(1) Passive dome growth still generates myriad red hot cascades of rocks during the recent eruption of Soufrière Hills Volcano, Montserrat. Photo: Paul Cole
(2) One of the 32 explosive eruptions that occurred in April 2021 at Soufrière, St Vincent. Photo Richie Robertson.
(3) Cumulative ash from explosions can have a profound impact on infrastructure. Roof collapse, on St Vincent, May 2021.
(4) View of the new volcanic crater of Soufrière, St Vincent. Take during Ex-X fieldwork December 2025. Photo Paul Cole
(5) Amelia Bain and Richie Robertson discuss the changes to the Soufriere, St Vincent crater, taken December 2025. Photo Paul Cole.
(6) Leanka Henry from the Soufriere Monitoring Unit at the National Emergency Organisation, St Vincent taking routine gas measurements at the crater in 2022. Photo Jenni Barclay
(7) Dome-forming eruptions frequently collapse generating fast-moving, hot pyroclastic flows. Here flows from Soufrière Hills Volcano are travelling over the sea. Photo: Paul Cole
(8) These pyroclastic flows also throw ash up in the air in hot convecting plumes. Soufriere Hills volcano, Montserrat. Photo: Paul Cole.
(9) Pyroclastic flows can travel rapidly downhill, and the rising ash dispersed over wide areas. Soufriere Hills Volcano, Montserrat. Photo: Paul Cole
