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The Raised Beaches of the North Coast of Sutherland, Scotland

Published online by Cambridge University Press:  01 May 2009

Cuchlaine A. M. King  and
P. T. Wheeler
Cuchlaine A. M. King
Affiliation:
Geography Department, The University, Nottingham.
P. T. Wheeler
Affiliation:
Geography Department, The University, Nottingham.
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Abstract

Measurements were made of features formed in relation to former sea-levels along the north coast of Sutherland between Melvich and Durness. The results suggest that four raised-levels can be identified. The uppermost, which is at a greater elevation on the east, is related to glacial and fluvio-glacial deposits, which indicate its formation in close proximity to glaciers. This level has been correlated with the “100 ft.” beach. The next level also shows slight tilting up to the east and seems to correspond with the “50 ft.” level elsewhere in Scotland. The two lowest levels are horizontal, and can be correlated with the “25 ft.” and “15 ft.” levels respectively.

Type
Articles
Information
Geological Magazine , Volume 100 , Issue 4 , August 1963 , pp. 299 - 320
Copyright
Copyright © Cambridge University Press 1963

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References

REFERENCES

Cadell, H. M., 1896. Geology and scenery of Sutherland. 2nd Edn. Edinburgh.Google Scholar
Charlesworth, J. K., 1954–1955. The late-glacial history of the Highlands and Islands of Scotland. Trans. roy. Soc. Edinb., 62, 769–928.CrossRefGoogle Scholar
Charlesworth, J. K., 1956. The Quaternary Era. London.Google Scholar
Crampton, C. B., and Carruthers, R. G., 1914. The geology of Caithness. Mem. geol. Surv. U.K.Google Scholar
Darling, F. Fraser, (Ed.), 1956. West Highland Survey. 2nd Edn., Oxford.Google Scholar
Donner, J. J., 1957. The geology and vegetation of late-glacial retreat stages in Scotland. Trans. roy. Soc. Edinb., 63, 221–261.CrossRefGoogle Scholar
Donner, J. J., 1959. The late-and post-glacial raised beaches in Scotland. Suomalaisen Tiedeakatemian Toimituksia Ann. Acad. Sci. Fennicae, III, Geol. Geog., 53, 5–25.Google Scholar
Durno, S. E., 1958, 1959. Pollen analysis in Sutherland and Caithness. Scot. geog. Mag., 74, 127–135, 75, 102–110.Google Scholar
Fairbridge, R. W., 1961. Eustatic changes in sea-level. From Physics and Chemistry of the Earth, Vol. 4, New York, 99–185.Google Scholar
Geikie, A., 1904. Presidential address of the Geological Society. Quart. J. geol. Soc. Lond., 60, lxxx–civ.Google Scholar
Ogilvie, A. G., 1923. The physiography of the Moray Firth coast. Trans. roy. Soc. Edinb., 53, 377–404.CrossRefGoogle Scholar
Reid, D. M., 1929. On a raised beach on the north coast of Scotland. Geol. Mag., 66, 177–180.CrossRefGoogle Scholar
Sissons, J. B., 1962. A re-interpretation of the literature on late-glacial shorelines in Scotland with particular reference to the Forth area. Trans. Edinb. geol. Soc., 19, 83–99.CrossRefGoogle Scholar
Synge, F. M., 1956. The glaciation of North-east Scotland. Scot. geog. Mag., 72, 129–143.Google Scholar
Valentin, H., 1953. Present vertical movements of the British Isles. Geog. Journ., 119, 299–305.CrossRefGoogle Scholar
Wright, W. B., 1936. The Quaternary Ice-age. 2nd Edn., London.Google Scholar