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Journal articles on the topic 'Piton de la Fournaise'

Author: Grafiati

Published: 4 June 2021

Last updated: 25 July 2025

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1

Richter, Nicole, and Jean-Luc Froger. "The role of Interferometric Synthetic Aperture Radar in Detecting, Mapping, Monitoring, and Modelling the Volcanic Activity of Piton de la Fournaise, La Réunion: A Review." Remote Sensing 12, no. 6 (2020): 1019. http://dx.doi.org/10.3390/rs12061019.

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Synthetic Aperture Radar (SAR) remote sensing plays a significant role in volcano monitoring despite the measurements’ non real-time nature. The technique’s capability of imaging the spatial extent of ground motion has especially helped to shed light on the location, shape, and dynamics of subsurface magmatic storage and transport as well as the overall state of activity of volcanoes worldwide. A variety of different deformation phenomena are observed at exceptionally active and frequently erupting volcanoes, like Piton de la Fournaise on La Réunion Island. Those offer a powerful means of inve

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2

Chen, Yu, Kefei Zhang, Jean-Luc Froger, et al. "Long-Term Subsidence in Lava Fields at Piton de la Fournaise Volcano Measured by InSAR: New Insights for Interpretation of the Eastern Flank Motion." Remote Sensing 10, no. 4 (2018): 597. http://dx.doi.org/10.3390/rs10040597.

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Long-term deformation often occurs in lava fields at volcanoes after flow emplacements. The investigation and interpretation of deformation in lava fields is one of the key factors for the assessment of volcanic hazards. As a typical Hawaiian volcano, Piton de la Fournaise volcano’s (La Réunion Island, France) main eruptive production is lava. Characteristics of the lava flows at Piton de la Fournaise, including the geometric parameters, location, and elevation, have been investigated by previous studies. However, no analysis focusing on the long-term post-emplacement deformation in its lava f

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3

Chevrel, Magdalena Oryaëlle, Nicolas Villeneuve, Raphaël Grandin, et al. "Lava flow daily monitoring: the case of the 19 September–5 October 2022 eruption at Piton de la Fournaise." Volcanica 6, no. 2 (2023): 391–404. http://dx.doi.org/10.30909/vol.06.02.391404.

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Taking prompt and effective actions to mitigate risks associated with an effusive eruption greatly depends on the monitoring of lava flow emplacement. Here we report on the monitoring of the lava flow emplaced during the 19 September to 05 October 2022 eruption at Piton de la Fournaise (La Réunion) that involves an unprecedentedly large data set acquired using multiple techniques and sensors. These include aerial photogrammetry to construct digital surface models and define lava flow geometry during and after emplacement. Complementary use of multiple satellite sensors (visible, infrared, and

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4

Cadet, Jean-Maurice, Hassan Bencherif, Nicolas Cadet, et al. "Solar UV Radiation in the Tropics: Human Exposure at Reunion Island (21° S, 55° E) during Summer Outdoor Activities." International Journal of Environmental Research and Public Health 17, no. 21 (2020): 8105. http://dx.doi.org/10.3390/ijerph17218105.

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Reunion Island is a popular tourist destination with sandy beaches, an active volcano (Piton de la Fournaise), and Piton des Neiges, the highest and most dominant geological feature on the island. Reunion is known to have high levels of solar ultraviolet radiation (UVR) with an ultraviolet index (UVI) which can reach 8 in winter and 16 in summer (climatological conditions). UVR has been linked to skin cancer, melanoma, and eye disease such as cataracts. The World Health Organization (WHO) devised the UVI as a tool for expressing UVR intensity. Thresholds ranging from low (UVI 1–2) to extreme (

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5

Poupin, Joseph, Nicole Crestey, and Jean-Paul Le Guelte. "Cave-dwelling crabs of the genus Karstarma from lava tubes of the volcano 'Piton de la Fournaise', in Réunion Island, with description of a new species and redescription of Karstarma jacksoni (Balss, 1934) from Christmas Island (Decapoda, Brachyura, Sesarmidae)." Zootaxa 4497, no. 3 (2018): 381–97. https://doi.org/10.11646/zootaxa.4497.3.3.

