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Most volcanoes form near subduction faults. When one plate slide under the edge of another plate, the edge of it melts under the rocky crust. Eventually, the pool of molten rock and gases that result get enough pressure that they force a pathway to the surface open, releasing the gas and magma as a volcano. However, some volcanoes form from hot spots, which are not well understood and can be located extremely far from the edge of a plate.

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