1114 Marash earthquake

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1114 Marash earthquake
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Local dateNovember 29, 1114
Magnitude7.4–7.7 Ms
Epicenter 37°54′N36°58′E / 37.90°N 36.97°E / 37.90; 36.97
Max. intensity EMS-98 IX (Destructive)
Casualties40,000 (Marash); tens of thousands (Sis); 400 (Azaz) [1]

The Marash earthquake occurred in the area of Marash during the early morning hours of November 29, 1114. It had an estimated surface-wave magnitude between 7.4 and 7.7 and an epicenter location in modern-day Turkey. The mainshock was preceded by two destructive foreshocks in August and November that same year. At least 40,000 people were killed in the earthquake; a number contested by historians due to the small population in the area at the time. These earthquakes were associated with seismic activity on the East Anatolian Fault.

Contents

Earthquake

The magnitude was estimated at 7.4–7.7 Ms and assigned a maximum EMS-92 intensity of IX. [2] The calculated moment magnitude was similar to that of the 6 February 2023 earthquake which measured Mw 7.8. [3] The mainshock and its foreshocks were associated with seismic activity along the East Anatolian Fault. Two large foreshocks were documented on 10 August and 13 November the same year. The 10 August foreshock destroyed several costal and fortified cities although unnamed and considered by historians as rhetoric. Marash was partly destroyed and all surrounding towns were levelled by the 13 November earthquake. There were many deaths in the region associated with the 13 November foreshock. At Antioch, large fissures occurred, causing buildings to settle into the ground. [4]

Damage and casualties

Marash was an important city with a large Christian population at that time. According to the contemporary sources, the city was completely underground. Matthew of Edessa records that no one living in the city survived the earthquake and that about 40,000 people living in Marash died. [5] That number seems excessive since the population of the town is estimated to have been a few thousand only. [6] Another estimate for the city's population suggested 24,000 residents. Michael the Syrian records that the city of Marash is a tomb for its own people. Al-Azimi records that it was dark before the earthquake, and then it snowed and covered with snow on all sides.

Apart from Marash, the earthquake also caused destruction in Elbistan, Sis, Mopsuestia, Keysun, Sümeysat (Samsat), Hısn-ı mansûr (Adıyaman), Raban, Edessa, Antioch, Harran, Aleppo, Azaz, Esârib, Zerdana and Balis. The earthquake caused the thirteen towers of the Edessa city wall and a part of the Harran city wall to collapse. While many monasteries and villages were destroyed in the city of Sis, tens of thousands of people died. It also destroyed the Azez fortress and caused the death of four hundred people. William of Tyre also records that this earthquake caused the most damage in the coastal region of Cilicia, Isauria, and Northern Syria. [1] The lord of Marash and the bishop of Marash, although both unnamed in sources, were killed in the earthquake. [6]

Walter the Chancellor who was in Antioch documented many city residents sought refuge in tents built on courtyards, gardens, groves and abandoned dwellings. Fulcher of Chartres reported most houses in towns around the Antioch region were razed to the ground, killing its residents. According to Ibn al-Qalanisi, many residents of Damascus were frightened. In the history book The Complete History by Ibn al-Athīr, he wrote about widespread destruction and fatalities in Al-Ruha, Harran, Samsat, Balis and other areas. The city of Mopsuestia was also partly destroyed. [7] Damage in Aleppo was limited to some collapsed homes in the city center and upper district where some residents died. A tower at the north gate of Aleppo, Atarib and Azaz fort were badly damaged. [4]

Related Research Articles

Coulomb stress transfer is a seismic-related geological process of stress changes to surrounding material caused by local discrete deformation events. Using mapped displacements of the Earth's surface during earthquakes, the computed Coulomb stress changes suggest that the stress relieved during an earthquake not only dissipates but can also move up and down fault segments, concentrating and promoting subsequent tremors. Importantly, Coulomb stress changes have been applied to earthquake-forecasting models that have been used to assess potential hazards related to earthquake activity.

<span class="mw-page-title-main">Samsat</span> Settlement in Eastern Turkey

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<span class="mw-page-title-main">Azaz</span> City in northwest Syria

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<span class="mw-page-title-main">Siege of Edessa (1146)</span> Crusaders siege on Zengid Edessa

The siege of Edessa in October–November 1146 marked the permanent end of the rule of the Frankish Counts of Edessa in the city on the eve of the Second Crusade. It was the second siege the city had suffered in as many years, the first siege of Edessa having ended in December 1144. In 1146, Joscelyn II of Edessa and Baldwin of Marash recaptured the city by stealth but could not take or even properly besiege the citadel. After a brief counter-siege, Zangid governor Nūr al-Dīn took the city. The population was massacred and the walls razed. This victory was pivotal in the rise of Nūr al-Dīn and the decline of the Christian city of Edessa.

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The 1941 Sa'dah earthquake or the Jabal Razih earthquake occurred on January 11 in Razih District of the Mutawakkilite Kingdom of Yemen. The earthquake had a surface-wave magnitude of 5.8–6.5 and a shallow focal depth. Despite the moderate size of this earthquake, an estimated 1,200 people perished and at least 200 injured. With a maximum MSK-64 intensity assigned at VIII, it destroyed many villages and collapsed homes in the region of North Yemen.

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The Lordship of Marash was a territorial lordship in northeastern Cilicia between 1104 and 1149, centred on the city of Marash. One of the lesser Crusader states, it played a major role in the defence of the northern frontier in the 1130s and 1140s under Lords Geoffrey and Baldwin. Its position became untenable after the fall of Edessa in 1146.

References

  1. 1 2 Kesik, Muharrem (2012). "Maraş Depremi (1114)" [Marash earthquake (1114)]. Tarih Dergisi (in Turkish). No. 42. Istanbul University. pp. 43–46. ISSN   1015-1818 . Retrieved 20 October 2022.
  2. 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).
  3. Sesetyan, K.; Stucchi, M.; Castelli, V.; Capera, A.A. Gomez (16 February 2023). "Large historical earthquakes of the earthquake-affected region: a preliminary report" (PDF). Kandilli Observatory and Earthquake Research Institute.{{cite journal}}: Cite journal requires |journal= (help)
  4. 1 2 Ambraseys, N. N. (2004). "The 12th century seismic paroxysm in the Middle East: A historical perspective". Annals of Geophysics. 47 (2). doi: 10.4401/ag-3303 .
  5. Chronique de Matthieu d'Édesse, p. 287-90.
  6. 1 2 Beech, George (January 1996). "The Crusader Lordship of Marash in Armenian Cilicia, 1104-1149". Viator. 27: 35–52. doi:10.1484/J.VIATOR.2.301121.
  7. Spacey, Beth (15 February 2023). "Buildings tumbling, survivors living in tents: medieval descriptions of an 1114 CE earthquake in present-day Turkey and Syria feel eerily familiar". The Conversation. Retrieved 9 August 2023.

Sources