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- Sedimentation is a geological process that results in the formation of sedimentary rock. It involves the deposition of sediments, from initial erosion through sediment transport and settling to the lithification of the sediments1. Sedimentation can also refer to a physical water treatment process that uses gravity to remove suspended solids from water2.Learn more:✕This summary was generated using AI based on multiple online sources. To view the original source information, use the "Learn more" links.In geology, sedimentation is the deposition of sediments which results in the formation of sedimentary rock. The term is broadly applied to the entire range of processes that result in the formation of sedimentary rock, from initial erosion through sediment transport and settling to the lithification of the sediments.en.wikipedia.org/wiki/SedimentationSedimentation is a physical water treatment process using gravity to remove suspended solids from water. Solid particles entrained by the turbulence of moving water may be removed naturally by sedimentation in the still water of lakes and oceans.en.wikipedia.org/wiki/Sedimentation_(water_treatm…
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Sedimentation is the deposition of sediments. It takes place when particles in suspension settle out of the fluid in which they are entrained and come to rest against a barrier. This is due to their motion through the fluid in response to the forces acting on them: these forces can be due to gravity, centrifugal … See more
Settling
Classification
Classification of sedimentation:
• Type … See moreIn chemistry, sedimentation has been used to measure the size of large molecules (macromolecule), where the force of gravity is augmented with centrifugal force in … See more
Wikipedia text under CC-BY-SA license WEBSedimentation is the process of deposition of a solid material from a fluid or glacial ice. Learn about the types, effects, and classification of sedimentary rocks and deposits, and the role of physical and chemical …
WEBMay 3, 2024 · sedimentary rock, rock formed at or near Earth’s surface by the accumulation and lithification of sediment (detrital rock) or by the precipitation from solution at normal surface temperatures (chemical rock).
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