Vents opening susceptibility map of the Colli Albani long dormant volcano

AbstractDespite their protracted periods of inactivity, long-dormant volcanoes may be highly hazardous, as their reactivation can be characterized by violent explosive eruptions. An example of such volcanoes is the Colli Albani caldera, onto which deposits Rome Capital City is built, Italy. Its last...

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Main Authors: Marina Bisson, Roberto Isaia, Rosella Nave, Alessandra Pensa, Guido Giordano
Format: Article
Language:English
Published: Taylor & Francis Group 2023-12-01
Series:Geomatics, Natural Hazards & Risk
Subjects:
Online Access:https://www.tandfonline.com/doi/10.1080/19475705.2023.2215905
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author Marina Bisson
Roberto Isaia
Rosella Nave
Alessandra Pensa
Guido Giordano
author_facet Marina Bisson
Roberto Isaia
Rosella Nave
Alessandra Pensa
Guido Giordano
author_sort Marina Bisson
collection DOAJ
description AbstractDespite their protracted periods of inactivity, long-dormant volcanoes may be highly hazardous, as their reactivation can be characterized by violent explosive eruptions. An example of such volcanoes is the Colli Albani caldera, onto which deposits Rome Capital City is built, Italy. Its last volcanic activity was characterized by voluminous maar-forming phreatomagmatic eruptions dated between 36 and 25ka, but the volcano has produced several maar lake overflows during the Holocene till historical times. Presently, Colli Albani is affected by recurrent seismic events, anomalous heat flow, ground uplifts, hydrothermal circulation and gas emissions. For these reasons, the Italian Civil Protection has recently listed Colli Albani among the ten active volcanoes of Italy, but products for the evaluation of its volcanic hazards lacking. This work presents the first study on vent opening susceptibility mapping at Colli Albani. We explore the potential of an available geological dataset for building, through geographic information system analysis, an index that classifies areas at different vents opening susceptibility (low, moderate and high). Such result highlights as a solid geological mapping is a prerequisite for the volcanic hazard assessment, especially in remote or poorly studied long-dormant volcanoes such as caldera systems where the location of new vents could occur in different volcano sectors.
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spelling doaj.art-8b3606bc4f40492da9fbe2decf0fcf2a2023-12-16T08:49:47ZengTaylor & Francis GroupGeomatics, Natural Hazards & Risk1947-57051947-57132023-12-0114110.1080/19475705.2023.2215905Vents opening susceptibility map of the Colli Albani long dormant volcanoMarina Bisson0Roberto Isaia1Rosella Nave2Alessandra Pensa3Guido Giordano4Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Pisa, Pisa, ItalyIstituto Nazionale di Geofisica e Vulcanologia, Osservatorio Vesuviano, Napoli, ItalyIstituto Nazionale di Geofisica e Vulcanologia, Osservatorio Vesuviano, Napoli, ItalyISPRA – Istituto Superiore per la Protezione e la Ricerca Ambientale, Rome, ItalyDipartimento di Scienze, Università degli Studi Roma Tre, Roma, ItalyAbstractDespite their protracted periods of inactivity, long-dormant volcanoes may be highly hazardous, as their reactivation can be characterized by violent explosive eruptions. An example of such volcanoes is the Colli Albani caldera, onto which deposits Rome Capital City is built, Italy. Its last volcanic activity was characterized by voluminous maar-forming phreatomagmatic eruptions dated between 36 and 25ka, but the volcano has produced several maar lake overflows during the Holocene till historical times. Presently, Colli Albani is affected by recurrent seismic events, anomalous heat flow, ground uplifts, hydrothermal circulation and gas emissions. For these reasons, the Italian Civil Protection has recently listed Colli Albani among the ten active volcanoes of Italy, but products for the evaluation of its volcanic hazards lacking. This work presents the first study on vent opening susceptibility mapping at Colli Albani. We explore the potential of an available geological dataset for building, through geographic information system analysis, an index that classifies areas at different vents opening susceptibility (low, moderate and high). Such result highlights as a solid geological mapping is a prerequisite for the volcanic hazard assessment, especially in remote or poorly studied long-dormant volcanoes such as caldera systems where the location of new vents could occur in different volcano sectors.https://www.tandfonline.com/doi/10.1080/19475705.2023.2215905Hazard mapvent opening susceptibilityColli Albani volcanolong dormant volcanoes
spellingShingle Marina Bisson
Roberto Isaia
Rosella Nave
Alessandra Pensa
Guido Giordano
Vents opening susceptibility map of the Colli Albani long dormant volcano
Geomatics, Natural Hazards & Risk
Hazard map
vent opening susceptibility
Colli Albani volcano
long dormant volcanoes
title Vents opening susceptibility map of the Colli Albani long dormant volcano
title_full Vents opening susceptibility map of the Colli Albani long dormant volcano
title_fullStr Vents opening susceptibility map of the Colli Albani long dormant volcano
title_full_unstemmed Vents opening susceptibility map of the Colli Albani long dormant volcano
title_short Vents opening susceptibility map of the Colli Albani long dormant volcano
title_sort vents opening susceptibility map of the colli albani long dormant volcano
topic Hazard map
vent opening susceptibility
Colli Albani volcano
long dormant volcanoes
url https://www.tandfonline.com/doi/10.1080/19475705.2023.2215905
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AT rosellanave ventsopeningsusceptibilitymapofthecollialbanilongdormantvolcano
AT alessandrapensa ventsopeningsusceptibilitymapofthecollialbanilongdormantvolcano
AT guidogiordano ventsopeningsusceptibilitymapofthecollialbanilongdormantvolcano