EGU23-16651, updated on 21 Apr 2023
https://doi.org/10.5194/egusphere-egu23-16651
EGU General Assembly 2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.

The San Bartolo lava flow field, Stromboli volcano, Italy: Reconstruction of the most recent historic flank eruption (2 kyr) affecting the inhabited area by photogrammetric and LIDAR from UASs aimed at hazard assessment

Annamaria Vicari1, Nicola Famiglietti1, Sonia Calvari2, Enrica Marotta3, Rosario Avino3, Pasquale Belviso3, Andrew Harris4, Giovanni De Luca1, Antonino Memmolo1, Felice Minichiello1, and Rosario Peluso3
Annamaria Vicari et al.
  • 1Istituto Nazionale di Geofisica e Vulcanologia, Sezione Irpinia, Avellino, Italy (annamaria.vicari@ingv.it)
  • 2Istituto Nazionale di Geofisica e Vulcanologia, Osservatorio Etneo, Catania, Italy
  • 3Istituto Nazionale di Geofisica e Vulcanologia, Osservatorio Vesuviano, Napoli, Italy
  • 4Universit ́e Clermont Auvergne, CNRS, IRD, OPGC, Laboratoire Magmas et Volcans, 63000 Clermont-Ferrand, France

The San Bartolo lava flow field is the most recent flank eruption occurred at Stromboli volcano about 2 ka ago on the NE flank of the island. Despite its importance in being the most recent example of flank activity outside the barren Sciara del Fuoco slope, where the recent activity concentrated, the eruption duration, its volume, and the sequence of events has not yet been reconstructed. In this paper, we present a new survey of the lava flow field, carried out both on the field and photogrammetric and LIDAR surveys from UASs, in order to estimate the erupted lava volume and to reconstruct the sequence of events and infer a possible duration and impact of the eruption. The analysis of the surveys allowed us to verify the contact with previous lava flow fields, allowing a more precise lateral extension of the lava delta along the coast, as well as an estimation of the thickness and volume, at least for the subaerial portion of the lava flow field. The morphology analysis of the lava flow field allowed us to recognize structures suggesting inflation and then stationing of the lava flow fronts, features indicating a long-lasting eruption and a complex interaction with the sea. Our results can provide a useful scenario should a flank eruption occur in the future, a possibility that was close to happening in 1998, when the ground deformation stations revealed a lateral intrusion in the shallow supply system of the volcano.

 

 

How to cite: Vicari, A., Famiglietti, N., Calvari, S., Marotta, E., Avino, R., Belviso, P., Harris, A., De Luca, G., Memmolo, A., Minichiello, F., and Peluso, R.: The San Bartolo lava flow field, Stromboli volcano, Italy: Reconstruction of the most recent historic flank eruption (2 kyr) affecting the inhabited area by photogrammetric and LIDAR from UASs aimed at hazard assessment, EGU General Assembly 2023, Vienna, Austria, 24–28 Apr 2023, EGU23-16651, https://doi.org/10.5194/egusphere-egu23-16651, 2023.