The geological processes that shape Earth’s features today are referred to as ‘geomorphological processes’. These processes include a variety of natural forces such as weathering, erosion, sedimentation, and tectonic activities that continuously mold the planet’s landscape.
To elaborate, geomorphology studies the structures and processes that create the Earth’s surface features over time. For example, weathering breaks down rock materials, while erosion involves the movement of these materials from one location to another. Sedimentation is the deposition of these materials, which can give rise to new landforms. Finally, tectonic processes such as earthquakes and volcanic activity are responsible for the formation of mountains, valleys, and other significant geological structures. Together, these processes are fundamental in understanding how our planet is constantly changing and being reshaped over geological time.