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Arid and Semi-AridArid and Semi-Arid
Landscapes ( AeolianLandscapes ( Aeolian
LandformLandform
World's DesertsWorld's Desertsabout 1/5th
of land
Types: subtropical, rain-shadow,
coastal, interior, polar
Arid and Semi-aridArid and Semi-arid
EgyptLibya
Tunisia
Algeria
Morocco
Wind-Borne Sediment causesWind-Borne Sediment causes
deflation and abrasiondeflation and abrasion
Sahara to Caribbean
Effect on Hurricanes
Surface creep
InselbergInselberg
UluruUluru (Ayers Rock)(Ayers Rock)
Pediment
MushroomMushroom
Types of DesertsTypes of Deserts
Erg - sea of sand
• vegetation rare
• sand probably formed during more humid
climate
Death Valley, California
Types of DesertsTypes of Deserts
Reg - desert “pavement” of pebbles
and stones
• all small materials and sand removed by wind
• may be very thin coating of stones
Desert pavement
Hamada - bedrock predominates
Erosional Landform - Deflation HollowErosional Landform - Deflation Hollow
Anecdote – How fast does this occur?
Abrasion Origin of VentifactsAbrasion Origin of Ventifacts
Erosional Landforms -Erosional Landforms - VentifactsVentifacts
Wind eroded (sand blasted) surfaces
Erosional Landform –Erosional Landform – Yardangs andYardangs and
ZeugenZeugen
Sphinx?
White Desert, EgyptWhite Desert, Egypt
Dune MigrationDune Migration
Just like ripples in a stream
Windward slope
erosion and transport
Slip face (deposition)
Star DunesStar Dunes
Copyright © Frank Eckardt 2002
Star DunesStar Dunes
Variable Wind DirectionVariable Wind Direction
Longitudinal DunesLongitudinal Dunes
Constant wind direction, no vegetation
Longitudinal DunesLongitudinal Dunes
Constant wind direction, no vegetation
Transverse DunesTransverse Dunes
Massive volumes of sand, low consistent winds
Transverse DunesTransverse Dunes
Massive volumes of sand, low consistent windsMassive volumes of sand, low consistent winds
Barchan DunesBarchan Dunes
Isolated Dunes, low sand supply, migrating across rock
Barchan DunesBarchan Dunes
• Isolated – low sand supply; migrating across rock
Parabolic DunesParabolic Dunes
Horns pinned by plants
Typical of coasts
Fig. 15-12a, p. 354
Parabolic DunesParabolic Dunes
• Stabilized “horns" point upwind
A Playa in Death Valley, CaliforniaA Playa in Death Valley, California
Evaporite Pan of dried-up PlayaEvaporite Pan of dried-up Playa
Playas
Differential Erosion
Desert LandformsDesert Landforms
• plateaus: a broad, flat-topped area elevated
above the surrounding land and bounded, at
least in part, by cliffs
• mesa: a broad, flat-topped hill bounded by cliffs
and capped with a resistant rock layer
• butte: a narrow hill of resistant rock with a flat
top and very steep sides
Inselberg or Bornhardt - highly
resistant rock landform; a type of
monadnock.
Bornhardt, Arches National Park, Utah

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Arid Aeolian Landform

Editor's Notes

  1. Figure 15.12a: Parabolic dunes typically form in coastal areas where there is a partial cover of vegetation, a strong onshore wind, and abundant sand.