The Discovery of the Source of the Nile — John Shaqi
The Discovery of the Source of the NileSpeke, John Hanning
History
The Discovery of the Source of the Nile
Speke, John Hanning
Africa, East -- Description and travel; Nile River; Nile River Valley -- Discovery and exploration; Uganda -- Description and travel
The continent of Africa is something like a dish turned upside down,
having a high and flat central plateau, with a higher rim of hills
surrounding it; from below which, exterially, it suddenly slopes down
to the flat strip of land bordering on the sea. A dish, however, is
generally uniform in shape--Africa is not. For instance, we find in
its centre a high group of hills surrounding the head of the Tanganyika
Lake, composed chiefly of argillaceous sandstones which I suppose to
be the Lunae Montes of Ptolemy, or the Soma Giri of the ancient Hindus.
Further, instead of a rim at the northern end, the country shelves down
from the equator to the Mediterranean Sea; and on the general surface of
the interior plateau there are basins full of water (lakes), from which,
when rains overflow them, rivers are formed, that, cutting through the
flanking rim of hills, find their way to the sea.
Atmospheric Agents
On the east coast, near Zanzibar, we find the rains following the track
of the sun, and lasting not more than forty days on any part that
the sun crosses; whilst the winds blow from south-west or north-east,
towards the regions heated by its vertical position. But in the centre
of the continent, within 5 deg. of the equator, we find the rains much more
lasting. For instance, at 5 deg. south latitude, for the whole six months
that the sun is in the south, rain continues to fall, and I have heard
that the same takes place at 5 deg. north; whilst on the equator, or rather
a trifle to northward of it, it rains more or less the whole year round,
but most at the equinoxes, as shown in the table on the following page.
The winds, though somewhat less steady, are still very determinable.
With an easterly tending, they deflect north and south, following the
sun. In the drier season they blow so cold that the sun's heat is not
distressing; and in consequence of this, and the average altitude of the
plateau, which is 3000 feet, the general temperature of the atmosphere
is very pleasant, as I found from experience; for I walked every inch
of the journey dressed in thick woollen clothes, and slept every night
between blankets.
The Number of Days on which Rain fell (more or less) during the March of
the East African Expedition from Zanzibar to Gondokoro.
1860 Days on 1861 Days on 1862 Days on
which which which
rain fell rain fell rain fell
Public-domain text, read in full here on John Shaqi.
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