Which feature is typically associated with a convergent boundary?

A convergent boundary is characterized by the movement of tectonic plates toward one another, often resulting in the formation of various geological features. One significant feature associated with this type of boundary is the formation of mountain ranges. When two continental plates collide, the intense pressure from the collision can cause the crust to buckle and fold, leading to the uplift of mountain ranges. Examples include the Himalayas, which were formed from the collision of the Indian Plate and the Eurasian Plate.

In contrast, mid-ocean ridges, right lateral faults, and seafloor spreading are linked to divergent boundaries or transform boundaries. Mid-ocean ridges are areas where tectonic plates are moving apart, allowing magma to rise and create new oceanic crust. Right lateral faults are related to strike-slip boundaries, where plates slide past each other horizontally. Seafloor spreading occurs at divergent boundaries where new oceanic crust is formed as plates separate. Thus, mountain ranges serve as a clear indicator of the processes associated with convergent boundaries.