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Oku Volcanic Field

Tipe
Medan gunung api
Ketinggian
3011 m
Letusan terakhir
Tidak diketahui
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).
Tipe
Medan gunung api
Negara
Kamerun
Wilayah
Afrika Utara / Western Africa Volcanic Province
Ketinggian
3011 m
Koordinat
6.250, 10.500
Letusan terakhir
Tidak diketahui
Kondisi tektonik
Intralempeng / Kerak benua (> 25 km)
Bentuk lahan
Gugusan gunung api
Batuan utama
Basal / Pikrobasal
Ringkasan geologi

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.

Ringkasan Wikipedia

Ringkasan Inggris

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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Riwayat letusan

2 tercatatGlosarium
Ringkasan (VEI dari waktu ke waktu)
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1550~1594 · 1 letusan · VEI maks. 31942~1986 · 1 letusan · VEI maks. ?15501637176818551942

Garis waktu rinci

  1. 1986VEI ?Metode tidak dinyatakan
    1986-08-21 – 1986-12-30
    Lake Nyos
  2. 1550 (±100 tahun)VEI 3Metode tidak dinyatakan
    1550 – akhir tidak diketahui
    Lake Nyos

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