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- W4387465907 abstract "The Kenya Rift lakes occupy grabens, sag basins, and depressions dammed by faulting and volcanic rocks. Modern lakes range from shallow (<1 m, Magadi) to deep (>100 m, Turkana) reflecting the development of accommodation space, rainfall patterns and sediment influx, which produce overfilled, balanced-filled and underfilled basins. Lakes in hydrologically open systems remain fresh, whereas closed lakes undergo evaporation and become saline and alkaline, following the principle of chemical divides. A few lakes are fresh because of subsurface outflow. Physical, chemical, and biological processes control the ecological variability and sedimentation in the lakes. Organic productivity is often high, especially in saline alkaline lakes. Clastic sedimentation varies with depositional environment (deltas, shorelines, pelagic settings), and also with the contrasting salinity and density between river inflow and basinal waters (homopycnal, hypopycnal and hyperpycnal flow). Carbonate sediments form in fresh and brackish lakes when and where conditions are favourable. Organic-rich sediments and lamination are preserved in stratified (meromictic) lakes. Sediments in saline lakes include evaporites, chert, Na-silicates and zeolitic mud. Changes in lake levels resulting from climate change and tectonics are a fundamental control of the geological and biological record of the Kenya Rift lakes." @default.
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- W4387465907 date "2023-01-01" @default.
- W4387465907 modified "2023-10-11" @default.
- W4387465907 title "Lake Processes and Sedimentation" @default.
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