International audienceInfrasonic and seismic waveforms were collected during violent strombolian activity at Yasur Volcano (Vanuatu). Averaging ~3000 seismic events showed stable waveforms, evidencing a low-frequency (0.1–0.3 Hz) signal preceding ~5–6 s the explosion. Infrasonic waveforms were mostly asymmetric with a sharp compressive (5–106 Pa) onset, followed by a small long-lasting rarefaction phase. Regardless of the pressure amplitude, the ratio between the positive and negative phases was constant. These waveform characteristics closely resembled blast waves. Infrared imagery showed an apparent cold spherical front ~20 m thick, which moved between 342 and 405 m/s before the explosive hot gas/fragments cloud. We interpret this cold fr...
Yasur is a small stratovolcano located inside a large caldeira, in the south-eastern part of Tanna I...
In order to clarify the time relation of the expansion of a gas pocket and failure of its overlying ...
We demonstrate the rise and expansion of a gas slug as a fluid dynamic source mechanism for infrason...
International audienceInfrasonic and seismic waveforms were collected during violent strombolian act...
In late 2008 we recorded a continuous multi-parameter data set including Doppler radar, infrared and...
International audienceThe seismic wavefield associated with Strombolian activity is usually dominate...
Volcanic processes occur in a wide range of temporal and spatial scales. However, a key step of magm...
Volcanic processes occur in a wide range of temporal and spatial scales. However, a key step of magm...
Volcanic processes occur in a wide range of temporal and spatial scales. However, a key step of magm...
We examined one year of seismic recordings collected in 2008 during a temporary experiment at Yasur ...
Yasur volcano, Vanuatu is a continuously active open-vent basaltic-andesite stratocone with persiste...
We explore the capabilities of volcano opto-acoustics, a promising technique for measuring explosion...
Analysis of infrasonic pressure waves generated by active volcanoes is essential to the understandin...
The origin of the volcanic tremor is still under debate. Many theories have been proposed in the las...
Yasur is a small stratovolcano located inside a large caldeira, in the south-eastern part of Tanna I...
In order to clarify the time relation of the expansion of a gas pocket and failure of its overlying ...
We demonstrate the rise and expansion of a gas slug as a fluid dynamic source mechanism for infrason...
International audienceInfrasonic and seismic waveforms were collected during violent strombolian act...
In late 2008 we recorded a continuous multi-parameter data set including Doppler radar, infrared and...
International audienceThe seismic wavefield associated with Strombolian activity is usually dominate...
Volcanic processes occur in a wide range of temporal and spatial scales. However, a key step of magm...
Volcanic processes occur in a wide range of temporal and spatial scales. However, a key step of magm...
Volcanic processes occur in a wide range of temporal and spatial scales. However, a key step of magm...
We examined one year of seismic recordings collected in 2008 during a temporary experiment at Yasur ...
Yasur volcano, Vanuatu is a continuously active open-vent basaltic-andesite stratocone with persiste...
We explore the capabilities of volcano opto-acoustics, a promising technique for measuring explosion...
Analysis of infrasonic pressure waves generated by active volcanoes is essential to the understandin...
The origin of the volcanic tremor is still under debate. Many theories have been proposed in the las...
Yasur is a small stratovolcano located inside a large caldeira, in the south-eastern part of Tanna I...
In order to clarify the time relation of the expansion of a gas pocket and failure of its overlying ...
We demonstrate the rise and expansion of a gas slug as a fluid dynamic source mechanism for infrason...