South Island
Lake Turkana South Island
Stratovolcano · Kenya · 800m

- Type
- Stratovolcano
- Country
- Kenya
- Region
- Eastern Africa Volcanic Regions / Kenyan Rift Volcanic Province
- Elevation
- 800m
- Coordinates
- 2.636, 36.596
- Last eruption
- 1888
- Tectonic setting
- Rift zone / Continental crust (> 25 km)
- Landform
- Shield
- Major rock type
- Basalt / Picro-Basalt
Geological summary
The southernmost and largest of the three volcanic islands in Lake Turkana, South Island (sometimes referred to as Hohnel Island), contains numerous tuff cones. Early stage cone formation may have been associated with a high stand of Lake Turkana dated at about 10,000 years ago, and later subaerial activity postdates the last high stand of the lake about 3,200 years ago. The island is within a volcanic horst that extends 10 km to the N beneath the lake surface. Dominantly basaltic lava flows erupted from a N-S fissure extending the 11-km length of the island are morphologically similar to Holocene flows from The Barrier volcano at the S end of Lake Turkana. An eruption from a scoria cone on the island was witnessed during Count von Teliki's 1888 expedition.
From Wikipedia
South Island, or Hohnel Island, is a fissure-formed volcanic island and the largest one out of 3 other major islands in Lake Turkana, Kenya. This volcano was discovered in 1888 while it was erupting by Count Teleki, a Hungarian explorer who led the first expedition into the region. It is a part of the Lake Turkana National Parks, which is a UNESCO World Heritage Site.
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Eruption history
Detailed timeline
- 1888VEI 1Observed1888 – Ongoing
External links
⚠ For reference only. Not for emergency response.