.4 billion years, in the  Bangalore city in India at the famous Lalbagh gardens and declared it as a National Geological Monument to propagate the knowledge of the rock formation among the public, since Lalbagh is frequented by visitors from all over the world.It is also called the Lalbagh rock.

text: Peninsular Gneiss is a term coined to highlight the older gneissic complex of the

text: metamorphic

text: s found all over the

text: Indian Peninsula

text: . This term was first fashioned by W.F.Smeeth of the Mysore Geological Department in 1916 based on the first scientific study of this rock exposure. The

text: Geological Survey of India

text: identified one of the best exposures of this rock mass, protruding high above the ground as a hillock (pictured), dated 2.5 to 3.4 billion years, in the

text: Bangalore

text: city in

text: India

text: at the famous

text: Lalbagh

text: gardens and declared it as a National Geological Monument to propagate the knowledge of the rock formation among the public, since

text: Lalbagh

text: is frequented by visitors from all over the world.It is also called the Lalbagh rock.

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answers: all over the Indian Peninsula

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text: He regards the rock as an "artistic form" and the pop music as, if anything, a marketing concept. Rock, in Carducci's view, is "rock and roll music made conscious of itself as a small band music".

text: He regards the rock as an "artistic form" and the pop music as, if anything, a

text: marketing

text: concept. Rock, in Carducci's view, is "rock and roll music made

text: conscious of itself

text: as a small band music".

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text: Highwall mining is another form of surface mining that evolved from auger mining. In Highwall mining, the coal seam is penetrated by a continuous miner propelled by a hydraulic Pushbeam Transfer Mechanism (PTM). A typical cycle includes sumping (launch-pushing forward) and shearing (raising and lowering the cutterhead boom to cut the entire height of the coal seam). As the coal recovery cycle continues, the cutterhead is progressively launched into the coal seam for 19.72 feet (6.01 m). Then, the Pushbeam Transfer Mechanism (PTM) automatically inserts a 19.72-foot (6.01 m) long rectangular Pushbeam (Screw-Conveyor Segment) into the center section of the machine between the Powerhead and the cutterhead. The Pushbeam system can penetrate nearly 1,000 feet (300 m) into the coal seam. One patented Highwall mining system uses augers enclosed inside the Pushbeam that prevent the mined coal from being contaminated by rock debris during the conveyance process. Using a video imaging and/or a gamma ray sensor and/or other Geo-Radar systems like a coal-rock interface detection sensor (CID), the operator can see ahead projection of the seam-rock interface and guide the continuous miner's progress. Highwall mining can produce thousands of tons of coal in contour-strip operations with narrow benches, previously mined areas, trench mine applications and steep-dip seams with controlled water-inflow pump system and/or a gas (inert) venting system.

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answers: The pushbeam system can penetrate nearly 1,000 feet (300 m) into the coal seam

answers: NDQ_005762

answers: sedimentary

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answers: gamma ray sensor

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answers: thickness

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answers: faster cooling forms smaller crystals

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answers: sumping

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answers: Highwall mining

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Provenance in geology, is the reconstruction of the origin of sediments. The Earth is not a static but a dynamic planet, all rocks are subject to transition between the three main rock types, which are sedimentary, metamorphic, and igneous rocks (the rock cycle). Rocks exposed to the surface, sooner or later, are broken down into sediments. Sediments are expected to be able to provide evidence of the erosion history of their parent source rocks. The purpose of provenance study is to restore the tectonic, paleo-geographic and paleo-climatic history.

text: Provenance in

text: geology

text: , is the reconstruction of the origin of

text: sediments

text: . The Earth is not a static but a dynamic planet, all rocks are subject to transition between the three main rock types, which are

text: sedimentary

text: metamorphic

text: , and

text: igneous rock

text: s (the

text: rock cycle

text: ). Rocks exposed to the surface, sooner or later, are broken down into sediments. Sediments are expected to be able to provide evidence of the

text: erosion

text: history of their parent source rocks. The purpose of provenance study is to restore the

text: tectonic

text: paleo-geographic

text: and

text: paleo-climatic

text: history.

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answers: NDQ_005761

answers: The Earth is not a static but a dynamic planet

answers: NDQ_005762

answers: sedimentary

answers: NDQ_005763

answers: tectonic

answers: NDQ_005764

answers: origin

answers: NDQ_005765

answers: transition between the three main rock types

answers: NDQ_005766

answers: igneous

answers: NDQ_005768

answers: slower cooling forms smaller crystals

answers: NDQ_005769

answers: metamorphic

answers: NDQ_005770

answers: all rocks are subject to transition

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: 1

text: Erosion continued into the Mesozoic, so the state has almost no rock record from this entire era of geologic time. The few rocks present were igneous and likely formed as a result of the rifting that divided Pangaea. No dinosaur fossils have ever been discovered in New Hampshire. No other fossils are known from this scant rock record either. Local erosion continued into the Cenozoic era. There is no local rock record for the entirety of the Tertiary. During the more recent Quaternary, New Hampshire was largely covered by glaciers. The local plant life resembled that of modern arctic Canada. This is supported by fossil plants and pollen preserved in sediments deposited when the glaciers melted.

text: Erosion continued into the

text: Mesozoic

text: , so the state has almost no rock record from this entire era of geologic time. The few rocks present were igneous and likely formed as a result of the

text: rift

text: ing that divided

text: Pangaea

text: . No

text: dinosaur

text: fossils have ever been discovered in New Hampshire. No other fossils are known from this scant rock record either. Local erosion continued into the

text: Cenozoic

text: era. There is no local rock record for the entirety of the

text: Tertiary

text: . During the more recent

text: Quaternary

text: , New Hampshire was largely covered by

text: glacier

text: s. The local plant life resembled that of modern

text: arctic

text: Canada. This is supported by fossil plants and pollen preserved in sediments deposited when the glaciers melted.

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answers: Yes

answers: NDQ_005762

answers: sedimentary

answers: NDQ_005763

answers: rifting

answers: NDQ_005764

answers: igneous

answers: NDQ_005765

answers: Erosion

answers: NDQ_005766

answers: igneous

answers: NDQ_005768

answers: faster cooling forms smaller crystals

answers: NDQ_005769

answers: glaciers

answers: NDQ_005770

answers: Quaternary

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Various geological processes create discontinuities at a broadly regular spacing. For example, bedding planes are the result of a repeated sedimentation cycle with a change of sedimentation material or change in structure and texture of the sediment at regular intervals, folding creates joints at regular separations to allow for shrinkage or expansion of the rock material, etc. Normally discontinuities with the same origin have broadly the same characteristics in terms of shear strength, spacing between discontinuities, roughness, infill, etc. The orientations of discontinuities with the same origin are related to the process that has created them and to the geological history of the rock mass. A discontinuity set or family denotes a series of discontinuities for which the geological origin (history, etc.), the orientation, spacing, and the mechanical characteristics (shear strength, roughness, infill material, etc.) are broadly the same.

text: Various geological processes create discontinuities at a broadly regular spacing. For example,

text: bedding planes

text: are the result of a repeated

text: sedimentation

text: cycle with a change of sedimentation material or change in structure and texture of the sediment at regular intervals,

text: folding

text: creates

text: joints

text: at regular separations to allow for shrinkage or expansion of the rock material, etc. Normally discontinuities with the same origin have broadly the same characteristics in terms of

text: shear strength

text: , spacing between discontinuities, roughness, infill, etc. The orientations of discontinuities with the same origin are related to the process that has created them and to the geological history of the rock mass. A discontinuity set or family denotes a series of discontinuities for which the geological origin (history, etc.), the orientation, spacing, and the mechanical characteristics (

text: shear strength

text: , roughness, infill material, etc.) are broadly the same.

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answers: Slower cooling forms smaller crystals

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answers: discontinuities with the same origin

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Other minerals, such as olivines, pyroxenes, amphiboles, micas, feldspars, and quartz, may be found in metamorphic rocks, but are not necessarily the result of the process of metamorphism. These minerals formed during the crystallization of igneous rocks. They are stable at high temperatures and pressures and may remain chemically unchanged during the metamorphic process. However, all minerals are stable only within certain limits, and the presence of some minerals in metamorphic rocks indicates the approximate temperatures and pressures at which they formed.

text: Other minerals, such as

text: olivine

text: s,

text: pyroxene

text: s,

text: amphibole

text: s,

text: mica

text: s,

text: feldspar

text: s, and

text: quartz

text: , may be found in metamorphic rocks, but are not necessarily the result of the process of metamorphism. These minerals formed during the

text: crystallization

text: of igneous rocks. They are stable at high temperatures and pressures and may remain chemically unchanged during the metamorphic process. However, all minerals are stable only within certain limits, and the presence of some minerals in metamorphic rocks indicates the approximate temperatures and pressures at which they formed.

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answers: metamorphism

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Metamorphic rocks can change without melting. Heat causes atomic bonds to break, and the atoms move and form new bonds with other atoms, creating new minerals with different chemical components or crystalline structures (neocrystallization), or enabling recrystallization. When pressure is applied, somewhat flattened grains that orient in the same direction have a more stable configuration.

text: Metamorphic rocks can change without melting. Heat causes atomic bonds to break, and the atoms move and form new bonds with other atoms, creating new minerals with different chemical components or crystalline structures (

text: neocrystallization

text: ), or enabling

text: recrystallization

text: . When pressure is applied, somewhat flattened grains that orient in the same direction have a more stable configuration.

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answers: Metamorphic rocks

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answers: Metamorphic rocks

answer: No

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text: Sedimentary rocks are types of rock that are formed by the deposition and subsequent cementation of that material at the Earth's surface and within bodies of water. Sedimentation is the collective name for processes that cause mineral and/or organic particles (detritus) to settle in place. The particles that form a sedimentary rock by accumulating are called sediment. Before being deposited, the sediment was formed by weathering and erosion from the source area, and then transported to the place of deposition by water, wind, ice, mass movement or glaciers, which are called agents of denudation. Sedimentation may also occur as minerals precipitate from water solution or shells of aquatic creatures settle out of suspension.

text: Sedimentary rocks are types of

text: rock

text: that are formed by the

text: deposition

text: and subsequent cementation of that material at the

text: Earth's surface

text: and within bodies of water.

text: Sedimentation

text: is the collective name for processes that cause

text: mineral

text: and/or

text: organic

text: particles (

text: detritus

text: ) to settle in place. The particles that form a sedimentary rock by accumulating are called

text: sediment

text: . Before being deposited, the sediment was formed by

text: weathering

text: and

text: erosion

text: from the source area, and then transported to the place of deposition by

text: water

text: wind

text: ice

text: mass movement

text: or

text: glacier

text: s, which are called agents of

text: denudation

text: . Sedimentation may also occur as minerals precipitate from water solution or shells of aquatic creatures settle out of suspension.

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answers: Sedimentation

answer: No

answer: No

answer: Yes

answer: No

answer: No

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text: Weather is one of the fundamental processes that shape the Earth. The process of weathering breaks down the rocks and soils into smaller fragments and then into their constituent substances. During rains precipitation, the water droplets absorb and dissolve carbon dioxide from the surrounding air. This causes the rainwater to be slightly acidic, which aids the erosive properties of water. The released sediment and chemicals are then free to take part in chemical reactions that can affect the surface further (such as acid rain), and sodium and chloride ions (salt) deposited in the seas/oceans. The sediment may reform in time and by geological forces into other rocks and soils. In this way, weather plays a major role in erosion of the surface.

text: Weather is one of the fundamental processes that shape the Earth. The process of weathering breaks down the rocks and soils into smaller fragments and then into their constituent substances. During rains precipitation, the water droplets absorb and dissolve carbon dioxide from the surrounding air. This causes the rainwater to be slightly acidic, which aids the erosive properties of water. The released sediment and chemicals are then free to take part in

text: chemical

text: reactions that can affect the surface further (such as

text: acid rain

text: ), and sodium and chloride ions

text: (salt)

text: deposited in the seas/oceans. The sediment may reform in time and by geological forces into other rocks and soils. In this way, weather plays a major role in

text: erosion

text: of the surface.

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answers: The sediment may reform in time

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answers: slower cooling forms smaller crystals

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answers: The sediment may reform in time

answer: No

answer: No

answer: No

answer: No

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answer: 1

text: The rocks follow the calc-alkaline trend of magmatic differentiation, containing silicic lavas such as dacite. Their overall composition ranges from basaltic andesite to dacite, and the dominant lava rocks are andesite and basalt. Andesites range from green to gray in colour, and dacites are pink- and light-gray. The andesitic lavas contain phenocrysts of andesine, hornblende, plagioclase and hypersthene. Dacites have biotite, hornblende, plagioclase and quartz phenocrysts. Textures range from porphyritic to vitreophyritic. Andesites are more common in Pliocene rocks, and Pleistocene rocks tend to be dacitic. At least five cycles of andesite rock formation have been found on the southwest side of Koh-i-Sultan. Its rocks are typical volcanic-arc rocks in elemental chemistry, and may stem from mantle-derived magma. The satellite centre rocks differ from the main centre rocks in composition, suggesting that different processes generated the magmas which constructed the cones. There is a compositional trend from Bazman over Taftan to Sultan, with the latter having more potassium in its rocks than the other centres. Such compositional trends may come from different partial melting ratios and different fluid contributions to magma generation at each volcano.

text: The rocks follow the

text: calc-alkaline

text: trend of

text: magmatic differentiation

text: , containing silicic lavas such as dacite. Their overall composition ranges from

text: basaltic andesite

text: to dacite, and the dominant lava rocks are andesite and

text: basalt

text: . Andesites range from green to gray in colour, and dacites are pink- and light-gray. The andesitic lavas contain

text: phenocryst

text: s of

text: andesine

text: hornblende

text: , plagioclase and

text: hypersthene

text: . Dacites have

text: biotite

text: , hornblende,

text: plagioclase

text: and

text: quartz

text: phenocryst

text: s. Textures range from

text: porphyritic

text: to

text: vitreophyritic

text: . Andesites are more common in

text: Pliocene

text: rocks, and

text: Pleistocene

text: rocks tend to be dacitic. At least five cycles of andesite rock formation have been found on the southwest side of Koh-i-Sultan. Its rocks are typical volcanic-arc rocks in elemental chemistry, and may stem from

text: mantle

text: -derived magma. The satellite centre rocks differ from the main centre rocks in composition, suggesting that different processes generated the magmas which constructed the cones. There is a compositional trend from Bazman over Taftan to Sultan, with the latter having more

text: potassium

text: in its rocks than the other centres. Such compositional trends may come from different

text: partial melting

text: ratios and different fluid contributions to magma generation at each volcano.

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answers: Rocks are typical volcanic-arc rocks

answers: NDQ_005762

answers: andesite

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answers: Its rocks are typical volcanic-arc rocks

answer: No

answer: No

answer: No

answer: No

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text: The rocks of Salt Point are sedimentary, mainly sandstone. All of these rocks are tilted, exposing older rocks. The rocks at the north end of the park's coast are younger than the rocks at of the southern end. Salt Point is named for the tafoni where the ocean water crystallizes in the honeycomb like crevices. This tafoni is caused when the salt crystals interact with the sandstone making parts of the sandstone harden while other parts soften.

text: The rocks of Salt Point are sedimentary, mainly sandstone. All of these rocks are tilted, exposing older rocks. The rocks at the north end of the park's coast are younger than the rocks at of the southern end. Salt Point is named for the

text: tafoni

text: where the ocean water crystallizes in the honeycomb like crevices. This tafoni is caused when the salt crystals interact with the sandstone making parts of the sandstone harden while other parts soften.

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answers: Yes

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answers: sedimentary

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answers: ocean water crystallizes in the honeycomb like crevices

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answers: tilted

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answers: tilted, exposing older rocks

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answers: slower cooling forms smaller crystals

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answers: salt crystallizes

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answers: The rocks of Salt Point are sedimentary

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The sixth match featured The Rock defending the WCW Championship against Booker T and Shane McMahon in a handicap match. Rock dominated Booker and McMahon in the earlier part of the match until Booker and McMahon started double-teaming Rock. At one point, McMahon tried to hit Rock with the WCW title belt but Rock avoided and Booker was hit with the belt instead. McMahon also hit Rock with the belt. McMahon attempted to hit a Leap of Faith on Rock but he rolled away. Booker was tagged in but Rock hit Booker and McMahon a double clothesline. Rock hit McMahon, a Rock Bottom and a Spinebuster on Booker. Test interfered in the match and prevented Rock from winning the match. Bradshaw came out to prevent Test from interfering. Booker tried to pin Rock but Mike Chioda and a WWF referee attacked the WCW referee Nick Patrick, who was refereeing the match. Earl Hebner replaced Patrick and took over as the official. Rock hit Booker with a Rock Bottom to win the match and retain the WCW Championship.

text: The sixth match featured

text: The Rock

text: defending the

text: WCW Championship

text: against

text: Booker T

text: and

text: Shane McMahon

text: in a

text: handicap match

text: . Rock dominated Booker and McMahon in the earlier part of the match until Booker and McMahon started double-teaming Rock. At one point, McMahon tried to hit Rock with the WCW title belt but Rock avoided and Booker was hit with the belt instead. McMahon also hit Rock with the belt. McMahon attempted to hit a

entity_name: Professional wrestling aerial techniques

text: Leap of Faith

text: on Rock but he rolled away. Booker was tagged in but Rock hit Booker and McMahon a

entity_name: Professional wrestling double-team maneuvers

text: double clothesline

text: . Rock hit McMahon, a

text: Rock Bottom

text: and a

text: Spinebuster

text: on Booker.

text: Test

text: interfered in the match and prevented Rock from winning the match.

text: Bradshaw

text: came out to prevent Test from interfering. Booker tried to pin Rock but

text: Mike Chioda

text: and a WWF referee attacked the WCW referee

text: Nick Patrick

text: , who was refereeing the match.

text: Earl Hebner

text: replaced Patrick and took over as the official. Rock hit Booker with a Rock Bottom to win the match and retain the WCW Championship.

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answers: Rock dominated Booker and McMahon

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answers: slower cooling forms smaller crystals

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answers: Rock

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 0

text: A similar type of crystal is a phenocryst, a large crystal in an igneous rock. Porphyroblasts are often confused with porphyroclasts, which can also be large outstanding crystals, but which are older than the matrix of the rock.

text: A similar type of crystal is a

text: phenocryst

text: , a large crystal in an

text: igneous rock

text: . Porphyroblasts are often confused with

text: porphyroclast

text: s, which can also be large outstanding crystals, but which are older than the matrix of the rock.

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answers: Yes

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answers: intrusive

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answers: large outstanding crystals

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answers: matrix

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answers: older than the matrix

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answers: igneous

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answers: Porphyroblasts

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answers: igneous rock

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Metamorphic rocks are formed by subjecting any rock type—sedimentary rock, igneous rock or another older metamorphic rock—to different temperature and pressure conditions than those in which the original rock was formed. This process is called metamorphism; meaning to "change in form". The result is a profound change in physical properties and chemistry of the stone. The original rock, known as the protolith, transforms into other mineral types or other forms of the same minerals, by recrystallization. The temperatures and pressures required for this process are always higher than those found at the Earth's surface: temperatures greater than 150 to 200 °C and pressures of 1500 bars. Metamorphic rocks compose 27.4% of the crust by volume.

text: Metamorphic rock

text: s are formed by subjecting any rock type—

text: sedimentary rock

text: igneous rock

text: or another older metamorphic rock—to different

text: temperature

text: and

text: pressure

text: conditions than those in which the original rock was formed. This process is called

text: metamorphism

text: ; meaning to "change in form". The result is a profound change in physical properties and chemistry of the stone. The original rock, known as the

text: protolith

text: , transforms into other mineral types or other forms of the same minerals, by

text: recrystallization

text: . The temperatures and pressures required for this process are always higher than those found at the Earth's surface: temperatures greater than 150 to 200 °C and pressures of 1500 bars. Metamorphic rocks compose 27.4% of the crust by volume.

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answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: As noted above, sometimes an election has no Condorcet winner because there is no candidate who is preferred by voters to all other candidates. When this occurs the situation is known as a 'majority rule cycle', 'circular ambiguity', 'circular tie', 'Condorcet paradox', or simply 'cycle'. This situation emerges when, once all votes have been added up, the preferences of voters with respect to some candidates form a circle in which every candidate is beaten by at least one other candidate. For example, if there are three candidates, Candidate Rock, Candidate Scissors, and Candidate Paper, there will be no Condorcet winner if voters prefer Candidate Rock over Candidate Scissors and Scissors over Paper, but also Candidate Paper over Rock. Depending on the context in which elections are held, circular ambiguities may or may not be common. Nonetheless an ambiguity is always possible, and so every Condorcet method must be capable of determining a winner when this occurs. A mechanism for resolving an ambiguity is known as ambiguity resolution or Condorcet completion method.

text: As noted above, sometimes an election has no Condorcet winner because there is no candidate who is preferred by voters to all other candidates. When this occurs the situation is known as a 'majority rule cycle', 'circular ambiguity', 'circular tie', 'Condorcet paradox', or simply 'cycle'. This situation emerges when, once all votes have been added up, the preferences of voters with respect to some candidates form a circle in which every candidate is beaten by at least one other candidate. For example, if there are three candidates,

text: Candidate Rock, Candidate Scissors, and Candidate Paper

text: , there will be no Condorcet winner if voters prefer Candidate Rock over Candidate Scissors and Scissors over Paper, but also Candidate Paper over Rock. Depending on the context in which elections are held, circular ambiguities may or may not be common. Nonetheless an ambiguity is always possible, and so every Condorcet method must be capable of determining a winner when this occurs. A mechanism for resolving an ambiguity is known as ambiguity resolution or Condorcet completion method.

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answers: Yes

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answers: Intrusive

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answers: the context in which elections are held

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answers: rock

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answers: there is no Condorcet winner

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answers: Paper

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answers: slower cooling forms smaller crystals

answers: NDQ_005769

answers: Condorcet paradox

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answers: no Condorcet winner

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 0

text: Petrological indicators of UHP metamorphism are usually preserved in eclogite. The presence of metamorphic coesite, diamond, or majoritic garnet are diagnostic; other potential mineralogical indicators of UHP metamorphism, such as alpha-PbO structured TiO, are not widely accepted. Mineral assemblages, rather than single minerals, can also be used to identify UHP rocks; these assemblages include magnesite + aragonite. Because minerals change composition in response to changes in pressure and temperature, mineral compositions can be used to calculate pressure and temperature; for UHP eclogite the best geobarometers involve garnet + clinopyroxene + K-white mica and garnet + clinopyroxene + kyanite + coesite/quartz. Most UHP rocks were metamorphosed at peak conditions of 800 °C and 3 GPa. At least two UHP localities record higher temperatures: the Bohemian and Kokchetav Massifs reached 1000–1200 °C at pressures of at least 4 GPa.

text: Petrological indicators of UHP metamorphism are usually preserved in

text: eclogite

text: . The presence of metamorphic coesite, diamond, or

text: majoritic garnet

text: are diagnostic; other potential mineralogical indicators of UHP metamorphism, such as alpha-PbO structured TiO, are not widely accepted. Mineral assemblages, rather than single minerals, can also be used to identify UHP rocks; these assemblages include magnesite + aragonite. Because minerals change composition in response to changes in pressure and temperature, mineral compositions can be used to calculate pressure and temperature; for UHP eclogite the best geobarometers involve garnet + clinopyroxene + K-white mica and garnet + clinopyroxene + kyanite + coesite/quartz. Most UHP rocks were metamorphosed at peak conditions of 800 °C and 3

text: GPa

text: . At least two UHP localities record higher temperatures: the Bohemian and Kokchetav Massifs reached 1000–1200 °C at pressures of at least 4 GPa.

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text: Parallel to the phenomenon of erosion, occurs a process of sedimentation: the extremity of the new Southern Island of Sangomar increases by 100 m per annum to the south and, on the opposite bank, the outskirts of the villages of Niodior and Dionewar are silting considerably, reducing traffic of vessels and contributing to the isolation of populations.

text: Parallel to the phenomenon of

text: erosion

text: , occurs a process of

text: sedimentation

text: : the extremity of the new Southern Island of Sangomar increases by 100 m per annum to the south and, on the opposite bank, the outskirts of the villages of

text: Niodior

text: and

text: Dionewar

text: are silting considerably, reducing traffic of vessels and contributing to the isolation of populations.

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text: In earth science, erosion is the action of surface processes (such as water flow or wind) that remove soil, rock, or dissolved material from one location on the Earth's crust, then transport it away to another location. The particulate breakdown of rock or soil into clastic sediment is referred to as physical or mechanical erosion; this contrasts with chemical erosion, where soil or rock material is removed from an area by its dissolving into a solvent (typically water), followed by the flow away of that solution. Eroded sediment or solutes may be transported just a few millimetres, or for thousands of kilometres.

text: In

text: earth science

text: , erosion is the action of surface processes (such as

text: water flow

text: or

text: wind

text: ) that remove

text: soil

text: rock

text: , or dissolved material from one location on the

text: Earth's crust

text: , then

text: transport

text: it away to another location. The particulate breakdown of rock or soil into

text: clastic

text: sediment

text: is referred to as physical or mechanical erosion; this contrasts with chemical erosion, where soil or rock material is removed from an area by its dissolving into a solvent (typically water), followed by the flow away of that solution. Eroded

text: sediment

text: or solutes may be transported just a few millimetres, or for thousands of kilometres.

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text: Sedimentary rocks can be subdivided into four groups based on the processes responsible for their formation: clastic sedimentary rocks, biochemical (biogenic) sedimentary rocks, chemical sedimentary rocks, and a fourth category for "other" sedimentary rocks formed by impacts, volcanism, and other minor processes.

text: Sedimentary rocks can be subdivided into four groups based on the processes responsible for their formation: clastic sedimentary rocks, biochemical (biogenic) sedimentary rocks, chemical sedimentary rocks, and a fourth category for "other" sedimentary rocks formed by impacts,

text: volcanism

text: , and other minor processes.

