UTC time | 2011-03-24 13:55:13 |
---|---|
ISC event | 16357310 |
USGS-ANSS | ComCat |
Local date | 24 March 2011 |
Local time | 20:25:13 (UTC+06:30) |
Magnitude | 6.8 Mw |
Depth | 10 km (6.21 mi) |
Epicenter | 20°39′54″N99°53′06″E / 20.665°N 99.885°E |
Max. intensity | VIII (Severe) |
Casualties | 75–151 killed, 212 injured |
The 2011 Tarlay earthquake occurred on 24 March in Shan State, Myanmar. The earthquake measured Mw 6.8 and had an epicenter northwest of the border between Myanmar, Thailand and Laos. It occurred in a region accommodating tectonic deformation brought by the collision between the Indo-Australian and Eurasian plates. Strike-slip faulting along the Nan Ma Fault was identified as the cause. There were between 75 and 151 fatalities; including one death in Thailand. An additional 212 people were injured. Hundreds of buildings and some transport infrastructure were damaged in Myanmar and Thailand. [1] In the aftermath of the disaster, the Burmese government provided aid and relief supplies to the affected region. Neighbouring countries China, India and Thailand provided monetary assistance. Several international humanitarian organizations also supported in the relief and recovery.
Myanmar lies at the junction of the Alpine–Himalayan Orogenic Belt and Indonesian Island Arc System. In northern Myanmar, continental collision is ongoing between the between the northward moving Indian Plate and the Eurasian Plate. Collision also occurs along the Indo-Burman Ranges (Patkai, Naga and Chin Hills) and Arakan Mountains of western Myanmar. [2] In this zone of highly oblique collision, most of the motion is accommodated by the north-south trending Sagaing Fault, a major right-lateral strike-slip fault that runs through the western and central part of Myanmar. Additional deformation is distributed and accommodated within eastern Myanmar and Thailand extending into Laos. Deformation within the Shan Plateau is partly accommodated by a set of southwest-northeast trending left-lateral strike-slip faults. Major faults in the Shan Plateau include the Mae Chan, Nam Ma, Menxing, Menglian, Nantinghe, Wanding, and Longling faults. [3] The faults closest to the epicenter are the Mae Chan and Nam Ma faults, about 400 km (250 mi) east of the Sagaing Fault. [4] [5]
The Mw 6.8 earthquake occurred with a focal depth of 10 km (6.2 mi) and epicenter north-northwest of Tachilek, Shan State; north of the Golden Triangle region. [6] It was one of the largest earthquake recorded in the area. A focal mechanism solution obtained for the earthquake indicated left-lateral slip along a vertical fault plane. Large earthquakes also struck the area in 1988 (Mw 7.0) and 1995 (Mw 6.8). [7]
The northeast-southwest trending Nan Ma Fault runs through Myanmar, northern Laos and China for a length of 215 km (134 mi). Geomorphic studies along the central section of the fault where the Mekong River crosses it suggest it was previously a right-lateral fault. It produced up to 30 km (19 mi) of right-lateral displacement between 5 and 20 million years ago. [8] The fault reactivated as a left-lateral fault and its average slip rate is estimated at 0.6–2.4 mm (0.024–0.094 in) per year. The fault branches from a single structure into multiple subparallel splay segments at its westernmost end. The earthquake ruptured one of these segments at the westernmost Nan Ma Fault. [7]
The mainshock produced a 30 km (19 mi) long surface rupture along the westernmost segment of the Nam Ma Fault. The surface offset peaked at almost 2 m (6 ft 7 in). Based on inferring InSAR data, the coseismic slip along the fault rupture was concentrated within the shallow 10 km (6.2 mi) of the crust. The maximum slip was estimated at 4 m (13 ft) at depths of 3–5 km (1.9–3.1 mi). [7] Clear surface faulting was observed on farmland; at the paddy fields 16 km (9.9 mi) southeast of the epicenter, 2 km (1.2 mi) of surface rupture was mapped. The measured offset ranged between 0.12 m (4.7 in) and 1.25 m (4 ft 1 in) with an average of 0.81 m (2 ft 8 in). In Tarlay, offsets were in the order of several tens of centimetres. [8]
The earthquake was associated with 24 seconds of significant ground motion. Resonance may have occurred in the frequency range of 1.82–2.1, affecting many low to medium-rise buildings. The horizontal ground motion was the primary cause of building destroyed during the earthquake. [9] The highest peak ground acceleration, 0.20 g, was instrumentally measured 28 km (17 mi) south of the epicenter in Mae Sai, Thailand. This measurement was the highest ever recorded in Thailand from an earthquake. [10]
