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Volcanoes are distributed as they are because most occur at the boundaries of the world's tectonic plates. Subducted crust rises as magma at constructive or destructive plate boundaries, and escapes through vents in the crust, often forming volcanoes on the surface. The only exceptions to volcanoes at plate boundaries are what are known as "hot-spot" volcanoes, that occur where a particular section of the Earth's crust is very thin and being heated by the mantle below. An example of this would be the Hawaiian Islands.

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