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Volcanic hazard assessment at the restless Campi Flegrei caldera

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Abstract

Eruption forecasting and hazard assessments at the restless Campi Flegrei caldera, within the Neapolitan volcanic area, have been performed using stratigraphical, volcanological, structural and petrological data.

On the basis of the reconstructed variation of eruption magnitude through time, we hypothesize that the most probable maximum expected event is a medium-magnitude explosive eruption, fed by trachytic magma. Such an eruption could likely occur in the north-eastern sector of the caldera floor that is under a tensile stress regime, when the ongoing deformation will generate mechanical failure of the rocks. A vent could open also in the western sector, at the intersection of two fault systems contemporaneously activated, as happened in the last eruption at Monte Nuovo. The eruption could likely be preceded by precursors apparent to the population, such as ground deformation, seismicity and increase in gas emissions. It will probably alternate between magmatic and phreatomagmatic phases with the generation of tephra fallout, and dilute and turbulent pyroclastic currents. During and/or after the eruption, the re-mobilization of ash by likely heavy rains, could probably generate mud flows.

In order to perform a zoning of the territory in relation to the expected volcanic hazards, we have constructed a comprehensive hazard map. On this map are delimited (I) areas of variable probability of opening of a new vent, (II) areas which could be affected by variable load of fallout deposits, and (III) areas over which pyroclastic currents could flow. The areas in which a vent could likely open have been defined on the basis of the dynamics of the ongoing deformation of the caldera floor. To construct the fallout hazard map we have used the frequency of deposition of fallout beds thicker than 10 cm, the frequency of load on the ground by tephra fallout and the direction of dispersal axes of the deposits of the last 5 ka, and the limit load of collapse for the variable types of roof construction. The pyroclastic-current hazard map is based on the areal distribution and frequency of pyroclastic-current deposits of the last 5 ka.

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References

  • Agip (1987) Modello geotermico del sistema flegreo (Sintesi). Servizi Centrali per l’Esplorazione SERG-MESG, San Donato, 23 pp

  • Alberico I, Lirer L, Petrosino P, Scandone R (2002) A methodology for the evaluation of long-term volcanic risk from pyroclastic flows in Campi Flegrei (Italy). J Volcanol Geotherm Res 116:63–78

    Google Scholar 

  • Allard P, Maiorani A, Tedesco D, Cortecci G, Turi B (1991) Isotopic study of the origin of sulphur and carbon in Solfatara fumaroles, Campi Flegrei Caldera. J Volcanol Geotherm Res 48:139–159

    Google Scholar 

  • Aloisi JC, Monaco A, Planchais N, Thommeret J, Thommeret Y (1978) The Holocene transgression in the Golfe du Lion, Southwestern France: paleogeographic and paleobotanical evolution. Geogr Phys Quat 32(2):145–162

    Google Scholar 

  • Barberi F, Innocenti F, Lirer L, Munno R, Pescatore T, Santacroce R (1978) The Campanian Ignimbrite: a major prehistoric eruption in the Neapolitan area (Italy). Bull Volcanol 41(1):1–22

    Google Scholar 

  • Barberi F, Corrado G, Innocenti F, Luongo, G (1984) Phlegraean Fields 1982–1984: Brief chronicle of a volcano emergency in a densely populated area. Bull Volcanol 47(2):175–185

    Google Scholar 

  • Barberi F, Carapezza M, Innocenti F, Luongo G, Santacroce R (1989) The problem of volcanic unrest: the Phlegraean Fields case history. Atti Conv Lincei 80:387–405

    Google Scholar 

  • Berrino G, Corrado G, Luongo G, Toro B (1984) Ground deformation and gravity change accompanying the 1982 Pozzuoli uplift. Bull Volcanol 47(2):187–200

    Google Scholar 

  • Blong R (2003) Building damage in Rabaul, Papua New Guinea, 1994. Bull Volcanol 65:43–54

