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II.—Some Changes of Level in the Glacial Period

Published online by Cambridge University Press:  01 May 2009

T. F. Jamieson
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Extract

In Scandinavia there have been various changes of level during the Glacial period, and some geologists of that country are of opinion that the load of ice which lay upon it affords a probable means of accounting for a depression and submergence of the land such as would lead tothe formation of those elevated beds of Arctic shells which are met with in the interior of that region. But there has been a later movement of quite a different nature, whereby the Baltic seemsto have been converted for a time into a fresh-water lake, and it is to this that I now want to draw attention, as I think the same cause which has been supposed to produce the depression affords a happy means of explaining this curious and later phenomenon also.

Type
Original Articles
Information
Geological Magazine , Volume 2 , Issue 11 , November 1905 , pp. 484 - 490
Copyright
Copyright © Cambridge University Press 1905

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References

page 484 note 1 “Neue Zeuglodonten aus dem unteren Mitteleocan vom Mokattam bei Cairo”: Geol. u. Palaeont. Abhand., neue Folge, Bd. vi, Heft 3; Jena, 1904.

page 488 note 1 See Adamson, J., in Wernerian Soc. Memoirs, vol. iv, p. 334; also Palæontographical Soc., vol. xxviii, p. 42.Google Scholar