scholarly journals The intrusive process leading to the Mt. Etna 2001 flank eruption: Constraints from 3-D attenuation tomography

2005 ◽  
Vol 32 (21) ◽  
Author(s):  
Carmen Martínez-Arévalo ◽  
Domenico Patanè ◽  
Andreas Rietbrock ◽  
Jesús M. Ibánez
Keyword(s):  
Flank Eruption ◽  
Mt Etna

Seismological constraints on the 2018 Mt. Etna (Italy) flank eruption and implications for the flank dynamics of the volcano

Terra Nova ◽  
2020 ◽  
Vol 32 (5) ◽  
pp. 334-344 ◽  
Author(s):  
Salvatore Alparone ◽  
Graziella Barberi ◽  
Elisabetta Giampiccolo ◽  
Vincenza Maiolino ◽  
Antonino Mostaccio ◽  
...  
Keyword(s):  
Flank Eruption ◽  
Mt Etna

Chronicle of the 1865, NE flank eruption of Mt. Etna and geomorphologic survey of the Mts. Sartorius area

2011 ◽  
Vol 73 (9) ◽  
pp. 1155-1162 ◽  
Author(s):  
Pietro Carveni ◽  
Giuliana Mele ◽  
Santo Benfatto ◽  
Sebastiano Imposa ◽  
Maria Salleo Puntillo
Keyword(s):  
Flank Eruption ◽  
Mt Etna

scholarly journals Results of a reconnaissance trip to Mt. Etna, Italy

2004 ◽  
Vol 37 (2) ◽  
pp. 47-61 ◽  
Author(s):  
Scott T. Barnard
Keyword(s):  
New Zealand ◽  
Seismic Activity ◽  
Unreinforced Masonry ◽  
Lava Flows ◽  
Masonry Structures ◽  
Flank Eruption ◽  
Mt Etna

This paper details the observations taken from a reconnaissance trip to Mt. Etna, Italy during the 2002 flank eruption, and utilizes those observations to identify potential hazards in New Zealand. It also makes recommendations for preparation and response to those hazards. The various types of hazards posed by Etna are primarily lava flows, ashfall and earthquakes. Lava flows caused intense damage in proximal areas, including forests, roads and the destruction of ski lifts and several buildings. Ashfall affected a much larger area, and was thus responsible for most of the damage economically. While earthquakes were not severe by New Zealand standards, the unreinforced masonry structures that predominate on Etna did not cope well with the seismic activity that accompanied the eruption. Several lessons taken from this eruption are applicable to New Zealand, both in effects of basaltic and more silicic types of volcanism.

Petrology of lavas from the 2004–2005 flank eruption of Mt. Etna, Italy: inferences on the dynamics of magma in the shallow plumbing system

2009 ◽  
Vol 71 (7) ◽  
pp. 781-793 ◽  
Author(s):  
Rosa Anna Corsaro ◽  
Lucia Civetta ◽  
Valeria Di Renzo ◽  
Lucia Miraglia
Keyword(s):  
Flank Eruption ◽  
Plumbing System ◽  
Mt Etna

scholarly journals Erratum to: Chronicle of the 1865, NE flank eruption of Mt. Etna and geomorphologic survey of the Mts. Sartorius area

2011 ◽  
Vol 73 (9) ◽  
pp. 1163-1163
Author(s):  
Pietro Carveni ◽  
Giuliana Mele ◽  
Santo Benfatto ◽  
Sebastiano Imposa ◽  
Maria Salleo Puntillo
Keyword(s):  
Flank Eruption ◽  
Mt Etna

Identification of Radon Anomalies at Mt. Etna (Sicily) by Using Three Different Methods

2010 ◽  
Vol 3 (1) ◽  
pp. 1-16 ◽  
Author(s):  
S. La Delfa ◽  
F. Vizzini ◽  
G. Patanè
Keyword(s):  
Mt Etna
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