The third episode of lava dome growth at Soufrière Hills Volcano began 1 August 2005 and ended 20 April 2007. Volumes of the dome and talus produced were measured using a photo-based method with a calibrated camera for increased accuracy. The total dense rock equivalent (DRE) volume of extruded andesite magma (306 ± 51 Mm3) was similar within error to that produced in the earlier episodes but the average extrusion rate was 5.6 ± 0.9 m3s−1 (DRE), higher than the previous episodes. Extrusion rates varied in a pulsatory manner from <0.5 m3s−1 to ∼20 m3s−1. On 18 May 2006, the lava dome had reached a volume of 85 Mm3 DRE and it was removed in its entirety during a massive dome collapse on 20 May 2006. Extrusion began again almost immediately an...
International audienceThe dynamics of the 2-12 January 2010 effusive eruption at Piton de la Fournai...
The lava dome collapse of 12–13 July 2003 was the largest of the Soufrière Hills Volcano eruption th...
During many lava dome-forming eruptions, persistent rockfalls and the concurrent development of a su...
The third episode of lava dome growth at Soufrière Hills Volcano began 1 August 2005 and ended 20 Ap...
The third episode of lava dome growth at Soufrière Hills Volcano began 1 August 2005 and ended 20 Ap...
[1] We estimate that about 1 km3 of andesitic lava has been produced at Soufrière Hills Volcano, M...
The third episode of lava dome growth at Soufrière Hills Volcano, Montserrat was characterised by hi...
A second extrusive phase of the currently ongoing 1995–2003 eruption of Soufrière Hills Volcano (SHV...
The 1995–present eruption of Soufrière Hills Volcano on Montserrat has produced over a cubic kilomet...
Exogenous growth of Peléean lava domes involves the addition of lava from a central summit vent and ...
In 2005 Soufrière Hills Volcano on Montserrat started its third major episode of dome growth since t...
In 2005 Soufrière Hills Volcano on Montserrat started its third major episode of dome growth since t...
The tiny Caribbean island of Montserrat has been in a state of crisis since the Soufrière Hills Volc...
The lava dome collapse of 12-13 July 2003 was the largest of the Soufrière Hills Volcano eruption th...
The formation of a lava dome involves fractionation of the lava into core and clastic components. We...
International audienceThe dynamics of the 2-12 January 2010 effusive eruption at Piton de la Fournai...
The lava dome collapse of 12–13 July 2003 was the largest of the Soufrière Hills Volcano eruption th...
During many lava dome-forming eruptions, persistent rockfalls and the concurrent development of a su...
The third episode of lava dome growth at Soufrière Hills Volcano began 1 August 2005 and ended 20 Ap...
The third episode of lava dome growth at Soufrière Hills Volcano began 1 August 2005 and ended 20 Ap...
[1] We estimate that about 1 km3 of andesitic lava has been produced at Soufrière Hills Volcano, M...
The third episode of lava dome growth at Soufrière Hills Volcano, Montserrat was characterised by hi...
A second extrusive phase of the currently ongoing 1995–2003 eruption of Soufrière Hills Volcano (SHV...
The 1995–present eruption of Soufrière Hills Volcano on Montserrat has produced over a cubic kilomet...
Exogenous growth of Peléean lava domes involves the addition of lava from a central summit vent and ...
In 2005 Soufrière Hills Volcano on Montserrat started its third major episode of dome growth since t...
In 2005 Soufrière Hills Volcano on Montserrat started its third major episode of dome growth since t...
The tiny Caribbean island of Montserrat has been in a state of crisis since the Soufrière Hills Volc...
The lava dome collapse of 12-13 July 2003 was the largest of the Soufrière Hills Volcano eruption th...
The formation of a lava dome involves fractionation of the lava into core and clastic components. We...
International audienceThe dynamics of the 2-12 January 2010 effusive eruption at Piton de la Fournai...
The lava dome collapse of 12–13 July 2003 was the largest of the Soufrière Hills Volcano eruption th...
During many lava dome-forming eruptions, persistent rockfalls and the concurrent development of a su...