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
_28th March._—We navigated to the neighbouring island, and passed
by it on the left, N.E. by N., just as the sun was rising. Where is
the meat that was to be put to-day into the Egyptian flesh-pots? The
Shilluks will be delighted at having tricked the Turks, for they are
really an extremely vitiated people. According to nature, corruption
of morals cannot take place in the very earliest stage of life,
and there might have been, therefore, a previous cultivation here
which has now disappeared, and left only the bad parts behind. But
how could they have gone back to the naked state? Slight clothing is
even necessary here: a people that has once worn a fig-leaf never
throws it off, although a cynic here and there may choose to lead
a free dog-life.
We labour with oars, yet all is in vain against the north wind; the
river itself remains on the average N.W. as far as Khartùm. About
nine o’clock we halt at the right shore, and see herds and villages
of the Shilluks opposite to us; but we must make our appetites
disappear again—“_Quid juvat adspectus, si non conceditur
usus!_” Really it was very vexatious; and in addition thereto,
the new moon has appeared for the last two days, and yet my bold
countryman whistles and roars, which is so very unusual at this time
that we conclude the same phenomena is taking place on the Nile.
It has been considered as a thing decided that the periodical
north winds blow the rain from the Mediterranean Sea against the
mountain terrace of Habesh. But these are winds which blow also on
the Western Ocean, along the coast of Africa, and find no opposition
on the sea and further beyond: the periodical gales cannot ride at
anchor so conveniently on the not very high mountains of Habesh
and last until the counter gust from India ensues, or until the
clouds have impregnated all the air of Habesh, and at last fall,
from their weight, and bring refreshing rain to the country. The
Mediterranean Sea seems to me to afford too small a tract for the sun
and wind to be able to draw a mass of water from it, like that of a
small deluge. Therefore, I think that quite different phenomena lay
the foundation of these violent rains, and that Habesh, beyond the
equator, may have its conductors of moisture from the Indian Sea, as
well as Egypt by the electrical course of its Nile. Otherwise Habesh
would be enveloped in an eternal sea of clouds, for the north winds
would be bottled up there half a year, and, by the same argument,
the south winds the other six months.
[Illustration: MOUNT LINANJIN, FROM THE ISLAND OF TSHÀNKAR, TOWARDS
SOUTH EAST
27TH JANUARY, 1841.]
Public-domain text, read in full here on John Shaqi.
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