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
=Wadi Defeit=, which is probably the most important Egyptian tributary
of Wadi Alaqi, has its heads in Gebels Heleikontî and Heianai, about
the meridian of 35°. Its general course is that of a flat circular
arc convex to the north and having its chord east and west; the total
length of its main channel, from its head in Gebel Heleikontî to
its junction with Wadi Alaqi in longitude 34° 10′, is over one
hundred kilometres, while its numerous tributaries probably reach a
total length three times as great. The principal head of Wadi Defeit
is called =Wadi Sarid=; its branches extend among the hills close to
the heads of Wadi Egat and Wadi Miaus. The name Defeit is applied
to the wadi where Wadi Sarid is joined by the feeders from Gebel
Heleikontî. Passing between the high ranges of Heianai on the north,
and Heleikontî and Shanaiyet on the south, Wadi Defeit receives
numerous feeders, of which the principal are the =Wadis Dauriai=
and =Hamidâ=, both entering it from the mountain to the south;
continuing westwards, it cuts through the north end of the mass of
Gebel Um el Tiur el Foqani, and on emergence is joined by the =Wadi
Bint el Feqoh=, a great westward-coursing tributary draining the
north flanks of the Heianai range and the more northerly mountain
of Anweyib. Continuing its westward course, Wadi Defeit passes
between Gebels Um el Tiur el Tahtani and Adraq; then it enters on an
extensive tract of more open country, receiving three main feeders,
=Wadi Meladoyeb=, =Rod Hauanin=, and =Wadi Bagharid=, from the hills
to the north, before joining Wadi Alaqi.
=Wadi Seiga=, the next great northern tributary of Wadi Alaqi, has
only been partially explored. Its head is in the watershed range near
the conspicuous twin peaks of Gebel Sheyenit. Pursuing at first a
southerly course, it cuts through the east side of the mass of Gebel
Seiga; and about thirty kilometres lower down passes through hills
with old gold mines on either hand. Below the mines, Wadi Seiga takes
a south-westerly course, and receives a large tributary from either
side. That from the west, called =Wadi Deheis=, heads in Gebel Deheis
and curves round east of Gebel Abu Brush, receiving in its course
two great feeders, the =Wadis Um Gholqa= and =Abu Had=, both of which
head far to the north in the main watershed. The eastern tributary,
called =Wadi Um Derera=, drains the south part of the hill-mass in
which the Seiga mines are situated. Wadi Seiga joins Wadi Alaqi in
longitude 33° 53′, some forty-five kilometres below the mines;
the junction is outside the limits of the maps in this volume.
* * * * *
[Footnote 84: Dry in 1906.]
[Footnote 85: To be distinguished from another mountain of the same
name further south, near the Wadi Hodein.]
[Footnote 86: To be distinguished from the better known Wadi Egat
much further south, a feeder of Wadi Alaqi.]
[Footnote 87: “L’Etbaye.” p. 1.]
Public-domain text, read in full here on John Shaqi.
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