Ghazal

Definition and stakes

William E. Garstin and Frank R. Cana,  1911 Encyclopædia Britannica (1910)

“ BAHR-EL-GHAZAL, the chief western affluent of the river Nile, N.E. Africa, which it joins in 9° 30′ N., 30° 25′ E. The Bahr-el-Ghazal (Gazelle river) is a deep stream formed by the junction of many rivers, of which the Jur (see below) is the most important. The basin of the Ghazal is a large one, extending north-west to Darfur, and south-west to the Congo watershed. The main northern feeder of the Ghazal is a large river, whose headwaters are in the country west of 24° E. where the Nile, Congo and Shari watersheds meet. ”
Source: Wikisource

Various,  Encyclopaedia Britannica, 11th Edition…

“ Turning north-east the channel becomes narrower and deeper, and is characterized by occasional reaches of papyrus. Finally, the Ghazal turns east and again becomes broader until Lake No is reached. As a rule the banks in this section are marked by anthills and scrub. The anthills in one valley are so close together "that they somewhat resemble a gigantic graveyard." (Sir William Garstin) . The rise of the Ghazal river in flood time is barely 3 ft., a depth sufficient, however, to place an enormous area of country under water. ”
Source: Gutenberg

William E. Garstin and Frank R. Cana,  1911 Encyclopædia Britannica (1910)

“ In their upper courses all the southern affluents of the Ghazal flow across a plateau of ferruginous laterite, their valleys having steep banks. North of 7° 20′ N. (where rapids interrupt the currents) the valleys open out and the rivers wind in tortuous channels often choked by sandbanks. This alluvial region, flooded in the rainy season, gives place about 9° N. to a sea of swamps, forming in fact part of the huge swamp region of the Nile (q.v.) ”
Source: Wikisource

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