Rxk Flashcards

1
Q

Olivine, pyroxene, amphibole, and biotite mica are the common of Earth’s crust.

A

dark silicate minerals

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2
Q

rich in iron and/or magnesium and are comparatively low in silica (SiO2).

A

Dark silicate

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3
Q

contain greater amounts of potassium, sodium, and calcium and are richer in silica

A

Light silicates

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4
Q

quartz, muscovite mica, and the most abundant mineral group, the feldspars

A

Light silicates

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5
Q

amphibole, pyroxene, and biotite mica, with the other dominant mineral being plagioclase feldspar

A

Andesitic

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6
Q

dense ferromagnesian minerals

A

Ultramafic

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7
Q

Although ultramafic rocks are rare at Earth’s surface, the rock * , which is composed mostly of the minerals olivine and pyroxene, is the main constituent of the upper mantle.

A

peridotite

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8
Q

coarse-grained igneous rock that forms where large masses of granitic magma slowly solidify at depth.

A

Granite

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9
Q

extrusive equivalent of granite

A

Rhyolite

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10
Q
  • is a common type of volcanic glass.
A

Obsidian

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11
Q

the intrusive equivalent of andesite,

A

Diorite

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12
Q

most common extrusive igneous rock is *, a very dark green to black, finegrained volcanic rock composed primarily of pyroxene, olivine, and plagioclase feldspar.

A

basalt

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13
Q

The coarse-grained, intrusive equivalent of basalt is *).

is not commonly exposed at the surface, but it makes up a significant percentage of the oceanic crust.

A

gabbro

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14
Q

Examples of igneous rocks

A
Basalt, gabbro
Rhyolite, granite, obsidian
Andesite, diorite
Ulramafic, peridotite
Pumice, scoria
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15
Q

the most common sedimentary rock, is made of very fine-grained sediment and composed mainly of clay minerals

A

Shale (mudstone)

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16
Q

an abundant sedimentary rock, is composed chiefly of the mineral calcite (CaCO3)

A

Limestone

17
Q

Nearly 90 percent of * is formed from biochemical sediments secreted by marine organisms, and the remaining amount consists of chemical sediments that precipitated directly from seawater.

A

Limestone

18
Q

Type of limestone that is a soft, porous rock made up almost entirely of the hard parts of microscopic organisms that are no larger than the head of a pin.

A

Chalk

19
Q

In contrast to sedimentary rocks that are calcite or silica rich, * consists mostly of organic matter. Because * is produced by biochemical activity and contains organic matter, it is often classified as a biochemical, or organic, rock.

A

coal

20
Q

These layers, called *, are the single most characteristic feature of sedimentary rocks

A

strata, or beds

21
Q
  • are produced from preexisting igneous, sedimentary, or even other metamorphic rocks (Figure 2.29). Thus, every * rock has a parent rock—the rock from which it was formed.
A

Metamorphic rocks

22
Q

under low-grade metamorphism, the common sedimentary rock shale becomes the more compact metamorphic rock *

A

slate

23
Q

Pr: shale, mudstone or siltstone

A

Slate, Phylitte, Schist

24
Q

Pr: shale, granite or volcanic rocks

A

Gneiss

25
Q

Limestone or dolostone

A

Marble

26
Q

Quartz or sandstone

A

Quartzite

27
Q
  • is a mineral’s ability to reflect light. The terms transparent, translucent, and opaque describe the degree to which a mineral can transmit light.
A

Luster