Sylvanite

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Sylvanite
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Sylvanite from the Cripple Creek mining district
General
Category Telluride mineral
Formula
(repeating unit)
(Ag,Au)Te2
Strunz classification 02.EA.05
Identification
Formula mass 429.89 gm
Color Silver-grey, Silver-white
Crystal habit Massive to Crystalline
Crystal system Monoclinic - Prismatic
Cleavage Perfect on the {010}
Fracture Uneven
Tenacity Brittle
Mohs scale hardness 1.5-2
Luster Metallic
Streak steel grey
Diaphaneity opaque
Specific gravity 8.2
Density 8.1
Optical properties Anisotropic
Pleochroism None
Ultraviolet fluorescence None
References [1][2][3]

Sylvanite or silver gold telluride, (Ag,Au)Te2, is the most common telluride of gold.

Properties

The gold:silver ratio varies from 3:1 to 1:1. It is a metallic mineral with a color that ranges from a steely gray to almost white. It is closely related to calaverite, which is more purely gold telluride with 3% silver. Sylvanite crystallizes in the monoclinic 2/m system. Crystals are rare and it is usually bladed or granular. It is very soft with a hardness of 1.5 - 2. It has a high relative density of 8 - 8.2. Sylvanite is photosensitive and can accumulate a dark tarnish if it is exposed to bright light for too long.

Occurrence

Sylvanite is found in Transylvania, from which its name is partially derived.[4] It is also found and mined in Australia in the East Kalgoorlie district. In Canada it is found in the Kirkland Lake Gold District, Ontario and the Rouyn District, Quebec. In the United States it occurs in California and in Colorado where it was mined as part of the Cripple Creek ore deposit. Sylvanite is associated with native gold, quartz, fluorite, rhodochrosite, pyrite, acanthite, nagyagite, calaverite, krennerite, and other rare telluride minerals. It is found most commonly in low temperature hydrothermal vein deposits.

Use

Sylvanite represents a minor ore of gold and tellurium.

References

  • Hurlbut, Cornelius S.; Klein, Cornelis, 1985, Manual of Mineralogy, 20th ed., ISBN 0-471-80580-7

External links

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