Penguin Island
성층화산 · Antarctica · 180m
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- 화산 유형
- 성층화산
- 국가
- Antarctica
- 지역
- Antarctic-Scotia Volcanic Regions / South Shetlands Volcanic Arc
- 해발
- 180m
- 좌표
- -62.100, -57.930
- 마지막 분화
- 1905년
- 판구조 환경
- Intraplate / Continental crust (> 25 km)
- 화산 지형
- Composite
- 주요 암석
- Basalt / Picro-Basalt
지질학적 요약
The 1.4 x 1.7 km Penguin Island is located off the SE coast of King George Island in Antarctica's South Shetland Islands, west of the axis of the Bransfield Rift. The most prominent feature is Deacon Peak, a basaltic scoria cone with a 350-m-wide summit crater on the SW side of the island. A small plug of basaltic lava occupies the 75-m-deep crater. Petrel Crater, a 300-m-wide maar, is located near the east coast. The formation of Deacon Peak was dated by lichenometry at about 300 years ago, and the younger Petrel Crater maar was dated at about 100 years (Birkenmajer, 1979). Some reports of fumarolic activity on nearby Bridgeman Island are attributed to the more youthful Penguin Island.
Wikipedia 요약
영어 요약Penguin Island is one of the smaller of the South Shetland Islands of Antarctica.
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분화 이력
상세 타임라인
- 1905년VEI ?지질학적 추정1905 ~ 진행 중NE flank (Petrel Crater)
- 1850년VEI ?관측 기록1850 ~ 진행 중Deacon Peak
- 1683년VEI ?지질학적 추정1683 ~ 진행 중Deacon Peak
외부 링크
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