Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/5963
Authors: Anzidei, M.* 
Riguzzi, F.* 
Stramondo, S.* 
Title: Current geodetic deformation of the Colli Albani volcano: a review
Issue Date: 20-Dec-2009
URI: http://hdl.handle.net/2122/5963
Keywords: Colli Albani, GPS, SAR, Levelling
Subject Classification04. Solid Earth::04.03. Geodesy::04.03.01. Crustal deformations 
Abstract: The quiescent Colli Albano volcano is presently characterised by moderate intensity earthquakes, seismic swarms, gas emissions and ongoing uplift that reflects the current evidences of its residual activity. An uplift of ~30 cm over the last 43 years was recently detected by levelling surveys performed in the time span 1950-1993 along a levelling line that crosses the highest elevation area of the western flank of the volcano. Space based GPS and Synthetic Aperture Radar Interferometry geodetic observations confirm that this uplift is distributed in a wide area around the craters of Albano and Nemi, where the most recent volcanic activity occurred. GPS data from continuous monitoring stations indicate that both horizontal and vertical deformations do occur and that can be addressed to a shallow magmatic source. All the geodetic observations are in agreement and highlight that the Colli Albani is still a potentially active volcano. Being located in a densely populated area close to Rome, the volcano should deserve the same monitoring and hazard assessment effort of any active volcano within urbanized areas. Here we review the geodetic results obtained during the last decades for the Colli Albani volcano.
Appears in Collections:Papers Published / Papers in press

Files in This Item:
File Description SizeFormat 
albani geodesy_GSL_REV_final091209.pdf1.45 MBAdobe PDFView/Open
Show full item record

Page view(s)

304
Last Week
0
Last month
0
checked on Aug 20, 2018

Download(s)

437
checked on Aug 20, 2018

Google ScholarTM

Check