Karst window
Template:Short description A karst window, also known as a karst fenster, is a geomorphic feature found in karst landscapes where an underground river is visible from the surface within a sinkhole.[1][2] In this feature, a spring emerges, then the discharge abruptly disappears into a sinkhole. The word fenster is German for 'window', as these features are windows into the karst landscape.
The term is used to denote an unroofed portion of a cavern which reveals part of a subterranean river.[3] A complex system of caves, known as karst topography, evolves from the effects of water erosion on carbonate rocks such as limestone, dolomite or gypsum. "A karst fenster is caused by a caving in of portions of the roof of a subterranean stream, thus making some of the underground stream visible from the surface".[4] Theories in the creation of karst topography and karst fensters involve vadose water above the water table, and deep-circulating phreatic water (water in the zone of saturation) eroding away subsurface rock. Karst fensters may also form because of weathering from above.
An example of a karst window or fenster, recognized by the Kentucky Geological Survey, is Short Creek in Pulaski County, where a small river emerges and disappears in a space of less than 100 meters in length.[5] An example of this formation on public parkland is Cedar Sink in Mammoth Cave National Park, Kentucky, where small watercourses emerge and disappear at the bottom of a large sinkhole.
References
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- ↑ Monroe, W.H., 1970. A glossary of karst terminology (No. 1899-K). US Govt. Printing Office
- ↑ *Easterbrook, Don J. Surface Processes and Landforms. Upper Saddle River, NJ: Prentice-Hall, Inc, 1999
- ↑ *Ritter, Michael E. The Physical Environment: an Introduction to Physical Geography. 2006. Dec 2009.
- ↑ Script error: No such module "citation/CS1".
- ↑ *Von Osinski, Wm. "Karst windows." In Proceedings of the Indiana Academy of Science, vol. 44, pp. 161-165. 1934. [1]
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