At ocean-continent convergent boundaries, oceanic crust subducts beneath continental crust, causing significant geological events like earthquakes and volcanic activity.
Convergent Boundaries: At an ocean-continent convergent boundary, oceanic crust subducts beneath continental crust, resulting in features like deep trenches, earthquakes, and volcanic activity forming a line of volcanoes. If two oceanic plates converge, a similar subduction process occurs, leading to the formation of islands along the boundary.
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