CHALCOALUMITE

    Class : Sulfates, chromates, molybdates
    Subclass : Hydrated sulfates
    Crystal system : Monoclinic
    Chemistry : CuAl4SO4(OH)12 3H2O
    Rarity : Rare to uncommon


Chalcoalumite is a hydrated sulfate of copper and aluminum. It is a secondary mineral of the oxidation zones of copper deposits. It owes its name to its chemical composition : from the Greek khalcos (copper) and the Latin alumen (alum). It essentially forms fibrous botryoidal encrustations, sometimes small triangular, finely lamellar crystals grouped into small spherules, of a pale bluish green to blue or blue-gray color. It transforms into copper-bearing gibbsite by dehydration.

Main photo : Chalcoalumite from Holbrook Mine, Arizona, USA © Rob Lavinsky

Chalcoalumite from Holbrook Mine, Arizona, USA © Stephan Wolfsried
Chalcoalumite from Funtana Raminosa Mine, Sardinia, Italy © Domenico Preite
Chalcoalumite from Grandview Mine, Arizona, USA © Bruce J. Kelley
Chalcoalumite from Holbrook Mine, Arizona, USA © Rob Lavinsky

Chalcoaluminite in the World

Chalcoalumite is known in beautiful specimens in Bisbee (Arizona) and Salmchâteau (Belgium), it is also found in other copper sites in Italy, Slovakia, England and the United States in particular.

Chalcoaluminite in France

In France, chalcoalumite is found in neoformation in the slag of Huelgoat (Finistère) as well as on the copper deposit of Valcroze (Gard).

Twinning and special crystallizations

A twin is known to have a re-entrant angle, but is difficult to identify.

Fakes and treatments

No fakes identified for this mineral species, confusion with chrysocolla or gibbsite may occur.



Hardness : 2.5
Density : 2.29
Fracture : Irregular
Streak : White



TP : Translucent to transparent
RI : 1.520 to 1.530
Birefringence : 0.010
Optical character : Biaxial +
Pleochroism : Low
Fluorescence : None


Solubility : Nitric acid and hydrochloric acid


Magnetism : None
Radioactivity : None

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