Abstract
Major volcanic hazards in the Lesser Antilles arc include powerful Plinian explosive eruptions that inject ash high into the atmosphere and produce dangerous pyroclastic density currents (PDC) on the ground. Understanding the key physical processes governing the dynamics and stability of past volcanic columns is a fundamental problem in volcanology as well as being central to assessing specific hazards in this region and elsewhere. However, the number of cases for which the transition of regime between a stable and collapsing eruptive plume is described in detail remains too small to constrain fully theoretical models of volcanic plumes. Here we present a detailed reconstruction of the time evolution of the P2 AD 280 eruption at Mt. Pelée volcano in Martinique, to expand the database available to test physical models. The P2 sequence, which forced the first inhabitants to flee to other islands for decades as suggested by archaeological evidence, starts with a basal ash layer interpreted as the result of an initial violent laterally directed explosion to the NE of the volcano. Most of the deposit sequence is made of a pumice fall deposit interbedded with a low-concentration PDC deposit interpreted as the result of a partial column collapse. The upper pumice fall unit shows an inverse gradation and is overlain by a final high-concentration PDC deposit or locally by the correlative low-concentration PDC deposit. Field data on deposit dispersal, thickness, and grain-size distribution are used together with physical models to reconstruct the dynamic evolution of this eruption. Empirical models of deposit thinning suggest that the minimum volume of pyroclastic deposits is 0.67–0.88 km3 dense rock equivalent (DRE), much larger than the 0.17 km3 DRE previously estimated. We find that the mass eruption rate increased from 6 × 107 to 1.1 × 108 kg s−1, producing an initially stable 23- to 26-km-high Plinian plume, which ultimately collapsed to form a fountain. We discuss the mechanisms leading to column collapse based on published data on magmatic water contents and our estimates of grain-size distributions and mass discharge rates. The eruption started close to the plume/fountain transition and the volcanic column ultimately collapsed mainly due to an increase in mass discharge rate. This marginally stable evolution was also inferred from analysis of the P1 AD 1300 eruption deposits, suggesting consistent behavior during the recent Plinian eruptions of Mt. Pelée volcano. In these two eruptions, the transition occurred at conditions well predicted by our theoretical model of volcanic plumes.
Similar content being viewed by others
References
Alibidirov M, Dingwell DB (1996) Magma fragmentation by rapid decompression. Nature 380:146–148
Arsandaux H (1929) L’éruption actuelle de la Montagne Pelée. Bull Volcanol 3:25–32
Arsandaux H (1934) L’éruption de la Montagne Pelée en 1929. Rev Scientifique 72:248–251
Bardintzeff JM, Miskovsky JC, Traineau H, Westercamp D (1989) The recent pumice eruptions of Mt. Pelée, Martinique. Part II: grain-size studies and modelling the last Plinian phase P1. J Volcan Geotherm Res 38:35–48
Bérard B (2007) The “South-Dominica” archaeological mission: the Soufrière site. In: XXII Conference of the International Association of Caribbean Archaeology, Jul. 2007, Kingston, Jamaica
Bérard B, Vernet G, Kieffer G, Raynal J-P (2001) Les éruptions volcaniques de la Montagne Pelée et le premier peuplement de la Martinique. XIXème Congrès international d’Archéologie de la Caraïbe, In, pp 70–87
Bernard M-L, Zamora M, Géraud Y, Boudon G (2007) Transport properties of pyroclastic rocks from Montagne Pelée volcano (Martinique, Lesser Antilles). J Geophys Res 112:B05205
Bonadonna C, Costa A (2012) Estimating the volume of tephra deposits: a new simple strategy. Geology 40(5):415–418
Bonadonna C, Costa A (2013) Plume height, volume, and classification of explosive volcanic eruptions based on the Weibull function. Bull Volcanol 75:742–761
