How do mountains typically form at convergent boundaries?

Mountains typically form at convergent boundaries through the collision and compression of tectonic plates, which leads to the uplift of the Earth's crust. When two tectonic plates push against each other, the intense pressure from the collision causes the crust to deform. This can result in the creation of mountain ranges as the land is folded, faulted, and uplifted. The Himalayas, for instance, were formed by the collision of the Indian Plate with the Eurasian Plate, demonstrating how such geological processes can create towering mountain ranges.

In addition to this uplift process, the compressional force involved can also create various geological features such as deep trenches and earthquake activity in surrounding areas, highlighting the dynamic nature of tectonic interactions at convergent boundaries.