January 31, 1866 Tsunami: Thera Island (Santorini), Greece
A tsunami caused by a volcano and a magnitude 6.1 earthquake began at Thera Island (Santorini), Greece on January 31, 1866. 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
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
- January 31, 1866
- Source
- Thera Island (Santorini), Greece
- Cause
- Volcano and earthquake
- Earthquake
- Magnitude 6.1
- Runups recorded
- 1
- Waters
- Ocean
- How certain
- Very doubtful tsunami
- Source location
- 36.400° N, 25.300° E
The toll
- Damage
- Moderate (about $1 to $5 million) with the earthquake or eruption that caused it
- Houses destroyed
- 52 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.
1866, January 28 (31). Aegean Sea, Island of Thira. Eruption of the volcano of Santorini began and was accompanied, according to some data by tsunami. According to Perrey [1870], there was no tsunami. (reference #2130)
1866, January 31, night. 36.4 N, 25.4 E, magnitude 6.1, intensity VII, tsunami intensity 1, reliability 0. Sea disturbance. (reference #2427)
1866, January 31 (28), tsunami reliability 1-2. (reference #9275)
1866, January 31, night. Kyriazopoulos (1979) reports that by the strong eruption of the volcano of Nea Karnene the islet George and the ephemeral Afroessa were formed and he cites a poem of his family collection where it is written that the progressive subsidence of a part of the islet Nea Kamene started on 18 January. The sea started to blow up, the coastal houses to crack and to disappear under the water. The ship masters tried to save their ships from the madness of the sea and from the eruption of the volcano. As main phase of this volcanic activity, the time interval from 16 January 1866 up to 15 October 1870 is considered (Georgalas, 1962; Skourtis, 1995). (reference #4408)
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 |
|---|---|---|---|---|---|---|---|
| Santorini | Greece | 245 | Eyewitness observation of water height |
More
Every tsunami in 1866The 1800sTsunamis of GreeceThe 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 2026-10-01. NCEI tsunami event 948.