Manda-Inakir (Arabic: ماندا-إناكير) is a system of fissure vents and cinder cones located along the borders between Djibouti, Eritrea and Ethiopia. Last erupting in 1928, it produced a cinder cone called Kammourta. It has an elevation of over 600 metres.
| Manda-Inakir ماندا-إناكير | |
|---|---|
 Manda-Inakir lava flows | |
| Highest point | |
| Elevation | 600+ metres (1,968 feet) |
| Coordinates | 12°38′N 42°20′E / 12.633°N 42.333°E |
| Geography | |
 | |
| Location | Djibouti, Eritrea and Ethiopia |
| Geology | |
| Rock age | Historical |
| Mountain type | Fissure vents |
| Last eruption | 1928 |
See also
editReferences
edit- "Manda-Inakir". Global Volcanism Program. Smithsonian Institution. Retrieved 2014-08-29.
- Manda-Inakir
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