Smithsonites found at Tsumeb are renowned for their diverse styles and colours. This specimen features a druse of transparent dark yellow-green Smithsonite crystals, with a combination of positive and negative rhombohedrons, including numerous offsets, all resting on an earlier generation of iron oxide-stained crystals. Sprays of yellow acicular mimetite crystals further enhance the aesthetic of the specimen, though some of the fragile micro-mimetites are damaged. The reverse side reveals micro drusy calcite crystals, along with aggregates of very light yellowish-green tabular microcrystals of an unidentified mineral. Tsumeb is famous for the variety of Smithsonite it produced, with the best copper-bearing green Smithsonites from this locality, widely regarded as one of the world’s greatest mineral sites.
Dr. Tarassoff acquired this specimen from Eugene E. Schlepp (Western Minerals) at the Tucson Gem and Mineral Show in 1979. Collected during the prime years of Tsumeb’s Smithsonite production in the 1960s to early 1980s, this specimen represents the high-quality material that made Tsumeb legendary among mineral collectors.
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