The death toll in Myanmar stood at 74 to 150; [11] [12] 212 people were injured; [13] 3,152 made homeless; and 18,000 were affected. [14] At least 413 buildings were damaged and one bridge collapsed in Shan State. [1] Around 90 villages were moderately or heavily damaged; in 50 of those villages, more than half the building stock were damaged or destroyed. In 40 other villages, damage was more than 30 percent of all buildings. [14] Damage in Tarlay corresponded to a Modified Mercalli intensity (MMI) of VIII (Severe). At least 40 people died and 50 others were injured in Tarlay; one hospital collapsed in the town. [15] Ground subsidence of 1.5 m (4 ft 11 in) was observed at a bridge between Kengtung and Tachileik. In Tachileik, two people died and six were injured. [16] Twenty-five people died and 57 were injured when a baptist church collapsed during a service in Kyakuni village. [17] In Monglin, at least 128 homes were razed. [18] Fourteen Buddhist monasteries and nine government infrastructure were damaged. [19]
In Mae Sai, Thailand, one person died when a wall collapsed. Sixteen people, including seven Burmese and five Chinese nationals were also injured. [20] Buildings in the district cracked and the spire of an 11th-century stupa toppled. No structural collapses occurred but ground effects such as liquefaction and lateral spreading were observed. The MMI in Mae Sai corresponded to VI (Strong). [10] Shaking also caused panic in Chiang Rai and Bangkok. [21] In Hanoi, Vietnam, windows shattered and some people evacuated from their homes. [22] Strong shaking was felt in the provinces of Luang Namtha and Bokeo in Laos without casualties or damage. In Xishuangbanna Prefecture, Yunnan, some homes and schools cracked. [23] Tall buildings were temporarily evacuated in Chiang Rai, Menghai County, Nanning and Hanoi. [24] [25]
On 28 March, The Irrawaddy reported many injured survivors at the Tachilek Hospital had "disappeared". The hospital was overwhelmed by an estimated 700 patients a day before the alleged disappearances. Remaining patients and hospital workers said the survivors were "sent away" by local authorities after journalists reported and distributed media on damage and casualties. Locals also reported up to 200 may have died in Shan State. [26]
Most residents in Tachileik spent the night outdoors after being advised by government officials about aftershocks through loudspeakers. Many people in the town did not return to their homes and businesses were closed. Authorities were hampered by road closures in their effort to locate some injured people in the affected areas. The United Nations Office for the Coordination of Humanitarian Affairs received reports of intermittent disruption of services including power, water and telecommunications. A damaged bridge at Tarlay made access to the town challenging for aid and rescue. [20]
More than US$ 3 million had been donated by various countries and organizations for the relief effort. [27] The government of Myanmar provided Ks 1,162 million worth of supplies to the area. [28] On 25 March, the Ministry of Social Welfare, Relief and Resettlement supplied relief tents, tarpaulins, blankets, clothing and food items via a military plane. [29] Two days later, government officials visited Tachilek and Tarlay, meeting affected residents. Affected families were also handled cash assistance, clothing and food. Patients at the Tachilek Station Hospital were also given cash. Government officials also surveyed repair works at the Kengtung–Tachilek Union Highway, Tachilek–Tahlay Road and Tahlay Bridge. By the afternoon of 27 March, buses and small vehicles could drive along the roads and bridge. [30]
The Chinese government provided US$500 thousand in disaster relief and reconstruction of damaged infrastructure. [31] On 26 March, the Thai government donated ฿3 million to the Burmese government and announced further assistance would be provided. [32] India's prime minister Manmohan Singh said his government would provide US$ 1 million for "relief and rehabilitation" in the affected area. [33] Korea also donated US$ 200 thousand to the Myanmar Red Cross Society. [34] Malteser International provided €10 thousand in emergency relief; at its Yangon warehouse, shelters and non-food items were prepared for 300 families. [35] World Vision distributed water and food to over 1,300 residents. [36]
The 1990 Luzon earthquake struck the island of Luzon in the Philippines at 4:26 p.m. on July 16 (PDT) or 3:26 p.m. (PST) with an estimated moment magnitude of 7.7 and a maximum Mercalli intensity of IX (Violent) and produced a 125 km-long ground rupture that stretched from Dingalan, Aurora to Kayapa, Nueva Vizcaya. The event was a result of strike-slip movements along the Philippine Fault and the Digdig Fault within the Philippine Fault System. The earthquake's epicenter was near the town of Rizal, Nueva Ecija, northeast of Cabanatuan. An estimated 1,621 people were killed, most of the fatalities located in Central Luzon and the Cordillera region.
