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they are primary, secondary, and surface waves
3 main, not sure if there's other devices. (seismoscope, seismometer, ???)
I think they are P or C Waves no..... S waves, Surface waves, or Shear waves cause the MOST damage (and i don't think 'C' waves are real), as they shake things sideways and/or up and down.
Scientists use devices called Seismographs to determine the epicenter of an earthquake. If 3 or more seismographs detect an earthquake, seismic wave activity can be measured and quantified and then cross-referenced with other data (the primary and secondary seismic waves) to determine the earthquake's location.
You can think of this in the same way that satellites work to find your location for the GPS in your car. An earthquake happens and it is picked up on 3+ seismometers. These seismometers measure the waves that the earthquake produced and the velocity at which they are traveling and you look at where all the seismometer calculations run together. You have the epicenter of your earthquake.
they are primary, secondary, and surface waves
The three types of earthquake waves are primary waves, surface waves, and secondary waves.
The simplified answer is that it works much in the same way you would determine the source of a sound (which is also in waves). Multiple measurements of the intensity are taken from different locations are used to triangulate an earthquake.
3 main, not sure if there's other devices. (seismoscope, seismometer, ???)
Seismic waves are the waves of force that travel through earth or other elastic bodies. eg: Result of an earthquake ,explosion or some other processes that imparts forces
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I think they are P or C Waves no..... S waves, Surface waves, or Shear waves cause the MOST damage (and i don't think 'C' waves are real), as they shake things sideways and/or up and down.
S-waves and P-waves emit from the focus (epicenter) at the same time, yet one of them is faster than the other. therefore the S waves and P waves are directly proportional to each other. So all one needs is to do the math and trace the distance between the waves and there, you have found the Focus (epicenter) of the earthquake.
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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.
1 The moon's gravitational pull on the water 2 The wind hitting the water 3 An underwater earthquake (Tsunami)