DEBRIS AVALANCHE OF THE 19S6 BEZYMIANNY ERUPTION

Bezymianny is one of the volcanoes of the Klyuchevskoy volcanic group located in the central part of the Kamchatka peninsula. Until 1955 the volcano was considered extinct. In the historic time (in this region beginning from 1697) the volcano did not exhibit the signs of activity. According to tephr...

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Bibliographic Details
Main Authors: Er B. Belousov, Genrietta E. Bogoyavlenskaya
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.534.946
http://kcs.dvo.ru/ivs/bibl/vulk/stbezim/kyoto.pdf
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Summary:Bezymianny is one of the volcanoes of the Klyuchevskoy volcanic group located in the central part of the Kamchatka peninsula. Until 1955 the volcano was considered extinct. In the historic time (in this region beginning from 1697) the volcano did not exhibit the signs of activity. According to tephrochronological studies the latest eruption at the volcano occurred about 1,000 years ago (Braitseva and Kirianov, 1982). Before the catastrophic eruption of 1956 this was a stratovolcano 3.085 m high composed of basaltic andesites and andesitic dacites. Several extrusive domes were observed in the crater and on the slopes of the volcano. The volcano manifested its activity in 1955. From September 29 frequent local earthquakes