Respuesta :

annelzajolin1

Answer:

Therefore, the farther a seismic recording station is from the earthquake epicenter the greater will be the difference in time of arrival between the P and S wave. ... For example, a magnitude 5 earthquake produces ten times greater ground motion than a magnitude 4 earthquake

floopdroop

Answer:

Beyond the above earthquakes can only get bigger by having more area on the fault to rupture. As an earthquake continues the rupture moves further and further away from the epicenter and thus dumps less and less energy at the epicenter.

Explanation:

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