Submarine pyroclastic eruptions at depths greater than a few hundred meters are generally
considered to be rare or absent because the pressure of the overlying water column is …

In explosive submarine eruptions, volcanic jets transport fragmented tephra and exsolved
gases from the conduit into the water column. Upon eruption the volcanic jet mixes with …

Subaqueous eruptions are the most abundant on earth, and the proportion of such eruptions
that are explosive is larger than generally appreciated though still poorly constrained …

High-resolution bathymetric mapping has shown that submarine flat-topped volcanic cones,
morphologically similar to ones on the deep sea floor and near mid-ocean ridges, are …

Hawaiian and Strombolian eruption styles are characteristic of silica-poor, low viscosity
magmas and represent the most frequent manifestations of explosive volcanism on Earth. In …

Volcanic eruptions are important events in Earth's cycle of magma generation and crustal
construction. Over durations of hours to years, eruptions produce new deposits of lava …

Conclusions Examination of the volumetric expansion of vesiculating water vapor at
temperatures and pressure corresponding to those of basaltic and rhyolitic magmas erupting …

The shapes of typical Hawaiian volcanoes are simply parameterized, and a relationship is
derived for the dependence of lava accumulation rates on volcano volume and volumetric …

Magmas erupted in deep-water environments (> 500 m) are subject to physical constraints
very different to those for subaerial eruptions, including hydrostatic pressure, bulk modulus …

Hawaiian eruptions are largely random phenomena displaying no periodicity; that is, future
eruptions are relatively independent of the date of the last eruption. Several simultaneous …