Earth's Interior and Plate Tectonics (wrocco)

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Created by:

wrocco  on December 8, 2009

Subjects:

Earth Science

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Earth's Interior and Plate Tectonics (wrocco)

Lithosphere
Made of the crust and the rigid mantle combined
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Lithosphere Made of the crust and the rigid mantle combined
Asthenosphere the plastic-like layer below the lithosphere
Oceanic crust Made of basalt, density 3.0g/cm3
Continental Crust Made of granite, density 2.7 g/cm3
Convergent boundary where two plates move together and form mountain ranges
Divergent boundary where two plates move away from each other
P-waves Primary waves - the fastest energy waves given off by an earthquake, can travel through solids, liquids, and gases
S-waves Secondary waves - the slower moving energy waves given off by an earthquake, can travel only through solids
Hot Spot an area where magma from deep within the mantle melts through the crust above it
Epicenter the point on Earth's surface directly above an earthquake's focus
Outer Core a liquid layer deep within Earth made primarily of iron and nickel
trench a deep canyon or ditch formed at a subduction zone
earthquake a sudden release of energy stored within earth's lithosphere
lag time the time difference between the arrival of the p-waves and s-waves
origin time the exact clock time that an earthquake occurred

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