The magmatic web beneath Hawai 'i

JD Wilding, W Zhu, ZE Ross, JM Jackson - Science, 2023 - science.org
The deep magmatic architecture of the Hawaiian volcanic system is central to understanding
the transport of magma from the upper mantle to the individual volcanoes. We leverage …

Seismicity under a dormant volcano: unveiling active crustal faulting beneath Piton des Neiges, La Réunion

L Firode, Z Duputel, V Ferrazzini… - Bulletin of the …, 2024 - pubs.geoscienceworld.org
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 …

[HTML][HTML] Unusually high SO2 emissions and plume height from Piton de la Fournaise volcano during the April 2020 eruption

C Hayer, M Burton, V Ferrazzini, B Esse… - Bulletin of Volcanology, 2023 - Springer
Piton de la Fournaise volcano, La Réunion, France, erupted between the 2 and 6 April 2020,
one of a series of eruptive phases which occur typically two or three times per year. Here, we …

The 1965 Mahavel Landslide (Réunion Island, Indian Ocean): Morphology, volumes, flow dynamics, and causes of a rock avalanche in tropical setting

L Michon, E Gayer, A Lucas, F Bellin… - Journal of …, 2023 - Wiley Online Library
In May 1965, a main landslide occurred in a deeply incised valley of Piton de la Fournaise
volcano, in Réunion Island. This event occurred one day after heavy rainfalls and was …

[HTML][HTML] Explosive volcanism of Piton des Neiges (Reunion Island) and excess age dispersion in sanidine: Insights into magma chamber processes in a hotspot …

MPC Melendez, A Di Muro, O Laurent, K Kuiper… - Chemical …, 2023 - Elsevier
Explosive eruptions of trachytic to trachyandesitic composition produced thick and
widespread pyroclastic deposits during the recent volcanic activity of Piton des Neiges …

Is stress modeling able to forecast intrusions and slip events at Piton de la Fournaise volcano?

Q Dumont, V Cayol, JL Froger - Earth and Planetary Science Letters, 2024 - Elsevier
Widespread evidence indicates that the stress field and the presence of major
discontinuities control the magma trajectory and the stability of volcanic edifices. These latter …

Comparison of continuously recorded seismic wavefields in tectonic and volcanic environments based on the network covariance matrix

A Barajas, C Journeau, K Obara… - Journal of Geophysical …, 2023 - Wiley Online Library
Extended and sufficiently dense seismic networks capture spatiotemporal properties of the
continuously recorded wavefields and can be used to compute the level of their coherence …

Pre‐eruptive damage, weakening and magma‐edifice coupling at Piton de la Fournaise volcano

JL Got, A Peltier, D Marsan, V Ferrazzini… - Journal of …, 2024 - Wiley Online Library
Eruptions in basaltic volcanoes are often preceded by increasing seismicity and surface
deformation, which progressively damage and weaken the volcanic edifice. We show how …

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, FJ Fontaine, A Peltier, JL Got… - Journal of Volcanology …, 2022 - Elsevier
Identifying the causes of flank destabilization of active volcanic edifices is key to prevent
catastrophic events. The persistent seismicity recorded below the eastern flank of Piton de la …

Network-based analysis of seismo-volcanic tremors

NM Shapiro, J Soubestre… - IAVCEI Book Modern …, 2023 - insu.hal.science
Volcanic tremors represent one of the most important class of seismo-volcanic signals due to
their abundant presence in seismic records, their wealth of information regarding magmatic …