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Published online by Cambridge University Press: 01 May 2009
It has become one of the truisms of geology that India, like Gaul, is divided into three parts, the Peninsular, the Extra-peninsular, and the Indo-gangetic alluvium.
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page 10 note 2 Mem. Geol. Surv. India, vol. xxii. chap. v. (1883)Google Scholar.
page 11 note 1 Comp. Medlicott, Mem. Geol. Surv. India, vol. iii.Google Scholar part 2, chaps, i. and iii.; also Manual of Geology of India, vol. ii. chap. xxii.Google Scholar
page 11 note 2 Oldham, , Rec. Geol. Surv. India, vol. xvii. p. 161 (1884);Google Scholar Middlemiss, , Mem. Geol. Surv. India, vol. xxiv. part. ii. 1890.Google Scholar
page 11 note 3 Mem. Geol. Surv. India, vol. xxii. chap. v.Google Scholar
page 12 note 1 Rec. Geol. Surv. India, vol. xxi. p. 161.Google Scholar
page 12 note 2 Rec. Geol. Surv. Ind. vol. ix. p. 54.Google Scholar
page 12 note 3 Mem. Geol. Surv. Ind. vol. xxiv. p. 184.Google Scholar
page 13 note 1 Mallet, , Mem. Geol. Surv. India, vol. xi. part i.;Google Scholar see also Godwin-Austen, , Journ. Asiatic Soc. Bengal, part ii. vol. xxxviii. p. 151;Google Scholar La Touche, , Records Geol. Surv. India, vol. xviii. p. 121.Google Scholar
page 15 note 1 Boulder gravels composed of well-rounded blocks of hard rock are also found in the beds of streams draining from the Upper Siwalik conglomerates; but such exceptions are obvious.
page 15 note 2 Middlemiss, , Mem. Geol. Surv. India, vol. xxiv. pt. 2.Google Scholar
page 16 note 1 Medlicott, , Rec. Geol. Surv. India, vol. ix. p. 57.Google Scholar
page 17 note 1 This question is more fully treated by my colleague, MrMiddlemiss, , in his recently published memoir, Mem. Geol. Surv. Ind. vol. xxiv. pt. ii.Google Scholar
page 18 note 1 Mem. Geol. Survey India, vol. iii. part ii. p. 135.Google Scholar
page 18 note 1 Lydekker, , Rec. Geol. Survey of India, vol. xiv. pp. 178–183 (1881).Google Scholar