A magnitude 6.0 earthquake struck off Japan’s Pacific coast near Shima early on Sunday, with no tsunami warning issued and no immediate reports of damage or casualties.

The United States Geological Survey (USGS) put the earthquake at 58 km south-southeast of Shima, in Mie Prefecture, at a depth of 352 km. It was recorded at 22:15 UTC on Saturday, 31 October, which was 07:15 in Japan on Sunday, 1 November, and 03:15 in Pakistan.

The Japan Meteorological Agency reported tremors measuring 3 on its seven-point seismic-intensity scale in parts of Fukushima Prefecture. No tsunami warning was issued, and the initial reports carried no accounts of injuries or property damage.

What happened

The earthquake struck offshore, southeast of Shima, a coastal city in Mie Prefecture on Japan’s main island of Honshu. Its magnitude was measured at 6.0, which counts as a strong earthquake, but its focus was unusually deep — 352 km below the surface.

That depth is the key detail in this event. Earthquakes are measured in two ways that matter here: magnitude, which describes how much energy was released at the source, and intensity, which describes how strongly the shaking was felt at a particular place. A deep earthquake releases its energy far below the surface, so by the time that energy reaches the ground above, it has spread over a wider area and weakened. That is why a magnitude 6.0 event at this depth produced only light reported shaking, rather than the strong shaking a shallow earthquake of the same magnitude could cause near its epicentre.

The reports so far describe the shaking in Fukushima Prefecture at intensity 3 on Japan’s scale. In general terms, intensity 3 means shaking felt by most people indoors, with hanging objects such as lamps swinging slightly. It is well below the levels at which buildings are normally damaged.

Why no tsunami warning was issued

No tsunami warning was issued for this earthquake, and the depth helps explain why. Tsunamis are most often generated when a shallow earthquake suddenly moves the sea floor up or down, displacing a large volume of water. A rupture 352 km underground does not move the sea floor in that way, so it does not set off the same kind of wave.

The absence of a warning at this stage does not mean authorities stopped watching. It means that, on the information available in the initial reports, no tsunami threat was identified for this event.

Japan and the Pacific Ring of Fire

Japan is one of the most seismically active countries in the world, because it sits along the Pacific Ring of Fire, where several major tectonic plates meet. The islands experience frequent earthquakes, and the country has built its warning systems, building standards and public drills around that reality.

That experience also explains the speed of the first reports. The USGS and the Japan Meteorological Agency publish magnitude, location and depth within minutes of a significant event, and local reports then add the observed intensity and any damage or tsunami information as it becomes available. In this case, the first reports were consistent: a strong but very deep offshore earthquake, light reported shaking, and no tsunami warning.

What happens next

For now, the picture is one of monitoring rather than emergency response. Authorities will continue to check for any damage reports and for aftershocks, and the initial measurements may be revised slightly as more seismic data is analysed. That is normal for earthquake reporting: early figures are preliminary, and agencies update them as stations across the region report in.

Readers in Japan are advised to follow official guidance from the Japan Meteorological Agency and local authorities if any further information is issued, rather than relying on unverified posts on social media.

Timeline

  • Saturday, 31 October 2026, 22:15 UTC: A magnitude 6.0 earthquake is recorded 58 km south-southeast of Shima, Mie Prefecture, at a depth of 352 km.
  • Sunday, 1 November 2026, 07:15 JST: The earthquake occurs in local time in Japan; 03:45 IST and 03:15 PKT the same morning.
  • Sunday, 1 November 2026, morning: The Japan Meteorological Agency reports intensity 3 tremors in parts of Fukushima Prefecture; no tsunami warning is issued.
  • Sunday, 1 November 2026, morning: Initial reports carry no immediate accounts of damage or casualties; further details are awaited.

Related coverage

Earlier in October, a stronger 6.9 quake off Vanuatu briefly triggered a tsunami warning before the threat passed. The contrast is instructive: that event was shallower and closer to the surface, which is why a warning was issued and then lifted, while the deep Shima earthquake prompted no warning at all.

For more international news, visit the World section.

Frequently asked questions

Was there a tsunami after the Japan earthquake?

No. No tsunami warning was issued for this earthquake, and the initial reports mention no tsunami. Its depth of 352 km meant it did not displace the sea floor in the way that generates a tsunami.

Was anyone hurt or was anything damaged?

No immediate reports of damage or casualties were available in the initial reports. Authorities were still assessing the situation when those reports were published.

Where exactly was the earthquake?

The USGS located it 58 km south-southeast of Shima, off the coast of Mie Prefecture in Japan, at a depth of 352 km.

When did it happen?

It was recorded at 22:15 UTC on Saturday, 31 October 2026, which was 07:15 on Sunday, 1 November in Japan, 03:45 in India and 03:15 in Pakistan.

Why did a magnitude 6.0 earthquake cause only light shaking?

Because it was very deep. At 352 km below the surface, the energy had spread and weakened before reaching the ground, so the reported intensity was only 3 on Japan’s seven-point scale in the areas mentioned.

Is Japan prone to earthquakes?

Yes. Japan lies along the Pacific Ring of Fire, where several tectonic plates meet, making it one of the most seismically active countries in the world.

Why this matters

On its own, this earthquake caused no reported harm, and that is the main news. It is also a useful reminder of how earthquake reporting works: magnitude alone does not tell the whole story. Depth, distance and local ground conditions decide how strongly people feel a quake, and whether a tsunami is possible. A magnitude 6.0 event that is 352 km deep is a very different event from a magnitude 6.0 event just a few kilometres below a city, even though the headline number looks the same.

For readers following seismic news, the details to watch in the next updates are any revision to the magnitude or depth, any damage reports, and any aftershock information — none of which had been reported in the initial accounts.

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