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Report on Bezymianny (Russia) — March 2021


Bezymianny

Bulletin of the Global Volcanism Network, vol. 46, no. 3 (March 2021)
Managing Editor: Edward Venzke. Edited by Kadie L. Bennis.

Bezymianny (Russia) Lava dome growth in November 2020 and continuing thermal anomalies

Please cite this report as:

Global Volcanism Program, 2021. Report on Bezymianny (Russia) (Bennis, K.L., and Venzke, E., eds.). Bulletin of the Global Volcanism Network, 46:3. Smithsonian Institution.



Bezymianny

Russia

55.972°N, 160.595°E; summit elev. 2882 m

All times are local (unless otherwise noted)


Bezymianny is located on the Kamchatka Peninsula as part of the Klyuchevskoy Group of volcanoes. It has had frequent eruptions dating back to 1955; the current eruptive period began in May 2010 and recent activity has been characterized by lava dome growth, thermal anomalies, and a single ash explosion that occurred on 22 October 2020 (BGVN 45:11). This report covers similar activity during November 2020 through February 2021 primarily using weekly and daily reports from the Kamchatka Volcano Eruptions Response Team (KVERT) and satellite data.

Activity during 1-13 November 2020 was characterized by continued lava dome growth in the summit crater, accompanied by strong fumarolic activity (figure 41) and a persistent thermal anomaly over the lava dome that was visible in satellite imagery on clear weather days. The KVERT weekly reports for 6 and 12 November reported that the N flank of the lava dome was active and had possibly advanced. Continuing gas-and-steam emissions and thermal anomalies were reported by KVERT from mid-November through the end of February 2021. The volcano was often obscured by clouds, making satellite observations difficult.

Figure (see Caption) Figure 41. Photo of Bezymianny showing strong fumarolic activity on 8 December 2020. Photo by S. Chirkov, IVS FEB RAS. Courtesy of IVS FEB RAS, KVERT.

The MIROVA (Middle InfraRed Observation of Volcanic Activity) volcano hotspot detection system based on the analysis of MODIS data showed relatively strong and frequent thermal anomalies during early November to early December due to the continuing lava dome growth, followed by variable, intermittent thermal activity into mid-January 2021. About four low-power anomalies were detected in mid-February (figure 42). This thermal activity was also reflected in Sentinel-2 thermal satellite imagery; thermal anomalies were observed in the summit crater over the lava dome, occasionally accompanied by white gas-and-steam emissions (figure 43).

Figure (see Caption) Figure 42. Relatively strong and frequent thermal anomalies at Bezymianny were recorded by the MIROVA system (Log Radiative Power) during November through early December 2020, due to the growing lava dome. Thermal activity continued at intermittent intervals through mid-February 2021. Four low-power thermal anomalies were detected in February. Courtesy of MIROVA.
Figure (see Caption) Figure 43. Sentinel-2 thermal satellite images showing a thermal anomaly (dark orange) over the lava dome at Bezymianny’s summit crater on 10 November (top left), 5 December (top right), 23 December 2020 (bottom left), and 29 January 2021 (bottom right). The thermal anomaly is frequently accompanied by strong gas-and-steam emissions, as shown in each of these images. Sentinel-2 satellite images with “Atmospheric penetration” (bands 12, 11, 8A) rendering. Courtesy of Sentinel Hub Playground.

Geological Summary. Prior to its noted 1955-56 eruption, Bezymianny had been considered extinct. The modern volcano, much smaller in size than its massive neighbors Kamen and Kliuchevskoi, was formed about 4700 years ago over a late-Pleistocene lava-dome complex and an ancestral edifice built about 11,000-7000 years ago. Three periods of intensified activity have occurred during the past 3000 years. The latest period, which was preceded by a 1000-year quiescence, began with the dramatic 1955-56 eruption. This eruption, similar to that of St. Helens in 1980, produced a large horseshoe-shaped crater that was formed by collapse of the summit and an associated lateral blast. Subsequent episodic but ongoing lava-dome growth, accompanied by intermittent explosive activity and pyroclastic flows, has largely filled the 1956 crater.

Information Contacts: Kamchatka Volcanic Eruptions Response Team (KVERT), Far Eastern Branch, Russian Academy of Sciences, 9 Piip Blvd., Petropavlovsk-Kamchatsky, 683006, Russia (URL: http://www.kscnet.ru/ivs/kvert/); MIROVA (Middle InfraRed Observation of Volcanic Activity), a collaborative project between the Universities of Turin and Florence (Italy) supported by the Centre for Volcanic Risk of the Italian Civil Protection Department (URL: http://www.mirovaweb.it/); Sentinel Hub Playground (URL: https://www.sentinel-hub.com/explore/sentinel-playground).