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...
Main Authors: | , , , |
---|---|
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 |
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 |
---|