Pāhala earthquake rattles Hawaii after magnitude 3.5 Terremoto

Pāhala earthquake rattles Hawaii after magnitude 3.5 Terremoto

A weak terremoto of magnitude 3.5 struck 0.8 km west-southwest of Pāhala, Hawaii, at 19:26 GMT on Tuesday, April 28, 2026. The quake was very shallow, at 32 km deep, and it was felt widely across the area.

For people near the epicenter, the shallow depth made the shaking feel stronger than a deeper earthquake of the same size. No injuries, damage, or emergency response details were provided.

Pāhala and the shallow depth

The earthquake’s location placed it close to Pāhala, in Hawaii County, Hawaii, United States, rather than far offshore. That proximity, combined with the 32 km depth, helps explain why a moderate event was noticeable to residents in the area.

Shallower quakes can transmit more of their energy to the surface before it fades, which is why the same magnitude can be felt more clearly near the epicenter. In this case, the reported shaking reached a wide area despite the quake’s weak magnitude.

What residents felt in Hawaii

The most immediate fact for anyone in the area is simple: the ground shook, and it was felt widely. The event did not come with any reported injuries or damage in the available facts, so the practical impact was limited to the shaking itself.

For nearby residents, the key point is the combination of location and depth. A magnitude 3.5 quake is not large, but 32 km of depth and a point just 0.8 km from Pāhala were enough to make it noticeable across the surrounding area.

April 28 at 19:26 GMT

The quake struck on Tuesday, April 28, 2026 at 19:26 GMT, which is the only timing detail provided in the available record. That fixed time is the main reference point for anyone checking whether they felt the shaking or comparing it with other seismic activity near Pāhala.

What follows for readers is straightforward: if you felt the tremor in Hawaii, this was the event. No further response, warning, or damage report was included in the facts, so the record ends with the quake itself and its measured characteristics.

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