McDonald Island
McDonald Islands
복합화산 · Australia · 263m

- 화산 유형
- 복합화산
- 국가
- Australia
- 지역
- 소말리아·남극 / Kerguelen Hotspot Volcano Group
- 해발
- 263m
- 좌표
- -53.039, 72.595
- 마지막 분화
- 2005년
- 판구조 환경
- Intraplate / Oceanic crust (< 15 km)
- 화산 지형
- Composite
- 주요 암석
- Phonolite
지질학적 요약
The McDonald Islands are located on the Kerguelen Plateau about 75 km W of Heard Island. The largest island, McDonald, is composed of a layered phonolitic tuff plateau cut by phonolitic dikes and lava domes. A possible nearby active submarine center was inferred from phonolitic pumice that washed up on Heard Island in 1992. Volcanic plumes were observed in December 1996 and January 1997 from McDonald Island. During March 1997 the crew of a vessel that sailed near the island noted vigorous steaming from a vent on the N side of the island along with possible pyroclastic deposits and lava flows. A satellite image taken in November 2001 showed the island to have more than doubled in area since previous reported observations in November 2000.
분화 이력
상세 타임라인
- 2005년VEI 0관측 기록2005-07-12 ~ 진행 중
- 2004년VEI 1지질학적 추정2004-11-14 ~ 2004-11-14
- 2001년VEI 1관측 기록2001-05-03 ~ 진행 중
- 1996년VEI 1관측 기록1996-12-16 ~ 1997-02-10Northern part of McDonald Island
- 1992년VEI 0관측 기록1992-12-16 ~ 진행 중Submarine vent near McDonald Islands
외부 링크
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