August 17, 1952 Tsunami: Desecheo Island, US Territories
A tsunami caused by a landslide began at Desecheo Island, US Territories on August 17, 1952. 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
- August 17, 1952
- Source
- Desecheo Island, US Territories
- Cause
- Landslide
- Runups recorded
- 1
- Waters
- Ocean
- How certain
- Questionable tsunami
- Source location
- 18.388° N, 67.479° 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.
Reference#13840:
On August 17, 1952, I was marooned for twelve hours on the small, uninhabited island of Desecheo, some fifteen miles off the north-west coast of Puerto Rico. Suddenly, at about 4.30 p.m. local time, the sea withdrew along the western coast, sea-level being lowered perhaps 10 ft. There was a dull, muffled sound, followed by a remarkably rapid churning of the seas towards the west-north-west. Three hours later, seas were still very high, and it was next morning before I could be brought from the island. It was very warm, sunny and balmy all day. Later, it was discovered that rough seas had occurred along both coasts of Mona Passage.
For this date the San Juan Observatory recorded practically minimum microseismic activity, and nothing unusual was recorded in Martinique.
A study of synoptic weather maps of the NorthSouth Atlantic and Caribbean Sea for the above dates rules out the possibility of the rough seas being attributed to meteorological conditions. If storms of rapid development, perhaps even too rapid to have been recorded on synoptic charts, were the cause, then it is strange that the wild seas were such localized occurrences. A detailed check has shown that on and about the above dates no other West Indian island nor even the neighbouring mainlands recorded unusual seas.
There is no indication of submarine volcanic activity being the cause.
It would appear that it was neither earthquakes, meteorological storms nor submarine volcanoes which were responsible for these peculiarly localized phenomena along the coasts of the islands mentioned. The effect was purely local and a local cause must be sought.
[…] From the point of view of slope stability, the steep slopes north of Desecheo must naturally be viewed with suspicion.
Reference #12345 lists as questionable tsunami with a landslide source. (accessed July 2024)
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 |
|---|---|---|---|---|---|---|---|
| Western Desecheo Island, PR | US Territories | 1 | Eyewitness observation of water height |
More
Every tsunami in 1952The 1900sTsunamis of US TerritoriesThis 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 2026-09-24. NCEI tsunami event 5935.