mer., 25 juil. 2007, 06:00
MVO reported that based on visual observations, the lava dome at Soufrière Hills changed very little during 25-26 July. Seismic activity was very low and low-level rockfall activity continued. The Alert Level remained elevated at 4 (on a scale of 0-5).
mer., 18 juil. 2007, 06:00
MVO reported that during 13-24 July, the lava dome at Soufrière Hills changed very little, based on visual observations. Seismic activity was very low and low-level rockfall activity continued. Heavy rainfall generated lahars in E drainages on 19 July.
mer., 11 juil. 2007, 06:00
MVO reported that during 6-13 July the lava dome at Soufrière Hills changed very little based on visual observations, and seismic activity was very low. Low-level rockfall activity continued. The Alert Level remained elevated at 4 (on a scale of 0-5).
Read allmer., 4 juil. 2007, 06:00
MVO reported that during 29 June-10 July the lava dome at Soufrière Hills changed very little based on visual observations, and seismic activity was very low. Low-level rockfall activity continued, however, and predominantly affected the Tar River Valley to the E. Heavy rainfall generated lahars in E drainages during 4-6 July.
Read allmer., 27 juin 2007, 06:00
MVO reported that during 22-29 June the lava dome at Soufrière Hills changed very little based on visual observations, and seismic activity was very low. Low-level rockfall and pyroclastic flow activity continued, however, and predominantly affected the Tar River Valley to the E. The volume of the dome was an estimated 208 million cubic meters.
Read allmer., 20 juin 2007, 06:00
MVO reported that during 20-25 June the lava dome at Soufrière Hills changed very little based on visual observations, and seismic activity was very low. Low-level rockfall and pyroclastic flow activity continued, however, and predominantly affected the Tar River Valley to the E. The Alert Level remained at 4 (on a scale of 0-5).
Read allmer., 13 juin 2007, 06:00
MVO reported that during 8-18 June the lava dome at Soufrière Hills changed very little based on visual observations, and seismic activity was very low. Low-level rockfall and pyroclastic flow activity continued. The Alert Level remained at 4 (on a scale of 0-5).
Read allmer., 6 juin 2007, 06:00
MVO reported that during 1-12 June the lava dome at Soufrière Hills changed very little based on visual observations from a helicopter and seismic activity was very low. Low-level rockfall and pyroclastic flow activity continued during 1-12 June. On 8 June, a small pyroclastic flow was observed in the upper parts of Farrell's Plain to the N.
Read allmer., 30 mai 2007, 06:00
MVO reported that during 25 May-1 June the lava dome at Soufrière Hills changed very little based on visual observations and seismic activity was very low. Low-level rockfall and pyroclastic flow activity continued. On 31 May, pyroclastic flows traveled approximately 1 km E in the Tar River Valley.
Read allmer., 23 mai 2007, 06:00
Based on visual observations, MVO reported that during 18-25 May lava-dome growth at Soufrière Hills likely ceased and the overall structure of the dome changed very little. Seismic activity was very low. The Alert Level remained at 4 (on a scale of 0-5).
Read allmer., 16 mai 2007, 06:00
Based on visual observations, MVO reported that during 11-21 May lava-dome growth at Soufrière Hills likely ceased and the overall structure of the dome changed very little. Low-level rockfall and pyroclastic flow activity continued. Seismic activity was very low.
Read allmer., 9 mai 2007, 06:00
Based on visual observations, MVO reported that during 4-11 May lava-dome growth at Soufrière Hills likely ceased and the overall structure of the dome changed very little. Rockfall activity continued. The Alert Level remained at 4 (on a scale of 0-5).
Read allmer., 25 avril 2007, 06:00
During 25 April-1 May, lava-dome growth at Soufrière Hills continued at a reduced rate. Rockfalls and pyroclastic flows occasionally occurred. On 30 April, two pyroclastic flows were observed to the NE in Tuitt's Ghaut.
Read allmer., 18 avril 2007, 06:00
During 13-20 April, visual observations suggested that lava-dome growth at Soufrière Hills continued at a reduced rate. Material originating from the lava dome's growing E-facing shear lobe was shed down the Tar River Valley. Heavy rains resulted in lahars in several drainages 16-17 April.
Read allmer., 11 avril 2007, 06:00
Based on visual observations, lava-dome growth at Soufrière Hills continued at a reduced rate during 6-13 April. Material originating from the E-facing shear lobe was shed down the Tar River Valley. Minor rockfalls and pyroclastic flows were noted.
Read alljeu., 5 avril 2007, 22:07
Over the past days, lava-dome growth at Soufrière Hills was reduced or possibly paused. Small, intermittent pyroclastic flows occurred in the Tar River Valley.
mer., 4 avril 2007, 06:00
During 30 March-9 April, lava-dome growth at Soufrière Hills remained reduced or had possibly ceased. Small, intermittent pyroclastic flows originating from the E-facing shear lobe occurred in the Tar River Valley. Fumarolic activity was observed around the SE and NW regions of a collapse scar at the head of Tyres Ghaut, and to the W, above Gages Valley.
Read allsam., 31 mars 2007, 17:46

View of the lava dome (photo taken on 29 March 2007, courtesy of Eric Tomme)
The lava dome at Soufrière Hills continues to grow, mainly on its NE side. Over the past week, pyroclastic flows mainly affected the sector from the ENE to the NW of the dome and traveled intermittently E down the Tar River Valley. Small flows (<500 m in length) occurred NW in Tyres Ghaut, and one flow was observed at the top of Farrell's Plain.
mer., 28 mars 2007, 06:00
During 23 March-3 April, lava-dome growth at Soufrière Hills was reduced or possibly paused. Small, intermittent pyroclastic flows occurred in the Tar River Valley. Fumarolic activity was observed around the region of a collapse scar at the head of Tyres Ghaut and was audible during 28-29 March.
Read allmer., 21 mars 2007, 20:25
During 2-9 March, lava-dome growth at Soufrière Hills continued and was concentrated on an E-facing lobe topped with blocky, spine-like protrusions. Rockfalls affected the E and NE flanks. Pyroclastic flows traveled 2 km and were confined E in the Tar River Valley. Heightened pyroclastic activity on 7 March resulted in an ash plume that rose to an estimated 2.4 km (8,000 ft) a.s.l. and drifted W. On 11 March, a pyroclastic flow traveled down the NE flank into White's Ghaut. On 12 March, a large, blocky spine leaned steeply towards the NE.
Read allmer., 21 mars 2007, 06:00
During 16-26 March, lava-dome growth at Soufrière Hills continued and was concentrated on the NE side. Pyroclastic flows mainly affected the sector from the ENE to the NW of the dome and traveled intermittently E down the Tar River Valley. Small flows (
Read allmer., 14 mars 2007, 06:00
During 9-16 March, lava-dome growth at Soufrière Hills continued and was concentrated on the NE side. Intermittent pyroclastic flows, possibly originating from the large blocky spine on the edge of the E lobe, traveled E down the Tar River Valley and produced large ash plumes. One of the plumes on 12 March rose to an altitude of 3 km (10,000 ft) a.s.l. and drifted NW.
Read allmer., 7 mars 2007, 06:00
During 2-9 March, lava-dome growth at Soufrière Hills continued and was concentrated on an E-facing lobe topped with blocky, spine-like protrusions. Rockfalls affected the E and NE flanks. Pyroclastic flows traveled 2 km and were confined E in the Tar River Valley.
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