Estimates of the magnitude range from about 7.8 to 8.5 on the Richter scale; the larger number is used by today's Chinese sources. Login or create a profile so that
It is mandatory to procure user consent prior to running these cookies on your website.This website uses cookies to improve your experience while you navigate through the website. In K. B. Penuel & M. Statler (Eds. It struck on December 16, 1920, with an epicenter in Haiyuan County, in what is now Ningxia Province (which was then part of the province of Kansu), in China. Destruction of the maximum intensity (XII on the Mercalli scale) was felt in the Lijunbu-Haiyuan-Ganyanchi area. The destruction of homes and granaries beneath collapsed hills subjected the initial survivors both to hunger and to exposure to the windstorms and snowfall that immediately followed the quake. Please log in from an authenticated institution or log into your member profile to access the email feature. Weibo’s start came at a turbulent time as both Twitter and Fanfou were temporarily blocked in June 2009. We found other relevant content for you on other SAGE platforms.Sign up for a free trial and experience all SAGE Knowledge has to offer.You must have a valid academic email address to sign up.Sign up for a free trial and experience all SAGE Knowledge has to offer.You must have a valid academic email address to sign up.Javascript must be enabled for the correct page displayWatch videos from a variety of sources bringing classroom topics to life
In some districts, local gentry and merchant associations set up soup kitchens and contributed emergency aid, while in others magistrates issued tents and grain to the public from official granaries.Gansu relief announcements on the front page of the Beijing daily Zhongguo minbao, 28 February 1921Modest amounts of relief monies and materials were raised and dispatched to the region by provincial and county governments elsewhere in China, by fundraising groups formed by Gansu natives sojourning in Beijing, Shanghai and elsewhere in China and overseas, by charities in provinces such as Hunan and Jilin, and from the central government’s relief bureau in Beijing.The catastrophe that hit Gansu in late 1920 and early 1921 struck just as a drought famine affecting 20-30 million people on the North China plain was reaching a climax and absorbing the limited attention and relief capacities of the Chinese state and general public; the resources generated for the relief and reconstruction of Gansu in 1921 was undoubtedly a tiny fraction of the enormous losses inflicted on its people by the earthquake.County and provincial archives in northwest China are surprisingly lacking in materials on the Haiyuan earthquake of 1920. The 1920 Haiyuan earthquake, usually referred to as the Kansu earthquake by contemporary Western sources, was one of the greatest earthquakes on record, and the fifth deadliest. It was also called the 1920 Gansu earthquake because Ningxia was a part of Gansu Province when the earthquake occurred. Post-quake investigations unfortunately do not make it clear what portion of total fatalities may have been due to ground-shaking versus landslides, or to starvation or exposure in the quake’s aftermath, a subject that requires further research.Soldiers and officers operating out of the regional garrisons commanded by General Ma Fuxiang, in Ningxia, and General Lu Hongtao, in Pingliang, provided the first intelligence on the disaster, and also served as first responders, distributing tents and emergency provisions to communities in some of the most hard-hit areas. Haiyuan earthquake (1920). Much less known is its earthquake recurrence behavior. The earthquake that hit China’s remote Gansu Province in late 1920 was the world’s second deadliest of the twentieth century.
A magnitude 9.0 earthquake can last for five minutes or longer, and the amount of energy released is about 1,000 times greater than that of a 7.0. Vulnerable to bandit activity, many thousands roamed in a deformed landscape that was stripped of its roads, and devoid of standing structures and familiar natural landmarks.
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