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A magnitude 6.3 earthquake struck south of the Kermadec Islands on 5th August 2026 at 07:43 UTC, occurring at a depth of 197 km. Because this was a deep-focus earthquake, the shaking was widely distributed but significantly reduced at the surface, with no reports of damage or tsunami activity.
The Kermadec region sits along the Kermadec-Tonga subduction zone, one of the most active seismic belts in the world. This area frequently experiences strong earthquakes due to the ongoing subduction of the Pacific Plate beneath the Indo‑Australian Plate.
Deep earthquakes like this one typically originate within the descending slab of the Pacific Plate. Although they can be powerful, their depth often prevents strong surface shaking.
The Kermadec Islands region has experienced several significant earthquakes throughout 2026, reflecting ongoing tectonic activity along the subduction zone. Deep events like this one help scientists understand stress patterns within the sinking Pacific Plate.
Related Guide
Why Earthquakes Happen — A Simple Explanation
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