PUCHERITE
Class : Phosphates, arsenates, vanadates
Subclass : Anhydrous vanadates
Crystal system : Orthorhombic
Chemistry : BiVO4
Rarity : Rare to very rare
Pucherite is a rare vanadate resulting from the alteration of bismuth minerals in the oxidation zone of hydrothermal vanadium deposits and granitic pegmatites. Its name comes from its place of discovery : the Pucher shaft of the Wolfgang mine (Saxony, Germany). It is a yellowish-brown to dark red-brown mineral that can form neat, equant to tabular, sometimes acicular crystals, but more often occurs as encrustations of tiny crystals. It is the polymorph of two other even rarer minerals : clinobisvanite and dreyerite.
Main photo : Pucherite from Pucher Shaft, Wolfgangmassen mines, Saxony, Germany © Elmar Lackner
Pucherite in the World
Pucherite is not present in the French underground. Pucherite pseudomorph after tourmaline crystals are known in Little Three Mine (California).
Twinning
No twins known for this mineral species.
Fakes and treatments
No fakes listed for this mineral species.
Hardness : 4
Density : 6.69
Fracture : Sub-conchoidal
Streak : Yellow
TP : Opaque to transparent
RI : 2.410 to 2.510
Birefringence : 0.100
Optical character : Biaxial -
Pleochroism : None
Fluorescence : None
Solubility : Hydrochloric acid
Magnetism : NoneRadioactivity : None