Niveltumisesta

Niveltumisesta is a term used in the field of geology and geography to describe the process of leveling or flattening of landforms over time. This phenomenon is primarily driven by natural forces such as erosion, weathering, and tectonic activity. Niveltumisesta can occur gradually over millions of years or more rapidly due to events like volcanic eruptions or earthquakes. The process often results in the creation of flat or gently sloping surfaces, such as plains and plateaus. In some cases, niveltumisesta can lead to the formation of new bodies of water, as the land is lowered below the surrounding water level. This process is a key factor in the evolution of landscapes and the distribution of geological features on Earth.