Historical tsunamis · Aug 24, 1942, 10:50 PM UTC
1942 S. Peru tsunami
Peru
The tsunami of Aug 24, 1942, 10:50 PM UTC originated near S. Peru (Peru).
Key facts
- Date
- Aug 24, 1942, 10:50 PM UTC
- Cause
- Earthquake and landslide
- Magnitude
- M8.2
- Depth
- 60 km
- Maximum documented water height
- 2.00 m
- Deaths
- 30
- Injuries
- 25
- Houses destroyed
- many (about 101–1,000)
- Damage
- severe (about US$ 5–25 million)
- Observation records
- 3
- Countries affected
- 1
It was triggered by a magnitude 8.2 earthquake at a depth of 60 km.
The highest documented water height was 2.00 m (Lomas, Peru).
3 observation sites in 1 countries are recorded.
The database records 30 deaths.
Houses destroyed: many (about 101–1,000).
Damage is estimated at severe (about US$ 5–25 million).
Map of observation sites
3Each 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.
- 0:00 hEarthquake (origin) · Aug 24, 1942, 10:50 PM UTC
- 0:39 hPeru · Matarani · 0.50 m
2 places with a documented arrival time
Observations by country
| Country | Observation records | Maximum documented water height | Deaths | Earliest arrival |
|---|---|---|---|---|
| 3 | 2.00 m Lomas | — | 0:39 h |
Highest documented water heights
3 / 3Individual documented observations for this event. Heights come from different measurement types and sources; not every location has a measured height.
| Location / station | Observed height | Distance from source | Country |
|---|---|---|---|
| Lomas · Arequipa | 2.00 m | 138 km | Peru |
| Callao la Punta · Callao | 1.60 m | 348 km | Peru |
| Matarani · Arequipa | 0.50 m | 472 km | Peru |
More tsunamis
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.