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XVI.—The Tertiary Geology of Raasay, Inner Hebrides

Published online by Cambridge University Press:  06 July 2012

Extract

Raasay, one of the major islands of the Inner Hebrides, lies between the Isle of Skye, from which it is separated by the Sound of Raasay, on the west, and the mainland district of Applecross on the east. From Rudha na Cloiche, the southernmost promontory, to Rudha nan Sgarbh in the extreme north, the island has a length of over 13 miles, while the breadth from west to east varies from 3 miles near Ósgaig to a ½ mile just south of Arnish or at An Caol. The total surface area is about 27 square miles. The island is separated from Rona on the north by Caol Rònach, studded with islets and submerged rocks, a little more than a mile wide.

Type
Research Article
Copyright
Copyright © Royal Society of Edinburgh 1935

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References

References to Literature

Allan, D. A., 1931. “A Nepheline-Basanite Sill at Fordell, Fife,” Proc. Liverpool Geol. Soc., vol. xv, p. 309.Google Scholar
Bailey, E. B., 1910. In “The Geology of East Lothian,” Mem. Geol. Surv. Scotland.Google Scholar
Bailey, E. B., Thomas, H. H., and others, 1924. “The Tertiary and Post-Tertiary Geology of Mull, etc.,” Mem. Geol. Surv. Scotland.Google Scholar
Barth, T. F. W., 1931. “Mineralogical Petrography of Pacific Lavas,” Amer. Journ. Sci., vol. xxi, ser. 5, pp. 377, 491.Google Scholar
Bowen, N. L., 1927. “The Origin of Ultra-Basic and Related Rocks,” Amer. Journ. Sci., vol. xiv, ser. 5, p. 89.Google Scholar
Bowen, N. L., 1928. The Evolution of the Igneous Rocks, Princeton.Google Scholar
MissCargill, H. K., Hawkes, L., and Miss Ledeboer, J. A., 1928. “The Major Intrusions of South-Eastern Iceland,” Quart. Journ. Geol. Soc., vol. lxxxiv, p. 505.Google Scholar
Daly, R. A., 1924. “The Geology of American Samoa,” Carnegie Inst. Washington, publ. 340.Google Scholar
Davidson, C. F., 1932. “An Olivine-Bearing Conglomerate from the Island of Raasay, Inverness-shire,” Geol. Mag., vol. lxix, p. 272.Google Scholar
Day, A. L., Allen, E. T., and Iddings, J. P., 1905. “The Isomorphism and Thermal Properties of the Feldspars,” Carnegie Inst. Washington, publ. 31.Google Scholar
Eyles, V. A., and MacGregor, A. G., 1923. In Summ. Prog. Geol. Surv., 1922, p. 94.Google Scholar
Fenner, C. N., 1926. “The Katmai Magmatic Province,” Journ. Geol., vol. xxxiv, p. 673.Google Scholar
Flett, J. S., 1911. In “The Geology of Knapdale, Jura, and North Kintyre,” Mem. Geol. Surv. Scotland.Google Scholar
Flett, J. S., 1931. “The Saline No. 1 Teschenite,” Summ. Prog. Geol. Surv., 1930, pt. ii, p. 44.Google Scholar
Geikie, A., 1897. The Ancient Volcanoes of Great Britain, 2 vols., London (vol. ii).Google Scholar
Goranson, R. W., 1932. “Some Notes on the Melting of Granite,” Amer. Journ. Sci., vol. xxiii, ser. 5, p. 227.Google Scholar
Greig, J. W., Shepherd, E. S., and Merwin, H. E., 1931. “Melting Temperatures of Granite and Basalt,” Carnegie Inst. Washington, Year Book, No. 30.Google Scholar
Miss Guppy, E. M., and Hawkes, L., 1925. “A Composite Dyke from Eastern Iceland,” Quart. Journ. Geol. Soc., vol. lxxxi, p. 325.Google Scholar
Harker, A., 1906. “The Tertiary Igneous Rocks of Skye,” Mem. Geol. Surv. Scotland.Google Scholar
Harker, A., 1908. “The Geology of the Small Isles of Inverness-shire,” Mem. Geol. Surv. Scotland.Google Scholar
Harker, A., 1909. The Natural History of the Igneous Rocks, London.Google Scholar
Harker, A., 1917. “Some Aspects of Igneous Action in Britain,” Pres. Address, Geol. Soc, London, Quart. Journ. Geol. Soc., vol. lxxiii, p. lxvii.Google Scholar
