Mount Kitayoko
Yokodake
성층화산 · Japan · 2480m
- 화산 유형
- 성층화산
- 국가
- Japan
- 지역
- Northwestern Pacific Volcanic Regions / Northeast Japan Volcanic Arc
- 해발
- 2480m
- 좌표
- 36.087, 138.320
- 마지막 분화
- 1200년
- 판구조 환경
- Subduction zone / Continental crust (> 25 km)
- 화산 지형
- Composite
- 주요 암석
- Andesite / Basaltic Andesite
지질학적 요약
Yokodake lava dome, capped by eight small craters, has been active into the Holocene. The most recent eruption took place about 800 years ago, when ash emission accompanied emplacement of a small lava flow. Yokodake is at the northern edge of the Kita-Yatsugatake (North Yatsugatake) group of stratovolcanoes and lava domes at the NW end of the NNW-SSE-trending Yatsugatake volcanic massif. The basaltic-to-dacitic Kita Yatsugatake group also contains the Tateshinayama, Shimagareyama, Chausuyama and Futagomine volcanoes. Tateshinayama is sometimes known as Suwa Fuji because of its conical profile. A large lava flow forms the Tateshina-kogen plateau south of Tateshinayama and Yokodake. A debris avalanche from edifice collapse in 888 CE created Matsubara Lake on the east side of the massif.
Wikipedia 요약
영어 요약Mount Yoko also known as Mount Kita Yoko, is an active lava dome located in the Northern Yatsugatake Volcanic Group of the Yatsugatake Mountains, Honshū, Japan. Mount Yoko has shown the most recent activity and is now considered an active volcano. It last erupted approximately 800 years ago. The eruption consisted of ash with a lava flow of some 3 million cubic meters. The eruption was dated by corrected radiocarbon dating. The next previous eruption was in or after 400 BCE.
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분화 이력
상세 타임라인
- 1200년 (±100년)VEI ?지질학적 추정1200 ~ 진행 중Yoko-dake
- 기원전 400년VEI ?지질학적 추정BCE 400 ~ 진행 중Yoko-dake
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