Page:EB1911 - Volume 11.djvu/822

 bank of the (q.v.) is in German territory. Several streams run south into the Orange; of those the chief is the Great Fish river, which has a course of nearly 500 m. Both the Kunene and the Orange carry water all the year round, but are not navigable. Neither is the Great Fish river, which, however, is rarely dry. The Okavango, which comes from the north and runs towards (q.v.), is perennial, but like the Kunene and Orange, belongs only partly to the hydrographic system of the country. From the inner slopes of the coast chain many streams go N.E. to join the Okavango. They cross the Omaheke waste and are usually dry. Ovampoland has a hydrographic system connected with the Kunene, and, in seasons of great flood, with that of Ngami. Before the Kunene breaks through the outer edge of the plateau, it sends divergent channels south-east to a large marsh or lake called Etosha, which is cut by 17° E. and 19° S. Of these channels the Kwamatuo or Okipoko, which is perennial, enters Etosha at its N.W. corner. The lake when full extends about 80 m. W. to E. and 50 m. N. to S. From its S.E. corner issues the Omuramba, which divides into two branches, known respectively as the Omaheke and the Ovampo. These streams have an easterly direction, their beds, often dry, joining the Okavango. The other rivers of the protectorate have as a rule plenty of water in their upper courses in the rainy season, though some river beds are dry for years together. After a heavy thunderstorm such a river bed will be suddenly filled with a turbid current half a mile wide. The water is, however, before long absorbed by the thirsty land. Only in exceptionally rainy years do the streams which cross the sand belt carry water to the ocean. But in the sand which fills the river beds water may be obtained by digging. Of rivers running direct to the Atlantic the Little Fish river enters the sea at Angra Pequena and the Kuisip in Walfish Bay. The Swakop rises in the hills near the Waterberg, and north of it is the Omaruru, which carries water for the greater part of the year. Hot springs are numerous, and it is remarkable that those of Windhoek flow more copiously during the dry than the rainy season. There are also many cold springs, and wells which contain water all the year.

Geology.—Gneiss and schist, with intrusive granites and porphyries, overlain to a great extent by sand and lateritic deposits, occupy the coast belt, coast mountains and the plateau of Damaraland. In the Huib and Han-ami plateaus of Great Namaqualand the crystalline rocks are overlain by sandstones, slates, quartzites and jasper rocks, and these in turn by dolomites. They are probably equivalent to the Transvaal and Pretoria series (see : Geology). The next oldest rocks are of recent geological date. The Kalahari Kalk, which extends over large areas to the south-east of Ovampoland, may be of Miocene age, but it has not yielded fossils. Extensive tracts of alluvium occur in the basin of the Ovampo, while the dunes and sand-tracts of the Kalahari occupy the eastern regions.

Climate.—On the coast the mean temperature is low, and there is little rainfall. Moisture is supplied by dense fogs, which rise almost daily. South-west winds prevail. Inland the climate is temperate rather than tropical, with bracing, clear atmosphere. There are considerable differences of temperature between day and night, and two well-marked seasons, one cold and dry from May to September, the other hot and rainy from October to April. In winter ice frequently forms during the night on open water on the plateau, but it never remains all day. The yearly rainfall is about 20 in. in the Damara Hills; there is more rain in the north than in the south, and in the east than in the west. In the greater part of the colony the climate is favourable for European settlement.

Flora and Fauna.—The vegetation corresponds exactly with the climate. In the dry littoral region are plants able to exist with the minimum of moisture they derive from the daily fog—Amarantaceae, Sarcocaula, Aloe dichotoma, Aristida subacaulis and the wonderful Welwitschia. Farther inland are plants which spring up and disappear with the rain, and others whose roots reach permanent water. The former are chiefly grasses, the latter exist almost solely in or near river-beds. Amongst the fine trees often seen here, the ana tree (Acacia albida) is the most noteworthy, its seeds being favourite fodder for all domestic animals. Acacia giraffae, Ac. horrida, Adansonia sterculia, near the Kunene the Hyphaene ventricosa, deserve special notice. The vegetation in the mountain valleys is luxuriant, and towards the north is of a tropical character. The palm zone extends a considerable distance south of the Kunene, and here vegetation spreads over the sand-dunes of the coast plain, which are covered with grasses.

Large game, formerly abundant, especially pachyderms, is scarce. Of antelopes the following species are plentiful in parts: springbok, steenbok, kudu, rietbok, pallah; of monkeys, the Cynocephalus porcarius is frequent. Various kinds of hyenas and jackals with fine fur (Canis mesomelas), also Felis caracal, abound. The spring-hare (Pedestea caffer) and rock-rabbit (Hyrax capensis) may often be observed. Of birds there are 728 species. Crocodiles, turtles and snakes are numerous.

