Historical tsunamis · Aug 21, 2003, 12:12 PM UTC

2003 South Island tsunami

New Zealand

The tsunami of Aug 21, 2003, 12:12 PM UTC originated near South Island (New Zealand).

Key facts

Date
Aug 21, 2003, 12:12 PM UTC
Cause
Earthquake and landslide
Magnitude
M7.2
Depth
28 km
Maximum documented water height
4.00 m
Injuries
few (up to about 50)
Damage
limited (under US$ 1 million)
Observation records
3
Countries affected
2

It was triggered by a magnitude 7.2 earthquake at a depth of 28 km.

The highest documented water height was 4.00 m (Charles Sound, New Zealand).

3 observation sites in 2 countries are recorded.

Outside the source country, the earliest documented arrival was at Port Kembla (Australia) after 3:26 h.

Damage is estimated at limited (under US$ 1 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) · Aug 21, 2003, 12:12 PM UTC
  2. 2:00 hNew Zealand · Jackson Bay · 0.15 m
  3. 3:26 hAustralia · Port Kembla · 0.07 m

2 places with a documented arrival time

Observations by country

CountryObservation recordsMaximum documented water heightDeathsEarliest arrival
New Zealand24.00 m
Charles Sound
—2:00 h
Australia10.07 m
Port Kembla
—3:26 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
Charles Sound4.00 m4 kmNew Zealand
Jackson Bay0.15 m172 kmNew Zealand
Port Kembla0.07 m1,818 kmAustralia

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.