The USGS has confirmed a magnitude 4.6 earthquake with its epicentre 28 km NNE of Kuji, Japan, occurring at 11:29 UTC on Monday, July 6, 2026. The event's focal depth — 67.0 km — is a key factor in understanding how this earthquake was experienced at the surface.
Why Depth Matters
At a focal depth of 67.0 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.
Depth is one of the most critical but least discussed parameters of any earthquake. Two earthquakes of identical magnitude can have dramatically different surface effects depending on how deep the rupture originates. Significant damage can occur to vulnerable structures — particularly unreinforced masonry, old adobe buildings, and poorly maintained older construction. Well-engineered modern buildings are designed to withstand this level of shaking with minimal structural impact, though contents may shift and non-structural elements (ceilings, partitions) can be damaged.
Magnitude 4.6: What the Science Says
On the moment magnitude scale, 4.6 represents a moderate earthquake. Moderate earthquakes are felt by virtually everyone near the epicentre. Strong shaking lasting 10–30 seconds can topple unsecured items, crack plaster, and cause poorly anchored objects to fall. Aftershocks are common following moderate events.
A magnitude 4.6 earthquake releases approximately roughly 500 tonnes of TNT of energy. For comparison, this exceeds the energy released by most conventional explosive events and is sufficient to shift tectonic stress in measurable ways across a wide region.
Tectonic Setting
Japan sits at the convergence of the Pacific, Philippine Sea, Eurasian, and North American tectonic plates, making it one of the most seismically active countries on Earth.
This region's seismic history is an important reminder that earthquake risk is a long-term reality that requires sustained preparedness. Japan experiences roughly 1,500 earthquakes per year that are strong enough to be felt. The country has developed one of the world's most sophisticated earthquake early-warning networks, capable of alerting millions of citizens within seconds of a major rupture.
Practical Safety Information
Regardless of the earthquake's depth or magnitude, standard safety procedures apply. Keep an earthquake emergency kit accessible at home. It should include at least 72 hours of water (4 litres per person per day), non-perishable food, a first aid kit, torch, battery-powered radio, copies of important documents, and essential medications. Reviewing and restocking this kit annually is strongly recommended.
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.
If you are in Japan, follow J-Alert instructions and refer to local municipal evacuation maps. Many buildings constructed after the 1981 revised building code are designed to withstand strong shaking.
Track This Event
All seismic data for this event is being updated in real time as the USGS refines its measurements. Initial magnitude and depth estimates are sometimes revised as more seismograph stations report in — a process that typically completes within hours of the event. Follow updates on our live earthquake map and consider submitting a felt report if you experienced this earthquake directly.
Aftershock Probability
After any significant earthquake, the probability of aftershocks follows a well-understood statistical pattern known as the Omori-Utsu Law: aftershock frequency decays roughly as the inverse of elapsed time since the main shock. For a magnitude 4.6 event, there is a meaningful probability of one or more felt aftershocks in the days following the main event. The USGS publishes real-time aftershock forecasts for significant earthquakes, which are updated as the sequence evolves.
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