Abstract
Destructive volcaniclastic flows are among the most recurrent and dangerous natural phenomena in volcanic areas. They can originate not only during or shortly after an eruption (syn-eruptive) but also during a period of volcanic quiescence (inter-eruptive), when heavy and/or persistent rains remobilize loose pyroclastic deposits. The area in Italy most prone to such flows is that of the Apennine Mountains bordering the southern Campania Plain. These steep slopes are covered by pyroclastic material of variable thickness (a few cm to several m) derived from the explosive activity of the Somma-Vesuvius and Campi Flegrei volcanoes a few tens of kilometers to the west. The largest and most recent devastating event occurred on May 5, 1998, causing the death of more than 150 people and considerable damage to villages at the foot of the Apennine Mountains. This tragic event was only the most recent of a number of volcaniclastic flows affecting the area in both historical and prehistoric times. Historical accounts report that more than 500 events have occurred in the last five centuries and that more than half of these occurred in the last 100 years, causing hundreds of deaths. In order to improve volcaniclastic flow hazard zonation and risk mitigation in the study area, we produced a zonation map that identifies the drainage basins potentially prone to disruption. This map was obtained by combining morphological characteristics (concavity and basin shape factor) and the mean slope distribution of drainage basins derived from a digital elevation model with a 10-m resolution. These parameters allowed for the classification of 1,069 drainage basins, which have been grouped into four different classes of proneness to disruption: low, moderate, high and very high. The map compiled in a GIS environment, as well as the linked database, can be rapidly queried.
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References
Barberi F, Macedonio G, Pareschi MT, Santacroce R (1990) Mapping the tephra fallout risk: an example from Vesuvius, Italy. Nature 344:142–144
Bisson M, Cosimi G, Favalli M, Leoni FM, Mazzarini F, Pareschi MT, Santacroce R, Sgrò S, Sulpizio R, Zanchetta G (2002) GIS database for the assessment of debris flow hazard in two areas of the Campania region (southern Italy). Il Nuovo Cimento 25C:433–447
Bisson M, Favalli M, Fornaciai A, Mazzarini F, Isola I, Zanchetta G, Pareschi MT (2005) A rapid method to assess fire-related debris flow hazard in the mediterranean region: an example from Sicily (Southern Italy). Int J Appl Earth Obs 7:217–231
Bisson M, Pareschi MT, Zanchetta G, Sulpizio R, Santacroce R (2007a) 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. B Volcanol 70:157–167. doi:10.1007/s00445-007-0127-4
Bisson M, Fornaciai A, Mazzarini F (2007b) SITOGEO: A geographic database used for GIS applications. Il Nuovo Cimento C–Note Brevi–30C(3). doi:10.1393/ncc/i2007-10243-9
Bonardi G, D’Argenio P, Perrone V (1988) Geological Map of Southern Apennines: Consiglio Nazionale delle Ricerche (CNR), scale 1:250,000, 3 sheets
Bovis MJ, Jakob M (1999) The role of debris supply conditions in predicting debris-flow activity. Earth Surf Proc Land 24:1039–1054
Burrough PA, McDonell RA (1998) Principles of geographical information systems. Oxford University Press, New York, p 190
Calcaterra D, Parise M, Palma B, Pelella L (1999) The May 5th 1998, landsliding event in Campania (southern Italy): inventory of slope movements in the Quindici area. In: Yagi N, Yamagami T, Jiang J (eds) Proceedings of international symposium on slope stability engineering, IS, Shikoku’99, Matsuyama, Shikoku, November 8–11, Balkema, Rotterdam, pp 1361–1366
Calcaterra D, Parise M, Palma B, Pelella L (2000) Multiple debrisflows in volcaniclastic materials mantling carbonate slopes. In: Wieczorek GF, Naeser ND (eds) Debris-flow hazards mitigation: mechanics, prediction, and assessment. Balkema, Rotterdam, pp 99–107
