Topic 3 Rocks and Minerals Flashcards

1
Q

What is the crust mainly made up of?

A

75% of crust composed of oxygen and silicon, 8% Aluminum, and 5% iron

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2
Q

What are the four major types of material that form Earth’s surface?

A

Rock, sediment, organic matter, and water

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3
Q

What is rock?

A

a solid, cohesive aggregate of grains composed of one or more materials. Grains are essentially all inorganic

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4
Q

What is sediment?

A

Generally, unconsolidated inorganic materials originally derived from the fractionation of rocks.

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5
Q

What is organic matter?

A

Deposits composed of mainly dead or decaying matter from organisms (such as plants or animals). Includes upper horizons of soil, peat, shell beds, organic muds, Also includes coal and oil shales (sometimes classified as rocks)

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6
Q

How much of Earth’s surface is covered in water?

A

70% of earth’s surface is covered in water

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7
Q

What are minerals?

A

Any naturally occuring inorganic, solid substance possesing a definite chemical composition and characteristics atomic structure (usually crystaline)

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8
Q

what are common types of minerals?

A

Felsic and Mafic minerals

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9
Q

felsic Minerals

A

Light in colour or white mineral. e.g. Quartz, plagioclase, orthoclase

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10
Q

Mafic Minerals

A

Dark green or black in colour mineral. e.g. Basalt, olivine, hornblende, augite

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11
Q

What are the 3 types of rocks?

A

igneous, sedimentary, and metamorphic rock

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12
Q

What are the two types of igneous rock?

A

Intrusive and extrusive

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13
Q

Intrusive (plutonic) igneous rocks

A

Magma cools slowly below the surface, creates large crystals (Dikes, sills, and batholith/large pool)

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14
Q

Extrusive (volcanic) igneous rocks

A

Magma cools rapidly above the surface, creates small crystals

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15
Q

Magma rich in Fe and Mg

A

Have a high content of mafic minerals (dark coloured rock)

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16
Q

Magma deficient in Fe and Mg, yet rich in Si and Al

A

produce abundant felsic minerals (Light coloured rocks)

17
Q

How are igneous rocks classified?

A

Based on the relative abundances of felsic and mafic mineral species in the rocks

18
Q

Types of weathering

A

Chemical weathering and physical weathering

19
Q

Chemical weathering

A

Examples: oxidation: addition of oxygen to minerals (e.g. Rust), Hydrolysis: addition of water to minerals (e.g. Granite reacts with water creating clay)

20
Q

Physical weathering

A

Breaks off individual mineral grains (fragmentation), facilitates chemical weathering

21
Q

formation of sedimentary rock

A

Weathering of rocks create small mineral particles; particles are transported by air, water or gravity; sediment is deposited in various environments; strata becomes burried; strata hardens, compacts and cemented to form sedimentary rock

simplified: Erosion, Deposition, compaction, cementation

22
Q

Types of sedimentary rocks

A

Clastic, precipitate, fossils, organic

23
Q

Clastic sedimentary rock

A

Inorganic rock and mineral fragments

24
Q

Precipitate sedimentary rock

A

Chemical precipitation of inorganic compounds from solution or as hard parts of organisms (e.g. shells, calcium carbonate precipitated on sea or lake floors)

25
Q

fossil sedimentary rock

A

organisms preserved as fossils when their bodies are burried by layers of sedimentary rock

26
Q

organic sedimentary rock

A

fragments of tissues of organisms (e.g. peat moss) can harden into coal

27
Q

Metamorphic Rock formation

A

when other types of rock are altered by intense heat and/or pressure (plate tectonics); often producing a harder, changed form of rock; recrystallization of existing materials/ formation of new crystals (e.g. mica from clays); foliation (preferred orientation of minerals within a rock); mineral layering due to different melting temperatures/ directional pressure (tectonic stress); classified by degree of metamorphism (grade)

28
Q

The Rock Cycle

A

Extrusive igneous rocks break down into small fragments, nature may move it, fragments settle, layering into sediment, get burried and compressed, turning into sedimentary rock, which is transformed by extreme heat and pressure through metamorphism, turning to metamorphic rock, which is melted by the even hotter heat and pressure turning to intrusive or extrusive igneous as it’s lifted: extrusive then repeats the cycle, intrusive is covered under the surface until it is revealed and which will break apart and too will repeat the cycle.

29
Q
A