On 26 December, after 5 months of quiet [but see 13:4], two vents from an intracrater scoria cone ejected bombs and ash. Bombs reached 300 m height. Rare gas/steam explosions, mixed with some ash, fed a 1-km eruption column. On 29 December, lava flows poured from a vent near the foot of the scoria cone (last active in July) onto the N and NW flanks. In January, pyroclastic material was ejected obliquely from the crater onto the volcano's flanks. The eruption decreased in intensity on 20 January. Images from the NOAA 9 polar orbiting satellite at 1617 on 21 January showed a 25-km-long plume spreading SW that had grown to 40 km by 0843 the next day.

Weather satellite images showed renewed activity on 17 February with larger plumes late 19 February. Plumes extended as much as 300 km from the volcano (table 1) and were continuing to form as of 20 February. Comparisons of plume temperatures and directions of plume movement with temperature and wind data recorded by radiosondes (launched 15 km to the N) indicated that plumes reached as much as 9 km altitude.

Table 1. Descriptions of Kliuchevskoi plumes from infrared weather satellite images, 17-20 February 1987. Plume altitudes were estimated by comparing wind data from radiosondes launched 15 km N of the volcano with directions of plume movement.

Geological Summary. 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: A. Khrenov and G. Bogoyavlenskaya, IV; M. Matson, S. Kusselson, and W. Gould, NOAA/NESDIS.