M 6.2 Eketahuna Mon, Jan 20 2014

This quake was widely felt in both islands. Strong shaking was reported as far as Palmerston North and Masterton.



Aftershocks following the Eketahuna earthquake up to 27/01/2014

Aftershocks following the Eketahuna earthquake up to 27/01/2014

24 hours of seismic activity recording at Mangatainoka River (MRZ) from 1530hrs Wednesday 22nd January to 1530hrs Thursday 23rd January, showing the Eketahuna earthquake aftershocks

24 hours of seismic activity recording at Mangatainoka River (MRZ) from 1530hrs Wednesday 22nd January to 1530hrs Thursday 23rd January, showing the Eketahuna earthquake aftershocks

Map showing accelerations measured for the Eketahuna earthquake

Map showing accelerations measured for the Eketahuna earthquake

The Eketahuna quake struck at 3:52 pm on Monday afternoon, and was centered 15 km east of Eketahuna, under the south-east of the North Island. The quake was felt strongly in both islands, and over 9.000 felt reports were received from the public, with multiple reports of damage. The focal mechanism showed it to be a normal fault earthquake.

The depth and location of this event placed it below the interface between the subducting Pacific plate and overriding Australian plate. Maximum peak ground acceleration recorded by GeoNet instruments was about one quarter of the acceleration due to gravity (0.26 g). This measurement was recorded in Woodville. Relatively strong shaking was also recorded on the Kapiti Coast (e.g. up to 0.2 g in Paraparaumu) whereas accelerations recorded in Wellington city were less than 0.05 g. In comparison, ground motions recorded in Wellington during the Cook Strait earthquakes six months earlier ranged up to 0.26 g.

Within five days a set of possible future scenarios and their likelihood was compiled and released, to better inform both responding agencies and the community.

GeoNet science response activities