Semisopochnoi Island
Semisopochnoi
성층화산 · United States · 1221m

- 화산 유형
- 성층화산
- 국가
- United States
- 지역
- North America Volcanic Regions / Aleutian Ridge Volcanic Arc
- 해발
- 1221m
- 좌표
- 51.930, 179.580
- 마지막 분화
- 2023년
- 판구조 환경
- Subduction zone / Intermediate crust (15-25 km)
- 화산 지형
- Composite
- 주요 암석
- Basalt / Picro-Basalt
지질학적 요약
Semisopochnoi, the largest subaerial volcano of the western Aleutians, is 20 km wide at sea level and contains an 8-km-wide caldera. It formed as a result of collapse of a low-angle, dominantly basaltic volcano following the eruption of a large volume of dacitic pumice. The high point of the island is Anvil Peak, a double-peaked late-Pleistocene cone that forms much of the island's northern part. The three-peaked Mount Cerberus (renamed Mount Young in 2023) was constructed within the caldera during the Holocene. Each of the peaks contains a summit crater; lava flows on the N flank appear younger than those on the south side. Other post-caldera volcanoes include the symmetrical Sugarloaf Peak SSE of the caldera and Lakeshore Cone, a small cinder cone at the edge of Fenner Lake in the NE part of the caldera. Most documented eruptions have originated from Young, although Coats (1950) considered that both Sugarloaf and Lakeshore Cone could have been recently active.
Wikipedia 요약
영어 요약Semisopochnoi Island or Unyak Island is part of the Rat Islands group in the western Aleutian Islands of Alaska. The island is uninhabited and provides an important nesting area for maritime birds. The island is of volcanic origin, containing several volcanoes including Mount Young. It has a land area of 85.558 square miles, measuring 11 miles (18 km) in length and 12 miles (20 km) in width.
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분화 이력
상세 타임라인
- 2021년VEI 2관측 기록2021-02-02 ~ 2023-05-05North Cerberus
- 2019년VEI 1관측 기록2019-12-07 ~ 2020-06-19North Cerberus
- 2019년VEI 1관측 기록2019-07-16 ~ 2019-08-24
- 2018년VEI 1관측 기록2018-09-08 ~ 2018-10-31North Cone of Mount Cerberus (Mount Young)
- 1987년VEI 2관측 기록1987-04-13 ~ 1987-04-18Sugarloaf ?
- 1873년VEI ?관측 기록1873 ~ 진행 중Cerberus
- 1830년VEI ?지질학적 추정1830 ~ 진행 중Cerberus
- 1792년VEI ?지질학적 추정1792 ~ 진행 중Cerberus
- 1790년VEI ?지질학적 추정1790 ~ 진행 중Cerberus
- 1772년VEI ?지질학적 추정1772 ~ 진행 중Cerberus
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