Kuchinoshima
성층화산 · Japan · 628m

- 화산 유형
- 성층화산
- 국가
- Japan
- 지역
- Western Pacific Volcanic Regions / Ryukyu Volcanic Arc
- 해발
- 628m
- 좌표
- 29.968, 129.926
- 마지막 분화
- 1190년
- 판구조 환경
- Subduction zone / Oceanic crust (< 15 km)
- 화산 지형
- Composite
- 주요 암석
- Andesite / Basaltic Andesite
지질학적 요약
Kuchinoshima, lying in the northern Ryukyu Islands between the volcanic islands of Nakanoshima and Kuchinoerabujima, consists of two andesitic stratovolcanoes and a NW-SE-trending chain of lava domes. Two small villages, Nishinohama and Kuchinoshima, lie at the northern end of the mostly uninhabited island. The compound 628-m-high Maedake lava dome, forming the highest point on the 3 x 7 km wide island, was constructed east of the summit of 501-m-high Yokodake stratovolcano. The last magmatic eruption took place about 1200-1300 years ago.
Wikipedia 요약
영어 요약Kuchinoshima (口之島), literally "mouth island", is one of the Tokara Islands, belonging to Kagoshima Prefecture. The island, 13.33 km2 (5.15 sq mi) in area, and has a population of 140 persons. The island can only be reached by boat as it has no airport; there is regular ferry service to the city of Kagoshima on the mainland. Travel time is about 6 hours. The islanders are dependent mainly on agriculture, fishing and seasonal tourism. The island is home to the rare Kuchinoshima breed of Japanese native cattle.
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분화 이력
상세 타임라인
- 1190년 (±40년)VEI ?지질학적 추정1190 ~ 진행 중
- 750년 (±50년)VEI ?지질학적 추정750 ~ 진행 중
- 기원전 900년VEI ?지질학적 추정BCE 900 ~ 진행 중
- 기원전 6750년 (±50년)VEI ?지질학적 추정BCE 6750 ~ 진행 중Yoko-dake, Mae-dake
외부 링크
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