GNGTS 2024 - Atti del 42° Convegno Nazionale

Session 3.2 GNGTS 2024 Fig 2 Resistvity model of the ERT3 line, in the transverse directon respect to the landslide. The availability of three-dimensional resistvity model and of the of the chargeability distributon of the subsoil, up to a depth of about 100 m below the surface, has highlighted the main lithological, hydrogeological and geo-geological characteristcs, identfying in detail the geometries of the conductve pelitc complex and of the surface separatng this formaton by the dolomite. (Fig 3)