Articles | Volume 21, issue 8
https://doi.org/10.5194/nhess-21-2355-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/nhess-21-2355-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
09 Aug 2021
Research article |
| 09 Aug 2021
| 09 Aug 2021
Lava flow hazard map of Piton de la Fournaise volcano
Magdalena Oryaëlle Chevrel
CORRESPONDING AUTHOR
Laboratoire Magmas et Volcans (LMV), Université Clermont Auvergne, CNRS, IRD, OPGC, 63000 Clermont-Ferrand, France
Massimiliano Favalli
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Via Battisti, 53, 56125 Pisa, Italy
Nicolas Villeneuve
Institut de Physique du Globe de Paris (IPGP), Université de Paris, CNRS, 75005 Paris, France
Laboratoire Géosciences Réunion (LGSR), Université de La Réunion, 97744 Saint-Denis, France
Observatoire Volcanologique du Piton de la Fournaise (OVPF), Institut de Physique du Globe de Paris, 97418 La Plaine des Cafres, France
Andrew J. L. Harris
Laboratoire Magmas et Volcans (LMV), Université Clermont Auvergne, CNRS, IRD, OPGC, 63000 Clermont-Ferrand, France
Alessandro Fornaciai
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Via Battisti, 53, 56125 Pisa, Italy
Nicole Richter
Institut de Physique du Globe de Paris (IPGP), Université de Paris, CNRS, 75005 Paris, France
Observatoire Volcanologique du Piton de la Fournaise (OVPF), Institut de Physique du Globe de Paris, 97418 La Plaine des Cafres, France
Helmholtz Centre Potsdam, German Research Centre for Geosciences
(GFZ), Telegrafenberg, 14473 Potsdam, Germany
Allan Derrien
Institut de Physique du Globe de Paris (IPGP), Université de Paris, CNRS, 75005 Paris, France
Observatoire Volcanologique du Piton de la Fournaise (OVPF), Institut de Physique du Globe de Paris, 97418 La Plaine des Cafres, France
Patrice Boissier
Institut de Physique du Globe de Paris (IPGP), Université de Paris, CNRS, 75005 Paris, France
Observatoire Volcanologique du Piton de la Fournaise (OVPF), Institut de Physique du Globe de Paris, 97418 La Plaine des Cafres, France
Andrea Di Muro
Institut de Physique du Globe de Paris (IPGP), Université de Paris, CNRS, 75005 Paris, France
Observatoire Volcanologique du Piton de la Fournaise (OVPF), Institut de Physique du Globe de Paris, 97418 La Plaine des Cafres, France
Aline Peltier
Institut de Physique du Globe de Paris (IPGP), Université de Paris, CNRS, 75005 Paris, France
Observatoire Volcanologique du Piton de la Fournaise (OVPF), Institut de Physique du Globe de Paris, 97418 La Plaine des Cafres, France
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Cited
18 citations as recorded by crossref.
- Tracking changes in magma transport from very-long-period seismic signals at Piton de la Fournaise volcano Z. Duputel et al. 10.1016/j.epsl.2023.118323
- Is stress modeling able to forecast intrusions and slip events at Piton de la Fournaise volcano? Q. Dumont et al. 10.1016/j.epsl.2023.118494
- Towards scientific forecasting of magmatic eruptions V. Acocella et al. 10.1038/s43017-023-00492-z
- Lava Volume from Remote Sensing Data: Comparisons with Reverse Petrological Approaches for Two Types of Effusive Eruption P. Verdurme et al. 10.3390/rs14020323
- Lava flow hazard modeling during the 2021 Fagradalsfjall eruption, Iceland: applications of MrLavaLoba G. Pedersen et al. 10.5194/nhess-23-3147-2023
- The effects of digital elevation model resolution on the PyFLOWGO thermorheological lava flow model I. Flynn et al. 10.1016/j.envsoft.2023.105768
- Communication when it is needed most—the past, present and future of volcano geoheritage J. Stix & G. Heiken 10.1007/s00445-022-01574-4
- Toward Next‐Generation Lava Flow Forecasting: Development of a Fast, Physics‐Based Lava Propagation Model D. Hyman et al. 10.1029/2022JB024998
- Benchmarking a new 2.5D shallow water model for lava flows E. Biagioli et al. 10.1016/j.jvolgeores.2023.107935
- Attempt to Model Lava Flow Faster Than Real Time: An Example of La Palma Using VolcFlow M. Marquez et al. 10.3390/geohazards3040027
- Tracking changes in the co-eruptive seismic tremor associated with magma degassing at Piton de la Fournaise volcano C. Journeau et al. 10.1016/j.jvolgeores.2023.107936
- High temperature spectral emissivity of glass and crystal-bearing basalts J. Biren et al. 10.1016/j.jvolgeores.2022.107623
- Vents opening susceptibility map of the Colli Albani long dormant volcano M. Bisson et al. 10.1080/19475705.2023.2215905
- Rapid provision of maps and volcanological parameters: quantification of the 2021 Etna volcano lava flows through the integration of multiple remote sensing techniques C. Proietti et al. 10.1007/s00445-023-01673-w
- Reappraisal of gap analysis for effusive crises at Piton de la Fournaise A. Peltier et al. 10.1186/s13617-021-00111-w
- An Experimental Model of Unconfined Bubbly Lava Flows: Importance of Localized Bubble Distribution A. Namiki et al. 10.1029/2022JB024139
- Volcano‐Magnetic Signal Reveals Rapid Evolution of the Inner Structure of Piton de la Fournaise L. Gailler et al. 10.1029/2022JB025290
- What causes the persistent seismicity below the eastern flank of Piton de la Fournaise (la Réunion Island)? Elasto-plastic models of magma inflation M. Gerbault et al. 10.1016/j.jvolgeores.2022.107628
18 citations as recorded by crossref.
