The magmatic web beneath Hawai 'i
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 …
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 …
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
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 …
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
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 …
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 …
Explosive eruptions of trachytic to trachyandesitic composition produced thick and
widespread pyroclastic deposits during the recent volcanic activity of Piton des Neiges …
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?
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 …
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 …
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
Eruptions in basaltic volcanoes are often preceded by increasing seismicity and surface
deformation, which progressively damage and weaken the volcanic edifice. We show how …
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
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 …
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 …
their abundant presence in seismic records, their wealth of information regarding magmatic …