Historical tsunamis · Oct 18, 1989, 12:04 AM UTC

1989 N. California tsunami

United States

The tsunami of Oct 18, 1989, 12:04 AM UTC originated near N. California (United States).

Key facts

Date
Oct 18, 1989, 12:04 AM UTC
Cause
Earthquake
Magnitude
M6.9
Depth
19 km
Maximum documented water height
1.00 m
Deaths
62
Injuries
3,757
Houses destroyed
many (about 101–1,000)
Damage
US$ 5,600 million
Observation records
4
Countries affected
2

It was triggered by a magnitude 6.9 earthquake at a depth of 19 km.

The highest documented water height was 1.00 m (Moss Landing, Ca, United States).

4 observation sites in 2 countries are recorded.

The database records 62 deaths.

Houses destroyed: many (about 101–1,000).

Damage is estimated at US$ 5,600 million.

Map of observation sites

4

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) · Oct 18, 1989, 12:04 AM UTC
  2. 0:21 hUnited States · Monterey, Ca · 0.20 m

1 places with a documented arrival time

Observations by country

CountryObservation recordsMaximum documented water heightDeathsEarliest arrival
United States31.00 m
Moss Landing, Ca
—0:21 h
Australia1———

Highest documented water heights

4 / 4

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
Moss Landing, Ca · Ca1.00 m28 kmUnited States
Monterey, Ca · Ca0.20 m48 kmUnited States
Fort Denison, Sydney Harbor—11,932 kmAustralia
Santa Cruz, Ca · Ca—14 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.