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1960 Valdivia earthquake

The 1960 Valdivia earthquake and tsunami or the Great Chilean earthquake occurred on 22 May 1960. Most studies have placed it at 9.4–9.6 on the moment magnitude scale, making it the strongest earthquake ever recorded, while some studies have placed the magnitude lower than 9.4. It occurred in the afternoon, and lasted 10 minutes. The resulting tsunamis affected southern Chile, Hawaii, Japan, the Philippines, eastern New Zealand, southeast Australia, and the Aleutian Islands.

Geological context
Chile is located along the Pacific Ring of Fire, a known zone of high seismicity. The earthquake was a megathrust earthquake resulting from the release of mechanical stress between the subducting Nazca plate and South American plate on the Peru–Chile Trench, off the coast of southern Chile. Because of its geography, Chile remains one of the most seismically active countries in the world. Tectonic interpretation The focus of the earthquake was relatively shallow at , considering that earthquakes in northern Chile and Argentina may reach depths of . A 2019 research paper postulates that the Liquiñe-Ofqui fault had a 9.07 strike-slip sub-event along with the 9.37 main thrust sub-event which could help account for how the plate boundary event seemingly "overspent" its tectonic budget. In other words, the previous and current more widely accepted explanation for the earthquake involves the Peru-Chile Trench slipping further than its accumulated slip deficit (the amount of slip available for an earthquake) should allow. The alternative explanation, with two faults slipping nearly simultaneously, could help explain the true mechanism of the earthquake. Subduction zones are known to produce the strongest earthquakes on Earth, as their particular structure allows more stress to build up before energy is released. Geophysicists consider it a matter of time before this earthquake will be surpassed in magnitude by another. The earthquake's rupture zone was long, stretching from Arauco (37° S) to below the Chiloé Archipelago (44° S). Rupture velocity, the speed at which a rupture front expands across the surface of the fault, has been estimated as per second. The average slip across all 27 Nazca sub-faults was estimated to be , with of slip south of the epicenter on offshore sub-faults. ==Earthquake sequence==
Earthquake sequence
Concepción earthquakes The 1960 Chilean earthquakes were a sequence of strong earthquakes that affected Chile between 21 May and 6 June 1960, centered in the Cautín, Malleco, Aysén, and Biobío provinces of the country. The first three quakes, all registering in the planet's top 10 by magnitude for 1960, are grouped together as the 1960 Concepción earthquakes. The first of these was the 8.1 Mw Concepción earthquake at on 21 May 1960. Its epicenter was near Curanilahue. Telecommunications to southern Chile were cut off and President Jorge Alessandri cancelled the traditional ceremony of the Battle of Iquique memorial holiday to oversee the emergency assistance efforts. The second and third Concepción earthquakes occurred the next day at (7.1 Mw) and (7.8 Mw) on 22 May. These earthquakes formed a southward migrating foreshock sequence to the main Valdivia shock, which occurred just 15 minutes after the third event. The earthquake interrupted and effectively ended a protest by coal miners from Lota, who were attempting to march to Concepción to demand higher salaries. Valdivia earthquake The Valdivia earthquake occurred at 15:11 UTC-4 on 22 May, and affected all of Chile between Talca and Chiloé Island, more than . Coastal villages, such as Toltén, were struck. At Corral, the main port of Valdivia, the water level rose before it began to recede. At 16:20 UTC-4, a wave of struck the Chilean coast, mainly between Concepción and Chiloé. Another wave measuring was reported ten minutes later. Hundreds of people were already reported dead by the time the tsunami struck. One ship, Canelo, starting at the mouth of the Valdivia River, sank after being moved backward and forward in the river; as of 2005, its mast was still visible from the road to Niebla. Soil subsidence also destroyed buildings, deepened local rivers and created wetlands in such places as the Río Cruces and Chorocomayo, a new aquatic park north of the city. Extensive areas of the city were flooded. The electricity and water systems of Valdivia were completely destroyed. Witnesses reported underground water flowing up through the soil. Despite the heavy rains of 21 May, the city was without a water supply. The river turned brown with sediment from landslides and was full of floating debris, including entire houses. The lack of potable water became a serious problem in one of Chile's rainiest regions. The earthquake did not strike all the territory with the same strength; measured with the Mercalli scale, tectonically depressed areas suffered heavier damage. The two most affected areas were Valdivia and Puerto Octay, near the northwest corner of Llanquihue Lake. Puerto Octay was the center of a north–south elliptical area in the Central Valley, where the intensity was at the highest outside the Valdivia Basin. With the exception of poor building sites, the zone of Mercalli scales intensities of VII or more all lay west of the Andes in a strip running from Lota (37° S) southwards. The area of intensities of VII or more did not penetrate into the Central Valley north of Lleulleu Lake (38° S) and south of Castro (42.5° S). This magnitude 7.7 earthquake probably occurred along the Liquiñe-Ofqui Fault, meaning that the fault would have moved as a consequence of the 22 May Valdivia earthquake. ==Natural disasters==
