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XXX.—Geology of the Outer Hebrides. Part II.—South Uist and Eriskay

Published online by Cambridge University Press:  06 July 2012

T. J. Jehu  and
R. M. Craig
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Extract

The origin of the name “Uist” or “Vist” is uncertain. It is probably either of Pictish or Scandinavian derivation. It is said to be found amongst the names of the early Pictish kings. Some authorities give “Ivist” as the earliest known name, and this may mean “Ey-vist,” the Island of Vist (the Pictish king), or may be rendered literally from the Norse as “dwelling-place.” Others believe that the name is derived from “vest” (Danish) signifying “the west island.” Originally Uist comprised what we now know as North Uist, Benbecula, South Uist, and possibly Barra as well.

Type
Research Article
Information
Earth and Environmental Science Transactions of The Royal Society of Edinburgh , Volume 53 , Issue 3 , 1925 , pp. 615 - 641
Copyright
Copyright © Royal Society of Edinburgh 1925

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References

page 615 note * History of the Outer Hebrides, by W. C. Mackenzie, 1903, p. xxxix.

page 615 note † A Description of the Western Isles of Scotland, by Macculloch, John, 1819, vol. i, p. 91Google Scholar.

page 619 note * “Geology of the Outer Hebrides. Part I.—The Barra Isles.” Professor Jehu, and Craig, R. M.. Trans. Roy. Soc. Edin. vol. liii, pp. 422–423Google Scholar.

page 619 note † A Description of the Western Isles of Scotland, 1819, vol. i, pp. 95–98Google Scholar.

page 620 note * A Vertebrate Fauna of the Outer Hebrides, by J. A. Harvie-Brown and T. E. Buckley, with notes by Professor Heddle, 1888, p. 236.

page 620 note † The Great Ice Age, 3rd ed., 1894, pp. 52, 156, 261.

page 620 note ‡ Third Edition, 1901, p. 118.

page 623 note * “The Geology of the Outer Hebrides. Part I.—The Barra Isles,” Trans. Roy. Soc. Edin., vol. liii, p. 424Google Scholar.

page 627 note * Mem. Geol. Survey, “The Geology of Ben Wyvis, Carn Chunneag, etc.,” 1912, p. 126; Mem. Geol. Survey, “The Geological Structure of the North-West Highlands of Scotland,” 1907, p. 142.

page 630 note * Aggregation and Flow of Solids, Macmillan & Co., 1921Google Scholar.

page 630 note † “Heat of Crystallisation of Quartz,” Proc. Roy. Soc., Series A, vol. ci, No. 713, pp. 509–516, 1922Google Scholar; “The Effect of Long Grinding on Quartz (Silver Sand),” Proc. Roy. Soc., Series A, vol. cii, No. 718, pp. 640–642, 1923Google Scholar.

page 630 note ‡ “Fusion of Sedimentary Rocks in Drill-Holes,” Bull. Geol. Soc. Arner., vol. xxxiv, part 3, pp. 431–448, 1923Google Scholar.

page 633 note * Summary of Progress of the Geological Survey of Great Britain for 1906 (London 1907)Google Scholar. Cf. also J. S. Flett, “On the Petrographical Characters of the Inliers of Lewisian Rocks among the Moine Gneisses of the North of Scotland.” Ibid., p. 155.

page 635 note * There is no evidence in the field as to the age of these dykes. They are obviously later than the movements which have affected the Archæan Complex. The presumption is that they are of Tertiary Age, as the trend is in the same direction as the other later dykes, and they are just as fresh in appearance.