American Geophysical Union Become an AGU Member
Subscribe to AGU Journals
AGU Home AGU Publications

Read Full Article (file size: 553068 bytes)    Cited by

GEOPHYSICAL RESEARCH LETTERS, VOL. 29, NO. 13, 1624, doi:10.1029/2001GL014397, 2002

Dike emplacement forerunning the Etna July 2001 eruption modeled through continuous tilt and GPS data

A. Bonaccorso

Istituto Nazionale di Geofisica e Vulcanologia–Sezione di Catania, Piazza Roma, Catania, Italy


M. Aloisi

Istituto Nazionale di Geofisica e Vulcanologia–Sezione di Catania, Piazza Roma, Catania, Italy


M. Mattia

Istituto Nazionale di Geofisica e Vulcanologia–Sezione di Catania, Piazza Roma, Catania, Italy


Abstract

Late on the night of July 17, 2001, a lateral eruption started from the slopes of Mt. Etna. A 7 km long field of ground fractures opened between 13 and 20 July. The eruption ended on August 9, 2001 after emitting a lava volume of approximately 48 · 106 m3. A strong seismic swarm earthquake was recorded between July 12 and 17. The evolution leading up to the July crisis was monitored through continuous tilt and GPS measurements, which constrained the intrusion preceding the eruption in time, and inferred the position and geometry of the uprising dike. We modeled the marked ground deformation changes recorded in the days before the eruption onset. The result shows that a tensile crack with an opening dislocation of ca. 3 m, crossing the volcano edifice slightly southeast of the crater area, can explain the recorded deformation pattern. The location of the modeled tensile source fits the zone of the seismic swarm occurring during the magma uprising. The ground deformation pattern associated with the final uprising and its modeling suggest a very fast dike emplacement which appears different, both in terms of rapidity (only a few days) and source position, with respect to the sources modeled for the other lateral eruptions in the last twenty years.

Published 2 July 2002.

Index Terms: 1204 Geodesy and Gravity: Control surveys; 5104 Physical Properties of Rocks: Fracture and flow; 8414 Volcanology: Eruption mechanisms; 8419 Volcanology: Eruption monitoring (7280).


Read Full Article (file size: 553068 bytes)    Cited by

Citation: Bonaccorso, A., M. Aloisi, and M. Mattia (2002), Dike emplacement forerunning the Etna July 2001 eruption modeled through continuous tilt and GPS data, Geophys. Res. Lett., 29(13), 1624, doi:10.1029/2001GL014397.