A geological feature formed by the convergence of tectonic plates is a mountain range. When two tectonic plates collide, the immense pressure and forces involved can cause the earth's crust to fold and uplift, resulting in the creation of mountain ranges over millions of years. This process is known as orogeny. The Himalayas, for instance, were formed by the collision of the Indian Plate with the Eurasian Plate. Such convergences can also lead to increased seismic activity, including earthquakes, as the plates interact. Studying these geological formations provides insights into the Earth's dynamic processes and the history of its surface.