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Please use this identifier to cite or link to this item: http://hdl.handle.net/20.500.12128/17542
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dc.contributor.authorAndrejczuk, Wiaczesław-
dc.date.accessioned2020-12-03T11:59:10Z-
dc.date.available2020-12-03T11:59:10Z-
dc.date.issued2014-
dc.identifier.citation"Prace Komisji Krajobrazu Kulturowego", Nr 26, 2014, s. 93-110pl_PL
dc.identifier.issn1896-1460-
dc.identifier.issn2391-5293-
dc.identifier.urihttp://hdl.handle.net/20.500.12128/17542-
dc.description.abstractGypsum is a rock having a wide spread in the earth's crust and on its surface. Due to the specified usable values gypsum is a desired raw material, mostly mined in quarries. Gypsum belongs to karstic rocks and easily dissolves in water. Therefore, a series of gypsum rocks, lying close to the earth surface and gypsum massifs usually are strongly karstified. Gypsum quarries almost always expose the karstified interior of gypsum massifs, rich in various karst forms both karstic and paleokarstic, including caves. The latter are often large and represent a valuable or even unique natural formations, which should be taken under protection. Karst formations frequently determine the total value of gypsum quarries as geosites. In the article, the values of various gypsum quarries of Podilla and Bukovina resulting from karst formations, especially the caves, are shown, as examples.pl_PL
dc.language.isoplpl_PL
dc.rightsUznanie autorstwa-Użycie niekomercyjne-Bez utworów zależnych 3.0 Polska*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/pl/*
dc.subjectgypsumpl_PL
dc.subjectgypsum karstpl_PL
dc.subjectquarrypl_PL
dc.subjectcavepl_PL
dc.subjectgeositepl_PL
dc.titleKamieniołomy gipsowe jako cenne geostanowiska krasowe : studium przypadku: Podole i Bukowina, Ukrainapl_PL
dc.title.alternativeGypsum quarries as valuable karst geosites. Case study: Podilla and Bukovina, Ukrainepl_PL
dc.typeinfo:eu-repo/semantics/articlepl_PL
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