Open-vent activity at volcanoes of low-silica composition, such as Stromboli (Italy), Villarrica (Chile), Mt. Erebus (Antarctica), Masaya (Nicaragua), is characterised by persistent passive gas emission and recurrent mild explosive outgassing. Four styles of bubble bursting activity have been recognised in such volcanoes: seething magma, small short-lived lava fountains, strombolian explosions and gas puffing. Whilst strombolian explosions are perhaps the most common among these volcanoes, seething magma and small lava fountains have been observed only at the surface of active lava lakes. At Villarrica, one of the two case study volcanoes of this thesis, seething magma consists of continual bursts of bubbles up to a few meters in diameter, ...
[1] In this paper we look at changes of the statistics of the stationary explosive process at a basa...
Ash fallout collected during 4 days of sampling at Stromboli confirms that a crystal-rich (HP) degas...
Investigating Etna’s long-term SO2 flux behaviour has led to important conclusions on the structure o...
Open-vent activity at volcanoes of low-silica composition, such as Stromboli (Italy), Villarrica (Ch...
The characteristics of the open vent activity of Villarrica volcano, Chile, were studied in detail b...
Visually unattainable magmatic processes in volcanic conduits, such as degassing, are closely linked...
Co-auteur étrangerInternational audienceVisually unattainable magmatic processes in volcanic conduit...
Stromboli is a persistently active, open-vent basaltic volcano whose activity is controlled by the b...
Open-vent, persistently degassing volcanoes—such as Stromboli and Etna (Italy), Villarrica (Chile), ...
The characteristics of the open vent activity of Villarrica volcano, Chile, were studied in detail b...
Explosive activity at Stromboli is explained in terms of dynamics of large gas bubbles that ascend i...
Quiescent and explosive magma degassing at Stromboli volcano sustain high temperature crater gas ve...
Basaltic activity is the most common class of volcanism on Earth, characterized by magmas of suffici...
[1] In this paper we look at changes of the statistics of the stationary explosive process at a basa...
Ash fallout collected during 4 days of sampling at Stromboli confirms that a crystal-rich (HP) degas...
Investigating Etna’s long-term SO2 flux behaviour has led to important conclusions on the structure o...
Open-vent activity at volcanoes of low-silica composition, such as Stromboli (Italy), Villarrica (Ch...
The characteristics of the open vent activity of Villarrica volcano, Chile, were studied in detail b...
Visually unattainable magmatic processes in volcanic conduits, such as degassing, are closely linked...
Co-auteur étrangerInternational audienceVisually unattainable magmatic processes in volcanic conduit...
Stromboli is a persistently active, open-vent basaltic volcano whose activity is controlled by the b...
Open-vent, persistently degassing volcanoes—such as Stromboli and Etna (Italy), Villarrica (Chile), ...
The characteristics of the open vent activity of Villarrica volcano, Chile, were studied in detail b...
Explosive activity at Stromboli is explained in terms of dynamics of large gas bubbles that ascend i...
Quiescent and explosive magma degassing at Stromboli volcano sustain high temperature crater gas ve...
Basaltic activity is the most common class of volcanism on Earth, characterized by magmas of suffici...
[1] In this paper we look at changes of the statistics of the stationary explosive process at a basa...
Ash fallout collected during 4 days of sampling at Stromboli confirms that a crystal-rich (HP) degas...
Investigating Etna’s long-term SO2 flux behaviour has led to important conclusions on the structure o...