[A Popular Account of Dr. Livingstone’s Expedition to the Zambesi and Its Tributaries by David Livingstone]@TWC D-Link book
A Popular Account of Dr. Livingstone’s Expedition to the Zambesi and Its Tributaries

CHAPTER II
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At Kuruman, when the thermometer stood above 84 degrees, rain might be expected; at Kolobeng, the point at which we looked for a storm was 96 degrees.

The Zambesi is in flood twice in the course of the year; the first flood, a partial one, attains its greatest height about the end of December or beginning of January; the second, and greatest, occurs after the river inundates the interior, in a manner similar to the overflow of the Nile, this rise not taking place at Tette until March.

The Portuguese say that the greatest height which the March floods attain is thirty feet at Tette, and this happens only about every fourth year; their observations, however, have never been very accurate on anything but ivory, and they have in this case trusted to memory alone.

The only fluviometer at Tette, or anywhere else on the river, was set up at our suggestion; and the first flood was at its greatest height of thirteen feet six inches on the 17th January, 1859, and then gradually fell a few feet, until succeeded by the greater flood of March.

The river rises suddenly, the water is highly discoloured and impure, and there is a four-knot current in many places; but in a day or two after the first rush of waters is passed, the current becomes more equally spread over the whole bed of the river, and resumes its usual rate in the channel, although continuing in flood.


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