    Google Scholar 

  • Bonafede M, Mazzanti M (1998) Modelling gravity variations consistent with ground deformation in the Campi Flegrei caldera (Italy). J Volcanol Geotherm Res 81:137–157

    Google Scholar 

  • Casertano L, Oliveri A, Quagliarello MT (1976) Hydrodynamics and geodynamics in the Phlegraean Fields area of Italy. Nature 264:161–164

    Google Scholar 

  • Celico P, Dall’Aglio M, Ghiara MR, Stanzione D, Brondi M, Prosperi M (1992) Geochemical monitoring of the thermal fluids in the phlegraean fields from 1970 to 1990. Boll Soc Geol It 111:409–422

    Google Scholar 

  • Cinque A, Rolandi G, Zamparelli V (1985) L’estensione dei depositi marini Olocenici nei Campi Flegrei in relazione alla vulcano-tettonica. Boll Soc Geol It 104:327–348

    Google Scholar 

  • Chiodini G, Marini L (1998) Hydrothermal gas equilibria: The H2O-H2-CO2-CO-CH4 system. Geochim Cosmochim Acta 62(15):2673–2687

    Article  CAS  Google Scholar 

  • 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 Research 108, 82, 2063 DOI 10.1029/2001JB000642

    Google Scholar 

  • Civetta L, Orsi G, Pappalardo L, Fisher RV, Heiken G, Ort M (1997) Geochemical zoning, mingling, eruptive dynamics and depositional processes—The Campanian Ignimbrite, Campi Flegrei caldera, Italy. J Volcanol Geotherm Res 75:183–219

    CAS  Google Scholar 

  • Corrado G, Guerra I, Lo Bascio A, Luongo G, Rampoldi F (1977) Inflation and microearthquake activity of Phlegraean Fields, Italy. Bull Volcanol 40(3):169–188

    Google Scholar 

  • Corrado G, De Lorenzo S, Mongelli F, Tramacere A, Zito G (1998) Surface heat flow density at Phlegraean Fields caldera (Southern Italy). Geothermics 27:469–484

    Article  Google Scholar 

  • D’Antonio M, Civetta L, Orsi G, Pappalardo L, Piochi M, Carandente A, de Vita S, Di Vito MA, Isaia R, Southon J (1999) The present state of the magmatic system of the Campi Flegrei caldera based on the reconstruction of its behaviour in the past 12 ka. J Volcanol Geotherm Res 91:247–268

    Google Scholar 

  • Deino AL, Orsi G, Piochi M, de Vita S (2004) The age of the Neapolitan Yellow Tuff caldera-forming eruption (Campi Flegrei caldera – Italy) assessed by 40Ar/39Ar dating method. J Volcanol Geotherm Res (in press)

  • Dellino P, La Volpe L (2000) Structures and grain size distribution in surge deposits as a tool for modelling the dynamics of dilute pyroclastic density currents at La Fossa di Vulcano (Aeolian Islands, Italy). J Volcanol Geoth Res 96:57–78

    Article  CAS  Google Scholar 

  • Dellino P, Isaia R, La Volpe L, Orsi G (2001) Statistical analysis of textural data from complex pyroclastic sequence: implication for fragmentation processes of the Agnano-Monte Spina eruption (4.1 ka), Phlegraean Fields, southern Italy. Bull Volcanol 63:443–461

    Article  Google Scholar 

  • Dellino P, Isaia R, La Volpe L, Orsi G (2004a) Interference of particles fallout on the emplacement of pyroclastic surge deposits of the Agnano-Monte Spina eruption (Phlegraean Fields, Southern Italy). J Volcanol Geotherm Res (in press)

  • Dellino P, Isaia R, Veneruso M (2004b) Turbulent boundary layer shear flow as an approximation of pyroclastic surge: implication for hazard assessment at Phlegraean Fields. J Volcanol Geotherm Res (in press)

