Seismic and volcanic activity at Soufrière Hills were at elevated levels during 17-24 June. The seismic network at the volcano recorded 8 hybrid earthquakes, 5 long-period earthquakes, 4 volcano-tectonic earthquakes, and 3 rockfalls. On 27 June a steam and ash cloud at ~3 km (9,800 ft) a.s.l. was reported to be drifting W. The daily recorded sulphur dioxide flux varied from a low of 430 metric tons per day (t/d) on 20 June, to a maximum of 1150 t/d on 23 June, with an average of 627 t/d for the week. By 28 June satellite imagery shows a plume of ash and steam at ~1.8 km (5,900 ft) a.s.l. extending NW of the volcano.

Geological Summary. 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.

Sources: Montserrat Volcano Observatory (MVO), Washington Volcanic Ash Advisory Center (VAAC)