1556 Shaanxi earthquake

Map of the Weihe–Shanxi Rift System along the southern and eastern margin of the Ordos Block

The 1556 Shaanxi earthquake (Postal romanization: Shensi), known in Chinese colloquially by its regnal year as the Jiajing Great Earthquake "{{#invoke:Lang|lang}}" (Jiājìng Dàdìzhèn) or officially by its epicenter as the Hua County Earthquake "{{#invoke:Lang|lang}}" (Huàxiàn Dìzhèn), occurred in the early morning of 2 February 1556 in Huaxian, Shaanxi, during the Ming dynasty.

Most of the residents there lived in yaodongs—artificial caves in loess cliffs—which collapsed and buried alive those sleeping inside. Modern estimates by China Earthquake Administration's publications put the direct deaths from the earthquake at roughly 100,000, while over 700,000 either migrated away or died from famine and plagues, which summed up to a total reduction of 830,000 people in Imperial hukou registration.<ref name="1998 law">Template:Cite book</ref><ref name="2008 Gao">Template:Cite journal</ref><ref name="2008 Q&A">Template:Cite book</ref><ref name="2005 Xie">颤抖的地球—地震科学 Template:Webarchive (2005). Researched by China Earthquake Administration seismologists 冯万鹏,薑文亮,龚丽霞,公茂盛,胡进军; Revised by CEA seismologists 王文清,续春荣,张宝红; Edited by CEA chiefs 谢礼立,张景发. Tsinghua University Press. Pages XIII, 162. "1556年陕西华县8级大地震，死亡的83万人中, 据估计死于瘟疫者不下七八成" [Among the 830,000 died, it is estimated that no less than 70% or 80% died from plagues]</ref> It is one of the deadliest earthquakes and one of the deadliest natural disasters in Chinese history.

Tectonic setting

Huaxian lies within the Weihe Basin, one of the rift basins that form the southern and eastern boundaries of the Ordos Block. To the east the basin is continuous with the Shanxi Rift System. The Weihe basin formed during the Paleogene in response to northwest–southeast directed extension. Following a tectonically quiet period during the late Paleogene the rift basins became active again in the Neogene in response to NNW–SSE directed extension, activity that continues to the present. The basins in the Weihe-Shanxi Rift System are bounded by large normal faults, which have been responsible for large historical earthquakes.<ref name="LI_etal_2015">Template:Cite journal</ref><ref>Template:Citation</ref> The Weihe Basin has an overall half-graben geometry, with the main controlling faults, such as the Huashan Fault and North Qinling Fault, forming the southern boundary.<ref name="Shi_etal_2019">Template:Cite journal</ref><ref name="Feng20">Template:Cite journal</ref>

Earthquake

The epicenter was in the Wei River Valley in Shaanxi Province, near Huaxian (now Huazhou District of Weinan), Weinan and Huayin. Huaxian was completely destroyed, killing more than half the residents of the city, with an estimated death toll in the hundreds of thousands. The situation in Weinan and Huayin was similar. In certain areas, Template:Convert crevices opened in the earth. Destruction and death were widespread, affecting places as far as Template:Convert from the epicenter. The earthquake also triggered landslides, which contributed to the massive death toll.<ref>History.com Template:Webarchive, History Channel's Record of the earthquake.</ref> The rupture occurred during the reign of the Jiajing Emperor of the Ming dynasty. Therefore, in the Chinese historical record, this earthquake is often referred to as the Jiajing Great Earthquake.<ref name="Bo2010">Template:Cite book</ref>

In the annals of China it was described in this manner:

In the winter of 1556, an earthquake catastrophe occurred in the Shaanxi and Shanxi Provinces. In our Hua County, various misfortunes took place. Mountains and rivers changed places and roads were destroyed. In some places, the ground suddenly rose up and formed new hills, or it sank abruptly and became new valleys. In other areas, a stream burst out in an instant, or the ground broke and new gullies appeared. Huts, official houses, temples and city walls collapsed all of a sudden.<ref>This quotation is from a translation of a Chinese study of historical earthquake. 賀明靜編著，(1990年)，《（1556年）華縣地震災害研究》，西安：陜西人民出版社，頁92。</ref>{{#if:|

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The earthquake damaged many of the Forest of Stone steles badly. Of the 114 Kaicheng Stone Classics, 40 were broken in the earthquake.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>

