CALEDONITE
Class : Sulfates, chromates, molybdates
Subclass : Anhydrous sulfates
Crystal system : Orthorhombic
Chemistry : Pb5Cu2(CO3)(SO4)3(OH)6
Rarity : Rare
Caledonite is a rare secondary mineral from the oxidation zone of lead-copper deposits in an arid climate. It accompanies other secondary minerals of lead and copper (cerussite, anglesite, malachite, azurite, chrysocolla...). It is also found in industrial slags. Its name comes from its place of discovery, Caledonia (former name of Scotland). Rarely massive, it mainly forms elongated and strongly striated prismatic crystals according to [001], of a characteristic blue-green, rarely sky blue.
Main photo : Caledonite from Mammoth-St-Antony Mine, Arizona, USA © Carsten Slotta
Caledonite in the World
Twinning
No twin known for this mineral species.
Fakes and treatments
No fake identified for this mineral species.
Hardness : 2.5 to 3
Density : 5.75
Fracture : Irregular
Streak : Blue-green to bluish white
TP : Translucent to transparent
RI : 1.818 to 1.909
Birefringence : 0.091
Optical character : Biaxial -
Pleochroism : Low
Fluorescence : None
Solubility : Nitric acid
Magnetism : None
Radioactivity : None