Hostname: page-component-78c5997874-4rdpn Total loading time: 0 Render date: 2024-11-07T09:26:15.319Z Has data issue: false hasContentIssue false

II.—The Glacial Deposits of Cromer

Published online by Cambridge University Press:  01 May 2009

Clement Reid
Affiliation:
H.M. Geological Survey of England and Wales.

Extract

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.

Type
Original Articles
Copyright
Copyright © Cambridge University Press 1880

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

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