Report on Sheveluch (Russia) — 1 May-7 May 2002
Smithsonian / US Geological Survey Weekly Volcanic Activity Report, 1 May-7 May 2002
Managing Editor: Gari Mayberry
Please cite this report as:
Global Volcanism Program, 2002. Report on Sheveluch (Russia). In: Mayberry, G (ed.), Weekly Volcanic Activity Report, 1 May-7 May 2002. Smithsonian Institution and US Geological Survey.
56.653°N, 161.36°E; summit elev. 3283 m
All times are local (unless otherwise noted)
During 26 April-3 May, there were several small emissions of gas and steam at Shiveluch. The character of seismicity changed in comparison to the previous week, with more deep earthquakes occuring and no significant events indicating explosions were registered. There were earthquakes with magnitudes less than or equal to 2.0 at depths of 0-9 km, many local shallow seismic signals, and intermittent episodes of weak volcanic tremor. Thermal anomalies were visible on AVHRR satellite imagery. On 5 May at 0945 an ash plume rose 1.5 km above the lava dome. Shiveluch remained at Concern Color Code Yellow ("volcano is restless").
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.