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
The drainage from the low hills on the =Peninsula of Ras Benas=,
except for a small portion which joins Wadi Mukhit, reaches the sea
by a multitude of small wadis, none of which bear special names. The
hills being nearer to the south side of the peninsula than to the
north, the wadis draining southwards are on the whole much shorter
and steeper than those draining northwards, and the latter cross a
sloping plain two or three kilometres wide to reach the sea. Passage
across the hills from south to north is only possible to camels at
a few places. The southern wadis are mostly barren, but the northern
ones contain abundance of a dark coloured grass of which camels are
fond. There is no permanent water source on the peninsula, the nearest
reliable source of supply being a galt in Wadi Mindeit, on the main
land, about twelve kilometres west of Berenice. The tip of the low
sandy projection of Ras Benas is marked by a sheikh’s tomb, one
of the largest on the coast. It is chiefly built of wreckage cast
up on the beach. From the hills it looks like a rectangular rock,
and I determined its position by triangulation as latitude 23°
53′ 50″ N., longitude 35° 47′ 13″ E. The sheikh’s memory
appears to be greatly venerated by sailors, and several of my camel
men made pilgrimages to the tomb to pray.
The =Island of Mukawar=, about six kilometres south of the sandy tip
of the ras, is nearly two kilometres in length from north to south. I
did not visit it, but it has the appearance of being made of coral;
its highest point, near the south end, is thirty-four metres above
the sea-level.
=Wadi Abu Daba= drains the eastern flanks of Gebel Eidab and Gebel
Um Maiat, and courses eastward through the lower hill country to
the coast plain, where it joins the drainage from Naait in Wadi
Mukhit. The principal feeder of Abu Daba is =Wadi Murra= which enters
it from the south-west a few kilometres before its emergence on to
the plain. At the head of Wadi Abu Daba there is said to be a rough
steep pass over the mountains into Wadi Eidab. The place where Abu
Daba debouches on to the coast plain is marked by a group of low
bouldery looking granite hills called Khasheib Abu Daba.
=Wadi Abu Dibban= is a short wadi draining eastwards from the hills
across the coast plain to the sea a little north of Berenice. In its
course across the plain it passes a little north of a conspicuous
granite hill called Sikeit, a well known landmark five kilometres
north-west of Berenice.
=Wadi Mindeit= drains the hills between Gebel Um Maiat and Gebel
Kalalat, entering the sea at Berenice.[91] =Wadi Um Sellim lil
Mindeit=, a shorter wadi coursing across the plain a little further
south, is interesting as furnishing the nearest fresh water source
to Berenice; it leads to a rock basin or galt among the hills, where
rain water collects. This source is some ten or twelve kilometres
from Berenice.
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