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s waves are about 60% slower than p waves, so basicaly p waves are about twice as fast. The actual time in like minutes or hours depends on where the epicenter is, and where you are recording from

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15y ago
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12y ago

the p wave is more stronger than the s wave one breaks it up and the other one shakes it rapidly.

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Q: What is the difference between arrival times of a p-wave and a s-wave?
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How do you do you locate earthquake epicenter?

You need to find the difference between the arrival times of P and S waves. From there three or more stations put their results and data together and make circles of distance with a chart. When all three of them cross at a point, that is roughly where the epicenter is.A more detailed explanation is included below:To locate an earthquake, you need the data from at least three seismometer stations.The process is known as triangulation and is described in more detail below.The seismometer records the P and S-wave arrival times. P-waves travel faster through the earth than S-waves and so they arrive at the seismometer station before the S-waves and are recorded by the seismometer first.The difference in arrival time between the two types of seismic wave can be used to calculate the distance of the earthquake's epicentre from the seismometer.DE = DeltaT x (VP - VS) / (VS x VP)Where:DE = Distance to epicentre (km)DeltaT = Difference between P and S-wave arrival time (s)VP = P-wave velocity (km/s)VS = S-wave velocity (km/s)This can then be plotted on a map, by drawing a circle with a radius equal to the distance to the epicenter around the seismometer station. This is then repeated for the other two seismometer stations and the point where the three circles intersect is the location of the earthquake's epicenter.The above procedure is commonly automated using computers and numerical techniques so that a large number of differing seismic episodes can be processed efficiently.It should be noted that this is an imperfect process as a number of assumptions must be made about the material through which the seismic waves travel in order to estimate their speed.


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An S-wave is a secondary wave that comes after P-waves, and can travel only through solids.


How do you do you locate earthquake epicenter?

You need to find the difference between the arrival times of P and S waves. From there three or more stations put their results and data together and make circles of distance with a chart. When all three of them cross at a point, that is roughly where the epicenter is.A more detailed explanation is included below:To locate an earthquake, you need the data from at least three seismometer stations.The process is known as triangulation and is described in more detail below.The seismometer records the P and S-wave arrival times. P-waves travel faster through the earth than S-waves and so they arrive at the seismometer station before the S-waves and are recorded by the seismometer first.The difference in arrival time between the two types of seismic wave can be used to calculate the distance of the earthquake's epicentre from the seismometer.DE = DeltaT x (VP - VS) / (VS x VP)Where:DE = Distance to epicentre (km)DeltaT = Difference between P and S-wave arrival time (s)VP = P-wave velocity (km/s)VS = S-wave velocity (km/s)This can then be plotted on a map, by drawing a circle with a radius equal to the distance to the epicenter around the seismometer station. This is then repeated for the other two seismometer stations and the point where the three circles intersect is the location of the earthquake's epicenter.The above procedure is commonly automated using computers and numerical techniques so that a large number of differing seismic episodes can be processed efficiently.It should be noted that this is an imperfect process as a number of assumptions must be made about the material through which the seismic waves travel in order to estimate their speed.


Whats the name of the animated band or artist with music videos in it a blue short haired men that's pointy big blue eyesshortskinnypop technoits not gorillaz?

Swave maybe? Though I hate that group, they copied Gorillaz >:-(


A string of linear density 1.5 gm is under a tension of 20 N. What should its length be if its fundamental resonance frequency is 220 Hz?

Linear density for stringμ=1.5 g/m=1.5*10-3 kg/mTension on stringT=20 NWave speed on stringv=√(T/μ)=√(20/1.5*10-3)=115 m/sWave lengthf=v/λλ=v/f=115/220=0.52 mFundamental resonance frequencyL=λ/2=0.26 mLength of string is 0.26 m


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