Expedition to discover the sources of the White Nile, in the years 1840, 1841, Vol. 2 (of 2)Werne, Ferdinand
History
Expedition to discover the sources of the White Nile, in the years 1840, 1841, Vol. 2 (of 2)
Werne, Ferdinand
Nile River
_14th March._ We navigate again on the right side, and go at half-past
seven o’clock with libàhn from S. by E., immediately S.E.,
where the north-east wind remains contrary to us, notwithstanding
the narrow water-tract. Some small and still green reed-huts hang
on the shore, sheltered from the north wind: these are stations for
hunters of hippopotami and crocodiles, or for fishermen, who, however,
have gone away, and taken with them their working implements, for
they are frightened of us. The durra seems to thrive famously on the
half-sandy shore, and rises cheerfully above the reeds; probably it is
sown,—that is, a handful thrown here and there on the vacant spots.
Eight o’clock—E. by N., and N.E. by E. The upper margin of
the right shore is planted throughout with durra, and some small
fishing-huts shew that men dwell there. Ten o’clock.—Hitherto
always N.E. within considerable deviations, and then N. by E.; where
we halt at the corner of the right shore on account of the wind,
for the river goes still further to the left: level land above,
some underwood, and a village at a little distance. A quarter before
one.—N. by W., and about one, in a bend to the right. When the
crew relieve one another at the rope, they imitate to perfection
the Uh-uh-i-ih of the tribes on the upper part of the White Stream,
and during the towing itself they sing the song à-à-à-jòk-jòk,
which would be difficult for a white man to do. The force of the
water is directed here against the right shore, which is without any
crust of vegetation, and seems to ascend to the uppermost margin,
as is proved by the gradations being washed away, and the thin layer
of humus, one foot to one and a half high, decreases perpendicularly,
whilst the lower part of the soil displays unmixed clay. It certainly
required a powerful pressure of water to wash this primary deposit
to such a depth; the left shore, on the contrary, has a coating of
slime and vegetation down to the water.
Public-domain text, read in full here on John Shaqi.
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