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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 development is the act of repairing damage to the formation caused by drilling procedures and increasing the porosity and permeability of the materials surrounding the intake portion of the well [6].?

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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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 sainte-baume (Keyword) returned 3 results for the whole karstbase:
Le karst de la Sainte-Baume (Bouches-du-Rhne et Var). Structure et volution : l'approche hydrogologique, 1986, Coulier, C.
THE SAINTE BAUME KARST (Bouches du Rhne 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).

Unusual flooding in the Calernakm shaft (Alpes-maritimes, France) Origin and consequences of the phenomen on the deep drainage organisation, 1998, Audra Ph.
The Calernakm shaft is located in the Southern french Alps, near Nice It contains large galleries reaching -478 m deep During unusual high waters, the lower part floods over 100 m height The flooding is linked to a semi-dammed karst structure The galleries organisation proves that the karstification privileges subhorizontal conduits in the epiphreatic zone, without favouring any deep phreatic passages The origin of deep phreatic karsts is discussed

Quelle est la dimension du massif karstique de la Sainte-Baume ? Elments pour une thorie spatiale et fractale du karst, 2000, Martin, Philippe
The dimension of the surface of Sainte Baume and its neighbourhood is close to 2,2. This value has been obtained the study of 5 contour lines (from 400 to 800 m) and 5 topographic profiles (3 N - S and 2 E - W). 3 methods were used for contour lines: box counting (DB); the information dimension (Di) and surface - perimeter relation (D(P)). Three methods have been used for topo_graphic profiles: the power spectrum (DSPEC); statistics R/S (DR/S) and vario_gramme (DVAR). Average results are: (DB) = 1.20; Di = 1.23; (D(P)) = 1.32; DSPEC = 1.17; DR/S = 1.24; DVAR = 1.23. Thus, the surface of Sainte Baume and its neighbourhood is fractal. It means, theoretically, that Sainte Baume can be characterised by an infi_nite surface in a bounded volume. This first approach focuses on karst surface approach, cave systems approach will be presented in a following paper (in this review). This result raises numerous geomorpho_logic questions. How to calculate a specific erosion? How to think forms in a theoretical frame, which could develo_ped out of the Euclidean geometry conventions? How to think an essential_ly irregular morphology? Elements of answer are brought on a theoretical plan. They constitute the first elements of a karst geometrical theory. Calculation of the specific erosion points out the problem of the size of the surface used. Due to fractal theories, this size is relative to the observation scale used. To be significant, specific erosion calcula_tion needs the use of an efficient scale, in regard of the erosion processes studied. Furthermore, specific erosion expresses only a balance of mass, not a morphoge_nesis. It corresponds to a chronological approach of the karst. Two dynamics can be distinguished in surface morphogenesis. In one hand, increase of the mean slopes is named spatial differentiation, in another hand, decrease of this value is classically called: aplanation or levelling. These 2 dynamics imply the wearing away of spatially various materials. It takes place essentially around thalwegs during the differentiation stage, around the crest during levelling. Thus morphology, space are important factors of the dynamics in the work. Space is not only a support, but an actor in morphogenesis.

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