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VII.—On the Junction of the Chalk with the Tertiary Beds in East Kent1

Published online by Cambridge University Press:  01 May 2009

George Dowker
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Extract

The Junction of the Chalk with the Lower Tertiaries is nearly always marked by the presence of green-coated flints; and in East Kent, where the Thanet Sands rest on the Chalk, numerous junction-sections are exposed, exhibiting the peculiarities which I now lay before you.

Type
Original Articles
Information
Geological Magazine , Volume 3 , Issue 23 , May 1866 , pp. 210 - 213
Copyright
Copyright © Cambridge University Press 1866

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Footnotes

1

See also Report of Proceedings of Geol. Soc., London, 03 21, for two other papers on similar subjects at p. 223.

References

page 210 note 2 Quart Journ. Geol. Soc., Vol. Viii., p. 243.Google Scholar

page 210 note 3 See Prestwich, paper on woolwich and Reading Series. Quart. Journal of Geological Society, Vol. x., p. 95. Mr. Whitaker in Geological survey Memoirs, on Sheet 13, and on Sheet 7.Google Scholar

page 210 note 4 See Mr.Whitaker's paper in Quart. Journ. Geol. Soc., Vol. xxi., p. 397.Google Scholar

page 211 note 1 For a beautiful example of a fractured flint, re-cemented by infiltrated silica, see the late Dr. S. P.Woodward's paper “On the Nature and Origin of Banded Flints,” in Geol. Mag., Vol. I., p.145, Pl. VIII. Fig.4.—Edit.Google Scholar

page 211 note 2 See Professor Morris's paper, Vol. xiii, p. 13, of Quarterly Journal of the Geological Society.Google Scholar

page 211 note 3 Chemical Geology, Vol. ii., p. 480, English Translation (Cavendish Society).Google Scholar

page 211 note 4 Op. cit.

page 212 note 1 Quarterly Journal of Gelogical Society, Vol. x., p. 123.Google Scholar