A loose, earthy, extremely fine-grained, natural sediment or soft rock composed primarily of clay-size or colloidal particles and characterized by high plasticity and by a considerable content of clay mineral and subordinate amounts of finely divided quartz, decomposed feldspar, carbonates, ferruginous matter, and other impurities; it forms a plastic, moldable mass when finely ground and mixed with water, retains its shape on drying, and becomes firm, rocklike and permanently hard on heating or firing. (Source: BJGEO)



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Suich H, Murphy C 2002. Crafty women: The livelihood impact of craft income in Caprivi.
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Research Discussion Paper 48_2002.pdf 250.99 KB
Heine K, Völkel J 2010. Soil clay minerals in Namibia and their significance for the terrestrial and marine past global change Research. African Study Monographs 40 31-50
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Soil clay minerals 2010.pdf 1.36 MB
Adekayode FO, Ogunkoya MO 2009. Comparitive study of clay and organic matter of termite mounds and the surrounding soils. African Crop Science Conference Proceedings 9 379-384
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organic matter.pdf 136.21 KB
Miller RM, Pickford M, Senut B 2010. The geology, palaeontology and evolution of the Etosha Pan, Namibia: Implications for terminal Kalahari deposition. South African Journal of Geology 113 (3) 307 - 334
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Cuvelai geology 307-334 Miller et.al_.pdf 2.28 MB