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S U M M A R Y Southern Mozambique is the southernmost expression of the continental East African Rift. Here, extension rates are low and rifting is achieved through normal faulting. Incipient rift environments provide an ideal location to investigate the role of reactivated pre-existing structures, aftershock sequences and fault interactions in rift development. In 2016 an Mw 5.6 earthquake occurred in the Zinave region of southern Mozambique, ∼10 km south-east of the Mw 7.

The decade-long Machaze–Zinave aftershock sequence in the slowly straining Mozambique Rift