Inhabitants.—Among the natives of German South-West Africa three classes may be distinguished. In the first class are the Namaqua (Hottentots) and Bushmen. The Namaqua probably came from the south, while the Bushmen may be looked upon as an indigenous race. The Hottentots, the purest existing types of that race, are divided into numerous tribes, independent of one another, such as the Witbois, Swartzbois, Bondelzwarts. The Bushmen are found scattered over the eastern parts of the country (see and ). The second class consists of the mountain Damara (Hau-Khoin), a race of doubtful affinities, probably of Bantu-Negro origin, but speaking the Hottentot language. The third class belongs to the Bantu-Negro stock, and came from the north-east, expelling and enslaving the mountain Damara, and settling in various parts of the country under different names. The most prominent are the Herero, thorough nomads and cattle-breeders; while the Ovampo (Ovambo or Ambo), in the northern part of the protectorate, are agriculturists. The (q.v.) are also known by the Hottentot name Damara, and by this name their country is generally called. The Bastaards, who live in Namaqualand, are a small tribe originating from a mingling of Cape Boers with Hottentots. They are Christians, and able to read and write. The other natives are spirit-worshippers, save for the comparatively few converts of the Protestant missions established in the country. Of white races represented the chief are Germans and Boers. In the S.E. Boer settlers form the bulk of the white population. There are also numbers of British colonists in this region—emigrants from the Cape. The immigration of Germans is encouraged by subsidies and in other ways.

Towns.—The chief port is Swakopmund, built on the northern bank of the Swakop river (the southern bank belonging to the British territory of Walfish Bay). The harbour is partially protected by a breakwater. There are also settlements at Lüderitz Bay (white pop. 1909, over 1000) and at Sandwich Harbour. Swakopmund is connected by a narrow gauge railway with Windhoek, the administrative capital of the colony, situated in a hilly district 180 m. due east of the port, but 237 m. by the railway. Karibib is the only place of consequence on the line. Otyimbingue is a government station 70 m. W.N.W. of Windhoek, and Tsumeb a mining centre 240 m. N.N.E. of the same place. Olukonda is a government post in Ovampoland. In the S.E. corner of the colony, 30 m. N. of the Orange river, is the town of Warmbad. Keetmanshoop, 100 m. N. of Warmbad and 180 m. E. of Lüderitz Bay, is the centre of a small mining industry. Gibeon is a government station and missionary settlement about midway between Keetmanshoop and Windhoek. Besides these places there are numbers of small native towns at which live a few white traders and missionaries. The missionaries have given Biblical names to several of their stations, such as Bethany and Beersheba in Namaqualand, and Rehoboth in Damaraland. In the Caprivi enclave are a German residency and the site of the town of Linyante, once the capital of the Makololo dynasty of Barotseland (see ).

Industries.—Agriculture is followed by the natives in the northern districts, but the chief industry is stock-raising. The scarcity of water in the southern parts is not favourable for agricultural pursuits, while the good grazing lands offer splendid pasturage for cattle, which the Herero raise in numbers amounting to many hundred thousands. Sheep and goats thrive well. Horses have been imported from the Cape. Unfortunately the climate does not suit them everywhere, and they are subject to a virulent distemper. Cattle and sheep also suffer from the diseases which are common in the Cape Colony. Camels have been imported, and are doing well. Wheat, maize and sorghum are the chief crops raised, though not enough is grown to meet even local requirements. Near the coast the natives collect the kernels of the nara, a wild-growing pumpkin which, in the words of an early traveller, C. J. Andersson, “are eaten by oxen, mice, men, ostriches and lions.” About half the European settlers are engaged in agriculture. They raise maize, wheat, tobacco, fruit and vegetables. Cotton cultivation and viticulture are carried on in some districts.

Minerals, especially copper, are plentiful in the country. The chief copper deposits are at Tsumeb, which is 4230 ft. above the sea, in the Otavi district. Diamonds are found on and near the surface of the soil in the Lüderitz Bay district, and diamonds have also been found in the neighbourhood of Gibeon. A little pottery is made, and the Hottentot women are clever in making fur cloths. In the north the Ovampo do a little smith-work and grass-plaiting. The external trade of the country was of slow growth. The exports, previous to the opening up of the Otavi mines, consisted chiefly of live stock—sent mainly to Cape Colony—guano, ivory, horns, hides and ostrich feathers. The chief imports are food stuffs, textiles and metals, and hardware. In 1903 the value of the exports was £168,560, that of the imports £388,210. The war which followed (see below, History) led to a great shrinking of exports, rendering the figures for the period 1904–1907 useless for purposes of comparison. About 85% of the imports are from Germany.

Communications.—The economic development of the country is largely dependent on transport facilities. The railway from