GAHNITE
Class : Oxides and hydroxides
Subclass : Oxides
Crystal system : Cubic
Chemistry : ZnAl2O4
Rarity : Quite common
Gahnite is a zinc-bearing aluminous spinel typical of certain rocks of contact metamorphism (marbles in particular), of replacement deposits containing zinc, and more rarely of granitic pegmatites. It is also a mineral that can be found in neoformation in foundry slag. It is a so-called “normal” spinel, the bivalent ions being all in tetrahedral sites. Gahnite forms two continuous series, one towards the ferrous term, hercynite, the other towards the aluminous term, spinel in the strict sense. It was named in honor of the Swedish mineralogist and chemist Johan Gottieb Gahn who discovered the mineral and isolated the element manganese. Gahnite is usually presented in octahedra, sometimes in dodecahedra, rarely in cubes. It can also be massive or in irregular, rounded grains. Its color is dark green to greenish black, sometimes bluish black or brownish.
Main photo : Gahnite from Franklin, Sussex County, New Jersey, USA © Modris Baum
Gahnite in the World
Twinning
A twin is known on {111}.
Fakes and treatments
No fakes recorded for this mineral species.
Hardness : 7.5 to 8
Density : 4.62
Fracture : Irregular to conchoidal
Streak : Gray
TP : Translucent to opaque
RI : -
Birefringence : 0
Optical character : None
Pleochroism : None
Fluorescence : None
Solubility : Sulfuric acid
Magnetism : Paramagnetic
Radioactivity : None