Tsunami Event Information
Tsunami Event Information
Year
Mo
Dy
Hr
Mn
Sec
Country
Tsunami Event Validity
Tsunami Cause Code
Oceanic Tsunami
Location
Latitude
Longitude
-2000
SYRIA
1
1
Y
SYRIAN COASTS
35.683
35.800
Tsunami Parameters
Maximum Water Height (m)
Number of Runups
Number of Deposits
Tsunami Magnitude (Abe)
Tsunami Magnitude (Iida)
Tsunami Intensity
Tsunami Effects
Deaths
Death Description
Missing
Missing Description
Injuries
Injuries Description
Damage ($Mil)
Damage Description
Houses Destroyed
Houses Destroyed Description
Houses Damaged
Houses Damaged Description
3
4
Total Effects (Earthquake and Tsunami, Volcano, etc.)
Total Deaths
Total Death Description
Total Missing
Total Missing Description
Total Injuries
Total Injuries Description
Total Damage ($Mil)
Total Damage Description
Total Houses Destroyed
Total Houses Destroyed Description
Total Houses Damaged
Total Houses Damaged Description
3
4
According to excavated cuneiform texts on clay boards, a tsunami of intensity vi [?] occurred in Syria. These writings most likely referred to the events of 1380 B.C. (1380+ 100) B.C., and to the period between 1700 B.C. and 1380 B.C. in accordance with other sources.
Aegean Sea, Island of Thira, Hellenic Arc, Island of Crete. The catastrophic eruption of the volcano of Santorini accompanied by earthquakes and a powerful tsunami. As a result of natural disasters, the potent Minoan Kingdom of the Late Bronze age ceased to exist on the islands of the Aegean Sea. No eyewitness account of these events has reached modem times. The reconstruction of events is based on the data of marine and ground geology, geochemistry, archaeology, in combination with fragmentary allusions in annals and legends written considerably later.
...Application of the methods of chemical analysis of isotopes has led to the conclusion that the first enormous eruption occurred earlier than 25,000 years ago, the second not earlier than 5,000 years ago. More accurately, the eruption has been dated at (1410 + 100) B.C. using the Carbon - 14 isotope inside the fragment of an ancient tree found under the ash layer on the present day Island of Thira. An estimation of the age of this sample, performed later, by the same method resulted in the earlier date of the eruption and of the ashfall: between 1700 and 1620 B.C., most likely, in 1640 - 1620 B.C.
...More reliable evidence that the tsunami generated by the eruption of Santorini did reach the shores of the Near East, actually retaining its destructive force, was obtained during the geological exploration carried out in the region of the Syrian city of Ugarit, which used to be the capital of the ancient North - Phoenician state. A library of clay boards filled up with cuneiform was excavated. Scientists deciphered one of the poems with an account of how the harbour and half of the city of Ugarit were washed out by a strong wave approximately in 1380 B.C. It is quite possible that precisely this date should be considered the most probable date for the paroxysmal eruption of Santorini and the tsunami that followed it.
(above from reference #2130)
2nd Millennium B.C., Syrian coasts. From cuneiform texts. (reference #15)
2nd Millennium B.C., Syrian coasts, 36.5 N, 25.5 E, Earthquake intensity X. Tsunami intensity VI on the Modified Sieberg Seismic Sea-Wave Intensity Scale, which is defined as: Disastrous. Partial or complete destruction of man-made structures for some distance from the shore. Flooding of coasts to great depths. Big ships severely damaged. Trees uprooted or broken. Many casualties. (reference #20)
2nd Millennium B.C., Syria, 35 deg 41 min N, 35 deg 48 min E, validity 2. The preceding describes earthquake destruction, and a probable tsunami, at Ugarit, Syrian coast. (reference #2815)