Bonadonna C, Houghton BF (2005) Total grain-size distribution and volume of tephra fall deposits. Bull Volcanol 67:441–456
Boudon G (1993) La montagne Pelée, Martinique: evolution volcanologique. Societé géologique de France, Paris
Boudon G, Lajoie J (1989) The 1902 Pelean deposits in the Fort Cemetery of St. Pierre, Martinique: a model for the accumulation of turbulent nuées ardentes. J Volcan Geoth Res 38:113–130
Boudon G, Le Friant A, Villemant B, Viode J-P (2005) Martinique. In: Lindsay JM, Robertson REA, Shepherd JB, Ali S (eds) Volcanic hazard atlas of the Lesser Antilles. Seismic Research Unit, The University of the West Indies, Trinidad and Tobago, pp 126–145
Boudon G, Villemant B, Le Friant A, Paterne M, Cortijo E (2013) Role of large flank-collapse events on magma evolution of volcanoes. Insights from the Lesser Antilles Arc. J Volcan Geotherm Res 263:224–237
Bourdier J-L, Gourgaud A, Vincent PM (1985) Magma mixing in a main stage of formation of Montagne Pelée: the Saint Vincent-type scoria flow sequence (Martinique, F.W.I.). J Volcan Geotherm Res 25:309–332
Bourdier JL, Boudon G, Gourgaud A (1989) Stratigraphy of the 1902 and 1929 nuée-ardente deposits, Mt. Pelée, Martinique. J Volcan Geotherm Res 38:77–96
Brunet M, Le Friant A, Boudon G, Lafuerza S, Talling P, Hornbach M, Ishizuka O, Lebas E, Guyard H, IODP Expedition 340 science Party (2016) Composition, geometry, and emplacement dynamics of a large volcanic island landslide offshore Martinique: from volcano flank-collapse to seafloor sediment failure? Geochem Geophys Geosyst 17(3):699–724
Bursik MI, Woods AW (1996) The dynamics and thermodynamics of large ash flows. Bull Volcanol 58:175–193
Calder ES, Cole PD, Dade WB, Druitt TH, Hoblitt RP, Huppert HE, Ritchie L, Sparks RSJ, Young SR (1999) Mobility of pyroclastic flows and surges at the Soufriere Hills Volcano, Montserrat. Geophys Res Lett 26:537–540
Carazzo G, Kaminski E, Tait S (2008a) On the dynamics of volcanic columns: a comparison of field data with a new model of negatively buoyant jets. J Volcanol Geoth Res 178:94–103. https://doi.org/10.1016/j.jvolgeores.2008.01.002
Carazzo G, Kaminski E, Tait S (2008b) On the rise of turbulent plumes: quantitative effects of variable entrainment for submarine hydrothermal vents, terrestrial and extra terrestrial explosive volcanism. J Geophys Res 113:B09201. https://doi.org/10.1029/2007JB00548
Carazzo G, Tait S, Kaminski E, Gardner JE (2012) The recent Plinian explosive activity of Mt. Pelée volcano (Lesser Antilles): the P1 AD 1300 eruption. Bull Volcanol 74:2187–2203
Carey S, Sigurdsson H (1987) Temporal variations in column height and magma discharge rate during the 79 AD eruption of Vesuvius. Geol Soc Am Bull 99:303–314
Carey S, Sigurdsson H (1989) The intensity of Plinian eruptions. Bull Volcanol 51:28–40
Carey S, Sparks RSJ (1986) Quantitative models of the fallout and dispersal of tephra from volcanic eruption columns. Bull Volcanol 48:109–125
Carey S, Sigurdsson H, Gardner JE, Criswell W (1990) Variations in column height and magma discharge during the May 18, 1980 eruption of Mount St. Helens. J Volcanol Geoth Res 43:99–112
Costa A, Suzuki YJ, Cerminara M, Devenish BJ, Esposito Ongaro T, Herzog M, Van Eaton AR, Denby LC, Bursik M, de' Michieli Vitturi M, Engwell S, Barsotti S, Folch A, Macedonio G, Girault F, Carazzo G, Tait S, Kaminski E, Mastin LG, Woodhouse MJ, Phillips JC, Hogg AJ, Degruyter W, Bonadonna C (2016) Results of the eruptive column model inter-comparison study. J Volcanol Geotherm Res 326:2–25
Dade WB, Huppert HE (1998) Long runout rockfalls. Geology 26:803–806
Daggit ML, Mather TA, Pyle DM, Page S (2014) AshCalc—a new tool for the comparison of the exponential, power-law and Weibull models of tephra deposition. J Appl Volcanol 3:7
Davidson J, Wilson M (2012) Differentiation and source processes at Mt Pelée and the Quill; active volcanoes in the Lesser Antilles arc. J Petrol 52(7–8):1493–1531
