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Relations of Torridonian to Durness Limestone in the Broadford–Strollamus district of Skye

Published online by Cambridge University Press:  01 May 2009

E. B. Bailey
E. B. Bailey
Affiliation:
19 Greenhill Gardens, Edinburgh.
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Abstract

Evidence strongly suggests that the Durness Limestone in Skye is a great thrust-slice between Torridonian above, at Broadford, and Torridonian below, at Strollamus and Scalpay.

Type
Articles
Information
Geological Magazine , Volume 91 , Issue 1 , February 1954 , pp. 73 - 78
Copyright
Copyright © Cambridge University Press 1954

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References

REFERENCES

Clough, C. T., 1907. See Peach and Others.Google Scholar
Clough, C. T., and Others, 1910. The Geology of Glenelg, Lochalsh and South-East Part of Skye (Sheet 71), Mem. Geol. Surv.Google Scholar
Geikie, A., 1888. On the Age of the Altered Limestone of Strath, Skye. Quart. Journ. Geol. Soc., xliv, 62.CrossRefGoogle Scholar
Geikie, A., 1896. Annual Report for 1895. Mem. Geol. Surv.Google Scholar
Harker, A., 1910. See Clough and Others.Google Scholar
King, B. C., 1953. Structure and Igneous Activity in the Creag Strollamus Area of Skye. Trans. Roy. Soc. Edinb., lxii, 357.Google Scholar
Peach, B. N., and Others, 1907. The Geological Structure of the North-West Highlands of Scotland. Mem. Geol. Surv.Google Scholar