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answers: Yes

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answers: Sedimentary rocks

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answers: sedimentary rocks

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answers: chemical sedimentary rocks

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answers: chemical sedimentary rocks

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answers: Sedimentary rocks

answers: NDQ_005769

answers: clastic

answers: NDQ_005770

answers: Sedimentary rocks

answer: No

answer: No

answer: Yes

answer: No

answer: No

answer: 1

text: Rocks in the tholeiitic magma series are classified as subalkaline (they contain less sodium than some other basalts) and are distinguished from rocks in the calc-alkaline magma series by the redox state of the magma they crystallized from (tholeiitic magmas are reduced; calc-alkaline magmas are oxidized).  When the parent magmas of basalts crystallize, they preferentially crystallize the more magnesium-rich and iron-poor forms of the silicate minerals olivine and pyroxene, causing the iron content of tholeiitic magmas to increase as the melt is depleted of iron-poor crystals.  However, a calc-alkaline magma is oxidized enough to precipitate significant amounts of the iron oxide magnetite, causing the iron content of the magma to remain more steady as it cools than with a tholeiitic magma.

text: Rocks in the tholeiitic magma series are classified as subalkaline (they contain less sodium than some other basalts) and are distinguished from rocks in the

text: calc-alkaline

text: magma series by the

text: redox

text: state of the magma they crystallized from (tholeiitic magmas are reduced; calc-alkaline magmas are oxidized).  When the parent magmas of basalts crystallize, they preferentially crystallize the more magnesium-rich and iron-poor forms of the silicate minerals

text: olivine

text: and

text: pyroxene

text: , causing the iron content of tholeiitic magmas to increase as the melt is depleted of iron-poor crystals.  However, a calc-alkaline magma is oxidized enough to precipitate significant amounts of the iron oxide

text: magnetite

text: , causing the iron content of the magma to remain more steady as it cools than with a tholeiitic magma.

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answers: 3

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answers: 0

answers: NDQ_005761

answers: Yes

answers: NDQ_005762

answers: intrusive

answers: NDQ_005763

answers: redox state

answers: NDQ_005764

answers: iron content

answers: NDQ_005765

answers: parent magmas of basalts crystallize

answers: NDQ_005766

answers: basalts

answers: NDQ_005768

answers: tholeiitic magmas are reduced

answers: NDQ_005769

answers: crystallize

answers: NDQ_005770

answers: magma series are classified as subalkaline

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Eastern Iran can be divided into two parts: Lut Block and Flysch Zone (flysch or coloured melange of Zabol–Baluch Zone). Located to the west of Zabol–Baluch Zone, Lut Block is the main body of Eastern Iran. Lut Block extends for about 900 km in a north–south direction. It is bounded in the north by Dorooneh fault and in the south by Jazmurian depression. In the east, it is separated from Flysch Zone by the Nehbandan fault, whereas the western boundary with Central Iran is Nayband fault and Shotori Mountains. The oldest units include upper Precambrian Lower Cambrian schists overlain by Permian limestone and other Paleozoic sedimentary rocks. Flysch Zone (Zabol–Baluch) is located between Lut Block to the west and Helmand (in Afghanistan) to the east. In contrast to Lut Block, the Flysch Zone is highly deformed and tectonized and consists of thick deep-sea sediments like argillaceous and silicic shales, radiolarite, and pelagic limestone and volcanic rocks such as basalt, spilitic basalt, diabase, andesite, dacite, rhyolite, and subordinate serpentinized ultramafic rocks. The basement is likely composed of an oceanic crust. Most rock units in this zone fall into three main groups: flyschoid sediments; volcanic, volcanosedimentary, and intrusive rocks; and ophiolitic series.

text: Eastern Iran can be divided into two parts: Lut Block and Flysch Zone (

text: flysch

text: or coloured melange of Zabol–Baluch Zone). Located to the west of Zabol–Baluch Zone, Lut Block is the main body of Eastern Iran. Lut Block extends for about 900 km in a north–south direction. It is bounded in the north by Dorooneh fault and in the south by Jazmurian depression. In the east, it is separated from Flysch Zone by the Nehbandan fault, whereas the western boundary with Central Iran is Nayband fault and Shotori Mountains. The oldest units include upper Precambrian Lower Cambrian schists overlain by

text: Permian

text: limestone and other Paleozoic sedimentary rocks. Flysch Zone (Zabol–Baluch) is located between Lut Block to the west and

text: Helmand

text: (in

text: Afghanistan

text: ) to the east. In contrast to Lut Block, the Flysch Zone is highly deformed and tectonized and consists of thick deep-sea sediments like argillaceous and silicic

text: shale

text: s,

text: radiolarite

text: , and pelagic limestone and volcanic rocks such as

text: basalt

text: , spilitic basalt,

text: diabase

text: andesite

text: dacite

text: rhyolite

text: , and subordinate serpentinized ultramafic rocks. The basement is likely composed of an oceanic crust. Most rock units in this zone fall into three main groups: flyschoid sediments; volcanic, volcanosedimentary, and intrusive rocks; and ophiolitic series.

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answers: 0

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answers: The basement is likely composed of an oceanic crust

answers: NDQ_005762

answers: flyschoid sediments

answers: NDQ_005763

answers: oceanic crust

answers: NDQ_005764

answers: basement

answers: NDQ_005765

answers: flyschoid sediments

answers: NDQ_005766

answers: basalt

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answers: faster cooling forms smaller crystals

answers: NDQ_005769

answers: volcanic

answers: NDQ_005770

answers: Most rock units in this zone fall into three main groups

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The rock types consist of : Corallian Limestone (top layer), Oxford Clay, Raven-scar Limestone and Shales and Ironstone.

text: The rock types consist of :

text: Corallian Limestone

text: (top layer),

text: Oxford Clay

text: , Raven-scar Limestone and

text: Shales

text: and

text: Ironstone

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answers: Yes

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answers: slower cooling forms smaller crystals

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answers: It is out of the rock cycle.

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The park's rock formations, made famous by Robert Stevens and Harold Williams, include oceanic crust and mantle rock exposed by the obduction process of plate tectonics, as well as sedimentary rock formed during the Ordovician, Precambrian granite and Palaeozoic igneous rocks.

text: The park's rock formations, made famous by Robert Stevens and

text: Harold Williams

text: , include

text: oceanic crust

text: and

text: mantle

text: rock exposed by the

text: obduction

text: process of

text: plate tectonics

text: , as well as

text: sedimentary

text: rock formed during the

text: Ordovician

text: Precambrian

text: granite

text: and

text: Palaeozoic

text: igneous

text: rocks.

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answer: No

answer: No

answer: No

answer: No

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answer: 1

text: Abrasion is the process by which sediments are transported in the flow. The rate of erosion done using abrasion is affected by the strength of the bedrock. Abrasion is also affected by the amount of sediment load present in the river. Too much sediment and most of the particles will not have enough energy; too little and not enough of the particles will come into contact with the bed. The process can erode individual grains, or flakes from the rocks surface. The most common indicators of abrasion is potholes in the bedrock or a trough-like shape to the river. There are three types of sediment transport in a fluvial process: dissolved load, suspended load, and bed load. The process that most affects a bedrock river is the suspended load.

text: Abrasion is the process by which sediments are transported in the flow. The rate of erosion done using abrasion is affected by the strength of the bedrock. Abrasion is also affected by the amount of sediment load present in the river. Too much sediment and most of the particles will not have enough energy; too little and not enough of the particles will come into contact with the bed. The process can erode individual grains, or flakes from the rocks surface. The most common indicators of abrasion is potholes in the bedrock or a trough-like shape to the river. There are three types of sediment transport in a fluvial process: dissolved load, suspended load, and bed load. The process that most affects a bedrock river is the suspended load.

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answers: Yes

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answers: The process can erode individual grains

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answers: dissolved load

answers: NDQ_005770

answers: It is out of the rock cycle.

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Metamorphic grade is an informal indication of the amount or degree of metamorphism. A more complete indication of this intensity or degree is provided with the concept of metamorphic facies.

text: Metamorphic grade is an informal indication of the amount or degree of metamorphism. A more complete indication of this intensity or degree is provided with the concept of

text: metamorphic facies

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text: Aphanitic (a = not, phaner = visible) rocks in contrast to phaneritic rocks, typically form from lava which crystallize rapidly on or near Earth' surface. Because extrusive rocks make contact with the atmosphere they cool quickly, so the minerals do not have time to form large crystals. The individual crystals in an aphanitic igneous rock are not distinguishable to the naked eye. Examples of aphanitic igneous rock include basalt, andesite and rhyolite.

text: Aphanitic (a = not, phaner = visible) rocks in contrast to phaneritic rocks, typically form from

text: lava

text: which crystallize rapidly on or near Earth' surface. Because extrusive rocks make contact with the

text: atmosphere

text: they cool quickly, so the minerals do not have time to form large crystals. The individual crystals in an aphanitic igneous rock are not distinguishable to the naked eye. Examples of aphanitic igneous rock include

text: basalt

text: andesite

text: and

text: rhyolite

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answers: extrusive

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answer: No

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text: Canadian rock describes a wide and diverse variety of music produced by Canadians, starting with American-style Rock and roll in the mid-20th century.   Since then Canada has had a considerable impact on the development of the modern popular music called rock. Canada has produced many of the genre's most significant groups and performers, while contributing significantly to the development of the most popular subgenres, which include alternative rock, pop rock, progressive rock, country rock, folk rock, hard rock, punk rock, metal and indie rock.

text: Canadian rock

text: describes a wide and diverse variety of music produced by Canadians, starting with American-style

text: Rock and roll

text: in the mid-20th century.   Since then Canada has had a considerable impact on the development of the modern

text: popular music

text: called rock. Canada has produced many of the genre's most significant groups and performers, while contributing significantly to the development of the most popular subgenres, which include

text: alternative rock

text: pop rock

text: progressive rock

text: country rock

text: folk rock

text: hard rock

text: punk rock

text: metal

text: and

text: indie rock

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answer: No

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text: The Tuzgle volcano proper is constructed from an older rhyodacite-mafic series and a more recent series constructed from andesites alone. These and neighbouring shoshonitic centres are formed from magmas with crustal contamination. Isotope analysis of magmatic rocks have shown La/Nb ratios of 1.31.6 and Ba/Ta ratios of 160260, lower than in the main volcanic front. The overall chemical composition is potassium-rich calc-alkaline. Thermobarometry indicates that the older magmas crystallized at pressures of  while younger ones crystallized at  and temperatures of about . These magma compositions indicate that the magmas are the result of complex mixing processes and also involve the transitional nature of the mantle beneath Tuzgle, where the more northern steep slab encounters the shallower southern subducting slab. Crystal fractionation and melting of upper crustal rocks further complicate the pattern. The lava domes which were erupted from the ground after the Tuzgle ignimbrite have volumes of , while the Platform and subsequent units have volumes of . The lava domes and San Antonio lava flows have porphyritic surfaces. San Antonio lavas contain large plagioclase xenocrystals and xenoliths. The ignimbrite contains Ordovician lithic fragments and 1020% pumice. Its eruption was presumably linked to high mantle melt rates; the resulting mafic magmas induced the generation of large amounts of silicic melts. Lower mantle melt rates would form mafic melts that incorporate silicic melts before erupting.

text: The Tuzgle volcano proper is constructed from an older

text: rhyodacite

text: -mafic series and a more recent series constructed from andesites alone. These and neighbouring shoshonitic centres are formed from magmas with crustal contamination. Isotope analysis of magmatic rocks have shown

text: La

text: Nb

text: ratios of 1.31.6 and

text: Ba

text: Ta

text: ratios of 160260, lower than in the main volcanic front. The overall chemical composition is

text: potassium

text: -rich

text: calc-alkaline

text: . Thermobarometry indicates that the older magmas crystallized at pressures of  while younger ones crystallized at  and temperatures of about . These magma compositions indicate that the magmas are the result of complex mixing processes and also involve the transitional nature of the mantle beneath Tuzgle, where the more northern steep slab encounters the shallower southern subducting slab.

text: Crystal fractionation

text: and melting of upper crustal rocks further complicate the pattern. The lava domes which were erupted from the ground after the Tuzgle ignimbrite have volumes of , while the Platform and subsequent units have volumes of . The lava domes and San Antonio lava flows have porphyritic surfaces. San Antonio lavas contain large

text: plagioclase

text: xenocryst

text: als and

text: xenolith

text: s. The ignimbrite contains Ordovician lithic fragments and 1020%

text: pumice

text: . Its eruption was presumably linked to high mantle melt rates; the resulting mafic magmas induced the generation of large amounts of silicic melts. Lower mantle melt rates would form mafic melts that incorporate silicic melts before erupting.

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answer: 1

text: The rock making up Vedauwoo's characteristic hoodoos and outcrops is the 1.4 billion year old Sherman Granite. These rocks represent some of the oldest rock in Wyoming (but are still more than a billion years younger than the Tetons).  It is exposed at the surface around Vedauwoo due to the uplift of the Laramie Mountains that began around 70 million years ago.  Younger layers of rock and sediment have progressively eroded, and this continues today.  The hard granite of vedauwoo is made of large crystals of quartz, orthoclase, plagioclase, and some mica and is more erosion-resistant, resulting in wind and water-sculpted forms.  Just east of Vedauwoo, along I-80, sandstone cliffs are formed of the Permian-age Fountain Formation, which is about 300 million years old.  Ancient sand dunes of a broad desert met with the salty waters of a shallow, epicontinental sea, producing examples of cross-stratification.  Fossils of sea urchins, snails, and sea lilies can be found in some of these rocks.

text: The rock making up Vedauwoo's characteristic

text: hoodoos

text: and outcrops is the 1.4 billion year old Sherman Granite. These rocks represent some of the oldest rock in Wyoming (but are still more than a billion years younger than the

text: Tetons

text: ).  It is exposed at the surface around Vedauwoo due to the uplift of the

text: Laramie Mountains

text: that began around 70 million years ago.  Younger layers of rock and sediment have progressively eroded, and this continues today.  The hard granite of vedauwoo is made of large crystals of

text: quartz

text: orthoclase

text: plagioclase

text: , and some

text: mica

text: and is more erosion-resistant, resulting in wind and water-sculpted forms.  Just east of Vedauwoo, along I-80, sandstone cliffs are formed of the

text: Permian

text: -age

text: Fountain Formation

text: , which is about 300 million years old.  Ancient sand dunes of a broad desert met with the salty waters of a shallow, epicontinental sea, producing examples of cross-stratification.  Fossils of sea urchins, snails, and sea lilies can be found in some of these rocks.

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answers: Yes

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answers: sedimentary

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answers: uplift of the Laramie Mountains

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answers: erosion-resistant

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answers: progressively eroded

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answers: Granite

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answers: Large crystals

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answers: stratification

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answers: It is exposed at the surface around Vedauwoo

answer: No

answer: No

answer: No

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answer: 1

text: Batholiths exposed at the surface are subjected to huge pressure differences between their former location deep in the earth and their new location at or near the surface. As a result, their crystal structure expands slightly over time. This manifests itself by a form of mass wasting called exfoliation. This form of weathering causes convex and relatively thin sheets of rock to slough off the exposed surfaces of batholiths (a process accelerated by frost wedging). The result is fairly clean and rounded rock faces. A well-known result of this process is Half Dome, located in Yosemite Valley.

text: Batholiths exposed at the surface are subjected to huge pressure differences between their former location deep in the earth and their new location at or near the surface. As a result, their

text: crystal structure

text: expands slightly over time. This manifests itself by a form of

text: mass wasting

text: called

text: exfoliation

text: . This form of weathering causes convex and relatively thin sheets of rock to slough off the exposed surfaces of batholiths (a process accelerated by

text: frost wedging

text: ). The result is fairly clean and rounded rock faces. A well-known result of this process is

text: Half Dome

text: , located in

text: Yosemite Valley

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answers: Yes

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answers: sedimentary

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answers: huge pressure differences between their former location deep in the earth and their new location

answers: NDQ_005764

answers: crystal structure expands slightly

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answers: mass wasting

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answers: Batholiths

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answers: process accelerated by frost wedging

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answers: exfoliation

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answers: Exfoliation

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The Coomb Volcanic Formation occupies much of the south-west of the Wrekin Terrane and its associated inliers. The sequence is the most recent suite of Neoproterozoic rocks identified in southern Britain. The formation comprises over 1000m of sediments deposited in a subaqueous environment (in contrast to the subaerial Uriconian). Explosive ash-flow tuffs mark the initial phase of deposition followed by rhyolite flows and domes. Bimodal deposition followed with lavas, minor intrusions, ash-flows and volcaniclastic rocks with some ash-flows exhibiting Ediacaran body fossils. The geochemistry notes that fractional crystallisation process within the magma chamber links the lavas with the tuffs and gives intra-plate as well as subduction geochemical signatures.

text: The

text: Coomb Volcanic Formation

text: occupies much of the south-west of the Wrekin Terrane and its associated

text: inlier

text: s. The sequence is the most recent suite of Neoproterozoic rocks identified in southern Britain. The formation comprises over 1000m of sediments deposited in a subaqueous environment (in contrast to the subaerial Uriconian). Explosive ash-flow tuffs mark the initial phase of deposition followed by rhyolite flows and domes. Bimodal deposition followed with lavas, minor intrusions, ash-flows and volcaniclastic rocks with some ash-flows exhibiting

text: Ediacaran

text: body fossils. The geochemistry notes that

text: fractional crystallisation

text: process within the magma chamber links the lavas with the tuffs and gives

text: intra-plate

text: as well as

text: subduction

text: geochemical signatures.

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answers: Yes

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answers: extrusive

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answers: fractional crystallisation process

answers: NDQ_005764

answers: fractional crystallisation

answers: NDQ_005765

answers: deposition

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answers: volcaniclastic rocks

answers: NDQ_005768

answers: fractional crystallisation

answers: NDQ_005769

answers: fractional crystallisation

answers: NDQ_005770

answers: Volcanic Formation

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The general lack of Hadean rocks (older than 3800 Ma) might be explained by the efficiency of the processes that either cycled those rocks back into the mantle or effaced any isotopic record of their antiquity. All rocks in the continental crust are subject to metamorphism, partial melting and tectonic erosion during multiple orogenic events, and the chance of survival at the surface decreases with increasing age. In addition, a period of intense meteorite bombardment at 4.0-3.8 Ga may have pulverized all rocks at the Earth's surface. The similar age of the oldest surviving rocks and the "late heavy bombardment" may not be coincidental.

text: The general lack of Hadean rocks (older than 3800 Ma) might be explained by the efficiency of the processes that either cycled those rocks back into the mantle or effaced any isotopic record of their antiquity. All rocks in the continental crust are subject to metamorphism, partial melting and tectonic erosion during multiple orogenic events, and the chance of survival at the surface decreases with increasing age. In addition, a period of intense meteorite bombardment at 4.0-3.8 Ga may have pulverized all rocks at the Earth's surface. The similar age of the oldest surviving rocks and the "

text: late heavy bombardment

text: " may not be coincidental.

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answers: All rocks

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answers: faster cooling forms smaller crystals

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answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: 1

text: There are two main types of rock tumbling: barrel (rotary) tumbling, and vibratory tumbling. Rotary tumbling is more common, simpler, quieter and less expensive than vibratory tumblers. There are two differentiating factors, however, that may lead one to use a vibratory tumbler. First, vibratory tumbler retain the overall shape of the rough rock, whereas rotary tumblers tend to make rocks round. Thus, it is important to use vibratory tumbler to make faceted shapes and tear drop forms. Second, vibratory tumblers tend to process much faster than rotary tumblers, generally reducing the process time to half.

text: There are two main types of rock tumbling: barrel (rotary) tumbling, and vibratory tumbling. Rotary tumbling is more common, simpler, quieter and less expensive than vibratory tumblers. There are two differentiating factors, however, that may lead one to use a vibratory tumbler. First, vibratory tumbler retain the overall shape of the rough rock, whereas rotary tumblers tend to make rocks round. Thus, it is important to use vibratory tumbler to make faceted shapes and tear drop forms. Second, vibratory tumblers tend to process much faster than rotary tumblers, generally reducing the process time to half.

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text: The break-up of Pangea resulted in the break-up of the Paleozoic metamorphic basement rock. The basement rock formed half-grabens where eroded sediments from the break-up were then deposited. These sediments created the metasedimentary rocks of the La Quinta formation. Development of the passive margin occurred after rifting. Characterized by carbonate and shale, the stable passive margin allowed for large amounts of clastic sediment to deposit and stay undisturbed until burial. Some of the most important source rocks come from this stage, including the La Luna and Socuy formations. The timing of the Paleogene collision is clearly recorded in the stratigraphy of the Maracaibo basin. There is an abrupt change in sediment type of the late Cretaceous made evident by the thickly deposited, pelagic shale of the Colon formation. This represents the beginnings of the Caribbean arc collision with the South American plate. As the collision continued, this region shifted from the passive margin stage to the foreland basin stage. These Paleogene sediments are characterized by fluvial and deltaic facies and make up the Misoa formation, fluvial sandstones that act as hydrocarbon reservoirs. Mountain building begins in the late Paleogene, producing mostly continental sandstone facies.

text: hydrocarbon

text: reservoirs. Mountain building begins in the late Paleogene, producing mostly continental sandstone facies.

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answers: The La Luna and Socuy formations

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answer: No

answer: No

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text: Most rocks are metamorphic and igneous. The District has several deposits of minerals.

text: Most rocks are metamorphic and igneous. The District has several deposits of minerals.

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text: Caprock or cap rock is a harder or more resistant rock type overlying a weaker or less resistant rock type.  Common types of caprock are sandstone and mafic rock types.  In processes such as scarp retreat, the caprock controls the rate of erosion of the scarp.  As the softer rock is cut away, periodically the caprock shears off.  Caprock is also found on the top of mesa formations.

text: Caprock or cap rock is a harder or more resistant

text: rock

text: type overlying a weaker or less resistant rock type.  Common types of caprock are

text: sandstone

text: and

text: mafic rock

text: types.  In processes such as

text: scarp retreat

text: , the caprock controls the rate of erosion of the scarp.  As the softer rock is cut away, periodically the caprock shears off.  Caprock is also found on the top of

text: mesa

text: formations.

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answers: faster cooling forms smaller crystals

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answer: No

answer: No

answer: Yes

answer: No

answer: No

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text: Metamorphic rocks are altered rocks from sedimentary and igneous origin and are formed due to intense pressure and temperature. Their composition includes amphibolites, quartz feldspar, Phyllites and slate. Metamorphic rocks are largely found at the western and eastern potion of the municipality (mountainous areas facing the Pacific Ocean).

text: Metamorphic rocks are altered rocks from sedimentary and igneous origin and are formed due to intense pressure and temperature. Their composition includes amphibolites, quartz feldspar, Phyllites and slate. Metamorphic rocks are largely found at the western and eastern potion of the municipality (mountainous areas facing the

text: Pacific Ocean

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answer: No

answer: No

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text: Action of water on rock over long periods of time typically leads to weathering and water erosion, physical processes that convert solid rocks and minerals into soil and sediment, but under some conditions chemical reactions with water occur as well, resulting in metasomatism or mineral hydration, a type of chemical alteration of a rock which produces clay minerals. It also occurs when Portland cement hardens.

text: Action of water on rock over long periods of time typically leads to

text: weathering

text: and

text: water erosion

text: , physical processes that convert solid rocks and minerals into soil and sediment, but under some conditions chemical reactions with water occur as well, resulting in

text: metasomatism

text: or

text: mineral hydration

text: , a type of chemical alteration of a rock which produces

text: clay minerals

text: . It also occurs when

text: Portland cement

text: hardens.

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text: Haloclasty is a type of physical weathering caused by the growth of salt crystals. The process is first started when saline water seeps into cracks and evaporates depositing salt crystals, when the rocks are then heated, the crystals will expand putting pressure on the surrounding rock which will over time splinter the stone into fragments.

text: Haloclasty is a type of

text: physical weathering

text: caused by the growth of

text: salt crystals

text: . The process is first started when

text: saline

text: water seeps into cracks and evaporates depositing salt crystals, when the rocks are then heated, the crystals will expand putting pressure on the surrounding rock which will over time splinter the stone into fragments.

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answers: Haloclasty

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Epigenetic change (secondary processes) may be arranged under a number of headings, each of which is typical of a group of rocks or rock-forming minerals, though usually more than one of these alterations will be found in progress in the same rock. Silicification, the replacement of the minerals by crystalline or crypto-crystalline silica, is most common in felsic rocks, such as rhyolite, but is also found in serpentine, etc. Kaolinization is the decomposition of the feldspars, which are the most common minerals in igneous rocks, into kaolin (along with quartz and other clay minerals); it is best shown by granites and syenites. Serpentinization is the alteration of olivine to serpentine (with magnetite); it is typical of peridotites, but occurs in most of the mafic rocks. In uralitization, secondary hornblende replaces augite; chloritization is the alteration of augite (biotite or hornblende) to chlorite, and is seen in many diabases, diorites and greenstones. Epidotization occurs also in rocks of this group, and consists in the development of epidote from biotite, hornblende, augite or plagioclase feldspar.

text: Epigenetic change (secondary processes) may be arranged under a number of headings, each of which is typical of a group of rocks or rock-forming minerals, though usually more than one of these alterations will be found in progress in the same rock.

text: Silicification

text: , the replacement of the minerals by crystalline or crypto-crystalline silica, is most common in

text: felsic

text: rocks, such as

text: rhyolite

text: , but is also found in serpentine, etc.

text: Kaolinization

text: is the decomposition of the

text: feldspar

text: s, which are the most common minerals in igneous rocks, into

text: kaolin

text: (along with quartz and other

text: clay minerals

text: ); it is best shown by

text: granite

text: s and

text: syenite

text: s.

text: Serpentinization

text: is the alteration of

text: olivine

text: to

text: serpentine

text: (with

text: magnetite

text: ); it is typical of

text: peridotite

text: s, but occurs in most of the

text: mafic

text: rocks. In

text: uralitization

text: , secondary

text: hornblende

text: replaces

text: augite

text: chloritization

text: is the alteration of augite (biotite or hornblende) to

text: chlorite

text: , and is seen in many diabases,

text: diorite

text: s and

text: greenstones

text: Epidotization

text: occurs also in rocks of this group, and consists in the development of

text: epidote

text: from biotite, hornblende, augite or plagioclase feldspar.

