November 30, 1823 Tsunami: Saint Pierre, Martinique
A tsunami caused by an earthquake began at Saint Pierre, Martinique on November 30, 1823. 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 30, 1823
- Source
- Saint Pierre, Martinique
- Cause
- Earthquake
- Earthquake
- The earthquake
- Runups recorded
- 1
- Tsunami intensity (Soloviev-Imamura)
- 2
- Waters
- Ocean
- How certain
- Definite tsunami
- Source location
- 14.400° N, 61.000° W
The toll
- Damage
- Limited (under about $1 million)
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.
At 2:45 local time a strong earthquake was followed by a tsunami at 3:10 am. Mallet (Reference #497) said, "The sea rose after the shock, and occasioned some damage in the harbours." There was damage in Saint-Pierre Harbor.
Reference #9688:
Archived exactly one year apart, respectively on 30 November 1823 and 30 November 1824, both of these events purportedly caused ‘damages in the harbour’ on those two dates - seemingly the Saint-Pierre harbour. Moreover, both events appear to have occurred following periods of high temperatures that were accompanied by torrential rains (Mallet, 1852, 1853, 1854). These similarities lead to two distinct hypotheses. It is entirely possible that these two purported tsunamis were in fact one single event, wrongly reported as separate events due to transcription of calendar mistakes. Alternatively, it is somewhat possible that the two events resulted from earthquakes that occurred exactly one-year apart. However it is highly unlikely that such coincidence in the day and month actually occurred. Finally, it is also entirely possible that the reported tsunamis were storm surges generated by hurricanes.
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 |
|---|---|---|---|---|---|---|---|
| Saint Pierre | Martinique | 42 | Eyewitness observation of water height |
More
Every tsunami in 1823The 1800sTsunamis of MartiniqueThe 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 644.