Live Seismic Telemetry • REVIEWED Event

Minor 3.3 Earthquake – New Zealand

8 days agoWednesday, September 9, 2026 at 06:24:08 PM UTC

A minor magnitude 3.3 earthquake struck near New Zealand on Wednesday, September 9, 2026 at 06:24:08 PM UTC. This intermediate focal depth (163.1 km depth) released energy equivalent to approximately 1 tons of TNT. Here is the verified GNS telemetry, live epicenter map, and ground shaking assessment.

3.3MAG
Minor EarthquakeIntermediate Focal Depth
New ZealandNew Zealand

Seismic Telemetry Specifications

Magnitude

3.3ML

Minor Seismic Class

Focal Depth

163.1km

Upper Mantle

Epicenter

38.381° S, 175.766° E

GPS Coordinates

Energy Yield

1 tons

TNT Equivalent Power

Network Source

GNS

USGS Real-time Feed

Epicenter Location & Tectonic Fault Map

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Is This Earthquake Dangerous?

A magnitude 3.3 event is classified as a minor earthquake. Often felt by people indoors, especially on upper floors. Hanging objects may swing slightly; structural damage is extremely rare.

Estimated Shaking Radius~25–50 km
Potential Damage ZoneNone
Focal Depth EffectModerate Damping

Estimated Shaking Across Nearby Communities

Auckland191.9 km (119.2 mi) NNW

Felt by almost no one except under extraordinarily favorable conditions.

MMI IImperceptible

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What Does Magnitude 3.3 Mean?

Earthquake strength is measured on a logarithmic scale. Compare this event with the full seismic scale:

1.0 – 2.9Micro
3.0 – 3.9Minor
This Event
4.0 – 4.9Light
5.0 – 5.9Moderate
6.0 – 6.9Strong
7.0 – 7.9Major
8.0+Great

Logarithmic Energy Multiplier

Because seismic scales are logarithmic, each whole integer increase represents:

10× Ground Motion Amplitude
The seismograph wave amplitude jumps tenfold for every 1.0 magnitude step.
~31.6× Radiated Kinetic Energy
Total energy release multiplies exponentially (101.5 ≈ 31.62 times per unit).

Why Did This Earthquake Happen?

New Zealand straddles the boundary between the Australian and Pacific tectonic plates. In the South Island, the Alpine Fault accommodates oblique strike-slip motion, while the Hikurangi Subduction Zone off the North Island generates subduction earthquakes along the southwestern edge of the Ring of Fire.

Originating at a depth of 163.1 km (Upper Mantle / Wadati-Benioff Zone (70–300 km)), this rupture occurred originated within the descending oceanic plate inside the upper mantle. shaking radiates over a wider geographic area with attenuated high frequencies.

Aftershock Outlook & Secondary Tremors

Micro-tremors and minor events of this scale are part of ongoing background tectonic relaxation. While isolated micro-aftershocks may occur, the likelihood of a damaging secondary event remains statistically low under normal seismic conditions.

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Earthquake Safety Action Plan

Complete Safety Guide →
During the Shaking
  • Drop, Cover, and Hold On: Take cover beneath a sturdy table or desk.
  • Stay indoors away from exterior glass windows and heavy unanchored fixtures.
  • If outdoors, move into an open area away from power lines and building facades.
Immediately After
  • Inspect utilities for damaged gas lines, water leaks, or electrical hazards.
  • Expect Aftershocks: Secondary tremors frequently strike after significant events.
  • Avoid damaged structures and listen to official emergency broadcasts.
Preparation & Kits
  • Maintain a 72-hour emergency go-bag with water, food, and first aid.
  • Anchor heavy furniture, water heaters, and appliances to structural studs.
  • Establish a family emergency communication protocol and meeting point.

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