Klyuchevskoy volcano (Kamchatka) activity update: strong steaming, likely strombolian activity in summit crater

Mo, 4. Nov 2013, 20:17
20:17 PM | VON: T
Current view of Klyuchevskoy volcano (KVERT webcam)
Current view of Klyuchevskoy volcano (KVERT webcam)
Tremor and degassing have increased with respect to the last report from KVERT. A steam plume rises about 2 km above the crater and a thermal anomaly over the volcano is visible on satellite data. This suggests that some volcanic activity (perhaps strombolian) has resumed (or continues).

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So, 3. Nov 2013, 11:23
The eruption seems to have ended. No more lava flows or strombolian explosions were seen during the past days. Read all
Di, 22. Okt 2013, 06:00
Klyuchevskoy volcano this morning (KVERT webcam)
The violent explosive phase of the eruption ended at 13:00 UTC on October 20. KVERT reported a decrease of the tremor from 150.4 mcm/s to 3.3 mcm/s and the cessation of ash emission that last reached 26,000 ft (8 km) altitude. Read all
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NASA photo of the eruption of Klyuchevsky volcano on 30 September, 1994, the volcano's largest explosion in 40 years. The large
NASA photo of the eruption of Klyuchevsky volcano on 30 September, 1994, the volcano's largest explosion in 40 years. The large

Background:

Kliuchevskoi is Kamchatka's highest and most active volcano.  Since its origin about 6000 years ago, the beautifully symmetrical, 4835-m-high basaltic stratovolcano has produced frequent moderate-volume explosive and effusive eruptions without major periods of inactivity.  Kliuchevskoi rises above a saddle NE of sharp-peaked Kamen volcano and lies SE of the broad Ushkovsky massif.  More than 100 flank eruptions have occurred at Kliuchevskoi during the past roughly 3000 years, with most lateral craters and cones occurring along radial fissures between the unconfined NE-to-SE flanks of the conical volcano between 500 m and 3600 m elevation.  The morphology of its 700-m-wide summit crater has been frequently modified by historical eruptions, which have been recorded since the late-17th century.  Historical eruptions have originated primarily from the summit crater, but have also included numerous major explosive and effusive eruptions from flank craters.


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Source: Klyuchevsky information by the GVP (Smithsonian Institution)



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