Tectonic Plates: The Earth'slithosphere is divided into several large and small tectonic plates that float on the semi-fluid asthenosphere. The movement and interaction of these plates play a crucial role in mountain building.
Folded Mountains: One of the most common types of mountains formed through orogenesis are folded mountains, which result from the folding and buckling of the Earth'scrust due to compressional forces.
By understanding the processes and mechanisms involved in mountain building, we can gain valuable insights into the dynamic nature of the Earth'scrust and the formation of some of the most spectacular landforms on our planet.