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Earths Dynamic 1

Crust & Interior

TermDefinition
Asthenosphere Also known as the upper mantle
Continental Crust Less Dense and thicker crust
Continental Drift Theory that the continents “Floats” around on the Moho
Convection Change in position due to density differences
Convergent Coming Together
Depositional Basins Large, low-lying areas where sediment is dropped off
Divergent Spreading apart
Down-Warping Bending down of rocks: Usually occurs at a convergent plate boundary
Earthquake Shaking of Earth due to release of frictional energy along a fault
Created by: sjjwhite
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