Limpopo River

Definition and stakes

Andrew A. Anderson,  Twenty-Five Years in a Waggon in South Africa…

“ The immensity of time it must have taken to wear away such deep and large holes in a granite rock, makes one pause to think of the period when this river was first formed, because it is only a portion of the year, when the floods come down, that the water acts upon the stones in these holes. The principal tributaries of the Limpopo that rise in the Transvaal are the Apies at Pretoria, Sand, Pinaars, Plat, Matlabatse, Pongola, Palala, Nylstroom, Houdt, Limvubu, and the Olifants river with its many tributaries, all flowing into the Limpopo on its right bank. ”
Source: Gutenberg

Various,  Encyclopaedia Britannica, 11th Edition…

“ In the low country it receives its chief affluent, the Olifants river (450 m. long) , which, rising in the high veld of the Transvaal east of the sources of the Limpopo, takes a more direct N.E. course than the main stream. The Limpopo enters the ocean in 25° 15′ S. The mouth, about 1000 ft. wide, is obstructed by sandbanks. In the rainy season the Limpopo loses a good deal of its water in the swampy region along its lower course. High-water level is 24 ft. above low-water level, when the depth in the shallowest part does not exceed 3 ft. ”
Source: Gutenberg

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