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Bismite
Bismuth trioxide, or Bi2O3 From Wikipedia, the free encyclopedia
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Bismite is a bismuth oxide mineral, bismuth trioxide or Bi2O3. It is a monoclinic 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 Mohs hardness of 4 to 5 and a specific gravity 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, Ore Mountains, Saxony, Germany.
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See also
- Bismuth trioxide – details on the chemistry of this substance
- Bismutite
- Bismuthinite
- Bismoclite
- Eulytine
References
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