http://www.cnr.it/ontology/cnr/individuo/prodotto/ID41781
Mass-movement, geologic structure and morhologic evolution of the Pizzotto-Greci slope (Calabria, Italy) (Articolo in rivista)
- Type
- Label
- 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
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- http://www.sciencedirect.com/science/article/pii/S0169555X99000513 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
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- 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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