Volcanism is one of the main mechanisms transferring mass and energy between the
interior of the Earth and the Earth's surface. However, the global mass flux of lava, volcanic …

Abstract The Cenozoic East African rift (EAR), Cameroon Volcanic Line (CVL), and Atlas
Mountains formed on the slow‐moving African continent, which last experienced orogeny …

The Cameroon Hot Line (CHL) is an active N30E tectono-magmatic alignment, extending
from Pagalu Island to Lake Chad. Its oceanic sector is comprised of six major volcanoes …

Gas exsolution and segregation are fundamental controls on eruption dynamics and magma
genesis. Basaltic magma loses gas relatively easily because of its low viscosity. However …

Africa's Cenozoic tectonism is often attributed to mantle plumes, particularly below East
Africa, but their morphology, number, location, and impact on the African lithosphere are …

One of Africa's newest struggles for liberation: Cameroon's Anglophone crisis, which
emerged from legal and education grievances in 2016, rapidly escalated into a secessionist …

Groundwater is the only reliable water resource for drinking, domestic, and agricultural
purposes for the people living in the Mount Cameroon area. Hydrogeochemical and R-mode …

This study was carried out to document the diversity and distribution of macrofungi in the
Mount Cameroon Region. These were assessed at low and high altitudinal ranges in the …

To help improve the safety of its population faced with natural disasters, the Cameroon
Government, with the support of the French Government, initiated a programme of …

The near 1700 km long Cameroon Line (CL) is an African intraplate 'fan-shaped'alkaline
volcano-plutonic rift zone of variable width (< 200 km), with a ca. 66 Ma history of magmatic …