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loess
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loess

Yellow loam, derived from glacial meltwater deposits and accumulated by wind in periglacial regions during the ice ages. Loess usually attains considerable depths, and the soil derived from it is very fertile. There are large deposits in central Europe (Hungary), China, and North America. It was first described in 1821 in the Rhine area, and takes its name from a village in Alsace.



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? Mentioned in ? References in periodicals archive
 
Wind tunnel test of the influence on the erodibility of loessial sandy loam soils by wind.
The northeastern part of the Gaza Strip, with loessial and alluvial soils, also contains some wadis.
 
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