Aeolian processes, also spelled eolian, are the processes of erosion, transport and deposition of sediments caused by wind at or near the surface of the Earth, and by extension of other planets. Although water is a much more powerful eroding force than wind, aeolian processes matter most where vegetation is sparse, soil moisture is low and a large supply of loose sediment exists, as in deserts, along shorelines and in areas of glacial outwash. Wind erodes by deflation, the lifting and removal of loose particles, and by abrasion, the sandblasting of exposed surfaces. It moves grains by creep, saltation and suspension, and it deposits sand as ripples, sand sheets and dunes and silt as loess. The term comes from Aeolus, the Greek keeper of the winds.
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Source Wikipedia: Aeolian processes
Source Wikipedia: Aeolian processes
Causes
Source Barchan (Wikipedia)
Source Schlatt (landform) (Wikipedia)
Source Tukulan (Wikipedia)
In Discipline
Source Wikipedia: Aeolian processes
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1. Wikipedia: Aeolian processes
WikipediaDefinition and setting
Aeolian processes are those processes of erosion, transport, and deposition of sediments that are caused by wind at or near the surface of the earth.
Transport
Aeolian transport from deserts plays an important role in ecosystems globally.
In Discipline: Geomorphology, Lead
pertain to wind activity in the study of geology and weather and specifically to the wind's ability to shape the surface of the Earth (or other planets)
Associated With: Dune, Deposition
Wind-deposited sand bodies occur as ripples and other small-scale features, sand sheets, and dunes.
Associated With: Desert Pavement, Deflation
Most aeolian deflation zones are composed of desert pavement, a sheet-like surface of rock fragments
View the Source Barchan (Wikipedia)
Causes: Barchan, Lead sectionQuote, Causes: Barchan, Lead section
Barchans "face" the wind, appearing convex, and are produced by wind action predominantly from one direction.
View the Source Tukulan (Wikipedia)
Causes: Tukulan, Lead sectionQuote, Causes: Tukulan, Lead section
Tukulans (Russian: Тукуланы; Yakut: Тукулаан, a term from Evenki origin) are relief forms shaped by aeolian processes of the Central Yakutian Lowland, Yakutia, Russian Federation.
View the Source Schlatt (landform) (Wikipedia)
Causes: Schlatt (landform), Lead sectionQuote, Causes: Schlatt (landform), Lead section
Most of them were formed as wind-blown hollows in the periglacial region of the last ice age.
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