The deep magmatic architecture of the Hawaiian volcanic system is central to understanding
the transport of magma from the upper mantle to the individual volcanoes. We leverage …

Geophysical characterization of calderas is fundamental in assessing their potential for
future catastrophic volcanic eruptions. The mechanism behind the unrest of Long Valley …

Fluids supplied by stored magma at depth are causal factors of volcanic unrest, as they can
cause pressurization/heating of hydrothermal systems. However, evidence for links between …

Abstract Since 1.25 Ma, three volcanic systems in the western US Cordillera hosted rhyolitic
eruptions of≳ 300 km 3 dense rock equivalent creating the Yellowstone (0.63 Ma), Long …

Repeating earthquakes, or repeaters, affecting overlap** rupture patches with a similar
focal mechanism, have important implications to track fault slip rates, aseismic deformation …

Recent seismic and geodetic observations suggest the involvement of pressurized fluid and
aseismic slip during earthquake swarms. However, the interaction between these two factors …

Abstract Analysis of a small earthquake swarm near Virginia City, NV, reveals complex
structural features, including an interplay of both fluid‐driven and aseismic‐driven …

The spatial and temporal evolutionary mechanisms of volatile components at plate
boundaries and their potential as earthquake precursors are not well understood. Based on …

Abstract Taupō volcano, New Zealand, is a large caldera volcano that has been highly
active through the Holocene. It most recently erupted∼ 1,800 years ago but there have been …

Both volcano‐tectonic (VTs) and deep long‐period earthquakes (DLPs) have been
documented at Akutan Volcano, Alaska and may reflect different active processes helpful for …