The Mozambique Ridge is an aseismic oceanic plateau in the southwester
n Indian Ocean. During the separation of Antarctica and South Africa i
n the Early Cretaceous, the Mozambique Ridge was segmented by fracture
zones which were assumed to become inactive during the Cenomanian, wh
en Africa and Antarctica were finally separated. However, the existenc
e of active normal faulting in the central part of the Mozambique Ridg
e was demonstrated by single and multichannel seismic surveys. Numeric
al modelling of the stress distribution caused by the crustal structur
e of the Mozambique Ridge and the adjacent oceanic basins suggests the
possible existence of a zone with average horizontal tension up to 70
MPa along the central part of this passive ridge, which may cause the
modern fault activity. These stresses also cause an additional dynami
c anomaly which can explain small variations of the geoid anomaly over
the ridge.