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Report on Soufriere Hills (United Kingdom) — 1 June-7 June 2005

Smithsonian / US Geological Survey Weekly Volcanic Activity Report, 1 June-7 June 2005
Managing Editor: Gari Mayberry

Please cite this report as:

Global Volcanism Program, 2005. Report on Soufriere Hills (United Kingdom). In: Mayberry, G (ed.), Weekly Volcanic Activity Report, 1 June-7 June 2005. Smithsonian Institution and US Geological Survey.

Volcano Profile |  Weekly Report (1 June-7 June 2005)


Soufriere Hills

United Kingdom

16.72°N, 62.18°W; summit elev. 915 m

All times are local (unless otherwise noted)


The seismic network at Soufrière Hills recorded 8 volcano-tectonic earthquakes during 27 May to 3 June. Steam venting continued on the NW side of the crater. The daily recorded sulfur-dioxide flux ranged from a low of 167 metric tons per day (t/d) on 2 June to a maximum of 392 t/d on 30 May, with an average of 261 t/d for the week. This was below the long-term eruption average of 500 t/d.

Geologic Background. The complex, dominantly andesitic Soufrière Hills volcano occupies the southern half of the island of Montserrat. The summit area consists primarily of a series of lava domes emplaced along an ESE-trending zone. The volcano is flanked by Pleistocene complexes to the north and south. English's Crater, a 1-km-wide crater breached widely to the east by edifice collapse, was formed about 2000 years ago as a result of the youngest of several collapse events producing submarine debris-avalanche deposits. Block-and-ash flow and surge deposits associated with dome growth predominate in flank deposits, including those from an eruption that likely preceded the 1632 CE settlement of the island, allowing cultivation on recently devegetated land to near the summit. Non-eruptive seismic swarms occurred at 30-year intervals in the 20th century, but no historical eruptions were recorded until 1995. Long-term small-to-moderate ash eruptions beginning in that year were later accompanied by lava-dome growth and pyroclastic flows that forced evacuation of the southern half of the island and ultimately destroyed the capital city of Plymouth, causing major social and economic disruption.

Source: Montserrat Volcano Observatory (MVO)