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CH 7.3 Landscapes Shaped by the Wind
Humid areas can resist wind because the moisture holds the soil together. Desert soils are dry and have less vegetation to hold soil in place.
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Remember the Dust Bowl? South Dakota before the Dust Bowl South Dakota after the Dust Bowl
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Deflation = lifting and removal of loose particles such as clay and silt.
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Saltation = jumping or skipping along the surface.
The wind moves coarse particles along the surface of a desert by saltation. Watch this closeup of Saltation!
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Blowout = shallow depressions resulting from deflation.
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Desert Pavement = surface layers of course pebbles and cobbles that are too heavy for the wind to move.
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Wind Abrasion = when wind blown sand cuts and polishes exposed rock.
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The wind rarely lifts sand more than a meter above the surface of the land.
Can these be the result of wind erosion?
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Loess = windblown silt that blankets a landscape.
Wind Deposits: When more is LOESS. China Loess = windblown silt that blankets a landscape. Loess Hills State Forest, Iowa
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The problem of having loess.
Loess crumbles! Memphis TN New Madrid Seizmic Zone Loess sinks! Loess slides!
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DUNES = sand deposited by winds in mounds or ridges.
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Dunes occur in places where the wind encounters an obstruction.
This is the Wind Direction The sand builds up then slides. This is sand. This is a rock.
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Barchan Types of Sand Dunes Namibia Namibia Mars Santa Maria, CA
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Types of Sand Dunes Longitudinal Arabia Padre Island, TX North Dakota
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Types of Sand Dunes Transverse Mojave, CA Brazil Namibia Morocco
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Types of Sand Dunes Parabolic Morocco Namibia
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Types of Sand Dunes Barchanoid Mars Libia Mars New Mexico
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Types of Sand Dunes Star Colorado China Algeria
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Mountain Peak V-shaped Valley 460 450 440 430 420 410 350 400 370 390
380 V-shaped Valley 360 1 2 3 4 5 6 9 8 7
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EXPLORATION LAB CH 7 Interpreting a Glacial Landscape
When you finish the lab, create study cards based on the information on pg 212 following the guidelines on your worksheet.
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