• Responsable d’équipe : Valérie Cayol.

    Responsable-adjoint : Karim Kelfoun.

    Notre équipe est l’une des plus importantes en volcanologie sur le plan international. Elle compte environ 45  personnes, dont environ 26 chercheurs et enseignants-chercheurs permanents, et une vingtaine de doctorants et post-doctorants.Nous abordons une large gamme de thématiques et de méthodes, depuis le transport et les conditions de stockage des magmas dans la croûte jusqu’à la dynamique interne des volcans et les processus éruptifs en surface, et leurs implications en terme de risques volcaniques. Notre approche consiste à coupler les observations et mesures (terrain et télédétection par satellite), aux expérimentations en laboratoire et modélisations numériques.Outre les collaborations avec de nombreux observatoires sur volcans actifs, nous portons un effort particulier sur les volcans des pays partenaires de l’IRD (Chili, Equateur, Indonésie, Pérou, Vanuatu).

    • Axes de recherche :
    Transport et stockage de magmas dans la croûte (flux et échelles de temps, formation des réservoirs)
    Processus physiques et structure interne des édifices (systèmes magmatiques et hydrothermaux, instabilités de flancs par des études géophysiques)
    Processus dans les conduits et les panaches (fragmentation, styles éruptifs, suivi et caractérisation par télédétection, dégazage magmatique)
    Écoulements volcaniques (modélisation des coulées de lave, écoulements pyroclastiques, avalanches de débris, tsunamis, lahars, et aléas associés)
    Évolution des édifices volcaniques (évolution pétro-géochimique, structurale et géomorphologique)

     

    • Collaborations sur le site de Clermont : LaMP (Laboratoire de Météorologie Physique), LPC (Laboratoire de Physique Corpusculaire), LM (Laboratoire de Mathèmatiques), LIMOS (Laboratoire Informatique, Modélisation et Optimisation des Systèmes), MSH (Maison des Sciences de l’Homme), CERDI (Centre d’Etude et de Recherches sur le Développement International).


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  • Liste du personnel

    51 personnes trouvées

    Aguilar Rigoberto
    Bani Philipson
    Battaglia Jean
    Bernard Karine
    Bonilauri Emmie
    Boudoire Guillaume
    Buvat Solène
    Carrara Alexandre
    Cayol Valérie
    Chevrel Oryaëlle
    Ciolczyk Damien
    Colavita Micaela
    Dabaghi Farshid
    Donnadieu Franck
    Druitt Tim
    Eychenne Julia
    Freret-Lorgeril Valentin
    Gailler Lydie
    Galarraga-Ortiz Michael
    Gouhier Mathieu
    Guillard Romain
    Gurioli Lucia
    Harris Andrew
    Haruel Christy
    Jessop David
    Jubertie Remy
    Kelfoun Karim
    Klein Amelie
    Labazuy Philippe
    Lacombe Tristan
    Lénat Jean-François
    Menand Thierry
    Merciecca Charley
    Merle Olivier
    Metcalfe Abigail
    Michaud-Dubuy Audrey
    Moune Séverine
    Pailot-Bonnetat Sophie
    Paris Raphaël
    Penlou Baptiste
    POUGET Manon
    Rafflin Victoria
    Roche Olivier
    Scholtes Luc
    Thouret Jean-Claude
    Tomasek Inès
    Vaerewyck Céline
    Van Wyk De Vries Benjamin
    Vasconez Freddy
    Verdurme Pauline
    Vernet Gérard

    Équipe Volcanologie en Juillet 2019

    L’équipe volcanologie est composée de 26 permanents (9 enseignants chercheurs, 8 physiciens, 4 CNRS, 3 IRD, 1 INRAP, 1 PRAG), 2 émérites, 2 post-doctorants et 14 doctorants.

  • La plateforme de Volcanologie regroupe des appareils de mesures géophysiques (DGPS, tomographie par résistivité, polarisation spontanée, sondages électromagnétiques, ERT, GPR, stations sismiques), les instruments permettant la caractérisation texturale des produits volcaniques (morpho-granulomètre G3, pycnomètres, et perméamètre du laboratoire d’analyse texturale), le laboratoire de volcanologie expérimentale , des logiciels maison de simulation numérique et des outils de télédétection satellitaire et sol (radars doppler, DOAS, MultiGas, caméras IR, drones et laboratoire de traitement d’image). A noter qu’une partie de ces instruments relèvent des services d’observation de l’OPGC.

    Géophysique
    Laboratoire d’analyse texturale
    Laboratoire de volcanologie expérimentale
    Modélisation numérique
    Télédétection

     

  • Rang A :

