Zambezi River

Definition and stakes

Frank Richardson Cana,  1911 Encyclopædia Britannica (1911)

“ Several of the Zambezi affluents are also navigable for many miles. The Lungwebungu, which enters the upper river, is navigable for a long distance, thus supplying communication with the extreme north-west corner of the Zambezi basin. Parts at least of the Luena, Kafukwe, Loangwa and the Kwando tributaries are also capable of being navigated. The possibility of connecting the Kwando with the navigable waters of the Okavango, at the point where the overflow mentioned below takes place, has likewise been suggested. ”
Source: Wikisource

Frank Richardson Cana,  1911 Encyclopædia Britannica (1911)

“ The region drained by the Zambezi may be represented as a vast broken-edged plateau 3000 or 4000 ft. high, composed in the remote interior of metamorphic beds and fringed with the igneous rocks of the Victoria Falls. At Shupanga, on the lower Zambezi, thin strata of grey and yellow sandstones, with an occasional band of limestone, crop out on the bed of the river in the dry season, and these persist beyond Tete, where they are associated with extensive seams of coal. Coal is also found in the district just below the Victoria Falls. Gold-bearing rocks occur in several places. ”
Source: Wikisource

Various,  Encyclopaedia Britannica, 11th Edition…

“ The southern border of this territory is the north bank of the Zambezi from the confluence of the Kafukwe to that of the Luangwa at Zumbo. Eastwards of Zumbo, British Central Africa is separated from the river Zambezi by the Portuguese possessions; nevertheless, considerably more than two-thirds of the country lies within the Zambezi basin, and is included within the subordinate basins of Lake Nyasa and of the rivers Luangwa and Luengwe-Kafukwe. ”
Source: Gutenberg

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