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Enviroscan Ukrainian Institute of Speleology and Karstology

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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 kame is a stratified glacial sand and gravel deposit forming a small, conical hill [16].?

Checkout all 2699 terms in the KarstBase Glossary of Karst and Cave Terms

What is Karstbase?



Browse Speleogenesis Issues:

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;
See all featured articles from other geoscience journals

Cave and Karst Science, 2006, Vol 33, Issue 2, p. 55-64
The hydrogeology of crystalline rocks as supporting evidence for tectonic inception in some epigean endokarsts
This paper reviews the considerable advances made in recent years to understand the processes leading to the creation of the triple porosity hydrogeology described for karstic limestones. These have concentrated on the physics and chemistry of slow karst dissolution during the inception phase of conduit evolution in sedimentary limestones prior to 'breakthrough', and then considered the subsequent and more rapid phreatic enlargement into networks with high hydraulic conductivity. However, it is not only soluble rocks that can exhibit significant conductivities. A review of the literature of the hydrogeology of 'crystalline' (i.e. igneous and metamorphic) non-carbonate 'hard rocks' that dates from the late-1980s reveals that such rocks can also act as aquifers, especially near the surface. Their discharges supply natural springs and household wells and boreholes, flood mines, and put at risk the underground containment of hazardous wastes. Fractures are utilised within the crystalline rocks (which have negligible primary porosity, and which are assumed not to develop solutional conduits), so that flow rates can exceed the breakthrough point that, in limestones, would mark the transition from laminar to turbulent flow conditions, and fast dissolution. Similar processes should also apply to metamorphic limestones, and, indeed, to sedimentary limestones, some of which are now known to exhibit open fractures created by seismic or aseismic tectonism. In these cases, the slow chemical inception phase may be bypassed, because some karst passages may develop under phreatic conditions, at high wall-retreat rates, immediately after the inundation of epigean fractures formed tectonically. New models of speleogenetic initiation should therefore recognise both the appropriateness of the (chemical) Inception Horizon Hypothesis for the development of deep, long-range, conduits over long periods of time, as well as the importance of fast speleogenesis initiated by tect***[record truncated]***.