Report on Karymsky (Russia) — 4 November-10 November 2009
Smithsonian / US Geological Survey Weekly Volcanic Activity Report,
4 November-10 November 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 November-10 November 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 above background levels during 29-31 October; data was not collected during 1-4 November due to technical reasons. Seismic signals possibly indicated that ash plumes rose to an altitude of 3.7 km (12,100 ft) a.s.l. on 31 October and 5 November. Analyses of satellite imagery during 29 October-5 November revealed almost daily thermal anomalies and intermittent ash plumes that drifted 180 km E. The Level of Aviation Color Code remained at Orange. Based on information from KEMSD, the Tokyo VAAC reported that eruptions on 8 and 10 November produced plumes that rose to altitudes of 3-3.4 km (10,000-11,000 ft) a.s.l. Ash was not identified on satellite imagery.
Geological Summary. 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.