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Originally posted by asala
Here is a few updates:
The Philippine Volcano Mount Mayon has finally been lowered,
Philippine volcano
And latest on the Congo
Democratic Republic of Congo
Originally posted by PuterMan
Chaiten has been showing the cam frozen at 09:08 all day so far
www2.sernageomin.cl...
Curious or what?
Update on that. It is now working again and showing thick cloud(?) and a wonderful shot of water droplets.
[edit on 19/2/2010 by PuterMan]
This is a subsequent edit. I am not going to post a picture, but go take a look at the cam and tell me what you think that might be. It loooks solid (white/grey). If you are on later and it has changed because of nightfall reply to this thread and I will post a picture of it as it is now @ 17:00 UTC.
it looks to be very foggy with drew drops on the lense or a thick ash cloud . but my guess would be foggy.
[edit on 19/2/2010 by PuterMan]
SOUFRIERE HILLS Montserrat 16.72°N, 62.18°W; summit elev. 915 m MVO reported that during 5-12 February activity from the Soufrière Hills lava dome increased significantly....
On 11 February part of the lava dome collapsed leaving a large collapse scar on the NE flank. Pyroclastic flows traveled NE and then, along with pyroclastic surges, across the sea at several places.......Pyroclastic flow deposits covered several hundred meters of the coastline.......also traveled NW into Tyers Ghaut and down the Belham valley as far a Cork Hill. An ash plume rose to an altitude of 15.2 km (50,000 ft) a.s.l. and drifted E and then SE. Ashfall occurred in NE Montserrat, SW Antigua (50 km NW), Guadeloupe (65 km SE), and Dominica (145 km SE).
Geologic Summary......Soufrière Hills volcano occupies the southern half of the island of Montserrat....series of lava domes emplaced along an ESE-trending zone......1-km-wide crater breached widely to the E, was formed during an eruption 4,000 years ago in which the summit collapsed, producing a large submarine avalanche. ...... Non-eruptive seismic swarms occurred at 30-year intervals in the 20th century, but with the exception of a 17th-century eruption that produced the Castle Peak lava dome, no historical eruptions were recorded on Montserrat 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.
Map
Map Sources: Montserrat Volcano Observatory (MVO), Agence France-Presse Soufrière Hills Information from the Global Volcanism Program