Processes
Sedimentation
Also Known As Deposition
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The settling of transported particles out of water, ice or air, building deltas, floodplains, dunes and the layered seafloor deposits that harden into sedimentary rock. It is the constructive half of the cycle erosion begins, and the layers it lays down, one on another, are the pages the stratigraphic record is written on.
Facts
TimescaleSettling happens in hours to seasons; burying deposits deep enough to become rock takes millions of years 1 Driving ForceThe loss of energy in the water, wind or ice transporting sediment, which allows particles to settle out under gravity. 1 Resulting FeatureDeposits sediment in layers whose grain size and structure record the energy and environment of the transporting medium, from riverbeds to the deep ocean floor. 1 SignificanceThe layering produced by sedimentation is the basis of stratigraphy and the principal way geologists read past environments from the rock record. 1 Cross-Tradition Connections
Associated With
Erosion strips and transports the material sedimentation later lays down.
Lithification turns the deposits sedimentation lays down into solid rock.
Sedimentology studies the deposition processes sedimentation names, alongside transport and diagenesis.
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