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A Restudy of the Ingletonian Series of Yorkshire1

Published online by Cambridge University Press:  01 May 2009

G. P. Leedal  and
G. P. L. Walker
G. P. Leedal
Affiliation:
(Department of Geology, University of Leeds)
G. P. L. Walker
Affiliation:
(Department of Geology, University of Leeds)
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Abstract

A description of the Ingletonian Series is given, with special reference to the sedimentary structures which occur and their use in determining the nature of the folding of the beds; this is shown to be isoclinal. The age of the series is discussed, and it is considered to be in all probability Pre-Cambrian.

Type
Articles
Information
Geological Magazine , Volume 87 , Issue 1 , February 1950 , pp. 57 - 66
Copyright
Copyright © Cambridge University Press 1950

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Footnotes

1

Since this paper was written we have learnt that Dr. G. Bond has been working on the Ingletonian and has reached conclusions similar to our own. He has kindly withdrawn his claims in our favour.

References

REFERENCES

Bailey, E. B., 1934. West Highland tectonics: Loch Leven to Glen Roy. Quart. Journ. Geol. Soc., 90, 462–523.CrossRefGoogle Scholar
Green, J. F. N., 1917. Note on the correlation of the Ingletonian Slates. Proc. Geol. Assoc., 28, 95–7.CrossRefGoogle Scholar
Gunn, W., 1890. In The geology of the country around Ingleborough. Mem. Geol. Surv. England and Wales, 3–17.Google Scholar
Hudson, S. N., 1937. The volcanic rocks and minor intrusions of the Cross Fell Inlier, Cumberland and Westmorland. Quart. Journ. Geol. Soc., 93, 368–403.Google Scholar
Hughes, T. McK., 1902. Ingleborough. Part II. Stratigraphy. Proc. Yorks. Geol. Soc., xiv, 323–343.CrossRefGoogle Scholar
King, W. B. R., 1932. A fossiliferous limestone associated with Ingletonian beds at Horton-in-Ribblesdale, Yorkshire. Quart. Journ. Geol. Soc., 88, 100–108.CrossRefGoogle Scholar
King, W. B. R. and Wilcockson, W. H., 1934. The Lower Palaeozoic rocks of Austwick and Horton-in-Ribblesdale, Yorkshire. Quart. Journ. Geol. Soc., 90, 7–29.Google Scholar
Rastall, R. H., 1906. The Ingletonian Series of West Yorkshire. Proc. Yorks. Geol. Soc., xvi, 87–100.CrossRefGoogle Scholar
Shotton, F. W., 1935. The stratigraphy and tectonics of the Cross Fell Inlier. Quart. Journ. Geol. Soc., 91, 639–701.Google Scholar
Wood, A., 1948. An excavation revealing the junction between Ingletonian and Coniston Limestone at Ingleton. Geol. Mag., lxxxv, 33–4.Google Scholar