2004
DOI: 10.1016/j.geomorph.2004.03.003
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Coastal processes and cliff recession between Gabicce and Pesaro (northern Adriatic Sea): a case history

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Cited by 31 publications
(22 citation statements)
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“…1), which has retreated by 300 to 1000 m in the last 6000 years (Colantoni et al 2004), the modern coast is accreted by an up to 1.2 km-wide depositional plain joining sand-gravel beaches seawards. The major South Emilia Romagna-Northern Marche rivers (i.e., from the NW, the Marecchia, Conca, Foglia, Metauro, Cesano and Misa rivers, Fig.…”
Section: Geological-geomorphological Settingmentioning
confidence: 99%
“…1), which has retreated by 300 to 1000 m in the last 6000 years (Colantoni et al 2004), the modern coast is accreted by an up to 1.2 km-wide depositional plain joining sand-gravel beaches seawards. The major South Emilia Romagna-Northern Marche rivers (i.e., from the NW, the Marecchia, Conca, Foglia, Metauro, Cesano and Misa rivers, Fig.…”
Section: Geological-geomorphological Settingmentioning
confidence: 99%
“…1). Part of the area (GabiccePesaro) is a cliff, the first rocky shore to interrupt the monotonous continuity of sandy beaches on the Italian side of the Adriatic Sea, south of Monfalcone (Trieste) (Colantoni et al 2004). It is also the seaward limit of the Monte San Bartolo Regional Natural Park, which was created in 1997 to protect an area of great naturalistic importance, since it lies along a main bird migratory route, includes the wintering habitats of many bird species, and also plays host to some rare plant species.…”
Section: Study Areamentioning
confidence: 99%
“…Regardless of such minor remoulding, several authors attest to the position of the 'Roman shoreline' based on both geomorphological and archaeological evidence (Coltorti, 1991(Coltorti, , 1997Curzi & Tonnarelli, 1991;Dall'Aglio, 1991;Elmi, Fanucci, Nesci, Beer, & Pignocchi, 1994;Elmi, Colantoni, Gabbianelli, & Nesci, 2001). At present, throughout the north-Marche area, except for two actively retreating rock cliffs (Colantoni, Mencucci, & Nesci, 2004), a 500 to more than 1000 m-wide sedimentary coastal plain separates the preserved fan apex and related wave-cut scarps from the shoreline.…”
Section: Map Descriptionmentioning
confidence: 95%