Hydrovolcanism is a type of volcanism where magma and water interact either explosively or
non-explosively. The less frequently used term, hydromagmatism, includes all the processes …

Abstract The Campi Flegrei caldera is one of the most dangerous volcanoes in the world
and since 2005 it is in unrest. Here we evaluate the 3D tomography of the b value at the …

A maar crater is the top of a much larger subsurface diatreme structure produced by
phreatomagmatic explosions and the size and shape of the crater reflects the growth history …

Campi Flegrei caldera is an Italian high-risk volcano experiencing a progressively more
intense long-term uplift, accompanied by increasing seismicity and geochemical emissions …

This paper furnishes a brief, but exhaustive, description of the tectonics and stratigraphy of
the Campania region (southern Italy). The attached geological map (Main Map) at 1 …

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

Accurate digital elevation models represent the basic tool for a large spectrum of
applications, including geological, architectonic, archaeological, and urbanistic studies …

Campi Flegrei is an active volcanic area situated in the Campanian Plain (Italy) and
dominated by a resurgent caldera. The great majority of past eruptions have been explosive …

Abstract Models of volcanic collapses proposed in the literature rely on combining field
examples with analogue and numerical modelling to connect superficial observables to sub …

The structure of a caldera may influence its activity, making its understanding crucial for
hazard assessment. Here, we analysed high-resolution seismic profiles in the Campi Flegrei …