About
Pyrargyrite is light sensitive. Prolonged exposure to bright light will darken its transparency and cause it to become darker. Exposure also may cause a dark, dull film to form on crystal faces; this film can be removed by brushing a specimen with soap and water.
Pyrargyrite is very similar to Proustite, and forms a series with it. Pyrargyrite is the antimony-rich member, and Proustite is the arsenic-rich member. It is often not possible to visually distinguish these two minerals from each other. Pyrargyrite is the more common of this series, although good crystals of both these minerals are difficult to come across. Most good material in collections today are from closed, historical localities.
Pyrargyrite is named from the Greek words Pyr, "Fire" in allusion to the color of this mineral, and Argyros, meaning silver, describing its silver content.
Crystal Forms & Aggregates
Striking Features
Environment
Uses
Noteworthy Localities
Other classic European Pyrargyrite localities include Jáchymov, Krušné Hory Mts, Bohemia, Czech Republic; Příbram, Bohemia, Czech Republic; and Hiendelaencina, Guadalajara, Spain.
Important South American localities for Pyrargyrite are the Uchucchacua Mine, Oyon, Lima Department, Peru; the San Genaro Mine, Castrovirreyna, Huancavelica Department, Peru; Porco and Colquechaca, Potosí Department, Bolivia; and Chañarcillo, Copiapó Province, Atacama Desert, Chile.
In Mexico, lustrous, complex crystals have come from Fresnillo, Zacatecas; and large crystals clusters from the San Juan de Rayas Mine, Guanajuato. Pyrargyrite is very rare in U.S., with few localities producing any specimens of note, though small microcrystals occur at the Advance Mine, Colorado Hill, Alpine Co., California.
Common Mineral Associations
Distinguishing Similar Minerals
Photos
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