  | |
| UTC time | 1937-07-26 03:47:15 |
|---|---|
| ISC event | 903178 |
| USGS- ANSS | n/a |
| Local date | July 25, 1937 |
| Local time | 21:47 |
| Magnitude | 7.3 Ms |
| Depth | 35 km (22 mi) [1] |
| Epicenter | 18°31′N 95°53′W / 18.52°N 95.88°W [1] |
| Areas affected | Mexico |
| Casualties | 34 |
The 1937 Orizaba earthquake occurred on July 26 at 03:47 UTC, near Orizaba, Veracruz, Mexico. It had a magnitude of 7.3 on the surface wave magnitude scale. [2] Thirty four people were reported dead. [3] Damage was reported in Esperanza, Puebla. This was an intraplate earthquake within the subducting Cocos Plate. [4] [5]
See also
References
- ^ a b 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. 677. ISBN 978-0124406520.
-
^
"Archived copy" (PDF). Archived from
the original (PDF) on 2012-03-24. Retrieved 2011-08-07.
{{ cite web}}: CS1 maint: archived copy as title ( link) - ^ Nava, Alejandro (1998). "I. Introducción". Terremotos. Fondo de Cultura Económica. ISBN 9681657683. Retrieved 8 April 2019.
- ^ http://mahabghodss.net/NewBooks/www/web/digital/nashrieh/bssa/2002/April%2092(3)/1060.pdf[ permanent dead link]
- ^ Lay, T.; Astiz, L.; Kanamori, H.; Christensen, D. H. (1989), "Temporal variation of large intraplate earthquakes in coupled subduction zones" (PDF), Physics of the Earth and Planetary Interiors, 54 (3–4): 258, Bibcode: 1989PEPI...54..258L, doi: 10.1016/0031-9201(89)90247-1, hdl: 2027.42/27966