Regular surveys with a PM695 FLIR thermal imaging camera from both the ground and from helicopter were conducted on Stromboli from October 2001. These measurements allow us to (i) examine changes in morphology of the summit craters produced by paroxystic explosions and (ii) track the increasing level of magma within the conduits of Stromboli that preceded and led to the 2002/03 effusive eruption. Two geophysical surveys in May and September/October 2002 demonstrated a clear increasing trend in the amplitude of VLP events, consistent with the presence of a higher magma column above the VLP source region. The observed increase in magma level was probably induced by an increase in the pressure of the magma feeding system at Stromboli, controll...
On 28 December 2002, the persistent Strombolian activity at Stromboli was interrupted by the sudden ...
The 5 April 2003 paroxysmal explosion at Stromboli volcano was one of the strongest explosive events...
On 28 December 2002, the persistent Strombolian activity at Stromboli was interrupted by the sudden ...
Regular surveys with a PM695 FLIR thermal imaging camera from both the ground and from helicopter we...
Effusive activity at Stromboli is uncommon, and the 2002–2003 flank eruption gave us the opportunity...
This work arises from the field observations made during the civil protection emergency period conne...
Twenty eruptive events from the Northeast Crater of Stromboli volcano recorded by a thermal monitor...
On 28 December 2002, the persistent Strombolian activity at Stromboli was interrupted by the sudden ...
On February 27, 2007, the Stromboli volcano, which has usually been characterized by moderate explos...
The 5 April 2003 eruption of Stromboli volcano (Italy) was the most violent in the past 50 years. It...
At Stromboli volcano, Italy, continuous seismic monitoring and periodic, visual observations of volc...
Using thermal infrared images recorded by a permanent thermal camera network maintained on Stromboli...
The 5 April 2003 eruption of Stromboli volcano (Italy) was the most violent of the past 50 years. It...
Using thermal infrared images recorded by a permanent thermal camera network maintained on Stromboli...
At 18:20 of 28 December 2002 an eruptive vent opened on the NE flank of the Sciara del Fuoco at 600 ...
On 28 December 2002, the persistent Strombolian activity at Stromboli was interrupted by the sudden ...
The 5 April 2003 paroxysmal explosion at Stromboli volcano was one of the strongest explosive events...
On 28 December 2002, the persistent Strombolian activity at Stromboli was interrupted by the sudden ...
Regular surveys with a PM695 FLIR thermal imaging camera from both the ground and from helicopter we...
Effusive activity at Stromboli is uncommon, and the 2002–2003 flank eruption gave us the opportunity...
This work arises from the field observations made during the civil protection emergency period conne...
Twenty eruptive events from the Northeast Crater of Stromboli volcano recorded by a thermal monitor...
On 28 December 2002, the persistent Strombolian activity at Stromboli was interrupted by the sudden ...
On February 27, 2007, the Stromboli volcano, which has usually been characterized by moderate explos...
The 5 April 2003 eruption of Stromboli volcano (Italy) was the most violent in the past 50 years. It...
At Stromboli volcano, Italy, continuous seismic monitoring and periodic, visual observations of volc...
Using thermal infrared images recorded by a permanent thermal camera network maintained on Stromboli...
The 5 April 2003 eruption of Stromboli volcano (Italy) was the most violent of the past 50 years. It...
Using thermal infrared images recorded by a permanent thermal camera network maintained on Stromboli...
At 18:20 of 28 December 2002 an eruptive vent opened on the NE flank of the Sciara del Fuoco at 600 ...
On 28 December 2002, the persistent Strombolian activity at Stromboli was interrupted by the sudden ...
The 5 April 2003 paroxysmal explosion at Stromboli volcano was one of the strongest explosive events...
On 28 December 2002, the persistent Strombolian activity at Stromboli was interrupted by the sudden ...