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V.—On some Middle and Upper-Lias Sections near Batcombe, Somerset

Published online by Cambridge University Press:  01 May 2009

L. Richardson
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Extract

In the neighbourhood of Batcombe the Marlstone of the Middle Lias is typically developed, and is succeeded by thin alternating layers of clay and limestone, which are in turn followed by pale-Yellow fine-grained sands—near Bruton, of considerable thickness.

Type
Original Articles
Information
Geological Magazine , Volume 6 , Issue 12 , December 1909 , pp. 540 - 542
Copyright
Copyright © Cambridge University Press 1909

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References

1 Geol. Mag., Dec. V, Vol. III, 1906, pp. 368–9.Google Scholar

2 Quart. Journ. Geol. Soc., 1907, vol. lxiii, p. 391Google Scholar; Geol. Mag., 1908, p. 510 (footnote).

3 Mem. Geol. Surv., 1846, vol. i, p. 280Google Scholar (footnote).

4 Mem. Geol. Surv., 1893, vol. iii, p. 207Google Scholar: “The Jurassic Rocks of Britain: The Lias of England and Wales (Yorkshire excepted).”

1 Mem. Geol. Surv., 1893, vol. iii, p. 207Google Scholar: “The Jurassic Rocks of Britain: The Lias of England and Wales (Yorkshire excepted).”

2 Étndes Pal. sur les Dépôts Jurassiques du Bassin du Rhone, 1869, 3ième pt., pl. xxix, fig. 8.

3 Ibid., pl. xl, fig. 7.