July 26, 1591 Tsunami: Azores, Portugal
A tsunami caused by an earthquake began at Azores, Portugal on July 26, 1591. 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
- July 26, 1591
- Source
- Azores, Portugal
- Cause
- Earthquake
- Earthquake
- The earthquake
- Runups recorded
- 1
- Waters
- Ocean
- How certain
- Very doubtful tsunami
- Source location
- 37.783° N, 25.500° W
The toll
- Deaths
- Many (about 101 to 1,000) with the earthquake or eruption that caused it
- Damage
- Limited (under about $1 million)
- Houses destroyed
- Few (about 1 to 50) 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.
1591, July 26. Azores, Ilha de Sao Miguel (37 deg 47'N., 25 deg 30'W.). Sea greatly agitated. All vessels within 20 leagues of the islands injured. (reference #41)
1591, July 26. Azores, St. Michael. Sea greatly agitated. (reference #132)
1591, July 26. Azores, St. Michel; sea waves. (reference #1055)
1591, July 26. Azores, especially St. Michel; and the sea for 20 leagues round. The sea was greatly agitated, and all vessels within 20 leagues of the islands were much injured. (reference #521)
1591, July 26. This tsunami is listed as an "erroneous entry" by ref #13057. [...] Hunt (1845) also mentions the numerous earthquakes at Vila Franca do Campo and adds that the sea flooded Vila da Povoacao valley, on the southern coast of S. Miguel Island. According to Silveira (2002), given the available documentation, it is not possible to relate the flood reference of Vila da Povoacao to the seismic crisis, a tsunami or even a storm since he is the only author to mention it and, moreover, does so about 250 years after it happened. This event is mentioned in several catalogues of the nineteenth and twentieth centuries related to the occurrence of earthquakes and/or tsunamis worldwide (e.g. Mallet and Mallet 1858; Milne 1899; Heck 1947; Berninghausen 1964; Andrade et al. 2006; Borges et al. 2008). The information contained in these documents mentions the sea’s disturbance and the damage to ships as was first written by Mandelslo ([1616–1644] 1719). However, the first and contemporary account of Linschoten [1596] 1997 only mentions the shaking of the boats and the sea’s disturbance as a result of the earthquakes, with no reference to ships sailing up to 20 leagues away from the shore nor to any type of flooding of the coastal zone. It is more likely that the sea’s agitation may be due to the ships’ movement on being hit by seismic P-waves. (reference #13057)
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 |
|---|---|---|---|---|---|---|---|
| Ilha DE Sao Miguel, Azores | Azores | 0 | Eyewitness observation of water height |
More
Every tsunami in 1591The 1500sTsunamis 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 199.