Over the past 25 years, our understanding of the physical processes that drive volcanic
eruptions has increased enormously thanks to major advances in computational and …

In the broadest sense, volcanic eruptions are either effusive or explosive. During explosive
eruptions magma fragments and eruption intensity is ultimately related to the fragmentation …

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 …

Gas exsolution and segregation are fundamental controls on eruption dynamics and magma
genesis. Basaltic magma loses gas relatively easily because of its low viscosity. However …

Lava dome eruptions commonly display fairly regular alternations between periods of high
and low or no activity with timescales typically of weeks to years and sudden transitions …

We present a model of effusive silicic volcanic eruptions which relates magma chamber and
conduit physics to time‐dependent data sets, including ground deformation and extrusion …

The eruption style of silicic magmas is affected by the loss of gas (outgassing) during ascent.
We investigate outgassing using a numerical model for one-dimensional, two-phase, steady …

We conducted geological and petrological analyses of the tephra fallout and pyroclastic
density current (PDC) products of the 22-23 April 2015 Calbuco eruptions. The eruptive …

Magma from Plinian volcanic eruptions contains an extraordinarily large numbers of
bubbles. Nucleation of those bubbles occurs because pressure decreases as magma rises …

Magma ascent velocities, v (d H/dt; where H is depth and t is time), can be determined from
decompression rates (d P/dt), and rates of cooling (d T/dt):, where ρ is magma density, P is …