A magnitude 5.6 earthquake struck New Zealand at 16:11 UTC on Thursday, August 13, 2026, with its epicentre recorded Kermadec Islands region at a depth of 10.0 km. If you felt this earthquake, you are not alone — and your experience is scientifically valuable.
Did You Feel It?
Community felt reports are an important part of modern earthquake science. The USGS "Did You Feel It?" (DYFI) system collects reports from people who experienced shaking, generating intensity maps that complement instrumental data. These reports help seismologists understand how shaking varied across the affected region and can improve earthquake hazard assessments.
A magnitude 5.6 earthquake is capable of causing significant damage, particularly to older or poorly built structures. Strong earthquakes cause severe shaking that is difficult to stand through. Duration can reach 30–60 seconds. Widespread damage to ordinary buildings is common; even some well-built structures may sustain damage. Strong ground motion can trigger landslides, liquefaction of saturated soils, and rupturing of underground infrastructure.
Understanding the 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.
The energy released by a magnitude 5.6 earthquake is approximately the equivalent of a large mining explosion or small nuclear device. This is 32 times more energy than a magnitude 4.6 event — the logarithmic nature of the magnitude scale means each whole number increase represents about 32 times more energy.
Why Here? The Geology Behind the Earthquake
New Zealand straddles the boundary between the Pacific and Indo-Australian tectonic plates. In the South Island, the Alpine Fault accommodates plate motion directly, while the North Island sits above the Hikurangi Subduction Zone, where the Pacific Plate dives beneath the Australian Plate.
New Zealand experiences around 15,000 earthquakes per year, of which about 100–150 are strong enough to be felt. The 2010–2011 Canterbury earthquake sequence — including the devastating M6.2 Christchurch aftershock of February 2011 — killed 185 people and destroyed much of the city centre, profoundly reshaping New Zealand's approach to earthquake resilience.
Structural Considerations
This magnitude class poses a serious threat to older and poorly constructed buildings. Collapse is possible in the most vulnerable structures. Modern seismically designed buildings are expected to remain standing, though repair or demolition may be necessary after inspection.
If you are in the affected area and notice damage to your building — cracks in load-bearing walls, shifted foundations, or distorted door frames — treat this as a potential sign of structural compromise and seek professional assessment before resuming normal occupation.
Safety Reminders
After an earthquake, expect aftershocks. Check yourself and others for injuries. Inspect your surroundings for hazards before moving — broken glass, gas leaks (smell), downed power lines, and structural damage. If you suspect a gas leak, open windows and evacuate without using electrical switches or open flames.
The internationally recommended action during earthquake shaking is Drop, Cover, and Hold On: drop to your hands and knees, take cover under a sturdy table or desk (or protect your head with your arms if no shelter is available), and hold on until shaking stops. Do not run outside during shaking — most injuries occur when people attempt to move.
GeoNet (operated by GNS Science) monitors New Zealand's earthquakes in near real-time. The National Emergency Management Agency (NEMA) coordinates civil defence responses. New Zealand's "ShakeOut" national earthquake drill occurs annually.
Share Your Experience on QuakeWatch
You can submit your own felt report directly on this earthquake's detail page on QuakeWatch. Your input — describing intensity, location, and what you observed — contributes to a richer picture of how this earthquake affected communities across the region. Visit our live map and click on this event to add your report.
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