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answers: rock-forming minerals

answers: NDQ_005762

answers: sedimentary

answers: NDQ_005763

answers: Epigenetic change

answers: NDQ_005764

answers: Kaolinization

answers: NDQ_005765

answers: Epigenetic change

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answers: Silicification

answers: NDQ_005769

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answers: NDQ_005770

answers: Epigenetic change

answer: Yes

answer: No

answer: Yes

answer: No

answer: No

answer: 1

text: Geologic formations are usually sedimentary rock layers, but may also be metamorphic rocks and volcanic flows.  Igneous intrusive rocks are generally not divided into formations.

text: Geologic formations are usually

text: sedimentary rock

text: layers, but may also be

text: metamorphic rocks

text: and

text: volcanic

text: flows.  Igneous intrusive rocks are generally not divided into formations.

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answers: formations

answers: NDQ_005765

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answers: NDQ_005768

answers: Igneous intrusive rocks

answers: NDQ_005769

answers: volcanic

answers: NDQ_005770

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answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Germany is located between the geologically very old (Precambrian) East European Craton (Baltica) to the north and north-east that further north is exposed as the Baltic Shield, and the geologically young (Cenozoic) Alpine-Carpathian Orogen to the south. The corresponding crustal provinces of Germany are thus geologically "middle-aged" and were accreted onto the East European Craton during the Paleozoic through plate tectonic processes. These areas form the geological basement of Germany. The basement is the oldest of the four geological crustal levels (German: Stockwerke) that overlap in Central Europe, north of the Alps. The levels mainly reflect the age relationships of rocks and the great tectonic trends that the Earth's crust was subjected to in the course of its geological history: crustal extension and widespread, mostly marine, sedimentation alternating with crustal compression/orogeny and extensive erosion. The surface geology of Germany has evolved to its current configuration due to regional differences in the action and appearance of external and internal forces over the past  20 million years. Germany can be divided into three physiographic regions: the Central European Depression, the Central European Blocks and the Alps.

text: Germany

text: is located between the geologically very old (

text: Precambrian

text: East European Craton

text: Baltica

text: ) to the north and north-east that further north is exposed as the

text: Baltic Shield

text: , and the geologically young (Cenozoic)

text: Alpine

text: Carpathian

text: Orogen

text: to the south. The corresponding

text: crustal

text: provinces of Germany are thus geologically "middle-aged" and were

text: accreted

text: onto the East European Craton during the Paleozoic through

text: plate tectonic

text: processes. These areas form the geological

text: basement

text: of Germany. The basement is the oldest of the four geological crustal levels (German: Stockwerke) that overlap in Central Europe, north of the

text: Alps

text: . The levels mainly reflect the age relationships of rocks and the great

text: tectonic

text: trends that the Earth's crust was subjected to in the course of its geological history: crustal extension and widespread, mostly marine, sedimentation alternating with crustal compression/orogeny and extensive

text: erosion

text: . The surface geology of Germany has evolved to its current configuration due to regional differences in the action and appearance of external and internal forces over the past  20 million years. Germany can be divided into three

text: physiographic regions

text: : the Central European Depression, the Central European Blocks and the Alps.

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text: In extensive regions of the Slave province of northern Canada, the magma that later became batholiths heated the surrounding rock to create metamorphic regions called aureoles about 2,575 million years ago. These regions are typically  wide. The creation of aureoles was a continuous process, but three recognizable metamorphic phases can be correlated with established deformational phases. The cycle began with a deformation phase unaccompanied by metamorphism. This evolved into the second phase accompanied by broad regional metamorphism as thermal doming began. With continued updoming of the isotherms, the third phase produced minor folding but caused major metamorphic recrystallization, resulting in the emplacement of granite at the core of the thermal dome. This phase occurred at lower pressure because of erosional unloading, but the temperatures were more extreme, ranging up to about . With deformation complete, the thermal dome decayed; minor mineralogical changes occurred during this decay phase. The region has since been effectively stable.

text: In extensive regions of the Slave province of northern Canada, the magma that later became batholiths heated the surrounding rock to create metamorphic regions called aureoles about 2,575 million years ago. These regions are typically  wide. The creation of aureoles was a continuous process, but three recognizable metamorphic phases can be correlated with established deformational phases. The cycle began with a deformation phase unaccompanied by metamorphism. This evolved into the second phase accompanied by broad regional metamorphism as thermal doming began. With continued updoming of the isotherms, the third phase produced minor folding but caused major metamorphic recrystallization, resulting in the emplacement of granite at the core of the thermal dome. This phase occurred at lower pressure because of erosional unloading, but the temperatures were more extreme, ranging up to about . With deformation complete, the thermal dome decayed; minor mineralogical changes occurred during this decay phase. The region has since been effectively stable.

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text: Some parts of Mars show inverted relief. This occurs when sediments are deposited on the floor of a stream and then become resistant to erosion, perhaps by cementation. Later the area may be buried. Eventually, erosion removes the covering layer and the former streams become visible since they are resistant to erosion. Mars Global Surveyor found several examples of this process. Many inverted streams have been discovered in various regions of Mars, especially in the Medusae Fossae Formation, Miyamoto Crater, Saheki Crater, and the Juventae Plateau.

text: Some parts of Mars show

text: inverted relief

text: . This occurs when sediments are deposited on the floor of a stream and then become resistant to erosion, perhaps by cementation. Later the area may be buried. Eventually, erosion removes the covering layer and the former streams become visible since they are resistant to erosion. Mars Global Surveyor found several examples of this process. Many inverted streams have been discovered in various regions of Mars, especially in the

text: Medusae Fossae Formation

text: Miyamoto Crater

text: Saheki Crater

text: , and the Juventae Plateau.

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answers: NDQ_005770

answers: inverted relief

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The type of rock influences the appearance of the mountain ranges very markedly, because erosion leads to very different topography depending on the hardness of the rock and its petrological structure. In addition to height and climate, other factors are the layering of the rock, its gradient and aspect, the types of waterbody and the lines of dislocation. For hard rock massifs, rugged rock faces (e.g. in the Dolomites) and mighty scree slopes are typical. By contrast, flysch or slate forms gentler mountain shapes and kuppen or domed mountaintops, because the rock is not porous, but easily shaped.

text: The type of rock influences the appearance of the mountain ranges very markedly, because

text: erosion

text: leads to very different topography depending on the

text: hardness

text: of the rock and its

text: petrological

text: structure. In addition to height and climate, other factors are the

text: layering

text: of the rock, its

text: gradient

text: and

text: aspect

text: , the types of

text: waterbody

text: and the lines of

text: dislocation

text: . For hard rock massifs, rugged rock faces (e.g. in the

text: Dolomites

text: ) and mighty

text: scree

text: slopes are typical. By contrast, flysch or slate forms gentler mountain shapes and

text: kuppen

text: or domed mountaintops, because the rock is not porous, but easily shaped.

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answers: NDQ_005761

answers: Yes

answers: NDQ_005762

answers: sedimentary

answers: NDQ_005763

answers: hardness of the rock

answers: NDQ_005764

answers: hardness

answers: NDQ_005765

answers: erosion

answers: NDQ_005766

answers: scree

answers: NDQ_005768

answers: faster cooling forms smaller crystals

answers: NDQ_005769

answers: erosion

answers: NDQ_005770

answers: It is not porous, but easily shaped

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: "Making a concentric ring around the core is the metamorphic zone. The rocks in this ring are all very old, as much as 2 billion years and older. This zone is very complex, filled with many diverse rock types. The rocks were originally sedimentary, until there was a collision between the North American continent and a terrane. This collision, called the Trans-Hudson Orogeny, caused the original rocks to fold and twist into a vast mountain range. Over the millions of years, these tilted rocks, which in many areas are tilted to 90 degrees or more, eroded. Today we see the evidence of this erosion in the Black Hills, where the metamorphic rocks end in an angular unconformity below the younger sedimentary layers.

text: "Making a concentric ring around the core is the

text: metamorphic

text: zone. The rocks in this ring are all very old, as much as 2 billion years and older. This zone is very complex, filled with many diverse rock types. The rocks were originally

text: sedimentary

text: , until there was a collision between the North American continent and a

text: terrane

text: . This collision, called the Trans-Hudson Orogeny, caused the original rocks to fold and twist into a vast mountain range. Over the millions of years, these tilted rocks, which in many areas are tilted to 90 degrees or more, eroded. Today we see the evidence of this erosion in the Black Hills, where the metamorphic rocks end in an angular

text: unconformity

text: below the younger sedimentary layers.

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answers: This zone is very complex

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answers: sedimentary

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answers: core

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answers: age

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answers: eroded

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answers: slower cooling forms smaller crystals

answers: NDQ_005769

answers: metamorphic

answers: NDQ_005770

answers: metamorphic

answer: No

answer: No

answer: No

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answer: No

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text: The main event was  Goldberg versus The Rock. Early into the match, The Rock taunted Goldberg at ringside to avoid wrestling him. As The Rock returned into the ring, Goldberg performed the Rock Bottom on him, gaining the early advantage. Goldberg attempt a spear, but The Rock dodged the spear, resulting in Goldberg hitting the ring post. The Rock took advantage over the situation, as he locked Goldberg in a sharpshooter. Goldberg broke the hold by grabbing the ring ropes and performed a successful spear on The Rock. The Rock was able to perform a spinebuster, Rock Bottom, and People's Elbow on Goldberg for a near-fall. Afterwards, Goldberg delivered two spears and a Jackhammer for the pinfall.

text: The

text: main event

text: was

text: Goldberg

text: versus

text: The Rock

text: . Early into the match, The Rock taunted Goldberg at ringside to avoid wrestling him. As The Rock returned into the ring, Goldberg performed the

text: Rock Bottom

text: on him, gaining the early advantage. Goldberg attempt a spear, but The Rock dodged the spear, resulting in Goldberg hitting the ring post. The Rock took advantage over the situation, as he locked Goldberg in a

text: sharpshooter

text: . Goldberg broke the hold by grabbing the ring ropes and performed a successful spear on The Rock. The Rock was able to perform a spinebuster, Rock Bottom, and

text: People's Elbow

text: on Goldberg for a near-fall. Afterwards, Goldberg delivered two spears and a

text: Jackhammer

text: for the pinfall.

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text: Much of the Lizard peninsula is known for its botany and geology, and about 375 million years ago the molten rock, which eventually became the Lizard, was about 10 km below the surface of the earth and under immense heat and pressure. One of the rocks (peridotite) is rich in magnesium and iron, and changed through heat and pressure to serpentinite as it pushed upwards from the Moho, the boundary of the earth's crust and mantle. It finally reached the crust's surface, about 30° south of the equator as part of an ocean ridge, in the Rheic Ocean. Over the next 80 million years the Rheic Ocean disappeared and the mass of rock heads north crossing the equator about 250 million years ago. The Tropic of Cancer is passed less than 100 million years ago and the rock, which becomes the Lizard, finally reached 50° north at about the start of the last Ice Age. There are two types of serpentine at Kynance: bastite and tremolite. The rocks at the car park, cliffs to the south and the path to the cove are bastite serpentine, which is the primary serpentine on the Lizard. The rock is coarse-grained with large shiny crystals of bastite which give a flecked appearance. The islands and stacks within the cove and the valley are of tremolite serpentine which is fine-grained and banded. Tremolite is different to the bastite serpentine because it was subject to higher pressure within the crust. Kynance Cove is an important site for geologists because of the exposures of the two types of ophiolitic serpentinite, together with granite and gneiss pods within the serpentine. The area has been designated as a Geological Conservation Review site.

text: Much of the Lizard peninsula is known for its

text: botany

text: and

text: geology

text: , and about 375 million years ago the molten rock, which eventually became the Lizard, was about 10 km below the surface of the earth and under immense heat and pressure. One of the rocks (

text: peridotite

text: ) is rich in

text: magnesium

text: and

text: iron

text: , and changed through heat and pressure to

text: serpentinite

text: as it pushed upwards from the

text: Moho

text: , the boundary of the earth's

text: crust

text: and

text: mantle

text: . It finally reached the crust's surface, about 30° south of the

text: equator

text: as part of an

text: ocean ridge

text: , in the

text: Rheic Ocean

text: . Over the next 80 million years the Rheic Ocean disappeared and the mass of rock heads north crossing the equator about 250 million years ago. The

text: Tropic of Cancer

text: is passed less than 100 million years ago and the rock, which becomes the Lizard, finally reached 50° north at about the start of the last

text: Ice Age

text: . There are two types of serpentine at Kynance: bastite and tremolite. The rocks at the car park, cliffs to the south and the path to the cove are bastite serpentine, which is the primary serpentine on the Lizard. The rock is coarse-grained with large shiny crystals of bastite which give a flecked appearance. The islands and stacks within the cove and the valley are of tremolite serpentine which is fine-grained and banded. Tremolite is different to the bastite serpentine because it was subject to higher pressure within the crust. Kynance Cove is an important site for geologists because of the exposures of the two types of

text: ophiolitic

text: serpentinite, together with granite and gneiss pods within the serpentine. The area has been designated as a

text: Geological Conservation Review

text: site.

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text: Rock Band also supports migration of content across games. This enables players to access music that was featured in other Rock Band titles within a single game. Rock Band 2 currently supports content imported from the original Rock Band, Lego Rock Band, and Green Day: Rock Band. Rock Band 3 allows players to not only access these songs but content exported from Rock Band 2 as well. While Lego Rock Band and Green Day: Rock Band allow players to export the full soundtrack from each game, Rock Band loses three songs from its soundtrack (four in the European version) during the export process due to licensing restrictions. Rock Band 2, likewise, will not allow players to export fourteen of the eighty-four songs offered on the disc (however nine of these missing songs were offered as a free download following the release of Rock Band 3). Two additional songs from the original Rock Band export were previously unavailable within Rock Band 3, however they have since been returned to availability through a patch. Two further songs which were released on-disc in the European version are unavailable in Rock Band 3, regardless of whether the songs were obtained through a disc export or through purchase as DLC (for the North American region). Due to the licensing agreement with Apple Corps, The Beatles: Rock Band does not allow any exporting of its content whatsoever. Rock Band Blitz shipped with twenty-five songs on its soundtrack (twenty-three of which are new, two of which were offered in Rock Band 2 but not exportable to 3) and all twenty-five songs are cross-compatible with Rock Band 3. Blitz itself is also able to use the full range of content offered on the Rock Band downloadable content catalog (including future content, previous imports, and RBN songs), integrating the existing charts into its own gameplay system. Harmonix is working to assure that as much as a player's existing song library will be playable within Rock Band 4 within the same console family.

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answer: No

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text: Erosion by moving water can happen in two ways. Firstly, the movement of water across the bed exerts a shear stress directly onto the bed. If the cohesive strength of the substrate is lower than the shear exerted, or the bed is composed of loose sediment which can be mobilized by such stresses, then the bed will be lowered purely by clearwater flow. However, if the river carries significant quantities of sediment, this material can act as tools to enhance wear of the bed (abrasion). At the same time the fragments themselves are ground down, becoming smaller and more rounded (attrition).

text: Erosion by moving water can happen in two ways. Firstly, the movement of water across the

text: bed

text: exerts a

text: shear stress

text: directly onto the bed. If the

text: cohesive

text: strength of the substrate is lower than the shear exerted, or the bed is composed of loose sediment which can be mobilized by such stresses, then the bed will be lowered purely by clearwater flow. However, if the river carries significant quantities of sediment, this material can act as tools to enhance wear of the bed (

text: abrasion

text: ). At the same time the fragments themselves are ground down, becoming smaller and more rounded (attrition).

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answers: Yes

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answers: sedimentary

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answers: cohesive strength of the substrate

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answers: cohesive strength

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answers: Attrition

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answers: attrition

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answers: Erosion

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Volcanism is the process that takes place at divergent boundaries by which one tectonic plate separates from another creating a rift in which molten rock (magma) erupts onto the surface of the Earth. This molten rock magma then cools and crystallizes, forming igneous rocks. If crystallization occurs at the Earth´s surface, extrusive igneous rocks are formed; if crystallization occurs within the Earth´s lithosphere, intrusive igneous rocks are formed which can then be brought to Earth´s surface by denudation.

text: Volcanism

text: is the process that takes place at divergent boundaries by which one

text: tectonic plate

text: separates from another creating a

text: rift

text: in which molten rock (

text: magma

text: ) erupts onto the surface of the

text: Earth

text: . This molten rock

text: magma

text: then cools and crystallizes, forming igneous rocks. If crystallization occurs at the Earth´s surface, extrusive

text: igneous rocks

text: are formed; if crystallization occurs within the Earth´s

text: lithosphere

text: , intrusive igneous rocks are formed which can then be brought to Earth´s surface by

text: denudation

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answers: Yes

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answers: intrusive

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answers: crystallization occurs at the Earth  s surface

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answers: crystallization

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answers: This molten rock magma then cools and crystallizes

answers: NDQ_005769

answers: crystallization

answers: NDQ_005770

answers: igneous rocks

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The exposed rock types in the vicinity of the thermal springs are sedimentary rocks of Mississippian to Ordovician age, with the exception of younger igneous rocks (Cretaceous age) exposed in two small areas about   southeast of the thermal springs (Potash Sulphur Spring and Magnet Cove, respectively), and in many small dikes and sills. Most dikes are less than  wide. There have been 80 dikes noted about  southeast of Hot Springs, on and near the Ouachita River.  There is no indication that igneous rock occurs where the thermal springs discharge.

text: The exposed rock types in the vicinity of the thermal springs are

text: sedimentary rock

text: s of

text: Mississippian

text: to

text: Ordovician

text: age, with the exception of younger

text: igneous rock

text: s (

text: Cretaceous

text: age) exposed in two small areas about   southeast of the thermal springs (Potash Sulphur Spring and

text: Magnet Cove

text: , respectively), and in many small

text: dikes

text: and

text: sills

text: . Most dikes are less than  wide. There have been 80 dikes noted about  southeast of Hot Springs, on and near the

text: Ouachita River

text: .  There is no indication that igneous rock occurs where the thermal springs discharge.

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answers: Younger igneous rocks

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answers: thermal spring

answers: NDQ_005770

answers: sedimentary rocks

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The ANS took about 300 million years to form. The oldest rocks associated with the formative cycle of the ANS crust formed by coalescence of Island arcs and back-arc basins and perhaps oceanic plateaus. The oldest rocks associated with this cycle are about 870 million years old and are found in eastern Sudan and SE Arabia. Some of the oldest rocks are ophiolites, which testify that formation of ANS continental crust began with formation of oceanic crust by seafloor spreading, followed by the development of subduction zones and Island arcs. The various island arcs collided and these tectonic terranes sutured together during the time period 780 to 620 Ma to form an increasingly broad and thick nucleus of juvenile continental crust. This thickening resulted in the formation of several suture zones, marked by obduction of ophiolites and intense deformation. Crustal thickening was also accompanied by melting and magmatic fractionation of mafic magmas that ponded deep in the crust. These melts rose upwards to be emplaced as granitic plutons. Magmatism during this episode is characterized by tholeiites and calc-alkaline suites.

text: The ANS took about 300 million years to form. The oldest rocks associated with the formative cycle of the ANS crust formed by coalescence of

text: Island arc

text: s and

text: back-arc basins

text: and perhaps oceanic plateaus. The oldest rocks associated with this cycle are about 870 million years old and are found in eastern Sudan and SE Arabia. Some of the oldest rocks are

text: ophiolites

text: , which testify that formation of ANS

text: continental crust

text: began with formation of

text: oceanic crust

text: by

text: seafloor spreading

text: , followed by the development of

text: subduction zones

text: and

text: Island arc

text: s. The various island arcs collided and these

text: tectonic terranes

text: sutured together during the time period 780 to 620 Ma to form an increasingly broad and thick nucleus of juvenile continental crust. This thickening resulted in the formation of several

text: suture zones

text: , marked by

text: obduction

text: of ophiolites and intense deformation. Crustal thickening was also accompanied by melting and magmatic fractionation of mafic magmas that ponded deep in the crust. These melts rose upwards to be emplaced as

text: granitic

text: plutons

text: . Magmatism during this episode is characterized by

text: tholeiite

text: s and

text: calc-alkaline

text: suites.

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answers: This thickening resulted in the formation of several suture zones

answer: No

answer: No

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answer: No

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text: Soil erosion (especially from agricultural activity) is considered to be the leading global cause of diffuse water pollution, due to the effects of the excess sediments flowing into the world's waterways. The sediments themselves act as pollutants, as well as being carriers for other pollutants, such as attached pesticide molecules or heavy metals.

text: Soil erosion (especially from agricultural activity) is considered to be the leading global cause of diffuse

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text: , due to the effects of the excess sediments flowing into the world's waterways. The sediments themselves act as pollutants, as well as being carriers for other pollutants, such as attached pesticide molecules or heavy metals.

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text: A list of rock types recognized by petrologists. There is no agreed number of specific types of rocks. Any unique combination of chemical composition, mineralogy, grain size, texture, or other distinguishing characteristics can describe rock types. Additionally, different classification systems exist for each major type of rock.

text: A list of

text: rock

text: types recognized by

text: petrologists

text: . There is no agreed number of specific types of rocks. Any unique combination of chemical composition, mineralogy, grain size, texture, or other distinguishing characteristics can describe rock types. Additionally, different classification systems exist for each major type of rock.

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answers: Yes

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answers: rocks are classified into four major groups

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answers: It is out of the rock cycle

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 0

text: Detritus (; adjective detrital ) is particles of rock derived from pre-existing rock through processes of weathering and erosion. A fragment of detritus is called a clast. Detrital particles can consist of lithic fragments (particles of recognisable rock), or of monomineralic fragments (mineral grains). Particles may be transported to riverbeds, lakes, or oceans, forming sedimentary successions. Diagenetic processes can transform these sediments into rock through cementation and lithification, forming sedimentary rocks such as sandstone. These rocks can then in turn again be weathered and eroded to form a second generation of sediment.

text: Detritus (; adjective detrital ) is particles of

text: rock

text: derived from pre-existing rock through processes of

text: weathering

text: and

text: erosion

text: . A fragment of detritus is called a

text: clast

text: . Detrital particles can consist of

text: lithic fragments

text: (particles of recognisable rock), or of monomineralic fragments (mineral grains). Particles may be transported to riverbeds, lakes, or oceans, forming sedimentary successions.

text: Diagenetic

text: processes can transform these sediments into rock through

text: cementation

text: and

text: lithification

text: , forming sedimentary rocks such as sandstone. These rocks can then in turn again be weathered and eroded to form a second generation of sediment.

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answers: Particles may be transported to riverbeds, lakes, or oceans

answers: NDQ_005762

answers: sedimentary

answers: NDQ_005763

answers: Detritus

answers: NDQ_005764

answers: lithification

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answers: weathering

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answers: sandstone

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answers: slower cooling forms smaller crystals

answers: NDQ_005769

answers: weathering

answers: NDQ_005770

answers: These rocks can then in turn again be weathered and eroded

answer: Yes

answer: No

answer: Yes

answer: No

answer: No

answer: 1

text: Ringing rocks are rocks that have the property of resonating like a bell when struck, such as the Musical Stones of Skiddaw in the English Lake District as well as the stones in Ringing Rocks Park, in Upper Black Eddy, Bucks County, Pennsylvania United States, the Ringing Rocks of Kiandra, near Cooma, NSW and also the Bell Rock Range of Western Australia.  Ringing rocks are also known as sonorous rocks or lithophonic rocks, as used in idiophonic musical instruments called lithophones.

text: Ringing rocks are rocks that have the property of resonating like a bell when struck, such as the

text: Musical Stones of Skiddaw

text: in the English

text: Lake District

text: as well as the stones in Ringing Rocks Park, in

text: Upper Black Eddy

text: Bucks County

text: Pennsylvania

text: United States, the Ringing Rocks of Kiandra, near Cooma, NSW and also the Bell Rock Range of Western Australia.  Ringing rocks are also known as sonorous rocks or

text: lithophonic

text: rocks, as used in

text: idiophonic

text: musical instruments called

text: lithophone

text: s.

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answers: Yes

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answers: intrusive

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answers: property of resonating like a bell

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answers: resonating

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answers: Ringing rocks

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answers: lithophonic

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answers: Ringing rocks

answers: NDQ_005769

answers: Black Eddy

answers: NDQ_005770

answers: The property of resonating like a bell when struck

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Geologically speaking, Colombian emeralds are said to be the purest emeralds in the world because Colombian emerald deposits are the only ones on earth found in sedimentary host rock rather than in Igneous rock. The tectonic movements that created the Andes Mountains force the raw materials of emeralds—beryllium, chromium, and vanadium—found in the ground into liquid and gaseous states. These materials, in such states, find their way into cracks in the already sedimentary medium surrounding them and then eventually cool and crystallize. A saline solution found in the sedimentary rock eventually washes out impurities such as iron that cloud other beryls from forming onto the crystallizing stone. This intricate process produces the emeralds found in the mines of Colombia.

text: Geologically speaking, Colombian emeralds are said to be the purest emeralds in the world because Colombian emerald deposits are the only ones on earth found in sedimentary host rock rather than in

text: Igneous rock

text: . The tectonic movements that created the Andes Mountains force the raw materials of emeralds—beryllium, chromium, and vanadium—found in the ground into liquid and gaseous states. These materials, in such states, find their way into cracks in the already sedimentary medium surrounding them and then eventually cool and crystallize. A saline solution found in the sedimentary rock eventually washes out impurities such as iron that cloud other beryls from forming onto the crystallizing stone. This intricate process produces the emeralds found in the mines of Colombia.

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answers: slower cooling forms smaller crystals

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answer: No

answer: No

answer: No

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text: The primary mechanism of soil creation is the weathering of rock. All rock types (igneous rock, metamorphic rock and sedimentary rock) may be broken down into small particles to create soil. Weathering mechanisms are physical weathering, chemical weathering, and biological weathering  Human activities such as excavation, blasting, and waste disposal, may also create soil. Over geologic time, deeply buried soils may be altered by pressure and temperature to become metamorphic or sedimentary rock, and if melted and solidified again, they would complete the geologic cycle by becoming igneous rock.

text: The primary mechanism of soil creation is the weathering of rock. All rock types (

text: igneous rock

text: metamorphic rock

text: and

text: sedimentary rock

text: ) may be broken down into small particles to create soil. Weathering mechanisms are physical weathering, chemical weathering, and biological weathering  Human activities such as excavation, blasting, and waste disposal, may also create soil. Over geologic time, deeply buried soils may be altered by pressure and temperature to become metamorphic or sedimentary rock, and if melted and solidified again, they would complete the geologic cycle by becoming igneous rock.

