It is commonly accepted that effusive activity emplaces the main emitted magmatic volume in
basaltic shield volcanoes. At Piton de La Fournaise (La Réunion Island, France), eruptive …

Multiphase flow in basaltic volcanic conduits is investigated using analog experiments and
theoretical approaches. Depending on gas supply, large gas bubbles (gas slugs) may rise …

Abstract Extensive vertical deformation (> 4.5 m) observed at Sierra Negra volcano
Galápagos, Ecuador, between 1992 and the 2005 eruption led scientists to hypothesize that …

An understanding of the mechanisms responsible for persistent volcanism can be acquired
through the integration of geophysical and geochemical data sets. By interpreting data on …

A key question for volcanic hazard assessment is the extent to which information can be
exchanged between volcanoes. This question is particularly pertinent to hazard forecasting …

The 1974 western flank eruption of Mount Etna produced a rare, nearly aphyric and
plagioclase‐free trachybasalt that could not be derived from the central volcano conduits …

Over the past decade, a proliferation of new technologies has pushed forward our ability to
measure the dynamics of volcanic emissions as they exit, and ascend above, the vent …

Subglacial volcanic eruptions can generate large volumes of meltwater that is stored and
transported beneath glaciers and released catastrophically in jökulhlaups. At typical basaltic …

Many early-forming asteroids differentiated, as a result of incorporating the heat-generating
isotope 26Al, and experienced various kinds of volcanic activity. The Dawn spacecraft's …

During the climactic Plinian phase of the 1886 basaltic eruption of Tarawera, New Zealand,
vents along the 17 km fissure erupted explosively with a wide range of dispersal. The 8 km …