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 Nilateib=, another small wadi further north, drains the
south end of Gebel Um Rasein and the north-east faces of the hills
close south-west of it. Coursing at first south-east for about three
kilometres, it then curves round the foot of Gebel Um Rasein to join
Wadi Hasium by two channels. There is a clear passage from the heads
of both Wadi Odruk and Wadi Nilateib into Wadi Merdiyeb. All the wadis
hereabouts contain plenty of trees and scrub, especially in their
upper parts; as Wadi Hasium is approached they become more sandy
and barren. It is, of course, the presence of vegetation available
for grazing which determines the possession of a name by such small
wadis as these two.
The drainage from the east face of Gebel Um Rasein joins Wadi
Hasium directly by many small channels, which appear not to bear
any special name.
=Wadi Medarai=, which forms the Wadi Ibib by its junction with Hasium,
ten kilometres due east of Gebel Um Rasein, has its main head in Gebel
Medarai, its length along its main channel being about twenty-five
kilometres. By numerous tributaries, many of which contain abundance
of trees and scrub, it drains the whole of the high hill country
between Gebel Medarai and Gebel Um Rasein, and it also takes a part
of the drainage from Kwat Hewah. One of its heads is said to lead
to a rather difficult pass, south of Gebel Medarai, into the =Wadi
Kirwau=, a tributary of Feqoh. For the first ten kilometres or so
of its length, Wadi Medarai courses a little north of east; it then
receives the feeder from Kwat Hewah above referred to, and changes
its direction to a little south of east, passing close north of Gebel
Um Rasein on its way to join Wadi Hasium on the sandy plain of the
numerous feeders of Wadi Medarai from the hills west and north of
Um Rasein, the principal is =Wadi Merdiyeb=, which originates ten
kilometres south-west of Gebel Um Rasein by the splitting of Wadi
Abu Hireiq. From this point of origin, it runs in a north-easterly
direction in a rather sinuous course among the hills for about twelve
or thirteen kilometres, joining Wadi Medarai close north of Gebel Um
Rasein. Another little feeder of Wadi Medarai, though only about two
kilometres long, is of some importance from its leading to =Bir Um
Rasein=, a small well among the north foot-hills of Gebel Um Rasein.
Vegetation ceases to be abundant both in Wadi Medarai and in Wadi
Hasium before their junction to form Wadi Ibib, and Wadi Ibib itself
is for the most part a barren sandy ill-defined channel coursing
north-eastward across a dreary plain for some fifty-seven kilometres
to Mersa Shab. In this fifty-seven kilometres its fall is very nearly
300 metres, giving an average slope of only a little over five metres
per kilometre. The slope of the lower part of Wadi Hasium is rather
steeper than this, while that of Wadi Medarai is about twice as great.
Public-domain text, read in full here on John Shaqi.
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