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Published online by Cambridge University Press: 01 May 2009
The graceful outlines, smooth curves, and flowing contours of the Chalk hills are well known to southern geologists; indeed these hills are the most marked feature of the south-east of England. Those who hold that their form has been given by the sea, point to the winding ridge, and say how like it is to many a coast with its succession of capes and coves; even so distinguished a writer as Sir C. Lyell remarking that “the geologist cannot fail to recognise in this view (of part of the South Downs) the exact likeness of a sea-cliff”. And truly it is so; but let us examine this likeness more closely, and it will be seen that the argument founded on it, plausible enough on the surface, is superficial only, and fails utterly when rigorously tested.
page 484 note 1 Elements of Geology Ed. 6, p. 359 1865. Sir Charles now allows, however, that the likeness is deceptive, see p. 449.Google Scholar
page 484 note 2 Hutton, , “Theory of the Earth,” vol. i.p. 489.Google Scholar
page 484 note 3 The top bed of the Chalk Marl, see Quart. Journ. Geol. Soc., vol. xxii. p. 398.Google Scholar
page 486 note 1 Quart. Journ. Geol. Soc., vol. x. p. 222 (1854).Google Scholar
page 490 note 1 Proc. Inst. Civ, Eng. vol. xxiii. p. 186, 1865, Where, and on an earlier paper by the same authorGoogle Scholar (ibid). vol. xi. p. 162, 1854, the destruction of the South-east coast of England is well treated of.
page 490 note 2 Quart. Journ. Geol. Soc., vol. xxii, p. 412.Google Scholar
page 490 note 3 See Jukes, , Brit. Assoc. Rep. for 1862 Trans. of Sections, p. 61.Google Scholar
page 490 note 4 Principles of Geology, Ed. 10, vol. i, pp. 565, 570 (1867).Google Scholar
page 492 note 1 Scrope, “The Geology, etc., of Central France”, Ed. 2. (1858), p. 208.Google Scholar