A multidisciplinary approach has been used to evaluate Late Holocene relative sea level change along theeastern coast of the Gulf of Trieste. Published data, together with new 14C dating, have been compared
with predicted curves in order to evaluate the tectonic behaviour of the studied area. Observations
derived from precise geomorphological, archaeological and sedimentological measurements dated from
10 ka cal., sampled at elevations ranging between -25 and +0.10 m. Tectonic rates range from 1.01 mm/y
(Gulf of Trieste) and -1.99 mm/y (Villaggio del Pescatore), but are probably higher in the northwestern
sector, where the elevation of post-Roman geomorphological markers is lower. A detailed surveying of
notches, beachrocks, submerged shore platforms and the geological setting of the coastal area highlight
the variability of tectonic subsidence, indicated by geophysical data collected in the central part of the
gulf. Analyzed data indicate active tectonism. The tectonic setting of the northernmost sector is affected
by the presence of strike-slip faults which cause differential downdrop of the shoreline, as suggested by
significant increases of notch depths, ranging between -1.0 m and -2.7 m.
