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Report on Klyuchevskoy (Russia) — February 1998


Klyuchevskoy

Bulletin of the Global Volcanism Network, vol. 23, no. 2 (February 1998)
Managing Editor: Richard Wunderman.

Klyuchevskoy (Russia) Earthquakes, tremor, and gas-and-steam plumes throughout February

Please cite this report as:

Global Volcanism Program, 1998. Report on Klyuchevskoy (Russia) (Wunderman, R., ed.). Bulletin of the Global Volcanism Network, 23:2. Smithsonian Institution. https://doi.org/10.5479/si.GVP.BGVN199802-300260



Klyuchevskoy

Russia

56.056°N, 160.642°E; summit elev. 4754 m

All times are local (unless otherwise noted)


Beginning at 0616 on 28 January and continuing until 1 March, seismicity at Kliuchevskoi was above background level. During 28 January-8 February, earthquakes registered at depths of 25-30 km under the volcano and were accompanied by volcanic tremor. Surface earthquakes accompanied by volcanic tremor were recorded during 9-22 February, and deep earthquakes were detected during 23 February-1 March.

Fumarolic plumes rose 1-3 km above the volcano on 27 January, 3 February, and 17 February. Gas-and-steam plumes rose 50-2000 m on 30 January, 4-5, 9, 11-15, 18-22, 24-28 February, and 1 March. The plumes drifted 1-10 km with prevailing winds.

Geological Summary. Klyuchevskoy is the highest and most active volcano on the Kamchatka Peninsula. Since its origin about 6,000 years ago, this symmetrical, basaltic stratovolcano has produced frequent moderate-volume explosive and effusive eruptions without major periods of inactivity. It rises above a saddle NE of Kamen volcano and lies SE of the broad Ushkovsky massif. More than 100 flank eruptions have occurred during approximately the past 3,000 years, with most lateral craters and cones occurring along radial fissures between the unconfined NE-to-SE flanks of the conical volcano between 500 and 3,600 m elevation. Eruptions recorded since the late 17th century have resulted in frequent changes to the morphology of the 700-m-wide summit crater. These eruptions over the past 400 years have originated primarily from the summit crater, but have also included numerous major explosive and effusive eruptions from flank craters.

Information Contacts: Vladimir Kirianov, Kamchatka Volcanic Eruptions Response Team (KVERT), Institute of Volcanic Geology and Geochemistry, Piip Ave. 9, Petropavlovsk-Kamchatsky, 683006, Russia; Tom Miller, Alaska Volcano Observatory (AVO), a cooperative program of a) U.S. Geological Survey, 4200 University Drive, Anchorage, AK 99508-4667, USA (URL: http://www.avo.alaska.edu/), b) Geophysical Institute, University of Alaska, PO Box 757320, Fairbanks, AK 99775-7320, USA, and c) Alaska Division of Geological & Geophysical Surveys, 794 University Ave., Suite 200, Fairbanks, AK 99709, USA.