Mt. Cameroon erupted simultaneously in March-April 1999 in two distinct pla
ces on its southwestern flank. A hawaiite (with An 83-76 plagioclase phenoc
rysts) and an alkali basalt (with Fo 84-80 olivine phenocrysts) have been s
imultaneously emitted respectively at 1 400 and 2 650 m of altitude a.s.l.
The eruption of these co-magmatic lavas attests to the occurrence of a uniq
ue magmatic reservoir inside which the magma differentiation took place by
crystal set-ring of denser mineral phases. (C) 2000 Academie des sciences /
Editions scientifiques et medicales Elsevier SAS.