Dolomite quarry, Rędziny, Czarnów, Rudawy Janowickie Mts, Lower Silesia (Dolnośląskie), Poland

Active quarry in dolomitic marbles, with rich polymetallic (Sn, Bi, Pb, As and Cu) and secondary mineralization. Minerals can be divided into primary rock-forming minerals, hydrothermal ore mineralization and hypergene mineralization.
Located near Czarnów.

References:
- Domańska, J.: Rędziny. Otoczak, nr. 29, p. 38-52.
- Parafiniuk J., Domanska J., 2002: Bismuth minerals form Rędziny (Rudawy Janowickie, SW Poland). Mineralogia Polonica, vol. 33 (2), 3-14.
- Gołębiowska B., Pieczka A., Parafiniuk J. 2005: Minerals of the bismuthinite-aikinite series from Rędziny (Western Sudetes). Mineralogical Society of Poland - Special Papers, vol. 26, 165-168.
- Pieczka A., Gołębiowska B., Parafiniuk J. 2005: Conditions of cassiterite formation in the Rędziny area (Western Sudetes). Mineralogical Society of Poland - Special Papers, vol. 26, 227-230.
- Gołębiowska B., Pieczka A., Parafiniuk J. 2006: Cu(Ag)-Pb-Bi(Sb)
sulphosalts from Rędziny (Western Sudetes, Poland). Mineralogia Polonica - Special Papers, vol. 28, 78-80.
- Gołębiowska B., A. Pieczka, & W. Franus: "Olivenite-adamite solid solution from oxidation zone in Redziny (West Sudetes, Poland)" Mineralogia Polonica 37 (2006) 101-111.
- Pieczka A., Gołębiowska B., Parafiniuk J. 2006: The stannite-group minerals from Rędziny (Lower Silesia, Poland). Mineralogia Polonica - Special Papers, vol. 28, 175-177.
- Parafiniuk, J. et al. (2008): Can. Mineral. 46, 1305-1315.