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s of the actual geography of South Africa (i.e., from primeval times to the present day), does, or does not, extend into Northern Africa. Looking at that much broader portion of the continent, we have some reason to surmise that the higher mountains also form, in a general sense, its flanks only."--President's Address, Royal Geographical Society, 1852, p. cxxiii. The characteristics of the rainy season in this wonderfully humid region may account in some measure for the periodical floods of the Zambesi, and perhaps the Nile. The rains seem to follow the course of the sun, for they fall in October and November, when the sun passes over this zone on his way south. On reaching the tropic of Capricorn in December, it is dry; and December and January are the months in which injurious droughts are most dreaded near that tropic (from Kolobeng to Linyanti). As he returns again to the north in February, March, and April, we have the great rains of the year; and the plains, which in October and November were well moistened, and imbibed rain like sponges, now become supersaturated, and pour forth those floods of clear water which inundate the banks of the Zambesi. Somewhat the same phenomenon probably causes the periodical inundations of the Nile. The two rivers rise in the same region; but there is a difference in the period of flood, possibly from their being on opposite sides of the equator. The waters of the Nile are said to become turbid in June; and the flood attains its greatest height in August, or the period when we may suppose the supersaturation to occur. The subject is worthy the investigation of those who may examine the region between the equator and 10 Deg. S.; for the Nile does not show much increase when the sun is at its farthest point north, or tropic of Cancer, but at the time of its returning to the equator, exactly as in the other case when he is on Capricorn, and the Zambesi is affected.* * The above is from my own observation, together with information derived from the Portuguese in the interior of Angola; and I may add that the result of many years' observation by Messrs. Gabriel and Brand at Loanda, on the west coast, is in accordance therewith. It rains there between the 1st and 30th of November, but January and December are usually both warm and dry. The heavier rains commence about the 1st of February, and last until the 15th of May. Then no rain fall
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