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answer: No

answer: No

answer: Yes

answer: No

answer: No

answer: 1

text: Rocks are geologically classified according to characteristics such as mineral and chemical composition, permeability, the texture of the constituent particles, and particle size. These physical properties are the end result of the processes that formed the rocks. Over the course of time, rocks can transform from one type into another, as described by the geological model called the rock cycle. These events produce three general classes of rock: igneous, sedimentary, and metamorphic.

text: Rocks are geologically classified according to characteristics such as mineral and chemical composition,

text: permeability

text: , the

text: texture

text: of the constituent particles, and

text: particle size

text: . These physical properties are the end result of the processes that formed the rocks. Over the course of time, rocks can transform from one type into another, as described by the geological model called the

text: rock cycle

text: . These events produce three general classes of rock:

text: igneous

text: sedimentary

text: , and

text: metamorphic

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text: The weathering of many rock types produce clay minerals as one of its last products. The understanding of these geochemical processes is also important for the understanding of geological evolution of landscapes and macroscopic properties of rocks and sediments. Presence of clay minerals in Mars, detected by the Mars Reconnaissance Orbiter in 2009 was another strong evidence of the existence of water on the planet in previous geological eras.

text: The

text: weathering

text: of many rock types produce clay minerals as one of its last products. The understanding of these geochemical processes is also important for the understanding of geological evolution of landscapes and macroscopic properties of rocks and sediments. Presence of clay minerals in

text: Mars

text: , detected by the

text: Mars Reconnaissance Orbiter

text: in 2009 was another strong evidence of the existence of water on the planet in previous geological eras.

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text: Crystal Rock features 12 distribution centers, and the Company manufactures and markets its own water and coffee brands, including Crystal Rock Waters, Vermont Pure Natural Spring Water and Cool Beans Coffee. Crystal Rock also features water filtration and dispensing systems, a variety of "small package waters" and a "robust coffee portfolio" that includes authorized dealer status for Keurig and Green Mountain coffee products.

text: Crystal Rock features 12 distribution centers, and the Company manufactures and markets its own water and coffee brands, including Crystal Rock Waters, Vermont Pure Natural Spring Water and Cool Beans Coffee. Crystal Rock also features water filtration and dispensing systems, a variety of "small package waters" and a "robust coffee portfolio" that includes authorized dealer status for Keurig and Green Mountain coffee products.

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text: The best specimens of the architecture of the Salasthambha period are the remains of the five rock-cut caves at Jogighopa on the bank of the Brahmaputra in the district of Bongaigaon. These are the unique examples of rock-cut architecture in Assam. Though these rock-cut caves are not of such architectural interest as those in Western India, these remains at Jogighopa are the clear evidence of the fact that Assam was not outside the movement of this particular type of art developed in India as it will be seen from description of the best preserved cave noticed at Jogighopa.

text: The best specimens of the architecture of the Salasthambha period are the remains of the five rock-cut caves at Jogighopa on the bank of the Brahmaputra in the district of Bongaigaon. These are the unique examples of rock-cut architecture in Assam. Though these rock-cut caves are not of such architectural interest as those in Western India, these remains at Jogighopa are the clear evidence of the fact that Assam was not outside the movement of this particular type of art developed in India as it will be seen from description of the best preserved cave noticed at Jogighopa.

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text: Metamorphic events may span multiple deformations. Sometimes it is useful to identify them similarly to the structural features for which they are responsible, e.g.; M. This may be possible by observing porphyroblast formation in cleavages of known deformation age, by identifying metamorphic mineral assemblages created by different events, or via geochronology.

text: Metamorphic events may span multiple deformations. Sometimes it is useful to identify them similarly to the structural features for which they are responsible, e.g.; M. This may be possible by observing

text: porphyroblast

text: formation in cleavages of known deformation age, by identifying metamorphic mineral assemblages created by different events, or via

text: geochronology

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text: The newly erupted volcanic material is subject to rapid erosion depending on the climate conditions. These sediments accumulate within the basins on either side of an island arc. As the sediments become more deeply buried lithification begins and sedimentary rock results.

text: The newly erupted volcanic material is subject to rapid erosion depending on the climate conditions. These sediments accumulate within the basins on either side of an island arc. As the sediments become more deeply buried lithification begins and sedimentary rock results.

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text: In geology, a large igneous province (LIP) is an extremely large accumulation of igneous rocks, including liquid rock (intrusive) or volcanic rock formations (extrusive), arising when hot magma extrudes from inside the Earth and flows out. The source of many or all LIPs is variously attributed to mantle plumes or to processes associated with plate tectonics. Types of LIPs can include large volcanic provinces (LVP), created through flood basalt, and large plutonic provinces (LPP). Rampino and Stothers (1988) cite eleven distinct flood-basalt episodes - occurring in the past 250 million years - which created volcanic provinces and plateaus and coincided with mass extinctions. However, more flood basalts have been recognized, such as the large Ontong Java Plateau, and the medium-sized Chilcotin Group, though the latter may be linked to the Columbia River Basalt Group. Formation depends on a range of factors, such as continental configuration, latitude, volume, rate, duration of eruption, style and setting (continental vs. oceanic), the pre-existing climate state, and the biota resilience to change.

text: In

text: geology

text: , a large igneous province (LIP) is an extremely large accumulation of

text: igneous rock

text: s, including liquid rock (

text: intrusive

text: ) or volcanic rock formations (

text: extrusive

text: ), arising when hot magma extrudes from inside the Earth and flows out. The source of many or all LIPs is variously attributed to

text: mantle plume

text: s or to processes associated with

text: plate tectonic

text: s. Types of LIPs can include large volcanic provinces (LVP), created through

text: flood basalt

text: , and large plutonic provinces (LPP). Rampino and Stothers (1988) cite eleven distinct flood-basalt episodes - occurring in the past 250 million years - which created volcanic provinces and plateaus and coincided with

text: mass extinctions

text: . However, more flood basalts have been recognized, such as the large

text: Ontong Java Plateau

text: , and the medium-sized

text: Chilcotin Group

text: , though the latter may be linked to the

text: Columbia River Basalt Group

text: . Formation depends on a range of factors, such as continental configuration, latitude, volume, rate, duration of eruption, style and setting (continental vs. oceanic), the pre-existing

text: climate state

text: , and the biota resilience to change.

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answer: No

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text: The main physical Weathering process on beaches is salt-crystal growth. Wind carries salt spray onto rocks, where it is absorbed into small pores and cracks within the rocks. There the water evaporates and the salt crystallises, creating pressure and often breaking down the rock. In some beaches calcium carbonate is able to bind together other sediments to form beachrock and in warmer areas dunerock. Wind erosion is also a form of erosion, dust and sand is carried around in the air and slowly erodes rock, this happens in a similar way in the sea were the salt and sand is washed up onto the rocks.

text: The main physical Weathering process on beaches is

text: salt-crystal growth

text: . Wind carries salt spray onto rocks, where it is absorbed into small pores and cracks within the rocks. There the water evaporates and the salt crystallises, creating pressure and often breaking down the rock. In some beaches calcium carbonate is able to bind together other sediments to form

text: beachrock

text: and in warmer areas

text: dunerock

text: . Wind erosion is also a form of erosion, dust and sand is carried around in the air and slowly erodes rock, this happens in a similar way in the sea were the salt and sand is washed up onto the rocks.

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answer: No

answer: No

answer: No

answer: No

answer: No

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text: By recrystallization in this manner peculiar rocks of very distinct types are often produced.  Thus shales may pass into cordierite rocks, or may show large crystals of andalusite (and chiastolite), staurolite, garnet, kyanite and sillimanite, all derived from the aluminous content of the original shale.  A considerable amount of mica (both muscovite and biotite) is often simultaneously formed, and the resulting product has a close resemblance to many kinds of schist.  Limestones, if pure, are often turned into coarsely crystalline marbles; but if there was an admixtureof clay or sand in the original rock such minerals as garnet, epidote, idocrase, wollastonite, will be present.  Sandstones when greatly heated may change into coarse quartzites composed of large clear grains of quartz.  These more intense stages of alteration are notso commonly seen in igneous rocks, because their minerals, being formed at high temperatures, are not so easily transformed or recrystallized.

text: By recrystallization in this manner peculiar rocks of very distinct types are often produced.  Thus shales may pass into

text: cordierite

text: rocks, or may show large crystals of

text: andalusite

text: (and

text: chiastolite

text: staurolite

text: garnet

text: kyanite

text: and

text: sillimanite

text: , all derived from the aluminous content of the original shale.  A considerable amount of

text: mica

text: (both muscovite and biotite) is often simultaneously formed, and the resulting product has a close resemblance to many kinds of schist.  Limestones, if pure, are often turned into coarsely crystalline marbles; but if there was an admixtureof clay or sand in the original rock such minerals as garnet,

text: epidote

text: idocrase

text: , wollastonite, will be present.  Sandstones when greatly heated may change into coarse quartzites composed of large clear grains of quartz.  These more intense stages of alteration are notso commonly seen in igneous rocks, because their minerals, being formed at high temperatures, are not so easily transformed or recrystallized.

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answers: recrystallization

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answers: By recrystallization

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: MC5 was an American rock band from Lincoln Park, Michigan, formed in 1964. The original band line-up consisted of vocalist Rob Tyner, guitarists Wayne Kramer and Fred "Sonic" Smith, bassist Michael Davis, and drummer Dennis Thompson. "Crystallizing the counterculture movement at its most volatile and threatening", according to AllMusic critic Stephen Thomas Erlewine, the MC5's far left political ties and anti-establishment lyrics and music positioned them as emerging innovators of the punk movement in the United States. Their loud, energetic style of back-to-basics rock and roll included elements of garage rock, hard rock, blues rock, and psychedelic rock.

text: MC5 was an

text: American

text: rock

text: band from

text: Lincoln Park, Michigan

text: , formed in 1964. The original band line-up consisted of vocalist

text: Rob Tyner

text: , guitarists

text: Wayne Kramer

text: and

text: Fred "Sonic" Smith

text: , bassist

text: Michael Davis

text: , and drummer

text: Dennis Thompson

text: . "Crystallizing the

text: counterculture movement

text: at its most volatile and threatening", according to

text: AllMusic

text: critic

text: Stephen Thomas Erlewine

text: , the MC5's

text: far left

text: political ties and

text: anti-establishment

text: lyrics and music positioned them as emerging innovators of the

text: punk movement

text: in the United States. Their loud, energetic style of back-to-basics

text: rock and roll

text: included elements of

text: garage rock

text: hard rock

text: blues rock

text: , and

text: psychedelic rock

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answers: Faster cooling forms larger crystals

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answers: MC5

answer: No

answer: No

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text: Hydrogen-ion metasomatism is the process that causes phyllic alteration. While the mineralogy of the rock is altered throughout, texture is preserved and primary porphyry structure (including position of original veins) may still be visible. If a rock undergoes phyllic alteration, then orthoclase feldspar, biotite and various silicates are altered in addition to plagioclase. Plagioclase will be altered to sericite (a fine-grained white mica) by sericitic alteration, and mafic minerals are replaced by quartz. Tourmaline may appear as radiating aggregate or prismatic crystals between the quartz-sericite assemblage. Phyllic alteration is often closely associated with argillic alteration, which occurs at lower temperatures and dominantly affects plagioclase.

text: Hydrogen-ion

text: metasomatism

text: is the process that causes phyllic alteration. While the

text: mineralogy

text: of the rock is altered throughout,

text: texture

text: is preserved and primary porphyry structure (including position of original veins) may still be visible. If a rock undergoes phyllic alteration, then

text: orthoclase

text: feldspar,

text: biotite

text: and various silicates are altered in addition to plagioclase. Plagioclase will be altered to sericite (a fine-grained white mica) by

text: sericitic alteration

text: , and mafic minerals are replaced by quartz.

text: Tourmaline

text: may appear as radiating aggregate or prismatic crystals between the quartz-sericite assemblage. Phyllic alteration is often closely associated with

text: argillic alteration

text: , which occurs at lower temperatures and dominantly affects plagioclase.

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text: Large, striking and uniquely shaped white sandstone and quartz rocks are found throughout the Bear Rocks Preserve area. Erosion has carved bowl-shaped cavities in many of these wind- and rain-sculpted sandstone boulders and these cavities are often filled with water (or ice) and algae. In addition to the sculpted boulders are "rock streams" formed during glacial periods. The freeze-thaw cycles heaved and split rock, creating rock streams up to  wide and hundreds of feet long. Other rock patterns include polygons and circles.

text: Large, striking and uniquely shaped white sandstone and quartz rocks are found throughout the Bear Rocks Preserve area. Erosion has carved bowl-shaped cavities in many of these wind- and rain-sculpted sandstone boulders and these cavities are often filled with water (or ice) and algae. In addition to the sculpted boulders are "rock streams" formed during glacial periods. The freeze-thaw cycles heaved and split rock, creating rock streams up to  wide and hundreds of feet long. Other rock patterns include polygons and circles.

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text: Rock and roll, acoustic, alternative rock, art rock, Britpop, blues rock, experimental rock, French rock, folk rock, funk rock, garage rock, glam rock, gothic rock, hard rock, indie rock, jam rock, post-Britpop, progressive rock, pop rock, psychedelia, punk rock, roots rock, space rock, steady and symphonic rock.

text: Rock and roll

text: , acoustic,

text: alternative rock

text: art rock

text: Britpop

text: blues rock

text: experimental rock

text: French rock

text: folk rock

text: funk rock

text: garage rock

text: glam rock

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text: hard rock

text: indie rock

text: jam rock

text: post-Britpop

text: progressive rock

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text: psychedelia

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answers: garage rock

answers: NDQ_005768

answers: symphonic rock

answers: NDQ_005769

answers: garage rock

answers: NDQ_005770

answers: rock

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: By 1835, his brother Henry was state geologist of Pennsylvania, and together the brothers unfolded the historical geology of the Appalachian chain. Among their joint special investigations were the study of the solvent action of water on various minerals and rocks, and the demonstration that "coal beds stand in close genetic relation to the amount of disturbance to which the inclosing strata have been submitted, the coal becoming harder and containing less volatile matter as the evidence of the disturbance increases". In modern terms, this was the realization that the geological process of metamorphism had gradually transformed softer grades of coal, such as lignite, into harder grades, such as anthracite.

text: By 1835, his brother Henry was state geologist of

text: Pennsylvania

text: , and together the brothers unfolded the historical geology of the

text: Appalachian

text: chain. Among their joint special investigations were the study of the solvent action of water on various minerals and rocks, and the demonstration that "coal beds stand in close genetic relation to the amount of disturbance to which the inclosing strata have been submitted, the coal becoming harder and containing less volatile matter as the evidence of the disturbance increases". In modern terms, this was the realization that the geological process of

text: metamorphism

text: had gradually transformed softer grades of coal, such as

text: lignite

text: , into harder grades, such as

text: anthracite

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answers: 4

answers: NDQ_005761

answers: geological process

answers: NDQ_005762

answers: sedimentary

answers: NDQ_005763

answers: the amount of disturbance

answers: NDQ_005764

answers: harder

answers: NDQ_005765

answers: metamorphism

answers: NDQ_005766

answers: lignite

answers: NDQ_005768

answers: faster cooling forms smaller crystals

answers: NDQ_005769

answers: volatile matter

answers: NDQ_005770

answers: metamorphism

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Thus, assigning age significance to a result requires studying the metasomatic and thermal history of the rock, any metamorphic events, and any evidence of fluid movement. A Rb-Sr date which is at variance with other geochronometers may not be useless, it may be providing data on an event which is not representing the age of formation of the rock.

text: Thus, assigning age significance to a result requires studying the metasomatic and thermal history of the rock, any metamorphic events, and any evidence of fluid movement. A Rb-Sr date which is at variance with other geochronometers may not be useless, it may be providing data on an event which is not representing the age of formation of the rock.

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answers: Rocks are part of the rock cycle

answers: NDQ_005762

answers: sedimentary

answers: NDQ_005763

answers: fluid movement

answers: NDQ_005764

answers: age

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answers: NDQ_005766

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answers: NDQ_005768

answers: Rb-Sr

answers: NDQ_005769

answers: metamorphic

answers: NDQ_005770

answers: metamorphic events

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The inner trench wall marks the edge of the overriding plate and the outermost forearc.  The forearc consists of igneous and metamorphic crust, and this crust acts as buttress to a growing accretionary prism (sediments scraped off the downgoing plate onto the inner trench wall, depending on how much sediment is supplied to the trench).  If the flux of sediments is high, material will be transferred from the subducting plate to the overriding plate.  In this case an accretionary prism grows and the location of the trench migrates progressively away from the volcanic arc over the life of the convergent margin. Convergent margins with growing accretionary prisms are called accretionary convergent margins and make up nearly half of all convergent margins.  If the sediment flux is low, material will be transferred from the overriding plate to the subducting plate by a process of tectonic ablation known as subduction erosion and carried down the subduction zone.  Forearcs undergoing subduction erosion typically expose igneous rocks.  In this case, the location of the trench will migrate towards the magmatic arc over the life of the convergent margin. Convergent margins experiencing subduction erosion are called nonaccretionary convergent margins and comprise more than half of convergent plate boundaries. This is an oversimplification, because different parts of a convergent margin can  experience sediment accretion and subduction erosion over its life.

text: The inner trench wall marks the edge of the overriding plate and the outermost forearc.  The forearc consists of

text: igneous

text: and

text: metamorphic

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

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answers: Yes

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answers: sedimentary

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answers: sediment flux

answers: NDQ_005764

answers: location of the trench

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answers: sediment accretion

answers: NDQ_005766

answers: igneous

answers: NDQ_005768

answers: faster cooling forms smaller crystals

answers: NDQ_005769

answers: subduction erosion

answers: NDQ_005770

answers: The inner trench wall marks the edge of the overriding plate

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The Eastern Andes Metamorphic Complex is a large coherent but varied group of metamorphic and sedimentary rocks –in other words a geologic complex– that crops out in the eastern Patagonian Andes in Chile and Argentina. The metamorphic grade of rocks varies but does not exceed greenschist facies, the only exception to this are rocks near plutons affected by contact metamorphism. The sedimentary protoliths sedimented in the Late Paleozoic. The pressures and temperatures of metamorphism of the Eastern Andes Metamorphic Complex are different those usually expected from accretionary complexes. The sedimentary protoliths of the Eastern Andes Metamorphic Complex were likely deposited in a passive continental margin.

text: The Eastern Andes Metamorphic Complex is a large coherent but varied group of

text: metamorphic

text: and

text: sedimentary rock

text: s –in other words a

text: geologic complex

text: – that

text: crops out

text: in the eastern

text: Patagonia

text: n

text: Andes

text: in Chile and Argentina. The

text: metamorphic grade

text: of rocks varies but does not exceed

text: greenschist facies

text: , the only exception to this are rocks near

text: pluton

text: s affected by

text: contact metamorphism

text: . The sedimentary

text: protolith

text: s sedimented in the

text: Late Paleozoic

text: . The pressures and temperatures of metamorphism of the Eastern Andes Metamorphic Complex are different those usually expected from

text: accretionary complex

text: es. The

text: sedimentary

text: protolith

text: s of the Eastern Andes Metamorphic Complex were likely deposited in a

text: passive continental margin

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answers: The Eastern Andes Metamorphic Complex

answers: NDQ_005762

answers: sedimentary

answers: NDQ_005763

answers: pressures and temperatures

answers: NDQ_005764

answers: pressures and temperatures

answers: NDQ_005765

answers: metamorphism

answers: NDQ_005766

answers: greenschist

answers: NDQ_005768

answers: slower cooling forms smaller crystals

answers: NDQ_005769

answers: metamorphism

answers: NDQ_005770

answers: Metamorphism

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The Timanide Orogen (, literally: "Protouralian–Timanide Orogen") is a pre-Uralian orogen that formed in northeastern Baltica during the Neoproterozoic in the Timanide orogeny. The orogen is about 3000 km long. Its extreme points include the southern Urals in the south and the Polar Urals, the Kanin and Varanger peninsulas in the north. The Timan Ridge is the type area of the orogen. To the west, at the Varanger Peninsula, the north-west oriented Timanide Orogen is truncated by the younger Scandinavian Caledonide Orogen that has an oblique disposition. The northeastern parts of the orogen are made up of volcanic and sedimentary rocks, granitoids and few ophiolites. In contrast the southwestern part of the orogen is made up mostly of sedimentary rocks. I and A type granitoids and volcanic rocks are common in the orogen.

text: The Timanide Orogen (, literally: "Protouralian–Timanide Orogen") is a

text: pre-Uralian

text: orogen

text: that formed in northeastern

text: Baltica

text: during the

text: Neoproterozoic

text: in the Timanide orogeny. The orogen is about 3000 km long. Its extreme points include the southern

text: Urals

text: in the south and the

text: Polar Urals

text: , the

text: Kanin

text: and

text: Varanger

text: peninsulas in the north. The

text: Timan Ridge

text: is the

text: type area

text: of the orogen. To the west, at the Varanger Peninsula, the north-west oriented Timanide Orogen is truncated by the younger

text: Scandinavian Caledonide Orogen

text: that has an oblique disposition. The northeastern parts of the orogen are made up of volcanic and sedimentary rocks, granitoids and few

text: ophiolite

text: s. In contrast the southwestern part of the orogen is made up mostly of

text: sedimentary rock

text: s.

text: I and A type

text: granitoid

text: s and

text: volcanic rock

text: s are common in the orogen.

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answers: Yes

answers: NDQ_005762

answers: sedimentary

answers: NDQ_005763

answers: Neoproterozoic

answers: NDQ_005764

answers: sedimentary rocks

answers: NDQ_005765

answers: orogeny

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answers: volcanic

answers: NDQ_005768

answers: slower cooling forms smaller crystals

answers: NDQ_005769

answers: volcanic

answers: NDQ_005770

answers: The Timanide Orogen

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: There is evidence suggesting that Jotnian cover rocks or a Jotnian platform once covered much of Fennoscandia and were not restricted to a few localities like today. The limited geographical extent of Jotnian sediments at present is indebted to their erosion over geological time. Sedimentary rocks as old as the Jotnian sediments age have a low preservation potential. The distribution of some Jotnian sediments is spatially associated with the occurrence of rapakivi granite. Korja and co-workers (1993) claim the Jotnian sediment–rapakivi granite coincidence at the Gulf of Finland and the Gulf of Bothnia is associated with the existence of thin crust at these locations. At present Jotnian sedimentary rocks are commonly found in half-grabens, narrow grabens, in slightly downfolded (syncline) positions or in mixed graben-synclines. Most of the grabens hosting Jotnian sediments are northwest-southeast oriented. The largest occurrence of Jotnian sediments appear however to occur neither in a rift or a graben and lie in Dalarna, Sweden. It has been suggested that the sedimentary basins hosting Jotnian sediments at Dalarna, Gävle, the Bothnian Sea, Satakunta and Lake Ladoga form an alignment of subsidence parallel to the area of inferred Hallandian-Danopolonian subduction, possibly corresponding to an ancient back-arc basin.

text: There is evidence suggesting that Jotnian cover rocks or a Jotnian

text: platform

text: once covered much of

text: Fennoscandia

text: and were not restricted to a few localities like today. The limited geographical extent of Jotnian sediments at present is indebted to their

text: erosion

text: over

text: geological time

text: . Sedimentary rocks as old as the Jotnian sediments age have a low preservation potential. The distribution of some Jotnian sediments is spatially associated with the occurrence of rapakivi granite. Korja and co-workers (1993) claim the Jotnian sediment–rapakivi granite coincidence at the Gulf of Finland and the Gulf of Bothnia is associated with the existence of thin

text: crust

text: at these locations. At present Jotnian sedimentary rocks are commonly found in

text: half-graben

text: s, narrow

text: graben

text: s, in slightly

text: downfolded

text: (syncline) positions or in mixed graben-synclines. Most of the grabens hosting Jotnian sediments are northwest-southeast oriented. The largest occurrence of Jotnian sediments appear however to occur neither in a rift or a graben and lie in

text: Dalarna

text: , Sweden. It has been suggested that the sedimentary basins hosting Jotnian sediments at Dalarna,

text: Gävle

text: , the

text: Bothnian Sea

text: Satakunta

text: and

text: Lake Ladoga

text: form an alignment of

text: subsidence

text: parallel to the area of inferred

text: Hallandian-Danopolonian

text: subduction

text: , possibly corresponding to an ancient

text: back-arc basin

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answers: Yes

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answers: sedimentary

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answers: thin crust

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answers: thin crust

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answers: erosion

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answers: granite

answers: NDQ_005768

answers: faster cooling forms smaller crystals

answers: NDQ_005769

answers: rift

answers: NDQ_005770

answers: Jotnian cover rocks or a Jotnian platform

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Liesegang rings () (also called Liesegangen rings or Liesegang bands) are colored bands of cement observed in sedimentary rocks that typically cut-across bedding.  These secondary (diagenetic) sedimentary structures exhibit bands of (authigenic) minerals that are arranged in a regular repeating pattern.    Liesegang rings are distinguishable from other sedimentary structures by their concentric or ring-like appearance.  The precise mechanism from which Liesegang rings form is not entirely known and is still under research,  however there is a precipitation process that is thought to be the catalyst for Liesegang ring formation referred to as the Ostwald-Liesegang supersaturation-nucleation-depletion cycle.  Though Liesegang rings are considered a frequent occurrence in sedimentary rocks, rings composed of iron oxide can also occur in permeable igneous and metamorphic rocks that have been chemically weathered.

text: Liesegang rings () (also called Liesegangen rings or Liesegang bands) are colored bands of

text: cement

text: observed in

text: sedimentary rock

text: s that typically cut-across

text: bedding

text: .  These

text: secondary

text: diagenetic

text: sedimentary structures

text: exhibit bands of (

text: authigenic

text: ) minerals that are arranged in a regular repeating pattern.    Liesegang rings are distinguishable from other

text: sedimentary structure

text: s by their concentric or ring-like appearance.  The precise mechanism from which Liesegang rings form is not entirely known and is still under research,  however there is a precipitation process that is thought to be the catalyst for Liesegang ring formation referred to as the Ostwald-Liesegang supersaturation-nucleation-depletion cycle.  Though Liesegang rings are considered a frequent occurrence in

text: sedimentary rocks

text: , rings composed of

text: iron oxide

text: can also occur in permeable

text: igneous

text: and

text: metamorphic rock

text: s that have been chemically

text: weathered

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answers: Yes

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answers: sedimentary

answers: NDQ_005763

answers: permeable igneous and metamorphic rocks

answers: NDQ_005764

answers: sedimentary structures

answers: NDQ_005765

answers: chemically weathered

answers: NDQ_005766

answers: igneous

answers: NDQ_005768

answers: Ostwald-Liesegang supersaturation

answers: NDQ_005769

answers: chemically

answers: NDQ_005770

answers: metamorphic rocks

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The parent granite material is a common type of igneous rock that is granular, with its grains large enough to be distinguished with the unaided eye (i.e., it is phaneritic in texture); it is composed of plagioclase feldspar, orthoclase feldspar, quartz, mica, and possibly other minerals. The chemical transformation of feldspar, one of the primary constituents of granite, into the clay mineral kaolin is one of the important weathering processes. The presence of clay allows water to seep in and further weaken the rock allowing it to fracture or crumble into smaller particles, where, ultimately, the grains of silica produced from the granite are relatively resistant to weathering, and may remain almost unaltered.

text: The parent

text: granite

text: material is a common type of

text: igneous rock

text: that is granular, with its grains large enough to be distinguished with the unaided eye (i.e., it is

text: phaneritic

text: in texture); it is composed of

text: plagioclase feldspar

text: orthoclase feldspar

text: quartz

text: mica

text: , and possibly other minerals. The chemical transformation of

text: feldspar

text: , one of the primary constituents of

text: granite

text: , into the clay mineral

text: kaolin

text: is one of the important weathering processes. The presence of clay allows water to seep in and further weaken the rock allowing it to fracture or crumble into smaller particles, where, ultimately, the grains of

text: silica

text: produced from the granite are relatively resistant to weathering, and may remain almost unaltered.

