- Also called:
- Michoacán earthquake of 1985
- Date:
- September 19, 1985
Mexico City earthquake of 1985
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What was the Mexico City earthquake of 1985?
The Mexico City earthquake occurred on the morning of September 19, 1985, at 7:18 am. The magnitude-8.0 quake struck off the coast of the state of Michoacán approximately 200 miles (320 km) from Mexico City, with the epicenter along the Middle America Trench, part of the volatile Circum-Pacific Belt.
The earthquake caused widespread destruction, particularly in Mexico City, due to its construction on the former bed of Lake Texcoco, where loose sediments amplified the shock waves. Buildings of 5 to 15 stories were most affected, with over 400 collapsing. The disaster was compounded by power outages and communication failures. Local residents led rescue efforts, and while official estimates placed the death toll at 10,000, journalists speculated it was much higher.
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When and where did the earthquake happen?
The Mexico City earthquake occurred on September 19, 1985. The magnitude-8.0 quake's epicenter was located off the coast of the Mexican state of Michoacán, approximately 200 miles (320 km) from Mexico City. The destruction was concentrated in Mexico City because it was constructed on the dry bed of Lake Texcoco. The loose sediments amplified the shock waves, and buildings of 5 to 15 stories were most affected.
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How strong was the earthquake?
The Mexico City earthquake of 1985 was a severe earthquake that occurred on September 19, 1985. The magnitude-8.1 quake's epicenter was off the coast of the Mexican state of Michoacán, approximately 200 miles (320 km) from Mexico City. The destruction was concentrated in Mexico City because the city's central area was constructed on the dry bed of the drained Lake Texcoco. The loose lacustrine sediments amplified the shock waves.
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What kind of damage did the earthquake cause?
The Mexico City earthquake of 1985 caused widespread destruction, particularly in Mexico City, due to its location on the dry bed of Lake Texcoco, where loose sediments amplified the seismic waves. Over 400 buildings collapsed, and thousands more sustained damage. The earthquake disrupted essential services, causing power outages that affected public transit and traffic lights, and it also damaged the telephone system, leaving the city incommunicado for days. Approximately 250,000 people lost their homes. The destruction of major hospitals further complicated medical treatment for the tens of thousands injured.
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How did the earthquake affect people living in Mexico City?
The Mexico City earthquake of 1985 caused widespread death, injuries, and catastrophic damage in Mexico’s capital. The earthquake led to the collapse of over 400 buildings and damage to thousands more.
The loss of electricity compounded the chaos in Mexico City, leaving the capital without public transit or working traffic lights. Damage to the telephone system left the city incommunicado for several days.
Local residents led relief efforts, excavating neighbors and colleagues from fallen buildings and organizing the distribution of needed supplies. Approximately 250,000 people were left without shelter.
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What changes were made in Mexico City as a result of this earthquake?
The 1985 Mexico City earthquake led to significant changes in the city's approach to disaster response and urban planning.
Following the earthquake, the government, with World Bank support, reconstructed or refurbished nearly 100,000 residences by 1988. The government addressed demands from the newly formed political body, Coordinadora Única de Damnificados (CUD), by expropriating destroyed properties and constructing new housing for displaced residents rather than relocating them. This reconstruction plan forced the ruling Institutional Revolutionary Party (PRI) to acknowledge opposition groups.
The earthquake also highlighted the dangers of building on the city's lacustrine subsoil, which amplified the shock waves and caused many buildings to collapse. This awareness likely contributed to later concerns about the region’s precarious geology, especially with the reemergence of volcanic activity in 1994.
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Mexico City earthquake of 1985, severe earthquake that occurred on September 19, 1985, off the coast of the Mexican state of Michoacán, causing widespread death and injuries and catastrophic damage in Mexico’s capital, Mexico City.
The magnitude-8.0 quake occurred at 7:18 am. Many sources place the location of the epicentre in the state of Michoacán—approximately 200 miles (320 km) from Mexico City—in a region of tectonic tension between the North American Plate and the subducting Cocos Plate. Some accounts, however, place the epicentre just off the coast of Michoacán in the Pacific Ocean. The expanse of the subduction zone along which the quake occurred was part of the Middle America Trench, the eastern boundary of the tectonically volatile Circum-Pacific Belt. That expanse was known as the Michoacán seismic gap because seismic energy had been accumulating there since a 1911 earthquake; temblors had occurred on either side during the 1970s. A second tremor of nearly equal magnitude occurred the following evening southeast of the first quake.
Although some damage occurred in Michoacán and surrounding regions—including the state of Jalisco, where nearly 600 adobe houses were reduced to rubble in Ciudad Guzmán—the destruction was concentrated in Mexico City as a result of the unique topography upon which the capital is situated. The central city, constructed on the dry bed of the drained Lake Texcoco, endured the heaviest shaking because loose lacustrine sediments amplified the shock waves. The ground motion in this area measured five times that in the outlying districts, which had different soil foundations. Buildings of 5 to 15 stories were most affected, as their interaction with the shock waves created a harmonic resonance, exacerbating the degree of swaying. More than 400 buildings collapsed, and thousands more were damaged.
The chaos in Mexico City was compounded by the loss of electricity, leaving the capital without public transit or working traffic lights. Though power was restored the day after the first quake, the tremor that evening knocked it out again. Damage to the telephone system rendered the city incommunicado for several days. Furthermore, Mexican Pres. Miguel de la Madrid and his advisers refused to fully deploy the national emergency plan. Some observers interpreted this inaction as a maneuver designed to prevent the military from appreciating political cachet by coordinating the rescue operations. De la Madrid declined early offers of international assistance as well but quickly reversed course, accepting supplies and money from a range of countries coordinated by the United Nations.
In the meantime, relief efforts were led by local residents, who began excavating neighbours and colleagues from fallen buildings and organizing the distribution of needed supplies themselves. Inhabitants of areas less affected by the quake journeyed to the devastated low-income districts composing the central city in order to assist. Though many were extricated from the wreckage alive, official estimates placed the final death toll at 10,000 people. Journalists and other eyewitnesses, however, speculated that several times that number had perished. Medical treatment of the tens of thousands who were injured was hampered by the fact that several of the city’s major hospitals had been damaged.
Approximately 250,000 people were left without shelter. As the government began formulating a reconstruction plan in the weeks following the disaster, these damnificados (literally, the damned), along with existing grassroots organizations, began to coalesce into a powerful political force ultimately known collectively as Coordinadora Única de Damnificados (CUD). De la Madrid and the ruling Institutional Revolutionary Party (PRI) were forced to acknowledge the opposition groups when the significance of their role in organizing the recovery became clear. Foremost among the demands of this newly constituted political body were that, rather than relocating those displaced by the temblor, the government expropriate the destroyed properties and construct new housing for the residents. De la Madrid’s government acceded, and two years later, with the help of World Bank funds, nearly 100,000 residences had been refurbished or newly constructed. The CUD dissolved in 1987 following the achievement of most of its goals, but some of the constituent groups formed the Asamblea de Barrios (Neighbourhood Assembly), which represented the housing interests of low-income residents.




