1822 Aleppo earthquakeSt. Simeon FaultDead Sea TransformSyria earthquake historystrike-slip fault

1822 Aleppo Earthquake: A Devastating Seismic Event in Northern Syria

1822 Aleppo Earthquake: A Devastating Seismic Event in Northern Syria On the evening of August 13, 1822, a powerful earthquake struck the northern regions of the Ottoman Empire, causing w...

1822 Aleppo Earthquake: A Devastating Seismic Event in Northern Syria

On the evening of August 13, 1822, a powerful earthquake struck the northern regions of the Ottoman Empire, causing widespread destruction across what is now northern Syria and the Hatay Province of Turkey. With an estimated magnitude of 7.0, the event left a lasting mark on the region's geography and urban development, particularly in the city of Aleppo.

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Key Facts

  • Date: August 13, 1822
  • Magnitude: 7.0
  • Epicenter: 36°06′N 36°45′E
  • Maximum Intensity: IX (Destructive) on the EMS-98 scale
  • Estimated Casualties: 20,000 to 60,000 deaths
  • Fault Line: St. Simeon Fault
  • Duration: 40 seconds

Tectonic Setting and Geological Cause

The earthquake occurred in a highly active seismic zone. Aleppo is situated near the Dead Sea Transform, a major fault system where the Arabian plate moves northward relative to the African plate at a rate of approximately 5 mm per year. This specific region has a long history of significant seismic activity, including major events in 115, 859, 1138, and 1170.

Geologists propose that the 1822 event was caused by a left lateral strike-slip movement—a type of faulting where two blocks of earth slide past each other horizontally—along the 140 km long St. Simeon Fault. This fault is a branch of the Missyaf Fault, which is part of the broader Dead Sea Transform system.

The Sequence of Events

The disaster did not happen in isolation. A series of foreshocks began on August 5, with the final major precursor occurring just thirty minutes before the mainshock. The main event lasted 40 seconds and was characterized by three distinct peaks in intensity. The immediate aftermath saw 30 aftershocks within the first eight minutes, and seismic activity continued for nearly two and a half years. The most destructive aftershock occurred on September 5, 1822.

Impact and Destruction

The earthquake's intensity was felt far and wide, reaching as far as Rhodes, Cyprus, and Gaza. On the European macroseismic scale (EMS), the intensity reached a maximum of IX (Destructive) in Al-Qusayr and Jisr al-Shughur.

Severe damage spanned a vast area, stretching from Gaziantep to Antakya in modern Turkey, and from Aleppo to Khan Sheikhun in modern Syria. Several towns experienced complete or near-complete destruction, including:

  • Turkey: Kilis, Gaziantep, Araplar, Burç, Kehriz, and Sağçe.
  • Syria: Armanaz, Harem, Darkush, Jisr al-Shughur, Khan Shiekhun, Ariha, Idlib, and Maarat.

The Decline of Aleppo

The city of Aleppo suffered catastrophic losses. The damage was so extensive that much of the old city center remained unrepaired. Residents began moving outside the ruined city walls, constructing new homes with wooden frames. The city's moat became filled with the rubble of collapsed buildings. This physical and economic devastation contributed to Aleppo's decline as a primary commercial center during this era.

Tsunami Reports

There is conflicting evidence regarding a tsunami (a seismic sea-wave). While some researchers, such as Ambraseys, found no evidence of one, other historical sources report a tsunami that affected the coasts of Cyprus, the Gulf of Iskenderun, and Lebanon.

Event Summary

Summary of the 1822 Aleppo Earthquake
Parameter Detail
Local Time 21:50
Depth 18 km (11 mi)
Fault Type Strike-slip (Left lateral)
Duration of Mainshock 40 seconds
Death Toll Range 20,000 – 60,000
Most Destructive Aftershock September 5, 1822

Frequently Asked Questions

What was the estimated magnitude of the 1822 earthquake?

The earthquake had an estimated magnitude of 7.0.

How many people are believed to have died in the event?

While reports range between 30,000 and 60,000 deaths for the entire sequence, 20,000 is considered a more likely figure.

Which fault line was responsible for the earthquake?

The earthquake is attributed to the St. Simeon Fault, a 140 km long branch of the Missyaf Fault within the Dead Sea Transform system.

Did the earthquake cause a tsunami?

Evidence is contradictory; some sources report a tsunami affecting Lebanon, Cyprus, and the Gulf of Iskenderun, while other researchers found no evidence of one.

How did the earthquake affect the city of Aleppo's status?

The severe destruction of the city center and the resulting displacement of the population contributed to Aleppo becoming less important as a commercial hub during that period.

References

  1. 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." (PDF). Annals of Geophysics. 48 (3): 347–435. Retrieved 22 September 2011.
  2. Ambraseys, N.N. (1989). "Temporary seismic quiescence: SE Turkey". Geophysical Journal International. 96 (2): 311–331. Bibcode:1989GeoJI..96..311A. doi:10.1111/j.1365-246X.1989.tb04453.x.
  3. Darawcheh, R.; Abdul-wahed, M.K.; Hasan, A. (2019). "The 13th-August-1822 Aleppo Earthquake: Implications for the Seismic Hazard Assessment at the Antakia Triple Junction". In Sundararajan, N.; Eshagh, N.; Meghraoui, M.; Al-Garni, M.; Giroux, B. (eds.). On Significant Applications of Geophysical Methods. CAJG 2018. Advances in Science, Technology & Innovation (IEREK Interdisciplinary Series for Sustainable Development). Springer. pp. 179–181. doi:10.1007/978-3-030-01656-2_40. ISBN 978-3-030-01656-2. S2CID 135271551.
  4. Gomez, F.; Karam, G.; Khawlie, M.; McClusky S.; Vernant P.; Reilinger R.; Jaafar R.; Tabet C.; Khair K.; Barazangi M. (2007). "Global Positioning System measurements of strain accumulation and slip transfer through the restraining bend along the Dead Sea fault system in Lebanon". Geophysical Journal International. 168 (3): 1021–1028. Bibcode:2007GeoJI.168.1021G. doi:10.1111/j.1365-246X.2006.03328.x. hdl:1885/36424.
  5. Khair, K.; Karakaisis, G.F.; Papadimitriou, E.E. (2000). "Seismic zonation of the Dead Sea Transform Fault area". Annals of Geophysics. 43: 61–79. doi:10.4401/ag-3620.