The Wellington Fault runs through the centre of the capital and the Hikurangi subduction margin lies immediately offshore; the 1855 Wairarapa earthquake, around Mw 8.2, lifted parts of the harbour shoreline by more than a metre.
72-hour composite hazard forecast
Recorded in the selected 14d period
Largest earthquake in the selected 14d period
Seismotectonic hazard assessment, structural exposure & historical context
Click to locate on map
--
Living within 180 km of the city centre
--
Mixed construction stock with regional engineering standards
Subduction Zone
Major plate boundary with high strain accumulation
No significant earthquakes recorded in the selected 14d period.
Every recorded earthquake in this area — filter by time range and sort by time or severity.
Verified scientific, operational, and emergency protocols