A map for volcaniclastic debris flow hazards in Apennine areas surrounding the Vesuvius volcano (Italy)

References

• Barberi , F. , Macedonio , G. , Pareschi , M. T. and Santacroce , R. 1990 . Mapping the tephra fallout risk: An example from Vesuvius, Italy . Nature , 344 : 142 – 144 .
   Web of Science ®Google Scholar
• Bisson , M. , Pareschi , M. T. , Zanchetta , G. , Sulpizio , R. and Santacroce , R. 2007 . Volcaniclastic debris flow occurrences in the Campania region (southern Italy) and their relation to Holocene – Late Pleistocene pyroclastic fall deposits: Implications for large-scale hazard mapping . Bulletin of Volcanology , 70 : 157 – 167 .
   Web of Science ®Google Scholar
• Bisson , M. , Sulpizio , R. , Zanchetta , G. , Demi , F. and Santacroce , R. 2010 . Rapid terrain based mapping of volcaniclastic flow hazard using gis-based automated methods: A case study from southern Campania, Italy . Natural Hazards , 55 : 371 – 387 . doi: 10.1007/s11069-010-9533-6
   Web of Science ®Google Scholar
• Bonardi, G., D'Argenio, P., & Perrone, V. (1988). Geological Map of Southern Apennines: Consiglio Nazionale delle Ricerche (CNR), scale 1:250,000, 3 sheets.
   Google Scholar
• Bovis , M. J. and Jakob , M. 1999 . The role of debris supply conditions in predicting debris-flow activity . Earth Surface Process and Landforms , 24 : 1039 – 1054 .
   Web of Science ®Google Scholar
• Calcaterra , D. and Santo , A. 2004 . The January 10, 1997 Pozzano landslide, Sorrento Peninsula, Italy . Engineering Geology , 75 : 181 – 200 .
   Web of Science ®Google Scholar
• Carrara , A. , Crosta , G. and Frattini , P. 2003 . Geomorphological and historical data in assessing landslide hazard . Earth Surface Process and Landforms , 28 : 1125 – 1142 .
   Web of Science ®Google Scholar
• Cioni , R. , Bertagnini , A. , Santacroce , R. and Andronico , D. 2008 . Explosive activity and eruption scenarios at Somma-Vesuvius (Italy): Towards a new classification scheme . Journal of Volcanology and Geothermal Research , 178 : 331 – 346 .
   Web of Science ®Google Scholar
• Cioni , R. , Longo , A. , Macedonio , G. , Santacroce , R. , Sbrana , A. , Sulpizio , R. and Andronico , D. 2003 . Assessing pyroclastic fall hazard through field data and numerical simulations: Example from Vesuvius . Journal of Geophysical Research , 108 : 2063 doi: 10.1029/2002JB002251
   Web of Science ®Google Scholar
• Costa , A. , Dell'Erba , F. , Di Vito , M. A. , Isaia , R. , Macedonio , G. , Orsi , G. and Pfeiffer , T. 2009 . Tephra fallout hazard assessment at the Campi Flegrei caldera (Italy) . Bulletin of Volcanology , 71 : 259 – 273 . doi: 10.1007/s00445-008- 0220-3
   Web of Science ®Google Scholar
• Del Prete , M. , Guadagno , F. M. and Hawkins , A. B. 1998 . Preliminary report on the landslides of 5 May 1998, Campania, southern Italy . Bulletin of Engineering Geology and Environment , 57 : 113 – 129 .
   Google Scholar
• De Riso, R., Budetta, P., Calcaterra, D., & Santo, A. (1999). Le colate rapide in terreni piroclastici del territorio campano, Atti Convegno Previsione e prevenzione di movimenti franosi rapidi, Trento, 17–19 giugno 1999, pp. 133–150.
   Google Scholar
• Dipartimento della Protezione Civile (1995). Pianificazione nazionale d'emergenza dell'area vesuviana. Dipartimento della Protezione Civile p. 157.
   Google Scholar
• Gabet , E. J. and Dunne , T. 2002 . Landslide on coastal sage-scrub and grassland hillslopes in a severe El Niño winter: The effects on conversion on sediment delivery . Geological Society of America Bulletin , 114 ( 8 ) : 983 – 990 .
   Web of Science ®Google Scholar
• Iverson , R. M. 1997 . The physics of debris flows . Reviews of Geophysics , 35 ( 3 ) : 254 – 296 .
   Web of Science ®Google Scholar
• Mazzarini, F., & Bisson, M. (2008). – Stabilità di versante dei depositi di ricaduta, Report tecnico INGV (Progetto Speed – Scenari di Pericolosità per la Prevenzione del Rischio dei Vulcani della Campania – Prodotto D2.4.2 – Prodotto D2.4.23) pp 3.
   Google Scholar
• Migale , L. S. and Milone , A. 1998 . Colate rapide di fango in terreni piroclastici della Campania. Primi dati della ricerca storica . Rassegna Storica Salernitana , 15 : 253 – 271 .
   Google Scholar
• Neri , A. , Aspinall , W. P. , Cioni , R. , Bertagnini , A. , Baxter , P. J. , Zuccaro , G. , Andronico , D. , Barsotti , S. , Cole , P. D. , Esposti Ongaro , T. , Hincks , T. K. , Macedonio , G. , Papale , P. , Rosi , M. , Santacroce , R. and Woo , G. 2008 . Developing an event tree for probabilistic hazard and risk assessment at Vesuvius . Journal of Volcanology and Geothermal Research , 178 : 397 – 415 . (this issue). doi: 10.1016/j.jvolgeores.2008.05.014
   Web of Science ®Google Scholar
• Pareschi , M. T. , Favalli , M. , Giannini , F. , Sulpizio , R. , Zanchetta , G. and Santacroce , R. 2000 . May 5, 1998, debris flows in circumvesuvian areas (southern Italy): Insights for hazard assessment . Geology , 28 : 639 – 642 .
   Web of Science ®Google Scholar
• Pareschi , M. T. , Santacroce , R. , Sulpizio , R. and Zanchetta , G. 2002 . Volcaniclastic debris flows in the Clanio Valley (Campania, Italy): Insights for the assessment of hazard potential . Geomorphology , 43 : 219 – 231 .
   Web of Science ®Google Scholar
• Tarquini , S. , Isola , I. , Favalli , M. , Mazzarini , F. , Bisson , M. , Pareschi , M. T. and Boschi , E. 2007 . TINITALY/01: A new Triangular Irregular Network of Italy . Annals of Geophysics , 50 ( 3 ) : 407 – 425 .
   Web of Science ®Google Scholar
• Zanchetta, G., Sulpizio, R., Pareschi, M. T., Bisson, M., Cosimi, G., Favalli, M., Santacroce, R., & Sgrò, S. (2003). Volcaniclastic debris flows in the Clanio Valley (Campania, Italy). In Fast slope movement prediction and prevention for risk mitigation, Sorrento 2003, FMS paper n. 036 (5 pp.).
   Google Scholar
• Zanchetta , G. , Sulpizio , R. , Pareschi , M. T. , Leoni , M. and Santacroce , R. 2004 . Characteristic of May 5–6, 1998 volcaniclastic debrisflows in the Sarno areas (Campania, southern Italy): Relationships to structural damage and hazard zonation . Journal of Volcanology and Geothermal Research , 133 : 377 – 393 .
   Web of Science ®Google Scholar