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 …

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 …

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 …

Brothers volcano, of the Kermadec intraoceanic arc, is host to a hydrothermal system unique
among seafloor hydrothermal systems known anywhere in the world. It has two distinct vent …

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 …

The geological evolution of seamounts has distinct influence on their interactions with the
ocean, their hydrology, geochemical fluxes, biology, resources, and geohazards. There are …

Since the 1919 foundation of the International Association of Volcanology and Chemistry of
the Earth's Interior (IAVCEI), the fields of volcano seismology and acoustics have seen …

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 …

Submarine volcanic activity releases large amounts of gases and metals in the water
column, affecting biogeochemical cycles and ecosystems at a regional and local scale. In …

Whether arc magmatism occurs above oceanic subduction zones is the forefront of studies
on convergent plate margins. The most important petrologic issue related to the evolution of …