|UTC time||1985-09-19 13:17:50|
|Local date||19 September 1985|
|Depth||20 km (12 mi)|
|Max. intensity||IX (Violent)|
|Aftershocks||7.5 Mw 20 September 1985 |
7.0 Mw 30 April 1986
|Casualties||5,000–45,000 dead |
The 1985 Mexico City earthquake struck in the early morning of 19 September at 07:17:50 (CST) with a moment magnitude of 8.0 and a Mercalli intensity of IX (Violent). The event caused serious damage to the Greater Mexico City area and the deaths of at least 5,000 people. The sequence of events included a foreshock of magnitude 5.2 that occurred the prior May, the main shock on 19 September, and two large aftershocks. The first of these occurred on 20 September with a magnitude of 7.5 and the second occurred seven months later on 30 April 1986 with a magnitude of 7.0. They were located off the coast along the Middle America Trench, more than 350 kilometres (220 mi) away, but the city suffered major damage due to its large magnitude and the ancient lake bed that Mexico City sits on. The event caused between three and four billion USD in damage as 412 buildings collapsed and another 3,124 were seriously damaged in the city.
The moment magnitude scale is a measure of an earthquake's magnitude based on its seismic moment, expressed in terms of the familiar magnitudes of the original "Richter" magnitude scale.
Greater Mexico City refers to the conurbation around Mexico City, officially called Valley of Mexico Metropolitan Area, constituted by Mexico City itself composed of 16 Municipalities—and 41 adjacent municipalities of the states of Mexico and Hidalgo. For normative purposes, however, Greater Mexico City most commonly refers to the Metropolitan Area of the Valley of Mexico an agglomeration that incorporates 18 additional municipalities. As of 2016 an estimated 21,157,000 people lived in Greater Mexico City, making it the largest metropolitan area in North America. It is surrounded by thin strips of highlands which separate it from other adjacent metropolitan areas, of which the biggest are Puebla, Toluca, and Cuernavaca-Cuautla, and together with which it makes up the Mexico City megalopolis.
The Middle America Trench is a major subduction zone, an oceanic trench in the eastern Pacific Ocean off the southwestern coast of Middle America, stretching from central Mexico to Costa Rica. The trench is 1,700 miles (2,750 km) long and is 21,880 feet at its deepest point. The trench is the boundary between the Rivera, Cocos, and Nazca plates on one side and the North American and Caribbean plates on the other. It is the 18th-deepest trench in the world. Many large earthquakes have occurred in the area of the Middle America Trench.
Much of Mexico's volcanic and seismic activity stems from the movement of the North American plate against the Cocos and Pacific plates and it is one of the most active trenches in the world.Each year more than 90 tremors above magnitude 4.0 are recorded in this zone.
While not on or near any fault line like San Francisco or Los Angeles, Mexico City is vulnerable to earthquakes. The main reason for this is the surface geology of the area, especially the downtown area. The city was originally built on an island in the middle of Lake Texcoco, and Aztec rulers built dikes to prevent floodingwhile Spanish colonial rulers later drained the lakes in response to major flooding. The near surface geology of this area is classified into three sections: the old lake bed which is soft clay from volcanic ash with a high water content, a piedmont area, much of which is capped by 5 to 30 meters of lava less than 2,500 years old, and an old river delta area.
Lake Texcoco was a natural lake within the "Anahuac" or Valley of Mexico. Lake Texcoco is best known as where the Aztecs built the city of Tenochtitlan, which was located on an island within the lake. After the Spanish conquest of the Aztec Empire, efforts to control flooding by the Spanish led to most of the lake being drained. The entire lake basin is now almost completely occupied by Mexico City, the capital of the present-day nation of Mexico.
Volcanic ash consists of fragments of pulverized rock, minerals and volcanic glass, created during volcanic eruptions and measuring less than 2 mm (0.079 inches) in diameter. The term volcanic ash is also often loosely used to refer to all explosive eruption products, including particles larger than 2 mm. Volcanic ash is formed during explosive volcanic eruptions when dissolved gases in magma expand and escape violently into the atmosphere. The force of the escaping gas shatters the magma and propels it into the atmosphere where it solidifies into fragments of volcanic rock and glass. Ash is also produced when magma comes into contact with water during phreatomagmatic eruptions, causing the water to explosively flash to steam leading to shattering of magma. Once in the air, ash is transported by wind up to thousands of kilometers away.
Foothills or piedmont are geographically defined as gradual increases in elevation at the base of a mountain range, higher hill range or an upland area. They are a transition zone between plains and low relief hills and the adjacent topographically higher mountains, hills, and uplands. Frequently foothills consist of alluvial fans, coalesced alluvial fans and dissected plateaus.
On the bed of the historic lake, the prevailing silt and volcanic clay sediments amplify seismic shaking. Damage to structures is worsened by soil liquefaction which causes the loss of foundation support and contributes to dramatic settlement of large buildings.Mexico City's downtown area mostly lies on the silt and volcanic clay sediments of the bed of the historic Lake Texcoco, which are between seven and thirty-seven meters deep and have a high water content. Above this is a layer of sand and above this is a layer of sand and rock. The western and northwestern parts of the city are outside the old lakeshores and are located on sands from eroding volcanic cones that surround the Valley of Mexico. The southern part of the city rests on hardened basalt lava flows. The old lakebed, with its high water content, is easily moved or compressed. The old lakeshore area also has a fairly high water content, allowing movement, though not as much as the lakebed. The old lava flows have little water content or movement in comparison and are therefore stable.