Natural disasters
Tsunamis at one-hour intervals Earthquake-induced tsunamis affected southern Chile, Hawaii, Japan, the Philippines, China, eastern New Zealand, southeast Australia, and the Aleutian Islands. Some localized tsunamis severely battered the Chilean coast, with waves up to . The main tsunami crossed the Pacific Ocean at a speed of several hundred km/h and devastated Hilo, Hawaii, killing 61 people. Most of the tsunami-related deaths in Japan occurred in the northeast Sanriku region of Honshu. In Valdivia, the tsunami swell penetrated along Calle-Calle River as far as Huellelhue, putting ashore piles of firewood that lay in the fields. After the 21 May Concepción earthquake, people in Ancud sought refuge in boats. A carabinero (police) boat, Gloria, was towing a few of these boats when the second earthquake struck on 22 May. As the sea regressed Gloria became stranded between Cerro Guaiguén and Cochinos Island. The stranded boat was wrecked when a tsunami wave engulfed it. These landslides did not cause many fatalities nor significant economic losses because most of the areas were uninhabited, with only minor roads. One landslide caused destruction following its blockage of the outflow of Riñihue Lake (see below). About south of Riñihue Lake, landslides in the mountains around Golgol River caused the river to dam up; when it burst through the earthen dam, it created a flood down to Puyehue Lake. The Golgol landslides destroyed parts of international Route 215-CH, which connects to Bariloche in Argentina through Cardenal Antonio Samoré Pass. While most landslides clustered around north–south strips in the Andes, other areas that were affected by large numbers of landslides were the coast, mainly the foot of the Chilean Coast Range, and the shores of Llanquihue Lake. Riñihue Lake's flood During the Great Chilean earthquake, several landslides west of Tralcán Mountain blocked the outflow of Riñihue Lake. Riñihue Lake is the lowest of the Seven Lakes chain and receives a constant inflow from the Enco River. The dammed San Pedro River, which drains the lake, passes through several towns before reaching the city of Valdivia near the coast. As the San Pedro River was impounded, the water level of Riñihue Lake started to rise quickly. Each meter the water level rose was equivalent to 20 million cubic meters, which meant that 480 million cubic meters of water would release into the San Pedro River, easily overpowering its flow capacity of per second if it rose above the final, 24-meter-high dam. This potential disaster would have violently flooded all the settlements along the course of the river in less than five hours, with more dire consequences if the dam suddenly broke. About 100,000 people lived in the affected zone. The eruption was believed to have been triggered by the earthquake. The eruption was first noticed and reported as an explosion by the crew of a United States Air Force plane that was heading to Santiago from Puerto Montt. The eruption fed a 5.5 km-long fissure on 135° heading where 21 individual vents have been found. These vents produced an output of about 0.25 km3 DRE both in form of lava flows and tephra. The eruption ended on 22 July, 59 days later. As a result of an evacuation plan, there were no reported human deaths associated with the eruption. ==Consequences and response==
Consequences and response
Urban impact The levels of material damage were relatively low despite the high magnitude of the earthquake. Part of the reason behind this was the limited infrastructure development of the region next to the rupture zone. The most affected structures were those built of concrete, which in some cases collapsed completely, because they were not built using modern earthquake engineering. Traditional wooden houses fared better; although many were uninhabitable if they did not collapse. Houses built upon elevated areas suffered considerably less damage compared to those on the lowlands, which absorbed great amounts of energy. Many city blocks with destroyed buildings in the city center remained empty until the 1990s and 2000s, with some of them still used as parking lots. Before the earthquake, some of these blocks had modern concrete buildings built after the Great Valdivia fire of 1909. Valdivia's bridges suffered only minor damage. The damage caused to Calle-Calle Bridge led to its temporary closure after the earthquake, with traffic redirected to Teja Island through Caucau River where people crossed it on boats and, reportedly, also a rudimentary and temporary wooden bridge. Land subsidence in Corral Bay improved navigability as shoal banks, produced earlier by sediments from Madre de Dios and other nearby gold mines, sank and were compacted. Parts of the botanical garden of the Austral University of Chile that were next to Cau-Cau River and the city's southern outskirts along Route 206 were permanently flooded. The earthquakes damaged an area that had suffered a long period of economic decline, which began with shifts in trade routes due to the expansion of railroads in southern Chile and the opening of the Panama Canal in 1914. Unlike Valdivia, Osorno was saved from major destruction. In Osorno