Earth Science
The Richter Scale is a logarithmic scale used to measure the magnitude of earthquakes, quantifying the amount of energy released during an earthquake. Developed in 1935 by Charles F. Richter, this scale provides a way to compare the sizes of different earthquakes, with each whole number increase on the scale representing a tenfold increase in measured amplitude and approximately 31.6 times more energy release. This scale is essential for understanding seismic activity and its potential impact.
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