ACTIVE VOLCANOES OF KAMCHATKA AND NORTHERN KURILES |
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| Bezymianny volcano |
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| Hazard synopsis | ||||||||||||||||||||||||||||||||
Moderate
potential hazards are caused by ash plumes, ash falls, pyroclastic
flows, hot avalanches and lahars.
The volcano constitutes a potential hazard to international and local airlines at Kamchatka because its eruptive clouds can rise to a height of 8-15 km ASL and extend for hundreds of kilometers from the volcano to different directions. Ash falls possible at: |
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| Monitoring status | ||||||||||||||||||||||||||||||||
| Seismic, visual, satellite monitoring, web video camera. | ||||||||||||||||||||||||||||||||
| Form and structure | ||||||||||||||||||||||||||||||||
A complex
massif: inside the explosive caldera 1956 in diameter 1.3x2.8 km,
opened to the east, proceeds a growth of the lava dome Novy (New). |
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| Volcanic activity | ||||||||||||||||||||||||||||||||
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| Location | ||||||||||||||||||||||||||||||||
The
volcano is located in the center of Klyuchevskaya group volcanoes
of the Kamchatka, at a distance of 40 km from Klyuchi and of 350
km from Petropavlovsk-Kamchatsky. |
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| Composition | ||||||||||||||||||||||||||||||||
| Andesites predominant, besides dacites, andesibasalts and basalts. | ||||||||||||||||||||||||||||||||
| Age | ||||||||||||||||||||||||||||||||
| About 10000-11000 – Pra-Bezymianny
volcano. About 5500 – Bezymianny volcano. |
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