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 Gerf= is the collective name given to a number of rather
complicated drainage channels forming tributaries to Wadi Muelih. The
principal heads are to the east and west of Gebel Nugrus. The eastern
head is called =Wadi Hangalia=; it commences at about an altitude
of 811 metres due east of the highest point of Gebel Nugrus, at a
difficult pass leading over the main watershed to Wadi el Nom, and
curves round the north spurs of Gebel Nugrus to join the western
head. In the Wadi Hangalia are some old ruins of a mining camp,
and also some recent prospecting workings and a well giving a poor
supply of water. The Western head of Wadi Gerf commences in nearly
level ground on the main divide west of Gebel Nugrus, at an altitude
of 691 metres. These two main heads unite close to the east of Gebel
Ras Shait, whence Wadi Gerf courses about north-west through low
hills. A third head is in lat. 24° 52′, at a pass leading into
Wadi Um Khariga. A fourth, called =Rod el Atut=, takes the drainage
from all sides of the conspicuous black cone of Gebel Atut. A fifth,
called =Rod Um el Farag=, drains from the mass of moderately high
hills further west called Um el Huetat; these hills contain some old
mines, chiefly in talc schists. The drainages from these various heads
all eventually take a west-south-west course among low hills and over
a sandy plain and enter Wadi Muelih by several openings near longitude
34°. Minor tributaries are =Wadi Abu Seyal= and =Wadi Um Seyal=,
south-east of Gebel Atut, =Rod el Ligaia=, in longitude 34° 10′;
and =Rod el Ligah=, in latitude 24° 50′.
The principal hills of the plain over which Wadi Gerf and its
tributaries run their course are some very remarkable small black
peaks collectively called Khusa el Faraon, a light coloured hill
called Marwot Rod el Ligah, and a ridge called Erf el Sagur; these
two last rise to 514 and 523 metres above sea-level respectively.
Wadi Gerf possesses a fair amount of vegetation, except where it
meanders over the sandy plains; in the tributaries Wadi Um Seyal
and Wadi Abu Seyal acacia trees are specially numerous.
=Wadi Sibrit= is a long narrow wadi following a course somewhat south
of west, originating to the west of Gebel Mudergeg and joining Wadi
Muelih in longitude 33° 50′. It possesses many trees and a good
well, =Bir Sibrit=. This latter is an excavation in the wadi floor,
in longitude 33° 58′; it is said to yield a constant supply. In
the spring of 1906 I found the water was at a depth of eight metres
below the surface, and of good quality.
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