“…According to the geomorphological map (scale 1: 55 000) of Ukraine, the investigated territory corresponds to Makariv moraine f luvioglacial wavy slightly dissected plain between Irpin's, Buchanka's, Teteriv's and Zdvyzh's River valleys. Knowing the physical-geographical and administrative location of the city, it is easy to identify that according to principles of engineering and geological classification, Irpin is situated in the limits of East-European Craton, the north-east slope of Ukrainian Shield province, Kyiv Polesia subprovince, engineering geological region of Makariv moraine f luvioglacial wavy slightly dissected plain (Paton et al, 2007). There are such engineering geological districts in the limits of Irpin according to engineering geomorphological zoning of Kyiv city district's map: erodible and depositional alluvial plain and denudation-depositional watershed moraine and f luvioglacial plain (Barshchevsky et al, 1989).…”