[en] Algeria displays various karst landscapes due to its diversity in lithology, relief, age and climate. On 16th June 1988, in the northwest of Algeria, a 60 m wide sudden collapse occurred in the Chelif Basin about 1 km north of a marginal carbonate platform. Despite this large event and visible karst dissolutions in the platform, this region has not been classified among the karst areas of Algeria yet. Our study focuses on this Messinian carbonates that form the northern piedmont of the Ouarsenis Mountain range and are covered to the north by Plio-Quaternary deposits. The geological and geomorphological data that we collected reveal that the present-day karstification is limited at the outcropping surface. Present-day carbonate dissolution is impeded by the absence of a topsoil supplying CO2 and by the presence of a calcrete improving the drainage. Although dissolution at depth is generally diffuse due to the porous and friable nature of the carbonates, two factors can, on the contrary, concentrate water infiltration: the presence of a network of more or less subvertical fractures and, occasionally, at the surface, the absence of calcrete, independently of the fracturing nodes There are few ponors and sinkholes present. The endokarst is still present as evidenced by rare caves. In epikarst, solution pipes and shelter caves are prevalent. The later results from differential weathering in relation with the carbonate facies and the progressive calcrete cementation in valleys and slopes during river incision. Near valley bottom, shelters are arranged in steps like terraces. This morphology is related to base-level lowering in relation with the deformation and uplift of the Ouarsenis piedmont. Near the southern edge of the Chelif Basin, deep (>55m) karstic voids are present and associated with paleo-valley incision presently burried by Plio-Quaternary deposits. We interpreted the large 1988 collapse in relation with this paleokarst and propose that its triggering was partly induced by a lowering of the aquifers due to a deficit of precipitation. The deep paleokarst formation and the buried river incision are attributed to the low base-level during the Messinian Salinity Crisis (5.97–5.33 Ma). We evidenced an upper karstic dissolution level filled that is attributed to a per ascendum evolution of the karstic phreatic network in relation with the following Pliocene aggradation.
Disciplines :
Earth sciences & physical geography
Author, co-author :
Moulana, Meriem L. ; Department of Geography, University of Liege, Liege, Belgium ; Faculty of Earth Sciences, Geographical and Territorial Planning, University of Science and Technology Houari Boumediene, Algiers, Algeria
Hubert, Aurelia ; Université de Liège - ULiège > Département de géographie > Géomorphologie et Géologie du Quaternaire
Guendouz, Mostefa; Faculty of Earth Sciences, Geographical and Territorial Planning, University of Science and Technology Houari Boumediene, Algiers, Algeria
Doutreloup, Sébastien ; Université de Liège - ULiège > Département de géographie > Climatologie et Topoclimatologie
Ek, Camille ; Université de Liège - ULiège > Département de géologie
Moulana, Meriem Lina ; Université de Liège - ULiège > Sphères ; Université de Liège - ULiège > Faculté des Sciences > Doct. scienc. (géographie) ; Université de Liège - ULiège > Département de géographie > Géomorphologie et Géologie du Quaternaire ; Université de Liège - ULiège > Département de géographie
Language :
English
Title :
Karstic geomorphology of carbonate Ouarsenis Piedmont (Boukadir region, Chelif) in Algeria: The role of the Messinian Salinity Crisis
The authors would like to thank Pr. Abdelhak BOUTALEB, director of the Laboratory of Metallogeny and Magmatism of Algeria (LMMA) FSTGAT – USTHB for his help and expertise especially in the field. We would also like to thank, Dr. Marthe LEFEVRE for her help, his proofreading and these suggestions and Pr. Med Said GUETTOUCHE, director of the Geomorphology and Geohazards (G&G) Laboratory, FSTGAT – USTHB for his help, and also the colleagues who accompanied us in the field: Mr. Abdeldjalil GOUMRASSA, Mr. Sofiane MEDDANE and Mr. Badreddine MOULANA. Many thanks to Pr. André OZER and Dr. Alexandre PEETERS, for their contributions in the observation and analysis of aerial photographs. We are grateful to the speleologists of the Caving Club of Algiers for having accompanied us to the collapse sinkhole of Bir Djeneb, to the managers of the quarry of Oued Sly and to the gendarmerie of Boukadir town. A special thanks to Mr. Saber ABDELAZIZ, speleologist for the photos. We warmly thank the Bejaia, Chelif and Oran speleology club.
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