[HTML][HTML] Self-potential as a tool to assess groundwater flow in hydrothermal systems: A review
In hydrothermal systems associated with volcanic areas, the flow of groundwater generates
an electrical current of electrokinetic nature, the so-called streaming current. This current is …
an electrical current of electrokinetic nature, the so-called streaming current. This current is …
Near-surface geophysical characterization of areas prone to natural hazards: a review of the current and perspective on the future
Natural hazards such as landslides, floods, rockfalls, earthquakes, volcanic eruptions,
sinkholes, and snow avalanches represent potential risks to our infrastructures, properties …
sinkholes, and snow avalanches represent potential risks to our infrastructures, properties …
Alteration‐induced volcano instability at la Soufrière de Guadeloupe (eastern Caribbean)
MJ Heap, TS Baumann… - Journal of …, 2021 - Wiley Online Library
Volcanoes are unstable structures that deform laterally and frequently experience mass
wasting events. Hydrothermal alteration is often invoked as a mechanism that contributes …
wasting events. Hydrothermal alteration is often invoked as a mechanism that contributes …
[HTML][HTML] Volcano electrical tomography unveils edifice collapse hazard linked to hydrothermal system structure and dynamics
M Rosas-Carbajal, JC Komorowski, F Nicollin… - Scientific reports, 2016 - nature.com
Catastrophic collapses of the flanks of stratovolcanoes constitute a major hazard threatening
numerous lives in many countries. Although many such collapses occurred following the …
numerous lives in many countries. Although many such collapses occurred following the …
The 2018 unrest phase at La Soufrière of Guadeloupe (French West Indies) andesitic volcano: Scrutiny of a failed but prodromal phreatic eruption
After 25 years of gradual increase, volcanic unrest at La Soufrière of Guadeloupe reached
its highest seismic energy level on 27 April 2018, with the largest felt volcano-tectonic (VT) …
its highest seismic energy level on 27 April 2018, with the largest felt volcano-tectonic (VT) …
The hydrothermal alteration of cooling lava domes
Hydrothermal alteration is a recognized cause of volcanic instability and edifice collapse,
including that of lava domes or dome complexes. Alteration by percolating fluids transforms …
including that of lava domes or dome complexes. Alteration by percolating fluids transforms …
[HTML][HTML] Modelling pyroclastic density currents from a subplinian eruption at La Soufrière de Guadeloupe (West Indies, France)
T Esposti Ongaro, JC Komorowski, Y Legendre… - Bulletin of …, 2020 - Springer
We have used a three-dimensional, non-equilibrium multiphase flow numerical model to
simulate subplinian eruption scenarios at La Soufrière de Guadeloupe (Lesser Antilles …
simulate subplinian eruption scenarios at La Soufrière de Guadeloupe (Lesser Antilles …
[HTML][HTML] Deep Electrical Resistivity Tomography for a 3D picture of the most active sector of Campi Flegrei caldera
The central sector of the Campi Flegrei volcano, including the Solfatara maar and Pisciarelli
fumarole field, is currently the most active area of the caldera as regards seismicity and …
fumarole field, is currently the most active area of the caldera as regards seismicity and …
[HTML][HTML] Modeling of partial dome collapse of La Soufrière of Guadeloupe volcano: implications for hazard assessment and monitoring
M Peruzzetto, JC Komorowski, A Le Friant… - Scientific Reports, 2019 - nature.com
Abstract Over the past 9,150 years, at least 9 flank collapses have been identified in the
history of La Soufrière of Guadeloupe volcano. On account of the volcano's current unrest …
history of La Soufrière of Guadeloupe volcano. On account of the volcano's current unrest …
The monitoring of natural soil CO2 emissions: Issues and perspectives
Natural soil CO 2 emissions constitute a substantial portion of the carbon emitted in the
atmosphere, particularly in volcano-tectonic areas where deep CO 2 supply is also present …
atmosphere, particularly in volcano-tectonic areas where deep CO 2 supply is also present …