1746 Lima–Callao earthquake

Tectonic setting

Peru lies above the convergent boundary where the Nazca plate is subducting beneath the South American plate at a rate of 61 mm per year. It has been the location for many large and damaging earthquakes since historical records began, most of which triggered devastating tsunamis. The southern segment of the Peruvian part of this plate boundary is affected by the presence of the Nazca aseismic ridge, on the downgoing plate. It also marks a major change in the subduction geometry between 'flat-slab' subduction to the northwest and normally dipping subduction to the southeast. The ridge appears to act as a barrier to rupture propagation, reducing the potential earthquake magnitude. The 1746 earthquake is interpreted to be a megathrust event that ruptured the whole of the northern segment of the plate interface within this zone.

Earthquake

The earthquake, with an estimated magnitude of 8.6–8.8 Mw, There were at least 200 aftershocks observed in the first 24 hours after the mainshock, out of a total of 1,700 recorded in the following 112 days, although they caused no further casualties or significant damage.

Damage

Earthquake

The earthquake completely destroyed the city of Lima in 3–4 minutes, and also destroyed Callao and everything else along the central Peruvian coast from Chancay in the north to Cañete in the south. In Lima, all offices and all 74 churches were either damaged or destroyed, leaving just 25 of the original 3,000 houses standing. Only 1,141 out of the population of 60,000 died in Lima from the earthquake shaking, despite the amount of damage. This is attributed to the intensity of the shaking increasing as the earthquake went on, giving the inhabitants the chance to abandon their homes and seek open spaces. The total number of casualties, including those from the tsunami, was almost 6,000, although some chroniclers give higher figures for Lima, partly due to the inclusion of the effects of subsequent epidemics.

Tsunami

The earthquake triggered a tsunami, which reached the coast half an hour following the shock, causing great damage at all Peruvian ports. Callao was the worst affected, with a 24-meter runup, and 5 kilometer inundation that destroyed all 23 vessels that were in its harbor. Callao's walls were destroyed and the city was inundated, killing most of the 5–6,000 inhabitants, leaving less than two hundred survivors. Eyewitness accounts indicate two waves, the first of which was up to 80 ft high. Four of the boats were carried across the ruined port and thrown up to nearly a mile inland, including the warships Fermín and San Antonio. The port city of Pisco was destroyed, despite having been rebuilt further inland after the devastating tsunami that accompanied the 1687 Peru earthquake. The tsunami was also noticed at Acapulco, Mexico. Other particularly devastating tsunamis have occurred in Peru in 1586, 1604, and 1868.

Aftermath

The rebuilding of Lima was planned by Jose Antonio Manso de Velasco then the viceroy of Peru, with the help of the French mathematician Louis Godin. A key part of these proposals was to restrict buildings to a single storey and widen the roads, but the plans were diluted following opposition from groups within the city and second floors were allowed as long as they used bamboo in their construction rather than adobe bricks.

In 1817, 70 years after the earthquake and the tsunami, the Russian-American Company employee, head of the Sitka office, Kiril Timofeevich Khlebnikov (1784–1838) visited Callao. His account of the events of what happened on 28 October 1746 may have slight factual mistakes, but he is generally considered a good witness of things he saw with his own eyes, and his attitude in writing history is characterised as sober and realistic. It is also known that he kept a diary. Khlebnikov wrote in his memoirs:

After this terrible devastation, bodies of the drowned were thrown to the beach by the waves of the ocean, and later they were collected and stacked in the cellars. In time the bodies decomposed, the cellars collapsed, and piles of skulls and bones came to the surface from the ruins. We stood for a long time in the Callao harbor in 1817, and we often took walks to the surrounding area, and with feelings of pity we looked upon the earthly remains of such a large group of people, people like us, scattered on the ground, to the shame of coming generations. When facing a sight such as this, views on the vanity of the world and all worldly things appear in our mind completely different from the views we earlier had when floating with the whirl of these vanities. |Kiril Timofeevich Khlebnikov}}

Remembrance

Because the mural of the Lord of Miracles survived the earthquake intact, it became a special object of veneration in the city. There is an annual procession in which the image is carried through the streets of Lima, and it is customary for the faithful to wear purple during the month of October in commemoration.

References

References

1. Chlieh, M.. (2011). "Interseismic Coupling and Seismic Potential along the Central Andes Subduction Zone". Journal of Geophysical Research.
2. "Earthquakes of Peru". United States Geological Survey.
3. A contemporary description of the events by one of the few survivors, the [[Francisco José de Ovando, 1st Marquis of Brindisi. Marqués de Ovando]], is to be found [https://archive.org/details/semanarioerudito1618vall/page/n247/mode/2up here]
4. Sladen, A.. (2010). "Source model of the 2007 Mw 8.0 Pisco, Peru earthquake: Implications for seismogenic behavior of subduction megathrusts". Journal of Geophysical Research.
5. Dorbath, L.. (1990). "Assessment of the size of large and great historical earthquakes in Peru". Bulletin of the Seismological Society of America.
6. National Geophysical Data Center / World Data Service (NGDC/WDS): NCEI/WDS Global Significant Earthquake Database. NOAA National Centers for Environmental Information. (1972). "Significant Earthquake Information". NOAA National Centers for Environmental Information.
7. National Geophysical Data Center. "Comments for the Tsunami Event".
8. Walker, C.F.. (2008). "Shaky Colonialism: The 1746 Earthquake-Tsunami in Lima, Peru, and Its Long Aftermath". Duke University Press.
9. Okal, E.A.. (2006). "Evaluation of Tsunami Risk from Regional Earthquakes at Pisco, Peru". Bulletin of the Seismological Society of America.
10. USC Tsunami Research Group. "Historical Tsunamis". University of Southern California.
11. GAR. (2011). "Box 1.1 A tale of two disasters". 2011 Global Assessment Report on Disaster Risk Reduction Revealing Risk, Redefining Development.
12. Svetlana G. Fedorova in Kiril Timofeevich Khlebnikov: ''Русская Америка в «записках» К. Т. Хлебникова: Ново-Архангельск.'' Наука, М., 1985, с. 7, 14. / ''Notes on [[Russian America]]. Part I: [[Sitka, Alaska. Novo-Arkhangel’sk]],'' p. xvi, xxii. Edited with an introduction by Svetlana G. Fedorova. Translated from the Russian edition of 1985 by Serge Lecomte and [[Richard Pierce (historian). Richard A. Pierce]]. [[The Limestone Press]], 1994.
13. Кирилъ Тимоѳеевичъ Хлѣбниковъ: "Взглядъ на полвѣка моей жизни", ''Сынъ отечества'', 1836, часть CLXXV, p. 371–372.
14. (2003). "Culture and Customs of Peru". Greenwood Publishing Group.