Volcano geodesy often involves the use of models to explain observed surface deformation.
A variety of forward models are used, from analytical point sources to numerical simulations …

Volcano deformation can be detected over timescales from seconds to decades, offering
valuable insights for magma dynamics. However, these signals are shaped by the long-term …

As volcanoes undergo unrest, understanding the conditions and timescales required for
magma reservoir failure, and the links to geodetic observations, are critical when evaluating …

Large igneous provinces erupt highly reactive, predominantly basaltic lavas onto Earth's
surface, which should boost the weathering flux leading to long-term CO2 drawdown and …

Geodetic timeseries suggest that volcanoes exhibit a wide range of deformation patterns.
Viscoelastic deformation around crustal magma storage zones is an expected contributor to …

Rapid emplacement of a mafic dyke or sill at mid-crustal depth heats and possibly melts the
felsic wall rock followed by solidification. Associated volume changes generate stresses …

Prior to intrusion, magma migrates through the crustal plumbing system that likely contains
layers or columns of crystal mush. To better understand the behavior of the crustal magmatic …

Rapid emplacement of a mafic dyke or sill at mid-crustal depth heats and possibly melts the
felsic wall rock followed by solidification. Associated volume changes generate stresses …