VIOLARITE

    Class : Sulfides and sulfosalts
    Subclass : Sulfides
    Crystal system : Cubic
    Chemistry : FeNi2S4
    Rarity : Rare


Violarite belongs to the linnaeite group, named after the most common mineral. This group with the formula X3S4 (with X = Co, Ni, Fe or Co + Cu) can be compared with that of spinels, with sulfur replacing oxygen ; the octahedral facies is also the most common in both groups. The linnaeite group is composed of three solid solutions : Co (linnaeite in the strict sense) - Ni (polydymite) the intermediate term being siegenite ; Ni (polydymite) - Fe (greigite), the intermediate term being violarite, and Co (linneite) - Cu. The latter solid solution is the only one that is incomplete and stops at carrollite. Violarite is an iron and nickel sulfide from hydrothermal cobalt and nickel deposits. Its name comes from the Latin violaris (violet), in allusion to the color of the mineral under the reflected light microscope. Violarite has a luminous gray to steel gray color with a slightly pinkish hue, tarnishing in reddish to purplish hues. Violarite is not known in crystals but only in masses or millimeter nodules. It is an accessory ore of nickel.

Main photo : Violarite from Perseverance Mine, Australia © Jean-François Carpentier

Violarite in the World

Violarite is present among others in Canadian nickel mines (notably Sudbury, Ontario), American (Julian, California), and Australian (Kambalda, Kalgoorlie).

Violarite in France

In France, violarite is reported in Alzen (Ariège), in the Trapp quarries (Vosges) and in certain amphibolites and serpentinites around Brioude (Haute-Loire).

Twinning

No known twinning for this mineral species.

Fakes and treatments

No fakes listed for this mineral species.



Hardness : 4.5 to 5.5
Density : 4.79
Fracture : Undetermined
Streak : Black


TP : Opaque
RI : -
Birefringence : 0
Optical character : None
Pleochroism : None
Fluorescence : None


Solubility : Nitric acid

Magnetism : NoneRadioactivity : None