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At a divergent plate boundary, oceanic ridges, such as the Mid-Atlantic Ridge, typically form. This occurs when tectonic plates move apart, allowing magma from the mantle to rise and create new crust as it solidifies. The process results in the formation of underwater mountain ranges characterized by volcanic activity and rift valleys. These features are primarily associated with oceanic rather than continental mountain formations.

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the divergent bounday forms new crust


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