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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 aven is 1. a hole in the roof of a cave passage that may be either a rather large blind roof pocket or a tributary inlet shaft into the cave system. a feature described as an aven when seen from below may equally be described as shaft when seen from above, and the naming of such a feature commonly depends purely upon the direction of exploration. many avens close upwards to impenetrable fissures but may still be important hydrological routes; few caves are without them. in parts of france, aven is equivalent to the british term, pothole [9]. 2. (french.) a vertical or highly inclined shaft in limestone, extending upward from a cave passage, generally to the surface; smaller than an abime. commonly related to enlarged vertical joints. compare cenote; natural well; pothole. 3. (british.) a vertical extension from a shaft in a passage or chamber roof that tapers upward rather like a very elongate cone [10]. compare dome pit.?

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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Original article

Die Hoehle, 2007, Vol 58, Issue -3, p. 25-34
Der Murmeltierschacht (2836/239) bei Semriach (Steiermark) und seine Knochenfunde
Abstract:
First results of scientific explorations in the recently discovered Murmeltierschacht (2836/239) are presented. At present the cave has a length of 23 m and reaches a depth of 9 m. Sandy sediments that nearly filled up all the chambers were partly removed. Mainly remains of marmots (Marmota marmota L.) were recovered within the sediment. The distribution pattern of the bones suggests that they were transported into the cave together with the water-lain sediment. A marmot bone yielded a conventional AMS radiocarbon age of 14,575 45 BP. The new marmot assemblage correlates both in terms of its chronology and metrical dimensions with numerous remains in the southeastern Alpine area. At the end of the Late Glacial Maximum and during the Late Glacial period Alpine marmot was a typical faunal element in the mountainous area near Graz and the adjacent basins.