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Report on Klyuchevskoy (Russia) — December 2003

Bulletin of the Global Volcanism Network, vol. 28, no. 12 (December 2003)
Managing Editor: Richard Wunderman.

Klyuchevskoy (Russia) 2003 ends with ~3-km-tall steam plumes, M 2 earthquakes, tremor

Please cite this report as:

Global Volcanism Program, 2003. Report on Klyuchevskoy (Russia). In: Wunderman, R. (ed.), Bulletin of the Global Volcanism Network, 28:12. Smithsonian Institution. https://doi.org/10.5479/si.GVP.BGVN200312-300260.

Volcano Profile |  Complete Bulletin


Klyuchevskoy

Russia

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

All times are local (unless otherwise noted)


Ash explosions and Strombolian activity was reported at Kliuchevskoi through early December 2003 (BGVN 28:11). KVERT reported that unrest continued at Kliuchevskoi over the month of December, with occasional and repeated explosions containing ash, gas and steam rising to 7-8 km altitude, and possible lava flows from the central crater. Seismicity was above background levels over the month. The alert level remained Orange.

Strombolian activity was seen from the town of Klyuchi on 7 December. At 1300 on 6 December an ash explosion up to 1 km above the crater was registered and, on the same day, a 3 km high gas-steam plume was evident. Gas plumes, possibly containing small amounts of ash, rose 100-500 m on 7-16 December, generally extending in various directions and visible to distances of 3-10 km. During this time satellites detected 1- to 9-pixel thermal anomalies. Strombolian activity was again noted from Klyuchi on 12 December.

During the week ending 12 December there were approximately 150 large shallow earthquakes of ML 1.2-2.25 and a large number of weak shallow earthquakes. For example, on 8 December, an earthquake of ML greater than 1.75 was registered at a depth of 5 km under the central crater. On 11 December, 3 earthquakes of ML 1.75-2.0 were registered at a depth of 3-6 km under the central crater. The number of earthquakes was similar during the week ending 19 December.

Tremor occurred often. An index of the tremor's size, reported in terms of relative velocity between the Earth and the seismograph's suspended mass (the ground motion), was 19-23 µm/s on 4-5 December, decreasing to ~ 6.7 µm/s on 9-10 December. On 12 December continuous spasmodic tremor had velocities of 2.5-9.2 µm/s. During the week ending 2 January, tremor had velocities of 2-4 µm/s.

During the week ending 26 December there were 135 large shallow earthquakes of ML 1.9-2.3 and a large number of weak shallow earthquakes were reported. On 19 December, one earthquake at a depth of 11 km and two earthquakes at a depth of 30 km below the central crater (ML less than 2.0) were registered. Continuous spasmodic tremor had velocities of 2.7-5.3 µm/s. Gas-steam plumes were seen rising up to 100 m above the crater on 22-23 December. The volcano was obscured by cloud at other times. A 1-pixel thermal anomaly over the volcano was registered by satellite on 23 December.

During the week ending 2 January 2004, the number of large (ML1.9-2.2) shallow earthquakes dropped to ~ 33, with a large number of weak shallow earthquakes. A 1-pixel thermal anomaly was registered on 26-27 December. On 27-29 December, gas plumes were observed rising up to 50-500 m above the volcano, but the volcano was obscured at other times.

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 Girina, Kamchatka Volcanic Eruptions Response Team (KVERT), a cooperative program of the Institute of Volcanic Geology and Geochemistry, Far East Division, Russian Academy of Sciences, Piip Ave. 9, Petropavlovsk-Kamchatsky, 683006, Russia, the Kamchatka Experimental and Methodical Seismological Department (KEMSD), GS RAS (Russia), and the Alaska Volcano Observatory (USA); Alaska Volcano Observatory (AVO), a cooperative program of the U.S. Geological Survey, 4200 University Drive, Anchorage, AK 99508-4667, USA (URL: http://www.avo.alaska.edu/), the Geophysical Institute, University of Alaska, PO Box 757320, Fairbanks, AK 99775-7320, USA, and the Alaska Division of Geological and Geophysical Surveys, 794 University Ave., Suite 200, Fairbanks, AK 99709, USA.