On steep, unvegetated slopes, sands (particle sizes 0.063 to 2 mm) and gravels (2–64 mm) erode from the shoreline of Lake Naivasha (Kenya) and enter the lake basin. This occurred freely where fringing papyrus (Cyperus papyrus) swamp had been cleared in favour...
CITATION STYLE
Boar, R. R., & Harper, D. M. (2002). Magnetic susceptibilities of lake sediment and soils on the shoreline of Lake Naivasha, Kenya. In Lake Naivasha, Kenya (pp. 81–88). Springer Netherlands. https://doi.org/10.1007/978-94-017-2031-1_7
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