Abstract

A detailed description of engineering-geological properties is given to loess-soil series at the key profile Dubno (Tarakaniv). The profile mainly represents loess and palaeopedological horizons of Upper Pleistocene at the Volyn Upland. Middle Pleistocene has small thickness here, but varies facially. The profile reviles palaeocryogenic deformations, especially final Pleistocene pseudomorphosis along recurring vein ice. Key words: loess, loess-soil series, key profile, fossil soil, engineering-geological properties, palaeocryogenesis.

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