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Published byAnis Lynch Modified over 8 years ago
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Crustal Features 8.9B relate plate tectonics to the formation of crustal features
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What is Earth’s crust? Earth’s crust covers the mantle. The crust is the outermost layer surface layer. – 25 miles thick under continents – 6.5 miles thick under oceans
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What makes up the crust? Oceanic crust – Rocks that make up the oceanic crust are relatively young compared to the rocks that make up the continental crust. It is mostly basalt rock. Continental crust – Continental crust is older than oceanic crust. It has two layers, mostly igneous rock. The upper crust is mostly granite. The lower crust is mostly basalt and diorite.
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Moving crust The crust is part of the lithosphere, the outermost layer of the crust. Plates are part of the crust. (continental crust/plate and oceanic crust/plate) The convection currents in the mantle layer below and perhaps also gravity cause the plates to move.
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What happens when plates move? When the plates move, the surface of the crusts change. Earthquakes, volcanoes, ocean ridges, and mountains are all crustal features that form when plates move.
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How do plates move?
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When two boundaries converge (come together), volcanoes and mountain building is common.
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When two boundaries diverge (move away) from one another, this is common in oceans to form rifts.
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When two boundaries transform (slide past) one another, earthquakes are common.
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Crustal plate boundaries is where you would expect to find the most activity.
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Look at where most earthquakes occur, along plate boundaries.
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Look at where most volcanoes are found, also along boundaries.
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