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The Geological Structure of Wirral

Published online by Cambridge University Press:  01 May 2009

David E. Owen
David E. Owen
Affiliation:
(Keeper of Geology, Liverpool Museums)
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Extract

The rocks of the Wirral Peninsula in Cheshire were originally described by John Cunningham in 1839, as three series, two moderately resistant to the east and the west, separated by a central region of soft sandstones and marls, dipping uniformly eastwards. G. H. Morton noted this in 1872, as a good description of the strata, ignoring faults, and pointed out the significance of the faulting. Since that date the faults have been mapped in great detail, and most of the structural features ascribed to them. G. H. Morton was particularly accurate with his mapping of faults both in Liverpool (1899), and in Storeton (G. H. Morton, 1883, and H. C. Beasley, 1914). The folding finds its first mention in the Geological Survey Memoir of 1923, two elongated synclines being mentioned, one from Heswall northwards and the other from Storeton to Prenton. The former is undoubtedly an important synclinal feature, but the latter is made up of two folds, a north to south anticline at Storeton, and an east to west syncline at Prenton. The only other records of folding in Wirral are by F. T. Maidwell in 1920 and by T. A. Jones in 1937, who mention an anticline at Ellesmere Port. This paper is therefore chiefly devoted to a description of the folding in the area.

Type
Articles
Information
Geological Magazine , Volume 83 , Issue 5 , October 1946 , pp. 230 - 236
Copyright
Copyright © Cambridge University Press 1946

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References

Beasley, H. C., and Lomas, J., 1892. On some East and West Faults at Caldy Grange. Proc. Liv. Geol. Soc., vi, 413–415.Google Scholar
Beasley, H. C., and Lomas, J., 1914. Note on a Map of the Faults in the Neighbourhood of Storeton made by the late Mr. G. H. Morton, F.G.S. Proc. Liv. Geol. Soc., xi, 311–316.Google Scholar
Cunningham, J., 1839. An Account of Footsteps of Cheirotherium and other unknown animals lately discovered in the Quarries of Storeton Hill, etc. Proc. Geol. Soc., iii, 12.Google Scholar
Jones, R. C. B., Tonks, L. H., and Wright, W. B., 1938. Wigan District. Memoirs of the Geological Survey.Google Scholar
Jones, T. A., 1937. Notes on the Geology of Ellesmere Port and Stanlow, Cheshire. Proc. Liv. Geol. Soc., xvii, 192–199.Google Scholar
Lomas, J., and Dwerryhouse, A. R., 1893. On some Faults exposed in Arno Quarry. Proc. Liv. Geol. Soc., vii, 118–120.Google Scholar
Maidwell, F. T., 1920. Some Borings through the Marshes bordering the Southern Shore of the Mersey Estuary. Proc. Liv. Geol. Soc., xii, 417–428.Google Scholar
Miller, A. A., 1938. Pre-Glacial Erosion Surfaces round the Irish Sea Basin. Proc. Yorks. Geol. Soc., xxiv, 31–59.CrossRefGoogle Scholar
Morton, G. H., 1863. The Geology of the Country around Liverpool. Liverpool,Google Scholar
Morton, G. H., 1872. Presidential Address. Proc. Liv. Geol. Soc., ii, 12th Session, 9–10.Google Scholar
Morton, G. H., 1883. Description of a Geological Map of the Storeton Quarries, Cheshire. Proc. Liv. Geol. Soc., iv, 406.Google Scholar
Morton, G. H., 1899. Description of a Geological Map of Liverpool. Proc. Liv. Geol. Soc., viii, 365–381.Google Scholar
Wedd, C. B., Smith, , Bernard, , Simmons, W. C., and Wray, D. A., 1923. The Geology of Liverpool with Wirral and part of the Flintshire Coalfield. Memoirs of the Geological Survey.Google Scholar