TYROLITE
Class : Phosphates, arsenates, vanadates
Subclass : Hydrated arsenates
Crystal system : Orthorhombic
Chemistry : CaCu5(AsO4)2(CO3)(OH)4 6H2O
Rarity : Uncommon to rare
Tyrolite is a fairly rare secondary arsenate from the oxidation zone of copper deposits. Some AsO4 groups are likely to be replaced by CO3 or SO4, which gives quite variable chemical compositions for this mineral. Its name comes from its region of discovery : Tyrol (Austria). Tyrolite generally occurs as sky blue to bluish green crystals, in the form of flattened laths or scales on {010} and elongated along [100] or [001]. The crystals are often grouped in radiate groups. Less commonly, tyrolite occurs as incrustations or as hummocky masses with a characteristic fibroradiated or micaceous texture. Tyrolite has a perfect micaceous cleavage according to {001}. It is an accessory ore of copper.
Main photo : Tyrolite from Mammoth Mine, Utah, USA © Rob Lavinsky
Tyrolite in the World
Twinning
No twinning known for this mineral species.
Fakes and treatments
No fakes listed for this mineral species.
Hardness : 1.5 to 2
Density : 3 to 3.2
Fracture : Undetermined
Streak : Pale green
TP : Translucent to transparent
RI : 1.694 to 1.730
Birefringence : 0.036
Optical character : Biaxial -
Pleochroism : Low
Fluorescence : None
Solubility : Acids, ammonia
Magnetism : NoneRadioactivity : None