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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 uplift is 1. the hydrostatic force of water exerted on or underneath a structure tending to cause a displacement of the structure. 2. the relative upward movement of a part of the earth's crust [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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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 karstic geosystem (Keyword) returned 3 results for the whole karstbase:
Karst 99, 1999,
The volume contains 36 papers presented to the European Conference "From Karst Landscape to Karstic Geosystems. Karst Dynamics, Structures and Indicators"

Les dolines deffondrement et les dolines-lacs des Causses du sud-ouest du Moyen-Atlas (Maroc) : des dpressions lies un contexte hydro-morphologique particulier (p. 19-24), 2001, Elkhalki Yahia, Akdim Brahim
The karstic geosystems of the Causses in the Middle Atlas present a number of old and present karstic landforms. The interference between karstic geomorphology and the process of deep karstification find expression in an important development of sinkholes and collapse zones. Inventory and spatial distribution of these superficial karstic landforms show a very close relationship with the apparition of saline springs. Water chemistry and the exported rock tonnage are analysed and point out the importance of caverning, which takes place in gypsum and salt Triassic formations.

Turbidit, indicateur du fonctionnement perturb du gosystme karstique de lAtlas de Beni Mellal (Moyen Atlas mridional, Maroc), 2002, Elkhalki Yahia, Hafid Abdellatif
Turbidity, as an indicator of perturbed functioning of karst geosystem of Beni Mellal Atlas (Southern Middle Atlas, Morocco) - The turbidity of karst springs is a general phenomenon of anthropized Mediterranean limestone mountains. But actually we note that it has been somewhat neglected by karstologists. In other respects, it represents a pertinent indicator of the dysfunctioning of karst geosystems which have undergone a strong impact of human action. Cloudy waters distinguish Asserdoune spring, as the main outlet of Liassic aquifer. After dry periods, followed by brutal storms, water turbidity can exceed 2000 JTU (Jackson Turbidity Unit). Three factors are united to favour the turbidity water: 1) The climate: autumn rain storms which follow a long dry season, fall on soils that are dry and badly protected by vegetation. They cause an important mobilisation of fine particles, which infiltrate the epikarst.2) Inner karst structure: the advance of cloudy water toward An Asserdoune spring is made easier by developed drains. Dye tracings have shown that the time of transit waters is comprised between 24 and 72 hours.3) Human impact: the agriculture modernisation of Tadla plain (140 000 ha irrigated) was accompanied with a violent action on forest resources of Beni Mellal Atlas. Clearings induced a large stripping of soils, which caused the excavation of covered karrens. Furthermore, the dysfunctioning of the karst geosystem of Beni Mellal Atlas is translated by the hindrance of present travertinisation at the downstream of springs.

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