Title: Wind Erosion
1Wind Erosion
2Take-Away Points
- Wind erosion has little effect on solid rock
- Wind mostly moves loose material
- Sand dunes depend on strength and steadiness of
wind and abundance of sand - Windblown silt is called loess
- Loess is the raw material for many mollisols, the
best agricultural soils
3Abrasion
- Ventifacts or Dreikanters
- Polishing,
- Undercutting
- Streamlining (Yardangs)
- On Mars, with billions of years of only wind
erosion, wind has had much greater effects
4Ventifacts, Antarctica
5Dreikanter, Wisconsin
6Wind Abrasion, Independence Rock, Wyoming
7Wind (Aeolian) Landforms
- Little Power to Attack Solid Rock
- Most Effective in Moving Loose Material
- Mechanisms
- Suspension (Silt)
- Saltation (Sand)
- Rolling
8Wind (Aeolian) Landforms
- Deposition
- Dunes
- Loess
- Erosion
- Deflation Basins (Blowouts)
- Lag Deposits, Desert Pavement
9Sand Dunes
10Longitudinal Dunes, Colorado
11Longitudinal Dunes, Colorado
12Longitudinal and Transverse Dunes, Colorado
13Transverse Dunes, Sand Hills, Nebraska
14Beach Dunes, Michigan
15Barchans, Sand Hills, Nebraska
16Snow Barchans, Wisconsin
17Snow Barchans, Wisconsin
18Star Dune, Nevada
19Great Sand Dunes, Colorado
20Great Sand Dunes, Colorado
21Great Sand Dunes, Colorado
22Desert Pavement, California
23Lag Deposit, Minnesota
24Blowout, Wisconsin
25Loess
- Silt-sized
- Derived from Glacial Outwash in U.S.
- Found in U.S., E. Europe, China
- Parent material of worlds prime agricultural
soils - Available nutrients
- Fine size lots of surface area
- Cohesive good root support
- Porous retains water well
- No Rocks!!!!
26Loess, Wisconsin
27Loess in the U.S.
28Loess in Europe
29Loess in China
30Take-Away Points
- Wind has little effect on solid rock
- Wind mostly moves loose material
- Sand dunes depend on strength and steadiness of
wind and abundance of sand - Windblown silt is called loess
- Loess is the raw material for many mollisols, the
best agricultural soils