[The Discovery of the Source of the Nile by John Hanning Speke]@TWC D-Link bookThe Discovery of the Source of the Nile INTRODUCTION 2/24
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.
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