Paleoseismic history of the intermountain Rieti Basin (Central Apennines, Italy)

Abstract. From the paleoseismological and seismotectonic point of view, the intermountain basins of the Central Apennines of Italy are one of the most studied areas worldwide. Within this context, however, the Rieti Basin, bounded at its sides by active normal faults and with its peculiar rhombohedral shape, is a relatively overlooked area, and its most recent paleoseismological studies date back to the 90s. This is a key area both for completing the paleoseismological history of this sector of the chain and for understanding how the present-day extensional regime is accommodated through time by the faults bounding the basin. With this aim in mind, we excavated 17 paleoseismological trenches along the normal faults bordering the Rieti Basin (Central Apennines, Italy) and unveiled at least 6 paleoearthquakes that ruptured the faults during the last ca. 20 kyr. Our analysis of the paleoearthquake succession along the basin-bounding faults suggests that a spatial pattern is followed during sequences of rupturing events, with a maximum credible earthquake of Mw 6.5, consistently within this sector of the Central Apennines.

Authors

Publication Details

Journal
Natural hazards and earth system sciences
Published
2026-01-15
DOI
https://doi.org/10.5194/nhess-26-131-2026
Primary Topic
earthquake and tectonic studies
Type
article
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article

Paleoseismic history of the intermountain Rieti Basin (Central Apennines, Italy)

Kathleen Nicoll, Valerio Materni, Giorgio Tringali, Stefano Urbini et al.
Natural hazards and earth system sciences
earthquake and tectonic studies
article

Paleoseismic history of the intermountain Rieti Basin (Central Apennines, Italy)

Kathleen Nicoll, Valerio Materni, Giorgio Tringali, Stefano Urbini, Valerio Ruscito, Vincenzo Sapia, R. Nappi, Gilberto Binda, Marco Pizza, Luca Maria Puzzilli, Valerio Comerci, Roberto Gambillara, Pio Di Manna, Emanuele Scaramuzzo, Paolo Lorenzoni, M. Colombo, Fiorenzo Fumanti, Anna Maria Blumetti, Mauro Roma, Maurizio Guerra, Frank Thomas, Argelia Silva Fragoso, Marco Caciagli, Alessandro M. Michetti, Rosella Nave, Aurora Rossi, Roberto Pompili, Maria F. Ferrario, Luca Guerrieri, Alba Peiro, Fernando Ferri, Franz A. Livio, Francesco Miscione, Andrea Zerboni
article en

Abstract

Abstract. From the paleoseismological and seismotectonic point of view, the intermountain basins of the Central Apennines of Italy are one of the most studied areas worldwide. Within this context, however, the Rieti Basin, bounded at its sides by active normal faults and with its peculiar rhombohedral shape, is a relatively overlooked area, and its most recent paleoseismological studies date back to the 90s. This is a key area both for completing the paleoseismological history of this sector of the chain and for understanding how the present-day extensional regime is accommodated through time by the faults bounding the basin. With this aim in mind, we excavated 17 paleoseismological trenches along the normal faults bordering the Rieti Basin (Central Apennines, Italy) and unveiled at least 6 paleoearthquakes that ruptured the faults during the last ca. 20 kyr. Our analysis of the paleoearthquake succession along the basin-bounding faults suggests that a spatial pattern is followed during sequences of rupturing events, with a maximum credible earthquake of Mw 6.5, consistently within this sector of the Central Apennines.

Natural hazards and earth system sciencesVol. 26(1)
Openalex Percentile: Top 91%
earthquake and tectonic studies
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