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The Coastal Plateaux of South Wales

Published online by Cambridge University Press:  01 May 2009

Extract

A long the coast of South Wales is a series of plateaux, mostly at heights up to just over 400 feet above sea-level. They meet the coast in lines of cliffs, varied in character and often of great beauty. The most westerly area, in south and west Pembrokeshire, is the most perfectly developed, its level sky-line having been commented on by numerous writers (Dixon, 1921, p. 2; North, 1929, p. 23). The Gower peninsula, which is detached from the other coastal plateaux by Carmarthen and Swansea Bays, shows similar features, as does also the Vale of Glamorgan which stretches from the shores of Swansea Bay almost to Cardiff.

Type
Original Articles
Copyright
Copyright © Cambridge University Press 1934

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References

REFERENCES

Barbell, J. (1920). “The Piedmont Terraces of the Northern Appalachians”: American Journ. Sci., 4, xliv, 242.Google Scholar
Cantrill, T. C. (1912). In “ Geology of the South Wales Coalfield. Part III: The Country around Cardiff”: Mem. Geol. Surv., 2nd ed.Google Scholar
Challinor, J. (19291930). “The Hill-top Surface of North Cardiganshire”: Geography, p. 652.Google Scholar
Cox, A. H. (1920). In “Handbook to Cardiff and the Neighbourhood”: Brit. Assoc. Handbook (Cardiff).Google Scholar
Cox, A. H., Sibly, T. F., and Trueman, A. E. (1920). “Excursion to Cardiff”: Proc. Geol. Assoc., xxxi, 205.Google Scholar
Dewey, H. (1918). “On the Origin of some Land-forms in Caernarvonshire, North Wales”: Geol. Mag., 145.CrossRefGoogle Scholar
Dixon, E. E. L. (1921). “The Geology of the South Wales Coalfield. Pt. xiii: Pembroke and Tenby”: Mem. Geol. Surv.Google Scholar
Fridley, H. M. (1929). “Identification of Erosion Surfaces in South-Central New York”: Journ. Geol., xxxvii, 113.CrossRefGoogle Scholar
Fridley, H. M., and Nölting, J. P. (1931). “Peneplains of the Appalachian Plateau”: Journ. Geol., xxxix, 749.CrossRefGoogle Scholar
George, T. N. (1932). “The Quaternary Beaches of Gower”: Proc. Geol. Assoc., xliii, 291.CrossRefGoogle Scholar
George, T. N. (1933). “The Coast of Gower”: Proc. Swansea Sci. and Field Nat. Soc., i, 192.Google Scholar
Greenly, E. (1919). “The Geology of Anglesey”: Mem. Geol. Surv., vol. ii.Google Scholar
Jones, O. T. (1924). “The Upper Towy Drainage-System”: Quart. Journ. Geol. Soc., lxxx, 56.Google Scholar
Jones, O. T. (1930). “Some Episodes in the Geological History of the Bristol Channel Region”: Pres. Add. Sect. C., Rep. Brit. Assoc.. (Bristol) p. 57.Google Scholar
Jones, R. O. (1931). “The Development of the Tawe Drainage”: Proc. Geol. Assoc., xlii, 305.CrossRefGoogle Scholar
Jukes-Browne, A. J. (1907). “The Age and Origin of the Plateaux around Torquay”: Quart. Journ. Geol. Soc., lxiii, 106.CrossRefGoogle Scholar
North, F. J. (1929). “The Evolution of the Bristol Channel, with special reference to the coast of South Wales”: Nat. Mus. Wales.Google Scholar
Strahan, A. (1907). “The Geology of the South Wales Coalfield. Part VII: The Country around Swansea”: Mem. Geol. Surv.Google Scholar
Trueman, A. E. (1922). “The Liassic Rocks of Glamorgan”: Proc Geol. Assoc., xxxiii, 245.CrossRefGoogle Scholar
Trueman, A. E. (1924). “The Geology of the Swansea District”: Proc Geol. Assoc., xxxv, 283.CrossRefGoogle Scholar
Wooldridge, S. W. (1928). “The 200-foot Platform in the London Basin”: Proc Geol. Assoc., xxxix, 1.CrossRefGoogle Scholar