M2.8 Earthquake Near Te Kaha, New Zealand

Published: 23 hours ago•Wednesday, November 11, 2026 at 7:52 PM UTC

A micro magnitude 2.8 earthquake struck 145 km north of Te Kaha, New Zealand at a depth of 178.4 km (intermediate focal zone), releasing seismic energy equivalent to approximately 239 kg of TNT. Tracked live on Earthquake Today, here is the verified GeoNet telemetry, interactive epicenter map, and ground shaking assessment.

2.8MAG
Micro EarthquakeIntermediate Focal Depth
Te Kaha, New ZealandNew Zealand(145 km north of)

Seismic Telemetry Specifications

Magnitude

2.8M

Micro Seismic Class

Focal Depth

178.4km

Upper Mantle

Epicenter

36.457° S, 177.444° E

GPS Coordinates

Energy Yield

239 kg

TNT Equivalent Power

Network Source

GeoNet

GNS Science (NZ)

Epicenter Location & Tectonic Fault Map

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Is This Earthquake Dangerous?

A magnitude 2.8 event is classified as a micro earthquake. Micro-earthquakes are rarely felt by humans and are typically recorded only by sensitive seismometers.

Estimated Shaking Radius< 10 km
Potential Damage ZoneNone
Focal Depth EffectModerate Damping

Estimated Shaking Across Nearby Communities

Te Kaha, New Zealand• 145 km (90.1 mi) S

Felt by almost no one except under extraordinarily favorable conditions.

MMI I • Imperceptible
Auckland• 243.1 km (151.1 mi) W

Felt by almost no one except under extraordinarily favorable conditions.

MMI I • Imperceptible

Did You Feel This Earthquake?

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Your immediate response verifies shaking boundaries and helps ground-truth instrumental models.

What Does Magnitude 2.8 Mean?

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

1.0 – 2.9Micro
This Event
3.0 – 3.9Minor
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 &approx; 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 178.4 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.

Frequently Asked Questions

Common questions and answers about this earthquake.

No. No tsunami warning, watch, or advisory was issued by the Pacific Tsunami Warning Center (PTWC) or the USGS for this M2.8 event. The focal depth (178.4 km) and magnitude did not generate sufficient vertical seafloor displacement to trigger a hazardous tsunami wave.

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