A porous flow model of flank eruptions on Mt. Etna: second-order perturbation theory
A porous flow model for magma migration from a deep source within a volcanic edifice is developed. The model is based on the assumption that an isotropic and homogeneous system of fractures allows magma migration from one localized feeding dyke up to the surface of the volcano. The maximum level tha...
Main Authors: | N. Cenni, M. Bonafede |
---|---|
Format: | Article |
Language: | English |
Published: |
Istituto Nazionale di Geofisica e Vulcanologia (INGV)
1997-06-01
|
Series: | Annals of Geophysics |
Subjects: | |
Online Access: | http://www.annalsofgeophysics.eu/index.php/annals/article/view/3848 |
Similar Items
-
Coupling Flank Collapse and Magma Dynamics on Stratovolcanoes: The Mt. Etna Example from InSAR and GNSS Observations
by: Giuseppe Pezzo, et al.
Published: (2023-02-01) -
Etna Output Rate during the Last Decade (2011–2022): Insights for Hazard Assessment
by: Sonia Calvari, et al.
Published: (2022-12-01) -
Magma ascent and degassing processes of the 2011 and 2017–18 eruptions of Shinmoedake in Kirishima volcano group, Japan, based on petrological characteristics and volatile content of magmas
by: Genji Saito, et al.
Published: (2023-05-01) -
Effusion Rates on Mt. Etna and Their Influence on Lava Flow Hazard Assessment
by: Francesco Zuccarello, et al.
Published: (2022-03-01) -
The Christmas 2018 Eruption at Mount Etna: Enlightening How the Volcano Factory Works Through a Multiparametric Inspection
by: Alfio Marco Borzi, et al.
Published: (2020-10-01)