Kikhpinych
성층화산 · Russia · 1515m

- 화산 유형
- 성층화산
- 국가
- Russia
- 지역
- Northwestern Pacific Volcanic Regions / Eastern Kamchatka Volcanic Arc
- 해발
- 1515m
- 좌표
- 54.489, 160.251
- 마지막 분화
- 1550년
- 판구조 환경
- Subduction zone / Continental crust (> 25 km)
- 화산 지형
- Composite
- 주요 암석
- Basalt / Picro-Basalt
지질학적 요약
Kikhpinych, the youngest stratovolcano of the Eastern Volcanic Zone of Kamchatka, contains three summits constructed along a roughly E-W line above the eroded Pleistocene Pik volcano, NE of the Uzon caldera. Growth of the modern volcano began during the mid-Holocene about 4,800 years ago with construction of the Zapadny cone. After a long quiescence, the younger Savich cone was built about 1,400 years ago, which included strong explosive activity that destroyed part of the Zapadny and Pik cones. Numerous young lava flows mantle the flanks of Savich; it was last active about 400 years ago, when the Krab lava dome grew on its E flank. Numerous thermal fields are found throughout the complex, including two geysers (now the site of vigorous fumaroles) that were active in the summit crater of Stary Kikhpinych prior to burial by a rockfall avalanche that occurred sometime between September 1981 and July 1982.
Wikipedia 요약
영어 요약Kikhpinych is a stratovolcano located in the eastern part of the Kamchatka Peninsula, which feeds the famous Valley of Geysers.
Wikipedia · CC BY-SA · 전체 기사 보기 →
분화 이력
상세 타임라인
- 1550년VEI ?지질학적 추정1550 ~ 진행 중East flank of Savich (Krab cone)
- 1350년VEI 4지질학적 추정1350 ~ 진행 중Savich cone and north flank
- 900년 (±50년)VEI 3지질학적 추정900 ~ 진행 중Savich cone
- 830년 (±25년)VEI ?지질학적 추정830 ~ 진행 중Savich cone
- 650년VEI ?지질학적 추정650 ~ 진행 중Savich cone
- 550년VEI 3지질학적 추정550 ~ 진행 중East side of Zapadny, Savich cone
- 기원전 2780년 (±25년)VEI 4지질학적 추정BCE 2780 ~ 진행 중Zapadny
- 기원전 2850년VEI 3지질학적 추정BCE 2850 ~ 진행 중Zapadny
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