Mount Rungwe
Rungwe
성층화산 · Tanzania · 2953m

- 화산 유형
- 성층화산
- 국가
- Tanzania
- 지역
- Eastern Africa Volcanic Regions / Rukwa Rift Volcanic Province
- 해발
- 2953m
- 좌표
- -9.135, 33.668
- 마지막 분화
- 1250년
- 판구조 환경
- Rift zone / Continental crust (> 25 km)
- 화산 지형
- Composite
- 주요 암석
- Trachyte / Trachydacite
지질학적 요약
Rungwe volcano, the largest in the Karonga basin NW of Lake Malawi (Lake Nyasa), is cut by a 4-km-wide caldera that is breached to the WSW. Hummocky terrain from a debris-avalanche deposit produced by collapse of the summit and western flank extends at least 20 km SW of the volcano. The trachytic caldera is largely filled by a series of youthful-looking uneroded and sparsely vegetated pumice cones, lava domes, and explosion craters. The latter are also found on the southern and northern flanks. A large area of basaltic cones and lava flows are found on the NW flank, and youthful-looking lava flows extend SW from vents inside the caldera. Explosive and effusive eruptions were produced during the Holocene; the largest explosive eruption took place about 4,000 years ago, and the most recent about 1,200 years ago.
Wikipedia 요약
영어 요약Mount Rungwe is a volcanic mountain in Mbeya Region, in Tanzania's Southern Highlands. At an altitude of 2,981 metres (9,780 ft), it is southern Tanzania's second-highest peak. Rungwe's volcano is currently inactive.
Wikipedia · CC BY-SA · 전체 기사 보기 →
분화 이력
상세 타임라인
- 1250년 (±40년)VEI ?지질학적 추정1250 ~ 진행 중
- 기원전 50년 (±100년)VEI 4지질학적 추정BCE 50 ~ 진행 중
- 기원전 2050년VEI 5지질학적 추정BCE 2050 ~ 진행 중
외부 링크
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