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 entirely separated by wadis, rises to 620 metres above sea;
its summit is marked by a triangulation beacon in latitude 22°
10′ 50″, longitude 35° 54′ 0″. In occupying Adar Aweib as
a station, it was approached from the Bani Sana pass by following
down the Wadi Warabeit and then turning up the Wadi Wieqwer, which
leads to the eastern foot of the mountain. The camp was placed
about a kilometre north-west of the beacon, at an altitude of 284
metres above sea, and the climb of 336 metres to the top took only
an hour and a half. A great variety of flowers could be gathered
in the lower part of the ascent; the upper portion was slippery,
the slopes consisting of debris of decomposed granite resting just
at the angle of repose. In descending from the mountain, I went
northwards on foot, whence a steep pass led down to Bir Meheriqa,
in the Wadi Di-ib; but the camels had to go round the south end of
the mountain by Wadi el Qurat, as the pass was too steep for them.
To the south of the group of hills just described, there is a rugged
tract of low hills stretching away south to Gebel Shiab. Eastwards
this tract becomes lower and more sandy, terminating in a sandy plain
with low rocky ridges, over which the Wadi Di-ib pursues its northward
course, becoming closed in again by hills abreast of Adar Aweib.
=The Mountains of the Alaqi Basin West of Adar Qaqa.=
The mountains of this group, which are scattered over an area of
some 5,000 square kilometres between latitudes 22° 0′ and 22°
22′, and longitudes 34° 0′ and 35° 20′, are comparatively
little known. The positions and heights of all the principal peaks
have been fixed by triangulation from considerable distances; but
with the single exception of Gebel Muqsim, which was occupied by
Mr. Villiers Stuart as his terminal point, none of the area has yet
been officially surveyed.
The positions determined for the principal peaks will be found
included in the list on pp. 51 to 64, and a general idea of the
relative positions of the mountains and drainage lines will be
obtained from the orographical map on Plate I. A brief reference
only to the principal mountains is possible here.
=Gebel Anweiyib= (921 metres) and =Eir Arib= (1,112 metres) are on
the main watershed. As seen from the north, the former appeared as
a long dark range, the latter as a light-coloured high short ridge
with a peak at its western end.
=Gebels Duag= (1,328 metres) and =Himeitra= (1,231 metres)
are connected with the watershed range of Adar Qaqa and Is by
westward-running spurs. Gebel Himeitra is a landmark for a well,
Bir Himeitra, which is situated a little south of the mountain,
and also for the ruins of Darahib, which lie in the Wadi Alaqi some
twelve kilometres south-south-west of it.
=Gebel Heianai= (1,256 metres) is a long range of mountains between
the Wadis Bint el Feqoh and Defeit.
=Gebel Heleikonti= (1,151 metres) appeared from the north as a short
high steep ridge with a little peak at its western end.
Public-domain text, read in full here on John Shaqi.
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