1157 Hama earthquake

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1157 Hama earthquake
Syria physical location map.svg
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Local date12 August 1157
Magnitude7.4 Ms [1]
Epicenter 35°06′N36°30′E / 35.1°N 36.5°E / 35.1; 36.5 [2]
Areas affected Syria (region)
Total damageExtreme [3]
Max. intensity MMI VIII (Severe) MMI IX (Violent)
Casualties8,000 [3]

After a year of foreshocks, an earthquake occurred on 12 August 1157 near the city of Hama, in west-central Syria (then under the Seljuk rule), where the most casualties were sustained. [2] In eastern Syria, near the Euphrates, the quake destroyed the predecessor of the citadel al-Rahba, subsequently rebuilt on the same strategic site. The earthquake also affected Christian monasteries and churches in the vicinity of Jerusalem.

See also

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<span class="mw-page-title-main">1170 Syria earthquake</span> Extreme level earthquake in Syria

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The 1856 Heraklion earthquake, also known as the Crete earthquake or Rhodes earthquake, occurred on the morning of October 12 at 02:45 am local time. This extremely catastrophic earthquake had an estimated magnitude of 7.7 to 8.3 at a depth of approximately 61 to 100 km. The earthquake was felt over a very wide area extending from Sicily, Italy to the Levant and North Africa. On the Greek island of Crete, the effects of the earthquake were cataclysmic, over 500 bodies were recovered in the city of Heraklion. Shockwaves from the earthquake were felt intensely, covering all of the Ottoman Empire; present-day Turkey, Cyprus and the Middle East where damage and human losses were reported. In Malta, the Għajn Ħadid Tower—a coastal watchtower built around the year 1638—was severely damaged in the earthquake, when its upper floor collapsed. In Cairo, Egypt, the earthquake destroyed buildings, created seiches in canals, and killed several people. Off the Egyptian and Italian coasts, sailors reported feeling a seaquake.

The northern part of the Ottoman Empire was struck by a major earthquake on 13 August 1822. It had an estimated magnitude of 7.0 Ms and a maximum felt intensity of IX (Destructive) on the European macroseismic scale (EMS). It may have triggered a tsunami, affecting nearby coasts. Damaging aftershocks continued for more than two years, with the most destructive being on 5 September 1822. The earthquake was felt over a large area including Rhodes, Cyprus and Gaza. The total death toll reported for this whole earthquake sequence ranges between 30,000 and 60,000, although 20,000 is regarded as a more likely number.

The 1872 Amik (Antakya) earthquake occurred on April 3 with an epicenter within the Amik Valley in the Ottoman Empire. Earthquake had an estimated magnitude of Mw  7.0–7.2 or Ms  7.2 and maximum MSK 64 rating of XI (Catastrophic). Turkey and Syria were devastated by this earthquake, and the region lost at least 1,800 residents.

A destructive earthquake affected present-day northwestern Syria and south-central Turkey in January 1344. Estimates of the seismic magnitude (Mw ) range between 6.8 and 7.6. The MSK 64 intensity was VII–VIII at Manbij; VI–VII at Aleppo and IV at Damascus. Thousands died in Syria and many structures were destroyed.

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." Annals of Geophysics. 48 (3): 347–435. doi: 10.4401/ag-3206 .
  2. 1 2 Ambraseys, Nicholas N. (2004). "The 12th century seismic paroxysm in the Middle East: a historical perspective" (PDF). Annals of Geophysics. 47 (2–3): 733, 738, 745, 750.
  3. 1 2 National Geophysical Data Center / World Data Service (NGDC/WDS) (1972), Significant Earthquake Information, National Geophysical Data Center, NOAA, doi:10.7289/V5TD9V7K