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XIII.—On the Age of the Old Red Sandstone of Shetland

Published online by Cambridge University Press:  06 July 2012

Extract

In spite of its remote situation, the Old Red Sandstone of Shetland attracted a considerable amount of attention from geologists during the last century. It is exposed in excellent coast sections, which often yield very beautiful cliff scenery; and, in addition to being the most northerly of the stratified rocks of Great Britain, it includes a rich succession of volcanic and intrusive rocks which are of great interest and variety. The axis or backbone of the Shetland archipelago consists of gneiss, mica schist, slate, and limestone, with epidiorites, serpentine, and talc schists. On each side of this there is an area of Old Red Sandstone; that on the east extending from Sumburgh Head, in the extreme south, to Rovey Head, a little north of Lerwick, and comprising also the islands of Bressay, Noss, and Mousa. On the west side of Shetland the Old Red Sandstone Series is much altered, probably by the heat of the granite and other intrusive rocks, so that they often have the appearance of quartzite, and were for a long time regarded as belonging to the metamorphic series. In 1879, however, Peach and Horne (28) showed that, in places, they contained fossil plants which indicated that they belonged to the Old Red Sandstone formation.

Type
Research Article
Copyright
Copyright © Royal Society of Edinburgh 1909

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References

Literature

(1)Boué, Ami, Éssai Géologique sur l'Écosse, p. 114 (n.d. probably 1820).Google Scholar
(2)Fleming, J., Mem. Wernerian Soc., vol. i., p. 174 (1808).Google Scholar
(3)Flett, John S., “On the Discovery in Orkney of the John o'Groat's Horizon of the Old Red Sandstone,” Proc. Roy. Phys. Soc. Edin., vol. xiii., p. 255 (1896).Google Scholar
Flett, John S., “The Old Red Sandstone of the Orkneys,” Trans. Roy. Soc. Edin., vol. xxxix., p. 383 (1898).Google Scholar
(4)Flett, John S., “The Old Red Sandstone of the Orkneys,” Trans. Roy. Soc. Edin., vol. xxxix., p. 409 (1898).Google Scholar
(5)Geikie, A. Sir, Memoir of Sir R. Murchison, vol. i., p. 139 (1875).Google Scholar
(6)Geikie, A. Sir, “The Old Red Sandstone of Western Europe (Part I.),” Trans. Roy. Soc. Edin., vol. xxviii., p. 345 (1878).CrossRefGoogle Scholar
(7)Geikie, A. Sir, “The Old Man of Hoy,” Geol. Mag., p. 49 (1878).CrossRefGoogle Scholar
Geikie, A. Sir, Geological Sketches, p. 76 (1882).Google Scholar
(8)Geikie, A. Sir, Text-Book of Geology, p. 1010 (1903).Google Scholar
(9)Geikie, A. Sir, Geological Map of Scotland (published by Bartholomew, Edinburgh).Google Scholar
(10)Geikie, A. Sir, Trans. Roy. Soc. Edin., vol. xxviii., p. 418 (1878).Google Scholar
(11)Geikie, A. Sir, Text-Book of Geology, p. 1012 (1903).Google Scholar
(12)Gibson, George, The Old Red Sandetone of Shetland (1877).Google Scholar
(13)Heddle, M. F., Mineralogical Magazine, vol. ii. (1879).Google Scholar
(14)Hibbert, Samuel, A Description of the Shetland Islands, p. 160, etc. (1822).Google Scholar
(15)Hooker, Joseph D., “Note on the Fossil Plants from the Shetlands,” Quart. Jour. Geol. Soc., vol. ix., p. 49 (1853).Google Scholar
(16)Jameson, E., Outline of the Mineralogy of the Shetland Isles, p. 15, etc. (1798).Google Scholar
Jameson, E.The Mineralogy of the Scottish Isles, vol. ii., p. 195, etc. (1800 and 1813).Google Scholar
(17)Kidston, R., Catalogue of Palœozoic Plants in the British Museum, pp. 233 and 238 (1886).Google Scholar
(18)Mackie, W. S., Sand Grains, Elgin (1894).Google Scholar
(19)Memoirs of the Geological Survey of Scotland: “The Geology of Lower Strathspey.”Google Scholar
(20)Min. May., vol. ii., p. 156.Google Scholar
(21)Murchison, Roderick I. Sir, “Note on the Age and Relative Position of the Sandstone containing Fossil Plants in the Shetland Isles,” Quart. Jour. Geol. Soc., vol. ix., pp. 50 and 50 bis. (1853).CrossRefGoogle Scholar
(22)Murchison, Roderick I. Sir, “On the Succession of the Older Rocks in the Northernmost Counties of Scotland, with some Observations on the Orkney and Shetland Islands,” Quart. Jour. Geol. Soc., vol. xv., p. 353 (1859).CrossRefGoogle Scholar
(23)Murchison, Roderick I. SirSiluria (4th ed.), p. 259 (1867).Google Scholar
(24)Nature, Nov. 23, 1899, vol. lxi., p. 80.Google Scholar
(25)Neill, Patrick, A Tour through some of the Islands of Orkney and Shetland, p. 72, etc. (1806).Google Scholar
(26)Newberry, J. S., Palaeozoic Fishes of N. America, p. 92 (1889).CrossRefGoogle Scholar
(27)Peach, C. W., Quart. Jour. Geol. Soc., vol. xxxv., p. 811 (1879).Google Scholar
(28)Peach, B. N., and Horne, J., “The Glaciation of the Shetland Isles,” Quart. Jour. Geol. Soc., vol. xxxv., p. 778 (1879).CrossRefGoogle Scholar
(29)Peach, B. N., “The Old Red Volcanic Rocks of Shetland,” Trans. Roy. Soc. Edin., vol. xxxii., p. 359 (1884).CrossRefGoogle Scholar
(30)Peach, B. N., “The Geology of Shetland,” in Tudor's The Orkneys and Shetland (1883).Google Scholar
(31), Rupert Jones, T., Quart. Jour. Geol. Soc., vol. xv., p. 404.Google Scholar
Rupert Jones, T., On Fossil Estheriæ and their Distribution, Quart. Jour. Geol. Soc., vol. xix., p. 140 (1862).Google Scholar
Rupert Jones, T., “Monograph of the Fossil Estheriæ,” Palæontographical Society, p. 14 (1862).Google Scholar
Rupert Jones, T., Geol. Mag., 1890, pi. xii., and 1891, p. 50.Google Scholar
(32)Salter, J. W., “On some Remains of Terrestrial Plants in the Old Red Sandstone of Caithness,” Quart. Jour. Geol. Soc., vol. xiv., p. 72 (1858).CrossRefGoogle Scholar
(33)Sedgwick, A., and Murchison, R. I., “On the Structure and Relations of the Deposits contained between the Primary Rocks and the Oolitic Series in the North of Scotland,” Trans. Geol. Soc., ser. ii., Vol. iii., p. 125 (1828).Google Scholar
(34)Shirepp, , Agriculture of the Shetland Islands (1814).Google Scholar
(35)Traquair, R. H., “On Cephalaspis magnifica (Traq.),” Proc. Roy. Phys. Soc. Edin., vol. xii., p. 269 (1893).Google Scholar
(36)Traquair, R. H., “Notes on the Devonian Fishes of Scaumenac Bay and Campbelltown in Canada,” Geol. Mag. [3], vol. vii., 1890, p. 16.Google Scholar
(37)Tuffnell, Henry, “Notice of the Discovery of Fossil Plants in the Shetland Isles,” Quart. Jour. Geol. Soc., vol. ix., p. 49 (1853).Google Scholar