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Speleology in Kazakhstan

Shakalov on 04 Jul, 2018
Hello everyone!   I pleased to invite you to the official site of Central Asian Karstic-Speleological commission ("Kaspeko")   There, we regularly publish reports about our expeditions, articles and reports on speleotopics, lecture course for instructors, photos etc. ...

Speleology in Kazakhstan

Shakalov on 04 Jul, 2018
Hello everyone!   I pleased to invite you to the official site of Central Asian Karstic-Speleological commission ("Kaspeko")   There, we regularly publish reports about our expeditions, articles and reports on speleotopics, lecture course for instructors, photos etc. ...

Speleology in Kazakhstan

Shakalov on 11 Jul, 2012
Hello everyone!   I pleased to invite you to the official site of Central Asian Karstic-Speleological commission ("Kaspeko")   There, we regularly publish reports about our expeditions, articles and reports on speleotopics, lecture course for instructors, photos etc. ...

New publications on hypogene speleogenesis

Klimchouk on 26 Mar, 2012
Dear Colleagues, This is to draw your attention to several recent publications added to KarstBase, relevant to hypogenic karst/speleogenesis: Corrosion of limestone tablets in sulfidic ground-water: measurements and speleogenetic implications Galdenzi,

The deepest terrestrial animal

Klimchouk on 23 Feb, 2012
A recent publication of Spanish researchers describes the biology of Krubera Cave, including the deepest terrestrial animal ever found: Jordana, Rafael; Baquero, Enrique; Reboleira, Sofía and Sendra, Alberto. ...

Caves - landscapes without light

akop on 05 Feb, 2012
Exhibition dedicated to caves is taking place in the Vienna Natural History Museum   The exhibition at the Natural History Museum presents the surprising variety of caves and cave formations such as stalactites and various crystals. ...

Did you know?

That evaporation opportunity is the amount of water made available for discharge into the atmosphere [16].?

Checkout all 2699 terms in the KarstBase Glossary of Karst and Cave Terms

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KarstBase a bibliography database in karst and cave science.

Featured articles from Cave & Karst Science Journals
Chemistry and Karst, White, William B.
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Calculating flux to predict future cave radon concentrations, Rowberry, Matt; Marti, Xavi; Frontera, Carlos; Van De Wiel, Marco; Briestensky, Milos
Microbial mediation of complex subterranean mineral structures, Tirato, Nicola; Torriano, Stefano F.F;, Monteux, Sylvain; Sauro, Francesco; De Waele, Jo; Lavagna, Maria Luisa; D’Angeli, Ilenia Maria; Chailloux, Daniel; Renda, Michel; Eglinton, Timothy I.; Bontognali, Tomaso Renzo Rezio
Evidence of a plate-wide tectonic pressure pulse provided by extensometric monitoring in the Balkan Mountains (Bulgaria), Briestensky, Milos; Rowberry, Matt; Stemberk, Josef; Stefanov, Petar; Vozar, Jozef; Sebela, Stanka; Petro, Lubomir; Bella, Pavel; Gaal, Ludovit; Ormukov, Cholponbek;
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PO BOX 746, TROY, NY 12181-0746 USA
Carbonates and Evaporites, 2002, Vol 17, Issue 2, p. 107-113
Speleology of gypsum caves in Oklahoma
Abstract:
The gypsum caves of western Oklahoma are situated in three separate areas of evaporite karst: (1) the Cimarron Gypsum Hills, in the northwest, along the Cimarron River; (2) the Weatherford Gypsum Hills, in west-central Oklahoma, to the north of the Wichita Mountains; and (3) the Mangum Gypsum Hills, in the southwest, west of the Wichita Mountains. Caves of the Cimarron Gypsum Hills and the Mangum Gypsum Hills are developed in the alternating dolomite, gypsum/anhydrite, and shale beds of the Permian Blaine Formation. Ranging from natural bridges to extensive cave systems, the largest is the 10 km of passages in Jester Cave in the Mangum Gypsum Hills. Cave passages formed in the normally paired gypsum and dolomite beds exhibit narrow (1.5-5 in wide), sinuous, canyon-like profiles. The development of broader passages, with widths from 5 in to more than 3 5 in, involve the shale beds. Some are bedding-plane passages with extremely low ceilings, whereas others are comfortable, walking-height passages with ceilings from 3-15 in high. The Blaine Formation, in the area of humanly mappable cave development, is from 12 in to approximately 50 in thick. The caves drain the bluffs/escarpments and normally end in karst spring resurgences. Roof collapse often modifies these resurgences into breakdown mazes. The Weatherford Gypsum Hills caves are formed in the Permian Cloud Chief Formation. The Cloud Chief gypsum is chalkier than the Blaine gypsums and the resultant cave development is more segmented, ranging from natural bridges (1.5-15 in in length) to cave segments (locally referred to as 'tunnels') that are tens of meters to more than one kilometer in length. These caves exhibit very little vertical development, and none of the bedding-plane development found in the Blaine Formation