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
it is situated about three kilometres up the Wadi Nubitra, among
high hills. One of the many heads of the small Wadi Nubitra leads
northwards by an easy pass into the head of Wadi Hamida.
The =Wadi Hamida= heads in the mountain of the same name, and courses
parallel to Wadi Aqwem, from which it is separated by a long ridge
of high hills. About one and a half kilometres below its head at the
easy pass into Wadi Nubitra above referred to, it receives a small
gully from the east; by following up this gully, which is narrow and
tortuous, for about a kilometre, one can reach a tiny spring called
=Megwel Hamida=. When I visited it in April 1908, the spring was a
mere trickle, very salt; a galt a little further up the gorge was
dry at the same time, but bears signs of holding a useful store of
water after rain. About three kilometres below the gully containing
the spring, Wadi Hamida reaches an opening whence one can either
go south-east for two kilometres to the easy pass of Bani Sana, or
north-west through a gap in the longitudinal ridge which encloses the
wadi on the left. Wadi Hamida itself, however, keeps straight on its
course past Gebel Geror, and joins Wadi Baueiwai south-east of the
hill of Ti-Keferiai. The heads of Wadi Hamida contain a fair amount
of vegetation, but its lower parts are more barren and very sandy.
=Wadi Di-it= drains the north parts of the hill mass of Sul Hamid,
and courses north-east to reach the coast independently about latitude
22° 29′. It has not been explored, and is of no great importance;
vegetation in it is probably confined to its upper parts among the
hills. Of its total course of about thirty-five kilometres, a large
portion lies over the sandy coast-plain.
=Wadi Eikwan= is a broad shallow and sandy channel draining the high
jagged hill called Qash Amir and the eastern parts of the low hill
mass of Sul Hamid. Its head is about four kilometres south of Qash
Amir, in the flat sandy plain. Taking at first a northerly direction
past the west side of Qash Amir, it turns to the north-east further on
and crosses the coast-plain to reach the sea only a little south of
the mouth of Di-it. Its total length is about thirty six kilometres,
and its average slope is about nine metres per kilometre.
Public-domain text, read in full here on John Shaqi.
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