Sediment and Sedimentation
Landscapes form and constantly change due to weathering and sedimentation. The area where a sediment accumulates and is later buried by other sediments is known as its depositional environment. There are many large-scale, or regional, environments of deposition, as well as hundreds of smaller subenvironments within these regions. For example, rivers are regional depositional environments. Some span distances of hundreds of miles and contain a large number of subenvironments, such as channels, backswamps, floodplains, abandoned channels, and sand bars. These depositional subenvironments can also be thought of as depositional landforms, that is, landforms produced by deposition rather than erosion.
Depositional environments are often separated into three general types, or settings: terrestrial (on land), marginal marine (coastal), and marine (open ocean). Examples of each of these three regional depositional settings are as follows: terrestrial-alluvial fans, glacial valleys, lakes; marginal marin-beaches, deltas, estuaries, tidal mud and sand flats; marine-coral reefs, abyssal plains, continental slope.
- Sediment and Sedimentation - Sedimentary Structures
- Sediment and Sedimentation - Chemical Deposition
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Science EncyclopediaScience & Philosophy: Jean-Paul Sartre Biography to Seminiferous tubulesSediment and Sedimentation - Weathering, Water, Wind, Glacial Ice, Sediment Erosion, Sediment Size, Sediment Load - Erosion and transport, Agents of erosion and transport, Deposition