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Mega-Yardangs

A Global Analysis

Bibliographic Data

ID5877645
AuthorsAndrew Goudie (0000-0002-5496-8207, University of Oxford, corresponding author), Andrew S Goudie
Year2007
Volume1
Issue1
Pages65-81
Publication date2007-01-01
Peer ReviewedYes
Open AccessYes
TypeARTICLE
VenueGeography Compass (JOURNAL)
Journal identifiersISSN: 1749-8198 • E-ISSN: 1749-8198
PublisherWiley (PUBLISHER • GB)
DOI10.1111/j.1749-8198.2006.00003.x
OpenAlexW2023640435
LanguageEN
Citations received1
References cited33

Yardangs, analogues of which occur on Mars and possibly on Venus, are wind moulded landforms that develop in the world's drylands. Mega-yardangs (wind-abraded, ridge, and swale features of regional extent) are easily identified on satellite images and these have been employed to map their global distribution. Areas where they are present include Central Asia, the Lut Desert of Iran, northern Saudi Arabia, Bahrain, the Libyan Desert in Egypt, the central Sahara, the Namib Desert, the high Andes and the Peruvian Desert. These features develop in a wide range of rock types, including sandstones, ignimbrites, limestones and basement rocks, occur in hyper-arid areas, form where winds tend to be unimodal in direction, are best developed in areas of sand transport rather than sand accumulation, and occur in plains rather than in mountainous areas

Aeolian processes · Arid · Earth science · Geography · Geomorphology · Landform · Mars Exploration Program · Physical geography · Ridge · Sand dune stabilization · Geology and Paleoclimatology Research · Marine and environmental studies · Planetary Science and Exploration · Geology · Paleontology

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Unique citing works1
Citations per year0,11
Citation span2017 - 2017 (1)
Citation velocityhistorical
Highly citedNo
Citation typesNeutral: 1

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