Seismologists have recorded a magnitude 6.6 earthquake in the Pacific region, with the epicentre located 80 km ENE of Tadine, New Caledonia. The event occurred at 21:23 UTC on Friday, September 25, 2026 and originated at a depth of 10.0 km.

Seismic Context for the Pacific region

The Pacific Ocean basin is ringed by the world's most active subduction zones, collectively known as the Ring of Fire. This region produces approximately 90% of the world's earthquakes and the great majority of its major tsunamis.

Pacific island nations face unique challenges: small land areas, limited evacuation options, and direct exposure to both strong shaking and tsunami inundation. The Pacific Tsunami Warning Center (PTWC) in Honolulu monitors the entire Pacific basin and issues alerts to member nations.

About This Event

At a focal depth of 10.0 km, this is classified as a shallow earthquake (0–70 km). Shallow events are typically the most damaging: the seismic energy has less distance to travel before reaching the surface, resulting in stronger and more abrupt ground shaking at the epicentre.

In terms of felt effects, a magnitude 6.6 earthquake is typically potentially destructive across a wide area, capable of causing widespread damage and casualties. Major earthquakes produce violent shaking that can last a minute or longer. Damage is widespread and severe. Ground rupture, large-scale landslides, liquefaction, and infrastructure failure are likely near the epicentre. Events at this magnitude can generate tsunamis if they occur under or near the ocean.

Understanding the Magnitude Scale

Earthquake magnitude is measured on a logarithmic scale — meaning each whole-number increase corresponds to roughly 32 times more energy released and approximately 10 times greater ground motion amplitude. A magnitude 6.6 event therefore releases significantly more energy than its number alone might suggest to the casual observer.

A magnitude 6.6 earthquake is among the most powerful geological events that regularly affect human populations. The energy released — approximately the energy of several large nuclear detonations — is comparable to the detonation of several nuclear weapons, spread over a fault rupture that can extend for tens or hundreds of kilometres.

Major earthquakes are capable of causing widespread building collapse, particularly in areas with high proportions of older or non-engineered construction. Casualties from building collapses and secondary hazards (fires, gas leaks, dam failure) are a serious concern. Emergency response systems are typically overwhelmed in the immediate aftermath.

What to Do After an Earthquake

Agree on an out-of-area contact that family members can reach if local communications are disrupted. Identify two meeting points: one near your home and one further away. Practise earthquake drills, especially with children and elderly household members.

If you are on or near a coast and experience strong or prolonged earthquake shaking, treat it as a potential tsunami warning and move immediately to high ground. Do not wait for an official alert — natural warning signs (severe shaking, unusual sea withdrawal) are your first alert.

Staying Informed

Coastal communities throughout the Pacific should treat any strong earthquake as a potential tsunami warning and move inland or to elevated ground without waiting for an official alert.

QuakeWatch publishes real-time earthquake data sourced from the USGS global catalog — covering every detected seismic event worldwide, 24 hours a day. Visit our live map to see this and all other recent earthquakes, or explore our guide to earthquake magnitude for a deeper understanding of what these numbers mean in practice.

Community Felt Reports

If you felt this earthquake, your experience contributes to an important scientific dataset. The USGS "Did You Feel It?" (DYFI) system and QuakeWatch's own community reports platform collect first-hand accounts of shaking intensity from people across the affected region. These reports — describing where people were, what they felt, and what moved or was damaged — help seismologists map shaking intensity across an area much larger than any single seismograph can cover. Visit the earthquake's detail page on our live map to submit your own report.

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