Ehi Mousgou
Voon, Tarso
성층화산 · Chad · 3100m

- 화산 유형
- 성층화산
- 국가
- Chad
- 지역
- 북아프리카 / East Central Sahara Volcanic Province
- 해발
- 3100m
- 좌표
- 20.920, 17.280
- 마지막 분화
- 미확인
- 판구조 환경
- Intraplate / Continental crust (> 25 km)
- 화산 지형
- Composite
- 주요 암석
- Trachyte / Trachydacite
지질학적 요약
The broad summit of Tarso Voon volcano, located in the west-central part of the Tibesti Range, is truncated by a shallow 14 x 18 km wide caldera. Ignimbrite deposits surround the caldera to distances of 15-35 km. It was constructed over a basement of Precambrian schists. Youthful-looking Quaternary basaltic lava flows have been erupted from vents near the caldera rim over a 180-degree area extending counterclockwise from the NE and from Ehi Mousgau, a 3100-m-high stratovolcano located to the NW. The Soborom solfatara field, the largest in the Tibesti Range, is located in an area of volcano-tectonic uplift 5 km west of the caldera rim. Its fumaroles, active mud pots, and boiling waters are visited by Tibesti peoples for medicinal uses.
분화 이력
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