Report on Sheveluch (Russia) — 2 June-8 June 2010
Smithsonian / US Geological Survey Weekly Volcanic Activity Report, 2 June-8 June 2010
Managing Editor: Sally Kuhn Sennert
Please cite this report as:
Global Volcanism Program, 2010. Report on Sheveluch (Russia). In: Sennert, S K (ed.), Weekly Volcanic Activity Report, 2 June-8 June 2010. 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 during 28 May-4 June seismic activity from Shiveluch was above background levels, suggesting that possible ash plumes rose to an altitude of 6.1 km (20,000 ft) a.s.l. Strong fumarolic activity was also noted and, at night, hot avalanches were seen. Ash plumes observed throughout the reporting period rose to an altitude of 4.5 km (14,800 ft) a.s.l. Satellite imagery showed a large daily thermal anomaly. Gas-and-steam plumes seen in imagery drifted 30 km W on 29 May, and an ash cloud 20 by 6 km in dimension was detected about 15 km N on 31 May. The Aviation Color Code level remained at Orange.
Geologic Background. The high, isolated massif of Sheveluch volcano (also spelled Shiveluch) rises above the lowlands NNE of the Kliuchevskaya volcano group. The 1300 km3 volcano is one of Kamchatka's largest and most active volcanic structures. 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 dot its outer flanks. The Molodoy Shiveluch lava dome complex was constructed during the Holocene within the large horseshoe-shaped caldera; Holocene lava dome extrusion also took place on the flanks of Stary Shiveluch. At least 60 large eruptions have occurred during the Holocene, making it the most vigorous andesitic volcano of the Kuril-Kamchatka arc. 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.