Report on Sheveluch (Russia) — 14 November-20 November 2001
Smithsonian / US Geological Survey Weekly Volcanic Activity Report,
14 November-20 November 2001
Managing Editor: Gari Mayberry
Please cite this report as:
Global Volcanism Program, 2001. Report on Sheveluch (Russia). In: Mayberry, G (ed.), Weekly Volcanic Activity Report, 14 November-20 November 2001. Smithsonian Institution and US Geological Survey.
56.653°N, 161.36°E; summit elev. 3283 m
All times are local (unless otherwise noted)
During 9-16 November a lava dome continued to grow in Shiveluch's active crater and several steam, gas, and ash explosions occurred. Seismic data suggested emissions from these explosions rose to a maximum height of ~4 km above the dome. A short-lived explosion on 9 November at 1200 produced an ash plume that was observed from Klyuchi, ~46 km from the volcano, rising ~1 km above the dome. The same day, during 1750-1810 incandescence was visible on the SE flank of the volcano 50 m below the summit. Thermal anomalies in the active dome area and ash clouds were visible on satellite imagery. Spasmodic volcanic tremor and weak, shallow seismic signals (possible collapses and avalanches) were registered. The intensity of volcanic tremor noticeably diminished during the week.
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.