Results 21 to 30 of about 355 (168)
A roadmap for amphibious drilling at the Campi Flegrei caldera: insights from a MagellanPlus workshop [PDF]
Large calderas are among the Earth's major volcanic features. They are associated with large magma reservoirs and elevated geothermal gradients. Caldera-forming eruptions result from the withdrawal and collapse of the magma chambers and produce large ...
M. Sacchi +26 more
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Event trees for eruption forecasting at Campi Flegrei caldera
Available studies for Event Trees at the Campi Flegrei caldera are based on the application of the Bayesian Event Tree model for eruption forecasting (BET_EF) and volcanic hazard (BET_VH). In this document we review such studies, which contain full implementation of the probabilistic eruption forecasting and volcanic hazard at Campi Flegrei ...
Doronzo, Domenico +3 more
openaire +2 more sources
Volcanic unrest at large calderas, led by the complex interaction between the degassing of the shallow magma reservoir and the overlying hydrothermal system, occurs at intervals of 10–100 years. Even if only a minority of bradyseismic crises ends with an
S. Lambert, G. Sottili
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GPS time series at Campi Flegrei caldera (2000-2013)
The Campi Flegrei caldera is an active volcanic system associated to a high volcanic risk, and represents a well known and peculiar example of ground deformations (bradyseism), characterized by intense uplift periods, followed by subsidence phases with ...
Prospero De Martino +2 more
doaj +1 more source
We report the occurrence of several sand liquefaction structures, such as sand dikes, in the stratigraphic record of the Campi Flegrei volcano, located both inside and outside the caldera. Five sites were analyzed within the caldera and two outside.
Stefano Vitale +4 more
doaj +1 more source
The Campi Flegrei caldera: unrest mechanisms and hazards
Abstract In the last four decades, Campi Flegrei caldera has been the world’s most active caldera characterized by intense unrest episodes involving huge ground deformation and seismicity, but, at the time of writing, has not culminated in an eruption.
G. DE NATALE +6 more
openaire +3 more sources
The dynamics of the Campi Flegrei caldera magma chamber.
The Campi Flegrei volcanic system is certainly a remarkable case study for what concerns magma chamber dynamics. In fact, its magmatic and volcanic history appears to have been largely driven by chamber processes like fractional crystallization, magma mixing, and volatile degassing.
Chiara Montagna +2 more
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Volcanic unrest scenarios and impact assessment at Campi Flegrei caldera, Southern Italy
At Campi Flegrei caldera, volcanic unrest hazards during 1982–1984 caused significant building damage and led to the evacuation of over 40,000 residents in the central town of Pozzuoli.
Danielle Charlton +2 more
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In recent decades, the Campi Flegrei caldera (Italy) showed unrest characterized by increases in seismicity, ground uplift, and hydrothermal activity. Currently, the seismic and hydrothermal phenomena are mostly concentrated in the Solfatara–Pisciarelli ...
Antonietta M. Esposito +3 more
doaj +1 more source
Thermally-assisted Magma Emplacement Explains Restless Calderas
Many calderas show repeated unrest over centuries. Though probably induced by magma, this unique behaviour is not understood and its dynamics remains elusive.
Antonella Amoruso +3 more
doaj +1 more source

