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See also:BECHUANALAND (a name given from its inhabitants, the See also:Bechuana, q.v.) , a See also:country of See also:British See also:South See also:Africa occupying the central See also:part of the vast tableland which stretches See also:north to the See also:Zambezi . It is bounded S. by the See also:Orange See also:river, N.E. and E. by Matabeleland, the See also:Transvaal and Orange River See also:Colony, and W. and N. by See also:German South-See also:West Africa . See also:Bechuanaland geographically and ethnically enjoys almost See also:complete unity, but politically it is divided as follows: I . British Bechuanaland, since 1895 an integral part of Cape Colony . See also:Area, 51,424 sq. m . Pop . (1904) 84,210, of whom 9276 were whites . II . The Bechuanaland See also:Protectorate, the See also:northern part of the country, governed on the lines of a British See also:crown colony . Area (estimated), 225,000 sq. m . Pop . (1904) 120,776, of whom Europeans numbered 1004 . The natives, in addition to the See also:Bechuana tribes, include some thousands of See also:Bushmen (Masarwa) . Administratively attached to the protectorate is the See also:Tati See also:con-cession, which covers 2500 sq. m. and forms geographically the south-west corner of Matabeleland . The Griqualand West See also:province of Cape Colony belongs also geographically to Bechuanaland, and except in the See also:Kimberley See also:diamond mines region is still largely inhabited by Bechuana . (See GRIQUALAND.) See also:Physical Features.—The See also:average height of the tableland of which Bechuanaland consists is nearly 4000 ft . The See also:surface is hilly and undulating with a See also:general slope to the west, where the level falls in considerable areas to little over 2000 ft . A large part of the country is covered with grass or See also:shrub, chiefly See also:acacia . There is very little See also:forest See also:land . The western region, the See also:Kalahari See also:Desert (q.v.), is mainly arid, with a sandy See also:soil, and is covered in part by dense See also:bush . In the northern region are large marshy depressions, in which the See also:water is often See also:salt . The best known of these depressions, See also:Ngami (q.v.), lies to the north-west and is the central point of an inland water See also:system apparently in See also:process of drying up . To the north-See also:east and connected with Ngami by the Botletle river, is the See also:great Makari-Kari salt See also:pan, which also drains a vast extent of territory, receiving in the See also:rainy See also:season a large See also:volume of water . The See also:marsh then becomes a great See also:lake, the water surface stretching beyond the See also:horizon, while in the dry season a See also:mirage is often seen .
The permanent marsh land covers a region 6o m. from south to north and from 30 to 6o m. east to west
.
In the south the See also:rivers, such as the Molopo and the See also:Kuruman, drain towards the Orange
.
Other streams are tributaries of the See also:Limpopo, which for some distance is the frontier between Bechuanaland and the Transvaal
.
The rivers of Bechuanaland are, with few exceptions, intermittent or lose themselves in the desert
.
It is evident, however, from the extent of the beds of these streams and of others now permanently dry, and from remains of See also:ancient forests, that at a former See also:period the country must have been abundantly watered
.
From the many See also:cattle-folds and walls of See also:defence scattered over the country, and ruins of ancient settlements, it is also evident that at that period See also:
From See also:December to See also:February violent
See also:thunder and See also:hail storms are experienced
.
In the winter or dry season there are occasional heavy dust storms
.
See also:Geology.—The greater part of Bechuanaland is covered with superficial deposits consisting of the sands of the desert regions of the Kalahari and the See also:alluvium and saliferous marls of the Okavango See also:basin
.
The See also:oldest rocks, granites, gneisses and schistose sandstones, the Ngami See also:series, rise to the surface in the east and south-east and doubtless immediately underlie much of the See also:sand areas
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A See also:sandstone found in the neighbourhood of Palapye is considered to be the See also:equivalent of the Waterberg formation of the Transvaal
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The See also:Karroo formation and See also:associate dolerites (Loalemandelstein) occur in the same region
.
A See also:deposit of See also:sinter and a calcareous sandstone, known as the Kalahari See also:Kalk, considered by Dr Passarge to be of See also:Miocene See also:age, overlies a sandstone and curious See also:breccia (Botletle Schnichten)
.
These deposits are held by Passarge to indicate See also:Tertiary desert conditions, to which the basin of the Zambezi is slowly reverting
.
See also:Fauna.—Until towards the See also:close of the 19th See also:century Bechuanaland abounded in big See also:game, and the Kalahari is still the See also:home of the See also:lion, See also:leopard, See also:hyena, See also:jackal, See also:elephant, See also:hippopotamus, See also:rhinoceros, See also:buffalo, See also:antelope of many See also:species, See also:ostrich and even the See also:giraffe
.
