s1 Flashcards

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

Large, visible crystals. Indicates slow cooling (intrusive).

A

Coarse-Grained Igneous Rock

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4
Q

Small, invisible crystals. Indicates rapid cooling (extrusive)

A

Fine-grained Igneous Rock

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5
Q

No crystals, very smooth. Indicates very rapid cooling (extrusive)

A

Glassy Igneous Rock

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6
Q

High in silica, and light-colored minerals (e.g., granite, rhyolite).

A

Felsic

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7
Q

Very low in silica, very high in magnesium and iron (e.g., peridotite).

A

Ultramafic

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8
Q

Over time, sediments are compacted and cemented together to form solid rock.

A

Compaction and Cementation

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9
Q

Formed from the precipitation of minerals from water

A

Chemical Sedimentary Rocks

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10
Q

Applies directed stress to the rock, leading to deformation and reorientation of minerals

A

Formation Process of Metamorphic Rocks - Pressure

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11
Q

Facilitate the exchange of ions, promoting new mineral growth and altering the rock’s composition.

A

Formation Process of Metamorphic Rocks - Chemically Active Fluids

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12
Q

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.

A

Contact Metamorphism

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13
Q

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.

A

Regional Metamorphism

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14
Q

A continuous process of rock formation, alteration, and recycling through geological processes.

A

The Rock Cycle

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15
Q
  1. Weathering and Erosion: Igneous rocks are broken down into sediments.
  2. Transportation and Deposition: Sediments are transported and deposited in layers.
  3. Compaction and Cementation: Sediments are compacted and cemented to form sedimentary rocks.
A

From Igneous to Sedimentary

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16
Q

1 = diamond

A

MOHS SCALE OF HARDNESS

17
Q

Metamorphic processes alter existing minerals into new minerals under different conditions.

A

Formation of Minerals: Changes in Pressure and Temperature

18
Q

Low in silica, dark-colored minerals (e.g., basalt, gabbro).

A

Mafic

19
Q

between felsic and mafic (e.g., andesite, diorite).

A

Intermediate

20
Q

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

A

Geothermal Energy

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

22
Q

Breakdown of rocks into smaller particles by physical, chemical, and biological processes.

A

Weathering

23
Q

Movement of sediments by water, wind, ice, or gravity.

A

Erosion and Transport

24
Q

Accumulation of sediments in various environments (e.g., rivers, lakes, oceans).

A

Deposition

25
Q

Rocks Formed from mechanical weathering debris.

A

Clastic Sedimentary

26
Q

Formed from the accumulation of plant or animal debris.

A

Organic Sedimentary Rocks

27
Q

Grain size (gravel, sand, silt, clay) determines the classification.

A

Clastic Sedimentary Rocks

28
Q

Presence of organic material, such as plant fibers or shells

A

Organic Sedimentary Rocks

29
Q

Formed from the alteration of existing rocks (igneous, sedimentary, or other metamorphic rocks) due to heat, pressure, and chemically active fluids.

A

Metamorphic Rocks

30
Q

Increases the temperature of the rock, causing minerals to recrystallize without melting.

A

Formation Process of Metamorphic Rocks - HEAT

31
Q

Formed under directed pressure, causing minerals to align in parallel layers or bands.

TEXTURE:
Exhibits a banded or layered appearance due to the alignment of minerals under directed pressure.

A

Foliated Metamorphic Rocks

32
Q

Formed under uniform pressure or from contact metamorphism, resulting in rocks without a layered texture.

TEXTURE:
Lacks a banded or layered texture, typically formed under uniform pressure.

A

Non-Foliated Metamorphic Rocks

33
Q

Naturally Occurring: Formed by natural geological processes.

Inorganic: Not made by biological organisms

Solid: Have a definite shape and volume.

Definite Chemical Composition: Each mineral has a specific chemical formula.

Crystalline Structure: Atoms are arranged in a systematic and repeating pattern\

A

Characteristics of Minerals

34
Q

Color - The visible hue of the mineral, though not always a reliable identification property due to variations.

A

Physical Properties of Minerals

35
Q

Contains silicon and oxygen, making up the majority of Earth’s crust (e.g., quartz, mica, feldspar).

A

Silicate Minerals

36
Q

Include carbonates (e.g., calcite), oxides (e.g., hematite), sulfates (e.g., gypsum), halides (e.g., halite), and native elements (e.g., gold).

A

non silicate