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A 1928 study of Tripolitania, indicated clearly the presence of loess-like deposits and described their nature, pointing out that 90% of the granular material was greater than 100 μm in diameter. Some authors suggest that there is a region of Peri-Sahara loess, although earlier observations indicate quite clearly that the Sahara region is free of loess. The proposed loess in North Africa, represented...
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