카메룬 · 화산군
Oku Volcanic Field
- 화산 유형
- 화산군
- 해발
- 3011m
- 마지막 분화
- 미확인

- 화산 유형
- 화산군
- 국가
- 카메룬
- 지역
- 북아프리카 / Western Africa Volcanic Province
- 해발
- 3011m
- 좌표
- 6.250, 10.500
- 마지막 분화
- 미확인
- 판구조 환경
- 판 내부 / 대륙 지각 (> 25 km)
- 화산 지형
- 화산군
- 주요 암석
- 현무암 / 피크로현무암
지질학적 요약
Numerous maars and basaltic cinder cones lie on or near the deeply dissected rhyolitic and trachytic Mount Oku massif along the Cameroon volcanic line. The Mount Oku stratovolcano is cut by a large caldera. The Oku volcanic field is noted for two crater lakes, Lake Nyos to the N and Lake Monoun to the S, that have produced catastrophic carbon-dioxide gas release events. The 15 August 1984 gas release at Lake Monoun was attributed to overturn of stratified lake water, triggered by an earthquake and landslide. The Lake Nyos event on 21 August 1986 caused at least 1,700 fatalities. The emission of ~1 km3 of magmatic carbon dioxide has been attributed either to overturn of stratified lake waters as a result of a non-volcanic process, or to phreatic explosions or injection of hot gas into the lake.
Wikipedia 요약
영어 요약The Oku Volcanic Field or Oku Massif is a group of volcanoes based on a swell in the Cameroon Volcanic Line, located in the Oku region of the Western High Plateau of Cameroon. The Mount Oku stratovolcano rises to 3,011 m above sea level.
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분화 이력
2건 기록용어집상세 타임라인
- 1986년VEI ?근거 미기재1986-08-21 ~ 1986-12-30Lake Nyos
- 1550년 (±100년)VEI 3근거 미기재1550 ~ 종료일 미상Lake Nyos
주변 화산
외부 링크
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