Modified Mercalli Intensity (MMI) Scale
An effects-based measure of shaking at a specific location — what people feel, hear, and see.
The Modified Mercalli Intensity scale measures the effects of shaking at a specific location: what people feel and hear, what they observe moving or breaking, and what structural damage occurs. Unlike magnitude — a single number describing energy released at the source — MMI varies from place to place depending on distance from the epicenter, local geology, and building construction.
Instrumental Intensity is the term used by USGS ShakeMap for MMI values derived from recorded ground motion rather than direct human reports. ShakeMap translates peak ground acceleration (PGA) and peak ground velocity (PGV) into the MMI scale using Ground-Motion–to–Intensity Conversion Equations (GMICEs). Intensity Lab uses the Worden et al. (2012) GMICE. These are instrument-derived estimates that draw on the same observational tradition as the original scale, extended to locations where seismographs are present but human observers may not be.
ShakeMap also integrates Did You Feel It? (DYFI) macroseismic data — crowdsourced shaking reports from people who experienced the earthquake — as additional constraints on the intensity map. ShakeMap values are approximate and typically improve over the hours and days following an event as more seismic station data and DYFI reports become available.
You are the sensor
The MMI scale is unique because it is based on human observation. You don't need a multi-million dollar seismometer to estimate the intensity at your location — your own experience is the measurement. Like the Beaufort Scale for wind — which grades conditions from "calm" to "hurricane" based on observable effects such as smoke drift, tree movement, and wave height — or the Douglas Sea Scale for ocean waves — which describes sea state from "glassy" to "phenomenal" using observations like whitecaps visible, spray, and foam streaks — MMI relies on what you see, hear, and feel.
If you felt an earthquake, select the level below that best matches your experience. Then report it to USGS Did You Feel It? to contribute to the scientific record.
Select a Level
How the scale works at different levels
At lower levels (I–IV), MMI is based almost entirely on human perception: whether people feel shaking at all, and how strongly. The descriptions center on sensory experience — whether someone asleep is awakened, whether dishes rattle, whether the shaking feels like a passing truck.
At higher levels (VII–X), human perception saturates — everyone is aware of severe shaking — and the descriptions shift to structural damage as the distinguishing criterion: the difference between cracked plaster and toppled chimneys, or between partial collapse and complete destruction. This dual nature reflects the original intent of the scale.
Quick Reference
| Intensity | Shaking | |
|---|---|---|
| I | Not felt | Details → |
| II | Weak | Details → |
| III | Weak | Details → |
| IV | Light | Details → |
| V | Moderate | Details → |
| VI | Strong | Details → |
| VII | Very strong | Details → |
| VIII | Severe | Details → |
| IX | Violent | Details → |
| X | Extreme | Details → |
Descriptions are verbatim from the USGS MMI Scale, based on Wood & Neumann (1931) and Richter (1958). Source: USGS Modified Mercalli Intensity Scale .
Instrumental intensity values and PGA/PGV ranges from USGS ShakeMap V4 Technical Documentation (Worden et al.). Intensity Lab reports MMI derived via the Worden et al. (2012) GMICE, interpolated from USGS ShakeMap. PGA/PGV ranges are approximate; actual values overlap between adjacent levels.