Report on Klyuchevskoy (Russia) — 27 October-2 November 2010
Smithsonian / US Geological Survey Weekly Volcanic Activity Report, 27 October-2 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, 27 October-2 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 22-29 October seismic activity at Kliuchevskoi was above background levels and Strombolian activity was observed. Satellite imagery analyses showed a large and intense daily thermal anomaly over the volcano and two lava flows descending the W and SW flanks from the summit crater. Ash plumes also detected in imagery drifted more than 2,300 km E. Ash plumes rose to altitudes of 8-9 km (26,200-29,500 ft) a.s.l. during 22-25 and 27 October. The Aviation Color Code level remained at Red. A news article from 29 October stated that ash from Kliuchevskoi and Shiveluch caused area flight diversions.
On 30 October explosive activity decreased along with the magnitude of volcanic tremor. Based on visual observations and analysis of satellite imagery, ash plumes rose to altitudes of 5-5.5 km (16,400-18,000 ft) a.s.l. and drifted 100 km SE. The Aviation Color Code level was lowered to Orange. The Tokyo VAAC reported that, based on analyses of satellite imagery and information from KVERT, eruptions on 31 October and 2 November, and a possible eruption on 1 November produced ash plumes that rose to altitudes of 5.2-6.7 km (17,000-22,000 ft) a.s.l. and drifted SE and E.
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.