November 4, 1958 Tsunami: East Pacific Rise, Pacific Ocean
A tsunami caused by a magnitude 6.1 earthquake began at East Pacific Rise, Pacific Ocean on November 4, 1958 at 22:54:46 UTC. The water rose as high as 0.1 meters. Its effects were recorded at 1 place.
Where the waves reached
The source (white) and every runup with a place, colored by the water height recorded there. A ring is a runup NCEI marks doubtful.
- Under 1 m
- 1 to 3 m
- 3 to 10 m
- 10 to 30 m
- 30 m and more
- Height not recorded
Travel times
How long the first wave took to reach each part of the ocean, one line for each hour up to 24, estimated from the source and the depth of the sea.
The travel times are computed in your browser, which needs JavaScript.
- 1 to 4 hours
- 5 to 6 hours
- 7 to 14 hours
- 15 hours and more
Computed in your browser the way NOAA’s own travel time maps are: the wave travels at the square root of gravity times the depth, over NOAA’s ETOPO1 depths averaged to a 10 arc-minute grid. Checked against NOAA NCEI’s maps for 21 tsunamis over the first 24 hours, these lines fall within 10 minutes of NCEI’s at half the points compared and within 52 minutes at 9 in 10. They give when the first wave could arrive, not how high it is; bays, harbors and island chains finer than the grid can see it later. Not for use in a warning: see tsunami.gov.
The tsunami
- Date
- November 4, 1958, 22:54:46 UTC
- Source
- East Pacific Rise, Pacific Ocean
- Cause
- Earthquake
- Earthquake
- Magnitude 6.1
- Maximum water height
- 0.1 m (0.3 ft)
- Runups recorded
- 1
- Waters
- Ocean
- How certain
- Very doubtful tsunami
- Source location
- 50.000° S, 115.000° W
The toll
The record gives no deaths, injuries or damage for this tsunami.
What the record says
NCEI’s account, from the sources it cites.
1958, November 4, 22:54:46 UTC, 50 S 115 W, magnitude 6.1 MS. An earthquake with its source within the area of the East Pacific Ridge generated a tsunami which was recorded by a number of tide gauge stations. After 15.6 hours the wave arrived at Midway Island and was recorded there with an amplitude of 10 cm and a peiod of 12 minutes (Brazee, Cloud, 1960; Iida et al., 1967; Pararas-Caraydnnis, 1969). The latter source expresses reservations regarding the authenticity of the report on this tsunami. (reference #415)
1958, November 4, 22:55. A magnitude 6.0 earthquake from the East Pacific rise is listed by Pararas-Carayannis (1967) as having possibly generated a tsunami that was recorded at Midway. Given the low magnitude of the earthquake, the usually non-tsunamigenic source region, the small wave amplitude of 0.1 m and the lack of other reports, this is a very doubtful tsunami. (reference #236)
Every runup
Nearest the source first. Heights are above sea level at the time; a tide gauge reads half the wave’s full height.
| Where | Country | Km from source | Water height, m | Inland, m | Measured by | First wave, UTC | Deaths |
|---|---|---|---|---|---|---|---|
| Midway Islands, HI | US Territories | 10,620 | 0.1 | Tide gauge (half the maximum wave height) | day 5, 14:31 |
More
Every tsunami in 1958The 1900sTsunamis of Pacific OceanThe earthquakeThis day in weather historyAlerts in force
Sources
Tsunami events and runups from NOAA’s National Centers for Environmental Information, Global Historical Hazard Database, cited as NCEI/WDS, doi:10.7289/V5PN93H7. Public domain. Read 2026-10-01. NCEI tsunami event 1883.