The Manawahe Fault line is a seismically active area in the Bay of Plenty Region of the central North Island of New Zealand with the potential to be involved with other faults in an Mw7.0 event.

[2] North of Lake Rotoma, volcanic ignimbrite sheets from multiple eruptions of the Ōkataina Caldera extend towards the Whakatane Graben with the volcanic region being separated from the tectonic Whakatane portion of the Taupō Rift by the Manawahe Fault.

The traces are presumed to merge within 3 km (1.9 mi) of the surface.

[3] The last rupture identified was 636 years ago, with recurrence intervals between 1580–2000 years of a fault with one of the highest slip rates so far defined in the Taupō Volcanic Zone.

[2] Although potentially ruptures could be up to Mw 7 if the fault ruptured at the same time as the longer Matata fault, only > Mw 5.5 can be definitely assigned on displacements characterised to date as there appears to have never been a single full length fault rupture which would result in a Mw 6.3event.