The scholar Qin Keda lived through the earthquake and recorded details. One conclusion he drew was that "at the very beginning of an earthquake, people indoors should not go out immediately. Just crouch down and wait. Even if the nest has collapsed, some eggs may remain intact."<ref>Kisti.re.kr Template:Webarchive, China virtual museums quake</ref> The shaking reduced the height of the Small Wild Goose Pagoda in Xi'an by three levels.<ref name="Pearson2017">Template:Cite book</ref>

Geology

Modern estimates, based on geological data, give the earthquake a magnitude of approximately 8 M_w on the moment magnitude scale and XI (catastrophic damage) on the Mercalli scale, though more recent discoveries have shown that it was more likely 7.9 M_w.<ref name="Int"/> Following the earthquake, aftershocks continued several times a month for half a year.<ref>Kepu.ac.cn Template:Webarchive, China virtual museums quake</ref>

Shaking was felt strongly across the Weihe Basin region. The maximum China seismic intensity was XI to XII occurring in Huaxian and Weinan. This would support the theory of the earthquake rupturing along the Huashan and Weinan faults. Intensity VIII was observed throughout the basin and the intensity X+ zone was Template:Cvt long.<ref name="Feng20" />

Studies about the earthquake published between 1998 and 2017 presumed scarps along the Huashan and Weinan faults, some higher than Template:Cvt, were produced by the 1556 earthquake. The fault zone is located northeast of Xi'an. This normal fault generally trends east–west and dips to the north. A 1995 study said scarps along the Huashan Fault were Template:Cvt high. Near the town of Huashan, the fault terrace contained Yangshao culture artefacts which were 4,000 years old. In a separate 1998 study, the fault scarps were about Template:Cvt high. Scarps of the Weinan Fault are less detailed in published works with most focused around the Chishui River area. Two studies in 1992 and 2010 estimated the fault scarps at Template:Cvt and Template:Cvt respectively. There has not been any research to confirm these scarps were produced by the earthquake or formed by multiple events. Assuming both faults ruptured during the earthquake, which runs for a total Template:Cvt, the Template:M would be 7.0–7.5, according to empirical scaling relationships between magnitude and fault rupture length. This suggest previous values for the earthquake's magnitude were overestimated.<ref name="Feng20" />

Affected area

More than 97 counties in the provinces of Shaanxi, Shanxi, Henan, Gansu, Hebei, Shandong, Hubei, Hunan, Jiangsu and Anhui were affected. Buildings were damaged slightly in the cities of Beijing, Chengdu and Shanghai.<ref>Science Museums of China Template:Webarchive Museum of Earthquakes, Ruins of Hua County Earthquake (1556)</ref> An Template:Convert area was destroyed,<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> and in some counties as much as 60% of the population was killed.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> The cost of damage done by the earthquake is almost impossible to measure in modern terms.

Death toll

Modern estimates by China Earthquake Administration's publications put the direct deaths from the earthquake to be roughly 100,000, while 730,000 either migrated away or died from famine and plagues, which summed up to a total reduction of 830,000 people in Imperial hukou registration.<ref name="2008 Gao"/><ref name="2008 Q&A"/><ref name="2005 Xie"/> However, the CEA did not explain how it estimated the number of direct deaths to be 100,000.

As the CEA did not estimate the total deaths (including subsequent famine and plagues), a handful of CEA staff scientists gave their own estimates, such as 450,000<ref name="CEA 2020">Template:Cite news</ref> or 530,000.<ref>Template:Cite journal</ref> Whatever the number may be, it is one of the deadliest earthquakes in China, in turn making it one of the top disasters in China by death toll.

Millions of people at the time lived in yaodongs—artificial loess caves—on high cliffs in the Loess Plateau. Much of the population in some of the affected areas lived in yaodongs. This was a major contributing factor to the very high death toll. The earthquake collapsed many caves and caused landslides which destroyed many more.<ref>Template:Cite book</ref><ref>Template:Cite book</ref>

Foreign reaction

The Portuguese Dominican friar Gaspar da Cruz, who visited Guangzhou later in 1556, heard about the earthquake, and later reported about it in the last chapter of his book A Treatise of China (1569). He viewed the earthquake as a possible punishment for people's sins, and the Great Comet of 1556 as, possibly, the sign of this calamity (as well as perhaps the sign of the birth of the Antichrist).<ref>Template:Citation (Translation of da Cruz's 1569 book, with C.R. Boxer's comments)</ref>

See also

• List of earthquakes in China
• List of disasters in China by death toll
• List of historical earthquakes

Further reading

• Template:Citation.

External links

• Ruins of Hua County Earthquake