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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 sandstone caves is most natural sandstone caves are surface river-cut notches at the foot of rock cliffs, or left part way up the cliff due to later downcutting. this origin accounts for most of the caves once inhabited by the pueblo indians in the sandstone cliffs of the western usa. true caves do occur in sandstone and some of these appear to be at least partially of dissolutional origin. their existence probably reflects matrix leaching by ground water moving through zones of especially high primary porosity and permeability. though sandstones with a calcite matrix cement are more prone to such development, even siliceous cement, which has a very low solubility in water, may be removed during a sufficiently long time span. the sandstone caves of the sarisarinama plateau, venezuela may be a special case of this type of development. these include shafts 300m in diameter and 200m deep, and passages up to 500m long. they were probably cut in the quartz sandstone by underground streams, after early leaching of the cement by hydrothermal solutions, and the shafts have been modified by later collapse [9].?

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.
See all featured articles
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 cave formation (Keyword) returned 67 results for the whole karstbase:
Showing 1 to 15 of 67
Calcite Bubbles - A New Cave Formation?, 1950, Warwick. Gordon T.

Artesian Flow and Cave Formation [Somerset], 1954, Glennie E. A.

Joints, Shale Bands and Cave Formation: A Special Case [Somerset], 1954, Stanton W. I.

C14 Dating of Cave Formations, 1959, Broecker W. S. , Olson E. Z.

Bat Erosion as a Factor in Cave Formation, 1960, Hooper J. H. D.

Bat Erosion as a Factor in Cave Formation, 1960, Kingwebster W. A. , Kenny J. S.

A Stream Piracy Theory of Cave Formation, 1961, Woodward, Herbert P.

The Development of Cocklebiddy Cave Eucla Basin, Western Australia, 1965, Lowry, D. C.

At present, the best account of cave formation in the Eucla Basin is that of Jennings (1961). However, the paper does not contain detailed information or maps of Cocklebiddy Cave, and this account should help to fill that need. The cave is the westernmost deep cave in the Eucla Basin (see area map in Anderson, 1964). It has received little attention from cave exploration parties from the Eastern States of Australia.


Electric-Analog Study of Cave Formation, 1966, Bedinger, M. S.

Damawewe Cave, Alotau, Papua New Guinea, 1981, Pain C. F. , Ollier C. D.

Damawewe Cave is a cave formed in Quaternary limestone near Alotau, Papua New Guinea. It consists of three sets of passages: the uppermost (and oldest) are the largest and the lowermost (active) are the smallest. Although the cave is mainly vadose, there is evidence of enlargement by corrosion and by collapse (in the uppermost level), and the sequence of cave formation has been interrupted by at least one phase of cave fill by clay and gravels.


Karst Development and Cave Formation in the Bocock Peak Area, British Columbia, Canada, 1985, Lowe D. J.

Glaciation and saline-freshwater mixing as a possible cause of cave formation in the eastern Midcontinent region of the United States; a conceptual model, 1990, Panno Samuel V. , Bourcier William L. ,

Recherches nouvelles sur les karsts des gypses et des vapo-rites associes (premire partie : processus et cavernement), 1992, Nicod, J.
NEW RESEARCH ON GYPSUM KARST AND ASSOCIATED EVAPORITES. FIRST PART: PROCESSES AND CAVE DEVELOPMENT - Drawing on the results of a great number of studies, this paper aims to stress the various processes and their interactions in gypsum karst and associated evaporites. They include the effect of diapirism, dissolution and chain reactions, cave collapse and external geomorphic processes. In the case of cave formation, the paper underlines the role of interstratal aquifers

GEOLOGICAL NOTE - CAVE FORMATION BY EXHUMATION OF PALEOZOIC PALEOKARST DEPOSITS AT JENOLAN CAVES, NEW-SOUTH-WALES, 1993, Osborne R. A. L. ,

Rapid flank margin cave formation in the fresh-water lens: An example from Isla de Mona, Puerto Rico., 1997, Mylroie J. E. , Lundberg J. , Carew J. L.

Results 1 to 15 of 67
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