Weathering and erosion transform rock into sediments of certain sizes.
erosion
It gets buried in sediment
Mudflows then occur after
the organism must be buried in sediment soon after it dies.
Picking up sediment and moving it to another area is known as sediment transport.
Mass wasting deposits sediment by the downslope movement of weathered rock or soil due to gravity. It can occur as landslides, rockfalls, mudslides, or other forms of mass movement, transporting sediment downslope where it may accumulate, creating sediment deposits.
It commonly occurs in bodies of water such as lakes or oceans.
During lithification, two processes occur: compaction, which involves the reduction of pore spaces between sediment grains due to the weight of overlying sediments, and cementation, which involves the precipitation of minerals in the pore spaces, binding the sediment grains together to form rock.
The process of moving sediment to other places is called sediment transport. It can occur through erosion, where sediments are lifted and carried by wind, water, or ice to be deposited in new locations. Sediment transport plays a key role in shaping landscapes and ecosystems.
Silt and clay size sediments form shale.
It most commonly occurs in bodies of still water such as lake or the sea.
Sandbars occur when sediment is deposited by water, usually in shallow areas such as rivers or coastlines. They can form due to changes in water flow, wave action, or changes in sediment supply. Sandbars are dynamic features that can change over time due to natural processes.