PICROPHARMACOLITE
Class : Sulfates, chromates, molybdates
Subclass : Hydrated arsenates
Crystal system : Triclinic
Chemistry : Ca4Mg(AsO4)2(HAsO4)2 11H2O
Rarity : Uncommon
Picropharmacolite is the most common calc-magnesium arsenate. It is formed by oxidation of primary arsenic minerals, mainly native arsenic and löllingite, but also realgar, in the upper part of the deposits. Its name comes from the Greek pikros (bitter) and pharmakon (remedy, poison), in reference to the taste of the mineral and its arsenic content. Picropharmacolite is common in newly formed efflorescence in old mining works where it composes aigrettes and spherules or sea urchins of white acicular crystals (sometimes pink when it presents traces of cobalt) up to 2 cm, frequently associated with pharmacolite. It is a highly hydrated mineral that easily loses its water in a dry atmosphere.
Main photo : Picropharmacolite from Giftgrube mine, Ste-Marie-aux-Mines, Haut-Rhin, France © William Peraud
Picropharmacolite in the World
Twinning
No twins known for this mineral species.
Fakes and treatments
No fakes listed for this mineral species.
Hardness : 1 to 2
Density : 2.55 to 2.64
Fracture : Fibrous to micaceous
Streak : White
TP : Translucent
RI : 1.556 to 1.585
Birefringence : 0.021
Optical character : Biaxial +
Pleochroism : None
Fluorescence : None
Solubility : -
Magnetism : NoneRadioactivity : None