Basaltic pyroclastic volcanism takes place over a range of scales and styles, from weak
discrete Strombolian explosions (∼ 102–103kgs− 1) to Plinian eruptions of moderate …

Monogenetic basaltic volcanoes are the most common volcanic landforms on the continents.
They encompass a range of morphologies from small pyroclastic constructs to larger shields …

Large igneous provinces (LIPs) are sites of the most frequently recurring, largest volume
basaltic and silicic eruptions in Earth history. These large-volume (> 1000km3 dense rock …

To facilitate the assessment of hazards and risk from volcanoes, we have created a
comprehensive global database of Quaternary Large Magnitude Explosive Volcanic …

The weakest explosive volcanic eruptions globally, Strombolian explosions and Hawaiian
fountaining, are also the most common. Yet, despite over a hundred years of observations …

Basaltic eruptions are the most common form of volcanism on Earth and planetary bodies.
The low viscosity of basaltic magmas inhibits fragmentation, which favours effusive and lava …

Understanding silicic eruption triggers is paramount for deciphering explosive volcanism
and its potential societal hazards. Here, we use phase equilibria modeling to determine the …

Bubble nucleation is at the heart of magma ascent and degassing. Nucleation kinetics
control how easily a magma exsolves its volatiles, and thereby its explosivity close to the …

Volcanic eruptions are driven by bubbles that form when volatile species exsolve from
magma. The conditions under which bubbles form depend mainly on magma composition …

Volcanic eruptions are common, with more than 50 volcanic eruptions in the United States
alone in the past 31 years. These eruptions can have devastating economic and social …