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87 earthquakes recorded in New Zealand regional monitoring zone

Real-Time Earthquakes in New Zealand

Continuous seismic tracking along the Alpine Fault System, Hikurangi Subduction Zone, and Kermadec Trench.

NEW ZEALAND EVENTS

87

TECTONIC SETTING

Pacific Plate & Australian Plate Boundary

TELEMETRY WINDOW

Live Telemetry Feed

LARGEST EVENT

M 5.7 55 km W of Taupo, G1, New Zealand

Recent Earthquakes in New Zealand

LIVE

Live telemetry feed and seismic report for earthquakes in New Zealand.

Active Fault Systems & Tectonic Setting

Geodynamic boundaries, subduction dynamics, and crustal deformation zones.

Subduction / Zone:ALPINE-HIKURANGI-KERMADEC
Slip Rate:30–45 mm/year relative motion
Stress Regime:Transpressional Strike-Slip & Subduction Megathrust

New Zealand straddles the active boundary between the Pacific and Australian tectonic plates. Oblique convergence creates complex faulting, including the Alpine Fault and Hikurangi Subduction Zone, monitored in real time by GeoNet.

Alpine Fault

Dextral Transpressional Strike-Slip

800 km fault running the length of the Southern Alps; ruptures in recurring M8.0 events roughly every 300 years.

Hikurangi Subduction Zone

Subduction Megathrust

Convergent interface off the North Island's East Coast capable of M8.5+ megathrust earthquakes.

Marlborough Fault System (Hope, Wairau, Awatere)

Dextral Strike-Slip

Network of parallel strike-slip faults transferring motion between Alpine Fault and Hikurangi Trench.

Wellington Fault

Dextral Strike-Slip

Major fault passing directly through downtown Wellington and the Hutt Valley.

Landmark & Historical Earthquakes

Significant seismic benchmarks, cataloged magnitudes, and geological impacts.

2011M 6.2

Christchurch, Canterbury

February 22, 2011

Shallow blind faulting directly under southeastern Christchurch with extreme ground accelerations (2.2g) and liquefaction.

2016M 7.8

Kaikōura, South Island

November 14, 2016

Complex multi-fault rupture across 20+ distinct onshore and offshore faults; uplifted coastline up to 6 meters.

1931M 7.8

Hawke's Bay / Napier

February 3, 1931

New Zealand's deadliest earthquake; raised the Ahuriri lagoon seabed and prompted art deco rebuilding.

Frequently Asked Questions

Common questions about seismic activity, safety, and monitoring in New Zealand.

What is New Zealand's 'Long or Strong, Get Gone' rule?▾

If you are near the coast and feel an earthquake that is either LONG (lasting more than a minute) or STRONG (hard to stand up), evacuate immediately to high ground without waiting for official tsunami sirens.

When is the next Alpine Fault earthquake expected?▾

The Alpine Fault has ruptured regularly roughly every 300 years (last in 1717 AD). Paleoseismic research estimates a 75% probability of a magnitude ~8.0 event within the next 50 years.

How does GeoNet monitor tremors in New Zealand?▾

GeoNet operates hundreds of seismometers, GPS stations, and acoustic sensors across New Zealand, streaming real-time earthquake and volcanic data to the public and emergency responders.