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Well, there doesn't seem to be any news as of tonight. INGV declared an end to the swarm around 6-7 p.m. local time Friday, but as Dr. Di Vito said, it's a crisis and they are monitoring it closely.
This Naples media source (Italian) summed up the situation (and if nerdy stuff appeals to you, here is the paper they mention, which came out four days ago).
Via GT:
The emphasis in that new paper also is on possible powerful earthquakes. This is consistent with recent public statements from INGV that the densely populated region could experience up to estimated magnitude 5 temblors.
Add in a strong hydrothermal explosion, probably much stronger than the one Yellowstone's Biscuit Basin produced this year -- although just as unexpected -- and yes, it's a crisis even though INGV has noted in bulletins that the uplift has been slowing down since August.
This Naples media source (Italian) summed up the situation (and if nerdy stuff appeals to you, here is the paper they mention, which came out four days ago).
Via GT:
Magnitude 3.4 in the area of via dei Gerolomini and at about 500 meters deep. At dawn yesterday Pozzuoli was awakened by a very strong shock after a truce of about three months...The strongest shock was included in a seismic swarm that lasted many hours and characterized in almost all cases by very superficial shocks, in a fairly limited area between via Gerolomini, via Suolo San Gennaro and via Napoli.
<b>New element of concern</b>
The presence of superficial shocks could constitute an element of concern in the complex crisis situation of the Campi Flegrei...A situation of high risk due to the possibility, far from remote, of phreatic eruptions, that is, explosive eruptions without the involvement of magma, but no less dangerous in terms of public safety since they are not predictable, as they do not manifest themselves with precursors that scientists are able to interpret.
<b>The recent study by INGV/b>
In short, the pressure in the hydrothermal system has increased as also attested by a recent study by INGV...The director of the Vesuvius Observatory, Mauro Di Vito, explained to TgR Campania the other day: «Putting all the data together in this study, it was seen that the source of overpressure would be located around four kilometers, we are not talking about magma, however to have such a strong emission of gas from the subsoil there needs to be a magmatic degassing».
...
...an enormous pressure pushes towards the hydrothermal system fed by fluids that derive from the magma that (it is estimated) is located between 5 and 6 kilometers. The weakening of the crust reported by increasingly superficial earthquakes could «blow the cork» and cause a sudden phreatic explosion. This is one of the concerns expressed by the Major Risks Commission in recent months. In the document following the meetings of 27 and 28 October, published exclusively by the «Corriere del Mezzogiorno», the fears were made explicit in a chapter entitled «Possible occurrence of phreatic eruptions»...
...Giuseppe Mastrolorenzo is also convinced that «high temperature and pressure values in the hydrothermal system and low-depth stresses detected by superficial earthquakes can lead to a phreatic explosion that is not predictable». In short, in the Phlegraean caldera, magma is only one of the problems.
The emphasis in that new paper also is on possible powerful earthquakes. This is consistent with recent public statements from INGV that the densely populated region could experience up to estimated magnitude 5 temblors.
Add in a strong hydrothermal explosion, probably much stronger than the one Yellowstone's Biscuit Basin produced this year -- although just as unexpected -- and yes, it's a crisis even though INGV has noted in bulletins that the uplift has been slowing down since August.