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answers: 4

answers: NDQ_005761

answers: Rocks are part of the rock cycle.

answers: NDQ_005762

answers: intrusive

answers: NDQ_005763

answers: parent granite material

answers: NDQ_005764

answers: texture

answers: NDQ_005765

answers: weathering

answers: NDQ_005766

answers: igneous

answers: NDQ_005768

answers: quartz

answers: NDQ_005769

answers: weathering

answers: NDQ_005770

answers: unaltered

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Rocks exposed to the atmosphere are variably unstable and subject to the processes of weathering and erosion. Weathering and erosion break the original rock down into smaller fragments and carry away dissolved material. This fragmented material accumulates and is buried by additional material. While an individual grain of sand is still a member of the class of rock it was formed from, a rock made up of such grains fused together is sedimentary. Sedimentary rocks can be formed from the lithification of these buried smaller fragments (clastic sedimentary rock), the accumulation and lithification of material generated by living organisms (biogenic sedimentary rock - fossils), or lithification of chemically precipitated material from a mineral bearing solution due to evaporation (precipitate sedimentary rock). Clastic rocks can be formed from fragments broken apart from larger rocks of any type, due to processes such as erosion or from organic material, like plant remains. Biogenic and precipitate rocks form from the deposition of minerals from chemicals dissolved from all other rock types.

text: Rocks exposed to the

text: atmosphere

text: are variably unstable and subject to the processes of

text: weathering

text: and

text: erosion

text: . Weathering and erosion break the original rock down into smaller fragments and carry away dissolved material. This fragmented material accumulates and is buried by additional material. While an individual grain of sand is still a member of the class of rock it was formed from, a rock made up of such grains fused together is sedimentary. Sedimentary rocks can be formed from the

text: lithification

text: of these buried smaller fragments (

text: clastic

text: sedimentary rock), the accumulation and lithification of material generated by living

text: organism

text: s (

text: biogenic

text: sedimentary rock -

text: fossil

text: s), or lithification of chemically precipitated material from a mineral bearing solution due to

text: evaporation

text: precipitate

text: sedimentary rock). Clastic rocks can be formed from fragments broken apart from larger rocks of any type, due to processes such as

text: erosion

text: or from organic material, like plant remains. Biogenic and precipitate rocks form from the deposition of

text: mineral

text: s from chemicals dissolved from all other rock types.

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answers: Yes

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answers: sedimentary

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answers: deposition of minerals

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answers: unstable

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answers: Biogenic

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answers: Rocks exposed to the atmosphere

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answers: precipitation

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answers: Sedimentary rocks

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: 1

text: Headlands and bays are often found on the same coastline. A bay is surrounded by land on three sides, whereas a headland is surrounded by water on three sides. Headlands and bays form on discordant coastlines, where bands of rock of alternating resistance run perpendicular to the coast. Bays form where weak (less resistant) rocks (such as sands and clays) are eroded, leaving bands of stronger (more resistant) rocks (such as chalk, limestone, granite) forming a headland, or peninsula. Through the deposition of sediment within the bay and the erosion of the headlands, coastlines eventually straighten out then start the same process all over again.

text: Headlands and bays

text: are often found on the same coastline. A bay is surrounded by land on three sides, whereas a headland is surrounded by water on three sides. Headlands and bays form on discordant coastlines, where bands of rock of alternating resistance run perpendicular to the coast. Bays form where weak (less resistant) rocks (such as sands and clays) are eroded, leaving bands of stronger (more resistant) rocks (such as chalk, limestone, granite) forming a headland, or peninsula. Through the deposition of sediment within the bay and the erosion of the headlands, coastlines eventually straighten out then start the same process all over again.

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answers: The same process all over again

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: There has been considerable debate over the years as to the depth of the Yogo dike and how many ounces of rough sapphires per ton it contains. In the late 1970s and early 1980s, Delmer L. Brown, a geological engineer and gemologist, conducted the most thorough scientific exploration up to that time, concluding that the dike was at least  deep and that the concentration of rough sapphires was not constant throughout the deposit. Brown found that the dike had intruded into a pre-existing fault that had been a conduit for groundwater circulation. The overlying shale, the Kibbey Formation, was deposited on an unconformity, an ancient Mississippian-age karst erosion surface, and was not intruded by the dike. This groundwater action produced collapsed zones which were intruded by the dike to form breccia zones. Recent erosion in the area removed the overlying shales and again exposed the limestone to groundwater action which produced collapse breccias which include fragments of the dike rock. He determined that the erosion of the dike in the current erosion cycle was minimal.

text: There has been considerable debate over the years as to the depth of the Yogo dike and how many ounces of rough sapphires per ton it contains. In the late 1970s and early 1980s, Delmer L. Brown, a

text: geological engineer

text: and gemologist, conducted the most thorough scientific exploration up to that time, concluding that the dike was at least  deep and that the concentration of rough sapphires was not constant throughout the deposit. Brown found that the dike had intruded into a pre-existing

text: fault

text: that had been a conduit for groundwater circulation. The overlying shale, the

text: Kibbey Formation

text: , was deposited on an

text: unconformity

text: , an ancient Mississippian-age

text: karst

text: erosion surface

text: , and was not intruded by the dike. This groundwater action produced collapsed zones which were intruded by the dike to form breccia zones. Recent erosion in the area removed the overlying shales and again exposed the limestone to groundwater action which produced collapse breccias which include fragments of the dike rock. He determined that the erosion of the dike in the current erosion cycle was minimal.

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answer: No

answer: No

answer: No

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text: The Svecofennian orogeny is a series of related orogenies that resulted in the formation of much of the continental crust in what is today Sweden and Finland plus some minor parts of Russia. The orogenies lasted from about 2000 to 1800 million years ago during the Paleoproterozoic Era. The resulting orogen is known as the Svecofennian orogen or Svecofennides. To the west and southwest the Svecofennian orogen limits with the generally younger Transscandinavian Igneous Belt. It is assumed that the westernmost fringes of the Svecofennian orogen have been reworked by the Sveconorwegian orogeny just as the western parts of the Transscandinavian Igneous Belt has. The Svecofennian orogeny  involved the accretion of numerous island arcs in such manner that the pre-existing craton grew with this new material from what is today northeast to the southwest. The accretion of the island arcs was also related to two other processes that occurred in the same period; the formation of magma that then cooled to form igneous rocks and the metamorphism of rocks.

text: The Svecofennian orogeny is a series of related

text: orogenies

text: that resulted in the formation of much of the

text: continental crust

text: in what is today

text: Sweden

text: and

text: Finland

text: plus some minor parts of

text: Russia

text: . The orogenies lasted from about 2000 to 1800

text: million years ago

text: during the

text: Paleoproterozoic Era

text: . The resulting orogen is known as the Svecofennian orogen or Svecofennides. To the west and southwest the Svecofennian orogen limits with the generally younger

text: Transscandinavian Igneous Belt

text: . It is assumed that the westernmost fringes of the Svecofennian orogen have been reworked by the

text: Sveconorwegian orogeny

text: just as the western parts of the Transscandinavian Igneous Belt has. The Svecofennian orogeny  involved the

text: accretion

text: of numerous

text: island arc

text: s in such manner that the pre-existing

text: craton

text: grew with this new material from what is today northeast to the southwest. The accretion of the island arcs was also related to two other processes that occurred in the same period;

text: the formation of magma

text: that then cooled to form

text: igneous rock

text: s and the

text: metamorphism

text: of rocks.

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answer: No

answer: No

answer: No

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text: In areas that are more geologically complex, such as those that contain intrusive rocks, faults, and/or metamorphism, stratigraphic columns can still indicate the relative locations of these units with respect to one another. However, in these cases, the stratigraphic column must either be a structural column, in which the units are stacked with respect to how they are observed in the field to have been moved by the faults, or a time column, in which the units are stacked in the order in which they were formed. They also show the lithology of the rock units.

text: In areas that are more geologically complex, such as those that contain

text: intrusive rock

text: s,

text: fault

text: s, and/or

text: metamorphism

text: , stratigraphic columns can still indicate the relative locations of these units with respect to one another. However, in these cases, the stratigraphic column must either be a structural column, in which the units are stacked with respect to how they are observed in the field to have been moved by the faults, or a time column, in which the units are stacked in the order in which they were formed. They also show the lithology of the rock units.

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text: The ML pipes are hosted within the nonmarine sedimentary rocks of the Wapiti Formation and were erupted onto an inland alluvial plain. The uppermost strata of the Wapiti have been removed by erosion in the area, and most of the bedrock is covered by glacial and post-glacial sediments of Quaternary age. The ML volcaniclastic rocks are more resistant to erosion than the surrounding Wapiti Formation rocks, so the ML cluster forms a small hill.

text: The ML pipes are hosted within the nonmarine

text: sedimentary rock

text: s of the

text: Wapiti Formation

text: and were erupted onto an inland

text: alluvial plain

text: . The uppermost strata of the Wapiti have been removed by erosion in the area, and most of the bedrock is covered by glacial and post-glacial sediments of

text: Quaternary

text: age. The ML

text: volcaniclastic

text: rocks are more resistant to erosion than the surrounding Wapiti Formation rocks, so the ML cluster forms a small hill.

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answers: resistant to erosion

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answers: ML volcaniclastic rocks

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answer: No

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text: This was followed by the second tournament match pitting Chris Jericho and The Rock for the World Championship. The two exchanged many holds and reversals in the beginning. Jericho hit a spinning heel kick, and a missile dropkick. Jericho knocked The Rock's head into the steel ring steps, and hit a flying back elbow. The Rock came back with a flying clothesline. Jericho applied a sleeper hold but The Rock fought out of it. Jericho then hit a one-handed bulldog and a Lionsault. Jericho went to the top rope, but The Rock crotched him on the top. The Rock tried a Superplex but Jericho knocked him down, and hit a flying crossbody, but The Rock rolled through. Jericho continued attacking The Rock, but The Rock sent Jericho's head into the ringpost. Jericho fell to the outside where he dropped The Rock onto the barricade, and catapulted him into the ringpost. Jericho then tried to hit a Rock Bottom through the announce table, but The Rock reversed it into a People's DDT through the table. The Rock threw Jericho into the ring and set him for a Rock Bottom, but Jericho countered it into a Breakdown. He set The Rock up for the People's Elbow, but The Rock caught his legs, and applied a Sharpshooter on Jericho. Jericho reversed it into his own Sharpshooter, but The Rock got to the ropes to break the hold. Jericho then applied the Walls of Jericho, but The Rock countered it into a roll-up. The Rock hit a Rock Bottom, as Mr. McMahon came down to ringside. The Rock went for the pinfall but McMahon distracted the referee. The Rock hit McMahon, and hit a Spinebuster on Jericho. He brought McMahon into the ring and hit Jericho with a People's Elbow. The Rock attacked McMahon and, while the referee checked McMahon, Jericho hit a low blow and a Rock Bottom to win the match, and the title.

text: This was followed by the second tournament match pitting

text: Chris Jericho

text: and

text: The Rock

text: for the

text: World Championship

text: . The two exchanged many

text: holds

text: and reversals in the beginning. Jericho hit a

text: spinning heel kick

text: , and a

text: missile dropkick

text: . Jericho knocked The Rock's head into the steel ring steps, and hit a

text: flying back elbow

text: . The Rock came back with a

text: flying clothesline

text: . Jericho applied a

text: sleeper hold

text: but The Rock fought out of it. Jericho then hit a

text: one-handed bulldog

text: and a

text: Lionsault

text: . Jericho went to the top rope, but The Rock crotched him on the top. The Rock tried a

text: Superplex

text: but Jericho knocked him down, and hit a flying crossbody, but The Rock rolled through. Jericho continued attacking The Rock, but The Rock sent Jericho's head into the ringpost. Jericho fell to the outside where he dropped The Rock onto the barricade, and

text: catapulted

text: him into the ringpost. Jericho then tried to hit a

text: Rock Bottom

text: through the announce table, but The Rock reversed it into a

text: People's DDT

text: through the table. The Rock threw Jericho into the ring and set him for a Rock Bottom, but Jericho countered it into a

text: Breakdown

text: . He set The Rock up for the People's Elbow, but The Rock caught his legs, and applied a

text: Sharpshooter

text: on Jericho. Jericho reversed it into his own Sharpshooter, but The Rock got to the ropes to break the hold. Jericho then applied the

text: Walls of Jericho

text: , but The Rock countered it into a

text: roll-up

text: . The Rock hit a

text: Rock Bottom

text: , as

text: Mr. McMahon

text: came down to ringside. The Rock went for the pinfall but McMahon distracted the referee. The Rock hit McMahon, and hit a

text: Spinebuster

text: on Jericho. He brought McMahon into the ring and hit Jericho with a

text: People's Elbow

text: . The Rock attacked McMahon and, while the referee checked McMahon, Jericho hit a

text: low blow

text: and a Rock Bottom to win the match, and the title.

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answers: Jericho

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answers: Jericho

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answers: Rock Bottom

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answers: a Rock Bottom

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answers: Spinebuster

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answers: Jericho

answers: NDQ_005769

answers: Spinebuster

answers: NDQ_005770

answers: The Rock then tried to hit a Rock Bottom through the announce table

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 0

text: From Rogers Pass, layers of quartzite and slate are visible, revealing the fact that the range was part of a large, silty continental shelf 600 million years ago. 185 million years ago, successive plate movements from the west began to crumple and compress this material, driving some of it deep underground, and some into the heights of the Selkirks.  Lime from coral and other organic life was compressed into limestone, which is seen in the Cougar Brook area.  Veins of marble are present in the metamorphic rock of the high peaks. Although erosion and the effects of the glaciers are constantly grinding down the mountain peaks, the pressure of the underlying rock continues to drive them upward.  Geologists have classed the rocks of the Columbia Mountains into groups, several of which appear in the northern Selkirks.  The slates are in the Horsethief Creek and Lardeau groups, quartzite is in the Hamill group, limestone is part of the Badshot Formation, while the metamorphic rocks are classed in the Shuswap Metamorphic Complex.

text: From Rogers Pass, layers of quartzite and slate are visible, revealing the fact that the range was part of a large, silty continental shelf 600 million years ago. 185 million years ago, successive plate movements from the west began to crumple and compress this material, driving some of it deep underground, and some into the heights of the Selkirks.  Lime from coral and other organic life was compressed into limestone, which is seen in the Cougar Brook area.  Veins of marble are present in the metamorphic rock of the high peaks. Although erosion and the effects of the glaciers are constantly grinding down the mountain peaks, the pressure of the underlying rock continues to drive them upward.  Geologists have classed the rocks of the Columbia Mountains into groups, several of which appear in the northern Selkirks.  The slates are in the Horsethief Creek and Lardeau groups, quartzite is in the Hamill group, limestone is part of the Badshot Formation, while the metamorphic rocks are classed in the Shuswap Metamorphic Complex.

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answers: 4

answers: NDQ_005761

answers: Yes

answers: NDQ_005762

answers: Extrusive

answers: NDQ_005763

answers: plate movements

answers: NDQ_005764

answers: limestone

answers: NDQ_005765

answers: successive plate movements

answers: NDQ_005766

answers: marble

answers: NDQ_005768

answers: Quartzite

answers: NDQ_005769

answers: metamorphic

answers: NDQ_005770

answers: metamorphic

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: A large part of the town is built on the Coulard Hill which consists of pale grey and yellow sandstones and with these is associated a cherty and calcareous band, known as  'the cherty rock of Stotfield' .  This rock is a form of silica that contains micro-crystalline quartz.  Also in the calcareous band of the Stotfield rock there is limestone with nodular masses of flint, crystals of galena (lead ore) and iron pyrites.  The quarry on the east side of the town that produced the stone for the building of Branderburgh produced the largest variety and total numbers of fossil reptiles from the late Triassic Period to have been found in the UK. This was a total of eight species and 97 individuals; five of the species are unique to Lossiemouth, one of which is an early form of dinosaur. This quarry is ranked as one of Britain's most important fossil bearing locations of this period.

text: A large part of the town is built on the Coulard Hill which consists of pale grey and yellow sandstones and with these is associated a cherty and calcareous band, known as  'the cherty rock of Stotfield' .  This rock is a form of silica that contains micro-crystalline quartz.  Also in the calcareous band of the Stotfield rock there is limestone with nodular masses of flint, crystals of galena (lead ore) and iron pyrites.  The quarry on the east side of the town that produced the stone for the building of Branderburgh produced the largest variety and total numbers of

text: fossil

text: reptile

text: s from the late

text: Triassic

text: Period to have been found in the UK. This was a total of eight species and 97 individuals; five of the species are unique to Lossiemouth, one of which is an early form of

text: dinosaur

text: . This quarry is ranked as one of Britain's most important fossil bearing locations of this period.

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answers: This rock is a form of silica that contains micro-crystalline quartz

answers: NDQ_005762

answers: sedimentary

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answers: calcareous

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answers: calcareous

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answers: calcareous

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answers: limestone

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answers: quartz

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answers: The quarry on the east side of the town

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The upper boundary of metamorphic conditions is related to the onset of melting processes in the rock. The maximum temperature for metamorphism is typically 700 – 900 °C, depending on the pressure and on the composition of the rock. Migmatites are rocks formed at this upper limit, which contain pods and veins of material that has started to melt but has not fully segregated from the refractory residue. Since the 1980s it has been recognized that, rarely, rocks are dry enough and of a refractory enough composition to record without melting "ultra-high" metamorphic temperatures of 900 – 1100 °C.

text: The upper boundary of metamorphic conditions is related to the onset of melting processes in the rock. The maximum temperature for metamorphism is typically 700 – 900 °C, depending on the pressure and on the composition of the rock.

text: Migmatite

text: s are rocks formed at this upper limit, which contain pods and veins of material that has started to melt but has not fully segregated from the refractory residue. Since the 1980s it has been recognized that, rarely, rocks are dry enough and of a refractory enough composition to record without melting "ultra-high" metamorphic temperatures of 900 – 1100 °C.

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text: Solar System accretion began about 4.56 b.y. ago. Hamilton (2015) summarized data supporting his interpretations. Earth had reached essentially full size by 4.50 b.y., and had already fractionated core and lower and upper mantles at high temperature. The pre-4.50 b.y. high upper-mantle rocks, the dominant rocks now preserved beneath Archean cratons, are not of partially-fractionated mantle as predicted by conventional interpretations, but instead are extremely refractory differentiates, depleted of most silicate materials that could have contributed partial melts of either continental or oceanic crustal rocks. These early-fractionated mantle rocks were originally capped directly by a thick mafic crust that contained the potential subsequent crustal components, including a large proportion of Earth’s major heat-producing elements. At about 4.0 b.y., Earth received, via a barrage of icy bolides initially formed in the outer part of the asteroid belt, the volatile components that evolved into its oceans and atmosphere. Downward cycling of volatiles enabled hydrous partial melting of protocrust to begin, forming a distinctive non-plate-tectonic granitic crust atop residual protocrust. The quite different geologic assemblages of the Archean and Proterozoic eons are explained in terms of variable radiogenic partial melting of the protocrust, after hydration began, to form granitic and volcanic melts that rose from it, and of delamination and sinking of residual protocrust, densified by loss of its lighter components, that began a long-continuing process of re-enriching the upper mantle, and that ultimately enabled plate tectonics.

text: Solar System accretion began about 4.56 b.y. ago. Hamilton (2015) summarized data supporting his interpretations. Earth had reached essentially full size by 4.50 b.y., and had already fractionated core and lower and upper mantles at high temperature. The pre-4.50 b.y. high upper-mantle rocks, the dominant rocks now preserved beneath Archean cratons, are not of partially-fractionated mantle as predicted by conventional interpretations, but instead are extremely refractory differentiates, depleted of most silicate materials that could have contributed partial melts of either continental or oceanic crustal rocks. These early-fractionated mantle rocks were originally capped directly by a thick mafic crust that contained the potential subsequent crustal components, including a large proportion of Earth’s major heat-producing elements. At about 4.0 b.y., Earth received, via a barrage of icy

text: bolides

text: initially formed in the outer part of the asteroid belt, the volatile components that evolved into its oceans and atmosphere. Downward cycling of volatiles enabled hydrous partial melting of protocrust to begin, forming a distinctive non-plate-tectonic granitic crust atop residual protocrust. The quite different geologic assemblages of the Archean and Proterozoic eons are explained in terms of variable radiogenic partial melting of the protocrust, after hydration began, to form granitic and volcanic melts that rose from it, and of delamination and sinking of residual protocrust, densified by loss of its lighter components, that began a long-continuing process of re-enriching the upper mantle, and that ultimately enabled plate tectonics.

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answers: Yes

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answers: sedimentary

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answers: radiogenic partial melting

answers: NDQ_005764

answers: densification

answers: NDQ_005765

answers: delamination and sinking

answers: NDQ_005766

answers: granitic

answers: NDQ_005768

answers: downward cycling of volatiles

answers: NDQ_005769

answers: fractionated

answers: NDQ_005770

answers: fractionated mantle

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Different phyllosilicates are associated with different anatomical regions. This seems to be a result of when they formed. Phyllosilicates primarily form by filling voids. Voids formed in the fossils as the carbon films were heated and released volatile components. Different types of kerogen – reflecting different initial conditions – mature (i.e. volatilize) at different temperatures and pressures. The first kerogens to mature are those that replace labile tissue such as guts and organs; cuticular regions produce more robust kerogens that mature later. Kaolinite (rich in Al/Si, low in Mg) is the first phyllosilicate to form, once the rock is metamorphosed to the oil window, and thus replicates the most labile regions of the fossil. Once the rock is heated and compressed further, to the gas window, illite (rich in K/Al) and chlorite (rich in Fe/Mg) start to form; once all the available K is used up, no further illite forms, so the last tissues to mature are replicated exclusively in chlorite. The precise mineral formation depends on the porewater (and thus rock) chemistry; the thickness of the films increases as metamorphism continues; and the minerals align with the prevailing strain. They are not present in comparable deposits with very little metamorphism.

text: Different phyllosilicates are associated with different anatomical regions. This seems to be a result of when they formed. Phyllosilicates primarily form by filling voids. Voids formed in the fossils as the carbon films were heated and released volatile components. Different types of kerogen – reflecting different initial conditions – mature (i.e. volatilize) at different temperatures and pressures. The first kerogens to mature are those that replace labile tissue such as guts and organs; cuticular regions produce more robust kerogens that mature later.

text: Kaolinite

text: (rich in Al/Si, low in Mg) is the first phyllosilicate to form, once the rock is metamorphosed to the oil window, and thus replicates the most labile regions of the fossil. Once the rock is heated and compressed further, to the gas window,

text: illite

text: (rich in K/Al) and chlorite (rich in Fe/Mg) start to form; once all the available K is used up, no further illite forms, so the last tissues to mature are replicated exclusively in chlorite. The precise mineral formation depends on the porewater (and thus rock) chemistry; the thickness of the films increases as metamorphism continues; and the minerals align with the prevailing strain. They are not present in comparable deposits with very little metamorphism.

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answers: 4

answers: NDQ_005761

answers: Yes

answers: NDQ_005762

answers: metamorphic

answers: NDQ_005763

answers: porewater

answers: NDQ_005764

answers: thickness of the films

answers: NDQ_005765

answers: metamorphism

answers: NDQ_005766

answers: illite

answers: NDQ_005768

answers: The precise mineral formation depends on the porewater

answers: NDQ_005769

answers: volatilize

answers: NDQ_005770

answers: metamorphism

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Sedimentary rocks are formed when sediment is deposited out of air, ice, wind, gravity, or water flows carrying the particles in suspension. This sediment is often formed when weathering and erosion break down a rock into loose material in a source area. The material is then transported from the source area to the deposition area. The type of sediment transported depends on the geology of the hinterland (the source area of the sediment). However, some sedimentary rocks, such as evaporites, are composed of material that form at the place of deposition. The nature of a sedimentary rock, therefore, not only depends on the sediment supply, but also on the sedimentary depositional environment in which it formed.

text: Sedimentary

text: rock

text: s are formed when

text: sediment

text: is

text: deposited

text: out of air, ice, wind, gravity, or water flows carrying the particles in

text: suspension

text: . This sediment is often formed when

text: weathering

text: and

text: erosion

text: break down a rock into loose material in a source area. The material is then

text: transported

text: from the source area to the deposition area. The type of sediment transported depends on the geology of the

text: hinterland

text: (the source area of the sediment). However, some sedimentary rocks, such as

text: evaporite

text: s, are composed of material that form at the place of deposition. The nature of a sedimentary rock, therefore, not only depends on the sediment supply, but also on the

text: sedimentary depositional environment

text: in which it formed.

