Report on Klyuchevskoy (Russia) — 3 November-9 November 2010
Smithsonian / US Geological Survey Weekly Volcanic Activity Report, 3 November-9 November 2010
Managing Editor: Sally Kuhn Sennert
Please cite this report as:
Global Volcanism Program, 2010. Report on Klyuchevskoy (Russia). In: Sennert, S K (ed.), Weekly Volcanic Activity Report, 3 November-9 November 2010. 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 29 October-3 November seismic activity at Kliuchevskoi was above background levels and Strombolian activity was observed. Satellite imagery analyses showed a thermal anomaly over the volcano and ash plumes that drifted 480 km SE. Vulcanian activity produced ash plumes that rose to an altitude of 7 km (23,000 ft) a.s.l. during 31 October and 1-4 November. Seismicity sharply decreased on 4 November, and only gas-and-steam activity was observed. On 9 November, KVERT reported that the eruption that began in August 2009 had finished on 4 November and that seismicity had continued to decrease. The Aviation Color Code level was lowered to Yellow.
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.