1973 Veracruz earthquake

The 1973 Veracruz earthquake, also known as El Terremoto de Orizaba, occurred at 3:50 a.m. local time (9:50 GMT) on August 28, with the epicenter located in the vicinity of Serdán in the Mexican state of Puebla. It registered 7.0 on the Richter magnitude scale and had a maximum perceived intensity of VIII (Severe) on the Mercalli intensity scale. The effects of the earthquake were felt in the Mexican states of Veracruz and Puebla in southeast Mexico.

1973 Veracruz earthquake
UTC time1973-08-28 09:50:41
ISC event757676
USGS-ANSSComCat
Local dateAugust 28, 1973 (1973-08-28)
Local time3:50 a.m.
Duration1–2 minutes[1]
Magnitude7.0 ML[2]
Depth84 km[3]
Epicenter18.23°N 96.61°W / 18.23; -96.61[4]
Areas affectedMexico
Total damageSevere[5]
Max. intensityVIII (Severe)[3]
TsunamiNo
Casualties539–1,000 dead[6]
thousands injured[6]

Geography

The area that was damaged in Veracruz is tropical and mountainous; Pico de Orizaba, Mexico's tallest peak, is located there. The earthquake occurred during the rainy season, with heavy rain coming down before and after the event making search and rescue difficult. Serdán is located in the rain shadow of the mountainous area and has a more arid climate.[7]

Past events

Mexico's southwest coast is much more seismically active than the southeast area near Orizaba. Earthquakes there have been relatively infrequent. The last prior strong event in the region was on June 17, 1928, when a magnitude-7.8 event occurred south of Serdán. However, the area 100 to 300 kilometers south of Serdán does see more very strong earthquakes, with three events over magnitude 7 in 1928 alone.[8]

Damage

There was extensive damage, leaving hundreds dead and widespread devastation, in several cities in Puebla. The death toll was at least 600, with as many as 1,200 dead, and 212 casualties alone in the small Ciudad Serdán.[9] Major cities affected were Ciudad Serdán, Orizaba, Ixtaczoquitlán, Córdoba, Ciudad Mendoza, Zongolica, Rio Blanco, and Acutzingo.

In Orizaba, a twelve-story apartment building collapsed as result of the earthquake. Many of the occupants, up to 100, were sleeping at the time, and this was the number proclaimed dead at that site.[10]

This event was the most disastrous earthquake in Puebla until the 1999 Tehuacán earthquake.[3]

See also

References
  1. Irvine 1973, p. 6
  2. Irvine 1973, p. 1
  3. Meehan 1974, p. 1
  4. Engdahl, E. R.; Vallaseñor, A. (2002). "Global seismicity: 1900–1999" (PDF). International Handbook of Earthquake & Engineering Seismology. Part A, Volume 81A (First ed.). Academic Press. p. 682. ISBN 978-0124406520.
  5. National Geophysical Data Center / World Data Service (NGDC/WDS) (1972), Significant Earthquake Database (Data Set), National Geophysical Data Center, NOAA, doi:10.7289/V5TD9V7K
  6. USGS (September 4, 2009), PAGER-CAT Earthquake Catalog, Version 2008_06.1, United States Geological Survey
  7. Irvine 1973, pp. 4, 6
  8. Irvine 1973, pp. 4, 5
  9. Frohlich, Cliff (2006). Deep earthquakes. Cambridge University Press. p. 479. ISBN 978-0-521-82869-7.
  10. "12-Story Apartment Collapses in Temblor; 100 Occupants Perish". Los Angeles Times. August 29, 1973.

Sources

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