    575 publication(s) trouvée(s).
    1. Aubry T.J., Engwell S.L., Bonadonna C., Mastin L.G., Carazzo G., Van Eaton A.R., Jessop D., Grainger R.G., Scollo S., Taylor I.A., Jellinek A.M., Schmidt A., Biass S., Gouhier M. (2023). New Insights Into the Relationship Between Mass Eruption Rate and Volcanic Column Height Based On the IVESPA Data Set. Geophysical Research Letters vol.50, - DOI:10.1029/2022GL102633 - lien HAL .
    2. Bablon M., Nauret F., Saillard M., Samaniego P., Vlastélic I., Hidalgo S., Le Pennec J.L., Ratzov G., Michaud F., Mothes P., Liorzou C., Gannoun A.M. (2023). An innovative isotopic method to identify the volcanic source of distal tephra. Earth and Planetary Science Letters vol.619, p.118283, - DOI:10.1016/j.epsl.2023.118283 - lien HAL .
    3. Brand B.D., Pollock N., Vallance J.W., Esposti Ongaro T., Roche O., Trolese M., Giordano G., Marshall A.A., Criswell C.W. (2023). Advances in our understanding of pyroclastic current behavior from the 1980 eruption sequence of Mount St. Helens volcano (Washington), USA. Bulletin of Volcanology vol.85, - DOI:10.1007/s00445-022-01617-w.
    4. Charbonnier S.J., Kelfoun K., Widiwijayanti C., Sri Sayudi D., Putra R. (2023). Assessing the Pyroclastic Density 16 : Current Hazards at Merapi: From Field Data to Numerical Simulations and Hazard Maps. Merapi Volcano, Active Volcanoes of the World. R. Gertisser et al. (eds.), - DOI:10.1007/978-3-031-15040-1_16.
    5. Chevrel O., Harris A. (2023). Monitoring Lava Flows. Modern Volcano Monitoring edited by: Zack Spica and Corentin Caudron ; Book series Advances in Volcanology, - lien HAL .
    6. Chevrel O., Latchimy T., Batier L., Delpoux R., Harris M., Kolzenburg S. (2023). A new portable field rotational viscometer for high-temperature melts. Review of Scientific Instruments vol.94, p.105116, - DOI:10.1063/5.0160247.
    7. Chevrel O., Latchimy T., Batier L., Delpoux R., Harris M., Kolzenburg S. (2023). A new portable field rotational viscometer for high-temperature melts. Review of Scientific Instruments vol.94, p.105116, - DOI:10.1063/5.0160247.
    8. Chevrel O., Villeneuve N., Grandin R., Froger J.L., Coppola D., Massimetti F., Campus A., Hrysiewicz A., Peltier A. (2023). Report : lava flow daily monitoring of the 19 September–05 October 2022 eruption at Piton de la Fournaise. Volcanica - DOI:10.30909/vol.06.02.391404.
    9. Daigle H., Duarte J.C., Fagereng A., Paris R., Persaud P., Gómez-García A.M. (2023). MagellanPlus Workshop: mission-specific platform approaches to assessing natural hazards that impact society. A définir vol.32, p.101-111, - DOI:10.5194/sd-32-101-2023.
    10. Eldursi K., Scholtes L., Conin M., Golfier F., Ledru P., Mercadier J., Collon P., Chemillac R. (2023). 3-D hydromechanical simulation of intersecting faults: Influences on fluid circulation and formation of oriented-orebodies. Journal of Structural Geology vol.171, p.104864, - DOI:10.1016/j.jsg.2023.104864.
    11. Flynn I.T.W, Chevrel O., Crown D.A., Ramsey M.S. (2023). The effects of digital elevation model resolution on the PyFLOWGO thermorheological lava flow model. Environmental Modelling & Software - DOI:10.1016/j.envsoft.2023.105768 - lien HAL .
    12. Flynn I.T.W., Chevrel O., Ramsey M.S. (2023). Adaptation of a Thermorheological Lava Flow Model for Venus Conditions. Journal of Geophysical Research - Planets vol.128, - DOI:10.1029/2022JE007710 - lien HAL .
    13. Galas A., Lewinska P., Aguilar R., Nowak L. (2023). Remote sensing data applied to the reconstruction of volcanic activity in the Valley of the Volcanoes, Central Volcanic Zone, Peru. Journal of Geodynamics vol.156, p.101972, - DOI:10.1016/j.jog.2023.101972.
    14. Giannoulis M., Harris A., Barra V. (2023). DITAN: A deep-learning domain agnostic framework for detection and interpretation of temporally-based multivariate Anomalies. A définir vol.143, p.109814, - DOI:10.1016/j.patcog.2023.109814.
    15. Guéhenneux Y., Charbonnier S., Roche O. (2023). PyroCLAST: a new experimental framework to investigate overspilling of channelized, concentrated pyroclastic currents. Bulletin of Volcanology vol.85, 5, - DOI:10.1007/s00445-022-01623-y - lien HAL .
    16. Habakaramo Macumu P., Boudoire G., Calabrese S., Rufino F., Coyte R.M., Tedesco D. (2023). Impacts of volcanic hazards on rural communities and adaptative strategies: A case study of the Virunga Volcanic Province (Democratic Republic of Congo). International Journal of Disaster Risk Reduction vol.86, p.103566, - DOI:10.1016/j.ijdrr.2023.103566 - lien HAL .
    17. Hamon C., Pereira G., Chevrel O., Aubry L., Siebe C., Quesada O., Reyes-Guzmán N. (2023). Present Use and Production of Metates and Molcajetes in Turícuaro (Michoacán, Mexico): Deciphering the Evolution of Food Preparation Practices. Ethnoarchaeology - DOI:10.1080/19442890.2023.2280379.
    18. Harris A., Latutrie B., Van Wyk De Vries B., Saubin E., Foucher M., Gurioli L., Zanella E., Médard E., Nauret F. (2023). Emplacement of monogenetic lava flows on eroded terrain, Part II: The case of the Arti`ere valley (Grave Noire, France). Journal of Volcanology and Geothermal Research vol.438, p.107812, - DOI:10.1016/j.jvolgeores.2023.107812.
    19. Heap M.J., Wadsworth F.B., Jessop D. (2023). The thermal conductivity of unlithified granular volcanic materials: The influence of hydrothermal alteration and degree of water saturation. Journal of Volcanology and Geothermal Research vol.435, p.107775, - DOI:10.1016/j.jvolgeores.2023.107775.
    20. Inostroza M., Moune S., Moretti R., Burckel P., Chilin-Eusebe E., Dessert C., Robert C., Gorge C. (2023). Major and trace element emission rates in hydrothermal plumes in a tropical environment. The case of La Soufrière de Guadeloupe volcano. Chemical Geology vol.632, p.121552, - DOI:10.1016/j.chemgeo.2023.121552.
