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 vertical
displacement 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.
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