1970 Tonghai earthquake
The 1970 Tonghai earthquake (Chinese: 1970年通海地震) occurred at 01:00:41 local time on January 5 with a moment magnitude of 7.1 and a maximum Mercalli intensity of X (Extreme). The strike-slip rupture originated on the Red River Fault, which had not experienced an earthquake above magnitude 7 since 1700, and affected Tonghai County, Yunnan province, China. At least 10,000 people were killed, making it one of the deadliest in its decade. The tremor caused between US$5 to $25 million in damage,[note 1] felt over an area of 8,781 km2 (3,390 sq mi). In Hanoi, North Vietnam, almost 483 km (300 mi) from the epicenter, victims left their homes as the rupture rumbled through the city.
|UTC time||1970-01-04 17:35:54|
|Local date||January 5, 1970|
|Depth||11 km (6.8 mi)|
|Areas affected||People's Republic of China|
|Total damage||Between USD 5 to 25 million|
|Max. intensity||X (Extreme)|
|Casualties||10,000–15,621 dead |
Occurring during the height of the Cultural Revolution, it was not widely publicized by the Chinese government for well over a decade. The amount of aid and finances distributed was described by the Beijing Morning Post as "pathetically small". Much of the aid provided to survivors was in "spiritual" form, including Mao Zedong badges and condolence letters. Nevertheless, the earthquake was among the first to be studied over a long term by the Chinese government. It was cited as one of the reasons behind creating the largest earthquake monitoring system in China, 25 years later.
Background and tectonicsEdit
Yunnan, the epicentral region, is one of the more seismically active Chinese provinces. The earliest earthquake recorded there was in the 9th century; however, moderate to strong ones have been observed since the 15th century. Since the 9th century, 32 earthquakes with a magnitude of 7 or greater have occurred in the province. Shallow strike-slip faulting is a characteristic of Yunnan quakes.
Earthquakes in southwestern Yunnan, such as the 1970 Tonghai event, are less frequent than in other parts of the province. The Red River Fault, the fault line on which this quake is alleged to have occurred, has lacked seismological activity as a whole. Red River temblors generally rise at high angles, as shown in a 1962 Ministry of Geology report. Marking in sedimentary rocks indicate that several large earthquakes formed on the fault during the Pleistocene and Holocene epochs. Until this quake, no earthquake above magnitude 7.0 on the Richter scale had occurred on this fault since about 1700, and the fault was believed to be "dead". Since the 1970 Tonghai rupture, it is believed that the Red River fault is instead experiencing a long seismic gap similar to that of the Japan Median Tectonic Line, on which no major temblor has formed since 700 but produced massive ones during the Holocene epoch.
Damage and casualtiesEdit
The epicenter of the quake was about 121 km (75 mi) southwest of Kunming and 97 km (60 mi) northwest of Gejiu; this area was mainly a tobacco-growing region. Effects of the rupture were felt over an area of 8,781 km2 (3,390 sq mi). In Hanoi, North Vietnam, almost 483 km (300 mi) from the epicenter, victims left their homes as the rupture rumbled through the city.
The earthquake measured 7.1 on the moment magnitude scale. It may have killed more than 15,000 people, making it the third deadliest in China during the 20th century, and injured an additional 26,783. The tremor caused between US$5 to $25 million in damage. A Reuters news report, the only one in the immediate aftermath, mentioned the recording of a "severe" quake by Hong Kong's Royal Observatory and cited an unconfirmed report that it might have destroyed part of Kunming. It caused 50 km (31 mi) of visible surface faulting on the Tonghai Fault. There was a maximum horizontal offset of 2.5 m (8 ft) and vertical offset of about 0.5 m (1.5 ft). As a result of inversion techniques, scientists were able to decide that several events comprised the surface faulting. This further confirmed that the earthquake, along with a later earthquake in Yunnan in 1973, corresponded to a fault within the area.
The earthquake was among the first to be studied over a long term by the Chinese government. More than 40 Chinese seismologists, engineers, and geologists visited the disaster zone to conduct research into the cause and damage of the earthquake; some spending as much as a year collecting soil samples and recording other primary research evidence for future study. Such data was collected over a broad area of almost 1,400 towns within the area.
According to the Reuters report, the survivors came together to "fight against the disaster". Much of the aid provided to survivors was in "spiritual" form. The Chinese government sent tens of thousands Quotations from Chairman Mao Zedong books and badges in his honor to victims as part of the relief effort, and survivors also received 14,350 sympathy letters. However, the amount of aid and finances distributed was described by the Beijing Morning Post 30 years later as "pathetically small."
