Live seismic activity in Uzbekistan — updated every 60 seconds from USGS data. Uzbekistan has moderate seismicity, especially in the eastern Tien Shan mountains.
Uzbekistan has moderate seismicity, especially in the eastern Tien Shan mountains. The 1966 Tashkent earthquake (M5.2) destroyed much of the city and killed up to 200 people. Major faults include Tien Shan fault system. Notable quakes include 1966 Tashkent (M5.2), 2002 Tashkent (M5.5). The seismic risk is moderate. Tectonically, Uzbekistan lies on intraplate – indian-eurasian collision influence. This page provides real‑time USGS data and historical context for Uzbekistan.
The region is defined by Tien Shan fault system, and the risk level is classified as Moderate. With a population of 35 million, understanding local seismic hazards is crucial.
Uzbekistan lies on Intraplate – Indian‑Eurasian collision influence. The movement of these plates builds up stress, which is released as earthquakes. In subduction zones, one plate dives beneath another, generating some of the largest quakes on Earth. In some regions, strike‑slip faults produce frequent moderate earthquakes.
The strongest recorded earthquake in Uzbekistan was the 1966 Tashkent earthquake (M5.2). 1966 Tashkent (M5.2)
Uzbekistan experiences approximately 50-200 earthquakes per year, with 5-20 felt (M3.0+) and 0-2 potentially damaging events (M5.0+) annually, according to USGS historical data.
The most recent major earthquake in Uzbekistan was the 1966 Tashkent earthquake (M5.2). 1966 Tashkent (M5.2)
Yes. Uzbekistan is crossed by Tien Shan fault system, making it prone to seismic activity. The seismic risk level is classified as Moderate.
Drop, cover, and hold on. Stay away from windows, and if outdoors, move to an open area. After the shaking stops, check for injuries and be ready for aftershocks. Prepare an emergency kit with water, food, first aid, and a flashlight.
Data sources: USGS real‑time feed, USGS historical archive, and Wikipedia. Page refreshes live earthquake data every 60 seconds.