Historical tsunamis · Apr 12, 1962, 12:52 AM UTC

1962 Sanriku tsunami

Japan

The tsunami of Apr 12, 1962, 12:52 AM UTC originated near Sanriku (Japan).

Key facts

Date
Apr 12, 1962, 12:52 AM UTC
Cause
Earthquake
Magnitude
M7.2
Depth
25 km
Maximum documented water height
1.00 m
Observation records
12
Countries affected
1

It was triggered by a magnitude 7.2 earthquake at a depth of 25 km.

The highest documented water height was 1.00 m.

12 observation sites in 1 countries are recorded.

Map of observation sites

12

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) · Apr 12, 1962, 12:52 AM UTC
  2. 0:29 hJapan · Kamaishi · 0.14 m

9 places with a documented arrival time

Observations by country

CountryObservation recordsMaximum documented water heightDeathsEarliest arrival
Japan120.50 m
Onagawa (Onagawacho)
—0:29 h

Highest documented water heights

12 / 12

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
Onagawa (Onagawacho) · Miyagi0.50 m120 kmJapan
Ayukawa · Miyagi0.28 m112 kmJapan
Onagawa · Miyagi0.21 m120 kmJapan
Onahama · Fukushima0.15 m206 kmJapan
Kamaishi · Iwate0.14 m152 kmJapan
Matsukawaura · Fukushima0.13 m157 kmJapan
Somako · Fukushima0.13 m160 kmJapan
Tsukihama · Miyagi0.09 m126 kmJapan
Choshi · Chiba0.04 m307 kmJapan
Minato-Ohashi · Ibaraki0.04 m272 kmJapan
Nakaminato · Ibaraki0.04 m272 kmJapan
Miyako · Iwate0.02 m187 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.