    21. Jiao L., Tapponnier P., Donzé F.V., Scholtes L., Gaudemer Y., Xu X. (2023). Discrete Element Modeling of Southeast Asia's 3D Lithospheric Deformation During the Indian Collision. Journal of Geophysical Research - Solid Earth vol.128, - DOI:10.1029/2022JB025578.
    22. Latutrie B., Harris A., Van Wyk De Vries B., Gurioli L., Médard E. (2023). Emplacement of lava flows on eroded terrain, part I: The case of the Tiretaine valley (Chaîne des Puys, France). Journal of Volcanology and Geothermal Research vol.438, p.107808, - DOI:10.1016/j.jvolgeores.2023.107808.
    23. Merle O., Aumar C., Labazuy P., Merciecca C., Buvat S. (2023). Structuration tertiaire et quaternaire du Plateau des Dômes (Chaîne des Puys, Massif central, France)Tertiary and Quaternary structural evolution of the Plateau des Dômes (Chaîne des Puys, Massif central, France). Géologie de la France vol.1, p.1-22.
    24. Merle O., Boivin P., Langlois E., de Larouzière F.-D., Michelin Y., Olive. C. (2023). Review - The UNESCO World Heritage Site of the Chaîne des Puys–Limagne Fault Tectonic Arena (Auvergne, France). Geosciences vol.13, p.198, - DOI:10.3390/geosciences13070198 - lien HAL .
    25. Metcalfe A, Moune S., Komorowski J.C., Robertson R., Christopher T.E., Joseph E.P., Moretti R. (2023). Earth-Science Reviews Diverse Magma Storage and Major and Volatile Magma Composition: What are the implications on the Eruptive Style Across a Volcanic Arc? An Example of the Lesser Antilles Arc. Earth Sciences Reviews vol.241, p.104440, - DOI:10.1016/j.earscirev.2023.104440.
    26. Metcalfe A., Moune S., Komorowski J.C., Robertson R., Christopher T.E., Joseph E.P., Moretti R. (2023). Diverse magma storage and major and volatile magma composition: What are the implications on the eruptive style across a volcanic arc? An example of the Lesser Antilles Arc. Earth Sciences Reviews vol.241, p.104440, - DOI:10.1016/j.earscirev.2023.104440.
    27. Metcalfe A., Moune S., Moretti R., Komorowski J.C., Aubry T.J. (2023). Volatile emissions from past eruptions at La Soufrière de Guadeloupe (Lesser Antilles): insights into degassing processes and atmospheric impacts. Frontiers in Earth Science vol.11, p.1143325, - DOI:10.3389/feart.2023.1143325.
    28. Michaud-Dubuy A., Carazzo G., Balcone-Boissard H., Boudon G., Kaminski E. (2023). Unsuspected explosive activity of Montagne Pelée (Lesser Antilles) during the 25–10 ka period. Journal of Volcanology and Geothermal Research vol.107873, - DOI:10.1016/j.jvolgeores.2023.107873 - lien HAL .
    29. Mostafa A., Scholtes L., Golfier F. (2023). Pore-scale hydro-mechanical modeling of gas transport in coal matrix. Fuel vol.345, p.128165, - DOI:10.1016/j.fuel.2023.128165.
    30. Paris R., Pelletier B., Roger J., Wassmer P., Sabatier P. (2023). Sedimentary evidence of tsunamis in New Caledonia, southwest Pacific. Marine Geology vol.463, p.107116, - DOI:10.1016/j.margeo.2023.107116.
    31. Penlou B., Roche O., Manga M., Van den Wildenberg S. (2023). Experimental Measurement of Enhanced and Hindered Particle Settling in Turbulent Gas-Particle Suspensions, and Geophysical Implications. Journal of Geophysical Research - Solid Earth vol.128, p.e2022JB025809, - DOI:10.1029/2022JB025809 - lien HAL .
    32. Polo-Sánchez A., Flaherty T., Hervé G., Druitt T., Fabbro G., Nomikou P., Balcone-Boissard H. (2023). Tracking timescales of magma reservoir recharge through caldera cycles at Santorini (Greece). Emphasis on an explosive eruption of Kameni Volcano. Frontiers in Earth Science vol.11, - DOI:1I 10.3389/feart.2023.1128083 - lien HAL .
    33. RAVE BONILA Y., Jessop D., Moune S., Garbin C., Moretti R. (2023). Numerical modelling of the volcanic plume dispersion from the hydrothermal system of La Soufrière de Guadeloupe. Volcanica vol.6, p.459-477, 2, - DOI:10.30909/vol.06.02.459477 - lien HAL .
    34. Reyes-Guzmán N., Siebe C., Chevrel O., Pereira G., Mahgoub A.N., Böhnel H. (2023). Holocene volcanic eruptions of the Malpaís de Zacapu and its pre-Hispanic settlement history. Ancient Mesoamerica - DOI:10.1017/S095653612100050X.
    35. Rizza U., Donnadieu F., Morichett M., Avolio E., Castorina G., Semprebello A., Magazu S., Passerin G., Mancinelli E., Biensan C. (2023). Airspace Contamination by Volcanic Ash from Sequences of Etna Paroxysms: Coupling the WRF-Chem Dispersion Model with Near-Source L-Band Radar Observations. Remote Sensing vol.15, p.376, - DOI:10.3390/rs15153760 - lien HAL .
    36. Sampietro D., Capponi M., Thebault E., Gailler L. (2023). Author Correction: An enhanced view on the Mediterranean Sea crust from potential fields data. Scientific Reports vol.13, - DOI:10.1038/s41598-023-37289-5.
    37. Santamarí S., Quidelleur X., Samaniego P., Qaudin L., Le Pennec J.L., Hidalgo S., Liorzou C., Guillou H. (2023). Timing of Quaternary volcanism and its relationship with tectonics in the central segment of the Ecuadorian Andes. Journal of Geophysical Research - Solid Earth vol.442, p.107895, - DOI:10.1016/j.jvolgeores.2023.107895.
    38. Sepulveda J.P., Cioni R., Aravena A. (2023). Morphology-based characterization of intermediate to silicic lava flows: Application to the Central Andean Volcanic Zone. Earth Sciences Reviews vol.241, p.104433, - DOI:10.1016/j.earscirev.2023.104433.
    39. Thivet S., Hess K.U., Dingwell D.B., Berthod C., Gurioli L., Di Muro A., Lacombe T., Komorowski J.C. (2023). Volatiles of the active Mayotte volcanic chain: STA & EGA-MS analysis of volcanic products. Chemical Geology vol.618, p.121297, - DOI:10.1016/j.chemgeo.2022.121297.
    40. Thouret J.C., Aisyah N., Jenkins S.F., de Bélizal E., Sulistiyani, Charbonnier S.J., Sri Sayudi D., Nandaka I.G.M.A., Mainsant G., Solikhin A. (2023). Merapi’s Lahars: Characteristics, 17 :Behaviour, Monitoring, Impact, Hazard Modelling and Risk Assessment. Merapi Volcano, Active Volcanoes of the World. R. Gertisser et al. (eds.), Springer, - DOI:10.1007/978-3-031-15040-1_17.
