PICKERINGITE
Class : Sulfates, chromates, molybdates
Subclass : Hydrated sulfates
Crystal system : Monoclinic
Chemistry : MgAl2(SO4)4 22H2O
Rarity : Quite common
Pickeringite is a highly hydrated sulfate of magnesium and aluminum. It is a fairly widespread mineral which essentially results from the supergene oxidation of sulfides in different contexts rich in aluminum : pyritic hydrothermal deposits, layers of coal with disseminated pyrite, etc... But it is also found in caves, and in hot spring deposits and in some volcanic fumaroles. It was named in honor of the American philosopher John Pickering. Pickeringite forms delicate fibrous to acicular crystals, frequently united in felted, tufted or spherolitic aggregates, encrustations or efflorescences. It is colorless or white, sometimes yellowish or pinkish.
Main photo : Pickeringite from California Rand No. 2 Mine, California, USA © Rock Currier
Pickeringite in the World
Twinning
No twins known for this mineral species.
Fakes and treatments
No fakes listed for this mineral species.
Hardness : 1.5
Density : 1.73 to 1.79
Fracture : Conchoidal
Streak : White
TP : Translucent
RI : 1.475 to 1.483
Birefringence : 0.008
Optical character : Biaxial -
Pleochroism : None
Fluorescence : None
Solubility : Water
Magnetism : NoneRadioactivity : None