Convergent plate boundaries occur when two tectonic plates collide and move toward each other. When plates of the same density collide, they tend to push against each other and form a subduction zone where one plate slides under the other. This can result in the formation of mountain ranges, volcanic activity, and earthquakes.
On the other hand, when plates of different densities collide, the denser plate will sink below the less-dense plate in a process called subduction. This can lead to the formation of ocean trenches and volcanic island arcs. The subducting plate can also melt and generate magma that rises to the surface, creating volcanic eruptions.
Overall, the main difference between convergent plate boundaries with plates of the same density and those with plates of different densities is the type of features that are formed. While both can lead to volcanic activity and earthquakes, convergent plate boundaries with plates of different densities tend to be associated with more intense volcanic activity and oceanic trenches.
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