Tsunamis in 358

August 24, 358 Tsunami: Marmara Sea, Turkey

August 24, 358 · Deaths: many · Very doubtful tsunami

A tsunami caused by an earthquake began at Marmara Sea, Turkey on August 24, 358. 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

Tsunami warnings in force

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
August 24, 358
Source
Marmara Sea, Turkey
Cause
Earthquake
Earthquake
The earthquake
Runups recorded
1
Waters
Ocean
How certain
Very doubtful tsunami
Source location
40.770° N, 29.900° E

The toll

Deaths
Many (about 101 to 1,000) with the earthquake or eruption that caused it
Damage
Severe (about $5 to $25 million) with the earthquake or eruption that caused it
Houses destroyed
Many (101 to 1,000) 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.

358, August 24. Nicomedia. A destructive earthquake in Bithynia in western Anatolia almost totally destroyed Nicomedia (Izmit) and its district. The shock was felt over a large area and had social repercussions... The flooding by the sea of the lower parts of Nicomedea was probably the result of the tempest, rather than a seismic sea wave. There is no mention of sea waves elsewhere ...

An oration was composed on the occasion, and the event is mentioned by almost all near-contemporary writers. However, it appears that the effects of the earthquake were less catastrophic than individual reports seem to indicate. Far more was rumored to have happened to those at a distance than had actually happened, and both pagan and ecclesiastical writers seem to exaggerate the destruction, attributing it to the wrath of their gods.

Impressively many sources survive for this earthquake: the effects on Nicomedea were of intense interest to near-contemporary ecclesiastical historians, insofar as the earthquake prevented a synod from being held in Nicomedea. This was at the time of the Arian dispute, and the Nicomedea Synod was intended as an orthodox rival to the Arian synod held in Arinium. Predictably the Arian writer Philostorgius sees the earthquake as suppressing an impious synod, and talks about the inundation of Nicomedea by a sea wave, while the orthodox writer Sozomen attemps to show that the accounts of the destruction of Nicomedea were exaggerated. By way of mitigation he points out that Nicaea, Perinthus and Constantinople were also affected, and that the citadel tower of Nicomedea survived.

(above from reference #9116)

358, August 24. A tremendous earthquake in Macedonia, Little Asia, Greece, Syria, Egypt, Tsunami, Nicomedia in Bithynia suffered most. (reference #1149)

Note: Ambraseys (2002) (reference #2955) states "This information implies that most probably the sea waves were due to the storm and that the earthquake, which we are told followed a wet period, triggered landslides which carried housed down the hillsides and into the sea. At least for Izmit [Nicomeda] it appears that the damaging waves were generated by landslides which fell into the sea or by slumping of the coast." However, in a later publication (reference #9116) this possible landslide generated tsunami is not mentioned though statements are made that the shock "probably triggered landslide". Reference #11164 (v.2) and #9275 give a validity of 4 (definite tsunami) to this event, citing reference #2955.

Every runup

Nearest the source first. Heights are above sea level at the time; a tide gauge reads half the wave’s full height.

WhereCountryKm from sourceWater height, mInland, mMeasured byFirst wave, UTCDeaths
Izmit (Nicomedea) doubtfulTurkey3Eyewitness observation of water height

More

Every tsunami in 358The 300sTsunamis 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 2314.