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 Um Heshenib= is a great ridge situated twenty-two kilometres
north-west of Gebel Hamata. The beacon on its highest point,
in latitude 24° 20′ 49″, longitude 34° 50′ 53″, has an
altitude of 1,135 metres above the sea. Its lower parts are granite,
but the upper third is of dark schists, while the actual ridge on
which the beacon stands is a grey porphyrite. Gebel Um Heshenib is
drained to the north by the Wadi el Abiad, a tributary of Wadi Gemal,
and to the south by tributaries of Wadi Huluz. I ascended it on two
occasions from opposite sides. The north approach is the easier road
for camels, as they can pass easily up the broad and sandy Wadi el
Abiad, while to reach it from Wadi Huluz one has to journey over
a rather stony pass and along narrow stony wadis. But the climb
is longer from the north side, being one of 635 metres against 380
metres from the south, and the southern climb is easier as well as
shorter. It is interesting to note that as the ground south of the
mountain lies at an average level of 250 metres higher than that to
the north, the plumb-line ought from theoretical considerations to
be attracted to the south by several seconds, and this was found
to be the case when the mountain was used as a latitude station
(_see_ p. 47) There is a very difficult pass east of the mountain
from the head of Wadi el Abiad into a tributary of Wadi Huluz; I
was told that loaded camels could not possibly get over the pass,
and have reason to believe the statement true, as although I did
not consent my men were desirous of going over it and volunteered
to carry the baggage over themselves to relieve the camels.
Public-domain text, read in full here on John Shaqi.
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