Colombia occupies a complex triple junction where the oceanic Nazca Plate and the Caribbean Plate subduct beneath the South American continental plate. The Bucaramanga Seismic Nest in Santander is the world’s second most active intermediate-depth earthquake source, alongside shallow strike-slip faulting along the Romeral and Boconó systems.
Real-time USGS seismic table displaying the 10 most recent earthquakes and latest earthquakes recorded today with verified moment magnitude (Mw), epicenter location, and focal depth.
| Time (UTC) | Magnitude | Location & Epicenter | Depth (km) |
|---|---|---|---|
| M 4.4 | M4.4 Earthquake — 10 km SW of El Cerrito, Colombia | 154.4 km | |
| M 5.3 | M5.3 Earthquake — 174 km NW of Port-Olry, Vanuatu | 10.0 km | |
| M 5.8 | M5.8 Earthquake — 182 km NW of Port-Olry, Vanuatu | 10.0 km | |
| M 4.8 | M4.8 Earthquake — 219 km WNW of Port-Olry, Vanuatu | 10.0 km | |
| M 5.1 | M5.1 Earthquake — 217 km NW of Port-Olry, Vanuatu | 10.0 km | |
| M 5.0 | M5.0 Earthquake — 161 km NW of Port-Olry, Vanuatu | 10.0 km | |
| M 5.3 | M5.3 Earthquake — 216 km W of Sola, Vanuatu | 10.0 km | |
| M 5.8 | M5.8 Earthquake — 203 km NW of Port-Olry, Vanuatu | 10.0 km | |
| M 5.7 | M5.7 Earthquake — 205 km NW of Port-Olry, Vanuatu | 10.0 km | |
| M 4.9 | M4.9 Earthquake — 186 km WNW of Port-Olry, Vanuatu | 10.0 km | |
| M 5.2 | M5.2 Earthquake — 202 km NW of Port-Olry, Vanuatu | 10.0 km |
You can check real-time earthquake activity in Colombia on this page. Our system streams live USGS telemetry updated every 60 seconds showing all recent seismic events with magnitude, depth, and epicenter coordinates.
Colombia experiences varying levels of seismic activity depending on its tectonic setting. You can view the complete 1-year historical archive and 24-hour counts on this live monitoring page.
Colombia occupies a complex triple junction where the oceanic Nazca Plate and the Caribbean Plate subduct beneath the South American continental plate. The Bucaramanga Seismic Nest in Santander is the world’s second most active intermediate-depth earthquake source, alongside shallow strike-slip faulting along the Romeral and Boconó systems.