Mallahle
Stratovolcano · Ethiopia-Eritrea · 1875m

- Type
- Stratovolcano
- Country
- Ethiopia-Eritrea
- Region
- Eastern Africa Volcanic Regions / Afar Rift Volcanic Province
- Elevation
- 1875m
- Coordinates
- 13.270, 41.650
- Last eruption
- Unknown
- Tectonic setting
- Rift zone / Intermediate crust (15-25 km)
- Landform
- Composite
- Major rock type
- Trachyte / Trachydacite
Geological summary
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.
From Wikipedia
Mallahle is a stratovolcano on the border of Ethiopia and Eritrea, with a 6 km wide caldera.
Wikipedia · CC BY-SA · Read full article →
Eruption history
Detailed timeline
No eruption records available.
External links
⚠ For reference only. Not for emergency response.