Eskolaite
| Eskolaite | |
|---|---|
|
Eskolaite from Russia | |
| General | |
| Category |
Oxide mineral Hematite group Corundum structural group |
| Formula (repeating unit) | Cr2O3 |
| Strunz classification | 04.CB.05 |
| Crystal symmetry |
Trigonal hexagonal scalenohedral H-M symbol: (32/m) Space group: R3c |
| Unit cell | a = 4.95 Å, c = 13.58 Å; Z=6 |
| Identification | |
| Color | Black to dark green |
| Crystal habit | Hexagonal prisms and plates |
| Crystal system | Trigonal |
| Cleavage | None |
| Tenacity | Brittle |
| Mohs scale hardness | 8 |
| Luster | Vitreous or metallic |
| Streak | Pale green |
| Diaphaneity | Opaque, translucent in thin edges |
| Specific gravity | 5.18 |
| Optical properties | Uniaxial |
| Pleochroism | Noted; emerald-green to olive-green |
| References | [1][2][3] |
Eskolaite is an uncommon chromium oxide mineral (chromium(III) oxide Cr2O3).
Discovery and occurrence
It was first described in 1958 for an occurrence in the Outokumpu ore deposit of eastern Finland.[2] It occurs in chromium bearing tremolite skarns, metamorphosed quartzites and chlorite bearing veins in Finland; in glacial boulder clays in Ireland and in stream pebbles in the Merume River of Guyana.[1] It has also been recognized as a rare component in chondrite meteorites.[1]
The mineral is named after the Finnish geologist Pentti Eskola (1883–1964).
Structure and physical properties
Eskolaite crystallizes with trigonal symmetry in the space group R3c and has the lattice parameters a = 4.95 Å and c = 13.58 Å at standard conditions. The unit cell contains six formula units. The lattice is analogous to that of corundum, with Cr3+ replacing Al3+.