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PLATE TECTONICS Prentice Hall
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Earth’s Interior Crust Ocean & Continent Mantle Lithosphere Asthenosphere Mesosphere Core Outer Inner
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Lithosphere Composed of: Uppermost mantle Crust Broken into rigid plates Plate motion Collide Move apart Slide past one another one another
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LITHOSPHERIC PLATES
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PLATE BOUNDARIES Diverging (move apart)– two plates spread apart; magma rises between plates; volcanoes form Converging (collide) Ocean/Continent - subduction of ocean plate beneath continent; volcanoes form Ocean/Ocean – subduction of one ocean plate beneath another; volcanoes form Continent/Continent – collision causes mountains to rise up; earthquakes occur Transform (slide past) – two plates slide past each other; transform faults
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DIVERGING BOUNDARY
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Divergent – Seafloor Spreading
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CONVERGING – SUBDUCTION Continent / Ocean
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CONVERGING – SUBDUCTION Ocean / Ocean
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CONVERGING CONTINENTAL COLLISION Continent / Continent
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Transform Boundary - slide
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TRANSFORM BOUNDARY
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Transform Fault Boundary
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EVIDENCE: Hot Spot Plume of magma rises from deep in mantle Hawaii sits on top of a Hot Spot
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Hot Spot Magma ‘burns’ a hole in the plate as it moves over the hot spot Hawaiian Islands get progressively older to the north
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Plate Motion Convection Currents
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Convection in the Mantle Hot currents rise & cold currents sink
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