“…Both the soil and the stratified rock masses show the nature of anisotropy. For this reason, theoretical or numerical models should be able to simulate this kind of layered soils and rocks as cross-anisotropic medium (Amadei et al, 1988;Barden, 1963;Gibson, 1974;Lee & Yang, 1998;Sekowski, 1986;Sheorey, 1994). In this paper, the soil mass is modelled as a linearly elastic medium with cross-anisotropic properties.…”