1,325 research outputs found
CAratterizzazione qualitativa del fiume Sele attraverso indagine biologica ed ecotossicologica
No full text
Depositional history and palaeogeographic reconstruction of sele coastal plain during magna grecia settlement of hera argiva (Southern Italy)
No full textThe Sele river coastal plain, located in Campania (southern Italy), is a broad subsiding area associated with rifting of the Tyrrhenian Sea. During the early Holocene, the fast sea-level rise led to a transgressive coastal system with landward shift of beach and marsh-lagoon deposits. During the late Holocene, the decrease of sea-level rise rate resulted in the coastal system progradation and lagoon infilling. Settlement of the sanctuary of Hera Argiva by Greeks, in the Sele coastal plain, occurred in 6 th century B.C. Reconstruction of environments at that time allows to locate the coastline 250 m landward with respect to the present. A coastal system comprising a beach and sand dune ridge was present, and extensive bogs and ponds were formed behind the dunes. The sanctuary founded on the levee of the Sele river at the edge of the marshes was surrounded by a natural garden with luxuriant vegetation. The presence of Myrtus plants perhaps introduced by man in the Hera Argiva garden is inferred
Carta Geologica d’Italia Scala 1:50000, Foglio 486 Foce del Sele, ISPRA - Servizio Geologico d’Italia
No full textCartografia Geologica alla scala 1:50000 dell'area emersa e sommersa, fino a -250 m di profondità, del territorio della regione Campania ricadente nel Foglio 486 Foce del Sele della Carta Geologica d'Italia alla scala 1:5000
Seismic vulnerability evaluation of Devil Bridge on Sele River
No full textObject of the present study is the masonry bridge, still standing, built in 1871, by Eng. Fiocca, on Sele River, near Salerno. This bridge has a single semi-elliptic arch, spanning 55.00 m, with a rise of 13.55 m and a width of 5.40 m; in order to reduce the dead loads the inner tympani were lightened employing ring-like vaults. The first step of this research has been the study of the bridge static behaviour, deduced by the material survey of the existing structure, but also analyzing, verifying and enriching matters treated in the Report of Eng. Sacco, a Fiocca’s collaborator, in which all phases of Devil Bridge designing and building are fully described. The second step has been the evaluation of its seismic vulnerability: a three-dimensional finite element model has been implemented in ABAQUS code. To assess the bridge seismic capacity, non-linear pushover analyses have been carried out
Depositional history and paleogeographic reconstruction on Sele coastal plain during Magna Grecia Settlement of Hera Argiva (Southern Italy)
No full textThe Sele river coastal plain, located in Campania (southern Italy), is a broad subsiding area associated with rifting of the Tyrrhenian Sea. During the early Holocene, the fast sea-level rise led to a transgressive coastal system with landward shift of beach and marsh-lagoon deposits. During the late Holocene, the decrease of sea-level rise rate resulted in the coastal system progradation and lagoon infilling. Settlement of the sanctuary of Hera Argiva by Greeks, in the Sele coastal plain, occurred in 6th century B.C. Reconstruction of environments at that time allows to locate the coastline 250 m landward with respect to the present. A coastal system comprising a beach and sand dune ridge was present, and extensive bogs and ponds were formed behind the dunes. The sanctuary founded on the levee of the Sele river at the edge of the marshes was surrounded by a natural garden with luxuriant vegetation. The presence of Myrtus plants perhaps introduced by man in the Hera Argiva garden is inferred
Depositional history and paleogeographic reconstruction on Sele coastal plain during Magna Grecia Settlement of Hera Argiva (Southern Italy)
No full textThe Sele river coastal plain, located in Campania (southern Italy), is a broad subsiding area associated with rifting of the Tyrrhenian Sea. During the early Holocene, the fast sea-level rise led to a transgressive coastal system with landward shift of beach and marsh-lagoon deposits. During the late Holocene, the decrease of sea-level rise rate resulted in the coastal system progradation and lagoon infilling. Settlement of the sanctuary of Hera Argiva by Greeks, in the Sele coastal plain, occurred in 6th century B.C. Reconstruction of environments at that time allows to locate the coastline 250 m landward with respect to the present. A coastal system comprising a beach and sand dune ridge was present, and extensive bogs and ponds were formed behind the dunes. The sanctuary founded on the levee of the Sele river at the edge of the marshes was surrounded by a natural garden with luxuriant vegetation. The presence of Myrtus plants perhaps introduced by man in the Hera Argiva garden is inferred
Carta Geologica Regionale 1:25000 Foce del Sele - 486 SE, foglio 486 Foce del Sele
No full textCartografia geologica regionale alla scala 1:25000 delle aree emerse e sommerse pro parte del territorio della regione Campania, ricadente nel settore meridionale del Foglo n°486 Foce del Sele della Carta Geologica d'Italia alla scala 1:50000
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