The geomorphological cycle, also known as the cycle of erosion, describes the process of landscape evolution over time. It involves the continuous transformation of landforms through weathering, erosion, transportation, and deposition. This cycle typically begins with the uplift of land, leading to the formation of mountains and valleys, which are then shaped by natural forces like water, wind, and ice. As these forces act on the landscape, they gradually wear down high areas and fill in low areas, creating a more level terrain. Eventually, the cycle can lead to the formation of features such as rivers, deltas, and coastal landforms. This process can take millions of years, illustrating the dynamic nature of Earth's surface.