Large,thick-crusted,nonvolcanic mountain belts,like the Himalayas,are associated with

Question

Quizplus · Accepted Answer

Large, thick-crusted, non-volcanic mountain belts are primarily formed due to continent-continent collisions. This is because during such collisions, the two plates crumple and thicken their crust, resulting in the formation of high mountains like the Himalayas. Mid-ocean ridges are associated with the formation of new oceanic crust, while hot spots are more commonly associated with the formation of volcanic islands. Subduction zones, on the other hand, can also result in the formation of mountain ranges, but they typically have a different type of crust and volcanic activity compared to non-volcanic mountain belts.

Large,thick-Crusted,nonvolcanic Mountain Belts,like the Himalayas,are Associated with