Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/5224
AuthorsRiguzzi, F.* 
Pietrantonio, G.* 
Devoti, R.* 
Atzori, S.* 
Anzidei, M.* 
TitleVolcanic unrest of the Colli Albani (central Italy) detected by GPS monitoring test
Issue DateNov-2009
Series/Report no./177 (2009)
DOI10.1016/j.pepi.2009.07.012
URIhttp://hdl.handle.net/2122/5224
KeywordsColli Albani
GPS
Volcano monitoring
Mogi source
Subject Classification04. Solid Earth::04.03. Geodesy::04.03.01. Crustal deformations 
AbstractThe Colli Albani volcanic complex, located in central Italy about 15km SE of Rome, has been dominated by periodic eruptive histories started about 561 ka and ending with the most recent and voluminous activity of the Albano maar (<70 ka) phase. Earthquakes of moderate intensity, gas emissions and significant ground deformations are the recent evidences of a residual activity. We decided to start a monitoring test by installing as first step three GPS permanent stations on the volcanic structure, in sites easily accessible. The analysis of about 2 years of GPS observations has evidenced a peculiar velocity pattern of the Colli Albani stations with respect to those located nearby, but outside the volcano edifice. With respect to Eurasia, the horizontal velocities are NE directed with magnitudes of 2.2±1.4mm/year (RDPI), 3.0±0.8mm/year (RMPO) and 3.3±1.2mm/year (NEMI). The uplift rates are determined with minor accuracy and range from 3.3 and 6.0mm/year. We used a non-linear inversion algorithm to determine the best-fit parameters for a Mogi spherical source based on the Levenberg–Marquardt least squares approach. The best-fit is obtained with a source at 4.6km depth beneath thewestern flank of the volcano and a volume variation of 3.6×10−4 km3/year. This result is in agreement with the volume rate retrieved by PS-InSAR technique and rather different from the rate inferred from leveling surveys. Consequently, non-linear trends of the hydrothermal system charge cannot be excluded apriori and the continuous GPS monitoring should be considered a priority in assessing the hazard of the Colli Albani.
Appears in Collections:Papers Published / Papers in press

Files in This Item:
File Description SizeFormat 
Riguzzi_et al._PEPI_2009.pdf1.81 MBAdobe PDFView/Open
Show full item record

Page view(s)

87
Last Week
0
Last month
checked on Jun 27, 2017

Download(s)

35
checked on Jun 27, 2017

Google ScholarTM

Check

Altmetric