The Gutenberg-Richter Law is a fundamental empirical relationship that describes the distribution of earthquake magnitudes in a given region over time. It states that the logarithm of the number of earthquakes with magnitudes greater than or equal to a certain value is linearly related to that magnitude. This law is crucial for understanding seismic source characterization as it helps estimate the frequency and size of earthquakes, which is essential for hazard assessment and risk management.
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