Interactive visualization showing relationships between different seismic magnitude scales
The original magnitude scale developed by Charles Richter in 1935. Measures the amplitude of seismic waves recorded on seismographs. Most accurate for local earthquakes (< 600 km) and magnitudes < 6.5.
The most reliable scale for large earthquakes. Based on the seismic moment, which measures the total energy released. Doesn't saturate for large earthquakes and is now the standard for reporting earthquake magnitudes.
Measures short-period P-waves (1 second). Useful for deep earthquakes and nuclear test detection. Tends to saturate around magnitude 6.5-6.8.
Based on the amplitude of Rayleigh surface waves with periods near 20 seconds. Good for shallow earthquakes at teleseismic distances. Saturates around magnitude 8.0.
Based on the total duration of seismic wave coda. Particularly useful for small to moderate earthquakes (M < 5). Easy to calculate and widely used for local earthquake monitoring. Less reliable for larger earthquakes.
Japan Meteorological Agency magnitude based on maximum amplitude. Optimized for Japanese earthquakes and seismic network. Well-calibrated for regional events but shows slight saturation for very large earthquakes.
Uses regional Lg waves (guided waves in the crust). Effective for continental earthquakes at regional distances (150-1500 km). Saturates around magnitude 6.5-7.0 due to Lg wave characteristics.