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III.—The Selbornian of Stonebarrow Cliff, Charmouth

Published online by Cambridge University Press:  01 May 2009

W. D. Lang
W. D. Lang
Affiliation:
The British Museum (Natural History).
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Extract

Although the succession of Cretaceous beds on Black Ven is well known and much has been written on the various members of the series, only cursory references have been made to those on Stonebarrow Cliff on the east of Charmouth, and the lower beds have never been recorded therefrom. A full list of the literature on the geology of this district, including all that has been written on the Selbornian, is given in the Survey Memoir on the “Geology of Sidmouth and Lyme Regis” and another bibliography in the account of the last excursion to Lyme by the Geologists’ Association.

Type
Original Articles
Information
Geological Magazine , Volume 4 , Issue 4 , April 1907 , pp. 150 - 156
Copyright
Copyright © Cambridge University Press 1907

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References

page 150 note 1 Woodward, H. B.: “Geology of Sidmouth and Lyme Regis,” 1906, pp. 86–88.Google Scholar

page 150 note 2 Proc. Geol. Assoc., vol. xix (1906), p. 340.

page 150 note 3 Jukes-Browne, A. J.: Proc. Dorset Nat. Hist. Club, vol. xviii (1897), p. 176; GEOL. MAG., 1898, p. 164.Google Scholar

page 150 note 4 Jukes-Browne, A. J., “Gault and Upper Greensand of England,” 1900, p. 185Google Scholar: Mem. Geol. Survey.

page 150 note 5 Lang, W. D., “The Zone of Hoplites interruptus at Black Ven”: Geol. Mag., 1904, p. 125.Google Scholar

page 154 note 1 Hitherto recorded from the Gault of this district as Lima parallela. See Woods, , “Cretaceous Lamellibranchs,” vol. ii (1904), pp. 31Google Scholar and 32: Mon. Pal. Soc.

page 154 note 2 Hitherto recorded from the Gault of this district as Pinna tetragona or P. subtetragona. See Woods, loc. cit., 1906, p. 98.

page 154 note 3 Lang, W. D., loc. cit.: GEOL. MAG., 1904, pp. 125 and 130.Google Scholar

page 154 note 4 Jukes-Browne, A. J., “Gault and Upper Greensand of England,” 1900, pp. 184Google Scholar and 185: Mem. Geol. Surv.