On 17 August 1999, a catastrophic magnitude 7.6 earthquake struck the Kocaeli Province of Turkey, causing monumental damage and between 17,127 and 18,373 deaths. Named for the quake's proximity to the northwestern city of İzmit, the earthquake is also commonly referred to as the 17 August Earthquake or the 1999 Gölcük Earthquake. The earthquake occurred at 03:01 local time at a shallow depth of 15 km. A maximum Mercalli intensity of X (Extreme) was observed. The earthquake lasted for 37 seconds, causing seismic damage and is widely remembered as one of the deadliest natural disasters in modern Turkish history.
The 2002 Bou'in-Zahra earthquake occurred on 22 June 2002. The epicenter was near the city of Bou'in-Zahra in Qazvin Province, a region of northwestern Iran which is crossed by several major faults that is known for destructive earthquakes. The shock measured 6.5 on the Mwc scale, had a maximum Mercalli intensity of VIII (Severe), and was followed by more than 20 aftershocks. At least 230 people were killed and 1,500 more were injured.
The Sagaing Fault is a major fault in Myanmar, a mainly continental right-lateral transform fault between the Indian Plate and Sunda Plate. It links the divergent boundary in the Andaman Sea with the zone of active continental collision along the Himalayan front. It passes through populated cities of Mandalay, Yamethin, Pyinmana, the capital Naypyidaw, Toungoo and Pegu before dropping off into the Gulf of Martaban, running for a total length of over 1200 kilometers.
The 2012 Indian Ocean earthquakes were magnitude 8.6 and 8.2 Mw undersea earthquakes that struck near the Indonesian province of Aceh on 11 April at 15:38 local time. Initially, authorities feared that the initial earthquake would cause a tsunami and warnings were issued across the Indian Ocean; however, these warnings were subsequently cancelled. These were unusually strong intraplate earthquakes and the largest strike-slip earthquake ever recorded.
The 2012 Shwebo earthquake occurred at 07:42 local time on 11 November in Myanmar. It had a magnitude of 6.8 on the moment magnitude scale and a maximum perceived intensity of VIII (Severe) on the Mercalli intensity scale. The epicenter was near the town of Male, 52 km NNE of the city of Shwebo, 64 km west of Mogok and 120 km north of Mandalay. Significant damage and possible casualties have been reported from near the epicenter, with up to 26 people dead and many more injured. Part of a bridge under construction fell into the Irrawaddy River near Shwebo and a gold mine collapsed at Sintku. An aftershock with a magnitude of 5.8 followed at 17:24 local time.
The 1930 Bago (Pegu) earthquake, also known as the Swa earthquake struck Myanmar on 5 May. The moment magnitude (Mw ) 7.4 earthquake had a focal depth of 35 km (22 mi) and maximum Rossi–Forel intensity of IX. The earthquake was the result of rupture along a 131 km (81 mi) segment of the Sagaing Fault—a major strike-slip fault that runs through the country. Extensive damage was reported in the southern part of the country, particularly in Bago and Yangon, where buildings collapsed and fires erupted. At least 550, and possibly up to 7,000 people were killed. A moderate tsunami was generated along the Burmese coast which caused minor damage to ships and a port. It was felt for over 570,000 km2 (220,000 sq mi) and as far as Shan State and Thailand. The mainshock was followed by many aftershocks; several were damaging; additional earthquakes occurred in July and December, killing dozens. The December earthquake was similarly sized which also occurred along the Sagaing Fault.
The Haiyuan Fault is a major active intracontinental strike-slip (sinistral) fault in Central Asia.
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.
