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Mount Cameroon

Webpages concerning "Mount Cameroon"

Cameroons cutting edge institution for integrated research on biodiversity, forestry and horticulture and provides services in a wide range of fields including wildlife, botany, ecology, vegetation mapping and socio-economics
http://www.mcbcclimbe.org/
Keywords:
Limbe, Botanical, and, Zoological, Gardens, /, Mount, Cameroon, Biodiversity, Conservation, Centre, Cameroon, Africa, Tropical, Rainforest, Wildlife

http://www.mcbcclimbe.org/

improving the resolution of digital elevation models by using SAR interferometry
http://www.dfd.dlr.de/app/iom/1998_11/
Keywords:
SAR, Interferometry, Mount Cameroon

http://www.dfd.dlr.de/app/iom/1998_11/

http://www.nri.org/TFF/TFFnews/issue4/tffiss4b.htm

http://www.nri.org/TFF/TFFnews/issue4/tffiss4b.htm

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Wikipedia-Article "Mount Cameroon"


Mount Cameroon

Craters from the 2000 eruptions
Elevation: 4,095 m (13,435 ft)
Location: Southwest Province, Cameroon
Prominence: 3,961 m (12,995 ft)
Coordinates: 4°12′N, 9°11′E
Type: stratovolcano
Age of rock:  ? yr
Last eruption: 2000
First ascent: 1861 by Sir Richard Francis Burton
Easiest route: scramble

Mount Cameroon (also known as Cameroon Mountain or Fako) is an active volcano in Cameroon, near the Gulf of Guinea and is part of a general area of volcanic activity the Cameroon Volcanic Line, which also includes Lake Nyos, the site of the 1986 Lake Nyos tragedy. The volcano last erupted on March 28, 1999 and May 28, 2000.

Mt. Cameroon, one of Africa's largest volcanoes, rises to 4095 m above the coast of west Cameroon. The massive steep-sided volcano of dominantly basaltic-to-trachybasaltic composition forms a volcanic horst constructed above a basement of Precambrian metamorphic rocks covered with Cretaceous to Quaternary sediments. More than 100 small cinder cones, often fissure-controlled parallel to the long axis of the massive 1400 cu km volcano, occur on the flanks and surrounding lowlands. A large satellitic peak, Etinde (also known as Little Cameroon), is located on the southern flank near the coast. Historical activity, the most frequent of west African volcanoes, was first observed in the 5th century BC by the Carthaginian navigator Hannon. During historical time, moderate explosive and effusive eruptions have occurred from both summit and flank vents. A 1922 SW-flank eruption produced a lava flow that reached the Atlantic coast, and a lava flow from a 1999 south-flank eruption stopped only 200 m from the sea.

The peak can be reached by hikers, while the annual Mount Cameroon Race scales the peak in around 4½ hours.

English explorer Mary Kingsley, one of the first Europeans to scale the mountain, recounts her expedition in her 1897 memoir Travels in West Africa.

Sources


  • Siebert, L. and T. Simkin (2002-). Volcanoes of the World: an Illustrated Catalog of Holocene Volcanoes and their Eruptions. Smithsonian Institution, Global Volcanism Program Digital Information Series, GVP-3. URL: http://www.volcano.si.edu/world/

External links

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