Venomous See also:reptiles, e.g. puff-adders and cobras, are met with, enormous frogs are common, and walking and flying locusts, mosquitoes, See also: In those containing water in the rainy season only, the fish preserve See also:life when the See also:bed is dry by burrowing deeply in the See also:ooze before it hardens . The See also:principal fish are the baba or See also:cat-fish (clarias sp.) and the yellow-fish, both of which attain considerable See also:size . Bustards (the great kori and the koorhaan) are common . See also:Flora.—In the eastern See also:district are stretches of grass land, both sweet and sour veld . In the " bush " are found tufts of tall coarse grass with the space between See also:bare or covered with herbaceous creepers or water-bearing tubers . A common creeper is one bearing a small See also:scarlet See also:cucumber, and a species of water-See also:melon called tsoma is also abundant . Of the melon and cucumber there are both See also:bitter and sweet varieties . Besides the grass and the creepers the bush is made up of See also:berry-yielding bushes (some of the bushes being See also:rich in aromatic resinous See also:matter), the wait-abit See also:thorn and white thorned See also:mimosa . The See also:indigo and See also:cotton See also:plants grow See also:wild . Among the rare big trees—found chiefly in the north-east—are See also:baobab and See also:palmyra and certain See also:fruit trees, one bearing a See also:pink See also:plum . There are remains of ancient forests consisting of wild See also:olive trees and the See also:camel thorn, near which grows the ngotuane, a plant with a profusion of See also:fine, strongly scented yellow See also:flowers . See also:Chief Towns.—The chief See also:town in See also:southern Bechuanaland, i.e. the part incorporated in Cape Colony, is See also:Mafeking (q.v.), near the headwaters of the Molopo river . It is the headquarters of the Barolong tribe, and although within the Cape border is the seat of the See also:administration of the protectorate . Vryburg (pop., 1904, 2985), founded by See also:Boer filibusters in 1882, and Taungs, are towns on the railway between Kimberley and Mafeking . Taungs has some 22,000 inhabitants, being the chief See also:kraal of the Batlapin tribe . About 7 M. south of Vryburg, at See also:Tiger Kloof, is an See also:Industrial Training See also:Institute for natives founded in 1904 by the See also:London Missionary Society . Upington (2508) on the north See also:bank of the Orange, an agricultural centre, is the chief town in Gordonia, the western See also:division of southern Bechuanaland . Kuruman (q.v.) is a native town near the source of the Kuruman river, 85 M. south-west of Vryburg . It has been the See also:scene of missionary labours since the See also:early years of the 19th century . North of Mafeking on the railway to See also:Bulawayo are the small towns of Gaberones and Francistown . The last named is the chief township in the Tati concession, the centre of a See also:gold-See also:mining region, and the most important white See also:settlement in the protectorate . Besides these places there are five or six large native towns, each the headquarters of a distinct tribe . The most important is Serowe, with over 20,000 inhabitants, the See also:capital of the Bamangwato, founded by the chief Khama in 1903 . It is about 250 M. north-north-east of Mafeking, and took the See also:place ofthe abandoned capital Palapye, which in its turn had succeeded See also:Shoshong . The chief centre in the western Kalahari is Lehututu . See also:Agriculture and See also:Trade.—The soil is very fertile, and if properly irrigated would yield abundant harvests . Unirrigated land laid under See also:wheat by the natives is said to yield twelve bushels an See also:acre . Cereals are grown in many of the river valleys . See also:Maize and See also:millet are the chief crops . The See also:wealth of the Bechuana consists principally in their cattle, which they tend with great care, showing a shrewd discrimination in the choice of pasture suited to oxen, See also:sheep and goats . Water can usually be obtained all the year See also:round by sinking See also:wells from 20 to 30 ft. deep . The " sweet veld " is specially suitable to cattle, and the finer shorter grass which succeeds it affords pasturage for sheep . Gold mines are worked in the Tati district, the first discoveries having been made there in 1864 . There are gold-bearing See also:quartz reefs at Madibi, near Mafeking, where mining began in 1906 . Diamonds have been found near Vryburg . The existence of See also:coal near, Palapye about 6o ft. below the surface has been proved . The coal, however, is not See also:mined, and much of the destruction of timber in southern Bechuanaland was caused by the demand for See also:fuel for Kimberly y . See also:Copper ore has been found near Francistown . Formerly there • as a trade in ostrich feathers and See also:ivory; but this has ceased, and the chief trade has since consisted in supplying the natives with See also:European goods in See also:exchange for cattle, hides, the skins and horns of game, firewood and See also:fencing poles, and in forwarding goods north and south . The protectorate is a member of the South See also:African Customs See also:Union . The value of the goods imported into the protectorate in 1906 was £118,322; the value of the exports was £77,736 . The See also:sale of See also:spirits to natives is forbidden. r Communications.—As the great See also:highway from Cape Colony to the north, Bechuanaland has been described as the " See also:Suez See also:canal of South Africa." The See also:trunk railway from Cape Town to the See also:Victoria Falls traverses the eastern edge of Bechuanaland throughout its length . The railway enters the country at Fourteen Streams, 695 m. from Cape Town, and at Ramaquabane, 584 M. farther north, crosses into See also:Rhodesia . The old trade route to Bulawayo, which skirts the eastern edge of the Kalahari, is now rarely used . See also:Wagon tracks See also:lead to Ngami, 320 m . N.W. from Palapye Road Station, and to all the settlements . From the scarcity of water on the See also:main routes through the Kalahari these roads are known as " the thirsts "; along some of them wells have been sunk by the administration . See also:Government.—The protectorate is administered by a See also:resident See also:commissioner, responsible to the high commissioner for South Africa .
