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Report on Bezymianny (Russia) — 2 June-8 June 2010


Bezymianny

Smithsonian / US Geological Survey Weekly Volcanic Activity Report,
2 June-8 June 2010
Managing Editor: Sally Kuhn Sennert

Please cite this report as:

Global Volcanism Program, 2010. Report on Bezymianny (Russia). In: Sennert, S K (ed.), Weekly Volcanic Activity Report, 2 June-8 June 2010. Smithsonian Institution and US Geological Survey.

Weekly Report (2 June-8 June 2010)

Bezymianny

Russia

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

All times are local (unless otherwise noted)


KVERT reported that after an explosive eruption from Bezymianny on 1 June two bright thermal anomalies on the flanks were seen in satellite imagery during 1-2 June, possibly from pyroclastic flow deposits. On 4 June KVERT noted that strong gas-and-steam emissions continued to rise from the lava dome. The Aviation Color Code level was lowered to Yellow.

Geological Summary. The modern Bezymianny, much smaller than its massive neighbors Kamen and Kliuchevskoi on the Kamchatka Peninsula, was formed about 4,700 years ago over a late-Pleistocene lava-dome complex and an ancestral edifice built about 11,000-7,000 years ago. Three periods of intensified activity have occurred during the past 3,000 years. The latest period, which was preceded by a 1,000-year quiescence, began with the dramatic 1955-56 eruption. This eruption, similar to that of St. Helens in 1980, produced a large open 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.

Source: Kamchatkan Volcanic Eruption Response Team (KVERT)