Earthquakes are essentially sound waves-called seismic waves-traveling through the earth. Because the earth is solid, it can support both longitudinal and transverse seismic waves. The speed of longitudinal waves, called P waves, is 8000 m/s. Transverse waves, called S waves, travel at a slower 4500 m/s. A seismograph records the two waves from a distant earthquake. If the S wave arrives 2.0 min after the P wave, how far away was the earthquake? You can assume that the waves travel in straight lines, although actual seismic waves follow more complex routes.

Leypoldon

Leypoldon

Answered question

2022-08-11

Earthquakes are essentially sound waves-called seismic waves-traveling through the earth. Because the earth is solid, it can support both longitudinal and transverse seismic waves. The speed of longitudinal waves, called P waves, is 8000 m/s. Transverse waves, called S waves, travel at a slower 4500 m/s. A seismograph records the two waves from a distant earthquake. If the S wave arrives 2.0 min after the P wave, how far away was the earthquake?
You can assume that the waves travel in straight lines, although actual seismic waves follow more complex routes.

Answer & Explanation

Alaina Mcintosh

Alaina Mcintosh

Beginner2022-08-12Added 16 answers

From the time delay, we can write:
t s t p = t
Knowing that t = d v , we rewrite the formula as
d v S d v P = d ( 1 v P 1 v S ) = t
From this we can find the distance to be
d = v S v P v P v S t = 8000 4500 8000 4500 120 = 1230 k m
Result:
1230 km

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