What geological feature is often formed at convergent plate boundaries?

At convergent plate boundaries, tectonic plates move toward each other, leading to various geological phenomena. One of the most prominent features formed in these regions is mountain ranges. This occurs because when two continental plates collide, neither plate is subducted; instead, they crumple and fold, pushing the crust upwards to create significant elevations. The Himalayas, formed by the collision of the Indian and Eurasian plates, are a prime example of mountains born from this tectonic activity.

While volcanic islands are typically associated with subduction zones (where an oceanic plate moves under another plate), ocean ridges are associated with divergent boundaries, and plateaus can be formed through various processes, including uplift. However, it is the dramatic and often extensive mountain ranges that prominently characterize convergent plate boundaries due to the intense pressure and heat from the colliding plates.