SL23 RSC Stanišovská Cave- treasures of the Earth

The cave is in the Liptovský Mikuláš district. The entrance is on the northwestern slope of Smrekovica in the Low Tatras National Park at elevation of 761 m. The cave was formed by erosion and corrosion activities of the underground stream of Štiavnica with the help of atmospheric waters and processes of rock crumbling and collapsing of weathered material along the tectonic faults and interbed surfaces in the Pleistocene and Holocene. The general direction of the cave is N-S. The flowstone fill of the cave is considerably destroyed mainly in the easily accessible parts.The cave has two developmental levels, the lower one is about 25 m below the flow of Štiavnica. The temperature in cave is from 6,4 °C to 7,0 °C. Air humidity reaches 95%. The lower level forms a horizontal passage with irregular profile with a debris of sharp fragments of the bedrock on the floor. Some parts of this passage have flowstone cascades and lakes on cave bottom. The upper level has cave fills in various forms and shapes, with abundant stick stalagmites. The Stanišovská Cave is together with nearby Malá Stanišovská Cave the most important wintering place for bats in the Jánska Valley. Seven species were found her by now. The most abundant is the Greater Mouse-Eared Bat (Myotis myotis). 

they knew different aspects of underground Sloakia. They knew something more about Slovak history