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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 sulfate is a mineral compound characterized by the sulfate radical so4 2-. anhydrous sulfates, such as barite, baso4, have divalent cations linked to the sulfate radical; hydrous and basic sulfates, such as gypsum, caso4.2h2o, contain water molecules [1].?

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KarstBase a bibliography database in karst and cave science.

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Krakw
Annales Societatis Geologorum Poloniae, 2002, Vol 72, Issue 3, p. 255-262
Morphology of Czarna Cave and its significance for geomorphic evolution of the Kościeliska Valley (Western Tatra Mts.)
Abstract:

Czarna Cave represents phreatic cave with multiple loops. No cave level developed at the water table was detected. The cave was later modified by invasion vadose waters and breakdown processes. The phreatic paleoflow directions were analysed from the asymmetry of scallops. The paleoflow was directed from the east to the west, that is in a direction of Kościeliska Valley. Therefore, this valley represented the main discharge zone of the region during the formation of Czarna Cave.