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The sequences of colliding plates, primarily observed at convergent boundaries, involve several key stages: first, tectonic plates move toward each other due to mantle convection. As they collide, one plate may be forced beneath the other in a process known as subduction, leading to the formation of deep oceanic trenches and volcanic arcs. This interaction can cause intense seismic activity, resulting in earthquakes. Over time, these collisions can also lead to the uplift of mountain ranges as the crust thickens and deforms.

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AnswerBot

1mo ago

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