2017 Sichuan landslide

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2017 Sichuan landslide
China Sichuan rel location map.svg
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Xinmo Village
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Location of the landslide in Xinmo Village, about 170 km to the north of Chengdu
Native name 2017年茂县山体垮塌事件
English name2017 Sichuan landslide
Date24 June 2017 (2017-06-24) (23 June 2017 (2017-06-23))
Time5:38:55 CST (21:38 UTC 23 June) [1]
LocationXinmo Village, Diexi Town, Mao County, Ngawa Prefecture, Sichuan Province (四川省阿坝藏族羌族自治州茂县叠溪镇新磨村) [2]
Coordinates 32°03′59″N103°39′01″E / 32.0663°N 103.6504°E / 32.0663; 103.6504
Casualties
10 dead (as of 10:00 27 June 2017) [3]
73 missing (as of 10:00 27 June 2017) [3]
Deaths10 killed
Missing73 missing

A landslide occurred at about 05:38 local time on 24 June 2017 in Diexi Town, Mao County, Sichuan Province in south-western China. It destroyed 40 homes in Xinmo Village and killed 10 people, with a further 73 people missing, as of 27 June. [1] A second smaller landslide at around 17:19 impeded rescue efforts.

Contents

Background

The location of Mao County between the Tibetan Plateau and the Sichuan Basin is characterized by deep mountain canyons with exposed batholith. In 1933, the landslide site became especially unstable after the 7.3-magnitude Diexi earthquake, whose epicenter was only a few kilometers away from Xinmo Village. [1] Major geological hazards occur on almost a yearly basis. [4]

Ngawa Tibetan and Qiang Autonomous Prefecture, also known as Aba, where Mao County is located, was one of the regions worst affected by the 2008 Sichuan earthquake. During the earthquake, 20,258 people in Aba and 3,933 in Mao County were confirmed killed, and 8,183 people in Mao County were injured. [5] A large factor in the fatality rate during both the 1933 and 2008 earthquakes was the landslides and the subsequent formation of landslide dam lakes. [4] [6] During the 1933 earthquake, a catastrophic landslide lake outburst flood occurred on the Minjiang River, which has its headwaters in Aba Prefecture and runs through the region of the landslide. [6]

The majority of Mao County residents, almost 90%, are of the Qiang ethnicity. Large numbers of students had also returned home from university studies. The landslide site is located near the locally known Songpinggou scenic area, where many tourists were staying in guest houses when the landslide struck. [5]

Landslide

The debris of the Xinmo village landslide as seen on 15 May 2018 from the reconstructed road. A red flag stands in memory of the victims. The Xinmo landslide deposit as of 15 May 2018.jpg
The debris of the Xinmo village landslide as seen on 15 May 2018 from the reconstructed road. A red flag stands in memory of the victims.
Diexi Lake, 1.9 kilometers from the 2017 landslide site, was created by a landslide over the Minjiang River in the 1933 earthquake. Overlap brook lake.JPG
Diexi Lake, 1.9 kilometers from the 2017 landslide site, was created by a landslide over the Minjiang River in the 1933 earthquake.
Before and after satellite imagery of the affected area 2017 Sichuan landslide.gif
Before and after satellite imagery of the affected area

The landslide occurred in the early morning on 24 June 2017 at about 05:38 local time (21:38 on 23 June UTC). It was preceded by three weeks of frequent, but not intense rains. [1] Forty homes were destroyed in Xinmo Village (新磨村), where more than 140 people from at least 62 families were initially feared buried. The landslide also blocked a 1.2-kilometre (0.75 mi) stretch of the Songping Stream (松坪沟), [1] as well as a 1,600 m section of road. [7] Approximately 4.5 million m3 (160 million cu ft) [1] [8] of rock was displaced from the mountain crest. However, while avalanching downslope, the rock mass fragmented heavily and incorporated a large amount of pre-existing debris. [8] The landslide finally formed a deposit of more than 13 million m3 (460 million cu ft). [1] The mass covered a distance of more than 2,600 m with a height relief of almost 1,200 m in less than 60 seconds. [1] It was estimated that the landslide hit the village at approximately 250 km/h. [1]

A second smaller landslide at around 20:15 on 24 June affected the rescue work. At least 1,959 rescue and medical workers were involved in the recovery effort. [9] Fears of new landslides from the adjacent areas temporarily halted the work, which was resumed after the installation of a monitoring system capable of providing a timely alarm. [1] Subsequent engineering analyses confirmed the possibility of new landslides coming from the same ridge. [10] They could run on the 2017 landslide deposit but also toward still-inhabited buildings located just upstream, and could potentially block the flow of the Songping Stream again. [10]

The landslide is thought to be a delayed effect of the rock weakening and cracking caused by the 1933 Diexi earthquake, which accelerated the chemo-mechanical degradation of the rock. [1] On the contrary, no apparent correlation with the 2008 Sichuan earthquake was found. [1]

