EGU26-18452, updated on 14 Mar 2026
https://doi.org/10.5194/egusphere-egu26-18452
EGU General Assembly 2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Oral | Friday, 08 May, 12:10–12:20 (CEST)
 
Room 0.96/97
CARG-based (Sheet 416, 417, and 364) volume reassessment for the caldera-forming, VEI 6/7 ignimbrites along the Roman Magmatic Province
Alessandro Frontoni1,3, Guilherme A. R. Gualda2, Andrea Bonamico3, Raffaello Cioni4, Sandro Conticelli1,4, José Pablo Sepulveda Birke1, and Guido Giordano1,3
Alessandro Frontoni et al.
  • 1Consiglio Nazionale delle Ricerche – Istituto di Geologia Ambientale e Geoingegneria (CNR-IGG), Area Territoriale della Ricerca Roma1, SP35d, 9, Montelibretti (RM), 00010, Italy (alessandro.frontoni@uniroma3.it)
  • 2Earth and Environmental Sciences, Vanderbilt University, 2301 Vanderbilt Place, Nashville, TN-37235, USA
  • 3Dipartimento di Scienze – Sezione di Geologia, Università degli Studi di Roma Tre, Largo S. Leonardo Murialdo, 1, Roma, 00146, Italy
  • 4Dipartimento di Scienze della Terra, Università degli studi di Firenze, Via Giorgio La Pira, 4, Firenze, 50121, Italy

The renewed start and funding of the CARG project in volcanic areas have enabled new surveys and refinements of data on the volumes and extents of ignimbrites across the Roman Magmatic Province (RMP). To date, the investigation has focused particularly on the Roccamonfina volcano (Sheets 416 Sessa Aurunca and 417 Teano) and the Bracciano caldera (Sheet 364 Bracciano). The project is enhancing field data from areas already surveyed in past decades, while integrating new models and technologies to obtain more accurate quantifications of erupted magma volumes and a consequent re-evaluation of eruption magnitudes. Preliminary results indicate that the volume of some ignimbrites increases by more than one order of magnitude, suggesting that many other ignimbrites within the RMP may have been significantly underestimated, such as the Brown Leucitic Tuff and the White Trachytic Tuff pertaining to the Roccamonfina volcano. This reassessment potentially characterizes the RMP as an ignimbrite flare-up system, comparable to some of the largest and most impactful volcanic provinces worldwide, such as the Taupo Volcanic Zone. In this framework, new field and literature data, borehole stratigraphy, and GIS-integrated methodologies were combined to refine the bulk volume, areal extension, and magnitude of a case-study ignimbrite, with the aim of developing a standardized procedure for computing and integrating field surveys applicable to all ignimbrites.

How to cite: Frontoni, A., Gualda, G. A. R., Bonamico, A., Cioni, R., Conticelli, S., Sepulveda Birke, J. P., and Giordano, G.: CARG-based (Sheet 416, 417, and 364) volume reassessment for the caldera-forming, VEI 6/7 ignimbrites along the Roman Magmatic Province, EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-18452, https://doi.org/10.5194/egusphere-egu26-18452, 2026.