Soil liquefaction occurs when a saturated or partially saturated soil substantially loses strength and stiffness in response to an applied stress such as shaking during an earthquake or other sudden change in stress condition, in which material that is ordinarily a solid behaves like a liquid.
Another factor is that the old lakebed resonates with certain seismic waves and low frequency signals.This lakebed has a natural "pitch" of one cycle every 2.5 seconds making everything built on the bed vibrate at the same frequency. This is the same "pitch" as a number of shallow earthquake waves. This resonance amplifies the effects of the shock waves coming from an earthquake far away.
Seismic waves are waves of energy that travel through the Earth's layers, and are a result of earthquakes, volcanic eruptions, magma movement, large landslides and large man-made explosions that give out low-frequency acoustic energy. Many other natural and anthropogenic sources create low-amplitude waves commonly referred to as ambient vibrations. Seismic waves are studied by geophysicists called seismologists. Seismic wave fields are recorded by a seismometer, hydrophone, or accelerometer.
However, only certain types of structures are vulnerable to this resonance effect. Taller buildings have their own frequencies of vibration. Those that are six to fifteen stories tall also vibrate at the 2.5-second cycle, making them act like tuning forks in the event of an earthquake. The low-frequency waves of an earthquake are amplified by the mud of the lakebed, which in turn, is amplified by the building itself. This causes these buildings to shake more violently than the earthquake proper as the earthquake progresses. Many of the older colonial buildings have survived hundreds of years on the lakebed simply because they are not tall enough to be affected by the resonance effect.
The earthquake occurred in the Pacific Ocean, off the coast of the Mexican state of Michoacán, a distance of more than 350 km (220 mi) from the city, in the Cocos Plate subduction zone, specifically in a section of the fault line known as the Michoacán seismic gap. The Cocos Plate pushes against and slides under the North American Plate, primarily along the coasts of the states of Michoacán and Guerrero in Mexico. Volatile trenches along the Cocos plate generally have had seismic events 30 to 70 years before 1985. This subduction zone outside the Michoacán gap was the source of 42 earthquakes of magnitude 7.8 or stronger in the 20th century prior to the 1985 event. However, this particular section of the subduction zone had not had an event for a much longer time.
Shockwaves from the earthquake hit the mouth of the Río Balsas on the coast at 7:17 am and hit Mexico City, 350 km (220 mi) away, two minutes later at 7:19 am. The 19 September quake was a multiple event with two epicenters and the second movement occurring 26 seconds after the first. Because of multiple breaks in the fault line, the event was of long duration. Ground shaking lasted more than five minutes in places along the coast and parts of Mexico City shook for three minutes, with an average shaking time of 3–4 minutes. It is estimated the movement along the fault was about three metres (9.8 ft). The main tremor was foreshadowed by a quake of magnitude 5.2 on 28 May 1985, and was followed by two significant aftershocks: one on 20 September 1985 of magnitude 7.5 lasting thirteen seconds and the third occurring seven months later on 30 April 1986 with magnitude 7.0 lasting ten seconds. However, at least twelve other minor aftershocks were associated with the seismic event.
The energy released during the main event was equivalent to approximately 1,114 nuclear weapons exploding.The earthquake was felt over 825,000 square kilometers, as far away as Los Angeles and Houston in the United States.
In the port of Lázaro Cárdenas, near the epicenter, the 19 September event registered as IX on the Modified Mercalli intensity scale; in parts of Mexico City, it registered the same, even at a distance of about 400 km (249 mi) away. There was no historic record of such a strong quake in Mexico.
While the fault line was located just off the Pacific coast of Mexico, there was relatively little effect on the sea itself. The earthquake did produce a number of tsunamis but they were small, ranging between one and three metres (3 ft 3 in and 9 ft 10 in) in height. Ecuador reported the highest waves of 60 cm (2.0 ft).
Most of the earthquake damage was to buildings. Two reasons are the resonance in the lakebed sediments and the long duration of the shaking.The buildings most damaged were from 6 to 15 stories in height. These buildings tended to resonate most with the energetic frequency band of the lakebed motions. One interesting characteristic was that many buildings had their upper floors collapse, leaving the lower floors relatively undamaged. In many damaged buildings, just one floor had collapsed. In some cases the damage was caused by the top of a lower, adjacent building banging against the walls and the supporting columns of its neighbor. Eventually, the columns gave way. In other cases, the first few floors of buildings were designed as parking garages, open lobbies or large shopping areas. These "soft" stories were particularly flexible and tended to collapse after prolonged shaking. Some types of foundations, particularly those involving piles driven into clay and held in place by friction, turned out to be weak. One nine-story building, for example, overturned. Its piles were pulled entirely out of the ground.
A survey by the government of the damage done found that few buildings from one to five stories suffered serious damage; the same was true for buildings over fifteen stories. When the buildings were built seemed to have an effect as well. Before the 1957 earthquake, there were no building codes with respect to earthquake resistance. Some regulations were passed in that year and more in 1976 after another, stronger earthquake shook the city. However, none of these regulations had an event like 1985's in mind when passed. Most of the seriously damaged buildings were built between 1957 and 1976, when the city was starting to build upwards, in the six-to-fifteen floor range. In second place were buildings from before 1957, possibly because they were weakened by the earlier earthquakes. Structures built between 1976 and 1985 suffered the least damage.
