Historical tsunamis · Aug 21, 1951, 10:57 AM UTC

1951 Hawaii tsunami

United States

The tsunami of Aug 21, 1951, 10:57 AM UTC originated near Hawaii (United States).

Key facts

Date
Aug 21, 1951, 10:57 AM UTC
Cause
Earthquake
Magnitude
M6.9
Depth
12 km
Maximum documented water height
3.60 m
Damage
limited (under US$ 1 million)
Observation records
7
Countries affected
1

It was triggered by a magnitude 6.9 earthquake at a depth of 12 km.

The highest documented water height was 3.60 m.

7 observation sites in 1 countries are recorded.

Damage is estimated at limited (under US$ 1 million).

Map of observation sites

7

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) · Aug 21, 1951, 10:57 AM UTC
  2. 0:38 hUnited States · Honolulu, Oahu, Hi · 0.03 m

2 places with a documented arrival time

Observations by country

CountryObservation recordsMaximum documented water heightDeathsEarliest arrival
United States71.20 m
Hookena, Hawaii, Hi
—0:38 h

Highest documented water heights

7 / 7

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
Hookena, Hawaii, Hi · Hi1.20 m17 kmUnited States
Milolii, Hawaii, Hi · Hi1.00 m36 kmUnited States
Kailua-Kona, Hawaii, Hi · Hi0.90 m14 kmUnited States
Napoopoo, Hawaii, Hi · Hi0.90 m9 kmUnited States
Hilo, Hawaii, Hi · Hi0.10 m102 kmUnited States
Port Allen, Kauai, Hi · Hi0.10 m458 kmUnited States
Honolulu, Oahu, Hi · Hi0.03 m279 kmUnited States

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.