What Led to the Discovery of the Source of the NileSpeke, John Hanning
History
What Led to the Discovery of the Source of the Nile
Speke, John Hanning
Horn of Africa -- Description and travel; Nile River; Tanganyika, Lake
At the same time, I have no hesitation in saying that ten times as
much merchandise might be got at less expense, if the trade were
protected by government means, and put on a legitimate footing. Those
countries teem with cattle. The indigenous cotton is of very superior
quality. Indigo, sugar-cane, coffee, tobacco, sesamum, and indeed all
things that will grow in a tropical climate, may be grown there within
3° of the equator, in luxurious profusion, and without any chance of
failure owing to those long periodical droughts which affect all lands
distant more than 3° from the equator.
When I was sailing down the Nile, I could not help remarking to all
the pashas I visited how strange it appeared that men so civilised as
they were should be living in such a barren, hot, and glaring land as
Egypt, when the negroes on the equator were absolutely living in the
richest and pleasantest garden in the world, so far as nature has made
the two countries.
Now, though I have dwelt so markedly on the surprising fertility of
Uganda and Unyoro in particular, I do not wish it to be supposed that
I consider those countries alone to be exclusively rich, for I believe
there is a continuous zone of fertility stretching right across Africa
from east to west, affected only by the nature of the soil. In
advancing this argument, I hold that the greatest discovery I have
made in Africa consists in my positive knowledge regarding the rainy
system of Africa; and to exemplify it irrespectively of my
meteorological observations, I will state emphatically that as surely
as I have determined the source of the Nile to lie within 3° of the
equator, and that it cannot emanate from any point farther south,
because all the lands beyond that limit are subject to long periodical
droughts--so certain am I that the Tanganyika is supplied from the
same source, or rainy zone, though draining in the opposite direction.
Again, to its west also, from the same source of supply, the
head-waters of the Zambézi take their origin. Still farther west, the
fountains of the Congo must have their birth. Again, farther west
still, the Chadda branch of the Niger can alone be thus supplied, and
the same must be the case with the Gaboon river.
To carry this argument still farther, I would direct attention to the
periodical conditions of the Blue Nile and Niger rivers. Both of these
rivers rise in high mountains on the coast-range, at about 10° north
latitude, but on opposite sides of the continent. They are considered
large rivers, but only in consequence of their great floodings, when
the sun, in his northern declination, brings the rains over the seats
of their birthplaces; for when the sun is in the south they shrink so
low that the waters of the Blue river would never have power to reach
the sea were they not assisted by the perennial stream of the White
Nile.
Public-domain text, read in full here on John Shaqi.
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