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
=Wadi Lahami=, which enters the sea north of the peninsula of Ras
Benas, is well known by reason of the easy pass over the main
watershed at its head forming an important means of access to
Berenice from the west. At this point, four kilometres north-east
of the white quartz cone called Marwot Elemikan, the watershed is
sandy, level, and low, being only 590 metres above the sea. The
drop on crossing the watershed is fairly rapid, the wadi winding
about among the hills in a general north-easterly direction. About
six kilometres below its head, Lahami receives the =Wadi Um Karaba=,
which drains the south face of Gebel Abu Gurdi. A little further on,
=Wadi Eidab= enters from the south-east; this feeder is said to head
in a rough steep pass over the hills into the Wadi Abu Daba. After
passing between the high hills of Gebels Um Goradi and Um Gunud, Wadi
Lahami receives the short =Wadi Um Gunud=, in which there are two
well known galts, or rock basins forming reservoirs of rain water;
these contained good supplies in 1906-7. Lower down, Wadi Lahami
crosses a stony sloping plain, where it receives the drainage from
the north and east flanks of Gebel Abu Gurdi and from the mountains
to the north of it, by a series of feeders, the principal of which
are =Wadi Um Rishan=, =Wadi Um Homar=, and =Wadi Sefent=. East of
the plain there is a sort of shunt or loop-line of Wadi Lahami,
called the =Wadi Abreik=, which is preferred to the main channel
for a road. Just receiving Wadi Sefent, Wadi Lahami turns sharply
eastward, and then north-eastward, receiving as feeders =Wadis Um
Khuzama=, =Um Ghobasha=, and =Gumudlum=, draining Gebels Um Sellim
and Gumudlum to the north; these feeders are said to contain natural
reservoirs full of water after rain. From the south, Lahami is fed by
the =Wadis Um Eshub= and =Abu Marwa lil Lahami=, draining the lower
hill country. The lower course of Wadi Lahami has not been traced in
detail. It passes north-west of the well marked granite peak called
Gebel Um Huk, as remarked above, and reaches the sea north of the
peninsula of Ras Benas. To get to Berenice, one leaves Wadi Lahami
about twenty-four kilometres below the pass at its head, and turns
off south-east up the tributary Wadi Abu Marwa, which leads to Wadi
Naait by an easy road.
Wadi Lahami is well supplied with trees; it presented a very green
appearance early in 1906, but the absence of rain for a year made
it much more desolate looking in 1907, all the foliage being then
blackened and withered. Its length is approximately fifty kilometres,
its average slope twelve metres per kilometre, and the area of its
basin is about 650 square kilometres.
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account