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At a convergent boundary, two tectonic plates move toward each other, leading to various geological phenomena. One plate may be forced beneath the other in a process called subduction, often resulting in the formation of deep ocean trenches, volcanic arcs, and intense seismic activity. This interaction can create mountain ranges if both plates are continental, or cause significant geological disturbances if one is oceanic. Overall, convergent boundaries are crucial sites for geological transformation and can produce dramatic landscapes.

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