October 6, 1944 Tsunami: Edremit Gulf, Aegean Sea, Turkey
A tsunami caused by a magnitude 6.7 earthquake began at Edremit Gulf, Aegean Sea, Turkey on October 6, 1944 at 02:34:47 UTC. Its effects were recorded at 1 place. It killed 30 people, counting the earthquake or eruption that caused it.
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
- October 6, 1944, 02:34:47 UTC
- Source
- Edremit Gulf, Aegean Sea, Turkey
- Cause
- Earthquake
- Earthquake
- Magnitude 6.7
- Runups recorded
- 1
- Tsunami intensity (Soloviev-Imamura)
- 2
- Waters
- Ocean
- How certain
- Probable tsunami
- Source location
- 39.509° N, 26.587° E
The toll
- Deaths
- 30 with the earthquake or eruption that caused it
- Damage
- Limited (under about $1 million); Extreme (about $25 million or more) with the earthquake or eruption that caused it
- Houses destroyed
- 5,500 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.
1944 Oct 06, 02:34:48.7 UTC, Tsunami intensity 1, Tsunami reliability 4. Numerous surface cracks and water gushes reported; coastal neighborhoods of the town of Ayvalik were flooded; inundation distance was 200 m in Ayvalik. (reference #9275)
1944 Oct 06, 02:34 UTC, Tsunami intensity 2, Tsunami reliability 3. (reference #11164)
Coastal neighborhoods in Ayvalik were flooded (Aksam, October 6, 1944; Ayvalik, October 12, 1944). Waves flooded the quarters of Hayrettinpasa and Vehbibey where 90% of the houses had been collapsed during the earthquake (Cumhuriyet, October 7, 1944). Aboard the ships ‘‘Ege’’ and ‘‘Kades’’ anchored offshore the small harbor of Ayvalik the passengers felt the shock strongly and have been affected (Yeni Sabah, October 8, 1944; Cumhuriyet, October 7, 1944) [...] The source of 1944 tsunami should be defined by the sea bottom changes occurred during the earthquake. Two most crucial geological findings for this historical earthquake are the effects of the fault rupture on the coastal line as well as the vertical offsets observed on the sea bottom extended along the main fault [...] The tsunami waves observed in the town of Ayvalik, which is 23 km far from the main through of the Gulf of Edremit, may also be caused by the vertical movement of the southern block during the main shock (reference #9640)
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 |
|---|---|---|---|---|---|---|---|
| Ayvalik | Turkey | 23 | 200 | Eyewitness observation of water height |
More
Every tsunami in 1944The 1900sTsunamis of TurkeyThe 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 5818.