1939 Chillán earthquake

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1939 Chillán earthquake
1939 Chillán earthquake is located in South America
Chillán
Chillán
1939 Chillán earthquake
Date January 24, 1939 (1939-01-24)
Magnitude 8.3 MS [1][2]
Depth 60;[1] 80-100[3] km
Epicenter 36°12′00″S 72°12′03″W / 36.20000°S 72.20083°W / -36.20000; -72.20083Coordinates: 36°12′00″S 72°12′03″W / 36.20000°S 72.20083°W / -36.20000; -72.20083 [1]
Areas affected Chillán, Chile
Casualties ~28,000

The 1939 Chillán earthquake occurred in south-central Chile on 24 January and had a surface wave magnitude of 8.3.[1][2] With a death toll of around 28,000,[4] compared to the 2,231 – 6,000 (official estimates vary greatly)[5][6] of the Great Chilean Earthquake of 1960, it is the single deadliest earthquake in Chile.

Earthquake[edit]

At 23:33, the earth began to shake strongly underneath Chillán, destroying more than half of it, at around 3,500 homes (including the recently constructed Casa Rabié) which then was in the city. After this quake, others came, which, although they were less intense, left the city completely destroyed. Until then, the Cathedral of Chillán had been one of the principal buildings of the area, but it was completely destroyed by the earthquake. The church that was built to replace the one destroyed in the earthquake was designed specifically to withstand future earthquakes.

Some minutes after the earthquake in Chillán, at 23:35, Concepción was violently hit. Almost all of the buildings (around 95% of the houses) were completely destroyed. There was a show going on in the theater of Concepción at the moment of the earthquake. The large chandelier that was suspended in the ceiling of the theater started to swing. The people inside were terrified, so they fled down the stairs, but the spiral staircase cracked, causing many people to fall into the gap. In the intersection of O’Higgins and Aníbal Pinto avenue the bodies accumulated, which were later brought to the cemetery, and interred in large strips of land.

The electricity was cut in all of the city and tens of fires were reported in various points of the city. The potable water supply was also seriously affected. The material damages in all of the city were evaluated to be more than three thousand million pesos. Various emblematic buildings of the city were destroyed, like the central market, Correos de Chile, but the most emblematic was the plaza of independence, which was seriously damaged. Its two towers leaned dangerously, and because of this they had to be demolished. Another building that was affected was the first building of the old Central Station of Concepción. In 1941, the construction of a second station building began.

Geology[edit]

The community of Chillán is situated in the continental territory of Chile. The city of Chillán was built on a tectonic structure at the end of the Tertiary Period in the part of the Longitudinal Valley which is identified with the Central level. Morphologically, the land corresponds to an alluvial plain, which predominates with fluvioglacial sediments, conformed during the Cuaternario by the action of the Rivers nuble and Cato in the north and the River Chillán in the south, both tributary streams of the large drainage basin of Itata. The natural flow of the enclave of Chillán is confirmed by later geological studies, found the root of the earthquake of 1939, when a prospection of more than 80 meters was carried out, without finding the bedrock.

Response[edit]

In the aftermath of the disastrous 1939 Chillán earthquake the government created CORFO (Spanish acronym for Production Development Corporation) to help in the reconstruction of the country and to industrialize the country, mechanize the agriculture and help mining to develop.[7][8]

Gallery[edit]

References[edit]

  1. ^ a b c d Servicio Sismológico Universidad de Chile, "Sismos importantes y/o destructivos desde (1570 - a la fecha) – Important and/or destructive earthquakes (1570-present)" (Spanish)
  2. ^ a b "Worst of the Century". TIME. 23 September 1985. Retrieved 24 January 2011.  (subscription required)
  3. ^ Beck, S.; Barrientos, S.; Kausel, E.; Reyes, M. (1998). "Source characteristics of historic earthquakes along the central Chile subduction Askew et alzone". Journal of South American Earth Sciences 11 (2). doi:10.1016/S0895-9811(98)00005-4. ISSN 0895-9811. 
  4. ^ "Earthquakes with 1,000 or More Deaths since 1900". Earthquake Hazards Program. USGS Earthquake.usgs.gov. 30 November 2012. Retrieved 9 January 2013. 
  5. ^ "The Largest Earthquake in the World – Articles". U.S. Geological Survey. Archived from the original on 7 January 2007. Retrieved 9 January 2012. 
  6. ^ "Emergency & Disasters Data Base". Centre for Research on the Epidemiology of Disasters (CRED). Archived from the original on 21 June 2007. Retrieved 9 January 2012.  (Exact data location missing from URL)
  7. ^ "Ley que crea la CORFO", Memoria histórica cámara de diputados (in Spanish), retrieved June 30, 2013 
  8. ^ "Cordporación de Fomento a la Producción (1939-1952)", Memoria chilena (in Spanish), retrieved June 30, 2013