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plate |
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plateOne of several relatively distinct sections of the lithosphere, approximately 100 km/60 mi thick, which together comprise the outermost layer of the Earth (like the pieces of the cracked shell of a hard-boiled egg). The plates are made up of two types of crustal material: oceanic crust (sima) and continental crust (sial), both of which are underlain by a solid layer of mantle. Dense oceanic crust lies beneath Earth's oceans and consists largely of basalt. Continental crust, which underlies the continents and the continental shelves, is thicker, less dense, and consists of rocks that are rich in silica and aluminium. Due to convection in the Earth's mantle (see plate tectonics) these pieces of lithosphere are in motion, riding on a more plastic layer of the mantle, called the asthenosphere. Mountains, volcanoes, earthquakes, and other geological features and events all come about as a result of interaction between these plates. How to thank TFD for its existence? Tell a friend about us, add a link to this page, add the site to iGoogle, or visit webmaster's page for free fun content. |
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But the largest quakes in the history of the contiguous United States have actually hit the supposed stable heartland, far from the edges of the crustal plate that carries North America. Subduction occurs when two crustal plates collide and one dives below the other. These great fractures in the Earth mark an area where the northwest-moving Pacific crustal plate grinds past the North American plate. |
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