One station is not enough; this task requires at least three seismic stations. If you solely have statistics from two recording stations, you will now not be capable to decide the actual epicenter, and you will no longer be in a position to triangulate the epicenter. Finding the precise role of the epicenter will be a venture as solely three recording stations are wished for the triangulation procedure. You can have two epicentres if you have two recording stations.
The specific area of the epicenter is decided the use of records from at least three stations the usage of the triangulation method. On the circle drawn round the recording station, the genuine epicenter of the earthquake will be located. The radius of this circle is the epicentral distance. A measuring station will produce an epicentral distance however the path of the incident waves is unknown. By evaluating the depth and segment of the waves, the epicenter can be found. The epicenter can solely be recognized with two stations as factors on a line. To “triangulate” the location, three stations are needed.
- Scientists want seismograms from at least three seismic stations to decide the epicenter.
- Scientists locate the distinction between the arrival instances of the main and secondary waves at every of the three stations.
- The time distinction is used to decide the distance from the epicenter of every station. The larger the time difference, the similarly away the epicenter.
- A circle is drawn round every station, with a radius corresponding to the distance from the epicenter to that station. The factor the place the three circles meet is the epicenter.
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