only about 20 houses were totally destroyed, although many firewalls and chimneys collapsed. Puerto Montt, a major city today, had in the early 1960s about 49,500 inhabitants. The bulk of the damage in Puerto Montt was located in the neighborhood of Barrio Modelo and the northern part of Bahía Angelmó, where artificial fills subsided. Angelmó and other coastal areas of Puerto Montt were among the few urban areas that suffered "total destruction" by the earthquake. After the earthquake a myth related the unusually warm and clear weather conditions prior to the earthquake to its triggering. When compared with the years that followed in the 1960s the autumn of 1960 in southern Chile was not particularly dry nor warm. Impact in the countryside , a steel factory closed a few years before the earthquake. The tsunami that struck the coast of southern Chile destroyed seaside farms, killing numerous livestock and people. Barns and industrial structures were destroyed by the quake. The scholar Erik Dahmén believes that the earthquake resulted in a "creative destruction" for farmers of Southern Chile. A large area of former pastures and cultivated fields around the lower course of Cruces River was permanently flooded as a result of c. 2 m of subsidence caused by the earthquake. Over the years the new wetlands were colonized chiefly by Egeria densa (). Egeria densa and other plants created a rich aquatic ecosystem that attracted a permanent bird fauna, notably black-necked swans. The economy of the coastal town of Queule had during the 1950s developed significantly. Its economy based on fishing, agriculture and industry had grown. Queule was connected by road in 1957 to the rest of the country and the town had developed into a balneario (resort town). This era of prosperity ended with the 1960 earthquake. Further north the earthquake destroyed numerous houses in the coal-mining town of Lebu. The coal mine of Pupunahue suffered severe damage which led to coal production recovering to "acceptable levels" only by 1963. Creation of a national emergency management agency After the earthquake, the Chilean Ministry of Economics began to develop a comprehensive reconstruction plan. The efforts of President Alessandri led to the creation of a new institutionality in order to facilitate future emergency preparation and to tackle the country's recovery after the earthquake. The then-newly named Ministry of Economics and Reconstruction was given the task of coordinating rebuilding efforts in joint venture with CORFO, an existing Chilean agency for the promotion of economic growth. Concomitantly, a ministerial-level committee, COPERE (Comisión de Planificación de la Economía y de Reconstrucción), was officially named as the government's Planning and Reconstruction Committee. CORFO acted the secretariat of the committee and was entrusted with the preparation of the reconstruction plan and its detailed execution. COPERE had also been entrusted with coordinating provincial activities while CORFO remained the technical secretariat of those provincial committees. A comprehensive national plan for emergencies that helped Chile better prepare for future disasters was enacted, in conjunction with legislation that increased the powers of the President in times of national emergency. CORFO also created the National Company of Telecommunications (ENTEL) out of a pressing need to improve and modernize communication efforts in times of disaster. The victim was 5-year-old José Luis Painecur, an "orphan" (huacho) whose mother had gone to work as a domestic worker in Santiago and left her son under the care of his father. == Previous and subsequent earthquakes ==
Previous and subsequent earthquakes
An earthquake of similar magnitude occurred in this area around 1800 BC, as has been determined by dating charcoal and shells washed into the Atacama Desert by the tsunami. This apparently caused the hunter-gatherers of the area to stop living near the coast for the next thousand years or so. There is evidence that a similar earthquake and landslide occurred in 1575 in Valdivia. This earthquake was of similar strength and also caused a Riñihuazo. According to the chronicle of Mariño de Lobera, corregidor of Valdivia in 1575, a landslide blocked the outflow of the lagoon of Renigua. Several months later in April, it caused a flood. He said that the Spanish settlers had evacuated and waited on high ground until after the dam burst, but many aboriginals died in the flood waters. On 27 February 2010 at 03:34 local time, an 8.8 magnitude earthquake occurred just to the north (off the coast of the Maule region of Chile, between Concepción and Santiago). This quake was reported to be centered approximately deep and several miles off shore. It may have been related or consequential to the 1960 Valdivia quake, the strongest as recorded using modern technology. This 2010 earthquake was the largest to affect Valdivia since the 1960 event. Thirty five houses were severely damaged and some 44 other suffered reparable damage. A survey showed that 434 persons in Valdivia had their homes damaged by the earthquake. The damage was to areas of poor soil quality, chiefly former wetlands and artificial fills. Some sidewalks near the river shore in Valdivia cracked and collapsed much like in the 1960 earthquake. Overall the 2010 areas of damage in Valdivia were few and highly localized. ==See also==
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