By J.W. LaMoreaux (auth.), Bartolomé Andreo, Francisco Carrasco, Juan José Durán, James W. LaMoreaux (eds.)
IV foreign Symposium on Karst Media, Malaga, Spain 2010 The Malaga Symposia sequence offers a global discussion board for clinical debate at the development made in study into karst environments. The 2010 assembly of the 4th foreign ISKA provides eighty papers in 4 key issues: karst hydrogeology and investigations, karst landscapes and ecosystems, human interplay with karst environments, relatively in caves, and engineering geology in karst parts. This publication might be an invaluable version to the libraries of specialists, scientists, academics, and coverage makers interested by the unique problems with karst terrains.
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Hydrological Processes, 12(10–11): 1659–1669 Sharp M, Gemmell JC, Tison JL (1989) Structure and stability of the former subglacial drainage system of the Glacier de Tsanfleuron, Switzerland. Earth Surface Processes and Landforms, 14(2): 119–134 Steck A, Epard JL, Escher A, Gouffon Y, Masson H (2001) Carte tectonique des Alpes de Suisse occidentale et des régions avoisinantes 1:100000. html Viviroli D, Weingartner R (2004) The hydrological significance of mountains: from regional to global scale.
Direction of view is northwest (upstream) Fig. 4 Upstream view of the vault and screen constructed above the entrance to Antioch Cave. Length of intake screen is 10 m Recharge Enhancement and Protection of a Karst Aquifer in Central Texas 41 4 Results of Flow Events at Antioch Cave Following completion of the second phase of the project, an ongoing drought prevented testing of the system. In September and October 2009, adequate rains occurred that led to two flow events at Antioch Cave. Both events were small compared to other events in the past, but there was sufficient flow from each event that the automated valve was triggered and water-quality data were recorded by the monitoring instruments (Fig.
Digital Elevation Model (DEM). T – Tectonics (T D 1–5 points) Two subfactors are being considered: density of faults T1 and dip of strata T2 . Geological maps, tectonics maps, aerial and satellite images. 8 points) L map is obtained based on the following lithological data: the type of carbonate rock (subfactor a), bedding (subfactor b) and mineralpetrographic impurities (subfactor c). Geological maps, lithological maps, borehole data, etc. O – Overlying layers (O D 1–5 points) Type and thickness of geological cover and soil.