Tsunamis in 1787

March 28, 1787 Tsunami: San Marcos, Mexico

March 28, 1787 · 4 m · 11 deaths · Definite tsunami

A tsunami caused by a magnitude 8.6 earthquake began at San Marcos, Mexico on March 28, 1787 at 17:30 UTC. The water rose as high as 4 meters. Its effects were recorded at 6 places. It killed 11 people.

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
March 28, 1787, 17:30 UTC
Source
San Marcos, Mexico
Cause
Earthquake
Earthquake
Magnitude 8.6
Maximum water height
4 m (13.1 ft)
Runups recorded
6
Tsunami intensity (Soloviev-Imamura)
2.5
Tsunami magnitude (Iida)
2
Waters
Ocean
How certain
Definite tsunami
Source location
16.500° N, 98.500° W

The toll

Deaths
11
Injuries
Few (about 1 to 50)
Damage
Severe (about $5 to $25 million)
Houses destroyed
Many (101 to 1,000)

Where the literature gives no number, NCEI records a description on a scale of 1 to 4, printed here in its words. Damage is in millions of US dollars of the year of the event, not adjusted for inflation.

What the record says

NCEI’s account, from the sources it cites.

1787, March (mistakenly April) 28 (mistakenly 14 and 18), at 11:30 [local time]. There was a large earthquake with source near San Marcos, affecting the coast of the states of Oaxaca, Guerrero and Michoacan and causing much destruction. The earthquake generated a tsunami that was observed in Acapulco and tore 11 men to pieces and left them to hang between the beams of a rather high bridge 6 km from the sea. The few who were saved were injured and very frightened. A galleon from the Philippine islands was riding in the harbor of Acapulco at a depth of 18 m. During the ebb tide, the water shallowed to 8.5 m. The city was destroyed. The wave was also observed in the region of Pochutla, Tehuantepec and other settlements in the state of Oaxaca. (reference #415)

1787, Mar. 14 (also Mar. 18, Mar. 28). Sea withdrew exposing rocks. Galleon reported 11 m lowering. Other places mentioned by Milne and by Heck are places where the earthquake was felt. Mar. 14 is date given by Belcher. Mallet gives both Mar. 14 and Mar. 18 but points out events on the two dates were probably the same. Mar. 28 is given by Sieberg and by Japan Meteorological Agency (Anon, 1964) and by Milne who also gives Apr. 3 [as end of quake series?]. (reference #79)

1787, Mar. 14 or 18. Mexico, near San Marcos. Felt along coast of Oaxaca, Michoacan, and south of Tehuantepec. Sea retired, leaving rocks of Punta Manzanilla dry, and returned very high, estimated at 36 feet by vessel at anchor." References Mallet (reference #497) and Becher (reference #1913). (reference #132)

1787 March 14. A violent earthquake in Acapulco. The sea retired as far as some rocks lying in the middle of the bay. The galleon of the Philippine Isles, which was mooored in 10 fathom water, found but 4 fathoms when the sea had retreated. The city was ruined. (reference #497)

1787, March 18, in the morning. Earthquake in Mexico extending from San Luigi de Potosi to Oaxaca, and from Vera-Cruz to Acapulco and Valladolid. Earthquake shocks from the S.E. At the city of Mexico the earth was in almost continual agitation for 24 hours. At Acapulco the sea retreated far from the shore, and returned high above its former level. From this circumstance it seems probable that the event of the 14th March has either been confounded with, or was the same at this. The city of Oaxaca was most injured. (reference #497)

The 1787 tsunami is not reported in the Japanese catalogs. As Hatori (1995) points out, the coast of Mexico faces the southwest Pacific and a tsunami generated on the Middle American Trench would not radiate energy towards Japan. If the tsunami propagated away from the coast of Mexico, it would have been observed on Easter Island and the Tuamotus; unfortunately, no written records existed on these islands at that time. (reference #14084)

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
Corralero (Alotengo)Mexico63Eyewitness observation of water height11
JamiltepecMexico822Eyewitness observation of water height
AcapulcoMexico1564Eyewitness observation of water height
Pochutla (Puerto Angel)Mexico235Eyewitness observation of water height
TehuantepecMexico3492Eyewitness observation of water height
Oaxaca CoastMexicoEyewitness observation of water height

More

Every tsunami in 1787The 1700sTsunamis of MexicoThe 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 2026-09-24. NCEI tsunami event 544.