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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...