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.
2. The fault slips and the seabed moves.
3. Water displacement spreads as a tsunami.
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
- JMA · October assessment
October observations
- JMA · Mechanism
Mechanism and history
- HERP · 2026 probabilities
M8–9, 30-year estimates
- HERP · Model guide
Models and uncertainty
- JMA · Tsunami
Tsunami generation
- JMA · N-net
12 March use; gains vary
- Japan · Advisory
Advisory actions
- Japan · Preparation
Preparation
- JMA · Warnings
Evacuation guidance