Published online by Cambridge University Press: 01 May 2009
During late years, by the opening of new sections, fresh information has been obtained of the geology of different parts of the country, and several fine excavations, the result of railway enterprise, have afforded great sections of the Kellaways beds in localities where only conceptions of them previously prevailed. Gaps have been filled up, and the continuity of the beds over extended areas confirmed. The principal revelations come from the Hull and Barnsley, and from the Swindon and Cirencester railways, opened respectively about 1881 and 1883, and the works now in progress in connexion with the widening of the main line at Oakley, near Bedford.
page 66 Note 1 An abstract of this paper was read in Section C, British Association, Cardiff, 1891.
page 66 Note 2 Phil, . Trans, vol. xvi. p. 183 (1785).Google Scholar
page 68 Note 1 Geol. MAG. Vol. II. June, 1885, on Cone-in-Cone Structure. Abstract of paper read to Geol. Soc. Glasgow.Google Scholar
page 69 Note 1 See Geol, . MAG. Dec. III. Vol. IV. p. 139 (1887), Prof. Hull's letterGoogle Scholar; Dec. III. Vol VI. p. 356 (1889), Jukes-Browne, A., On the Occurrence of Granite in a Boriug at Bletchley.Google Scholar
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page 70 Note 1 Outlines of the Geology of England and Wales, p. 264 (1822).Google Scholar