After the event, several cracks were identified from satellite imagery and significant surface deformation was found to have preceded the landslide by several months. [1] [11] [12] However, these precursory signals went unnoticed as no systematic remote sensing of the area was being carried out, and the cracks were not visible from the town or from the valley. [11]

Aftermath and recovery efforts

Three people from the same family had been pulled alive from the rubble by the evening of 24 June. [13] By 10:00 on 25 June, 15 people had been confirmed killed, with a further 118 listed as missing. [14] By 14:00 on the same day, the number of missing was reduced to 93, after more people were confirmed to be alive or were rescued. [7]

At least 300 people who survived the landslide were relocated to facilities in Diexi town, including a school and a hotel. The prefecture's civil affairs bureau sent clothing, two electric generators, 20 tents and 400 quilts to the survivors. [7] [15] [16]

See also

Related Research Articles

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Landslides, also known as landslips, or rockslides, are several forms of mass wasting that may include a wide range of ground movements, such as rockfalls, mudflows, shallow or deep-seated slope failures and debris flows. Landslides occur in a variety of environments, characterized by either steep or gentle slope gradients, from mountain ranges to coastal cliffs or even underwater, in which case they are called submarine landslides.

<span class="mw-page-title-main">Ngawa Tibetan and Qiang Autonomous Prefecture</span> Autonomous prefecture in Sichuan, China

Ngawa Tibetan and Qiang Autonomous Prefecture, also known as Aba, is an autonomous prefecture of northwestern Sichuan, bordering Gansu to the north and northeast and Qinghai to the northwest. Its seat is in Barkam, and it has an area of 83,201 km2 (32,124 sq mi). The population was 895,200 by 2022.

Qiang language, called Rma (尔玛) or Rme by its speakers, is a Sino-Tibetan language cluster of the Qiangic branch spoken by approximately 140,000 people in north-central Sichuan Province, China.

<span class="mw-page-title-main">Sturzstrom</span> Type of landslide

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<span class="mw-page-title-main">Wenchuan County</span> County in Sichuan, China

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<span class="mw-page-title-main">Mao County</span> County in Ngawa Prefecture, Sichuan Province, China

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<span class="mw-page-title-main">Diexi, Mao County</span> Town in Mao County, Ngawa Prefecture, Sichuan Province, China

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<span class="mw-page-title-main">Diexi Lake</span> Landslide dam-created lake in Mao County, Sichuan

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References

  1. 1 2 3 4 5 6 7 8 9 10 11 12 13 Fan, Xuanmei; Xu, Qiang; Scaringi, Gianvito; Dai, Lanxin; Li, Weile; Xiujun, Dong; Zhu, Xing; Pei, Xiangjun; Dai, Keren (10 October 2017). "Failure mechanism and kinematics of the deadly June 24th 2017 Xinmo landslide, Maoxian, Sichuan, China". Landslides. 14 (6): 2129–2146. doi:10.1007/s10346-017-0907-7. S2CID   133681894.
  2. ↑ "牵挂·守望·搜救——四川茂县山体垮塌灾害３６小时救援纪实". Xinhua News Agency. 26 June 2017.
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  5. 1 2 In pictures: Landslide in Sichuan buries over 100 people. (in Chinese). QQ News.
  6. 1 2 Cheng, Genwei; Wang, Xiaodan; He, Xiubin; Fan, Jihui; Fan, Jianrong (September 2008). "Outburst risk of barrier lakes in Sichuan, China". Journal of Mountain Science. 5 (3): 189–193. doi:10.1007/s11629-008-0208-7. S2CID   129231570.
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  9. ↑ "China landslide: more than 100 feared buried as village destroyed". The Sunday Morning Herald. 24 June 2017. Retrieved 24 June 2017.
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  12. ↑ Intrieri, Emanuele; Raspini, Federico; Fumagalli, Alfio; Lu, Ping; Sara, I; Conte, Del; Farina, Paolo; Allievi, Jacopo; Ferretti, Alessandro (9 November 2017). "The Maoxian landslide as seen from space: detecting precursors of failure with Sentinel-1 data". Landslides. 15: 123–133. doi: 10.1007/s10346-017-0915-7 . hdl: 2158/1102061 .
  13. ↑ "China landslide: at least 10 dead and more than 100 feared buried". The Guardian. Reuters. 24 June 2017. Retrieved 25 June 2017.
  14. ↑ "临近救援黄金72小时 四川茂县山体垮塌118人失踪". 南洋视界. 25 June 2017.
  15. ↑ "Hopes fade in grim search for Xinmo landslide survivors". AlJazeera. 26 June 2017. Retrieved 26 June 2017. Rescue workers in southwestern China have recovered several bodies as hopes fade in the search for 93 other people missing...
  16. ↑ Sue-Lin Wong (26 June 2017). "Villagers begin to mourn dead after deadly China landslide". Xinmo, China: Reuters . Retrieved 26 June 2017. Villagers...mourn loved ones lost..with little hope of finding anyone alive after more than 48 hours of fruitless searching... at least 93 people are missing after the landslide...
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