What is a mountain belt?

A mountain belt is a larger unit of mountain ranges and mountain systems, typically characterized by a linear arrangement. It forms due to tectonic plate interactions, including convergent plate boundaries, where plates collide or subduct, leading to intense folding, faulting, and uplift. Mountain belts often span vast geographical areas and consist of multiple mountain ranges.

A mountain belt refers to a region or zone on Earth's surface characterized by a series of closely spaced mountain ranges or mountain systems. These mountain ranges typically run parallel to each other and are often formed by tectonic processes such as the collision of tectonic plates or the uplift caused by geological forces. Mountain belts can span vast distances and are often associated with significant geological activity, including earthquakes, volcanic eruptions, and the formation of various rock types through processes like folding, faulting, and erosion. Examples of prominent mountain belts include the Himalayas in Asia, the Andes in South America, and the Rocky Mountains in North America.