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Sediments

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Part of the Encyclopedia of Earth Sciences Series book series (EESS)

Synonyms

Accumulation; Deposit

Definition

Sediments are solid, fragmented particulate matter (silt, sand, and gravel), which are transported and deposited by physical processes such as water, wind, and ice. Sediments consist of loose, solid particles originating from the weathering and erosion of rocks, or chemical precipitation from solution, including secretion by organisms in water.

Sediment Characteristics

Sediments vary in terms of particle size, shape (round, oblong, and angular), density, and composition. For example, the most common mineral in river sediment is normally quartz (Williams 2012). Over time sediments become sedimentary rocks through lithification. Sedimentary rocks are basically clastic, chemical, or organic in nature. Common sedimentary structures include bedding (cross-bedding, graded bedding), mud cracks, ripple marks, and fossils.

Sediment Classification

Sediment classification is based on particle size (texture), location (grain deposition), source, and...

Keywords

  • Alluvial Environments
  • Upward Velocity
  • Sediment Classification
  • Settling Velocity
  • Vegetation Mantle

These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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Correspondence to Nicolas R. Dalezios .

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Dalezios, N.R., Eslamian, S., Ostad-Ali-Askari, K., Rabbani, S., Saeidi-Rizi, A. (2018). Sediments. In: Bobrowsky, P., Marker, B. (eds) Encyclopedia of Engineering Geology. Encyclopedia of Earth Sciences Series. Springer, Cham. https://doi.org/10.1007/978-3-319-12127-7_254-1

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  • DOI: https://doi.org/10.1007/978-3-319-12127-7_254-1

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  • Publisher Name: Springer, Cham

  • Print ISBN: 978-3-319-12127-7

  • Online ISBN: 978-3-319-12127-7

  • eBook Packages: Springer Reference Earth & Environm. ScienceReference Module Physical and Materials Science