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Regolith, Terrestrial

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Encyclopedia of Astrobiology
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Synonyms

Laterites; Soil

Definition

The terrestrial regolith (ῥῆγος = rhegos = blanket; λίθος = lithos = rock) is a layer of unconsolidated material overlying solid rock. It forms as a result of mechanical and chemical weathering, biological processes, deposition of loose material, or brecciation of rock. It may consist of soil, alluvium, and other sedimentary deposits; fractured and oxidized rock; and volcanic ash or scoria. Its thickness varies from negligible to several hundred meters. Regoliths have been observed on Earth, Moon, some asteroids, and other planets.

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Correspondence to Nicholas Arndt .

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Arndt, N. (2021). Regolith, Terrestrial. In: Gargaud, M., et al. Encyclopedia of Astrobiology. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-27833-4_1365-4

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  • DOI: https://doi.org/10.1007/978-3-642-27833-4_1365-4

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  • Print ISBN: 978-3-642-27833-4

  • Online ISBN: 978-3-642-27833-4

  • eBook Packages: Springer Reference Physics and AstronomyReference Module Physical and Materials ScienceReference Module Chemistry, Materials and Physics

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Chapter history

  1. Latest

    Regolith, Terrestrial
    Published:
    19 November 2020

    DOI: https://doi.org/10.1007/978-3-642-27833-4_1365-4

  2. Original

    Regolith, Terrestrial
    Published:
    04 May 2015

    DOI: https://doi.org/10.1007/978-3-642-27833-4_1365-3