theres two kinds of waves that are produced...P-waves and S-waves. its kinda hard to explain the difference between them, but if you Google them you can find out more.
They radiate out in concentric circles - expanding laterally as they go.
the spread by gaining strenght
The source of earthquake waves is the epicenter of the earthquake.
The epicenter is directly above the point where an earthquake originated. Shock waves are produced and propagate spherically along the epicenter.
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 farther you go from the epicenter, the seismic waves become weaker.
No. S waves and P waves are energy waves sent from the epicenter of the earthquake. But they are the part of an earthquake that causes damage.
distance to the epicenter of an earthquake. [:
The source of earthquake waves is the epicenter of the earthquake.
s waves
seismic waves
the energy of an earthquake, called seismic waves,originates from a point called the ? epicenter
The epicenter is directly above the point where an earthquake originated. Shock waves are produced and propagate spherically along the epicenter.
It depends where the epicenter is.
It depends where does the epicenter is.
epicenter and seiesmic waves, find the distance and seismograph stations
Primary (P) and Secondary (S) waves
By finding the arrival time of the P waves and S 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.