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The difference in arrival times of P and S waves.
s waves
s waves
No.
the energy of an earthquake, called seismic waves,originates from a point called the ? epicenter
P-waves (Primary) and S-waves (Secondary). Using the difference in time between the arrival of P- and S-waves, you can then determine the distance from the epicenter. Once you've determined the distance from the epicenter of three different stations, you'll be able to triangulate the epicenter (the point where all three circles cross).
epicenter and seiesmic waves, find the distance and seismograph stations
Given the difference in arrival times, you can determine the distance from the epicenter.
distance to the epicenter of an earthquake. [:
The difference in arrival times of P and S waves.
The distance to the epicenter
4,000 kilometers
P waves, also called primary waves, are the first waves to be registered on a seismograph. The S waves, or secondary waves, are the second and slower wave to register on the seismograph. When locating an earthquakes epicenter seismologists take the first reading of the P wave, and then take the reading from the S wave. At the station of where the earthquake was recorded, seismologists draw a large circle from where the earthquakes epicenter could be. TO exactly located the earthquakes epicenter there needs to be at least 3 dfferent staions where the earthquake hit to determine its epicenter using the S and P time interval.
The distance of an epicenter from a seismograph station can determined by the time it takes for the seismic waves to reach each station. You need at least 3 seismic stations to record the event to determine this. The time taken for each seismic station to resisted the event will be different as they are different distances from the epicenter. The distance to the epicenter can then be calculated for each station and a epicenter can be determined by a triangulation from all stations that have registered the event.
The epicenter can be determined by measuring the time difference between the arrival of P and S waves, and then calculating the distance of the epicenter from each of the 3 stations. Once you have estimated the distance for each station you then draw a circle around each one. The place where the circles meet or intersect, is the epicenter.
The difference in arrival time is used to find the distance to an Earthquake's epicentre.
4. shear waves and compression waves travel at different speeds, therefore the difference in arrival time can be used to fix the distance.