Hostname: page-component-cd9895bd7-p9bg8 Total loading time: 0 Render date: 2024-12-23T21:04:38.669Z Has data issue: false hasContentIssue false

I.—Flowing Wells and Sub-Surface Water in Kharga Oasis

Published online by Cambridge University Press:  01 May 2009

Extract

With the exception of an article written by me for Sir William Willcocks and published in his “Nile in 1904,” and a reference to the relations of the Eocene and Cretaceous in the oasis of Kharga in a paper read before the Geological Society in 1905, nothing has, I believe, been published on the water-supply and geology of this district since Dr. Ball's report in 1900.

Type
Original Articles
Copyright
Copyright © Cambridge University Press 1908

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

page 49 note 1 “The Oases and the Geology of the Nile Valley,” being Chapter 5 of “The Nile in 1904,” by sirWillcocks, William K.C.M.G.,, Cairo, 1904.CrossRefGoogle Scholar

page 49 note 2 The Relations of the Eocene and Cretaceous Systems in the Esna-Aswan Reach of the Nile Valley”: Quart. Journ. Geol. Soc., vol. lxi (1905), pp. 667678.Google Scholar

page 49 note 3 “Kharga Oasis: its topography and geology”: Egypt. Geol. Surv. Report, Cairo, 1900.Google Scholar

page 52 note 1 Op. cit.: Q.J.G.S., vol. lxi (1905), p. 675.Google Scholar

page 52 note 2 Op. cit., p. 94.

page 52 note 3 “Dakhla Oasis: its topography and geology”: Egypt. Geol. Surv. Report, Cairo, 1901.Google Scholar

page 53 note 1 The localities referred to in this paper are shown on the accompanying map, p. 51, the topography of which is based on the maps of the Survey Departmental Report. The scale (1: 500, 000) is of course too small to show each division of the Eoceue and Cretaceous, and the boundaries of such as are indicated must only be taken as approximate. On the Survey maps the names of the two prominent outliers of the plateau on the east side of the depression have their names reversed; the most northerly is Jebel el Ghennima, the other to the south Jebel Um el Ghennaim.

page 54 note 1 Op. cit., pp. 95–97.

page 56 note 1 The headquarters of the Corporation of Western Egypt, Ltd.; the area over which the boring operations referred to in this paper extend is shown on the accompanying map (Fig. 1, p. 51) by a dotted line.

page 56 note 2 For the analyses quoted in this paper I am indebted to Mr. William Garsed, formerly of the Oasis Headquarters Staff.