Report on Klyuchevskoy (Russia) — 10 March-16 March 2010
Smithsonian / US Geological Survey Weekly Volcanic Activity Report,
10 March-16 March 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, 10 March-16 March 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 5-12 March seismic activity from Kliuchevskoi was above background levels. Strombolian activity ejected material 300 m above the crater. Gas-and-steam plumes rose to altitudes of 5-6.8 km (16,000-22,000 ft) a.s.l. and were occasionally seen on satellite imagery drifting 80 km E. On 4 March new lava flows traveled down the S and NE flanks. A satellite image from 9 March showed that the S-flank lava flow was about 1.3 km long. Phreatic explosions sometimes occurred from the fronts of the lava flows. Satellite imagery also revealed a large daily thermal anomaly at the volcano. The Aviation Color Code level remained at Orange.
Geological Summary. 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.