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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 bank storage is 1. subsurface conduit water that has been driven back up into older, higher karst levels and into the surrounding rock matrix during a high flow period. 2. river water that has infiltrated river banks during a high flow period and being retained in temporary storage [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.

Featured articles from Cave & Karst Science Journals
Chemistry and Karst, White, William B.
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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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Geodinamica Acta, 1999, Vol 12, Issue 0, p. 249-257
Structures tectoniques et contraintes de cheminement des eaux dans les aquiferes karstiques du barrois (Lorraine/Champagne, France)
Abstract:
Between Lorraine and Champagne, in the east of the Paris Basin, covered karst is developed in Portlandien limestone of Barrois in contact with sand and clay of the Perthois Cretaceous. The cuesta landscape is altered by folding tectonics (syncline of Treveray) and faulting tectonics (fault trough of the Marne). These govern the organization of underground flow. In low water period, hydrological methods (smoothed hydrological profiles, water tracing) display disturbances of the Barrois river (Saulx, Marne) and limits of underground watershed ('Rupt-du-Puits' cave system, 21 km long, 13 km). Macro-tectonics influence vertical infiltration (pit). Fault and dip (Macro-tectonics) divide the aquifer into different sections. Hydrological methods with flow studies confirm structural tilting of the area to the west.ResumeEntre Lorraine et Champagne, dans l'est du Bassin parisien, au contact des calcaires portlandiens du Barrois et des sables et argiles cretaces du Perthois, se developpe un karst couvert. Le paysage de cotes est ici perturbe par une tectonique souple (synclinal de Treveray) et cassante (fosse d'effon-drement de la Marne) determinant l'organisation spatiale des ecoulements. En periode d'etiage, les methodes hydrologiques (profils hydrologiques lisses, tracages), permettent de montrer l'influence de cette tectonique d'ondulation et de basculement sur l'ecoulement des rivieres barroises (Saulx, Marne). Fractures et microfractures influencent la zone de transit vertical des eaux du karst (zone des puits) tandis que les failles compartimentent les aquiferes (systeme du Rupt-du-Puits, 21 km de conduits, 13 km2). Les methodes d'etudes hydrologiques, confirment le basculement de la region vers l'ouest deduit des comparaisons de nivellement