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The Broadlaw “Granite”

Published online by Cambridge University Press:  01 May 2009

D. D. C. Pochin Mould
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Extract

The Broadlaw “Granite” is one of the small granitic intrusions of Caledonian age found in the eastern part of the Southern Uplands of Scotland. It is situated on the north-west flank of Broadlaw in the Moorfoot Hills, three miles south-west of Middleton House.

Type
Articles
Information
Geological Magazine , Volume 84 , Issue 3 , June 1947 , pp. 178 - 180
Copyright
Copyright © Cambridge University Press 1947

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References

REFERENCES

Lovegrove, E. J., and Waller, Page, 1929. Attrition Tests of British Roadstones. Mem. Geol. Survey, Nos. 221 and 221a, pp. 20–1, 62–3.Google Scholar
MacGregor, A. G., 1945. The Mineral Resources of the Lothians. Wartime Pamphlet, Geol. Survey, pp. 25, 26.Google Scholar
Pringle, J., 1935. The South of Scotland. British Regional Geology, p. 96.Google Scholar
Walker, F., 1925. Four Granitic Intrusions in South-Eastern Scotland. Trans. Edinb. Geol. Soc., xi, part iii, 357–365.CrossRefGoogle Scholar
Walker, F., 1928. The Plutonic Intrusions of the Southern Uplands East of the Nith Valley. Geol. Mag, lxv, 153–162.CrossRefGoogle Scholar