У статті розглядається стратиграфія палеолітичної стоянки Радомишль у Житомирському Поліссі.
Paper discusses the attempt of N.P. Gerasimenko to “block” the stratigraphy of the Late Palaeolithic site of Radomyshl’. The author supposes - and there are grounds for this - the cultural layer of this site is situated practically in the lowermost part of Prichernomorie sub-aerial loams, on the buried soil of Dofinovka age (Stillfried B). Industry of Radomyshl’, according to its typological peculiarities, is epi-Aurignacian, to the author notion. It is very likely, that it might be confirmed by the stratigraphy of the site. As it stressed, the portion of profile has signs of aeolian or aeolian-deluvial genesis, signs of loesslike loams.