The National Geographic Magazine, Vol. I., No. 2, April, 1889 — John Shaqi
The National Geographic Magazine, Vol. I., No. 2, April, 1889Various
History
The National Geographic Magazine, Vol. I., No. 2, April, 1889
Various
Geography -- Periodicals
Careful computations have been made to ascertain the average elevation
of the continent. The mean of the most careful estimates is a little
over 2,000 feet. The interior is therefore elevated above the miasmatic
influences of the coast, but exactly what effect this elevation has
upon the temperature can only be ascertained after careful
investigation and a series of observations. North of Guinea and
Senegambia the coast is less unhealthy; but, as the Desert of Sahara
extends to the ocean, the country is of little value, and is therefore
left to the native tribes, unclaimed by Europeans.
In the International Scientific Series it is stated that there are in
Africa ten active volcanoes,--four on the west coast, and six on the
east,--but I have not found any corroboration of this report, and think
it very doubtful if there are any volcanoes now in eruption. The Kilima
Njaro and Kamerun were formerly active volcanoes, for the craters still
exist. In the south the diamond-fields are of volcanic ash formation.
EQUATORIAL AFRICA.
The lake region of Africa stretches from the head waters of the upper
Nile three degrees south, to the waters of the Zambezi, fifteen degrees
south,--a lake region unequalled, in extent and volume of water, except
by our lakes. Here is the Victoria Nyanza, the queen of inland seas,
4,000 feet above the sea-level; and a long series of lakes, great and
small, at equal elevation. The more striking are Bangweolo to the
south-west, the grave of Livingstone, and Nyassa on the south-east. In
their depths the Nile, the Kongo River, and the Shire (the main branch
of the Zambezi) have their source.
The great belt of equatorial Africa, situated between the 15th parallel
of north latitude and the 15th parallel of south latitude, has
continuous rains, is everywhere well watered, and has a rich and
fertile soil. Some portions are thickly populated, and it is capable of
sustaining a dense population. North and south of this belt there are
two other belts of nearly equal width. In each of these belts there are
wet and dry seasons, with abundant rain for the crops. The heaviest
rainfall in the north belt is in June, while in the south belt it is in
December. The rainfall gradually grows less toward the north, and also
toward the south, until it ceases in the Desert of Sahara on the north,
and in the Desert of Kalahari on the south. On the edge of these
deserts are Lake Chad on the north, and Lake Ngami on the south. North
of the Desert of Sahara, and south of the Desert of Kalahari, there is
an abundant rainfall, a healthy climate, and fertile soil. Morocco,
Algiers, and Tripoli, on the Mediterranean, are in the north region;
and Zulu-Land, the Orange Free State, and Cape Colony, in the
corresponding region of the south.
Public-domain text, read in full here on John Shaqi.
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