Volcanic activity primarily occurs at convergent and divergent plate boundaries.
Volcanic activity is most often associated with convergent plate boundaries and divergent plate boundaries. Convergent boundaries experience volcanic activity due to subduction, where oceanic plates dive under continental plates, leading to magma formation and volcanic eruptions. Divergent boundaries, such as mid-ocean ridges, also exhibit volcanic activity as plates move away from each other, allowing molten lava to erupt through fissures.
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