Assessing the volcanic hazard for Rome: 40Ar/39Ar and In-SAR constraints on the most recent eruptive activity and present-day uplift at Colli Albani Volcanic District
Author(s)
Language
English
Obiettivo Specifico
1V. Storia eruttiva
Status
Published
JCR Journal
JCR Journal
Peer review journal
Yes
Journal
Issue/vol(year)
/43 (2016)
Pages (printed)
6898-6906
Date Issued
2016
Abstract
We present new 40 Ar/ 39 Ar data which allow us to refine the recurrence time for the most recent
eruptive activity occurred at Colli Albani Volcanic District (CAVD) and constrain its geographic area. Time
elapsed since the last eruption (36 kyr) overruns the recurrence time (31 kyr) in the last 100 kyr. New
interferometric synthetic aperture radar data, covering the years 1993–2010, reveal ongoing inflation with
maximum uplift rates (>2 mm/yr) in the area hosting the most recent (<200 ka) vents, suggesting that the
observed uplift might be caused by magma injection within the youngest plumbing system. Finally, we
frame the present deformation within the structural pattern of the area of Rome, characterized by 50 m of
regional uplift since 200 ka and by geologic evidence for a recent (<2000 years) switch of the local stress-field,
highlighting that the precursors of a new phase of volcanic activity are likely occurring at the CAVD.
eruptive activity occurred at Colli Albani Volcanic District (CAVD) and constrain its geographic area. Time
elapsed since the last eruption (36 kyr) overruns the recurrence time (31 kyr) in the last 100 kyr. New
interferometric synthetic aperture radar data, covering the years 1993–2010, reveal ongoing inflation with
maximum uplift rates (>2 mm/yr) in the area hosting the most recent (<200 ka) vents, suggesting that the
observed uplift might be caused by magma injection within the youngest plumbing system. Finally, we
frame the present deformation within the structural pattern of the area of Rome, characterized by 50 m of
regional uplift since 200 ka and by geologic evidence for a recent (<2000 years) switch of the local stress-field,
highlighting that the precursors of a new phase of volcanic activity are likely occurring at the CAVD.
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article
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