Karsts des craies et calcarénites de la Montagne Saint-Pierre (Basse Meuse liégeoise)Willems, Luc ; ; Ek, Camille et alin Bulletin des Chercheurs de la Wallonie (2007), XLVI The “Montagne Saint-Pierre” (Sint Pietersberg) is a separate part of the Hesbaye plateau, isolated between the lower valleys of the Geer and the Meuse rivers. It is exploited by a big open-air quarry and ... [more ▼] The “Montagne Saint-Pierre” (Sint Pietersberg) is a separate part of the Hesbaye plateau, isolated between the lower valleys of the Geer and the Meuse rivers. It is exploited by a big open-air quarry and by numerous underground quarries developing galleries on hundreds of kilometers long. Excavated in Cretaceous chalk and calcarenite, these artificial networks allow an exceptional 3-D observation of karsts inside a very porous and permeable rock, less favourable to a concentrated solution. The most numerous of them are “organ pipes” or “earth pipes”. They are vertical tubular solution pipes that may exceed 60 m in depth. Sponge networks and subhorizontal caves occur, without any visible connection with fracturation. Finally, downwards to at least 20 m below the alluvial plain of the Meuse river, pluridecametric nodes of weathered chalk are found. By their size and rounded morphology, the nodes resemble to the natural caves occurring in the calcarenite and intersected by the underground quarries. All the studied karsts allow us to propose a scenario for the genesis of a polyphase karst system. Independently of surface conditions, caves are generated deeply in the phreatic zone (endokarsts). During the downcutting of theMeuse valley, and related to the fluvial terraces, solution pipes (input karsts) are generated. Due to the valley incision and to the lowering of the aquifer,theses solution pipes progress downward and cut the endokarsts. A concentrated water circulation takes place. In the dewatered upper part of the system, caves cut by solution pipes are rapidly filled by superficial deposits. The high porosity of the calcarenite makes it comparable to a sponge. The rock absorbs quickly the out-flows coming from the surface and causes a rapid deposit of the fine particles transported inside horizontal passages. The sealing of these conduits allows their conservation inside a very crumbly rock. [less ▲] Detailed reference viewed: 37 (10 ULg)![]() Contribution à l'étude de la flore et de l'écologie des plantes de quelques grottes wallonnes.Garbacki, Nancy ![]() in Bulletin des Chercheurs de la Wallonie (1997), XXXVI Detailed reference viewed: 9 (1 ULg) Démographie d'un peuplement de coléoptères troglobies pyrénéens (Genre Speonomus) dans une grotte belge et aspects de leur biologieBrouwir, Christine ![]() in Bulletin des Chercheurs de la Wallonie (1988), 28 Etude (dans le cadre d'un mémoire en Sciences Zoologiques) d'une transplantation de coléoptères cavernicoles pyrénéens dans une grotte de la région liégeoise (grotte de Ramioul) Detailed reference viewed: 39 (17 ULg) |
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