When carrying out our research work on the Quaternary landform evolution of the CentraI River, South West Africa Namib Desert 1972, we visited the middle part of Kuiseb river between Hudaob and Gobabeb. 1). From Hudaob downstream to its delta at Walvis Bay the river separates the Dune Namib in the south from the Namib flats in the north. Keywords: Allochthonic fluvial activity, Arid-stable geomorphic environment, Calcrete formation, Crust formation, Dendritic pattern, Fossil high water sediment, Lake deposits, Landforms, Mica schists, Stages of morphogenesis, Tributary valleys.