Extremely voluminous magmatic systems known as large igneous provinces (LIPs)
punctuate Earth's history, and the gases they release plausibly link large-scale geodynamic …

Pyroclastic density currents (PDCs) are mixtures of two components, namely solid particles
and fluid (gas) phase. They macroscopically behave as dense, multiphase gravity currents …

Compositional gaps are common in volcanic series worldwide. The pervasive generation of
compositional gaps influences the mechanical and thermal properties of the crust, and holds …

If fractional crystallization coupled with some crustal assimilation (AFC) is the dominant
process for generating evolved magmas in the Earth's crust, large quantities of igneous …

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 …

Pyroclastic density currents are generated in explosive volcanic eruptions when gas and
particle mixtures remain denser than the surrounding atmosphere. These mobile currents …

Heterogeneities in crustal magma chambers are generated by incomplete mixing of different
batches of magmas, precipitation or remelting of solids~ 10–20% denser than surrounding …

Abstract The Taupo Volcanic Zone (TVZ), located in the North Island of New Zealand,
represents part of a magmatic arc that is at present undergoing active extension. Around 0· 9 …

Partially molten rocks, often called a mush, are examples of a hydrogranular mixture where
the dynamics are controlled by both fluid and crystal‐crystal interactions. An obstacle to …

Volcanic eruptions can trigger tsunamis, which may cause significant damage to coastal
communities and infrastructure. Tsunami generation during volcanic eruptions is complex …