Live USGS
EarthquakeMap.live › Earthquakes Today › Democratic Republic of the Congo

Democratic Republic of the Congo Earthquakes Today: Live Tracker

Live seismic activity in Democratic Republic of the Congo — updated every 60 seconds from USGS data. The DRC has moderate seismicity, mainly along the East African Rift system in the east, including active volcanoes in the Virunga range.

🕐 Loading...
📊 Regional seismic profile
🌋 Risk level
Moderate
🏔️ Major faults
Albertine Rift, Tanganyika Rift, Virunga volcanic fault system
📅 Notable quakes
2005 Lake Tanganyika (M6.8), 1998 M6.3, 2002 volcanic tremors
👥 Population affected
95 million
🧩 Tectonic setting
East African Rift – divergent boundary, Western Rift branch
📌 Did you know? Mount Nyiragongo in eastern DRC is one of the world's most active volcanoes, and its 2002 eruption destroyed parts of Goma city.
📋 Local earthquakes (past 24h)
No local earthquakes in the past 24 hours.

About Earthquake Activity in Democratic Republic of the Congo

The Democratic Republic of the Congo has moderate seismicity, mainly along the East African Rift system in the east, including the active volcanoes of the Virunga range (Nyiragongo, Nyamuragira). The 2005 Lake Tanganyika earthquake (M6.8) was strongly felt in eastern DRC. Major faults include the Albertine Rift, the Tanganyika Rift, and the Virunga volcanic fault system. Notable quakes include 2005 Lake Tanganyika (M6.8), 2002 Nyiragongo eruption‑related tremors, 1998 M6.3. The seismic risk is moderate. Tectonically, the DRC lies on the Nubian Plate, with active rift faults and volcanic activity in the Virunga region. This page provides real‑time USGS data and historical context for the DRC.

The region is defined by Albertine Rift, Tanganyika Rift, Virunga volcanic fault system, and the risk level is classified as Moderate. With a population of 95 million, understanding local seismic hazards is crucial.

Why does Democratic Republic of the Congo experience earthquakes?

Democratic Republic of the Congo lies on East African Rift – divergent boundary, Western Rift branch. 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.

Key facts about Democratic Republic of the Congo seismicity

Frequently Asked Questions about Democratic Republic of the Congo Earthquakes

❓ What was the strongest earthquake in Democratic Republic of the Congo?

The strongest recorded earthquake in Democratic Republic of the Congo was the 2005 Lake Tanganyika earthquake (M6.8). 2005 Lake Tanganyika (M6.8)

❓ How often do earthquakes occur in Democratic Republic of the Congo?

Democratic Republic of the Congo 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.

❓ When was the last major earthquake in Democratic Republic of the Congo?

The most recent major earthquake in Democratic Republic of the Congo was the 2005 Lake Tanganyika earthquake (M6.8). 2005 Lake Tanganyika (M6.8)

❓ Is Democratic Republic of the Congo on a fault line?

Yes. Democratic Republic of the Congo is crossed by Albertine Rift, Tanganyika Rift, Virunga volcanic fault system, making it prone to seismic activity. The seismic risk level is classified as Moderate.

❓ What should I do during an earthquake in Democratic Republic of the Congo?

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.

Other seismically active regions

Data sources: USGS real‑time feed, USGS historical archive, and Wikipedia. Page refreshes live earthquake data every 60 seconds.

← Back to global earthquake map