The United States Geological Survey recorded a Magnitude 5.5 Earthquake at a depth of 10 km, in Pingwu County in northern Sichaun Province, slightly before 2.15 pm local time (slightly before 6.15 am GMT) on Saturday 30 September 2017. The quake is reported to have caused minor damage to several buildings, and triggered a number of small landslides, causing disruption to transport networks, but no injuries. It would felt across much of the southern plain of Sichuan.
Small landslide in Qingchuan County, Sichuan, triggered by the 30 September 2017 Earthquake. 新闻中心_腾讯网.
Much of western China and neighbouring areas of Central Asia and the Himalayas, are prone to Earthquakes caused by the impact of the Indian Plate into Eurasia from the south. The Indian Plate is moving northwards at a rate of 5 cm per year, causing it to impact into Eurasia, which is also moving northward, but only at a rate of 2 cm per year. When two tectonic plates collide in this way and one or both are oceanic then one will be subducted beneath the other (if one of the plates is continental then the other will be subducted), but if both plates are continental then subduction will not fully occur, but instead the plates will crumple, leading to folding and uplift (and quite a lot of Earthquakes). The collision of the Indian and Eurasian plates has lead to the formation of the Himalayan Mountains, the Tibetan Plateau, and the mountains of southwest China, Central Asia and the Hindu Kush.
The movement of India into Eurasia over the last 71 million years. USGS.
Witness accounts of Earthquakes can help geologists to understand these events, and the structures that cause them. The international non-profit organisation Earthquake Report is interested in hearing from people who may have felt this event; if you felt this quake then you can report it to Earthquake Report here.
The approximate location of the 30 September 2017 Sichuan Earthquake. USGS.
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