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At constructive boundaries, magma from the earth's interior rises to the surface and forms mostly fissure volcanoes, but a few other tyopes as well, and forms new crust which pushes away older crust

At destructive boundaries, in a process called subduction, an oceanic plate slides into the earth's mantle, where it melts. The molten roick then rises to the surface and fornms a chain of volcanoes, mostly stratovolcanoes, but a few of other types as well

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At constructive plate margins, tectonic plates move apart, creating space for magma to rise from the mantle. As the magma reaches the surface, it erupts and forms volcanic activity. Over time, repeated eruptions build up layers of volcanic material, leading to the formation of a volcano.

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9mo ago
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16y ago
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Q: How do volcanoes form at constructive plate margins?
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