Orogenic processes refer to the geological activities that lead to the formation of mountain ranges. These processes typically occur at tectonic plate boundaries, where plates collide, pull apart, or slide past each other. The intense pressure and heat generated during these interactions can cause the Earth's crust to fold, fault, and uplift, resulting in the creation of mountains. Common examples of orogenic processes include subduction, where one tectonic plate is forced under another, and continental collision, where two continental plates push against each other. These processes not only shape the landscape but also influence local ecosystems and climate patterns.