2008
DOI: 10.1007/s10064-008-0169-7
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Geostructural survey and stability analysis of the calcareous cliff of Vieste (Gargano-Southern Italy)

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Cited by 3 publications
(2 citation statements)
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“…At the present-time, the lagoon is mostly fed by (a) 22 small streams with a drainage area of around 530 km 2 , (b) 6 main karstic springs situated in the NW sector of the carbonate Gargano Promontory, (c) direct precipitation, and (d) sea water inflow through the Acquarotta and Schiapparo canals. The maximum seasonal discharge of the springs has been estimated at 1130 l/s (Cotecchia and Magri, 1966). Mean annual precipitation is around 650 mm and the estimated summer evaporation in the lagoon is roughly equal to this value.…”
Section: Hydrology Of the Lesina Lagoon And Anthropogenic Changesmentioning
confidence: 98%
“…At the present-time, the lagoon is mostly fed by (a) 22 small streams with a drainage area of around 530 km 2 , (b) 6 main karstic springs situated in the NW sector of the carbonate Gargano Promontory, (c) direct precipitation, and (d) sea water inflow through the Acquarotta and Schiapparo canals. The maximum seasonal discharge of the springs has been estimated at 1130 l/s (Cotecchia and Magri, 1966). Mean annual precipitation is around 650 mm and the estimated summer evaporation in the lagoon is roughly equal to this value.…”
Section: Hydrology Of the Lesina Lagoon And Anthropogenic Changesmentioning
confidence: 98%
“…Furthermore, in the northern part of Tavoliere delle Puglie, in correspondence with the Candelaro fault (Figure 2), saltwater reaches even farther inland, since this tectonic structure enhances the water flow rather than acting as a hydraulic barrier. Many authors [47][48][49][50] report high watertemperature and salinity values linked to the mixing of deep water and freshwater.…”
Section: Study Area: the Gulf Of Manfredoniamentioning
confidence: 99%