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Poupin, Joseph, Crestey, Nicole, Guelte, Jean-Paul Le (2018): Cave-dwelling crabs of the genus Karstarma from lava tubes of the volcano 'Piton de la Fournaise', in Réunion Island, with description of a new species and redescription of Karstarma jacksoni (Balss, 1934) from Christmas Island (Decapoda, Brachyura, Sesarmidae). Zootaxa 4497 (3): 381-397, DOI: 10.11646/zootaxa.4497.3.3

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6

Toutain, J. P., H. Delorme, G. Robaye, and J. P. Quisefit. "Mineralogy and geochemistry of PITON de la fournaise sublimates." Chemical Geology 70, no. 1-2 (1988): 155. http://dx.doi.org/10.1016/0009-2541(88)90653-5.

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7

Chevrel, Magdalena Oryaëlle, Andrew Harris, Aline Peltier, et al. "Volcanic crisis management supported by near real-time lava flow hazard assessment at Piton de la Fournaise, La Réunion." Volcanica 5, no. 2 (2022): 313–34. http://dx.doi.org/10.30909/vol.05.02.313334.

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Since 1979, Piton de la Fournaise (La Réunion) has erupted on average two times per year, with 95 % of these eruptions occurring within an uninhabited caldera. However, lava flows have occasionally impacted populated regions on the island, as in 1977 and 1986. Since 2014, an integrated satellite data–driven multinational response to effusive crises has been developed to rapidly assess lava inundation area and flow runout distance. In 2018, this protocol was implemented as a standalone software to provide a lava flow hazard map showing the probability of flow coverage and runouts as a function

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8

Chevrel, Magdalena Oryaëlle, Massimiliano Favalli, Nicolas Villeneuve, et al. "Lava flow hazard map of Piton de la Fournaise volcano." Natural Hazards and Earth System Sciences 21, no. 8 (2021): 2355–77. http://dx.doi.org/10.5194/nhess-21-2355-2021.

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Abstract. Piton de la Fournaise, situated on La Réunion island (France), is one of the most active hot spot basaltic shield volcanoes worldwide, experiencing at least two eruptions per year since the establishment of the volcanological observatory in 1979. Eruptions are typically fissure-fed and form extensive lava flow fields. About 95 % of some ∼ 250 historical events (since the first confidently dated eruption in 1708) have occurred inside an uninhabited horseshoe-shaped caldera (hereafter referred to as the Enclos), which is open to the ocean on its eastern side. Rarely (12 times since the

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9

Vlastélic, Ivan, Catherine Deniel, Chantal Bosq, et al. "Pb isotope geochemistry of Piton de la Fournaise historical lavas." Journal of Volcanology and Geothermal Research 184, no. 1-2 (2009): 63–78. http://dx.doi.org/10.1016/j.jvolgeores.2008.08.008.

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10

Lanzafame, Gabriele, Alexander Bolam, Andrea Di Muro, et al. "Geochemistry and Petrology of the Bellecombe Lava Sequence, Enclos Fouqué Caldera, Piton de la Fournaise Volcano (Réunion, France)." Minerals 13, no. 6 (2023): 751. http://dx.doi.org/10.3390/min13060751.

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Piton de la Fournaise is an active shield volcano located in the eastern area of the Réunion Island (Indian Ocean) whose activity is characterized by effusive and explosive episodes with the emission of scarcely differentiated magmas with mostly tholeiitic affinity. The presently active edifice has grown within the Enclos Fouqué caldera, a polylobate plain bounded on its western side by the 80–200 m high Bellecombe vertical cliffs. This escarpment exposes a vertical sequence of 12 lava flows cut by a dike with an age > 5.5 kyrs. In this work, the Bellecombe products were investigated by X-r

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11

Lénat, Jean-François, Patrick Bachèlery, and Olivier Merle. "Anatomy of Piton de la Fournaise volcano (La Réunion, Indian Ocean)." Bulletin of Volcanology 74, no. 9 (2012): 1945–61. http://dx.doi.org/10.1007/s00445-012-0640-y.

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12

Rousset, Dominique, Alain Lesquer, Alain Bonneville, and Jean François Lénat. "Complete gravity study of Piton de la Fournaise volcano, Reunion Island." Journal of Volcanology and Geothermal Research 36, no. 1-3 (1989): 37–52. http://dx.doi.org/10.1016/0377-0273(89)90004-8.

