Hostname: page-component-cd9895bd7-p9bg8 Total loading time: 0 Render date: 2024-12-23T15:29:52.941Z Has data issue: false hasContentIssue false
  • English
  • Français

A Search for the Alleged Sinemurian in the Wadi Araba, Eastern Desert of Egypt

Published online by Cambridge University Press:  01 May 2009

W. J. Arkell
Get access Rights & Permissions [Opens in a new window]

Abstract

Marine Lower Lias, with Ammonites bucklandi and other fossils, was recorded in the Wadi Araba by Figari Bey in 1864. No one has since been able to find marine Lias in Egypt, but in 1915 Greco figured a Sinemurian faunule, including an Arnioceras, from the Figari Egyptian collections at Florence, and claimed that Figari's discovery was confirmed. A special search for the locality was made in 1951, without success. The paper reviews the evidence and records Carboniferous rocks and fossils that were found. Some general remarks are also made on the structure and origin of the Wadi Araba.

Type
Articles
Information
Geological Magazine , Volume 88 , Issue 5 , October 1951 , pp. 305 - 314
Copyright
Copyright © Cambridge University Press 1951

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

REFERENCES

Andrew, G., 1937. The late Tertiary igneous rocks of Egypt (field relations). Bull. Fac. Sci. Egyptian Univ., no. 10.Google Scholar
Ball, J., 1910. On the origin of the Nile valley and the Gulf of Suez. Geol. Mag., xlvii, 71.CrossRefGoogle Scholar
Ball, J., 1916. The Geography and Geology of West-Central Sinai. Survey Dept., Cairo.Google Scholar
Carpentier, A., and Farag, I., 1948. Sur une flore probablement rhétienne à EI Galala el Bahariˇya. C. R. Acad. Sci. Paris, ccxxvi, 686.Google Scholar
Cuvillier, J., 1937. Présence du Carbonifère marin dans l' Ouadi Abou Darag (Désert Arabique). C. R. Acad. Sci. Paris, cciv, 1834.Google Scholar
Figari, C. A., 1864. Studii scientifici sull' Egitto e sue adiacenze, compresa la Penisola dell' Arabia Petrea (2 vols.). Vol. 1, 51, 62–3, 142–3.Google Scholar
Fourtau, R., 1904. Contribution à l'étude de la faune crétacique d' Egypte. Bull. Inst. Egyptien (4), iv, 240–2.Google Scholar
Greco, B., 1915. II Sinemuriano nel Deserto Arabico settentrionale. Boll. Soc. Geol. Ital., xxxiv, 505.Google Scholar
Greco, B., 1916. Fauna cretacea dell' Egitto raccolta dal Figari Bey. Part 2, Pal. Italica, xxii, 103.Google Scholar
Moon, F. W., and Sadek, H., 1921. Topography and geology of Northern Sinai. Petroleum Research Bull., no. 10 (Cairo).Google Scholar
Sadek, H., 1925. The distribution of the Jurassic formation in Egypt and Sinai. C. R. Congr. géol. intern., xiii (Belgium, 1922), 1039.Google Scholar
Sadek, H., 1926. The Geography and Geology of the district between Gebel Ataqa and El-Galala El-Bahariya. Surv. Egypt Paper, no. 40.Google Scholar
Schellwien, E., 1894. Ueber eine angebliche Kohlenkalk-Fauna aus der ägyptisch-arabischen Wüste. Zeit. Deutsch. Geol. Gesell., xlvi, 68.Google Scholar
Schweinfurth, G., 1886. Sur la découverte d'une faune Paléozoique dans le Grès d' Egypte. Bull. Inst. Egyptien (2), vi, 239.Google Scholar
Walther, J., 1890. Ueber eine Kohlenkalk-Fauna aus der ägyptisch-arabischen Wüste. Zeit. Deutsch. Geol. Gesell., xlii, 419.Google Scholar