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| The eruption occurred ~4.2 ka BP. It started as a minor explosive eruption, tephra of which was dispersed at a distance of ~20 km from the source. The flanks of the whole edifice are host rocks uplifted due to lava intrusion.
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| Author(s): Maria Pevzner |
| Source: IVS FEB RAS. Holocene Kamchatka Volcanoes http://www.kscnet.ru/ivs/volcanoes/holocene/ |
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| Any use of the image may be carried out only with the permission of the author (authors). Please cite the author(s) and the Geoportal when using this image. |
| © IVS FEB RAS Geoportal |
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