    41. Thouret J.C., Taillandier M., Arapa E., Wavelet E. (2023). Vulnerable settlements to debris flows in Arequipa, Peru: population characteristics, hazard knowledge, risk perception, and disaster risk management. Natural Hazards - DOI:10.1007/s11069-023-06167-8.
    42. Thouret J.C., Taillandier M., wavelet E., Azzaoui N., Santoni O., Tjahjono B. (2023). Semeru volcano, Indonesia: measuring hazard, exposure and response of densely populated neighbourhoods facing persistent volcanic threats. Natural Hazards 10.1007/s11069-023-05910-5, - DOI:10.1007/s11069-023-05910-5.
    43. Verdurme P., Le Losq C., Chevrel O., Pannefieu S., Médard E., Berthod C., Komorowski J.C., Bachèlery P., Neuville D.R., Gurioli L. (2023). Viscosity of crystal-free silicate melts from the active submarine volcanic chain of Mayotte. Chemical Geology vol.620, - DOI:10.1016/j.chemgeo.2023.121326 - lien HAL .
    44. Şen E., Aydar E., Şen P., Gourgaud A. (2023). Insight into a rift volcanism with the petrogenesis of ultramafic enclaves and the host basalts: Kula Volcanic Field, Western Anatolia, Turkey. Italian Journal of Geosciences vol.142, p.291-315, 2, - DOI:10.3301/IJG.2023.16.
    45. Aravena A., Bevilacqua A., de’ Michieli Vitturi M., Esposti Ongaro T., Neri A., Cioni R. (2022). Calibration strategies of PDC kinetic energy models and their application to the construction of hazard maps. Bulletin of Volcanology vol.84, 29, - DOI:10.1007/s00445-022-01538-8 - lien HAL .
    46. Aravena A., Roche O. (2022). Influence of the topography of stratovolcanoes on the propagation and channelization of1 dense pyroclastic density currents analyzed through numerical simulations. Bulletin of Volcanology vol.84, 7, - DOI:10.1007/s00445-022-01576-2 - lien HAL .
    47. Arghavani S., Arghavani C., Banson S., Lupascu A., Gouhier M., Sellegri K., Planche C. (2022). The Effect of Using a New Parameterization of Nucleation in the WRF-Chem Model on New Particle Formation in a Passive Volcanic Plum. Atmosphere vol.13, p.15, - DOI:10.3390/atmos13010015.
    48. Aumar C., Merle O., Bosse V., Monié P. (2022). Syn-rift Cretaceous deformation in the Agly Variscan Massif (Eastern Pyrenees, France). BSGF - Earth Sciences Bulletin vol.193, 6, - DOI:10.1051/bsgf/2022006.
    49. Bablon M., Ratzov G., Nauret F., Samaniego P., Michaud F., Saillard M., Proust J.N., Le Pennec J.L., Collot J.Y., Devidal J.L., Orange F., Liorzou C., Migeon S., Vallejo S., Hidalgo S., Mothes P., Gonzalez M. (2022). Holocene marine tephra offshore Ecuador and Southern Colombia: First trench‐to‐arc correlations and implication for magnitude of major eruptions. Geochemistry, Geophysics, Geosystems vol.23, p.e2022GC010466, 9, - DOI:10.1029/2022GC010466 - lien HAL .
    50. Bani P., Oppenheimer C., Tsanev V., Scaillet B., Primulyana S., Boyson Saing U., Alfianti H., Marlia M. (2022). Modest volcanic SO 2 emissions from the Indonesian archipelago. Nature Communications vol.13, p.3366, - DOI:10.1038/s41467-022-31043-7.
    51. Bennett G., Van Reybroucka J., Shemsanga C., Kisaka M., Tomasek I., Fontijn K., Kervyn M., WalraevensK. (2022). Identification of low fluoride areas using conceptual groundwater flow model and 1 hydrogeochemical system analysis in the aquifer system on the flanks of an active 2 volcano: Mount Meru, Northern Tanzania. Science of the Total Environment - DOI:10.1016/j.scitotenv.2021.152682 - lien HAL .
    52. Bernard K., Van Wyk De Vries B., Samaniego P., Valderrama P., Marino J. (2022). Collisional interactions and the transition between lava dome sector collapse and pyroclastic density currents at Tutupaca volcano (Southern Peru). Journal of Volcanology and Geothermal Research vol.431, p.107668, - DOI:10.1016/j.jvolgeores.2022.107668.
    53. Bevilacqua A., Aravena A., Aspinall W., Costa A., Mahony S., Neri A., Sparks S., Hill B. (2022). Assessing minimum pyroclastic density current mass to impact critical infrastructures: example from Aso caldera (Japan). Natural Hazard and Earth System Sciences vol.22, p.3329-3348, - DOI:10.5194/nhess-22-3329-2022 - lien HAL .
    54. Bodart O., Cayol V., Dabaghi F., Koko J. (2022). An inverse problem in an elastic domain with a crack : a fictitious domain approach. Computational Geosciences - DOI:10.1007/s10596-021-10121-7 - lien HAL .
    55. Cayol V., Peltier A., Froger J.L., Beauducel F. (2022). Monitoring of Volcano deformation. p.95-153, Hazards and Monitoring of Volcanic Activity, Volume 2, Sismology, deformation and remote sensing, ISTE Science Publishing LTD.
    56. Cayol V., Peltier A., Froger J.L., Beauducel F. (2022). Surveillance de la déformation des volcans. p.103-176, Aléas et surveillance de l’activité volcanique, Volume 2, Sismologie, deformation and télédétection, ISTE Science Publishing LTD.
    57. Constantinescu R., White J.T., Connor C.B., Hopulele-Gligo A., Charbonnier S., Thouret J.C., Lindsay J.M., Bertin D. (2022). Uncertainty Quantification of Eruption Source Parameters Estimated From Tephra Fall Deposits. Geophysical Research Letters vol.49, p.e2021GL097425, - DOI:10.1029/2021GL097425.
    58. Donnadieu F., Jessop D., Bani P., Moune S. (2022). Volcano Remote Sensing with Ground-based Techniques. p.211-289, Hazards and Monitoring of Volcanic Activity 2 - Seismology, Deformation and Remote Sensing, Lénat Jean-François (ed.), ISTE/WILEY.
    59. Doronzo D.M., Di Vito M.A., Arienzo I., Bini M., Galusi B., Cerminara M., Corradini S., de Vita S., Giaccio B., Gurioli L., Mannella G., Ricciardi G.P., Rucco I., Sparice D., Todesco M., Trasatti E., Zanchetta G. (2022). The 79 CE eruption of Vesuvius: A lesson from the past and the need of a multidisciplinary approach for developments in volcanology. Earth Sciences Reviews vol.231, p.104072, - DOI:10.1016/j.earscirev.2022.104072.
