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Published online by Cambridge University Press: 01 May 2009
Taking into account the large number of papers that have been published on the Glacial Deposits near Cromer, any further description may appear unnecessary; and it was with this impression that I commenced the systematic examination of the coast three years ago. Before long, however, I found that in many important points the actual facts do not support the accepted theories of the origin of the deposits; and having now made a thorough examination, I lay the results before the reader.
page 55 note 1 This paper was read before the Geological Society, but only published in abstract.
page 55 note 2 Phil. Mag. vol. lxiii. p. 81.Google Scholar
page 55 note 3 ibid.. 2nd ser. vol. i. pp. 277, 346, 426.
page 55 note 4 ibid.. 3rd ser. vol. xvi. p. 345.
page 56 note 1 Palæontographical Society, vol. xxv. (issued for 1871.)Google Scholar
page 56 note 2 Quart. Journ. Geol. Soc. vol. xxxiii. p. 74.Google Scholar
page 56 note 3 Geol. Mag. Dec. II. Vol. IV. p. 156.Google Scholar
page 56 note 4 ibid. p. 479.
page 56 note 5 ibid. p. 300.
page 58 note 1 Ordinary variations in temperature and in the rate of condensation from year to year, are fully sufficient to explain this well-known phenomenon.—Edit. Geol. Mag.
page 59 note 1 Quart. Journ. Geol. Soc. vol. xxxiii. p. 78.Google Scholar
page 59 note 2 See Woodward, H. B., Proc. Norwich Geol. Soc. vol. i. p. 58.Google Scholar
page 60 note 1 Geol. Mag. 1868, Vol. V. p. 550.Google Scholar
page 65 note 1 See also, with regard to the similar large disturbances in the Island of Moen, now proved to be of Glacial origin, Johnstrup, in Zeitschrift der Deutschen Geol. Gesellschaft, 1874, p. 533.Google Scholar
