Expedition to discover the sources of the White Nile, in the years 1840, 1841, Vol. 1 (of 2)Werne, Ferdinand
History
Expedition to discover the sources of the White Nile, in the years 1840, 1841, Vol. 1 (of 2)
Werne, Ferdinand
Nile River
17th December.—Immediately after sunrise we sailed S.S.E.; at eight
o’clock, S.S.W., and at nine o’clock, S.W. by S. The stream we
navigate is tolerably broad, and appears, so far as we can see over
the reedy-sea, to be the only one. On the right shore we have still
the dhellèb-palms of yesterday in sight; the land retreats towards
S.E., whilst the left shore comes nearer, and lets us see individual
tokuls and villages. Some blacks stand on the shore, which approaches
us at nine o’clock within gun-shot. They greet us and make signs,
but we cannot go to them on account of the reeds, willingly as we
would make their acquaintance, in order to provide ourselves again
with meat. Ten o’clock. The left shore appears to go S.W. with the
river, calculating from some trees and dhellèb-palms. The east wind
is tolerably strong; we make three miles. A large pelican was shot,
and there were found in the pouch under its bill twenty-four fresh
fish, the size of moderate herrings. This burden had impeded its
flight from our vessels, and prevented it from swallowing its prey,
on the death-shot, as is usual with these birds.
If we consider this enigmatical stream territory, we ask ourselves
whether the white river, of and _by itself_, with such a weight of
water, can maintain these lagoons under an African sun? Were the Nile
_one_ stream, it must flow off faster; for the rains have already
ceased here, and previously, indeed, under the Equator itself. How
could the Nile, which still shews its peculiar disposable mass of
water, in its main-stream, supply, quite _alone_, that enormous mass
of water, and even to the present time maintain under water these
immense reedy lakes, unless other tributary streams, the mouths of
which stagnate, owing to the level nature of the ground, and the
counter-pressure of the main-stream, supplied a nourishment great
beyond belief, to this, with which it equally rises and falls? For the
whole mass of water _in complexu_ must suffer an incredible diminution
during such a long tract in its slow ebbing, under a burning sun,
or this Bahr-el-Abiad must have real giant-springs in its source.
Public-domain text, read in full here on John Shaqi.
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