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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