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answers: 4

answers: NDQ_005761

answers: Yes

answers: NDQ_005762

answers: sedimentary

answers: NDQ_005763

answers: geology of the hinterland

answers: NDQ_005764

answers: The type of sediment transported

answers: NDQ_005765

answers: weathering

answers: NDQ_005766

answers: evaporites

answers: NDQ_005768

answers: faster cooling forms smaller crystals

answers: NDQ_005769

answers: evaporites

answers: NDQ_005770

answers: The nature of a sedimentary rock

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Two types of magma have been determined to have generated in the Earth's upper mantle by partial melting of mantle rocks. One of these magma types is basaltic in composition, composed of plagioclase, titanium-rich pyroxene, and olivine. The other magma type crystallized to nepheline, melilite, pyroxene, and, in some of the rocks, plagioclase. Some nepheline-bearing igneous rocks contain rounded inclusions of spinel peridotite, an ultramafic rock that may represent fragments of the upper mantle incorporated into the magma during its ascent to the surface. Most of the igneous rocks on the surface probably are not representative of the original magmas formed in the mantle; certain processes, such as separation of phenocrysts from the liquid from which they crystallized have altered their original chemical compositions at depths shallower than the mantle.

text: Two types of magma have been determined to have generated in the Earth's upper mantle by partial melting of

text: mantle

text: rocks. One of these magma types is basaltic in composition, composed of

text: plagioclase

text: , titanium-rich

text: pyroxene

text: , and

text: olivine

text: . The other magma type crystallized to

text: nepheline

text: melilite

text: pyroxene

text: , and, in some of the rocks,

text: plagioclase

text: . Some nepheline-bearing igneous rocks contain rounded inclusions of spinel

text: peridotite

text: , an

text: ultramafic

text: rock that may represent fragments of the upper mantle incorporated into the magma during its ascent to the surface. Most of the igneous rocks on the surface probably are not representative of the original magmas formed in the mantle; certain processes, such as separation of phenocrysts from the liquid from which they crystallized have altered their original chemical compositions at depths shallower than the mantle.

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answers: Yes

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answers: intrusive

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answers: composition

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answers: original chemical compositions

answers: NDQ_005765

answers: partial melting of mantle rocks

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answers: magma

answers: NDQ_005768

answers: magma

answers: NDQ_005769

answers: separation

answers: NDQ_005770

answers: The other magma type crystallized

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Contact metamorphism is the name given to the changes that take place when magma is injected into the surrounding solid rock (country rock). The changes that occur are greatest wherever the magma comes into contact with the rock because the temperatures are highest at this boundary and decrease with distance from it. Around the igneous rock that forms from the cooling magma is a metamorphosed zone called a contact metamorphism aureole. Aureoles may show all degrees of metamorphism from the contact area to unmetamorphosed (unchanged) country rock some distance away. The formation of important ore minerals may occur by the process of metasomatism at or near the contact zone.

text: Contact metamorphism is the name given to the changes that take place when magma is injected into the surrounding solid rock (country rock). The changes that occur are greatest wherever the magma comes into contact with the rock because the temperatures are highest at this boundary and decrease with distance from it. Around the igneous rock that forms from the cooling magma is a metamorphosed zone called a contact metamorphism aureole. Aureoles may show all degrees of metamorphism from the contact area to unmetamorphosed (unchanged) country rock some distance away. The formation of important

text: ore

text: minerals may occur by the process of

text: metasomatism

text: at or near the contact zone.

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answers: Yes

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answers: intrusive

answers: NDQ_005763

answers: all degrees of metamorphism

answers: NDQ_005764

answers: degrees of metamorphism

answers: NDQ_005765

answers: The formation of important ore minerals

answers: NDQ_005766

answers: igneous

answers: NDQ_005768

answers: faster cooling forms smaller crystals

answers: NDQ_005769

answers: metamorphism

answers: NDQ_005770

answers: unmetamorphosed

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Metaigneous and metavolcanic rocks form the largest component of cratons and are high in silica. Igneous and volcanic rocks are also high in silica but with non-metamorphosed rock, weathering becomes faster and the mobilization of ions is more widespread. Rocks high in silica produce silicic acid as a weathering product. There are few rock types that lead to localized enrichment of some of the biologically limiting elements like phosphorus (P) and nitrogen (N). Phosphatic shale (<15% PO) and phosphorite (>15% PO) form in anoxic deep water basins that preserve organic material. Greenstone (metabasalt), phyllite and schist release up to 30-50% of the nitrogen pool.<ref>{{cite journal|last1=Holloway|first1= J.|last2= Dahlgren|first2= R.|date= 1999|title= Geologic nitrogen in terrestrial biogeochemical cycling|journal=Geology|volume= 27|issue= 6|page= 567|doi=10.1130/0091-7613(1999)027

text: Metaigneous and metavolcanic rocks form the largest component of cratons and are high in silica. Igneous and volcanic rocks are also high in

text: silica

text: but with non-metamorphosed rock, weathering becomes faster and the mobilization of ions is more widespread. Rocks high in silica produce silicic acid as a weathering product. There are few rock types that lead to localized enrichment of some of the biologically limiting elements like

text: phosphorus

text: (P) and

text: nitrogen

text: (N). Phosphatic shale (<15% PO) and phosphorite (>15% PO) form in

text: anoxic

text: deep water basins that preserve organic material. Greenstone (

text: metabasalt

text: phyllite

text: and

text: schist

text: release up to 30-50% of the nitrogen pool.<ref>{{cite journal|last1=Holloway|first1= J.|last2= Dahlgren|first2= R.|date= 1999|title= Geologic nitrogen in terrestrial biogeochemical cycling|journal=Geology|volume= 27|issue= 6|page= 567|doi=10.1130/0091-7613(1999)027

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answers: 3

answers: NDQ_005761

answers: Yes

answers: NDQ_005762

answers: Rocks are classified into four major groups, reflecting how they formed

answers: NDQ_005763

answers: high in silica

answers: NDQ_005764

answers: high in silica

answers: NDQ_005765

answers: weathering

answers: NDQ_005766

answers: metamorphosed

answers: NDQ_005768

answers: Faster cooling forms larger crystals.

answers: NDQ_005769

answers: weathering

answers: NDQ_005770

answers: Metaigneous and metavolcanic rocks

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: In pressure release, also known as unloading, overlying materials (not necessarily rocks) are removed (by erosion, or other processes), which causes underlying rocks to expand and fracture parallel to the surface.

text: In pressure release, also known as unloading, overlying materials (not necessarily rocks) are removed (by erosion, or other processes), which causes underlying rocks to expand and fracture parallel to the surface.

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text: A cataclastic rock is a type of metamorphic rock that has been wholly or partly formed by the progressive fracturing and comminution of existing rock, a process known as cataclasis, and is mainly found associated with fault zones. Mylonite was originally defined as a cataclastic rock but is now understood to have formed mainly by crystal-plastic processes.

text: A cataclastic rock is a type of

text: metamorphic rock

text: that has been wholly or partly formed by the progressive fracturing and

text: comminution

text: of existing rock, a process known as cataclasis, and is mainly found associated with

text: fault

text: zones.

text: Mylonite

text: was originally defined as a cataclastic rock but is now understood to have formed mainly by crystal-plastic processes.

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answer: 1

text: The main rivalry heading into SummerSlam was between The Rock and Booker T, battling over the WCW Championship. After losing the WWF Championship to Steve Austin at WrestleMania X-Seven, The Rock took a hiatus from professional wrestling to film the movie, The Scorpion King. On the edition of July 9, 2001 of Raw Is War, campaigning for The Rock's return began. Following the campaigning, The Rock returned to the WWF on the edition of July 30, 2001 of Raw Is War, where he chose to align himself with the WWF instead of The Alliance for The Invasion. This action was shown by The Rock delivering a Rock Bottom and the people's elbow onto Shane McMahon, The Alliance leader. Later that week on SmackDown!, Booker T and The Rock cut a promo, where Booker T challenged The Rock to a match at SummerSlam; the beginning of the The Rock-Booker T rivalry. Seeking revenge for the attack on the edition of July 30, 2001 of Raw is War, McMahon fought The Rock in a Street Fight on the edition of August 6 of Raw is War, where The Rock pinned McMahon. The rivalry between The Rock and Booker T intensified after the match, where Booker T and Shane McMahon double-teamed The Rock. Later that week on SmackDown!, in retaliation, The Rock accepted Booker T's challenge. On the edition of August 13 of Raw is War, The Rock was involved in a tag team match, where he teamed with Chris Jericho in a loss to Booker T and Rhyno. After the match, Booker T delivered his variation of the Rock Bottom on The Rock, a move dubbed, The Book End. On the final edition of SmackDown! before SummerSlam, McMahon announced that Booker T would defend the WCW Championship at SummerSlam against The Rock. Later that night, the rivalry continued to intensify during a Lights Out match between Booker T and The Rock, after Booker T delivered a Book End onto The Rock through a commentators announce table.

text: The main

text: rivalry

text: heading into SummerSlam was between

text: The Rock

text: and

text: Booker T

text: , battling over the

text: WCW Championship

text: . After losing the

text: WWF Championship

text: to

text: Steve Austin

text: at

text: WrestleMania X-Seven

text: , The Rock took a hiatus from

text: professional wrestling

text: to film the movie,

text: The Scorpion King

text: . On the edition of July 9, 2001 of

text: Raw Is War

text: , campaigning for The Rock's return began. Following the campaigning, The Rock returned to the WWF on the edition of July 30, 2001 of Raw Is War, where he chose to align himself with the WWF instead of

text: The Alliance

text: for

text: The Invasion

text: . This action was shown by The Rock delivering a

text: Rock Bottom

text: and the people's elbow onto

text: Shane McMahon

text: , The Alliance leader. Later that week on

text: SmackDown!

text: , Booker T and The Rock cut a

text: promo

text: , where Booker T challenged The Rock to a match at SummerSlam; the beginning of the The Rock-Booker T rivalry. Seeking revenge for the attack on the edition of July 30, 2001 of Raw is War, McMahon fought The Rock in a

text: Street Fight

text: on the edition of August 6 of Raw is War, where The Rock pinned McMahon. The rivalry between The Rock and Booker T intensified after the match, where Booker T and Shane McMahon

text: double-teamed

text: The Rock. Later that week on SmackDown!, in retaliation, The Rock accepted Booker T's challenge. On the edition of August 13 of Raw is War, The Rock was involved in a

text: tag team match

text: , where he teamed with

text: Chris Jericho

text: in a loss to Booker T and

text: Rhyno

text: . After the match, Booker T delivered his variation of the Rock Bottom on The Rock, a move dubbed, The Book End. On the final edition of SmackDown! before SummerSlam, McMahon announced that Booker T would defend the WCW Championship at SummerSlam against The Rock. Later that night, the rivalry continued to intensify during a

text: Lights Out match

text: between Booker T and The Rock, after Booker T delivered a Book End onto The Rock through a commentators announce table.

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

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answer: No

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answer: No

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answer: No

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text: In geology and astronomy, the term silicate is used to denote types of rock that consist predominantly of silicate minerals.  On Earth, a wide variety of silicate minerals occur in an even wider range of combinations as a result of the processes that form and re-work the crust. These processes include partial melting, crystallization, fractionation, metamorphism, weathering and diagenesis. Living things also contribute to the silicate cycle near the Earth's surface. A type of plankton known as diatoms construct their exoskeletons, known as tests, from silica. The tests of dead diatoms are a major constituent of deep ocean sediment.

text: In

text: geology

text: and

text: astronomy

text: , the term silicate is used to denote types of

text: rock

text: that consist predominantly of

text: silicate minerals

text: .  On Earth, a wide variety of silicate minerals occur in an even wider range of combinations as a result of the processes that form and re-work the crust. These processes include partial

text: melting

text: crystallization

text: fractionation

text: metamorphism

text: weathering

text: and

text: diagenesis

text: . Living things also contribute to the silicate cycle near the Earth's surface. A type of

text: plankton

text: known as

text: diatom

text: s construct their

text: exoskeleton

text: s, known as tests, from silica. The tests of dead diatoms are a major constituent of

text: deep ocean

text: sediment

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answer: Yes

answer: Yes

answer: Yes

answer: Yes

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answer: 1

text: Although some of the 1960s bands performed covers of songs by hard rock pioneers like Cream and Jimi Hendrix Experience, hard rock gained large popularity in the early 1970s with the works of progressive rock bands Pop Mašina, YU Grupa and Smak. Pop Mašina, formed in 1971, was one of the first Serbian and Yugoslav bands to move away from rhythm and blues towards harder sound. Their sound featured progressive, hard, psychedelic and acid rock elements. Pop Mašina disbanded in 1977. YU Grupa, formed in 1970, performed progressive/hard rock, and their songs often featured traditional music elements. The band disbanded in 1981, only to reunite in 1987. Since their comeback album, Od zlata jabuka (1987), their work has been mostly hard rock-oriented. Smak, formed in 1971, performed jazz-influenced progressive rock, but their sound often featured hard rock, blues and folk elements. The band moved towards more commercial hard rock at the beginning of the 1980s with the album Rock cirkus, but the album saw little success and the band disbanded shortly after, having constant reunions disbandments throughout the 1980s and 1990s.

text: Although some of the 1960s bands performed covers of songs by

text: hard rock

text: pioneers like

text: Cream

text: and

text: Jimi Hendrix Experience

text: , hard rock gained large popularity in the early 1970s with the works of

text: progressive rock

text: bands

text: Pop Mašina

text: YU Grupa

text: and

text: Smak

text: . Pop Mašina, formed in 1971, was one of the first Serbian and Yugoslav bands to move away from

text: rhythm and blues

text: towards harder sound. Their sound featured

text: progressive

text: , hard,

text: psychedelic

text: and

text: acid rock

text: elements. Pop Mašina disbanded in 1977. YU Grupa, formed in 1970, performed progressive/hard rock, and their songs often featured

text: traditional music

text: elements. The band disbanded in 1981, only to reunite in 1987. Since their comeback album,

text: Od zlata jabuka

text: (1987), their work has been mostly hard rock-oriented. Smak, formed in 1971, performed

text: jazz

text: -influenced progressive rock, but their sound often featured hard rock,

text: blues

text: and folk elements. The band moved towards more commercial hard rock at the beginning of the 1980s with the album

text: Rock cirkus

text: , but the album saw little success and the band disbanded shortly after, having constant reunions disbandments throughout the 1980s and 1990s.

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answers: Rock cirkus

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answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Metasomatism is the drastic change in the bulk chemical composition of a rock that often occurs during the processes of metamorphism. It is due to the introduction of chemicals from other surrounding rocks. Water may transport these chemicals rapidly over great distances. Because of the role played by water, metamorphic rocks generally contain many elements absent from the original rock, and lack some that originally were present. Still, the introduction of new chemicals is not necessary for recrystallization to occur.

text: Metasomatism is the drastic change in the bulk chemical composition of a rock that often occurs during the processes of metamorphism. It is due to the introduction of chemicals from other surrounding rocks. Water may transport these chemicals rapidly over great distances. Because of the role played by water, metamorphic rocks generally contain many elements absent from the original rock, and lack some that originally were present. Still, the introduction of new chemicals is not necessary for recrystallization to occur.

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answers: slower cooling forms smaller crystals

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answers: Metasomatism

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: A set with a cyclic order is called a cyclically ordered set or simply a cycle. Some familiar cycles are discrete, having only a finite number of elements: there are seven days of the week, four cardinal directions, twelve notes in the chromatic scale, and three plays in rock-paper-scissors. In a finite cycle, each element has a "next element" and a "previous element". There are also continuously variable cycles with infinitely many elements, such as the oriented unit circle in the plane.

text: A

text: set

text: with a cyclic order is called a cyclically ordered set or simply a cycle. Some familiar cycles are discrete, having only a

text: finite number

text: of

text: element

text: s: there are seven

text: days of the week

text: , four

text: cardinal direction

text: s, twelve notes in the

text: chromatic scale

text: , and three plays in

text: rock-paper-scissors

text: . In a finite cycle, each element has a "next element" and a "previous element". There are also continuously variable cycles with infinitely many elements, such as the oriented

text: unit circle

text: in the plane.

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answers: The oriented unit circle in the plane

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Among the three major types of rock, fossils are most commonly found in sedimentary rock. Unlike most igneous and metamorphic rocks, sedimentary rocks form at temperatures and pressures that do not destroy fossil remnants. Often these fossils may only be visible under magnification.

text: Among the three major types of rock, fossils are most commonly found in sedimentary rock. Unlike most igneous and metamorphic rocks, sedimentary rocks form at temperatures and pressures that do not destroy fossil remnants. Often these fossils may only be visible under

text: magnification

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text: Crystallization of polymers is a process associated with partial alignment of their molecular chains. These chains fold together and form ordered regions called lamellae, which compose larger spheroidal structures named spherulites. Polymers can crystallize upon cooling from the melt, mechanical stretching or solvent evaporation. Crystallization affects optical, mechanical, thermal and chemical properties of the polymer. The degree of crystallinity is estimated by different analytical methods and it typically ranges between 10 and 80%, thus crystallized polymers are often called "semi-crystalline". The properties of semi-crystalline polymers are determined not only by the degree of crystallinity, but also by the size and orientation of the molecular chains.

text: Crystallization of polymers is a process associated with partial alignment of their molecular chains. These chains fold together and form ordered regions called

text: lamellae

text: , which compose larger spheroidal structures named

text: spherulite

text: s.

text: Polymer

text: s can crystallize upon cooling from the melt, mechanical stretching or solvent evaporation. Crystallization affects optical, mechanical, thermal and chemical properties of the polymer. The degree of

text: crystallinity

text: is estimated by different analytical methods and it typically ranges between 10 and 80%, thus crystallized polymers are often called "semi-crystalline". The properties of semi-crystalline polymers are determined not only by the degree of crystallinity, but also by the size and orientation of the molecular chains.

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answers: Crystallization of polymers

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 0

text: Deep-seated intrusions are recognized from the way they have burst through the overlying strata. Ramifying veins result from filled cracks, and the high temperature involved in this process is evident from the altered adjacent country rock. Since heat dissipates slowly and since the rock is under pressure, crystals form and no vitreous rapidly chilled matter is present. As the intrusions have had time to rest before crystallizing, they are not fluidal. Their contained gases have not been able to escape through the thick layer of strata, beneath which they were injected. Such gases form cavities, which can often be observed in these minerals. Such gases have also resulted in many important modifications in the crystallization of the rock. Because their crystals are of approximately equal size these rocks are said to be granular.

text: Deep-seated intrusions are recognized from the way they have burst through the overlying

text: strata

text: . Ramifying veins result from filled cracks, and the high temperature involved in this process is evident from the altered adjacent country rock. Since heat dissipates slowly and since the rock is under pressure, crystals form and no

text: vitreous

text: rapidly chilled matter is present. As the intrusions have had time to rest before crystallizing, they are not

text: fluidal

text: . Their contained gases have not been able to escape through the thick layer of strata, beneath which they were injected. Such gases form cavities, which can often be observed in these minerals. Such gases have also resulted in many important modifications in the crystallization of the rock. Because their crystals are of approximately equal size these rocks are said to be granular.

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answers: Yes

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answers: Because their crystals are of approximately equal size

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answers: crystallizing

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answers: crystallization

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: A typical thermochronological study will involve the dates of a number of rock samples from different areas in a region, often from a vertical transect along a steep canyon, cliff face, or slope. These samples are then dated. With some knowledge of the subsurface thermal structure, these dates are translated into depths and times at which that particular sample was at the mineral's closure temperature. If the rock is today at the surface, this process gives the exhumation rate of the rock.

text: A typical thermochronological study will involve the dates of a number of rock samples from different areas in a region, often from a vertical transect along a steep canyon, cliff face, or slope. These samples are then dated. With some knowledge of the subsurface thermal structure, these dates are translated into depths and times at which that particular sample was at the mineral's closure temperature. If the rock is today at the surface, this process gives the

text: exhumation

text: rate of the rock.

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answers: Yes

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answer: No

answer: No

answer: No

answer: No

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answer: 1

text: "Sick Cycle Carousel" is a song by American alternative rock band Lifehouse. It is the second single released from their debut studio album No Name Face (2000). The track was written by Lifehouse lead singer Jason Wade and Scott Faircloff, who says he felt freedom when writing songs for the album. American record producers Ron Aniello and Brendan O'Brien produced and mixed the song, respectively. Musically, "Sick Cycle Carousel" is a moderate rock song with an influence of soft rock. The song was released on June 4, 2001 by DreamWorks Records.

text: "Sick Cycle Carousel" is a song by American

text: alternative rock

text: band

text: Lifehouse

text: . It is the second single released from their debut studio album

text: No Name Face

text: (2000). The track was written by Lifehouse lead singer

text: Jason Wade

text: and Scott Faircloff, who says he felt freedom when writing songs for the album. American record producers

text: Ron Aniello

text: and

text: Brendan O'Brien

text: produced and mixed the song, respectively. Musically, "Sick Cycle Carousel" is a moderate

text: rock

text: song with an influence of

text: soft rock

text: . The song was released on June 4, 2001 by

text: DreamWorks Records

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answers: slower cooling forms smaller crystals

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answers: The song was released on June 4, 2001

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text: Erosion occurring between the eruptions deposited deep layers of sediment between the lava flows, which eventually lithified into sedimentary rock, such as the conglomerate rock Mount Toby is composed of. The resulting "layer cake" of basalt and sedimentary sheets eventually faulted and tilted upward. Subsequent erosion wore away the weaker sedimentary layers a faster rate than the basalt layers, leaving the abruptly tilted edges of the basalt sheets exposed, creating the distinct linear ridge and dramatic cliff faces visible today. One way to imagine this is to picture a layer cake tilted slightly up with some of the frosting (the sedimentary layer) removed in between. A good example of this layer-cake structure can be found on the Robert Frost Trail beneath Mount Norwottuck at the Horse Caves. The summit of Norwottuck is made of basalt; directly beneath the summit are the Horse Caves, a deep overhang where the weaker sedimentary layer has worn away at a more rapid rate that the basalt layer above it. Mount Toby is also part of such a geologic layer cake. The bottom layer is composed of arkose sandstone, visible across the Connecticut River on Sugarloaf Mountain in Deerfield, Massachusetts. The middle layer is composed basalt; it is most visible as the geology of the Pocumtuck Ridge, to the northwest of Mount Toby. The top (youngest) layer is composed of Mount Toby Conglomerate.

text: Erosion occurring between the eruptions deposited deep layers of sediment between the lava flows, which eventually lithified into

text: sedimentary rock

text: , such as the conglomerate rock Mount Toby is composed of. The resulting "layer cake" of basalt and sedimentary sheets eventually

text: faulted

text: and tilted upward. Subsequent

text: erosion

text: wore away the weaker sedimentary layers a faster rate than the basalt layers, leaving the abruptly tilted edges of the basalt sheets exposed, creating the distinct linear ridge and dramatic cliff faces visible today. One way to imagine this is to picture a layer cake tilted slightly up with some of the frosting (the sedimentary layer) removed in between. A good example of this layer-cake structure can be found on the Robert Frost Trail beneath Mount Norwottuck at the Horse Caves. The summit of Norwottuck is made of basalt; directly beneath the summit are the Horse Caves, a deep overhang where the weaker sedimentary layer has worn away at a more rapid rate that the basalt layer above it. Mount Toby is also part of such a geologic layer cake. The bottom layer is composed of

text: arkose

text: sandstone, visible across the Connecticut River on

text: Sugarloaf Mountain

text: in

text: Deerfield, Massachusetts

text: . The middle layer is composed

text: basalt

text: ; it is most visible as the geology of the

text: Pocumtuck Ridge

text: , to the northwest of Mount Toby. The top (youngest) layer is composed of Mount Toby Conglomerate.

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answers: Mount Toby

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answers: sedimentary

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answers: Erosion

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answers: lithified

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answers: Erosion

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answers: Slower cooling forms smaller crystals

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answers: Mount Toby Conglomerate

answer: No

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text: The park is known for its unique turbidites. It has very exposed turbidities with white calcite veins. Turbidites are rocks or sediments that travel into the ocean as suspended particles in the flow of water, causing a sedimentary layering effect on the ocean floor. Over time the sediments and rock compact and the process repeats as a constant cycle. The park also is known for its tectonic mélanges that have been deemed 'smell rocks' by the locals due to its strong petroleum odor. Mélanges are large individual rocks that are large enough that they are accounted for in map drawings. The Olympic mélanges can be as large as a house.

text: The park is known for its unique

text: turbidites

text: . It has very exposed turbidities with white calcite veins. Turbidites are rocks or sediments that travel into the ocean as suspended particles in the flow of water, causing a sedimentary layering effect on the ocean floor. Over time the sediments and rock compact and the process repeats as a constant cycle. The park also is known for its tectonic

text: mélange

text: s that have been deemed 'smell rocks' by the locals due to its strong petroleum odor. Mélanges are large individual rocks that are large enough that they are accounted for in map drawings. The Olympic mélanges can be as large as a house.

