Forecasting eruptions is a fundamental goal of volcanology. However, difficulties in
identifying eruptive precursors, fragmented approaches and lack of resources make eruption …

The stress field controls patterns of crustal deformation, including which faults are likeliest to
cause earthquakes or transmit fluids. Since the 1950s, maps of maximum horizontal stress …

The study of volcano deformation has grown significantly through they year 2020 since the
development of interferometric synthetic aperture radar (InSAR) in the 1990s. This relatively …

Abstract The 2018 Sierra Negra eruption resulted in meter‐scale subsidence due to basaltic
magma extraction from a deflating reservoir. The eruption was also characterized by dike …

On 16 April 2013, an M w= 7.7 earthquake struck the border of Iran and Pakistan in the
central part of the Makran subduction zone with a reported depth of 80 km by USGS. This …

Simulating magma propagation pathways requires both a well‐calibrated model for the
stress state of the volcano and models for dike advance within such a stress field. Here, we …

Shallow magmatic reservoirs that produce measurable volcanic surface deformation are
often considered as discrete independent systems. However, petrological analyses of …

Dykes are magma‐filled fractures propagating through the brittle crust. Understanding the
physics of dyking process is essential to mitigate the volcanic hazard associated with the …

Previous work at Fernandina, the most active volcano of the Western Galápagos (Ecuador),
revealed evidence for both a shallow and a deep magma reservoir, but the relative …

Constraining stresses in the Earth's crust in volcanic regions is critical for understanding
many mechanical processes related to eruptive activity. Dike pathways, in particular, are …