Historical tsunamis · Apr 2, 1977, 7:15 AM UTC

1977 Samoa Islands tsunami

Samoa

The tsunami of Apr 2, 1977, 7:15 AM UTC originated near Samoa Islands (Samoa).

Key facts

Date
Apr 2, 1977, 7:15 AM UTC
Cause
Earthquake
Magnitude
M7.6
Depth
33 km
Maximum documented water height
0.08 m
Damage
limited (under US$ 1 million)
Observation records
2
Countries affected
2

It was triggered by a magnitude 7.6 earthquake at a depth of 33 km.

The highest documented water height was 0.08 m (Pago Pago, American Samoa, USA Territory).

2 observation sites in 2 countries are recorded.

Outside the source country, the earliest documented arrival was at Pago Pago, American Samoa (USA Territory) after 0:30 h.

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

Map of observation sites

2

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 2, 1977, 7:15 AM UTC
  2. 0:30 hUSA Territory · Pago Pago, American Samoa · 0.08 m
  3. 0:39 hSamoa · Apia, Upolu Island · 0.02 m

2 places with a documented arrival time

Observations by country

CountryObservation recordsMaximum documented water heightDeathsEarliest arrival
USA Territory10.08 m
Pago Pago, American Samoa
—0:30 h
Samoa10.02 m
Apia, Upolu Island
—0:39 h

Highest documented water heights

2 / 2

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
Pago Pago, American Samoa · As0.08 m307 kmUSA Territory
Apia, Upolu Island0.02 m320 kmSamoa

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.