Historical tsunamis · Feb 28, 1973, 6:37 AM UTC

1973 N. Kuril Islands tsunami

Russia

The tsunami of Feb 28, 1973, 6:37 AM UTC originated near N. Kuril Islands (Russia).

Key facts

Date
Feb 28, 1973, 6:37 AM UTC
Cause
Earthquake
Magnitude
M7.2
Depth
27 km
Maximum documented water height
1.50 m
Observation records
6
Countries affected
2

It was triggered by a magnitude 7.2 earthquake at a depth of 27 km.

The highest documented water height was 1.50 m.

6 observation sites in 2 countries are recorded.

Map of observation sites

6

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) · Feb 28, 1973, 6:37 AM UTC
  2. 0:07 hRussia · Shumshu Island, Kurilskiye · 0.60 m

4 places with a documented arrival time

Observations by country

CountryObservation recordsMaximum documented water heightDeathsEarliest arrival
Russia40.80 m
Cape Vasileva, Paramushir I, Kurils
—0:07 h
United States20.10 m
Attu, Massacre Bay, Ak
——

Highest documented water heights

6 / 6

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
Cape Vasileva, Paramushir I, Kurils · Kuril Islands0.80 m102 kmRussia
Severo-Kurilsk, Paramushir Island · Kuril Islands0.76 m39 kmRussia
Shumshu Island, Kurilskiye · Kuril Islands0.60 m28 kmRussia
Attu, Massacre Bay, Ak · Ak0.10 m1,175 kmUnited States
Shemya Island, Ak · Ak0.08 m1,234 kmUnited States
Matua, Kurilskiye · Kuril Islands0.07 m362 kmRussia

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.