PROUSTITE MINERAL FACTS Nevada Turquoise gem stones
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Proustite Mineral Facts:

Chemical Formula: AgAsS3 (Light Ruby Silver)Sulfo-arsenite of silver, silver is 64.5 % by weight. May contain a small amount of antimony substituting for arsenic.

Colors: Ruby Red to Brownish red
Its color is scarlet in transparent pieces by transmitted light. Under the long-continued influence of daylight the color deepens until it becomes darker than that of pyrargyrite. Its streak is  deep red to brownish black.

Hardness: 2.0

Density: 5.5

Cleavage: Imperfect, but  it is easily sectile, and can be cut with a knife like lead.

Crystallography: Rhombohedral
Found in p
ointed crystals, but more commonly occurs as granular and massive forms.

Luster:. Adamantine luster. Transparent to translucent. High refractive index.

Optics: (Refractive Index):  w= 3.0877, e= 2.7924


Composition, Structure and Associated Minerals:
Proustite, or light ruby silver, is isomorphous with pyrargyrite. It differs from the latter mineral in containing arsenic in place of antimony. It occurs both massive and in crystals, and like pyrargyrite is an important silver ore. The mineral occurs in veins associated with other compounds of silver such as native silver, acanthite (argentite), stephanite, and sometimes with galena and arsenopyrite. It is most commonly found in the zone of secondary enrichment of silver veins, but also is formed as a primary ore mineral in some near surface epithermal systems rich in silver.

Identification and Diagnostics
Characterized chiefly by its ruby-red color and streak and its brilliant luster. Its reaction for silver serves to distinguish it from cuprite, cinnabar and realgar, which it sometimes resembles. Proustite differs from pyrargyrite in its color, transparency and streak, as well as in its arsenic reactions. Proustite gives reactions for arsenic where this mineral reacts for antimony, and yields only sulphur when dissolved in HNO3. From its solution in KOH a yellow precipitate of As2S3 is thrown down upon the addition of HC1 (compare with pyrargyrite).

Occurrence, Localities and Origins:
Overall, proustite is a fairly  rare mineral, occurring in silver veins associated with various other sulpharsenites and sulphantimonites. It is generally less abundant than pyrargyrite. Found in the silver mines of Saxony; Bohemia; at Chaftarcillo, Chile, in fine crystals; common in the silver mines of Peru and Mexico. Found in Colorado in the silver mines of the San Juan Mountains and elsewhere; in various epithermal silver districts in Nevada, etc.

Handsome crystal specimens of proustite occur at Freiberg and other places in Saxony, at Wolfach in Baden, at Markirchen in Alsace and at Chanarcillo in Chile. It is associated with pyrargyrite and with other ores of silver. In parts of the western United States it is quite abundant, more particularly in the Ruby district, Colorado, at Poorman lode in Idaho, and in all other localities where pyrargyrite occurs. In some locations it is an important silver ore.

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Please note that the author, Chris Ralph, retains all copyrights to this entire document and it may not be reproduced, quoted or copied without permission.

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