
Mont Cameroun
Mountain · 4,040 m
Mont Cameroun is a mountain rising to 4,040 metres (13,255 ft) in Cameroon, in the Africa region. From PeakBagger.com, with kind permission..
Mount Cameroon is an active stratovolcano in the Southwest Region of Cameroon next to the city of Buea near the Gulf of Guinea. Mount Cameroon is also known as Cameroon Mountain or Fako (the name of the higher of its two peaks) or by its indigenous name Mongo ma Ndemi ("Mountain of Greatness"). Mount Cameroon is ranked 22nd by topographic isolation.
It is the highest point in sub-Saharan western and central Africa, the fourth-most prominent peak in Africa, and 31st-most prominent in the world.
The mountain is part of the area of volcanic activity known as the Cameroon Volcanic Line, which also includes Lake Nyos, the site of a disaster in 1986. The eruption of 28 April-June 1909 caused the German colonial government of Kamerun to temporarily move from Buea to Douala. The most recent eruption occurred on February 3, 2012.
Adapted from Wikipedia: Mount Cameroon (CC BY-SA 4.0).
- Elevation
- 4,040 m (13,255 ft)
- Global rank
- #121 of 641 indexed
- Region
- Africa (#11)
- Country
- Cameroon
- Coordinates
- 4.2200°, 9.1700°
Of the 641 named summits indexed in YearMaps, Mont Cameroun ranks #121 by elevation, below Cerro San Valentín (4,058 m) and above Dombai-Ulgen (4,038 m).
- Ranges:
- Marrah Mountains (Africa), Guinea Highlands (Africa)
- Neighbouring summits:
- Pico de Santa Isabel (3,008 m), Mount Oku (3,011 m), Chappal Wadi (2,419 m)
More about Mont Cameroun
Geology
Mount Cameroon lies on the Cameroon Volcanic Line, a 1,600 km (990 mi) NE–SW belt of oceanic and continental volcanoes stretching from Pagalu Island in the Gulf of Guinea to northern Cameroon. The volcano forms an elliptical stratovolcano about 50 km × 35 km with a volume of roughly 1,200 km3. It sits on a horst of Precambrian granite and gneiss overlain by Cretaceous to Quaternary sediments. The summit is cut by several tectonic axes, notably the Debundscha axis (N60–70°), Limbe axis (N140–150°) and Batoke axis (N30–40°), inherited from basement shear zones. Gravity and wavelet-analysis studies reveal dense mantle intrusions rising into the crust and suggest that the Tiko and Ekona faults focus magma ascent to depths of at least 25 km.
Sections adapted from Wikipedia: Mount Cameroon (CC BY-SA 4.0).
Mont Cameroun: Key Facts
| Topographic prominence | 3,901 m |
|---|---|
| Mountain range | Cameroon line |
Facts from Wikidata Q190562 (CC0).


