At a continental convergent zone, two tectonic plates collide, often leading to the formation of mountain ranges, such as the Himalayas created by the collision of the Indian and Eurasian plates. This convergence can also result in intense seismic activity, including earthquakes, due to the stress and friction between the plates. Additionally, subduction can occur if one plate is forced beneath another, leading to volcanic activity and the creation of deep ocean trenches nearby.
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