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IV.—On a New Locality for the Arctic Fauna of the “Basement” Boulder Clay in Youkshire1

Published online by Cambridge University Press:  01 May 2009

G. W. Lamplugh
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Extract

During the course of a systematic investigation of the drifts of Flamborough Head, I have somewhat unexpectedly come across a fragment of marine Arctic beds enclosed in Boulder-clay, similar to those which form the well-known fossiliferous deposits of Bridlington and Dimlington; and as this occurs under very different conditions from those already described, it adds materially to our knowledge of the beds, and illustrates more clearly their origin.

Type
Original Articles
Information
Geological Magazine , Volume 7 , Issue 2 , February 1890 , pp. 61 - 70
Copyright
Copyright © Cambridge University Press 1890

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Footnotes

1

Read at the Brit. Assoc. Newcastle, before Section C (Geology), Sept. 1889.

References

page 61 note 2 For description of the Bridlington and Dimlington beds see Reid's, Clement Survey Memoir on Holderness, pp. 8–26Google Scholar, and my papers in Geol. Mag. Dec. II. Vol. VIII. pp. 535–546, 1881Google Scholar; and Q.J.G.S. vol. xl. p. 312, 1884Google Scholar.

page 61 note 3 These sections have already attracted some attention from geologists, and are mentioned by Phillips, J., Geol. of Yorksh. pt. i. 3rd ed. p. 91Google Scholar; Reade, T. Mellard, A Traverse of the Yorkshire Drift, Proc. Liverpool Geol. Soc. 1882–1883, p. 11Google Scholar; Wood, and Rome, , Q.J.G.S. vol. xxiv. p. 180Google Scholar; and Dakyns, J. R., Prpc. Yorks. Geol. and Polyt. Soc. vol. vii. p. 249 (1880)Google Scholar.

page 64 note 1 Q.J.G.S. vol. xl. p. 317Google Scholar.

page 67 note 1 Survey Memoirs: “Cromer,” p. 90Google Scholar, and “Holderness,” p. 43Google Scholar.

page 70 note 1 See Report on Buried Cliff at Sewerby, British Association for 1888 (p. 33)Google Scholar