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PLATE BOUNDARIES Seafloor Spreading and Continental Drift Combined B40c
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CONTINENTAL DRIFT to PLATE TECTONICS
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PLATE TECTONICS PLATE = piece of the lithosphere (crust and upper mantle) TECTONICS = movement plates are moving on the asthenosphere (fluid, lower mantle)
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CONVECTION CURRENTS movement of asthenosphere due to temperature/density differences heating, rising, cooling, sinking asthenosphere drags lithosphere with it as it moves (B3, Figure 11)
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LOCATIONS OF PLATE BOUNDARIES (B3, Figure 12)
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DIVERGENT PLATE BOUNDARY plates moving away from each other asthenosphere rises below boundary, turns and pulls plates apart mid-Atlantic ridge earthquakes volcanoes (B5, Figure 14)
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CONVERGENT PLATE BOUNDARY plates moving towards each other asthenosphere sinks below boundary, pulls plate with it earthquakes Volcanoes (at some) 3 types (B5, Figure 15)
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TRANSFORM PLATE BOUNDARY two plates slide horizontally past each other San Andreas Fault earthquakes (B5, Figure 13)
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ASSIGNMENT Draw each of the three types of plate boundaries. Label the direction of plate movement for each. For divergent and convergent, draw the convection current below the boundary.
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