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seismographs

A seismograph is an instrument that detects and records seismic waves produced by earthquakes. It consists of a mass suspended on a spring; when the ground shakes during an earthquake, the mass remains still while the base moves, creating a trace on a recording medium. This trace, called a seismogram, shows the intensity and duration of the quake. By analyzing these recordings, scientists can determine the earthquake's location, depth, and magnitude, helping to understand geological activity and improve safety measures for communities at risk.

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    Seismographs are instruments that detect and record the vibrations caused by earthquakes or other seismic events. They consist of a mass suspended on a spring, which remains still while the ground shakes. As the ground moves, the mass sways, and this movement is converted into electrical signals, creating a visual record called a seismogram. Seismographs help scientists analyze the strength, duration, and location of seismic waves, providing crucial information for understanding earthquakes, assessing risks, and improving building safety. Their data is vital for monitoring seismic activity worldwide.