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
and its western ones to Wadi Abu Hamamid, a tributary of Wadi Kharit.
PLATE XII.
[Illustration]
[Illustration: Typical Views among the Mountains of Hamata and Abu
Hamamid. (The high peak in the distance in the lower view is Gebel
Hamata).]
=Gebel Um Semiuki= is a sharp cone rising to 1,283 metres above the
sea among a mass of lower hills three kilometres north-east of Gebel
Abu Hamamid. It is of a reddish aspect, due to a film which covers
the weathered surface of the green and grey hornfels of which it is
composed. It is drained by the Wadi Um Semiuki.
=Gebel Abu Argub= is a very conspicuous mountain, almost conical in
shape, seven and a half kilometres south-south-west of Gebel Abu
Hamamid, from which it is separated by lower hills. To the south,
Gebel Abu Argub overlooks the plain of Selaia. Its peak, 1,690 metres
above sea-level, is a good landmark from the south and west.
=Gebel Kahfa= is a many-peaked mountain of granite rising abruptly
to a height of 1,018 metres above sea from among lower hills of dark
schists, nineteen kilometres south-west of Gebel Abu Hamamid. It is
detached from the main mountain-mass, being separated from it by the
heads of Wadi Um Retba. Its faces are in many places sheer precipices
of several hundred metres (_see_ Plate XIII), but the ascent of it
from the north is not very difficult. In occupying Kahfa as a station
I approached it from Bir Shadli by a well-marked track which skirts
the western foot-hills and leads to the Wadi Helie. Leaving this track
where it crosses Wadi Um Hargal some six kilometres from Bir Shadli, I
ascended the Wadi Um Hargal and crossed the pass at its head into the
head of Wadi Um Retba, where I pitched my camp at an altitude of 563
metres, at the foot of Gebel Kahfa 1·3 kilometres north-north-east of
the beacon on its summit. The climb of 455 metres from this camp to
the top occupied three hours. There is good bivouacking ground close
east of the summit, between two ridges. The beacon which marks the
triangulation point is in latitude 24° 8′ 18″, longitude 34°
38′ 55″. A walk round the top is full of interest; one can reach
many points overlooking tremendous precipices, and the forms assumed
by the granite peaks are very remarkable. On the west side of the
mountain is a rather large open space forming the head of Wadi Helie,
but elsewhere one is surrounded by low hills. The principal drainers
of Kahfa are the Wadis Um Hargal and Um Retba (tributaries of Wadi
el Sheikh) to the north, and Helie and Abu Hashim (tributaries of
Wadi Kharit) to the south.
=Gebel Medsus= is a small group of high hills rising among lower
ones between Gebel Abu Hamamid and Bir Shadli.
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