Physical and chemical weathering

J. L. Gooding, R. E. Arvidson, Mikhail Zolotov

Research output: Chapter in Book/Report/Conference proceedingChapter

46 Scopus citations

Abstract

Although Viking Lander data suggest oxidized, palagonite-like weathering rinds on some rocks and bulk surface sediments possibly composed of clay-salt mixtures, studies of Martian weathering have remained largely theoretical with few observational constraints. Physical weathering may have included rock splitting through growth of ice, salt or secondary silicate crystals in voids. Chemical weathering probably involved reactions of minerals with water, oxygen and carbon dioxide although predicted products vary sensitively with the abundance and physical form postulated for the water. -from Authors

Original languageEnglish (US)
Title of host publicationMars
EditorsH.H. Kieffer
PublisherUniversity of Arizona Press, Space Science Series
Pages626-651
Number of pages26
StatePublished - 1992
Externally publishedYes

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ASJC Scopus subject areas

  • Earth and Planetary Sciences(all)
  • Environmental Science(all)

Cite this

Gooding, J. L., Arvidson, R. E., & Zolotov, M. (1992). Physical and chemical weathering. In H. H. Kieffer (Ed.), Mars (pp. 626-651). University of Arizona Press, Space Science Series.