http://www.cnr.it/ontology/cnr/individuo/prodotto/ID292461
Mutual interactions between slope-scale gravitational processes and morpho-structural evolution of central Apennines (Italy): review of some selected case histories (Articolo in rivista)
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- Mutual interactions between slope-scale gravitational processes and morpho-structural evolution of central Apennines (Italy): review of some selected case histories (Articolo in rivista) (literal)
- Anno
- 2014-01-01T00:00:00+01:00 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
- 10.1007/s12210-014-0348-3 (literal)
- Alternative label
Esposito C.*, Di Luzio E.**, Scarascia Mugnozza G.**, Bianchi Fasani G*** (2014)
Mutual interactions between slope-scale gravitational processes and morpho-structural evolution of central Apennines (Italy): review of some selected case histories
in Rendiconti lincei. Scienze fisiche e naturali; Springer Verlag Italia, Milano (Italia)
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- Esposito C.*, Di Luzio E.**, Scarascia Mugnozza G.**, Bianchi Fasani G*** (literal)
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- * Dipartimento di Scienze della Terra, Sapienza Universita` di Roma,
** CNR-ITABC (ex IGAG)
*** Centro di Ricerca Casaccia, ENEA Agenzia nazionale per le nuove tecnologie, l'energia e lo sviluppo economico sostenibile. (literal)
- Titolo
- Mutual interactions between slope-scale gravitational processes and morpho-structural evolution of central Apennines (Italy): review of some selected case histories (literal)
- Abstract
- This short note focuses on the review of some selected large slope instabilities, such as massive rock slope failures, that occurred in slopes well representative of
widespread morpho-structural settings in the central Apennines (Italy). The analyses of such case histories highlight (a) the role of inherited geological and morphostructural
features on failure mechanisms and (b) the interplay between such processes and the Quaternary morpho-structural evolution of the mountain chain.
Some of the here described rock slope failures are framed within wider slope sections showing evidence of slope-scale gravitational deformation processes. Some cases demonstrate
that the activation of the latter is strongly controlled by stress variations induced on the slopes by the combination of erosional processes and tectonic offset, i.e. topographic stress
increase that typically accompanied the Quaternary morpho-structural evolution of the orogen.
Furthermore, some case studies confirm also for central Apennine that the occurrence of large-sized rock slope failures actively contributed to morpho-genesis, as the effect of the deposition
of the related debris on the valley bottom can result in long-term impacts on environmental conditions, such as topographic, hydrologic and hydrogeological variations. (literal)
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