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Bismite
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Bismite is a mineral, or Bi2O3. It is a mineral, but the typical form of occurrence is massive and clay-like with no macroscopic crystals. The color varies from green to yellow. It has a of 4 to 5 and a of 8.5 to 9.5, quite high for a nonmetallic mineral.

Bismite is a secondary oxidation zone mineral which forms from primary bismuth minerals.

It was first described from Goldfield, Nevada in 1868, and later from the Schneeberg District, , , .


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