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The deposits in Poland are appearing in the Miocene gypsum sediments located on the northern, marginal part of the Carpathians Foredeep subsidence basin. Up to the fifties of 20th century and the discover of the biggest sulphur deposits in all the world, the sulphuric mining existed only in Swoszowice near Krakow, Czarkowy near Stasz?w, Psz?w near Rybnik and also Pos?dza, located about 30 km northeast of Krakow. The first record of organised mining in Swoszowice appears in document dated 1415. It was a licence for...

Krakow ? the former capital of Poland ? is situated on border Krakow-Silesian monocline and Carpathians Flysch separated by narrow zone of the Carpathian Foredeep. In the geological structure of Krakow, the Jurassic and Cretaceous are exposed on the surface sediments. The Neogene sediments fill the Vistula valley. For thousands of years the sacred and secular constructions have been built using Jurassic limestones coming from local quarries. These quarries were founded on fault ridges, from the early Middle Ages t...