Ascent of magma through Earth's crust is normally associated with, among other effects,
ground deformation and gravity changes. Geodesy is thus a valuable tool for monitoring and …

Large volume effusive eruptions with relatively minor observed precursory signals are at
odds with widely used models to interpret volcano deformation. Here we propose a new …

Seismic noise interferometry is an exciting technique for studying volcanoes, providing a
continuous measurement of seismic velocity changes (dv/v), which are sensitive to …

Abstract Moderate earthquakes (Mw> 5) with moment tensors (MTs) dominated by a vertical
compensated‐linear‐vector‐dipole (vertical‐CLVD) component are often generated by dip …

This study brings new insights to elucidate the 3-D seismic velocity structure of the Aegean
region of Turkey by using Local Earthquake Tomography (LET). The study area has …

Deciphering eruptive dynamics in near-real time is essential when dealing with hazard
assessment and population evacuation. Recognition of specific patterns in time-series …

Abstract On August 16, 2014, an intense seismic swarm started below the eastern part of
Bárðarbunga caldera in the north-western part of Vatnajökull ice cap, Iceland, marking the …

Continental flood basalts intruded and erupted millions of km3 of magma over∼ 1–5 Ma.
Previous work proposed the presence of large (–106 km3) crustal magma reservoirs to feed …

We report how data from satellite and aerial synthetic aperture radar (SAR) observations
were integrated into monitoring of the 2014–2015 Holuhraun eruption in the Bárðarbunga …

Dike intrusions are often associated with surface deformation and propagating swarms of
earthquakes. These are understood to be manifestations of the same underlying physical …