FREIBERGITE
Class : Sulfides and sulfosalts
Subclass : Sulfides
Crystal system : Cubic
Chemistry : (Ag,Cu,Fe)12(Sb,As)4S13
Rarity : Common
Freibergite is the least common mineral of the gray copper group. It forms a series (continuous solid solution) with tetrahedrite, the antimoniferous pole, and some authors still consider it as an argentiferous variety of this mineral. Freibergite remains much rarer than the latter, but is frequently associated with it in deposits rich in silver. It is known in polymetallic veins and gold-bearing epithermal veins, as well as in massive sulfide masses where its easy alteration into blue and green carbonates (azurite, malachite) makes it easily detectable. It was named after its location of discovery : Freiberg (Saxony, Germany). Freibergite has a metallic luster and an iron gray to black color, with a sub-conchoidal fracture and a generally tetrahedral appearance. It is an accessory ore of copper and silver. It is likely that it was confused with tetrahedrite in many deposits.
Main photo : Freibergite on rhodochrosite from Freiberg, Saxony, Germany © Jordi Fabre
Freibergite in the World
The most remarkable crystals of freibergite, centimeter-sized tetrahedra, were extracted from the mines of Freiberg (Germany), Mount Isa (Australia), Kutna Hora (Czech Republic) and numerous mines in Japan.
Twinning
Twins are known on {111}.
Fakes and treatments
No fakes recorded for this mineral species.
Hardness : 3 to 4
Density : 4.97
Fracture : Sub-conchoidal
Streak : Reddish to black
TP : Opaque
RI : -
Birefringence : 0
Optical character : None
Pleochroism : None
Fluorescence : None
Solubility : Nitric acid
Magnetism : Paramagnetic
Radioactivity : None