*Earthquakes and Plate Tectonics Set 1 review

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Created by:

cscaduto  on January 22, 2012

Subjects:

Earth Science

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*Earthquakes and Plate Tectonics Set 1 review

Continental Crust
The portion of the earth's crust that primarily contains granite, is less dense than oceanic crust
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Continental Crust The portion of the earth's crust that primarily contains granite, is less dense than oceanic crust
Continental Drift Wegener's theory that the continents were joined as a single land mass called Pangaea, and drift slowly across earth's surface
Convection Current current in the earth's mantle set in motion by differences in density of the mantle
convergent plate boundary places where edges of adjacent plates are colliding
divergent boundary places where edges of adjacent plates are spreading apart
Mid-Atlantic ridge divergent boundary in the middle of the Atlantic Ocean
mid-ocean ridge a chain of undersea mountains running through the center of an ocean
oceanic crust The portion of earth's crust that primarily contains basalt, is relatively dense
Pangaea ancient land mass made up of all the continents that began to break apart about 200 million years ago
plate tectonics the theory that the earth's crust consists of large rigid plates resting on a fluid like layer of denser rock. These plates slide around causing the edges to collide, separate, and slide past each other
Alfred Wegener A German scientist who proposed the theory of continental drift

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