    60. Dumont Q., Cayol V., Froger J.L., Peltier A. (2022). 22 years of satellite imagery reveal a major destabilization structure at Piton de la Fournaise. Nature Communications vol.13, p.2649, - DOI:10.1038/s41467-022-30109-w - lien HAL .
    61. Eychenne J., Engwell S. (2022). The grainsize of volcanic fall deposits: Spatial trends and physical controls. GSA Bulletin - DOI:10.1130/B36275.1 - lien HAL .
    62. Eychenne J., Gurioli L., Damby D., Belville C., Schiavi F., Marceau G., Szczepaniaks C., Blavignacs C., Laumonier M., Gardes E., Le Pennec J.L., Nedelec J.-M., Blanchon L., Sapin V. (2022). Spatial distribution and physicochemical properties of respirable volcanic ash from the 16-17 August 2006 Tungurahua eruption (Ecuador), and alveolar epithelium response in-vitro. GeoHealth - DOI:10.1029/2022GH000680 - lien HAL .
    63. Feignon J., Cluzel N., Schiavi F., Moune S., Roche O., Clavero J., Schiano P., Auxerre M. (2022). High CO2 content in magmas of the explosive andesitic Enco eruption of Mocho‑Choshuenco volcano (Chile). Bulletin of Volcanology vol.84, p.40, - DOI:10.1007/s00445-022-01550-y - lien HAL .
    64. Flaherty T., Druitt T., Francalanci L., Schiano P., Sigmarsson O. (2022). Temporal variations in the diversity of primitive melts supplied to the Santorini silicic magmatic system and links to lithospheric stresses. Contributions to Mineralogy & Petrology vol.177, p.79, 9, - DOI:10.1007/s00410-022-01941-6.
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    547. Grosse P., Euillades P.A., Euillades L.D., Van Wyk De Vries B. (2014). A global database of composite volcano morphometry. Bulletin of Volcanology vol.76, p.784, - DOI:10.1007/s00445-013-0784-4.
    548. Gurioli L., Colo L., Bollasina A.J., Harris A., Whittington A., Ripepe M. (2014). Dynamics of Strombolian explosions: Inferences from field and laboratory studies of erupted bombs from Stromboli volcano. Journal of Geophysical Research: Solid Earth 119, 319–345. - DOI:10.1002/2013JB010355 - lien HAL .
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    550. Kassouk Z., Thouret J.C., Solikhin A., Gupta A., Liew S.C. (2014). Object-oriented classification of very high resolution panchromatic imagery for geologic mapping of an active volcano: Semeru volcano, Indonesia. Geomorphology 221, 18-33. - DOI:10.1016/j.geomorph.2014.04.022.
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    553. Martin H., Moyen J.F., Guitreau M., Blichert-Toft J., Le Pennec J.L. (2014). Why Archaean TTG cannot be generated by MORB melting in subduction zones. Lithos 198-199, 1-13. - DOI:10.1016/j.lithos.2014.02.017.
    554. Moghadam H.S., Ghorbani G., Zaki Khedr M., Fazinia N., Chiaradia M., Eyuboglu Y., Santosh M., Galindo Francisco C., Lopez Martinez M., Gourgaud A., Arai S. (2014). Late Miocene K-rich volcanism in the Eslamieh Peninsula (Saray), NW Iran: implications for geodynamic evolution of the Turkish-Iranian High Plateau. Gondwana Research 26, 1028-1050. - DOI:10.1016/j.gr.2013.09.015.
    555. Ménard G., Moune S., Vlastélic I., Aguilera F., Valade S., Bontemps M., González R. (2014). Gas and aerosol emissions from Lascar volcano (Northern Chile): insights into the origin of gases and their links with the volcanic activity. Journal of Volcanology and Geothermal Research 287, 51-67. - DOI:10.1016/j.jvolgeores.2014.09.004.
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    557. Paris R., Switzer A.D., Belousova M., Belousov A., Ontowirjo B., Whelley P.L., Ulvrova M. (2014). Volcanic tsunami: a review of source mechanisms, past events and hazards in Southeast Asia (Indonesia, Philippines, Papua New Guinea). Natural Hazards 70, 447-470. - DOI:10.1007/s11069-013-0822-8.
    558. Paris R., Wassmer P., Lavigne F., Belousov A., Belousova E., Iskandarsyah Y., Benbakkar M., Ontowirjo B., Mazzoni N. (2014). Coupling eruption and tsunami records: the Krakatau 1883 case study, Indonesia. Bulletin of Volcanology 74, 814. - DOI:10.1007/s00445-014-0814-x.
    559. Remy D., Froger J.L., Perfettini H., Bonvalot S., Gabalda G., Albino F., Cayol V., Legrand D., De Saint Blanquat M. (2014). Persistent uplift of the Lazufre volcanic complex (Central Andes): New insights from PCAIM inversion of InSAR time series and GPS data. Geochemistry Geophysics Geosystems 15. - DOI:10.1002/2014GC005370.
    560. Rivera M., Thouret J.C., Samaniego P., Le Pennec J.L. (2014). The 2006–2009 activity of the Ubinas volcano (Peru): Petrology of the 2006 eruptive products and insights into genesis of andesite magmas, magma recharge and plumbing system. Journal of Volcanology and Geothermal Research 270, 122-114. - DOI:10.1016/j.jvolgeores.2013.11.010.
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    571. Ulvrová M., Paris R., Kelfoun K., Nomikou P. (2014). Numerical simulations of tsunami generated by underwater volcanic explosions at Karymskoye Lake (Kamchatka, Russia) and Kolumbo volcano (Aegean Sea, Greece). Natural Hazards and Earth System Sciences 14, 401-412. - DOI:10.5194/nhess-14-401-2014.
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    575. Varol E., Temel A., Yürür T., Gourgaud A., Bellon H. (2014). Petrogenesis of the Neogene bimodal magmatism of the Galatean Volcanic Province, Central Anatolia, Turkey. Journal of Volcanology and Geothermal Research 280, 14-29. - DOI:10.1016/j.jvolgeores.2014.04.014.
  • Les réponses à ces questions ont été élaborées en réponse à des questions d’élèves et d’étudiants par plusieurs chercheurs du laboratoire, Luca Teray, Raphael Paris, Karim Kelfoun et Valérie Cayol. Si toutefois ces réponses ne répondaient pas à vos questionnements, veuillez vous adresser à Valérie Cayol (valerie.cayol@uca.fr) ou à Karim Kelfoun (karim.kelfoun@uca.fr).

