Algodonite | |
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Category: | Sulfide mineral |
Formula: | Cu6As |
Imasymbol: | Ago[1] |
Molweight: | 456.2 g/mol |
Strunz: | 2.AA.10a |
System: | Hexagonal |
Class: | Dihexagonal dipyramidal (6/mmm) H-M symbol: (6/m 2/m 2/m) |
Symmetry: | P63/mmc |
Unit Cell: | a = 2.6, c = 4.228 [Å]; Z = 2 |
Color: | Gray, silver white, steel gray, tarnishes dull bronze |
Habit: | Massive, granular. Common texture observed in granite and other igneous rock |
Fracture: | Sub-conchoidal |
Mohs: | 4 |
Luster: | Metallic |
Diaphaneity: | Opaque |
Gravity: | 8.38 (measured), 8.72 (calculated) |
Other: | Non-magnetic, non-fluorescent |
References: | [2] [3] [4] |
Algodonite is a copper arsenide mineral with formula: Cu6As. It is a gray white metallic mineral crystallizing in the hexagonal system. It has a Mohs hardness of 4 and a specific gravity of 8.38 – 8.72.
It was first described in 1857 from the Algodones silver mine, Coquimbo, Chile.