PARATACAMITE
Class : Halides
Subclass : Oxychlorides
Crystal system : Trigonal
Chemistry : Cu2Cl(OH)3
Rarity : Rare
Paratacamite is an alteration mineral from copper deposits occurring in arid and saline conditions. More rarely it is a mineral from fumarolic deposits or an alteration product of the underwater sulfides of black smokers. It has three polymorphs: botallackite, clinoatacamite and atacamite. Its name comes from the Greek para (near) and its dimorphic relationship with atacamite. Paratacamite occurs in rhombohedral crystals, commonly twinned, in masses, in powdery encrustations, sometimes fibrous and spherolitic in appearance. Like atacamite, paratacamite has a bright luster, and an emerald green to blackish green, rarely light green color.
Main photo : Paratacamite from La Vendida Mine, Chile © Matteo Chinellato
Paratacamite in the World
Twinning
Twins on {10-11} are common, sometimes polysynthetic.
Fakes and treatments
No fakes listed for this mineral species.
Hardness : 3
Density : 3.72 to 3.74
Fracture : Irregular to conchoidal
Streak : Green
TP : Translucent to opaque
RI : 1.826 to 1.837
Birefringence : 0.007
Optical character : Uniaxial -
Pleochroism : Low
Fluorescence : None
Solubility : Acids
Magnetism : NoneRadioactivity : None