Earth Materials and the Cycle of Rock Transformation Flashcards

1
Q

______ the outermost layer of the planet

A

earths crust

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2
Q

Crust’s thickness ranges between

A

n 8 to 80 km and comprises the continents and ocean basin

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3
Q

the thickness of the oceanic crust is generally

A

less than 10 k

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4
Q

continental crust

A

averages about 40 km

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5
Q

About 10 percent of the crust exceeds 50 km, with the greatest thickness reported in the ________, where it is about 80 km

A

Himalayas

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6
Q

mineral definition

A

A mineralcan be defined as a naturally occurring, inorganic substance that has a definite chemical composition and a characteristic atomic structure. This gives each mineral its distinctive properties, such as colour, lustre, and hardness. Most minerals have a crystalline structure that reflects the internal arrangement of its composing atoms

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7
Q

When minerals are combined they form

A

rock

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8
Q

are solidified from mineral matter in a high temperature molten state. The mineral grains in igneous rocks are tightly interlocked, and the rock is normally very strong

A

igneous rock

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9
Q

magma

A

cools and solidifies between about 600 and 1,200 °C, either below the surface as intrusive rocks, such as granite, or on the surface as extrusive rocks, such as volcanic lava

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10
Q

Layered accumulations of mineral particles which are derived mostly by weathering and erosion of pre-existing rock lead to the formation of

A

sedimentery rock

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11
Q

Diagenesis

A

reveals the various chemical, physical, and biological changes that occur as layers of sediment transform into rocks. The resulting rock layers are called strata.

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12
Q

s are the most common exposed rock types and cover about 75 percent of the Earth’s surface. However, they account for only about 5 percent of the total mass of the Earth’s rocks because they are only found within a comparatively thin layer over igneous and metamorphic rock

A

sedimentery rocks

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13
Q

Unlike igneous and metamorphic rocks, sedimentary rocks often contain______

A

fosils

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14
Q

When igneous or sedimentary rocks are physically or chemically changed, due to the subsequent application of heat and pressure during episodes of significant crustal movement, they turn intto

A

metamorphic rocks

The process of metamorphismcreates new minerals and rock structures

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15
Q

formation of igneou rock

A

Igneous rock crystallizes from hot, molten magma that originates deep below the surface of the Earth. The molten rock migrates upward from the magma chambers through fractures in older solid rock and eventually solidifies within (igneous intrusive rock; intrusion) or on top (extrusive igneous rock; lava) of the Earth’s crust

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16
Q

The _________ and ______are the main determinants of rock composition and crystal size

A

chemical composition of the magma and the rate of cooling

17
Q

the _____________ that form igneous rocks are chemical compounds that contain silicon and oxygen atoms, combined with various proportions of other elements, particularly aluminum, iron, calcium, sodium, potassium, and magnesium

A

silicate minerals

18
Q

quartz

A

) is one of the most common minerals. It is quite hard and resists chemical breakdow

19
Q

silicate aluminim minerals

A

feldspars

20
Q

Quartz and feldspar form the ______mineral group

A

felsic

These minerals are light in colour (white, pink, or grayish) and lower in density than the other silicate minerals; they form at comparatively low temperatures.

21
Q

Other common silicate minerals include the biotite, amphibole, and pyroxene groups. All three contain aluminum, magnesium, iron, and potassium or calcium. These minerals are described as __________

A

mafic

(“ma” for magnesium; “f ” from the chemical symbol Fe for iron).

All of these mafic minerals are dark in colour(usually black) and are denser than the felsicminerals. The mafic minerals are characteristically found in rocks that solidify at high temperature

22
Q

Granite is one of the most common intrusive igneous rocks. Typical graniteconsists mainly of potassium feldspar, with lesser amounts of quartz and Na-plagioclase, and some mica and amphibole. Because most of the volume of granite is of felsicminerals, granite is classified as _________

A

felsic igneou rock

23
Q

rocks cool very slowly — over hundreds or thousands of years — and, as a result, develop large, readily seen crystals (granite and diorite are good examples of coarse-textured intrusive igneous rocks).

A

intruive rocks

24
Q

which cools rapidly, is fine-textured, and the individual crystals can only be seen through a microscope. Most lava solidifies as a dense, uniform rock with a dark, dull surface. Sometimes lava cools to form shiny obsidian or volcanic glass. If the lava contains dissolved gases, it may solidify to form scoria, a rock with a frothy, bubble-filled texture.

A

extrusive rocks

25
Q

body of intrusive igneous rock is called

A

pluton

26
Q

ranite typically accumulates in enormous plutons, called

A

batholiths

27
Q

chemical weathering

A

Once exposed, igneous rock minerals may also be altered by water and dissolved gase

28
Q

mechanical weathering

A

Weathering also includes physical forces, like frost action, that break up rock into small fragments and separate the component minerals, grain by grain. Rock fragmentation caused in this way is termed mechanical weathering (accelerates mineral alteration because it greatly increases the surface area that is exposed to chemically active solutions)

29
Q

n the process of mineral alteration, solid rock is weakened, softened, and fragmented, yielding particles of many sizes and mineral compositions. When transported by a fluid medium, such as water or air, these particles are known collectively a

A

sediment

30
Q

e three major types of sedimentary material

A

the first type is clastic sediment, which consists of inorganic rock and mineral fragments called clasts. The second type is chemically precipitated sediment, which consists of inorganic mineral compounds precipitated from a chemical solution. The third class is organic sediment, which consists of the tissues of plants and animals, accumulated and preserved after death.

31
Q

coal

A

is the end result of this process, with individual coal seams interbedded with shale, sandstone, and limestone strata.

32
Q

oil deposits and natural gas

A

f organic origin, but they are classed as mineral fuels rather than minerals. Oil and gas deposits commonly occupy open, interconnected pores in a thick sedimentary rock layer, such as a porous sandstone

33
Q

Igneous or sedimentary rock may be altered by the tremendous pressures and high temperatures that accompany crustal deformation processes, such as the creation of mountain ranges. The result is rock so changed in texture and structure that it is reclassified a

A

metamorphic

34
Q

Igneous, sedimentary, and metamorphic rocks are transformed from one to another in a continuous cycle over the course of many millions of years. Igneous rock forms when pre-existing rock of any class melts and this magma subsequently cools and solidifies. Through weathering and erosion, pre-existing rock breaks down and the fragments accumulate in layers that eventually become compacted, forming sedimentary rock

A

qqq

35
Q

(cycle of rock transformation or the rock cycle

A

Heat and pressure, without complete melting, convert igneous and sedimentary rock to metamorphic rock. These combined processes constitute a single system that creates and recycles Earth materials from one form to another over geologic time