Report on Klyuchevskoy (Russia) — 27 January-2 February 2021
Smithsonian / US Geological Survey Weekly Volcanic Activity Report,
27 January-2 February 2021
Managing Editor: Sally Kuhn Sennert
Please cite this report as:
Global Volcanism Program, 2021. Report on Klyuchevskoy (Russia). In: Sennert, S K (ed.), Weekly Volcanic Activity Report, 27 January-2 February 2021. Smithsonian Institution and US Geological Survey.
56.056°N, 160.642°E; summit elev. 4754 m
All times are local (unless otherwise noted)
KVERT reported that Strombolian and sometimes Vulcanian activity at Klyuchevskoy continued during 22-29 January and lava advanced down the Kozyrevsky drainage on the S flank and the Apakhonchich drainage on the SE flank. A large bright thermal anomaly was identified daily in satellite images. Steam-and-gas plumes with some ash rose to 6 km (19,700 ft) a.s.l. and drifted 125 km in multiple directions. On 24 January collapses from the lava flow sent large amounts of material and pyroclastic flows down the Apakhonchich drainage. An ash cloud rose to 9.6 km (31,500 ft) a.s.l. and drifted 60 km N then NE. The Aviation Color Code remined at Orange (the second highest level on a four-color scale).
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.