Friday, May 28, 2004

Arabian Desert, Soils

Mechanical weathering, which physically breaks down coarse particles into finer grains, is the most significant process in the formation of desert soils. Quartz sand abounds, covering more than a third of the desert surface. Granular debris from the Precambrian crystalline basement forms pebbly fans about the bases of hills. Sands and silts are washed down to

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