  • De Natale G, Pingue F (1993) Ground deformation in collapsed caldera structures. J Volcanol Geotherm Res 57:19–38

    Google Scholar 

  • De Vivo B, Rolandi G, Gans PB, Calvert A, Bohrson WA, Spera FJ, Belkin AE (2001) New constraints on the pyroclastic eruption history of the Campanian volcanic plain (Italy). Mineral Petrol 73:47–65

    Article  Google Scholar 

  • de Vita S, Orsi G, Civetta L, Carandente A, D’Antonio M, Di Cesare T, Di Vito M, Fisher RV, Isaia R, Marotta E, Ort M, Pappalardo L, Piochi M, Southon J (1999) The Agnano-Monte Spina eruption (4.1 ka) in the resurgent, nested Campi Flegrei caldera (Italy). J Volcanol Geotherm Res 91:269–301

    Google Scholar 

  • Di Maio R, Patella D, Petrillo Z, Siniscalchi A, Cecere G, De Martino P (2000) Application of electric and electromagnetic methods to the definition of the Campi Flegrei caldera (Italy). Annali di Geofisica 43:315–390

    Google Scholar 

  • Di Vito MA, Lirer L, Mastrolorenzo G, Rolandi G (1987) The Monte Nuovo eruption (Campi Flegrei, Italy). Bull Volcanol 49:608–615

    Google Scholar 

  • Di Vito MA, Isaia R, Orsi G, Southon J, de Vita S, D’Antonio M, Pappalardo L, Piochi M (1999) Volcanic and deformational history of the Campi Flegrei caldera in the past 12 ka. J Volcanol Geotherm Res 91:221–246

    Google Scholar 

  • Dvorak JJ, Gasparini P (1991) History of earthquakes and vertical movement in Campi Flegrei caldera, Southern Italy: comparison of precursory events to the a.d. 1538 eruption of Monte Nuovo and activity since 1968. J Volcanol Geotherm Res 48:77–92

    Google Scholar 

  • Fedele F, Giaccio B, Isaia R, Orsi G (2002) Ecosystem impact of the Campanian Ignimbrite eruption in Late Pleistocene Europe. Quaternary Research 57:420–424

    Article  Google Scholar 

  • Fedele F, Giaccio B, Isaia R, Orsi G (2003). The Campanian Ignimbrite eruption, Heinrich Event 4, and Palaeolithic change in Europe: a high-resolution investigation. In: Volcanism and Earth’s Atmosphere. AGU Geophys Monograph 139:301–325

    Google Scholar 

  • Fisher RV, Orsi G, Ort M, Heiken G (1993) Mobility of large-volume pyroclastic flow—emplacement of the Campanian Ignimbrite, Italy. J Volcanol Geotherm Res 56:205–220

    CAS  Google Scholar 

  • Isaia R, D’Antonio M, Dell’Erba F, Di Vito M, Orsi G (2004) The Astroni volcano: the only example of close eruptions within the same vent area in the recent history of the Campi Flegrei caldera (Italy). J Volcanol Geotherm Res (in press)

    Google Scholar 

  • Iuliano T, Mauriello P, Patella D (2000) A probability tomographic approach to the analysis of potential field surveys in the Campi Flegrei caldera (Italy). Annali di Geofisica 44:403–420

    Google Scholar 

  • Lirer L, Mastrolorenzo G, Rolandi G (1987) Un evento pliniano nell’attività recente dei Campi Flegrei. Boll Soc Geol It 106:461–473

    Google Scholar 

  • Lirer L, Petrosino P, Alberico I (2001) Volcanic hazard assessment at volcanic fields: the Campi Flegrei case history. J Volcanol Geotherm Res 112:55–75

    Article  Google Scholar 

  • Lundgren P, Usai S, Sansosti E, Lanari R, Tesauro M, Eonaro G, Berardino P (2001) Modeling surface deformation observed with synthetic aperture interferometry at Campi Flegrei caldera. J Geophys Research 106:19,355–19,366

