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

- Tipo
- Estratovolcán
- País
- Kenya
- Región
- Eastern Africa Volcanic Regions / Kenyan Rift Volcanic Province
- Altitud
- 800 m
- Coordenadas
- 2.636, 36.596
- Última erupción
- 1888
- Contexto tectónico
- Rift zone / Continental crust (> 25 km)
- Forma volcánica
- Shield
- Roca principal
- Basalt / Picro-Basalt
Resumen geológico
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.
Resumen de Wikipedia
Resumen en inglésSouth 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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Historial de erupciones
Línea de tiempo detallada
- 1888VEI 1Observado1888 – En curso
Enlaces externos
⚠ Solo como referencia. No apto para respuesta ante emergencias.