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Published byMolly Russo Modified over 11 years ago
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Plate Tectonics What evidence do scientists have to support the fact that the Earth’s crust is continuously moving?
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Plate Tectonics The theory that describes how tectonic plates move and shape Earth’s surface Tectonic plates are huge pieces of crust that fit together at their edges to cover Earth’s surface.
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About 12 plates exist on Earth
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Earth’s Interior Crust – Rigid outer shell of Earth Mantle
Oceanic and Continental Crust Mantle Upper mantle is partially molten Lower mantle is rigid (solid)
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Earth’s Interior Core Outer core is molten iron, source of Earth’s magnetic field Inner core is solid, Iron and Nickel
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Plate Boundaries Divergent Boundary Convergent Boundary
Transform Boundary
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Divergent Boundary Two tectonic plates move apart from each other
Rift valleys – long narrow depressions Rift valley in East Africa
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Convergent Boundary Two tectonic plates move towards each other (come together) Oceanic Plates are more dense Continental Plates are less dense
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Subduction Process when one tectonic plate slips beneath another plate
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Oceanic – Oceanic Subduction Occurs Deep Sea Trenches (Marianas Trench)
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Oceanic – Continental Subduction Occurs Trench and Volcanic Arch (Peru – Chile Trench)
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Continental – Continental
Mountain Building Himalayas Aleutian Islands
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Transform Boundary Region where two plates slide past each other
Earthquakes occur at transform boundaries San Andreas Fault in San Francisco
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San Andreas Fault
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