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A tsunami is a series of waves in a water body caused by the displacement of a large volume of water, generally in an ocean or a large lake. Earthquakes, volcanic eruptions and other underwater explosions above or below water all have the potential to generate a tsunami. Unlike normal ocean waves, which are generated by wind, or tides, which are generated by the gravitational pull of the Moon and the Sun, a tsunami is generated by the displacement of water from a large event.
Year 991 (CMXCI) was a common year starting on Thursday of the Julian calendar.
Year 551 (DLI) was a common year starting on Sunday of the Julian calendar. The denomination 551 for this year has been used since the early medieval period, when the Anno Domini calendar era became the prevalent method in Europe for naming years.
The 365 Crete earthquake occurred at about sunrise on 21 July 365 in the Eastern Mediterranean, with an assumed epicentre near Crete. Geologists today estimate the undersea earthquake to have been a moment magnitude 8.5 or higher. It caused widespread destruction in the central and southern Diocese of Macedonia, Africa Proconsularis, Egypt, Cyprus, Sicily, and Hispania (Spain). On Crete, nearly all towns were destroyed.
The 426 BC Malian Gulf tsunami devastated the coasts of the Malian and Euboean Gulfs, Greece, in the summer of 426 BC. Thucydides inquired into its causes, and concluded that the tsunami must have been caused by an earthquake. He was thus historically the first known to correctly interpret the cause of a tsunami as a preceding geological event. Herodotus, in contrast, had attributed the Potidaea tsunami to the divine wrath of Poseidon.
A devastating earthquake known in scientific literature as the Earthquake of 749 struck on January 18, 749, in areas of the Umayyad Caliphate, with the epicenter in Galilee. The most severely affected areas were parts of Palestine and western Transjordan. The cities of Tiberias, Beit She'an, Pella, Gadara, and Hippos were largely destroyed while many other cities across the Levant were heavily damaged. The casualties numbered in the tens of thousands.
The 1303 Crete earthquake occurred at about dawn on 8 August. It had an estimated magnitude of about 8, a maximum intensity of IX (Violent) on the Mercalli intensity scale, and triggered a major tsunami that caused severe damage and loss of life on Crete and at Alexandria. It badly damaged the Lighthouse of Alexandria.
The 1222 Cyprus earthquake occurred at about 06:15 UTC on 11 May. It had an estimated magnitude of 7.0–7.5 and triggered a tsunami that was recorded in Libya and Alexandria. The strongest shaking was felt in Nicosia, Limassol and Paphos. Many people died, although there are no estimates for the total number of casualties.
The 957 Caspian Sea earthquake took place in the Caspian Sea and its vicinity in 957.
The 881 Acre earthquake took place in the vicinity of Acre in 881. Alexandria was reportedly affected by the same earthquake.
The 859 Syrian coast earthquake affected the Mediterranean coast of Syria in the year 859 or 860 CE. It caused almost the complete destruction of Latakia and Jableh, major damage at Antioch and led to many deaths.
The 803 Mopsuestia earthquake took place in the vicinity of Mopsuestia and the Gulf of Alexandretta (İskenderun) in 802 or 803 CE.
The 740 Constantinople earthquake took place on 26 October, 740, in the vicinity of Constantinople and the Sea of Marmara.
The 554 Anatolia earthquake took place on August 15, in the southwest coasts of Anatolia. It affected the Güllük Gulf, and the island of Kos.
The 551 Malian Gulf earthquake took place in the Spring of 551 in the vicinity of the Malian Gulf. It affected the cities of Echinus and Tarphe.
The 542 Sea of Marmara earthquake took place in the winter of 542 in the vicinity of the Sea of Marmara. It also affected the coasts of Thrace and the Edremit Gulf. The earthquake affected the eastern Roman empire during the reign of the emperor Justinian I.
The devastating eruption of Oshima–Ōshima began on the 18th of August, 1741 and ended on May 1 the next year. Eleven days into the eruption, the Kampo tsunami with estimated maximum heights of over 90 meters swept across neighboring islands in Japan and the Korean Peninsula.
The Shōnai offshore earthquake occurred at around 14:00 on December 7, 1833. It struck with an epicenter in the Sea of Japan, off the coast of Yamagata Prefecture, Japan. A tsunami was triggered by the estimated MJMA 7.5–7.7 earthquake. One hundred and fifty people were killed and there was severe damage in the prefecture.
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