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Volcanic processes, products and hazards |
1 Montserrat Volcano Observatory, , Mongo Hill, Montserrat, West Indies
2 Department of Geosciences, Penn State University, , University Park PA16802, USA
3 School of Environmental Sciences, University of East Anglia, , Norwich NR4 7TJ, UK
4 British Geological Survey, , Keyworth, Nottingham NG12 5GG, UK
5 OVS-IPGP, , Le Houlement 97113, Guadeloupe, West Indies
6 Geowalks, , 23 Summerfield Place, Edinburgh EH6 8AZ, UK
7 Earth Sciences Department, University of Bristol, , Queen's Road, Bristol BS8 1RJ, UK
8 Preparatory Commission for the CTBTO, , PO Box 1250, A-1400 Wien, Austria
During the 1995 to 1998 phase of dome growth at Soufrière Hills Volcano on Montserrat, we documented instability of the steep southern rim of English's Crater, known as Galway's Wall. The horseshoe-shaped English's Crater provided good evidence for previous sector collapses, and assessments undertaken in late 1996 anticipated the possibility of a partial sector collapse and a SW-directed explosion, hazards previously unrecognized on Montserrat.
A change from predominantly endogenous to exogenous growth of the lava dome at the end of 1996 eased the stress on the southern sector. However, rapid dome growth in November and December 1997 led to severe reloading and eventual sector failure at the base of the buried Galway's Wall and in the adjacent hot-spring area. This failure resulted in the debris avalanche and lateral blast of 26 December 1997.
Similar sector collapses at a number of small volcanoes in the Caribbean, as well as worldwide, are evidence that edifice instability develops commonly in dome-forming eruptions. The hazards from a sector collapse and a consequent lateral blast are extreme, and monitoring operations and disaster planning at such volcanoes should focus on these, as well as on the more common hazards of conventional pyroclastic flows associated with dome growth.
