Geomorphic Processes
Geomorphic processes refer to the dynamic interactions of both endogenic and exogenic forces that lead to changes in the earth's surface. Endogenic processes, such as diastrophism and volcanism, exert physical stresses that shape the earth from within. In contrast, exogenic processes are responsible for modifying the earth’s surface through mechanisms like weathering, mass wasting, erosion, and deposition. This chapter focuses extensively on these exogenic processes.
Exogenic agents, like water, ice, wind, and gravity, play a crucial role in moving earth materials across landscapes. As these agents become mobile due to gravitational gradients, they remove materials from higher elevations and deposit them at lower levels. It is essential to distinguish the geomorphic agents and processes as processes involve forces acting on earth materials, while agents are the mediums that facilitate the movement and deposition of those materials.
Gravity is highlighted as a fundamental force in geomorphic processes, as it initiates the mobility of materials through its weight-driven effects. Without gravity, processes like erosion, transportation, and deposition would be largely inhibited.