Chapter 2 Flashcards

(37 cards)

1
Q

naturally occurring solids •formed by inorganic
processes
•building blocks of rocks •Examples: quartz, sulfides,
halides

A

Minerals

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2
Q

•relatively hard, naturally occurring mineral material
•made up of two of more
minerals, mixed up through
geological processes
• Examples: igneous, sedimentary,
and metamorphic rocks

A

Rocks

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3
Q

Physical Properties of Rock-Forming Minerals

A

Color
Hardness
Luster
Cleavage

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4
Q

it is a measure of the resistance of a mineral (not specifically surface) to abrasion

A

Hardness

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5
Q

measures the scratch resistance of various minerals based on the ability of a harder material/mineral to scratch a softer one

A

The Mohs Scale of Hardness

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6
Q

describes how the mineral reflects light

A

Luster

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7
Q

2 types of luster

A

Metallic luster
Non-metallic luster

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8
Q

looks like a shiny metal such as chrome, steel, silver, or gold.

A

Metallic luster

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9
Q

may be shiny and reflect light, however, they do not look like a metal.

A

Non-metallic luster

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10
Q

the property of some minerals to break along specific planes of weakness to form smooth, flat surfaces.

A

Cleavage

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11
Q

is the property of a mineral breaking in a more or less random pattern with no smooth planar surfaces.

A

Fracture

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12
Q

Cleavage in one direction

A

Muscovite

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13
Q

Cleavage in two directions

A

Feldspar

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14
Q

Cleavage in three directions

A

Halite

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15
Q

Cleavage in four directions

A

Calcite

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16
Q

Mineral Groups

A

Silicates
Oxides
Carbonates
Halides

17
Q

minerals containing the two most abundant elements in the Earth’s crust, namely, silicon and oxygen

18
Q

minerals composed of oxygen anion (O2-) combined with one or more metal ions

19
Q

minerals containing the carbonate (CO3)2- anion combined with other elements

20
Q

minerals containing halogen elements combined with one or more metal

21
Q

There are almost —— known mineral species, yet the vast majority of rocks are formed from combinations of a few common minerals, referred to as “——————”.

A

5000
Rock-forming minerals

22
Q

are naturally occurring and coherent aggregate of one or more minerals
basic unit of which the solid Earth

23
Q

3 major types of rocks

A

Igneous, sedimentary, metamorphic

24
Q

those that solidify from magma

25
magma cools quickly above ground (extrusive)
Volcanic igneous rock
26
magma cools and solidifies slowly underground (intrusive)
Plutonic igneous rock
27
those that are deposited and lithified (compacted and cemented together) at the Earth’s surface
Sedimentary
28
compacted broken rocks (sandstone)
Clastic
29
compacted dissolved minerals (limestone)
Chemical
30
compacted biogenic matter (coal)
Organic
31
is a process that squeezes, or compacts sediments.
Compaction
32
“glue” – takes place when dissolved minerals are deposited in the tiny spaces among sediments.
Cementation
33
formed by changes in preexisting rocks under the influence of high temperature, pressure, and chemically active solutions
Metamorphic rocks
34
2 types of metamorphic rocks
Foliated Non-foliated
35
have a layered or banded appearance
Foliated
36
do not have a layered or banded appearance
Non-foliated
37
is a web of processes that outlines how each of the three major rock types—igneous, metamorphic, and sedimentary—form and break down based on the different applications of heat and pressure over time.
Rock cycle