Advancing our knowledge of caldera volcanoes enables better assessment of hazard and
more efficient harnessing of resources. In this paper we review developments in concepts of …

Vanguard efforts in forecasting volcanic eruptions are turning to physics-based models,
which require quantitative estimates of magma conditions during pre-eruptive storage …

Seismic imaging methods have provided detailed three-dimensional constraints on the
physical properties of magmatic systems leading to invaluable insight into the storage …

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 overlap** of …

Seismic inversion for three-dimensional variations of velocity and attenuation are often used
to delineate magma bodies in the crust and upper mantle. Problems related to spatial …

In volcanoes with active hydrothermal systems, diffuse CO2 degassing may constitute the
primary mode of volcanic degassing. The monitoring of CO2 emissions can provide …

Campi Flegrei is an active, resurgent caldera that is located a few kilometres west of the city
of Naples, a densely populated urban settlement in southern Italy. Identifying, locating at …

For the first time a physical model, constrained by monitoring data, is used to derive a
quantitative estimate of the evolution in time of magmatic gases that enter a hydrothermal …

Passive high‐resolution attenuation tomography is used here to image the geological
structure in the first upper 4 km of the shallow crust beneath the Campi Flegrei caldera …

We have analyzed a multiparametric data set of seismological, geodetic and geochemical
data recorded at Campi Flegrei caldera since 1982. We focus here on the period 1989 …