Sedimentation Processes

Sedimentation processes refer to the ways in which particles like soil, sand, and rocks settle out of water or air and accumulate in layers over time. In historical geomorphology, these processes help us understand how landscapes have changed throughout history. For example, rivers may carry sediments that build up riverbanks or deltas, while wind can create dunes. By studying these sediment layers, scientists can reconstruct past environments, climate conditions, and geological events, providing insights into how our Earth’s surface has evolved over millions of years.