Continental collision is a geological process that occurs when two continental plates collide with each other, leading to the convergence and eventual collision of the continental crust. This collision typically results in the deformation and uplift of the crust, leading to the formation of mountain ranges. Continental collision is a key process in the formation of major mountain ranges such as the Himalayas, the Alps, and the Rocky Mountains. It can also result in the formation of large-scale geological structures such as suture zones and accretionary wedges. The collision of continental plates can have significant geological and geophysical consequences, including the creation of earthquakes, the development of seismically active fault zones, and the generation of large-scale tectonic plates. Scientists study continental collision to better understand the processes and dynamics of plate tectonics, the formation of mountain ranges, and the geological evolution of the Earth's crust. Studying continental collisions can also help scientists better understand the distribution of natural resources, the formation of mineral deposits, and the potential hazards associated with tectonic activity.