An inclined Vulcanian explosion and associated products.
| dc.contributor.author | Cole, P. D | |
| dc.contributor.author | Stinton, A. J | |
| dc.contributor.author | Odbert, H. M | |
| dc.contributor.author | Bonadonna, C | |
| dc.contributor.author | Stewart, R. C | |
| dc.date.accessioned | 2026-02-20T19:23:59Z | |
| dc.date.created | 2015 | |
| dc.description.abstract | Vulcanian explosions generate some of the most hazardous types of volcanic phenomena, including pyroclastic density currents. Non-vertical directionality of an explosion promotes asymmetrical distribution of proximal hazards around the volcano. Although critical, such behaviour is relatively uncommon and has been seldom documented. Here we present, for the first time, evidence both from geophysical monitoring and field survey data that records the occurrence of such an event. Thermal imagery captures a Vulcanian explosion at Soufrière Hills Volcano, Montserrat, which occurred during a large partial lava dome collapse in February 2010, and was inclined at about 25° from the vertical in a northerly direction. | |
| dc.identifier | https://doi.org/10.1144/jgs2014-099 | |
| dc.identifier.uri | https://hdl.handle.net/2139/58431 | |
| dc.publisher | Geological Society of London | |
| dc.relation.ispartofseries | Journal of the Geological Society, volume 172, number 3, 287–293 | |
| dc.subject.lcsh | Soufrière Hills Volcano, Montserrat | |
| dc.subject.lcsh | Pyroclastic | |
| dc.subject.lcsh | Geophysical monitoring | |
| dc.title | An inclined Vulcanian explosion and associated products. | |
| dc.type |
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