Tsunamis in 1952

August 17, 1952 Tsunami: Desecheo Island, US Territories

August 17, 1952 · Questionable tsunami

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

Tsunami warnings in force

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.

WhereCountryKm from sourceWater height, mInland, mMeasured byFirst wave, UTCDeaths
Western Desecheo Island, PRUS Territories1Eyewitness 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.