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Oku Volcanic Field

Volcanic field · Cameroon · 3011m

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. · Photo: Photo by Jack Lockwood, 1986 (U.S. Geological Survey).
Type
Volcanic field
Country
Cameroon
Region
Northern Africa Volcanic Regions / Western Africa Volcanic Province
Elevation
3011m
Coordinates
6.250, 10.500
Last eruption
Unknown
Tectonic setting
Intraplate / Continental crust (> 25 km)
Landform
Cluster
Major rock type
Basalt / Picro-Basalt
Geological summary

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.

From Wikipedia

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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Eruption history

Summary (VEI over time)
Click a bar to see individual eruptions
1550~1594 · 1 eruptions · max VEI 31942~1986 · 1 eruptions · max VEI ?15501637176818551942

Detailed timeline

  1. 1986VEI ?Geological estimate
    1986-08-21 – 1986-12-30
    Lake Nyos
  2. 1550 (±100 yrs)VEI 3Geological estimate
    1550 – Ongoing
    Lake Nyos

External links

⚠ For reference only. Not for emergency response.