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answers: sedimentary

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answers: calcite veins

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answers: Turbidites

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answers: It has very exposed turbidities with white calcite veins

answer: Yes

answer: Yes

answer: No

answer: Yes

answer: No

answer: 1

text: The 1970s were marked by rock genres such as hard rock, progressive rock, jazz rock, art rock, glam rock, folk rock, symphonic rock, blues rock and boogie rock. In that period, some of the greatest Yugoslav stadium rock bands emerged: YU grupa, Time, Smak, Parni valjak, Atomsko Sklonište, Leb i Sol, Teška industrija and Galija.

text: The 1970s were marked by rock genres such as

text: hard rock

text: progressive rock

text: jazz rock

text: art rock

text: glam rock

text: folk rock

text: symphonic rock

text: blues rock

text: and

text: boogie rock

text: . In that period, some of the greatest Yugoslav

text: stadium rock bands

text: emerged:

text: YU grupa

text: Time

text: Smak

text: Parni valjak

text: Atomsko Sklonište

text: Leb i Sol

text: , Teška industrija and

text: Galija

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answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: In geology, a platform is a continental area covered by relatively flat or gently tilted, mainly sedimentary strata, which overlie a basement of consolidated igneous or metamorphic rocks of an earlier deformation. Platforms, shields and the basement rocks together constitute cratons. Platform sediments can be classified into the following groups: a "protoplatform" of metamorphosed sediments at the bottom, a "quasiplatform" of slightly deformed sediments, a "cataplatform", and a "orthoplatform" at the top. The Mesoproterozoic Jotnian sediments of the  Baltic area are examples of a "quasiplatform". The post-Ordovician rocks of the South American Platform are examples of an orthoplatform.

text: In geology, a platform is a continental area covered by relatively flat or gently tilted, mainly

text: sediment

text: ary

text: strata

text: , which overlie a

text: basement

text: of consolidated

text: igneous

text: or

text: metamorphic rocks

text: of an earlier deformation. Platforms,

text: shields

text: and the

text: basement rocks

text: together constitute

text: craton

text: s. Platform sediments can be classified into the following groups: a "protoplatform" of

text: metamorphosed

text: sediments at the bottom, a "quasiplatform" of slightly deformed sediments, a "cataplatform", and a "orthoplatform" at the top. The

text: Mesoproterozoic

text: Jotnian sediments

text: of the

text: Baltic area

text: are examples of a "quasiplatform". The post-

text: Ordovician

text: rocks of the South American Platform are examples of an orthoplatform.

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answers: Platforms, shields and the basement rocks

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answers: faster cooling forms smaller crystals

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answers: metamorphic rocks

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Windimurra contains in excess of 13,000m of intact igneous stratigraphy  formed of cumulate layering by a process of fractional crystallization. Individual rock types can be grouped into a troctolite phase or series, a gabbro phase or series and a gabbronorite phase or series. Anorthosite cumulates are preserved in the roof sections, most of which are sheared and faulted off. A marginal granophyre complex exists in the roof and wall rocks, formed by advective heat transfer causing melting of the country rocks.

text: Windimurra contains in excess of 13,000m of intact igneous

text: stratigraphy

text: formed of

text: cumulate

text: layering by a process of

text: fractional crystallization

text: . Individual rock types can be grouped into a

text: troctolite

text: phase or series, a

text: gabbro

text: phase or series and a gabbro

text: norite

text: phase or series.

text: Anorthosite

text: cumulates are preserved in the roof sections, most of which are sheared and faulted off. A marginal

text: granophyre

text: complex exists in the roof and wall rocks, formed by advective heat transfer causing melting of the country rocks.

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answers: rock types can be grouped

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answers: fractional crystallization

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Metamorphic rocks arise from the transformation of existing rock types, in a process called metamorphism, which means "change in form". The original rock (protolith) is subjected to heat (temperatures greater than 150 to 200 °C) and pressure (1500 bars), causing profound physical and/or chemical change. The protolith may be a sedimentary rock, an igneous rock or another older metamorphic rock.

text: Metamorphic rocks arise from the transformation of existing

text: rock

text: types, in a process called

text: metamorphism

text: , which means "change in form". The original rock (

text: protolith

text: ) is subjected to heat (temperatures greater than 150 to 200 °C) and pressure (1500

text: bar

text: s), causing profound physical and/or chemical change. The protolith may be a

text: sedimentary rock

text: , an

text: igneous rock

text: or another older metamorphic rock.

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answers: Metamorphic rocks

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answers: The protolith

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answers: slower cooling forms smaller crystals

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answers: Metamorphic rocks

answer: No

answer: No

answer: Yes

answer: No

answer: No

answer: 1

text: Heazlewoodite is formed within terrestrial rocks by metamorphism of peridotite and dunite via a process of nucleation. Heazlewoodite is the least sulfur saturated of nickel sulfide minerals and is only formed via metamorphic exsolution of sulfur from the lattice of metamorphic olivine.

text: Heazlewoodite is formed within terrestrial rocks by

text: metamorphism

text: of

text: peridotite

text: and

text: dunite

text: via a process of nucleation. Heazlewoodite is the least sulfur saturated of nickel sulfide minerals and is only formed via metamorphic

text: exsolution

text: of sulfur from the lattice of metamorphic

text: olivine

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answers: least sulfur saturated

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answers: Heazlewoodite

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answer: No

answer: No

answer: No

answer: No

answer: No

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text: Tectonic uplift during the creation of high mountainous regions can produce incredible surface elevations and therefore exposure of rocks to wind and water. High precipitation can drive enhanced erosion of the exposed rocks and lead to rapid denudation of sediment from the mountains. Buoyancy of the crust, or isostasy, will then drive further tectonic uplift, in order to achieve equilibrium, as sediment is continuously stripped from the top.  Enhanced uplift will then create higher topography, drive increased precipitation which will concentrate erosion, and further uplift.

text: Tectonic uplift during the creation of high mountainous regions can produce incredible surface elevations and therefore exposure of rocks to wind and water. High precipitation can drive enhanced erosion of the exposed rocks and lead to rapid

text: denudation

text: of sediment from the mountains. Buoyancy of the crust, or

text: isostasy

text: , will then drive further tectonic uplift, in order to achieve equilibrium, as sediment is continuously stripped from the top.  Enhanced uplift will then create higher topography, drive increased precipitation which will concentrate erosion, and further uplift.

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answers: Yes

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answers: sedimentary

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answers: Tectonic uplift

answers: NDQ_005764

answers: Buoyancy

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answers: erosion

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answers: mountainous

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answers: Faster cooling forms larger crystals

answers: NDQ_005769

answers: denudation

answers: NDQ_005770

answers: Tectonic uplift

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Detrital zircons are part of the sediment derived from weathering and erosion of pre-existing rocks. Since zircons are heavy and highly resistant at Earth's surface, many zircons are transported, deposited and preserved as detrital zircon grains in sedimentary rocks. (See Figure 2, note that the diagram is used for concept illustration. Detrital zircon in reality can be products from all kind of rocks, not necessarily igneous rocks)

text: Detrital zircons are part of the

text: sediment

text: derived from

text: weathering

text: and

text: erosion

text: of pre-existing rocks. Since zircons are heavy and highly resistant at Earth's surface, many zircons are transported, deposited and preserved as detrital zircon grains in

text: sedimentary rock

text: s. (See Figure 2, note that the diagram is used for concept illustration. Detrital zircon in reality can be products from all kind of rocks, not necessarily igneous rocks)

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answers: Yes

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answers: sedimentary

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answers: Earth's surface

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answers: highly resistant

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answers: weathering

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answers: igneous rocks

answers: NDQ_005768

answers: slower cooling forms smaller crystals

answers: NDQ_005769

answers: weathering

answers: NDQ_005770

answers: Detrital zircon

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The scapolite limestones and contact metamorphic rocks. As silicates rich in calcium, it is to be expected that these minerals will be found where impure limestones have been crystallized by contact with an igneous magma. Even meionite (the variety richest in soda) occurs in this association, being principally obtained in small crystals lining cavities in ejected blocks of crystalline limestone at Vesuvius and the craters of the Eifel in Germany. Scapolite and wernerite are far more common at the contacts of limestone with intrusive masses. The minerals that accompany them are calcite, epidote, vesuvianite, garnet, wollastonite, diopside and amphibole. The scapolites are colorless, flesh-colored, grey or greenish; occasionally they are nearly black from the presence of very small enclosures of graphitic material. They are not in very perfect crystals, though sometimes incomplete octagonal sections are visible; the tetragonal cleavage, strong double refraction and uniaxial interference figure distinguish them readily from other minerals. Commonly they weather to micaceous aggregates, but sometimes an isotropic substance of unknown nature is seen replacing them. In crystalline limestones and calc–silicate rocks they occur in small and usually inconspicuous grains mingled with the other components of the rock. Large, nearly idiomorphic crystals are sometimes found in argillaceous rocks (altered calcareous shales) that have suffered thermal metamorphism. In the Pyrenees there are extensive outcrops of limestone penetrated by igneous rocks described as ophites (varieties of diabase) and iherzolites (peridotites). At the contacts scapolite occurs in a great number of places, both in the limestones and in the calcareous shales that accompany them. In some of these rocks large crystals of one of the scapolite minerals (an inch or two in length) occur, usually as octagonal prisms with imperfect terminations. In others the mineral is found in small irregular grains. It is sometimes clear, but often crowded with minute enclosures of augite, tourmaline, biotite and other minerals, such as constitute the surrounding matrix. From these districts also a black variety is well known, filled with minute graphitic enclosures, often exceedingly small and rendering the mineral nearly opaque. The names couzeranite and dipyre are often given to this kind of scapolite. Apparently the presence of chlorine in small quantities, which may often be detected in limestones, to some extent determines the formation of the mineral.

text: The scapolite limestones and contact

text: metamorphic rocks

text: . As silicates rich in

text: calcium

text: , it is to be expected that these minerals will be found where impure limestones have been crystallized by contact with an igneous

text: magma

text: . Even meionite (the variety richest in soda) occurs in this association, being principally obtained in small crystals lining cavities in ejected blocks of crystalline limestone at Vesuvius and the craters of the Eifel in Germany. Scapolite and wernerite are far more common at the contacts of limestone with intrusive masses. The minerals that accompany them are

text: calcite

text: epidote

text: vesuvianite

text: garnet

text: wollastonite

text: diopside

text: and

text: amphibole

text: . The scapolites are colorless, flesh-colored, grey or greenish; occasionally they are nearly black from the presence of very small enclosures of

text: graphitic

text: material. They are not in very perfect crystals, though sometimes incomplete octagonal sections are visible; the tetragonal cleavage, strong double refraction and uniaxial interference figure distinguish them readily from other minerals. Commonly they weather to micaceous aggregates, but sometimes an isotropic substance of unknown nature is seen replacing them. In crystalline limestones and

text: calc–silicate rock

text: s they occur in small and usually inconspicuous grains mingled with the other components of the rock. Large, nearly idiomorphic crystals are sometimes found in

text: argillaceous rocks

text: (altered calcareous

text: shale

text: s) that have suffered thermal metamorphism. In the Pyrenees there are extensive outcrops of limestone penetrated by igneous rocks described as ophites (varieties of

text: diabase

text: ) and iherzolites (

text: peridotite

text: s). At the contacts scapolite occurs in a great number of places, both in the limestones and in the calcareous shales that accompany them. In some of these rocks large crystals of one of the scapolite minerals (an inch or two in length) occur, usually as octagonal prisms with imperfect terminations. In others the mineral is found in small irregular grains. It is sometimes clear, but often crowded with minute enclosures of

text: augite

text: tourmaline

text: biotite

text: and other minerals, such as constitute the surrounding matrix. From these districts also a black variety is well known, filled with minute graphitic enclosures, often exceedingly small and rendering the mineral nearly opaque. The names couzeranite and dipyre are often given to this kind of scapolite. Apparently the presence of

text: chlorine

text: in small quantities, which may often be detected in limestones, to some extent determines the formation of the mineral.

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answers: scapolite limestones and contact metamorphic rocks

answers: NDQ_005762

answers: crystals are sometimes found

answers: NDQ_005763

answers: calcium

answers: NDQ_005764

answers: colorless

answers: NDQ_005765

answers: crystallized

answers: NDQ_005766

answers: argillaceous

answers: NDQ_005768

answers: crystals lining cavities

answers: NDQ_005769

answers: metamorphism

answers: NDQ_005770

answers: contact metamorphic rocks

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: There are two known processes by which magma ceases to exist: by volcanic eruption, or by crystallization within the crust or mantle to form a pluton. In both cases the bulk of the magma eventually cools and forms igneous rocks.

text: There are two known processes by which magma ceases to exist: by

text: volcanic eruption

text: , or by crystallization within the crust or mantle to form a

text: pluton

text: . In both cases the bulk of the magma eventually cools and forms

text: igneous rock

text: s.

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text: Live rock is highly valued in the aquarium trade. It introduces a diverse array of bacteria, algae, and invertebrates to the closed marine environment and functions as a superior biological filter that hosts aerobic and anaerobic nitrifying bacteria required for the nitrogen cycle that processes waste. Live rock becomes the main biological nitrification base or biological filter of a saltwater aquarium. Additionally, live rocks have a stabilizing effect on the water chemistry, in particular on helping to maintain constant pH by release of calcium carbonate. Lastly, live rock, especially when encrusted with multiple colors of coralline algae, becomes a major decorative element of the aquarium and provides shelter for the inhabitants. It is often used to build caves, arches, overhangs, or other structures in the tank, a practice known as aquascaping.

text: Live rock is highly valued in the aquarium trade. It introduces a diverse array of bacteria, algae, and invertebrates to the closed marine environment and functions as a superior

text: biological filter

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text: . Live rock becomes the main biological nitrification base or biological filter of a saltwater aquarium. Additionally, live rocks have a stabilizing effect on the water chemistry, in particular on helping to maintain constant

text: pH

text: by release of

text: calcium carbonate

text: . Lastly, live rock, especially when encrusted with multiple colors of coralline algae, becomes a major decorative element of the aquarium and provides shelter for the inhabitants. It is often used to build caves, arches, overhangs, or other structures in the tank, a practice known as

text: aquascaping

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text: FutureGen was to capture carbon dioxide produced during the gasification process and pump it into deep rock formations thousands of feet under ground. FutureGen specifically targeted rock formations containing saline water, as these are one of the most abundant types of geologic formations that can be used to store carbon dioxide worldwide. A study by the Global Energy Technology Strategy Program estimates the storage capacity of these saline rock formations in the U.S. to be 2,970 gigatons of carbon dioxide, compared to a capacity of 77 gigatons of carbon dioxide for all other types of reservoirs, such as depleted gas fields. Focusing on rock formations with saline water was intended to help ensure that the lessons learned from the project are broadly transferable throughout the U.S. and around the world.

text: FutureGen was to capture carbon dioxide produced during the gasification process and pump it into deep rock formations thousands of feet under ground. FutureGen specifically targeted rock formations containing saline water, as these are one of the most abundant types of geologic formations that can be used to store carbon dioxide worldwide. A study by the Global Energy Technology Strategy Program estimates the storage capacity of these saline rock formations in the U.S. to be 2,970 gigatons of carbon dioxide, compared to a capacity of 77 gigatons of carbon dioxide for all other types of reservoirs, such as depleted gas fields. Focusing on rock formations with saline water was intended to help ensure that the lessons learned from the project are broadly transferable throughout the U.S. and around the world.

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answers: pump it into deep rock formations

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answers: faster cooling forms smaller crystals

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answers: gasification

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answers: formations with saline water

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 0

text: Many of the rocks exposed in Turkey were formed long before this process began. Turkey contains outcrops of Precambrian rocks, (more than 540 million years old).

text: Many of the rocks exposed in Turkey were formed long before this process began. Turkey contains outcrops of

text: Precambrian

text: rocks, (more than 540 million years old).

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answer: No

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text: By the late 1960s, referred to as the "golden age"  or "classic rock" period, a number of distinct rock music subgenres had emerged, including hybrids like blues rock, folk rock, country rock, raga rock, and jazz-rock, many of which contributed to the development of psychedelic rock, which was influenced by the countercultural psychedelic scene. New genres that emerged from this scene included progressive rock, which extended the artistic elements; glam rock, which highlighted showmanship and visual style; and the diverse and enduring subgenre of heavy metal, which emphasized volume, power, and speed. In the second half of the 1970s, punk rock reacted against the perceived overblown, inauthentic and overly mainstream aspects of these genres to produce a stripped-down, energetic form of music valuing raw expression and often lyrically characterised by social and political critiques. Punk was an influence into the 1980s on the subsequent development of other subgenres, including new wave, post-punk and eventually the alternative rock movement. From the 1990s alternative rock began to dominate rock music and break through into the mainstream in the form of grunge, Britpop, and indie rock. Further fusion subgenres have since emerged, including pop punk, rap rock, and rap metal, as well as conscious attempts to revisit rock's history, including the garage rock/post-punk and synthpop revivals at the beginning of the new millennium.

text: By the late 1960s, referred to as the "golden age"  or "classic rock" period, a number of distinct rock music subgenres had emerged, including hybrids like

text: blues rock

text: folk rock

text: country rock

text: raga rock

text: , and

text: jazz-rock

text: , many of which contributed to the development of

text: psychedelic rock

text: , which was influenced by the

text: countercultural

text: psychedelic scene

text: . New genres that emerged from this scene included

text: progressive rock

text: , which extended the artistic elements;

text: glam rock

text: , which highlighted showmanship and visual style; and the diverse and enduring subgenre of

text: heavy metal

text: , which emphasized volume, power, and speed. In the second half of the 1970s,

text: punk rock

text: reacted against the perceived overblown, inauthentic and overly mainstream aspects of these genres to produce a stripped-down, energetic form of music valuing raw expression and often lyrically characterised by social and political critiques. Punk was an influence into the 1980s on the subsequent development of other subgenres, including

text: new wave

text: post-punk

text: and eventually the

text: alternative rock

text: movement. From the 1990s alternative rock began to dominate rock music and break through into the mainstream in the form of

text: grunge

text: Britpop

text: , and

text: indie rock

text: . Further fusion subgenres have since emerged, including

text: pop punk

text: rap rock

text: , and

text: rap metal

text: , as well as conscious attempts to revisit rock's history, including the

text: garage rock

text: post-punk

text: and

text: synthpop

text: revivals at the beginning of the new millennium.

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answers: Faster cooling forms larger crystals

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text: With the beginning of the Cenozoic era, some 70 million years ago, the process of erosion of the Hercynian mountain ranges changed. During the Tertiary, alpidic mountain building took place, in the course of which strong forces deformed the stumps of the Hercynian mountains. As these rocks were already folded, further tension led to cracks and fractures, which in turn created fault blocks. These blocks were later uplifted (forming horsts such as the Harz), or downfaulted (trough faults or graben such as the Upper Rhine Valley) or thrust over one another (tilted fault blocks such as the Ore Mountains). Thus the German Central Uplands exhibit the widest variety of forms, something that is also attributable to the erosion of sediments from the Mesozoic (Triassic, Jurassic and Cretaceous). In some ranges the sediments have been relatively well-preserved, in others they have been carried away completely. The determining factor is the geographical location and associated intensity of exogenous processes.

text: With the beginning of the

text: Cenozoic

text: era, some 70 million years ago, the process of erosion of the Hercynian mountain ranges changed. During the

text: Tertiary

text: alpidic mountain building

text: took place, in the course of which strong forces deformed the stumps of the Hercynian mountains. As these rocks were already folded, further tension led to cracks and fractures, which in turn created

text: fault block

text: s. These blocks were later uplifted (forming

text: horsts

text: such as the

text: Harz

text: ), or downfaulted (trough faults or

text: graben

text: such as the

text: Upper Rhine Valley

text: ) or thrust over one another (tilted

text: fault block

text: s such as the

text: Ore Mountains

text: ). Thus the German Central Uplands exhibit the widest variety of forms, something that is also attributable to the erosion of sediments from the

text: Mesozoic

text: Triassic

text: Jurassic

text: and

text: Cretaceous

text: ). In some ranges the sediments have been relatively well-preserved, in others they have been carried away completely. The determining factor is the geographical location and associated intensity of exogenous processes.

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answers: The widest variety of forms

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answers: faster cooling forms smaller crystals

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answers: During the Tertiary, alpidic mountain building

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The rock cycle  is a basic concept in geology that describes the time-consuming transitions through geologic time among the three main rock types: sedimentary, metamorphic, and igneous. As the adjacent diagram illustrates, each of the types of rocks is altered or destroyed when it is forced out of its equilibrium conditions. An igneous rock such as basalt may break down and dissolve when exposed to the atmosphere, or melt as it is subducted under a continent. Due to the driving forces of the rock cycle, plate tectonics and the water cycle, rocks do not remain in equilibrium and are forced to change as they encounter new environments. The rock cycle is an illustration that explains how the three rock types are related to each other, and how processes change from one type to another over time. This cyclical aspect makes rock change a geologic cycle and, on planets containing life, a biogeochemical cycle.

text: The rock cycle  is a basic concept in

text: geology

text: that describes the time-consuming transitions through

text: geologic time

text: among the three main

text: rock

text: types:

text: sedimentary

text: metamorphic

text: , and

text: igneous

text: . As the adjacent diagram illustrates, each of the types of rocks is altered or destroyed when it is forced out of its equilibrium conditions. An igneous rock such as

text: basalt

text: may break down and dissolve when exposed to the

text: atmosphere

text: , or melt as it is

text: subducted

text: under a

text: continent

text: . Due to the driving forces of the rock cycle,

text: plate tectonics

text: and the

text: water cycle

text: , rocks do not remain in equilibrium and are forced to change as they encounter new environments. The rock cycle is an illustration that explains how the three rock types are related to each other, and how processes change from one type to another over time. This cyclical aspect makes rock change a geologic cycle and, on planets containing

text: life

text: , a

text: biogeochemical cycle

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answers: melt

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answers: it is altered or destroyed when it is forced out of its equilibrium conditions

answer: Yes

answer: Yes

answer: Yes

answer: Yes

answer: No

answer: 1

text: Rock units are typically represented by colors. Instead of (or in addition to) colors, certain symbols can be used. Different geologic mapping agencies and authorities have different standards for the colors and symbols to be used for rocks of differing types and ages.

text: Rock units are typically represented by colors. Instead of (or in addition to) colors, certain symbols can be used. Different geologic mapping agencies and authorities have different standards for the colors and symbols to be used for rocks of differing types and ages.

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answers: rock units are typically represented by colors

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answer: No

answer: No

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text: The flow of bicarbonate ions from rocks weathered by the carbonic acid in rainwater is an important part of the carbon cycle.

text: The flow of bicarbonate ions from rocks weathered by the carbonic acid in rainwater is an important part of the

text: carbon cycle

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answers: weathering

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answers: weathered

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answers: weathered

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answers: slower cooling forms smaller crystals

answers: NDQ_005769

answers: weathering

answers: NDQ_005770

answers: The carbon cycle

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Aluminium (Al) has 22 known isotopes from Al to Al and 4 known isomers. Only Al (stable isotope) and Al (radioactive isotope, t = 7.2 × 10 y) occur naturally, however Al has a natural abundance of 99.9+ %. Other than Al, all radioisotopes have half-lives under 7 minutes, most under a second.  Relative atomic mass is 26.9815386(8). Al is produced from argon in the atmosphere by spallation caused by cosmic-ray protons. Aluminium isotopes have found practical application in dating marine sediments, manganese nodules, glacial ice, quartz in rock exposures, and meteorites. The ratio of Al to Be has been used to study the role of sediment transport, deposition, and storage, as well as burial times, and erosion, on 10 to 10 year time scales.

text: Aluminium

text: (Al) has 22 known

text: isotope

text: s from Al to Al and 4 known

text: isomers

text: . Only Al (

text: stable isotope

text: ) and Al (

text: radioactive

text: isotope,

text: t

text: = 7.2 × 10

text: y

text: ) occur naturally, however Al has a natural abundance of 99.9+ %. Other than Al, all radioisotopes have half-lives under 7 minutes, most under a second.

text: Relative atomic mass

text: is 26.9815386(8). Al is produced from

text: argon

text: in the

text: atmosphere

text: by

text: spallation

text: caused by

text: cosmic-ray

text: proton

text: s. Aluminium isotopes have found practical application in dating

text: marine

text: sediment

text: s,

text: manganese nodule

text: s, glacial ice,

text: quartz

text: in

text: rock

text: exposures, and

text: meteorite

text: s. The ratio of Al to

text: Be

text: has been used to study the role of sediment

text: transport

text: deposition

text: , and storage, as well as burial times, and erosion, on 10 to 10 year time scales.

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answers: Yes

answers: NDQ_005762

answers: sedimentary

answers: NDQ_005763

answers: The ratio of Al to Be

answers: NDQ_005764

answers: burial times

answers: NDQ_005765

answers: burial

answers: NDQ_005766

answers: meteorites

answers: NDQ_005768

answers: Aluminium isotopes

answers: NDQ_005769

answers: spallation

answers: NDQ_005770

answers: burial times, and erosion

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The rock type along a fault can have a large effect on the amount of frictional resistance present. Most crystalline rock types will have a much higher coefficient of friction as opposed to sedimentary rocks, due to their higher cohesion and a greater surface area of asperities. The rock type also controls the effect that water will have on fault friction. Laboratory experiments have proved that the presence of water will promote the rupture of a fault in carbonate rocks (marble). However, these experiments also showed that in silica-bearing rock types (microgabbro), the presence of water may delay or even inhibit the rupture of a fault. This is because when a silica-bearing fault ruptures, the rupture occurs through the “flash melting” (instantaneous melting) of the asperities. In other words, the microscopic grain contacts which hold the fault in place instantly melt due to high stresses. The presence of water delays this “flash melting” basically by cooling the contacts, and keeping them in solid form. In fault through a carbonate, the rupture occurs when these asperities experience a brittle failure. In this case, the water acts as a lubricant which promotes the failure of these asperities. The major controlling factor pertaining to the influence of rock type is not necessarily the composition of the rock, but more importantly the “roughness” of the rock at the fault interface.

