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V.—The Neolithic Remains of Colonsay, in the Western Isles of Scotland1

Published online by Cambridge University Press:  01 May 2009

W. B. Wright  and
Angus M. Peach
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Extract

The more exact investigation of the distribution and mode of occurrence of Neolithic remains has received a much needed stimulus from the publication of Professor Brögger's memoir dealing with the position of the strandlines in South-Eastern Norway during the stone age of that country. It has been clearly demonstrated in this important work that it is possible to distinguish, even in the relatively short-lived Neolithic culture, certain phases of chronological value, and to correlate these phases, by means of the distribution of the implements which characterize them, with the successive stages in the elevation of the land which affected Scandinavia in postglacial times. It has become clear, therefore, that the careful registration and description of Neolithic relics may lead to the most important scientific results, and it will be realized by all who indulge in archæological collecting that an exact determination of the locality of any find and of the relations it bears to the superficial deposits of the neighbourhood, more especially to the old shorelines which border the coasts of the British Isles, is of the utmost importance.

Type
Original Articles
Information
Geological Magazine , Volume 8 , Issue 4 , April 1911 , pp. 164 - 175
Copyright
Copyright © Cambridge University Press 1911

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Footnotes

1

Published by permission of the Director of the Geological Survey of Great Britain.

References

page 164 note 2 Brögger, W. C., “Strandliniens Beliggenhed under Stenalderen i det Sydöstlige Norge”: Norges Geol. Undersögelse, No. 41, 1905.Google Scholar

page 165 note 1 Noyer, G. V. Du, “On Flint Flakes from Carrickfergus and Larne”: Q.J.G.S., vol. xxv, p. 48, 1869.Google Scholar

page 165 note 2 Proc. Belfast, Nat. Field Club (2), iii, pp. 198–210, 1890.Google Scholar

page 165 note 3 Coffey, George & Praeger, R. Lloyd, “The Larne Raised Beach, a Contribution to the Neolithic History of the North of Ireland”: Proc. Roy. Irish Acad., vol. xxv, section C, p. 146, 1904.Google Scholar

page 166 note 1 Lamplugh, G. W., “The Geology of the Isle of Man”: Mem. Geol. Survey U.K., 1903, p. 403.Google Scholar

page 166 note 2 Mem. Geol. Survey Scot., Explanation of Sheet 31, Edin., 1879, p. 54.Google Scholar

page 167 note 1 Grieve, Symington, “Notice of the Discovery of Remains of the Great Auk or Garefowl (Alca impennis) on the Island of Oronsay, Argyllshire”: Journ. Linn. Soc., Zoology, vol. xvi, p. 479, 1883.Google Scholar

page 169 note 1 In connexion with this account of the circumstances of the find, however, it must be noted that even with an excessive estimate of the size of the outlet and of the rate of flow in it the surface of the lake could not have been lowered anything like 2 feet in less than twenty-four hours.

page 170 note 1 Brögger, W. C., “Strandliniens Beliggenhed under Stenalderen i det Sydöstlige Norge”: Norges Geologiske Undersögelse, No. 41; Kristiania, 1905.Google Scholar

page 170 note 2 We have found a small scraper at about the same level in the Kiloran sand-hills and two worked fragments of flint on the surface of the ‘25-foot’ beach in Port nan Fliuchan (Uragaig), as well as some rude chips on the links near Machrins. The latter are not obviously Neolithic, and none of the other cases are good enough to give much assistance.

page 171 note 1 Mr. T. C. Cantrill informs me that he has found a number of such elongated pebbles, averaging 6 inches in length, on flint chipping-floors in Pembrokeshire, and believes they are flaking-tools.

page 174 note 1 Hoernes, Moriz, Der Diluviale Mensch in Europa; Brunswick, 1903.Google Scholar