Soil-paleoecologic objects of Suzdal Opolye as nature monuments

It is shown, that the structure of automorphic soil profiles territories of research territories depends on a structure of the parent rock. If the parent rock represents the complex layered thickness and has the attrib-utes of latest glacial pedolithogenesis, the soils with the complexes profiles having numerous attributes of polygenesis and heterochronism are formed on it. If the parent rock represents the single-component layer which has been not last through latest glacial pedolithogenesis the morphologically obvious attributes of holocenic soil formations are present only at it even if the thickness of the single-component layer does not exceed 05-meter. Comes out with the assumption with what exactly presence of attributes of the latest glacial pedolithogenesis provides the formation of typical holocenic soil profile.