    Google Scholar 

  • Malin MC, Sheridan M (1982) Computer assisted mapping of pyroclastic surges. Science 217:637–640

    Google Scholar 

  • Marianelli P, Proto M, Sbrana A (2003) Water content variability in Ignimbrite Campana melts. New insights on magma chamber history. GNV Gen Ass, Rome, June 9–11, Abstracts, 208 pp

  • Orsi G, Gallo G, Zanchi A (1991) Simple shearing block resurgence in caldera depressions. A model from Pantelleria and Ischia. J Volcanol Geotherm Res 47:1–11

    Google Scholar 

  • Orsi G, D’Antonio M, de Vita S, Gallo G (1992) The Neapolitan Yellow Tuff, a large-magnitude trachytic phreatoplinian eruption: eruptive dynamics, magma withdrawal and caldera collapse. J Volcanol Geotherm Res 53:275–287

    Google Scholar 

  • Orsi G, Civetta L, D’Antonio M, Di Girolamo P, Piochi M (1995) Step-filling and development of a three-layers magma chamber: the Neapolitan Yellow Tuff case history. J Volcanol Geotherm Res 67:291–312

    Google Scholar 

  • Orsi G, de Vita S, Di Vito M (1996) The restless, resurgent Campi Flegrei nested caldera (Italy): constraints on its evolution and configuration. J Volcanol Geotherm Res 74:179–214

    CAS  Google Scholar 

  • Orsi G, Civetta L, Del Gaudio C, de Vita S, Di Vito MA, Isaia R, Petrazzuoli S, Ricciardi G, Ricco C (1999a) Short-Term Ground Deformations and Seismicity in the Nested Campi Flegrei Caldera (Italy): an example of active block resurgence in a densely populated area. J Volcanol Geotherm Res 91:415–451

    Google Scholar 

  • Orsi G, Petrazzuoli S, Wohletz K (1999b) The interplay of mechanical and thermo-fluid dynamical systems during an unrest episode in calderas: the Campi Flegrei caldera (Italy) case. J Volcanol Geotherm Res 91:453–470

    Google Scholar 

  • Orsi G, de Vita S, Di Vito M, Nave R, Heiken G (2003) Facing volcanic and related hazards in the Neapolitan area. In: Heiken G, Fakundiny R, Sutter J (eds) Earth Sciences in the Cities: a reader. AGU, Sp Publ Series, Vol. 56, Washington, DC, pp 121–170

  • Pappalardo L, Civetta L, D’Antonio M, Deino A, Di Vito MA, Orsi G, Carandente A, de Vita S, Isaia R, Piochi M (1999) Chemical and isotopical evolution of the Phlegraean magmatic system before the Campanian Ignimbrite (37 ka) and the Neapolitan Yellow Tuff (12 ka) eruptions. J Volcanol Geotherm Res 91:141–166

    Google Scholar 

  • Pappalardo L, Civetta L, De Vita S, Di Vito MA, Orsi G, Carandente A, Fisher RV (2002a) Timing of magma extraction during the Campanian Ignimbrite eruption (Campi Flegrei caldera). J Volcanol Geotherm Res 114:479–497

    Google Scholar 

  • Pappalardo L, Piochi M, D’Antonio M, Civetta L, Petrini R (2002b) Evidence for multi-stage magmatic evolution during the past 60 ka at Campi Flegrei (Italy) deduced from Sr, Nd and Pb isotope data. J Petrol 43(8):1415–1434

    Article  CAS  Google Scholar 

  • Parascandola A (1947) I fenomeni bradisismici del Serapeo di Pozzuoli. Genovesi Napoli

  • Pareschi MT, Cavarra L, Favalli M, Giannini F, Meriggi A (2000) Gis and volcanic risk management. Nat Hazards 21:361–379

