Spatial and temporal quantification of subaerial volcanism from 1980 to 2019: solid products, masses, and average eruptive rates
Volcanism is one of the main mechanisms transferring mass and energy between the
interior of the Earth and the Earth's surface. However, the global mass flux of lava, volcanic …
interior of the Earth and the Earth's surface. However, the global mass flux of lava, volcanic …
[HTML][HTML] The Independent Volcanic Eruption Source Parameter Archive (IVESPA, version 1.0): A new observational database to support explosive eruptive column …
Eruptive column models are powerful tools for investigating the transport of volcanic gas and
ash, reconstructing past explosive eruptions, and simulating future hazards. However, the …
ash, reconstructing past explosive eruptions, and simulating future hazards. However, the …
Hazard assessment and monitoring of Ecuadorian volcanoes: challenges and progresses during four decades since IG-EPN foundation
Abstract The Instituto Geofísico (IG-EPN) was created in 1983 by faculty of the Escuela
Politécnica Nacional, a public university in Quito, Ecuador, with the objective of assessing …
Politécnica Nacional, a public university in Quito, Ecuador, with the objective of assessing …
Brittle‐ductile deformation and tensile rupture of dome lava during inflation at Santiaguito, Guatemala
Gas‐and‐ash explosions at the Santiaguito dome complex, Guatemala, commonly occur
through arcuate fractures, following a 5‐to 6‐min period of inflation observed in long‐period …
through arcuate fractures, following a 5‐to 6‐min period of inflation observed in long‐period …
[HTML][HTML] Adapting to changes in volcanic behaviour: Formal and informal interactions for enhanced risk management at Tungurahua Volcano, Ecuador
This paper provides an example of how communities can adapt to extreme forms of
environmental change and uncertainty over the longer term. We analyse the interactions …
environmental change and uncertainty over the longer term. We analyse the interactions …
Petrologic monitoring at Volcán de Fuego, Guatemala
EJ Liu, KV Cashman, E Miller, H Moore… - Journal of Volcanology …, 2020 - Elsevier
Paroxysmal activity represents an end-member in the common range of activity at mafic arc
volcanoes, characterised by rapid transitions across the effusive-explosive interface and …
volcanoes, characterised by rapid transitions across the effusive-explosive interface and …
[HTML][HTML] Living with Volcan Tungurahua: The dynamics of vulnerability during prolonged volcanic activity
For the people that live around many of the world's volcanos, the effects of eruptive activity
on livelihoods and wellbeing are seldom experienced as a one-off event. Not only do …
on livelihoods and wellbeing are seldom experienced as a one-off event. Not only do …
Breathing and Coughing: The Extraordinarily High Degassing of Popocatépetl Volcano Investigated With an SO2 Camera
How do lava domes release volcanic gases? Studying this problem is crucial to understand,
and potentially anticipate, the generation of the sudden and dangerous explosive eruptions …
and potentially anticipate, the generation of the sudden and dangerous explosive eruptions …
VIGIA: A thermal and visible imagery system to track volcanic explosions
The monitoring of the frequency, intensity/magnitude and dynamics of explosive events at
volcanoes in a state of unrest is key to surveying and forecasting their activity. Thermal and …
volcanoes in a state of unrest is key to surveying and forecasting their activity. Thermal and …
Ash clouds temperature estimation. Implication on dilute and concentrated PDCs coupling and topography confinement
Pyroclastic density currents (PDCs) are among the most hazardous of all volcanic processes
in terms of high speeds and unpredictable extent. While concentrated PDCs are usually …
in terms of high speeds and unpredictable extent. While concentrated PDCs are usually …