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Neoglyphioceras cf. spirale (Phillips) from Ingleborough

Published online by Cambridge University Press:  01 May 2009

William Hopkins
William Hopkins
Affiliation:
Geology Department, University Science Laboratories, Durham.
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Abstract

The occurrence of a goniatite horizon in the Yoredale Series exposed on Ingleborough can now be recorded. The goniatite, Neoglyphioceras cf. spirale (Phillips) was found in shales underlying a limestone which may probably be the Five Yard.

Type
Articles
Information
Geological Magazine , Volume 93 , Issue 2 , April 1956 , pp. 173 - 174
Copyright
Copyright © Cambridge University Press 1956

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References

REFERENCES

Dakyns, J. R., Tiddeman, R. H., Gunn, W., and Strahan, A., 1890. The Geology of the country around Ingleborough, etc. Mem. Geol. Surv.Google Scholar
Hughes, McKenny T., 1908. Ingleborough, Part VI. The Carboniferous Rocks. Proc. Yorks. Geol. Soc., xvi, 253–320.CrossRefGoogle Scholar
Rayner, D. H., 1953. The Lower Carboniferous Rocks in the north of England. Proc. Yorks. Geol. Soc., xxviii, 231–315.CrossRefGoogle Scholar
Dunham, K. C., Hemingway, J. E., Versey, H. C., and Wilcockson, W. H., 1953. A Guide to the Geology of the district round Ingleborough. Proc. Yorks. Geol. Soc., xxix, 77–115.CrossRefGoogle Scholar
Bisat, W. S., 1955. On Neoglyphioceras spirale (Phill.) and allied species. Publ. Ass. Étud. Paléont., xxi, 15–18.Google Scholar