Menengai
순상화산 · Kenya · 2278m

- 화산 유형
- 순상화산
- 국가
- Kenya
- 지역
- Eastern Africa Volcanic Regions / Kenyan Rift Volcanic Province
- 해발
- 2278m
- 좌표
- -0.200, 36.070
- 마지막 분화
- -6050년
- 판구조 환경
- Rift zone / Continental crust (> 25 km)
- 화산 지형
- Shield
- 주요 암석
- Trachyte / Trachydacite
지질학적 요약
The massive Menengai shield volcano occupies the floor of the East African Rift. Construction of a 30 km3 shield volcano beginning about 200,000 years ago was followed by the eruption of two voluminous ash-flow tuffs, each preceded by major pumice falls. The first took place about 29,000 years ago and produced a large caldera. The second, producing about 30 km3 of compositionally zoned peralkaline trachytic magma about 8000 years ago, was associated with formation of the present-day 8 x 12 km summit caldera. More than 70 post-caldera lava flows cover the caldera floor, the youngest of which may be only a few hundred years old. No historical eruptions are known. Fumarolic activity is restricted to the caldera.
Wikipedia 요약
영어 요약Menengai Crater is a massive shield volcano with one of the biggest calderas in the world, in the Great Rift Valley, Kenya. It is the largest volcano caldera in Kenya and the second largest volcano caldera in Africa. Volcanic formed rich loam soils enrich the adjacent farmland around its flanks. The crater is on the floor of the Rift Valley. The volcano formed about 200,000 years ago and the prominent 12 x 8 km caldera formed about 8000 years ago. The caldera floor is covered with numerous post caldera lava flows. The Menengai volcano is considered one of the best-preserved Krakatau-style calderas in the world. Menengai has very little sediment in the caldera which is a thick mass of lava boulders and inaccessible ridges. Volcanic activity continues and a current project under the GDC is at an advanced stage towards geothermal power generation.
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분화 이력
상세 타임라인
- 기원전 6050년VEI 6지질학적 추정BCE 6050 ~ 진행 중
- 기원전 7350년 (±500년)VEI ?지질학적 추정BCE 7350 ~ 진행 중
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