Late Pleistocene and early Holocene palaeohydrology of the Sahara (∼11 to 8 ka). The catchments of the megalakes that form corridors across the Sahara are indicated with letters A–D, while the river catchments that link with many of these megalake basins to form the vast Saharan inland waterway are indicated with letters E–I: (A) Lake Megachad, (B) Lake Megafezzan, (C) Ahnet-Mouydir Megalake, (D) the Basin of the Chotts, (E) Senegal River, (F) Nile River, (G) Sahabi River, (H) Kufra River, and (I) Niger River. Numbers indicate the location of fan, tectonic and lake outflow links between basins: () Nile Basin/Chad Basin, () Chad Basin/Niger Basin, () Niger Basin/Senegal Basin, () Niger/Basin West Ahaggar Mountains, () West Ahaggar Mountains/Ahnet-Mouydir Basin, () Ahnet-Mouydir Basin/Chotts Basin, () Chotts Basin/Fezzan Basin, () Fezzan Basin/Serir Tibesti, and () Serir Tibesti/Kufra Basin. The 200-mm isohyet indicates the current limit of the Sahara Desert.