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13

Tulet, Pierre, Andréa Di Muro, Aurélie Colomb, et al. "First results of the Piton de la Fournaise STRAP 2015 experiment: multidisciplinary tracking of a volcanic gas and aerosol plume." Atmospheric Chemistry and Physics 17, no. 8 (2017): 5355–78. http://dx.doi.org/10.5194/acp-17-5355-2017.

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Abstract. The STRAP (Synergie Transdisciplinaire pour Répondre aux Aléas liés aux Panaches volcaniques) campaign was conducted over the entire year of 2015 to investigate the volcanic plumes of Piton de La Fournaise (La Réunion, France). For the first time, measurements at the local (near the vent) and at the regional scales were conducted around the island. The STRAP 2015 campaign has become possible thanks to strong cross-disciplinary collaboration between volcanologists and meteorologists. The main observations during four eruptive periods (85 days) are summarised. They include the estimate

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14

Froger, Jean-Luc, Virginie Pinel, Mary-Grace Bato, et al. "Apport des données SAR à la compréhension et à la surveillance des volcans : exemple du Piton de la Fournaise." Revue Française de Photogrammétrie et de Télédétection, no. 219-220 (January 19, 2020): 83–90. http://dx.doi.org/10.52638/rfpt.2019.470.

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La télédétection s'est révélée au cours des deux dernières décennies comme un outil essentiel à la fois pour améliorer notre connaissance des systèmes volcaniques mais également pour assurer la surveillance des volcans actifs. En utilisant l'exemple du Piton de la Fournaise, le plus actif des volcans français, nous illustrons ici comment les données radar satellitaires (SAR), dont l'utilisation n'est pas empêchée par la présence de nuages, permettent non seulement de cartographier les dépôts éruptifs et d'estimer leur volume mais aussi de mesurer la topographie de l'édifice volcanique (avec un

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15

Simonetto, Elisabeth, Frédéric Durand, Laurent Morel, Jean-Luc Froger, and Joëlle Nicolas. "InSAR tropospheric correction combining GNSS data and a global atmospheric model." Revue Française de Photogrammétrie et de Télédétection, no. 217-218 (September 21, 2018): 3–9. http://dx.doi.org/10.52638/rfpt.2018.414.

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Les mesures issues de l'interférométrie d'images radar (InSAR), notamment satellitales, doivent être corrigées du délai dû à la propagation des ondes dans l'atmosphère. Plusieurs travaux ont déjà montré l'intérêt de cette correction. Cet article présente une méthode d'estimation de la phase troposphérique qui utilise à la fois des mesures GNSS (Global Navigation Satellite System) et un modèle d'atmosphère global (ERA-Interim). Pour évaluer cette méthode, nous comparons alors les mesures de déplacements interférométriques avant et après la correction avec les déplacements mesurés par GNSS, cons

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16

Carter, Adam, Benjamin van Wyk de Vries, Karim Kelfoun, Patrick Bachèlery, and Pierre Briole. "Pits, rifts and slumps: the summit structure of Piton de la Fournaise." Bulletin of Volcanology 69, no. 7 (2006): 741–56. http://dx.doi.org/10.1007/s00445-006-0103-4.

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17

Peltier, Aline, Magdalena Oryaëlle Chevrel, Andrew J. L. Harris, and Nicolas Villeneuve. "Reappraisal of gap analysis for effusive crises at Piton de la Fournaise." Journal of Applied Volcanology 11, no. 1 (2022). http://dx.doi.org/10.1186/s13617-021-00111-w.

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AbstractEffective and rapid effusive crisis response is necessary to mitigate the risks associated with lava flows that could threaten or inundate inhabited or visited areas. At Piton de la Fournaise (La Réunion, France), well-established protocols between Observatoire Volcanologique du Piton de la Fournaise – Institut de Physique du Globe de Paris (OVPF-IPGP) and civil protection, and between scientists of a multinational array of institutes, allow effective tracking of eruptive crises and hazard management embracing all stakeholders. To assess the outstanding needs for such responses Tsang a

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18

Vlastelic, I., P. Bachèlery, O. Sigmarsson, et al. "Prolonged Trachyte Storage and Unusual Remobilization at Piton de la Fournaise, La Réunion Island, Indian Ocean: Li, O, Sr, Nd, Pb and Th Isotope Study." Journal of Petrology 62, no. 7 (2021). http://dx.doi.org/10.1093/petrology/egab048.

