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Published online by Cambridge University Press: 01 May 2009
In the south-east of England considerable tracts are covered by sheets or patches of gravel. It is mainly composed of flints from the Chalk, has a thickness of, say, from 6 to 20 feet, is generally stratified, and rests upon an uneven surface of the older strata. The top is nearly always flat and inclined at a low angle.
Read before the British Association, Section C (Geology), Glasgow, Sept., 1901.
page 511 note 1 Quart. Journ. Geol. Soc., 1892, vol. xlviii, p. 29;Google Scholar 1898, vol. liv, p. 184.
page 511 note 2 “Geology of London” : Mem. Geol. Surv., 1889, vol. i, p. 391.Google Scholar
page 513 note 1 Quart. Journ. Geol. Soc., 1890, vol. xlvi, p. 333.Google Scholar