Calcaterra D, de Riso R, Evangelista A, Nicotera MV, Santo A, Scotto di Santolo A (2003a) Slope instabilities in the pyroclastic deposits of the carbonate Apennine and Phlegrean district. In: Picarelli L (ed) Fast slope movements prediction and prevention for risk mitigation, Naples, May 11–13, 2003. Patron, Bologna, pp 61–75
Calcaterra D, Parise M, Palma B (2003b) Combining historical and geological data for the assessment of the landslide hazard: a case study from Campania, Italy. Nat Hazards Earth Syst 3:3–16
Capra L, Poblete MA, Alvarado R (2004) The 1997 and 2001 lahars of Popocatépetl volcano (Central Mexico): textural and sedimentological constraints on their origin and hazards. J Volcanol Geoth Res 131:351–369
Carrasco-Núñez G, Vallance J, Rose WI (1993) A voluminous avalanche-induced lahar from Citlaltépetl Volcano, Mexico: implications for hazard assessment. J Volcanol Geotherm Res 59:33–46
Cioni R, Longo A, Macedonio G, Santacroce R, Sbrana A, Sulpizio R, Andronico D (2003) Assessing pyroclastic fall hazard through field data and numerical simulations: example from Vesuvius. J Geophys Res 108:2063. doi:10.1029/2002JB002251
Costa A, Dell’Erba F, Di Vito MA, Isaia R, Macedonio G, Orsi G, Pfeiffer T (2009) Tephra fallout hazard assessment at the Campi Flegrei caldera (Italy). B Volcanol 71:259–273. doi:10.1007/s00445-008-0220-3
De Riso R, Buretta 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
Del Prete M, Guadagno FM, Hawkins AB (1998) Preliminary report on the landslides of 5 May 1998, Campania, southern Italy. B Eng Geol Environ 57:113–129
Di Crescenzo G, Santo A (1999) Analisi geomorfologica delle frane da scorrimento-colata rapida in depositi piroclastici della Penisola Sorrentina. Geografia Fisica e Dinamica Quaternaria 22:57–72
Di Crescenzo G, Santo A (2005) Debris slides–rapid earth flows in the carbonate massifs of the Campania region (Southern Italy): morphological and morphometric data for evaluating triggering susceptibility. Geomorphology 66:255–276
Environmental systems research institute (ESRI) ArcView GIS. Redlands, 1996
Favalli M, Pareschi MT (2004) Digital elevation model construction from structured topographic data: the DEST algorithm. J Geophys Res 109:F04004. doi:10.1029/2004JF000150
Ferrucci M, Pertusati S, Sulpizio R, Zanchetta G, Pareschi MT, Santacroce R (2005) Volcaniclastic debris flows at La Fossa Volcano (Vulcano Island, southern Italy): insights for erosion behaviour of loose pyroclastic material on steep slopes. J Volcanol Geotherm Res 145:173–191
Fiorillo F, Guadagno FM, Equino S, De Blasio A (2001) The December 1999 Cervinara landslides: further debris flows in the pyroclastic deposits of Campania (southern Italy). B Eng Geol Environ 60:171–184
Gabet EJ, Dunne T (2002) Landslide on coastal sage-scrub and grassland hillslopes in a severe El Ninõ winter: the effects on conversion on sediment delivery. Geol Soc Am Bull 114(8):983–990
Iverson RM (1997) The physics of debris flows. Rev Geophys 35(3):254–296
Lowe DR, Williams SN, Leigh E, Connor CC, Gemmell JB, Stoiber RE (1986) Lahars initiated by the 13 November eruption of Nevado del Ruiz, Colombia. Nature 324:51–53
Macías J, Capra L, Scott KM, Espíndola JM, García-Palomo A, Costa JE (2004) The 26 May 1982 breakout flows derived from failure of a volcanic dam at El Chichón, Chiapas, Mexico. Geo Soc Am Bull 116:233–246
Mejìa-Navarro M, Wohl EW, Oaks SD (1994) Geological hazards, vulnerability and risk assessment using GIS: model for Glenwood Spring, Colorado. Geomorphology 10:331–354
Migale LS, Milone A (1998) Colate di Fango in terreni piroclastici della Campania. Primi dati della ricerca storica: Rassegna Storica Salernitana, vol 15, pp 235–271
Newhall G, Punongbayan RS (eds) (1996) Fire and mud: eruption and lahars of Mount Pinatubo, Philippines. PHIVOLCS, Quezon City and University of Washington Press, Seattle
Onorati G, Braca G, Iritano G (1999) Evento idrogeologico del 4, 5 e 6 maggio 1998 in Campania. Monitoraggio e analisi idrologica. Atti Accademia Nazionale dei Lincei 154:103–108
Pareschi MT, Favalli M, Giannini F, Sulpizio R, Zanchetta G, Santacroce R (2000) May 5, 1998, debris flows in circumvesuvian areas (southern Italy): insights for hazard assessment. Geology 28:639–642
