NANTOKITE

    Class : Halides
    Subclass : Chlorides
    Crystal system : Cubic
    Chemistry : CuCl
    Rarity : Very rare


Nantokite is a very rare copper chloride. It is a secondary mineral present in the oxidation zone of copper deposits, where it accompanies other secondary copper minerals (cuprite, atacamite, native copper, etc...). It is exceptional in volcanic fumaroles. Its name comes from its place of discovery : Nantoko (Chile). Nantokite is colorless or white, weathering to grayish or greenish. It rarely forms lamellae, more commonly granular masses or tetrahedra. By exposure to air it transforms into paratacamite.

Main photo : Nantokite partially decomposed in paratacamite from Baratti slags, Tuscany, Italy © Marco Bonifazi

Nantokite in the World

Twinned nantokite decomposed in paratacamite (before/after) from Baratti slags, Tuscany, Italy © Marco Bonifazi

Magnificent blades of nantokite were discovered at the Ojuela mine near Mapimi (Mexico), they measure up to 2 cm, they are the most beautiful specimens known. Nantokite is known from several other mines around the world, including Carmen Bajo near Nantoko (Chile), Broken Hill (Australia) and Bisbee (Arizona).

Nantokite in France

Nantokite is not present in the French underground.

Twinning

Twins are known on {111}.

Fakes and treatments

No fakes recorded for this mineral species.



Hardness : 2 to 2.5
Density : 3.93 to 4.3
Fracture : Conchoidal
Streak : White


TP : Translucent to transparent
RI : 1.930
Birefringence : 0
Optical character : None
Pleochroism : None
Fluorescence : None


Solubility : Water, hydrochloric acid, ammonic

Magnetism : NoneRadioactivity : None

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