November 14, 1816 Tsunami: Central Mexico
A tsunami caused by an earthquake began at Central Mexico on November 14, 1816. The water rose as high as 25 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
The tsunami
- Date
- November 14, 1816
- Source
- Central Mexico
- Cause
- Earthquake
- Earthquake
- The earthquake
- Maximum water height
- 25 m (82.0 ft)
- Runups recorded
- 1
- Waters
- Ocean
- How certain
- Probable tsunami
The toll
- Damage
- Limited (under about $1 million); Severe (about $5 to $25 million) with the earthquake or eruption that caused it
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.
1816 November 13. Maximum intensity 5 at Zapotlan (Cuidad Guzman). Strong shaking for eight days. The sea retreated more than 600 paces, inundating the saltworks of San Pantaleon (reference #13024)
14 November 1816: The San Pantaleon earthquake and tsunami. On 14 November, the priest Geronimo Arzac (AHAG, 1816a) was heading to Tecoman and mentioned the occurrence of several earthquakes, the strongest of which occurred on 13 November at 18:00 hr, another one on 14 November at 1:00 hr, and a third one at 10:00 hr (local time). These earthquakes caused significant damage in Colima and Tecoman and also damaged some churches and public buildings in Guadalajara (Biblioteca Publica del Estado de Jalisco [BPEJ], 1816), Tecolotlan, Suchitlan, Ayotitlan (AHAG, 1816b), Zapotlan El Grande (Vizcaino, 1986), and Colima (Río de la Loza, 1863). Figure 4c shows a facsimile of the handwritten report by priest Jose Antonio Enriquez del Castillo (Archivo de la Parroquia de Tecoman [APT], 1817) who was an eyewitness and described a tsunami event on “November 13th of 1816 two o’clock in the morning” when “the sea…” incursion reached 60 codos high (25 m); “…the water receded…” causing destruction of the salt beds, that is, harvest infrastructure (an ancient method of salt extraction). The 1816 and 1818 events occurred in the middle of the Independence War, and this might explain the relative scarcity of information. Tsunami generation: earthquake / landslide?. The San Pantaleon tsunami of 1816 was presumably produced by a medium-sized earthquake. The 1816 earthquake and tsunami description indicates that the saltworks were flooded with a wave 25 m in height (APT, 1817). (reference #13627)
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 |
|---|---|---|---|---|---|---|---|
| San Pantaleon, Colima Coast | Mexico | 25 | 825 | Eyewitness observation of water height |
More
Every tsunami in 1816The 1800sTsunamis 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 5893.