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II.—The Fayûm Depression: A Preliminary Notice of the Geology of a District in Egypt containing a new Palæogene Vertebrate Fauna1

Published online by Cambridge University Press:  01 May 2009

Hugh J. L. Beadnell
Affiliation:
Geological Survey of Egypt.

Extract

The Fayûm, one of the largest depressions of the Libyan Desert, is situated some 50 miles south-west of Cairo. It is cut out in rocks of Eocene and Oligocene age, while still younger deposits of Pliocene and Post-Pliocene date are found within the hollow. The depression owes its origin to the action of the ordinary subærial denuding agents, which I have shown in previous papers were capable of producing the oases-depressions of Baharia, Farafra, Dakhla, etc. Faulting, which has played so important a part in the formation of the Nile Valley, appears to have had little or nothing to do with the production of the Fayûm and other depressions of the Libyan Desert.

Type
Original Articles
Copyright
Copyright © Cambridge University Press 1901

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Footnotes

1

Communicated in abstract to the British Association at Glasgow, 1901, by permission of Sir William Garstin, K.C.M.G., Under-Secretary of State, and Capt. H. G. Lyons, Director-General of the Survey Department, Cairo.

References

1 Beadnell, : “Recent Geological Discoveries in the Nile Valley and Libyan Desert”; London, 1901Google Scholar.