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 (the equation to do this can be seen at the bottom of this answer).
This can then be plotted on a map, by drawing a circle with a radius equal to the distance to the epicentre 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 earthquakes epicentre.
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.
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)
A seismograph is an instrument used to measure the vibrations produced by the movement of waves through the Earth. These waves are produced by the release of energy during an earthquake. Since different directions of motions are produced by earthquakes, there are different types of seismographs. Some of the seismographs record horizontal motions while others record vertical motions.
A seismograph is an instrument used to measure the vibrations produced by the movement of waves through the Earth. These waves are produced by the release of energy during an earthquake. Since different directions of motions are produced by earthquakes, there are different types of seismographs. Some of the seismographs record horizontal motions while others record vertical motions.
Based on the difference in arrival times of P and S waves as recorded on a seismometer you can estimate the distance of the seismometer from the earthquake epicentre, however you will have no idea of the direction.
Seismologists (or more correctly automated computer programs written by seismologists) plot the distance to the earthquakes epicentre by drawing a circle round the seismometer loaction on a map with a radius equal to the epicentral distance.
If this is done for two stations located in differing places the circles will intersect in two places. This narrows down the location of the epicentre to either of those two points. If you add in the data from a third station, all three of the circles should intersect at a single common point marking the epicentre of the earthquake. As such the minimum number of seismometer stations required to locate the epicentre of an aerthquake is 3.
because each seismograph measures a particular type of wave and also because one seismograph can only determine how far away the epicenter is, not in which direction
Wroug
Three
Triangulation for accuracy. The method is called "triangulation" ... same method used by GPS units to coordinate the exact locations. Please see the related question for more information.
co-ordinates or position
I'm pretty sure what you're asking is which particle can you not pinpoint exactly, and the answer to that is the electron
Wroug
Three
Three seismographs stations are needed to pinpoint the location of the epicentre of an earthquake.
Triangulation for accuracy. The method is called "triangulation" ... same method used by GPS units to coordinate the exact locations. Please see the related question for more information.
At least three.Please see the related question for an explanation as to why.A minimum of three seismograph or seismometer stations are required to locate the epicentre of an earthquake.
I would imagine you would need a minimum of three surrounding the epicenter in order to triangulate it.
They determine the centre of an earthquake by using varies of facility, such as sioesomagraph which is a tiny pencdil that measures every milly scond of the tectonic ploate,or a monographs that are signals that detect an earthyquake
Three stations would best pinpoint the epicentre by triangulation.
Latitude and longitude are able to pinpoint a certain location on Earth accurately on a map.
my name is Edwerd choi! sorry I don't know to
"Epicenter" usually refers to a point on the Earth's surface directly above the "focus" of an earthquake. When a quake occurs, a seismic monitoring station can determine how far away it was from the shock wave pattern -- that is called the "epicentral distance" -- but not the exact direction. But with three or more monitoring stations' epicentral distances, one can draw intersecting circles to pinpoint the exact location.
"Epicenter" usually refers to a point on the Earth's surface directly above the "focus" of an earthquake. When a quake occurs, a seismic monitoring station can determine how far away it was from the shock wave pattern -- that is called the "epicentral distance" -- but not the exact direction. But with three or more monitoring stations' epicentral distances, one can draw intersecting circles to pinpoint the exact location.