Geology -- Egypt; Nile River; Water-supply -- Egypt
17. =The Sudd region.=--The Sudd region of the Albert Nile lies north of
Ghaba Shambe and corresponds to that part of the river where not only do
the floods overflow the banks, but the summer supplies can do so in many
places. It is the delta of the river in a very embryonic stage. There
are two main branches to the river, the Albert Nile proper and the
Zeraf, which have both been already described. Both these rivers are
liable to be blocked by sudd or blocks of living vegetation. These
blocks are sometimes as much as 5 metres thick and capable of turning
nearly the whole supply of the river out of its course. They are formed
of papyrus, weeds and watergrasses, which grow on the half sandy half
peaty banks of the lagoons and marshes traversed by the river, and
which, under the double action of a rising flood and strong winds, are
torn up and driven into the channels wherever they are confined in
width, and there jammed into solid masses of floating weeds, filling the
whole width of the river, very nearly the whole depth, and sometimes
over a kilometre in length. In addition to the local weeds and grasses,
there are always at hand in high floods dense masses of pistea weeds
which have come from the upper waters of the Albert Nile south of
Dufile. While the sudd floats it is not so bad as when it sinks, as it
has done at block No. 15 north of Gaba Shambe, where the Nile has left
its course for 37 kilometres owing to sunken sudd. When the sudd sinks,
its becomes putrid and especially loathsome.
The Sudd region is unmistakably, as Lombardini pointed out years ago, an
old lake which has silted up and become full of peat and sand deposits.
At one time the lake must have had an extreme length of 400 kilometres
and width of 400 kilometres and been a larger sheet of water than lake
Victoria. The Sobat river flowed into it, and the Blue Nile may have
flowed backwards up the bed of the present White Nile for tens of
thousands of years. The north-east corner has been better filled with
deposit than any other part.
The dense masses of papyrus and water-grasses which shut out the horizon
in every direction intimidated the expedition sent up the Nile by Nero,
and it returned northwards without having accomplished anything. From
Nero’s time to that of Mehemet Ali little was known of these regions.
Mehemet Ali made a determined effort to discover what lay beyond these
inhospitable regions, and sent up a well-equipped expedition under
D’Arnaud.
Public-domain text, read in full here on John Shaqi.
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