Report on Sheveluch (Russia) — 10 October-16 October 2001
Smithsonian / US Geological Survey Weekly Volcanic Activity Report,
10 October-16 October 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, 10 October-16 October 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 6-12 October a lava dome continued to grow in Shiveluch's active crater, and several eruptions produced ash and steam-and-gas clouds. The highest reported steam-and-gas cloud was produced from an eruption on 9 October at 1630 and rose 2 km above the dome. On 10 October at 2250 the reflection from incandescent lava was visible on the dome. Short pyroclastic flows and 400-m-high ash plumes were produced from small explosions on 11 October at 1515 and 1610. Thermal anomalies in the active dome area were visible on satellite imagery. Spasmodic volcanic tremor and weak, shallow seismic signals (possible collapses and avalanches) were registered. Shiveluch remained at Concern Color Code Orange.
Geological Summary. 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.