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DESERTS AND WIND ACTION

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Presentation on theme: "DESERTS AND WIND ACTION"— Presentation transcript:

1 DESERTS AND WIND ACTION

2 DESERTS 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

3 DESERTS AND WIND ACTION
Desert (arid climate) and steppe (semiarid climate) areas on Earth

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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

5 DESERTS AND WIND ACTION
Blowout or deflation hollow

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Deflation Hollow---Blowout

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abrasion is the “sandblasting”effect on materials caused by the impact with particles carried by the wind—frosted 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

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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 CYBER GEOLOGY COURSE FOLKS
THAT’S ALL THE CYBER GEOLOGY COURSE FOLKS


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