The last caldera-forming eruption in Kamchatka: Ksudach volcano, 1700-1800 14C-years ago

A catastrophic explosive eruption occurred 1700-1800 14C-years ago at Ksudach Volcano in Kamchatka. It was one of the AD greatest Plinian-type eruptions. It erupted 18-19 km3 of pyroclastic material and produced a collapse caldera 4 × 6.5 km in size and 6.5-7 km3 in volume. The eruptive column rose...

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Bibliographic Details
Main Authors: Braitseva O.A., Melekestsev I.V., Ponomareva V.V., Kirianov V.Yu.
Format: Text
Language:English
Published: 1995
Subjects:
Online Access:http://repo.kscnet.ru/1109/
http://www.scopus.com/inward/record.url?eid=2-s2.0-0029528279&partnerID=40&md5=f3a4fdafbc47c80c6083692021ef0a42
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Summary:A catastrophic explosive eruption occurred 1700-1800 14C-years ago at Ksudach Volcano in Kamchatka. It was one of the AD greatest Plinian-type eruptions. It erupted 18-19 km3 of pyroclastic material and produced a collapse caldera 4 × 6.5 km in size and 6.5-7 km3 in volume. The eruptive column rose to a height of 23 km. It was the last caldera-forming eruption in the Kuril-Kamchatka region. It resembled an eruption that occurred at Krakatau in 1883 in type and size. The eruption was bound to have a climatic impact, impaired the Earth's ozone layer, and produced an acid peak in the Greenland ice sheet. -from Journal summary