Gahnite - Encyclopedia

    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

The largest crystals, exceeding 12 cm, come from the metamorphic zinc deposits of New Jersey (Franklin and Sterling Hill). Dark blue-green octahedrons measuring 25 mm were discovered in Topsham, Maine. Beautiful crystals also come from Tiriolo (Calabria, Italy), pegmatites from Brazil, Finland, as well as quartzites from lead-zinc deposits in Australia and South Africa.

Gahnite in France

In France, gahnite is reported at the Charrier mine near Vichy (Allier), at Chessy (Rhône), at Taurinya (Pyrénées-Orientales), in alluvium near Vannes (Morbihan) and in the slag of Vialas (Lozère) .

Twinning

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

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