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Earthquake Risk Explorer

Runs in your browserLive data from earthquake.usgs.gov, nominatim.openstreetmap.org, tile.openstreetmap.org

Choose any place on Earth, pull the live USGS catalogue into your browser, and see long-term statistical recurrence probabilities — not predictions — with plate and fault overlays.

Important: No one can predict the exact time, place and size of an earthquake. The numbers here are long-term statistical probabilities from past earthquake rates (a time-independent Poisson model). Real hazard also depends on local faults, soil and buildings. For safety guidance follow your national authority (for example PMD / NDMA in Pakistan). These are not predictions.
Click anywhere on the map to choose a location.

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How to use this tool

  1. Open the Earthquake Risk Explorer — no account needed.
  2. Click the map, search a place, use Use my location or a city preset, then set radius and minimum magnitude.
  3. Press Analyse this area. Your browser fetches matching USGS events and computes recurrence statistics locally.
  4. Use filters, charts, heatmap, share link or CSV/GeoJSON export. Optional in-tab alerts need your permission and only run while the tab is open.

What this explorer shows

The Earthquake Risk Explorer is an interactive map that pulls the public USGS earthquake catalogue into your browser and turns the past record into simple long-term statistics for any circle you choose on Earth. Pick a place by clicking the map, searching a city name, using your device location, a preset, or typing latitude and longitude, then set a radius in kilometres and a minimum magnitude. The page queries the USGS FDSN event API live (CORS is allowed), counts every earthquake of that size inside the circle since 1900, and summarises how often such events have occurred. It also overlays plate boundaries from the PB2002 model and, if you switch them on, a simplified copy of the GEM Global Active Faults database.

Statistical probabilities, not predictions

No model on this page — or anywhere else — can say that a quake of a certain size will strike a certain town on a certain day. What you see are long-term statistical probabilities from a time-independent Poisson model: if events of magnitude M or larger happened at an average rate of r per year in that circle, the chance of at least one in the next t years is 1 − e^(−r·t). That is a statement about average behaviour over decades, not a forecast of the next rupture. Real hazard also depends on which fault is loaded, how soft the soil is, and how buildings are built. Use the numbers for study and education; for safety follow your national seismic authority.

How the rate is estimated

Older catalogues miss smaller shocks, so the tool only starts the rate clock when the chosen magnitude is reasonably complete worldwide: from 1900 for M≥7, from 1964 for M≥6, and from 1973 for smaller thresholds. By default it then removes aftershocks with Gardner–Knopoff (1974) space–time windows so the remaining events are closer to independent mainshocks; you can turn that off with the checkbox. The annual rate is N divided by the years in that completeness window. If N is zero, the page refuses to print a false 0% and instead shows a 95% upper bound using the rule of three. The Gutenberg–Richter b-value is estimated with the Aki–Utsu maximum-likelihood formula (Mc = your minimum magnitude, ΔM = 0.1) when at least ten events are available. Only events with eventtype=earthquake are counted.

Live feeds, alerts, charts and sharing

Beside the analysis panel you will find a nearby list sorted by distance, optional in-tab browser notifications when a new quake above your chosen magnitude appears inside the radius while the tab stays open, canvas charts of events per year and a magnitude histogram, a heatmap-style density toggle, a dark map basemap, filters by magnitude, depth and year, an estimate of distance to the nearest plate boundary or loaded fault, and CSV or GeoJSON export. Shareable addresses use the form #lat,lon,radius,minmag. Map tiles come from OpenStreetMap; place search uses Nominatim and runs only when you press Search. Attribution for USGS ComCat, PB2002, GEM (CC BY-SA 4.0), OpenStreetMap and Nominatim is listed on the tool itself.

Frequently asked questions

Can this tool predict the next earthquake?

No. It estimates long-term statistical probabilities from past rates using a Poisson model. It cannot predict the exact time, place or size of a future quake.

Where does the earthquake data come from?

From the public USGS ComCat FDSN event service and USGS real-time GeoJSON feeds, requested live by your browser. Plate boundaries are PB2002 (Bird 2003); active faults are a simplified GEM Global Active Faults layer (CC BY-SA 4.0).

Why do smaller magnitudes start later than 1900?

Global catalogues are incomplete for moderate quakes in the early twentieth century. The tool uses completeness windows of 1900 for M≥7, 1964 for M≥6 and 1973 otherwise, matching common practice.

What does “remove aftershocks” do?

It applies Gardner–Knopoff (1974) declustering so aftershocks inside a mainshock’s space–time window are dropped before the rate is calculated. You can turn it off to use the raw catalogue.

Do location or alerts leave my device?

Geolocation and Notification prompts stay in your browser. Coordinates and alert settings are not uploaded to Toolzy. The browser talks directly to USGS, Nominatim and OpenStreetMap tile servers.

Who should I trust for safety advice?

Your national seismic or disaster authority (for example PMD and NDMA in Pakistan). This page is for study and education, not an official warning service.

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