The 2021 Assam earthquake struck 11 km away from Dhekiajuli, Assam, India at 07:51 (IST) on April 28, 2021 with a moment magnitude of 6.0 at 34.0 km (21.1 mi) depth. The quake struck with an epicenter 140 km north of the main city of Guwahati. It resulted in two fatalities and at least 12 injuries.
The 2020 Kashgar earthquake, also known as the Jiashi earthquake occurred on 19 January 2020 at 21:27:56 China Standard Time in Xinjiang Province, China. According to the United States Geological Survey, the earthquake had a moment magnitude of 6.0 and a surface wave magnitude of 6.4 according to the China Earthquake Network Center. It struck at a shallow depth of 5.6 km according to the USGS while the CENC has the figure at 16 km. Local emergency management agencies said the earthquake damaged more than 1,000 homes and businesses in the nearby populated towns and villages. One person is known to have died while two other children were injured.
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, the quake killed eleven 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.
The 1979 Ghaenat earthquakes were a series of large earthquakes in Qaen County, Khorasan Province, northeast Iran, near the Afghanistan border. The first mainshock, known as the Korizan earthquake with a surface wave magnitude (Ms ) of 6.6 and moment magnitude (Mw ) of 6.8, struck on November 14, while the Ms 7.1 or Mw 7.2 Koli-Boniabad earthquake struck on November 27. The two mainshocks were assigned a maximum Modified Mercalli intensity of VIII (Severe) and X (Extreme), respectively. The earthquakes caused extensive damage throughout northeastern Iran, killing an estimated 297 to 440 people and left at least 279 injured.
The 1889 Chilik earthquake occurred on July 11 on the Gregorian calendar, or June 30 on the Julian calendar at 15:14 local time in the Tien Shan mountains. The earthquake measured an estimated Mw 7.9–8.0 on the moment magnitude scale and was assigned a maximum intensity of X (Devastating) on the MSK 64 and Rossi-Forel scales. Over 92 people across Kazakhstan, Kyrgyzstan and China were killed.
An earthquake occurred 112 km, offshore, north of Maumere in the Flores Sea on December 14. The quake had a moment magnitude of 7.3 according to the United States Geological Survey (USGS). One person was killed and 173 others suffered injuries.
The 1915 Imperial Valley earthquakes were two destructive shocks centered near El Centro, California on June 22. The earthquakes measured Ms 6.25 and occurred nearly one hour apart at 19:59 and 20:57 PST. Both shocks were assigned VIII (Severe) on the Modified Mercalli intensity scale. Heavy damage occurred in the areas of Mexicali and El Centro, amounting to $900,000. At least six people were killed in the earthquakes.
The 1997 Bojnurd earthquake occurred on 4 February at 14:07 IRST in Iran. The epicenter of the Mw 6.5 earthquake was in the Kopet Dag mountains of North Khorasan, near the Iran–Turkmenistan border, about 579 km (360 mi) northeast of Tehran. The earthquake is characterized by shallow strike-slip faulting in a zone of active faults. Seismic activity is present as the Kopet Dag is actively accommodating tectonics through faulting. The earthquake left 88 dead, 1,948 injured, and affected 173 villages, including four which were destroyed. Damage also occurred in Shirvan and Bojnord counties. The total cost of damage was estimated to be over US$ 30 million.
The 1986 Malatya earthquake was a Mw 6.1 earthquake that occurred in the early morning hours of May 5, 1986. It registered a maximum Modified Mercalli Intensity of VIII (Severe). It occurred near the city of Malatya, Turkey.
The 1983 Kaoiki earthquake struck southern Hawaii Island on the morning of November 16, 1983. Measuring Mw 6.7, it was the largest to hit the island since 1975. The epicenter was located 50 km southeast of Hilo with an approximated depth of 12 km. The shallow strike-slip earthquake was assigned a maximum intensity of IX (Violent) on the Modified Mercalli scale. 6 people were injured, widespread damage and landslides were reported across the island.
The 1980 Livermore earthquake occurred on January 24 at 11:00 PST in California. The epicenter of the 5.8 Mw earthquake was a hilly area 12 km (7.5 mi) southeast of Mount Diablo and north of Livermore Valley. The earthquake had a maximum Modified Mercalli intensity of VII. Forty four people were injured and damage across the San Francisco Bay Area totaled $11.5 million, with the majority inflicted at the Lawrence Livermore National Laboratory.
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