GNGTS 2023 - Atti del 41° Convegno Nazionale

Session 1.1 - POSTER GNGTS 2023 Fig. 3 - a) Landscape view of the Dajti thrust; b) Quaternary normal fault; c) Old breccias connecting to the present slope; d) Influence on drainage by growth of the Makaresh anticline. At the foot of the Dajti-Kruja main thrust, an Early Oligocene-Late Miocene succession of mainly clay and sandstone deposits crops out, with a prominent bedding steeply dipping SW. The tectonic uplift and the differential rate of the erosional processes have generated impressive