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it records the frequency of the earthquake !
Seismometers or Seismographs are instruments that measure motions of the ground, including those of seismic waves generated by earthquakes, volcanic eruptions, and other seismic sources.
Seisometers are used to measure how much the ground moves, but the only real way to detect them is to look at previous records as to how long it has been since an earthquake; if it a long time, an earthquake could happen soon.
That depends on what information you are interested in. A single seismic station station measuring the P and S-wave arrival time can make an estimate of the distance to the epicentre of the earthquake and based on this information and the amplitude of the measured waves can make an estimate of the earthquakes magnitude, whereas a minimum of three stations are needed to find the location of the epicentre. For more information on this process, please see the related question.
Seismologists measure and record earthquakes to understand their characteristics, including magnitude, depth, and location. This data helps in assessing earthquake hazards, studying the Earth's interior structure, and improving our understanding of plate tectonics and seismic activity. It also allows for the development of early warning systems to protect lives and infrastructure in earthquake-prone areas.
A seismogram is a record of an earthquake that's obtained from a seismic instrument. It's in the form of a graph.
The seismic stations record data on the other side of the planet by disturbing the timing of the electrical current. The horizontal magnetic directions are hit by a shock wave, allowing information about the area closer to the earthquake. The seismologists average their data and do final calculations. Within two weeks, they have their data.
this is where the seismic waves recorded; measures vertical earth motion
To try to predict earthquakes, and get advanced warning of them.
On the drum of a seismic recorder, the pen moves up or down according to the earthquake waves reaching it, giving a 2D record.
it records the frequency of the earthquake !
At many different earthquake centers. When an earthquake happens the tree nearest earthquake centers record the magnitude and intensity of the seismic waves produced by the earthquake in order to find the origin or epicenter
"Shake, Rattle, and Roll". But seriously folks, it's called a "seismogram".
Seismometers or Seismographs are instruments that measure motions of the ground, including those of seismic waves generated by earthquakes, volcanic eruptions, and other seismic sources.
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Seismographs record the arrival time and amplitude of seismic waves. They can be used to locate the earthquakes epicentre and estimate the earthquake's magnitude. Please see the related question.