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II.—On the Age of the Reptile Faunas contained in the Magnesian Conglomerate at Bristol and in the Elgin Sandstone

Published online by Cambridge University Press:  01 May 2009

Friedrich Baron Huene
Friedrich Baron Huene
Affiliation:
Tübingen, Germany.
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Extract

According to Etheridge (Quart. Journ. Geol. Soc., vol. xxvi, 1870, pp. 174–192) the Magnesian Conglomerate at Bristol is of the same age as the German Muschelkalk, but Moore (Quart. Journ. Geol. Soc., vol. xxxvii, 1881, pp. 67–82) was of opinion that it was Rhætic. Since that time no special paper on the subject has been published, but now the present writer has been able to find some new evidence.

Type
Original Articles
Information
Geological Magazine , Volume 5 , Issue 3 , March 1908 , pp. 99 - 100
Copyright
Copyright © Cambridge University Press 1908

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