Abstract The Yellowstone Plateau Volcanic Field is characterized by extensive seismicity,
episodes of uplift and subsidence, and a hydrothermal system that comprises more than …

An accelerating process of ground deformation that began 10 years ago is currently affecting
the Campi Flegrei caldera. The deformation pattern is here explained with the overlapping of …

Fluids are naturally present in the crust from subsoil to several kilometers deep. The
representation of the Earth's crust as a purely elastic medium ignores the effects of fluids …

To develop a model of both the structure and evolution of the Campi Flegrei caldera (CFc)
magmatic feeding system, geochronological, geochemical and Sr, Nd, Pb and B isotopic …

The inter-arrival times of the post 2000 seismicity at Campi Flegrei caldera are statistically
distributed into different populations. The low inter-arrival times population represents …

We analyze 1980–2010 ground displacements, to discern similarities or differences
between Campi Flegrei (CF) inflations and deflations and highlight possible anomalies in …

Campi Flegrei (CF) is an active and densely populated caldera in Southern Italy, which has
manifested signs of significant unrest in the last 50 years. Due to the high volcanic risk …

In this work we assess how volcano geodetic observations can be used to gain insights into
hydrothermal system dynamics. We designed a range of numerical models of hydrothermal …

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 …

Summary Campi Flegrei collapse caldera (Italy) is a high-risk volcanic area located close to
Naples and includes part of the densely populated city. This area is characterised by large …