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1 Layer: Lithosphere
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2 Layer: Mantal
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3 Layer: Asthenosphere
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4 Layer: Core
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Alfred Wegener: A German scientist who proposed the theroy of continental drift
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Asthenosphere: Less ridiged than the lithosphere the rock is soild
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Cause of Plate Movement: when plates move because of convection currents and the mantle
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Continental Crust: the older, thicker, and less dense part of Earth's crust; the bulk of Earth's land masses made of granite
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Convergent Boundary: A tectonic plate boundary where two plates collide, come together, or crash into each other.
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fault: break in the rock
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fold: fold squeezed into a bend in the rock
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geologist: scientist that studies earth crust
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Inner Core: Solid metal
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Oceanic Crust: The portion of earth's crust that primarily contains basalt, is relatively dense
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Outer: Malten metal iron, nickel
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Plastic: Hard but can still bend and move.
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Plate Tectonics: the theory that proposes that earth's outer shell consists of individual plates that interact in various ways and thereby produce earthquakes, volcanoes, mountains, and the crust itself
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Subduction Zone: the region where an oceanic plate sinks down into the asthenosphere at a convergent boundary, usually between continental and oceanic plates