Wavelength - how far away did earthquake occur

In summary: So, the P-waves are 60 seconds ahead of the S-waves.(deltaX/Vs) - (deltaX/Vp) = 60In summary, the distance of the earthquake can be calculated by taking the difference between the times it takes for P-waves and S-waves to reach a seismic station and using the formula deltaX = (Vs x Vp / (Vp - Vs)) x 60.
  • #1
mathcrzy
47
0

Homework Statement



Assuming typical speeds of 8.9 km/s and 5.8 km/s for P and S waves, respectively, how far away did the earthquake occur if a particular seismic station detects the arrival of these two types of waves 1.0 min apart?
_____km


Homework Equations



v=(lamba)(f)
1/T=frequncy
lamba=one wave length
T=period

X=same

Vpwave=deltaX/T

Vswave=dletaX/T+60

The Attempt at a Solution



8.9=

5.8=
 
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  • #2
mathcrzy said:
Vpwave=deltaX/T = 8.9 km/sec

Vswave=dletaX/T+60 = 5.8 km/sec

This is basically what you need. Solve the first equation for an expression for T and substitute it into the second equation, so you can eliminate the unknown T. You now have an equation you can solve for deltaX.

[As a check, consider this. Both types of waves started from the same "source". About how much do the P-waves gain on the S-waves each second? How much longer do the S-waves need to make up the difference? How long will it take for the S-waves to be a full minute behind? How far will the P-waves have traveled in that time? The algebraic solution described above is equivalent to answering these questions.]
 
Last edited:
  • #3
Vp=deltaX/T
VpT=deltaX
T=deltaX/Vp

Vs=deltaX/T+60
Vs(T+60)=deltaX
VsT+Vs60=deltaX
T=deltaX-Vs60/Vp

deltaX-Vs60/Vp=deltaX/Vp
deltaX-Vs60=deltaX
deltaX=Vs60

Is this how you solve for deltaX
 
  • #4
mathcrzy said:
Vp=deltaX/T
VpT=deltaX
T=deltaX/Vp

Vs=deltaX/T+60
Vs(T+60)=deltaX
VsT+Vs60=deltaX

You were OK to here. The next line would then be

T = (deltaX - Vs·60)/Vs ,

so from there,

(deltaX - Vs·60)/Vs=deltaX/Vp

(deltaX/Vs) - (deltaX/Vp) = 60

(deltaX) · [ (1/Vs) - (1/Vp) ] = 60

delta X = [ (Vs·Vp) / (Vp - Vs) ] · 60
 
  • #5
i got the answer but just wondering how you got from:

(deltaX - Vs·60)/Vs=deltaX/Vp

to

(deltaX/Vs) - (deltaX/Vp) = 60
 
  • #6
(deltaX - Vs·60)/Vs = deltaX/Vp

(deltaX)/Vs - (Vs·60)/Vs = deltaX/Vp

(deltaX)/Vs - (60) = deltaX/Vp

(deltaX/Vs) - (deltaX/Vp) = 60

In fact, you could really start right from here because this just says that the difference between the time it takes the S-waves to reach the station and the time it takes for the P-waves to do so is 60 seconds.
 

Related to Wavelength - how far away did earthquake occur

1. What is a wavelength?

A wavelength is a measure of the distance between two consecutive peaks or troughs in a wave. It is typically represented by the Greek letter lambda (λ).

2. How is wavelength related to earthquakes?

In the context of earthquakes, wavelength refers to the distance between the earthquake's epicenter (the point on the Earth's surface directly above the earthquake's focus) and a specific location where the earthquake's waves are being measured.

3. How is wavelength measured in relation to an earthquake?

Wavelength can be measured using a seismometer, which detects and records the ground motion caused by an earthquake. By comparing the arrival times and amplitudes of different types of seismic waves (such as P-waves and S-waves), scientists can calculate the wavelength and determine the distance to the earthquake's epicenter.

4. Why is it important to know the wavelength of an earthquake?

Knowing the wavelength of an earthquake is important for determining the earthquake's location and magnitude, as well as the potential impact on nearby areas. It can also help scientists better understand the characteristics of the Earth's interior and how seismic waves travel through it.

5. Can the wavelength of an earthquake change?

Yes, the wavelength of an earthquake can vary depending on the location and magnitude of the earthquake, as well as the type of seismic waves being measured. It can also be affected by the composition and structure of the Earth's crust and mantle in the surrounding area.

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