Volcanic activity is more likely to occur along divergent and convergent plate boundaries than either other type of plate boundary. At a boundary that diverges, two plate boundaries exist.
Tectonic plates are constantly drifting apart. Since magma continuously rises from the mantle into this boundary and creates new plate material on both sides, they never truly separate. The Mid-Atlantic Ridge is the location of a divergent plate boundary in the volcanic of the Atlantic Ocean.
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