Olkaria
Kerucut piroklastik · Kenya · 2434 m

- Tipe
- Kerucut piroklastik
- Negara
- Kenya
- Wilayah
- Eastern Africa Volcanic Regions / Kenyan Rift Volcanic Province
- Ketinggian
- 2434 m
- Koordinat
- -0.904, 36.292
- Letusan terakhir
- 1770
- Kondisi tektonik
- Rift zone / Continental crust (> 25 km)
- Bentuk lahan
- Cluster
- Batuan utama
- Rhyolite
Ringkasan geologi
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.
Ringkasan Wikipedia
Ringkasan InggrisThe 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.
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Riwayat letusan
Garis waktu rinci
- 1770 (±50 tahun)VEI ?Perkiraan geologi1770 – BerlangsungOlolbutot
- 4050 SMVEI ?Perkiraan geologiBCE 4050 – Berlangsung
- 6050 SMVEI ?Perkiraan geologiBCE 6050 – BerlangsungNE side (Gorge Farm)
Tautan eksternal
⚠ Untuk referensi saja. Bukan untuk tanggap darurat.