|
Chemical Formula |
Bi |
|
Composition |
Bismuth, usually with traces of arsenic, antimony, and sulfur |
|
Variable Formula |
(Bi,As,Sb,S) |
|
Color |
Silver-white, sometimes with reddish hue. Oxidizes yellowish to dark gray. |
|
Streak |
Silver-white |
|
Hardness |
2 - 2.5 |
|
Crystal System |
Hexagonal |
|
Crystal Forms |
Crystals, which are uncommon, are usually flat hexagons occurring in parallel groupings. Bismuth also occurs massive and as waterworn nugget in stream beds. Pseudocubic, hopper-like crystal groupings are almost never found in nature, but are laboratory-produced. |
|
Transparency |
Opaque |
|
Specific Gravity |
9.7 - 9.8 |
|
Luster |
Metallic |
|
Cleavage |
2,1 - prismatic ; 3,1 - basal |
|
Fracture |
Hackly to uneven |
|
Tenacity |
Brittle and slightly sectile |
|
Other ID Marks |
1) Tarnishes yellow to dark gray. |
|
Complex Tests |
Becomes slightly malleable when heated, expands when solidifying, and is strongly diamagnetic. |
|
In Group |
Native Elements; Semi-Metallic Elements |
|
Striking Features |
Color, tarnish, sectility, and striations on cleaved surfaces. |
|
Environment |
In mesothermal veins, in hydrothermal replacement deposits, and in granite pegmatites. |
|
Rock Type |
Igneous, Metamorphic |
|
Popularity (1-4) |
2 |
|
Prevalence (1-3) |
1 |
|
Demand (1-3) |
2 |

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