The Richter Scale is a numerical scale used to measure the magnitude of earthquakes, quantifying the amount of energy released during seismic events. Developed in 1935 by Charles F. Richter, this scale ranges from 0 to 10, with each whole number increase representing a tenfold increase in measured amplitude and roughly 31.6 times more energy release. The scale provides a simple way to communicate the severity of earthquakes, making it easier to understand their potential impact on communities and environments.
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