The Anglo-Egyptian Sudan: a compendium prepared by officers of the Sudan government, Vol. 1 (of 2) — John Shaqi
The Anglo-Egyptian Sudan: a compendium prepared by officers of the Sudan government, Vol. 1 (of 2)Sudan. Wizarat al-Naql wa-al-Muwasalat
History
The Anglo-Egyptian Sudan: a compendium prepared by officers of the Sudan government, Vol. 1 (of 2)
Sudan. Wizarat al-Naql wa-al-Muwasalat
Sudan -- Description and travel; Sudan -- History
The causes of the flood are, briefly, as follows:—The rains in
southern Abyssinia cause the Sobat to rise about the middle or end
of April. The yellowish-white water caused by this flood reaches
Kodok the last week in April. The equatorial rains cause the Bahr
El Zeraf and White Nile, above the Sobat, to rise about the end of
May. The effect of the first rise is felt at Halfa about the 20th
May. The Blue Nile begins to rise about this time, and brings the
red fertilizing flood down to Khartoum about the 20th June, and
to Halfa about the middle of July. The muddy Atbara flood (June to
August) rises very rapidly after the Blue Nile, and causes the flood
to attain its maximum about the end of August; at this period the
river is muddiest. The White Nile continues to rise slowly, and its
effects (clear white water) are felt at Halfa till October, when it
falls very slowly. The Blue Nile falls rapidly after the middle of
September, and the Atbara has generally disappeared by October. The
Sobat begins to fall at Nasser early in December.
The Bahr El Ghazal rivers rise slightly in May. These soon subside,
and the main floods take place in July and August.
The above is a description of an average year. An early maximum
(_i.e._, about the middle of August) generally means a low summer
flood, and _vice versâ_. The flood at its height moves at about
100 miles a day (below the Atbara).[17]
The above dates vary largely in accordance with the time and amount
of rainfall in the upper valleys of the rivers.
Of the flood water annually brought down by the rivers, about half
now runs to waste into the Mediterranean sea. The Aswan dam regulates
and utilizes this to a certain extent, but a large proportion remains
over. This it is proposed to utilize in the future for irrigating the
Sudan by means of flood and catchment basins; but the time is still
distant when this surplus will be entirely devoted to this purpose.
[Sidenote: Historical.]
Up to comparatively recent times the sources of the Nile were involved
in mystery.[18] In ancient days many guesses were hazarded at their
origin, some geographers maintaining that the Nile rose in the Atlas
Mountains of Marocco; others were positive that the Niger formed the
upper portion of the great river. During the 17th and 18th centuries
it was held that the sources were to be found in the “Mountains of
the Moon.” These have since been speculatively identified with the
Ruwenzori Mountains between Lakes Albert and Albert Edward, and, if
this theory is correct, the ancient geographers were not so far out.
Public-domain text, read in full here on John Shaqi.
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