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Featured articles from Cave & Karst Science Journals
Characterization of minothems at Libiola (NW Italy): morphological, mineralogical, and geochemical study, Carbone Cristina; Dinelli Enrico; De Waele Jo
Chemistry and Karst, White, William B.
The karst paradigm: changes, trends and perspectives, Klimchouk, Alexander
Long-term erosion rate measurements in gypsum caves of Sorbas (SE Spain) by the Micro-Erosion Meter method, Sanna, Laura; De Waele, Jo; Calaforra, José Maria; Forti, Paolo
The use of damaged speleothems and in situ fault displacement monitoring to characterise active tectonic structures: an example from Zapadni Cave, Czech Republic , Briestensky, Milos; Stemberk, Josef; Rowberry, Matt D.;
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;
Karstologia, 1994, Issue 23, p. 9-18
Nouveaux traçages sur le massif de la Pierre Saint-Martin (Pyrénées-Atlantiques)
Douat M. , Salomon J. N.
Abstract:
In 1982 and 1992 cavers observed the contamination of the B3 and Couey-Lotge underground rivers emerging at the Issaux springs This contamination was thought to be caused by the PSM water purificatlon station which discharges effluents into a fracture. The ARSIP and the LGPA laboratories were asked by the DDA (Pyrenees-Atlantiques administration) to carry out an hydrogeological study to prove the origin of this contamination and determine the limit of the Issaux catchment in the Guillers area in order to find a new site for a modern water purification station. Three uranine tracings were made (Water purification station - B3 underground river - BG. 106 shaft). The first two tracings emerged at the Issaux springs and the third tracing came out at the Bentia spring (Sainte-Engrace). These tracings confirm the hypothesis on the surficial basin limits between Issaux and Saint Vincent.
In 1982 and 1992 cavers observed the contamination of the B3 and Couey-Lotge underground rivers emerging at the Issaux springs This contamination was thought to be caused by the PSM water purificatlon station which discharges effluents into a fracture. The ARSIP and the LGPA laboratories were asked by the DDA (Pyrenees-Atlantiques administration) to carry out an hydrogeological study to prove the origin of this contamination and determine the limit of the Issaux catchment in the Guillers area in order to find a new site for a modern water purification station. Three uranine tracings were made (Water purification station - B3 underground river - BG. 106 shaft). The first two tracings emerged at the Issaux springs and the third tracing came out at the Bentia spring (Sainte-Engrace). These tracings confirm the hypothesis on the surficial basin limits between Issaux and Saint Vincent.