Articles | Volume 25, issue 9
https://doi.org/10.5194/nhess-25-3421-2025
https://doi.org/10.5194/nhess-25-3421-2025
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16 Sep 2025
Research article | Highlight paper |  | 16 Sep 2025

The 1538 eruption at the Campi Flegrei resurgent caldera: implications for future unrest and eruptive scenarios

Giuseppe Rolandi, Claudia Troise, Marco Sacchi, Massimo Di Lascio, and Giuseppe De Natale

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Cited articles

Acocella, V.: Evaluating fracture patterns within a resurgent caldera: Campi Flegrei, Italy, B. Volcanol., 72, 623–638, 2010. 
Alberico, I., Petrosino, P., and Lirer, L.: Volcanic hazard and risk assessment in a multi-source volcanic area: the example of Napoli city (Southern Italy), Nat. Hazards Earth Syst. Sci., 11, 1057–1070, https://doi.org/10.5194/nhess-11-1057-2011, 2011. 
Amato, L. and Gialanella, C.: New evidences on the Phlegraean bradyseism in the area of Puteolis harbour, in: Geotechnical Engineering for the Preservation of Monuments and Historic Sites, edited by: Bilotta, Flora, Lirer and Viggiani, Taylor and Francis, London, UK, 137–143, https://doi.org/10.13140/2.1.2326.0482, 2013. 
Annecchino, R.: Agnano, l'origine del nome e del lago, Bollettino Flegreo, 5, 1931.  
Aster, R. and Meyer, R.: Three-dimensional velocity structure and hypocenter distribution in the Campi Flegrei caldera, Italy, Tectonophysics, 149, 195–218, 1988. 
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Executive editor
I would like to support the proposal by the reviewer and the handling editor. This innovative study reconstructs the precursory phenomena of the 1538 Campi Flegrei eruption using historical records and recent volcanological data to develop two alternative scenarios that inform civil protection strategies for managing current unrest and potential eruptions in the densely populated area.
Short summary
We compare recent unrest episodes at the Campi Flegrei caldera (Naples, Italy) with phenomena that occurred during the historical eruption in 1538. Besides proposing a new, accurate reconstruction of the ground movements in the area since the 8th century BCE, we deduce a striking similarity of the present unrest with the precursors to the 1538 eruption. We then infer that, if the ground uplift continues, earthquakes of up to magnitude 5 are expected, as well as a considerable eruption risk in the next few decades.
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