미쿠라섬
Mikurajima
성층화산 · Japan · 851m

- 화산 유형
- 성층화산
- 국가
- Japan
- 지역
- 북서태평양 / Izu Volcanic Arc
- 해발
- 851m
- 좌표
- 33.874, 139.602
- 마지막 분화
- -4100년
- 판구조 환경
- Subduction zone / Oceanic crust (< 15 km)
- 화산 지형
- Composite
- 주요 암석
- Basalt / Picro-Basalt
지질학적 요약
Mikurajima is a small steep-sided island located between the more well-known Miyakejima and Hachijojima volcanoes. Oyama forms the summit of the basaltic-to-andesitic island, which is surrounded by cliffs and dissected on the southern-to-eastern sides. The sparsely populated island consists of a large stratovolcano with lava domes on the SE side. Several small sea stacks are located immediately offshore. Growth of the stratovolcano took place until about 7,000 years ago, and the latest activity occurred about 6,000 years ago, when explosive eruptions and pyroclastic surges accompanied lava dome growth.
Wikipedia 요약
영어 요약Mikura-jima (御蔵島) is an inhabited volcanic Japanese island in the Pacific Ocean. The island is administered by Tōkyō Metropolis and is located approximately 200 kilometres (120 mi) south of Tokyo and 19 kilometres (12 mi) south-southeast of Miyakejima. It is one of the Izu Seven Islands group of the seven northern islands of the Izu archipelago. Mikurashima is administratively part of Mikurashima Village under Miyake Subprefecture of Tokyo Metropolis. As of 2009, the island's population was 351. Mikura-shima is also within the boundaries of the Fuji-Hakone-Izu National Park.
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분화 이력
상세 타임라인
- 기원전 4100년 (±100년)VEI ?지질학적 추정BCE 4100 ~ 진행 중Tsubunegamori & Yasukajigamori domes
- 기원전 5050년VEI ?지질학적 추정BCE 5050 ~ 진행 중
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