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Sediment that builds up on land can come from sources like rocks breaking down, erosion from water, wind, or glaciers, and deposition of materials carried by rivers and streams. Over time, these processes contribute to the formation of soil and landforms.
The breaking up of rocks into sediments is called weathering. Weathering can be physical (mechanical) or chemical in nature, and it is a key process in the formation of sedimentary rocks.
Sediment, compressed dead solid organisms.
Sediment, compressed dead solid organisms.
Erosion can sure help in the breakdown of rocks, but technically, erosion is the movement of material from one place to another place. Weathering is the term used to describe the breaking down of rocks.