0000000000654244

AUTHOR

Bartolomeo Vigna

showing 2 related works from this author

Evaporite karst in Italy: A review

2017

none 16 si Although outcropping rarely in Italy, evaporite (gypsum and anhydrite) karst has been described in detail since the early 20th 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 studies were carried out in many gypsum areas, resulting in a comprehensive overview, promoting further research in these special karst regions. More recent and detailed studies focused…

geology010504 meteorology & atmospheric sciencesEvaporitehazardQH301-705.5Settore GEO/04 - Geografia Fisica E GeomorfologiaSinkhole[SDE.MCG]Environmental Sciences/Global ChangesGeochemistrySinkholes010502 geochemistry & geophysicsPalaeoclimatepalaeoclimate01 natural sciencesgypsum karst; Italy; geology; geomorphology; palaeoclimate; hazards; sinkholesgypsum karstCaveSpeleogenesisBiology (General)Geomorphology0105 earth and related environmental sciencesEarth-Surface Processesgypsum karst Italy geology geomorphology palaeoclimate hazards sinkholesQE1-996.5geographygeography.geographical_feature_category[SDE.IE]Environmental Sciences/Environmental EngineeringHazardssinkholesGeologyGeomorphologygeomorphology[SHS.GEO]Humanities and Social Sciences/GeographyKarst[SDE.ES]Environmental Sciences/Environmental and SocietyGeology; Geomorphology; Gypsum karst; Hazards; Italy; Palaeoclimate; Sinkholes; Geology; Earth-Surface ProcessesItaly[SDE.BE]Environmental Sciences/Biodiversity and EcologySettore GEO/05 - Geologia ApplicataGypsum karstGeologyGypsum karst
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A review on hypogene caves in Italy

2014

Although hypogene cave systems have been described since the beginning of the 20th century, the importance in speleogenesis of ascending fluids that acquired their aggressiveness from in-depth sources has been fully realized only in the last decades. Aggressiveness of waters can be related to carbonic and sulfuric acids and the related corrosion-dissolution processes give rise to different types of caves and underground morphologies. The abundance of hydrothermal springs and associated travertine deposits, and the widespread interaction between volcanic or sub-volcanic phenomena and karst in many sectors of the Italian peninsula are a strong evidence of hypogene speleogenesis. Furthermore, …

SpeleogenesisHypogene caveItalySettore GEO/04 - Geografia Fisica E Geomorfologiahypogene caves
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