Doyle EE, Hogg AJ, Mader HM, Sparks RSJ (2010) A two-layer model for the evolution and propagation of dense and dilute regions of pyroclastic currents. J Volcanol Geotherm Res 190:365–378
Dupuy C, Dostal J, Traineau H (1985) Geochemistry of volcanic rocks from Mt. Pelée, Martinique. J Volcanol Geotherm Res 26:147–165
Fierstein J, Nathenson M (1992) Another look at the calculation of fallout tephra volumes. Bull Volcanol 54(2):156–167
Fisher RV, Smith AL, Roobol MJ (1980) Destruction of St. Pierre, Martinique, by ash-cloud surges, May 8 and 20, 1902. Geology 8:472–476
Genevey A, Gallet Y, Boudon G (2002) Secular variation study from non-welded pyroclastic deposits from Montagne Pelée volcano, Martinique (West Indies). Earth Planet Sci Lett 201:369–382
Germa A, Quidelleur X, Labanieh S, Chauvel C, Lahitte P (2011) The volcanic evolution of Martinique Island: insights from K-Ar dating into the Lesser Antilles arc migration since the Oligocene. J Volcan Geotherm Res 208:122–135
Germa A, Lahitte P, Quidelleur X (2015) Construction and destruction of Mont Pelée volcano: volumes and rates constrained from a geomorphological model of evolution. J Geophys Res Earth Surf 120:1206–1226
Girault F, Carazzo G, Tait S, Ferrucci F, Kaminski E (2014) The effect of total grain-size distribution on the dynamics of turbulent volcanic plumes. Earth Plan Sci Lett 394:124–134
Girault F, Carazzo G, Tait S, Kaminski E (2016) Combined effects of total grain-size distribution and crosswind on the rise of eruptive volcanic columns. J Volcanol Geotherm Res 326:103–113
Hartmann WK (1969) Terrestrial lunar and interplanetary rock fragmentation. Icarus 10:201–213
Kaminski E, Jaupart C (1998) The size distribution of pyroclasts and the fragmentation sequence in explosive volcanic eruptions. J Geophys Res 103:29,759–29,779
Komorowski JC, Legendre Y, Caron B, Boudon G (2008) Reconstruction and analysis of sub-plinian tephra dispersal during the 1530 AD Soufriere (Guadeloupe) eruption: implications for scenario definition and hazards assessment. J Volcanol Geotherm Res 178:491–515
Koyaguchi T, Ohno M (2001) Reconstruction of eruption column dynamics on the basis of grain size of tephra fall deposits 1. Methods. J Geophys Res 106:6499–6512
Koyaguchi T, Suzuki YJ, Kozono T (2010) Effects of the crater on eruption column dynamics. J Geophys Res 115:B07205
Kueppers U, Perugini D, Dingwell DB (2006) “Explosive energy” during volcanic eruptions from fractal analysis of pyroclasts. Earth Planet Sci Lett 248:800–807
Lacroix A (1904) La Montagne Pelée et ses éruptions. Masson, Paris
Lajoie J, Boudon G, Bourdier J-L (1989) Depositional mechanics of the 1902 pyroclastic nuée-ardente deposits of Mt. Pelée, Martinique. J Volcanol Geotherm Res 38:131–142
Le Friant A, Boudon G, Deplus C, Villemant B (2003) Large-scale flank collapse events during the activity of Montagne Pelée, Martinique, Lesser Antilles. J Geophys Res 108(B1):2055
Lindsay JM, Smith AL, Roobol MJ, Stasiuk MV (2005) Dominica. In: Lindsay JM, Robertson REA, Shepherd JB, Ali S (eds) Volcanic hazard atlas of the Lesser Antilles. Seismic Research Unit, The University of the West Indies, Trinidad and Tobago, pp 1–48
Martel C (2012) Eruption dynamics inferred from microlite crystallization experiments: application to Plinian and dome-forming eruptions of Mt Pelée (Martinique, Lesser Antilles). J Petrol 53(4):699–725
Martel C, Poussineau S (2007) Diversity of eruptive styles inferred from the microlites of Mt. Pelée andesite (Martinique, Lesser Antilles). J Volcanol Geotherm Res 166:233–254
Martel C, Pichavant M, Bourdier J-L, Traineau H, Holtz F, Scaillet B (1998) Magma storage conditions and control of eruption regime in silicic volcanoes: experimental evidence from Mt. Pelée. Earth Planet Sci Lett 156:89–99
