The Alpine Fault's last rupture was stronger than previously thought, according to University of Canterbury research.
Geological sciences doctoral student Gregory De Pascale, working with Dr Robert Langridge of GNS Science, found the 1717 earthquake saw at least 380km of the fault rupture at a depth of 12km.
The rupture stretched from Haupiri River on the West Coast of the South Island down at least as far as Milford Sound and the two researchers estimate it reached a magnitude of 8.1, higher than the previously thought mean magnitude of 7.9.
However it is not known whether the fault ruptured further south as it goes out to sea at Milford Sound, Mr De Pascale said.
"If it did rupture out to sea, then the magnitude may have been bigger than the 8.1 we've calculated," he said.