At the time of the earthquake, Mexico City had one of the most stringent building codes,[ compared to? ] based on experience gained from earthquakes in 1957 and 1979. However, the codes were not designed for seismic activity of the intensity experienced in 1985. The event was one of the most intense ever recorded, and macroseismic waves arrived in the Valley of Mexico with unusually high energy content. Prior to the event, estimates about ground movement on the lakebed were generally accepted and a number of buildings were built on these estimates.
Several notable buildings were relatively untouched by the quake. One significant example is the Torre Latinoamericana. Despite being 44 stories tall, it survived the 1985 event almost undamaged. It was constructed with two hundred piles extending down over one hundred feet (30 m) into the stable earth stratum.
Mexico City is divided into boroughs. Eighty percent of the earthquake damage was confined to four of them: Venustiano Carranza, Cuauhtémoc, Benito Juárez and Gustavo A. Madero. two to four kilometres (1.2 to 2.5 mi) of the Alameda Central. Nearly all the buildings that collapsed were located in this lake zone that extended from Tlatelolco in the north to Viaducto Miguel Alemán in the south, Chapultepec Park in the west and to a short distance east of the Zócalo or main plaza.The damage area corresponds to the western part of the lake zone within
Cuauhtémoc, which includes the historic downtown, suffered the most damage. In this particular area, 258 buildings completely crumbled, 143 partially collapsed and 181 were seriously damaged. The next seriously affected area was Venustiano Carranza where 83 buildings collapsed, 128 partially collapsed and 2,000 structures were seriously damaged.Damage was localized to the center parts of the city, leaving much of the residential outer rim unscathed, but the damage in the affected area was extensive. Over 720,000 tons of debris was removed during the first six weeks after the event. The Metropolitan Commission for Emergencies of the Federal District reported 2,831 buildings damaged for the entire city: 31% or 880 were completely ruined, 13% were reinhabitable with major repairs and the rest, totaling 1581, were recoverable with minor repairs. This translates to more than 30,000 housing units completely destroyed and another 68,000 units damaged.
One of the most visible government institutions to fall in the event was the tower of Hospital Juárez, one of the oldest hospital institutions in Mexico. It was founded in 1847, converting the old convent of San Pablo to treat wounded soldiers from the Mexican–American War. It originally was called San Pablo Hospital but its name was changed to Juárez Hospital in 1872.
The "Torre de Hospitalización" was built in 1970 with the main building being twelve stories tall. It had two wings, one facing north and the other south, with an inpatient capacity of 536 beds. At the top was a helipad. It was also surrounded by a number of other buildings belonging to the hospital complex such as a blood bank, teaching facilities, offices as well as the original convent. At the time of the earthquake, the hospital was 80% full, and it was shift change time for nurses, doctors and residents. Within minutes, the steel-frame structure collapsed, crushing and trapping many people inside.
Those who were rescued first were taken to another building for treatment, as the ambulances were trapped inside the collapsed tower. The hospital did not have an emergency plan but nonetheless, surviving hospital workers and neighbors quickly improvised, under the management of the hospital, setting up aid stations and scavenging supplies. Rescue workers soon arrived to start digging through the rubble. A second quake made rescue work slower, because of fear of further collapse. Most bodies were identified by personal effects, some by dental records and some were so mangled that they wound up being cremated without ever being identified, due to the lack of morgue facilities. 561 bodies were found and 188 were never identified. 266 were hospital workers and 44 were medical residents. The majority who were rescued were found in the first five days. The number of bodies recovered was high during those first days as well but the numbers dramatically increased between days 17 and 31.
Heavy machinery was unable to get to the site until five days after the earthquake. Numbers of dead did not include unidentified body parts found. Most of the injured had contusion injuries and many suffered from dehydration, with the severity of the dehydration increasing with those rescued later.
However, the most memorable story to come from this event was the rescue of nearly all the newborn babies that were in the nursery at the time. These babies were pulled out of the wreckage mostly unscathed but lost their mothers.The infants were found seven days after the initial event and came to be known as the "Miracle Babies" or the "Miracle of Hospital Juárez", having survived without nourishment, water, warmth or human contact during that time.
On Manuel José Othón Street, in the Colonia Obrera neighborhood, near Metro station San Antonio Abad, was one of the many garment factories located in the city center area. It was destroyed along with approximately 1,200 other workshops.
Called "Topeka", it was one of three buildings that collapsed on this block. The magazine Proceso reported that by the time rescue workers reached the building, the owners were already in a hurry to demolish it, without trying to rescue or recover the workers trapped inside.About 150 bodies of workers had already been pulled from the wreckage by fellow employees using their bare hands.
The collapse of this factory exposed the deplorable conditions to which many of these women were subjected. The building that collapsed, as well as many others, were found to be decrepit. It came to be known that many of the women had to work extended hours with little or no compensation, and few, if any, of the labor laws on the books were being followed. This event made the garment industry a labor embarrassment.All that remains of the factory is a small empty lot with a bronze statue of a woman sewing. Apartments were built on the remainder of the property.
On Eje Central and Xola Avenue, at the southern end of the lakebed zone was (and is) the Secretaría de Comunicaciones y Transportes (Ministry of Communication and Transportation), a reinforced concrete structure with its microwave tower. This structure failed, causing the near total collapse of long distance communications between Mexico City and the rest of the world.
