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Report on Klyuchevskoy (Russia) — April 1991


Klyuchevskoy

Bulletin of the Global Volcanism Network, vol. 16, no. 4 (April 1991)
Managing Editor: Lindsay McClelland.

Klyuchevskoy (Russia) Small summit plume; ash on SE flank

Please cite this report as:

Global Volcanism Program, 1991. Report on Klyuchevskoy (Russia) (McClelland, L., ed.). Bulletin of the Global Volcanism Network, 16:4. Smithsonian Institution. https://doi.org/10.5479/si.GVP.BGVN199104-300260



Klyuchevskoy

Russia

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

All times are local (unless otherwise noted)


A Space Shuttle photograph on 29 April at 1248 shows a plume, apparently containing ash, rising about 1 km above the summit and extending about 15 km downwind. Snow on the SE flank appeared to be ash-covered. A small summit eruption occurred on 8 April, but no additional eruptive activity has been reported.

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: C. Evans, Lockheed, Houston.