Pregled bibliografske jedinice broj: 774486
Geomorfological and archaeological evidences of co-seismic subsidence on the northeastern Adriatic coasts
Geomorfological and archaeological evidences of co-seismic subsidence on the northeastern Adriatic coasts // 23 Congresso nazionale GNDTS, Riassunti estesi delle comunicazioni
Rim, 2004. str. 277-278 (predavanje, međunarodna recenzija, sažetak, znanstveni)
CROSBI ID: 774486 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Geomorfological and archaeological evidences of co-seismic subsidence on the northeastern Adriatic coasts
Autori
Antonioli, Fabricio ; Auriemma, Rita ; Faivre, Sanja ; Fouache, Eric ; Furlani, Stefano ; Kovačić, Vladimir ; Mauro, S.
Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, znanstveni
Izvornik
23 Congresso nazionale GNDTS, Riassunti estesi delle comunicazioni
/ - Rim, 2004, 277-278
Skup
23 Congresso nazionale GNDTS
Mjesto i datum
Rim, Italija, 14.12.2004. - 15.12.2004
Vrsta sudjelovanja
Predavanje
Vrsta recenzije
Međunarodna recenzija
Ključne riječi
tidal notch; sea-level; Adriatic
Sažetak
With the aim to study the last 2 ka sea level change, Pirazzoli 1980, Fouache et al., 2000, Antonioli et al., 2003, Benac et al., 2004, have done geomorfological, archaeological and sismotectonic researches along the coast of Duino (Ts), southern Istria, up to Rijeka Bay (Croatia). Along the limestone coast, the quoted Authors revealed the quasi-continuous occurrence of a submerged tidal notch at a depth between -0.6 e -1.8 m. In addition, roman age archeological markers are under 0, 5 m depth and often over 1 m depth. In light of new geomorphological and archaeological observations we support the idea of possible and extend to a larger area the early interpretation of Benac et al., 2004 who relate the subsidence of the notch to a the A.D. 361 seismic event.
Izvorni jezik
Engleski
Znanstvena područja
Geografija
