M2 Subtopic 1 Flashcards

(75 cards)

1
Q

Aggregates of one or more minerals

A

Rocks

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2
Q

Naturally occurring, inorganic solids with a definite chemical composition and crystalline structure

A

Minerals

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3
Q

Formed from the cooling and solidification of magma or lava

A

Igneous Rocks

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4
Q

Coarse-grained, intrusive, composed of quartz, feldspar, and mica. Used in construction and monuments

A

Granite

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5
Q

Fine-grained, extrusive, primarily composed of plagioclase and pyroxene. Used in road base and construction

A

Basalt

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6
Q

Volcanic glass formed from rapid cooling of lava. Used in cutting tools and ornamental objects

A

Obsidian

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7
Q

Composed mainly of plagioclase feldspar and amphibole. Used as dimension stone and in construction

A

Diorite

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8
Q

Formed from the slow cooling of magma beneath the Earth’s surface

A

Intrusive Igneous Rocks (Plutonic Rocks)

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9
Q

Formed from the rapid cooling of lava on or near the Earth’s surface.

A

Extrusive Igneous Rocks (Volcanic Rocks)

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10
Q

Two examples of Intrusive Igneous Rocs

A

Granite
Diorite

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11
Q

Two examples of extrusive igneous rocks

A

Basalt
Obsidian

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12
Q

Large, visible crystals. Indicates slow cooling.

A

Coarse-grained

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13
Q

Small, invisible crystals. Indicates rapid cooling

A

Fine-grained

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14
Q

No crystals, very smooth. Indicates very rapid cooling

A

Glassy

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15
Q

High in silica, and light-colored minerals

A

Felsic

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16
Q

Low in silica, dark-colored minerals

A

Mafic

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17
Q

Between felsic and mafic

A

Intermediate

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18
Q

Very low in silica, very high in magnesium and iron

A

Ultramafic

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19
Q

Igneous rocks can host valuable mineral deposits, such as precious metals (gold, silver), base metals (copper, lead), and gemstones

A

Mining

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20
Q

Areas with extensive igneous activity, such as volcanic regions, can be geothermal energy sources, providing a renewable energy resources

A

Geothermal Energy

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21
Q

Formed from the compaction and cementation of sediments, which are particles derived from the weathering and erosion of existing rocks

A

Sedimentary Rocks

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22
Q

Enumerate the Formation Process of Sedimentary Rocks

A

Weathering
Erosion and Transport
Deposition
Compaction and Cementation

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23
Q

Enumerate the Types of Sedimentary Rocks

A

Clastic, Chemical, Organic

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24
Q

Rocks Formed from mechanical weathering debris.

