Test 2 Chapter 3 Flashcards

1
Q

Use the rock cycle to explain the statement “One rock is the raw material for another”.

A

The rock cycle illustrates that any rock type can be transformed into any other rock type. As an
example, igneous rocks may be weathered and compacted into sedimentary rocks. Those
sedimentary rocks may be subjected to heat and pressure to become metamorphic rocks. Depending
on the conditions, rocks can be continually transformed into different types of rock.

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2
Q

What is magma? How does magma differ from lava?

A

Magma is liquid, molten rock. It is found underground, whereas lava is found extrusively, or outside
Earth’s interior.

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3
Q

In what basic settings do intrusive and extrusive igneous rocks originate?

A

Intrusive igneous rocks cool below the surface of the Earth. Extrusive igneous rocks cool outside the
Earth’s interior.

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4
Q

How does the rate of cooling influence crystal size? What other factors influence the texture of
igneous rocks?

A

Faster cooling correlates with smaller crystal size. Other influential factors include the
composition of the magma and the presence of gases, such as in a volcano, which can cause a
vesicular texture.

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5
Q

What does a porphyritic texture indicate about the history of an igneous rock?

A

A porphyritic texture, where the rock has some large and some small crystals, indicates that the rock
started to cool slowly and then experienced a change of environment or cooling temperature where
the rest of the rock cooled more quickly.

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6
Q

List and distinguish among the four basic compositional groups of igneous rocks

A

Granitic – felsic or light colored rocks where the dominant minerals are quartz and potassium feldspar.
Andesitic – intermediate rocks where the dominant minerals are amphibole and plagioclase. These are neither light nor dark.
Basaltic – mafic or dark colored rocks with high amounts of magnesium and/or iron. The dominant minerals are pyroxene and plagioclase feldspar.
Ultramafic – these are uncommon rocks with very high amounts of magnesium and/or iron. The dominant minerals are olivine and pyroxene.

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7
Q

How are granite and rhyolite different? In what way are they similar?

A

Granite has a phaneritic, or coarse-grained texture whereas rhyolite is aphanitic, or fine-grained.
They are compositionally similar, being granitic or felsic rocks. They could be from the same
magma type but the rate of cooling has affected their crystal sizes

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8
Q

What is magmatic differentiation? How might this process lead to the formation of several different
igneous rocks from a single magma?

A

Magmatic differentiation occurs as magma cools and crystals of minerals with higher melting
temperatures crystallize out of the magma, changing the magmatic composition. By depleting the
magma, or melt, of these minerals, the next rocks to form from the cooling magma will have a
different composition than those that formed at higher temperatures.

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9
Q

Why are sedimentary rocks important?

A

Sedimentary rocks contain almost all of the fossil record. Sedimentary rocks make up about 75% of
continental rock outcrops and contain clues to the history of the Earth’s surface. They also have
economic importance; for example: limestone used for cement is a sedimentary rock and other
natural resources, including energy resources, are extracted from sedimentary rocks.

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10
Q

What minerals are most abundant in detrital sedimentary rocks? In which rocks do these sediments
predominate?

A

Quartz and clay minerals, especially from feldspars, are most abundant. These rocks predominate
in conglomerate, breccia, sandstone, arkose, siltstone, and shale.

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11
Q

Distinguish between conglomerate and breccia

A

Both conglomerate and breccia are made of large-sized sedimentary grains. However,
conglomerate consists of grains that have been rounded before compaction and breccia contains
angular grains of rock and minerals

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12
Q

What are the two groups of chemical sedimentary rocks? Give an example of a rock that belongs to
each group.

A

The two categories of chemical sedimentary rock are: chemical and biochemical.
A chemical sedimentary rock is travertine limestone. Another is chert. A biochemical rock is
coquina or coal.

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13
Q

How do evaporites form. Give an example.

A

Evaporites form when minerals are dissolved in solution and the water of that solution evaporates
away. One example is rock salt.

