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Theory of Plate Tectonics Plate Tectonics Plate Boundaries Causes of Plate Tectonics
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Plate Tectonics
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What is Plate Tectonics The Earth’s crust and upper mantle are broken into sections called plates. Plates move around on top of the mantle like rafts.
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What is the Lithosphere? The crust and part of the upper mantle = lithosphere –100 km thick –Less dense than the material below it so it “floats”
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What is the Asthenoshere? The plastic layer below the lithosphere = asthenosphere The plates of the lithosphere float on the asthenosphere.
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2 Types of Plates Oceanic plates - plates below the oceans. –Contain mostly basalt. Continental plates - plates below the continents. –Contain mostly rhyolite.
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Plate Boundaries
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Divergent Boundaries Boundary between two plates that are moving apart or rifting. RIFTING causes SEAFLOOR SPREADING.
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Features of Divergent Boundaries Mid-ocean ridges Rift valleys Fissure volcanoes
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Convergent Boundaries Boundaries between two plates that are colliding. There are 3 types…
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Type 1 Oceanic plate colliding with a less dense continental plate. Subduction Zone: where the more dense plate slides under the less dense plate. VOLCANOES occur at subduction zones. Ring of FireRing of Fire AnimationsAnimations
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Andes Mountains, South America
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Type 2 Oceanic plate colliding with another oceanic plate. The more dense plate slides under the less dense plate creating a subduction zone called a TRENCH.
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Aleutian Islands, Alaska
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Type 3 A continental plate colliding with another continental plate. Have Collision Zones: –a place where folded and thrust faulted mountains form.
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Transform Fault Boundaries Boundary between two plates that are sliding past each other. EARTHQUAKES occur along these faults.
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San Andreas Fault, CA
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Causes of Plate Tectonics
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Convection Currents Hot magma in the Earth moves toward the surface, cools, then sinks again. Creates convection currents beneath the plates that cause the plates to move.
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