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Published online by Cambridge University Press: 01 May 2009
Just out of Seaford the Chalk rises sharply from beneath the sand of the Woolwich Beds, on an outlier of which the small town is buUt. The dip however soon lessens, until the Chalk is flat, with slight waves. Some of the layers of flint are continuous, and some nearly so, but most are not continuous, and they are rather closer together in the lower part of the cliff. There are a few thin beds of hard chalk, and at the top a capping of “clay-with-flints.”
page 198 note 1 Quart Journ. Geol. Soc. vol. xiv. p. 322.Google Scholar
page 200 note 1 Trans. Geol. Soc. i. vol. v. p. 16.Google Scholar
page 200 note 2 Not noticed by Phillips, as it does not occur on the coast he described. See Quart. Journ. Geol. Soc. vol. xxi p. 395.Google Scholar