One of the most spectacular building collapses was that of the Conjunto Pino Suárez, which was a complex of five steel-frame buildings. A 20-story tower, Tower Four, doubled over at the third floor and fell south onto a fourteen-story building.The fall left a huge piece of concrete blocking the road that leads to the Zócalo. People at the scene stated that there was simply no time to run and escape the building's fall. The other three 20-story buildings were closed because of damage, as well as the Metro entrance next door. The building was occupied by family courts and offices of the public defender. The area is now a market.
The Hotel Regis was built in the beginning of the 20th century as a luxury hotel in neo-Classical style. It had its own cabaret, gourmet restaurant and a small but luxurious cinema with wide reclining armchairs.
It was located at the corner of Balderas and Avenida Juárez in the historic center and completely collapsed within moments of the quake.Shortly after its collapse, it began to burn due to a gas leak, which made it extremely difficult to rescue survivors. Nothing survived of the hotel. The space is now the Plaza de la Solidaridad park. The Museo Mural Diego Rivera on the north side of the park houses a mural by Diego Rivera which was originally housed in the huge Hotel Del Prado across the street. That hotel was irreparably damaged in the earthquake and subsequently demolished.
There were two apartment complexes in the area of the city called Tlatelolco to the north of the historic center that became major scenes of disaster, the Conjunto Urbano Nonoalco Tlatelolco and the "Multifamiliares Juárez" near the Metro Centro Médico. Together, these apartment complexes were a large percentage of the 30,000 units lost, with the city losing about 30% of its living space.
Nonoalco Tlatelolco was located on Paseo de la Reforma Norte #668, two km2 (0.77 sq mi). It had 102 buildings with seven medical facilities, twenty-two schools and about 500 small businesses, serving the 80,000 people who lived there. Constructed under the presidency of Adolfo López Mateos, it was considered the most important complex of its kind in the country.covering an area of about
In the Conjunto Urbano, two of the three modules of the building called "Nuevo León", at thirteen stories tall, completely collapsed, while the other one was severely damaged. In other buildings, dozens of people terrified by the event jumped from high windows to their deaths, trying to escape.People became trapped in stairwells, elevators and their apartments without any way to contact the outside world. At the collapsed building, lines of 50–100 people passed rubble by hand and buckets, trying to reach victims. During these rescue efforts, a nearby building, called Oaxaca, began to creak noisily, causing everyone to run and abandon the site temporarily, but it did not collapse.
All the buildings suffered damage but along with the collapsed Nuevo León building, buildings such as those called Veracruz, Coahuila, Zacatecas, Oaxaca, Puebla, Jalisco, Churubusco, Guelatao, 2 de Abril, 15 de Septiembre, Chihuahua, Tamaulipas, ISSSTE 11, Querétaro, Guanajuato, Ignacio Comonfort, Ignacio M. Altamirano, Jesús Terán, Ponciano Arriaga, Niños Héroes and 20 de Noviembre suffered severe damage such as deeply cracked foundations. In the days after the quake, military and police cordoned off ten buildings to keep people out, leading a number of them to sleep on the streets.Twelve buildings in the complex were so badly damaged that they were demolished in the next six months.
Buildings A1, B2 and C3 of the Multifamiliar Juárez complex partially collapsed with a total of nine structures eventually being demolished.
One of the more famous images of the event was the live broadcast of Hoy Mismo, a news program in the Televisa television network, when the earthquake struck. In the video, movement can be seen, especially in the lights above the newscasters. The three newscasters were María Victoria Llamas (substituting for Guillermo Ochoa), Lourdes Guerrero and Juan Dosal. As the movement began Llamas reports grabbing the underside of the desk, and whispering quickly to her colleagues that she hoped no one could see how scared she was. it's still shaking a little (sigue temblando un poquitito), but we must take it calmly. We will wait just a second so we can keep talking." Then the image disappeared.The last image broadcast from the studio was that of Lourdes Guerrero stating "...
The transmission ended because a nearby 10-ton antenna had bent over and crushed parts of Televisa's buildings that were located on Niños Héroes and Dr. Río de la Loza Streets in Colonia Doctores.Everyone ran from the studio but Llamas and Guerrero stayed, hiding under their anchor desks. After the shaking stopped, they both left the Televisa studios through a back door, and hours later they were back on the air in the studios of Canal de las Estrellas to broadcast live what was happening. Some members of the Hoy Mismo staff died, including producer Ernesto Villanueva and engineer David Mendoza Córcega, who had just parked at the Televisa building, but had no time to escape from his car. The falling debris also killed street vendors who worked just outside the studio building. Reconstruction of the studio building began in 1995 and ended in 2000.
The region's infrastructure was severely affected. The number of people with potable water went from six million to 90,000. 6,500 metres (4.0 mi) of primary and secondary water and drainage pipes suffered breaks in 163 places, cutting off water and contaminating it. 516,000 m2 (5,550,000 sq ft) of asphalt was damaged, and 137 schools collapsed. The number of jobs lost due to the event was estimated at 200,000. Forty percent of the population was without electricity and seventy percent without telephone service.as
1,687 school buildings were damaged. Interruption of classes, either to the lack of facilities and/or the need to help with rescue efforts, affected over 1.5 million students.
