Online Encyclopedia

KALAHARI DESERT

Online Encyclopedia
Originally appearing in Volume V15, Page 638 of the 1911 Encyclopedia Britannica.
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KALAHARI
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DESERT
  , a region of South Africa, lying mainly between 20° and 28° S. and 19° and 24° E., and covering fully 120,000 sq. m . The greater
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part of this territory forms the western portion of the (
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British) Bechuanaland
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protectorate, but it extends south into that part of Bechuanaland annexed to the Cape and west into German South-West Africa . The Orange
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river marks its
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southern limit; westward it reaches to the
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foot of the Nama and Damara hills, eastward to the cultivable parts of Bechuanaland, northward and north-westward to the valley of the Okavango and the bed of Lake
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Ngami . The
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Kalahari, part of the immense inner table-
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land of South Africa, has an
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average
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elevation of over 3000 ft. with a general slope from east to west and a dip northward to Ngami . Described by Robert Moffat as " the southern
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Sahara," the Kalahari resembles the
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great
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desert of North Africa in being generally arid and in being scored by the beds of dried-up rivers . It presents however many points of difference from the Sahara . The
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surface
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soil is mainly red sand, but in places
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limestone overlies shale and conglomerates . The ground is undulating and its appearance is comparable with that of the ocean at times of heavy swell . The crests of the waves are represented by sand
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dunes, rising from 30 to 100 ft.; the troughs between the dunes vary greatly in breadth . On the eastern border long tongues of sand project into the veld, while the veld in places penetrates far into the desert . There are also, and especially along the river beds, extensive mud flats . After heavy rain these become pans or lakes, and
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water is then also found in mud-bottomed pools along the beds of the rivers .

The water in the pans is often brackish, and in some cases thickly encrusted with

salt . Pans also occur in
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crater-like depressions where rock rises above the desert sands . A tough, sun-bleached grass, growing knee-high in tufts at intervals of about 15 in., covers the dunes and gives the general colour of the landscape . Considerable parts of the Kalahari, chiefly in the west and north, are however covered, with dense scrub and there are occasional patches of
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forest . Next to the lack of water the chief characteristics of the desert are the tuberous and herbaceous
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plants and the large numbers of big
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game found in it . Of the plants the most remarkable is the water-melon, of which both the bitter and sweet variety are found, and which supplies both man and beast with water . The game includes the lion,
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leopard, hippopotamus,
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rhinoceros,
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buffalo,
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zebra, quagga, many kinds of
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antelope (among them the
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kudu and
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gnu), baboon and
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ostrich . The
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elephant,
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giraffe and
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eland are also found . The hunting of these three last-named animals is prohibited, and for all game there is a close time from the beginning of September to the end of
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February . The
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climate is hot, dry and healthy, save in the neighbourhood of the large marshes in the north, where malarial fever is prevalent . In this region the drainage is N.E. to the great Makarikari marsh and the Botletle, the river connecting the marsh with the Ngami
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system . In the south the drainage is towards the Orange .

The Molopo and the

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Kuruman, which in their upper course in eastern Bechuanaland are perennial streams, lose their water by evaporation and percolation on their way westward through the Kalahari . The Molopo, a very imposing river on the map, is dry in its
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lower stretches . The
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annual rainfall does not exceed ro in . It occurs in the summer months, September to March, and chiefly in thunderstorms . The country is suffering from progressive desiccation, but there is good evidence of an abundant supply of water not far beneath the surface . In the water-melon season a few white farmers living on the edge of the desert send their herds thither to graze . Such few spots as have been under cultivation by artificial irrigation yield excellent returns to the farmer; but the chief commercial products of the desert are the skins of animals . The Kalahari is the home of wandering Bushmen (q.v.), who live entirely by the chase, killing their prey with poisoned arrows, of Ba-Kalahari, and along the western border of
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Hottentots, who are both hunters and cattle-rearers . The Ba-Kalahari (men of the Kalahari), who constitute the majority of the inhabitants, appear to belong to the Batau tribe of the Bechuanas, now no longer having
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separate tribal existence, and traditionally reported to be the
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oldest of the
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Bechuana tribes . Their features are markedly
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negroid, though their skin is less.black than that of many negro peoples . They have thin legs and arms . The Ba-Kalahari are said to have possessed enormous herds of large horned cattle until deprived of them and driven into the desert by a fresh
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migration of more powerful Bechuana tribes .

Unlike the Bushmen, and in spite of desert

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life, the Ba-Kalahari have a true passion for agriculture and cattle-breeding . They carefully cultivate their gardens, though in many cases all they can grow is a scanty supply of melons and pumpkins, and they
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rear small herds of goats . They are also
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clever hunters, and from the neighbouring Bechuana chiefs obtain spears, knives,
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tobacco and
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dogs in
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exchange for the skins of the animals they kill . In disposition they are peaceful to timidity,
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grave and almost morose . Livingstone states that he never saw Ba-Kalahari children at
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play . An ingenious method is employed to obtain water where there is no open well or
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running stream . To one end of a reed about 2 ft. long a bunch of grass is tied, and this end of the reed is inserted in a hole dug at a spot where water is known to exist under-ground, the wet sand being rammed down firmly round it . An ostrich egg-shell, the usual water vessel, is placed on the ground alongside the reed . The water-drawer, generally a' woman, then sucks up the water through the reed, dexterously squirting it into the adjacent egg-shell . To aid her aim she places between her lips a
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straw, the other end of which is inserted in the shell . The shells, when filled, are buried, the
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object of the Ba-Kalahari being to preserve their supplies from any sudden
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raid by Bushmen or other foe . Early travellers stated that no amount of bullying or hunting in a Ba-Kalahari
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village would result in a find of water; but that on friendly relations being established the natives would bring a supply, however arid the
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district .

The British

government has since sunk wells in one or two districts . Though the Ba Kalahari have no religion in the strict sense of the word, they show traces of
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totemism, and as Batau, i.e . " men of the lion," revere rather than fear that beast . The Kalahari was first crossed to Lake Ngami by David Living-stone, accompanied by William C . Oswell, in 1849 . In 1878-1879 a party of Boers, with about three
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hundred wagons, trekked from the
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Transvaal across the Kalahari to Ngami and thence to the hinterland of
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Angola . Many of the party, men,
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women and children, perished of thirst during the journey . Survivors stated that in all some 250
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people and 9000 cattle died . See BECHUANALAND . Die Kalahari, by Dr Siegfried Passarge (Berlin, 1904), is a valuable
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treatise on the geology, topography, hydrography, climate and
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flora of the desert, with maps and bibliography . The author spent two years (1896-1898) in the Kalahari . See also Missionary Travels and Researches in South Africa, &c., by David Livingstone (
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London, 1857) .

End of Article: KALAHARI DESERT
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