The simplest and the
most well-known dune is the barchan dune. The barchan
dune is a crescent-shaped dune usually located in desert climates.
The arms or "horns" of the dune point downwind,
and move faster than the center of the dune.
Barchan
dunes have a ten to one ratio of width to height. Their relatively
small size allows for barchan dunes to move between
8 and 12 feet per year. When enough sand is present, barchan dunes
coalesce into what is known as barchanoid ridges.
If these dunes continue to develop they can eventually form transverse
dunes. |
Illustration
of a barchan dune (from Great Sand Dunes National Park at www.nps.gov/archive/grsa/resources/barchan.htm).
|

Barchan dune
at White Sands National Monument, New Mexico. (Photo by Keene Swett.
University of Iowa Geosciences Slides Collection) |
These
dunes form when there is a hard, flat landscape
with wind flowing in one direction, very sparse
vegetation and a limited sand supply.
But these conditions are rarely found, even in desert environments
making this a rather uncommon dune. In fact, barchan dunes only
comprise a small percentage of the world's dunes.
In the
United States, barchan dunes can be found in deserts such as White
Sand Dunes National Monument (New Mexico)and Great Sand Dunes National
Park (Colorado). |