KVERT reported that during 8-10 November seismic activity at Kliuchevskoi was at background levels. During 9-10 November strong fumarolic activity was seen and a weak thermal anomaly over the crater was observed in satellite imagery. Based on analyses of satellite imagery and information from KVERT, the Tokyo VAAC reported that on 13 November an eruption produced a plume that drifted NE. Later that day, images showed that the ash had dissipated. The Aviation Color Code level remained at Yellow.

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.

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