Arid and semiarid landscapes appear to preserve more evidence of former environmental conditions, although high contemporary erosion rates and the paucity of long terrestrial-sedimentary sequences hinder their complete elucidation. This paper focuses on the late Quaternary environmental change in the Namibia in southern Africa. The Namibia is located at the interface of tropical, subtropical and temperate atmospheric and oceanic systems. Despite the fact that southern Africa was not subject to Quaternary glaciation per se, the influence of variations in amount and seasonality of rainfall has been very marked indeed. The relationship between geomorphology and climate in Namibia reveals the degree and extent to which its landscapes are determined by changing environmental conditions, especially during the Late Quaternary. Case studies of late Quaternary environmental changes in the northern, western and central Namibia are presented. In the western Namibia, over the last 140 ka during the Late Pleistocene, lower leaf-wax δD and higher δ13C (more C4 grasses) were recorded in a marine sediment core at 23°S off the coast of Namibia, which indicates wetter Southern Hemisphere (SH) summer conditions and increased seasonality, during SH insolation maxima relative to minima and during the last glacial period relative to the Holocene and the last interglacial period. In the central part of the Namibia, the application of OSL dating to both aeolian and fluvial sediments from the Namib Desert is contributing to the understanding of palaeohydrological, palaeoenvironmental and palaeoclimatic change in the region. OSL chronologies from two complex linear dune features close to Gobabeb suggest the current dunes are young (Holocene age), with important messages about the dynamics of the system and migration rates, whilst OSL ages from dunes in the southern part of the Sand Sea suggests older material of up to 24 ka at 5 m depth. The Holocene environmental change in northern Namibia can be deduced from evidences from soils and sediments in the Otjiwarongo thornbush savanna. In this region degradation and desertification (man-made aridification) of drylands are developed during the Holocene. Vertisol– Kastanozem–Calcisol soil associations occur widely (as patches of several hundred hectares in extent). They have formed in fine-grained Mid-Holocene sediments which accumulated on both sides of the subcontinental watershed. Kastanozem formation cannot be explained by the environments that exist at present. The humification suggests open savanna environments in the past and does not accord with the shrublands and thornbush savanna at present. Pedological and geomorphic investigations distinguish separate degradational stages in space and time caused by different periods of human impact. Landscape degradation seems to have started in pre-colonial times (Bantu immigration?) most likely as a consequence of cattle farming, and was increased by farming since the end of the 19th century by European settlers. Degradation of vegetation and soils, and river channel formation, seem to be the main causes of farmland aridification. These examples from different regions of the Namibia document an increasing intensity of human impact on landscapes to the extent that people now play the dominant geomorphological role, especially in semiarid and coastal areas. The conclusion offers pointers as to how geomorphological evidence of Quaternary change can be used to assist in the better management of contemporary and future environmental conditions. [ABSTRACT FROM AUTHOR]