The slow formation of clays and thin soils in the desert is primarily due to the arid climate, which limits weathering processes. In deserts, low moisture levels inhibit the breakdown of rocks into finer particles, resulting in minimal soil development. Additionally, high temperatures can lead to rapid evaporation, causing salts to accumulate and further hindering soil formation. As a result, the process is prolonged, resulting in thin and nutrient-poor soils.
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