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The mid-ocean ridges are divergent plate boundaries-areas where earth's lithospheric plates are moving away from each other. This movement causes the crust to "thin out". The thinning allows the magma to come to the surface in the form of volcanoes.

Mid-ocean ridge volcanism is just one part of the larger, all-encompassing, and evolving theory of plate tectonics. The production of lava and new crust at the mid-ocean ridges is largely a reaction to gravity induced subduction of oceanic crust at convergent plate boundaries.

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King Boyer

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3y ago

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