ABSTRACT
Engineering geological conditions of landslide area are determined on the basis of engineering geological mapping of the landslide area. The rock units found in the area of the Brus slide consist of Paleogene flysch deposit, i.e. series of interbedded sandstone and marls, clearly visible in the main as well as lateral scarps, Figure 1. Flysch bedrock is covered by thin superficial deposit of transported soil and residual soil.
