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Historical
Earthquakes in China
George Pararas Carayannis
(Excerpts from Unpublished Manuscript)
Introduction
Collision of India with the Asian mainland during the earliest Eocene (~50 Ma) has resulted in the growth of the world's largest orogenic belt, the Himalayas, and the associated Tibetan plateau. The seimotectonic tectonic evolution of China is characterized by the merger of several microcontinents throughout the entire Phanerozoic (Zhang et al., 1984; Hendrix and Davis, 2001). The collision and associated convergence and extension has created 64 major tectonic zones in China, which can be subdivided into a smaller number of tectonic "regions" (Zhang et al.,1984; Yin and Nie,1996).
Thus, China is located in one of the most active seismic regions
of the world that has been plagued by numerous
destructive earthquakes
during its long history. The most significant of the historical
earthquakes, in terms of lives lost, was that which occurred
in 1556. However, since 1900 China has experienced
several more destructive earthquakes. The most destructive
earthquakes of the 20th Century were those of
1927 in Tsinghai, of 1932 in Gansu, of 1933 in Sichuan,
of 1969 in Bohai Sea,
of 1970 in Tonghai (Yunnan), of 1974 in Zhaotong (Yunnan),
of 1975 in Haicheng, and of 1976 in Tangshan (Hebei Province)
. The
more recent earthquake of May
12,
2008 in Sichuan Province was
the latest
of the more destructive earthquakes that have struck
China in the new millennium. The following is a brief account
of the 1556 event and of some of the more destructive earthquakes
since 1900.

The Great China Earthquake of 1556
The worse natural disaster in recorded history - at least
in terms of lives lost - was caused by an earthquake
in Hausien, in the
Shaanxi Province of China in the morning
of 23 January 1556. In
Chinese historical record, this event is often referred as
the "Jiajing Great Earthquake" because it occurred
during the reign of Emperor Jiajing of the Ming dynasty.
The
"Shaanxi Earthquake" as it became later known,
had an estimated magnitude ranging from 8.0 to 8.3
on the
Richter scale (final assigned Moment Magnitude of 8), and
had an estimated intensity of XI on the Modified Mercalli
scale. Its epicenter was near
Mount Hua in Shaanxi, close to present
day Weinan city.
The earthquake was responsible for the devastation
of
98
counties
and eight
provinces in Central China, but particularly destructive
in the Province of Shaanxi. The
destruction extended over an area of 500 miles. In
some of the counties, the average death toll was estimated
to be about 60 percent of the population.
According to historical records, a total of 830,000 people
lost their lives, most from the collapse of
poorly
constructed houses and of Loess cave dwellings.
Destructive
Earthquakes in China in the 20th Century in relation to
the most recent earthquake of May 12, 2008 (modified graphic
of Western Australia Un.)
The Haicheng Earthquake of February 4, 1975
On February 4, 1975, Haicheng, a town with about 100,000
inhabitants in the Liaoning Province of northeast China,
was struck by
a 7.3 magnitude earthquake. As early as 1970, the State
Seismological Bureau, had identified the Liaoning Province
as an area of
high
earthquake risk. Six months before the earthquake,
there had been a series of smaller quakes in the region
- which intensified on February 3rd.
Based on studies of such precursor events and on unusual behavior exhibited by animals, a warning was issued by local authorities on February 3rd and in the early morning of February 4th.Thus, when the earthquake struck at 7:36 p.m. that evening of February 4, there were few lives lost as most inhabitants had evacuated to safer places. The death toll was relatively smaller than what could have been without the warning. Only 1,328 people lost their lives. However property damage was high.
The
Tangshan Earthquake of July 28, 1976
No other earthquake in this century has been as
catastrophic or has claimed as many lives as
the earthquake
that struck the city of Tangshan in Northern
China on July 28, 1976 (27 July 1976 local date). Tangshan,
a thriving industrial city with one million inhabitants,
is
located
in the Province
of Hebei, about
95
miles east
and slightly south
of Beijing and about 280 miles southwest
of Haicheng - where in the previous year another very destructive
earthquake had occurred. Although
the region had experienced moderate
seismic activity
in the past, there were no foreshocks this
time, and no warning.
