2017
DOI: 10.5038/1827-806x.46.2.2107
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Evaporite karst in Italy: a review

Abstract: Abstract:Although outcropping rarely in Italy, evaporite (gypsum and anhydrite) karst has been described in detail since the early 20 th century. Gypsum caves are now known from almost all Italian regions, but are mainly localised along the northern border of the Apennine chain (Emilia Romagna and Marche), Calabria, and Sicily, where the major outcrops occur. Recently, important caves have also been discovered in the underground gypsum mines in Piedmont. During the late 80s and 90s several multidisciplinary st… Show more

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Cited by 49 publications
(46 citation statements)
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References 70 publications
(69 reference statements)
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“…The recharge of these systems is both autogenic (direct infiltration into the gypsum rocks through numerous dolines) and allogenic, through sinking rivers flowing from adjacent low permeability terrains. Geochemical analysis of infiltrating and spring waters, together with multiparametric monitoring of some of the most important springs has allowed characterization of these aquifers from a hydrogeological point of view (Bergianti et al, 2013;Tedeschi et al, 2015;D'Angeli et al, 2017).…”
Section: General Hydrogeologymentioning
confidence: 99%
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“…The recharge of these systems is both autogenic (direct infiltration into the gypsum rocks through numerous dolines) and allogenic, through sinking rivers flowing from adjacent low permeability terrains. Geochemical analysis of infiltrating and spring waters, together with multiparametric monitoring of some of the most important springs has allowed characterization of these aquifers from a hydrogeological point of view (Bergianti et al, 2013;Tedeschi et al, 2015;D'Angeli et al, 2017).…”
Section: General Hydrogeologymentioning
confidence: 99%
“…Gypsum crops out in almost all Italian regions, but the most significant evaporite karst areas are located in Piedmont, Emilia-Romagna, Marche, Tuscany, Calabria, and Sicily (Madonia & Forti, 2003;De Waele et al, 2017). Gypsum caves are often of the throughflow type, with a blind valley (sinking stream) and a downstream spring.…”
Section: Introductionmentioning
confidence: 99%
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“…3E). The above-cited events are probably the best known in NE Italy related to evaporite subsidence phenomena (De Waele et al, 2017), but the surroundings of Quinis and Enemonzo villages are heavily affected by evaporite dissolution processes. Gortani (1965) reported the occurrence of three significant collapses, one in October 1962 and the other two in October 1964.…”
Section: Sinkhole Inventorymentioning
confidence: 99%