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Magnitude | Mw 7.5 |
Depth | 12 km |
Epicenter | 15°23′N 96°07′W / 15.38°N 96.12°W / 15.38; -96.12 |
Casualties | 6 |
The 1965 Oaxaca earthquake occurred in Mexico on August 23 at 13:46 with a moment magnitude of 7.5. Five people were reported dead in Mexico City and 1 in Oaxaca. There was an anomalous change in seismic activities before the earthquake. There was a quiescent stage from late 1963 to mid-1964, and it was followed by a renewal of seismic activities before the main shock. This earthquake was a shallow thrust earthquake in the interplate subduction zone, in which the Cocos Plate is subducting beneath the North American Plate.
References
- E. Chael, G. Stewart, "Recent large earthquakes along the Middle America trench and their implications for the subduction process"
- A. Iglesias, S. K. Singh, M. Ordaz, M. A. Santoyo, J. Pacheco, "The seismic alert system for Mexico City: An evaluation of performance and a strategy for its improvement"
- Ohtake, M.; Matumoto, T.; Latham, Gary (1977), "Seismicity gap near Oaxaca, southern Mexico as a probable precursor to a large earthquake" (PDF), Pure and Applied Geophysics, 115, Springer: 375–385
- http://www.geology.wisc.edu/~chuck/PDF/FCM_Oax_GJI08.pdf
- http://www.eri.u-tokyo.ac.jp/seno/Papers/epsl_kato_seno.pdf
← Earthquakes in 1965 → | |
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† indicates earthquake resulting in at least 30 deaths ‡ indicates the deadliest earthquake of the year |