Live seismic activity in Kyrgyzstan — updated every 60 seconds from USGS data. Kyrgyzstan is highly seismic due to the India‑Eurasia collision, with frequent M5+ events.
Kyrgyzstan is highly seismic due to the India‑Eurasia collision, with frequent M5+ events. The 1911 Kebin earthquake (M8.0) also severely affected Kyrgyzstan. Major faults include Tien Shan fault system, Issyk-Kul Fault. Notable quakes include 1911 Kebin (M8.0), 2008 Nura (M6.6). The seismic risk is high. Tectonically, Kyrgyzstan lies on intraplate – collision zone. This page provides real‑time USGS data and historical context for Kyrgyzstan.
The region is defined by Tien Shan fault system, Issyk-Kul Fault, and the risk level is classified as High. With a population of 6.5 million, understanding local seismic hazards is crucial.
Kyrgyzstan lies on Intraplate – collision zone. 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 Kyrgyzstan was the 1911 Kebin earthquake (M8.0). 1911 Kebin (M8.0)
Kyrgyzstan experiences approximately 200-500 earthquakes per year, with 20-50 felt (M3.0+) and 2-5 potentially damaging events (M5.0+) annually, according to USGS historical data.
The most recent major earthquake in Kyrgyzstan was the 1911 Kebin earthquake (M8.0). 1911 Kebin (M8.0)
Yes. Kyrgyzstan is crossed by Tien Shan fault system, Issyk-Kul Fault, making it prone to seismic activity. The seismic risk level is classified as High.
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.