O'a Caldera
Shala
Caldera · Ethiopia · 2075m

- Type
- Caldera
- Country
- Ethiopia
- Region
- Eastern Africa Volcanic Regions / Main Ethiopian Rift Volcanic Province
- Elevation
- 2075m
- Coordinates
- 7.457, 38.557
- Last eruption
- Unknown
- Tectonic setting
- Rift zone / Continental crust (> 25 km)
- Landform
- Caldera
- Major rock type
- Rhyolite
Geological summary
The Shala (also known as O'a) caldera along the central Main Ethiopian Rift forms the eastern portion of the 15 x 25 km Lake Shala. Formation of the caldera about 240,000 years ago was accompanied by the eruption of two ignimbrite deposits, the first of which was strongly welded. The only post-caldera activity consists of two pyroclastic cones to the N, one silicic and the other basaltic, and a group of tuff rings, spatter cones, and lava flows of Holocene age near the SW shore of the lake. These were erupted along the Corbetti-Shalla segment of the Wonji Fault Belt, which extends N from Corbetti caldera. Fumarolic activity continues on all sides of the lake.
From Wikipedia
The O'a Caldera, also known as Shala, is a volcanic caldera in Ethiopia. It has two lakes: Lake Shala and a small maar called Lake Chitu. Sub-features include Mount Fike and Mount Billa.
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Eruption history
Detailed timeline
No eruption records available.
External links
⚠ For reference only. Not for emergency response.