The geography and geology of south-eastern EgyptBall, John
Science
The geography and geology of south-eastern Egypt
Ball, John
Geology -- Egypt; Physical geography -- Egypt
[Footnote 75: In particular, the adoption of the above three
longitudes as of equal accuracy with Suez will lead to a better
longitude for Jidda. The longitude of Jidda is at present fixed only
by chronometer transport from Suez, a distance of some 650 miles; but
by regarding Halaib as a fixed point the distance of comparison can
be reduced to 150 miles. The data for this revision of the longitude
of Jidda already exist in the Reports of the “Pola” expedition,
and the discussion is certainly worth undertaking before any future
surveys are conducted in the central portion of the Red Sea.]
[Footnote 76: The disturbance of the needle was of course most
frequent in the areas where dark igneous and metamorphic rocks
prevailed; in these regions disturbances of 10° were very frequent,
and in some cases, as for example on the serpentine deposits of
Sikait, as much as 40° was noticed. In the sandstone areas no
disturbances were marked.]
[Footnote 77: I have given a somewhat fuller account of this
process in a little paper on “Long-distance Tacheometry.” _Cairo
Scientific Journal_, Vol. IV, February 1910.]
[Footnote 78: JORDAN, _Handbuch der Vermessungskunde_. Stuttgart,
1897. Bd. II, p. 522.]
[Footnote 79: _A New Method of Coast Surveying_, Survey Department
Paper, No. 21. Cairo, 1911.]
[Footnote 80: The observations at Halaib were made at a point far
enough from the fort to avoid any chance of disturbance by the iron
rails which form part of the building.]
[Footnote 81: _Berichte der Commission für Oceanographische
Forschungen_, Sechste Reihe. Wien, 1898. pp. 221, 223.]
[Footnote 82: _Magnetic Observations in Egypt_, 1895-1905, Survey
Dept. Paper, No. 6. Cairo, 1907. p. 18.]
[Footnote 83: _Red Sea and Gulf of Aden Pilot._ 5th
edition. 1900. p. 7.]
CHAPTER IV.
* * * * *
=THE WADIS DRAINING WESTWARDS TO THE NILE.=
* * * * *
It has been already mentioned (p. 21) that all the drainage westward
from the main watershed ultimately reaches the Nile by the three
great trunk Wadis Shait, Kharit, and Alaqi. In the present chapter
a detailed description will be given of those parts of these
wadis and their tributaries which are known within the area under
discussion. The following scheme shows the relations of the principal
tributaries, important feeders of the tributaries themselves being
indicated in (brackets):—
{ Wadi Dweig.
{
WADI SHAIT { Wadi Muelih (Wadi Gerf, Rod el Ligah, Wadi Sibrit).
{
{ Wadi Hamish.
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