    Questions :

    Réponses :

    Quel est le nom précis de votre métier ?

    Pratiquement, la dénomination de notre métier est chercheur, enseignants chercheur, professeur ou physicien. On peut aussi être doctorant ou post-doctorant, mais ces postes correspondent à des CDD. Notre objet d’étude ce sont les volcans. On est chercheur en volcanologie. On peut aussi dire volcanologue ou vulcanologue bien sûr.

    Ce métier se situe dans quel secteur professionnel ?

    La fonction publique.

    Qui est votre employeur ?

    Les employeurs des chercheurs du Laboratoire Magmas et Volcans sont variés. Ce sont le Centre National de la Recherche Scientifique (CNRS), l’Université Clermont Auvergne (UCA) ou l’Institut de Recherches et Développement (IRD).

    Où se situe votre lieu de travail ?

    Les chercheurs ont des bureaux à l’université mais ils sont aussi amenés à faire des analyses en laboratoire et des campagnes de mesures sur des terrains parfois situés sur d’autres continents. Le laboratoire de recherche auquel nous sommes rattachés est une unité mixte de recherche, ce qui veut dire qu’il associe des chercheurs CNRS et une université. L’IRD est aussi associé au laboratoire.

    Quel est votre rythme de travail ?

    Statutairement les chercheurs travaillent 35 heures par semaines, et ont droit à 9 semaines de vacances. Mais les chercheurs sont en général passionnés par leur métier. C’est aussi un métier compétitif, si bien que les chercheurs ne comptent pas leurs heures. En pratique, les chercheurs travaillant 50 heures par semaine et il n’est pas rare qu’ils prennent moins de 5 semaines de vacances/an.

    Pourquoi avoir choisi ce métier ?

    Parce que c’est un métier qui permet de satisfaire sa curiosité. L’approche est très satisfaisante puisqu’elle consiste généralement à faire des allers retours entre observations de terrain, observations de laboratoire et simulations. En outre, on a une relative liberté dans le choix des domaines de recherches, des approches et des horaires.

    Quelle est la finalité de votre métier ?

    Voir par exemple la vidéo de présentation de l’équipe volcanologie https://lmv.uca.fr/recherche/volcanologie/ .

    Au Laboratoire Magmas et Volcans, nous cherchons à comprendre le volcanisme depuis sa source dans le manteau terrestre jusqu’à l’émission de produits volcaniques dans l’atmosphère. Les questions que l’on se pose sont de savoir pourquoi les volcans entrent en éruption, quels sont les signes précurseurs d’une éruption, quel type d’activité va survenir, comment cette activité évolue, quel est son impact sur les activités humaines (aviation, agriculture, santé, etc.), les plantes, les animaux et le climat. Outre les risques immédiatement liés à l’activité volcanique (coulées de lave, coulées de boues, coulées pyroclastiques, explosions, bombes volcaniques et cendres, tsunamis), les volcans rejettent des gaz à effet de serre (CO2), des gaz acides (SO2) et des cendres ayant un impact sur le climat et les populations.

