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XXX.—The Dolerite Isles of the North Minch

Published online by Cambridge University Press:  06 July 2012

Frederick Walker
Affiliation:
Lecturer in Geology, University of St Andrews.

Extract

North of Skye the waters of the Minch conceal Tertiary igneous rocks, probably of great interest, the nature of which may be surmised only from the study of a few small skerries or islands projecting above sea-level. The group of the Shiant Isles is the best known and most interesting of these, and has been described elsewhere; but the more southerly islets, which form the subject of the present communication, are not without importance in themselves, besides forming a useful geological connecting link between the Shiants and Trotternish. As shown in the sketch map (fig. 1), they comprise the little archipelago a league off the Trotternish coast, which will be referred to as the Fladda group; the island of Trodday, two miles north-east of Rudha Hunish in Skye, and three small rocks or skerries lying close to the track of the Harris mail steamer.

Type
Research Article
Copyright
Copyright © Royal Society of Edinburgh 1931

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References

page 753 note * Walker, F., Q.J.G.S., vol. lxxxvi (1930), pp. 355–98CrossRefGoogle Scholar.

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page 758 note † Mem. Geol. Surv., “Colonsay,” 1911, p. 35.

page 760 note * F. Walker, op. cit., p. 370.

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page 762 note * Cf. Tyrrell, G. W., Geol. Mag., 1915, p. 309Google Scholar).

page 762 note † F. Walker, op. cit., p. 392.

page 764 note * F. Walker, op. cit., pp. 373–7.

page 764 note † Tyrrell, G. W., Q.J.G.S., vol. lxxxiv (1928), p. 566Google Scholar.

page 765 note * Harker, A., Mem. Geol. Surv., “The Tertiary Igneous Rooks of Skye,” 1904, p. 237Google Scholar.

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