Archived
Volcano Data
GMT |
Hourly VT |
Cumulative VT |
Multiply By |
Predicted Daily VT Events
Total |
Predicted Total Seismic Activity
(RF + VT) |
21:00 |
No data available |
340 |
1.09 |
|
|
22:00 |
21 |
361 |
1.04 |
|
|
23:00 |
29 |
390 |
1 |
|
|
GMT |
Hourly RF |
Cumulative RF |
Multiply By |
Predicted Daily RF Events Total |
Predicted Total Seismic Activity
(RF + VT)
|
21:00 |
No data available |
184 |
1.09 |
|
|
22:00 |
17 |
201 |
1.04 |
|
|
23:00 |
19 |
220 |
1 |
|
|
Observations from September 3rd
Strong winds and heavy rain from Sept 2nd
caused flash floods and made viewing the top of the dome
difficult.
Almost all of the volcanic activity on the dome has
been on the eastern side, although steaming has been coming from many areas on the dome. The Western side shows
signs of being unstable and likely to cause pyroclastic flows
of an unknown size.
Septermber 3rd has seen two or more hours of increasing
rock fall activity and small pyroclastic flows.
There were less flows than expected, given the amount
of seismic activity. If we do not see many more flows in the
next few days, the pressure in the volcanic vents could grow
enormously.
Moderate ash clouds of 3 km or less have spread
north- westwards, with 1 to 2 cm of ash having fallen in the Cork
Hill area. The few pyroclastic flows today produced ash clouds
that rose 6 km, but there was no sign of vertical ash cloud columns
from the summit of the dome. Ash has fallen
on nearly every part of the island from St. Patrick's in the
South West, to St. John's in the North, and from Plymouth in the West to Long
Ground in the North East, including Bramble Airport.
Volcanic tremors have continued
to occur in short bursts, the frequency of which has increased
over the past three days. The tremors were similar to those
in the previous weeks and were located at depths
of less than 2 km (below sea level) beneath the crater. They
are generally too small to be felt in occupied areas.
|