An excellent specimen showcasing a combination of several different well formed mineral species. The core of the specimen shows an initial growth of galena and sphalerite followed by pointed tabular arsenopyrite almost entirely covering the specimen. From some of the recesses clusters of quartz that developed, numerous scepters can be found. Lastly light-coloured, botryoidal rhodochrosite settled upon the surface, covering roughly half the specimen. A great example for this locality. For anywhere, really!
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