Earthquake Magnitude Calculator
Four modes covering magnitude scales, seismic energy comparisons, Modified Mercalli Intensity (I-XII), and Richter magnitude from seismograph amplitude. Presets include historic earthquakes.
Seismograph Waveform
Waveform amplitude is proportional to magnitude. Higher M = larger displacement.
Controls
Results
Energy Comparison (Log Scale)
Each magnitude step = 31.6× more energy. Two steps = 1,000×.
Modified Mercalli Intensity Scale (I-XII)
Not felt except by a very few under especially favorable conditions.
Felt only by a few persons at rest, especially on upper floors. Delicately suspended objects may swing.
Felt quite noticeably by persons indoors. Many do not recognize it as an earthquake. Vibration like a passing truck.
Felt indoors by many. Dishes, windows, and doors disturbed. Walls make cracking sound.
Felt by nearly everyone. Some dishes and windows broken. Unstable objects overturned.
Felt by all. Some heavy furniture moved. A few instances of fallen plaster. Damage slight.
Damage negligible in well-built structures. Considerable damage in poor structures. Some chimneys broken.
Damage slight in specially designed structures. Considerable damage in ordinary buildings with partial collapse. Panel walls thrown out of frame structures.
Damage considerable in specially designed structures. Well-designed frame structures thrown out of plumb. Ground cracked conspicuously.
Some well-built wooden structures destroyed. Most masonry and frame structures destroyed. Rails bent. Landslides considerable.
Few if any masonry structures remain standing. Bridges destroyed. Broad fissures in ground.
Damage total. Lines of sight and level are distorted. Objects thrown into the air.
Reference Guide
Richter Scale (Mₗ)
The Richter scale (local magnitude Mₗ) was developed by Charles Richter in 1935. It measures the maximum amplitude recorded by a Wood-Anderson seismometer at 100 km from the epicenter.
where A is the measured amplitude and A₀ is a reference amplitude at the same distance. Each whole number increase represents a tenfold increase in amplitude, but 31.6× more seismic energy.
Moment Magnitude (M𝑤)
Moment magnitude is the modern standard for measuring large earthquakes. It is derived from the seismic moment M₀ (in N·m), which captures the fault area, slip distance, and rock rigidity.
The 2011 Tohoku earthquake had a seismic moment of about 3.9 × 10^22 N·m giving M𝑤 = 9.1. Unlike the Richter scale, M𝑤 does not saturate for very large events and remains accurate above M7.
μ = shear modulus (~3×10^10 Pa), A = fault area, D = average slip
Seismic Energy
The Gutenberg-Richter energy-magnitude relation converts magnitude to radiated seismic energy in joules:
Each 1.0 magnitude increase = 10^1.5 ≈ 31.6× more energy. Two steps = 1,000×. A M9 earthquake releases about 31.6^4 ≈ one million times more energy than M5.
Modified Mercalli Intensity
The Modified Mercalli Intensity (MMI) scale describes earthquake effects on people, structures, and the environment using Roman numerals I (not felt) through XII (total destruction). Unlike magnitude, MMI varies with distance from the epicenter.
Empirical correlation: MMI ≈ 1.5M - 1.4. A M6.5 earthquake typically produces MMI VIII at the epicenter and MMI V-VI at 50 km distance.