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53 (2014) 3 Karst Forms Are Missing Bulletin Bibliographique Spéléologique Speleological Abstracts 53 46e année / 46th year N° 53 2014 Speleological Abstracts Bulletin Bibliographique Spéléologique Commission of Bibliography of the International Union of Speleology Commission de Bibliographie de l’Union Internationale de Spéléologie Swiss Speleological Society with the participation of / avec la participation de Società Speleologica British Cave Italiana Research Association Administration Commission de bibliographie de l’Union internationale de Spéléologie Patrick DERIAZ, Chemin des Invuettes 1, CH-1614 Granges E-Mail: [email protected] Ce numéro contient les analyses des publications parues en 2014. Elles sont intégrées dans la base de données disponible depuis décembre 2020 sous wikicaves.org Tirage : 20 exemplaires réservés aux centres de documentation de l’UIS ISSN : ISSN 0253-8296 Grotte de la Crête de Vaas Un grand merci aux collaborateurs de ce numéro 53 : Alessandro Pastorelli, Anamaria Häuselmann, Bernard Chirol, Bernard Lebreton, Carlos Benedetto, Christophe Bès, Christophe Lavorel, Christophe Prévot, Patrick Deriaz, Yvonne Droms, Eric de Valicourt, Xavier Foucrier, Gerhard Stein, Gina Moseley, Gregory Middleton, Joanne Dernie, Johannes Lundberg, Liz Price, Marcel Meyssonnier, Michele Sivelli, Mickael Laumanns, Natalie T. Uomini, Nathalie Goffioul, Christa Pfarr, Philipp Hauselmann, Philippe Drouin, Pino Guidi, Thomas Rathgeber, René Carlin, Jean Taisne, Torstein Finnesand, Cécile Vuilleumier 1.1 Karstology Holland and close to Amsterdam Schiphol Karstologie Airport, a series of false limestone exposures 1.11 Karst morphology and morphogenesis have been constructed as an amenity. Slabs of Morphologie et morphogenèse kars- Upper Palaeozoic, presumably Mississippian, tique limestones are arrayed in 'beds' at the heads of AA (2014) : La 24e Rencontre d'octobre à artificial gullies radiating from the southwest Azé. Un grand cru corner of a lake. Less convincing are (rare) La Lettre du Spéléo-club de Paris, n°329 (no- vertical beds, drill holes and the flow of water vembre) : 1. from the lake into the gullies, not vice versa. Près de 80 participants se sont retrouvés à Azé A bridge, similar in appearance to a natural (Saône-et-Loire) pour ces Rencontres, avec bridge, spans a gully and has partly collapsed. des présentations de D. Cailhol, B. Lismonde, (Author, GM). J.-Y. Bigot, S. Jaillet, P. Bancel, L. Barriquand, 2014.0003 entre autres. (JT). 2014.0001 KNAPPE, Hartmut (2014) : Zur Entwicklung der Karststrukturen im Riffkalkstein von Iberg DE SWART, Herman (2014) : Over grotten en und Winterberg bei Bad Grund (Westharz). grotvorming (3/4): karstverschijnselen aan de Mitt. Verb. dt. Höhlen- u. Karstforsch., 60 opervlakte (3+4) : 80-90. Spelerpes, n° 2 : 46-51. In Dutch, photos. On the development of karst structures in the Article sur la formation des grottes, plus préci- western Harz/Germany. (ML). sément les phénomènes karstiques de surface. 2014.0004 L'article donne un aperçu de ces phénomènes: lapiaz, sources, diaclases, limestone, dolines, RINGSET, Narve (2014) : Strandsone-karren poljes, les différents types de roches.. (NG). på Voksa, Sande, Sunnmøre 2014.0002 Norsk Grotteblad, no 63 (Desember 2014) : 18. Photos. DONOVAN, Stephen K (2014) : An unnatural At the island Voksa at Sunnmøre, a locality bridge within an artificial limestone environ- with littoral karren is found at a marble stripe ment in the Netherlands just above the littoral zone. The Kamenitzas or Cave and Karst Science, Vol. 41, no 3 (De- bowl karren are circular to elliptical bowls, ca. cember 2014) : 118-119. 10 cm deep with detailed solution forms. Or- The surface geology of the Netherlands is ganic mud is probably an important source of mainly Quaternary; it lacks surface rock acid, karstforming environment at this seawa- exposures except in the south and east. In the ter influenced shoreline. Where wave action is Haarlemmermeersebos, a public park in Noord more dominant, the bowls are eroded and the Speleological Abstracts / Bulletin Bibliographique Spéléologique N° 53 (2014) 3 karst forms are missing. (Author, TF). By placing water depth and temperature re- 2014.0005 corders at Main Rising and Whirlpool Rising in Speedwell Cavern, Nigel Ball is starting 1.12 Hydrology to produce a picture of the strange repeated Hydrologie pulsing of the water flow in this cave system. (Author, GM). AMAEL, Poulain; ROCHEZ, Gaëtan; HAL- 2014.0009 LET, Vincent; DEWAIDE, L. (2013) : La Lesse souterraine à Furfooz : résultats des BANCILLON, Jean (2014) : Hydrogéologie. premières études hydrogéologiques Spéléo Magazine, n° 87 (Septembre 2014) : 9. Plaquette – programme des Journées 2013 de Brève note hydrogéologique et des traçages Spéléologie Scientifique, 16 et 17 novembre sur la source de Burle dans le contexte des 2013 : 20. gorges du Tarn (Sainte-Enimie, Lozère). (Fx). Résumé de poster. Présentation des premiers 2014.0010 essais de traçage réalisés sur la Lesse souter- raine dans la région de Furfooz. (NG). CALANDRI, Gilberto (2014) : La sorgente di 2014.0006 Renara (Massa) caratteri chimico-fisici Bollettino del Gruppo Speleologico Imperiese AMAËL, Poulain; ROCHEZ, Gaëtan; HAL- CAI, n° 65, anno XLIII (gennaio dicembre LET, Vincent (2014) : Projet KARAG (Karst 2013) : 15-17. 