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COUNTRY PROFILE

Earthquakes in Peru

Peru sits along the western margin of South America where the Nazca Plate subducts beneath the South American Plate, generating powerful earthquakes and shaping the Andes. Andean seismicity makes Peru one of the most earthquake-prone countries in the Americas.

1

Events this week

M2.0+

M4.5

Largest this week

28

Events this year

M5.0+

62

Historic M7+ events

Since 1900

Why Peru has so many earthquakes

The Nazca Plate subducts beneath Peru at a rate of approximately 6-7 centimeters per year, making the Peru-Chile Trench one of the most seismically active convergent boundaries on Earth. This subduction generates earthquakes at a wide range of depths, from shallow coastal events to deep tremors hundreds of kilometers beneath the Andes.

Peru's seismicity is further complicated by the geometry of the subducting plate. Beneath central Peru, the Nazca Plate subducts at an unusually shallow angle — a phenomenon known as flat-slab subduction — which transmits tectonic stress far inland and produces earthquakes deep within the continental interior. This means that seismic hazard in Peru is not confined to the coast but extends across the entire width of the Andes.

The country's vulnerability is heightened by the prevalence of adobe and unreinforced masonry construction, particularly in the Andean highlands and older urban neighborhoods. Peru has experienced some of the deadliest earthquakes in South American history, and the combination of tectonic setting, construction practices, and mountainous terrain — which can trigger devastating landslides and avalanches — creates a compounding risk.

Recent earthquakes

4.5

19 km E of Coayllo, Peru

April 9, 2026

Peru's most significant earthquakes

Peru's earthquake history includes some of the most catastrophic seismic events in the Americas. The combination of powerful subduction earthquakes, vulnerable construction, and unstable mountain terrain has produced disasters of staggering scale.

7.9

The Ancash Earthquake

May 31, 1970

On the afternoon of May 31, 1970, a magnitude 7.9 earthquake struck off the coast of Peru's Ancash department. The earthquake itself was devastating, destroying towns and villages across a wide area of the Peruvian highlands. But it was a secondary effect that transformed this disaster into one of the deadliest in the history of the Americas: the shaking dislodged a massive section of the north face of Mount Huascaran, Peru's tallest peak at 6,768 meters, sending an enormous avalanche of rock, ice, and mud thundering down the mountainside at speeds exceeding 300 kilometers per hour.

The avalanche obliterated the town of Yungay, burying it under as much as 15 meters of debris. Of the town's approximately 25,000 inhabitants, only a few hundred survived — those who happened to be on high ground or in the cemetery, which sat on a small hill above the town. The neighboring town of Ranrahirca was also largely destroyed. Across the entire affected region, an estimated 70,000 people perished, 140,000 were injured, and over 500,000 were left homeless. It remains the deadliest earthquake-related disaster in South American history.

The 1970 Ancash earthquake fundamentally changed how scientists and disaster planners think about compound hazards — the cascading chain of events where an earthquake triggers landslides, avalanches, or floods that prove far more destructive than the shaking itself. The Huascaran avalanche became a landmark case study in disaster science. For Peru, the tragedy spurred the creation of new civil defense institutions and the beginning of efforts to map and mitigate landslide risk in the Andes, work that continues to this day.

8.0

The Pisco Earthquake

August 15, 2007

On the evening of August 15, 2007, a magnitude 8.0 earthquake struck the central coast of Peru, centered near the city of Pisco approximately 200 kilometers south of Lima. The shaking lasted nearly two minutes and was felt throughout the capital and across much of the country. In Pisco and the surrounding Ica region, the destruction was severe — adobe buildings, which constitute a large percentage of the housing stock in Peru's coastal cities, collapsed en masse. The historic San Clemente cathedral in Pisco fell during an evening service, killing many worshippers.

The earthquake killed approximately 520 people and left over 300,000 homeless. While the death toll was far lower than the 1970 disaster, the Pisco earthquake revealed the continuing vulnerability of Peruvian cities to seismic shaking. The city of Ica, a regional capital of over 200,000 people, suffered extensive damage. Infrastructure failures, including the collapse of the Pan-American Highway in several locations, hampered rescue and relief operations in the critical first hours.

The 2007 earthquake served as a wake-up call for Peru's seismic preparedness, particularly regarding the vulnerability of adobe construction. In the years since, Peru has invested in strengthening building codes and developing seismic reinforcement techniques for traditional construction. The disaster also highlighted the need for improved tsunami warning capabilities along the Peruvian coast, as the earthquake generated a modest tsunami that added to the disruption in coastal communities.

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