Burundi
Embed This Widget
Add the script tag and a data attribute to embed this widget.
Embed via iframe for maximum compatibility.
<iframe src="https://quakefyi.com/iframe/entity//" width="420" height="400" frameborder="0" style="border:0;border-radius:10px;max-width:100%" loading="lazy"></iframe>Paste this URL in WordPress, Medium, or any oEmbed-compatible platform.
https://quakefyi.com/entity//Add a dynamic SVG badge to your README or docs.
[](https://quakefyi.com/entity//)Use the native HTML custom element.
Burundi is located in Africa and has a Moderate seismic risk classification. A total of 2 earthquakes have been recorded in the country's seismic history. The largest earthquake recorded in the country reached a magnitude of 4.4. With a population of 12,332,788 and a land area of 27,834 km², seismic events can have significant implications for infrastructure and public safety.
Seismic Overview
Burundi is one of the smaller countries in central Africa, but its seismic exposure is significant because it straddles the western branch of the East African Rift System. Lake Tanganyika, which forms Burundi's western border with the Democratic Republic of Congo, occupies one of the deepest rift-valley lakes on Earth, sitting in a graben bounded by active normal [[fault]]s that have been extending the crust for roughly 12 million years. These faults generate moderate-to-large earthquakes capable of causing damage in the country's densely populated lakeside areas.
The [[epicenter]]s of most Burundian earthquakes cluster along the margins of Lake Tanganyika and in the hills immediately east of the lake. The Tanganyika Rift basin has produced several magnitude 5.5 to 6.5 events in the 20th and 21st centuries. On 30 August 2024, a magnitude 5.8 earthquake struck near the northern end of Lake Tanganyika close to Bujumbura, damaging buildings in the capital and killing several people. Earthquakes in this zone can also trigger underwater landslides on the steep lacustrine slopes, which in turn can generate localised [[tsunami]]-like waves within the lake — a hazard known as a seiche or impulse wave.
Historically, Burundi's seismic record is intertwined with that of the wider Lake Tanganyika region. A magnitude 6.2 earthquake in 1903 caused damage around the northern lake shore. A sequence of events in 1919 and 1920 also produced moderate shaking across the region. Because Burundi is one of the most densely populated countries in Africa with widespread informal construction, the exposure of the population to seismic hazard is high relative to the moderate level of ground shaking expected.
The tectonic framework of Burundi involves the slow separation of the Nubian plate to the west from the Somalian plate to the east along the western rift branch. Extension rates in the Tanganyika Rift are estimated at two to four millimetres per year. The rift valley is characterised by half-graben basins bounded by major border faults on alternating sides of the valley. [[seismic-wave]] studies of local events show predominantly normal-faulting mechanisms consistent with this extensional setting. The thick sedimentary fill within Lake Tanganyika provides a long archive of past earthquake activity detectable through sub-bottom seismic profiling.
Recent Earthquakes
| Mag | Location | Time | |
|---|---|---|---|
| No recent earthquakes. | |||
Notable Historical Events
Earthquakes Near Major Cities in Burundi
Frequently Asked Questions
Burundi has a moderate level of seismic activity. Significant earthquakes occur periodically. A total of 2 earthquakes have been recorded in Burundi's seismic history.
The largest recorded earthquake in Burundi had a magnitude of 4.4. Earthquakes of this size can cause significant damage depending on depth, location, and local building standards.
Burundi has had 2 recorded earthquakes. This count includes events of all magnitudes detected by seismic monitoring networks. The actual number of earthquakes may be higher, as smaller events can go undetected.
Burundi is classified in the "Moderate" seismic zone, located in Africa. Seismic zones indicate the relative level of earthquake hazard based on historical activity, geological conditions, and proximity to tectonic plate boundaries.
During an earthquake, Drop, Cover, and Hold On. Get under a sturdy desk or table, protect your head and neck, and hold on until shaking stops. Move away from windows and heavy objects. After the earthquake, check for injuries and be prepared for aftershocks.
Country earthquake risk is assessed using several factors: proximity to tectonic plate boundaries, historical seismicity (frequency and magnitude of past events), geological conditions, population density in seismic zones, and building code enforcement. QuakeFYI assigns seismic zones from 0 (no risk) to 4 (very high) based on these factors.
A seismic zone is a geographic area classified by the level of earthquake hazard. Zone 0 has negligible risk, Zone 1 has low risk, Zone 2 has moderate risk, Zone 3 has high risk, and Zone 4 has very high risk. These zones are determined by historical earthquake data, tectonic setting, and geological conditions.
Countries along the Pacific Ring of Fire experience the most earthquakes. Japan, Indonesia, Chile, the Philippines, and Iran consistently record the highest seismic activity. The United States (especially Alaska and California), Turkey, and Mexico are also among the most seismically active nations.
Population density amplifies earthquake risk because more people and infrastructure are exposed to potential damage. A magnitude 7.0 earthquake in a densely populated city can cause thousands of casualties, while the same event in an uninhabited area may cause none. Building codes and emergency preparedness greatly reduce risk in populated areas.
Seismic density measures the concentration of earthquake activity relative to a country's land area, expressed as earthquakes per 1,000 square kilometers. A high seismic density indicates frequent earthquake activity per unit area, helping compare seismic risk between countries of different sizes.
Seismic Metrics
Nearby Seismic Activity
Yearly Summary
Earthquake Safety
Burundi is in a moderate seismic risk zone. Basic earthquake preparedness is advisable.
- Drop, Cover, and Hold On during shaking
- Keep an emergency supply kit with water, food, and first aid
- Identify safe spots in each room away from windows and heavy objects
- Know tsunami evacuation routes if in a coastal area