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The Base of the Devonian, with special reference to the Welsh Borderland.

Published online by Cambridge University Press:  01 May 2009

L. Dudley Stamp
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Extract

The classification set forth in this paper is founded essentially on an examination of the junction-beds between the Silurian and the Devonian in the field. All the localities described have been studied personally by the writer, and in most cases the actual junction has been mapped on the 6-inch scale. The names of localities are taken from the 6-inch Ordnance Survey maps, the sheet number being quoted in each case.

Type
Original Articles
Information
Geological Magazine , Volume 60 , Issue 7 , July 1923 , pp. 331 - 336
Copyright
Copyright © Cambridge University Press 1923

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References

page 333 note 1 Lapworth, & Watts, , “Shropshire” in “Geology in the Field”: Jub. Vol. Geol. Assoc., 1910, p. 756.Google Scholar

page 333 note 2 Elles, & Slater, , op. cit., p. 204.Google Scholar

page 333 note 3 Stamp, , op. cit., supra, 1918.Google Scholar

page 334 note 1 Trans. Caradoc Field Club, vol. i, pt. iv, issued for 1896, 1897, pp. 181–3.Google Scholar

page 334 note 2 In this and all other tabulated successions the rocks are Downtonian unless otherwise stated.

page 335 note 1 Op. cit., p. 209.Google Scholar

page 335 note 2 To economize space by avoiding the repetition of fossil names, the fossils recorded are indicated by numbers referring to the lists in a later section.

page 336 note 1 Stamp, , op. cit., 1918, p. 238.Google Scholar