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May 29 -
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A 4.2-magnitude earthquake came offshore of the southern coast of the Big Island on Tuesday morning, reminding residents of the region's geologic crisis. The earthquake was powerful enough to be felt throughout parts of the island, but authorities quickly assured that there had been no tsunami warning and no damage was expected. It is one of a series of earthquakes that continue to afflict the region, especially in and around active volcanic regions.
Here, we'll explore what happened, why Hawaii is susceptible to such quakes, the contribution of nearby volcanoes like Kīlauea and Mauna Loa, and what citizens can do to be prepared for such quakes in the future.
At 9:37 a.m. local time, May 28, 2025, the U.S. Geological Survey (USGS) recorded a magnitude-4.2 earthquake approximately 5 miles southeast of Pāhala, along the coast of Ka'u. The quake was approximately 20 miles beneath the seafloor, depths typical of tectonic activity related to volcanic processes.
Although the earthquake itself did not result in any major disruption, it was felt because it was preceded by a series of small tremors days prior, telling of the geologic restlessness of the island.
The Hawaiian Islands sit above a hotspot in the Earth's mantle and thus are among the most volcanically active sites on the planet. Hawaiian earthquakes are generally due to volcanic activity, shifting magma, or tectonic movement deep below the island.
Here are some reasons that could be some of the reasons for the earthquake.
The USGS reported that seismic swarms have been occurring by Pāhala since 2019, with reports as early as the 1960s. The trends aren't new, but are closely monitored for any sign of acceleration.
Though the earthquake was close to two of Hawaii's most active volcanoes, Kīlauea and Mauna Loa, scientists say the quake did not directly impact their activity.
Both volcanoes lie within the broader landscape of the Big Island. The earthquake itself on Tuesday did not impact volcanic activity, but it occurred in a known hotspot for energy related to the subsurface movement of magma.
The 4.2 earthquake is only one in a sequence of small earthquakes, also known as a seismic swarm. Swarms persist for days or weeks and are monitored closely for evidence of a pending eruption.
While this particular event is not a sign of a forthcoming eruption, the normal activity is a reminder that Hawaii's geologic processes are constantly in motion beneath the surface.
No damage was reported, residents and tourists must be prepared for seismic activity. The Hawaiian Islands have a system in place to manage larger earthquakes and eruptions, but personal preparation remains key.
Here are some tips for residents to keep them safe:
Tuesday's off-shore quake off the Big Island was a gentle but unmistakable reminder of Hawaii's dynamic geology. Though it did no damage and posed no threat of a tsunami, it is another notch on the belt of the ongoing string of quakes that scientists are keeping watch on closely. With volcanoes erupting nearby as we speak and centuries of seismic record, preparedness is not just a precautionary step, it's a way of life for those who live on the beautiful but dynamic Hawaiian Islands.
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