Any low-lying land bordered by higher ground; especially an elongate, relatively large, gently sloping depression of the Earth's surface, commonly situated between two mountains or between ranges of hills or mountains, and often containing a stream with an outlet. It is usually developed by stream erosion, but may be formed by faulting. (Source: BJGEO)

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Stapff FM 1887. Das untere Khuisebthal und sein Strandgebiet. Gesellschaft für Erdkunde zu Berlin 45-66
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Das untere Khuisebthal und sein Strandgebiet_1887.pdf 13.46 MB
Mabbutt JA 1951. The evolution of the middle Ugab Valley, Damaraland, South West Africa. Transactions of the Royal Society of South Africa 33 (3) 333-363
Smith ND, McCarthy TS, Ellery WN, Merry CL, Ruther H 1997. Avulsion and anastomosis in the panhandle region of the Okavango Fan, Botswana. Geomophology 20 49 - 65