On the day of the quake, the Metro stopped service and completely shut down for fear of electrocution. This caused people to get out of the tunnels from wherever they were and onto the street to try to get where they were going.At the time, the Metro had 101 stations, with 32 closed to the public in the weeks after the event. On Line 1, there was no service in stations Merced, Pino Suárez, Isabel la Católica, Salto del Agua, Balderas or Cuauhtémoc. On Line 2, there was no service between stations Bellas Artes and Taxqueña. On Line 3 only Juárez and Balderas were closed. Line 4 continued to operate normally. All of the closed stations were in the historic center area, with the exception of the stations of Line 2 south of Pino Suárez. These stations were located above ground. The reason these stations were closed was not due to damage to the Metro proper, but rather because of surface rescue work and clearing of debris.
The area most severely hit by the earthquake had the highest concentration of hospitals. Most of the damage occurred in secondary and tertiary hospitals.Thirteen hospitals of six or more floors were partially or totally destroyed, most of these public institutions. One out of every four then-available beds were lost.
The National Medical Center of the Mexican Social Security Institute (IMSS) was considered the most important hospital complex in Latin America with over 2,300 beds and the largest medical library in the country. It had to be evacuated because all of its 25 buildings suffered severe damage. Most of the beds that it lost were dedicated to tertiary, high-technology care. The ISSSTE hospital for government workers lost 36 percent of its capacity. The 2,158 beds of the Ministry of Health (SSA) were lost, representing 43 percent of its capacity in the city. This included the 700 beds lost with the complete collapse of Juárez Hospital and the gynecology-obstetrics tower of the General Hospital of Mexico. In total, the city lost more than 4,000 public hospital beds in the earthquake, severely disrupting these institutions' ability to handle the crisis. In addition, five of the largest private hospitals had to be evacuated. More than 900 patients, physicians, nurses and paramedical workers died in the initial shock.
In contrast, the network of twenty four community general hospitals with 1,600 beds belonging to the city (federal district) were not affected as these were spread out beyond the city center and the old lakebed.
Although much closer to the epicenter, the states of Jalisco, Colima, Guerrero and Michoacán suffered only mild to moderate damage. Landslides caused damage at Atenquique, Jalisco, and near Jala, Nayarit. Rockslides were reported along highways near Ixtapa, Guerrero, with sand volcanos and ground cracks in Lazaro Cardenas. Students at the Universidad de las Américas in nearby Puebla reported feeling as if the cafeteria had been lifted and rocked back and forth, shattering windows and injuring some people but mostly causing panic. A small tsunami caused only mild damage to Lázaro Cárdenas and Zihuatanejo. Some fishing boats were reported missing but these reports were never confirmed.One exceptional case was in Ciudad Guzmán, Jalisco, where about 60 percent of the buildings were destroyed, with about 50 dead. Some damage also occurred as far away as the states of Mexico, Morelos and parts of Veracruz, on the Gulf coast. Coastal and most inland damage was moderated by the fact that most of the west of Mexico sits on bedrock, which serves to transmit the shockwaves without amplifying them. La Villita, and Infiernillo Dams, near the coast, were superficially damaged and undamaged respectively.
Off the coasts of Michoacán and Guerrero, the 19 and 20 September events caused a rupture in the seabed 240 km long and 70 km wide, located between the subduction trench and the coastline. This is an intertidal zone and the event caused widespread mortality in a number of species living in the area such as algae and shellfish.
To this day, the death toll has been in dispute. About 5,000 bodies were recovered from the debris and represent the total of legally certified deaths but does not include those who were missing and never recovered. am, when people were awake but not in the many schools and office buildings that were severely damaged.Reports have numbered the dead anywhere from 5,000 to 30,000 (claimed by a number of citizens' groups) to 45,000 claimed by the National Seismological Service. However, the most commonly cited figures are around 10,000. While high as an absolute number, it compares to other earthquakes of similar strength in Asia and other parts of Latin America where death tolls have run between 66,000 and 242,000 for earthquakes of magnitude 7.8 or above. Part of the explanation for that was the hour in which the earthquake struck, approximately 7:20
However, the death toll was great enough to require the use of the IMSS baseball field as a morgue, using ice to conserve bodies for identification.
The main reason that the figures have been disputed is the government's response to the tragedy.President Miguel de la Madrid ordered a news blackout and did not address the situation at all for 39 hours after the event. When the government did give estimates of the number killed, they ranged from 7,000 to 35,000. Consequently, most of the populace believes that the true numbers have never been revealed.
According to government figures, approximately 250,000 people lost their homes directly due to the earthquake. Unofficial sources put that figure much higher.Some sources say that more than 50,000 families lost their homes. INEGI reports that 700,000 people in the Federal District and the suburbs in the State of Mexico lost their homes.
In the hours and days immediately after the first shock, there was an enormous response and solidarity among the city population of 18 million people. Ordinary citizens organized brigades to help with rescue efforts and to provide food, clothing and emotional support to the homeless.
Patients had to be moved from damaged hospitals, especially the National Medical Center. Many of these patients were very ill. 1,900 patients were successfully moved from here, without any deaths, in just four hours.
More than 4,000 people were rescued alive. 9,600 injured people received treatment, including 1,879 who needed hospitalization. Despite the loss of 5,000 hospital beds, there was never a shortage of facilities for the injured. Some of the reason for this was that those with postponable care were discharged, but mostly because the public and private facilities unified de facto during the crisis.There were also people rescued as late as ten days after the initial event.
The military was deployed to patrol streets to prevent looting after a curfew was imposed,as well as rescue, sanitary efforts and other, with 1,836 soldiers initially sent in and another 1,500 conscripts sent later. The federal government's first public response was President de la Madrid's declaration of a period of mourning for three days starting from 20 September 1985.
