Data of the flank eruptions of Etna from over the last 400 years were extracted from the new geological map for the lava flow extensions and vent positions, and from the catalogs of historical eruptions for the eruption durations and lava volumes. The partially or widely hidden lava fields on the new geological map were retrieved from older geological maps. The distributions of the eruption durations and lava volumes were analyzed, with the definition of six eruptive classes for use in numerical simulations. The threshold values for the eruption durations and lava volumes were set at 45 days and at 35 × 106 m3 and 100 × 106 m3, respectively. A global analysis was performed on the whole volcano to evaluate the recurrence of the classes, and ...
Knowledge of Etna's eruptions has been profoundly influenced by the illustrations, though these can ...
The 2002-03 Mt Etna flank eruption began on 26 October and finished on 28 January 2003, after three...
Mount Etna is an open conduit volcano, characterised by persistent activity, consisting of degassing...
Data of the flank eruptions of Etna from over the last 400 years were extracted from the new geologi...
[1] Mount Etna despite being an extremely active volcano which, during the last 400 years, has produ...
Mount Etna despite being an extremely active volcano which, during the last 400 years, has produced ...
Lava flows produced during Etna flank eruptions represent severe hazards for the nearby inhabited ar...
Invasion of inhabited areas and destruction of human property by lava flows represents the greatest ...
We analyzed the space–time distribution of the lateral eruptions of Mt Etna during the last 5centuri...
Improving lava flow hazard assessment is one of the most important and challenging fields of volcano...
A methodology for constructing a probability map of lava inundation by considering the past eruptive...
This special issue of Annals of Geophysics contains seventeen peer-reviewed papers that cover a wide...
The 1669 AD flank eruption was the most destructive event on Etna volcano in historical times (~700 ...
This report presents a retrospective methodology to validate a long-term hazard map related to lava-...
The formation of new craters or cones in active volcanoes can influence the style and frequency of ...
Knowledge of Etna's eruptions has been profoundly influenced by the illustrations, though these can ...
The 2002-03 Mt Etna flank eruption began on 26 October and finished on 28 January 2003, after three...
Mount Etna is an open conduit volcano, characterised by persistent activity, consisting of degassing...
Data of the flank eruptions of Etna from over the last 400 years were extracted from the new geologi...
[1] Mount Etna despite being an extremely active volcano which, during the last 400 years, has produ...
Mount Etna despite being an extremely active volcano which, during the last 400 years, has produced ...
Lava flows produced during Etna flank eruptions represent severe hazards for the nearby inhabited ar...
Invasion of inhabited areas and destruction of human property by lava flows represents the greatest ...
We analyzed the space–time distribution of the lateral eruptions of Mt Etna during the last 5centuri...
Improving lava flow hazard assessment is one of the most important and challenging fields of volcano...
A methodology for constructing a probability map of lava inundation by considering the past eruptive...
This special issue of Annals of Geophysics contains seventeen peer-reviewed papers that cover a wide...
The 1669 AD flank eruption was the most destructive event on Etna volcano in historical times (~700 ...
This report presents a retrospective methodology to validate a long-term hazard map related to lava-...
The formation of new craters or cones in active volcanoes can influence the style and frequency of ...
Knowledge of Etna's eruptions has been profoundly influenced by the illustrations, though these can ...
The 2002-03 Mt Etna flank eruption began on 26 October and finished on 28 January 2003, after three...
Mount Etna is an open conduit volcano, characterised by persistent activity, consisting of degassing...