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Macizo Oku

Oku Volcanic Field

Campo volcánico · Cameroon · 3011 m

Lake Nyos is the most renowned of the numerous maars and basaltic cinder cones associated with the deeply dissected Mount Oku massif. The 1.2 x 1.9 km wide lake, seen here from the south, was the site of a gas-release event on 21 August 1986 that caused at least 1,700 fatalities. Wave damage stripped the peninsula at the left of vegetation. The emission of around 1 km3 of magmatic carbon dioxide has been attributed to either non-volcanic overturn of stratified lake waters, to phreatic explosions, or to injection of hot gas into the lake.
Lake Nyos is the most renowned of the numerous maars and basaltic cinder cones associated with the deeply dissected Mount Oku massif. The 1.2 x 1.9 km wide lake, seen here from the south, was the site of a gas-release event on 21 August 1986 that caused at least 1,700 fatalities. Wave damage stripped the peninsula at the left of vegetation. The emission of around 1 km3 of magmatic carbon dioxide has been attributed to either non-volcanic overturn of stratified lake waters, to phreatic explosions, or to injection of hot gas into the lake. · Foto: Photo by Jack Lockwood, 1986 (U.S. Geological Survey).
Tipo
Campo volcánico
País
Cameroon
Región
Northern Africa Volcanic Regions / Western Africa Volcanic Province
Altitud
3011 m
Coordenadas
6.250, 10.500
Última erupción
Desconocido
Contexto tectónico
Intraplate / Continental crust (> 25 km)
Forma volcánica
Cluster
Roca principal
Basalt / Picro-Basalt
Resumen geológico

Numerous maars and basaltic cinder cones lie on or near the deeply dissected rhyolitic and trachytic Mount Oku massif along the Cameroon volcanic line. The Mount Oku stratovolcano is cut by a large caldera. The Oku volcanic field is noted for two crater lakes, Lake Nyos to the N and Lake Monoun to the S, that have produced catastrophic carbon-dioxide gas release events. The 15 August 1984 gas release at Lake Monoun was attributed to overturn of stratified lake water, triggered by an earthquake and landslide. The Lake Nyos event on 21 August 1986 caused at least 1,700 fatalities. The emission of ~1 km3 of magmatic carbon dioxide has been attributed either to overturn of stratified lake waters as a result of a non-volcanic process, or to phreatic explosions or injection of hot gas into the lake.

Resumen de Wikipedia

El Campo Volcánico Oku o Macizo Oku es un grupo de volcanes en la Línea Volcánica de Camerún, ubicado en la región Oku del Altiplano Occidental de Camerún. El estratovolcán del Monte Oku se eleva a 3.011 m sobre el nivel del mar.

Wikipedia · CC BY-SA · Leer artículo completo

Historial de erupciones

Resumen (VEI en el tiempo)
Haga clic en una barra para ver erupciones individuales
1550~1594 · 1 erupciones · VEI máx. 31942~1986 · 1 erupciones · VEI máx. ?15501637176818551942

Línea de tiempo detallada

  1. 1986VEI ?Estimación geológica
    1986-08-21 – 1986-12-30
    Lake Nyos
  2. 1550 (±100 años)VEI 3Estimación geológica
    1550 – En curso
    Lake Nyos

Enlaces externos

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