Harker, A., 1932. Metamorphism, London.Google Scholar
Hawkes, L., 1929. “On a Partially Fused Quartz-Felspar Rock and on Glomero-Granular Texture,” Min. Mag., vol. xxii, p. 166.Google Scholar
Holmes, A., and Harwood, H. F., 1928. “The Age and Composition of the Whin Sill,” Min. Mag., vol. xxi, p. 538.Google Scholar
Horne, J., 1894. “On Two Volcanic Necks in Applecross, Ross-shire,” Trans. Edin. Geol. Soc., vol. vii, p. 35.Google Scholar
Jameson, R., 1800. Mineralogy of the Scottish Isles, 2 vols., London and Edinburgh (vol. ii).Google Scholar
Kennedy, W. Q., 1931. “On Composite Lava Flows,” Geol. Mag., vol. lxviii, p. 178.Google Scholar
Kennedy, W. Q., 1933. “Trends of Differentiation in Basaltic Magmas,” Amer. Journ. Sci., vol. xxv, ser. 5, p. 239.Google Scholar
Krokström, T., 1929. “Über Olivin aus Olivin-‘Bomben’ in einem Basalte aus Schonen,” Bull. Geol. Instn. Upsala, vol. xxii, p. 213.Google Scholar
Krokström, T., 1932. “The Breven Dolerite Dyke: A Petrogenetic Study,” Bull. Geol. Instn. Upsala, vol. xxiii, p. 243.Google Scholar
Lacroix, A., 1924. “Les laves analcimiques de l'Afrique du Nord, et d'une façon générale, la classification des laves renfermant de l'analcime,” C.R. Acad. Sci. Paris, clxxviii, p. 529.Google Scholar
Lee, G. W., 1920. “The Mesozoic Rocks of Applecross, Raasay, and North-East Skye,” Mem. Geol. Surv. Scotland.Google Scholar
Macculloch, J., 1819. A Description of the Western Isles of Scotland, 3 vols., London (vol. ii).Google Scholar
Nockolds, S. R., 1934. “The Production of Normal Rock Types by Contamination,” Geol. Mag., vol. lxxi, p. 31.Google Scholar
Peach, B. N., 1907. In “The Geology of the North-West Highlands of Scotland,” Mem. Geol. Surv. Scotland, p. 435.Google Scholar
Peacock, M. A., 1926. “The Geology of Viðey, S.W. Iceland,” Trans. Roy. Soc. Edin., vol. liv, p. 441.Google Scholar
Schaller, W. T., 1925. “The Genesis of Lithium Pegmatites,” Amer. Journ. Sci., vol. x, ser. 5, p. 269.Google Scholar
Teall, J. J. H., 1907. In “The Geology of the North-West Highlands of Scotland,” Mem. Geol. Surv. Scotland.Google Scholar
Tsuboi, S., 1932. “The Course of Crystallisation of Pyroxenes from Rock Magmas,” Japanese Journ. Geol. Geogr., vol. x, p. 67.Google Scholar
Tyrrell, G. W., 1928 a. “Dolerite Sills containing Analcite-Syenite in Central Ayrshire,” Quart. Journ. Geol. Soc., vol. lxxxiv, p. 540.Google Scholar
Tyrrell, G. W., 1928 b. “A Further Contribution to the Petrography of the Late Palæozoic Igneous Suite of the West of Scotland,” Trans. Geol. Soc. Glasgow, vol. xviii, p. 275.Google Scholar
Tyrrell, G. W., 1930. The Principles of Petrology. 2nd ed. London.Google Scholar
Vogt, J. H. L., 1931. “The Physical Chemistry of the Magmatic Differentiation of Igneous Rocks,” Part III (2), p. 125, Skr. Norske Vidensk. -Akad., Mat.-Naturv. Kl., 1930, No. 3.Google Scholar
Walker, F., and Irving, J., 1928. “The Igneous Intrusions between St Andrews and Loch Leven,” Trans. Roy. Soc. Edin., vol. lvi, p. 1.Google Scholar
Walker, F., 1930. “The Geology of the Shiant Isles,” Quart. Journ. Geol. Soc., vol. lxxxvi, p. 355.Google Scholar
Walker, F., 1931. “The Dolerite Isles of the North Minch,” Trans. Roy. Soc. Edin., vol. lvi, p. 753.Google Scholar
Walker, F., 1932. “Differentiation in the Sills of Northern Trotternish, Skye,” Trans. Roy. Soc. Edin., vol. lvii, p. 241.Google Scholar
Walker, F., 1934. “The Term ‘Crinanite,’” Geol. Mag., vol. lxxi, p. 122.Google Scholar
Woodward, H. B., 1914. “Notes on the Geology of Raasay,” Trans. Edin. Geol. Soc., vol. x, p. 164.Google Scholar
Wright, W. B., 1916. In “The Geology of Ben Nevis and Glen Coe,” Mem. Geol. Surv. Scotland.Google Scholar