They need three stations to accurately tell where the location of something is. By measuring the time where it hit one station to the next, they can determine its location through a process called triangulation.
Typically, at least three seismic stations are needed to accurately locate an earthquake by using triangulation. The more stations that record the earthquake, the more accurate the determination of its location can be.
At least three stations are needed to locate the epicenter of an earthquake using triangulation. By comparing the arrival times of seismic waves at these stations, seismologists can pinpoint the epicenter. Additional stations can improve the accuracy of the location.
Typically, at least three seismometer measurements are needed to determine an earthquake's epicenter. By analyzing the time difference of arrival of seismic waves at each monitoring station, scientists can triangulate the epicenter of the earthquake.
At least three seismic stations are needed to compare results and determine the epicenter of an earthquake using the method of triangulation. By measuring the arrival times of seismic waves at different stations, scientists can pinpoint the epicenter where the waves intersect.
Triangulation.
They need three stations to accurately tell where the location of something is. By measuring the time where it hit one station to the next, they can determine its location through a process called triangulation.
Three stations would best pinpoint the epicentre by triangulation.
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. 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.
Seismometer was created in 1880.
No. A minimum of three seismometer stations are required to locate an earthquakes epicentre. Please see the related question for more information.
Walter F. Reynolds has written: 'Triangulation in Maine' -- subject(s): Triangulation, Geodesy 'First-order triangulation in southeast Alaska' -- subject(s): Triangulation, Geodesy
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.
Scientists use seismographs to monitor earthquakes. Though, a seismograph merely registers an earthquake. By using at least three seismograph stations, and using triangulation, the epicentre of the earthquake is able to be plotted.
They are given this name in seismology because they are the fastest travelling of the seismic body waves released by an earthquake. Because they are the fastest, they are detected by seismometer stations first. Hence P for primary wave.
seismometer
the recording produced by a seismometer