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II.—On the Occurrence of Freshwater Remains in the Boulder-clay at Bridlington

Published online by Cambridge University Press:  01 May 2009

Extract

On this part of the Yorkshire coast, the storms of last winter have often bared parts of the beach, for a time, of their usual covering of sand and shingle, and have thus exposed to observation many interesting features in connexion with the Drift series. Of these, the most instructive point which has come under my notice is the one which forms the immediate subject of the present communication.

Type
Original Articles
Copyright
Copyright © Cambridge University Press 1879

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References

page 393 note 1 Quart. Journ. Geol. Soe. vol. xxiv. p. 146.Google Scholar

page 393 note 2 Geol. Mao. 1878, p. 509; see also Note, p. 573.Google Scholar

page 396 note 1 Quart. Journ. Geol. Soc. 1870, vol. xxvi. p. 90.Google Scholar

page 396 note 2 GEOL. MAG. May, 1879, p. 238.Google Scholar

page 396 note 3 Quart. Journ. Geol. Soc. 1868, vol. xxiv. p. 149.Google Scholar

page 398 note 1 Quart. Journ. Geol. Soc. 1868, vol. xxiv. p. 146.Google Scholar

page 398 note 2 Q. J. G.S. vol. xxvi. p. 90.Google Scholar