    A quels besoin répondez-vous en exerçant ce métier ?

    A un besoin de compréhension du monde qui nous entoure . Certaines de nos recherches permettent aussi de mieux évaluer les risques associés au volcanisme. Nous participons également à la transmission des savoirs à la société via les enseignements à l’université et nos échanges avec les médias (journaux, télévision, radio, cinéma, festivals).

    Pouvez-vous décrire concrètement les activités que vous faites souvent, pour que je me représente votre quotidien au travail ?

    Pour mener à bien nos recherches nous combinons les observations sur le terrain (avec des appareils de mesures in situ ou à distance, avec des drones ou des satellites), les observations de laboratoire (analyse physico-chimique des produits volcaniques, expériences physiques), et les modèles qu’ils soient effectués par des dispositifs de laboratoire ou sur des ordinateurs. Le but de ces modèles est de mieux comprendre les processus physiques qui gouvernent les comportements observés. La nature étant complexe, on simplifie les problèmes pour étudier des paramètres particuliers. Mais, comme beaucoup de gens, au quotidien nous passons la plupart de notre temps devant un ordinateur, car il faut non seulement traiter les données mais aussi monter des projets pour obtenir des financements, rédiger des rapports et des publications, préparer des conférences, discuter par mail ou visioconférences avec d’autres collègues, ce à quoi se rajoute un peu de travail administratif.

    Racontez-moi une journée-type au travail

    Les chercheurs passent du temps à encadrer des étudiant, à écrire des projets, à administrer leur recherche et celle des autres, à lire et écrire des articles, préparer des conférences et aussi bien sûr faire leur recherche (analyse de séries de données, analyses en laboratoire, modélisations, etc.).

    Quels sont les autres professionnels avec qui vous travaillez ? (travail seul / en équipe / partenaires…)

    Nous sommes chacun spécialiste d’un domaine bien spécifique (les coulées de lave, les séismes volcaniques, les tsunamis, les gaz, etc.). Pour mieux comprendre le volcanisme et son impact, nous devons travailler avec d’autres chercheurs du laboratoire ayant des spécialités complémentaires, et avec les chercheurs d’autres laboratoires : des mathématiciens, des informaticiens, des physiciens, des médecins, etc. Comme nos études impliquent des observations de volcans, nous collaborons avec des observatoires volcanologiques situés sur le territoire national (à l’île de la Réunion, à la Guadeloupe ou à la Martinique) ou à l’étranger. Nous collaborons aussi parfois avec des professionnels du secteur privé pour des recherches liées aux géomatériaux, à l’hydrologie, à la géothermie ou aux risques naturels.

    Quels sont les qualités indispensables pour réaliser votre métier ?

    Il faut être curieux et passionné, avoir un bon sens physique, et être excellent d’un point de vue académique. Il faut être très autonome et avoir ses propres questionnements, tout en ayant la capacité de travailler en équipe. Il faut aussi savoir communiquer oralement dans des conférences, comme par écrit au travers d’articles qui seront publiés en anglais dans des revues scientifiques. Il est de nos jours nécessaire de parler couramment anglais.

    Présentez-moi les points positifs sur votre métier

    C’est un métier qui nourrit nos questionnements sur le monde qui nous entoure. La possibilité de satisfaire notre curiosité est une grande source de satisfaction pour beaucoup de chercheurs.

    Nous avons une grande liberté : liberté de choisir nos thèmes de recherches dans la mesure où ces thèmes nous permettent d’obtenir des financements, liberté de choisir avec qui on veut travailler, relative liberté d’horaires. Tout ceci est possible à condition de produire des connaissances au travers d’articles publiés dans des revues scientifiques et de communications à des conférences.

    C’est aussi un métier qui permet d’être au carrefour de beaucoup de disciplines scientifiques (géologie, physique, chimie, mathématiques, informatique, géographie, économie, sociologie notamment), ce qui est très enrichissant, et qui donne l’opportunité de voyager et de rencontrer des gens de cultures différentes.

    En plus de leur recherche, les enseignants-chercheurs enseignent également, aussi bien en Licence (les trois premières années d’études après le bac) qu’en Master (quatrième et cinquième années d’étude après le bac). Les chercheurs et enseignants-chercheurs encadrent aussi des doctorants (trois ans de recherche après un Master). Nous sommes ainsi en contact permanent avec les étudiants, à enseigner, à questionner et à être questionnés.

    Présentez-moi les points négatifs sur votre métier

    Il est difficile de fixer des limites à ce que l’on veut et peut faire. On amène souvent du travail chez nous et il est parfois difficile de se « déconnecter » du travail. C’est un métier passion qui a les défauts de ses qualités. Les salaires des chercheurs ne sont pas particulièrement élevés et diffèrent peu selon leur grade et les responsabilités qui leur incombent. Les possibilités de promotion sont limitées. Bref, on ne fait pas ce métier pour l’argent. Par exemple, un chercheur avec dix années d’ancienneté gagne à peine 2500 euros nets par mois.

    Est ce qu’un volcanologue va près des volcans actifs pour les étudier ?

