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
As the Arabs do not keep thermometers, scientific instruments, or
properly distributed months and seasons, I must say for them that from
2° to 6° south latitude we found the mean temperature in the hottest
month, August, to be only 80°; that Uganda must be quite 4000 feet
above the sea, to be higher than the lake which it borders; that the
rainy season is during our winter months, but most so in the spring;
and that the rivers, as we see by the Malagarazi, increase more after
than before that date; that as the movement of the rains tends from
the southward to the northward, advancing with the sun, the same
influence that swells the Malagarazi would also affect the Uganda
rivers, as they rise merely on opposite sides of the axis of the same
mountains. The Arabs say, as we also have found it, "that thunder
accompanies nearly all the storms, and the lightning there is
excessive, and so destructive that the King of Uganda expresses the
greatest dread of it--indeed his own palace has been often destroyed
by lightning. The Kitangulé and Katonga rivers are affected by the
rainy season in the same proportion as the Malagarazi, and flow
north-easterly towards the lake.[65] There the Kivira (island) river
(Nile) of which they bring information, flows somewhere to the
northward, and is not a slow sluggish stream like the other two, but
is rapid and boisterous, showing that the country drops to the
northward." Now here, in 3° north latitude, where this river is said
to flow with such great rapidity, I think will be found the southern
base-line of those small hills, 2000 feet high, lying to the south of
Gondokoro, as the missionaries describe them; though these hills, to
any one looking at them from the northern side, where the land is low,
might appear a barrier to the waters of the lake lying beyond them.
This idea would not occur to any one standing on the southern side,
where the land is nearly, if not quite, as high as these hills
themselves. Indeed, from the levels given, the two countries about
Kibuga[66] (Palace of Uganda) and Gondokoro may be described as two
landings, with the fall between them representing a staircase formed
by the hills in question. The country in latitudes 2° and 5° north is
therefore terraced like a hanging garden.[67]
Public-domain text, read in full here on John Shaqi.
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