- Tracking changes in magma transport from very-long-period seismic signals at Piton de la Fournaise volcano Z. Duputel et al. 10.1016/j.epsl.2023.118323
- Is stress modeling able to forecast intrusions and slip events at Piton de la Fournaise volcano? Q. Dumont et al. 10.1016/j.epsl.2023.118494
- Towards scientific forecasting of magmatic eruptions V. Acocella et al. 10.1038/s43017-023-00492-z
- Lava Volume from Remote Sensing Data: Comparisons with Reverse Petrological Approaches for Two Types of Effusive Eruption P. Verdurme et al. 10.3390/rs14020323
- Lava flow hazard modeling during the 2021 Fagradalsfjall eruption, Iceland: applications of MrLavaLoba G. Pedersen et al. 10.5194/nhess-23-3147-2023
- The effects of digital elevation model resolution on the PyFLOWGO thermorheological lava flow model I. Flynn et al. 10.1016/j.envsoft.2023.105768
- Communication when it is needed most—the past, present and future of volcano geoheritage J. Stix & G. Heiken 10.1007/s00445-022-01574-4
- Toward Next‐Generation Lava Flow Forecasting: Development of a Fast, Physics‐Based Lava Propagation Model D. Hyman et al. 10.1029/2022JB024998
- Benchmarking a new 2.5D shallow water model for lava flows E. Biagioli et al. 10.1016/j.jvolgeores.2023.107935
- Attempt to Model Lava Flow Faster Than Real Time: An Example of La Palma Using VolcFlow M. Marquez et al. 10.3390/geohazards3040027
- Tracking changes in the co-eruptive seismic tremor associated with magma degassing at Piton de la Fournaise volcano C. Journeau et al. 10.1016/j.jvolgeores.2023.107936
- High temperature spectral emissivity of glass and crystal-bearing basalts J. Biren et al. 10.1016/j.jvolgeores.2022.107623
- Vents opening susceptibility map of the Colli Albani long dormant volcano M. Bisson et al. 10.1080/19475705.2023.2215905
- Rapid provision of maps and volcanological parameters: quantification of the 2021 Etna volcano lava flows through the integration of multiple remote sensing techniques C. Proietti et al. 10.1007/s00445-023-01673-w
- Reappraisal of gap analysis for effusive crises at Piton de la Fournaise A. Peltier et al. 10.1186/s13617-021-00111-w
- An Experimental Model of Unconfined Bubbly Lava Flows: Importance of Localized Bubble Distribution A. Namiki et al. 10.1029/2022JB024139
- Volcano‐Magnetic Signal Reveals Rapid Evolution of the Inner Structure of Piton de la Fournaise L. Gailler et al. 10.1029/2022JB025290
- What causes the persistent seismicity below the eastern flank of Piton de la Fournaise (la Réunion Island)? Elasto-plastic models of magma inflation M. Gerbault et al. 10.1016/j.jvolgeores.2022.107628
Latest update: 26 Apr 2024
Short summary
At Piton de la Fournaise, eruptions are typically fissure-fed and form extensive lava flow fields. Most historical events have occurred inside an uninhabited caldera, but rarely has lava flowed where population and infrastructure might be at risk. We present an up-to-date lava flow hazard map to visualize the probability of inundation by a lava flow per unit area that is an essential tool for hazard mitigation and guiding crises response management.
At Piton de la Fournaise, eruptions are typically fissure-fed and form extensive lava flow...
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