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Barrier (volcán)

Barrier, The

Volcán en escudo · Kenya · 1032 m

A northward-looking aerial view shows the summit caldera of Kakorinya volcano of The Barrier volcanic complex with Lake Turkana in the distance. The 3.8-km-wide summit caldera was formed about 92,000 years ago, and post-caldera lava domes and flows fill much of the caldera floor. Fresh-looking lava flows and tuff cones occur along the shores of Lake Turkana. Teleki's Cone on the northern flank and Andrew's Cone (lower left foreground) on the southern flank have been the source of historical lava flows.
A northward-looking aerial view shows the summit caldera of Kakorinya volcano of The Barrier volcanic complex with Lake Turkana in the distance. The 3.8-km-wide summit caldera was formed about 92,000 years ago, and post-caldera lava domes and flows fill much of the caldera floor. Fresh-looking lava flows and tuff cones occur along the shores of Lake Turkana. Teleki's Cone on the northern flank and Andrew's Cone (lower left foreground) on the southern flank have been the source of historical lava flows. · Foto: Photo by Martin Smith, 1993 (copyright British Geological Survey, NERC).
Tipo
Volcán en escudo
País
Kenya
Región
Eastern Africa Volcanic Regions / Kenyan Rift Volcanic Province
Altitud
1032 m
Coordenadas
2.320, 36.570
Última erupción
1921
Contexto tectónico
Rift zone / Continental crust (> 25 km)
Forma volcánica
Shield
Roca principal
Trachyte / Trachydacite
Resumen geológico

The Barrier volcanic complex separates Lake Turkana from the broad Suguta Trough to the S, the site of a former lake. The volcano is comprised of four overlapping shield volcanoes, with the youngest, Kakorinya, located over the axis of the East African Rift. Kalolenyang volcano lies W of Kakorinya, and Likaiu West and Likaiu East are located to the ENE. A 3.8-km-wide summit caldera was formed at Kakorinya about 92,000 years ago. Youthful-looking trachytic and phonolitic lava domes and flows erupted within the caldera and along its ring fracture fill much of the caldera floor. Early Holocene fissure-related scoria cones and lava flows dot the S and N flanks. Solfataric fields are located within the caldera and on the W and S flanks. Historical eruptions from Teleki's and Andrew's cones on the N and S flanks, respectively, have produced basaltic explosive activity and lava flows during the 19th and 20th centuries.

Resumen de Wikipedia

El Barrier es un volcán en escudo del Valle Suguta. Recibe su nombre porque forma una barrera de unos 20 km separando el valle del Suguta del lago Turkana.

Wikipedia · CC BY-SA · Leer artículo completo

Historial de erupciones

Resumen (VEI en el tiempo)
Haga clic en una barra para ver erupciones individuales
7710 BCE~7389 BCE · 1 erupciones · VEI máx. ?958~1279 · 3 erupciones · VEI máx. 01600~1921 · 8 erupciones · VEI máx. 27710 BCE5463 BCE2894 BCE647 BCE1600

Línea de tiempo detallada

  1. 1921VEI 2Observado
    1921-12-31 – En curso
    North flank (Teleki)
  2. 1920 (±3 años)VEI ?Estimación geológica
    1920 – En curso
    South flank (Andrew's Volcano)
  3. 1917VEI 2Observado
    1917 – En curso
    Andrew's or Teleki's Volcanoes
  4. 1906VEI ?Estimación geológica
    1906 – En curso
    Andrew's or Teleki's Cones
  5. 1897VEI 2Observado
    1897-05 – En curso
    North flank (Teleki) and Likaiu
  6. 1895VEI 2Observado
    1895 – En curso
    North flank (Teleki's Cone)
  7. 1888VEI 0Observado
    1888 – En curso
    North flank (Teleki's Cone)
  8. 1871 (±3 años)VEI 2Observado
    1871 – En curso
    North flank (Teleki's Cone)
  9. 1090 (±50 años)VEI 0Estimación geológica
    1090 – En curso
    North flank
  10. 1050 (±150 años)VEI 0Estimación geológica
    1050 – En curso
    North flank
  11. 1030 (±150 años)VEI 0Estimación geológica
    1030 – En curso
    North flank
  12. 7710 a. C. (±200 años)VEI ?Estimación geológica
    BCE 7710 – En curso
    North (Abili Agituk) and south flanks

Enlaces externos

⚠ Solo como referencia. No apto para respuesta ante emergencias.