Earth Science Lecture Notes

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22 Terms

1
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Lithosphere vs. Asthenosphere

Mechanically stronger than the asthenosphere; not as rigid as the lithosphere.

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Differentiation

Transformation early in Earth's history to create layers.

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Marine Magnetic Anomalies

Variations of magnetism seen in the seafloor as Earth's polarity changes.

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Examples of Minerals

Ice, galena, calcite, rock salt.

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Well-Developed Crystal Faces

When mineral growth occurs without obstruction from physical constraints or impurities.

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Magma

Below ground molten material.

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Lava

Above ground molten material.

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Pyroclastic Debris

Fragments of rock & other material erupted from a volcano

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Flux Melting

Melting triggered by the subduction of an ocean plate.

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Decompression Melting

Melting that occurs when hot rock rises from greater depths to shallower depths.

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Physical Weathering

Mechanical breakdown of rock into smaller fragments.

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Chemical Weathering

Chemical breakdown of a rock by chemical reactions.

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Epicenter

The point directly above the focus of an earthquake.

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Viscosity

Resistance to flow.

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Elastically Deformed Material

It returns to its original shape before stress was applied.

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Why Three Seismograph Stations are Needed

Where their radius intersects gives you the location.

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Stress and Strain Relationship

Stress causes strain (strain = change in shape).

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Source of Freshwater

Glaciers (and upstate New York).

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Greatest Challenge on Earth

Climate Change!

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Rock B Characteristics

Poorly sorted, angular sediment.

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Rock B Deposition

Deposited closer to its origin.

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Rock A Sediment

Sediment was transported a long distance from its origin.