Report on Klyuchevskoy (Russia) — 1 June-7 June 2011
Smithsonian / US Geological Survey Weekly Volcanic Activity Report, 1 June-7 June 2011
Managing Editor: Sally Kuhn Sennert
Please cite this report as:
Global Volcanism Program, 2011. Report on Klyuchevskoy (Russia). In: Sennert, S K (ed.), Weekly Volcanic Activity Report, 1 June-7 June 2011. Smithsonian Institution and US Geological Survey.
56.056°N, 160.642°E; summit elev. 4754 m
All times are local (unless otherwise noted)
KVERT reported that during 27 May-3 June seismic activity at Kliuchevskoi was detected. Moderate steam-and-gas activity was observed on 30 May and 1 June; cloud cover prevented observations on the other days of the week. The Aviation Color Code was lowered to Green.
The Tokyo VAAC reported that on 6 June a possible eruption detected in satellite imagery produced a plume that rose to an altitude of 6.1 km (20,000 ft) a.s.l. and drifted NE. The VAAC stated that the ash could have also originated at Bezymianny.
Geologic Background. Klyuchevskoy (also spelled 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. It 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 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 the 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.