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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. ...

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. ...

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. ...

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 vadose cave is 1. a cave that underwent most of its development above the water table. within the vadose zone, drainage is freeflowing under gravity, and cave passages therefore have air above any water surface. the gravitational control of vadose flow means that all vadose cave passages drain downslope, they exist in the upper part of a karst aquifer, and they ultimately drain into the phreatic zone or out to the surface. active stream caves, explorable by non-diving cavers, are by definition vadose (though they generally have phreatic origins). characteristics of vadose caves are uneroded ceilings (except for immature phreatic features pre-dating the vadose conditions) and continuous downhill gradients (unless interrupted by short perched sumps). the main passage forms are canyons, with meanders and potholes, broken by subcylindrical, spray-corroded shafts that may demonstrate waterfall retreat. some of the caves of monte canin, italy, are spectacularly long and deep vadose systems [9]. 2. older, higher cave passages found in the vadose zone; usually vadose caves have been abandoned by the ground water except in times of extreme aquifer recharge. passages are usually appear as canyons and keyholes.?

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

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Featured articles from Cave & Karst Science Journals
Chemistry and Karst, White, William B.
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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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Karstologia, 2001, Issue 38, p. 1-12
Contribution spéléologique à la gestion durable d’un lac de montagne : traçages sur le bassin-versant du Königsee (Alpes de Berchtesgaden, Bavière, Allemagne)
Abstract:
Two dye tracings were made in Simetsberg massif, a part of Steinernes Meer (“Rocky sea”) in Western limestone Alps, in the heart of Berchtesgaden National Park (Bavaria, Germany). The goal was to determine drainage direction and characteristic so as to assess the Königssee vulnerability, which represents on the first hand high ecological value (oligotrophe high quality water) and on the second hand one of the most famous tourist spot in Bavaria (800.000 visitor / year in St-Bartolomä). This study was managed by Berchtesgaden National Park in collaboration with French karst scientists. The first goal was to put in evidence the Salzgrabenhöhle outlets, this cave being one of the most important in this alpine area. The second goal was to trace three lake sinkholes on the high massif, one being close to a main mountain cottage, which could constitute a pollution source for both surface and underground water. These projects put in evidence a direct high transmissivity connection first between the sinkholes and the Salzgraben cave and secondly with the Königssee lake. A catchment control is necessary for the lake conservation.