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
=Gebel Abu Hamamid= is a great ridge of hard greenish schists towering
above the surrounding mountains to a height of 1,747 metres above
sea. Its crest is broken into a number of separate summits, which
appear from most aspects of almost a sugar loaf form; the beacon
is on the most northerly and highest of these, its position being
latitude 24° 14′ 41″, longitude 34° 47′ 38″. The mountain
is best ascended from the Wadi Um Semiuki, a tributary of Huluz,
which drains its north-east face. By ascending this wadi till camels
could go no higher owing to its increasingly rough and stony floor,
I was able to pitch a camp at 865 metres above sea-level and two and
a quarter kilometres north-east of the summit, leaving an ascent of
882 metres to be made on foot. The ascent, which occupied four hours,
was free from difficulty till within about one hundred metres of the
top, but the last portion was extremely steep and was only negotiated
with considerable trouble; it represents pretty nearly the limit of
possibility in getting instruments up difficult places. Once the top
was reached, however, the magnificence of the view obtainable, and the
excellence of the point as a station for triangulating the principal
peaks among the thousands visible, seemed an ample recompense for the
trouble of reaching it. The top of the ridge (_see_ Plate VII, p. 166)
is very rough and narrow, only a little over a metre wide, and it is
difficult to find a spot near the summit where one can spread one’s
blankets for the night with even a slight approach to comfort. The
eight nights of enforced bivouacking which I was obliged to spend on
the top of Abu Hamamid in February 1906, before I could complete my
observations, belong to the least pleasant of my experiences in the
desert. A little work only was possible the first day, owing to haze
obscuring the more distant peaks. On the second day clouds enveloped
us in a wet drizzle, and a bitterly cold north wind blew with great
violence; a rude rubble shelter which my men built on the summit,
covered with a blanket, was a very poor protection, and I found it
better to throw a rubble embankment across a steep gully on the lee
side, forming a small level platform where we were sheltered from the
biting wind. For the next five days, we were alternately wrapped in
clouds or left free under a brilliant blue sky with clouds covering
all the surrounding country. It was curious on these days to look over
the surface of the clouds, as over a boundless level sea, with only
the highest peaks projecting sharp and black above the white surface,
and to see the sun rise and set exactly as though one were on the
ocean. Then at last the clouds began to disappear, and on the first
clear day a very large amount of triangulation was accomplished, all
the more prominent peaks within a radius of about sixty kilometres
being observed. Gebel Abu Hamamid forms a culminating point on the
Nile — Red Sea watershed, its eastern parts draining to Wadi Huluz
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