50°58'36"N 20°22'17"E
(50.97692, 20.3716)
It is located at the western end of the Oblęgorskie Range near the village of Kuźniaki, where there are ruins of a blast furnace from the 19th century.
It is built of Dolnotriasic sandstones that sometimes form rock debris. On the hillside there is a rock block, the side planes of which constitute a tectonic mirror - a smooth rock surface created as a result of smoothing by rock masses moving relative to each other. It is not a frequent phenomenon in the Świętokrzyskie Mountains - tectonic mirrors are the most numerous in the Tatra Mountains.