Hercynite | |
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General | |
Category | Oxide minerals Spinel group Spinel structural group |
Formula (repeating unit) | Fe2+Al2O4 |
IMA symbol | Hc[1] |
Strunz classification | 4.BB.05 |
Crystal system | Isometric |
Crystal class | Hexoctahedral (m3m) H-M symbol: (4/m 3 2/m) |
Space group | Fd3m (no. 227) |
Identification | |
Formula mass | 173.81 g/mol |
Color | Black |
Crystal habit | Euhedral crystals. Also massive to granular |
Cleavage | [111] indistinct |
Fracture | Uneven – flat surfaces (not cleavage) fractured in an uneven pattern. |
Mohs scale hardness | 7.5 |
Luster | Vitreous (glassy) |
Streak | dark green |
Specific gravity | 3.95 |
Optical properties | Isotropic |
Refractive index | n = 1.8 |
Other characteristics | non-radioactive |
References | [2][3][4] |
Hercynite is a spinel mineral with the formula FeAl2O4.
It occurs in high-grade metamorphosed iron-rich argillaceous (clay-containing) sediments as well as in mafic and ultramafic igneous rocks. Due to its hardness it also is found in placers.[2]
It was first described in 1847 and its name originates from the Latin name for the Harz, Silva Hercynia, where the species was first found.[2][3]
Hercynite is a spinel of regular symmetry and normal cation distribution, but some disorder occurs in its structure. It consists of ferrous (Fe2+) ions and aluminium ions (Al3+); however some ferric ions (Fe3+) may be located in the structure of hercynite.[5]
Melting point of this mineral is inbetween 1,692–1,767 °C (3,078–3,213 °F).[6]