Mount Cameroon Eruptions, Related Hazards and Effects on the Ecosystem
Abstract ID#: 33674
The relatively high carbon dioxide (CO2) content in MC Glass inclusions support the interpretation that the CO2 responsible for the 1984 Lakes Monoun and 1986 Nyos disasters is magmatic in origin, which killed 37 and over 1800 people respectively.
Months before the latest 2000 eruption, MC was characterized by a seismic swarm recorded in 03/2000 by analogue seismic stations. The co-eruptive period from May 28th to June 19th, 2000 was characterized by sequences of earth quakes, swarms and volcanic tremor. The main shock had a magnitude 3.2 event and a modified Mercalli intensity of 3 to 4. The largest seismic event recorded had a magnitude of 4. An explosion on 5th June, 2000, injured many members of a surveillance team, and a helicopter crash five days later killed both pilots. It also led to lava flow across the Limbe-Idenau highway, damage of forest and palm plantations in Bakingili, and the evacuation of its 600 inhabitants.
Never the less MC has positive impacts on the environment such as increased soil fertility where agro-industrial plantations have taken advantage, and more touristic sites have developed.
After the last eruption of 2000, a number of seismographs have been placed along MC site network in Ekona, Esuke and Banga-Bakundu.
