Abstract
The Terek‐Kuma Sands, including the Bazhigan Sands where this study has been carried out for 18 years, are typical of this region with respect to landscape and climatic characteristics. The structure of the sands is stratified because of repeated exposure to wind action. Several layers of buried soil are observed in their profile. The relief of the territory is hilly. The water table is at a depth varying from 1.5 to 3 m in the depressions between the hills to more than 9 m in the
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