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The Ordovician and Associated Pre-Cambrian Rocks of the Pontesford District, Shropshire

Published online by Cambridge University Press:  01 May 2009

W. T. Dean  and
D. L. Dineley
W. T. Dean
Affiliation:
British Museum (Nat. Hist.), London, S.W. 7.
D. L. Dineley
Affiliation:
Dept. of Geology, University of Ottawa.
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Abstract

Following a recent re-mapping of the district east of Pontesford Hill, Shropshire, it now seems likely that the Uriconian and Longmyndian rocks at The Lyd Hole are faulted against one another, and that the Pontesford Shales form two outcrops, separated by faulting, and not a single outcrop as previously suggested. Doubt is cast on the validity of the so-called “rhyolite” of Habberley Brook, and the faunas and correlation of the Pontesford Shales are reviewed in the light of new evidence.

Type
Articles
Information
Geological Magazine , Volume 98 , Issue 5 , October 1961 , pp. 367 - 376
Copyright
Copyright © Cambridge University Press 1961

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References

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