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14
Q

Describe the two processes by which sediments are transformed into sedimentary rocks. Which is
the more effective process in the lithification of sand- and gravel-sized sediments.

A

The two processes by which sediments are transformed into sedimentary rocks are:
Compaction – where pressure is placed on loosely packed sediment. The volume of the sediment
is reduced and water is squeezed out.
Cementation – when mineral-bearing water circulates among the grains, hardens, and cements
the sediment grains together. This process is most effective for lithifying sand and gravel-sized
sediments.

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15
Q

List three common cements. How might each be identified?

A

Three common sedimentary cements are:
Calcite – effervesces when a drop of weak HCl is placed on it.
Silica – hardest cement, will scratch glass.
Iron oxide – oxidizes to a rusty red color.

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16
Q

What is the single most characteristic of sedimentary rocks?

A

The most characteristic features of sedimentary rocks are strata, or layers that are formed
as these rocks are laid down.

17
Q

Metamorphism means “to change form”. Describe how a rock may change during metamorphism

A

During metamorphism, a rock may change its mineralogy, its texture, and sometimes its chemical
composition

18
Q

Explain what is meant by the statement “every metamorphic rock has a parent rock”.

A

Metamorphic rocks are existing rocks that have been altered by heat and/or pressure. Therefore,
every metamorphic rock was another type of rock, a parent rock, initially

19
Q

List the four agents of metamorphism and describe the role of each

A

The four agents of metamorphism are:
Heat – triggers chemical reactions that result in the recrystallization of existing minerals and
the formation of new minerals.
Confining pressure – buried rocks experience even pressure from all directions, which creates
a more compact, denser rock.
Differential stress – often occurs during mountain building where rocks experience unequal
forces from different directions. This creates rocks that have been deformed, often with flattened
mineral grains.
Chemically active fluids – ion-rich fluids invade the rock and enhance ion migration. Often hot,
these fluids can generate mineral recrystallization.

20
Q

Distinguish between regional metamorphism and contact metamorphism

A

Regional metamorphism is associated with mountain building and involves large amounts of
pressure and high temperatures. It results in large-scale rock deformation. Contact metamorphism
occurs when rock is in contact with hot magma. In these cases, metamorphism is heat-related.

21
Q

What feature easily distinguished schist and gneiss from quartzite and marble?

A

Schist and gneiss are foliated; quartzite and marble are not foliated.

22
Q

In what ways do metamorphic rocks differ from the igneous and sedimentary rocks from which they
formed?

A

Metamorphic rocks are typically more compact than the parent igneous and sedimentary rocks.
Metamorphic rocks may also exhibit minerals aligned in one particular direction rather than
randomly dispersed in the rock. Minerals also may segregate during metamorphism.

23
Q

List two types of hydrothermal deposits.

A

The two general types of hydrothermal deposits are:
Vein deposits and disseminated deposits.

24
Q

Nonmetallic resources are commonly divided into two broad groups. What are the two groups and
what are some examples of materials that belong to each?

A

The two groups of nonmetallic resources are:
Building materials – aggregate, crushed rock, gypsum, clay, and limestone.
Industrial minerals – fluorite, limestone, corundum, garnet, sylvite

25
Q

Why are coal, oil, and natural gas called “fossil fuels”?

A

Coal, oil, and natural gas are called fossil fuels because these are all created from organisms that
lived long ago. In the case of coal, it is lithified plant matter, for example.

26
Q

What is an oil trap? What do all oil traps have in common?

A

An oil trap is a geologic environment that allows for significant amounts of oil and gas to
accumulate.

27
Q

Describe the circumstances in which hydraulic fracturing is used.

A

Hydraulic fracturing is used where significant reserves of natural gas exist in low permeability
rocks. This process injects fluids at high pressures into the subsurface, breaking the shale rock, and
opening up cracks where the natural gas can flow into wells and be brought to the surface