The Lake Regions of Central Africa: A Picture of Exploration, Vol. 1Burton, Richard Francis, Sir
History
The Lake Regions of Central Africa: A Picture of Exploration, Vol. 1
Burton, Richard Francis, Sir
Africa, Central -- Description and travel
The mountains are well supplied with water, which tastes sweet after the
brackish produce of the maritime valley, and good when not rendered soft
and slimy by lying long on rushy beds. Upon the middle inclines the
burns and runnels of the upper heights form terraces of considerable
extent, and of a picturesque aspect. The wide and open sole, filled with
the whitest and cleanest sand, and retaining pools of fresh clear water,
or shallow wells, is edged by low steep ledges of a dull red clay, lined
with glorious patriarchs of the forest, and often in the bed is a
thickly wooded branch or shoal-islet, at whose upper extremity heavy
driftwood, arrested by the gnarled mimosa-clumps, and the wall of
shrubs, attests the violence of the rufous-tinted bore of waves with
which a few showers fill the broadest courses. Lower down the channels
which convey to the plains the surplus drainage of the mountains are
heaps and sheets of granite, with long reaches of rough gravel; their
stony walls, overrun with vegetation, tower high on either hand, and the
excess of inclination produces after heavy rains torrents like
avalanches, which cut their way deep into the lower plains. During the
dry season, water is drawn from pits sunk from a few inches to 20 feet
in the re-entering angles of the beds. Fed by the percolations of the
soil, they unite the purity of springs with the abundance of
rain-supplies,--a comfort fully appreciated by down-caravans after the
frequent tirikeza, or droughty afternoon-marches in the western regions.
The versant of the mountains varies. In the seaward and the central
sections streams flow eastward, and swell the Kingani and other rivers.
The southern hills discharge their waters south and south-west through
the Maroro River, and various smaller tributaries, into the “Rwaha,”
which is the proper name for the upper course of the Rufiji. In the
lateral plains between the ridges, and in the hill-girt basins, stagnant
pools, which even during the Masika, or rainy season, inundate, but will
not flow, repose upon beds of porous black earth, and engendering, by
their profuse herbage of reeds and rush-like grass, with the luxuriant
crops produced by artificial irrigation, a malarious atmosphere, cause a
degradation in the people.
Public-domain text, read in full here on John Shaqi.
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