Mount Oku

Some of the rocks have ages starting from 24.9 to 22.1 million years ago, but much more recent activity has occurred. The mountain is built of basaltic and hawaiitic lavas, succeeded by trachytes, and then by large volumes of trachytic and rhyolitic ignimbrites with a thickness of up to 1,000 m. Further trachytic lavas, tuffs and breccias were produced, and the most recent phase produced pyroclastic cones and explosion craters. One of these craters holds Lake Oku, from which flows of basalt issued in the north, and of rhyolitic and phonolitic lavas in the south. ==Ecology==

A small sphagnum community with associated wetland plant species was discovered at 2,900 m in 1997, near the summit of the volcano, the highest sphagnum bog in West Africa. This site includes several plant species endemic to the Kilum-Ijim area, and is of extremely high conservation importance. The 200 km2 of forests of the Kilum-Ijim area around the mountain form the largest remaining patch of montane forest in West Africa, an important habitat for endemic species of animals and plants. The forest is at risk, since it is surrounded by a high density of human settlements. BirdLife International and the Ministry of the Environment and Forestry are jointly operating the Kilum-Ijim Forest Project, which aims to conserve the forest biome, maintain biodiversity and ensure sustainable reuse. The montane grassland above the forest belt is home to the endemic Mittendorf's striped grass mouse. ==See also==