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Contents

   



(Top)
 


1 Tectonic setting  





2 Earthquake  





3 Impact  





4 See also  





5 References  














1913 Eshan earthquake







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Coordinates: 24°1550N 102°4937E / 24.264°N 102.827°E / 24.264; 102.827
 

From Wikipedia, the free encyclopedia
 


1913 Eshan earthquake
1913 Eshan earthquake is located in Yunnan
1913 Eshan earthquake
UTC time1913-12-21 15:37:56
ISC event914108
USGS-ANSSComCat
Local date21 December 1913
MagnitudeMw 6.8
Depth15 km (9 mi)
Epicenter24°15′50N 102°49′37E / 24.264°N 102.827°E / 24.264; 102.827
TypeStrike-slip
Areas affectedYunnan, China
Max. intensityMMI IX (Violent)
Casualties942–1,900 fatalities

The 1913 Eshan earthquake struck China's Yunnan Province on 21 December with a moment magnitude of 6.8 and maximum Mercalli intensity of IX (Violent).[1] The shock devastated Eshan County; at least 942 people died and thousands of homes were destroyed. The earthquake ruptured along a section of the strike-slip Qujiang Fault.

Tectonic setting

[edit]

Major earthquakes in eastern Yunnan and the border with Sichuan are associated with the north–south striking Xiaojiang Fault; the west–northwest striking Zemuhe Fault to its north; and the northwest trending Qujiang–Shiping Fault. Some of these faults, including the Red River Fault, represent the boundaries of tectonic blocks within both provinces. The Qujiang–Shiping Fault comprises two fault segments (north and south) with a total length of 120 km (75 mi) that strikes northwest to west–northwest and eventually east–west at its southern part. Its slip mechanism comprises right-lateral strike-slip with a notable thrust component. The region is one of the most seismically active zone in Yunnan.[2]

Earthquake

[edit]

The Qujiang Fault runs northeast and parallel to the much longer Red River Fault, striking northwest–west-northwest. Three ≥M7.0 earthquakes, including the 1913 earthquake, occurred on this fault in 1599 and 1970. The 1970 earthquake measuring Ms  7.7 caused a 60 km (37 mi) surface rupture.[3] The northwestern Qujiang Fault ruptured during the 1913 earthquake while its southeastern portion was associated with the earthquake in 1970.[4]

Impact

[edit]

More than 18,000 homes were destroyed and the earthquake affected a 3,000 km2 (1,200 sq mi) area. When the earthquake struck, the region was experiencing heavy snowfall which caused many survivors to die from freezing and starvation. A plague further added to the suffering on top of the lack of food and clothes. Looting was also taking place.[5] In Eshan County, at least 942 people died while the death toll may be as high as 1,900. Another 112 people were also injured. Eighty to ninety percent of residential homes were demolished; all schools, temples and government buildings were also destroyed. Many bridges and city walls were also razed. On agricultural land, large cracks opened, erupting sand and water. Many people reportedly fall into these cracks. In Tonghai, several structures collapsed. Nine people died and 1,000 homes were destroyed in villages. One person died in Hexi; an 8 m (26 ft) section of parapet collapsed; many homes and government buildings also toppled. Sixteen people died in Yuxi; old houses in the county were also destroyed. In Xinping, the room of a government office collapsed and killed three.[6] Landslides affected a 2,839 km2 (1,096 sq mi) area.[7]

See also

[edit]

References

[edit]
  1. ^ ISC (27 June 2022), ISC-GEM Global Instrumental Earthquake Catalogue (1900–2009), Version 9.1, International Seismological Centre
  • ^ Wen, XueZe; Du, Fang; Long, Feng; Fan, Jun; Zhu, Hang (2011). "Tectonic dynamics and correlation of major earthquake sequences of the Xiaojiang and Qujiang-Shiping fault systems, Yunnan, China". Science China Earth Sciences. 54 (10): 1563–1575. Bibcode:2011ScChD..54.1563W. doi:10.1007/s11430-011-4231-0. S2CID 131667346.
  • ^ Guo, Peng; Han, Zhujun; Dong, Shaopeng; Mao, Zebin; Hu, Nan; Gao, Fan; Li, Jiani (2021). "Latest Quaternary Active Faulting and Paleoearthquakes on the Southern Segment of the Xiaojiang Fault Zone, SE Tibetan Plateau". Lithosphere. 2021 (1). Bibcode:2021Lsphe202166379G. doi:10.2113/2021/7866379.
  • ^ Yu, Houyun; Zhang, Wenqiang; Zhang, Zhenguo; Li, Zhengbo; Chen, Xiaofei (2020). "Investigation on the Dynamic Rupture of the 1970 Ms 7.7 Tonghai, Yunnan, China, Earthquake on the Qujiang Fault" (PDF). Bulletin of the Seismological Society of America. 110 (2): 898–919. Bibcode:2020BuSSA.110..898Y. doi:10.1785/0120190185. S2CID 213502598.
  • ^ Sichuan Provincial Seismological Bureau (21 December 2021). "民国时期云南死亡超千人的地震,诞生我国第一篇地震专题考察报告" [An earthquake in Yunnan that killed more than 1,000 people during the Republic of China produced my country's first special earthquake investigation report]. Sohu (in Chinese). Retrieved 23 December 2023.
  • ^ National Geophysical Data Center (1972). "National Geophysical Data Center / World Data Service (NGDC/WDS): NCEI/WDS Global Significant Earthquake Database. NOAA National Centers for Environmental Information". NOAA National Centers for Environmental Information. doi:10.7289/V5TD9V7K.
  • ^ Chen, X. L.; Zhou, Q.; Ran, H.; Dong, R. (2012). "Earthquake-triggered landslides in southwest China". Natural Hazards and Earth System Science. 12 (2): 351–363. Bibcode:2012NHESS..12..351C. doi:10.5194/nhess-12-351-2012.

  • Retrieved from "https://en.wikipedia.org/w/index.php?title=1913_Eshan_earthquake&oldid=1191700936"

    Categories: 
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    1913 earthquakes
    1913 in China
    Eshan Yi Autonomous County
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    This page was last edited on 25 December 2023, at 04:57 (UTC).

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