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Published online by Cambridge University Press: 01 May 2009
The central position of Leicestershire gives it not only a peculiar relationship in regard to river-drainage, streams radiating from its plateau-frontier on the one hand to the north, flowing into the Humber, and on the other to the south into the Bristol Channel, separated alone by a now comparatively insignificant divide in the neighbourhood of Lutterworth. Also the very fact that this divide is given, by the otherwise lowland character of the tract to the north and south, a barrier-like aspect, renders it highly probable that the flora and fauna in this basin-like area is more or less homogeneous. That it has been uniform in character, no doubt from pre-Glacial times, when doubtless the existing drainage systems (though probably still more ancient fundamentally) received their most recent stamp, having been little modified (except in depth or width) during Glacial or later times. For this purpose we must needs summarize all that is known as to the occurrence of plants or land and fresh water Mollusca in post-Pleistocene alluvial deposits.
page 542 note 1 The Jurassic Rocks of Britain—The Lower Oolitic Rocks of England (Yorkshire excepted), vol. iv (1894), p. 307.Google Scholar
page 542 note 2 Proc. Cotteswold, Nat. F.C. vol. xvi, pt. i, p. 32, 1907Google Scholar; see also Geology in the Field (Jubilee vol. of the Geol. Assoc), pt. 2, p. 356, 01, 1910.Google Scholar
page 543 note 1 A list of these up to 1889 was given in The Vertebrate Animals of Leicestershire and Rutland. It was summarized recently in the “Victoria County History” by Mr. R. Lydekker. Many additions must, however, be made to both.
page 543 note 2 Report, Leic. Lit. and Phil. Soc., 1875, p. 42.Google Scholar
page 543 note 3 Mr. J. Plant found Rhinoceros teeth with Succinea, Zimnæa, etc., in the Abbey Park Road, a little north of the south end.
page 543 note 4 Ibid., 1878, pp. 26–8.
page 544 note 1 Trans. Leic. Lit. and Phil. Soc., 1901, p. 30.
page 544 note 2 Burton-on-Trent, its History, its waters, and its Breweries, 1869, p. 182.
page 546 note 1 About 30 feet below the surface in the gravels a deer's horn was found.
page 546 note 2 Vide The Geology of the Country between Derby, Burton-on-Trent, and Lough-borough, 1905, p. 64.
page 547 note 1 Found in E. and W. Norfolk, Cambridge, Worcester, Montgomery, N. Lines, S. and W. Lanes.
page 547 note 2 The nearest counties where this is now found are: Kent, Berks, Bucks, E. Suffolk, E. Norfolk, Huntingdon, N.E. and S.E. York, N. Lincoln, Huntingdon.
page 547 note 3 Quart. Journ. Geol. Soc., vol. lii, pp. 497–500, 1896.Google Scholar
page 548 note 1 The Geology of the Country between Newark and Nottingham (Mem. Geol. Surv.), 1908, p. 86.
page 549 note 1 The Geology of the Melton Mowbray District and South-East Nottinghamshire(Mem. Geol. Surv.), 1909, p. 89.
page 549 note 2 Geology of Rutland, 1875, p. 56
page 550 note 1 Deeley, R. M., Quart. Journ. Geol. Soc., vol. xlii, p. 437, 1886.CrossRefGoogle Scholar
page 550 note 2 At Beasley's Pit, Aylestone, Mr. G. W. Lamplugh and the late C. Fox Strangways found Tellina balthica.
page 550 note 3 Quart. Journ. Geol. Soc., vol. ix, p. 321, fig. 2, 1853.Google Scholar
page 552 note 1 GEOL. MAS., 1895, pp. 1–3, reprint.
page 552 note 2 Proc. Geol. Assoc., 1910, p. 485.
page 552 note 3 The Origin of the British Flora, Clement Reid, F.R.S., 1899, p. 13.
page 552 note 4 Ibid., p. 66.
page 553 note 1 The Origin of the British Flora, Clement Reid, F.R.S., 1899, p. 61.