Lake Michigan Coastal Dunes
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Lake Michigan Coastal Dune Home
Introduction to Lake Michigan Coastal Dunes
Features and Types of Dunes
Wind, Sand and Coastal Dunes
Climate, Dune, Lake and Seasonal Factors
Methods, Results and Research Students
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Basic Processes - Wind Erosion


Wind erosion occurs both when either the wind alone or wind carrying moving sand grains erodes surfaces or objects.

Deflation is the net removal of material by the wind. (The word comes from the Latin deflare: 'to blow away'). Surfaces with loose particles are susceptible to deflation when they are exposed to strong winds.

Abrasion is the wearing away of materials by impacts from grains in motion. Saltating sand grains can impart considerable energy when they collide with surfaces. Driftwood and other objects exposed to aeolian abrasion take on an appropriately-named 'sand-blasted' look.


Deflation and abrasion removed sand from this area, leaving small rocks with streamlined tails of sand behind.
There is a pencil tip in the photo for scale.

(Green Mountain Beach parabolic dune in November 2002.)


Basic Processes : previous page / next page / Return to Sand Movement page

 

 

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Last updated 03/23/10.