Titlebook: H2Karst Research in Limestone Hydrogeology; Jacques Mudry,Fran?ois Zwahlen,James W. LaMoreaux Book 2014 The Editor(s) (if applicable) and

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https://doi.org/10.1007/978-1-349-11888-5ntecedent geological conditions, from local geomorphology and climate, and from the patterns of solutional conduits (including accessible caves) and their relationships with any matrix or fracture flow. Much is being learned from study of calcite and other precipitates in such caves. Where not direc

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J. H. Reedman B.Sc., M.Phil., M.I.M.M.he hydraulic properties and specific regime of groundwater in karst are, in many cases, the source of catastrophic failures. The most common destructive influence of groundwater is the consequence of: massive turbulent flows; the fast erosion of unconsolidated deposits in caverns and joints; the gre

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Jun Hee Lee,Kook Nam Han,Hyun Koo KimGPR) and electrical resistivity imaging or tomography (RESTOM). A case study near Cherea area (NE Algeria) demonstrates the applicability of these methods. Nine GPR profiles and two-dimensional RESTOM have been applied, with relative success, to locate paleo-collapses and cavities, and to detect and

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