Jordanite | |
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General | |
Category | Sulfosalt minerals |
Formula (repeating unit) | Pb 14(As,Sb) 6S 23 |
Strunz classification | 2.JB.30a |
Crystal system | Monoclinic |
Crystal class | Prismatic (2/m) (same H-M symbol) |
Space group | P21/m |
Identification | |
Colour | Lead-grey |
Cleavage | Perfect |
Fracture | Conchoidal |
Tenacity | Brittle |
Mohs scale hardness | 3 |
Metallic|re|er}} | Metallic |
Streak | Black |
Density | 6.4 |
Pleochroism | Visible |
Jordanite is a sulfosalt mineral with chemical formula Pb
14(As,Sb)
6S
23 in the monoclinic crystal system,[2] named after the German scientist H. Jordan (1808–1887) who discovered it in 1864.
Lead-grey in colour (frequently displaying an iridescent tarnish), its streak is black and its lustre is metallic. Jordanite has a hardness of 3 on Mohs scale, has a density of approximately 6.4, and a conchoidal fracture.[2]
The type locality is the Lengenbach Quarry in the Binn Valley, Wallis, Switzerland .[2]
Original source: https://en.wikipedia.org/wiki/Jordanite.
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