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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 irrotation flow is potential flow or flow with no rotational component [16].?

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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 haute-savoie (Keyword) returned 11 results for the whole karstbase:
A preliminary note on the spatial distribution of Meta menardi, Triphosa dubitata, Triphosa sabaudiata, Nelima aurantiaca and Culex pipiens within a cave ecosystem (Grotte de la Scierie: Haute-Savoie)., 1976, Bourne John D.
Following 8 months of observations in a richly populated cave, (Grotte de la Scierie, HauteSavoie, France), it has been possible to outline the movements and distribution of Meta menardi (Araneae), Nelima aurantiaca (Opiliones), Triphosa dubitata and Triphosa sabaudiata (Lepidoptera) and Culex pipiens (Diptera) within the cave ecosystem. Although no general rule can be postulated it appears that the morphology of the cave walls and the climatic conditions regulate the distribution of these 5 species within the cave ecosystem. The interactions between the 5 species have been investigated.

Le rseau de la Diau, 1983, Lismonde, B.
The DIAU SYSTEM - Diau Cave is the resurgence of an important underground drainage system in the massif des Bornes in Haute-Savoie (France). The system's catchment is approximately 9km2, between an altitude of 1200m and 1800m. The average discharge is about 4001/s. Speleological explorations have discovered two sections of the master drainage cave (Diau and Pertuis caves). Two tributaries have also been explored. The total length of the Diau cave system is 14.9km with a height difference of 702m. The master cave occurs in the bottom of the Pertuis syncline at the boundary between the urgonian limestone and hauterivian marls. According to the gradient and the fractures, four types of gallery structure occur, of which two are vadose. The two known tributaries (inlet of the Grenoblois and Tanne des Mtores) follow a NW-SE anticlockwise shear fault, which exists in the Parmelan plateau fracture zone.

Hydrologie du lac de Lessy (Haute--Savoie), 1983, Sesiano J. , Muller A.
SOME HYDROGEOLOGICAL OBSERVA-TIONS IN LAC DE LESSY (Haute-Savoie, France) - Located in the French Prealps near Annecy, lake Lessy is a 70,000m3 body of water, at an altitude of 1800m. a.s.l., in a karstic area. It has no visible outlet. A dye tracing was made during september, 1981, in order to identify which spring in the valley is fed by the lake. The experiment was successful: a strait distance of 3.5 km was covered underground in about 15 hours. It also appeared that the major part of the water flowing from this spring does not come from the lake, but from the surrounding plateaus

Un exemple de karst haut-alpin : le Dsert de Plat (Haute-Savoie), 1984, Maire, R.
AN EXAMPLE OF HIGH ALPINE KARST: THE DSERT DE PLAT (HAUTE-SAVOIE) - Situated in the French Northern Alps between 1600m and 2800m elevation, the Dsert de Plat is characterised by a wet, cold and very snowy climate (P = 2400-2800 mm/year). We observe several morphoclimatic levels: the upper mountain karst (1500-1700m), the subalpine karst (1700-1950m), the alpine karst (1950 - 2600m) and the proglacial karst (well developed in the Haut-Giffre massif. Glacio-karstic landforms like cirque-dolines and pavements (Schichttreppenkarst) are inherited from the quaternary glaciations. The deep karst underlines the part of quaternary climatic sequence with complex drainage and fillings. Now, the karstic flow is a nival type (maximum during the spring and summer minimum) but the hydrochemical cycles are opposite (spring minimum). Nevertheless, because of a very abundant underground discharge during hot season (80%), the exported limestone reaches 75% of annual amount. The specific dissolution is strong (104 mm/ky), but it does not reach the optimum of forest mountain karst, like Vercors (120-170mm/ky).

Le massif du Parmelan, Haute-Savoie, relations fractura-tion-karstification, 1985, Masson, M.
THE MASSIF OF PARMELAN, HAUTE-SAVOIE, FRANCE: RELATIONS BETWEEN FRACTURATION AND KARSTIFICATION - The massif of Parmelan (Haute-Savoie), encloses a well-karstified and highly organised perched aquifer. Its simple geological structure and easy-speleological penetration (more than 45km are known) have allowed a statistical study of the fracturation and karstification parameters at different scales. This study shows that the karst has developed on the most frequent fracturation directions (study of the cumulated lengths), whereas its directional distribution in frequency is relatively homogeneous; the most used fractures are the tension faults, linked with the folding of the massif.

