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Published bySusan Price Modified over 9 years ago
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Theory of Plate Tectonics Theory that pieces of lithosphere move around on top of the asthenosphere
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Plate Boundaries The edges of different pieces of The lithosphere meet at lines called plate boundaries
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Plate Boundaries Plate Videos
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So the plates move. Now What? As the plates move, they produce changes in Earth’s surface, including volcanoes, earthquakes, mountain ranges, and deep- ocean trenches.
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3 Types of Plate Boundaries Divergent Convergent Transform Divergent Transform
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3 Types of Boundaries Divergent boundary= two plates move apart Magma rises and creates new crust or seafloor Causes: mid- ocean ridges, rift valleys, new crust, volcanoes
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Divergent Boundaries © All Rights Reserved. Diverging Africa
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Diverging Iceland
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3 Types of Boundaries Convergent= when two tectonic plates push into one another.
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Convergent Boundaries Continental vs. Continental Continental vs. Oceanic Oceanic vs. Oceanic
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Continental vs. Continental When two continental crustal plates collide, the continents buckle upward and form mountains. Himalayas- Asia
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Oceanic vs. Continental The oceanic plate slides under the continental plate. The continental crust crumbles and forms new mountains.
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Oceanic vs. Continental Ex: Andes mtn in S. America Cascade Mtns. in N. America- Mt. St. HelensMt. St. Helens
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Oceanic vs. Oceanic Two oceanic plates collide, one of the oceanic plates slides under the other. oceanic plates slides also called a subduction zone subduction zone
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Hawaiian Islands Oceanic vs. Oceanic
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Transform boundary When two tectonic plates slide past each other horizontally Produces? Earthquakes
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San Andreas Fault
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New Madrid Fault
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How do the plates move? CONVECTION CURRENTS Hot material rises while cooler material near the surface sinks Convection example
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How do the plates move? CONVECTION CURRENTS Hot material from deep within the Earth rises while cooler material near the surface sinks
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Convection currents
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How do we know? Sea-floor spreading =new ocean floor is created as two lithospheric plates pull away from one another.
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Seafloor spreading
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The Plates Move… So what now? Which way? 50 million years
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