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Flashcards from lecture notes.
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Lithosphere vs. Asthenosphere
Mechanically stronger than the asthenosphere; not as rigid as the lithosphere.
Differentiation
Transformation early in Earth's history to create layers.
Marine Magnetic Anomalies
Variations of magnetism seen in the seafloor as Earth's polarity changes.
Examples of Minerals
Ice, galena, calcite, rock salt.
Well-Developed Crystal Faces
When mineral growth occurs without obstruction from physical constraints or impurities.
Magma
Below ground molten material.
Lava
Above ground molten material.
Pyroclastic Debris
Fragments of rock & other material erupted from a volcano
Flux Melting
Melting triggered by the subduction of an ocean plate.
Decompression Melting
Melting that occurs when hot rock rises from greater depths to shallower depths.
Physical Weathering
Mechanical breakdown of rock into smaller fragments.
Chemical Weathering
Chemical breakdown of a rock by chemical reactions.
Epicenter
The point directly above the focus of an earthquake.
Viscosity
Resistance to flow.
Elastically Deformed Material
It returns to its original shape before stress was applied.
Why Three Seismograph Stations are Needed
Where their radius intersects gives you the location.
Stress and Strain Relationship
Stress causes strain (strain = change in shape).
Source of Freshwater
Glaciers (and upstate New York).
Greatest Challenge on Earth
Climate Change!
Rock B Characteristics
Poorly sorted, angular sediment.
Rock B Deposition
Deposited closer to its origin.
Rock A Sediment
Sediment was transported a long distance from its origin.