Historical tsunamis · Jan 13, 1941, 4:27 PM UTC

1941 Bismarck Sea tsunami

Papua New Guinea

The tsunami of Jan 13, 1941, 4:27 PM UTC originated near Bismarck Sea (Papua New Guinea).

Key facts

Date
Jan 13, 1941, 4:27 PM UTC
Cause
Earthquake
Magnitude
M7.4
Depth
15 km
Maximum documented water height
0.15 m
Deaths
4
Houses destroyed
1
Damage
moderate (about US$ 1–5 million)
Observation records
3
Countries affected
1

It was triggered by a magnitude 7.4 earthquake at a depth of 15 km.

The highest documented water height was 0.15 m (Rabaul, New Britain, Papua New Guinea).

3 observation sites in 1 countries are recorded.

The database records 4 deaths.

Houses destroyed: 1.

Damage is estimated at moderate (about US$ 1–5 million).

Map of observation sites

3

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) · Jan 13, 1941, 4:27 PM UTC
  2. 0:02 hPapua New Guinea · Rabaul, New Britain · 0.15 m

1 places with a documented arrival time

Observations by country

CountryObservation recordsMaximum documented water heightDeathsEarliest arrival
Papua New Guinea30.15 m
Rabaul, New Britain
—0:02 h

Highest documented water heights

3 / 3

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
Rabaul, New Britain · East New Britain0.15 m13 kmPapua New Guinea
Bainings, New Britain—37 kmPapua New Guinea
Blanche Bay, New Britain · East New Britain—27 kmPapua New Guinea

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.