These earthquakes created many political difficulties for the then-ruling Partido Revolucionario Institucional (PRI) or Institutional Revolutionary Party. The crisis was severe enough to have tested the capabilities of wealthier countries, but the government from local PRI bosses to President de la Madrid himself exacerbated the problem aside from the lack of money.The Ministry of Foreign Affairs declared it would not request aid; it specifically rejected help from the United States. It was also widely reported in the days after the earthquake that the military assisted factory owners in retrieving their machinery rather than in removing the bodies of dead factory workers. At many levels of the government, who was helped and by how much was determined by one's standing vis-à-vis the PRI. Those belonging to the party received preference and those considered opposition received the runaround. President de la Madrid refused to cut foreign debt payments to use the money to help with the recovery effort. The government's response to the earthquake was widely criticized at various levels of Mexican society, being seen as both authoritarian and incompetent. As most of the collapsed buildings were of recent construction and public works projects, the government was seen at fault due to mismanagement and corruption in these constructions. The government itself realized that it could not handle the crisis alone through already-established institutions and decided to open the process up to "opposition groups".
On the other hand, the disaster created an opportunity for political opponents, especially at the grassroots level. Much of the community organizing focused on helping those left homeless by the earthquake. The three largest and most effective organizations were based in Tlatelolco and Colonia Roma. These consisted of families from the "Multifamiliar Juárez" housing project, which completely collapsed and the combined colonias (neighborhoods) of Centro, Morelos, Guerrero, Doctores, Obrera, Peralvillo, Asturias, Nicolás Bravo among others which housed the working and lower classes. These groups along with the Sindicato Nacional de Costureras united to form the Coordinadora Única de Damnificados (CUD).
CUD and other popular movement representatives met the head of the Secretariat of Urban Development and Ecology (SEDUE) Guillermo Carrillo Arena on 27 September 1985. Carrillo Arena at first insisted that the movements incorporate themselves into the PRI before gaining any concessions. This was refused. Many media outlets expressed support for the popular movements and marches like that of 2 October 1985, demanding that the reconstruction process be more "democratic", meaning the inclusion of non-PRI political organizations into the decision-making process. On 11 October 1985, the President granted a seven-minute audience to the heads of a dozen popular movements, which turned into a 45-minute meeting where de la Madrid was handed a document outlining what would remain the movements' core demands: expropriation of all condemned buildings, followed by a "popular" and "democratic" reconstruction project which would include the active participation of the community movement. De la Madrid conceded some with the expropriation of 5,500 properties in the four most affected boroughs.
After the government created the Programa de Renovación Habitacional Popular (PRHP) on 14 October to help deal with the crisis, friction between the government and community groups grew again, PRHP used PRI-membership as a requirement to be included into the census of earthquake victims. More protests followed on 26 October calling for, among other things, the firing of SEDUE head Carrillo Arena. Things got worse through February 1986, mostly due to the ineffectiveness of SEDUE and PRHP. Finally Carrillo Arena was fired from SEDUE and replaced by Manuel Camacho Solís.
In March, only weeks after taking office, Camacho Solís changed the charged atmosphere between SEDUE and the community groups. He actively integrated Tlateloloco citizen groups into a new program meant for that area, defusing the most volatile area of the city. Camacho Solís continued to work to integrate and smooth relations between his agency and the community groups. On 16 May 1986, Camacho Solís met with the heads of all the major groups. He offered a commitment to build 48,000 housing units in one year if the groups would all sign a "Convenio de concertación democrática para la reconstrucción de vivienda" (Democratic agreement for the reconstruction of housing). Basically, this document required the cooperation of community groups in exchange for solid commitments from the agency. All sides would compromise in order to get something done. The deal generally worked; movements like CUD moderated their stances and agencies like SEDUE and PRHP made progress in rebuilding housing, regardless of political affiliation.
At the time of the earthquake, Mexico was in its fifth year of a foreign debt crisis, and a contracting economy causing serious political problems for the Institutional Revolutionary Party (PRI). Much of the PRI's authoritarian nature was tolerated because the country had seen four decades of economic expansion of six percent or better. When this disappeared, the PRI's power base began to shrink. Its reputation was damaged further when the government seemed to be deliberately downplaying the number of earthquake victims. President de la Madrid made relatively few public appearances afterwards and during those he did, he received strong heckling, in contrast to the near-reverence that past presidents enjoyed at such events.
The severe damage in so many buildings, including in many public works construction projects to house the rapidly growing population of Mexico City, was blamed on lax enforcement of building codes. Critics argued that the lack of enforcement of such codes was indicative of corrupt practices in all levels of government.
The stepping-in of non-PRI organizations to take over where the government could not, also took its toll on PRI's reputation. Burton Kirkwood stated, "Out of the disaster emerged the realization that a viable civil society existed in Mexico. This revelation also caused many to consider why they needed a centralized state that so obviously could not care for its people. As a consequence, the opposition movements pointed to the government's shortcomings and advanced candidates for the greater goal of defeating the PRI."
Shortly after the event, the PRI began to face serious challenges at the polls, forcing it to rig elections, sometimes in embarrassingly messy ways.
One preparation that was made for any future events was the alert system, Sistema de Alerta Sísmica (SAS), which sends early-warning messages electronically from sensors along the coastal subduction zone in Guerrero. It was expanded to a similar area on the coast of Oaxaca.An alarm is supposed to go off in Mexico City (similar to an air-raid siren) when an earthquake of 6.0 or higher is detected. However, it does not always work.
