Scientists use an insrument with the name of a seismograph
A seismologist. Names, I'm not so good at.
Semogram
well it's a scientist. it first came from the word seismic. there was no wave added until an earthquake happened to cross the scientist who made the word seismic.
A seismograph is an instrument that produces a record of seismic waves by detecting and measuring the vibrations caused by earthquakes or other seismic events. It consists of a seismometer to detect ground motion and a recording device to produce a trace of the detected seismic waves.
To try to predict earthquakes, and get advanced warning of them.
Seismographs do not record air movements caused by seismic waves. Seismographs specifically detect and record ground movements, such as vibrations or oscillations in the Earth's crust, produced by seismic waves generated by earthquakes or other sources. The air movements caused by seismic waves do not directly influence the seismograph readings.
A seismometer or seismograph is a device used to record seismic waves generated by earthquakes or other sources. It detects and measures the vibrations caused by these waves, providing valuable data for studying the Earth's interior and understanding seismic activity.
scientist use a specail tool called a seismograph wich drows the strength of a seismic wave
this is where the seismic waves recorded; measures vertical earth motion
seismologists
Scientists measure seismic waves using seismometers, which are instruments that detect and record the vibrations of the Earth caused by seismic activity. Seismometers generate data that can be used to determine the magnitude, location, and depth of earthquakes, as well as study the structure of the Earth's interior. The data collected by seismometers help scientists better understand the behavior of seismic waves and improve earthquake prediction and hazard assessment.
Seismic waves are measured using seismometers, which detect the ground vibrations created by seismic events like earthquakes. Seismometers record the data in the form of seismograms, which show the amplitude and arrival times of different types of seismic waves such as P-waves and S-waves. By analyzing these seismograms, scientists can determine the characteristics of the seismic event and its location.