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When two tectonic plates with different densities converge, the denser plate typically subducts beneath the less dense plate. This subduction process can lead to the formation of trenches, volcanic arcs, and mountain ranges, depending on the nature of the plates involved (oceanic vs. continental). The subducting plate melts in the mantle, which can cause volcanic activity and earthquakes in the region. This interaction is a significant driver of geological processes and features on Earth.

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1mo ago

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