1 cartina, 1 ril., 3 foto, 4 dis. Aquifer Research by Geophysics) : résultats La sorgente di Renara, valle del Frigido (Alpi des premiers essais de traçage dans le karst de Apuane, MS) drena le acque del M. Altissimo, la Wamme-Lomme M. Pelato e M. Macina, vengono descritti i pa- Plaquette – programme des Journées 2014 de rametri chimico-fisici; bibliografia essenziale. Spéléologie Scientifique, 15 et 16 novembre (Author, AP). 2014 : 1 p. 2014.0011 Résumé de communication. Le projet Karag, lancé en 2013, a pour but d'améliorer notre D'ANTONI-NOBECOURT, Jean-Claude; connaissance des aquifères karstiques via une AUDRA, Philippe (2014) : Un -1000 dans les approche multidisciplinaire alliant la géophy- Alpes-de-Haute-Provence ? sique et l'hydrogéologie. (NG). Spelunca, n° 133, mars 2014 : 25-31. 11 pho- 2014.0007 tos, 2 figures. Après la présentation du massif qui abrite la BACKAERT, D.; ROCHEZ, Gaëtan; HAL- grotte des Chamois (12km) et un bref histo- LET, Vincent (2013) : Rôle de la formation de rique, les auteurs relatent l'organisation d'un Nismes sur l'hydrologie karstique de la vallée traçage souterrain destiné à connaître les de Lesve origines des eaux de la source du Coulomp. Ce Plaquette – programme des Journées 2013 de traçage a eu lieu en altitude dans la dépression Spéléologie Scientifique, 16 et 17 novembre du Lignin. La fluorescéine est bien ressortie 2013 : 18. quelques jours après à la source du Coulomp Résumé de communication. L'étude montre mettant en évidence une percée hydrogéolo- que dans le vallon de Lesve, la formation de gique de plus de 6 km de long et 1000m de Nismes joue son rôle de barrière hydrogéolo- dénivelé. (CB). gique séparant ainsi les deux systèmes kars- 2014.0012 tiques. (NG). 2014.0008 FRANCFORT, Stanislas (2014) : De l'utilité d'un conductimètre en campagne d'exploration BALL, Nigel (2014) : The Flooding Characte- Spelunca, n° 133, mars 2014 : 12-18. 19 pho- ristics of Speedwell Cavern tos, 3 figures, 4 tableaux. Speleology, No 19 : 38-39. L'auteur montre comment exploiter des me- 4 Speleological Abstracts / Bulletin Bibliographique Spéléologique N° 53 (2014) sures de conductivité peuvent apporter de an aquifer. NCGRT researchers have installed nombreux enseignements en exploration the world's largest collection of drip-water souterraine. Ces essais ont eu lieu en Crête lors measuring devices in Wellington Caves. They de la campagne d'exploration “Karydi 2013”. will also use stalagmites to estimate when Ils ont permis la découverte de nouveaux af- groundwater recharge has occurred. (GJM). fluents, confirmé des hypothèses de connexion 2014.0016 entre cavités et vers des résurgences connues et de révéler une source hydrothermale. (CB). POULAIN, Amael; ROCHEZ, Gaëtan; HAL- 2014.0013 LET, Vincent (2013) : Présentation du projet KARAG (Karst Aquifer Research by Geophy- GREIG, Iain (2014) : Smoo Cave Dye Testing sic). Approche géophysique : perspectives et Grampian Speleological Group Bulletin 5th objectifs de l'étude de l'épikarst de la grotte de Series, Vol. 1, no 2 : 17-18. 2 ill. Lorette et de la Lomme à Rochefort Determining the sinkpoints for water issues Plaquette – programme des Journées 2013 de within Smoo Cave. Dye traces were detected Spéléologie Scientifique, 16 et 17 novembre in both the static sump in the inner passage, 2013 : 13-14. and from a small stream flowing out of a Résumé de communication. Ce projet, étalé stalagmite slope in the main chamber. (Author, sur 4 ans, tentera d'améliorer la connaissance GM). du stockage et des transferts des eaux dans 2014.0014 les systèmes épikarstiques et karstiques de la région de Rochefort. (NG). JUNGELS, Cécile (2014) : Visite aux grottes 2014.0017 de Rosée et Lyell Les Chercheurs de la Wallonie, n° 218 : 5-13. POWELL, Connor; VERMETTE, Stephen Photos. (2014) : The Powell and Vermette Equation: Compte rendu d'un prélèvement d'échantil- Calculating American Cave Temperatures lons d'eau dans les grottes de Rosée et Lyell, NSS News, Vol. 72, no 3 (March 2014) : 18- par AQUALE en février 2014, afin de vérifier 19. 2 graphs. l'apport en sulfate dans le sol et les eaux sou- The authors independently developed a new terraines. (NG). equation for approximating cave temperatures 2014.0015 in vadose zones, which seems to give more accurate results
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