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A note on the structure and succession at Abereiddy Bay, Pembrokeshire

Published online by Cambridge University Press:  01 May 2009

A. C. Waltham
A. C. Waltham
Affiliation:
Geology Department, Trent Polytechnic, Nottingham
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Summary

A study of the Ordovician rocks on the northern side of Abereiddy Bay has revealed that the succession is locally overturned. Consequently the stratigraphic levels of two horizons are reassessed—the Castell Limestone is placed above the Dicranograptus Shale, and the Llanrian Volcanic Series is allocated to the Lower Llanvirnian.

Type
Articles
Information
Geological Magazine , Volume 108 , Issue 1 , January 1971 , pp. 49 - 52
Copyright
Copyright © Cambridge University Press 1971

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References

Cantrill, T. C. & Thomas, H. H. 1909. Geology of the country around Carmarthen. Mem. geol. Surv. U.K. (Sheet 229).Google Scholar
Cox, A. H. 1915. The geology of the district between Abereiddy and Abercastle (Pembrokeshire). Q. Jl geol. Soc. Lond. 71, 273.CrossRefGoogle Scholar