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An account of the struy lead mines, Inverness-shire, and of wulfenite, harmotome, and other minerals which occur there
Published online by Cambridge University Press: 14 March 2018
Extract
The Struy lead mines (Six-inch ordnance Survey, Inverness-shire, sheet 17) are situated on the west side of Strath Glass, about two miles south-west of Struy village, and comprise three distinct sets of small long-abandoned workings, two of them being in the nature of trials only. All three workings are shown on the six-inch map, and are on veins traversing the Moine schists. The Geological Survey Memoir of the district says that four veins may be traced on the hill face between the Dùn south of Struy school and Crelevan; if this is correct there are two outcrops I have not seen. The mines are on what was until a few years ago part of Lord Lovat's estate. The date of their discovery is not known, but they were apparently worked about the year 1818 by Thomas Alexander Fraser (afterwards 12th Lord Lovat) at the same time as his graphite mine in Strath Farrar; most of the work seems, however, to have been done by him between 1838 and 1845, when miners were brought from England and housed in cottages specially built for them in Struy village. In 1864 the Loch na Mèine workings were cleared and prospected, but since then no further work has been done.
- Type
- Research Article
- Information
- Mineralogical magazine and journal of the Mineralogical Society , Volume 27 , Issue 192 , March 1946 , pp. 147 - 154
- Copyright
- Copyright © The Mineralogical Society of Great Britain and Ireland 1946
References
page 147 note 1 Mem. Geol. Surv. Scotland, The Geology of the country round Beauly and Inverness, 1914, pp. 98–99.
page 147 note 2 The lead, zinc, copper and nickel ores of Scotland, 1921, pp. 108–109.
page 151 note 1 Axial ratios and letters for this and the other minerals here described as in Dana's System of mineralogy, 6th edition, 1892.
page 152 note 1 Lacroix, A., Minéralogie de la France et de ses Colonies. 1910, vol. 4, p. 9–73, fig. 7.Google Scholar