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Rammelsbergite from the southern uplands of Scotland

Published online by Cambridge University Press:  14 March 2018

A. K. Temple
A. K. Temple*
Affiliation:
Department of Geology, University of Leeds
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Extract

During an investigation of the mineralization of the Leadhills- Wanlockhead lead and zinc mining district, rammelsbergite (NiAs2) was identified as an associate of niceolite (NiAs), reputed to have come from no. 4 level on the west branch of the New Glencrieff vein. The identification was confirmed on further material collected from the dumps at the Glenerieff mine, Wanlockhead, Dumfriesshire, and on specimens from the Scottish Mineral Collection (nos. 1952.5.18; 20; 21).

Type
Research Article
Information
Mineralogical magazine and journal of the Mineralogical Society , Volume 30 , Issue 227 , December 1954 , pp. 541 - 543
Copyright
Copyright © 1954, The Mineralogical Society

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References

Notes

page 541 note 1 Brown, R., More about the mines and minerals of Wanlockhead and Leadhills. Trans. Dumfries. and Galloway Nat. Hist. Antiq. Soe., 1927. vol. 13 (for 1925-26), pp. 58.79 (p. 75. [M.A. 4-468.]Google Scholar

page 542 note 1 Uytenbogaardt, W., Tables for microscopic identification of ore minerals. Princeton and London, 1951. [M.A. 126 . ]Google Scholar

page 542 note 2 Goodchild, J.G., supplement in M.F. Heddle, The mineralogy of Scotland, 1901. vol. 2, p. 195. [M.A. 324.]Google Scholar