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Chapter 16 Wind driven erosion
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Wind Erosion deflation desert pavement deflation hollow ventifacts Dunes barchan parabolic transverse longitudinal Loess
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Wind Erosion deflation ~ this means to “blow away”
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Wind Erosion deflation desert pavement~ this is what is left after the small stuff has blown away. This is near Reno, Nevada.
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Wind Erosion deflation hollow~ the deflation has left a hole. In the Sandhills, we call this a “blowout”
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Wind Erosion ventifacts~ rocks smoothed by wind erosion. This one is in Antarctica.
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Wind Erosion ventifacts~ rocks smoothed by wind erosion. This one is in not.
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Dunes barchan
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The open face (slip face) faces away from the wind.
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The open face (slip face) faces away from the wind.
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parabolic transverse longitudinal
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Loess
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Wind moves sand by a process known as
Saltation c. Emergence Abrasion d. Depression
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The most common kind of wind erosion is
Migration c. Saltation Abrasion d. Deflation
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Sand dunes move primarily by
Abrasion c. Migration Deflation d. Submergence
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