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Plate Tectonics
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Plate Tectonics The theory that pieces of Earth’s lithosphere are in constant motion, driven by convection currents in the mantle. CD + SFS + “plates” = Plate Tectonics!
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Breaks in earth’s crust where rocks move
Faults Breaks in earth’s crust where rocks move
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Faults meet at Boundaries
3 kinds of boundaries: Convergent Divergent Transform
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Where 2 plates move apart
Divergent Boundary Where 2 plates move apart Mid-ocean ridge (oceanic) Rift Valley (continental)
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Mid-Ocean Ridge (SFS)
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Rift Valley
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Convergent Boundary Where 2 plates collide Oceanic-Oceanic
Oceanic-Continental Continental-Continental Outcome determined by DENSITY
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Oceanic-Oceanic Convergent Boundary
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Oceanic-Continental Convergent Boundary
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Continental-Continental Convergent Boundary
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Transform Boundary 2 plates slide past each other in opposite directions
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