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answers: Yes

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answers: sedimentary

answers: NDQ_005763

answers: the “roughness” of the rock

answers: NDQ_005764

answers: coefficient of friction

answers: NDQ_005765

answers: the “roughness” of the rock at the fault interface

answers: NDQ_005766

answers: crystalline

answers: NDQ_005768

answers: Slower cooling forms smaller crystals.

answers: NDQ_005769

answers: flash melting

answers: NDQ_005770

answers: The rock type also controls the effect that water will have on fault friction

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Metamorphic rocks make up a large part of the Earth's crust and form 12% of the Earth's current land surface. They are classified by texture and by chemical and mineral assemblage (metamorphic facies). They may be formed simply by being deep beneath the Earth's surface, subjected to high temperatures and the great pressure of the rock layers above it. They can form from tectonic processes such as continental collisions, which cause horizontal pressure, friction and distortion. They are also formed when rock is heated up by the intrusion of hot molten rock called magma from the Earth's interior. The study of metamorphic rocks (now exposed at the Earth's surface following erosion and uplift) provides information about the temperatures and pressures that occur at great depths within the Earth's crust.Some examples of metamorphic rocks are gneiss, slate, marble, schist, and quartzite.

text: Metamorphic rocks make up a large part of the

text: Earth

text: 's

text: crust

text: and form 12% of the Earth's current land surface. They are classified by

text: texture

text: and by

text: chemical

text: and

text: mineral

text: assemblage (

text: metamorphic facies

text: ). They may be formed simply by being deep beneath the Earth's surface, subjected to high temperatures and the great pressure of the rock layers above it. They can form from

text: tectonic

text: processes such as continental collisions, which cause horizontal pressure, friction and distortion. They are also formed when rock is heated up by the

text: intrusion

text: of hot molten rock called

text: magma

text: from the Earth's interior. The study of metamorphic rocks (now exposed at the Earth's surface following erosion and uplift) provides information about the temperatures and pressures that occur at great depths within the Earth's crust.Some examples of metamorphic rocks are

text: gneiss

text: slate

text: marble

text: schist

text: , and

text: quartzite

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text: The rocks observed on the Yalours and surrounding areas are predominantly igneous intrusives that have cooled deep under ground. The main rock type is grey to black gabbro composed of small crystals of grey-white feldspar and black pyroxene. The rocks here were formed by much the same process that the rest of the peninsula was formed; the Pacific plate sliding under the Antarctic Peninsula in an ocean/continent subduction-type tectonic event. This process, called orogenesis, is one of the most common ways for a mountain chain to form. The Andres and the coast ranges of North America are other classic examples of this type of tectonism. The mountain building has nearly stopped though; it is only at the very tip of the peninsula and in the South Shetland Islands that the process continues. For the rest of the peninsula, it erosion and gravity’s turn to shape the landscape.

text: The rocks observed on the Yalours and surrounding areas are predominantly igneous intrusives that have cooled deep under ground. The main rock type is grey to black gabbro composed of small crystals of grey-white feldspar and black pyroxene. The rocks here were formed by much the same process that the rest of the peninsula was formed; the Pacific plate sliding under the Antarctic Peninsula in an ocean/continent subduction-type tectonic event. This process, called orogenesis, is one of the most common ways for a mountain chain to form. The Andres and the coast ranges of North America are other classic examples of this type of tectonism. The mountain building has nearly stopped though; it is only at the very tip of the peninsula and in the South Shetland Islands that the process continues. For the rest of the peninsula, it erosion and gravity’s turn to shape the landscape.

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answers: The main rock type is grey to black gabbro

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answers: intrusive

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answers: Pacific plate sliding under the Antarctic Peninsula

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answers: The main rock type is grey to black gabbro

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answers: orogenesis

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answers: orogenesis, is one of the most common ways for a mountain chain to form

answer: No

answer: No

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text: In the last match, John Cena challenged WWE Champion The Miz (accompanied by Alex Riley). During the match, Cena delivered the Five Knuckle Shuffle to The Miz. Cena attempted the Attitude Adjustment, but Miz countered with a DDT. There was a lot of back and forth action until The Miz executed the Skull Crushing Finale and Cena executed an Attitude Adjustment on Miz - both for near-falls. Both men fought outside of the ring, knocking each other out in the process, and were counted out. The Rock came out to intervene, when a message from the Anonymous Raw General Manager arrived. The Rock went to read it, but then disregarded it and restarted the match under no disqualification, no countout, no time limit stipulations. Cena dragged Miz back inside the ring and attempted an Attitude Adjustment. The Rock stalked Cena from behind and performed a Rock Bottom on him. Taking advantage, The Miz then pinned Cena for the win. After the match, The Rock had a staredown with Miz until Rock delivered a spinebuster and a People’s Elbow. WrestleMania XXVII went off air with The Rock posing on top of the turnbuckles for the fans.

text: In the last match,

text: John Cena

text: challenged

text: WWE Champion

text: The Miz

text: (accompanied by

text: Alex Riley

text: ). During the match, Cena delivered the

text: Five Knuckle Shuffle

text: to The Miz. Cena attempted the

text: Attitude Adjustment

text: , but Miz countered with a

text: DDT

text: . There was a lot of back and forth action until The Miz executed the

text: Skull Crushing Finale

text: and Cena executed an Attitude Adjustment on Miz - both for near-falls. Both men fought outside of the ring, knocking each other out in the process, and were counted out.

text: The Rock

text: came out to intervene, when a message from the Anonymous Raw General Manager arrived. The Rock went to read it, but then disregarded it and restarted the match under no disqualification, no countout, no time limit stipulations. Cena dragged Miz back inside the ring and attempted an Attitude Adjustment. The Rock stalked Cena from behind and performed a

text: Rock Bottom

text: on him. Taking advantage, The Miz then pinned Cena for the win. After the match, The Rock had a staredown with Miz until Rock delivered a spinebuster and a

text: People’s Elbow

text: . WrestleMania XXVII went off air with The Rock posing on top of the turnbuckles for the fans.

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answers: faster cooling forms smaller crystals

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answers: Rock Bottom on him

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 0

text: In geology and geomorphology an erosion surface is a surface of rock or regolith that was formed by erosion and not by construction (e.g. lava flows, sediment deposition) nor fault displacement. Erosional surfaces within the stratigraphic record are known as unconformities, but not all unconformities are buried erosion surfaces. Erosion surfaces can be either small or large. Particularly large and flat erosion surfaces receive the names of peneplain, paleoplain, planation surface or pediplain.

text: In

text: geology

text: and

text: geomorphology

text: an erosion surface is a surface of

text: rock

text: or

text: regolith

text: that was formed by

text: erosion

text: and not by construction (e.g. lava flows, sediment deposition) nor

text: fault displacement

text: . Erosional surfaces within the

text: stratigraphic record

text: are known as

text: unconformities

text: , but not all unconformities are buried erosion surfaces. Erosion surfaces can be either small or large. Particularly large and flat erosion surfaces receive the names of

text: peneplain

text: paleoplain

text: planation surface

text: or

text: pediplain

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answers: Erosional surfaces

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Crystallization mechanism forms the core of all the problems in crystal engineering. A proper understanding of crystallization mechanisms will enable us to sort among the various possibilities generated by say CSP. Moreover, it will help a crystal engineer to design a solid with particular function. It is therefore of immense importance to understand the progression from solution to the nucleus to the crystal structures, in other terms, how the entropy dominated situation in solution converts to an enthalpy driven one in the crystals through the nucleation step. As the nucleus is difficult to identify, the approaches made towards this end can be generally divided into two categories. The first type centers on the studies in solution through various spectroscopic techniques to understand the structure of the assembly in the solution and these studies give an idea about the initial stages of crystallization. The second type of approach take into account all the relevant crystal structures of a given compound and this constitutes a structural landscape. Each structure in a structural landscape is considered as an individual data point and while taken together it provides a holistic viewpoint towards the crystallization mechanism. A special situation happens when multiple components are observed in an asymmetric unit (Z′>1). These structures result from the interrupted crystallization and therefore shed lights on the intermediate stages of crystallization.

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answer: No

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text: Dunite ( or ) (also known as olivinite, not to be confused with the mineral olivenite) is an igneous, plutonic rock, of ultramafic composition, with coarse-grained or phaneritic texture. The mineral assemblage is greater than 90% olivine, with minor amounts of other minerals such as pyroxene, chromite, magnetite, and pyrope. Dunite is the olivine-rich end-member of the peridotite group of mantle-derived rocks. Dunite and other peridotite rocks are considered the major constituents of the Earth's mantle above a depth of about 400 kilometers. Dunite is rarely found within continental rocks, but where it is found, it typically occurs at the base of ophiolite sequences where slabs of mantle rock from a subduction zone have been thrust onto continental crust by obduction during continental or island arc collisions (orogeny). It is also found in alpine peridotite massifs that represent slivers of sub-continental mantle exposed during collisional orogeny. Dunite typically undergoes retrograde metamorphism in near-surface environments and is altered to serpentinite and soapstone.

text: Dunite ( or ) (also known as olivinite, not to be confused with the mineral

text: olivenite

text: ) is an

text: igneous

text: plutonic

text: rock

text: , of

text: ultramafic

text: composition, with coarse-grained or

text: phaneritic

text: texture. The

text: mineral

text: assemblage is greater than 90%

text: olivine

text: , with minor amounts of other minerals such as

text: pyroxene

text: chromite

text: magnetite

text: , and

text: pyrope

text: . Dunite is the olivine-rich end-member of the

text: peridotite

text: group of mantle-derived rocks. Dunite and other peridotite rocks are considered the major constituents of the Earth's

text: mantle

text: above a depth of about 400 kilometers. Dunite is rarely found within continental rocks, but where it is found, it typically occurs at the base of

text: ophiolite

text: sequences where slabs of mantle rock from a

text: subduction zone

text: have been thrust onto

text: continental crust

text: by

text: obduction

text: during continental or

text: island arc

text: collisions (

text: orogeny

text: ). It is also found in alpine peridotite massifs that represent slivers of sub-continental mantle exposed during collisional orogeny. Dunite typically undergoes retrograde

text: metamorphism

text: in near-surface environments and is altered to

text: serpentinite

text: and

text: soapstone

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answers: All rocks are part of the rock cycle.

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answers: Metamorphism

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Rastoke as a place name has different meanings. The term generally refers to the branching of rivers. At Rastoke, the Slunjčica river (also called Slušnica by local people) splits into several river branches flowing across cascades and small waterfalls into the Korana river. Rastoke also refers to a certain kind of limestone called rastopina or rastok in the Croatian language. This stone, called travertine or tufa (Croatian sedra), is a product of permanent natural activities created by natural dissolution and sedimentation of calcium carbonate. The flowing water dissolves limestone into calcium carbonate. These particles in turn sediment along the cascades where the water is being stirred up. The quantity of carbon dioxide in the water plays a major role in this process of sedimentation. This effect slowly but permanently creates new rock along the river's cascades.

text: Rastoke as a place name has different meanings. The term generally refers to the branching of rivers. At Rastoke, the

text: Slunjčica

text: river (also called Slušnica by local people) splits into several river branches flowing across

text: cascade

text: s and small

text: waterfall

text: s into the

text: Korana

text: river. Rastoke also refers to a certain kind of limestone called rastopina or rastok in the

text: Croatian language

text: . This stone, called

text: travertine

text: or

text: tufa

text: (Croatian sedra), is a product of permanent natural activities created by natural dissolution and sedimentation of

text: calcium carbonate

text: . The flowing water dissolves limestone into calcium carbonate. These particles in turn sediment along the cascades where the water is being stirred up. The quantity of

text: carbon dioxide

text: in the water plays a major role in this process of sedimentation. This effect slowly but permanently creates new rock along the river's cascades.

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answers: This effect slowly but permanently creates new rock

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answers: The quantity of carbon dioxide

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answers: sedimentation

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answers: tufa

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answers: This effect slowly but permanently creates new rock along the river's cascades

answers: NDQ_005769

answers: sedimentation

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answers: permanently

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Variations in stability of the underlying rock influence development of a bedrock-channeled river, as the waters erode different rock types at different rates. Victoria Falls, on the Zambezi River, is a spectacular example of this. The gorges visible by satellite imagery illustrate the erosional processes behind the formation of the falls. Here, much of the surface rock is a massive basalt sill, with large cracks filled with easily weathered sandstone made visible by the Zambezi's course across the land. The gorges downstream of the falls through which it flows were eroded over time by the action of the water.

text: Variations in stability of the underlying rock influence development of a bedrock-channeled river, as the waters erode different rock types at different rates.

text: Victoria Falls

text: , on the

text: Zambezi River

text: , is a spectacular example of this. The gorges visible by satellite imagery illustrate the

text: erosion

text: al processes behind the formation of the falls. Here, much of the surface rock is a massive

text: basalt

text: sill

text: , with large cracks filled with easily weathered

text: sandstone

text: made visible by the Zambezi's course across the land. The

text: gorge

text: s downstream of the falls through which it flows were eroded over time by the action of the water.

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answers: Different rock types at different rates

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answers: stability

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answers: basalt sill

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answers: faster cooling forms smaller crystals

answers: NDQ_005769

answers: weathering

answers: NDQ_005770

answers: erode different rock types at different rates

answer: No

answer: No

answer: Yes

answer: No

answer: No

answer: 1

text: Crystal Rock began as a delivery company in 1914 in Stamford, Connecticut, started by Henry Baker, Sr. In 1939, the company established its first water bottling plant in Stamford. Crystal Rock Waters was born in 1965, with Henry Baker Jr. serving as President and Chairman of the Board of Directors of the company. Since then, Crystal Rock has grown rapidly in delivering water and non-perishable snack refreshments. In 1988, Crystal Rock moved its official headquarters to Watertown. In 1990, Henry Baker, Jr. was honored by the Bottled Water Hall of Fame and three years later, Peter and Jack Baker were appointed Co-Presidents of Crystal Rock. In 2000, Crystal Rock merged with Vermont Pure water company to cooperate in the bottled water company. In May 2010, Vermont Pure Holdings, Ltd. changed its corporate name to Crystal Rock Holdings, Inc. In 2010, the company went public on the New York Stock Exchange as Crystal Rock Holdings, Inc ( NYSE MKT: CRVP). Crystal Rock has sold office products under its Crystal Rock Office brand since 2011.  In 2012, Crystal Rock Learning & Development Center was opened in Watertown for corporate education. In the same year, Crystal Rock acquired the assets of Hartford Stamp and merged the company with Crystal Rock Office brand. In 2013 Crystal Rock Holdings, Inc. acquired the assets of Universal Business Equipment Corp.

text: Crystal Rock began as a delivery company in 1914 in

text: Stamford

text: Connecticut

text: , started by Henry Baker, Sr. In 1939, the company established its first water bottling plant in Stamford. Crystal Rock Waters was born in 1965, with Henry Baker Jr. serving as President and Chairman of the Board of Directors of the company. Since then, Crystal Rock has grown rapidly in delivering water and non-perishable snack refreshments. In 1988, Crystal Rock moved its official headquarters to

text: Watertown

text: . In 1990, Henry Baker, Jr. was honored by the Bottled Water Hall of Fame and three years later, Peter and Jack Baker were appointed Co-Presidents of Crystal Rock. In 2000, Crystal Rock merged with Vermont Pure water company to cooperate in the bottled water company. In May 2010, Vermont Pure Holdings, Ltd. changed its corporate name to Crystal Rock Holdings, Inc. In 2010, the company went public on the

text: New York Stock Exchange

text: as Crystal Rock Holdings, Inc (

text: NYSE

text: MKT: CRVP). Crystal Rock has sold office products under its Crystal Rock Office brand since 2011.  In 2012, Crystal Rock Learning & Development Center was opened in Watertown for corporate education. In the same year, Crystal Rock acquired the assets of Hartford Stamp and merged the company with Crystal Rock Office brand. In 2013 Crystal Rock Holdings, Inc. acquired the assets of Universal Business Equipment Corp.

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text: Rock Monster wakes up and chases Clutch to the underground Power Miner headquarters. Clutch escapes into a tunnel, but finds out that the crystal is actually a baby rock monster. He returns it to the queen, who gives a crystal to Clutch.  Clutch then returns to his home in the Lego City and hands the crystal to his boss Kjeld Playwell (Paul Michael Glaser) who assigns him some new teammates: Brick Masterson (Roger Rose), a firefighter, weapons specialist, and demolition expert; Peg Mooring (Yvonne Strahovski) a biologist, and Bernie von Beam (Jeff Bennett) an engineer. Playwell informs of an incident in the Space Police prison planet when chaos occurs regarding to the imprisonment of the three most wanted criminals in the Lego galaxy. Clutch and his team investigate the situation at once, despite the team's lack of cooperation and Clutch's intent of working alone. They soon arrive at the planet. There, they hear a rumbling sound turning out to be Brick's stomach who then burps green gas 3 times in satisfaction.

text: Rock Monster wakes up and chases Clutch to the underground Power Miner headquarters. Clutch escapes into a tunnel, but finds out that the crystal is actually a baby rock monster. He returns it to the queen, who gives a crystal to Clutch.  Clutch then returns to his home in the

text: Lego City

text: and hands the crystal to his boss Kjeld Playwell (

text: Paul Michael Glaser

text: ) who assigns him some new teammates: Brick Masterson (

text: Roger Rose

text: ), a

text: firefighter

text: , weapons specialist, and demolition expert; Peg Mooring (

text: Yvonne Strahovski

text: ) a

text: biologist

text: , and Bernie von Beam (

text: Jeff Bennett

text: ) an

text: engineer

text: . Playwell informs of an incident in the

text: Space Police

text: prison planet when chaos occurs regarding to the imprisonment of the three most wanted criminals in the Lego galaxy. Clutch and his team investigate the situation at once, despite the team's lack of cooperation and Clutch's intent of working alone. They soon arrive at the planet. There, they hear a rumbling sound turning out to be Brick's stomach who then burps green gas 3 times in satisfaction.

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text: Tides often determine the range over which sediment is deposited or eroded. Areas with high tidal ranges allow waves to reach farther up the shore, and areas with lower tidal ranges produce deprossosition at a smaller elevation interval. The tidal range is influenced by the size and shape of the coastline. Tides do not typically cause erosion by themselves; however, tidal bores can erode as the waves surge up river estuaries from the ocean.

text: Tide

text: s often determine the range over which

text: sediment

text: is deposited or eroded. Areas with high tidal ranges allow waves to reach farther up the shore, and areas with lower tidal ranges produce deprossosition at a smaller elevation interval. The tidal range is influenced by the size and shape of the coastline. Tides do not typically cause erosion by themselves; however,

text: tidal bore

text: s can erode as the waves surge up river

text: estuaries

text: from the ocean.

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answers: eroded

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answers: faster cooling forms smaller crystals

answers: NDQ_005769

answers: erosion

answers: NDQ_005770

answers: deprossosition

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: Carbonatites are rare, peculiar igneous rocks formed by unusual processes and from unusual source rocks. Three models of their formation exist:

text: Carbonatites are rare, peculiar igneous rocks formed by unusual processes and from unusual source rocks. Three models of their formation exist:

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answers: 4: The answer is mostly relevant and complete, with minor gaps or inaccuracies.

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answers: Yes

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answers: Carbonatites

answers: NDQ_005763

answers: unusual processes and from unusual source rocks

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answers: peculiar

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answers: Carbonatites

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answers: Carbonatites

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answers: slower cooling forms smaller crystals

answers: NDQ_005769

answers: Carbonatites

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answers: Carbonatites

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: While the water cycle is itself a biogeochemical cycle, flow of water over and beneath the Earth is a key component of the cycling of other biogeochemicals. Runoff is responsible for almost all of the transport of eroded sediment and phosphorus from land to waterbodies. The salinity of the oceans is derived from erosion and transport of dissolved salts from the land. Cultural eutrophication of lakes is primarily due to phosphorus, applied in excess to agricultural fields in fertilizers, and then transported overland and down rivers. Both runoff and groundwater flow play significant roles in transporting nitrogen from the land to waterbodies. The dead zone at the outlet of the Mississippi River is a consequence of nitrates from fertilizer being carried off agricultural fields and funnelled down the river system to the Gulf of Mexico. Runoff also plays a part in the carbon cycle, again through the transport of eroded rock and soil.

text: While the water cycle is itself a

text: biogeochemical cycle

text: , flow of water over and beneath the Earth is a key component of the cycling of other biogeochemicals. Runoff is responsible for almost all of the transport of

text: eroded

text: sediment

text: and

text: phosphorus

text: from land to

text: waterbodies

text: . The

text: salinity

text: of the oceans is derived from erosion and transport of dissolved salts from the land. Cultural

text: eutrophication

text: of lakes is primarily due to phosphorus, applied in excess to

text: agricultural fields

text: in

text: fertilizer

text: s, and then transported overland and down rivers. Both runoff and groundwater flow play significant roles in transporting nitrogen from the land to waterbodies. The

text: dead zone

text: at the outlet of the

text: Mississippi River

text: is a consequence of

text: nitrate

text: s from fertilizer being carried off agricultural fields and funnelled down the

text: river system

text: to the

text: Gulf of Mexico

text: . Runoff also plays a part in the

text: carbon cycle

text: , again through the transport of eroded rock and soil.

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answers: Yes

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answers: sedimentary

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answers: flow of water

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answers: carbon cycle

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answers: Runoff

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answers: faster cooling forms smaller crystals

answers: NDQ_005769

answers: Dead zone

answers: NDQ_005770

answers: The dead zone at the outlet of the Mississippi River

answer: No

answer: No

answer: No

answer: No

answer: No

answer: 1

text: The Rock Monsters are the enemies of the miners (Duke, Brains, Rex, and Doc). They appear in all the sets from the Power Miners series. They are made of different colored rock and crystals. There are five different kinds of Rock Monster. The rock monsters are Meltrox, Boulderax, Glaciator, Sulfurix, Firox, Geolix, Tremorox and RockRage (Crystal King). They are shown to have some primitive technology, like monster launchers. The Rock Monsters eat crystals, which give them power. If a rock monster eats a different colored crystal to what it is it will burp and break wind.

text: The Rock Monsters are the enemies of the miners (Duke, Brains, Rex, and Doc). They appear in all the sets from the Power Miners series. They are made of different colored rock and crystals. There are five different kinds of Rock Monster. The rock monsters are Meltrox, Boulderax, Glaciator, Sulfurix, Firox, Geolix, Tremorox and RockRage (Crystal King). They are shown to have some primitive technology, like monster launchers. The Rock Monsters eat crystals, which give them power. If a rock monster eats a different colored crystal to what it is it will burp and break wind.

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answers: The Rock Monsters eat crystals

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answers: The Rock Monsters eat crystals

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answers: slower cooling forms smaller crystals

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answers: Rock Monsters eat crystals, which give them power

answer: No

answer: No

answer: No

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text: Pipe can be made of materials such as PVC, polyethylene, polypropylene, ductile iron, and steel as long as it can be pulled through the drilled hole. Directional boring is not practical if there are voids in the rock or incomplete layers of rock. The best material is solid rock or sedimentary material. Soils with cobblestone are not recommended. There are different types of heads used in the pilot-hole process, and they depend on the geological material.

text: Pipe can be made of materials such as

text: PVC

text: polyethylene

text: polypropylene

text: ductile iron

text: , and

text: steel

text: as long as it can be pulled through the drilled hole. Directional boring is not practical if there are voids in the rock or incomplete layers of rock. The best material is solid rock or sedimentary material. Soils with cobblestone are not recommended. There are different types of heads used in the pilot-hole process, and they depend on the geological material.

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answers: solid rock

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answers: faster cooling forms smaller crystals

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answer: No

answer: No

answer: No

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answer: 1

text: The final match on the undercard featured The Rock defending the WCW Championship against Chris Jericho. As the match started, Rock tried to perform a Rock Bottom on Jericho but Jericho countered it into the Walls of Jericho but Rock caught the ropes. Jericho hit Rock with a Springboard Dropkick through the ring apron. Jericho used several of his moves on Rock and got several near-falls until Rock made a comeback into the match by clotheslining Jericho. Rock planted Jericho in the corner and delivered him a Superplex. Rock performed a Snap Belly to Belly Suplex and a Samoan Drop for a near-fall. Rock and Jericho continued to assault each other and the action even spilled to the outside on numerous occasions until Jericho started mocking Rock by using his moves. Jericho hit Rock with his own finisher Rock Bottom, followed by a Lionsault for a nearfall. Jericho hit Rock with a One-handed Bulldog. Jericho attempted to hit Rock's own finisher People's Elbow but Rock avoided the move and applied a Sharpshooter on Jericho. Jericho reached the ropes and caught them. Rock left the ring and removed the top of the Spanish announce table and removed the monitors. Rock brought Jericho outside the ring and pulled him on the table and performed a Rock Bottom on the table. The action returned to the ring where Rock hit Jericho, a Spinebuster and attempted to hit a People's Elbow but Jericho countered it into the Walls of Jericho. Stephanie McMahon interfered in the match and came down to the ringside. She threw a chair in the ring. Jericho started chasing Stephanie. Rock took advantage and hit Jericho, a Snap DDT. Rock focused on Stephanie, pulled her into the ring and hit her with a Rock Bottom. Jericho took advantage and grabbed Rock from behind and performed his new finisher, the Breakdown on Rock on the chair to pin him for the WCW Championship. After the match, Rock grabbed the chair in his hand but gave it to Jericho and left.

text: The final match on the

text: undercard

text: featured

text: The Rock

text: defending the

text: WCW Championship

text: against

text: Chris Jericho

text: . As the match started, Rock tried to perform a

text: Rock Bottom

text: on Jericho but Jericho countered it into the

text: Walls of Jericho

text: but Rock caught the ropes. Jericho hit Rock with a

text: Springboard Dropkick

text: through the ring apron. Jericho used several of

text: his moves

text: on Rock and got several near-falls until Rock made a comeback into the match by clotheslining Jericho. Rock planted Jericho in the corner and delivered him a

text: Superplex

text: . Rock performed a

text: Snap

text: Belly to Belly Suplex

text: and a

text: Samoan Drop

text: for a near-fall. Rock and Jericho continued to assault each other and the action even spilled to the outside on numerous occasions until Jericho started mocking Rock by using his moves. Jericho hit Rock with his own finisher Rock Bottom, followed by a

text: Lionsault

text: for a nearfall. Jericho hit Rock with a

text: One-handed Bulldog

text: . Jericho attempted to hit Rock's own finisher

text: People's Elbow

text: but Rock avoided the move and applied a

text: Sharpshooter

text: on Jericho. Jericho reached the ropes and caught them. Rock left the ring and removed the top of the Spanish announce table and removed the monitors. Rock brought Jericho outside the ring and pulled him on the table and performed a Rock Bottom on the table. The action returned to the ring where Rock hit Jericho, a

text: Spinebuster

text: and attempted to hit a People's Elbow but Jericho countered it into the Walls of Jericho.

text: Stephanie McMahon

text: interfered in the match and came down to the ringside. She threw a chair in the ring. Jericho started chasing Stephanie. Rock took advantage and hit Jericho, a

text: Snap DDT

text: . Rock focused on Stephanie, pulled her into the ring and hit her with a Rock Bottom. Jericho took advantage and grabbed Rock from behind and performed his new finisher, the

text: Breakdown

text: on Rock on the chair to pin him for the WCW Championship. After the match, Rock grabbed the chair in his hand but gave it to Jericho and left.

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