They measure the difference in arrival times of P and S seismic waves as measured on a seismograph. From this (based on an estimate of their relative velocities) they can calculate the distance of the seismometer from the earthquakes epicentre using the following equation:
Distance to epicentre (km) = Time Difference (s) x (VP - VS) / (VS x VP)
Where:
VP = P-wave velocity (km/s)
VS = S-wave velocity (km/s)
Seismographs measure the arrival time of the various types of seismic waves along with their frequency and amplitude.
Using the difference between the arrival time of the P and S Waves, seismologists can then calculate the distance to the earthquake epicentre.
Please see the related question for more information.
Scientists can calculate the depth to the earthquake's Focus (NOT epicentre) by measuring the time difference between arrival times of the two or more sets of waves, and using the distance on a travel time graph at which the P-wave and S-wave have the same separation.
s-p time method
how do seismologist know how to find the location of a epicenter
a seismograph can find the severity of an earthquake by graphing the measures of distances and strength of an earthquake.
Ground motion, earthquakes and nuclear explosions for example.
P-waves and S-waves are released by an earthquake at the same time and travel out from the epicentre in all directions. However P-waves travel faster than S-waves so the further away from the earthquake's epicentre the greater the lead the P-waves have on the S-waves. Observation of the seismogram trace at the seismometer station will allow the scientists to find the P-wave and S-wave arrival times and measure the difference between them. As the P-waves are faster they always arrive first (hence their name - primary wave). The greater the difference between the time that the P-waves and S-waves first arrive (i.e. the greater the lead the P-waves have), the further the distance to the epicentre. They are able to use the time difference along with an estimate of the speed of the P-waves and S-waves to find the distance from the station to the earthquakes epicentre. For more information on this please see the related question.
They use the Richter scale to measure the speed of the earthquakes. Levels of earthquakes 2.0 ---> can't be felt 4.0 ---> do not cause damage 5.0---> can cause damage 6.0 ---> considered strong 7.0---> is a major earthquake +++ That is not correct. You have confused speed with intensity. The Richter scale, which is logarithmic, measures the intensity ("strength" if you like). The speed is measured in ordinary linear units like metre/second or km/hr, calculated from observing the earthquake's waves' progress past seismographs around the world.
epicenter and seiesmic waves, find the distance and seismograph stations
they used the focus
At least 3 stations are required to find the epicenter
It takes 3 stations.
No. One seismograph station will only allow you to calculate the distance to the earthquake's focus. (The epicentre is on the surface above.) To find its exact location you need the recordings from at least 3 seismograph stations.For more information on the SP time method, please see the related question.
seismic waves
the distance from a epicenter to an earthquake :)
It would depend on the size of the quake. It is certainly possible to use only one seismograph, it would just be impossible to use triangulation to find the epicenter of the tremble, as it requires at least three.
The distance of an earthquake epicenter from a seismic station. Using the Three point method, the distance from 3 seismic stations are used to locate the epicenter by triangulation.
The distance of an earthquake epicenter from a seismic station. Using the Three point method, the distance from 3 seismic stations are used to locate the epicenter by triangulation.
the find the epicenter the find the focus from the epicenter
A travel time graph can be used to find the distance from the epicenter of an earthquake.