Mass-movement, geologic structure and morhologic evolution of the Pizzotto-Greci slope (Calabria, Italy) (Articolo in rivista)

Type
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  • Mass-movement, geologic structure and morhologic evolution of the Pizzotto-Greci slope (Calabria, Italy) (Articolo in rivista) (literal)
Anno
  • 1999-01-01T00:00:00+01:00 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
  • 10.1016/S0169-555X(99)00051-3 (literal)
Alternative label
  • Sorriso-Valvo M. (1), Gullà G. (1), Antronico L. (1), Tansi C. (1), Amelio M. (2) (1999)
    Mass-movement, geologic structure and morhologic evolution of the Pizzotto-Greci slope (Calabria, Italy)
    in Geomorphology (Amst.); ELSEVIER SCIENCE BV, PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS, AMSTERDAM (Paesi Bassi)
    (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
  • Sorriso-Valvo M. (1), Gullà G. (1), Antronico L. (1), Tansi C. (1), Amelio M. (2) (literal)
Pagina inizio
  • 147 (literal)
Pagina fine
  • 163 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#url
  • http://www.sciencedirect.com/science/article/pii/S0169555X99000513 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
  • 30 (literal)
Rivista
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#pagineTotali
  • 17 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroFascicolo
  • 1-2 (literal)
Note
  • Scopu (literal)
  • ISI Web of Science (WOS) (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
  • (1) Consiglio Nazionale delle Ricerche Istituto di Ricerca per la Protezione Idrogeologica - Via Cavour, 87030 Roges di Rende (CS), Italy (2) Università degli Studi della Calabria, Dipartimento di Scienze della Terra, 87036 Arcavacata di Rende (CS), Italy (literal)
Titolo
  • Mass-movement, geologic structure and morhologic evolution of the Pizzotto-Greci slope (Calabria, Italy) (literal)
Abstract
  • The main aspects of the geological and geomorphological studies and some preliminary geotechnical data are presented here, along with a conceptual model aimed at describing the relationships between the mass-movements on the slope and the constructionrdestruction stages of the fan at the base of the slope. The model is based on the assumption that aggradation has a stabilising effect on the slope, thus debris-flow activity is reduced and, consequently, destruction of the fan occurs, bringing the slope again towards unstable conditions. The reactivation of mass-movement, however, leads to the reconstruction of the fan and the buttressing effect at the base of the slope is restored. Thus, the process is cyclic and self-regulating. (literal)
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