Mostolinka

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This name is used for the location between Radčí, Maršov u Úpice and Libňatov, which is mostly wooded and has a rich geological composition under the soil cover. While the spring site is located on Cenozoic sandy-loamy to clay-sandy sediments, the immediate vicinity hides either consolidated sediments from the Upper Permian or consolidated sediments from the Lower Permian, where in places...
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