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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 tubular passage; tube; tube passage is 1. cave passage formed by approximately equal dissolution all round when full of flowing water within the phreas. relict tubes, abandoned as the water table was lowered, are common in old caves, and may be partially filled by sediment, breakdown or stalagmite, or entrenched to form keyhole passages. tube sizes range to over 15m in diameter, but the larger ones are rarely of uniform section. peak cavern in derbyshire is well known for its fine circular phreatic tubes. some of the trunk passages of mammoth cave, kentucky, are spectacular tubes of elliptical section, formed by dissolution rates that were higher along the bedding than across [9]. 2. these are nearly horizontal cave passages (tunnels) with round or elliptical cross sections and are either straight or winding. at mammoth cave they vary in size up to 30 feet high and nearly 100 feet wide. they are formed while completely filled with flowing water. whereas they are typically wider than high as a result of dissolution along horizontal cracks and beddingplane partings, they may also form as high, narrow, straight fissures along major vertical or near vertical fractures [15]. see also canyon passage; keyhole passage; passage; vertical shaft.?

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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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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;
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Your search for norway (Keyword) returned 67 results for the whole karstbase:
Showing 16 to 30 of 67
Kvannlihola 2 and other caves in Fiplingdal and other areas of Nordland, Norway, 1983, Faulkner T. L.

Mean Annual Runoff and the Scallop Flow Regime in a Subarctic Environment: Preliminary Results from Svartisen, Norway, 1983, Lauritzen Se. , Ive A. , Wilkinson B.

Water chemistry of some karst environments in Norway, 1984, Bakalowicz M.

Morphology and Hydraulics of an Active Phreatic Conduit [Norway], 1985, Lauritzen Se. , Abbot J. , Arnesen R. , Crossley G. , Grepperud D. , Ive A. , Johnson S.

Norway's Longest and Deepest Caves, 1985, St. Pierre D. , St. Pierre S.

KVITHOLA AT FAUSKE, NORTHERN NORWAY - AN EXAMPLE OF ICE-CONTACT SPELEOGENESIS, 1986, Lauritzen S. E. ,

Caves of Lower Glomdal, Rana, Norway, 1987, Bottrell S. H.

Caves of the Jordbruelv and Jordhulefjell, South Nordland, Norway, 1987, Faulkner T. L.

Geological Controls on Speleogenesis in Lower Glomdal, Norway, 1988, Bottrell S. H.

Cave Studies in Norway (In memory of Shirley St. Pierre), 1988, Faulkner T. L. , St. Pierre D.

Tertiary Caves in Nordland, Norway, 1988, Haugane E. , Gronlie A.

Some Kendal Caving Club Discoveries in Norway, 1988, Heap D.

The Arthropod Fauna of Grnligrotta, Norway, 1988, Hippa H. , Koponen S.

Palaeokarst in Norway, 1988, Lauritzen Se.

Revised Magnetostratigraphic Age Estimate of Cave Sediments from Grnligrotta, Norway, 1988, Lovlie R. , Giljenilson H. , Lauritzen Se.

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