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Published online by Cambridge University Press: 01 May 2009
One of the most important and most interesting features of the geology of the Cambridge district is the deposit at Barrington, so widely known for its richness in mammalian remains. This bone-bed has been described many times, and the literature is large. Most of the descriptions, however, confine themselves chiefly to the organic contents, mentioning briefly the character of the larger stones and pebbles, and saying little or nothing about the nature of the finer matrix in which these are embedded.
page 253 note 1 “The Mineral Composition of some Cambridgeshire Sands and Gravels”: Proc. Camb. Phil. Soc., vol. xvii, pp. 132–43, 1913.Google Scholar
page 253 note 2 “On a Mammaliferous Deposit at Barrington, near Cambridge”: Quart. Journ. Geol. Soc, vol. xxxv, pp. 670–7, 1879.Google Scholar
page 253 note 3 For the most recent description see Hughes, “Excursion to Cambridge and Barrington”: Proc. Geol. Assoc, vol. xxii, pp. 268–78, 1911.Google Scholar
page 255 note 1 See Proc. Camb. Phil. Soc, vol. xvii, p. 142, 1913.Google Scholar