551 Beirut earthquake

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551 Beirut earthquake
Lebanon location map Topographic.png
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Local date9 July 551 (0551-07-09)
Magnitude7.5 Mw
Epicenter 33°54′N35°30′E / 33.9°N 35.5°E / 33.9; 35.5
Areas affected Phoenice (Roman province), Byzantine Empire (now Lebanon)
Max. intensity X (Extreme)
Tsunamiyes
Casualtiesabove 30,000
Main tectonic features of Lebanon Lebanon tectonics.png
Main tectonic features of Lebanon

The 551 Beirut earthquake occurred on 9 July with an estimated magnitude of about 7.5 on the moment magnitude scale and a maximum felt intensity of X (Extreme) on the Mercalli intensity scale. It triggered a devastating tsunami which affected the coastal towns of Byzantine Phoenicia, causing great destruction and sinking many ships. Overall large numbers of people were reported killed, with one estimate of 30,000 by the anonymous pilgrim of Piacenza for Beirut alone. [1]

Contents

Tectonic setting

The earthquake occurred during the reign of Justinian I (pictured) as Eastern Roman emperor. Meister von San Vitale in Ravenna.jpg
The earthquake occurred during the reign of Justinian I (pictured) as Eastern Roman emperor.

What is now Lebanon lies astride the Dead Sea Transform, which forms part of the boundary between the Arabian Plate and the African Plate. In Lebanon the fault zone forms a restraining bend associated with a right stepping offset of the fault trace. Transpressional deformation associated with this bend has formed a number of thrust faults, such as the recently identified Mount Lebanon thrust, which underlies the city and is interpreted to crop out at the seabed offshore. [2]

Damage

There is little in the way of detailed descriptions of the damage caused by this earthquake in contemporary accounts. Sources refer to the coastal cities from Tyre to Tripoli being reduced to ruins with many thousands of casualties. [1] The Anonymous pilgrim of Piacenza reported that 30,000 people died in Beirut alone. [1] Reports of damage at Petra and other locations in the Jordan Valley associated with the 551 event have been re-analyzed, suggesting that a later earthquake was more likely to be responsible. [3]

Characteristics

Earthquake

The earthquake was felt over a wide area from Alexandria in the southwest to Antioch in the north previously damaged by the earthquake of 526. The area of felt intensity of VIII or more extends from Tripoli in the north to Tyre in the south. Estimates for the magnitude vary from 7.2 on the surface wave magnitude scale to a possible 7.5 on the moment magnitude scale. [2] The rupture length is estimated to be greater than 100 kilometres (62 mi) and possibly as long as 150 kilometres (93 mi). The origin of the tsunami was thought to have been due to an underwater landslide triggered by an earthquake on the Dead Sea Transform itself. [4] More recent analysis suggested that an offshore continuation of the Roum Fault mapped onshore may have been responsible. [5] However, seabed surveys have discounted this possibility and the discovery of geologically recent fault scarps at seabed indicate that movement on the newly identified Mount Lebanon Thrust was the cause of the earthquake and the resulting tsunami. Quaternary uplift recorded by a series of marine-cut terraces between Tripoli and Beirut are consistent with continuing upward movement of the hanging wall of the proposed thrust. At a smaller scale, an uplifted vermetid bench, which indicates vertical movement of about 80 cm, is dated to the sixth century A.D. Continued uplift above this thrust since the late Miocene may explain the formation of the Mount Lebanon range. [2]

Tsunami

The tsunami affected the whole of the coast from Tyre to Tripoli. Withdrawal of the sea by up to two miles was recorded in some contemporary accounts. [1]

Future seismic hazard

The estimated return time for large earthquakes on the Mount Lebanon thrust is 1500–1750 years, although a shorter return time is also possible depending on the dating of the most recent sea-level highstand. This latter possibility would indicate that a repeat of this event may be long overdue. [2]

See also

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References

  1. 1 2 3 4 Sbeinati, M.R.; Darawcheh R.; Mouty M (2005). "The historical earthquakes of Syria: an analysis of large and moderate earthquakes from 1365 B.C. to 1900 A.D." Annals of Geophysics. 48 (3): 347–435. doi: 10.4401/ag-3206 .
  2. 1 2 3 4 Elias, A.; Tapponnier P.; Singh S.C.; King G.C.P.; Briais A.; Daëron M.; Carton H.; Sursock A.; Jacques E.; Jomaa R.; Klinger Y. (2007). "Active thrusting offshore Mount Lebanon: Source of the tsunamigenic A.D. 551 Beirut-Tripoli earthquake". Geology. 35 (8): 755–758. Bibcode:2007Geo....35..755E. doi:10.1130/G23631A.1. S2CID   54934422.
  3. ↑ Rucker, J.D.; Niemi, T.M. (2010). "Historical earthquake catalogues and archaeological data: Achieving synthesis without circular reasoning". In Sintubin M.; Stewart I.S.; Niemi T.M.; Altunel E. (eds.). Ancient Earthquakes. Special Paper. Vol. 471. Geological Society of America. pp. 97–106. ISBN   978-0-8137-2471-3 . Retrieved 2 March 2011.
  4. ↑ Ambraseys, N. N.; Melville, C. P.; Adams, R.D. (1994). The seismicity of Egypt, Arabia, and the Red Sea: a historical review. Cambridge University Press. p. 181. ISBN   978-0-521-39120-7.
  5. ↑ Darawcheh, R.; Sbeinati M.R.; Margottini C.; Paolini S. (2000). "The 9 July 551 AD Beirut earthquake, eastern Mediterranean region". Journal of Earthquake Engineering. 4 (4): 403–414. Bibcode:2000JEaEn...4..403D. doi:10.1080/13632460009350377. S2CID   140571362.
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