Title: DESERTS AND WIND ACTION
1DESERTS AND WIND ACTION
2DESERTS AND WIND ACTION
- Desert regions and wind erosion
- Desert and adjacent region
- desert
- region which has an arid climate
- steppe
- region adjacent to a desert with semiarid climate
3DESERTS AND WIND ACTION
Desert (arid climate) and steppe
(semiarid climate) areas on Earth
4DESERTS AND WIND ACTION
- Wind erosion processes
- deflation is the removal of rock waste from the
land by the wind - blowout or deflation hollow is a depression
excavated by the wind in materials as sand and
silt deposits easily eroded because of a lack of
the presence of adequate vegetation which impedes
deflation
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Blowout or deflation hollow
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Deflation Hollow---Blowout
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abrasion is the sandblastingeffect on materials
caused by the impact with particles carried by
the windfrosted windows in houses and ventifacts
form
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- Wind erosion loads
- suspended load
- suspended wind blown particles
- consists primarily of silt or clay size particles
and if highly concentrated can result in dust
storms - deposition of the suspended load can result in
large deposits of loess lacking layering or
stratification
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Dust Storms
10DESERTS AND WIND ACTION
Loess Deposits
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- bed load
- particles bounced along the ground
- usually consists of sand size particles
- accumulation of the bed load forms desert sand
dunes which can migrate easily(active dunes) - Active sand dunes
- Nature of active (unstable) dunes
- dune profile
- consists of a more gentle windward slope and
steeper leeward slope or slipface
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Dune profile
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- shifting dunes
- shift downwind and can bury roads, airport
runways, homes, etc. - Categories of active dunes
- based on shape of dune in plan view
- barchan
- crescent shaped with convex portion facing the
wind direction - formed with a constant wind direction and limited
sand supply
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Barchan dunes
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- transverse
- elongated perpendicular to direction of wind
- formed with a constant direction of wind and
large supply of sand
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- longitudinal or seif
- elongated in general direction of wind
- formed with slightly different wind directions
and limited sand supply
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- star or complex
- formed with variable wind direction
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- Desert landscape and evolution
- Alluvial fan
- fan shaped deposit formed at the foot of
mountains in the desert valley or basin
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a bajada is an apron of sediment resulting from a
coalescence of alluvial fans
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Playa lake and playa a temporary shallow lake
formed in the central basin of a desert during a
rare abundant rainfall--a playa is the dry flat
lake bed that remains
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- Inselberg
- an isolated erosional remnant present after long
term erosion of mountain areas which are reduced
to these bedrock knobs elevated above the
surrounding sediment filled basin
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- Pediment
- a carved gently sloping erosional surface on the
bedrock in a desert mountainous area
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Stages of landscape in mountainous desert
regions
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- Inactive or stable dune---mostly non-desert
- Parabolic dune(foredune)
- formed along coastlines of oceans or large lakes
- winds cause blowouts in sand resulting in a
crescent shape with the concave side facing the
prevailing wind direction
25 THATS ALL THE CYBER GEOLOGY COURSE
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