What is a characteristic feature of continental-continental convergence?

Continental-continental convergence is characterized by the collision of two continental tectonic plates. When these plates collide, they do not subduct like oceanic plates would; instead, the crust is pushed upward, resulting in the formation of high mountain ranges. This process can create extensive mountain systems and is exemplified by the Himalayas, formed by the ongoing collision of the Indian and Eurasian plates. These mountain ranges can be significantly tall and are typically characterized by steep slopes and rugged terrain.

Ocean trenches, volcanic activity, and seafloor spreading are features associated with other types of tectonic interactions, such as oceanic-oceanic and oceanic-continental convergence. Therefore, the formation of high mountain ranges is distinctively associated with the convergence of continental plates.