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Earthquakes produce several types of shock waves. The most well known are the P-waves (P for primary or pressure) and the S-waves (S for secondary or shear). In the earth’s crust, P-waves travel at about 6.5 km/sand S-waves move at about 3.5 km/s. The time delay between the arrival of these two waves at a seismic recording station tells geologists how far away an earthquake occurred. If the time delay is, how far from the seismic station did the earthquake occur?

Short Answer

Expert verified

the distance from the seismic station and the earthquake is 250 km.

Step by step solution

01

Identification of the given data

The given data can be expressed below as:

  • The P-waves travel by about 6.5 km/s.
  • The S-waves move by about 3.5 km/s.
  • The time delay amongst the two waves is 33 s.
02

Significance of the Newton’s first law for the occurrence of the earthquake

This law states that an object will continue to be in rest or in motion unless the object is acted by an external force.

The equation of motion along a straight line gives the time required to evaluate the distance of the seismic station from the occurrence of the earthquake.

03

Determination of the distance of the seismic station from the occurrence of the earthquake

Assuming that the earthquake happened at about D km away from the station. However, the P-wave and the S-wave will reach the station in a time of-

tp=Dvpand

ts=Dvs

Hence, the difference in the time of the P-wave and the S-wave is expressed as:

Δt=ts−tp=D1vs−1vp

From the above equation, the distance can be expressed as:

D=∆tvsVpvp-vs

The value ofrole="math" localid="1668401141504" vsandvpare 3.5 km/s and 6.5 km/s respectively. Hence, substituting the values in the above equation, we get-

D=33s×3.5km/s×6.5km/s(6.5−3.5)km/s=250km

Thus, the distance from the seismic station and the earthquake is 250 km.

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