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- W2028421899 abstract "Summary Dr. Celia Kamau is on the staff of Kenyatta University College, Nairobi. She has carried out exhaustive research on the lake basins of the central Rift Valley, much of it in association with archaeologists. The Lake Naivasha basin in the Kenya Rift Valley contains evidence that the lake has formerly stood well above its 1972 level of about 1890 m. This evidence was located and levelling was undertaken to determine the elevation of the former high lake shoreline or shorelines. A possible beach ridge was located at an elevation of 2006–2008 m, and beach gravels of obsidian, lava and pumice occurred at many localities up to a maximum of 1990–1996 m. It may tentatively be concluded that the lake rose to a maximum level of 2000±10 m. No conclusive proof of a lower shoreline level could be found. At present a rising lake in this basin would flow southwards down the Njorowa Gorge when it reached an elevation of 1940–1950 m: lowering of the terrain in this area has clearly taken place since the time of th..." @default.
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- W2028421899 date "1975-01-01" @default.
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- W2028421899 title "Late Quaternary Shorelines of Lake Naivasha, Kenya" @default.
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- W2028421899 doi "https://doi.org/10.1080/00672707509511614" @default.
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