Geology -- Egypt; Nile River; Water-supply -- Egypt
The maximum discharge of the Albert Nile at Hillet-el-Nuer may be taken
as 450 cubic metres per second, and into Lake No as 320 cubic metres per
second. The water of the river is dark-coloured and contains no
sediment. Very little ambatch is met with north of Ghaba Shambe.
Between Ghaba Shambe and Lake No on the left bank, in the first 120
kilometres, three channels carrying very appreciable quantities of water
flow into the Albert Nile. These are considered to be the tails of the
river Yei. At Hillet-el-Nuer, about 170 kilometres north of Ghaba
Shambe, a branch takes off from the west side of the Albert Nile, known
as Gage’s channel, with 35 metres of clear waterway, 1 metre depth and
0·60 metre per second velocity, discharging 20 cubic metres per second.
This stream flows westwards and is lost in the swamps. On the right
bank, downstream of Ghaba Shambe, are the two heads of the Bahr Zeraf,
one natural and the other artificial made by Sir Samuel Baker. About 90
kilometres north of Ghaba Shambe a few spills take water towards the
Zeraf river.
[Illustration: PLATE VI.
THE ALBERT NILE.
FROM GONDOKORO TO THE SOBAT JUNCTION
Scale 1 : 2,000,000
Lith. Sur. Dep. Cairo.
Part of Albert Nile
_South of Sudd No. 15_]
From Lake No to the Sobat mouth, on a length of 134 kilometres is the
tail reach of the Albert Nile. The Albert Nile flows into Lake No in its
south-eastern corner and leaves it on its east side. On the west side
the Gazelle river flows into the lake. Lake No has an area of some 20
square kilometres in times of low supply and 100 square kilometres in
flood. In low supply the depth is between 1·50 and 2·50 metres. In the
reach between Lake No and the Sobat mouth, the river is very fairly
straight; the summer channel is about 170 metres wide and as a rule
about 5 metres deep upstream of the mouth of the Lolle, though in one
place about 8 kilometres from Lake No it becomes only 50 metres wide for
a short distance. Between the tail of the Lolle river and the mouth of
the Sobat river, the summer width widens out to about 400 metres with 3
metres depth of water. However extensive the marshes may be, the high
land forming the limit of the inundation is everywhere in this reach
visible from the main stream. The Gazelle river, which flows into Lake
No, has a discharge varying from 0 to 40 cubic metres per second. The
Lolle river which flows in on the left bank upstream of the Sobat mouth
is probably an arm of the Albert Nile or an overflow of the Gazelle and
has a discharge varying from 0 to 40 cubic metres per second. On the
right bank, the Zeraf river flows into the Albert Nile, with a discharge
varying from 30 to 160 cubic metres per second. The Megahid river flows
in 30 kilometres below the tail of the Zeraf river and adds an
undetermined quota of water.
Public-domain text, read in full here on John Shaqi.
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