Seismic waves, which are the waves of energy that travel through the Earth during an earthquake, typically occur at frequencies below the range of human hearing. Most seismic waves are low-frequency and fall into the infrasound range, which means they have frequencies below 20 hertz. Since the human ear is not sensitive to these very low frequencies, people generally CANNOT HEAR the seismic waves DIRECTLY. However, there are instances where individuals near the epicenter of a strong earthquake r
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Seismic waves, which are the waves of energy that travel through the Earth during an earthquake, typically occur at frequencies below the range of human hearing. Most seismic waves are low-frequency and fall into the infrasound range, which means they have frequencies below 20 hertz. Since the human ear is not sensitive to these very low frequencies, people generally CANNOT HEAR the seismic waves DIRECTLY. However, there are instances where individuals near the epicenter of a strong earthquake r
549 viewsDec 4, 2023
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