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Making sense of Nankai earthquake risk

Connect the moving plates, probability and practical preparation.

Monthly assessment
Probability reference date
Sources checked

Two timescales of risk

On 2 November, JMA’s latest listed monthly assessment was 7 October 2026: no special increase above baseline, with high long-term M8–9 risk. Check new announcements for updates.[1]

Plates lock, bend and slip

From Suruga Bay to Hyuga-nada, the Philippine Sea Plate sinks beneath the landward plate by several cm yearly. Locked areas deform the upper plate; slip releases seismic waves.

A bent ruler pictures stored deformation and release. Real faults have complex rock and friction.[2] [5]

1. Locked plates accumulate deformation.

Locked plates accumulate deformation.Cross-section of an oceanic plate moving beneath a landward plate

2. The fault slips and the seabed moves.

The fault slips and the seabed moves.Simplified fault slip and upward movement of the upper plate

3. Water displacement spreads as a tsunami.

Water displacement spreads as a tsunami.Surface displacement propagates outward after seabed movement
Simplified subduction, slip and water displacement; geometry, waves and timing are illustrative.

History shows several patterns

A broad rupture occurred in 1707. The 1854 pair was 32 hours apart; the 1944–1946 pair, two years. December 2026 marks 80 years since 1946. Future timing and extent remain uncertain. Follow instructions after a major event.[2]

What does “within 30 years” mean?

As of 1 January 2026, HERP gives 30-year M8–9 probabilities of “around 60–90% or higher” using intervals and uplift, and “20–50%” using intervals alone. Both rank high.

A 15-year-old reaches 45 over this window. A hypothetical 70% means about 70 of 100 comparable 30-year histories contain such an event. The official estimates are the ranges above. The models use three uplift records or six intervals. Data and assumptions matter; HERP advises preparing with the higher estimate in mind.[3] [4]

From seafloor movement to waves

Seafloor movement displaces water and sends waves outward, like lifting a panel beneath a bath. Waves travel faster in deep water; the coast and seabed shape local height. Wave height, land inundation depth and elevation reached use different reference points.[5]

More time to react

From 12 March 2026, JMA uses 18 N-net coastal stations. Warning gains for Shikoku–Hyuga-nada reach about six seconds, or 20 with the full network. Faster detection after onset gives variable time to lower yourself and protect your head.[6]

Read the action instructions

Extra attention calls for checking preparations and evacuation readiness. Alert may require a week of advance evacuation in designated areas where escape after onset could be too late. Follow local instructions.[7]

Know your route

Check hazard maps and higher evacuation places and routes near home or your hotel. Plan family contact; charge phones and backup batteries. Near coasts or rivers, strong or prolonged shaking calls for immediate evacuation. Act before seeing waves; remain until warnings and advisories end and follow local orders.[8] [9]

Sources and scope

  1. JMA · October assessment

    October observations

  2. JMA · Mechanism

    Mechanism and history

  3. HERP · 2026 probabilities

    M8–9, 30-year estimates

  4. HERP · Model guide

    Models and uncertainty

  5. JMA · Tsunami

    Tsunami generation

  6. JMA · N-net

    12 March use; gains vary

  7. Japan · Advisory

    Advisory actions

  8. Japan · Preparation

    Preparation

  9. JMA · Warnings

    Evacuation guidance

Explore the idea

Explore tsunami depth and flow Understand wave height and inundation
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