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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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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Publisher Name: Springer, Berlin, Heidelberg
Print ISBN: 978-3-642-27833-4
Online ISBN: 978-3-642-27833-4
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Regolith, Terrestrial- Published:
- 19 November 2020
DOI: https://doi.org/10.1007/978-3-642-27833-4_1365-4
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Regolith, Terrestrial- Published:
- 04 May 2015
DOI: https://doi.org/10.1007/978-3-642-27833-4_1365-3