UTC time | 1937-07-31 20:35:51 |
---|---|
1937-08-01 10:41:09 | |
ISC event | 903183 |
903185 | |
USGS-ANSS | ComCat |
ComCat | |
Local date | August 1, 1937 |
Local time | 04:35:51 |
18:41:09 | |
Magnitude | 7.0 Mw , 6.7 Mw |
Depth | 25 km |
Epicenter | 37°04′N114°29′E / 37.067°N 114.483°E |
Areas affected | China |
Max. intensity | CSIS IX |
Casualties | 3,252 dead, 12,701 injured |
The 1937 Heze earthquakes struck the Mudan District in Shandong Province, China on July 31 and August 1 respectively. The moment magnitude 7.0 and 6.7 earthquakes were centered near the city of Heze. Although the total number of casualties has never been finalized, at least 3,252 people died and 12,701 were injured. The earthquakes also killed more than 6,000 livestock and destroyed 470,000 homes. Due to the outbreak of the Second Sino-Japanese War, rescue operations by the Chinese government were ineffective.
Seismic activity in the North China Plain occur as a result of interaction between three crustal blocks that form the North China Craton. The western part of the craton consists of a continental rift system and the tectonically stable Ordos Plateau. At the center of the block is another rift that forms the North China Plain, and to the east, the Bohai Sea. Several large fault systems bound the North China Craton, including the Tanlu Fault. These faults have generated magnitude 8.0+ earthquakes in the past centuries including the 1668 Shandong and 1679 Sanhe-Pinggu earthquakes. The North China Plain also hosted the 1975 Haicheng and 1976 Tangshan earthquakes. [1]
The two earthquakes have been often attributed to being triggered along the 230 km (140 mi) Liaokao Fault Zone. The average slip rate along the fault over the past 47 years is measured at 9.24 mm (0.364 in) per year, and it has a strike-slip sense of movement. [2] It is predominantly buried beneath the south-central part of the North China Plain. In the epicenter region, nearby faults lie beneath sediments deposited by the Yellow River. The northern Liaokao Fault Zone was active during the late Pleistocene and presently active along its southern segment. Based on analysing the isoseismal lines, surface ruptures and fault plane solutions, these shocks were likely produced on the Xiaoliu-Xieyuanji and Dongming-Chengwu faults; north-northeast west-northwest trending faults, respectively. [3]
Prior to the mainshocks, residents noted extremely unusual weather patterns in the area. Heavy rains and strong winds battered the region. The region also became unusually hot and humid, where several residents suffered heat injuries, and many livestock died. The temperature was so high that the walls of homes overheated and burned. The water level in wells also fluctuated many times. In some instances, the water rose and overflowed from these wells. Discoloration, bubbling, and foaming of well water were also observed. [4]
A mere two or three days before the earthquakes, animals displayed peculiar behaviors. Swallow flocks did not disperse but slept around the area. Cattle did not consume grass, and horses refused to enter their stables. Mice were observed fleeing the epicenter area, and dogs barked continuously. The residents also reported witnessing glowing red fireballs rising from the ground and into the air. Thunderous sounds were heard coming from the ground. [4]
In the meizoseismal area where the maximum seismic intensity was assigned IX (Violent), all buildings collapsed and severe liquefaction occurred. The area encompassed the towns of Xieyuanji and Muli Malinggang. From Hezhe; Malinggangzhen to the east; Wubagang and Dongming to the west; Tongguji in the south, and northward to Genghai. Intensity IX covered an area of 82 km2. The second mainshock had a maximum intensity of VIII (Severe). [5]
In all, more than 3,252 people died, 12,701 were injured and over 470,000 homes were destroyed. The earthquakes caused damage in 40 counties across the provinces of Shandong, Henan, Anhui, Jiangsu, and Hebei. [6] Its effects were also felt along the coast of the Bohai Sea, in Beijing, Zhenjiang, and Luoyang. At Xuzhou in Jiangsu, 50 homes collapsed, killing over 20 people. Homes also collapsed in Feixiang and Daming, Hebei Province. Several huts fell in Dangshan County, Anhui. [4]
An estimated 30 percent of all residential homes in Heze were destroyed. Some sections of the city walls and battlements were torn down. The well-known Guanyin Temple also collapsed. Water ejected from the ground through wells. In Dongming County, 20 percent of the county homes were lost. Six people died and ground fissures erupted water. Some fissures were up to one meter wide and were reported as far as 30 km from the epicenter. A farmer fell into one of the fissures and was washed away by rushing water. [5]
The 1976 Tangshan earthquake was a Mw 7.6 earthquake that hit the region around Tangshan, Hebei, China, at 3:42 a.m. on 28 July 1976. The maximum intensity of the earthquake was XI (Extreme) on the Mercalli scale. In minutes, 85 percent of the buildings in Tangshan collapsed or were rendered unusable, all services failed, and most of the highway and railway bridges collapsed or were seriously damaged. The official report claimed 242,769 deaths and 164,851 serious injuries in Tangshan, but when taken into account the missing, the injured who later died and the deaths in nearby Beijing and Tianjin, scholars accepted at least 300,000 died, making it one of the deadliest earthquakes in recorded history and worst disasters in China by death toll.
