Georgia occupies the compressed corridor between the Greater and Lesser Caucasus mountains, accommodating the continental collision of the Arabian and Eurasian plates. Active deformation is dominated by fold-and-thrust belts along the Greater Caucasus frontal thrust and Trialeti system, generating powerful shallow thrust events such as the 1991 Mw 7.0 Racha earthquake—the strongest recorded in the country—as well as shallow intraplate events beneath vulnerable urban centers like the 2002 Tbilisi earthquake.
72-hour composite hazard forecast
Recorded in the last 30 days
Largest earthquake in the last 30 days
Counts cover the seismic belts this platform monitors in Georgia, not its administrative borders. A monitored belt can reach across a border, and events there are listed with the country of their epicentre.
2 Holocene volcanoes under seismic monitoring
Georgia occupies the compressed corridor between the Greater and Lesser Caucasus mountains, accommodating the continental collision of the Arabian and Eurasian plates. Active deformation is dominated by fold-and-thrust belts along the Greater Caucasus frontal thrust and Trialeti system, generating powerful shallow thrust events such as the 1991 Mw 7.0 Racha earthquake—the strongest recorded in the country—as well as shallow intraplate events beneath vulnerable urban centers like the 2002 Tbilisi earthquake.
The emergency number in Georgia is 112, answered by Emergency Management Service, Ministry of Internal Affairs. After strong shaking, keep the line free for those trapped or injured and check official channels for aftershock and tsunami advisories.
The national seismic authority is Institute of Earth Sciences and National Seismic Monitoring Centre, Ilia State University (IES / NSMC). EarthquakeLive cross-checks its bulletins against 18 international networks, so an event may appear here with a slightly different magnitude until the agencies converge on a final solution.