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Enviroscan Ukrainian Institute of Speleology and Karstology


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Featured article from geoscience journal


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PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS

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Geomorphology, 2005, Vol 67, Issue 0, p. 457-471

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Morphometry and distribution of isolated caves as a guide for phreatic and confined paleohydrological conditions

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Abstract:

Isolated caves are a special cave type common in most karst terrains, formed by prolonged slow water flow where aggressivity is locally boosted. The morphometry and distribution of isolated caves are used here to reconstruct the pateohydrology of a karstic mountain range. Within a homogenous karstic rock sequence, two main types of isolated caves are distinguished, and each is associated with a special hydrogeologic setting: maze caves form by rising water in the confined zone of the aquifer, under the Mt. Scopus Group (Israel) confinement, while chamber caves are formed in phreatic conditions, apparently by lateral flow mixing with a vadose input from above. (c) 2004 Elsevier B.V. All rights reserved

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Keywords: aquifer, c, cave, cave formation, cave morphology, caves, chamber, chamber caves, confinement, distribution, flow, form, groundwater dissolution, hydrogeologic setting, input, israel, karst, karst aquifer, karst systems, karst terrain, karst terrains, limestone caves, maze caves, mixing, models, morphometry, mountain, origin, phreatic, range, rising water, rock, sequence, terrain, time, times, water, water-flow, zone,

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