Traditional Culture Encyclopedia - Weather inquiry - Did anyone die in the Xinjiang earthquake on June 30?
Did anyone die in the Xinjiang earthquake on June 30?
At 5: 07 on the 30th, an earthquake of magnitude 6.6 occurred at the junction of xinyuan county, Bayinguoleng Mongolian Autonomous Prefecture and Jingxian County in Yili Kazakh Autonomous Prefecture, with a focal depth of 7 kilometers.
As of 30th 13, an earthquake of magnitude 6.6 occurred at the junction of xinyuan county and Hejing County in Xinjiang, which has injured 30 people and caused some houses to crack or collapse.
At 5: 07 on June 30th, an earthquake of magnitude 6.6 occurred at the junction of xinyuan county and Jingxian in Bayinguoleng Mongolian Autonomous Prefecture, Ili Kazakh Autonomous Prefecture, Xinjiang Uygur Autonomous Region. Subsequently, several earthquakes of magnitude 3-4 occurred in the above areas respectively.
There are 1 1 villages and towns in the county affected to varying degrees, with a population of 22,000.
There was a strong earthquake in Urumqi, lasting about 10 second. The cable TV signal was blurred instantly, and the objects in the building shook violently. Some residents in the residential area were awakened and rushed to the emergency office of Lanzhou Military Region in the open space downstairs. At the meeting, it was revealed that as of June 30th 15, the Ili Army Division had mobilized more than 330 people from its emergency rescue teams and key militia in affected towns to participate in disaster relief, carried out resettlement, investigation and search for the affected people, and transferred more than 50 people15.
The epicenter of this earthquake is about 3500 meters above sea level, and historical earthquakes around the epicenter are relatively active. There have been two earthquakes of magnitude 6 and two earthquakes of magnitude 7 within the range of 100km since 1900, and the nearest earthquake of magnitude 7 is Manas earthquake of magnitude 7.7+0906. Since 1970, earthquakes with M ≥ 5 around the epicenter are mainly residual earthquakes and isolated earthquakes.
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