The Dnieper river valley, in spite of being an old one, has only young terraces preserved in the section between Orsha and Shklov : two Vistulian-Young Pleniglacial terraces and two levels of the Late Glacial-Holocene floodplains with a large
and Early Holocene. Kame terraces are interstratified and covered with angular debris of supraglacial derivation, protecting them against post-depositional erosion and denudation. The thermoluminescence dating of kame sediments yielded a date which suggests