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Ventifact

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Aventifact(alsowind-faceted stone,windkanter[1]) is arockthat has been abraded, pitted, etched, grooved, or polished by wind-driven sand or ice crystals.[2]The word “Ventifact” is derived from theLatinword “Ventus” meaning ‘wind’. These geomorphic features are most typically found in arid environments where there is littlevegetationto interfere withaeolianparticle transport, where there are frequently strongwinds,and where there is a steady but not overwhelming supply ofsand.

Wind-carved "mushroom"shaped rocks are the centerpiece ofWhite Desert National Park,Egypt

Ventifacts can be abraded (abrasion) to eye-catching natural sculptures such as the main features of theWhite Desert National ParknearFarafra OasisinEgypt.In moderately tall, isolated rock outcrops,mushroomshaped pillars ofrockmay form as the outcrop is eroded bysaltatingsand grains. This occurs because, even in strongwinds,sandgrains can't be continuously held in theair.Instead, theparticlesbounce along the ground, rarely reaching higher than a few feet above theEarth.Over time, the bouncingsandgrains can erode the lower portions of a ventifact, while leaving a larger less eroded cap. The resulting forms thus frequently resemble fantasticalstonemushrooms.

Individual stones, such as those formingdesert pavement,are often found with grooved, etched, or polishedsurfaceswhere these same wind-driven processes have slowly worn away therock.

Ventifacts are typically of three types - •Einkantershaving one polished side (excluding the bottom part) (Germanword ‘ein’ means ‘one’) •Zweinkantershaving two polished sides (excluding the bottom part)(Germanword ‘zwei’ means ‘two’) •Dreinkantershaving three polished surface (excluding the polished surface at bottom) those meet up at sharp angles(Germanword ‘drei’ means ‘three’)[3]

When ancient ventifacts are preserved without being moved or disturbed, they may serve as a paleo-windindicators. The wind direction at the time the ventifact formed will be parallel to grooves orstriationscut into therock.

Ventifacts have also been discovered onMars,where such sharp immobilerockshave caused significant damage to the wheels of theCuriosityrover.[4]An example of aMartianventifact was namedJake Matijevic.By analyzing its shape, it was possible to reconstruct the mainwinddirection which sculpted therock.[5]

See also[edit]

  • Arkenu structures– pair of geological features in Libya
  • Blowout (geomorphology)– Depressions in a sand dune ecosystem caused by the removal of sediments by wind
  • Dune– Hill of loose sand built by aeolian processes or the flow of water
  • Yardang– Streamlined aeolian landform
  • Ventifact Knobs– Geographic feature in Antarctica,Antarctica

References[edit]

  1. ^Klaus K. E. Neuendorf,Glossary of Geology,p. 723
  2. ^Laity, Julie E. (2009). "19. Landforms, landscapes, and processes of aeolian erosion". In Parsons, Anthony J.; Abrahams, Athol D. (eds.).Geomorphology of desert environments(2nd. ed.). [Dordrecht]: Springer. pp. 597–628.ISBN978-1402057199.
  3. ^Livingstone, Ian; Warren, Andrew (1996).Aeolian geomorphology: an introduction.Harlow: Longman.ISBN978-0-582-08704-0.
  4. ^NASA,Premature Wear of the MSL Wheels,2017-09-26
  5. ^Patrick Zasada (2013)Entstehung des Mars-Gesteins "Jake Matijevic".Sternzeit,issue 2/2013:pp. 98–101. (German language).

External links[edit]