where does mountain formation generally occur? divergent boundaries transform and convergent boundaries divergent and convergent boundaries transform boundaries

Mountain formation generally occurs at convergent boundaries, where tectonic plates move toward each other. At these boundaries, one of the colliding plates is often forced beneath the other in a process called subduction. This results in intense geological activity, including the formation of mountain ranges.

At divergent boundaries, tectonic plates move away from each other, and new oceanic crust is formed through volcanic activity, but this typically doesn't result in the formation of large mountain ranges.

Transform boundaries involve the sliding past of tectonic plates horizontally. While they can cause earthquakes and influence the landscape, they are not typically associated with the formation of extensive mountain ranges.

In summary, mountain formation is primarily associated with convergent boundaries where tectonic plates collide and one plate is forced beneath the other, leading to the uplift and creation of mountain ranges.