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The incised valley of Ventimiglia, located along the Ligurian coast (NW Italy), was cut by deep river erosion during the Messinian sea-level fall and is connected seawards to a slope canyon. During Pliocene, the valley was flooded by the sea and transformed into a coastal embayment or ria. The infill sequence of the incised valley is up to 500 m thick. The paleovalley floor is locally paved by thin...
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