^{page 246 note 1} The writer has recently found that Tylor, A. (Geol. Mag., 1868, p. 576, and 1872, p. 392)Google Scholar anticipated even Belt in relating the origin of coral reefs to the shift of ocean-level consequent on deglaciation. Wright, W. B. (The Quaternary Ice Age, London, 1914, p. 417)Google Scholar believes the submerged forests of the British Isles prove a eustatic shift of 55 to 60 feet, if not of considerably greater amount, and attributes it to deglaciation.

^{page 248 note 1} Goldthwait, J. W., Amer. Journ. Sci., vol. xxxii, 1911, pp. 293–4.Google Scholar

^{page 248 note 2} Twenhofel, W. H., Amer. Journ. Sci., vol. xxx, 1910, pp. 66, 69.Google Scholar

^{page 248 note 3} Ibid., vol. xxviii, 1909, p. 147.

^{page 248 note 4} Smith, G. O., Bastin, E. S., and Brown, C. W., Penobscot Bay folio, U.S. Geol. Survey, 1907, p. 13.Google Scholar

^{page 248 note 5} Stone, G. H., Monograph 34, U.S. Geol. Surv., 1899, p. 53.Google Scholar

^{page 249 note 1} Mayor, A. G., Proc. Nat. Acad. Sci. vol. iii, 1917, p. 523.Google Scholar

^{page 249 note 2} Ibid., p. 522.

^{page 252 note 1} Geikie, A., The Scenery of Scotland, 2nd ed., London 1887, pp. 381–2.Google Scholar

^{page 252 note 2} Clough, C. T., The Geology of the Glasgow District (Mem. Geol. Surv. Scotland), 1911, p. 192.Google Scholar

^{page 252 note 3} Jamieson, T. F., Quart. Journ. Geol. Soc., vol. xxi, 1865, pp. 188–90.Google Scholar

^{page 252 note 4} Wright, W. B., The Quaternary Ice Age, London, 1914, p. 422. According to a personal communication from Mr. Wright (November, 1919) the zero isobase should be drawn considerably farther south in Ireland and Wales.Google Scholar

^{page 252 note 5} Kinahan, G. H., Manual of the Geology of Ireland, London, 1878, pp. 251–8Google Scholar; Hull, E., The Physical Geology and Geography of Ireland, 2nd ed., London, 1891, p. 137.Google Scholar

^{page 253 note 1} Wright, W. B., The Quaternary Ice Age, London, 1914, p. 423;Google Scholar The Geology of the British Isles, edited by Evans, J. W. (Handbuch der regionalen Geologie, iii, 1), The Hague, 1918, p. 299.Google Scholar Prestwich, Cf. J., Quart. Journ. Geol. Soc., vol. xlviii, 1892, p. 263.CrossRefGoogle Scholar

^{page 254 note 1} Fuller, Cf. M., Prof. Paper No. 82, U.S. Geol. Surv., 1914, p. 222.Google Scholar

^{page 254 note 2} Matson, G. C. and Sanford, S., Water-supply Paper No. 319, U.S. Geol. Surv., 1913, p. 34.Google Scholar

^{page 254 note 3} Veatch, O. and Stephenson, L. W., Bull. 26, Geol. Surv. of Georgia. 1911, pp. 36, 437.Google Scholar

^{page 254 note 4} Vaughan, T. W., “A Contribution to the Geological History of the Floridian Plateau“: Papers of the Marine Laboratory, Carnegie Institution of Washington, 1910, p. 180.Google Scholar “Preliminary Remarks on the Geology of the Bahamas”: ibid. 1914 p. 50. Yearbook No. 13, Carnegie Institution of Washington, 1914, p. 230.

^{page 255 note 1} Hill, R. T., Amer. Journ. Science, vol. xlviii, 1894, p. 203;Google Scholar Bull. 34, Museum Compar. Zoology, Cambridge, Mass., 1899, p. 99Google Scholar. Systematic discussion of the Atlantic Islands would include Bermuda, where Tarr, R. S. (Amer. Geol. vol. xix, 1897, p. 293) found a recent terrace reaching 15 or more feet above sea.Google Scholar

^{page 255 note 2} Branner, J. C., Bull. 44, Museum Compar. Zoology, Cambridge, Mass., 1904, p. 170 et ante.Google Scholar

^{page 255 note 3} Halle, T. G., Bull. Geol. Inst. Univ. Upsala, vol. ix, 1910, pp. 99, 117.Google Scholar

^{page 255 note 4} Andersson, J. G., Bull. Geol. Inst. Univ. Upsala, vol. viii, 1908, p. 182.Google Scholar

^{page 255 note 5} Ibid., p. 57.

^{page 255 note 6} Bulletin No. 10, 1910, p. 29; No. 15, 1912, p. 50; No. 16, 1913, p. 77; No. 20, 1918, pp. 112–13 and p. 4.Google Scholar

^{page 256 note 1} Andrews, E. C., New South Wales Handbook, Brit. Assoc. Adv. Science, 1914, pp. 525, 532:Google Scholar Süssmilch, C. A., Introduction to the Geology of New South Weles, Sydney, 1911, p. 154Google Scholar; Jack, R. L. and Etheridge, R., Geology and Palæontology of Queensland and New Guinea, London, 1892, pp. 614 ff.Google Scholar

^{page 256 note 2} Cadell, H. M., Trans. Edinburgh Geol. Soc., vol. vii, 1897, p. 179.Google Scholar

^{page 256 note 3} Agassiz, A., Memoirs, Museum Compar. Zoology, Cambridge, Mass., vol. xxviii, 1903, p. 20.Google Scholar

^{page 256 note 4} David, T. W. E. and Sweet, G., The Atoll of Funafuti, London, 1904, pp. 68, 84, 85.Google Scholar

^{page 256 note 5} Mawson, D., Proc. Linn. Soc. New South Wales, 1905, pt. iii, pp. 400 ff.Google Scholar

^{page 256 note 6} Mayor, A. G., Papers from the Department of Marine Biology, Carnegie Institution of Washington, vol. ix, 1918, p. 9.Google Scholar

^{page 256 note 7} Elschner, C., “The Leeward Islands of the Hawaiian Group”: reprint from the Sunday Advertiser, Honolulu, 1915, p. 9.Google Scholar

^{page 257 note 1} Lawson, A. C., Bull. Dep. Geol. Univ. California, vol. i, 1893, p. 53.Google Scholar

^{page 257 note 2} In a verbal communication Dr. E. O. Hovey has stated that at many parts of the Greenland coast he observed beaches with crests 15 to 20 feet above mean sea.level.Google Scholar

^{page 257 note 3} See reference above, and also Geol. Mag., Vol. viii, 1911, p. 99.Google Scholar

^{page 259 note 1} Brögger, W. C., Norges geol. Unders., No. 31, 1901, p. 713, and No. 41, 1905.Google Scholar

^{page 259 note 2} Wright, W. B., The Quaternary Ice Age, London, 1914, pp. 384–5.Google Scholar