Report on Sheveluch (Russia) — 28 May-3 June 2008
Smithsonian / US Geological Survey Weekly Volcanic Activity Report,
28 May-3 June 2008
Managing Editor: Sally Kuhn Sennert
Please cite this report as:
Global Volcanism Program, 2008. Report on Sheveluch (Russia). In: Sennert, S K (ed.), Weekly Volcanic Activity Report, 28 May-3 June 2008. 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 slightly above background levels during 27-28 May and at background levels the other days during 23-30 May. Gas-and-ash explosions may have occurred on 22, 27, and 28 May and produced plumes to an altitude of 4.7 km (15,400 ft) a.s.l. According to video footage and visual observations, hot avalanches descended the lava dome and ash plumes rose to an altitude of 3.6 km (11,800 ft) a.s.l. during 26-27 May. Fumarolic activity was noted during 23-27 May. Observations of satellite imagery revealed a daily thermal anomaly in the crater, and an ash-and-steam plume that drifted 17 km SW on 28 May. The Level of Concern Color Code remained at Orange.
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.