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File:Sylvanite ((Au,Ag)2Te4), Cripple Creek Diatreme.jpg

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Summary

Description

Sylvanite ((Au,Ag)2Te4) (silver-colored) from the Cripple Creek Diatreme (Early Oligocene, 32 Ma) of central Colorado, USA (ER # 1956, Ed Raines loan to Colorado School of Mines Geology Museum, Golden, Colorado, USA).

The Cripple Creek Gold District of central Colorado, USA is famous for its unusual gold and silver mineralization. Precious metal mineralization occurs in the Cripple Creek Diatreme, the root zone of a deeply eroded volcano dating to the Early Oligocene (32 Ma).

The dominant lithology at Cripple Creek is the scarce igneous rock phonolite, an alkaline, intermediate, extrusive igneous rock. Cripple Creek gold can be found in its native state (Au), but it typically occurs in the form of gold telluride minerals (for example, sylvanite - (Au,Ag)2Te4, calaverite - AuTe2, petzite - Ag3AuTe2, krennerite - (Au,Ag)Te2, and nagyagite - Pb5Au(Sb,Bi)Te2S6). Silver also occurs in some Cripple Creek minerals, including sylvanite, petzite, krennerite, hessite - Ag2Te, tennantite - (Cu,Ag,Fe,Zn)12As4S13, acanthite - Ag2S, and tetrahedrite - (Cu,Fe,Ag,Zn)12Sb4S13.
Date
Source Sylvanite ((Au,Ag)2Te4), Cripple Creek Diatreme (Early Oligocene, 32 Ma), central Colorado
Author James St. John

Licensing

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attribution
This file is licensed under the Creative Commons Attribution 2.0 Generic license.
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This image was originally posted to Flickr by jsj1771 at https://www.flickr.com/photos/47445767@N05/14733661181. It was reviewed on 1 August 2014 by FlickreviewR and was confirmed to be licensed under the terms of the cc-by-2.0.

1 August 2014

Captions

Sylvanite sample

Items portrayed in this file

depicts

25 July 2007

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200 millimetre

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Date/TimeThumbnailDimensionsUserComment
current22:44, 31 July 2014Thumbnail for version as of 22:44, 31 July 20141,750 × 1,099 (1.6 MB)TillmanTransferred from Flickr via Flickr2commons
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