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1944 Tōnankai Earthquake (M8.1) — Japan's Wartime Quake Hidden by Censorship

M 8.1Magnitude
7 Dec 1944Date
~1,223Deaths
FieldData
Magnitude8.1 Mw (8.2 Ms)
Date & time7 Dec 1944, 04:35 UTC (13:35 JST)
Depth~30 km
FaultNankai Trough megathrust, Philippine Sea Plate
Tsunami6-8 m, Wakayama/Mie/Shizuoka coasts
Deaths~1,223 official; est. up to ~1,900
Related quakesM6.8 Mikawa (13 Jan 1945), M8.1 Nankai (20 Dec 1946)
SourceUSGS, NOAA NCEI, Japan Meteorological Agency
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At 13:35 local time (04:35 UTC) on 7 December 1944, a magnitude 8.1 earthquake ruptured a segment of the Nankai Trough off the eastern Kii Peninsula, at a depth of about 30 km, where the Philippine Sea Plate subducts beneath Japan. It is one of a recurring series of great megathrust earthquakes that have broken the Nankai Trough roughly every 100 to 150 years.

Japanese fishing harbour coastline, the kind of coastal community struck by the 1944 Tōnankai earthquake and tsunami

The shaking and the tsunami that followed — waves up to 6-8 metres along the coasts of Wakayama, Mie and Shizuoka prefectures — officially killed about 1,223 people and destroyed or damaged tens of thousands of homes. Because Japan was fighting the final months of the Second World War, the government censored news coverage to protect wartime morale and conceal damage to aircraft factories, including a Nakajima plant producing parts for Zero fighters that collapsed on its workforce; researchers who later combed through uncounted regional records believe the true toll may run closer to 1,900.

Powerful ocean wave, the kind of tsunami wave that struck Wakayama, Mie and Shizuoka in 1944

Just 37 days later, on 13 January 1945, the magnitude 6.8 Mikawa earthquake struck nearby Aichi Prefecture, killing at least 1,180 more people — with some estimates above 2,000 — in a second quake whose damage was, again, kept out of the wartime press. Two years after that, on 20 December 1946, the adjacent segment of the same subduction trench ruptured in the magnitude 8.1 Nankai earthquake, completing a chain of sequential ruptures along the Nankai Trough within a single decade.

Traditional wooden houses in a Japanese village, similar to those damaged along the Kii Peninsula in 1944

Because so much of the 1944 disaster went unreported at the time, it remained one of the least-documented major earthquakes of the 20th century for years afterwards. Declassified records and post-war seismic surveys have since folded it into Japan's official hazard models for the Nankai Trough, which the Japan Meteorological Agency and Japanese government consider overdue for its next great rupture — a scenario now planned for under Japan's Nankai Trough megaquake early-warning system.

Frequently asked questions

Why was the 1944 Tōnankai earthquake censored?

Japan was fighting the final months of the Second World War, and the government suppressed news of the earthquake to protect wartime morale and hide damage to aircraft factories producing parts for Zero fighters, leaving the disaster's true scale undocumented for decades.

Is the 1944 Tōnankai earthquake linked to the 1946 Nankai earthquake?

Yes. Both ruptured adjacent segments of the same Nankai Trough subduction zone within two years of each other, part of a recurring pattern of megathrust earthquakes that break this trough roughly every 100 to 150 years.

How many people died in the 1944 Tōnankai earthquake?

Officially about 1,223 people died, but because wartime censorship suppressed reporting, researchers who later reviewed uncounted regional and industrial casualties believe the true toll may be closer to 1,900.

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See also

1946 Nankai Earthquake (M8.1)1995 Kobe Earthquake (M6.9)Earthquakes in Japan