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Ol Doinyo Eburru

Eburru, Ol Doinyo

Complex volcano · Kenya · 2856m

Vegetated Eburru volcano (center) is elongated perpendicular to the Gregory Rift NW of Lake Naivasha (lower right). The E-W-trending main edifice is eroded, but young craters cut the E part of the summit ridge and probably-Holocene rhyolitic domes occur on the E flank. Extensive fumarolic activity occurs at scoria cones and craters constructed along faults cutting the massif. Lava flows of the Elmenteita Badlands are visible at the top-center portion of this Landsat image.
Vegetated Eburru volcano (center) is elongated perpendicular to the Gregory Rift NW of Lake Naivasha (lower right). The E-W-trending main edifice is eroded, but young craters cut the E part of the summit ridge and probably-Holocene rhyolitic domes occur on the E flank. Extensive fumarolic activity occurs at scoria cones and craters constructed along faults cutting the massif. Lava flows of the Elmenteita Badlands are visible at the top-center portion of this Landsat image. · Photo: NASA Landsat image, 1999 (courtesy of Hawaii Synergy Project, Univ. of Hawaii Institute of Geophysics & Planetology). · Wikimedia Commons
Type
Complex volcano
Country
Kenya
Region
Eastern Africa Volcanic Regions / Kenyan Rift Volcanic Province
Elevation
2856m
Coordinates
-0.650, 36.220
Last eruption
Unknown
Tectonic setting
Rift zone / Continental crust (> 25 km)
Landform
Composite
Major rock type
Rhyolite
Geological summary

Eburru volcano is elongated E-W perpendicular to the Gregory Rift NW of Lake Naivasha. The main edifice is eroded, but young partly vegetated rhyolitic domes occur on the E flank and are probably of Holocene age (Thompson and Dodson, 1963). Pleistocene phonolitic and trachytic lava flows are overlain by rhyolitic obsidian lava flows forming much of the N and NE slopes of the main massif. A prominent late-Pleistocene rhyolitic lava flow from a SE-flank vent extends almost to Lake Naivasha. Extensive fumarolic activity occurs at cinder cones and craters constructed along dominantly N-S faults cutting the massif.

From Wikipedia

Ol Doinyo Eburru is an active complex of volcanoes in the Great Rift Valley, Kenya to the northwest of Lake Naivasha. It is being exploited for geothermal energy. Soysambu Conservancy is located to the north of the massif, between Lake Elmenteita to the east and Lake Nakuru to the west.

Wikipedia · CC BY-SA · Read full article

Eruption history

Detailed timeline

No eruption records available.

External links

⚠ For reference only. Not for emergency response.