May 7, 1822 Tsunami: Matina, Costa Rica
A tsunami caused by a magnitude 7.6 earthquake began at Matina, Costa Rica on May 7, 1822. Its effects were recorded at 3 places in at least 2 countries.
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
- May 7, 1822
- Source
- Matina, Costa Rica
- Cause
- Earthquake
- Earthquake
- Magnitude 7.6
- Runups recorded
- 3
- Waters
- Ocean
- How certain
- Probable tsunami
- Source location
- 9.500° N, 83.000° W
The toll
- Damage
- Moderate (about $1 to $5 million) with the earthquake or eruption that caused it
- Houses destroyed
- Some (about 51 to 100) 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.
A local tsunami was reported at Matina. The rivers and bays experienced flooding (possible description of a tsunami). (reference #53)
1822, May 7. 9.5 N, 83 W, magnitude 7.6 Ms. Matina, Costa Rica. (reference #273)
in Matina three shocks were felt as violent as no neighbor remembered having ever felt; the shaking continued almost for twenty-four hours without interruption [...] the rivers and bays grew and caused floods; that the neighbors decided to come to Cartago. (reference #1539) (Note: unofficial translation)
7 May 1822 – Confirmed tsunami. [Reference #1539] reports from historic papers that “in (Boca) Matina there were three violent shakes as no resident remember to had felt before; […] that the rivers and bay grew and caused floods” (p. 21; translated by the authors). The flooding caused by rivers can be explained by plugging caused by landslides consequence of the earthquake, but the “grew” of the bay and its subsequent flooding can only be explained as a tsunami. (reference #12928)
The observations that have been interpreted likely indicate the occurrence of a tsunami associated with the San Estanislao earthquake, suggesting that this event had a reverse fault rupture mechanism, similar to that of the 1991 earthquake and also we can conclude that the hypocenter is located on the Caribbean side of the southern countries of Central America. Likewise, the damage distribution clearly shows that the hypocenter must have occurred in the Caribbean region of Costa Rica. (reference #12929) (Note: unofficial translation)
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 |
|---|---|---|---|---|---|---|---|
| Punta Mona | Costa Rica | 43 | Eyewitness observation of water height | ||||
| Boca del Rio Matina | Costa Rica | 72 | Eyewitness observation of water height | ||||
| Bocas del Toro | Panama | 84 | Eyewitness observation of water height |
More
Every tsunami in 1822The 1800sTsunamis of Costa RicaThe 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 640.