in 1985, a magnitude 8.1 earthquake hit the pacific coast of mexico. interestingly, low rise and high rise buildings remain standing , while many medium sized buildings collapsed and incurred serious damage. what do you think were the factors that caused this type of destruction?
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The low-frequency waves of an earthquake are amplified by the mud of the lakebed, which in turn, is amplified by the building itself. This causes these buildings to shake more violently than the earthquake proper as the earthquake progresses.
Answer:
Cocos Plate subduction zone
The earthquake occurred in the Pacific Ocean, off the coast of the Mexican state of Michoacán, a distance of more than 350 km (220 mi) from the city, in the Cocos Plate subduction zone, specifically in a section of the fault line known as the Michoacán seismic gap.
Explanation:
ain't sure though