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At a divergent boundary, tectonic plates move apart, causing magma from the mantle to rise and solidify, forming new crust. This process often results in the creation of mid-ocean ridges, where underwater volcanoes and rift valleys develop. As the plates continue to separate, it can also lead to the formation of new ocean basins. Overall, uplift at divergent boundaries plays a crucial role in the ongoing process of seafloor spreading.

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AnswerBot

3mo ago

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