Dome collapse and explosive activity at Soufriere Hills Volcano

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Dome collapse and explosive activity at Soufriere Hills Volcano
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From: Sue Loughlin <sue@xxxxxx>


Montserrat Volcano Observatory
Montserrat, W.I.

Interim report for the period midday 19 May to midday 22 May 2006

A major lava dome collapse took place at the Soufriere Hills Volcano on the
morning of 20 May 2006. A helicopter flight in the afternoon confirmed that most
of the lava dome has gone, together with some remnants of the 2003 lava dome,
leaving a broad, deep, eastward-sloping crater at the summit of the volcano. The
volume of the lava dome was believed to be about 90 million cubic metres and
most of this collapsed over a period of less than three hours. Views of the
western part of the crater where ash venting is continuing were not possible but
it is unlikely that there is significant dome material remaining there. 

There was a single precursor long period seismic event 3km below the dome at
2:22am local time on 20 May. A brief episode of heightened seismic amplitude
corresponding to ash venting occurred at 3-3:30am.

During heavy rain, another episode of increased seismic amplitude, interpreted
as ash venting, began at 5:52am and this gradually increased and developed into
a high amplitude seismic signal. The heavy rain was causing mudflows in Belham
River valley at this time. By 06:32 low-level ash clouds were drifting to the
northwest of the volcano from the crater area and a steam-rich plume was rising
to 6,000ft. Unconfirmed reports suggest that pyroclastic flows first reached the
sea at about 06:45. 

Regular pulses of pyroclastic flows were reaching the sea down the Tar River
valley by 07:20 with major pulses recorded in seismic amplitude at 07:36, 07:43
and between 08:01 and 08:04. Also between 07:30 and 08:10 a number of
long-period seismic events were detected.

At 07:40 an ash cloud was reported at nearly 17km (55,000ft) the highest
reported ash cloud during the ten years of the eruption. At 07:43 pyroclastic
surges were observed spreading across the northeastern flanks of the volcano
reaching the Spanish Point area. It was also estimated that surges had spread
3km offshore from Tar River valley, across the surface of the ocean. 

By 07:50 lithics (pieces of lava dome) were falling in areas northwest of the
volcano, most were less than 3.5 cm across, the largest found in the inhabited
area was 6cm across. Six car windscreens were reported broken. The deepest ash
fall in inhabited areas was about 3 cm.

Activity began to reduce in intensity after 08:15am and a high amplitude seismic
signal remained until about 9am. During and following the collapse, residents in
the Old Towne and Salem area were subjected to high levels of volcanic gases
particularly hydrogen chloride causing some to move north to get out of the
volcanic plume. Widespread and noisy mudflows were reported in the Trants area
to the northeast of the volcano. Vigorous ash venting from a vent in the western
part of the crater continued until about 5:00pm when it began to decline in
vigour. 

A 1m high tsunami was reported from Deshaies beach in Guadeloupe and swells were
detected in Little Bay, Montserrat and at Jolly Harbour and English Harbour,
Antigua.

Relatively light ash and steam venting has been continuous since then.  Wind
direction shifted towards the north late on 21 May causing ash fall and raining
mud on most parts of the island.

Scientists remain alert to the possibility of further explosive activity but
seismic activity has been low since the event on Saturday.

For further explanations of the volcanic phenomena described, and information
about the Soufrière Hills Volcano and the ongoing eruption, please look at the
observatory's website: http://www.mvo.ms.

Noon, Monday, 22 May 2006

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