Lakes of Africa 2023
DOI: 10.1016/b978-0-323-95527-0.00015-4
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History and formation of African Lakes

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Cited by 3 publications
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“…The physiographic data on Tunisia present moderate hilly terrain with the slope geomorphology ranging from zero m in the coastal areas at water level to the maximum at 3781 m and mean at 432 m, according to the General Bathymetric Chart of the Oceans (GEBCO) DEM grid. The geographical location of these sebkhas is related to the environmental historical development of north Sahara with related aeolian and fluvial pro-cesses [69,70]. Located in the arid environment of north Africa, saline lakes and surrounding landscapes experience changes in volume and extent due to the extreme temperatures: during the summer heat period, lakes dry out almost entirely and become a crust of salt and minerals due to the evaporated moisture.…”
Section: Study Areamentioning
confidence: 99%
“…The physiographic data on Tunisia present moderate hilly terrain with the slope geomorphology ranging from zero m in the coastal areas at water level to the maximum at 3781 m and mean at 432 m, according to the General Bathymetric Chart of the Oceans (GEBCO) DEM grid. The geographical location of these sebkhas is related to the environmental historical development of north Sahara with related aeolian and fluvial pro-cesses [69,70]. Located in the arid environment of north Africa, saline lakes and surrounding landscapes experience changes in volume and extent due to the extreme temperatures: during the summer heat period, lakes dry out almost entirely and become a crust of salt and minerals due to the evaporated moisture.…”
Section: Study Areamentioning
confidence: 99%