Previous studies performed on Mt. Etna on short and discontinuous time intervals indicate the North East Crater (NEC) as the most active source of infrasound. The source mechanism of NEC infrasound events was modeled as a double resonance. This lead to infer the connection between the NEC and both the southeast crater (SEC) and the eruptive fissure (EF), that opened at the beginning of the 2008–2009 eruption. Nevertheless, there are still several open questions that need to be addressed. For instance, the steadiness of NEC event features should be studied, as well as the orderliness of spectral changes of NEC events time-related to eruptive activity of other vents. The investigation of such topics is strongly enhanced by the possibility of ...
Active volcanoes characterized by open conduit conditions generate sonic and infrasonic signals, who...
Active volcanoes characterized by open conduit conditions generate sonic and infrasonic signals, who...
A fundamental goal of volcano seismology is to understand the dynamics of active magmatic systems i...
On 13 May 2008, an eruption began at Mt. Etna from an eruptive fissure that opened on the upper eas...
Active volcanoes produce inaudible infrasound due to the coupling between surface magmatic processes...
The success in eruption forecasting needs the knowledge of the eruptive processes and the plumbing s...
The period September–November 2007 was characterized at Mount Etna by explosive activity and intense...
In December 2018, Mount Etna (Italy) experienced a period of increased eruptive activity that culmin...
On 16 November 2006, a 1 day long paroxysmal eruption occurred at the summit craters of Mt. Etna vo...
Infrasound is increasing applied as a tool to investigate magma dynamics at active volcanoes, especi...
Following the installation of a broadband network on Mt. Etna, sustained Long- Period (LP) activity ...
Between January 2011 and April 2013, Mt. Etna's eruptive activity consisted of episodic intra-crater...
Volcanic tremor and low frequency events, together with infrasound signals, can represent important ...
An edited version of this paper was published by AGU. Copyright (2009) American Geophysical Union.On...
Active volcanoes characterized by open conduit conditions generate sonic and infrasonic signals, who...
Active volcanoes characterized by open conduit conditions generate sonic and infrasonic signals, who...
A fundamental goal of volcano seismology is to understand the dynamics of active magmatic systems i...
On 13 May 2008, an eruption began at Mt. Etna from an eruptive fissure that opened on the upper eas...
Active volcanoes produce inaudible infrasound due to the coupling between surface magmatic processes...
The success in eruption forecasting needs the knowledge of the eruptive processes and the plumbing s...
The period September–November 2007 was characterized at Mount Etna by explosive activity and intense...
In December 2018, Mount Etna (Italy) experienced a period of increased eruptive activity that culmin...
On 16 November 2006, a 1 day long paroxysmal eruption occurred at the summit craters of Mt. Etna vo...
Infrasound is increasing applied as a tool to investigate magma dynamics at active volcanoes, especi...
Following the installation of a broadband network on Mt. Etna, sustained Long- Period (LP) activity ...
Between January 2011 and April 2013, Mt. Etna's eruptive activity consisted of episodic intra-crater...
Volcanic tremor and low frequency events, together with infrasound signals, can represent important ...
An edited version of this paper was published by AGU. Copyright (2009) American Geophysical Union.On...
Active volcanoes characterized by open conduit conditions generate sonic and infrasonic signals, who...
Active volcanoes characterized by open conduit conditions generate sonic and infrasonic signals, who...
A fundamental goal of volcano seismology is to understand the dynamics of active magmatic systems i...