Sedimentation is a natural process in which sediments, such as sand, mud, or mineral particles, are deposited on the bottom of bodies of water, such as rivers, lakes, or seas.
During sedimentation, suspended particles in the water gradually settle due to gravity, creating layers of sediment on the bed. This process is important for soil formation, the creation of sedimentary rocks, and the preservation of fossils.
Sedimentation can also be influenced by human factors, such as soil erosion caused by deforestation or intensive agriculture.
