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Unit 4 Plate Tectonics

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Term
Definition
Tectonic/Crustal plates   Large, moving pieces of Earth’s lithosphere that rest on the asthenosphere  
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Tectonic/Crustal plates   Commonly carries both oceanic and continental crust  
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Continental Drift   A hypothesis made by Alfred Wegener in 1912  
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Continental Drift   Continents were once joined together but moved apart over time  
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Pangaea   Supercontinent that included all of the landmasses on Earth; began breaking apart about 200 million years ago  
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Plate Tectonics   Theory that pieces of Earth’s lithosphere are in constant motion, driven by convection currents in the mantle  
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Divergent Boundary   Boundary along which two tectonic plates move away from each other  
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Divergent Boundary   The sea floor spreads apart and new crust is formed  
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Convergent Boundary   Boundary along which two tectonic plates move toward each other  
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Convergent Boundary   Characterized by subduction or continental collision  
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Convergent Boundary   Crust is usually destroyed  
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Transform Boundary   Boundary along which two tectonic plates scrape past each other  
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Transform Boundary   Characterized by earthquakes; crust isn’t created or destroyed  
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Hot spot   An area where a column of hot material rises from deep within the mantle. -Lithosphere above is heated, causing volcanic activity at the surface  
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Subduction   The process by which denser crust sinks beneath less dense crust  
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Rift valley   A deep valley formed as tectonic plates move away from each other at a divergent boundary  
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Mid-ocean ridge   An underwater mountain range where new ocean crust is formed by volcanic activity along a divergent boundary  
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Ocean basin   A great depression occupied by the ocean on the surface of the lithosphere  
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