Long) to Chindio, on the north bank of the Zambezi, was opened.
The common or true duiker (C. grimmi) is found in bush-country from the Cape to the Zambezi and Nyasaland, and ranges northward on the west coast to Angola.
South of the Zambezi the group reappears in the shape of the asse-fox or fennec. (V.
But they still hold their ground as the ruling element in the region between the Limpopo and the middle Zambezi, which from them takes the name of Matabeleland.
The Victoria Falls bridge over the Zambezi, designed by Sir Douglas Fox, and completed in 1905, is a combination of girder and arch having a total length of 650 ft.
SPRINGBUCK, or Springbok (Antidorcas euchore), an aberrant South African gazelle inhabiting the country south of the Zambezi, but ranging north-westwards to Mossamedes.
The Paris Society, represented especially by Francois Coillard, has been successful along the Zambezi, and Scottish, German, Moravian and Jesuit agencies are also well represented.
Mackenzie for the Zambezi region and J.
The Zambezi itself is, however, unsatisfactory as a waterway, and the direct connexion of Nyasaland with an ocean port was at length undertaken in 1920, with the building of a railway (170 m.
The line progressed rapidly, and by the end of 1921 only the dredging of the Zambezi remained to be accomplished.
In the east the tableland falls away to the basins of the Congo and Zambezi, to the south it merges into a barren sandy desert.
In the south-east part of the province the rivers belong either to the Zambezi system, or, like the Okavango, drain to Lake Ngami.
Up to the end of the 19th century the hold of Portugal over the interior of the province was slight, though its influence extended to the Congo and Zambezi basins.
In old maps of south-east Africa, derived originally from Portuguese and from Dutch sources, an extensive region on the Cuama or Zambezi and to the south of it is styled regnum monomotapae.
Several 17th-century writers extend the " empire " to the north of the Zambezi, Bocarro giving it in all " a circumference of more than three hundred leagues."
Another railway, part of the Cape to Cairo connexion, runs north-west from Bulawayo, Grossing the Zambezi just below the Victoria Falls.
Other writers confine the term to the British possessions south of the Zambezi, but in this case British South Africa is the proper designation.
The coast line, from the mouth of the Kunene on the west to the delta of the Zambezi on the east, is little indented and contains only two sheltered natural harbours of any size - Saldanha Bay on the west and Delagoa Bay on the east.
In the south the drainage is to the Atlantic, chiefly through the Orange River, in the north to the Indian Ocean through the Zambezi, Limpopo and other streams. A large number of smaller rivers rise on the outer slopes of the mountain ramparts and flow direct to the sea.
In consequence of their great slope and the intermittent supply of water the rivers - except the Zambezi - are unnavigable save for a few miles from their mouths.
In the Kalahari and in the eastern lowlands (from Zululand to the Zambezi delta) most of these animals are still found, as well as the eland, wildebeest and gemsbok.
South of the mouth of the Zambezi, but they got no further south nor do they appear to have penetrated inland, though they traded for gold and other articles with the inhabitants of the northern part of the plateau - the builders of the zimbabwes and other ruins in what is now Rhodesia (q.v.) The Asiatic inhabitants of South Africa of the present day are mainly Indian Population (1904).
From the seaports of Cape Town, Port Elizabeth, East London, Durban, Lourenco Marques and Beira railway lines run to Kimberley, Bloemfontein, Johannesburg and Pretoria, while a trunk line extends north from Kimberley through Rhodesia (in which gold mining began on an extensive scale in 1898) and across the Zambezi below the Victoria Falls into the Congo basin, where it serves the Katanga mineral area.
At the head of their organizations are vicars-apostolic for the Cape (eastern district), the Cape (western district), Natal, Orange River, Kimberley and the Transvaal, and prefects-apostolic for Basutoland and Zambezi (or Rhodesia).
