At 825,615 km2 (318,772 sq mi), Namibia is the world’s thirty-fourth largest country (after Venezuela). It lies mostly between latitudes 17° and 29°S (a small area is north of 17°), and longitudes 11° and 26°E.
Being situated between the Namib and the Kalahari deserts, Namibia has the least rainfall of any country in sub-Saharan Africa.
The Namibian landscape consists generally of five geographical areas, each with characteristic abiotic conditions and vegetation, with some variation within and overlap between them: the Central Plateau, the Namib, the Great Escarpment, the Bushveld, and the Kalahari Desert.
The Central Plateau runs from north to south, bordered by the Skeleton Coast to the northwest, the Namib Desert and its coastal plains to the southwest, the Orange River to the south, and the Kalahari Desert to the east. The Central Plateau is home to the highest point in Namibia at Königstein elevation 2,606 metres (8,550 ft).
The Namib is a broad expanse of hyper-arid gravel plains and dunes that stretches along Namibia’s entire coastline. It varies between 100 and many hundreds of kilometres in width. Areas within the Namib include the Skeleton Coast and the Kaokoveld in the north and the extensive Namib Sand Sea along the central coast.
The Great Escarpment swiftly rises to over 2,000 metres (6,562 ft). Average temperatures and temperature ranges increase further inland from the cold Atlantic waters, while the lingering coastal fogs slowly diminish. Although the area is rocky with poorly developed soils, it is significantly more productive than the Namib Desert. As summer winds are forced over the Escarpment, moisture is extracted as precipitation.
The Bushveld is found in north-eastern Namibia along the Angolan border and in the Caprivi Strip. The area receives a significantly greater amount of precipitation than the rest of the country, averaging around 400 mm (15.7 in) per year. The area is generally flat and the soils sandy, limiting their ability to retain water and support agriculture.
The Kalahari Desert, an arid region that extends into South Africa and Botswana, is one of Namibia’s well-known geographical features. The Kalahari, while popularly known as a desert, has a variety of localised environments, including some verdant and technically non-desert areas. The Succulent Karoo is home to over 5,000 species of plants, nearly half of them endemic; approximately 10 percent of the world’s succulents are found in the Karoo. The reason behind this high productivity and endemism may be the relatively stable nature of precipitation.
Namibia’s Coastal Desert is one of the oldest deserts in the world. Its sand dunes, created by the strong onshore winds, are the highest in the world. Because of the location of the shoreline, at the point where the Atlantic’s cold water reaches Africa’s hot climate, often extremely dense fog forms along the coast. Near the coast there are areas where the dunes are vegetated with hammocks. Namibia has rich coastal and marine resources that remain largely unexplored.
