Instructions   //   H
Volcano Data

GMT VT RF Observations
10:00 42 21 Semi-continuous pyroclastic flow production into the Tar River valley progressively unroofed the eastern flank of the dome.
09:00 37 28 Formation of many pyroclastic flows in the Tar River valley.
08:00 23 28 Ash clouds surrounding Soufrière Hills make it increasingly more difficult to visually monitor the events occurring at Soufrière Hills
07:00 21 25
06:00 18 22
05:00 33 17
04:00 28 22 A probable increase in pyroclastic flow production triggering intense explosive activity with asymmetric projection of large projectiles to the NE and the formation of a 14 km eruption column, and the dispersal of pumiceous and lithic tephra-fall over much of the south of the island
03:00 22 18
02:00 36 12 Explosive dome collapse was initiated, triggered by further mass removal associated with possible pyroclastic flow formation
01:00 12 16 Dome complex has reached its highest volume
Frequent VT earthquake swarms
00:00 30 16 Diminishing production of pyroclastic flows in the Tar River valley
Seismic activity is increasing
A period of reduced activity at Soufrière Hills