Geoscience

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38 Terms

1
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Extrusive vs. intrusive?

  • Extrusive: Forms from lava at the surface; cools fast; small/no crystals.

  • Intrusive: Forms from magma underground; cools slowly; large crystals.

2
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Coarse vs. fine-grained?

  • Coarse: Large crystals (slow cooling).

  • Fine: Small crystals (fast cooling).

3
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Mafic vs. felsic?

  • Mafic: Low silica, dark color, high density.

  • Felsic: High silica, light color, low density.

4
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Q: What controls the texture of an igneous rock?

Cooling rate.

5
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Vesicular texture?

Full of gas bubble holes.

6
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Glassy texture?

Very rapid cooling; no crystals.

7
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Fine-grained texture?

Rapid cooling; tiny crystals.

8
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Porphyritic texture?

large and small crystals

9
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How does cooling rate affect crystal size?

Slow cooling → large crystals; fast cooling → small crystals.

10
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How does porphyritic texture form?

Two-stage cooling: slow underground, then fast at the surface.

11
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Effect of silica content on magma?

High silica = thicker, lighter color, less dense.

12
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What is an ultramafic rock & where is it found?

Very low silica, very dark, very dense; found in Earth’s mantle.

13
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Where are most sedimentary rocks found?

At or near Earth’s surface.

14
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What are the 3 main sedimentary groups?

  • Clastic: From broken rock fragments.

  • Organic/Biochemical: From once-living material (shells, plant remains).

  • Chemical: From minerals precipitating out of solution.

15
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Q: Why are sedimentary rocks layered?

A: They form from repeated deposition of sediments.

16
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Q: Why/how are sediments sorted?

A: By size; water/wind sort them based on energy levels.

17
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Q: Why are quartz and feldspar common in sand & sed rocks?

A: They are very resistant to weathering.

18
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Q: Two ways sediments become sedimentary rock?

A: Compaction and cementation.

19
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Q: How are sediments usually transported?

A: Mostly by running water.

20
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Q: Why are some sediments angular vs. rounded?

A: Longer travel = more rounding.

21
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Q: Weathering vs. erosion vs. deposition?

  • Weathering: Breaking down rocks.

  • Erosion: Moving sediments.

  • Deposition: Dropping sediments to rest.

22
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: What 3 processes create metamorphic rocks?

A: Heat, pressure, and chemical fluids.

23
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Q: Regional vs. contact vs. hydrothermal metamorphism?

  • Regional: Mountain-building; large areas; high pressure.

  • Contact: Magma heats nearby rock.

  • Hydrothermal: Hot fluids alter rock.

24
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: Foliated vs. nonfoliated?

  • Foliated: Minerals aligned in layers/bands.

  • Nonfoliated: No visible banding; uniform texture.

25
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3 changes metamorphism causes?

New minerals, new texture (foliation), increased density.

26
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Q: What is the rock cycle?

A: The processes that transform rocks between igneous, sedimentary, and metamorphic through melting, cooling, weathering, erosion, deposition, heat/pressure, and uplift.

27
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Q: Perpetual vs. renewable vs. non-renewable?

  • Perpetual: Never runs out (sun, wind).

  • Renewable: Replenishes but can run out short-term (trees, water).

  • Non-renewable: Takes millions of years to form (oil, coal, gas).

28
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Q: What is energy & past vs. present sources?

Energy = ability to do work.
Historically: wood, coal.
Today: oil, natural gas, renewables.

29
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How is oil created?

A: Burial of marine organisms, heat + pressure over millions of years.

30
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Q: Why is oil non-renewable?

A: Takes millions of years to form; we use it much faster than it forms.

31
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Q: Oil–food–population connection?

A: Oil powers farming, transport, fertilizers → supports large populations.

32
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Q: Issues with the U.S. importing ~50% of oil?

A: Economic risk, political dependence, rising costs.

33
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Q: What is “Peak Oil”?

A: The point when oil production reaches its maximum, then declines.

34
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Q: Examples of energy alternatives?

A: Solar, wind, hydro, nuclear, geothermal, biofuels.

35
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Q: Pros & cons of alternatives?

  • Pros: Clean, renewable, reduces emissions.

  • Cons: Expensive, location-dependent, storage issues.

36
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: What is fracking & why does it matter?

A: Injecting fluid to crack rock and release oil/gas; increases production but can cause environmental issues.

37
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3 ways to transition from cheap to expensive oil?

A: Efficiency, alternative energy, new technology.

38
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Q: Conventional vs. unconventional oil?

  • Conventional: Flows easily; cheap.

  • Unconventional: Harder to extract (shale, tar sands).