Pareschi MT, Santacroce R, Sulpizio R, Zanchetta G (2002) Volcaniclastic debris flows in the Clanio Valley (Campania, Italy): insights for the assessment of hazard potential. Geomorphology 43:219–231
Pierson TC (1985) Initiation and flow behavior of the 1980 Pine Creek and Muddy River lahars, Mt. St. Helens, Washington. Geo Soc Am Bull 96:1056–1069
Pierson TC (1995) Flow characteristic of large eruption-triggered debris flows at snow-clad volcanoes: constraints for debris-flow models. J Volcanol Geoth Res 66:283–294
Rosi M, Principe C, Vecci R (1993) The 1631 eruption of Vesuvius reconstructed from the review of chronicles and study of deposits. J Volcanol Geoth Res 58:151–182
Scott KM (1989) Magnitude and frequency of lahars and lahar-runout flows in the Toutle-Cowlitz River system. US Geol Surv Prof Pap 1447-B:33
Scott KM, Vallance JW, Pringl PT (1995) Sedimentology, behavior, and hazard of debris flows at Mount Rainer, Washington. US Geol Surv Prof Pap 1547:56
Scott KM, Macìas JL, Naranjo JA, Rodriguez S, McGeehin JP (2001) Catastrophic debris flows transformed from landslide in volcanic terrains: mobility, hazard assessment and mitigation strategies. US Geol Surv Prof Pap 1630:1–59
Scott KM, Vallance JW, Kerle N, Macìas JL, Strauch W, Devoli G (2005) Catastrophic precipitation-triggered lahar at Casita volcano, Nicaragua: occurrence, bulking and transformation. Earth Surf Proc Land 30:59–79
Sheridan MF (1979) Emplacement of pyroclastic flows: a review. In: Chapin CE, Elston WE (eds) Ash-flow Tuffs. Geol Soc Am Spec Pap 180:125–136
Sheridan MF, Malin MC (1983) Application of computer assisted mapping to volcanic hazard evaluation of surge eruptions: Vulcano, Lipari and Vesuvius. J Volcanol Geotherm Res 17:187–202
Sulpizio R, Zanchetta G, Demi F, Di Vito MA, Pareschi MT, Santacroce R (2006) The Holocene syneruptive volcaniclastic debris flows in the Vesuvian area: geological data as a clue for hazard assessment. Geol Soc Am Spec Pap 402:203–221
Tarquini S, Isola I, Favalli M, Mazzarini F, Bisson M, Pareschi MT, Boschi E (2007) TINITALY/01: a new triangular irregular network of Italy. Ann Geophys 50:407–425
Waitt RB, Pierson TC, MacLeod NS, Janda RJ, Voight B, Holcomb RT (1983) Eruption-triggered avalanches, flood, and lahar at Mount St. Helens: effect of winter snowpack. Science 221:1393–1397
Zanchetta G, Sulpizio R, Santacroce R, Cosimi G, Sgrò S, Pareschi MT, Bisson M, Favalli M (2003) Volcaniclastic debris flows in the Clanio valley (Campania, Italy). In: Picarelli L (ed) Fast slope movements prediction and prevention for risk mitigation, Naples, May 11–13, 2003. Patron, Bologna, pp 537–540
Zanchetta G, Sulpizio R, Pareschi MT, Leoni M, Santacroce R (2004a) Characteristic of May 5–6, 1998 volcaniclastic debrisflows in the Sarno areas (Campania, southern Italy): relationships to structural damage and hazard zonation. J Volcanol Geoth Res 133:377–393
Zanchetta G, Sulpizio R, Di Vito MA (2004b) The role of volcanic activity and climate in alluvial fan growth at volcanic areas: an example from southern Campania (Italy). Sediment Geol 168:249–280
Zeverbergen LW, Thorne CR (1987) Quantitative analysis of land surface topography. Earth Surf Proc Land 12:47–56
Acknowledgments
This work was funded by INGV-DPC Speed Project 2007–2008 (Task 2.4.1: Pericolosità da alluvionamenti e scorrimento di lahar—Responsible: F. Mazzarini). We thank Josè Luis Macias for reviewing the first draft of the manuscript. Two anonymous reviewers provided very useful suggestions for improving the manuscript.
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Bisson, M., Sulpizio, R., Zanchetta, G. et al. Rapid terrain-based mapping of some volcaniclastic flow hazard using Gis-based automated methods: a case study from southern Campania, Italy. Nat Hazards 55, 371–387 (2010). https://doi.org/10.1007/s11069-010-9533-6
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DOI: https://doi.org/10.1007/s11069-010-9533-6