At the Shoshone Falls the river makes a sudden plunge of nearly 200 ft., and the Falls have been compared with the Niagara and Zambezi; a short distance back of the main fall is a cataract of 125 ft., the Bridal Veil.
At last he succeeded, and reached the Chobe (Kwando), a southern tributary of the Zambezi, and in the end of June reached the Zambezi itself at the town of Sesheke.
Ascending the Zambezi, he, however, found no place free from the tsetse fly, and therefore resolved to discover a route to the interior from either the west or east coast.
For Livingstone's purposes the route to the west was unavailable, and he decided to follow the Zambezi to its mouth.
The Zambezi expedition, of which Livingstone thus became commander, sailed from Liverpool in H.M.S.
"Pearl" on the 10th of March 1858, and reached the mouth of the Zambezi on the 14th of May.
On the 30th of January 1862, at the Zambezi mouth, Livingstone welcomed his wife and the ladies.
Returning to the Zambezi in the beginning of 1863, he found that the desolation caused by the slave trade was more horrible and widespread than ever.
To Mafeking (870 m.), Bulawayo (1360m.), the Victoria Falls on the Zambezi (1623 m.) and the Belgian Congo frontier, whilst a branch from Bulawayo runs via Salisbury to Beira,- 2037 m.
The Indian Ocean receives few large rivers, the chief being the Zambezi, the Shat-el-Arab, the Indus, the Ganges, the Brahmaputra and the Irawadi.
Both the Argasidae and Ixodidae contain pathogenic species, of which the best known are the following: Ornithodoros monbata, belonging to the Argasidae, and called bibo in Uganda, monbata in Angola, and tampan on the Zambezi, is widely distributed in tropical Africa from Uganda in the north to the Transvaal in the south.
Of the rivers flowing to the Indian Ocean the only one draining any large part of the interior plateaus is the Zambezi, whose western branches rise in the west coast highlands.
In the south-west the Zambezi system interlaces with that of the Taukhe (or Tioghe), from which it at times receives surplus water.
During Miocene times Passarge considers that the region of the Zambezi underwent extreme desiccation.
The additional strata consist of the immense quantities of volcanic material on the plateau of East Africa, the basalt flows of West Africa and possibly those of the Zambezi basin.
It is true that stone implements of palaeolithic and neolithic types are found sporadically in the Nile valley, Somaliland, on the Zambezi, in Cape Colony and the northern portions of the Congo Free State, as well as in Algeria and Tunisia; but the localities are far too few and too widely separated to warrant the inference that they are to be in any way connected.
The penetration of the forest area must certainly have taken longer and was probably accomplished as much from the south-east, up the Zambezi valley, as from any other quarter.
Thus those qualities, physical and otherwise, in which the Bantu approach the Hamites gradually fade as we proceed westward through the Congo basin, while in the east, among the tribes to the west of Tanganyika and on the upper Zambezi, " transitional " forms of culture are found.
The more extensive Zang (Zenj) empire, of which the name Zanzibar (Zanguebar) is a lasting memorial, extending along the sea-board from Somaliland to the Zambezi, was also extinct.
Stuhlmann into the Older Bantu (Wanyamwezi, Wasukuma, Wasambara, Waseguha, Wasagara, Wasaramo, &c.) and the Bantu of Later Immigration (Wakikuyu, Wakamba, Wapokomo, Wataita, Wachaga, &c.), who are more strongly Hamitized and in many cases have adopted Masai customs. These peoples, from the Victoria Nyanza to the Zambezi, may conveniently be termed the " Eastern Bantu."
VICTORIA FALLS, the greatest waterfall in the world, forming the most remarkable feature of the river Zambezi, Central Africa.
The falls are about midway in the course of the Zambezi in 17° 51' S., 25° 41' E.
At the spot where the Zambezi is at its widest -- over 1860 yds.
These deposits are held by Passarge to indicate Tertiary desert conditions, to which the basin of the Zambezi is slowly reverting.