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Speleology in Kazakhstan

Shakalov on 11 Jul, 2012
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 Also we have forum there. ...

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 oceanic water is sea water with a total salt content of about 34,500 ppm [16].?

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.

Latest news:

Eurokarst-2016 - submission deadline postponed
The deadline for submitting abstracts (French or English) to the Eurokarst conference is slightly postponed to the 15th of October.
Karst Session at the 10th International Conference on Remediation of Chlorinated and Recalcitrant Compounds
The International Conference on Remediation of Chlorinated and Recalcitrant Compounds is the world’s largest and most comprehensive meeting on the application of innovative and existing technologies and approaches for characterization, monitoring and management of chlorinated and complex sites.
Science and challenges into the deepest cave of Spain
The Geological Survey of Spain (IGME) is conducting a research into the Cerro del Cuevon (-1589 m), the deepest cave of Spain and one of the top ten around the world.
International Speleological Congress 2017 in Sydney, Australia
International Speleological Congress will be held in 2017 in Sydney, Australia
Call for papers for Special issue on the topic of "Geophysical imaging in karst terrain"
Contributions are invited for the special issue on the topic of "Geophysical imaging in karst terrain", which will be published in AIMS Geosciences in 2016.

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Did you know?

That partition is 1. a nearly vertical residual rock mass in a cave. 2. a continuous rock span across a cave [10].?

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

Featured articles from Cave & Karst Science Journals
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Featured articles from other Geoscience Journals
Turkish karst aquifers, Gunay, G.; Guner, N.; Tork, K.
Sulphuric acid speleogenesis and landscape evolution: Montecchio cave, Albegna river valley (Southern Tuscany, Italy), Piccini, Leonardo; De Waele, Jo; Galli, Ermanno; Polyak, Victor J.; Bernasconi, Stefano M., Asmerom, Yemane
The role of condensation in the evolution of dissolutional forms in gypsum caves: Study case in the karst of Sorbas (SE Spain), Gazquez, Fernando; Calaforra, José Maria; Forti, Paolo; De Waele, Jo; Sanna, Laura
See all featured articles from other geoscience journals

Glossary of Karst and Cave Terms

Based on "A Lexicon of Cave and Karst Terminology with Special to Environmental Karst Hydrology" EPA/600/R-02/003, 2002, EPA: Washington, DC., Speleogenesis Glossary includes 2699 cave & karst terms



A type of limestone resembling a breccia, in which angular limestone fragments are cemented together by limestones of different composition. Pseudo-breccias are common in many preserved limestone sequences and may owe their origin to the dissolutional removal of originally interbedded and interstitial sulfate minerals followed by break-up and redistribution of the residual carbonate component [9].

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