PYRARGYRITE
Class : Sulfides and sulfosalts
Subclass : Sulfosalts
Crystal system : Trigonal
Chemistry : Ag3SbS3
Rarity : Uncommon
Pyrargyrite is the isomorph of proustite. It is a common primary mineral of silver-bearing hydrothermal veins. It is also found alongside numerous minerals of silver, antimony, copper and lead. Its name comes from the Greek pûr (fire) and arguros (silver) in reference to its color and its silver content. Pyrargyrite forms compact masses and hexagonal prismatic crystals with planar or rhombohedral pyramidal endings which only exceptionally exceed 5 cm. Fresh it is superb : transparent with a strong metallic luster and has a deep red color, but in daylight, it loses its transparency by being covered with a gray-black superficial film of acanthite. In museums, samples are often protected from prolonged exposure to light by a shutter. It is an important silver ore, actively exploited in many mines.
Main photo : Pyrargyrite from St-Andréasberg, Germany © Dr. Günter Grundmann
Pyrargyrite in the World
In France, pyrargyrite is known in millimeter crystals at Peyrebrune (Tarn), at the Fournial mine (Cantal), at Vitrac (Puy-de-Dôme), at Ste-Marie-aux-Mines (Haut-Rhin). It has also been described in numerous mines in Haute-Loire, in Farges (Corrèze), in Chalanches (Isère), etc...
Twinning
Twins are common on {10-14}, less common on {10-11} {11-20} and rare on {01-20}.
Fakes and treatments
No fakes listed for this mineral species.
Hardness : 2.5
Density : 5.82
Fracture : Irregular to cocnhoidal
Streak : Purplish red
TP : Translucent
RI : 2.881 to 3.084
Birefringence : 0.203
Optical character : Uniaxial -
Pleochroism : Low
Fluorescence : None
Solubility : Nitric acid
Magnetism : NoneRadioactivity : None