1957 Guerrero earthquake

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1957 Guerrero earthquake
009520-003 DANOS DEL SISMO DEL DIA 28 JULIO 29 1957 (30953952424).jpg
Nike's sculpture (Winged Victory) fallen after the earthquake.
Mexico Guerrero location map.svg
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Mexico relief location map.jpg
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UTC  time1957-07-28 08:40:12
ISC  event 886928
USGS-ANSS ComCat
Local date28 July 1957
Local time2:40
Duration90 seconds [1]
Magnitude7.6 Mw
Depth37.8 km (23 mi)
Epicenter 17°03′18″N99°05′31″W / 17.055°N 99.092°W / 17.055; -99.092
Areas affectedMexico
Total damageUS$ 25 million
Max. intensity MMI VII (Very strong)
TsunamiMax. wave height = 1.3 m [2]
Casualties54–160 dead

The 1957 Guerrero earthquake occurred on 28 July at 08:40 UTC. [3] It had a magnitude of 7.6 Mw and a maximum perceived intensity of VII (very strong) on the Modified Mercalli intensity scale. Mexico City and Chilpancingo were particularly badly affected. It caused the deaths of between 54 and 160 people. [4] A small tsunami was triggered but caused little damage. [2]

Contents

Tectonic setting

The state of Guerrero lies adjacent to part of the Middle America Trench where the Cocos Plate is being subducted beneath the North American Plate. The convergence between these plates at this location is about 65 mm per year. There have been many large and destructive earthquakes in the past, such as the M 7.6 1911 Guerrero earthquake. [5] The Guerrero seismic gap is a ca. 200 km long segment of the subduction interface, which has not had a large earthquake since the 1911 event. Although several slow earthquakes have been observed in that time interval, an earthquake in the range M 7.9–8.0 could still be expected within the Guerrero gap. [6]

Earthquake

The earthquake originally had an estimated magnitude of 7.9 Ms . [4] This was recalculated by the International Seismological Centre in their ISC-GEM catalogue as 7.6 Mw. [3] The duration of strong shaking was recorded as 90 seconds in Mexico City. [1] The earthquake is thought to have ruptured the plate interface at the southeastern end of the Guerrero seismic gap. [6]

Damage

The greatest damage was observed in Mexico City, where many buildings were destroyed. Chilpancingo was also badly affected with 90% of buildings being damaged. The towns of Ayutla, Chilapa, Huamuxtitlán, San Luis Acatlan, San Marcos, Tlapa and Huitzuco all sustained significant damage. [4]

See also

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References

  1. 1 2 Rosenblueth, E. (1960). "The Earthquake of 28 July 1957 in Mexico City" (PDF). Proc. 2nd World Conference on Earthquake Engineering. pp. 359–379.
  2. 1 2 National Centers for Environmental Information. "Comments on the 1957 Guerrero tsunami" . Retrieved 4 October 2019.
  3. 1 2 ANSS. "Guerrero 1957: M 7.6 - Guerrero, Mexico". Comprehensive Catalog. U.S. Geological Survey. Retrieved 4 October 2019.
  4. 1 2 3 National Centers for Environmental Information. "Comments for the 1957 Guerrero earthquake" . Retrieved 4 October 2019.
  5. ANSS. "Guerrero 2014: M 7.2 - 33km ESE of Petatlan, Mexico". Comprehensive Catalog. U.S. Geological Survey. Retrieved 5 October 2019.
  6. 1 2 Lowry, A.R.; Larson, K.M.; Kostoglodov, V.; Samchez, O. (2005). "The fault slip budget in Guerrero, southern Mexico". Geophysical Journal International. 200: 1–15.