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Abstract La Réunion Island includes two major volcanic systems. About 0·5 Myr ago, Piton des Neiges volcano declined, while Piton de la Fournaise volcano grew on its flank. Since then the Piton de la Fournaise shield volcano has produced homogeneous lavas with chemical compositions transitional between alkali and tholeiitic basalts. In April 2007, the volcano emitted a very small volume of trachytic pumice during its largest historical eruption. We conducted a comprehensive petrological and geochemical study of the pumice to understand the occurrence of such silicic melt in the feeding system

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19

Firode, Lise, Zacharie Duputel, Valérie Ferrazzini, and Olivier Lengliné. "Seismicity under a Dormant Volcano: Unveiling Active Crustal Faulting beneath Piton des Neiges, La Réunion." Bulletin of the Seismological Society of America, February 16, 2024. http://dx.doi.org/10.1785/0120230284.

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ABSTRACT Volcanic environments are commonly associated with seismic activity. The two prominent shield volcanoes of La Réunion island—Piton des Neiges and Piton de la Fournaise, exhibit sustained seismic activity. Whereas the seismicity at Piton de la Fournaise is tied to its volcanic activity, the seismic activity beneath Piton des Neiges, which has been dormant for 27,000 yr, remains poorly understood. The occurrence of earthquakes under the north flank of Piton des Neiges, often felt by the population, led to the deployment of several seismic stations in the area since 2012. In this study,

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20

GOT, Jean-Luc. "Data, results and software for the article: PRE-ERUPTIVE DAMAGE, WEAKENING AND MAGMA-EDIFICE COUPLING AT PITON DE LA FOURNAISE VOLCANO." December 15, 2022. https://doi.org/10.5281/zenodo.7442591.

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This file contains the data, results and software for the article: PRE-ERUPTIVE DAMAGE, WEAKENING AND MAGMA-EDIFICE COUPLING AT PITON DE LA FOURNAISE VOLCANO submitted to Journal of Geophysical Research - Solid Earth - version of Dec. 15, 2022.

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21

"Report on Piton de la Fournaise (France)." Bulletin of the Global Volcanism Network 21, no. 12 (1996). http://dx.doi.org/10.5479/si.gvp.bgvn199612-233020.

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22

"Report on Piton de la Fournaise (France)." Bulletin of the Global Volcanism Network 23, no. 2 (1998). http://dx.doi.org/10.5479/si.gvp.bgvn199802-233020.

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23

"Report on Piton de la Fournaise (France)." Bulletin of the Global Volcanism Network 23, no. 3 (1998). http://dx.doi.org/10.5479/si.gvp.bgvn199803-233020.

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24

"Report on Piton de la Fournaise (France)." Bulletin of the Global Volcanism Network 23, no. 6 (1998). http://dx.doi.org/10.5479/si.gvp.bgvn199806-233020.

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25

"Report on Piton de la Fournaise (France)." Bulletin of the Global Volcanism Network 23, no. 7 (1998). http://dx.doi.org/10.5479/si.gvp.bgvn199807-233020.

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26

"Report on Piton de la Fournaise (France)." Bulletin of the Global Volcanism Network 23, no. 9 (1998). http://dx.doi.org/10.5479/si.gvp.bgvn199809-233020.

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27

"Report on Piton de la Fournaise (France)." Bulletin of the Global Volcanism Network 24, no. 7 (1999). http://dx.doi.org/10.5479/si.gvp.bgvn199907-233020.

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28

"Report on Piton de la Fournaise (France)." Bulletin of the Global Volcanism Network 24, no. 9 (1999). http://dx.doi.org/10.5479/si.gvp.bgvn199909-233020.

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29

"Report on Piton de la Fournaise (France)." Bulletin of the Global Volcanism Network 25, no. 1 (2000). http://dx.doi.org/10.5479/si.gvp.bgvn200001-233020.

