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IV.—On the Carboniferous Basement Beds at Ingleton

Published online by Cambridge University Press:  01 May 2009

Cosmo Johns
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Extract

During the Spring meeting of the Yorkshire Geological Society at Pateley Bridge it was suggested that, as a first step towards the zonal classification of the Lower Carboniferous rocks of Yorkshire, it would be desirable to determine the horizon of the basement beds at Ingleton as compared with the Avon sequence. As the Yorkshire Naturalists Union had arranged a meeting at Ingleton for May 12–14th, the geological route was arranged so as to include as many exposures of the basement beds as possible. The result of the observations made then and during subsequent visits is the subject of this communication.

Type
Original Articles
Information
Geological Magazine , Volume 3 , Issue 7 , July 1906 , pp. 320 - 323
Copyright
Copyright © Cambridge University Press 1906

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References

page 321 note 1 Quart. Journ. Geol. Soc., 1905, p. 181 et seqq.Google Scholar

page 321 note 2 Summary of Progress, 1904, p. 43.Google Scholar

page 321 note 3 Quart. Journ. Geol. Soc., 1906, p. 324 et seqq.Google Scholar

page 321 note 4 Wedd: Quart. Journ. Geol. Soc., 1906, p. 379.Google Scholar

page 321 note 5 Quart. Journ. Geol. Soc., 1906, p. 275 et seqq.Google Scholar

page 321 note 6 Trans. Leeds Geol. Assoc., part v, p. 26.

page 321 note 7 Quart. Journ. Geol. Soc., 1905, p. 263.Google Scholar

page 321 note 8 Ibid., p. 250.

page 321 note 9 Summary of Progress, 1904, p. 44.Google Scholar

page 321 note 10 Quart. Journ. Geol. Soc., 1906, p. 288.Google Scholar

page 322 note 1 Before a final opinion can be expressed as to the exact position which these beds occupy in the Avonian sequence, it will be necessary to have several of the corals sliced, and to study the Brachiopod fragments more minutely. I do not, however, anticipate that the result of such further work will in any way affect the main, conclusion which is here stated.

page 323 note 1 Summary of Progress, 1904, p. 44.Google Scholar

page 323 note 2 Quart. Journ. Geol. Soc., vol. lxii (1906), p. 285.Google Scholar