The 2002 Hindu Kush earthquakes struck in northern Afghanistan during the month of March. At least 166 people were killed with a very large and intermediate-depth mainshock on March 3. Three weeks later, at least 1,200 were killed during a moderate but shallow event that had a maximum Mercalli intensity of VII. The M7.4 and M6.1 reverse events were focused in the Hindu Kush mountain range area.
The 1948 Fukui earthquake occurred in Fukui Prefecture, Japan. The magnitude 6.8 quake struck at 4:13:31 p.m.(JDT) on June 28, 1948. The quake's hypocenter was approximately 10 km north-northeast of Fukui, in the present-day neighborhood of Maruoka, Sakai City. The strongest shaking occurred in the city of Fukui, where it was recorded as 6 on the Japan Meteorological Agency seismic intensity scale.
The 1918 Shantou earthquake occurred in Shantou, Guangdong, Republic of China. Serious damage and high casualty numbers were reported in Guangdong and the surrounding provinces. It also caused some damage in colonial Hong Kong.
The 2003 Zhaosu earthquake, also known as the Syumbinskoe earthquake, occurred on December 1 at 01:38 UTC. The epicenter was located in the Almaty Region, Kazakhstan, near the Sino–Kazakh border. The earthquake had a magnitude of Mw 6.0 and had a maximum observed intensity of VII on the Medvedev–Sponheuer–Karnik scale. The epicenter was close to the Zhaosu County, Xinjiang, where 10 people were reported dead, 73 people injured, and more than 800 buildings collapsed. Some people were evacuated in Zhaosu. The earthquake occurred in the cold winter, and the 30 cm ground snow covered the roads in the mountainous region and hindered the relief work.
The 1936 State Line earthquake struck at 23:08 Pacific time on July 15, 1936. The earthquake had an estimated magnitude of 5.8 and a maximum Mercalli intensity of VII. The epicenter was near the Oregon/Washington state line approximately 6 miles (9.7 km) northwest of Milton-Freewater, Oregon and southwest of Walla Walla, Washington and was felt throughout the Pacific Northwest, including as far away as Bonners Ferry, Idaho near the Canadian border and by seismographs as far away as San Diego, California.
The 1988 Lancang–Gengma earthquakes, also known as the 11.6 earthquakes by the Chinese media were a pair of devastating seismic events that struck Lancang and Gengma counties, Yunnan, near the border with Shan State, Burma. The earthquake measured moment magnitude (Mw ) 7.0 and was followed 13 minutes later by a 6.9 Mw shock. These earthquakes were assigned a maximum China seismic intensity of IX and X, respectively. Between 748 and 939 people were killed; more than 7,700 were injured. Both earthquakes resulted in US$270 million in damage and economic losses. Moderately large aftershocks continued to rock the region, causing additional casualties and damage.
A major earthquake occurred during the rule of the Qing dynasty in Shandong Province on July 25, 1668. It had an estimated magnitude of Ms 8.5, making it the largest historical earthquake in East China, and one of the largest to occur on land. An estimated 43,000 to 50,000 people were killed, and its effects were widely felt. Its epicenter may have been located between Ju and Tancheng counties, northeast of the prefecture-level city of Linyi in southern Shandong.
The 1902 Turkestan earthquake devastated Xinjiang, China, near the Kyrgyzstan border. It occurred on August 22, 1902, at 03:00:22 with an epicenter in the Tien Shan mountains. The thrust earthquake measured 7.7 on the moment magnitude scale (Mw ) and had a depth of 18 km (11 mi).
The 1994 Mascara earthquake occurred on August 18 at 02:13 local time with an epicenter in a rural part of Algeria. The earthquake measured 5.8 on the moment magnitude scale (Mw ) and had a depth of 10 km (6.2 mi). It caused the deaths of 171 people, left up to 12,500 homeless, and destroyed thousands of homes in Mascara Province. Many homes were damaged or destroyed due to poor building quality which collapsed on the inhabitants and resulted in a majority of the casualties. The national government launched a rapid response effort in its aftermath.
The 2021 Maduo earthquake, also known as the 5.22 earthquake struck Madoi County in Qinghai Province, China on 22 May at 02:04 local time. The earthquake had a moment magnitude and surface-wave magnitude of 7.4. Highway bridges, roads and walls collapsed as a result of the earthquake. According to an anonymous source, at least 20 people were killed, 300 were injured, and 13 were missing. Officials stated that there were no deaths but 19 people sustained minor injuries. It was the strongest in China since 2008. It was assigned a maximum intensity of X in Machali, Maduo County on the China seismic intensity scale and Modified Mercalli intensity scale. This earthquake was preceded by another unrelated earthquake that occurred 5 hours earlier in Yunnan.
The 1995 Menglian earthquake or 1995 Myanmar–China earthquake occurred on 12 July at 05:46:43 local time in the Myanmar–China border region. The earthquake had an epicenter on the Myanmar side of the border, located in the mountainous region of Shan State. It registered 7.3 on the Chinese surface wave magnitude scale (Ms ) and 6.8 on the moment magnitude scale (Mw ). With a maximum Mercalli intensity assigned at VIII, it killed 11 people and left another 136 injured. Over 100,000 homes in both countries were destroyed and 42,000 seriously damaged. Some damage to structures were also reported in Chiang Mai and Chiang Rai, Thailand. The low death toll from this earthquake was attributed to an early warning issued prior to it happening. Precursor events including foreshocks and some seismic anomalies led to an evacuation of the area before the mainshock struck. It is thought to be one of the few successfully predicted earthquakes in history.
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