Report on Karymsky (Russia) — 3 October-9 October 2007
Smithsonian / US Geological Survey Weekly Volcanic Activity Report,
3 October-9 October 2007
Managing Editor: Sally Kuhn Sennert
Please cite this report as:
Global Volcanism Program, 2007. Report on Karymsky (Russia). In: Sennert, S K (ed.), Weekly Volcanic Activity Report, 3 October-9 October 2007. 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 28 September-5 October. Based on seismic interpretation, ash plumes may have risen to an altitude of 3.5 km (11,500 ft) a.s.l. during the reporting period. Observations of satellite imagery revealed that a thermal anomaly was present in the crater during 27 and 29-30 September and 1 and 3 October. Ash plumes drifted SE and E on 30 September and 1 and 3 October. The Level of Concern Color Code remained at Orange.
Based on information from KEMSD and KVERT, observations in the Petropavlovsk-Kamchatsky Flight Information Region (FIR), and pilot reports, the Tokyo VAAC reported that ash plumes rose to an altitude of 3-3.7 km (10,000-12,000 ft) a.s.l. on 5, 7, and 8 October. Plumes drifted E and NE.
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.