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Camerun · Campo vulcanico

Massiccio dell'Oku

Oku Volcanic Field

Tipo
Campo vulcanico
Altitudine
3011 m
Ultima eruzione
Sconosciuto
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
Camerun
Regione
Africa settentrionale / Western Africa Volcanic Province
Altitudine
3011 m
Coordinate
6.250, 10.500
Ultima eruzione
Sconosciuto
Contesto tettonico
Intraplacca / Crosta continentale (> 25 km)
Forma vulcanica
Gruppo vulcanico
Roccia principale
Basalto / Picrobasalto
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

Riassunto in inglese

The Oku Volcanic Field or Oku Massif is a group of volcanoes based on a swell in the Cameroon Volcanic Line, located in the Oku region of the Western High Plateau of Cameroon. The Mount Oku stratovolcano rises to 3,011 m above sea level.

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Storia delle eruzioni

2 registrateGlossario
Riepilogo (VEI nel tempo)
Fai clic su una barra per vedere le singole eruzioni · Usa le frecce per spostarti tra le barre, Invio per aprire
1550~1594 · 1 eruzioni · VEI max. 31942~1986 · 1 eruzioni · VEI max. ?15501637176818551942

Cronologia dettagliata

  1. 1986VEI ?Metodo non indicato
    1986-08-21 – 1986-12-30
    Lake Nyos
  2. 1550 (±100 anni)VEI 3Metodo non indicato
    1550 – fine sconosciuta
    Lake Nyos

Vulcani nelle vicinanze

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