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A landslide occurred at about 5:38 am local time on 24 June 2017 in Diexi Town,
Mao County Mao County or Maoxian (; ; Qiang: ʂqini) is a county in Ngawa Prefecture, Sichuan Province, China. It has an area of 3,903 and a population of 106,700 as of 2006. 88.9% of the population are Qiang people. The county seat is Fengyi (). Natu ...
,
Sichuan Province Sichuan (; zh, c=, labels=no, ; zh, p=Sìchuān; alternatively romanized as Szechuan or Szechwan; formerly also referred to as "West China" or "Western China" by Protestant missions) is a province in Southwest China occupying most of the ...
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. A second smaller landslide at around 17:19 pm impeded rescue efforts.


Background

The location of
Mao County Mao County or Maoxian (; ; Qiang: ʂqini) is a county in Ngawa Prefecture, Sichuan Province, China. It has an area of 3,903 and a population of 106,700 as of 2006. 88.9% of the population are Qiang people. The county seat is Fengyi (). Natu ...
between the
Tibetan Plateau The Tibetan Plateau (, also known as the Qinghai–Tibet Plateau or the Qing–Zang Plateau () or as the Himalayan Plateau in India, is a vast elevated plateau located at the intersection of Central, South and East Asia covering most of the ...
and the
Sichuan Basin The Sichuan Basin (), formerly transliterated as the Szechwan Basin, sometimes called the Red Basin, is a lowland region in southwestern China. It is surrounded by mountains on all sides and is drained by the upper Yangtze River and its tributar ...
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 The epicenter, epicentre () or epicentrum in seismology is the point on the Earth's surface directly above a hypocenter or focus, the point where an earthquake or an underground explosion originates. Surface damage Before the instrumental pe ...
was only a few kilometers away from Xinmo Village. Major geological hazards occur on almost a yearly basis.
Ngawa Tibetan and Qiang Autonomous Prefecture Ngawa Tibetan and Qiang Autonomous Prefecture, also known as Aba (; Qiang: ; ), 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 ar ...
, 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.In pictures: Landslide in Sichuan buries over 100 people
(in Chinese). QQ News.
A large factor in the fatality rate during both the 1933 and 2008 earthquakes was the landslides and the subsequent formation of
landslide dam A landslide dam or barrier lake is the natural damming of a river by some kind of landslide, such as a debris flow, rock avalanche or volcanic eruption. If the damming landslide is caused by an earthquake, it may also be called a quake lake. Some ...
lakes. During the 1933 earthquake, a catastrophic landslide lake
outburst flood In geomorphology, an outburst flood—a type of megaflood—is a high-magnitude, low-frequency catastrophic flood involving the sudden release of a large quantity of water. During the last deglaciation, numerous glacial lake outburst floods were ca ...
occurred on the Minjiang River, which has its headwaters in Aba Prefecture and runs through the region of the landslide. 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.


Landslide

The landslide occurred in the early morning on 24 June 2017 at about 5:38 am local time (21:38 on 23 June UTC). It was preceded by three weeks of frequent, but not intense rains. 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 stretch of the Songping Stream (松坪沟), as well as a 1,600 m section of road. Approximately 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. The landslide finally formed a deposit of more than . 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. It was estimated that the landslide hit the village at approximately 250 km/h. A second smaller landslide around 8:15 pm on 24 June affected the rescue work. At least 1,959 rescue and medical workers were involved in the recovery effort. 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. Subsequent engineering analyses confirmed the possibility of new landslides coming from the same ridge. 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. The landslide is thought to be a delayed effect of the rock weakening and cracking caused by the
1933 Diexi earthquake The 1933 Diexi earthquake occurred in Diexi, Mao County, Szechwan, Republic of China on August 25 with a moment magnitude of 7.3 and a maximum Mercalli intensity of X (''Extreme''). With up to 9,300 killed, this was the deadliest earthquake in 19 ...
, which accelerated the chemo-mechanical degradation of the rock. On the contrary, no apparent correlation with the 2008 Sichuan earthquake was found. After the event, several cracks were identified from satellite imagery and significant surface deformation was found to have preceded the landslide by several months. 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.


Aftermath and recovery efforts

Three people from the same family had been pulled alive from the rubble by the evening of 24 June. By 10 am on 25 June, 15 people had been confirmed killed, with a further 118 listed as missing. By 2 pm on the same day, the number of missing was reduced to 93, after more people were confirmed to be alive or were rescued. 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.


See also

*
2010 Gansu mudslide The 2010 Gansu mudslide was a deadly mudslide in Zhouqu County, Gansu Province, Gannan Tibetan Autonomous Prefecture, China that occurred at midnight on 8 August 2010. The floods were triggered after decades of clear cut logging practices h ...
*1933 Diexi earthquake * 2008 Sichuan earthquake


References


External links


Xinmo Village before being buried by the landslide
* {{DEFAULTSORT:Sichuan landslide Landslides in 2017 Landslides in China Environmental disasters in China History of Sichuan 2017 disasters in China June 2017 events in China