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Massiccio dell'Oku

Oku Volcanic Field

Campo vulcanico · 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 vulcanico
Paese
Cameroon
Regione
Northern Africa Volcanic Regions / Western Africa Volcanic Province
Altitudine
3011 m
Coordinate
6.250, 10.500
Ultima eruzione
Sconosciuto
Contesto tettonico
Intraplate / Continental crust (> 25 km)
Forma vulcanica
Cluster
Roccia principale
Basalt / Picro-Basalt
Sintesi geologica

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.

Sintesi da Wikipedia

Il Massiccio dell'Oku, o Campo vulcanico dell'Oku, è un gruppo di vulcani che fanno parte della linea vulcanica del Camerun. Il massiccio è situato nella regione di Oku, nell'Altopiano Occidentale del Camerun e a sud si fonde con i Monti Bambouto.

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Storia delle eruzioni

Riepilogo (VEI nel tempo)
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1550~1594 · 1 eruzioni · VEI max. 31942~1986 · 1 eruzioni · VEI max. ?15501637176818551942

Cronologia dettagliata

  1. 1986VEI ?Stima geologica
    1986-08-21 – 1986-12-30
    Lake Nyos
  2. 1550 (±100 anni)VEI 3Stima geologica
    1550 – In corso
    Lake Nyos

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