    Article  Google Scholar 

  • Pomonis A, Spence R, Baxter P (1999) Risk assessment of residential buildings for an eruption of Furnas Volcano, Sao Miguel, The Azores. J Volcanol Geotherm Res 92:107–131

    CAS  Google Scholar 

  • Rosi M, Vezzoli L, Aleotti P, De Cenzi M (1996) Interaction between caldera collapse and eruptive dynamics during the Campanian Ignimbrite eruption, Phlegraean Fields, Italy. Bull Volcanol 57:541–554

    Article  Google Scholar 

  • Rosi M, Vezzoli L, Castelmenzano A, Grieco G (1999) Plinian pumice fall deposit of the Campanian Ignimbrite eruption (Phlegraean Fields, Italy). J Volcanol Geotherm Res 91:179–198

    Article  CAS  Google Scholar 

  • Scarpati C, Cole P, Perrotta A (1993) The Neapolitan Yellow Tuff—A large volume mutiphase eruption from Campi Flegrei, Southern Italy. Bull Volcanol 55:343–356

    Google Scholar 

  • Sparks RSJ (2003) Forecasting volcanic eruptions. Earth Planet Sci Lett 210:1–15

    Article  CAS  Google Scholar 

  • Spence RJS, Pomonis A, Baxter PJ, Coburn AW, White M, Dayrit M, Field Epidemiology Training Program Team (1996) Building damage caused by the Mount Pinatubo eruption of June 15, 1991. In: Newall CG, Punongbayan RS (eds) Fire and Mud: eruptions and lahars of Mount Pinatubo, Philippines. Philippine Institute of Volcanology and Seismology, University of Washington Press, Seattle, pp 1055–1061

  • Walker GPL (1984) Characteristics of dune-bedded pyroclastic surge bedsets. J Volcanol Geotherm Res 87:117–140

    Google Scholar 

  • Wohletz K, Orsi G, de Vita S (1995) Eruptive mechanisms of the Neapolitan Yellow Tuff interpreted from stratigraphic, chemical and granulometric data. J Volcanol Geotherm Res 67:263–290

    CAS  Google Scholar 

  • Wohletz K, Civetta L, Orsi G (1999) Thermal evolution of the Phlegraean magmatic system. J Volcanol Geotherm Res 91:381–414

    Article  CAS  Google Scholar 

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Acknowledgements

We acknowledge L. Civetta for constructive discussions and review of the manuscript, P. De Simone for the geo-technical analyses and interpretation of the results, and F. Dell’Erba for the enthusiastic help given during field work. The Soprintendenza Archeologica di Napoli e Caserta is thanked for allowing us to visit archaeological excavations, and in particular A. Marzocchella, D. Gianpaola and E. Laforgia for fruitful discussions on both volcanological and archaeological implications on the excavations exposures. The authors are indebted to E. Bellucci Sessa for generously elaborating the pyroclastic dispersion and load maps by Arcinfo, and to V. Augusti and F. Sansivero for preparation of the illustrations. This manuscript benefited greatly from detailed reviews and useful suggestions by S. Sparks and C. Newhall. The research has been carried out within the 2000–2003 Framework Program of the Gruppo Nazionale per la Vulcanologia with the financial support of the Italian Department for Civil Defence.

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  1. Osservatorio Vesuviano, Via Diocleziano 328, 80124 , Napoli, Italy

    Giovanni Orsi, Mauro Antonio Di Vito & Roberto Isaia

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  1. Giovanni Orsi
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  2. Mauro Antonio Di Vito
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  3. Roberto Isaia
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Correspondence to Giovanni Orsi.

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Orsi, G., Di Vito, M.A. & Isaia, R. Volcanic hazard assessment at the restless Campi Flegrei caldera. Bull Volcanol 66, 514–530 (2004). https://doi.org/10.1007/s00445-003-0336-4

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