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Loess records

  • Onn Crouvi
  • , Jimin Sun
  • , Denis Didier Rousseau
  • , Daniel R. Muhs
  • , Marcelo A. Zárate
  • , Samuel Marx
  • Geological Survey of Israel
  • CAS - Institute of Geology and Geophysics
  • Géosciences Montpellier
  • Columbia University
  • United States Geological Survey
  • Universidad Nacional de La Pampa
  • University of Wollongong

Research output: Chapter in Book/Report/Conference proceeding › Chapter › peer-review

4 Citations (Scopus)

Abstract

Loess is an eolian deposit, composed mainly of silt grains, which can be identified in the field as a distinct sedimentary body. It covers a significant portion of the land surface of the Earth and is one of the most important terrestrial archives of long-term dust deposition. Loess appears on almost all continents, and ranges in thickness up to several hundred of meters. Most loess sequences include buried soils (paleosols), alternating with unaltered loess layers. As the formation of loess is controlled, at least partly, by climate, alternating loess deposits and buried soils hold valuable information of Quaternary climatic and environmental conditions, especially of past wind regimes.

Original languageEnglish
Title of host publicationEncyclopedia of Quaternary Science
PublisherElsevier
PagesVol3:505-Vol3:528
ISBN (Electronic)9780323999311
ISBN (Print)9780443299971
DOIs
Publication statusPublished - 1 Jan 2024

ASJC Scopus subject areas

  • General Earth and Planetary Sciences

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