Seismograms are graphical representations of seismic waves produced by earthquakes or other ground vibrations. To interpret them, we analyze the amplitude, frequency, and arrival times of different wave types: P-waves (primary waves) arrive first, followed by S-waves (secondary waves), and surface waves. By measuring the time difference between these arrivals, we can determine the distance to the earthquake's epicenter. Additionally, the amplitude of the waves helps assess the earthquake's magnitude and intensity.
Seismograms are also known as seismographs or ground motion records.
I think this would be Seismograms.
seismograms measure any motion so, they show exactly when and how the motion comes.by Brianna m. Chappelle
Seismograms record a strong earthquake. They also record and calculate the location and magnitude of an EQ. They show how the ground moves with the passage of time.
Seismograms record a strong earthquake. They also record and calculate the location and magnitude of an EQ. They show how the ground moves with the passage of time.
You compare them both
the location and strength of the earthquake
Seismograms are called so because they are graphical representations of seismic waves generated by earthquakes or other ground motions. The term "seismo" comes from the Greek word "seismos," meaning earthquake, while "gram" refers to a written record. Thus, a seismogram essentially records the intensity and duration of seismic activity, allowing scientists to analyze and understand the Earth's movements.
P. W. Basham has written: 'Canadian seismic data for Project Rulison' 'Comparison of Montreal P-wave magnitudes from short-period and intermediate-period seismograms' -- subject- s -: Observations, Seismic waves, Seismograms, Seismology
To read a seismograph and interpret seismic activity accurately, first, understand that a seismograph records ground motion caused by earthquakes. Look at the seismograph's wavy lines, called seismograms, which show the intensity and duration of seismic waves. Identify the P-waves (primary waves) and S-waves (secondary waves) to determine the earthquake's location and magnitude. Compare the seismogram with data from other seismographs to confirm the earthquake's characteristics.
seismogram are the records or paper copies that are produced by seismographs used to calculate the location and magnitude of an earthquack
Seismograms give information about the path of seismic waves and the speed of seismic waves. The speed of seismic waves depends on the density of the material the seismic wave is traveling in. We know, for example, that the core of Earth is liquid, because S waves do not travel through the center of Earth.