Historical tsunamis · May 16, 1968, 10:39 AM UTC

1968 Off Coast of Honshu Island tsunami

Japan

The tsunami of May 16, 1968, 10:39 AM UTC originated near Off Coast of Honshu Island (Japan).

Key facts

Date
May 16, 1968, 10:39 AM UTC
Cause
Earthquake
Magnitude
M7.5
Depth
33 km
Maximum documented water height
0.58 m
Observation records
10
Countries affected
2

It was triggered by a magnitude 7.5 earthquake at a depth of 33 km.

The highest documented water height was 0.58 m (Hiroo, Japan).

10 observation sites in 2 countries are recorded.

Map of observation sites

10

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) · May 16, 1968, 10:39 AM UTC
  2. 0:28 hJapan · Urakawa · 0.55 m

8 places with a documented arrival time

Observations by country

CountryObservation recordsMaximum documented water heightDeathsEarliest arrival
Japan80.58 m
Hiroo
—0:28 h
Canada20.07 m
Tofino (Clayoquot),British Columbia
——

Highest documented water heights

10 / 10

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
Hiroo · Hokkaido0.58 m101 kmJapan
Urakawa · Hokkaido0.55 m74 kmJapan
Miyako · Iwate0.52 m214 kmJapan
Hachinohe · Aomori0.48 m146 kmJapan
Muroran · Hokkaido0.28 m173 kmJapan
Ofunato · Iwate0.23 m287 kmJapan
Enoshima · Miyagi0.14 m357 kmJapan
Tofino (Clayoquot),British Columbia · Bc Classified as doubtful0.07 m6,768 kmCanada
Ayukawa · Miyagi—370 kmJapan
Port Alberni, British Columbia · Bc Classified as doubtful—6,832 kmCanada

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.