Report on Sheveluch (Russia) — 4 March-10 March 2009
Smithsonian / US Geological Survey Weekly Volcanic Activity Report,
4 March-10 March 2009
Managing Editor: Sally Kuhn Sennert
Please cite this report as:
Global Volcanism Program, 2009. Report on Sheveluch (Russia). In: Sennert, S K (ed.), Weekly Volcanic Activity Report, 4 March-10 March 2009. Smithsonian Institution and US Geological Survey.
56.653°N, 161.36°E; summit elev. 3283 m
All times are local (unless otherwise noted)
KVERT reported that seismic activity at Shiveluch was above background levels during 27 February-6 March. Based on interpretations of seismic data, ash plumes likely rose to an altitude of 5.4 km (17,700 ft) a.s.l. According to observers, fumaroles were active during 28 February and 3-5 March. Ash plumes rose to an altitude of 4.7 km (15,400 ft) a.s.l. and drifted NE during 3-4 March. Analysis of satellite imagery revealed a daily thermal anomaly on the lava dome and an ash plume that drifted 84 km E on 4 March. The Level of Concern Color Code remained at Orange.
Based on information from KEMSD, the Tokyo VAAC reported that eruptions on 8 and 10 March produced plumes that rose to altitudes of 6.1-6.4 km (20,000-21,000 ft) a.s.l. Plumes drifted SE on 10 March.
Geological Summary. The high, isolated massif of Sheveluch volcano (also spelled Shiveluch) rises above the lowlands NNE of the Kliuchevskaya volcano group. The 1,300 km3 andesitic volcano is one of Kamchatka's largest and most active volcanic structures, with at least 60 large eruptions during the Holocene. The summit of roughly 65,000-year-old Stary Shiveluch is truncated by a broad 9-km-wide late-Pleistocene caldera breached to the south. Many lava domes occur on its outer flanks. The Molodoy Shiveluch lava dome complex was constructed during the Holocene within the large open caldera; Holocene lava dome extrusion also took place on the flanks of Stary Shiveluch. Widespread tephra layers from these eruptions have provided valuable time markers for dating volcanic events in Kamchatka. Frequent collapses of dome complexes, most recently in 1964, have produced debris avalanches whose deposits cover much of the floor of the breached caldera.