Ethiopia · Volcanic field
Bishoftu Volcanic Field
- Type
- Volcanic field
- Elevation
- 1850m
- Last eruption
- Unknown
- Type
- Volcanic field
- Country
- Ethiopia
- Region
- Eastern Africa / Main Ethiopian Rift Volcanic Province
- Elevation
- 1850m
- Coordinates
- 8.780, 38.980
- Last eruption
- Unknown
- Tectonic setting
- Rift zone / Continental crust (> 25 km)
- Landform
- Cluster
- Major rock type
- Basalt / Picro-basalt
Geological summary
The Bishoftu volcanic field, also known as Debre Zeit, consists of an area of fissure-fed Holocene lava flows, cinder cones, tuff rings, and maars. Several of the maars are filled by lakes, which are popular recreational destinations from the nearby capital city of Addis Ababa. Most of the craters and cones are aligned NE-SW, parallel to the direction of the Ethiopian Rift Valley. The 750 x 1000 m Haro Maja tuff ring and its neighbor, lake-filled Kilole, are offset to the east. The cones and maars of the volcanic field were erupted through rhyolitic welded tuffs.
Eruption history
GlossaryDetailed timeline
No eruption records available.
Nearby volcanoes
External links
- Not yet on Wikipedia (English). You can contribute on Wikidata.
- Smithsonian GVP source page
⚠ For reference only. Not for emergency response.