Overview
The geological evolution of mountain belts is a complex process influenced by tectonic activity, erosion, and sedimentation. Mountain ranges are primarily formed through the collision of tectonic plates, which creates immense pressure and leads to the uplift of land. Over time, these mountains are s...
Key Terms
Example: The Pacific Plate is one of the largest tectonic plates.
Example: The Mariana Trench is a subduction zone.
Example: Rivers can cause erosion by carrying away soil.
Example: Chemical weathering can change granite into clay.
Example: Sedimentation occurs in river deltas.
Example: The Andes is a major mountain range in South America.