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What Would Happen If the M 7.3 (1721) and M 7.4 (1780) Historical Earthquakes of Tabriz City (NW Iran) Occurred Again in 2021?

Journal

Publisher

MDPI
DOI: 10.3390/ijgi10100657

Keywords

earthquake; intensity; vulnerability; seismic hazard; GIS; Tabriz

Funding

  1. Japanese Society for the Promotion of Science (JSPS)
  2. KAKENHI [20H02411, 19H02408]
  3. Science and Technology Research Partnership for Sustainable Development (SATREPS)
  4. University of Tabriz, International and Academic Cooperation Directorate
  5. Grants-in-Aid for Scientific Research [20H02411] Funding Source: KAKEN

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This study used the scenario building method to investigate the potential damage and casualties if the major earthquakes of 1721 and 1780 were to occur in 2021. Results showed that the 1721 earthquake caused significant destruction in the north of Tabriz, while the 1780 earthquake resulted in less damage.
Tabriz is located in the northwest of Iran. Two huge earthquakes with magnitudes of 7.4 and 7.3 occurred there in 1780 and 1721. These earthquakes caused considerable damage and casualties in Tabriz. Using the method of scenario building, we aim to investigate what would happen if such earthquakes occurred in 2021. This scenario building was carried out using deterministic and GIS-oriented techniques to find the levels of damage and casualties that would occur. This procedure included two steps. In the first step, a database of factors affecting the destructive power of earthquakes was prepared. In the next step, hierarchical analysis was used to weigh the data, and then the weighted data were combined with an earthquake intensity map. The obtained results were used to predict the earthquake intensity in Tabriz. According to our results, the earthquake with a magnitude of 7.3 that occurred in 1721 caused huge destruction in the north of Tabriz, as this earthquake occurred inside the site. However, this earthquake caused minimal damage to the south of the city owing to the geological situation of this area of Tabriz. The earthquake with a magnitude of 7.3 that occurred in 1780 caused less damage because of its distance from the site. In the third step of this analysis, the vulnerability of buildings and the population were examined. According to the estimates, District 4 would experience the highest damage rate in the earthquake of 1721, with 15,477 buildings destroyed, while this area would have a lower damage rate in the earthquake that occurred in 1780. The total casualties in Tabriz would number 152,092 and 505 people in the earthquakes of 1721 and 1780, respectively.

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