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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 constructive waterfall is a large rimstone dam on a surface stream [10]. see rimstone dam. synonyms: (french.) chute incrustante; (german.) waberfall, inkrustierender?, sinter...?, sinterbecken; (greek.) katarraktis; (italian.) (vasche d'incrostazione); (spanish.) dique travertinico; (turkish.) dusum; (yugoslavian.) slap, precaga.?

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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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;

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Sesiano, J.

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Abstract:
Dye tracing and physico-chemical analysis of two important springs in the Arve valley (Haute-Savoie, France) - Several dye-tracing experiments and physico-chemical analysis of water samples taken during 18 months were performed at two important springs in the Arve valley (Haute-Savoie, France). The water origin and the type of flow, very different from one to the other, are thus explained. The first spring collects water from both a bare high-altitude karst and a forested karst at a lower elevation. It gathers also waters from the lakes Flaine and Vernant. The drainage is superficial, with strong but short water outbursts; water storage is nevertheless important, the spring being perennial. The physico-chemistry of its water is similar to that of springs located in the Northern Prealps. The second spring is very different. The physico-chemistry variations being much smoother. It comes from a basin filled with fluvio-glacial deposits and located under the Gers Lake. Its physico-chemical properties are rather similar to those of typical springs located in Provence and Southern Provence.