The natives of British Central Africa — John Shaqi
The natives of British Central AfricaWerner, Alice
History
The natives of British Central Africa
Werner, Alice
Ethnology -- Malawi; Malawi -- Description and travel; Malawi -- Social conditions
Lake Nyasa is a narrow trough, 360 miles long, between mountain-ranges
which hem it in closely on the west (sending down, during the rains,
innumerable small torrents from their steep slopes), and retreat
somewhat from it on the east, leaving room for a few larger, but still
inconsiderable streams, such as the Songwe, the Rukuru, the Bua, and one
or two more. The Shiré is the lake’s only outlet, flowing through a level
alluvial valley (something like a delta reversed) till, a little below
Matope, it comes to the edge of the plateau and plunges over in a series
of falls known as the Murchison Cataracts. These extend over forty miles
of river, and make a difference in its level of some 1200 feet, though
none of them, individually, are of any great height.
The level of the lake, and consequently of the river which it feeds,
is very different at different seasons of the year. During the rains,
and for some time after, steamers can go to the foot of the Murchison
Cataracts—the usual terminus is Katunga’s, about twelve miles below them.
In the dry season they cannot always come within sight of Chiromo, and,
during the great drought of 1903, the natives of that place were hoeing
their maize-gardens far out in the channel of the river. The salt Lake
Chilwa, east of the Shiré, disappeared almost, if not quite, at that
time, but reappeared with subsequent rains. It is thought, however, that
there is a continuous fall in the level of Nyasa, which is unaffected by
the rise and fall of successive seasons. In some places a series of old
beaches can be traced, ascending like terraces from the lake-shore to the
foot-hills.
This fall is attributed to several causes—the wearing away of the outlet
channel, allowing more water to escape; the disappearance of the forests
and consequent diminution of the rainfall; and the raising of the ground
by volcanic action. There are not now any active volcanoes in the
country, but earthquakes are common in the neighbourhood of the lake, and
there are hot springs near Kotakota, and also on Mount Morambala (Lower
Shiré). Mlanje Mountain is of volcanic origin; in the German territory,
north of Nyasa, there are numerous extinct volcanoes and crater-lakes.
Public-domain text, read in full here on John Shaqi.
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