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Olkaria

Pyroclastic cone · Kenya · 2434m

Vents of the northern part of the Olkaria volcanic complex are visible immediately S of Lake Naivasha (upper right). It comprises up to 80 individual rhyolitic centers, many of which are visible in this Landsat image. The youngest known eruption has a radiocarbon age of about 180 years. Fumarolic activity occurs at the Njorowa Gorge and at the Orengingnai and Orkaria (Olgaria) pumice cones.
Vents of the northern part of the Olkaria volcanic complex are visible immediately S of Lake Naivasha (upper right). It comprises up to 80 individual rhyolitic centers, many of which are visible in this Landsat image. The youngest known eruption has a radiocarbon age of about 180 years. Fumarolic activity occurs at the Njorowa Gorge and at the Orengingnai and Orkaria (Olgaria) pumice cones. · Photo: NASA Landsat image, 1999 (courtesy of Hawaii Synergy Project, Univ. of Hawaii Institute of Geophysics & Planetology). · Wikimedia Commons
Type
Pyroclastic cone
Country
Kenya
Region
Eastern Africa Volcanic Regions / Kenyan Rift Volcanic Province
Elevation
2434m
Coordinates
-0.904, 36.292
Last eruption
1770
Tectonic setting
Rift zone / Continental crust (> 25 km)
Landform
Cluster
Major rock type
Rhyolite
Geological summary

The Olkaria volcanic complex, located immediately S of Lake Naivasha and W of Longonot volcano, comprises up to 80 individual alkali rhyolite centers. A thick, geochemically diverse basal complex is overlain by a dominantly silicic lava-dome and lava-flow complex constructed within a largely obscured 11 x 7.5-km-wide caldera that formed about 20,000 years ago following the eruption of welded alkali rhyolite ignimbrites. The youngest known eruption originated from the Ololbutot fissure on the SW side of the complex and produced a 5 km3 lava flow and a pumice flow that has a radiocarbon age of about 180 years. Fumarolic activity occurs at the Njorowa Gorge, and at the Orengingnai and Olkaria (Orgaria) pumice cones. Olkaria is the site of a large 50-80 km3 high-temperature geothermal field.

From Wikipedia

The Olkaria Area is a region located immediately to the south of Lake Naivasha in the Great Rift Valley of Kenya, Africa. It is geothermally active and is being used to generate clean electric power. The region has an estimated potential of 2,000 MW. This is almost double the maximum daily electricity peak demand recorded in 2008/2009 for the entire country.

Wikipedia · CC BY-SA · Read full article

Eruption history

Summary (VEI over time)
Click a bar to see individual eruptions
6050 BCE~5789 BCE · 1 eruptions · max VEI ?4225 BCE~3965 BCE · 1 eruptions · max VEI ?1509~1770 · 1 eruptions · max VEI ?6050 BCE4225 BCE2140 BCE315 BCE1509

Detailed timeline

  1. 1770 (±50 yrs)VEI ?Geological estimate
    1770 – Ongoing
    Ololbutot
  2. 4050 BCEVEI ?Geological estimate
    BCE 4050 – Ongoing
  3. 6050 BCEVEI ?Geological estimate
    BCE 6050 – Ongoing
    NE side (Gorge Farm)

External links

⚠ For reference only. Not for emergency response.