Togo
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.
Togo is located in Africa and has a Low seismic risk classification. A total of 0 earthquakes have been recorded in the country's seismic history. With a population of 8,095,498 and a land area of 56,785 km², seismic events can have significant implications for infrastructure and public safety.
Seismic Overview
Togo is a narrow coastal nation in West Africa, situated on the West African craton and the Dahomeyide mobile belt — an ancient Pan-African orogenic structure that runs north-south through the country, marking the suture zone where the Volta Basin was accreted to the West African craton approximately 600 million years ago. While this orogenic belt preserves a record of ancient collision and deformation, it has been tectonically locked and geologically inactive for hundreds of millions of years and generates no significant contemporary seismicity.
The southern part of Togo faces the Gulf of Guinea passive margin, which formed during the Mesozoic opening of the South Atlantic. The passive margin geology is characterised by thick Cretaceous and Cenozoic sedimentary sequences deposited in the offshore Togo-Benin Basin. These sediments are not associated with active tectonic deformation or significant seismicity.
The Atakora Mountains in northwestern Togo represent a northward continuation of the Atacora fold belt that runs through Benin and Burkina Faso. These ancient structures are mechanically inert and produce no modern seismicity. The Mono River valley, which forms part of Togo's border with Benin, occupies an ancient geological depression but is not associated with active faulting.
Historical earthquake records for Togo are essentially blank. No earthquake has been documented to have caused casualties or structural damage in Togo's history. Occasional [[seismic-wave]] signals detected at regional networks near the Ghana-Togo border may be associated with Ghana's Akwapim fault zone activity, but events originating within Togo's territory are essentially unknown. [[magnitude]] events above 4.0 are not documented in the global earthquake catalogues for Togo.
Recent Earthquakes
| Mag | Location | Time | |
|---|---|---|---|
| No recent earthquakes. | |||
Notable Historical Events
Earthquakes Near Major Cities in Togo
Frequently Asked Questions
Togo has a low level of seismic activity. Large earthquakes are infrequent but not impossible. A total of 0 earthquakes have been recorded in Togo's seismic history.
Togo has had 0 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.
Togo is classified in the "Low" 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.