Harman Patil

1970 Ancash earthquake

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Origin time  15:23:29 local
Magnitude  7.9 Mw
Areas affected  Peru
Date  31 May 1970
Duration  ~ 45 seconds
Depth  45 km (28 mi)
Max. intensity  VIII (Severe)
1970 Ancash earthquake Top 10 Deadliest Earthquakes In History
Similar  2007 Peru earthquake, 1746 Lima–Callao earthquake, 1976 Guatemala earthquake, 1972 Nicaragua earthquake, 2001 southern Peru eart

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The 1970 Ancash earthquake (also known as the Great Peruvian earthquake) occurred on 31 May off the coast of Peru in the Pacific Ocean at 15:23:29 local time. Combined with a resultant landslide, it was the worst catastrophic natural disaster in the history of Peru. Due to the large amounts of snow and ice included in the landslide and its estimated 66,794 to 70,000 casualties, it is also considered to be the world's deadliest avalanche.

Contents

Earthquake

1970 Ancash earthquake thegeosphere Ancash Peru

The undersea earthquake struck on a Sunday afternoon and lasted about 45 seconds. The shock affected the Peruvian regions of Ancash and La Libertad. The epicenter was located 35 km (22 mi) off the coast of Casma and Chimbote on the Pacific Ocean, where the Nazca Plate is being subducted by the South American Plate. It had a moment magnitude of 7.9 and a maximum Mercalli intensity of VIII (Severe).

Damage

1970 Ancash earthquake 1970 Great Peruvian Earthquake RIP Yungay

The earthquake affected an area of about 83,000 km², an area larger than Belgium and the Netherlands combined, in the north central coast and the Sierra (highlands) of the Ancash Region and southern La Libertad Region. Reports of damage and casualties from Tumbes to Pisco and Iquitos in the east. Damage and panic scenes were reported in some parts of Ecuador. Tremors were felt too in western and central Brazil.

1970 Ancash earthquake httpsuploadwikimediaorgwikipediacommonsthu

It was a system-wide disaster, impacting such a widespread area that the regional infrastructure of communications, commerce, and transportation was destroyed. Economic losses surpassed half a billion US dollars. Cities, towns, villages as well as the homes, industries, public buildings, schools, electrical, water, sanitary and communications facilities on them were seriously damaged or destroyed.

Areas hard hit were the coastal towns and cities of Chimbote (the largest city in Ancash), Casma, Supe and Huarmey; but the Andean valley known as the Callejón de Huaylas suffered the most intense and sweeping damage, with the regional capital, Huaraz, as well as Caraz and Aija being partially destroyed. Trujillo, the country's third largest city, and Huarmey suffered minor damage.

In Chimbote, Carhuaz and Recuay, about 80% to 90% of buildings were destroyed, affecting about 3 million people.

1970 Ancash earthquake thegeosphere Ancash Peru

The Pan-American highway was also damaged, which made the arrival of humanitarian aid difficult. The Cañón del Pato hydroelectricity generator was damaged by the Santa River and the railway connecting Chimbote with the Santa Valley was left unusable on 60% of its route.

The Peruvian government has forbidden excavation in the area where the town of Yungay is buried, declaring it a national cemetery. The children who survived in the oca stadium were resettled around the world. In 2000, the tragedy inspired the government to declare 31 May as Natural Disaster Education and Reflection Day.

Every 31 May, many schools of Peru practice an earthquake drill to commemorate this disaster.

Landslide

The northern wall of Mount Huascarán was destabilized, causing a rock, ice and snow avalanche and burying the towns of Yungay and Ranrahirca. The avalanche started as a sliding mass of glacial ice and rock about 910 metres (2,990 ft) wide and 1.6 km (1 mile) long. It advanced about 18 kilometres (11 mi) to the village of Yungay at an average speed of 280 to 335 km per hour. The fast-moving mass picked up glacial deposits and by the time it reached Yungay, it is estimated to have consisted of about 80 million m³ of water, mud and rocks.

References

1970 Ancash earthquake Wikipedia


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