In the 2018, two earth scientists from Slovakia, Pavol Zahorec and Peter Vajda have teamed up with colleagues from Osservatorio Etneo, Istituto Nazionale di Geofisica e Vulcanologia (INGV) in Catania (Sicily), Daniele Carbone, Filippo Greco and Massimo Cantarero to conduct a one week campaign of field work devoted to volcano gravimetric measurements.
Their objective was to verify in–situ the newly developed methodology devoted to treating deformation–induced gravimetric effects in interpretation of spatio-temporal gravity changes observed and interpreted in volcanic areas that are used to learn as much as possible about magmatic and volcanic processes and to predict volcanic hazard and mitigate damages caused by eruptions or volcanic unrest.
A curious by–product of their observations was the determination of the current elevation of Etna, which is a quantity changing in time due to eruptions, using geodetic GNSS (GPS).
Thank you to those of you who contributed descriptions of your work for the annual highlights reports. We are always interested in new work to highlight, if you publish something yourself, or see something in-print that would be worthy of…
IAVCE is piloting an eVolcano video project to curate and distribute Volcanology videos. Please consider contributing some content! The eVolcano pilot project includes peer-reviewed videos that are 20-30min long scientific lectures covering different fields and subjects in Volcanology, targeting the…
We are pleased to announce the launch of a volcano model verification and validation initiative “Drivers of Volcano Deformation” (DVD), sponsored by CONVERSE/IAVCEI/Modeling Collaboratory for Subduction. DVD Phase 1 consists of several exercises to test commonly used models for ground deformation at volcanoes. As forward and inverse models of volcano deformation increase in complexity, it…
The IMO (Icelandic Met Office) published the interferogram showing new dike intrusion on Reykjanes Peninsula and deformation associated with the M 5.47 earthquake on 31 July 2022. Through this interferogram, it’s possible to observe approximately 16 cm of northwestward displacement…