    L’image du volcanologue est, dans l’imaginaire collectif, attachée à celle d’un aventurier en combinaison réfléchissante effectuant des mesures à quelques mètres de la lave en fusion, ou bien descendant dans un cratère fumant ! Cette vision provient en grande partie des documentaires et des ouvrages d’Haroun Tazieff et de Katia et Maurice Kraft qui ont effectués dans la seconde moitié du 20e siècle. Néanmoins, elle ne correspond plus vraiment à la réalité du travail de volcanologue. De nos jours, il est désormais possible de surveiller les volcans à distance, à l’aide de satellites, de drones ou de stations installées sur les volcans qui transmettent leurs mesures à l’autre bout du monde. Les volcanologues ne sont donc plus les baroudeurs des années 70. Beaucoup de chercheurs étudient aussi les volcans en laboratoire ou numériquement, ce qui ne demande pas de se rendre sur le terrain. Cependant, il restera toujours nécessaire d’aller près des volcans actifs pour mieux les comprendre. Parmi les activités du volcanologue d’aujourd’hui sur le terrain qui ne vont pas disparaître de si tôt, on recense notamment:

    • l’installation et la maintenance de stations de mesure (sismomètres, gnss, caméras, analyseurs de gaz, etc…) sur les volcans
    • la récolte d’échantillons (roches, cendres, lave, gaz) que l’on analysera au laboratoire pour mieux comprendre les éruptions récentes comme anciennes
    •  le test de nouvelles techniques de mesure et d’observation en cours de développement au laboratoire et qui seront amenées à faire partie dans le futur de la panoplie des volcanologues (l’exemple le plus emblématique est l’application des drones pour la volcanologie).
    •  la réalisation d’enquête (cartographiques mais aussi géographiques et sociologiques) dans les régions volcaniques pour évaluer la vulnérabilité aux aléas volcaniques et le risque qui en découle

    Notons enfin que certaines de ces activités nécessitent parfois de se rendre dans des zones très actives (coulées de lave, lèvre de cratère, ou encore champ de fumerolles par exemple) même si c’est de plus en plus rare. Ces opérations se font bien entendu après une évaluation extrêmement rigoureuse des risques et avec un équipement spécialement conçu pour se protéger des dangers éventuels.

    Si jamais vous devez aller sur le terrain, quelles sont les premières difficultés que vous rencontrerez lors de ces excursions ?

    Les terrains volcaniques sont très variés, ils peuvent se situer sur tous les continents avec toutes les variétés de régime politique que cela implique, ils peuvent se trouver au niveau de la mer à Hawaii jusqu’à presque 7000m d’altitude dans les Andes (sans parler des volcans sous-marins), il peut faire plus de 40°C dans la région de l’Afar en Ethiopie, comme -20°C sur l’Erebus en Antarctique. Ils peuvent se situer à quelques minutes d’une grande ville (comme par exemple le Vésuve et Naples) comme à des centaines de km de toute zone habitée (certains volcans des îles Aléoutiennes par exemple). Le volcan peut-être inactif comme en éruption. Bref, il faut s’attendre à tout ! C’est pourquoi toutes les missions doivent être soigneusement préparées, tant du point de vue scientifique (programme de travail et plans de secours), naturel (météo, activité) que logistique (logement, transport, alimentation, santé), sans négliger les aspects administratifs (autorisations, douanes) qui peuvent s’avérer décisifs. En résumé, une mission très bien préparée est souvent une mission réussie (quelle que soient les conditions), et le plus difficile est surtout de bien se préparer, ce qui s’apprend par expérience.

    Quel est le diplôme ou la formation nécessaire aujourd’hui pour exercer votre métier ?

    Il faut un doctorat (baccalauréat + 8 années d’études), et en général avoir effectué un ou plusieurs post-doctorats (CDD en recherche), souvent à l’étranger. Il faut avoir un parcours académique exemplaire et avoir montré que l’on menait une recherche autonome amenant à des publications dans des revues internationales réputées. Typiquement, le CNRS recrute 5 chercheurs en sciences de la terre par an pour tout le pays. En 2020, il y a 80 candidats pour ces 5 postes. Les dernier chercheurs recrutés par le CNRS dans l’équipe Volcanologie du Laboratoire Magmas et Volcans l’ont été en 2006 et 2020. En ce qui concerne les autres types de postes, l’équipe Volcanologie a recruté 1 professeur, 2 maîtres de conférence, 2 physiciens et 3 chercheurs rattachés à l’IRD sur les dix dernières années. C’est donc un métier très compétitif. La compétition continue encore pour obtenir des financements permettant de mener à bien nos projets (environ 10 % des projets déposés à l’Agence Nationale de la Recherche sont subventionnés). Pour faire face à cette compétition, et persévérer malgré les difficultés qui se peuvent se présenter, il faut une solide motivation.

  •  

    Nos volcans cibles

    La compréhension du volcanisme nécessite l’acquisition de données de terrain : imagerie visible et thermique, campagnes géophysiques, prélèvements de gaz, de roches et de cendres pour analyses pétrologiques et géochimiques, cartographie des dépôts et des destructions, etc

    Nos cibles dépendent de l’activité en cours, des thématiques de recherches et de nos collaborations avec les laboratoires et observatoires français et des pays partenaires.

    La Soufrière de Guadeloupe
    Le Piton de la Fournaise
    Les volcans italiens
    Les volcans indonésiens
    Le volcanisme andin
    Les volcans africains

     

  • Prochaines réunions :

    Jeudi 20 février 2023 15h00
    Jeudi 16 mars 2023 15h00
    Jeudi 27 avril 2023 15h00
    Lundi 15 mai 2023 annulée
    Mercredi 21 juin 15h00
    Lundi 24 juillet Annulée
    Jeudi 7 septembre 2023 14h30
    Lundi 9 octobre 2023 16h00
    Jeudi 16 novembre 2023 14h00
    Lundi 11 décembre 2023 14h00
    Jeudi 18 janvier 14h00
    Lundi 12 février 14h00
    Jeudi 14 mars 14h00
    Lundi 15 avril 14h00
    Jeudi 16 mai 14h00
    Lundi 17 juin 14h00
    Jeudi 18 juillet 14h00
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