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Published online by Cambridge University Press: 01 May 2009
The interpretation of the sands and gravels intercalated in the glacial drift is one of the most interesting problems in glacial geology. Do they, on the one hand, represent the deposits of one or more mild intervals alternating with periods of intense cold; or were they, on the other, laid down during one continuous cold period marked by such slight oscillations as can be shown to occur in connection with existing glaciers and ice-sheets?
page 337 note 1 “Great Ice Age,” p. 165.Google Scholar
page 337 note 2 Ditto, , p. 204.Google Scholar
page 338 note 1 See Brit. Assoc. Reports, 1889, pp. 556–558.Google Scholar
page 338 note 2 Great Ice Age, p. 393.Google Scholar
page 339 note 1 Records Geol. Surv. India, vol. xiv. pp. 44–45.Google Scholar
page 340 note 1 Nordenskiöld, , Geol. Mag. Vol. IX. p. 393.Google Scholar
page 340 note 2 p. 62.
page 340 note 3 “Glaciers of Savoy,” Translation. Edited by Prof. George Forbes, pp. 156–7.
page 341 note 1 Geology of London, Geol. Surv. Mem. pp. 52, 53.Google Scholar
page 341 note 2 Q.J.G.S. vol. xlii. pp. 373Google Scholar–4.
page 341 note 3 Op. cit. p. 383.Google Scholar
page 341 note 4 Q.J.G.S. vol. xxxix. p. 83.Google Scholar
page 343 note 1 Q.J.G.S. 1874, p. 124.Google Scholar
page 345 note 1 Great Ice Age, p. 491.Google Scholar
page 346 note 1 Great Ice Age, pp. 405–6.Google Scholar
page 346 note 2 Edinburgh New Philosophical Journal, 1855, p. 14.Google Scholar
page 346 note 3 Edin. New Phil. Journ. 1855, p. 18.Google Scholar