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I.—Geology of the London Extension of the Manchester, Sheffield, and Lincolnshire Railway. Part II: Rugby to Quainton Road, near Aylesbury1

Published online by Cambridge University Press:  01 May 2009

Horace B. Woodward
Affiliation:
(Communicated by permission of the Director-General of the Geological Surrey.)

Extract

The cuttings along this new line of railway from Annesley to a little south of Rugby have been described by Mr. Fox-Strangways, and it is now proposed to note the chief geological features along the line as far as Quainton Road, near Aylesbury. This portion of the railway crosses the country from north to south, and south-east for a distance of about 35 miles. The following notes were made partly in November, 1895, when the cuttings were examined from Willoughby, near Rugby, to Helmdon; and partly in May of the following year, when the examination was continued to Quainton Road.

Type
Original Aricles
Copyright
Copyright © Cambridge University Press 1897

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Footnotes

1

The substance of this paper was communicated to the Liverpool Meeting of the British Association in 1896.

References

page 98 note 1 A. Ibex has been recorded from the Kilsby tunnel.

page 98 note 2 Proc. Geol. Assoc., vol. xiv, pp. 422, 428.Google Scholar

page 99 note 1 H. B. W., “Lias of England and Wales,” p. 225.

page 99 note 2 “Outlines of the Geology of England and Wales,” 1822, p. 248.

page 100 note 1 Proc. Geol. Assoc., vol. xiv, p. 427.Google Scholar

page 102 note 1 Judd, , “Geol. Rutland,” p. 189, etc.Google Scholar; H. B. W., “Lower Oolitic Rocks of England,” p. 402.Google Scholar

page 102 note 2 “Nat. Hist. Northants,” 1705, pp. 108, 126.Google Scholar

page 102 note 3 “Lower Oolitic Rocks of England,” p. 475.Google Scholar