Very strong and shallow earthquake measuring M 6.4 (downgraded from 6.8) on the Richter scale hit Guerrero, Mexico on May 8, 2014 at 17:00 UTC.
Epicenter was located 15 km (9 miles) WSW of Tecpan de Galeana, 31 km (19 miles) NW of Atoyac de Alvare and 277 km (172 miles) SW of Mexico City, Mexico.
There are about 765 359 people living within 100 km radius.
USGS issued green alert for shaking-related fatalities and economic losses. There is a low likelihood of casualties and damage.
Overall, the population in this region resides in structures that are a mix of vulnerable and earthquake resistant construction. The predominant vulnerable building types are mud wall and unreinforced brick masonry construction. Recent earthquakes in this area have caused secondary hazards such as landslides that might have contributed to losses.
USGS reader from Mexico City (277 km from epicenter) wrote: "The quake in itself was not as bad as the one two weeks ago. I got worried because it lasted longer… at least it seemed like it. Nothing damaged, but some things fell of the contraption I use to dry my dishes."
Their reader from Morelia wrote (265 km from epicenter): "Very strong shaking. Felt stronger than the 7.2 in the same area 4/18/14. Lasted several minutes. Existing cracks in walls grew larger. Paint chips fell from roof."
Seismotectonics of Mexico
Located atop three of the large tectonic plates, Mexico is one of the world's most seismically active regions. The relative motion of these crustal plates causes frequent earthquakes and occasional volcanic eruptions. 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.
The area west of the Gulf of California, including Mexico's Baja California Peninsula, is moving northwestward with the Pacific plate at about 50 mm per year. Here, the Pacific and North American plates grind past each other creating strike-slip faulting, the southern extension of California's San Andreas fault. In the past, this relative plate motion pulled Baja California away from the coast forming the Gulf of California and is the cause of earthquakes in the Gulf of California region today.
Mexico has a long history of destructive earthquakes and volcanic eruptions. In September 1985, a magnitude 8.1 earthquake killed more than 9,500 people in Mexico City. In southern Mexico, Volcán de Colima and El Chichón erupted in 2005 and 1982, respectively. Paricutín volcano, west of Mexico City, began venting smoke in a cornfield in 1943; a decade later this new volcano had grown to a height of 424 meters. Popocatépetl and Ixtaccíhuatl volcanos ("smoking mountain" and "white lady", respectively), southeast of Mexico City, occasionally vent gas that can be clearly seen from the City, a reminder that volcanic activity is ongoing. In 1994 and 2000 Popocatépetl renewed its activity forcing the evacuation of nearby towns, causing seismologists and government officials to be concerned about the effect a large-scale eruption might have on the heavily populated region. Popocatépetl volcano last erupted in 2010. (USGS) More information on regional seismicity and tectonics
Featured image: USGS
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