Mallahle
성층화산 · Ethiopia-Eritrea · 1875m

- 화산 유형
- 성층화산
- 국가
- Ethiopia-Eritrea
- 지역
- Eastern Africa Volcanic Regions / Afar Rift Volcanic Province
- 해발
- 1875m
- 좌표
- 13.270, 41.650
- 마지막 분화
- 미확인
- 판구조 환경
- Rift zone / Intermediate crust (15-25 km)
- 화산 지형
- Composite
- 주요 암석
- Trachyte / Trachydacite
지질학적 요약
Mallahle is the central of three NE-SW-trending stratovolcanoes (along with Asavyo and Nabro) in the Danakil horst SW of Dubbi volcano. These volcanoes, plus Sork'Ale, form the Bidu Volcanic Complex. The volcano is truncated by a steep-walled 6-km-wide caldera, and is formed of rhyolitic lava flows and pyroclastics. Basaltic lava flows cover the slopes. Recent obsidian flows are found on the NW flank, and older obsidian flows were erupted on the northern caldera floor. Flank spatter and scoria cones are most numerous on the western side of the volcano. Extensive ignimbrite deposits associated with the collapse of Mallahle and Nabro volcanoes cover the countryside.
Wikipedia 요약
영어 요약Mallahle is a stratovolcano on the border of Ethiopia and Eritrea, with a 6 km wide caldera.
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