Martel C, Bourdier JL, Pichavant M, Traineau H (2000) Textures, water content and degassing of silicic andesites from recent Plinian and dome-forming eruptions at Mt. Pelée volcano (Martinique, Lesser Antilles arc). J Volcanol Geotherm Res 96:191–206
Mattioni M (1976) Les grandes familles de formes du saladoïde insulaire du site de Vivé à la Martinique. Proceedings of the 6th International congress for the study of the pre-Columbian cultures of the Lesser Antilles, pp 11–33
Michaud-Dubuy A, Carazzo G, Kaminski E, Girault F (2018) A revisit of the role of gas entrapment on the stability conditions of explosive volcanic columns. J Volcanol Geotherm Res 357:349–361
Neri A, Dobran F (1994) Influence of eruption parameters on the thermofluid dynamics of collapsing volcanic columns. J Geophys Res 99(B6):11,833–11,857
Newhall CG, Self S (1982) The volcanic explosivity index (VEI): an estimate of explosive magnitude for historical volcanism. J Geophys Res 87:1231–1238
Perret FA (1931a) Le nouveau dôme de la Montagne Pelée. Compt Rend Acad Sci, Paris 193:1342–1344
Perret FA (1931b) Le dôme recent de la Montagne Pelée. Compt Rend Acad Sci, Paris 193:1439–1442
Perret FA (1935) The eruption of Mount Pelée 1929-1932. Carnegie Institution of Washington, Washington, DC, p 125
Perrey A (1853) Note sur les tremblements de terre en 1851. Memoire Académie Sciences, Arts et Belles-Lettres, Dijon 2:1–65
Pyle DM (1989) The thickness, volume and grainsize of tephra fall deposits. Bull Volcanol 51:1–15
Pyle DM (1995) Mass and energy budgets of explosive volcanic eruptions. Geophys Res Lett 22:563–566
Pyle DM (2000) Sizes of volcanic eruptions. In: Sigurdsson H, Houghton B, Reimer H, Stiw J, McNutt S (eds) Encyclopedia of volcanoes. Academic, San Diego, pp 263–269
Quantin P, Balesdent J, Bouleau A, Delaune FC (1991) Premiers stades d’altération de ponces volaniques en climat tropical humide (Montagne Pelée, Martinique). Geoderma 50:125–148
Revert E (1931) La Montagne Pelée et ses dernières éruptions. Ann Geogr 40:275–291
Revert E (1948) Fouilles et sites précolombiens de la Martinique. Etudes rhodaniennes 23:172–176
Rodriguez-Loubet F (1994) Les Antilles, un des derniers peuplements précolombiens de l’Amérique. Bull Soc Préhisto Fr 91:324–332
Romer M (1931) La dernière eruption de la Montagne Pelée. Bull Volcanol 8:89–116
Romer M (1934) L’éruption de la Montagne Pelée (Martinique) de 1929 à 1933. Ann. Phys. Globe France Outre Mer 5:129–147
Roobol MJ, Smith AL (1976) Mount Pelée, Martinique: a pattern of alternating eruptive styles. Geology 4:521–524
Roobol MJ, Smith AL (1980) Pumice eruptions of the Lesser Antilles. Bull Volcanol 43:277–286
Roobol MJ, Smith AL (2004) Volcanology of Saba and St. Eustatius, Northern Lesser Antilles. Koninklijke nederlandse Akademie van wetenschappen
Ruzié L, Moreira M (2010) Magma degassing process during plinian eruptions. J Volcanol Geotherm Res 192:142–150
Saunders NJ (2005) The peoples of the Caribbean: an encyclopedia of Caribbean archaeology and traditional culture. ABC, Santa Barbara
Sigurdsson H, Carey S (1989) Plinian and co-ignimbrite tephra fall from the 1815 eruption of Tambora volcano. Bull Volcanol 51:243–270
Sigurdsson H, Carey S, Fisher RV (1984) The 1982 eruptions of El Chichon volcano, Mexico: stratigraphy of pyroclastic deposits. J Volcanol Geotherm Res 23:11–37
Suzuki YJ, Koyaguchi T, Ogawa M, Hachisu I (2005) A numerical study of turbulent mixing in eruption clouds using a three-dimensional fluid dynamics model. J Geophys Res 110:B08201
Traineau H, Westercamp D, Coulon C (1983) Mélanges magmatiques à la Montagne Pelée (Martinique). Origine des éruptions de type Saint-Vincent. Bull Volcanol 46(3):243–269
Traineau H, Westercamp D, Bardintzeff JM, Miskovsky JC (1989) The recent pumice eruptions of Mt. Pelée volcano, Martinique. Part I: depositional sequences, description of pumiceous deposits. J Volcanol Geotherm Res 38:17–33
Turcotte DL (1986) Fractals and fragmentation. J Geophys Res 91:1921–1926
