Franklinite
| Franklinite | |
|---|---|
|
Franklinite (black) with Zincite (red) | |
| General | |
| Category |
Oxide minerals Spinel group Spinel structural group |
| Formula (repeating unit) | ZnFe2O4 |
| Strunz classification | 04.BB.05 |
| Identification | |
| Color | black |
| Crystal habit | octahedral |
| Crystal system | isometric/cubic |
| Fracture | irregular/uneven, conchoidal |
| Mohs scale hardness | 5½-6 |
| Luster | metallic, often dull |
| Streak | reddish brown to black |
| Diaphaneity | opaque |
| Specific gravity | 5.07 - 5.22 |
| Solubility | HCl soluble |
| Other characteristics | magnetic |
Franklinite is an oxide mineral belonging to the normal spinel subgroup's iron (Fe) series, with the formula ZnFe3+2O4.
As with another spinel member magnetite, both ferrous (2+) and ferric (3+) iron may be present in Franklinite samples. Divalent iron and/or manganese (Mn) may commonly accompany zinc (Zn) and trivalent manganese may substitute for some ferric iron.
At its type locality, Franklinite can be found with a wide array of minerals, many of which are fluorescent. More commonly, it occurs with willemite, calcite, and red zincite. In these rocks, it forms as disseminated small black crystals with their octahedral faces visible at times. It may rarely be found as a single large euhedral crystal.
Franklinite was a minor ore of zinc, manganese, and iron. It is named after its local discovery at the Franklin Mine and Sterling Hill Mines in New Jersey.
See also
References
External links
Media related to Franklinite at Wikimedia Commons