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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 marginal polje is 1. flat plain surrounded by higher limestone country on all except one side which consists of impermeable ridges or hills. such a feature is normally found on the edge of a karst area or region [20]. 2. flat limestone plain which is surrounded by higher country but is bordered on one side by impervious rock [10]. synonyms: (french.) polje marginal; (german.) randpolje, semipolje; (greek.) perithoriakon 'polje'; (italian.) polje marginale; (spanish.) polje marginal; (turkish.) kenar golova; (yugoslavian.) rubno polje, robno polje. see randpolje. compare blind valley.?

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

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Browse Speleogenesis Issues:

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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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

Ukrainian Institute of Speleology and Karstology, Simferopol
Hypogene speleogenesis and karst hydrogeology of artesian basins, 2009, p. 121-127

Among the ca. 14,000 registered caves of Austria few have been attributed to hypogene speleogenesis. This paper provides an overview of hypogene caves in Austria. A few dozen examples are known around the Vienna Basin. Some of these caves, such as Eisensteinhhle and Nasser Schacht, display a thermally anomalous microclimate and are associated with thermal springs. Other caves are inactive, but their morphology and deposits are suggestive of a hypogene origin. Preliminary morphologic observations suggest sulfuric speleogenesis for Stephanshhle near Bad Deutsch Altenburg. In the Northern Calcareous Alps, which host the majority of caves of Austria, only very few have previously been identi?ed as hypogene (e.g., Mrchenhhle, Wasserhhle), but the number of such caves is likely to increase in the near future. Also, “normal” (epigenetic) cave systems sometimes show morphological evidence suggestive of a hypogene origin, but conclusive proof is lacking. The only Austrian cave where a sulfuric acid speleogenesis is well documented is Kraushhle. In marbles of the Central Alps lukewarm and thermal springs are present and cavities of likely hypogene origin were encountered during tunnel construction near Lend. In a nearby cave, Entrische Kirche, isotopic evidence of marble alteration by warm paleowaters was recently identi?ed. Extensive calcite deposits are also known from nearby Stegbachgraben, and ongoing isotopic and fluid-inclusion studies strongly suggest hypogene water-rock interaction at lukewarm (<40°C) temperatures there. A few caves in the Southern Calcareous Alps also show morphological evidence of a hypogene origin (e.g. Kozakhhle), which is U/Th-dated to older than ca. 144,000 years. CO2 -rich springs discharge nearby.