A pale brass-yellow to silver-white ore of gold and silver, chiefly (Au,Ag)Te2.
[French, after TRANSYLVANIA.]
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A pale brass-yellow to silver-white ore of gold and silver, chiefly (Au,Ag)Te2.
[French, after TRANSYLVANIA.]
Environment
Rare; in late low-temperature precious metal ore veins.
Crystal descriptionUsually in crystals, deeply striated, elongated parallel to a horizontal axis. Commonly twinned and difficult to orient; structurally a real challenge. Also granular and massive.
Physical propertiesPale brass yellow to silver-white. Luster metallic; hardness 2Ɖ specific gravity 8.2 (sylvanite) to 9.3 (calaverite); fracture uneven; cleavage none or (sylvanite) a side pinacoid cleavage. Brittle.
CompositionInseparable tellurides of gold and of silver (44.03% Au, 55.97% Te). Calaverite becomes sylvanite when 13.4% of its gold is replaced by silver.
TestsGives ice blue tint to flames flaring from bead on charcoal, eventually shrinking into a gold button. A higher silver content of sylvanite makes bead whiter.
Distinguishing characteristicsThe deeply striated, elongated, and flat-lying crystals are unmistakable; they are usually the lone metallic glints on specimens. The gold assay bead is easy to obtain and can hardly be misidentified.
OccurrenceCalaverite is a rare mineral, but an important ore of gold in Kalgoorlie, Western Australia; Calaveras Co., California; and Cripple Creek, Colorado. In the veins it is associated only with sylvanite, other tellurides, tellurium, quartz, and fluorite, as a rule with no base metal ores. Cripple Creek was the only really spectacular occurrence of this mineral. Sylvanite is also found with related minerals in Nagyág and Offenbånya in Transylvania. "Blister-gold" specimens, sold long ago in Colorado to tourists as natural gold when Cripple Creek was in production, are actually examples of these two ores that were roasted to drive off the tellurium and bring bubbles of gold to the surface. The structure of these minerals has proved one of the most tantalizing problems that x-ray mineralogists have encountered. Current thinking has classified them as triclinic and twinned.
The noun has one meaning:
Meaning #1:
a silver-white mineral consisting of silver gold telluride; a source of gold in Australia and America
Synonym: graphic tellurium
Sylvanite or silver gold telluride, (Ag,Au)Te2, is the most common telluride of gold. 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. 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.
Sylvanite is found in Transylvania from which its name is derived. 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.
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![]() | Dictionary. The American Heritage® Dictionary of the English Language, Fourth Edition Copyright © 2007, 2000 by Houghton Mifflin Company. Updated in 2007. Published by Houghton Mifflin Company. All rights reserved. Read more | |
![]() | Rock & Mineral Guide. Peterson Field Guide to Rocks and Minerals, by Frederick H. Pough. Copyright © 1998 by Houghton Mifflin Company. Published by Houghton Mifflin Company. All rights reserved. Read more | |
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![]() | Wikipedia. This article is licensed under the GNU Free Documentation License. It uses material from the Wikipedia article "Sylvanite". Read more |
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