Recent work on the North Fiji Basin axial spreading ridge and on the a
ctive propagating ridge located west of the Fiji Islands has establish
ed the existence of two active spreading ridges that have been functio
ning synchronously in the basin since at least 1 or 1.5 Ma. This hypot
hesis is tested and the kinematics of the twin active ridges are refin
ed further on the basis of analysis of bathymetric and magnetic data.