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ocean-continent convergent forms volcanoes and trench |
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continent to continent convergent boundary forms mountains (not volcanoes) |
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divergent plate boundary forms new oceanic crust |
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transform plate boundary no crust created or destroyed |
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| oceanic plate moves under another plate at a convergent plate boundary. Crust is destroyed. |
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| developed the theory of continental drift |
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| new seafloor created at mid-ocean ridge. Provides mechanism for how plates move. |
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| Solid iron. Very hot but solid because of intense pressure. |
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| heat causes material to become less dense and rise. More dense material sinks |
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| liquid portion of upper mantle |
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| only liquid portion of center of the earth |
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| creates the "plates" in plate tectonics. Solid upper portion of mantle and crust |
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| Outer shell of the earth. Oceanic crust is more dense then continental crust. |
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| created by transform boundary |
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| created by continental-continental convergent boundary |
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| passive continental margin |
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| edge of a continent that is not a plate boundary (East Coast of US) |
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| active continental margin |
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Definition
| edge of continent is on a plate boundary (West Coast of US) |
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| all lands. Super continent named by Alfred Wegener |
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