Live seismic activity in Ethiopia — updated every 60 seconds from USGS data. Ethiopia has significant seismicity due to the East African Rift system.
Ethiopia has significant seismicity due to the East African Rift system. The 2005 Afar earthquake swarm included over 100 events, some M5+. Major faults include East African Rift, Ethiopian Rift. Notable quakes include 1961 Karakore (M6.7), 2005 Afar swarm (M5.5+). The seismic risk is moderate. Tectonically, Ethiopia lies on nubian and somalian plates diverging (rift). This page provides real‑time USGS data and historical context for Ethiopia.
The region is defined by East African Rift, Ethiopian Rift, and the risk level is classified as Moderate. With a population of 120 million, understanding local seismic hazards is crucial.
Ethiopia lies on Nubian and Somalian plates diverging (rift). 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 Ethiopia was the 1961 Karakore earthquake (M6.7). 1961 Karakore (M6.7)
Ethiopia 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 Ethiopia was the 1961 Karakore earthquake (M6.7). 1961 Karakore (M6.7)
Yes. Ethiopia is crossed by East African Rift, Ethiopian Rift, 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.