Earthquakesnearme:findseismicactivityinyourarea

This page combines global seismic data with your browser's geolocation to answer a simple question: are there any earthquakes near me right now? When you grant location access, the system calculates the Haversine great-circle distance between your coordinates and every earthquake in the live feed, then sorts them by proximity. The result is a personalized view of seismic activity ranked by how close each event is to your current position.

Earthquake data is sourced from global monitoring networks including the USGS (United States Geological Survey), the EMSC (European-Mediterranean Seismological Centre), and JMA (Japan Meteorological Agency). These networks operate thousands of seismometers worldwide that detect ground motion and transmit readings to data centers within seconds of an event. Our pipeline ingests and normalizes this data so that earthquakes from any region appear in a consistent format with magnitude, depth, location, and timestamp.

All processing happens client-side — your location coordinates never leave your browser and are not stored or transmitted to our servers. If you decline location access, the page still functions as a comprehensive global earthquake tracker; it simply cannot personalize the distance rankings. You can revisit the page and grant location access at any time through your browser settings.

Magnitude measures the energy released at an earthquake's source, but what you feel depends heavily on your distance from the epicenter. The Modified Mercalli Intensity (MMI) scale describes the effects of an earthquake at a specific location, and intensity decreases with distance as seismic waves spread and lose energy. A magnitude 6.0 earthquake directly beneath a city can cause severe damage, while the same event 300 km away might only produce gentle swaying noticed on upper floors of tall buildings.

Depth matters as much as horizontal distance. Shallow earthquakes (less than 20 km deep) concentrate energy near the surface and produce more intense shaking over smaller areas. Deep earthquakes (100-700 km) distribute energy across wider regions but with lower peak intensity. This is why two earthquakes of identical magnitude can have vastly different effects depending on their depth and your distance from the rupture zone.

Soil conditions at your location also affect felt intensity. Soft sediments (clay, fill, reclaimed land) amplify seismic waves, a phenomenon called site amplification. Areas built on bedrock experience less amplification. This means two people equidistant from an earthquake can experience very different shaking depending on the ground beneath them — a factor that explains why some neighborhoods sustain heavy damage while nearby areas on different geology are largely unaffected.

If you see an earthquake listed within 200 km of your location, the most important action depends on whether the event is current or already concluded. For an active earthquake (shaking in progress), follow the universally recommended Drop, Cover, and Hold On protocol: drop to your hands and knees, take cover under a sturdy piece of furniture, and hold on until the shaking stops. Do not run outside during shaking — most injuries occur from falling debris near building exteriors.

After the shaking stops, be prepared for aftershocks. Aftershocks can occur minutes, hours, or even weeks after the mainshock and can be strong enough to cause additional damage, especially to structures weakened by the initial event. Move to an open area away from damaged buildings if you can do so safely. Check for gas leaks, water line breaks, and structural damage before re-entering buildings.

If you are in a coastal area and feel strong shaking lasting more than 20 seconds, move to higher ground immediately — this is a natural tsunami warning. Do not wait for an official alert. Check our tsunami warnings page for current alerts. For ongoing situational awareness, the earthquakes today tracker provides a broader view of global seismic activity beyond your immediate vicinity.

The earthquake data on this page comes from a global network of seismometers — instruments that detect and record ground motion. The USGS Global Seismographic Network operates over 150 stations in more than 80 countries, providing near-real-time detection of earthquakes worldwide. The EMSC coordinates data from national seismological agencies across Europe and the Mediterranean. Japan's JMA operates one of the densest seismic monitoring networks on Earth, with over 4,000 observation points across the Japanese archipelago.

Modern seismometers are extraordinarily sensitive — they can detect ground displacements smaller than the width of an atom. When an earthquake occurs, the nearest stations detect P-waves (compression waves) first, followed by S-waves (shear waves). By measuring the time difference between P and S wave arrivals at multiple stations, seismologists can triangulate the earthquake's location, depth, and magnitude within minutes. For larger events, automated systems issue preliminary alerts within seconds.

These monitoring networks feed data to global aggregation systems that publish earthquake information through APIs and public feeds. Our platform subscribes to multiple feeds and cross-references them, ensuring that even if one network is slow to report an event, it appears promptly from another source. This redundancy is critical for timely earthquake notification, especially for events in regions where monitoring infrastructure is sparse. The global disaster tracker puts seismic data alongside floods, wildfires, and severe weather for a comprehensive view of natural hazard activity.