Report on Karymsky (Russia) — 4 March-10 March 2009
Smithsonian / US Geological Survey Weekly Volcanic Activity Report, 4 March-10 March 2009
Managing Editor: Sally Kuhn Sennert
Please cite this report as:
Global Volcanism Program, 2009. Report on Karymsky (Russia). In: Sennert, S K (ed.), Weekly Volcanic Activity Report, 4 March-10 March 2009. Smithsonian Institution and US Geological Survey.
54.049°N, 159.443°E; summit elev. 1513 m
All times are local (unless otherwise noted)
KVERT reported that seismic activity at Karymsky was at background levels during 27 February-6 March. Based on interpretations of seismic data, ash plumes likely rose to an altitude of 3.5 km (11,500 ft) a.s.l. Analysis of satellite imagery revealed a thermal anomaly on the lava dome during 27-28 February and 1-4 March, and an ash plume that drifted 120 km SE on 4 March. Ash deposits on the volcano were noted. On 3 March, pilots reported an ash plume that rose to an altitude of 3.5 km (11,500 ft) a.s.l. and drifted E. The Level of Concern Color Code remained at Orange.
Based on information from KEMSD and analysis of satellite imagery, the Tokyo VAAC reported that an eruption on 6 March produced a plume that rose to an altitude of 3 km (10,000 ft) a.s.l.
Geologic Background. Karymsky, the most active volcano of Kamchatka's eastern volcanic zone, is a symmetrical stratovolcano constructed within a 5-km-wide caldera that formed during the early Holocene. The caldera cuts the south side of the Pleistocene Dvor volcano and is located outside the north margin of the large mid-Pleistocene Polovinka caldera, which contains the smaller Akademia Nauk and Odnoboky calderas. Most seismicity preceding Karymsky eruptions originated beneath Akademia Nauk caldera, located immediately south. The caldera enclosing Karymsky formed about 7600-7700 radiocarbon years ago; construction of the stratovolcano began about 2000 years later. The latest eruptive period began about 500 years ago, following a 2300-year quiescence. Much of the cone is mantled by lava flows less than 200 years old. Historical eruptions have been vulcanian or vulcanian-strombolian with moderate explosive activity and occasional lava flows from the summit crater.