A

Clastic Sedimentary

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25
Composed of rounded gravel-sized particles
Conglomerate
26
Composed of sand-sized particles, often quartz
Sandstone
27
Composed of clay-sized particles, splits easily into thin layers
Shale
28
Formed from the precipitation of minerals from water
Chemical Sedimentary
29
Composed mainly of calcite, often from marine organisms
Limestone
30
Formed from the evaporation of saline water, known as rock salt
Halite
31
Formed from the evaporation of water containing dissolved sulfate and calcium
Gypsum
32
Formed from the accumulation of plant or animal debris
Organic Sedimentary
33
Formed from compressed plant material, primarily in swampy environments
Coal
34
Composed of microscopic marine organisms (foraminifera), a form of limestone
Chalk
35
Its grain size determines the classification
Clastic Texture
36
Due to mineral precipitation, forms crystalline.
Chemical Texture
37
Presence of organic material, such as plant fibers or shells.
Organic Texture
38
Determined by the Types of Minerals and rock fragments
Clastic composition
39
Determined by the minerals precipitated from the solution
Chemical Composition
40
Determined by the types of organic materials present
Organic Composition
41
Formed from the alteration of existing rocks (igneous, sedimentary, or other metamorphic rocks) due to heat, pressure, and chemically active fluids
Metamorphic Rocks
42
Formation Process of Metamorphic Rocks
Heat Pressure Chemically-Active Fluids
43
Increases the temperature of the rock, causing minerals to recrystallize without melting
Heat
44
Applies directed stress to the rock, leading to deformation and reorientation of minerals
Pressure
45
Facilitate the exchange of ions, promoting new mineral growth and altering the rock's composition
Chemically-Active Fluids
46
Occurs when rocks are heated by nearby magma or lava. Typically affects a small area surrounding the heat source. Results in non-foliated rocks due to uniform pressure from heat
Contact Metamorphism
47
Occurs over large areas due to tectonic forces that produce high pressure and temperature. Common in mountain-building regions. Results in foliated rocks due to directed pressure from tectonic forces.
Regional Metamorphism
48
Two types of Metamorphic Rocks
Foliated and Non-foliated
49
Formed under directed pressure, causing minerals to align in parallel layers or bands
Foliated Metamorphic Rocks
50
Formed under uniform pressure or from contact metamorphism, resulting in rocks without a layered texture
Non-Foliated Metamorphic Rocks
51
Examples of Foliated Metamorphic Rocks
Slate Schist Gneiss
52
Examples of Non-foliated Metamorphic Rocks
Marble Anthracite Quartzite
53
Fine-grained, formed from shale, splits easily into thin sheets. Used in roofing and flooring
Slate
54
Medium to coarse-grained, characterized by visible mineral grains aligned in parallel. Used as a decorative stone
Schist
55
Coarse-grained, banded appearance, formed from high-grade metamorphism. Used in construction and as a decorative stone
Gneiss
56
Formed from limestone, composed mainly of calcite. Used in sculpture and as a building material
Marble
57
Formed from sandstone, composed mainly of quartz. Used in construction and as a decorative stone
Quartzite
58
High-grade metamorphic form of coal, with a shiny appearance and high carbon content. Used as a high-quality fuel
Anthracite
59
A continuous process of rock formation, alteration, and recycling through geological processes.
The Rock Cycle
60
Recite the Rock Cycle.
Igneous to Sedimentary (Weathering/Erosion, Transportation/Deposition, Compaction/Cementation) Sedimentary to Metamorphic (Burial and Metamorphism) Metamorphic to Igneous (Melting, Cooling and Solidification)
61
Naturally occurring, inorganic solids with a definite chemical composition and an ordered atomic arrangement
Minerals
62
Enumerate the Characteristics of Minerals
Naturally-occuring Inorganic Solid Definite Chemical Composition Crystalline Structure
63
Enumerate the Physical Properties of Minerals
Color, Streak, Luster, Hardness, Cleavage, Fracture, Specific Gravity, Crystal Form
64
The visible hue of the mineral, though not always a reliable identification property due to variations
Color
65
The color of the mineral in powdered form, observed by rubbing the mineral on a streak plate
Streak
66
The way a mineral reflects light (e.g., metallic, vitreous, pearly).
Luster
67
Resistance to scratching, measured by the Mohs scale (1-10).
Hardness
68
The tendency of a mineral to break along flat planes of weakness
Cleavage
69
The pattern in which a mineral breaks (e.g., conchoidal, fibrous, uneven).
Fracture
70
The density of the mineral relative to the density of water.
Specific Gravity
71
The external shape of the mineral, reflecting its internal atomic structure
Crystal Form
72
Special Properties Exhibited by Minerals
Odor, Taste, Attraction to Magnets, Fluorescence, Radioactivity, Reactivity
73
The largest group of minerals contains silicon and oxygen
Silicates
74
Include carbonates (e.g., calcite), oxides (e.g., hematite), sulfates (e.g., gypsum), halides (e.g., halite), and native elements (e.g., gold).
Non-Silicates
75
Formation of Minerals
Crystallization from Magma Precipitation Changes in Pressure and Temperature Biological Processes