Abstract

Established the thickness of alluvium (loamy facia) on the segmental-maned and flattened floodplain of Voja-river near Bagramovo-village. Within the various morphological types of the floodplain, the presence of both relatively ancient and younger sites has been determined. Revealed spatial features of the distribution of the buried soils, their thickness in the profile, depth of occurrence. Showing the main features of the relief of the valley of Voja-river in the study area, the ratio of the width of the mainstream and floodplain, the presence of old channels, including significantly greater than the width of the modern channel of Voja-river.

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