Earthquakes are measured using two primary frameworks: Magnitude (the total energy released) and Intensity (the shaking experienced at a specific location). The fundamental unit used to express this energy mathematically is the Moment Magnitude \(M_{w}\), which has largely replaced the older Richter scale. [1, 2]
Here are the specific scales and units used to measure earthquakes:
1. Earthquake Magnitude (Energy)
- Moment Magnitude Scale (Mw): The modern standard used by seismologists worldwide. It measures the physical area of the fault rupture and the total energy (M₀ representing seismic moment) released during the quake. [, 2]
- Richter Scale: Developed in 1935, this scale measures the maximum amplitude of seismic waves. It is generally used for smaller, local earthquakes. [1, 2]
2. Earthquake Intensity (Shaking & Damage)
3. Physical Ground Motion (Engineering)
For structural engineering and hazard assessment, seismologists measure the physical ground waves directly using an instrument called an accelerograph. [1]
- Peak Ground Acceleration (PGA): Measures the maximum acceleration of the ground during shaking, often expressed as a percentage of standard gravity (g).
- Peak Ground Velocity (PGV) & Displacement (PGD): Measures how fast and how far the ground moves during the seismic event. [1]
Further Exploration
- Understand the physics of fault lines via USGS Earthquake Glossary.
- View the exact Roman numeral definitions on the Michigan Tech Modified Mercalli Scale.
- Learn how the Richter scale operates mathematically through the Britannica Richter Scale Guide.
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