1985 Wuqia earthquake explained

1985 Wuqia earthquake
Timestamp:1985-08-23 12:42:01
Isc-Event:518737
Anss-Url:iscgem518737
Local-Time:20:42:01
Magnitude: 7.4
Depth:6.8km (04.2miles)
Location:39.413°N 75.224°W
Countries Affected:China
Casualties:71 dead, 162 injured

The 1985 Wuqia earthquake occurred on August 23, 1985, at 20:42 local time (12:42 UTC) near the border of Wuqia County and Shufu County, Xinjiang, China. It had a magnitude of 7.4 and caused 71 deaths, 162 injuries, and left 15,000 homeless, as well as destroying 85% of buildings and highways. The source of this earthquake is the Kazkeaerte Fault (卡兹克阿尔特断裂). The earthquake could be felt throughout much of the Fergana Basin, USSR, as well as in Pakistan.[1]

The slipping of the earth during this earthquake caused a deformation zone along the Kezilesu River valley stretching 15frac=3NaNfrac=3 long and 800frac=2NaNfrac=2 wide. The zone is made up of smaller faults, fissures, and pressure ridges.[2]

Notes and References

  1. Wang, Xiaorong. "1985 Xinjiang Autonomous Region Wuqia Earthquake."National Earthquake Science. China Earthquakes Network Center, n.d. Web
  2. Deformation Zone of the Wuqia Earthquake in 1985. Feng. Xian-yue. 2008. Seismology and Geology.