Deposition is a geological process where sediments, soil, and rocks are added to a landform or landmass. This process occurs when the agents of erosion—such as water, ice, wind, or gravity—lose their energy and can no longer transport the particles they were carrying.
Several factors can influence the deposition process, including the type of sediment being carried, the velocity of the transporting agent, and the shape of the landform or landmass receiving the sediment.
There are different types of deposition, including:
Here are some key points to remember about deposition:
How does the velocity of water affect the process of alluvial deposition?
Answer: The higher the velocity of water, the larger and heavier sediments it can transport. When the velocity decreases, the water loses its carrying capacity and deposits the sediments it was carrying, leading to alluvial deposition.