The Senqunyane River is a river of central Lesotho. The river rises in the Maluti Mountains in northwest Lesotho, and flows southwards and then westwards for 120 kilometres before joining the Senqu River (Orange River)[1] in the southwest.[2]
The source of the Senqunyane is the meeting point of three districts: Thaba-Tseka District, Berea District and Leribe District. It forms the border between Thaba-Tseka District and first Berea and then Maseru District, as well as a small section of the Mafeteng District that is separated from the rest of its district and located high in the Maluti Mountains, for much of its length.
Tributaries include the Bokong River,[3] as well as the Jordane River and Likalaneng River, which join the Senqunyane shortly before the Mohale Dam.[4]: 33
The river is home to the rare Rock-catfish ("Austroglanis sclateri").[5] The Semonkong Waterfall acts as a migration barrier separating distinct fish communities.[5]
The Senqunyane Valley is the site of a number of archaeological and rock art sites.[6] The valley was first inhabited in the Middle Stone Age.[6]
The sandstone gorge with steep cliffs poses a problem to access. A notable bridge build in 2011 crosses the river near its confluence with the Orange River.[7][8]
^Fitzpatrick, M., Blond, B., Pitcher, G., Richmond, S., and Warren, M. (2004) South Africa, Lesotho and Swaziland. Footscray, VIC: Lonely Planet
^van Vuuren, Sanet Janse; Walt, Nicolene van der; Swanepoel, Annelie (2007). "Changes in algal composition and environmental variables in the high-altitude Mohale Dam — an important water supply reservoir to South Africa". African Journal of Aquatic Science. 32 (3): 265–274. doi:10.2989/ajas.2007.32.3.6.305. S2CID85354207.
^Consortium, Lahmeyer McDonald; Consortium, Olivier Shand (1986). Lesotho Highlands Water Project: H14-19. Kingdom of Lesotho, Ministry of Water, Energy and Mining.
^ abBousman, Britt (1988). "Prehistoric Settlement Patterns in the Senqunyane Valley, Lesotho". The South African Archaeological Bulletin. 43 (147): 33–37. doi:10.2307/3887611. JSTOR3887611.
