LIVE Connected
🇳🇿

Wellington Seismic Zone • 250 km Monitoring Radius

Real-Time Earthquakes in Wellington, New Zealand

Live seismic telemetry, active fault rupture tracking, and ground motion hazard monitoring for the Wellington metropolitan area.

TECTONIC SETTING:Hikurangi Subduction Zone & Marlborough Fault System Transition
METRO POPULATION:215,000 (435,000 Region)
OBSERVATORY:GeoNet →

WELLINGTON EVENTS (250 KM)

2

NEAREST ACTIVE FAULT

Wellington Fault (1 km)

TELEMETRY WINDOW

Live Telemetry Feed

Recent Earthquakes Near Wellington

LIVE

Live telemetry feed and hypocenter reports recorded within a 250 km radius of Wellington.

Landmark Historical Earthquakes in Wellington

Significant seismic benchmarks, cataloged damage, and engineering lessons shaping modern safety standards.

1855M 8.2

Wairarapa Fault / Cook Strait

1855-01-23•30 km from Wellington•MMI X (Extreme)

New Zealand’s most powerful historical earthquake; uplifted the Wellington shoreline by 1.5 to 2 meters, draining the swampy Basin Reserve and creating the modern harbor roadway.

2016M 7.8

Kaikōura / Culversden

2016-11-14•180 km from Wellington•MMI VIII in Wellington

Complex multi-fault rupture that transmitted severe long-period waves into central Wellington, causing structural damage that required demolishing numerous multi-story office buildings.

Seismic Geology & Soil Amplification in Wellington

Plate boundaries, tectonic kinematics, and local geotechnical ground response characteristics.

PLATE BOUNDARY:Pacific Plate & Australian Plate Oblique Transpression
SLIP RATE:40–45 mm/year oblique convergence
STRESS REGIME:Dextral Strike-Slip Shear & Subduction Thrusting

Wellington, New Zealand’s capital, is located on Cook Strait directly astride the active Wellington Fault. It represents the complex tectonic transition where the offshore Hikurangi Subduction Zone gives way to the strike-slip Alpine Fault system of the South Island.

🏗️

Local Soil Profile & Ground Motion Resonance

Wellington Harbour (Te Whanganui-a-Tara) reclaimed land, CentrePort, and Thorndon contain soft marine silts and artificial fill that suffered major liquefaction during the 2016 Kaikōura earthquake.

Major Active Fault Systems Near Wellington

Seismogenic fault lines, maximum credible magnitudes (MCE), and proximity to the metropolitan center.

1 KM FROM CITYM 7.5

Wellington Fault

Right-Lateral Strike-Slip6–8 mm/year

Runs directly along the western edge of Wellington Harbour, Thorndon, and the Hutt Valley; recurs every 500–1000 years.

25 KM FROM CITYM 8.5–9.0

Hikurangi Subduction Megathrust

Subduction Megathrust40 mm/year

Offshore subduction interface dipping directly beneath Wellington and the North Island.

Seismic Safety, Observatory & Building Codes

Official seismological monitoring, building construction standards, early warnings, and emergency response.

🏛️
OFFICIAL SEISMIC OBSERVATORY

GeoNet / GNS Science (GeoNet)

Emergency Mobile Alerts (EMA) & GeoNet Rapid Telemetry
BUILDING CODE STANDARD:New Zealand Building Code (NZS 1170.5) with Earthquake Prone Building (EPB) Register
Visit Official Observatory (GeoNet) →
🚨
EMERGENCY HOTLINE
111
🌊 COASTAL TSUNAMI PROTOCOL

If an earthquake is LONG or STRONG, GET GONE. Do not wait for official warnings if shaking lasts more than a minute; move uphill out of all tsunami evacuation zones.

Drop, Cover, and Hold. Remember the "Long or Strong, Get Gone" coastal tsunami rule.

Frequently Asked Questions About Earthquakes in Wellington

Authoritative answers to common questions regarding seismic risks, building safety, and preparedness in Wellington.

What is New Zealand’s "Long or Strong, Get Gone" tsunami rule?▾

In New Zealand, if you feel an earthquake that lasts longer than a minute or is strong enough that it is hard to stand up, coastal tsunamis can arrive in minutes; evacuate inland or uphill immediately without waiting for sirens.