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 Naait=[92] is a narrow tortuous gorge, with a sandy floor
shut in by high hills, coursing eastward to the coast plain a
little south of the 24th parallel. Though only a small wadi some
sixteen kilometres in length, it is well known because it forms
the usual road from Wadi Lahami to Berenice. Its actual head has
not been surveyed, but lies probably between the mountains of Um
Gunud and Um Hegilig. Its principal feeders are =Wadis Um Sumer=
and =Abu Marwa lil Naait=, which enter it from the north-west, and
=Wadi Abu Ghalqa=, entering from the north and draining the granite
hills called Gebel Abu Ghalqa. All three of these feeders enter Naait
near together, some ten kilometres before it emerges on the plain;
the lower part of the wadi is free from lateral branches. The fall
is ten metres per kilometre among the hills. On emerging from the
hills on to the sandy coast plain, it joins an ill-defined drainage
line called =Wadi el Mukhit=, which enters the sea at Port Berenice,
some fifteen kilometres further east. The name Wadi el Mukhit is also
given to other ill-marked drainage lines entering Port Berenice from
the sandy tract between the hills of the main land and the hills
of the peninsula of Ras Benas. Some three kilometres north-east
of the mouth of Wadi Naait, on the coast plain, is a conspicuous
isolated low hill, forming a well-known landmark and called =Grain el
Rih=. The plain drained by Wadi el Mukhit is a dreary sandy waste,
and the crossing of it in a high wind is very trying by reason of
the immense clouds of sand raised and carried in the air.
Public-domain text, read in full here on John Shaqi.
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