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., Pieczka, A., Franus, W. (2006): Olivenite-adamite solid solution from oxidation zone in Rędziny (West Sudetes, Poland). Mineralogia Polonica, 37, 101-110.
- 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.
Mineral List
108 entries listed. 97 valid minerals.
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