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III.—Notes on the Faunal Succession in the Carboniferous Limestone of Westmoreland and Neighbouring Portions of Lancashire and Yorkshire

Published online by Cambridge University Press:  01 May 2009

E. J. Garwood
E. J. Garwood
Affiliation:
Professor of Geology in University College, London.
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Extract

In August last, at the meeting of the British Association at York, I gave a general account of the zonal succession of the Carboniferous Limestone as developed in Westmoreland and North Lancashire, and I instituted a comparison with beds of a similar age in the Ingleborough and North Pennine districts.

Type
Original Articles
Information
Geological Magazine , Volume 4 , Issue 2 , February 1907 , pp. 70 - 74
Copyright
Copyright © Cambridge University Press 1907

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References

page 71 note 1 See Cosmo Johns & Vaughan: Geol. Mag., 1906.

page 71 note 2 Dr. Vaughan: Q.J.G.S., vol. lxi, p. 254, footnote.

page 71 note 3 T. F. Sibley: op. cit., vol. lxii, p. 376.

page 72 note 1 Kindly determined for me by Dr. Vaughan.

page 72 note 2 Lower Limestone Shales of the Government Map.

page 74 note 1 I here limit the term giganteus to the large coarse-ribbed forma found, as far as I am aware, only in the Dibtuiophyllum zone, and usually confined to the upper part of that zone.