Earthquakes are measured using a device called a seismometer, which records the vibrations caused by seismic waves that travel through the Earth's crust. The magnitude of an earthquake is determined by measuring the amplitude of the seismic waves recorded by the seismometer. The most commonly used scale for measuring earthquake magnitude is the Richter scale, which was developed by Charles Richter in 1935. The Richter scale is a logarithmic scale, which means that each increase in magnitude represents a tenfold increase in the amplitude of the seismic waves.
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Earthquakes are measured using a device called a seismometer, which records the vibrations caused by seismic waves that travel through the Earth's crust. The magnitude of an earthquake is determined by measuring the amplitude of the seismic waves recorded by the seismometer. The most commonly used scale for measuring earthquake magnitude is the Richter scale, which was developed by Charles Richter in 1935. The Richter scale is a logarithmic scale, which means that each increase in magnitude represents a tenfold increase in the amplitude of the seismic waves.
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Earthquakes are measured using seismographs, which monitor the seismic waves that travel through the Earth after an earthquake strikes.
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