Sylvanite or silver gold telluride, chemical formula (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.1 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. Sylvanium, an obsolete term for tellurium, derived its name from sylvanite.2
External links
Wikimedia Commons has media related to Sylvanite.Chisholm, Hugh, ed. (1911). "Sylvanite" . Encyclopædia Britannica (11th ed.). Cambridge University Press.
References
Jolyon, Ralph. "Sylvanite". mindat.org. Retrieved 18 January 2013. http://www.mindat.org/min-3849.html ↩
Klein, Cornelis (1985), Hurlbut, Cornelius S. (ed.), Manual of Mineralogy: (after James D. Dana) (20th ed.), Albuquerque, US-NM: Wiley, p. 290, ISBN 0-471-80580-7, retrieved 2017-06-28 0-471-80580-7 ↩