Solid Earth
Caldera unrest prior to intense volcanism in Campi Flegrei (Italy) at 4.0 ka B.P.: Implications for caldera dynamics and future eruptive scenarios
Article first published online: 7 NOV 2009
DOI: 10.1029/2009GL040513
Copyright 2009 by the American Geophysical Union.
Additional Information
How to Cite
, , and (2009), Caldera unrest prior to intense volcanism in Campi Flegrei (Italy) at 4.0 ka B.P.: Implications for caldera dynamics and future eruptive scenarios, Geophys. Res. Lett., 36, L21303, doi:10.1029/2009GL040513.
Publication History
- Issue published online: 7 NOV 2009
- Article first published online: 7 NOV 2009
- Manuscript Accepted: 8 OCT 2009
- Manuscript Revised: 7 OCT 2009
- Manuscript Received: 11 AUG 2009
Keywords:
- volcanism;
- ground uplift;
- Campi Flegrei caldera
[1] The Campi Flegrei caldera is one of the highest risk volcanic areas on the Earth. Our research documents a 150 year-long period of intense volcanism following less than 200 years of repose after the Agnano-Monte Spina Plinian eruption (4.1 ka). The new data show that the renewal of volcanism was preceded by an uplift of a few tens of meters, triggered by mafic refilling of reservoirs at depths of 3 km or less. Our studies also indicate for the first time the occurrence of contemporaneous eruptions from at locations in different sectors of the caldera. These results suggest that a future eruptive crisis will likely be preceded by several meters of caldera-wide uplift in response to magma movements at depth. The trend of uplift of the caldera since 1969 may thus represent the unrest expected before a renewal of volcanism within an interval of decades to centuries.

1944-8007/asset/olbannerleft.jpg?v=1&s=8efe58b4bccbbac51c9740677fc27dec62622c0b)
1944-8007/asset/olbannerright.jpg?v=1&s=4147b7adc92f6020ebf1ced4d118944fcf4a9a0b)
