Manda-Inakir
Sign in to saveAlso known as Manda Inakir
Manda-Inakir () 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.
In the Vinony graph
Within Vinony's link graph, Manda-Inakir is referenced by 5 other articles, and connects out to Ethiopia, Arabic and Eritrea.
The entry is geolocated on the map in mountain, across 2 mapped points.
Vinony files it under Cinder cones, Fissure vents and Volcanoes of Djibouti.
Its subject is documented across 12 Wikipedia language editions.
Key facts
- Mountain.name
- Manda-Inakirماندا-إناكير
- Mountain.photo
- Manda-Inakir.jpg
- Mountain.photo_caption
- Manda-Inakir lava flows
- Mountain.elevation
- 600+ metres (1,968 feet)
- Mountain.location
- Djibouti, Eritrea and Ethiopia
- Mountain.type
- Fissure vents
- Mountain.age
- Historical
- Mountain.last_eruption
- 1928
via Wikipedia infobox
Wikidata facts
- Instance of
- mountain
- Part of
- Great Rift Valley
- Country
- Eritrea
- Located in
- Awsi Rasu
- Elevation
- 600
- Material used
- basalt
- Image
- Manda-Inakir.jpg
via Wikidata · CC0
~1 min read
Encyclopedic overview
2 sectionsContents
- See also
- References
Manda-Inakir () 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.
==See also== Emba Soira
Excerpted from Wikipedia’s “Manda-Inakir” article, available under the CC BY-SA 4.0 licence.
On the map
2 mapped locations