What landscape feature is typically associated with the compression process in geology?

Thrust faults are geological features that result from the compression of Earth's crust. During this process, two tectonic plates move toward each other, causing one plate to be pushed up and over the other due to immense pressure. This upward movement of rock layers is typically seen in regions experiencing significant tectonic stress, such as convergent plate boundaries.

Thrust faults often lead to the formation of mountain ranges and are characterized by steeply inclined fault planes. They are crucial to understanding orogenic (mountain-building) processes and play a significant role in shaping various geological formations. Because of their association with compressive forces, thrust faults are pivotal indicators of tectonic activity and landscape evolution in regions under stress.