Chalcocite | |
---|---|
General | |
Category | Sulfide minerals |
Formula (repeating unit) | copper(I) sulfide: Cu2S |
IMA symbol | Cc[1] |
Strunz classification | 2.BA.05a |
Crystal system | Monoclinic |
Crystal class | Prismatic (2/m) (same H-M symbol) |
Space group | P21/c |
Unit cell | a = 15.246(4) Å, b = 11.884(2) Å, c = 13.494(3) Å; β = 116.35(1)°; Z = 48 |
Identification | |
Color | Dark gray to black |
Crystal habit | Tabular to prismatic crystals also massive to granular, (pseudo-orthorhombic) |
Twinning | Common on {110} yielding pseudohexagonal stellate forms |
Cleavage | Indistinct on {110} |
Fracture | Conchoidal |
Tenacity | Brittle to sectile |
Mohs scale hardness | 2+1⁄2–3 |
Luster | Metallic |
Streak | Shiny black to lead gray |
Diaphaneity | Opaque |
Specific gravity | 5.5–5.8 |
Fusibility | 2–2.5 |
References | [2][3][4][5] |
Chalcocite (/ˈkælkəˌsaɪt/),[6][7] copper(I) sulfide (Cu2S), is an important copper ore mineral. It is opaque and dark gray to black, with a metallic luster. It has a hardness of 2.5–3 on the Mohs scale. It is a sulfide with a monoclinic crystal system.
The term chalcocite from the Greek khalkos, meaning "copper". It is also known as redruthite, vitreous copper, or copper-glance.[8]