One of the biggest challenges in volcanic hazard assessment is to understand how and why
eruptive style changes within the same eruptive period or even from one eruption to the next …

More than 800 million people live in proximity to active volcanoes and could be directly
impacted by potential eruptions. Mitigation of future volcanic hazards requires adequate …

Over the last few decades, significant advances in using geophysical techniques to image
the structure of magma plumbing systems have enabled the identification of zones of melt …

Currently, it is only possible to look inside an active volcano using indirect geophysical
methods. One such method is to measure surface deformation, which results from …

Abstract Global Synthetic Aperture Radar (SAR) measurements made over the past decades
provide insights into the lateral extent of magmatic domains, and capture volcanic process …

Understanding and managing unrest at a volcano include i) ascertaining the magmatic
distribution and migration, and ii) tracking the evolution of the shallow plumbing system …

Twenty years of continuous Earth observation by satellite SAR have resulted in numerous
new insights into active volcanism, including a better understanding of subsurface magma …

Observations of volcanoes from space are a critical component of volcano monitoring, but
we lack quantitative integrated models to interpret them. The atmospheric sulfur yields of …

Abstract The East African Rift System (EARS) is composed of around 78 Holocene
volcanoes, but relatively little is known about their past and present activity. This lack of …

Volcanic eruptions are fed by plumbing systems that transport magma from its source to the
surface, mostly fed by dykes. Here we present laboratory experiments that model dyke …