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Earthquakes are caused by friction between tectonic plates. The Earth's crust is made up of tectonic plates that basically float around on the magma in the Earths mantle. When these plates collide or move against each other, it causes great amounts of friction and tension in the crust. When enough tension builds up and is released at once, the result is an earthquake. Earthquakes happen near Coastlines because that is commonly where the tectonic plate collisions occur.

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