To better help deal with major disasters, the Civil Protection Committee was created.This committee organizes drills in cooperation with rescue workers, police, hospital staff and even metro personnel. Affiliated with the Civil Protection Committee is the "Brigada de Topos de Tlatelolco" (Mole Brigade of Tlatelolco). This group arose from youths who spontaneously volunteered to risk their lives crawling into collapsed buildings to look for survivors. Despite having no equipment, training or knowledge of rescue tactics, these youths were instrumental in saving a number of lives, including the babies rescued from the collapse of the Juárez Hospital. Shortly thereafter, these youths decided to formally band together in February 1986. These "topos" have developed into highly trained specialists in times of disaster, with branches in other parts of Mexico. They are now expertly trained and even have scent dogs to help them. They have gained international fame as they have helped in disasters in San Salvador, Taiwan, in the countries of the rim of the Indian Ocean after the tsunami there in 2004, and in the January 2010 Haiti earthquake.
Despite warnings and predictions, in 2005, an estimated 32 million people live in the high-risk lakebed area.
As of 2005, there are still two camps where approximately eighty families are still waiting for relocation from the earthquake.
Centuries-old structures have been reinforced across the city and new construction must comply with very strict codes.There are several instances of tall buildings in Mexico City incorporating earthquake-resistant engineering. A few notable examples are: the Torre Latinoamericana, one of the first buildings in Mexico City to do so, the Torre Ejecutiva Pemex, built before the 1985 earthquake, and the Torre Mayor, built in 2003.
Every 19 September, in all public buildings at Mexico City and all the nation the civil protection authorities conduct evacuation drills to evaluate the evacuation response in the case of an earthquake. On September 19, 2017, 32 years after the 1985 earthquake, Mexico City also faced another earthquake at around 13:14 CDT (18:14 UTC), nearly two hours after the earthquake drills took place.
The Soda Stereo hit "Cuando pase el temblor" which was coincidentally released just weeks after the disaster was temporarily banned from airplay in Mexico due to the magnitude of the events of September 19 and 20. However, most music analysts consider the track to be one that combines the agony and frustration of a people that struggled with the hardships of the time. To this day the track can still be relevant in many ways especially when it comes to difficult situations.
Cuauhtémoc, named after the former Aztec leader, is one of the 16 boroughs of Mexico City. It consists of the oldest parts of the city, extending over what was the entire city in the 1920s. This area is the historic and cultural center of the city, although it is not the geographical center. While it ranks only sixth in population, it generates about a third of the entire city's GDP, mostly through commerce and services. It is home to the Mexican Stock Exchange, the important tourist attractions of the historic center and Zona Rosa, and various skyscrapers such as the Torre Mayor and the Mexican headquarters of HSBC. It also contains numerous museums, libraries, government offices, markets and other commercial centers which can bring in as many as 5 million people each day to work, shop or visit cultural sites. This area has had problems with urban decay, especially in the historic center. Efforts to revitalize the historic center and some other areas have been ongoing since the 1990s, by both government and private entities. Such efforts have resulted in better public parks, such as the Alameda Central, which was renovated; the modification of streets such as 16 de Septiembre and Madero that have become exclusive for pedestrians.
The 2009 L'Aquila earthquake occurred in the region of Abruzzo, in central Italy. The main shock occurred at 03:32 CEST on 6 April 2009, and was rated 5.8 or 5.9 on the Richter magnitude scale and 6.3 on the moment magnitude scale; its epicentre was near L'Aquila, the capital of Abruzzo, which together with surrounding villages suffered the most damage. There have been several thousand foreshocks and aftershocks since December 2008, more than thirty of which had a Richter magnitude greater than 3.5.
The Brigada Internacional de Rescate Tlatelolco A.C, better known as the Topos de Tlatelolco is a professional non-profit Mexican rescue team.
The 2010 Baja California earthquake occurred on April 4 with a moment magnitude of 7.2 and a maximum Mercalli intensity of VII. The shock originated at 15:40:41 local time south of Guadalupe Victoria, Baja California, Mexico.
The 2010 Oaxaca earthquake struck Oaxaca, Mexico on June 30, 2010, with an Mw magnitude of 6.3. Many people in different cities left their beds and ran into the street, as the quake struck at 2:22 am. Helicopters and police vehicles were sent to inspect possible damage in Mexico City, primarily in downtown and central areas, where some buildings were evacuated. In Mexico City, some cases of power outage in Azcapotzalco, Iztapalapa, and Benito Juárez and cracks in buildings were reported. 1 person died in San Andrés Huaxpaltepec, Oaxaca.
The Conjunto Urbano Nonoalco Tlatelolco is the largest apartment complex in Mexico, and second largest in North America, after New York's Co-op City. The complex is located in the Cuauhtémoc borough of Mexico City. It was built in the 1960s by architect Mario Pani. Originally, the complex had 102 apartment buildings, with its own schools, hospitals, stores and more, to make it a city within a city. It was also created to be a kind of human habitat and includes artwork such as murals and green spaces such as the Santiago Tlatelolco Garden. Today, the complex is smaller than it was and in a state of deterioration, mostly due the effects and after effects of the 1985 Mexico City earthquake. This quake caused the immediate collapse of the Nuevo León building with others being demolished in the months afterwards. Further earthquakes in 1993 caused the condemnation of more buildings. In addition to the lost buildings, many residents eventually undersold or abandoned their apartments, as repairs were either never made or made poorly.