Valentine GA, Wohletz KH (1989) Numerical models of Plinian eruption columns and pyroclastic flows. J Geophys Res 94:1867–1887
Vidal CM, Komorowski J-C, Métrich N, Pratomo I, Kartadinata N, Prambada O, Michel A, Carazzo G, Lavigne F, Rodysill J, Fontijn K, Surono (2015) Dynamics of the major Plinian eruption of Samala in 1257 AD (Lombok, Indonesia). Bull Volcanol 77:73. https://doi.org/10.1007/s00445-015-0960-9
Villemant B, Boudon G (1998) Transition from dome-forming to plinian eruptive styles controlled by H20 and Cl degassing. Nature 392:65–69
Villemant B, Boudon G (1999) H20 and halogen (F, Cl, Br) behaviour during shallow magma degassing processes. Earth Planet Sci Lett 168:271–286
Villemant B, Boudon G, Komorowski JC (1996) U-series disequilibrium in arc magmas induced by water-magma interaction. Earth Planet Sci Lett 140:259–267
Vincent PM, Bourdier J-L, Boudon G (1989) The primitive volcano of Mount Pelée: its construction and partial destruction by flank collapse. J Volcanol Geotherm Res 38:1–15
Walker GPL (1980) The Taupo pumice: product of the most powerful known (ultraplinian) eruption. J Volcanol Geoth Res 8:69–94
Westercamp D, Traineau H (1983) The past 5,000 years of volcanic activity at Mt. Pelée Martinique (F.W.I.): implications for assessment of volcanic hazards. J Volcanol Geotherm Res 17:159–185
Wilson L (1976) Explosive volcanic eruptions—III. Plinian eruption columns. Geophys J R Astrom Soc 45:543–556
Wilson L, Sparks RSJ, Walker GPL (1980) Explosive volcanic eruptions—IV. The control of magma properties and conduit geometry on eruption column behaviour. Geophys J R Astrom Soc 63:117–148
Woods AW, Bursik MI (1991) Particle fallout, thermal disequilibrium and volcanic plumes. Bull Volcanol 53:559–570
Woods AW, Bower SM (1995) The decompression of volcanic jets in a crater during explosive volcanic eruptions. Earth Plan Sci Lett 131:189–205
Wright JV, Smith AL, Roobol MJ, Mattioli GS, Fryxell JE (2016) Distal ash hurricane (pyroclastic density current) deposits from a ca. 2000 yr B.P. Plinian-style eruption of Mount Pelée, Martinique: distribution, grain-size characteristics, and implications for future hazards. Geol Soc Am Bull 128:777–791
Acknowledgments
The authors warmly thank S. Self, two anonymous reviewers, and the editor, J. Dufek, for their constructive comments. We are very grateful to C. Martel and C. M. Vidal for fruitful discussions on magmatic water contents at Mt. Pelée volcano. We warmly thank G. Delaviel-Anger, A. Fries, and A. Michaud-Dubuy for their hard work in the field and for stimulating discussions. We thank J.E. Gardner, U. Kueppers, and D. Perugini for valuable assistance in the field and for their insightful comments on the P2 stratigraphy and grain-size distributions. We are grateful to our colleagues of the Institut National de Recherches Archéologiques Préventives, A. Jégouzo, A. Bolle, C. Martin, E. Moizan, C. Dunikowski, and O. Dayrens for sharing their field data. We are also indebted to the staff of the Mt. Pelée volcanological observatory (OVSM) for field and administrative assistance. We also thank J.-P. Dumoulin, L. Beck, E. Delque-Kolic, and C. Moreau (LMC14, CNRS UMS2572) who performed the 14C dating. This work was partially funded by the Institut National des Sciences de l’Univers—Centre National de la Recherche Scientifique progam CT3-ALEA, INSU-CNRS Artemis 2016 for 14C dating, CASAVA (ANR contract ANR-09-ANR-RISK-002), and RAVEX (ANR contract ANR-16-CE03-0002). This is IPGP contribution No. 3998.
Author information
Authors and Affiliations
Corresponding author
Additional information
Editorial responsibility: J. Dufek
Rights and permissions
About this article
Cite this article
Carazzo, G., Tait, S. & Kaminski, E. Marginally stable recent Plinian eruptions of Mt. Pelée volcano (Lesser Antilles): the P2 AD 280 eruption. Bull Volcanol 81, 3 (2019). https://doi.org/10.1007/s00445-018-1265-6
Received:
Accepted:
Published:
DOI: https://doi.org/10.1007/s00445-018-1265-6