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CH 7.3 Landscapes Shaped by the Wind Humid areas can resist wind because the moisture holds the soil Desert soils are dry and have less vegetation to hold soil in place.

CH 7.3 Landscapes Shaped by the Wind

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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. Remember the Dust Bowl?. South Dakota before the Dust Bowl. South Dakota after the Dust Bowl. - PowerPoint PPT Presentation

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Page 1: CH 7.3 Landscapes Shaped by the Wind

CH 7.3 Landscapes Shaped by the WindHumid areas can resist wind because the moisture holds the soil together.

Desert soils are dry and have less vegetation to hold soil in place.

Page 2: CH 7.3 Landscapes Shaped by the Wind

South Dakota after the Dust Bowl

Remember the Dust Bowl?

South Dakota before the Dust Bowl

Page 3: CH 7.3 Landscapes Shaped by the Wind

Deflation = lifting and removal of loose particles such as clay and silt.

Page 4: CH 7.3 Landscapes Shaped by the Wind

Saltation = jumping or skipping along the surface.

The wind moves coarse particles along the surface of a desert by saltation.

http://www.weru.ksu.edu/new_weru/multimedia/movies/dust003.mpgWatch this closeup of Saltation!

Page 5: CH 7.3 Landscapes Shaped by the Wind

Blowout = shallow depressions resulting from deflation.

Page 6: CH 7.3 Landscapes Shaped by the Wind

Desert Pavement = surface layers of course pebbles and cobbles that are too heavy for the wind to move.

Page 7: CH 7.3 Landscapes Shaped by the Wind

Wind Abrasion = when wind blown sand cuts and polishes exposed rock.

Page 8: CH 7.3 Landscapes Shaped by the Wind

Can these be the result of wind erosion?

The wind rarely lifts sand more than a meter above the surface of the land.

Page 9: CH 7.3 Landscapes Shaped by the Wind

Wind Deposits: When more is LOESS.

China

Loess = windblown silt that blankets a landscape.

Loess Hills State Forest, Iowa

Page 10: CH 7.3 Landscapes Shaped by the Wind

Loess slides!

Loess crumbles!

The problem of having loess.

Loess sinks!New Madrid Seizmic Zone

Memphis TN

Page 11: CH 7.3 Landscapes Shaped by the Wind

DUNES= sand deposited by winds in mounds or ridges.

Page 12: CH 7.3 Landscapes Shaped by the Wind

Dunes occur in places where the wind encounters an obstruction.

This is a rock.

This is the Wind Direction

This is sand.

The sand builds up then slides.

http://www.fisica.ufc.br/hans/dunes.html

Page 13: CH 7.3 Landscapes Shaped by the Wind

Barchan

NamibiaSanta Maria, CANamibia

Types of Sand Dunes

NamibiaMars

Page 14: CH 7.3 Landscapes Shaped by the Wind

Types of Sand Dunes Longitudinal

Padre Island, TXNorth DakotaArabia

Page 15: CH 7.3 Landscapes Shaped by the Wind

Types of Sand Dunes TransverseMojave, CABrazilNamibiaMorocco

Page 16: CH 7.3 Landscapes Shaped by the Wind

Types of Sand Dunes ParabolicMoroccoNamibia

Page 17: CH 7.3 Landscapes Shaped by the Wind

Types of Sand Dunes BarchanoidMars

LibiaNew Mexico

Mars

Page 18: CH 7.3 Landscapes Shaped by the Wind

Types of Sand Dunes StarColoradoChinaAlgeria

Page 19: CH 7.3 Landscapes Shaped by the Wind
Page 20: CH 7.3 Landscapes Shaped by the Wind

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V-shaped Valley

Page 21: CH 7.3 Landscapes Shaped by the Wind

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.