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Permafrost Structures on Sully Island, Glamorgan

Published online by Cambridge University Press:  01 May 2009

R. Bradshaw  and
D. Ingle Smith
R. Bradshaw
Affiliation:
Departments of Geology and Geography, University of Bristol.
D. Ingle Smith
Affiliation:
Departments of Geology and Geography, University of Bristol.
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Abstract

Folds in the uppermost 10 feet of Triassic rocks in the cliffs of Sully Island, Glamorgan, are described and their origin is related to processes operating when the area was subject to permafrost.

Type
Articles
Information
Geological Magazine , Volume 100 , Issue 6 , December 1963 , pp. 556 - 564
Copyright
Copyright © Cambridge University Press 1963

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References

Born, A., 1929. Über atektonische Faltung bei Kimberley, S.A.U.Z. dtsch. geol. Ges., 81, 540–541.Google Scholar
Campbell, M. R., 1906. Rock Folds due to Weathering. J. Geol., 14, 718–721.CrossRefGoogle Scholar
Curtis, L. F., and James, J. H., 1959. Frost Heaved Soil of Barrow, Rutland. Proc. Geol. Ass. Lond., 70, 310–314.CrossRefGoogle Scholar
Jones, F. O., 1907. Glacial Rock Sliding. J. Geol., 15, 485–487.CrossRefGoogle Scholar
Keilhack, K., 1931. Über „atektonische Faltung ” (Stiche) in der Trias des Harzvorlandes und über einen merkwurdigen Fall von Haken-schlagen. Z. dtsch. geol. Ges., 83, 184–189.Google Scholar
Kellaway, G. A., in discussion following Hawkins, H. L., 1952. A Pinnacle of Chalk penetrating the Eocene on the Floor of a buried river Channel at Ashford Hill, near Newbury, Berkshire. Quart. J. geol. Soc. Lond., 108, 233–260.Google Scholar
Krüger, H., 1933, Periglaziale Frostverwitterung im Bereich der Borgen-treicher Börde (zur Entstehung der ′ Stiche ”). Z. Geomorph., 7, 206–230.Google Scholar
Muller, S. W., 1947, Permafrost or Permanently Frozen Ground and Related Engineering Problems. Ann Arbor, Michigan, Edwards, J. W..Google Scholar
Müller, F., 1959. Beobachtungen über Pingos. Medd. Grønland, 153, n. 3, 1–127.Google Scholar
Paterson, T. T., 1940. The Effects of Frost Action and Solifluxion around Baffin Bay and in the Cambridge District. Quart. J. geol. Soc. Lond., 96, 99–130.CrossRefGoogle Scholar
Sardeson, F. W., 1905. A Particular Case of Glacial Erosion. J. Geol., 13, 351–357.CrossRefGoogle Scholar
Sardeson, F. W., 1906. The Folding of Subjacent Strata by Glacial Action. J. Geol., 15, 226–232.CrossRefGoogle Scholar
Schafer, J. P., 1949. Some Periglacial features in Central Montana. J. Geol., 57, 154–174.CrossRefGoogle Scholar
Slater, G., 1927. Studies in the Drift Deposits of the S.W. part of Suffolk. Proc. Geol. Ass. Lond., 38, 157–217.CrossRefGoogle Scholar
Strahan, A., and Cantrill, T. C., 1912. The Geology of the South Wales Coalfield, Part III, The County around Cardiff (Sheet 263). Mem. Geol. Surv., (2nd ed.).Google Scholar
Suslov, S. P., 1961. Physical Geography of Asiatic Russia (trans. Gershevsky, N. D.). San Francisco. W. H. Freeman and Co.Google Scholar
Te, Punga M. T., 1957. Periglaciation in Southern England. Tijdschr. Kon. Ned. Aardr. Gen., Dl. 64, 401–412.Google Scholar
Washburn, A. L., 1950. Patterned Ground. Rev. canad. Géogr., 4, 5–54.Google Scholar
Waters, R. S., 1960. Pre-Würm Periglacial Phenomena in Britain. Biuletyn Peryglacjalny, 9, 163–176.Google Scholar
Zaruba, Q., 1952. Frozen Ground Phenomena of Pleistocene Age and their Significance in Engineering Problems. Proc. Int. geol. Congress London, Pt. XIII, 264–269.Google Scholar