The event
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.
The earthquake
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 in 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 MMI of VIII (Severe).
The shaking damage of the earthquake
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.
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.
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 deadly Yungay and Ranrahirca 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.[6] 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.
The government estimated that around 20,000 people have died due to the landslide.
Every year an In Memoriam through Earthquake drills
Each year around May 31, many schools of Peru practice an earthquake drill to commemorate this disaster.
Can this happen again?
Yes, it can.
Traveling through Ecuador shows many hanging glaciers, even on volcanoes. As volcano eruptions can be better predicted, whole valleys can be evacuated before such a disaster happens again but science is not able yet to predict massive earthquakes and the possible impact on glaciers.