Introduction
Karst is characterized by spectacular surface topographies, caves, and subterranean drainage systems that have developed in soluble limestone, dolostone, or gypsum bedrocks (e.g., Jennings, 1971, 1985; Sweeting, 1973; Bögli, 1980; Trudgill, 1985). Karst is geologically complex because it represents the balance between the diametrically opposed processes of dissolution and precipitation which are mediated by groundwater that flows over and through the bedrock. Thus, from a geological perspective karst is a subaerial diagenetic terrain. Esteban and Klappa (1983) defined karst as “... a diagenetic facies, an overprint in subaerially exposed carbonate bodies, produced and controlled by dissolution and migration of calcium carbonate in meteoric waters, occurring in a wide variety of climatic and tectonic settings, and generating a recognizable landscape.” Similarly, Choquette and James (1988)defined karst to “... include all of the diagenetic features—macroscopic and...
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© 1978 Dowden, Hutchinson & Ross, Inc.
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Jones, B. (1978). Ancient karst. In: Middleton, G.V., Church, M.J., Coniglio, M., Hardie, L.A., Longstaffe, F.J. (eds) Encyclopedia of Sediments and Sedimentary Rocks. Encyclopedia of Earth Sciences Series. Springer, Dordrecht. https://doi.org/10.1007/978-1-4020-3609-5_5
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