SeismoTotalOpen observatory
Worldwide data · automatic updates

The planet moves.
See it happen.

Recent earthquakes on a world map, verifiable seismic history and a transparent estimate of observed frequency around any coordinates.

visual signal · recent activity
USGS global catalogue
Syncing…
PAN · ZOOM · SELECT AN EVENT
Strongest—No data
Source USGS Earthquake HazardsPublic data · no API key

03 · Historical catalogue

Travel back
in time.

Choose a date range and minimum magnitude. See the global count, monthly trend and strongest events in the sample.

The chart displays at most 2,000 events; the untruncated total is queried separately.

The historical explorer is ready.

Choose a period and query the catalogue. Years of data are not loaded until you ask for them.

04 · Local statistics

Place a point.
Read its history.

Calculate the frequency of recorded earthquakes within a radius and the mathematical probability of at least one event in a future horizon, assuming the historical rate remains stable.

Coordinates

One-time search with OpenStreetMap/Nominatim. It does not run while you type.

Examples:
This is not an earthquake prediction. It is a descriptive statistical extrapolation. It does not replace official hazard maps, fault studies, geotechnics or building codes.

Your point is still empty.

Enter coordinates or try an example. The calculation only runs when you press the button.

05 · How to read SeismoTotal

Real data.
Visible limits.

Live map

Your browser loads USGS GeoJSON feeds and refreshes the map every five minutes. Open an event to check its time, depth and magnitude in the original record: the catalogue can be revised later.

Historical catalogue

The interval includes both complete UTC dates. The total is queried separately; the chart and highlighted events use at most the 2,000 most recent events. A capped chart does not describe the entire period's monthly trend.

Statistical model

The observed rate is λ=N/H: recorded events divided by observation years. P(≥1)=1−exp(−λT) assumes a constant rate and independent events. Historical blocks do not share boundary instants.

Interpretation limits

Aftershocks and detection changes can violate these assumptions. Radius measures distance to the epicentre, not shaking intensity at your location. Sample size does not measure accuracy or validate the model. Use official sources for hazard, construction and emergencies.