Titlebook: Landscapes and Landforms of Botswana; Frank D. Eckardt Book 2022 Springer Nature Switzerland AG 2022 Geomorphology of Botswana.Botswana la

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The Chobe-Zambezi Channel-Floodplain System: Anatomy of a Wetland in a Dryland,and Zambezi rivers approaching their confluence. This area is located in the ‘Four Corners’ region, the informal term given to the region where the Botswana, Namibia, Zambia and Zimbabwe borders meet. The large-scale structure and medium-term (10.–10. years) development of the channel-floodplain sys

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Dunes of the Southern Kalahari,that are both marginally dynamic as well as more stabilised, research has focussed both on the processes operating on partially and variably vegetated surfaces, and the palaeoenvironmental histories of dunefield accumulation. Whilst commonly classified as linear dunes, this chapter examines the rang

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Dunes of the Northern Kalahari,ay. Striking for their distinct patterning in the landscape evident from the air and in satellite imagery, on the ground these are subdued features that in places can be barely discernible apart from through the patterning of vegetation. Overall, these features have characteristics that attest to th

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Kalahari Pans: Quaternary Evolution and Processes of Ephemeral Lakes,nd semi-arid regions with low relief. In the Kalahari Basin, small pans are widespread and they function as ephemeral lakes and sedimentary sinks. They are characterised by their flat, salty to clayey surface and slightly elevated surroundings. Some principle sedimentary processes are distinctive fo

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Dry Valleys (,),ing water. Ephemeral rivers occur in the eastern hardveld, but the most extensive components of the surface drainage are the networks of fossil or dry valleys (termed . in Setswana and . in various San languages) that cross the sandveld. This chapter presents the first holistic review of current kno

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Landscape Evolution of the Stampriet Transboundary Basin and Relation to the Groundwater System: Thesting location to explore landscape evolution and the interaction of a range of surface and subsurface geomorphological processes. This chapter aims to introduce the importance of the STAS. It outlines the geological and hydrogeological framework, the range of surface geomorphological features and

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Calcretes, Silcretes and Intergrade Duricrusts, holistic overview of current knowledge about these duricrusts at a national scale. It does so by considering the distribution, classification, macromorphology, geochemistry and mineralogy of each duricrust type in turn, alongside various models used to explain their formation. The chapter then revi

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