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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. ...

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 dripstone is calcium carbonate deposited from water dripping from the ceiling or wall of a cave or from the overhanging edge of a rock shelter; commonly refers to the rock in stalactites, stalagmites, and other similar speleothems; in some places composed of aragonite or gypsum [10]. synonyms: (french.) concretions; (german.) tropfstein, stalagmit, stalaktit; (greek.) stalaktitis, stalagmitis; (italian.) concrezione; (russian.) kapeljnik; (spanish.) concrecion (estalagmitjca o estalactitica); (turkish.) damlatasi; (yugoslavian.) sige, smugori. see also flowstone.?

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.
See all featured articles
Featured articles from other Geoscience Journals
Karst environment, Culver D.C.
Mushroom Speleothems: Stromatolites That Formed in the Absence of Phototrophs, Bontognali, Tomaso R.R.; D’Angeli Ilenia M.; Tisato, Nicola; Vasconcelos, Crisogono; Bernasconi, Stefano M.; Gonzales, Esteban R. G.; De Waele, Jo
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;
See all featured articles from other geoscience journals

NSS
Journal of Cave and Karst Studies, 2002, Vol 64, Issue 1, p. 63-70
Using Geographic Information Systems to Develop a Cave Potential Map for Wind Cave, South Dakota
Abstract:
The cave potential map concept was originally developed to address management concerns, but other uses rose to the forefront, including the likely maximum boundaries of Wind Cave, the potential surveyable length of the cave, and the possibilities of a connection with Jewel Cave. In addition, this method may provide means to judge the exploration potential for any section of the cave and to evaluate hypotheses regarding the caves origin. The cave potential map was based on structural geologic factors, surface contour maps, cave survey data, surface blowhole locations, and hydrologic maps. Geographic information systems (GIS) were used to combine these data with GIS-generated triangular irregular networks, slope and aspect, orthophotoquads, a park boundary map, and land ownership maps. By combining these datasets and deriving buffers and overlays, it was determined that the current cave boundaries cover 1/10 of the total potential or maximum likely extent of the cave. The likely maximum potential boundaries are 97% inside of the current boundaries of Wind Cave National Park. Based on passage density, the length of the Wind Cave survey could range from 400-1760 km. Since the current 166 km of survey represents no more than 40% of the minimum predicted length of the cave or as little as 9% of the maximum predicted length of the cave, a tremendous amount of surveyable passage remains in the system.