The details of the earthquake were not widely publicized by Chinese authorities until about 18 years after its occurrence. In China's first decades of Communist rule, its policy was to not disclose natural disasters or accidents unless foreigners were injured. While the Chinese official press had not released a comprehensive report, Reuters and the Royal Hong Kong Observatory both released information soon after the disaster. At the time of the quake, the Xinhua News Agency briefly mentioned a smaller magnitude quake but did not provide information on damage or casualties.
On 19 November 1988, nearly nineteen years later, Chen Zhangli of the State Seismology Bureau, speaking at a news conference for another earthquake that had recently occurred, estimated the death toll of the 1970 quake to be 10,000. He did not give a reason why his government had not previously disclosed this knowledge. Government officials from China released a different estimate in 2000, putting the death toll at 15,621. China published the estimate after a memorial service for survivors and relatives was held in Yuxi on January 5. A Yuxi Seismology Bureau official noted that the information had been classified for "political reasons" and the death toll estimate had been known among bureaucrats as early as 1997.
Twenty-five years after the earthquake, the largest earthquake-monitoring network nationally was established in Yunnan. It set up earthquake offices in every county to prepare for another large rupture. The 1970 Tonghai earthquake was cited as one of the reasons behind creating the monitoring system.
- ISC (2015), ISC-GEM Global Instrumental Earthquake Catalogue (1900–2009), Version 2.0, International Seismological Centre
- Hui-Lan Zhou; Clarence R. Allen; Hiroo Kanamori (1983). "Rupture complexity of the 1970 Tonghai and 1973 Luhuo earthquakes, China, from P-wave inversion, and relationship to surface faulting". Bulletin of the Seismological Survey of America. 73 (6a): 1585–1597.
- USGS (September 4, 2009), PAGER-CAT Earthquake Catalog, Version 2008_06.1, United States Geological Survey
- Kurtenbach, Elaine (8 January 2000). "China finally talking about devastating earthquake of 1970". Philadelphia Inquirer. NewsBank. p. AO5. Retrieved 6 November 2008.
- Allen et al. (1984), p. 689.
- Chen & Scawthorn (2002), p. 442.
- Allen et al. (1984), p. 687.
- Allen et al. (1984), p. 686.
- "Today in Earthquake History: January 4". United States Geological Survey. United States Department of the Interior. 16 July 2008. Retrieved 16 November 2008.
- "China breaks silence on devastation from quake 30 years ago". Saint Louis Post-Dispatch. NewsBank. 8 January 2000. Retrieved 2008-11-06.
- Zchau & Küppers (2003), p. 482.
- "Magnitude 6.0 YUNNAN, CHINA". United States Geological Survey. United States Department of the Interior. 21 July 2003. Retrieved 9 November 2008.
- Kristof, Nicholas D. (19 November 1988). "Chinese Disclose That Quake In 1970 Killed About 10,000". The New York Times. The New York Times Company. Retrieved 8 November 2008.
- Hu et al. (1996), p. 107.
- Reuters (9 January 1970). "Severe Quake in Yunnan Is Confirmed by Peking" (PDF). The New York Times. The New York Times Company. p. 30. Retrieved 26 January 2009.
- "China's Largest Earthquake Monitoring System in Yunnan". Xinhua News Agency. HighBeam Research, Inc. 11 October 1995. Retrieved 8 November 2008.[dead link]
- Allen, C. R.; A. R. Gillespie; Han Yuan; Kerry E. Sieh; Zhang Buchun; Zhu Chengnan (June 1984). "Red River and associated faults, Yunnan Province, China; Quaternary geology, slip rates, and seismic hazard". Geological Society of America Bulletin. 95 (6): 686–700. Bibcode:1984GSAB...95..686A. doi:10.1130/0016-7606(1984)95<686:RRAAFY>2.0.CO;2.
- Chen, Wai-Fah; Charles Scawthorn (2002). Earthquake Engineering Handbook. CRC Press. ISBN 978-0-8493-0068-4.
- Hu, Yu-Xian; Shih Chi Liu; Weimin Dong (1996). Earthquake Engineering. Taylor & Francis. ISBN 978-0-419-20590-6.
- Zschau, Jochen; Andreas N. Küppers (2003). Early Warning Systems for Natural Disaster Reduction. Springer. ISBN 978-3-540-67962-2.