The Centro Urbano Benito Juárez, more commonly called the Multifamiliar Juárez, was a large apartment complex built on the southeast section of Colonia Roma, Mexico City in the late 1940s and early 1950s. It was one of several projects of this type by architect Mario Pani, designed to be semi-autonomous and incorporate as much outdoors space as possible. It also featured one of the largest mural works of the 20th century by artist Carlos Mérida. Most of the complex, and the mural work with it, were destroyed by the 1985 Mexico City earthquake and the demolition of many of the damaged buildings. Only a few of the original buildings still remain. Despite this, the Cuauhtémoc borough in which it is located still lists it as a separate colonia or neighborhood.
The 1985 Rapel Lake earthquake occurred on 8 April at 21:56:59 local time with a moment magnitude of 7.5 and a maximum perceived intensity of VII. The shock was centered 75 kilometres (47 mi) southwest of Santiago, Chile, with a focal depth of 37.8 km (23 mi).
The 2011 Guerrero earthquake struck with a moment magnitude of 5.7 in southern Mexico at 08:24 local time on Thursday, 5 May. It was positioned west of Ometepec, Guerrero, with a focal depth of 24 km (14.9 mi), and was lightly felt in many adjacent areas.
The 2011 Lorca earthquake was a moderate 5.1 Mw earthquake that occurred 6:47 p.m. CEST on 11 May 2011, near the town of Lorca, causing significant localized damage in the Region of Murcia, Spain, and panic among locals, and displacing many from their homes. The quake was preceded by a magnitude 4.4 (Mw) foreshock at 17:05, that inflicted substantial damage to many older structures in the area, including the historical Espolón Tower of Lorca Castle, the Hermitage of San Clemente and the Convent of Virgen de Las Huertas. Three people were killed by a falling cornice. A total of nine deaths have been confirmed, while dozens are reported injured. The earthquake was the worst to hit the region since a 5.0 Mw tremor struck west of Albolote, Granada in 1956.
The 2012 Guerrero–Oaxaca earthquake struck southern Mexico with a moment magnitude of 7.4 at 12:02 local time on Tuesday, 20 March. Its epicenter was near Ometepec, in the border between the states of Guerrero and Oaxaca. With a shallow focus of 15 to 20 km, the earthquake caused strong shaking over a large area along the Oaxaca–Guerrero border and the adjacent Pacific coastline. Significant tremors were felt in areas up to several hundred kilometers away, including Mexico City and also in Guatemala. Two people were killed and over 30,000 houses were damaged or destroyed.
In May 2012, two major earthquakes struck Northern Italy, causing 27 deaths and widespread damage. In Italy they became known as the 2012 Emilia earthquakes.
The 2012 Costa Rica earthquake occurred at 08:42 local time on September 5. The epicenter of the 7.6 Mw earthquake was in the Nicoya Peninsula, 11 kilometers east-southeast of Nicoya. A tsunami warning was issued shortly afterwards, but later cancelled. Two people are known to have died, one from a heart attack and another, a construction worker, crushed by a collapsing wall. It was the second strongest earthquake recorded in Costa Rica's history, following the 1991 Limon earthquake.
The 2012 Guatemala earthquake occurred on November 7 at 10:35:45 local time. The shock had a moment magnitude of 7.4 and a maximum Mercalli Intensity of VII. The epicenter was located in the Pacific Ocean, 35 kilometres (22 mi) south of Champerico in the department of Retalhuleu. The region is one of many earthquakes, where the Cocos Plate is being subducted along the Middle America Trench beneath the North American and the Caribbean Plates, near their triple junction.
The 2013 Bohol earthquake occurred on October 15 at 8:12:31 PST in Bohol, an island province located in Central Visayas, Philippines. The magnitude of the earthquake was recorded at Mw 7.2, with epicenter 6 kilometres (3.7 mi) S 24° W of Sagbayan, and its depth of focus was 12 kilometres (7.5 mi). It affected the whole Central Visayas region, particularly Bohol and Cebu. The quake was felt in the whole Visayas area and as far as Masbate island in the north and Cotabato provinces in southern Mindanao.
The 1983 Popayán earthquake occurred on 31 March in Popayán, Colombia. It had a magnitude of at least 5.5 with an epicenter south west of Popayán at a depth of 12–15 kilometers (7.5–9.3 mi). The earthquake killed 267 people and resulted in the passing of new laws requiring earthquake resistant building materials in zones at risk of tremors.
A series of major earthquakes struck Central Italy between the Marche and Umbria regions in October 2016. The third quake on 30 October was the largest in Italy in 36 years, since the 1980 Irpinia earthquake.
The 2017 Chiapas earthquake struck at 23:49 CDT on 7 September in the Gulf of Tehuantepec off the southern coast of Mexico, near state of Chiapas, approximately 87 kilometres (54 mi) southwest of Pijijiapan, with a Mercalli intensity of IX (Violent). The magnitude was estimated to be Mw 8.2.
The 2017 Puebla earthquake struck at 13:14 CDT on 19 September 2017 with an estimated magnitude of Mw 7.1 and strong shaking for about 20 seconds. Its epicenter was about 55 km (34 mi) south of the city of Puebla. The earthquake caused damage in the Mexican states of Puebla and Morelos and in the Greater Mexico City area, including the collapse of more than 40 buildings. 370 people were killed by the earthquake and related building collapses, including 228 in Mexico City, and more than 6,000 were injured.