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Enviroscan Ukrainian Institute of Speleology and Karstology

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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 alkaline is any of various soluble mineral salts found in natural water and arid soils having a ph greater than 7. in water analysis, it represents the carbonates, bicarbonates, hydroxides, and occasionally the borates, silicates, and phosphates in the water [6].?

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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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;
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Vienna
Die Hoehle/Die Höhle, 2004, Vol 55, Issue 0, p. 19-33
Speläologische Charakterisierung und Analyse des Hochschwab-Plateaus, Steiermark.
Abstract:
The Hochschwab is one of the major karst massifs of the Northern Calcareous Alps (NCA), situated in the north of the Austrian province of Styria and provides freshwater for the city of Vienna. Karstmorphological mapping of 44 km² of its plateau brought the discovery of 770 new caves. Together with formerly recorded caves and possible caves detected on aerial photographs a total of 1284, mainly vertical objects are integrated into a GIS. In combination with additional digital datasets, statistical analyses are performed considering the spatial distribution of cave density as well as the dependence on altitude and lithology. Beside this, the most important caves within the study area are characterised. The investigated caves are mainly pits and vertical canyons which developed in the vadose zone. Phreatic cave levels associated with former valley floors, which are common in the NCA, do not exist in the Hochschwab. A few caves of phreatic origin developed above aquitard geological units. The average cave density in the investigation area is 24 objects/km². In glacially strongly overprinted areas it increases to more than 400 caves per km². Remarkable facts of the dependence on lithology are that the limestone of the Dachstein Formation does not show an increased cave density. In contrast, the diverse facies of the limestones of the Wetterstein Formation exhibit major differences.[Hundsbodenschacht (1744/11), G'hacktsteinschacht (1744/14), Furtowischacht (1744/310), Sargdeckelschacht (1744/363), TremmelSchacht-413 (1744/413), EBNK-Schacht (1744/426), Schrägschacht (1744/442), Hirschgrubenhöhle (1744/450), Melkbodeneishöhle (1745/1), Eis-Schacht-39 (1745/39), Spaltenschacht (1745/43)]