Historical tsunamis · Sep 2, 1923, 2:46 AM UTC

1923 Ryukyu Islands tsunami

Japan

The tsunami of Sep 2, 1923, 2:46 AM UTC originated near Ryukyu Islands (Japan).

Key facts

Date
Sep 2, 1923, 2:46 AM UTC
Cause
Earthquake
Magnitude
M7.7
Depth
20 km
Maximum documented water height
0.30 m
Observation records
6
Countries affected
2

It was triggered by a magnitude 7.7 earthquake at a depth of 20 km.

The highest documented water height was 0.30 m (Sunosaki, Japan).

6 observation sites in 2 countries are recorded.

Outside the source country, the earliest documented arrival was at Tofino (Clayoquot),British Columbia (Canada) after 13:00 h.

Map of observation sites

6

Each dot is a documented observation site; colour and size show the observed water height. The triangle marks the source.

Tsunami arrival times

Documented arrival times from the NOAA/NCEI database, showing the earliest recorded location per country. Coverage is incomplete: a country without an entry was not necessarily spared.

  1. 0:00 hEarthquake (origin) · Sep 2, 1923, 2:46 AM UTC
  2. 13:00 hCanada · Tofino (Clayoquot),British Columbia · 0.05 m

1 places with a documented arrival time

Observations by country

CountryObservation recordsMaximum documented water heightDeathsEarliest arrival
Japan50.30 m
Sunosaki
——
Canada10.05 m
Tofino (Clayoquot),British Columbia
—13:00 h

Highest documented water heights

6 / 6

Individual documented observations for this event. Heights come from different measurement types and sources; not every location has a measured height.

Location / stationObserved heightDistance from sourceCountry
Sunosaki · Chiba0.30 m41 kmJapan
Tofino (Clayoquot),British Columbia · Bc0.05 m7,428 kmCanada
Atami · Shizuoka—105 kmJapan
Ito (Itoshi) · Shizuoka—101 kmJapan
Kamakura · Kanagawa—75 kmJapan
Katsuura (Katsuurashi) · Chiba—30 kmJapan

Source: NOAA National Centers for Environmental Information (NCEI), Global Historical Tsunami Database. Confirmed events only. Deaths and damage are database estimates; older records are incomplete. Water heights come from different types of observation.