M 7.4 - 12 km SSW of Santa María Zapotitlán, Oaxaca, Mexico

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SUMMARY

The earthquake measuring 7.4 magnitude occurred on June 23, 2020, at 15:29:05 UTC, located 12 km SSW of Santa María Zapotitlán, Oaxaca, Mexico, at a depth of 26.3 km. This seismic event is attributed to the subduction of the Cocos plate beneath the North American plate, resulting in geological phenomena such as the formation of the Middle American trench and the Cordillera Neovolcánica volcanic region. The discussion highlights the impact of tectonic movements on the region's geology and the importance of monitoring seismic activity.

PREREQUISITES
  • Understanding of tectonic plate movements, specifically the North American and Cocos plates.
  • Knowledge of seismic measurement tools, such as seismometers.
  • Familiarity with geological formations like subduction zones and volcanic arcs.
  • Awareness of earthquake magnitude scales and their implications.
NEXT STEPS
  • Research the geological implications of subduction zones in plate tectonics.
  • Learn about the operation and calibration of seismometers for earthquake monitoring.
  • Explore the characteristics and formation of the Cordillera Neovolcánica volcanic region.
  • Investigate earthquake preparedness and response strategies in seismically active areas.
USEFUL FOR

Geologists, seismologists, emergency management professionals, and anyone interested in understanding the dynamics of earthquakes and volcanic activity in southern Mexico.

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https://earthquake.usgs.gov/earthquakes/eventpage/us6000ah9t/executive
  • 2020-06-23 15:29:05 (UTC)
  • 16.029°N 95.901°W
  • 26.3 km depth
Earthquake in southern Oaxaca near coast.

Most of the Mexican landmass is on the westward moving North American plate. The Pacific Ocean floor south of Mexico is being carried northeastward by the underlying Cocos plate. Because oceanic crust is relatively dense, when the Pacific Ocean floor encounters the lighter continental crust of the Mexican landmass, the ocean floor is subducted beneath the North American plate creating the deep Middle American trench along Mexico's southern coast. Also as a result of this convergence, the westward moving Mexico landmass is slowed and crumpled creating the mountain ranges of southern Mexico and earthquakes near Mexico's southern coast. As the oceanic crust is pulled downward, it melts; the molten material is then forced upward through weaknesses in the overlying continental crust. This process has created a region of volcanoes across south-central Mexico known as the Cordillera Neovolcánica.
https://earthquake.usgs.gov/earthquakes/eventpage/us6000ah9t/region-info

@davenn , did your seismometer register it?
 
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Astronuc said:
@davenn , did your seismometer register it?
Yes, very well, still early morning here. I saw it when I switched on the seismo. computer monitor this morning.
I hadn't had a chance to post a thread before leaving for work

zhi.gif
 
“Cordillera Neovolcánica,” I think I’ve found the perfect name for my next pet labradoodle!
 
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