Fluorite from Kletno can be found on a heap near the Uranium Mine. Rainy weather is conducive to searching
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Fluorspar is a mineral with a characteristic glassy shine, often occurring in various colors - from colorless, through shades of green, purple, blue, to yellow. It occurs in the form of cubes or massive clusters.
After a flood, fluorspar from the heap may show surface changes, such as worn edges or smoothing, caused by the intensive action of water.
Historical and geological significance:
The uranium mine in Kletno operated in the 1940s and 1950s, and its heaps are today an interesting geological area where you can find remains of many minerals, including fluorspar. Flooding in such an area can additionally change the landscape and expose new layers of material, which increases the possibility of finding rare forms of fluorite and other minerals.
In summary, fluorite from the heap after the flood in Kletno can be an interesting specimen not only from a geological point of view, but also as evidence of the influence of natural forces on minerals.
