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- W1965573818 abstract "The existence of fossiliferous deposits on the western coast of Tjörnes (Northern Iceland) has been known to science for nearly 160 years. They were first mentioned by the famous Egbert Olafsson in his book entitled ‘Enarrationes historicæ de Islandiæ Natura & Constitutione,’ etc., published at Copenhagen in 1749. In 1871 the Danish conchologist O. A. L. Mörch published a paper ‘On the Mollusca of the Crag-formation of Iceland,’ wherein he enumerated 61 species of molluscs, and arrived at the conclusion that in the Crag-period the temperature of the northern coast of Iceland must have been much milder than now, ‘at least as at present on the west coast by Reikiavik’ [Reykjavik], <i>op. cit.</i> p. 394. Some years later, Mr. J. Starkie Gardner collected 33 species of Pliocene molluscs in Iceland, which were studied by Gwyn Jeffreys and Searles V. Wood. In the opinion of Wood, the deposits in question cannot be younger than Middle Red Crag, while Jeffreys thinks that they are somewhat younger. Gardner himself is, however (Quart. Journ. Geol. Soc. vol. xli, 1885, p. 97), ‘inclined to assign a greater age to the deposit from its general appearance on the spot, than Dr. Gwyn Jeffreys may do, or even than Mr. Searles Wood.’ The most important paper in existence on the fauna of the Icelandic Crag dates from 1884, but only exists in a manuscript, which has been deposited in the archives of the Geological Museum of Copenhagen. It is written by C. M. Poulsen, and is in" @default.
- W1965573818 created "2016-06-24" @default.
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- W1965573818 date "1906-02-01" @default.
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- W1965573818 title "The Crag of Iceland: an Intercalation in the Basalt-Formation" @default.
- W1965573818 doi "https://doi.org/10.1144/gsl.jgs.1906.062.01-04.33" @default.
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