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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
transgenders istanbul

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
travesti rehberi

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 lake is 1. as used in speleology, a body of standing water too deep to walk across [10]. 2. in caving, a body of standing water in a cave, but used for what would be called a pond or pool on the surface [25]. 3. a body of fresh inland water [16].?

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

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Featured articles from Cave & Karst Science Journals

Characterization of minothems at Libiola (NW Italy): morphological, mineralogical, and geochemical study, Carbone Cristina; Dinelli Enrico; De Waele Jo

Chemistry and Karst, White, William B.

The karst paradigm: changes, trends and perspectives, Klimchouk, Alexander

Long-term erosion rate measurements in gypsum caves of Sorbas (SE Spain) by the Micro-Erosion Meter method, Sanna, Laura; De Waele, Jo; Calaforra, José Maria; Forti, Paolo

The use of damaged speleothems and in situ fault displacement monitoring to characterise active tectonic structures: an example from Zapadni Cave, Czech Republic , Briestensky, Milos; Stemberk, Josef; Rowberry, Matt D.;

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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

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Coulier, C.

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Abstract:
THE SAINTE BAUME KARST (Bouches du Rh�ne and Var, France), STRUCTURE AND EVOLUTION: THE HYDROGEOLOGICAL APPROACH - The Sainte-Baume range constitutes the highest and southernmost mountain of Basse-Provence. Its complex structure is due to an Upper Eocene tectonic overthrust, however, the main karstified part has developed after the Upper Miocene. Some of the most important springs have been studied and the hydrodynamical and physico-chemical characteristics are given. These results reveal two main types of springs: 1/ springs resulting from important karstification where infiltration dominates and water transit is rapid; 2/ springs resulting from weak karstification, poorly drained, where a certain storage of water controls their action. This second type of springs appears to be related to a poorly organised deep drainage level, which partly feeds a coastal karstic system (Port-Miou).