Live seismic activity in Kenya — updated every 60 seconds from USGS data. Kenya experiences earthquakes mainly along the East African Rift Valley.
Kenya experiences earthquakes mainly along the East African Rift Valley. The 1928 Subukia earthquake (M6.9) caused widespread damage. Major faults include Gregory Rift faults. Notable quakes include 1928 Subukia (M6.9), 2007 Nairobi (M5.1). The seismic risk is moderate. Tectonically, Kenya lies on east african rift (divergent boundary). This page provides real‑time USGS data and historical context for Kenya.
The region is defined by Gregory Rift faults, and the risk level is classified as Moderate. With a population of 55 million, understanding local seismic hazards is crucial.
Kenya lies on East African Rift (divergent boundary). 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 Kenya was the 1928 Subukia earthquake (M6.9). 1928 Subukia (M6.9)
Kenya 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 Kenya was the 1928 Subukia earthquake (M6.9). 1928 Subukia (M6.9)
Yes. Kenya is crossed by Gregory Rift faults, 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.