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

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dc.contributor.author Braitseva O.A.
dc.contributor.author Melekestsev I.V.
dc.contributor.author Ponomareva V.V.
dc.contributor.author Kirianov V.Yu.
dc.date.accessioned 2019-08-29T10:27:31Z
dc.date.available 2019-08-29T10:27:31Z
dc.date.issued 1995
dc.identifier http://repo.kscnet.ru/1109/
dc.identifier http://www.scopus.com/inward/record.url?eid=2-s2.0-0029528279&partnerID=40&md5=f3a4fdafbc47c80c6083692021ef0a42
dc.identifier.citation Braitseva O.A., Melekestsev I.V., Ponomareva V.V., Kirianov V.Yu. (1995) The last caldera-forming eruption in Kamchatka: Ksudach volcano, 1700-1800 14C-years ago // Volcanology and Seismology. Vol. 17, No. 2. pp. 147-168.
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/4353
dc.description.abstract 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
dc.language.iso en
dc.subject 38.37.25 Вулканология
dc.subject Ксудач
dc.title The last caldera-forming eruption in Kamchatka: Ksudach volcano, 1700-1800 14C-years ago
dc.type Статья


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