Activity was similar during 0900-1200 on 14 April, except for the NE-most cone, which produced two gray turbulent columns until 1000.

In some cases additional feature type, elevation, or location details are provided.Mount Cameroon, one of Africa's largest volcanoes, rises above the coast of west Cameroon. On the basis of first-hand knowledge of some of their co-authors, Wantim and others (2011) stated that the eruption occurred during 28 May and 20 July 2000. It was difficult to locate the earthquakes because of inadequate seismic equipment.The Assistant Director of the Institute for Mining and Geological Research (IRGM) at Ekona, Richard Ubangoh, disclosed on 13 October that during 4-6 October, 54 seismic events ("earth tremors") were recorded. The first eruption site was located at 04°12'40" N and 09°10'45" E at 4,000 m altitude.

The lava-flow temperature measured at 300 m from one of the vents was 972°C.The main hazards from this eruption were lava flows and volcanic ash, which was blown SW into villages along the coast.

It can be constrained from channel morphology and down-flow evolution of crystal content.Lava flow hazard and risk were assessed by simulating probable lava flow paths using the DOWNFLOW code (Tarquini and Favalli, 2011). It is an active volcano. The tourists reported hearing strong explosions followed by observations of "flames" and ash.This report discusses recent research on the 2000 eruption of Mount Cameroon and then summarizes news articles on a smaller 2012 explosion.
Ateba B, Ntepe N, 1997. The town sits on the Atlantic coastal plain, an area bordered on its E and N sides by high, steep slopes of unconsolidated pyroclastic cones. Cameroon, during 26-27 June 2001. FLOWGO (Harris and Rowland, 2001) was the only model that enables full inversion of the thermo-rheological properties of lava flows. Mount Cameroon is one of Africa's most active volcanoes. After the last eruption of 2000, a number of seismographs have been placed along the MC site network with one at the Ekona Station, Esuke and Banga-Bakundu. This study provides new quantitative constraints for rheological and dynamic characteristics of lava flow effusion at Mount Cameroon during the 1982 and 2000 eruptions. It can be constrained from channel morphology and down-flow evolution of crystal content.Lava flow hazard and risk were assessed by simulating probable lava flow paths using the DOWNFLOW code (Tarquini and Favalli, 2011).

378-389Chirico G.D., Favalli, M., Papale, P., Pareschi, M.T., Boschi, E., 2009, Lava flow hazard at Nyiragongo volcano, D.R.C. This study provides new quantitative constraints for rheological and dynamic characteristics of lava flow effusion at Mount Cameroon during the 1982 and 2000 eruptions.

In addition to the conventional risk mapping described above, the authors also present (1) two reversed risk maps (one for buildings and one for roads), where each point on the volcano is classified according to the total damage expected as a consequence of vent opening at that point; (2) maps of the lava catchments for the two main towns of Limbe and Buea, illustrating the expected damage upon venting at any point in the catchment basin. Expand each entry for additional details.The maps shown below have been scanned from the GVP map archives and include the volcano on this page. Increased seismicity was recorded in November 1975, but no eruption occurred. , Kervyn, M., Ernst, G.G.J, del Marmol, M.A., Suh, C.E.. and Jacobs, P., 2013, Numerical experiments on the dynamics of channelised lava flows at Mount Cameroon volcano with the FLOWGO thermo-rheological model, Journal of Volcanology and Geothermal Research, Volume 253, pp. A violent explosion lasted a couple of seconds and lightly injured two of the porters and guides on the mountain, according to a 6 February 2012 Associated Press report.Lava flow hazard and risk, and weathering studies. Fitton J G, Kilburn C R J, Thirlwall M F, Hughes D J, 1983. There are about 500,000 people living near the volcano.2012, 2000, 1999, 1989, 1982, 1959, 1954, 1925, 1922, 1909, 1871, 1868, 1866, 1865, 1852, 1845-46, 1838-39, The monthly number of events was consistently below 30 after October 1993, until December 1994 (figure 1). On the morning of 10 April the front was at 120 m elevation, 600 m from the Limbe-Idenau road near the Atlantic coast, between Batoke and Bakingili. Journal of Volcanology and Geothermal Research, 204:27-39. doi:10.1016/j.jvolgeores.2011.05.001Wantim, M.N. The upper 2000 flow is one of the shortest (850 m) recorded for historical lava flows here despite having descended steep slopes (10-25°). An eruption during October-November 1982 produced lava fountaining from a radial fissure 6.5 km SW of the summit and a lava flow that moved 12 km down the SW flank. According to Favalli and others (2010), Mt. Many other sections of the town, including Down Beach Limbe, also suffered significant losses and damage. Multicriteria decision making: The analytic hierarchy process.


The mountain is host to many exotic birds and plants,many of the plants being used for medicinal purposes.

This weathering is a major factor in the cohesion of steep slopes, and thus these studies address slope stability, another kind of volcano-related hazard that could occur even in times of volcanic quiescence.Socio-economic vulnerability study.


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