Volcaniclastic sediments, broadly defined as clastic deposits derived from the transport,
deposition and/or redeposition of the products of volcanic activity, have long been a …

This review describes a range of natural processes leading to the formation of turbulent
buoyant plumes, largely relating to volcanic processes, in which there are localized, intense …

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 …

We utilize a theoretical analysis of the generation, ascent, intrusion and eruption of basaltic
magma on the Moon to develop new insights into magma source depths, supply processes …

Two contrasting models of the dynamics of explosive basaltic eruptions are in current usage.
These are referred to as the rise speed dependent (RSD) model and the collapsing foam …

Subduction of oceanic crust and the formation of volcanic arcs above the subduction zone
are important components in Earth's geological and geochemical cycles. Subduction …

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 …

The abundance of volatile compounds, and particularly CO2, in the upper oceanic mantle
affects the style of volcanic eruptions. At mid-ocean ridges, eruptions are generally …

Extraordinary video and hydrophone observations of a submarine explosive eruption were
made with a remotely operated vehicle in April 2006 at a depth of 550–560 m on NW Rota‐1 …

We model the chemical evolution of Titan, wherein primordial NH3 reacts with sulfate-rich
brines leached from the silicate core during its hydration. The resulting differentiated body …