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Report on Klyuchevskoy (Russia) — January 1999

Bulletin of the Global Volcanism Network, vol. 24, no. 1 (January 1999)
Managing Editor: Richard Wunderman.

Klyuchevskoy (Russia) Series of deep and shallow earthquakes

Please cite this report as:

Global Volcanism Program, 1999. Report on Klyuchevskoy (Russia). In: Wunderman, R (ed.), Bulletin of the Global Volcanism Network, 24:1. Smithsonian Institution. https://doi.org/10.5479/si.GVP.BGVN199901-300260.

Volcano Profile |  Complete Bulletin


Klyuchevskoy

Russia

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

All times are local (unless otherwise noted)


Elevated seismicity persisted through January. Background seismicity was concentrated near the summit crater and at depths of 25-30 km. Beginning at 1514 on 2 January, a series of shallow earthquakes began to be detected. These earthquakes prevailed until 13 January when a 22-minute series was recorded. At 0055 on 15 January a series of deep (25-50 km) earthquakes began. By the end of the month, seismicity had returned to background levels and the alert level was lowered from yellow to green.

Fumarolic plumes rising several hundreds of meters above the summit were seen on 8, 13, 14, 19, and 23-28 January. Some of these plumes were blown by winds as far as 20 km from the volcano. On many days during January direct observation was prevented by poor weather.

Geologic Background. Klyuchevskoy (also spelled Kliuchevskoi) is Kamchatka's highest and most active volcano. Since its origin about 6000 years ago, the beautifully symmetrical, 4835-m-high basaltic stratovolcano has produced frequent moderate-volume explosive and effusive eruptions without major periods of inactivity. It rises above a saddle NE of sharp-peaked Kamen volcano and lies SE of the broad Ushkovsky massif. More than 100 flank eruptions have occurred during the past roughly 3000 years, with most lateral craters and cones occurring along radial fissures between the unconfined NE-to-SE flanks of the conical volcano between 500 m and 3600 m elevation. The morphology of the 700-m-wide summit crater has been frequently modified by historical eruptions, which have been recorded since the late-17th century. Historical eruptions have originated primarily from the summit crater, but have also included numerous major explosive and effusive eruptions from flank craters.

Information Contacts: Olga Chubarova, 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.