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VI—On the Cause of the Depression and Re-Elevation of the Land During the Glacial Period

Published online by Cambridge University Press:  01 May 2009

Thomas F. Jamieson
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Extract

In England the ice seems to have been heaviest in Wales and the N.W., and lightest on the East and S.E., where it appears to have thinned off altogether, and the evidence of depression corresponds with this. If we draw a line from Dover to Anglesea, we find proof of great submergence in Wales, decreasing to zero as we approach the English Channel. and Prof. Hughes of Cambridge, in a recent paper “On the Evidence of the Later Movements of Elevation and Depression in the British Isles,” read before the Victoria Institute, says: “As we trace these movements north to the borders of the mountains, we find evidence of greater sinking and greater elevation.”

Type
Original Articles
Information
Geological Magazine , Volume 9 , Issue 10 , October 1882 , pp. 457 - 466
Copyright
Copyright © Cambridge University Press 1882

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References

page 458 note 1 Daua says the terraces on the north side of Lake Ontario are very much higher than those on the south side. See his “Manual of Geology,” 2nd ed. p. 552.Google Scholar

page 459 note 1 See Newberry's Surface Geology of Ohio, p. 76;Google Scholar also, Hinde, G. J. in the Canadian Journ. for 04, 1877Google Scholar; and Manual, Dana's, 2nd edition, p. 536.Google Scholar

page 461 note 1 Students' Elements of Geology, 2nd ed. p. 133. See also Lyell's Antiquity of Man, chap. xvi. for fuller details regarding the Loess.Google Scholar

page 462 note 1 See Lyell's Principles, 11th ed. vol. ii. p. 196;Google Scholar also Proceedings of the Geol. Soc. vol. ii. p. 208;Google Scholar and Brown, K. in the Quart. Journ. of the Geol. Soc. vol. xxvi.p. 691, 1870.Google Scholar

page 462 note 2 Geol. Magazine, for 1872, Vol. IX.Google Scholar

page 464 note 1 Quart. Journ. of the Geol. Soc. vol. xviii. p. 179, 02. 1862.Google Scholar

page 465 note 1 Schwankungen des Meeresspiegels, Jahrb. der Geograph. München, Gesellschaftzu, bd. vii. 1882.Google Scholar