Identification of potentially active structures along the Sava river using topographic, and leveling line data

Anomalies in vertical displacement rates related to recent geodynamics were determined between Rate e and Ljubljana by comparing leveling line data with topography of the Sava river longitudinal profile. Beside the general trend showing increase of verticaldisplacement in the S-N direction, segmentation of the area is noted. The later suggests that active geological structures exist in the northern part of the Ljubljana basin and in the Upper Sava valley respectively.