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30

"Report on Piton de la Fournaise (France)." Bulletin of the Global Volcanism Network 25, no. 7 (2000). http://dx.doi.org/10.5479/si.gvp.bgvn200007-233020.

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31

"Report on Piton de la Fournaise (France)." Bulletin of the Global Volcanism Network 25, no. 12 (2000). http://dx.doi.org/10.5479/si.gvp.bgvn200012-233020.

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32

"Report on Piton de la Fournaise (France)." Bulletin of the Global Volcanism Network 26, no. 5 (2001). http://dx.doi.org/10.5479/si.gvp.bgvn200105-233020.

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33

"Report on Piton de la Fournaise (France)." Bulletin of the Global Volcanism Network 26, no. 7 (2001). http://dx.doi.org/10.5479/si.gvp.bgvn200107-233020.

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34

"Report on Piton de la Fournaise (France)." Bulletin of the Global Volcanism Network 26, no. 12 (2001). http://dx.doi.org/10.5479/si.gvp.bgvn200112-233020.

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35

"Report on Piton de la Fournaise (France)." Bulletin of the Global Volcanism Network 27, no. 11 (2002). http://dx.doi.org/10.5479/si.gvp.bgvn200211-233020.

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36

"Report on Piton de la Fournaise (France)." Bulletin of the Global Volcanism Network 28, no. 2 (2003). http://dx.doi.org/10.5479/si.gvp.bgvn200302-233020.

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37

"Report on Piton de la Fournaise (France)." Bulletin of the Global Volcanism Network 28, no. 5 (2003). http://dx.doi.org/10.5479/si.gvp.bgvn200305-233020.

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38

"Report on Piton de la Fournaise (France)." Bulletin of the Global Volcanism Network 28, no. 6 (2003). http://dx.doi.org/10.5479/si.gvp.bgvn200306-233020.

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39

"Report on Piton de la Fournaise (France)." Bulletin of the Global Volcanism Network 28, no. 8 (2003). http://dx.doi.org/10.5479/si.gvp.bgvn200308-233020.

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40

"Report on Piton de la Fournaise (France)." Bulletin of the Global Volcanism Network 28, no. 9 (2003). http://dx.doi.org/10.5479/si.gvp.bgvn200309-233020.

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41

"Report on Piton de la Fournaise (France)." Bulletin of the Global Volcanism Network 29, no. 3 (2004). http://dx.doi.org/10.5479/si.gvp.bgvn200403-233020.

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42

"Report on Piton de la Fournaise (France)." Bulletin of the Global Volcanism Network 29, no. 5 (2004). http://dx.doi.org/10.5479/si.gvp.bgvn200405-233020.

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43

"Report on Piton de la Fournaise (France)." Bulletin of the Global Volcanism Network 29, no. 12 (2004). http://dx.doi.org/10.5479/si.gvp.bgvn200412-233020.

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44

"Report on Piton de la Fournaise (France)." Bulletin of the Global Volcanism Network 30, no. 11 (2005). http://dx.doi.org/10.5479/si.gvp.bgvn200511-233020.

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45

"Report on Piton de la Fournaise (France)." Bulletin of the Global Volcanism Network 31, no. 6 (2006). http://dx.doi.org/10.5479/si.gvp.bgvn200606-233020.

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46

"Report on Piton de la Fournaise (France)." Bulletin of the Global Volcanism Network 32, no. 1 (2007). http://dx.doi.org/10.5479/si.gvp.bgvn200701-233020.

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47

"Report on Piton de la Fournaise (France)." Bulletin of the Global Volcanism Network 32, no. 12 (2007). http://dx.doi.org/10.5479/si.gvp.bgvn200712-233020.

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48

"Report on Piton de la Fournaise (France)." Bulletin of the Global Volcanism Network 34, no. 2 (2009). http://dx.doi.org/10.5479/si.gvp.bgvn200902-233020.

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49

"Report on Piton de la Fournaise (France)." Bulletin of the Global Volcanism Network 35, no. 3 (2010). http://dx.doi.org/10.5479/si.gvp.bgvn201003-233020.

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50

"Report on Piton de la Fournaise (France)." Bulletin of the Global Volcanism Network 37, no. 3 (2012). http://dx.doi.org/10.5479/si.gvp.bgvn201203-233020.

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