VOLTAITE
Class : Sulfates, chromates, molybdates
Subclass : Hydrated sulfates
Crystal system : Cubic
Chemistry : K2Fe9(SO4)12 18H2O
Rarity : Common
Voltaite is a double sulfate of potassium and ferrous (Fe2+) and ferric (Fe3+) iron. It is a rare secondary mineral formed by the alteration of iron sulfides, mainly in arid climates, which is part of a classic mineralogical procession to which other iron sulfates belong (copiapite, jarosite, coquimbite, botryogen, etc...). These sulfates result, like it, from precipitation from "natural" sulfuric acid, formed by the reaction of surface water with iron sulfides ; by changing the environmental conditions (temperature, pH, oxidation-reduction potential) they are easily hydrolyzed into ferric hydroxides (goethite and limonite). Voltaite is also known from volcanic fumaroles. It was named in honor of Alessandro Giusepe Antonio Anastasio Volta, an Italian physicist who discovered the electric battery in 1800. Voltaite occurs in the form of cubes, octahedra, rarely dodecahedra, of a black to greenish-black color.
Main photo : Voltaïte from Monte Arsiccio Mine, Tuscany, Italy © Uwe Haubenreisser
Voltaite in the World
Twinning
No twinning known for this mineral species.
Fakes and treatments
No fakes listed for this mineral species.
Hardness : 3 to 3.5
Density : 2.65
Fracture : Conchoidal
Streak : Gray-green
TP : Opaque
RI : 1.593 to 1.608
Birefringence : 0
Optical character : None
Pleochroism : None
Fluorescence : None
Solubility : Water, acids
Magnetism : NoneRadioactivity : None