Pyroclastic density currents (PDCs) are among the most lethal volcanic phenomena...
Between December 2020 and February 2022 a series of more than 60 paroxysmal events...
The K-alkaline, Quaternary Roman Magmatic Province (RMP) includes several active...
The eruptive style of mafic volcanoes is critically influenced by magma rheology,...
Crystallisation kinetics play a fundamental role in controlling conduit dynamics...
Paroxysmal mafic activity is a relevant source of hazard at many active volcanoes....
Understanding the rheological evolution of solidifying magma during its migration...
Stromboli is a unique open-conduit mafic volcano known for persistent Strombolian...
The 472 CE sub-Plinian eruption of Somma-Vesuvius represents a critical reference...
Small- to moderate-volume eruptions at caldera systems often involve complex and...
Throughout Earth’s history, eruptions from volcanic fissures have been responsible...
Reconstructing the eruptive history of Antarctic volcanoes is often challenging due...