Similarly, a zweikanter has two wind facets, an einkanter, has only one wind facet. 
Most places on the planet have several weathering processes acting at the same time, so finding good examples of Dreikanters is often difficult. Antarctica is a good location for finding such ventifacts since wind is usually the only active weathering agent. Many specimens in the Northeastern United States were formed during the Pleistocene era when the absence of vegetation made for little cover from wind-blown sediment.
In areas where there is a prevailing wind, sand and debris cause a rock face to become flattened and polished. This changes the mass distribution of the rock, and may cause it to turn another surface toward the wind. If this process continues undisturbed, the resulting rock will have three distinct flattened and polished faces. Dreikanters generally form in dry, arid environments from hard rocks.
- Wade, A. 1910. On the formation of dreikanter in desert regions. The Geological Magazine, Decade V, 7(9):394-398.
- "Трехгранники". Brockhaus and Efron Encyclopedic Dictionary (in Russian). 1906.
- WeatherTalk - Jargon Archived October 19, 2012, at the Wayback Machine.
- Greeley, R., N. T. Bridges, R. O. Kuzmin, and J. E. Laity, Terrestrial analogs to wind-related features at the Viking and Pathfinder landing sites on Mars, J. Geophys. Res., 107(E1), 10.1029/2000JE001481, 2002.
- Dutch, Steven. "Wind Erosion". University of Wisconsin. Retrieved 10 October 2012.
- U.S. Geological Survey Photographic Library ( http://libraryphoto.cr.usgs.gov/ )
- "Ventifact (stone)". Britannica Online Encyclopedia. Retrieved 10 October 2012.
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