COQUIMBITE
Class : Sulfates, chromates, molybdates
Subclass : Hydrated sulfates
Crystal system : Trigonal
Chemistry : Fe2(SO4)3 9H2O
Rarity : Rare to uncommon
Coquimbite is a rare iron sulphate formed by alteration of iron sulfides in an arid climate. It is a secondary mineral which is part of a classic mineralogical procession to which other iron sulfates belong (copiapite, voltaite, jarosite, amarantite, botryogen, fibroferrite, etc...), resulting like it from precipitation from “natural” sulfuric acid formed by reaction of surface water with iron sulphides. By changing environmental conditions (temperature, pH, redox potential) these sulfates are easily hydrolyzed into ferric hydroxides (goethite and limonite). Its name is linked to its supposed discovery location : the province of Coquimbo (Chile). Coquimbite forms prismatic crystals with a hexagonal outline, purple in color, sometimes greenish or greenish yellow, exceptionally purplish red.
Main photo : Coquimbite from Monte Arsiccio Mine, Toscane, Italie © Quebul Fine Minerals
Coquimbite in the World
Twinning
No twin known for this mineral species.
Fakes and treatments
No fake identified for this mineral species.
Hardness : 2.5
Density : 2.11
Fracture : Sub-conchoidal
Streak : White
TP : Transparent
RI : 1.539 to 1.548
Birefringence : 0.009
Optical character : Uniaxial +
Pleochroism : None
Fluorescence : None
Solubility : Water and acids
Magnetism : None
Radioactivity : None