December 18, 1926 Tsunami: Portugal
A tsunami caused by an earthquake and a landslide began at Portugal on December 18, 1926 at 14:45 UTC. 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
- December 18, 1926, 14:45 UTC
- Source
- Portugal
- Cause
- Earthquake and landslide
- Earthquake
- The earthquake
- Runups recorded
- 1
- Waters
- Ocean
- How certain
- Questionable tsunami
- Source location
- 38.700° N, 9.200° W
The toll
- Damage
- Moderate (about $1 to $5 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.
The waters of the Tagus River rose considerably and soon the water was covered with thousands of fish. (reference #41)
Reference #2076 states the Tagus [river] in Lisbon stirred, and the same happened with the sea in front of Cascais, with the water reaching the railway line.
Reference #4649:
Event reliability 4 (definite tsunami).
The Lisbon newspaper Diario de Noticias (1926) reports “[. . . ] Great agitation in the Tagus, it was felt in most boats that were leaned to the wall [. . . ]. A curious report by several persons, that were using the Tagus ferries, is that the fishes were alarmed with the agitation of the sea and came to the surface in groups [. . . ]. Groups of brave individuals approached the “Column Quay” to watch what was going on in the river [. . . ]”. This event shares some similarity with the 1531 Tagus event. Berninghausen (1964) reports the 1926 tsunami quoting the Seismological Dispatches of the University of Georgetwon. Cascais tide gauge station shows no clear tsunami waveform; the Seismological Dispatches of Georgetown university for this year report: ”[. . . ] Lisbon, Portugal, Dec. 18 A violent earthquake lasting three seconds, today alarmed all Lisbon [. . . ]” and for the next day: ”[. . . ] Lisbon, Portugal Dec. 19 – Lisbon has experienced a severe earthquake. The first shock Saturday lasted ten seconds. It was accompanied by subterraneous noise; the waters of the Tagus river rose considerably and soon the surface was covered with thousands of fish [. . . ] (Tendorf, 1926).
In the case of the 1926 Tagus event, and taking into consideration the low presumed magnitude of the associated earthquake, and the lack of coherent tsunami signal in Cascais tide gauge, out of the Lisbon bar, we consider as the most probable cause an earthquake marine slide in the Estuary.
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 |
|---|---|---|---|---|---|---|---|
| Cascais | Portugal | 19 | Eyewitness observation of water height |
More
Every tsunami in 1926The 1900sTsunamis of PortugalThe 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 1574.