In this research, we studied the marine flood risk of the Cagliari plain in relation to the depressed coastal area, which includes a zone of the extremely high population density (almost half of the population of Sardinia) and major industrial infrastructures. The critical inundation altitudes in the Cagliari plain occur well above the average sea level, as demonstrated by the fact that, during meteorological -marine events with SW and SE winds, the normal and extreme meteorological tides reach heights of approximately +1.0 m in the Santa Gilla coastline and “high water” of + 1.5 m on the Santa Gilla lagoon, located in the western sector of the plain. In order to analyze the way the lagoon fills in and to recognise any active subsidence ...
Integrated archaeological and geological studies conducted on Mistras coastal barrier system of cent...
Two major synthems have been recognised along the coasts of Sardinia. The older one is composed of ...
The Middle Pleistocene–Holocene Sardinian stratigraphy has been revised to identify the roles played...
In this research, we studied the marine flood risk of the Cagliari plain in relation to the depresse...
Study The response of coastal barrier - lagoon systems to late Holocene high frequency sea level osc...
Multiproxy analysis composed of biostratigraphy and pollen analysis allowed reconstructing the palae...
We provide new data on relative sea-level change from the late Holocene for two locations in the cen...
We provide new data on relative sea-level change from the late Holocene for two locations in the cen...
Multiproxy analysis composed of biostratigraphy and pollen analysis allowed reconstructing the palae...
We provide new data on relative sea-level change from the late Holocene for two locations in the cen...
For its relative stability during Quaternary (from the isotopic stage 5 about 125,000 years ago) and...
We provide new data on relative sea-level change from the late Holocene for two locations in the cen...
Several boreholes were studied in detail through different analytical methods in order to highlight ...
Several sites, from the Cagliari and Oristano Gulfs and some spots distributed in central and southe...
Integrated archaeological and geological studies conducted on Mistras coastal barrier system of cent...
Two major synthems have been recognised along the coasts of Sardinia. The older one is composed of ...
The Middle Pleistocene–Holocene Sardinian stratigraphy has been revised to identify the roles played...
In this research, we studied the marine flood risk of the Cagliari plain in relation to the depresse...
Study The response of coastal barrier - lagoon systems to late Holocene high frequency sea level osc...
Multiproxy analysis composed of biostratigraphy and pollen analysis allowed reconstructing the palae...
We provide new data on relative sea-level change from the late Holocene for two locations in the cen...
We provide new data on relative sea-level change from the late Holocene for two locations in the cen...
Multiproxy analysis composed of biostratigraphy and pollen analysis allowed reconstructing the palae...
We provide new data on relative sea-level change from the late Holocene for two locations in the cen...
For its relative stability during Quaternary (from the isotopic stage 5 about 125,000 years ago) and...
We provide new data on relative sea-level change from the late Holocene for two locations in the cen...
Several boreholes were studied in detail through different analytical methods in order to highlight ...
Several sites, from the Cagliari and Oristano Gulfs and some spots distributed in central and southe...
Integrated archaeological and geological studies conducted on Mistras coastal barrier system of cent...
Two major synthems have been recognised along the coasts of Sardinia. The older one is composed of ...
The Middle Pleistocene–Holocene Sardinian stratigraphy has been revised to identify the roles played...