Legislation is enacted by proclamations in the name of the high commissioner
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See also:Order is maintained by a small force of semi-military See also:police recruited in See also:Basutoland and officered by Europeans
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See also:Revenue is obtained mostly from customs and a hut tax, while the chief items of See also:expenditure have been the police force and a See also:subsidy of £20,000 per annum towards the cost of the railway, a liability which terminated in the year 1908
.
The average See also:annual revenue for the five years ending the 31st of See also:
Lichtenstein (1804) and W
.
J
.
Burchell (1811-1812), both distinguished naturalists, and other explorers, had made See also:familiar the general characteristics of the southern part of the
country
.
The Rev
.
John See also: Andersson (1853–1858) and others, covered almost every part of the country hitherto unknown . In 1864 Karl Mauch discovered gold in the Tati district . At the See also:time of the first contact of the Bechuana with white men the Cape government was the only civilized authority in South Africa; and from this cause, and the circumstance that the missionaries who lived among and exercised great See also:influence over them were of British See also:nationality, the connexion between Bechuanaland and the Cape became close . As early as 1836 an See also:act was passed extending the See also:jurisdiction of the Cape ccurts in certain cases as far north as 25° S.—a limit which included the southern part of Bechuanaland . Although under strong British influence the country was nevertheless ruled by its own chiefs, among whom the best-known in the See also:middle of the 19th century were Montsioa, chief of the Barolong, and Sechele, chief of the Bakwena and the friend of Livingstone . At this period the Transvaal Boers were in a very unsettled See also:state, and those living in the western districts showed a marked inclination to encroach upon the lands of the Bechuana . In 1852 Great See also:Britain by the Sand river See also:convention acknowledged the See also:independence of the Transvaal . See also:Save the See also:Vaal river no frontier was indicated, and " boasting," writes Livingstone in his Missionary Travels, " that the See also:English had given up all the blacks into their See also:power . . . they (the Boers) assaulted the Bakwains " (Bakwena) . With this event the See also:political history of Bechuanaland may be said to have begun . Not only was Sechele attacked at his capital Kolobeng, and the European stores and Livingstone's See also:house there looted, but the Boers stopped a trader named M'Cabe from going northward . Again to quote Livingstone, " The Boers resolved to shut up the interior and I determined to open the country." In 1858 the Boers told the missionaries that they must not go north without their (the Boers') consent . Moffat complained to Sir See also:George See also:Grey, the See also:governor of Cape Colony, through whose intervention the molestation by Transvaal Boers of British subjects in their passage through Bechuanaland was stopped . At a later date (1865) the Boers tried to raise taxes from the Barolong, but without success, a See also:commando sent against them in 1868 being driven off by Montsioa's See also:brother Molema . This led to a protest (in 187o) from Montsioa, which he lodged with a landdrost at See also:Potchefstroom in the Transvaal, threatening to submit the matter to the British high commissioner if any further See also:attempt at See also:taxation were made on the part of the Boers . The Boers then resorted to cajolery, and at a See also:meeting held in See also:August 187o, at which See also:President See also:Pretorius and See also:Paul See also:Kruger represented the Transvaal, invited the Barolong to join their territories with that of the See also:republic, in order to save them from becoming British . Montsioa's reply was See also:short: " No one ever spanned-in an See also:ass with an ox in one yoke." In the following year the claims of the Boers, the Barolong, and other tribes were submitted to the See also:arbitration of R . W . See also:Keate, See also:lieutenant-governor of See also:Natal, and his See also:award placed Montsioa's territory outside the limits of the Transvaal . This attempt of the Boers to gain See also:possession of Bechuanaland having failed, T . F . See also:Burgers, the president of the Transvaal in 1872, endeavoured to replace Montsioa as chief of the Barolong by Moshette, whomhe declared to be the rightful ruler and See also:paramount chief of that See also:people . The attacks of the Boers at length became so unbearable that Montsioa in 1874 made a See also:request to the British authorities to be taken under their See also:protection . In formulating this See also:appeal he declared that when the Boers were at See also:war with Mosilikatze, chief of the Matabele, he had aided them on the See also:solemn under-See also:standing that they were to respect his boundaries .
This promise they had broken
.
Khama, chief of the Bamangwato in northern Bechuanaland, wrote in August 1876 to Sir See also: The Transvaal War of that date offered opportunities to the freebooting Boers of the west which were not to be lost . At this time the British, wearied of South African troubles, were disinclined to See also:respond to native appeals for help . Conse |