China's Seismic Zones
Collision of India with the Asian mainland during the earliest Eocene (~50 Ma) has resulted in the growth of the world's largest orogenic belt, the Himalayas, and the associated Tibetan plateau. The seimotectonic tectonic evolution of China is characterized by the merger of several microcontinents throughout the entire Phanerozoic (e.g. Zhang et al., 1984; Hendrix and Davis, 2001).The collision and associated convergence and extension has created 64 major tectonic zones in China, which can be subdivided into a smaller number of tectonic "regions" (Zhang et al.,1984; Yin and Nie,1996.
The eartquake (with a magnitude reported in the literature as ranging from 7.5 to 8.0), struck at 3:42 a.m. in the early morning hours of July 28, the worst time when the city was asleep. What made matters worse, was the fact that this city is located in the center of an area with major crustal faults on four sides and most structures had been built on unstable, alluvial soils. Only a few of its structures were earthquake-resistant. The earthquake, with its epicenter right on Tangshan, broke a five-mile section of a 25-mile long fault that passes through the city. Along the west side of this fault the land moved five feet northward in relation to the land on the east side. The east block tipped downward at the northern end of the break and upward toward the south end.
Hotel
in Tangshan 
Complete Destruction of the City of Tangshan by the July 28, 1976 Earthquake (Photo source: China Earthquake Administration)
Ground motions lasted for about 90 seconds and, during this time interval, about 90 percent of the houses and buildings in Tangshan collapsed. Over a four-by-five mile area the devastation of the city was nearly total. The force of the ground motions were so strong that people reported being thrown in the air. Within seconds, thousands died. Property destruction was unbelievable. Bridges, railroads, homes, factories were completely leveled.
In the harbor city of Tientsin, 60 miles to the southwest, and in Beijing to the west, the strong ground motions forced thousands of frightened people into the streets seeking refuge from the aftershocks. The extent of the destruction and number of deaths in Tangshan and elsewhere in the region has been uncertain. According to official reports a total of 242,769 people died and 169,851 were severely injured. However, based on the density of population, it was fairly accurately estimated that there were at least 655,000 people dead and 780,000 injured. These figures make the 1976 Tangshan earthquake, the second worse earthquake in recorded history. The most destructive earthquake ever, as reported earlier, occurred in 1556.
Since 1976 the city of Tangshan has been growing and its population has increased by more than 50 percent. A number of new structures have been built, including high rise structures like the Phoenix Hotel with a height of 112 meters. Although most stuctures built since 1976 have been designed to be earthquake resistant and in accordance to revised seismic construction codes, it is still uncertain what damage could be inflicted on the city of Tangshan when another stong earthquake strikes again in the future.
REFERENCES AND ADDITIONAL READING
Hendrix, M.S., and Davis, G.A., 2001, Paleozoic and Mesozoic tectonic evolution of central Asia: from continental assembly to intracontinental deformation: Boulder, Colo., Geological Society of America, vi, 447 p.
Yin, A., and Nie, S., 1996, A Phanerozoic palinspastic reconstruction of China and its neighboring regions, in Yin, A., and Harrison, T. M., eds., The Tectonic evolution of Asia: Cambridge [England] ; New York, Cambridge University Press, p. 442-485.
Zhang, Z.M., Liou, J.G., and Coleman, R.G., 1984, An outline of the plate tectonics of China: Geological Society of America Bulletin, v. 95, p. 295-312.
SEE ALSO: EARTHQUAKE OF MAY 12, 2008 IN THE SICHUAN PROVINCE OF CHINA
THE TANGSHAN EARTHQUAKE OF JULY 28, 1976
THE EARTHQUAKE OF FEBRUARY 4, 1975 IN HAICHENG
EARTHQUAKE
PREDICTION IN CHINA
EARTHQUAKE OF SEPTEMBER 20, 1999 IN TAIWAN
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