Akusekijima
성층화산 · Japan · 555m

- 화산 유형
- 성층화산
- 국가
- Japan
- 지역
- Western Pacific Volcanic Regions / Ryukyu Volcanic Arc
- 해발
- 555m
- 좌표
- 29.465, 129.594
- 마지막 분화
- 미확인
- 판구조 환경
- Subduction zone / Oceanic crust (< 15 km)
- 화산 지형
- Composite
- 주요 암석
- Andesite / Basaltic Andesite
지질학적 요약
Akusekijima is a small stratovolcano in the southern Ryukyu Islands. Most of the island is surrounded by steep cliffs, and beaches are found only on the SW and SE sides. The andesitic-dacitic volcano consists of two older somma volcanoes, Biroyama and Nakadake. Mitake lava dome forms the high point of the small 2.5 x 3.2 km wide island. The dacitic Omune lava flow on the NE flank was K-Ar dated at less than 80,000 BP; its youthful morphology and lack of overlying tephra layers suggests it could be as young as the Holocene (Furuyama et al., 2002). The lava flow, the youngest product of the volcano, forms a low-angle plateau overlying cliffs forming the northern coast.
Wikipedia 요약
영어 요약Akusekijima is one of the Tokara Islands, a subgroup of the Satsunan Islands belonging to Kagoshima Prefecture, Japan. The island, 7.42 km² in area, has a population of 59 persons. The island can only be reached by boat, as it has no airport; there is a ferry service twice per week to the city of Kagoshima on the mainland. Travel time is about 11 hours. The islanders are dependent mainly on fishing and seasonal tourism.
Wikipedia · CC BY-SA · 전체 기사 보기 →
분화 이력
상세 타임라인
분화 기록이 없습니다.
외부 링크
⚠ 참고용 정보입니다. 재난 대응에 사용하지 마세요.