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Eolian Landforms
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Wind An agent of erosion –“eolian” refers to wind 2 types of eolian erosion: –abrasion: sandblasting YARDANG –deflation: blowing away loose particles DESERT PAVEMENT
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Dust storms and sand storms Dust Storm: –strong winds –sparsely vegetated –dust is carried high into air; dark cloud
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Dust storms and sand storms Sand Storm: –sand can be carried only 1-2 meters high –can be heard –sand moves by SALTATION
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DUNE Accumulation of sand, shaped by wind Dunes have windward and leeward slopes
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angle of repose Angle at which loose material is stable 30 – 34 ° for sand
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Types of Sand Dunes: 1.Barchan –point downwind –windward slope is gradual –leeward slope is steeper
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Types of Sand Dunes: 2. Transverse: waves of sand crests are perpendicular to wind
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Types of Dunes 3. Barchanoid ridge of coalesced barchans
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Types of Sand Dunes: 4. Parabolic: point upwind vegetation anchors arms large blowout depression in center
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Coastal Blowout Dune –a type of parabolic –coastal location (Great Lakes) –point upwind
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Hairpin –type of parabolic –long and narrow –point upwind
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5. Longitudinal –parallel to wind direction
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6. Star Dunes –wind from all directions
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Loess Silt-sized, wind-deposited deposit From outwash deposits of Pleistocene glaciers
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