Hydrogologie de la rgion entre Araches et Flaine (Haute-Savoie), 1985, Sesiano, J.
NEW HYDROGEOLOGICAL INVESTIGATIoNS IN THE Massif de Plat BETWEEN ARACHES AND Flaine (HAUTE-SAVOIE, FRANCE) - During 1983 and 1984 several dye-tracing experiments have been performed in the French Prealps (Haute-Savoie). The studied area covered about 30 km2, with altitudes ranging between 500m and 2500m. An underground drainage model has been set up, taking into account the fact that there is a common water outlet. The model is based upon the regional tectonic setting, the drainage pattern following thrust and fault planes

L'accident de Tchernobyl : une retombe positive en hydrogologie, 1986, Sesiano J. , Bueche M.
THE TCHERNOBYL ACCIDENT: A POSITIVE HYDROGEOLOGICAL ASPECT - As a continuation of dye-tracing studies of underground waters in Haute-Savoie, France, over the last few years, we have used the radioactive elements released by the Chernobyl nuclear accident as artificial tracers. The event happened simultaneously with the onset of the spring high waters. The response of the system was thus delayed by more than two weeks, the time for the water to percolate and for the aquifer to recharge. On the third week, a very faint signal was detected by gammametry and by liquid scintillation counters at the two surveyed springs.

Les importantes mergences de Magland, dans la valle de l'Arve (Haute-Savoie) : physico-chimie et origine des eaux, 1989, Sesiano, J.
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.

Qualit physico chimique et bactriologique des sources du domaine de Plat (Haute-Savoie), 1990, Buissonvodinh, J.
PHYSICO CHEMISTRY AND BACTERIOLOGY OF THE DOMAIN OF PLATE SPRINGS (HAUTE SAVOIE, FRANCE) - On the high alpine karst of Plat (Haute-Savoie), eight springs on four catchments have been submitted to physico-chemical and bacteriological analysis. The skiing resort of Flaine is situated on one of the catchments, the others are not very frequented (mountain pasture, cattle). These springs have a good physico-chemical quality but only one is drinkable. Pathological germs contained in human and animal excrements contaminate the others. This phenomenon is amplified by the ground and earth leaching due to rainstorms. On the other hand, the skiing resort of Flaine could be responsible of a chronic pollution of the Salles spring. All traditional frequentation of this area makes the water unusable and undrinkable, and all additional development on the karst could only aggravate this situation and compromise the use of water.

Le gouffre Jean-Bernard (1602 m, Haute-Savoie), coulements souterrains et formation du rseau, 1993, Lips B. , Gresse A. , Delamette M. , Maire R.
With its depth of 1602m and development of more than 20 km, the Jean-Bernard system provides a clear view of an alpine karst system with a steep gradient and reduced watershed (4 km2). Over the last 30 years, hundreds of explorations led by the caving club Vulcain (Lyon) have resulted in a thorough knowledge of the cave. The system develops in a syncline formed from urgonian limestone (Lower Cretaceous). Two parts may be distinguished: a complex upper part with numerous dry phreatic tubes, and a lower part, which is restricted to a high meander. A tracing carried out in 1992 has allowed us to locate the outlet in the riverbed of the Clvieux creek (alt. 780m). The former spring of the upper part must have been situated on the level of the lower entrance (about 1800m) and could date back to the end of the Tertiary when the valley was less deep. The quaternary period is responsible of the entrenching of the old galleries, for the destruction of speleothems and the genesis of the lower underground delta, between -1400m and -1600m.

Nouvelles observations sur lhydrogologie du vallon du Cruet, Haute-Savoie (France), 1998, Sesiano, Jean
Following a recent dye-tracing experiment the hydrogeological model for the Cruet valley, in the northern French Prealps has had to be modified. Faults, parallel and transverse to the valley, allow a mixing of waters from different origins. There is thus possible contamina_tion of several Cruet valley springs used for human consumption by surface pollutions.

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