The Tokyo VAAC received reports that Kliuchevskoi began erupting on 27 February at 1455. Reportedly, an ash cloud was produced to a height of ~6.4 km a.s.l. and drifted to the NE. No ash was visible on satellite imagery. According to reports KVERT received from the Research Laboratory of Seismic and Volcanic Activity in Kamchatka, there was neither a seismic signal detected at Kliuchevskoi on 27 February at 1455 nor an ash plume visible on video footage.

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.

Sources: Kamchatkan Volcanic Eruption Response Team (KVERT), Tokyo Volcanic Ash Advisory Center (VAAC)