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Veniaminof volcano (Alaska): weak ash emissions
Tuesday Jun 11, 2013 11:24 AM | BY: T
Weak ash plume from Veniaminof (FAA webcam, annotated by Blog Culture Volcan)
Current seismic recording from Veniaminof (VNHG station, AVO)
A weak eruptive activity has started from the volcano. Since last night, weak ash emissions have appeared from the central cone of the caldera of the volcano.
The new activity is accompanied by a persistent steam plume and increasing volcanic tremor. So far there seem to be no lava flows or other significant eruptive processes.
The new ash emissions are very diluted and reach about 200-300 m height. They were first observed on the Aciation camera of Perryville from last night at around 17-18h local time. AVO who has not yet reported about the ash confirmed to Blog Culture Volcan that the plume indeed contains very small amounts of ash, which pose no problems to aviation (for now).
Links / Sources:
Monday, Jun 10, 2013
The week starts with relatively little volcanic activity worldwide: ...
Sunday, Jun 09, 2013
Veniaminof (Alaska Peninsula, USA)
: Over the past 2 days, AVO has detected gradually increasing seismic tremor beneath Veniaminof and therefore raised the Aviation Color Code to Yellow and the Volcano Alert Level to Advisory. ...
Saturday, Jun 08, 2013
Pavlov (Alaska Peninsula, USA)
: Weak eruptive activity continues, producing small steam and ash plumes drifting at about 18-20,000 ft (5-6 km) altitude SSE as detected on satellite data (VAAC Anchorage). ...
Friday, Jun 07, 2013
Etna (Sicily, Italy)
: During a visit to the summit craters today, we could observe a new hot fumarole in the western pit of the Bocca Nuova, increased bluish degassing from a vent in the saddle between the old and new SE crater and hear deep-seated explosions inside the NE crater. ...
More on VolcanoDiscovery:
Igneous or magmatic rocks
: The most primitive rock type forms when magma (molten rock) solidifies - either inside the earth (plutonic rocks) or during volcanic eruptions (volcanic rocks). A short overview.